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THE
Pio Owl DINGS
or THE
LISMEAN OOGIETY
OF
New Sou WALES
FOR THE YEAR
1939
VOL. LXIV.
WITH TWELVE PLATES
3 Maps and 496 Text-figures.
SYDNEY:
PRINTED AND PUBLISHED FOR THE SOCIETY BY
AUSTRALASIAN MEDICAL PUBLISHING CO., LTD,
Seamer Street, Glebe, Sydney,
and
SOLD BY THE SOCIETY.
1939.
li
CONTENTS OF PROCEEDINGS, 1939.
PARTS I-II (Nos. 281-282).
(Issued 15th May, 1939.)
Pages.
Presidential Address, delivered at the Sixty-fourth Annual General
Meeting, 29th March, 1939, by Mr. T. C. Roughley .. i-xxvli
Elections XXVii
Balance-sheets for the year ending 28th February, 1939 Pad te oie hy, VA XXVili-xxx
Abstractzorubrocecdines’ 4.455%) 5 Ree a ee! NE ee ae XXXI-XXxX1i
The Ecology of the Upper Williams River and Barrington Tops Districts.
iii. The EHucalypt Forests, and General Discussion. By Lilian Fraser,
D.Sce., and Joyce W. Vickery, M.Sc. (Plates i-iii.) .. 1-33
Miscellaneous Notes on Australian Diptera. v. On Hye-coloration, and
other Notes. By G. H. Hardy. (One Text-figure.) .. 34-50
Description of a New Genus and Two New Species from Papua. Family
Pyrgotidae (Diptera). By J. R. Malloch. (Communicated by Frank
H. Taylor, F.R.E.S., F.Z.8S.) (Two Text-figures. ) 51-53
Revision of Australian Lepidoptera. Oecophoridae. viii. By A. Jefferis
Turner, M.D., F.R.E.S. 54-72
Trombidiid Larvae in New Guinea (Acarina: Trombidiidae). By Carl
HEH. M. Gunther, M.B., B.S., D.T.M. (Communicated by Frank H.
Taylor, F.R.E.S., F.Z.S.) (Forty Text-figures.) 73-96
The Diptera of the Territory of New Guinea. vii. Family Otitidae
(Ortalidae). By John R. Malloch. (Communicated by Frank H.
Taylor, F.R.ES., F.Z.S.) (Plates iv—v.) 97-154
The Diptera of the Territory of New Guinea. viii. Dolichopodidae. By
VYabbé O. Parent. (Communicated by Frank H. Taylor, F.R.E.S.,
F.Z.8.) (Thirty-one Text-figures.) 155-168
The Diptera of the Territory of New Guinea. ix. Family Phytalmiidae.
By John R. Malloch. (Communicated by Frank H. Taylor, F.R.E.S.,
F.Z.S.) (Thirteen Text-figures.) 169-180
Taxonomic Notes on the Order Embioptera. i. The Genotype of
Oligotoma Westwood. By Consett Davis, M.Se. (Five Text-figures.) 181-190
A Key to the Marine Algae of New South Wales. Part 2. Melanophyceae
(Phaeophyceae). By Valerie May, B.Sc. ..
191-215
CONTENTS.
PARTS III-IV (Nos. 283-284).
(Issued 15th September, 1939.)
Taxonomic Notes on the Order Embioptera. ii. A New Neotropical Genus
of Embioptera. By Consett Davis, M.Sc. (Twenty-one Text-figures. )
A New Species of Chalcid (Genus Hurytoma) associated with Tepperella
trilineata Cam., a Wasp causing Galling of the Flower Buds of
Acacia decurrens. By N. S. Noble, D.Sc.Agr., M.Se., D.I.C. (Twelve
Text-figures. )
The Upper Palaeozoic meer Retna Mourit George Hand Wanenams N. S.
Wales. By A. H. Voisey, M.Sc. (One Map and three Text-figures.)
The Lorne Triassic Basin and Associated Rocks. By A. H. Voisey, M.Sc.
(One Map and two Text-figures.) .
A New Species of Megastigmus parasitic on Crenpenctla, Hilinenia Can a
Wasp causing Galling of the Flower Buds of Acacia decurrens. By
N. S. Noble, D.Sc.Agr., M.Sec., D.I.C. (Ten Text-figures.) ERNST
A Reconnaissance Survey of the Vegetation of the Myall Lakes. By Prof.
T. G. B. Osborn, D.Sc., F.L.S., and R. N. Robertson, Ph.D.,. B.Sc.
(Plates vi-vii and three Text-figures.) Arora Puen hy Geary esi
Australian Coleoptera. Notes and New Species. No. xi. (Mostly
Elateridae.). By H. J. Carter, B.A., F.R.H.S. (Plates viii-ix and
one Text-figure.)
The Genus Adrama, with eceriptions, of Three New Bpccice) (Diptera,
Trypetidae). By John R. Malloch. (Communicated by Frank H.
Taylor, F.R.E.S., F.Z.S.) (Two Text-figures.) .. 5
A New Family of Lepidoptera. By A. Jefferis Turner, M. D., F. R. H. S.
Hymenopterous Parasites of Hmbioptera. By Alan P. Dodd Bae
Miscellaneous Notes on Australian Diptera. vi. Dolichopodinae. By
G. H. Hardy ;
Observations on the Bionomies on Morpiolosy of Sénen Spevics of tite
Tribe Paropsini (Chrysomelidae). By D. Margaret Cumpston,
M.Se., Linnean Macleay Fellow of the Society in Zoology. (Plate x
and twenty-two Text-figures.) PEN Tae sack RONEN, OE REL a
The Diptera of the Territory of New Cine x. Family Ceratopogonidae.
By J. W. S. Macfie, M.A., D.Sc., F.R.E.S. (Communicated by Frank H.
Taylor, F.R.E.S., F.Z.S.) (Two Text-figures.) .. aster ee niece
Taxonomic Notes on the Order Embioptera. iii. The Genus Burmitembia
Cockerell. By Consett Davis, M.Se. (Six Text-figures.)
Taxonomic Notes on the Order Embioptera. iv. The Genus Cloiloda
Enderlein. By Consett Davis, M.Sc. (Twenty-five Text-figures.) .
Taxonomic Notes on the Order Embioptera. v. The Genus Donaconethis
Enderlein. By Consett Davis, M.Se. (Five Text-figures.) :
The Geology of the County of Buller, N.'S.W. By A. H. Norsey, M.Se.
(One Map and two Text-figures.) Sieh
The Geology of the Lower Manning District of New Soni ‘juales, By
A. H. Voisey, M.Se. (One Map and one Text-figure.) PE Tor I
A Note on the Synonymy of Leptops (Coleoptera: Curculionidae). By
K. C. McKeown .. : Sickie ag EStck a MnO PS A
The Diptera of the mMonritory. of Mew feuinied! xi. Family Trypetidae.
By John R. Malloch. (Communicated by Frank H. Taylor, F.R.E.S.,
F.Z.S.) (Plate xi and fifteen Text-figures. )
iii
Pages.
217-222
223-241
242-254
"955-265
266-278
279-296
297-330
331-334
335-337
338-344
345-352
353-366
367-368
369-372
373-380
381-384
385-393
394-407
408
409-465
iv CONTENTS.
PARTS V-VI (Nos. 285-286).
(Issued 15th December, 1939.)
Pages.
The Association between the Larva described as Vrombicula hirsti var.
buloloensis Gunther 1939, and Trombicula minor Berlese 1904.
(Acarina: Trombidiidae.) By C. E. M. Gunther, M.B., B.S., D.T.M.
(Three Text-figures. ) We) | Rep eee deb al rc lel (ca RU Aeon ee bo a O40)
Observations on the Life-history of Neoschéngastia kallipygos Gunther
1939. (Acarina: Trombidiidae.) By C. E. M. Gunther, M.B., B.S.,
DUVME Sa WO Mhext-neures.)) ii tkm meee cle a Ban. Se ae, ESE oe NEAT ATS
Taxonomic Notes on the Order Embioptera. vi-x. By Consett Davis,
IMISO5 (Caiksaiaycdapeerey UNepqeaitbhResh)) do ell aohu tek col toe ce odo tee es
Elementary Hydrography of South-eastern Australia. By Frank A. Craft,
B.Se. (Ten Text-figures.) Dis ean Meat cgosh cai/itp atest Laitircr hs gies aay RAEY aU EO Ge by ey
Strongylate Nematodes from Marsupials in New South Wales. By
Professor T. Harvey Johnston and Patricia M. Mawson. (Sixty-six
Text-figures. ) Ties a PREC Urol) is ce aa Onee role heb cs | Tes Ste FL Brak
Ectocarpus confervoides (Roth) Le Jol. By Valerie May, B.Se., Linnean
Macleay Fellow of the Society in Botany. (Forty-six Text-figures.) 537-554
A Note on the Re-examination of Australian Species of Ceratopogonidae
(Diptera). By J. W. S. Macfie. (Communicated by Frank H. Taylor,
PURI SL LGoSo)) | (CAM ORES) AMES UTNE) 50 oo oe too oo co co Oo
Taxonomic Notes on the Order Embioptera. xi-xiv. By Consett Davis,
MeESC= a Chibty-onelRext-211neSs) snl ween non nae Hah TA tao eos Hoos
The General Geology of the District east of Yass, N.S.W. By Kathleen
Sherrard, M.Se. (Plate xii and three Text-figures. ) So eee Wyle wD n= 000
Contributions to the Microbiology of Australian Soils. v. Abundance of
Microorganisms and Production of Mineral Nitrogen in relation to
Temperature. By H. L. Jensen, Macleay Bacteriologist ‘2 the Society.
GHIVEECRENEUTES i. ca. cic. eSic ll cir ok bata ACR OLS ewe eer HOOT 60S
IADSLLact Ofeenroceedingsie 2S) ot ds RR a Pn ae XXXi1i-xXxxvili
Donations and Exchanges PDN NN v in, SUN eh ane iam <2 Mee mle SA a eh aU XXXix—xlix
TLE: Ope IN ACS oo XS ES) ee scenery ME BPE Fa Vern Genco cad sre gin eRON ncke lary eiere L-liv
Index EAE Pragifatea Gus. 2 © Grctast yrattety Phathay oy ee og cee I eae re he eee a a a lv—lxvi
SI SHORE IATCS INAS Veith we! wh! dt TTD SR Te eT ae ea * 1xvii
isSuroOresNewiHaniyrand (Genera os) ts + eee 8 Fan et ee ces Ixvii
CORRIGENDUM.
Paracardiophorus assimilis n. sp., was unfortunately omitted from the table,
page 312. Its place therein would be as follows:
8. Hinder pair of maculae round, basal oblong.
(a) -BasalmaculaekwidevananODliguemersicy..8-) ete terial een niente fulvosignatus Cand.
(b) Basal maculae narrow and longitudinal (dumb-bell-like) ........ assimilis, n. sp.
ANNUAL GENERAL MEETING.
WEDNESDAY, 29th Marcu, 1939.
The Sixty-fourth Annual General Meeting was held in the Society’s Rooms,
Science House, Gloucester Street, Sydney, on Wednesday, 29th March, 1939.
Mr. T. C. Roughley, B.Sc., F.R.Z.S., President, in the Chair.
The minutes of the preceding Annual General Meeting (30th March, 1938) were
read and confirmed.
PRESIDENTIAL ADDRHESS.
The concluding part of Volume Ixiii of the Society’s ProckEDINGsS was issued
in December. The complete volume (467 plus Ixxx pages, twenty-two plates and
255 text-figures) contains thirty-three papers on a variety of subjects in Natural
History.
Exchanges from scientific societies and institutions totalled 1,860 for the
session, compared with 2,069, 1,795 and 1,865 for the three preceding years.
Since the last Annual Meeting the names of twelve members have been added
to the list, five members and one Corresponding member have been lost by death,
the names of five have been removed on account of arrears of subscription and
two have resigned.
Mary ELLEN FuLier, who died suddenly at her mother’s home in Sydney on
25th September, 1938, had been a member of the Society since 1930. She graduated
Bachelor of Science at the University of Sydney in 1929, her final subjects being
Botany and Entomology. In January, 1929, she was appointed to the staff of the
Division of Economic Entomology of the Council for Scientific and Industrial
Research to work at Canberra on the blowfly problem. She continued to work
on this problem till her death—first under the late Dr. R. J. Tillyard and later
under Dr. I. M. Mackerras. As results of her work on Diptera she published
eighteen papers (eleven of them in our PRockEEDINGS) and at the time of her
death had completed the material for three more papers.
SARAH HYNES, who died at her home in Randwick on 28th May, 1938, at the
age of seventy-eight, was the first woman member of the Society. She became an
Associate member in 1892, and in 1909, when women were first admitted to full
membership, she became an Ordinary member. Her early education was received
in London and Edinburgh, and she was one of the early women graduates at the
University of Sydney, where she obtained the degree of Bachelor of Arts in 1891.
Her chief scientific interest was botany, and she served for a time on the staff
of the Technological Museum and also at the Sydney Botanic Gardens. She was
chiefly instrumental in having the Commonwealth Government acquire the
collection of paintings of Australian flowers by the late Mrs. Ellis Rowan. She
was included in the Honours list in 1934, being made M.B.E.
Epwarp Meyrick, who died at Marlborough, England, on 31st March, 1938,
was born on 24th November, 1854. In December, 1877, he came to Sydney as
A
li PRESIDENTIAL ADDRESS.
Classics Master at Sydney Grammar School. While in Australia he had the
opportunity to collect systematically at many localities in New South Wales, and
also in Tasmania and Western Australia. He returned to England in 1887 to
become Classics Master at Marlborough College, where he remained until he
retired in 1914. He was the chief authority on the Microlepidoptera, and bequeathed
his collection of about 100,000 specimens to the British Museum of Natural
History. He was elected a Fellow of the Royal Society of London in 1904. He
had been a Corresponding member of our Society since 1902 and had contributed
thirty-two papers to the Procrrpines. Since 1912 he had published privately a
journal entitled Hxotic Microlepidoptera, containing his descriptions of many
species of this special group.
LESLIE JOHN WILLIAM NEWMAN, who died at Claremont, Western Australia,
on 8th December, 1938, was born in Melbourne in 1878. He had been a member
of this Society since 1913. He was appointed an inspector under the Plant
Diseases Act in Western Australia in 1904, Assistant Entomologist, Western
Australia, in 1908 and Entomologist in 1920, occupying the latter position until
his death. He had collected in New South Wales and Victoria as well as in
Western Australia, and had published a large number of papers and reports, chiefly
in the Journal of the Department of Agriculture of Western Australia.
Monragu AUSTIN PHILLIPS, who died in England on 11th January, 1939, at
the age of fifty-nine years, was a well-known lecturer on Natural History subjects
and had for many years been associated with the British Museum of Natural
History as a guide-lecturer. He had been a member of this Society since 1921 and
was a fellow of a number of the scientific societies in London.
JOHN JAMES WALKER, who died at his home, “Aorangi’, Lonsdale Road,
Summertown, Oxford, England, on 12th January, 1939, had been a member of
the Society since 1900. He paid two visits to Australia, in H.M.S. “Penguin”
(1890-91), and in H.M.S. “Ringarooma”’ (1900-1904). During these visits he had
many opportunities of collecting insects, and has described his experiences in
two series of papers in the Hntomologists’ Monthly Magazine (1891-92 and
1905-06).
In May, 1938, the Linnean Society of London celebrated the 150th Anniversary
of its foundation, and Professor T. G. B. Osborn represented our Society at the
celebrations.
The Australian and New Zealand Association for the Advancement of Science
held its jubilee meeting at Canberra in January last, this Society being
represented by the President and Mr. H. J. Carter.
In August last, the Australian National Research Council commenced
publication of a new journal of general science, the Australian Journal of ‘Science.
There appears to be some need for such a journal in Australia, and we may offer
our best wishes for the success of this new venture.
During the year the Council decided to include each year in its list of
nominations of members of Council, the names of two members who have not
been members of the Council for the whole of the preceding year. The two
members who have retired this year in terms of this resolve are Mr. H. J.
Carter and Mr. A. R. Woodhill, and I should like to take this opportunity of
expressing our appreciation of Mr. Carter’s services to the Society and to the
Council over a long period of years. Mr. Woodhill leaves for England shortly for
a period of a year and we wish him a pleasant and profitable trip.
The year’s work of the Society’s research staff may be summarized thus:
PRESIDENTIAL ADDRESS. lii
Mr. H. L. Jensen, Macleay Bacteriologist to the Society, concluded his work
on nitrogen fixation in the wheat soils. Additional soils were tested for content
of nitrogen-fixing bacteria, so that the survey is now based on eighty-five soils
altogether; five more strains of Azotobacter have been tested for nitrogen fixation
in pure culture and have, like those previously examined, been found to possess a
normal but not outstanding N-fixing capacity; a few other organisms have been
tested with a negative result. Further experiments on nitrogen fixation in soil
with addition of straw have been conducted over periods of one to three months
and have given results in. full agreement with those of previous experiments: no
nitrogen is fixed unless Azotobacter develops abundantly and the decomposition
of the organic matter of the straw takes place under conditions of high moisture.
It has been shown that with free access of oxygen (i.e. in soil of moderate or
low moisture content) only the water-soluble constituents of the straw can serve
as food material for Azotobacter. Only under conditions that are hardly ever
fulfilled in the wheat soils can a gain of about three parts of nitrogen per 1,000
parts of straw be expected. Qualitative tests with a large number of wheat soils
have shown that these are practically all too poor in available phosphoric acid to
allow a vigorous growth of Azotobacter. Certain blue-green algae have again been
found capable of fixing elementary nitrogen, but not in quantities that can be
considered significant under the conditions obtaining in the wheat fields. A
paper giving a full and detailed account of these and the previous experiments on
non-symbiotic nitrogen fixation, aS well as a discussion of the literature dealing
with the importance of this phenomenon under field conditions, has been prepared
and submitted to the Society. Preliminary work has been commenced on the
isolation of cellulose-decomposing microorganisms in order to test their ability
to produce food material for nitrogen-fixing bacteria when growing in association
with these.
Miss Hlizabeth Pope, Linnean Macleay Fellow of the Society in Zoology,
has continued her work on the anatomy of the Port Jackson Shark and has
completed a paper on the nervous system. The morphology of the brain and
central nervous system have been described in detail and the paths of the main
peripheral nerves traced. The organs of special sense were also described, since
differences in detail from published accounts were found. Although strictly not
part of the nervous system, the histological structure of the pituitary gland was
included. Another paper on the blood vascular system is in course of preparation.
It should supply the need for an account of this system in the Heterodonti and
thus complete the series in which the other groups, namely the Notidani, Scylioidei,
Squaliformes and Raja, have already been dealt with adequately. The surveys at
Long Reef have been continued and as far as possible a list of the larger animals
and their habitats and biotic relationships have been recorded. Certain groups
of animals will have to be omitted owing to difficulties in determining their
names. Some interesting facts have, however, emerged from this work. There
are two types of community present on the area. One type is confined to the
rocky platform and consists of animals capable of withstanding exposure to all
the elements. The other type of community inhabits an area which character-
istically consists of small rocks and boulders lying on a substratum of coarse
sand. This latter type of community is inhabited by forms which require shelter
and which live on the lower surface of the rocks or which burrow in the sand.
Mr. Consett Davis, Linnean Macleay Fellow of the Society in Zoology, has
continued work on the Order Embioptera, chiefly on the taxonomic side. Some
work has also been done on the bionomics of the Order. One paper on the
iv PRESIDENTIAL ADDRESS.
taxonomy of the genus Metoligotoma, and related problems, submitted during the
previous year, has been revised and enlarged, and published in the Procerprngs.
Further work has been carried out on the ecology of the Five Islands, and the
first paper of a series on this subject has been published, with Messrs. M. Day
and D. Waterhouse as co-authors. Subsequently, further data have been collected
for later papers in this series. By permission of the Council, six weeks were
devoted to work on the plant ecology of the Bulli District, the first paper of this
series having been published in the Procrrpines in 1936. As a result of this
work, concerned mainly with the collection and analysis of soil samples, the
data necessary for the compilation of the remaining papers of this series were
completed. Mr. Davis was able, by the Council’s grant of three months’ special
leave without pay, to spend some time abroad carrying out research. He worked
for some time in the United States and also in England, France and other
countries. Research carried out oyerseas was concerned with a study of the
physiology of respiration in aquatic beetles at the University of California, and
with the taxonomy of the Order Embioptera from a world standpoint. This latter
work consisted chiefly of an examination of the types of inadequately described
species, and was carried out chiefly at the Museum of Comparative Zoology,
Harvard University; the British Museum of Natural History, London; and the
Museum d’Histoire Naturelle, Paris. Type specimens were also obtained from
other Huropean museums, and examined at the British Museum, and several
collections of unidentified Embioptera were borrowed for further study. In all,
some eighty species of exotic HEmbioptera were examined, mostly from the types.
Mr. A. H. Voisey, Linnean Macleay Fellow of the Society in Geology,
continued his geological field work on the Upper Palaeozoic rocks of the North
Coast region, particularly in the Upper Clarence and Manning River Districts.
A number of reconnaissance trips were carried out. The aim of the work was
to describe rocks ranging from Devonian to Tertiary in age and to attempt a
correlation between them and other beds in New South Wales and Queensland.
Two reports were published which referred to work done in 1937. A third small
paper related to rocks in the neighbourhood of Armidale. Four more reports
were prepared and are awaiting publication.
Miss Ilma M. Pidgeon, Linnean Macleay Fellow of the Society in Botany,
attempted to summarize in one scheme the mosaic of vegetation of the Central
Coast of New South Wales, with special reference to the succession of plant
communities under various climatic and soil conditions. The succession on sand-
dunes has been investigated. One outstanding fact, which has not previously
been recorded in the literature, is that the chloride content of dune-soils increases
with distance from the sea. This is explained by the fact that the leaching of
chlorine ions is minimized by the presence of humus in the soil, and the humus
content increases with distance from the sea. Work has been continued on the
effects of variation in climate on the structure of forests on sandstone and shale;
data for this work are now almost complete. In addition to the ecological work, an
investigation was begun on the comparative anatomy and physiology of mature
and juvenile leaf-forms of Hucalyptus globulus. This problem has proved to be
very interesting. The results are briefly summarized: Preliminary anatomical
investigations indicate that (i) the two leaf-types differ in internal structure and
arrangement of palisade and mesophyll cells; (ii) stomatal index (which is
usually constant for a species) is twice as high in the juvenile as in the mature
leaves; (ili) stomatal frequency is approximately three times higher in the
juvenile leaves. It has been established also that the transpiration rate of mature
PRESIDENTIAL ADDRESS. Vv
leaves is greater than that of juvenile leaves. Thus transpiration is not pro-
portional to stomatal frequency. In addition, the ratio of the transpiration rates
of the two leaf-types, as measured by potometers, is reversed on the second and
third days of the experiment. This indicates that stomatal behaviour is different
in the two forms, and this matter is now being investigated. Another interesting
fact which has been established, and which hitherto has not been recorded from
any leaves, is that there are curious irregularities in the transpiration rate at
different places over the surface of individual leaves. Observations of the osmotic
pressure of the cell sap, by Barger’s method, reveal the fact that the osmotic
pressure of the mature leaves is higher than that of the juvenile leaves.
Six applications for Linnean Macleay Fellowships were received in response
to the Council’s invitation of 28th September, 1938. I have pleasure in reminding
you that the Council reappointed Miss BHlizabeth C. Pope, Mr. Consett Davis,
Mr. A. H. Voisey and Miss Ilma M. Pidgeon to Fellowships in Zoology, Zoology,
Geology and Botany respectively for one year from 1st March, 1939. Subsequently
Mr. Consett Davis and Mr. A. H. Voisey were appointed to Lectureships in Biology,
and Geology and Geography respectively in the New England University College
at Armidale, and resigned their Fellowships as from 28th February, 1939. The
Council then decided to invite applications for the two vacant Fellowships and
three applications were received. I have pleasure in announcing that the Council
has appointed Miss D. M. Cumpston, B.Se., and Miss Valerie May, B.Sc., to Linnean
Macleay Fellowships in Entomology and Botany respectively for the period
ist April, 1939, to 29th February, 1940.
Miss Margaret Cumpston graduated in Science in 1938 with First Class
Honours in Entomology, and was awarded a Science Research Scholarship in the
University of Sydney. For her honours degree she presented a thesis on the
biology and larval morphology of the genus Paropsis, which added very con-
siderably to our knowledge of the genus, and whilst holding the Research
Scholarship she has done similar work on the family Scarabaeidae, her results
now having been submitted for the M.Sc. degree.
Miss Valerie May graduated in Science in 1937 with First Class Honours in
Botany, having been placed first in Botany in all four years during her University
course. She then, for 1937-38, was awarded a Science Research Scholarship, and
for 1988-39 a Commonwealth Research Scholarship. She has worked on the
Marine Algae of New South Wales, having prepared for publication keys to the
Chlorophyceae and Melanophyceae. She has also described an albino form of
Macrozamia spiralis, and has in preparation papers on the distribution of Mistletoe
in New South Wales, and the life-history of Hctocarpus confervoides.
During the coming year Miss Pope and Miss Pidgeon will continue the
researches already commenced, Miss Cumpston will conduct investigations on
species of larval Scarabaeidae, and Miss May will study drought-resistance of
plants in New South Wales. We wish all four a very successful tenure of their
Fellowships. We also offer our congratulations to Messrs. Consett Davis and
Voisey on their appointments to the New England University College, and wish
them every success in their new sphere.
vi PRESIDENTIAL ADDRESS.
A REVIEW OF THE SCIENTIFIC INVESTIGATION OF THE FISHERIES OF
New SoutH WALES.
In choosing this subject for my Presidential Address I was guided by the fact
that Australia is now embarking on a new era of scientific investigation of the
fisheries. At Fisheries Conferences held in Melbourne in 1927 and in Sydney in
1929, at which all States of the Commonwealth were represented, a strong recom-
mendation was made that the Commonwealth Government establish a Department
of Fisheries for the purpose of investigating the potentialities of the Australian
coast for fisheries development. In 1937 the Commonwealth Government announced
that a sum of £80,000 was being set aside for investigation work of this character,
and the control of the investigation was placed in the hands of the Council for
Scientific and Industrial Research. A boat, the “Warreen’’, suitable for various
types of fishing, but more especially for the capture of pelagic fish, was constructed,
and Dr. Harold Thompson was brought from Newfoundland to take charge of
the investigations.
With a suitable boat, and a staff capable of handling the large-scale
investigations which confront our fisheries, we are at the beginning of a period
of activity the like of which has never before been known in our history. The
time appeared opportune, then, to take stock of the scientific work that has already
been accomplished, and I have therefore endeavoured to present in this address
a brief outline of the essential features of these investigations.
The volume of this scientific research is singularly small. Much work of a
general nature, based on observations that all too frequently cannot be regarded
as critical, has been published, but, lacking a strictly scientific foundation, it can
scarcely be considered as coming within the range of this discussion. In sorting
over the great amount of literature that has appeared on our fisheries, I have been
guided in my choice largely, but not solely, by the consideration of whether
it has been published in scientific journals. Of course, taxonomic investigation,
in which field great activity has been displayed over a long period of years by
a number of capable workers, does not fall within the scope of the subject of my
address.
Small as is the scientific work on the fisheries of New South Wales, it is far
smaller in the other States, and little of importance has been accomplished there.
This will be remedied to some extent by the Commonwealth investigations recently
inaugurated, for, although the base of operations has been established at Port
Hacking, near Sydney, the field will embrace all States. It is probable that the
most intensive work will be directed to the waters adjacent to the areas of densest
population, for the problem of marketing fish over long distances in a warm climate
is one that must be weighed in any plan of economic exploitation. ‘
Trawling Investigations.
Until 1915 the only methods used for the capture of bottom-dwelling fishes
offshore, not only in New South Wales, but in all the other States, consisted of
hand-lines and long-lines. Now, in the principal fisheries of the northern
hemisphere these methods of fishing had been largely replaced by trawlers, which,
dragging a large net over the bottom, caught fish in much greater quantities and
far more economically. Concerning the economic possibilities of trawlers operating
on the Australian coast there had long been a division of opinion, and although
several attempts, dating back as far as 1857, had been made to test the offshore
waters in various localities, the results obtained were so conflicting, owing to the
unsuitability of both vessels and gear, that little information of value was
PRESIDENTIAL ADDRESS. vii
obtained. In 1907, however, the Commonwealth Government decided to make a
thorough survey of the possibilities of trawling on the Australian coast by means
of an investigation trawler. This trawler, the “Hndeavour’’, was constructed at
the New South Wales Government dockyards at Newcastle and was placed in
commission on the 9th March, 1909, with H. C. Dannevig in charge of the
investigations.
The principal objects of the investigation were: (1) by various means of
capture to ascertain what marketable food-fishes may be obtained in the ocean
waters adjacent to Australia; (2) in what quantity they may be taken; (3) to
what extent they migrate, and where; (4) how they may conveniently and
economically be captured; and (5) by systematic survey to discover and chart
suitable fishing grounds.
The Commonwealth Investigation Trawler carried out this survey from
9th March, 1909, to December, 1914, when she was lost with all hands while
returning from a cruise to Macquarie Island. It was discovered that two extensive
areas carried fish in payable quantities, one on the south-east coast, the other in
the Great Australian Bight. The former was found to extend from near Port
Stephens in New South Wales southwards to Gabo Island, and to continue
across the eastern slope of Bass Strait, past Flinders Island to Tasmania. It
covered approximately 6,000 square miles within easy access to Sydney and
Melbourne. The other ground was found to lie along the edge of the continental
shelf in the Great Australian Bight and to cover an area of 4,000 square miles,
the depth varying from 80 to 300 fathoms, although the greater portion is situated
between 100 and 200 fathoms. This ground is about two days’ steaming from
Adelaide and Albany. Although great hopes had been entertained that the
extensive area of bottom in Bass Strait would prove to be a rich trawling ground,
the “Hndeavour’ found that only limited portions carried fish in payable quantities.
It was seen that the “Hndeavour’s’ catches compared favourably with the
average catches obtained in the North Sea by commercial vessels of modern type
and working in accordance with long-established experience of the movements of
the fish.
The Sydney—Gabo Island section was examined during whole or part of
sixteen different cruises at intervals between April, 1909, and August, 1913. During
this period the trawl was on the bottom for 2284 hours, and produced a total of
84,721 lb. of marketable fish, or at the rate of 371 lb. per hour of fishing.
The area south of Gabo Island, including the eastern. slope and Flinders
Island, was visited during twenty-three cruises over the same period, the actual
trawling time occupying 4324 hours, and the total catch of marketable fish
amounted to 81,715 lb., or an average of 189 lb. per hour of fishing.
In the Great Australian Bight, five cruises were devoted to an examination of
the edge of the continental shelf, two during February and March, 1912, and the
other three between February and April, 1913. The net was fishing for 144 hours,
and landed 29,232 lb. of marketable fish, the average being 203 lb. per hour of
fishing. The deeper section of the Bight was examined during three cruises
in May and June, 1913, when the actual fishing time occupied 122 hours, and the
catch of marketable fish amounted to 13,939 lb., at an average rate of 118 lb. per
hour.
As Dannevig (1913) pointed out, it was to be reasonably expected that a
commercial trawler would obtain results which would considerably exceed the
catches of the “Hndeavour’, for this vessel had to cover as much ground as possible
consistent with systematic work; and frequently she had to leave rich grounds
and proceed to others which were either quite unexplored or which previous
Vili PRESIDENTIAL ADDRESS.
experience indicated were likely to be inferior. A commercial trawler would,
however, remain on a rich ground and revisit it as long as the catches proved to
be good.
Thus the “Hndeavour’, under the capable direction of Dannevig, was able to
establish beyond doubt that rich trawling grounds existed on at least two areas
of the Australian coast, and the New South Wales Government decided to exploit
them commercially. Now, the commercial development of trawling scarcely comes
within the scope of this address, but in view of the unexpected decline in
productiveness of the trawling grounds on the south-eastern Australian coast
during recent years, a brief review of the trawling industry seems fairly warranted.
In May, 1915, the New South Wales Government initiated commercial trawling
with three modern steam trawlers, and began at once to reap a rich harvest. In
1919 a larger trawler was launched from the Government dockyards at Newcastle;
this was intended both for trawling and investigational work, and was shortly
afterwards sold to the Queensland Government; but in these northern waters she
worked with so little success that in 1922 she was sold and returned to New South
Wales. In 1920 four more steel trawlers and a fish-carrier were commissioned
from Newcastle. But in spite of the fact that consistently good hauls were
obtained and there was a satisfactory demand for the fish, the State Government,
facing a loss of £330,000 since the beginning of the industry, decided in 1923 to
cease commercial trawling.
The vessels were purchased by private firms and individuals, and under their
new management returned a considerable profit to their owners. In 1928 the fleet
had increased to nineteen, but, beginning in 1926, the productiveness of those
grounds nearest to Sydney fell away alarmingly, forcing the trawlers further
afield and increasing their operating costs considerably. It was at first thought
that this decline might be only temporary, perhaps a seasonal fluctuation, but
unfortunately it has been maintained to the present day, and the number of
trawlers operating has been reduced to fifteen. Here we shall leave them for a
moment, but we shall have occasion to discuss in greater detail certain features
of this decline when reviewing an investigation of the most important fish yielded
by them.
The Productivity of the Sea.
In 1929 Professor W. J. Dakin was appointed to the chair of zoology in
the University of Sydney, and he at once planned to conduct research into marine
biological problems, with special reference to the fisheries.
Up to this time research into the fisheries of New South Wales had, as we
have seen, consisted for the most part of observations on the adult fishes, their
seasonal migrations, spawning habits, their food as indicated by the contents of
their stomachs, and the best methods of catching them. But practically no work
had been done on the more fundamental problems, such as why they migrated
seasonally, the reason for their fluctuating numbers, their young stages from the
egg to the post-larva, their age at various sizes and their rate of growth. With
the exception of the last-mentioned, such problems cannot be solved by a study of
the adult fishes. For instance, if the catch of a certain species of edible fish
suddenly drops to a low level at a period when it may be expected from previous
experience to be much more abundant, it will probably be found quite useless to
study the conditions that obtain in the waters of its occurrence during the season
when the low returns were actually noted; rather must the reason be sought for
much earlier. Perhaps certain biological, physical or chemical conditions of the
water militated against a heavy spawning, or were so unfavourable during the
early stages after hatching that relatively few survived. But we cannot investigate
PRESIDENTIAL ADDRESS. ix
these questions at the time the actual paucity of fish is noticed, at a time, in
other words, when they have reached a size which warrants their capture for
market; they can be solved only by an investigation when the unfavourable
conditions themselves obtained, perhaps four or five years earlier. If, for instance,
it is found that there is a lack of sufficient food for the vast population of these
young fish, or, perhaps, that one of the many other conditions that influence the
rate of survival is adverse at this critical period, the number that can possibly
survive will necessarily be restricted, and it will be known long before these fish
are taken in the fishermen’s nets that the catch will be a poor one. Indeed, as the
result of continuous research along these lines in the North Sea, it has been found
possible with some species of fish to predict with reasonable certainty the extent of
the probable catches for some seasons ahead.
Clearly, therefore, much light has been thrown on the fundamental problems
of the productivity of the sea in Huropean waters, and it will help us who face
similar problems in the waters of Australia, if we are familiar with the knowledge
gained there. On account of its great productivity over a long period and its
proximity to scientific marine laboratories, the North Sea and the English Channel
have received most study, and I therefore propose to summarize one aspect,
probably the most important aspect, of the discoveries that have been made in
that region.
We shall have much to say about the plankton, and it is therefore advisable
that we understand clearly just what the plankton is. It consists of a great
drifting community of plant and animal life, most of it microscopic. The plant
life of this community is known as the phytoplankton, and the animal life as the
zooplankton.
In the English Channel and the North Sea, during the early months of the
year, March and April (spring in Europe), when the strength of the light is
increasing, a great change in the plankton occurs. The phytoplankton increases
enormously. Now, these microscopic plants form the food of a host of marine
animals, and with such an abundant food supply available, these animals in turn
multiply greatly; so greatly, indeed, that the supply of plant life cannot long
stand up to the strain, and by May or June it is found to have diminished very
strikingly. It has not only maintained the animal life that swarms at the surface,
but much of it has also fallen to the bottom, where it is consumed by the animal
communities that favour that environment. It has served the purpose of developing
a great, a new animal plankton which continues to survive during the summer
period of diminished plant life by warring amongst itself, the larger forms preying
on the smaller.
In the autumn, about October, there is another outburst of plant life, but never
so great as in the spring, and then follows, during the winter months, a period
when the plankton is at its very lowest, but always with sufficient of all forms
surviving to give birth to the great increase characteristic of the spring months.
The abundance of these forms of life in the plankton determines the ultimate
productivity of the sea. The phytoplankton provides food for the zooplankton,
the smaller forms of which are consumed by the larger, which in turn provide food
for the small fishes and other marine creatures adapted to consuming them, and
these in their turn fall a prey to the larger fishes that provide a diet for man.
If, then, there were no phytoplankton in the sea, there would be no fishes for man
to harvest. A knowledge of the seasonal abundance of the plankton is, therefore,
a fundamental necessity before the abundance or scarcity of the fishes can be
understood.
x PRESIDENTIAL ADDRESS.
But we have not yet gone back to the very beginning, for it is necessary that
we know the causes of the fluctuations of the plankton and the succession of
life in the sea. This problem, too, has received careful study by European scientists
during recent years and much light has been thrown on it.
The plant life, which, as we have seen, forms the basis of the food of the
animal life of the sea, is dependent for its existence on the nutrient salts
contained in sea water, and on the strength of the light which will enable it to use
these salts for the storage of nourishment in its tissues. If, therefore, these
forms of nourishment in solution are not constant, and if the light varies in its
intensity, we should expect to find the plant life of the plankton to vary
accordingly. And this is just what has been found to occur.
Of the many constituents of sea water the phosphates and the nitrates have
been found to play, more than any others, a determining role in regulating the
quantity of plant life that may develop in the sea. In the North Sea these
salts are present in greatest quantities during the winter months and up to the
beginning of March. It is in March, as we have seen, that the great outburst of
plant life occurs; why, then, if the requisite nutrient salts were abundant during
the winter, did it not develop then? It is here that the intensity of the light
plays its part. During the winter the days in the North Sea are short and the
intensity of the light at its poorest, so poor in fact that the plant life in
the plankton is unable to avail itself of the salts at its disposal. As the days
lengthen and the light increases, more and more of these salts can be absorbed
and thus it is that the great outburst occurs in the spring. So great a toll is
taken of the available salts that they are quickly used up and within about a
month or six weeks little remains, and the further increase of the plant life is
inhibited. It does not remain stationary, however, for much of it perishes for
lack of further nutriment, and great quantities are consumed by the animal life
of the plankton which, too, has developed enormously as the result of the abundant
food supply the plant life has provided.
But we still have the increase of plant life in the autumn to account for.
The heat of the sun’s rays during the summer has caused a rise in temperature
of the surface waters, but not in the deeper layers, and while the nutrient salts
have been used up at the surface, they have been maintained in the deeper
layers by the large quantities of animals that have died at the surface and fallen
to the bottom. It is not till the autumn, however, when the surface waters cool
down, that the two layers are able to mix, and this is aided considerably by the
gales that are common in the North Sea during that season. And so the surface
layers are replenished with nitrates and phosphates in sufficient quantities to
allow of another marked outburst of plant life.
Plankton Fluctuations in New South Wales Waters.
That, in brief, is the story that has unfolded itself after many years of
research by a considerable number of marine biologists and chemists. But how far
has our knowledge of these fundamental data progressed in Australia? What is
the nature of the plankton in the seas washing our coast? In what way, both in
the types to be found here and in their seasonal abundance, does this plankton
differ from that of EKuropean waters? Is there a great seasonal fluctuation such
as has been found to be a characteristic feature of the plankton of the North Sea?
Concerning these questions we in Australia knew practically nothing, and it
was these and related problems that Dakin set about to investigate, for a knowledge
of them will enable us to explain the natural fluctuations of the fish in the sea,
PRESIDENTIAL ADDRESS. xi
and will help us to account for the migrations that many of these fish undertake
periodically. But these migrations may be very extensive; they may extend in
some cases from the waters of Tasmania, cooled by an antarctic current, to those
of Queensland, warmed by a tropical current from the north. A complete under-
standing of these movements will therefore be gained only if the conditions
throughout the range of the migration be understood, and this would involve
continuous work at a series of stations from Tasmania to Queensland. Dakin had
to limit the sphere of his activities practically to one restricted area, in the
vicinity of Sydney; even then it was a giant’s task for one investigator to
undertake, and it was rendered all the more difficult by the lack of a boat which
would allow of the work being carried out in reasonable comfort. Nevertheless,
in the comparatively short time of ten years he has succeeded in throwing much
light on the problems he set about to solve.
An area, four miles east of North Head, Port Jackson, was chosen for the
investigation, and efforts were made to reach this spot at fortnightly intervals, at
or about the hour of high water, and at about the same time of day on each
occasion. The period of high water was chosen to ensure that the water where
the investigations were to be carried out would not be contaminated by the water
flowing from Sydney Harbour on the ebb tide.
After two years’ work, Dakin (1931) was able to announce that the catches
of plankton were very uniform compared with the seasonal variations of those of
the North Atlantic. But there were variations, nevertheless, both in quality
and quantity, and the regular hauls of plankton over this period at last enabled
a comparison to be made with the catches in other waters. For two years two
nets had been towed twice a week in the Irish Sea, the average plankton catch
being 14 c.c. Two similar nets towed each fortnight in the sea off Sydney
Harbour gave an average of only 4 e«.c., and Dakin’ pertinently asks if this is a
measure of the relative productivity of the two regions in fish food.
In a conjoint paper published in these Procrepines, Dakin and Colefax (1933),
working in the area previously selected by Dakin, discussed the species of diatoms
most prominent in their catches; they found that at this station they consisted of
the usual admixture of oceanic and neritic species, which might be expected
within the vicinity of a continental shelf and the open ocean, with, as usual, only
a few species quantitatively of great significance. All the important species were
found to be well-known types, those predominating belonging to the genera
Chaetoceras, Asterionella, and Thalassiosira, which have a wide distribution in the
seas of the northern hemisphere. With few exceptions, however, they were recorded
from Australian waters for the first time. While peculiarly Antarctic species
played little part in their catches, there was found to be an admixture of temperate
and tropical types.
Quantitatively, these authors confirmed Dakin’s previous conclusion that the
changes in volume of the diatom catches during the year east of Sydney is nothing
like so marked as it is in certain colder seas. Seasonal variations were scarcely
obvious from inspections of the nets, and it was not until their enumerations
were complete that a picture of diatom change directly comparable with that of
northern seas became clear, the net result being a curve representing the rise
and fall in the quantity of the plant plankton, with a peak in early spring and
another smaller one in late autumn. There is, therefore, a striking similarity
with the plankton rhythm of Huropean seas, and this was the first time a
rhythm of this kind had been discovered in the southern hemisphere. The
Xil PRESIDENTIAL ADDRESS.
abundance of planktonic algae in spring is nothing like so great as in the colder
waters about Britain, but it is nevertheless quite marked, though it is relatively
earlier than in British seas.
An analysis was also made of the animal plankton, and a clear indication
was obtained that the chief constituents of the zooplankton have their maxima
just after those of the phytoplankton. Thus the zooplankton presents a maximum
in the summer, with peaks in the early summer (November to December) and
another in autumn. The zooplankton maxima were found to be due principally to
Copepoda and Cladocera.
Fish Eggs in the Plankton.
During these investigations, also, Dakin and Colefax discovered eggs of several
species of fish in considerable abundance. Anchovy eggs, distinctive on account
of their elliptical shape and characteristically segmented yolk, were found in
large numbers in January, 1931, and in November of that year they again began
to appear and remained in the catches till January, 1932, although in January
they were not found in large numbers. Eggs of two different sizes, but very
striking on account of a vitelline membrane with a distinct blue tinge, a
relatively large perivitelline space and a segmented yolk, were found in great
abundance between June and August, 1931. These were thought to be clupeid
eggs, possibly those of Sardinops neopilchardus, the common pilchard of New
South Wales waters. From January to April, 1932, eggs of several unknown
species of fish also occurred in considerable numbers, the peak being reached in
March.
In March the following year Dakin and Colefax (1934) were able to state
definitely that these “blue” eggs were actually those of the Australian pilchard,
for early stages from those newly hatched to young fish up to 28 mm. in length
were obtained, and these allowed of a definite determination being made. The
eggs were abundant in three successive years during the months of June, July
and August. Actually, in 1933 the eggs were first found in the catches late in
May. Special efforts were then made to obtain later and later larval stages, and
in this great success was attained until, at the beginning of August, they
disappeared. The eggs range from 1:27 mm. to 1:5 mm. in diameter, the average
being 1-44 mm. The bluish tinge previously noted is purely optical and not due
to the presence of pigment; it disappears when the membrane is dissected away
from the egg. A single oil globule is present as in the Huropean and Japanese
pilchard eggs. In addition to these characters of the egg, the authors describe in
detail those of the young fish till it reaches a length of 28 mm.
The number of eggs and larvae captured was at times considerable. For
instance, in a net of cheese cloth with a circular mouth three feet in diameter and
towed only for ten minutes near the surface, 406 eggs of S. neopilchardus were
obtained on 18th July, 1931, and over a thousand in a similar haul on 21st June of
that year.
This was a very important discovery, for, although it has been known tor a
long time that pilchards may be found to occur on the eastern Australian and
Tasmanian coasts in great quantities, there are very few reliable records of the
season of their occurrence, for satisfactory identification of the actual species
comprising the shoals has all too frequently not been obtained. If a shoal of small
fishes is seen breaking the surface of the water, it is usually assumed that they
are pilchards, whereas in many cases a more critical examination of actual
specimens might possibly have disclosed that they were sprats, anchovies,
PRESIDENTIAL ADDRESS. xiii
maray, or perhaps herrings. There has been a good deal of evidence, however,
to show that pilchards do occur on the New South Wales coast during the winter
months, and the finding of the eggs and the early stages of the young fish at that
period during three successive years is not only a striking confirmation of these
observations, but it has the additional importance that in the area of these
investigations, from Port Stephens on the north to Port Hacking on the south
at least, the fish were spawning at that time.
Further investigations by Dakin (1937) indicated that the spawning of the
pilchard on the coast of New South Wales occurs over a much longer period
than was indicated previously, for small pilchard larvae varying between 8 and
20 mm. in length were taken in the months from April to November. Large
numbers of eggs were obtained at Port Hacking at the beginning of May, and
some very large catches were made off Broken Bay in October. Since, however,
larvae were obtained in April, it may be assumed that some spawning takes place
in February, and Dakin suggests that possibly eggs may be taken in every
month of the year. The largest catches made to date, however, were obtained
during May, July and October.
In this paper, also, the occurrence of pilchards at the entrance to Broken
Bay was recorded for four consecutive weeks in May, 1935, and in the same
locality in July, 1937. Shoals of maray were seen and captured at the entrance
of Sydney Harbour in August, 1937, and sandy sprats about the same locality in
June, while freshwater herring in full roe were marketed from the freshwater
reaches of the Clarence River in July, 1937.
Physical and Chemical Conditions of the Sea Water.
In 19385, Dakin and Colefax published some observations on the seasonal
changes in temperature, salinity, phosphates, nitrate nitrogen and oxygen of the
ocean waters on the continental shelf of New South Wales and their relationship
to plankton production. The records were obtained at the same station as
previously, about four miles east of North Head, Sydney Harbour.
The total range of temperature variation of the surface water was found to
be only about 7° C., the average range at a depth of 30 fathoms being still less.
The highest temperatures reached are usually between 22° and 23° C. and occur in
February and March. The lowest-surface temperatures, 15°-16° C., occur in August
and September. During the period that the temperature is at its lowest the water
at the surface and the bottom is almost at the same temperature, while from the
date in spring when the surface waters begin to rise in temperature the difference
between the surface and the bottom becomes more and more pronounced. The
condition in summer will therefore hinder any rapid regeneration of nitrate and
phosphate supplies if these substances are exhausted in the surface waters by the
activity of the plankton, for the pronounced “layering” will tend to prevent supplies
passing upwards from the sea bottom. Abnormal weather conditions may, however,
on the continental shelf, bring about a temporary destruction of the summer
conditions.
At this station the water had an average salinity of approximately 35:5%., the
extremes on the surface in 1933 being 35-80%, and 35:36%,.. No seasonal rhythm
was apparent.
The phosphate content was found on the whole to be very stable throughout
the year; there are variations, but the average during the summer is not appre-
ciably less than during the winter, and at the surface it varies between about 15
and 25 milligrams of P.O; per cubic metre. On the whole, the coastal water of
xiv PRESIDENTIAL ADDRESS.
New South Wales approximates somewhat to the English Channel conditions, but
without the exhaustion of P.O; in the summer. A seasonal cycle is therefore not
pronounced. There are, nevertheless, some important variations, but they are
usually of brief duration; for instance, the phosphate content was almost down to
zero during the whole month of September and the first week of October, 1934.
The plankton catches provided a striking confirmation of the theories advanced in
Europe to explain the variation in nitrate and phosphate content of the surface
waters of the sea during the year, for they showed that the phosphate content
never went down to zero without there being an unusual (for this place) develop-
ment of diatoms.
Notwithstanding the fact, however, that a large outburst of phytoplankton
will bring down the phosphate content of our coastal waters to zero, this condition
does not continue for the long season noted in British waters. On occasions in
1933, when the phosphate in the surface waters was reduced to a trace, it was
again normal ten days or so afterwards. After the spring diatom maximum in
September, 1934, the phosphates were down to zero for about three weeks.
Regeneration from deeper waters then resulted in the amount rising to 20 mg.
per cubic metre, and this figure was maintained during the summer.
While, therefore, the presence of large numbers of diatoms and other phyto-
planktonic organisms may reduce the phosphate content of our waters, it cannot
be said that the spring or autumn maxima of the phytoplankton are dependent
upon the phosphates gradually attaining a maximum. Phosphate has been avail-
able in sufficient quantity for two or three months before the spring plankton
maximum, and it is also present during the greater part of the summer.
The rapid regeneration of phosphate in the surface waters after the diminution
in the speed of plant production may be accounted for by the quantity present in
deeper water. On all occasions in 1933 when the surface phosphate was reduced
to zero, it was never less than 13 mg. per cubic metre at 50 feet, and was between
20 and 38 mg. per cubic metre at 150 feet.
Dakin and Colefax also found that in New South Wales waters there are
fluctuations in the nitrate nitrogen content of the sea which can be correlated
quite clearly with fluctuations in the productivity of the sea in plankton. But
here, too, it was found that the seasonal changes are not nearly of such amplitude
as those of the Hnglish Channel. Of special interest, however, is the discovery that
the nitrogen content is apparently much more sensitive to the reproduction of the
phytoplankton than is the phosphate.
In the spring of both 1933 and 1934 the nitrate nitrogen was reduced to zero,
and on both occasions the reduction was accompanied by a great diatom outburst.
During 1934 the concentration of the nitrate nitrogen in the surface water remained
below 10 mg. per cubic metre for practically the whole of the summer.
Trawled Flathead. =
Of all the species of fish marketed in New South Wales the tiger flathead
(Neoplatycephalus macrodon) taken in the nets of the trawlers is the most
abundant; it may also be regarded as the most important. We have seen that
commercial trawling was initiated in New South Wales in 1915 when three trawlers
began operations. From the beginning the predominant fish caught was the tiger
flathead, which rapidly replaced the sea mullet (Mugil dobula) as the species
marketed in greatest abundance in New South Wales. The trawling grounds
exploited in the early years of the industry extended from Newcastle to Cape
Howe, although only circumscribed areas of sea bottom were fished. For several
PRESIDENTIAL ADDRESS. XV
years the grounds situated nearest to Sydney, particularly that lying north-east of
Sydney Harbour and that extending some distance north and south of Botany Bay,
which are usually referred to as the ‘‘Home Grounds”, were found to yield great
quantities of flathead every year between early September and the beginning of
December or at times a little later. Then in 1926 these grounds failed to produce
their customary supplies and the trawlers were forced further afield during that
period. Unfortunately, this proved to be not an isolated experience, for these
grounds, so prolific in their yield for about eleven years, have remained poor
right to the present day.
During these early days of the industry it was found, also, that the “southern”
grounds situated in the Hden—Green Cape area, produced fish in prolific quantities
during the period from January to July, but these grounds, too, deteriorated, not
only in their production of flathead, but of all other classes of fish, which formerly
were found in great abundance. The trawlers were consequently forced still further
afield, and in 1929 the grounds discovered by the “Hndeavour” off Cape Everard in
Victoria and east of Flinders Island were explored. These were found to yield
rich hauls and an intensive fishery was conducted there, but their subsequent
history was little different from that of the grounds previously worked, and in
the course of a few years their yield showed a marked decline.
Now, as the trawlers were forced further and further away from their base,
the operating costs mounted considerably; the cruises, which originally lasted
from three to six days, were now occupying from seven to ten days, involving a
much heavier consumption of coal, an increased wages bill and the provision of
much greater quantities of ice. Moreover, there has been a considerable decline
in the hourly yield of both flathead and other fish.
What has happened? When we come to reflect that the trawling grounds in
European waters, such as those of the North Sea, which, although they have shown
a decline in productiveness, have withstood a fishery extending over several genera-
tions with a far greater number of trawlers operating, the much more rapid decline
in the yield of the New South Wales trawling grounds gives much food for thought.
It must be realized, however, that the total area of the grounds worked by the New
South Wales trawlers embraces about 6,000 square miles, while those of the North
Sea embrace about 130,000 square miles. Have our trawlers, confined to a very
restricted area, removed fish from our waters at a greater rate than they can with-
stand? An excellent comparison between the rate of catch here and that of the
Irish Sea has been made by Dakin (1931), who stated: “The present New South
Wales grounds all added together are only about two-thirds of the Irish Sea—the
area of water between Ireland and Hngland—and this from the point of view of
steam trawling is nothing more than a huge lake. Discussions are frequent in
Europe on the impoverishment of the Irish Sea and North Sea owing to the
enormous fishing. Well, we have removed from our coastal area, in one year by
trawling alone, four times the catch that the Irish Sea has provided in the same
time with its far more boats and men.”
Are the fish caught by the New South Wales trawlers more susceptible to over-
fishing than those of Huropean waters? If so, how can we stay the decline? Can
we restore the grounds to the level of their former productiveness? Those are the
vital questions facing the trawling industry today, but before we can hope to solve
them we must know much more about the natural history of the various fish
comprising the catches than we do at present.
On account of the great economic importance of this branch of our fisheries,
and because of the fact, too, that we knew practically nothing of the habits of the
xvi PRESIDENTIAL ADDRESS.
fish, such as the flathead, that formed the basis. of the industry, A. N. Colefax
decided in 1930 to devote considerable attention to the study of trawled fish, with
particular reference to the flathead, the most important species caught. The results
of this investigation were published in this Society’s ProcrErpines in 1934 when the
distribution, supply and length statistics were discussed, and in 1938 when its
feeding and breeding habits were described.
Beginning in 1930, Colefax made thirteen cruises in trawlers over a period of
twelve months, the length of trip varying from seven to nine days. Practically
all of the trawling grounds were visited at least once, and in some cases several
visits were made. He found that the decline in the yield of “mixed’’ fish is one
of the most important changes that have occurred during the later years of the
industry. The average hourly catch for the year 1930 was found to be 2:97 ecwt.
only, compared with 4:56 cwt. during 1921 and 4-68 cwt. during 1922. This
decline was even greater than the figures indicate, for fishing operations were
conducted in 1930 with much increased efficiency, and an improved form of otter
trawl (the Vigneron-Dahl) was in use. Reducing the production figures to curves,
Coletax found that perhaps the most striking feature of the 1930 curve for all
species, flathead included, apart from the general low level of the catches, was its
“flatness” when compared with corresponding curves for, say, 1921 or 1922. This
was due to the almost entire disappearance of fish from the Botany area, and the
considerable decline in the yield of the southern grounds.
Length measurements of the flathead, as they occurred in the hauls, were
conducted with several objects in view. Firstly, as Colefax states, it is well
known that if taken over a sufficiently long period at different seasons and
without artificial selection of the samples, they may present a picture of size
classes which may be used for the determination of age. The distribution of size
classes can be used for the discovery of migratory movements of the fish, and,
finally, comparative treatments of length measurements may give valuable
information regarding over-fishing.
In waters where the range of temperature between summer and winter is more
marked than it is in New South Wales, the growth-rate during those seasons
frequently shows itself in the form of well-defined bands on the scales, and in
the uneven development of the otoliths, opercular bones and vertebrae, so that the
age of a fish can be readily determined by a study of those parts. In the more
equable waters of New South Wales, however, the growth-rate of the fish appears
to be much more regular; the secondary indications on the scales are not nearly
so clearly delineated, and the age of the fish cannot usually be determined with
the same degree of certainty. Recent experiments by Professor Dakin in the
grinding down of the otoliths give promise, however, of throwing much light on
this question.
Another very valuable method, which not only gives an accurate picture of
the growth-rate over a certain period, but also gives an indication of the migration
of fish, is that of tagging them when caught and immediately liberating them.
This method is scarcely open to an investigator working on board a commercial
trawler, for the reason that most of the fish when brought to the surface are dead.
It should have practicable application, however, on a boat using a Danish seine
net, in which most of the fish are brought up alive, and this should be kept
in mind in subsequent investigations of this nature.
The measurements of some 35,000 flathead were taken by Colefax during a
series of monthly cruises, the period ranging from March, 1930, to April, 1931,
and over an area of coast extending from Port Stephens to Cape Everard. It was
PRESIDENTIAL ADDRESS. Xvii
found that four age groups were readily distinguishable, the first being represented
by fish 24 cm. in length, the second by fish 30-36 cm., with a tendency to
predominance at 31-33 cm., the third mainly by fish of 42 cm., the range being
41-44 em., and the fourth by fish of 54 cm. in length. But a serious discrepancy
was found inasmuch as flathead less than 20 cm. were not taken in numbers, so
that data regarding the sizes from 1 to 20 cm. are entirely lacking. The intervals
between these ‘“‘peaks” are approximately equal, about 8-10 cm., and it is reasonable
to assume that they correspond with four age groups. If, therefore, the period
from 1 to 20 cm. be denoted by the symbol “x” years, then the ages of the
succeeding groups are x+1, x+2, and x+3 years respeetively.
It was also found that there is a tendency for the flathead of one age group
to remain on the same ground for long periods, and for the fish to move about
in age groups, while on two occasions the study of the measurements of the fish
indicated important migratory movements.
In his investigations of the feeding habits of the tiger flathead, Colefax (1938)
found abundant confirmation of the experience of the men engaged in trawling
that only on rare occasions can flathead be caught after dark. It has become
the custom for the trawlers to fish up till about 7 p.m. and then cease operations
until the following morning, though heavy catches of flathead have been taken
on occasions during the night, indicating that the fish do not always leave the
bottom. This migration from the bottom towards the surface at night is apparently
correlated with the feeding habits of the fish, for the contents of the stomachs
examined indicated that it preys extensively on the HEuphausid, Nyctiphanes
australis, the stomachs of even the largest individuals being frequently found
distended with this small crustacean, while some of the remaining food-types
were found to be mid-water or even surface-swimming forms.
Gut samples were taken on each cruise over a period of some fifteen months
from practically every fishing ground along the coast. For all sizes of flathead the
most common constituent is fish (51:2%), followed by crustaceans (25%). Of the
fish, Apogonops anomalus is consumed in greatest numbers, comprising 36°4% of
the total. This is quite a small fish, seldom exceeding five inches in length, and it
must be very abundant on the trawling grounds at times, for considerable
quantities are occasionally brought up in the nets, in spite of their wide mesh.
The most abundant crustacean found in the flathead’s stomach was Nyctiphanes
australis, which constituted 60% of the whole of the crustaceans consumed. It
was found that the flathead tends to change its diet as it becomes larger, the
proportion of fish consumed increasing with the size of the flathead.
On account of the great prominence of Apogonops in the diet of the flathead,
considerable attention was paid to the diet of this small fish, and it was found
that the main item consisted of copepods (76%), followed by Nyctiphanes larvae
(26:3%), Nyctiphanes (13:1%), with a smaller percentage of bottom mud and
unrecognizable debris. It is in part, therefore, a plankton feeder, and this suggests
that the flathead may pursue it into the upper layers of the water.
Colefax also found. that the smaller sizes of flathead tend to occur in the
shallow water near the coast, while hauls made in deeper water provided
individuals of a larger average size, and he found evidence that would appear to
indicate that this is largely due to the marked difference in the types of food
available in those regions.
Coming now to the breeding habits of the flathead, it was found that the first
definite indication of the breeding season occurs in September, although as early
as July the ovaries may show signs of development. Breeding extends almost to
B
xviii PRESIDENTIAL ADDRESS.
the end of summer, but the actual breeding grounds were not discovered, for only
about a half-dozen really ripe females were seen amengst thousands of fish
examined, and spent females were also scarce, this presumably indicating that
the flathead were not spawning on the actual fishing grounds. The northern
flathead were found to spawn earlier than those on the southern grounds, the
spawning period in the north terminating about the middle of December. It was
determined also that the tiger flathead produces up to two and a half million
eggs in one season.
The smallest flathead examined with partially ripe ovaries measured 30 cm.
(11:8 inches) in length. This is interesting in view of the fact that the minimum
lawful size for the sale of this fish is 13 inches. The smallest sexually mature
male examined was 23 cm. in length, 10 cm. shorter than the smallest female.
There appears to be a size dimorphism in the two sexes and a probability that
the females mature more slowly.
The Life History of New South Wales Prawns.
The prawn industry of New South Wales is one of considerable economic
importance, the value of the yield averaging about £38,000 annually, an unusually
high figure being recorded in 1931, when the quantity obtained amounted to
1,537,420 lb., valued at £76,871. Yet, although a good deal was known about
the habits of our commercial prawns in the adult stage, practically nothing was
known until the last few years about their breeding habits, a knowledge of which
is essential before sound measures can be applied towards their conservation.
Actually, there are two principal commercial species in New South Wales
waters, one known as the king prawn (Penaeus plebejus), the other as the school
prawn (Penaeopsis macleayi). The habits of the adults of both species are very
similar. They are found in estuaries and so-called lakes, which usually have
a narrow outlet to the sea, and are caught in greatest abundance as they make
a Mass migration to the sea during the period after full moon, before the moon
actually rises, when the nights are at their darkest.
But why this migration to the sea? Although it was assumed in some quarters
that they were making to the sea to spawn, they were rarely found with roe, and
most fishermen were firmly of the opinion, without any real evidence, however,
to support it, that spawning took place in the estuaries. On account of the
importance of the fishery, and in an effort to establish beyond doubt the breeding
place of these prawns, Professor Dakin included this investigation in his
programme, concentrating his attention on the king prawn.
Dakin (1935) found that in Port Jackson the only time when king prawns
were taken with well developed roes was in late summer, and they were always
located near the entrance. But always when large king prawns were obtained
from the ocean (these were brought up in the trawl nets) the gonads were well
developed. Early larval stages of king prawns were obtained in plankton nets
at sea, but never in the estuaries and lakes, and this was regarded as reasonable
evidence that this prawn, at least, spawns at sea.
Continuing this work, Dakin (1938) was able to obtain sufficient evidence to
establish this without any possible doubt. So far he has not located the eggs
and the very earliest stage of the newly hatched young, the nauplii, but the
capture of an almost complete series beyond those stages has enabled a fairly
full picture to be presented.
The evidence from the plankton collections indicates that this prawn breeds
over a long period of the year; this will explain the occurrence of prawns of
PRESIDENTIAL ADDRESS. Ib
such different sizes as can be obtained in any particular week from different
localities on the same river estuary. The captures of larvae in the plankton
indicate the deposition of eggs between January and June, and also in August,
the largest captures during 1937 being taken in March and April.
It was found that it is during the post-Mysis stage and later planktonic stages
that the young prawns enter the harbours and estuaries and migrate to the
upper waters of these regions. The earliest stage at which the king prawn
leaves the plankton and seeks the bottom is that in which eight, nine or ten
rostral teeth are present, and when it is approximately 17 mm. in length. The
growth of the king prawn, like that of related species overseas, appears to be
very rapid, for the evidence obtainable indicates that many large king prawns,
leaving the estuaries for the sea in February, entered the estuaries as post-larval
stages approximately twelve months before. In some cases it may be even less;
in others, where growth has been retarded or the lake has been closed, the age
will naturally be greater, and two years may be necessary before maturity is
reached. Dakin is also of the opinion that from four to eight months elapse
between the time when the prawns make to the sea and when they are ready
to spawn; in other words, that it is probably eighteen months at least before the
first sexual maturity is attained, the final development of the gonads being
accompanied by a very considerable increase in the size of the animal.
Dakin observes, also, that nothing is more certain than the fact that these
large prawns never re-enter the estuaries after spawning, for they would be at
once recognized by their size, but no evidence has been obtained to show whether
the mature prawn dies after one season’s reproduction, or whether it remains in the
ocean to breed more than once. He inclines towards the former view because no
very large specimens with spent gonads have been obtained from the sea.
The Murray Cod.
Although the Murray cod (Maccullochella macquariensis) is the most important
freshwater edible fish found in New South Wales, scant attention has been given
to the study of its habits and life history. Owing to the rather alarming state-
ments that are made from time to time concerning its rapid depletion, Dakin
joined forces with G. L. Kesteven, a young scientist until recently on the staff of
State Fisheries, in a preliminary investigation of this fish, with particular reference
to its life history and its artificial propagation with a view to re-stockng the streams
of its occurrence.
Dakin and Kesteven (1938) found that it is possible to hold the Murray cod
in cages of relatively small dimensions for considerable periods when suspended
in the river; after thirteen weeks’ confinement the fish appeared to be quite healthy
and became so tame that they fed out of the keeper’s hand. In a system of ponds
it should therefore be possible to keep them alive indefinitely.
The spawning period appears to vary considerably according to locality, and it
is possible to find some fish in full roe from October (and possibly September) to
January.
During their experiments on artificial propagation it was found that only when
approaching full development of the roe was it possible to distinguish males from
females; at this period the female showed a greater swelling of the abdomen and
the genital opening became more swollen than that of the male. It was seen, also,
that when the female is ripe the eggs come away very easily, but considerable
pressure has to be exerted to strip the male. The actual procedure in artificial
fertilization consisted of stripping the milt from the male into a flat dish containing.
\¢
i
xX PRESIDENTIAL ADDRESS.
a small quantity of river water; the milt was stirred well in the water and then
the eggs were stripped into it. The sperm of the Murray cod is immobile until
it makes contact with water, and it lives only a few minutes, while the eggs, after
fertilization takes place, become adhesive. More than 90 per cent. of the eggs
produced larvae, the actual hatching period occupying nine days at a temperature
which varied from 62°F. to 74° F., with an average of approximately 68° F.
Following the success of their experiments the authors consider that there should
be no difficulty in the hatching of the Murray cod on a large scale, though there
would appear to be considerable difficulty in obtaining a sufficient number of both
females and males in a spawning condition at the same time.
The development of the Murray cod after hatching was found to be rather
rapid; the yolk sac had almost disappeared ten days after hatching, and in less
than nineteen days the adult form of the fish was well developed. They were kept
alive for 32 days and during this time the growth-rate was noted, but a reliable
comparison between the growth-rate of young fish kept in an aquarium, as these
were, and those in a large body of water can scarcely be made, for apart from the
consideration of the most suitable types of food, experience with other fish reared
in captivity indicates that the small body of water contained in the aquarium is
itself a deterrent to rapid growth.
The Oyster.
As in other branches of the fisheries of New South Wales, scant attention was
paid until recent years to the scientific investigation of the oyster. There are
several species found on the coast of New South Wales, and in the early days of
the Colony two of them were common; one, the present commercial oyster, Ostrea
commercialis (cucullata), was extremely abundant from the Queensland to the
Victorian border, the other, O. angasi, was prevalent only along the southern half
of the coast. Owing principally to the ravages of the mud worm (Polydora ciliata),
O. angasi has been almost exterminated throughout its range on the New South
Wales coast, but O. commercialis, more valuable on account of its superior edible
and keeping qualities, has been cultivated extensively and forms a valuable
industry, the average annual production for the years 1928 to 1937 being valued
at £75,600.
In 1883 Tenison-Woods stated that the sexes of the common commercial oyster
(O. commercialis) are distinct, and the eggs are probably discharged into the
water where they may easily meet with sperm from the males. By mixing “the
male and female fluid” it was found that fertilization of the ova readily occurred.
Later, in 1888, Tenison-Woods appears to have altered his views on the discharge
of the sexual products into the water, for he stated that the “young oysters are
reared in the gill-chambers of the mother, in the case of the Australian oyster,
O. mordax”’. It seems probable that Tenison-Woods was confused with his species,
tor the taxonomy of the New South Wales oysters was at that time very unstable.
In the first instance, he was apparently dealing with the oviparous O. commercialis,
and in the second with the larviparous O. angasi, both of which were then plentiful
in the neighbourhood of Sydney. Altogether Tenison-Woods’s observations were
quite confusing and threw little real light on the subject.
The work of Saville-Kent (1890), although it erred in a number of particulars,
contained much of value. He stated that in the case of O. glomerata (commer-
cialis) fertilization takes place in the water, “the young embryos .. . being thrown
upon their own resources from the earliest period of their existence”, and that
the embryos of O. angasi are retained within the mantle cavity of the parent.
PRESIDENTIAL ADDRESS. Xxi
Saville-Kent described the embryonic development of O. commercialis as far as
the complete envelopment of the embryo by a shell, but erroneously assumed and
actually illustrated their attachment at that stage as spat, stating that the length
of larval life occupied, under favourable conditions, four days.
The “Mud Worm’. f
{
In the early days of the oyster industry, the bulk of the oysters were obtained
for market from beds situated below low-tide level, and, a dredge being: necessary
to gather them, the grounds on which they were grown came to be known as
“dredge” beds. About 1870, however, the oysters growing on the dredge beds of
the Hunter River were found to be dying in large numbers, and an examination
disclosed that the shells of the oysters were extensively infected with mud worms
(Polydora ciliata). Until that time there appears to have been no reference to
such an infection, and there is no satisfactory evidence as to the cause of the
outbreak. Gradually, however, it spread to other rivers and in the course of time
rendered the principal dredge beds of the State useless for the cultivation of
oysters. With the deterioration of the oyster-bearing grounds situated below low-
tide level, oyster growers were forced to confine their cultivation to the inter-tidal
zone. The mud worm has therefore had a profound effect on the cultivation of
oysters in New South Wales, and it remains to this day the greatest pest the
oyster growers have to combat.
Much light was thrown on the attacks of this worm by an investigation carried
out by Thomas Whitelegge (1890), a zoologist of the Australian Museum.
Whitelegge found that the attacks were most severe on the mud flats about low-
water mark. He formed the opinion that the worm in its early larval stage swims
into the oyster and fixes itself by its head on the margin of the shell; here it
immediately begins to construct a tube and rapidly accumulates a large quantity
of mud, which is at once covered over by the oyster with a thin layer of shelly
matter; if the oyster is healthy the deposit is laid down quickly, confining the
worm with its patch of mud to a very small space. On the other hand, if the
oyster is unhealthy and already infected, deposition of the shell material is slower
and the worm collects a large patch of mud before the layer is solidified. Hence
it is that the size of these accumulations gets larger as the attacks increase and
the oyster gets weaker.
Whitelegge studied the life history of the worm and found that for the first
six days the larvae swim about vigorously, after which they begin to settle down
and are capable of attaching themselves by the head with leech-like tenacity, a
faculty which appears to be of great value to the worm for it enables it, when it
swims between the gaping valves of the shell of an oyster, to exercise some choice
in its place of attachment.
Whitelegge found that if the oysters were removed from the beds, washed free
of mud, and then placed where they were sheltered from the sun’s rays for a
period of about ten days, the worms were killed and the oysters survived.
Winter Mortality of Oysters.
Of recent years the oysters from Port Stephens on the north to the Victorian
border on the south have been subject to a mortality during the late winter months;
this varies in its intensity from year to year, but usually causes heavy losses to
the oyster growers. On account of the mortality making its appearance during
the coldest months of the year, it was thought that it was the outcome of the
chilling of the oysters, and many oyster growers considered that it was caused by
XXii PRESIDENTIAL ADDRESS.
the trost lying on them when bared by the tide. This mortality was investigated
by me at the George’s River during the winters of 1924 and 1925, and an account
was published in these ProcreEpines in 1926.
It was found that the mortality was not caused by frost, nor even by the direct
action of low temperatures, for experiments carried out during both winters
actually shioowed that those oysters survived which were exposed to the cold air
longest, while those submerged during the winter in the more equable temperature
of the water died in large numbers. During this investigation it was found that the
lowest temperature to which the oysters were exposed was 36° F.; that after
packing oysters in ice for 72 hours few of them died when replaced on the beds;
and that oysters whose tissues were lightly frozen by a combination of ice and
salt survived for a period up to two months afterwards, and even after their
tissues had been frozen hard they lived for some weeks.
The food extracted from the oysters’ stomachs corresponded, in the types
comprising the bulk of it, with that extracted from the stomachs of the oysters
at Port Hacking and the Hawkesbury River, where no abnormal winter mortality
had been known to occur. The volume of the food obtained by the oysters was
found to increase with a rise in the temperature of the water, and on the flood
tide as against the ebb. At a temperature of or below 50° F. the shells of the
oysters remain closed.
Where a heavy mortality occurred during the winter of 1924 many of the
oysters still remaining alive had abscesses, ulcerations or inflammation of the
tissues, particularly common on the labial palps, gills and inner surfaces of the
mantles, but they also occurred in the gonad, digestive diverticula, stomach and
adductor muscle. Where the mortality was greatest ulcerated oysters were most
prevalent; in fact, a fairly definite ratio of ulceration to mortality was seen. The
cause of the abscesses and ulcerations was not determined, though microscopical
examination of the pathological areas indicated that they probably have a bacterial
origin. It was found that adverse conditions other than low temperatures, such as
lack of aeration, food, and the presence of decomposition products of dead oysters,
may also result in the formation of abscesses and ulcers.
Although the actual cause of the mortality was not discovered, the incidence
of the disease as determined by experiments conducted during both winters suggests
that it might be avoided by raising the oysters on wire-netting racks during the
menths from June to September inclusive.
The Life History of the New South Wales Oyster.
In 1928 I was able to announce that a sex-change occurs in the common
commercial oyster (0. commercialis) of New South Wales, which is an oviparous
species. Previous to this discovery all oviparous oysters were regarded as
unisexual, but subsequently it has been shown that the dominant oviparous species
of the Atlantic coast of North America (0. virginica), of Japan (O. gigas), of
India (0. cucullata), and of Portugal (O. angulata) also undergo a sex-change.
The results of an investigation of the life history of the New South Wales
oyster, conducted by me at intervals over a number of years, the field work being
carried out at Port Macquarie and the Hawkesbury River, were published in these
PROCEEDINGS (1933).
The spawning of the oyster on the coast of New South Wales is very irregular.
With the warming of the water during spring the gonads develop rapidly, and may
become fully developed by the middle of December. Spawning frequently occurs in
such oysters during the high spring tides round about the Christmas period.
PRESIDENTIAL ADDRESS. XXxiii
These oysters may spawn again in late summer. If, however, owing to an
abnormally cool spring, the gonad develops slowly, spawning may occur in January,
or even as late as April or May. In other cases there may be several partial
spawnings throughout the summer months. Spawning is not confined to the
summer months, however, for on rare occasions intermittent light spawnings may
occur throughout the winter, as shown by an irregular winter catch of spat. When,
as is usual, spawning is completed by the end of summer, the gonad displays great
activity during the winter in the storage of glycogen in the vesicular tissue in
preparation for the development of ova and sperm in the spring.
This oyster was found to spawn on the ebb tide following a high spring-tide,
the temperature of the water being 68° F. and the density 1:020. The rate of
development of artificially fertilized eggs decreases as the density of the water
is lowered. At a density of 1:005 a large proportion of the eggs remained
unfertilized, and in no case did development proceed beyond the morula stage. At
a temperature varying from 68°F. to 70° F. and a water density of 1-021, the
free-swimming stage was reached in seven hours, and the embryos were completely
enveloped in shells in 34 hours. At an average temperature of 78° F. the embryos
began to swim as trochophores in six hours, while at an average temperature of
62° F. the same stage was not reached until 22 hours after fertilization.
Although practically all, if not all, young oysters spawn for the first time
as males, it was found that the sex-ratio of 3,000 oysters of marketable size from
the principal oyster-bearing grounds of New South Wales presented a very
different picture, for females always predominated, varying from 54 per cent. to
88 per cent. The average percentage was found to be: females 73, and males 27;
in other words, there were 2:7 times as many females as males. The determination
of sex in this oyster does not appear to be governed by the amount of food
available, as has been suggested for other oviparous oysters.
Fishery Investigations by the Commonwealth Government.
As I stated at the beginning of this address, a new outlook on fishery research
is dawning in Australia, for the Commonwealth Government has already begun a
large-scale investigation into various branches of our fisheries which should lay
a foundation for the sound development of new industries, just as the exploratory
work of the Commonwealth Investigation Trawler ‘‘Hndeavour’ did for our
trawling industry. But these investigations are intended to go much further than
did those of the “Hndeavour”, for, in addition to the all-important task of
discovering new sources of wealth in our fisheries, the research will be directed
towards the determination of the limits beyond which the exploitation of those
fisheries may proceed with safety in order that we may avoid the spectacle, already
seen here and in most of the fisheries of the world, of the removal of fish from
the sea at a greater rate than they can be replenished. When a new fishery is
established, it is customary to exploit it to the limit the available markets will
stand, without thought of the limit the fishery itself will stand, and all too
frequently the production is suddenly found to be subject to a progressive decline,
which, if not stayed, leads eventually to the failure of the industry. It is far
preferable that the limits of the fishery be realized at the beginning and the
extent of the catches so regulated that the fishery is maintained permanently
at a fairly uniform level, rather than that a spectacular rise in production occur,
to be followed by a similarly depressing fall in the yield. That is to be the
constant aim of the Commonwealth fisheries investigations.
XXiv PRESIDENTIAL ADDRESS.
The exploratory investigations of the Council for Scientific and Industrial
Research, which has been entrusted with the work, have, as stated by Dr. Harold
Thompson (1939) in a recent address to the meeting of the Australian and New
Zealand Association for the Advancement of Science held at Canberra, been
divided into two sections embracing tropical and temperate areas. Of these,
the latter will receive first consideration, and the region chosen for immediate
exploration extends from about the tropic of Capricorn on the north to Tasmania
and South Australia on the south. This is a natural choice, for it embraces the
most populous areas of five States.
We have already seen that no great extensions of the trawling industry are
likely, and I am convinced that the problems of our estuarine fisheries are for
the most part those of conservation rather than exploitation; if, therefore, there
is to be any large-scale development of Australian fisheries it would appear that
it can come only from our pelagic fishes, such as tunny, Australian salmon,
barracouta, pilchards, sprats and anchovies. And it is on these that the Common-
wealth investigations are being especially concentrated. We have known for some
time that the blue-fin tunny occurs in large shoals on the southern half of the
coast of New South Wales during the spring months, September, October and
November, and we have found that it cans excellently, but three months (or,
perhaps, one should say a maximum of three months) is a rather restricted
period for the commercial exploitation of this species with its present somewhat
uncertain methods of capture on a large scale. Would it be possible to can fish
of other species during the intervening period when tunny are no longer on our
coast in large shoals? Now, the Australian salmon, which, incidentally is a very
different species from the salmon of the northern hemisphere, is one of the most
abundant fish on the south-eastern Australian coast, but unfortunately it is not
regarded as a fish of prime edible quality. Would it be possible to improve the
quality of this fish when canned? Experiments to determine this were under-
taken by me, and it was found that, provided the fish were penned up for several
weeks, as is done in Victoria, before they are marketed, the palatableness and
texture of the fish improve considerably when canned. A factory was established
on the banks of the Wagonga River, on the south coast of New South Wales, and
provision has already been made for the disposal in Australia of over four
million tins during the next two years. So busy has the factory been in the
canning of salmon that the initial plans for the canning of tunny have had to
be left in abeyance.
But what becomes of the tunny when they leave the coast of New South Wales?
No evidence at all was available on this question until the Council for Scientific
and Industrial Research, at the suggestion of one of the officers of its fishery
section, S. Fowler, decided to carry out an aerial survey of the waters of south-
eastern Australia for the purpose of locating shoals of this and other species of
pelagic fish. Fowler (1937) found that during February and March very large
shoals of tunny and salmon were lying in an area extending from near Babel
Island, east of Bass Strait, to Schouten Island, on the eastern Tasmanian coast, a
distance of about 140 miles. The shoals generally were from about five to fifteen
miles offshore. This was an important observation and fully justified the survey,
for the occurrence of shoals of such magnitude had not been observed by the
fishermen operating in that region, possibly because they work usually closer
inshore, and it is conceivable that they might have been missed by an investigation
vessel, which, with its much more restricted range of observation, might easily
have failed to locate them. An interesting point arises as to whether the tunny
PRESIDENTIAL ADDRESS. XXV
seen in that area are the same fish as those which earlier were found on the
southern New South Wales coast. They may, of course, be a different race, but
anglers fishing for them on the south coast of New South Wales have reported
that late in the season the tunny appear to make off in a southerly direction.
The great value of the discovery, however, is that the season of the occurrence
of this important fish appears now to extend from September to March at the
least, although the regularity of its appearance in more southerly waters at the
season of these aerial observations has yet to be established. And then, of course,
the question arises as to the distance to be travelled to obtain the fish. Actually,
this should present no real obstacles, for, when it is realized that California tuna
boats travel up to three thousand miles for their fish, the distance to be travelled
in Australian waters to secure them is a relatively short one.
During these aerial observations, also, Fowler observed a shoal of salmon
lying in the Wagonga River, New South Wales, which he estimated to weigh a
thousand tons, while many thousands of tons were lying offshore adjacent to the
mouth of the river and in the vicinity of Montague Island. During a later aerial
survey (July, 1937) he also saw large concentrations of small fish, which he
believed to be pilchards, extending for about twenty miles in the vicinity of Port
Stephens, New South Wales, and at various points in the area bounded by Coff’s
Harbour on the south and Cakora Point on the north. These shoals were from
two to eight miles from the coast.
As Thompson states (1939), the outcome to date of this aerial work, which
has now been proceeding on and off for two years, is that the general distribution
of some of the more prolific pelagic fishes such as the tunny, salmon, pilchard and
related species, has been distinguished, and valuable guidance, at least in the
preliminary stages, has been given to the movements of the research vessel, which
has by her catches confirmed the evidence obtained from the aerial reconnaissance.
Naturally, the vessel will at times catch tunny which rise to the lure from deeper
water where they cannot be observed from the air, and to this extent the agree-
ment is imperfect, but it has led to the avoidance of much fruitless cruising of
the vessel.
In the ten months that the Commonwealth Research Vessel ‘“‘Warreen”’ has
been in commission it has been found possible to maintain touch with the chief
tunny shoals in the south-eastern area, from the first onshore manifestation in the
Jervis Bay—Eden sector (October-December) to the later appearances (January—
May) in Tasmanian and South Australian waters. Blue-fin tunny chiefly, and to a
lesser extent striped tunny and long-finned tunny (albacore), have been found to
occur in what appear to be sufficient quantity to support a fishery—subject to the
development of satisfactory means of capture.
An important commercial species, the yellow-fin tunny, has been located in
Queensland waters, but its distribution and numbers remain to be determined.
It is here, perhaps, that a warning should be issued. If great shoals of a
valuable species of edible fish are located at a certain season of the year, it must
not at once be assumed that their commercial exploitation is warranted, for subse-
quent investigations may reveal that during the following season they may not
appear in that region at all; they may, owing to certain physical and biological
conditions, have moved to other grounds. For this reason, therefore, an investiga-
tion must extend over a period of at least three years before the regular seasonal
appearance of the fish can be assumed with any degree of confidence, and then, as
Dr. Thompson points out, if a certain species, of good quality, can be shown to occur
in great numbers with a good average size and growth-rate, and if this species is
xxvi PRESIDENTIAL ADDRESS.
present with a high measure of reliability over a period of several years, there is
little danger in stating that a reliable and enduring fishery can be based on it—
that is, if it can also be shown that it can be caught with a fair measure of ease,
and if safe harbours exist nearby.
The programme of the Commonwealth investigations, therefore, includes
continuous investigations of pelagic fishes for at least three years in the south-
eastern area; these embrace the study of the regions of their occurrence, move-
ments, biological features such as growth-rate, food, age and size at first maturity,
migrations, influence of hydrographic and plankton conditions, and the systematic
relationship of species, especially the tunnies, to similar types abroad. Chemical
studies are also being undertaken to determine the value of certain species for the
production of fish meal, the fluctuations in chemical composition, and the best
seasons for such processes as canning and smoking.
The programme is a formidable one but, for the first time in the history of
Australia, adequate resources have been made available for the purpose, and we
may confidently expect that much light is about to penetrate the darkness that has
enveloped our fisheries for a period that has been unreasonably prolonged.
References.
DANNEVIG, H. C., 1913.—Notes on Australia’s Fisheries, with a Summary of the Results
Obtained by F.1.S. “Endeavour”. Published by the Commonwealth of Australia,
Dept. of Trade and Customs, 1913.
CoLEerax, A. N., 1934.—A Preliminary Investigation of the Natural History of the Tiger
Flathead (Neoplatycephalus macrodon) on the South-eastern Australian Coast. I.
Distribution and Supply; Length Statistics. Proc. LInn. Soc. N.S.W., Vol. lix, Parts
1-2, 1934.
, 1938.—A Preliminary Investigation of the Natural History of the Tiger Flat-
head (Neoplatycephalus macrodon) on the South-eastern Australian Coast. II.
Feeding Habits; Breeding Habits. Proc. LINN. Soc. N.S.W., Vol. lxiii, Parts 1-2, 1938.
DakIN, W. J., 1931.—Migrations and Productivity in the Sea. Pres. Address, Aust.
Zoologist, Vol. vii, Part 1, 1931.
, 1934.—Science and Sea Fisheries with Special Reference to Australia. Pap.
and Proc. Roy. Soc. Tasmania, 1934.
, 1937.—The Occurrence of the Australian Pilchard, Sardinops neopilchardus
(Steind.), and its Spawning Season in New South Wales Waters, Together with
Brief Notes on Other New South Wales Clupeids. Proc Linn. Soc. N.S.W., Vol. Lxii,
Parts 3-4, 1937.
, 1988.—The Habits and Life-history of a Penaeid Prawn (Penaeus plebejus
Hesse). Proc. Zool. Soc. London, Series A, Vol. 108, Part 2, 1938.
DAKIN, W. J., and Couprax, A. N., 1933.—The Marine Plankton of the Coastal Waters
of New South Wales. I. The Chief Planktonic Forms and their Seasonal Distribu-
tion. Proc. LINN. Soc. N.S.W., Vol. lviii, Parts 3-4, 1933.
, 1934.—The Eggs and Early Larval Stages of the Australian Pilchard—
Sardinia neopilchardus (Steind.). Rec. Aust. Mus., Vol. xix, No. 2, 1934.
, 1935.—Observations on the Seasonal Changes in Temperature, Salinity, Phos-
phates, and Nitrate Nitrogen and Oxygen of the Ocean Waters on the Continental
Shelf off New South Wales and the Relationship to Plankton Production. Proc.
LINN. Soo. N.S.W., Vol. Ix, Parts 5-6, 1935.
DAKIN, W. J., and KESTEVEN, G. L., 1938.—The Murray Cod (Maccullochella macquari-
ensis, Cuv. et Val.). Research Bulletin, No. 1, State Fisheries, N.S.W. Govt. Printer.
FOWLER, S., 1937.—Aerial Observations of Pelagic Fish. Departmental Report (unpub-
lished), Council for Scientific and Industrial Research, 1937.
ROuUGHLEY, T. C., 1926.—An Investigation of the Cause of an Oyster Mortality on the
George’s River, New South Wales, 1924-5. Proc. Linn. Soc. N.S.W., Vol. li, Part 4,
1926. :
, 1928.—The Dominant Species of Ostrea. Nature, Vol. 122, No. 3074, Sept. 29,
1928.
, 1933.—The Life History of the Australian Oyster (Ostrea commercialis). Proc.
LINN. Soc. N.S.W., Vol. lviii, Parts 3-4, 1933.
PRESIDENTIAL ADDRESS. XXVI1i
SAVILLE-KENT, W., 1890.—Notes on the Embryology of the Australian Rock Oyster
(Ostrea glémerata [commercialis]). Proc. Roy. Soc. Queensland, Vol. 7, Part 1,
1890.
TENISON-Woops, J. E., 18838. Fish and Fisheries of New South Wales. Sydney, Govern-
ment Printer. 1883.
THOMPSON, H., 1939.—The Investigation of the Fishery Resources of the Australian
Commonwealth. Paper read before meeting of the Aust. and N.Z. Assoc. for the
Advancement of Science, Canberra, Jan., 1939. (Published in Aust. Journ. Sci., i,
No. 5, 1939.)
WHITBLEGGE, T., 1890.—Report on the Worm Disease Affecting the Oysters on the Coast
of New South Wales. Rec. Aust. Mus., Vol. i, No. 2, 1890.
Dr. G. A. Waterhouse, Honorary Treasurer, presented the balance-sheets for
the year ended 28th February, 1939, duly signed by the Auditor, Mr. F. H.
Rayment, F.C.A. (Aust.); and he moved that they be received and adopted, which
was carried unanimously.
No nominations of other candidates having been received, the Chairman
declared the following elections for the ensuing session to be duly made:
President: Professor J. Macdonald Holmes, B.Sc., Ph.D.
Members of Council: C. Anderson, M.A., D.Sc., Professor HE. Ashby, D.Sc.,
Professor J. Macdonald Holmes, B.Sc., Ph.D., A. F. Basset Hull, M.B.E., T. C.
Roughley, B.Sc., F.R.Z.S., C. A. Sussmilch, F.G.S., E. Le G. Troughton, C.M.Z.S.
Auditor: F. H. Rayment, F.C.A. (Aust.).
A cordial vote of thanks to the retiring President was carried by acclamation.
XXVili
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ABSTRACT OF PROCEEDINGS. XXxXi
ABSTRACT OF PROCEEDINGS.
ORDINARY MONTHLY MEETING.
29th Marcu, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
The Donations and Exchanges received since the previous Monthly Meeting
(30th November, 1938), amounting to 53 Volumes, 504 Parts or Numbers, 29
Bulletins, 12 Reports and 27 Pamphlets, received from 178 Societies and Institu-
tions and 4 private donors, were laid upon the table.
PAPERS READ.
1. The Ecology of the Upper Williams River and Barrington Tops Districts.
iii. The Eucalypt Forests and General Discussion. By Lilian Fraser, D.Sc., and
Joyce W. Vickery, M.Sc.
2. Revision of Australian Lepidoptera. Oecophoridae. viii. By A. Jefferis
Turner, M.D., F.R.E.S.
ORDINARY MONTHLY MEETING.
26th Aprin, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
Miss Frances M. V. Hackney, Summer Hill, and Mr. G. F. K. Naylor, M.A.,
M.Sc., Dip.Ed., Sydney, were elected Ordinary Members of the Society.
The Chairman announced that the Council had elected Dr. W. L. Waterhouse,
Mr. C. A. Sussmilch, Mr. H. C. Andrews and Mr. T. C. Roughley to be Vice-
Presidents for the Session 1939-40.
The Chairman also announced that the Council had elected Dr. G. A.
Waterhouse to be Honorary Treasurer for the Session 1939-40.
The Donations and Exchanges received since the previous Monthly Meeting
(29th March, 1939), amounting to 17 Volumes, 126 Parts or Numbers, 6 Bulletins,
2 Reports and 40 Pamphlets, received from 71 Societies and Institutions and 2
private donors, were laid upon the table.
PAPERS READ.
1. A Key to the Marine Algae of New South Wales. ii. Melanophyceae
(Phaeophyceae). By Valerie May, B.Sc.
2. Miscellaneous Notes on Australian Diptera. v. On Eye-coloration and other
Notes. By G. H. Hardy.
3. Papuan Diptera. ii. Description of a New Genus and Two New Species
from Papua. Fam. Pyrgotidae (Diptera). By J. R. Malloch. (Communicated by
F. H. Taylor, F.R.E.S., F.Z.8.)
4. The Diptera of the Territory of New Guinea. Family Phytalmiidae. By
J. R. Malloch. (Communicated by F. H. Taylor, F.R.E.S., F.Z.8.)
5. The Diptera of the Territory of New Guinea. Family Otitidae (Ortalidae).
By J. R. Malloch. (Communicated by F. H. Taylor, F.R.EWS., F.Z.8.)
XXXil ABSTRACT OF PROCEEDINGS.
6. The Diptera of the Territory of New Guinea. Dolichopodidae. By l’abbé
O. Parent. (Communicated by F. H. Taylor, F.R.E.S., F.Z.8.)
7. Trombidiid Larvae in New Guinea (Acarina: Trombidiidae). By Carl
E. M. Gunther, M.B., B.S., D.T.M. (Communicated by F. H. Taylor, F.R.ES.,
F.Z.8.)
8. Taxonomic Notes on the Order Embioptera. i. The Genotype of
Oligotoma Westwood. By Consett Davis, M.Sc.
NOTES AND EXHIBITS.
Miss J. W. Vickery exhibited a specimen of Trianthema portulacastrum L.
recently received by the National Herbarium from Mr. W. W. Hardy of Narrabri,
who stated that it is exhibiting a vigorous growth in several places in the town.
This species has not previously been recorded in New South Wales, though it has
been known since about 1917 in Queensland, where it bears the vernacular name
of “Giant Pig Weed’. It is a common weed of cultivation, roadsides and waste
places in tropical regions, such as in the Philippines, Java, India, the West Indies,
tropical America and subtropical United States.
In 1917 it had already become a troublesome weed of cultivation at Bowen in
Queensland, but it is less likely to be a serious nuisance in New South Wales than
it is further north. As stock are said to be fond of it, it may have some value as a
fodder plant in pastoral districts.
Mr. E. Cheel exhibited fresh flowering specimens of Dahlia raised by Mr. W.
Sharland of Malvern, Victoria, from seed obtained from cultivated Dahlias “single
crimson-red” crossed with a ‘‘semi double yellow”. The new variety raised by Mr.
Sharland differs from the commonly cultivated forms in being of an “evergreen
perennial duration” whereas the ordinary cultivated varieties are cut down by
frosts in winter and new growth is obtained from the tubers in spring. The well-
known “Tree Dahlias” (Dahlia imperialis and Dahlia excelsa) also die down in
winter and commence new growth in summer from a perennial root-stock. Mr.
Sharland has raised the question of certain hereditary factors being dormant for
a long period and now transmitted to the new variety called “Sharlandia”.
Although the Dahlia was first mentioned by Hernandes in 1651 and by Cervantes
in 1789, it was not properly described until 1805, when Cavanilles prepared a
formal description from plants cultivated in Madrid. Since that time formal
descriptions have been published for D. coccinea, D. variabilis and D. frustranea,
which are probably the parents of the cultivated varieties of Dahlia. More recently
two species, viz., D. Popenovii and D. Maxonii, have been collected in Guatemala.
The two latter are said to be “Tree Dahlias”. Photographic illustrations were
also exhibited on behalf of Mr. Sharland.
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One 4
THE ECOLOGY OF THE UPPER WILLIAMS RIVER AND BARRINGTON TOPS
DISTRICTS. III.
THE EUCALYPT FORESTS, AND GENERAL DISCUSSION.
By Linran Fraser, D.Sc., and Joyce W. Vickery, M.Sc.
(Plates i-iii.)
[Read 29th March, 1939.]
THE HUCALYPT ForREstTS: Structure and Composition; Conclusions.
GENERAL DISCUSSION. GENERAL SUMMARY.
The rain-forests of the Williams River and associated valley systems have
been described in a previous paper (Fraser and Vickery, 1938). These forests
occupy sheltered and moist areas in the valleys and on the slopes above 900 feet
altitude. The surrounding country is occupied by a more open type of forest in
which species of the genus Hucalyptus predominate. This forest forms part of the
Kucalypt-forest formation which occurs throughout the coast and adjacent high-
lands of New South Wales. It extends from the valley floors bordering and below
the sub-tropical rain-forest, along the crests and upper parts of spurs and ridges
to the Barrington Tops Plateau. It comprises a number of well marked, altitude-
delimited communities which grade into each other so that the forest forms a
continuous whole. These communities have been grouped, according to their
occurrence, into associations which are interpreted as local expressions of large
associations widely distributed elsewhere. Hach community will be described
separately.
The general structure of the forest is similar throughout. Three main strata
can be distinguished: (a) Tree, (b) Shrub, and (c) Ground Flora. The tree
stratum may be considered to consist of two parts, viz., trees whose foliage forms
the canopy, and smaller trees, 30-35 feet in height, which do not reach the canopy.
The leaves of the tall trees are leathery, and all of the same form, narrow
lanceolate-faleate. As in most species of Hucalyptus, the leaves hang almost
vertically, so that, though the canopy is more or less continuous, a considerable
amount of sunlight reaches the ground.
The tallest forest occurs in the valley floor, and there is a continuous gradation
between this and the plateau forest, which is comparatively stunted. The taller
trees range from 120 to 180 feet in height, those on the plateau from 30 to 60 feet.
The smaller trees are rarely present in sufficient numbers to give a distinctive
appearance to the forest, and they never form a continuous stratum. Usually they
are far less frequent than the tall trees, but in places on certain slopes may become
important. The ground flora forms a more or less continuous stratum in all the
communities. It comprises mostly hemicryptophytes and chamaephytes with some
geophytes and therophytes. Grasses are conspicuous, becoming more so with
increasing altitude. Between the tree and herb or ground strata is the shrub
stratum which may be important and continuous, sparse, or even entirely absent
Cc
2 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS. III,
over large areas. As in the tree stratum it is possible to distinguish two sections:
a tall-shrub layer, attaining a height of 6 to 12 feet, in places forming dense
communities, but usually very discontinuous in all associations, and a low-shrub
layer 1 to 6 feet in height, which also varies from very dense and continuous to
discontinuous and scanty. The members of the tall-shrub layer have moderately
large, but sclerophyllous types of leaves; those of the lower stratum have for the
most part very small, coriaceous, stiff leaves.
Lianes and epiphytic ferns and angiosperms, which are such a feature of the
sub-tropical rain-forest, are, with one exception, absent from the Eucalypt forest.
The exception is the epiphytic orchid Cymbidium suave, which grows almost
exclusively in the dead branch gaps of HEucalypts. It does not extend upwards
beyond an altitude of about 2,000 feet as far as could be observed. Occasionally
plants of Davallia pyxidata, Platycerium bifurcatum and Cyclophorus serpens may
be present on Casuarina torulosa and Trochocarpa laurina trees along the margins
of the sub-tropical rain-forest, but these are obviously intruders from the rain-
forest and do not form a natural part of the Hucalypt-forest associations.
Mosses and lichens are very uncommon in the lower parts of the Hucalypt
forest, but with increasing altitude their importance increases, especially as the
mist zone is approached. Above 4,000 feet any exposed rock surface is densely
covered with mosses and lichens. Even at these altitudes their development is
not so great in the Hucalypt forest as it is in the adjoining sub-antarctic rain-
forest, while nothing in the Hucalypt forest can compare with the development
of mosses in the most humid parts of the sub-tropical rain-forest. Mosses and
lichens are fewer in the plateau forests, which, being more exposed to the drying
action of the westerly wind than the upper slopes of the ranges, are consequently
less humid.
THE HUCALYPT FORESTS.
Structure and Composition.
(a) The Forests of the Valley Floor.
1. The forest of the lower valley, below 900 feet.
The boundary of the Chichester State Forest cuts at right angles across the
valley of the Williams River at the lower limit of the sub-tropical rain-forest at
an altitude of about 900 feet. Practically all the EHucalypt forest south of this,
both in the valley floor and in the adjacent spurs, has been cleared for pastoral
purposes. Little remains of the original flora except scattered trees which have
been left for shade. A detailed study of this part of the forest has not been
attempted. Hucalyptus tereticornis, Casuarina torulosa and Angophora subvelutina
are the most important trees, but Hucalyptus maculata and EF. hemiphloia are
dominants over large areas, becoming of greater importance further from the rain-
forest, at comparatively low altitudes. Species which are widely distributed but
not as a rule very numerous are EH. paniculata and EH. eugenioides. EH. saligna and
Syncarpia laurifolia occur in restricted areas of specially good soil-moisture. They
may be regarded as outliers of the main H. saligna-S. laurifolia forest which occurs
at an altitude of 1,000 to 1,200 feet.
On the flats by the river Angophora subvelutina is most common, occasionally
attaining a height of more than 100 feet. Melaleuca linariifolia, a small tree not
exceeding 30 feet, is present in dense communities in damp places in the flat valley-
floor. Casuarina Cunninghamiana and Callistemon viminalis form a narrow fringe
along the river bank mingling with species intrusive from the rain-forest, e.g.,
Tristania laurina and Hugenia spp. Angophora subvelutina extends part of the
oN)
BY LILIAN FRASER AND JOYCE VICKERY.
way up the east-facing slopes of the enclosing mountain ranges, but is absent from
the drier parts and from the west-facing slopes. Another tree of importance on the
river flats is Eucalyptus amplifolia.
The pasture is composed largely of native grasses, of which Hragrostis
leptostachya, Sporobolus indicus, Microlaena stipoides, Bothriochloa decipiens,
Panicum effusum, Entolasia marginata, Themeda australis, Echinopogon
caespitosus, Agrostis avenacea, Danthonia penicillata, Cynodon dactylon and
Poa caespitosa are most prominent. Occasional large patches of Imperata cylindrica
var. Koenigii, which is harsh and useless for grazing, and the bracken fern
Pteridium aquilinum detract from the value of the pastures. Some Paspalum
dilatatum is present on the river flats, and Paspalum distichum in very moist places.
On these river flats large, ungrazed clumps of Carex longifolia are sometimes
present, a relic of the original vegetation which has spread under the new
conditions. EHphemerals such as Aira caespitosa, Wahlenbergia gracilis,
Gnaphalium japonicum, Siegesbeckia orientalis, Stellaria flaccida and Swainsona
coronillifolia are common in the more disturbed areas. Notholaena Brownii and
Pteris paradoxa (which are the only ferns except Pteridium aquilinum), Lomandra
longifolia, Ranunculus lappaceus and the common trailing Hibbertia volubilis are
present and appear to have formed part of the original vegetation.
2. The forest of the valley floor at 900 to 1,400 feet.
The sub-tropical rain-forest at its lower limit occupies a relatively narrow area
each side of the river. The remainder of the valley floor and the sheltered lower
slopes of the adjacent mountain ranges are occupied by an association in which
Hucalyptus saligna and Syncarpia laurifolia are dominants. These species are
also present throughout the sub-tropical rain-forest (see Fraser and Vickery, 1938).
The valley floor narrows rather rapidly above the State Forest boundary, and after
about one-half mile from the boundary is occupied entirely by rain-forest, so that
the Hucalypt forest is restricted to the slopes of the spurs. An approximately
complete list of species present in this part of the formation is given in Table 1,
column 1. It can be seen that the numbers of herbs and low shrubs are greatly in
excess of the numbers of tall shrubs and trees.
The density of the forest varies considerably from place to place. On dry
westerly-ftacing slopes the trees are somewhat shorter, and are slightly less
numerous than on the more sheltered slopes and on the valley floor. On an
easterly-facing slope of the Williams Range, the average density of the trees in
the Hucalyptus saligna forest was observed to be 4 per 1,000 square feet.
The Hucalyptus saligna—Syncarpia laurifolia association extends upwards to
an altitude varying with the exposure of the slope. On dry, westerly-facing slopes,
the upper margin is only about 200 feet above the valley floor, i.e., at an altitude
of 1,200 feet. Along sheltered gullies, especially in the easterly-facing slopes, the
association may extend upward to about 2,500 feet, and scattered members of it to
3,000 feet. The tree stratum forms a continuous canopy (PI. i, figs. 1, 3). Because
of this, and because of the physiographic position in which the forest is developed,
less light reaches the forest floor here than on the ridges and upper slopes.
Hucalyptus saligna occurs throughout the association and forms pure
communities on westerly-facing spurs or sunny, dry, upper parts of northerly-
facing slopes. The necessary requirements for the growth of H. saligna appear
to be a deep, good, rather heavy soil, and abundant moisture. Its light require-
ments are not restricted. It is able to develop satisfactorily in areas of maximum
light intensity, but is also capable of equally good development under conditions [yy
of shade which are unsatisfactory for most other species of Hucalyptus. Was Walrus ys*
So
aN
& : Ae
aol ie
Fae \ =
4 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS. III,
Syncarpia laurifolia is found fairly frequently throughout the lower forest
association, but does not extend so far beyond its edge as Hucalyptus saligna,
particularly on sunny slopes. It is fairly abundant on the valley floor and on
moist parts of westerly-facing slopes, but the lower parts of northerly- and
southerly-tacing slopes which receive least light do not appear to be particularly
well suited for its growth, and it may be absent entirely from large areas occupied
by Eucalyptus saligna.
Hucalyptus amplifolia is found only along the lower edges where the £. saligna-—
Syncarpia lauwrifolia association abuts on the association of the lower valley, of
which EH. amplifolia is a subordinate species. H. acmenioides occurs near the border
of the adjoining forest association of which it is a subordinate species, on sheltered
but fairly dry slopes.
The height of the Hucalyptus saligna and Syncarpia laurifolia trees ranges
from 180 feet in the valley floor to 100 feet on the upper parts of the slopes. The
diameter of mature specimens on the valley floor may commonly reach 6 feet.
The small-tree stratum is very discontinuous, the only species being Callistemon
salignus, Casuarina torulosa and Acacia spp. Callistemon salignus forms local,
dense communities in damp areas. Casuarina torulosa appears to prefer cool slopes,
and is often abundant on the north, north-west and south-east sides of ridges. The
transition from Eucalypt forest from which it is absent to forest in which it is
present is often very marked. Acacia spp. are scanty except after fire, when they
form dense thickets (see Fraser and Vickery, 1938).
The tall-shrub stratum is absent (Pl. i, figs. 2, 3). The small-shrub stratum
is discontinuous, scanty and not widespread. It occurs over small areas in shaded
localities only.
The nature of the ground flora varies considerably with aspect. The floor of
the valley, which is shaded for a considerable part of the day, is relatively moist
at all times and supports the following species: Brunella vulgaris, Gratiola
peruviand, Mentha gracilis, Plectranthus parviflorus, Veronica plebeja, Hranthemum
variabile, Hydrocotyle geraniifolia, and a number of grasses, notably Microlaena
stipoides, Poa caespitosa and Panicum pygmaeum.
The slopes afford several different types of habitats. The sheltered slope near
to the creek or valley just above the rain-forest is usually cool and humid. Here
Culcita dubia torms almost a pure ground community (PI. ii, fig. 10). Other
important species are Blechnum cartilagineum, Microlaena stipoides, Themeda
australis, Poa caespitosa, Pterostylis spp. and Viola spp.
Other slopes which may be sheltered and shaded by virtue of their position
on the spurs on the protected sides of ranges are relatively much drier than the
valley areas on account of their steepness. These support a less dense ftora. The
most common species here is Imperata cylindrica var. Koenigii, which in places
forms an almost pure community (PI. i, fig. 2). Other species are Desmodium spp.,
Entolasia marginata, Vernonia cinerea, Lagenophora Billardieri and Hibbertia
volubilis.
Pockets or flat areas on such slopes, where moisture collects, show the develop-
ment of a greater amount of grass and finally of ferns. The most rigorous type of
habitat of this association occurs on westerly-facing, well-drained spurs. These
are comparatively dry and sunny (PI. i, fig. 2). Imperata cylindrica var. Koenigii
is the dominant species in the ground flora, forming very dense stands; other
species are Botrychium australe, Pteridium aquilinum and Hibbertia volubilis.
In addition to the typical Eucalypt-forest species, a number of species occur
around the edge of the rain-forest which are intrusive from it. Of these the tree-
BY LILIAN FRASER AND JOYCE VICKERY. 5
fern Alsophila australis is one of the most conspicuous, forming communities in
advance of the rain-forest in sheltered localities (Pl. ix, fig. 19, in Fraser and
Vickery, 1938), associated with Culcita dubia.
(bo) The Forests of the Valley Sides at 1,400-3,000 feet.
At about 1,200 feet on dry slopes and 1,500 feet on sheltered slopes, the
Hucalyptus saligna—Syncarpia laurifolia forest grades into a forest in which
EH. campanulata, E. punctata and E. acmenioides occur. The gradation takes place
over a vertical range of about 300 feet or more because of the variability in the
range of EH. saligna. An approximately complete list of the species occurring in
this part of the forest is given in Table 1, column 2.
This part of the forest is dominated by Hucalyptus campanulata and HE.
punctata. It is of considerable extent, occupying the crests and upper slopes of
the lower ranges and extending upwards to an altitude of 3,000 feet. It occupies
soil derived at the lower levels from mudstone, and at the upper levels from
basalt, but, as far as could be seen, the change of soil type exerted little or no
influence on the flora over this area.
The composition of the forest varies from place to place, largely as the result
of aspect.
Eucalyptus acmenioides is confined to the lower sheltered parts of slopes,
particuiarly easterly-facing slopes, where it merges into the EH. saligna association
(Pl. i, fig. 4). In places it forms almost a pure community, but at higher altitudes
it is associated with HL. campanulata (Pl. i, fig. 5). It appears to have higher soil-
moisture requirements than H. campanulata. E. Wilkinsoniana also occupies the
lower slopes (PI. i, fig. 5), but is confined to areas of high soil-moisture as well as
shelter. On sunny, dry, westerly-facing slopes H. acmenioides may be lacking or
very scanty, and the #. saligna association grades almost directly into the
EH. campanulata—E. punctata association.
E. campanulata is the most abundant species, and is found throughout the
association, particularly on westerly-facing or upper slopes (PI. i, fig. 8), where
it occurs in an almost pure state. It does not grow at low altitudes on shaded
slopes, but comes down to 1,200 feet on westerly-facing slopes, which are light
and well-drained. It is not found around moist, sheltered, shady gullies even as
high as 1,800 feet. H. punctata prefers sunny, fairly moist localities (PI. i, fig. 6).
It is common on ridges, especially on the Chichester Range (PI. i, fig. 7), but is
absent from the driest parts of the ridge tops (PI. i, fig. 8). It extends upwards
to an altitude of 2,000 feet only.
Of the smaller trees, Casuarina torulosa is the only species occurring in this
part of the forest. It is more abundant on sheltered northerly- and easterly-facing
hillsides in regions of relatively abundant moisture (PI. i, fig. 5), and is relatively
less important on southerly- and westerly-facing slopes. It does not extend upwards
beyond an altitude of about 2,000 feet.
The tree stratum forms a closed or nearly closed canopy. The height of the
trees varies from 120 feet on the lower slopes to 60 feet on the crests and flat tops
of ridges. The lateral spread of each tree may be considerable, especially on ridge
tops. The density is much the same as in the Eucalyptus saligna forest in the
same locality, averaging 4:12 trees per 1,000 square feet, and ranging from 1 to 6
per 1,000 square feet.
Above 2,000 feet the forest consists almost entirely of Eucalyptus campanulata,
until about 3,000 feet, where it gives place rather abruptly to the next type of
6 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS. III,
forest. The abruptness of this transition is much more marked than the transition
between the #. saligna and EL. campanulata forest types.
The tall-shrub stratum is very discontinuous and scanty. Acacia mollissima
forms local thickets, but these are not of wide extent and may have resulted from
burning. Persoonia linearis and Xanthorrhoea resinosa are present on sheltered
slopes.
The low-shrub stratum is also discontinuous and scanty, but is more abundant
than the tall-shrub stratum. It is best developed in regions of greatest light, such
as on the crests of spurs, where Leucopogon lanceolatus, Oxylobium trilobatum and
other shrubs may form local thickets. A few less xeromorphic species such as
Indigofera australis and Desmodium rhytidophyllum appear to be restricted to
shaded, humid slopes.
In the ground stratum Poa caespitosa and Lomandra longifolia are most
important at higher levels. Other grasses, including IJmperata cylindrica var.
Koenigii, Themeda australis and Microlaena stipoides, are dominant, especially at
lower levels. These form a continuous ground-cover which is rather thin, especially
on well-drained, shaded slopes. Moist areas support a denser cover, the more
common species being Desmodium spp., Viola spp., Podolepis acuminata and
Lagenophora Billardieri, in addition to the above-mentioned grasses. Culcita dubia
forms dense communities above the rain-forest margin in humid parts.
(c) The Forests of the Upper Spurs.
Below 3,000 feet zonation of the Hucalypt species is rather masked by the
differential effect of aspect on the various species, but above that level it is most
conspicuous. The forest consists of successive zones of different species. The
lowest zone is formed by #. obliqua, which occupies the crests and upper slopes of
the ranges approaching the plateau between 2,800 feet and 3,500 feet. The average
tree-height is about 80 feet and diameter 2 to 3 feet. The canopy is fairly thick
and continuous or nearly so. Because this forest type occurs mainly on the ridge
tops and upper slopes, a considerable amount of light reaches the ground stratum.
This region also, since it occurs at high altitudes, probably receives more rain
than the lower spurs and ranges. In addition the soil is derived from basalt and
has a high water-retaining capacity. These factors of high soil-moisture and
strong light intensity lead to an extensive development of the ground flora. This
is very dense, much more so than in the lower forests, the average height being
12 to 18 inches.
The transition from the Hucalyptus campanulata forest to the EH. obliqua forest
takes place over a vertical range of about 100 feet, and in this zone the two
species occur mingled together. The other tree species of the H#. campanulata
zone do not extend upwards to this altitude. H. saligna, however, which reaches
its Maximum development in the valley at 1,000 feet, extends upwards to the
#. obliqua zone along sheltered creek sides to 3,000 feet (PI. ii, fig. 10).
At about 3,500 feet H. obliqua gives place to EL. viminalis. The transition zone
is fairly wide, taking place over a vertical range of about 250 feet. In the greater
part of this zone the two species are present in about equal amounts (PI. i, fig. 11).
The trees are spaced to about the same degree as in the lower forest, and have an
average height of about 80 feet and a diameter of 2-2-5 feet. The canopy on the
whole is rather thinner than that of the H. obliqua forest, but is continuous or
nearly so.
The associated shrubs and herbs are similar in both the Hucalyptus viminalis
and the #. obliqua forests. A list of the most prominent species is given in Table 1,
BY LILIAN FRASER AND JOYCE VICKERY. U
column 8. Some of these are of special interest. Hakea eriantha, a diffuse shrub
attaining a height of about 10 feet, has a sporadic distribution between 3,000 and
3,500 feet. Acacia melanoxylon is common throughout both forests in regions of
specially high soil-moisture. It attains the dimensions of a small tree, 20 to 25
feet in height with a diameter of 10 inches. This species occurs in the valley
below the sub-tropical rain-forest at 800 to 900 feet, chiefly along river banks, but
it is absent from the lower Hucalypt associations. Acacia floribunda has a very
limited vertical range, forming thickets at about 3,000 feet. Banksia integrifolia,
growing to a tree 30 to 35 feet high, is a conspicuous member of both forests
(Pl. ii, fig. 12). It reaches its maximum development in the Hucalyptus viminalis
forest, but extends upwards beyond its limits, and in places also downwards as far
as the EH. campanulata forest.
The low shrubs, of which Leucopogon lanceolatus is the most common, are
scanty, forming occasional communities. Senecio amygdalifolius, S. dryadeus and
Olearia Nernstii, forming shrubs up to 5 feet in height, are locally common. The
ground flora is very dense and continuous. Poa caespitosa and Lomandra longifolia
are .o-dominants. Scattered throughout this community are single plants and
small groups of WHibbertia volubilis, Dianella coerulea, Scutellaria humilis,
Plectranthus parviflorus, Festuca Hookeriana (?), Pteridium aquilinum and
Helichrysum lucidum. These are specially common on moist slopes where the soil
is rather shallow and continual seepage of water takes place; in addition, Ajuga
australis, Crassula Sieberiana, Luzula campestris, the ferns Asplenium flabelli-
folium, Pleopeltis diversifolia, Polystichum aculeatum, and the trailing Angiosperms
Tecoma australis, Rubus parvifolius and Smilax australis are frequent.
The large number of ferns in the Eucalyptus obliqua—E. viminalis forests can
be related to the very moist conditions prevailing there, this region being within
the mist belt. Above this, though the conditions are no less moist, the ferns are
less frequent, probably because of the colder temperatures. The moist conditions
are reflected in the large number of mosses present on exposed rock surfaces and
the lower parts of tree trunks.
(d@) The Hucalyptus fastigata Forest.
At an altitude of 4,200—4,500 feet there is a considerable area to the south-east,
east and north-east of the highest part of the plateau occupied by a distinctive
forest in which Hucalyptus fastigata is dominant. EH. viminalis is present as a sub-
dominant species in the lower part of this forest, but does not extend upwards
above 4,300 feet. This region is fairly flat for the most part, constituting the tops
of the ridges diverging from the plateau whose sides are occupied by sub-antarctic
rain-forest and by the #. obliqua—E. viminalis forests. The soil is particularly
moist and the whole habitat distinctly more sheltered and less cold than the actual
plateau. It is chiefly this forest area which is being invaded by the beech forest
(see Fraser and Vickery, 1938) (PI. ii, fig. 14). The transition between it and the
E. viminalis forest is not abrupt, considerable mixing taking place in the ecotone
region. On slopes or areas exposed to the action of the westerly wind this forest
type is replaced by communities of Hucalyptus paucifiora invading from the plateau
forest.
The trees of the H. fastigata forest average 60 to 80 feet in height and have a
diameter of 2 to 3 feet (Pl. ii, fig. 13). The canopy is nearly closed but not dense.
The ground flora is particularly well developed. The important component species
are shown in Table 1, column 4. The low-shrub communities are rather more
common and better developed than in the lower forests, forming mixed or pure
8 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS. ITI,
communities over considerable areas. The individual plants are often evenly
scattered. The tree-fern Dicksonia antarctica is common in damp areas, together
with Polystichum aculeatum and such herbs as Stellaria flaccida and Veronica
calycina. The herb stratum is dense and continuous. Poa caespitosa is perhaps
slightly more abundant than Lomandra longifolia over most of the area. The
bracken fern Pteridium aquilinum is fairly widely distributed, but does not form
dense stands here. The only small tree is Banksia integrifolia, which is wide-
spread and fairly abundant.
Tall shrubs, such as occur in the lower forests, are absent, and their place
is taken by a shrub stratum 5 to 8 feet high comprising species which do not
occur at lower altitudes, such as Gaultheria appressa, Drimys purpurascens, and
Olearia spp., which in places form dense thickets. Acacia melanoxylon, Tieghemo-
panax sambucifolius and Lomatia arborescens are also part of this layer. The
species of this stratum are marked off very distinctly from those of the low-shrub
stratum by their larger size and larger leaves. The low-shrub communities are
rather more common and better developed than in the lower forests, forming mixed
or pure communities of large extent. The component species are small, woody
perennials with stiff, small leaves, and rarely exceed 2 feet in height. Lewcopogon
Hookeri and Omphacomeria acerba are amongst the most important.
(e) The Vegetation of the Plateau.
1. The Eucalypt forest.
The plateau region at an altitude of 4,500 to 5,000 feet is exposed to consider-
able wind action, and is the only area in this region where snow lies for more
than a few days at a time. At 4,500 feet the H. fastigata forest gives place to the
typical forest of the Barrington Tops Plateau, in which E. pauciflora is the
dominant species. On northerly, fairly sheltered slopes this species may attain a
height of 60 feet and a diameter of 2 feet (PI. ii, fig. 16). It becomes smaller with
increasing exposure, and at 5,000 feet rarely exceeds 40 feet in height (PI. ii,
fig. 15). It is commonly rather gnarled and twisted. Possibly owing to the action
of wind and snow and also to the rather brittle nature of the branches, fallen trees
and broken limbs are a conspicuous feature of this forest community (PI. ii, figs. 14,
16, 17), and are the more striking because of their absence or rarity in the lower
forests.
The canopy is nearly continuous but very thin, and a considerable amount of
light reaches the ground stratum. Hucalyptus stellulata, the only other tree occur-
ring in this forest, is not a prominent species. It is most commonly found near
water, and forms a community along creek banks and swamp margins.
The species found in this forest are shown in Table 1, column 5. The shrub
strata reach their best development on the eastern and northern slopes of the hills.
There are two strata, similar to those of the H. fastigata forest. The tall-shrub
stratum includes such species as Acacia dealbata,
Species.
Oxylobium ellipticum R.Br. var.
alpinum Maide . & Betche
trilobatum Benth.
Pultenaea fasciculata Benth.
Sphaerolobium vimineum Sm.
Trifolium repens L.
Zornia diphylla Pers.
Geraniaceae.
Geranium pilosum Forst. ..
Rutaceae.
Phebalium squamulosum Vent.
Polygalaceae.
Comesperma sylvestre Lindl.
Euphorbiaceae.
Breynia oblongifolia J.Muell.
Poranthera microphylla Brongn. ..
Celastraceae.
Celasirus Cunninghamii F.v.M.
Dilleniaceae.
Hibbertia dentata R.Br.
volubilis Andr.
Guttiferae.
Hypericum japonicum Thunb.
Violaceae.
Hymenanthera dentata R.Br.
Viola betonicifolia Sm.
hederacea Labill.
Thymeliaceae.
Pimelea ligustrina Labill. ..
linifolia Sm.
Myrtaceae.
Angophora subvelutina F.v.M.
Baeckea Gunniana
latifolia Benth.
Callistemon pallidus DC.
salignus DC. 8 ae
Eucalyptus acmenioides Schau.
amplifolia Naudin
campanulata R.T.Baker
fastigata Deane & Maiden
obliqua L’ Hér.
pauciflora Sieb.
punctata DC.
saligna Sm.
stellulata Sieb.
viminalis Labill. . . Ee
Wilkinsoniana R.T.Baker
Leptospermum flavescens Sm.
myrtifolium Sieb.. .
Myrtus Beckleri F.v.M.
Syncarpia laurifolia Ten. ..
Tristania laurina R.Br.
Oenotheraceae.
Epilobium glabellum G.Forst.
Halorrhagaceae.
Halorrhagis micrantha R.Br.
tetragyna Hook. f.
teucrioides P. DC. ng
Myriophyllum pedunculatum Hook. f.
Schau. var.
Life
Form. 1
N
N
Ch (W)
Ch
H
Ch Ss
Th R
N
N
N SS)
Ch-Th Ss
N S
Ch-N Ss
Ch-N Ss
Th N)
N
H N)
H-Ch F
N
N
MM NS)
N
M
M LC
MM Ss
MM SS)
MM
MM
MM
M
MM
MM Cc
M
MM
MM R
N
N
N bs)
MM F
N-M LC
H-Ch
Th
Ch NS)
Ch
HH
LC
ym
LC
Qn
LC
5 6
s
LC LC
S) SS)
R
s
R
F S)
SS) s
S) tS)
NS)
Fr LC
FE
SS)
VC
LC
Fr
s S)
T!
LC
LC
LC
LC
30 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS.
Species.
Araliaceae.
Astrotricha floccosa DC. ‘
Tieghemopanax sambucifolius
R.Viguier Sie
Umbelliferae.
Apium leptophyllum F.v.M.
Daucus brachiatus Sieb.
Hydrocotyle geranifolia F.v.M.
hirta R.Br. of
Oreomyrrhis andicola Endl.
Ericaceae.
Gaultheria appressa A.W.Hill
Epacridaceae.
Epacris microphylla R.Br. var.
rhombifolia Fraser & Vickery
breviflora Stapf. 3
Leucopogon collinus R.Br...
Hookeri Sond.
lanceolatus R.Br...
Myrsinaceae.
Rapanea variabilis Mez.
Primulaceae.
Iysimachia japonica Thunb.
Oleaceae.
Notelaea venosa F.v.M.
Loganiaceae.
Mitrasacme serpyllifolia R.Br.
Gentianaceae.
Gentiana diemensis Griseb. var.
Convolvulaceae.
Dichondra repens R. & G.Forst.
Borraginaceae.
Myosotis australis R.Br.
Labiatae.
Ajuga australis R.Br.
Brunella vulgaris DC.
Mentha gracilis R.Br.
Plectranthus parviflorus Henck.
Scutellaria humilis R.Br.
Prostanthera lasianthos Labill.
Scrophulariaceae.
Euphrasia Brownii F.v.M. var.
Gratiola peruviana L.
Veronica calycina R.Br.
plebeja R.Br.
Bignoniaceae.
Tecoma australis R.Br.
Lentibulariaceae.
Utricularia dichotoma Labill.
Acanthaceae.
Eranthemum variabile R.Br.
Plantaginaceae.
Plantago palustris Fraser & Vickery
varia R.Br.
Rubiaceae.
Asperula conferta Hook. f.
Coprosma Billardieri Hook. f.
hirtella Labill.
Galium australe DC.
TABLE 1,—Continued.
Form.
He m A
zag
ANN
LC
LC
LC
nn
LC
LC
LC
LC
LC
LC
LC
LC
Ill,
6 7
Ss ibe
LC
LC
LC
TC
c
F Ss
Giace
F LC
s C
G
1610
s iy
LC
BY LILIAN FRASER AND JOYCE VICKERY. 31
TABLE 1.—Continued.
Species.
Campanulaceae.
Lobelia gibbosa Labill.
pedunculata R.Br. Ae
Wahlenbergia gracilis A. DC.
Goodeniaceae.
Goodenia hederacea Sm.
Scaevola Hookerit F.v.M.
microcarpa Cav.
Velleia montana Hook. f.
Candolleaceae.
Candollea serrulata Labill.
Compositae.
Centipeda orbicularis Lour.
Cotula australis Hook. f.
filicula Thunb.
Craspedia Richea Cass.
Erechtites arguita DC.
Erigeron pappochromus Labill.
Gnaphalium japonicum Thunb.
Helichrysum lucidum Henck.
elatum A.Cunn.
ferrugineum Less.
scorpoides Labill.
Lagenophora Billardieri Cass.
emphysopus Hook. f.
Olearia chrysophylla Benth.
Nernstii F.v.M. ..
stellulata DC.
Picris hieracioides L.
Podolepis acuminata R.Br.
Senecio amygdalifolius F.v.M.
dryadeus Sieb.
Stegesbeckia orientalis L. ..
Vernonia cinerea Less.
LC
fo)
i=
nm
ney
N R R LC
N LC
TABLE 2.
4 5 6 7
F F F F
Ss) F FE
EF LC LC
Fr
Cc VC C
SS)
iS) R
LC Cc Cc
R
LC Ss
SS) LC LC
LC Cc
s
F
S iS) LC
F LC
LC
LC rs)
LC LC
LC LC
iS)
Species Common to the Sub-alpine Forest or Grassland and the Swamps.
Acacia Clunies-Rossiae.
Ajuga australis.
Asperula conferta
Cardamine hirsuta var.
folia.
Deyeuxia breviglumis.
Diuris venosa.
Epilobium glabellum.
Erigeron pappochromus.
Euphrasia Brownii var.
Geranium pilosum.
tenui-
Halorrhagis micrantha.
Hydrocotyle hirta.
Hypolaena lateriflora.
Lagenophora Billardiert.
Lobelia pedunculata.
Microtis parviflorus.
Microtis porrifolius.
Mitrasacme serpyllifolia.
Oreomyrrhis andicola.
Plantago varia.
Poa caespitosa.
Prasophyllum brevilabre.
Prasophyllum odoratum.
Ranunculus lappaceus.
Scaevola Hookeri.
Schoenus apogon.
Schoenus ericetorum.
Scirpus setaceus.
Scleranthus biflorus.
Thelymitra ixioides.
Viola hederacea.
32 ECOLOGY OF UPPER WILLIAMS RIVER AND BARRINGTON TOPS DISTRICTS. III,
TABLE 3.
Distribution of the Sub-alpine and Montane Species.
3 : a a = ai
s ; Z eee ae
5 2 E 58 Eee) os
Species. = 8 3 488 o Sita Beis
; g iS 64.) Bia esheets eis
a > ae na a Oa Aa
Adenochilus Nortoni .. oe x x
Atherosperma moschatum x x Xs x
Baeckea Gunniana var. latifolia x x x %
Blechnum penna-marina x x De x x x
Bossiaea neo-anglica aK: x x
Callistemon pallidus x x x X Bg x
Carex cernua var. lobolepis x >.¢
Chiloglottis Gunnii x X x x
Claytonia australasica. . Xs x x x x x
Comesperma sylvestre x X:
Coprosma Billardieri .. X: x x x xe X
hirtella ae ei ae b.¢ x i. x x x x
Cotula filicula ae ae axe X: x x x
Deyeuxia breviglumis . . So ae x x x x
Diuris venosa .. x
Drimys lanceolata xe x: x x x: x
purpurascens 5 x
Elaeocarpus holopetalus x x eX: xe xe xe
Epacris breviflora <2 sie xx x x x x x
microphylla var. rhombifolia x x
Erigeron pappochromus 6 x. x x
Exocarpus nana 4 x x x
Festuca Hookeriana (?) x xe x x
Gaultheria appressa xx x x x
Gentiana diemensis B:¢ > X
(form)
Hakea microcarpa x X x x xX x X:
Helichrysum ferrugineum x ™ x x x
Hierochloa redolens x x x x
Juncus faleatus X: x x x
Lagenophora emphysopus x x X X X:
Leptospermum myrtifolium x xe xe xe X
Leucopogon collinus x x x X: x
Hookeri are aie Xs Se x x Ss x
Libertia pulchella 5a tne _ Xx: X x x
Lycopodium clavatum var. fastigiatum °K X: x x
Mitrasacme serpyllifolia x x x x x
Myriophyllum pedunculatum x x x Xs x
Olearia chrysophylla x >
stellulata x x x x
Oreomyrrhis andicola Au xe xe xe >.¢ x x x
Oxylobium ellipticum var. alpinum .. x > x x
Persoonia oxycoccoides Xi: x x xe
Plantago palustris x
Prasophyllum Rogersit x
Pultenaea fasciculata Se x D6 x
Restio australis x x x xe x
Scaevola Hookeri xe x Xe x xe x x
Scleranthus biflorus x x xe x x x x
Uncinia riparia x x x x
Velleia montana x x ae ve xe
PLATE I.
Soc. N.S.W., 1939.
Proc. LINN.
of Williams River and Barrington Tops District.
Ecology
7 at
leh eae
. Zp 7
Wc
2) > TINY CQ 1 | IS 7 @)
Proc. Linn. Soc. N.S.W., 1939. PLATE It.
Ecology of Williams River and Barrington Tops District.
ne
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Proc. Linn. Soc. N.S.W., 1939. PLATE III.
33
BY LILIAN FRASER AND JOYCE VICKERY.
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34
MISCELLANEOUS NOTES ON AUSTRALIAN DIPTERA. V.
ON EYE-COLORATION, AND OTHER NOTES.
By G. H. Harpy.
(One Text-figure. )
[Read 26th April, 1939.]
A theory of the Eye-marking.—David Sharp (Cambridge Natural History, vi,
part 2, 1899, p. 440), referring to eye marks on living flies, states that it is uncertain
what use the variegated eye-coloration may have; subsequent authors seem to
have limited their interests, in print, to the needs of taxonomy, and they figure
markings more effectively than they describe them. There does not seem to be
any plan upon which a uniform system of descriptions can be based. Enough,
however, has been published to indicate that eye-marking is a phenomenon in
the evolutionary process of the insect.
Probably the primitive eye-colour is black; this is common in the Nematocera,
but limited to the lowest section in the Brachycera, where black is rarely found.
The first advance is indicated by the possession of red eyes, a common feature
throughout the Brachycera, with other hues, which may partly or completely
cover the eye. The variegated colour pattern so frequently found seems always
to be based on a red eye, and is never found on the primitive black eye.
The most advanced eye is normally green, rarely yellow, blue, or some other
colour, and it is the change from the red to green that is considered here.
The change takes place in two ways. In some cases the green invades the
red uniformly so that there first appears the red eye with green reflections,
changing to red and green equally reflected, then green with red reflections, and
finally the eye becomes wholly green. The other method is a change through
the colour-band development, an account of which is given below. Actually several
large genera show a range from a species with red eyes, through species with the
red invaded with green to varying degrees, to a species with entirely green eyes.
The variegated eyes can be arranged in a series to show how the change proceeded,
and this seems to follow a uniform plan for all genera, but varies in the details
with each genus.
The consistency of marking retained by each species suggests that some
slight change in structure within the eye may take place uniformly with the
change in colour; thus there are produced the marked contours that vary very
little on any one species, although some variation in actual colour is not unusual.
I make no attempt to explain why colour changes should proceed through the
colour-band system, but it seems advisable to point out that perhaps vision given
by black eyes is less efficient than that by red eyes, whilst the green may be
much superior to both; even a small area of green in a red field may be
advantageous. Entirely green eyes occur consistently throughout the Asilidae
and are common in many other predaceous Brachycera, whilst blood-sucking forms
BY G. H. HARDY. 35
have both red and green, as well as the variegated eyes. Black eyes occur rarely
in Stratiomyiidae, but apparently always in Cyrtidae, and perhaps in most
Conopidae. Exotic Leptidae are often recorded with green eyes, but in the
Australian species the eyes always seem to be red.
The theory of colour-band development.—By simplifying the complexities seen
in colour marks, it becomes apparent that there first develops a green spot which
extends laterally across the red field at antennal level, and lying in band
formation practically parallel with the central line of the insect from head to
abdomen, no matter what this direction may be in relation to the major axis
of the eye. The band of green becomes complete when it reaches the anterior
and posterior eye-margins. Above and below the green band so formed, the red
areas of the eye form two blotches touching respectively the upper and the lower
eye-margins and in either or both of these, further green spots form, running
to bands parallel to the original one. By this process red bands are isolated;
the blotches which still retain contact with the eye-margins above and below
become smaller in area, and between them now lie alternating green and red bands.
Complications are introduced by the green having a tendency to spread,
upsetting the band formation by invading the red areas in another way. In the
lower Brachycera, this takes place largely by the green invading along the eye-
margin, and in the higher Brachycera the invasion is strongly marked in the
central field of the eye. It is also quite normal to see this spread more pronounced
over the lower half of the eye than the upper half. The green thus encroaches
over the red areas until the bands and blotches disappear. There is no uniformity
in this matter; many species have eye-markings which may be used with
conspicuous success in specific determinations, and any large genus may exhibit
grades in markings, all being of the one general type.
HKye-coloration and markings may take some other form, as in Syrphidae,
where some unusually active Hristalis have yellow eyes with minute black spots
that survive death, but the chief interest lies in the colour-band type found in
the following families: Stratiomyiidae, Tabanidae and Therevidae (colour band
range very wide), Syrphidae (colour band at least in genus Bacchus), Ortalidae
(colour band plentiful, but not studied in detail), and Calliphoridae (colour band
limited to Rhiniinae).
A Scheme for Describing Eye-markings.
1. The primary green band.—All marks are orientated about that green band
which forms the original invasion of the red eye and is situated at antennal
level. It is to be noted that the area at antennal level is almost invariably
green at least in part. This colour may extend indefinitely above and below, the
nature of the band thus becoming lost in the general green field on species with
advanced eye marks.
2. The red bands.—With the development of additional green bands above and
below the primary one, red bands are left between them. Thus one red band
lies just above, another just below the primary green band; rarely do either
of these red bands lie in a position that can be confused with the antennal level.
3. The multiplicity of bands——Further green bands may develop above and
below, leaving red bands between them. This division of the red area may
develop until seven green and six red bands are present, these being the maximum
numbers of true bands observed in Diptera, although the green may spread along
the eye-margins (as in some Rhiniinae), making the remnant of the original
red blotch at the upper and lower eye-margins resemble a further band of red.
36 MISCELLANEOUS NOTES ON AUSTRALIAN DIPTERA. V,
4. The blotches.—With the formation of the primary band, there are left two
red areas retaining contact with the upper and lower eye-margins respectively.
These two portions of red are the blotches, and they become smaller with every
successive increase in the number of bands formed in the red areas. If perchance
the green colour isolates the blotch from contact with the eye-margin, then the
area of red left becomes a spot and the term blotch will no longer apply.
5. The spots—This may apply either to the red or the green areas that do
not touch the eye-margins and that are sufficiently spot-like to warrant the term.
6. Colour invasion and elimination.—Together with the tendency to build up
the eye-markings to a maximum number of green and red bands, there is also
a tendency for the green to invade and eliminate the bands formed and blotches
left. This extra invasion by the green mostly takes place along the eye-margin
in the lower Brachycera and largely in the central area in the higher Brachycera.
In this way there is a trend towards the production of two markedly distinct
eye-patterns, both traceable to band formations when analysed. The red colour
disappears by suppression and the green increases by invasion and by the fusion
of one green area with another. For descriptive purposes, when bands and blotches
have been enumerated relative to antennal level, then this further invasion of
green, bringing distortions and alterations in the red areas, is described only when
marked effects are present.
7. Abortive band development.—It sometimes happens that the eye-marks
show an abortive development, as in the case of Wallacea. Here the band at
antennal level does not develop, but remains as a small elongate spot in a field
of red, and above it in the same field are two other small elongate spots of green.
This has produced an apparent blotch containing markings within, but on analysis
with regard to antennal level they are readily interpreted. There are other
abnormal markings which need to be interpreted in another way.
8. Abnormal band development.—That the simple horizontal band development
does not apply in all cases is well illustrated in the case of some exotic Tabanidae,
but is not yet known in the Australian fauna. In the genus Chrysops studied in
the Palaearctic and the two American regions, the band development is vertical
and irregular in shape; the blotches lie along the anterior and posterior eye-
margins when present. Further invasion by the green takes place along the
eye-margins and the red bars give way to spots that retain strong traces of their
original irregularity. The genus Chrysops has its antennae placed near the
eye-centre level, but Tabanus has the antennae nearly level with the lower eye-
margin, and it is interesting to note the angle in these two cases; the line between
the eye-centre and antennae compared with the direction of the eye-bands is
about the same. p
9. Variations in colour.—IiIn the eye-colour the green and the red are not
necessarily constant. Blue and purple may develop in their place, or an area may
be bordered with these colours, and more rarely the green may give place to yellow.
Melanism may appear in the eye, or at least a deepening of the shade resembling
black may give this effect, but the actual markings seem nearly always to remain
constant for each species.
10. Irregularities in bands and blotches.—Bands may disappear by elimination
of the red and fusion of the green; they may reach the eye-border or fail to do so;
the size of the blotches may depend on the number of bands formed, all lending
themselves to description in general terms in conformity with the present
discussion. In addition, markings are frequently different in the sexes, but usually
BY G. H. HARDY. 37
these have their salient points in common and differ in details. The markings
may become distorted even to the extent of hiding the band formation, such as
forming circular rings, but seldom do marks require special description apart
from that outlined here.
STRATIOM YIIDAE.
NEOEXAIRETA SPINIGERA Wiedemann.
In life the eyes are entirely black and the habits are striking when regarded
in this light, for the fly is particularly active and wary of movements so as to be
not readily caught. It breeds in piles of decayed vegetation in gardens and
orchards, where it mostly abounds, and is often abundant around sheds; it rarely
enters houses, apparently avoiding dark places. The fly is very rapid in flight
and has quick dodging movements.
ACTINA BRISBANENSIS, Nn. Sp.
Actina incisuralis (dark form), Hardy, Proc. Roy. Soc. Queensland, xliii, 1932, 53.
The exact identity of Actina incisuralis is uncertain; it is regarded as being
that form most commonly met with in Sydney, but owing to variations found
in collections there would appear to be several forms already discussed by me.
This incisuralis group, which includes the Tasmanian form as a possible sub-
species, becomes difficult to unravel. Possibly more than one species occurs in
Tasmania and certainly two occur in Queensland; the one described here is not
known to me outside this State with certainty, but is very common at times in
Brisbane, where it would seem to be the only species occurring.
The other Queensland species, still regarded as being incisuralis, has on the
female a red band at one-quarter of the eye-depth from the summit in a green
field and stretching from the anterior margin three-quarters of the way towards
the posterior margin, which marking differs from the present species considerably.
3, 2. Very like A. incisuralis Macq., but the black markings on the tergites
are invariably broadly black, thus reducing the orange colour, which may be
entirely eliminated in the case of the male. The orange colour varies in amount,
but never seems to increase in size comparable with that of the other various
forms of incisuralis seen. The eyes on both sexes have the red and green
intermingling with shot effect in more or less equal amounts, and there is no
trace of a marking in the eye.
Hab.—A very long series taken in Brisbane over many years, throughout the
summer half of the year; it seems quite common in the autumn on the underside
of the leaves of the Moreton Bay Fig trees in the Botanical Gardens and
University grounds.
LECOMYIA CYANEA White.
At the time of capture (10.10.1923), I made a sketch of the eye-marks on this
species, and this shows a blue-green field with a red band above antennal level,
strongly angulated near, but not reaching, the posterior margin. This is the
effect of a sudden broadening of the band just before terminating; the narrowest
part is about the centre. The green band above is thus very irregular in shape
and fuses along the posterior eye-border with the green covering the eye below
the red band. The upper red blotch reaches about half the length of the frons.
A pair of these rather rare flies recently captured (Sunnybank, October, 1938)
shows a normal green field on both sexes and, instead of the upper blotch, a second
red band which slopes about 45 degrees upwards from the middle of the frons,
38 MISCELLANEOUS NOTES ON AUSTRALIAN DIPTERA. V,
petering out to a point before reaching the posterior eye-margin. The latter is
perhaps the normal, the former the variation as the ground-colour is abnormal.
Also there is a common Brisbane Ortalid in some swamps that shows two forms
of eye-marks, a red band being either present or absent, an alternative variation
that might suggest how certain abnormal markings occur by suppression of red
on certain specific areas, not as a gradual development but rather as an abrupt
change. Alternative variations like these seem to be very rare.
Genus DAMAROMYIA Kertesz.
Hardy, Ann. Mag. Nat. Hist., (10) viii, 1931, 120-8.
D. whitei Hardy has the eyes green with a red band just above antennal
level, and the band curves upwards posteriorly, but does not reach the posterior
eye-margin. D. clivosa Hardy has a green band at antennal level between a red
band below and a red blotch above; below this the eye is green. A sketch pinned
with the specimen shows the blotch has a sinuous lower border, making the
green band irregular in depth.
Two new species described below run out at couplet 5 of my key which can
be used here by substituting the following new rendering of couplet 5 and adding
the couplets 12 and 13:
5. Frons with a median deep depression; frons one-fifth to one-sixth head-width .. 6
Frons without the depression; scutellum with one marginal depression .......... 12
12. Hair-pits plentiful on frons and with the hairs abnormally long there; body hairs
also much more conspicuous than normal. Frons one-quarter the head-width
OES tc Gao OO Oe CISTR I Sea MERC MEMO CRONE Ot One ho Ol tate er Oia ao oraio ahem ats hirsuta Hardy
ELAIT=Pits AN AUINAITS MOLINA lars, ore versus cite co ede eho ic cuenenesetene, Cusvole setae cere nua aVetet emo onseora cs aieretene 13
ie erons one-quarter thes head-width seers aeierie es chetoniencieaierenenens neohirsuta, n. sp.
Mrons! one-sixthe the Neaadswidthl Mies sels ees oe eeila este as Seen similis, n. sp.
D. neohirsuta is one of the two species recorded by me as near D. hirsuta;
the other referred to is in the Ferguson collection and from Sydney; no further
specimens have come before me. D. similis is quite a new form and both sexes
are known.
DAMAROMYIA SIMILIS, N. Sp.
©. Frons converging towards antennae, median width one-sixth that of the
head. The hair-pits are arranged two together each side of the ocellar triangle
and increase to three in a diagonal row towards the antennae; these lie mostly
in a long slight depression each side of the very narrow grooved carina. The eyes
in life are red shot with green and the eye-frons-eye proportions are 15:6:15.
The thorax, scutellum and abdomen dorsally are completely covered with punctures
uniformly dense and the triangular scutellum, lying in a plane with the thorax,
has but one marginal depression. The coxae are black, the remainder of the
legs is yellow, usually fuscated centrally on the femora and tibiae.
¢. Body characters very much as in the female, with occasional small areas
on which the punctures may be less dense. The eyes are contiguous, with the
lower third (antennal level and below) green in life, the remainder red.
Variations from this normal do not seem to occur, and although there is a
general depression each side of the carina, this may be due to shrinkage after
death and is not to be confused with those deep depressions on the lower section
of the frons and seen on other species. Those species having the frons one-sixth
the head-width or near are distinguished by the presence of the depression
and in additional characters; confusa has two marginal scutellar depressions,
tasmanica has a parallel-sided frons, whitei has a distinctive eye-mark when alive,
BY G. H. HARDY. 39
and trina is less regularly pitted on the body. The raised scutellum distinguishes
recemipuncta, the only other species with a narrow frons and also without the
deep frontal depression.
Hab.—Queensland: Brisbane, September and October, 1932 to 1937, mostly in
the latter year. 10 g, 18 ? from a persimmon tree and nearby foliage in my
garden at Sunnybank. I have no hesitation in relegating the male to this
position, as the only other species taken was represented by two females referred
to below and apparently were stray visitors, and not breeding in the locality.
DAMAROMYIA NEOHIRSUTA, N. Sp.
2. Very like D. similis, but differing by the frons being one-fourth head-width,
with coarser punctures more generally distributed, reaching nearer the eyes over
most of the length, and there are four punctures in a diagonal line anteriorly.
The eyes, when alive, have the lower quarter green, the remainder red. The
eye-frons-eye proportions are 9:6:9. The abdomen also differs in the punctures
being less dense than on the thorax and scutellum; on the two latter they are as
on D. similis. The male is not known.
The female is liable to be confused only with D. hirsuta because the characters
on other known species with a wide frons differ in many ways, but hirsuta differs
in having a greater density of hair-pits from head to scutellum and very con-
spicuous hairs; the hair-pits of the frons are too dense for the regular rows to be
seen.
Hab.—Queensland: Brisbane, September, 1937, 2 females taken on a persimmon
tree in my garden at Sunnybank, and in company with D. similis. Another
female (now without a head) was taken in September, 1929.
WALLACEA SPLENDENS Hardy.
In both sexes the eyes are green, with a large apparent, rounded, red blotch
on the upper third. As the antennae are situated very high on the head, the
blotch descends below the antennal level, where, within the blotch, a short
green band occurs. This band tapers to its ends, and above it is another band
which widens at the ends, but is hardly longer, and again above these is yet a
third green band that resembles the first. These green bands and the red
blotch are all subject to colour variation, peacock-blue, purple, etc., being sub-
stituted. Apparently the species is not uncommon at Sunnybank, as students
have collected a series, now in the Queensland University, and I myself have
added more to my collection.
OPHIODESMA INNODUS Hardy.
A sketch that I made some years ago shows that the female of this species
has a green band at antennal level, bordered above and below with a red-purple
band, the upper one being the shorter, but neither reaches the posterior eye-border,
nor does the next red band above, which resembles in general proportions the
lowest of these three. The two intervening green bands are thus fused with each
other along the posterior eye-margin and also with the green broad areas above
and below the three central red bands. The lower of these green areas is
/ exceptionally wide and fuses with yet another green band, along the anterior
eye-margin this time, that lies between the outer red curved band and the
blotch. Similarly these red and green bands are repeated in general shape and
contour just below the red blotch at the upper eye-margin. Hence there are, in
a green field, three central red bands that fail to reach the posterior eye-margin,
40 MISCELLANEOUS NOTES ON AUSTRALIAN DIPTERA. V,
whilst above and below these respectively, there is another red band that fails
to reach the anterior eye-margin, and also the two blotches. This makes two red
blotches and five red bands alternating with six green bands, one of which is
very wide. It will be noted that this is only one red and one green band less
than the maximum yet noted in Diptera, and possibly a red band has disappeared
from the very wide green area in the lower half of the eye. This forms the most
complete example of retained eye bands I have yet noted in the Stratiomyiidae, but
none of the red bands are complete, nor are any quite regular. The central red
band is slightly curved and is the narrowest, the adjacent ones above and below
expand towards the rear and only the lower of these two is reasonably straight.
The other two bands, adjacent to the blotches, are strongly curved, one upwards,
the lower one downwards following the contour of the equal blotches. The
symmetry of the markings is very striking.
TABANIDAE.
Genus PELECORRHYNCHUS Macq.
Two species, P. personatus Walk. and P. fergusoni, n. sp., definitely have
entirely red eyes, which character I believe to be consistent throughout the genus.
Pelecorrhynchus fusconiger-group.
In the first part of this series I defined three groups within the genus, of
which the present one is the second, containing five described species and several
undescribed.
Distribution—Only one species occurs in Tasmania and this, fusconiger
Walker, extends as a coastal species at least as far north as Sydney. The more
northern coastal species, fergusoni, seems to have a very limited range from the
Brisbane area and Stradbroke Island and possibly the northern parts of New
South Wales. Of these two, only the former reaches the mountain areas where
all the other known species occur, some showing a limited range even there.
It is to be particularly noted that the group is unknown from the Tasmanian
mountains.
Key to species of the fusconiger growp.
1. Wings with two contrasting colours; black and yellow ....................0- Z
WANE SsUNICOLOUITEd s mMOrenOrslessuhyalincenneee eee eOL oes 3
2. Thorax mainly yellow with a thin median black stripe ........... deuqueti Hardy
Thorax mainly black with a pair of yellow stripes ............ flavipennis Ferguson
3. With some dense white pubescence at base of abdomen. Thorax mainly black with a
pair of very broad, narrowly separated grey stripes, within each of which occurs
a short black stripe near the scutellum. The grey stripe is bordered laterally
withvathinswhitish: live) opr iserosnepouexers ik yeu toned Pathe hrohn overeteWeusn sae tillyardi Taylor
White pubescence at base of abdomen if present sparse and the thorax otherwise
T0828 alto) 6 US eek See a Ane Sol OR A Mem stem abe ALI Ah he ea a tide a SN 4
4. Species with some fiery red hairs on thorax and abdomen ...... claripennis Ricardo
SPeCLes WAC OUE PEGA AINS! wapeiciie.oevscts tlhe) wwsuishcey tev/etoneie Gamage nel sym peas eee CWS Cale eIIGN = Paresh oate eae thoy Clare 5
5. Thorax black with a pair of very thin whitish stripes interrupted just behind the
transverse suture, and broadening out to meet along the apical margin. (From
Barring ton! LOPS)! Pi erate atetae sieve are ara hate eNete epee Oe yc terera areas ok tone mietace netic aia ltetey’s sp.
Thorax brown or slate-greyish. The white stripes are complete or incomplete, but
CoCo Yojenpoal\-18" cee SO OR OC Ori OOOO DOGG TOC OO OOo pO TD AoC 1400 0 OOo D Oma 6
6. Thorax velvet-brown throughout with the whitish stripes conspicuous, at most,
before the transverse suture and faintly indicated beyond this; often limited
to a spot at the transverse suture. Rarely do black marks appear ..........
SA O.0 Cod GIG GOI. ORO OI OCI CO CIS FRCERIO G or ote 6.540 Otero Aicin a1 rons fusconiger Walk.
Thorax more or less strongly slate-grey coloured with a conspicuous pair of whitish
stripes complete and partly bordered laterally with thin black marks. There
may also be a thin median black stripe .................... fergusoni, n. sp.
BY G. H. HARDY. 41
In literature, under the name fusconiger, there are records of specimens
with red hairs on the body, and these doubtless should all be referred to
claripennis Ricardo. According to specimens in collections named by Mackerras,
there are two species that run to claripennis, both before me, the new one having
the wings strongly suffused with yellow and with a nebulous median spot; the
thorax of the two agrees in markings with that of fuwsconiger.
PELECORRHYNCHUS FERGUSONI, Nn. Sp.
P. fusconiger of authors in part.—Ferguson, Proc. Roy. Soc. Victoria, xxxiii, 1921,
2 (Queensland variety only).
Ricardo (1910) refers to fusconiger as occurring between Sydney and Moreton
Bay, but specimens from the latter locality should be referred here. Taylor (1917)
gives Stradbroke Island, and again all those specimens belong here. Ferguson
(1921) records differences in the Stradbroke Island specimens, but did not regard
the characters as more than a local variety at the time. Subsequently Mackerras
has shown (but not published) that specific differences occur in the terminalia,
and I have mounts of these made by him. fFerguson’s description and the
characters given in the key above are ample for the recognition of this species.
Hab.—Brisbane, August to October, 1924 to 1937, at the Sunnybank swamps.
Also Stradbroke Is., from which many specimens come, as far as I know, all
captured in September.
The flies do not seem to occur on the wing in any year for longer than a
fortnight or three weeks, usually about the middle of September, varying with the
early and late seasons. During 1937, a drought year, they appeared first in late
August, then disappeared, but came again in very late September and early
October. Similarly, P. personatus Walker, which normally comes in late September,
became plentiful on the same swamps in October only. These are the only two
species of the genus known to occur in the Brisbane district.
ScapriA (DIATOMINEURA) PULCHRA Ricardo.
On the female a red narrow band occurs well above antennal level, about
half eye-depth; the area above this is blackish, and below it green. These colour
marks are based upon a small series from Mt. Glorious, Brisbane.
SCAPTIA (DIATOMINEURA) AURIFLUA Don.
On the female a blue blotch margined below with red extends from the
summit to about two-thirds the distance towards the anterior eye-corners, and
below this the eye is mainly green, but the blue extends along the posterior margin
and peters out at the lowermost point of the eye. The description is from Brisbane
specimens.
ECTINOPSIS VULPECUNA Wied.
In literature two varieties are recorded and the exact determination of them
is not clear to me. On the Brisbane form the eyes of the male are green with a
thin red band about antennal level, tapering to a point and not reaching the
posterior border. ‘This red marking is broader but similar on the female and
situated at about level with the anterior eye-corners.
Genus TABANUS Lin.
Except for occasional references to the eyes on a species being green (red on
T. cyaneus Wied.),* there are no records yet made concerning eye-marks on
* Species of Tabanus seen by me show unusually green eyes, or green with slight
red reflections, but one unidentified species has red eyes with slight reflections green,
thus bridging the gap between TJ. cyaneus, which I have not examined alive, and the
more normal forms.
42 MISCELLANEOUS NOTES ON AUSTRALIAN DIPTERA. V,
Australian species and I myself have manuscript notes in only two cases. There
is a considerable difficulty met with in identifying species, and there is no
unanimous opinion concerning the interrelationship between species. Ricardo
made a number of groups that failed to hold. The hairy eye, as against the bare
eye, is about the last of these characters used. White indicated his ideas by
suggesting one hairy-eyed species is allied to a bare-eyed species that also has the
very long and narrow frons, and this is the first suggestion that breaks away
from the traditional scheme. It is proposed here to follow this lead, as it certainly
helps in the natural grouping of species.
Already I have grouped into order those species known from Tasmania, where
only hairy-eyed forms occur, and here I extend this section in order to incorporate
the mainland forms. Most bare-eyed species seem to conform to one or other of
those groups already formed, and some groups previously suggested are now
reduced by amalgamation. These main features are to be recognized in the
following key, the exceptions being few and perhaps not particularly important
if the key be used only as a guide.
Key to sections in genus Tabanus.
I, IMTS VGA Daron ail PEMENIKIESOCl GoscscobcacooddooobuEdoooC due DS Section 1
INTFONSENOLIN A] HCO MV CL VA WLC OG eyes ol cusscrede ye Cue S TG LGNS Rae ay cHotvon/ayeneies Se ete efor RAR ea oR: ae NIE ES 2
Ze VMrOnsSGlVvereine towards antennaey cacrcsy.cetetatcns) teenie rel stalkers horeteieio eterna one Section 2
TONS MPATAllel=SiGeG. rece storscicneler on eel else Sens lore seteiehees cr siletetace'e; eOnM ESR EOP RE Re ote Section 3
MLOnSNCOnVELEINe BLOW ALGS -ANCENMAC! Zoster cheicropene sushi alepeyenens cheyesielotene) er enene ie Section 4
Section 1.
Tabanus avidus-group.
This new group contains inter-related species, including: Tabanus alternatus
Ferg. & Hill (with synonyms limbatinervis Macq. and macquarti Ric., both names
preoccupied), 7. avidus Bigot (with synonyms fuscipes Taylor and taylori Austen),
T. davidsoni Taylor, T. doddi Taylor (with synonym abstersus Taylor, nec Walker),
T. duplonotatus Ricardo (with synonym parvicalosus Tayl., nee Ric.), 7. ochraceo-
flavus Ferg. & Henry, 7. palmensis Ferg. & Hill (with synonym nigropicta Macq.
preoce.), 7. sanguineus Bigot, JT. torresi Ferguson, T. victoriensis Ricardo and
var. heroni Ferguson, var. wentworthi Ferg. & Hill.
The two varieties are regarded as such by Ferguson, who reduced their rank,
but the matter is by no means assured yet. All these are without the appendix,
and agree in the frons, antennae and general characters. From others that I have
seen (unidentified) and from various descriptions, I suspect several more names
will fall here.
Nearest to this group, amid the hairy-eyed species, comes the Tabanus
microdonta-group, of which only one species is known and is limited to Tasmania.
It is not possible at present to draw a limit to section 1, so I cannot tell with
certainty if this will come here, but White thought it should be included with
T. victoriensis Ric.
Section 2.
This contains the gentilis-group, the gregarius-group and the regisgeorgii-
group, all of which seem likely to maintain their status. All species so far placed
in them have hairy eyes.
Section 3.
The exulans-group seems to be the hardest to understand and contains the
species most confused in literature; the limits are uncertain as they verge towards
section 2, but with this paper the hairy-eyed species are now fairly well isolated.
BY G. H. HARDY. 43
Section 4.
The Tabanus pallipennis-group is a new one and is well isolated from the
other sections and apparently it is the outskirts of a palaearctic fauna, whilst
the other three are apparently limited to the Australian region or almost so. As
far as I know, this is the only group in Australia that has banded eyes, all others
seem to have entirely green eyes except 7. cyaneus Wied., which is said to have
red eyes.
ie)
10.
ele
12.
13.
14.
15.
16.
Key to species of Tabanus with hairy eyes.
Fourth radial vein without an appendix, frons rather narrow (microdonta-group) ....
i MPR ROR HR cret fon aoa cere ee aunts Sea eri ce oyaiboman etrahia -eemopeltotisl sis a" ancen sieves microdonta Macq.
Fourth radial vein with an appendix. Frons not more than four times longer than
WAG wUISUalvapMat Ch LSS Seve eepedcuets ta lhe oir cme ceter aa le ts cuba lone tela -a a oteratalens ies retain sat ele 2
Frons of female diverging towards antennae, normally becoming there one and a
halPatinvesmwAGder sth ania tu. Cite retary wie) sweyetenc we ciksesianecgatodel erencuskenaeush< suede eels wie ce 3
Frons of the female parallel-sided ..................---.- exulans-group ...... 5
Thorax with well-defined dark stripes, four anteriorly and three posteriorly on a
STE VOT OU Ueeerwracn worst steep enie cine rse ler aiisionel ons teases eM chonsnars cl sis)tere wes. regisgeorgii-group
Thorax with rather ill-defined markings on dorsum, two to five light thin stripes
Oia CEN S fea TOLWOTO LN Gross cag oO. O HOS CIC CROCE ORCC IC OIG CIE ELA MEI cn ORE es hese nn ae 4
Thorax with a median light stripe normal, but sometimes very obscure if not quite
ODSOlETCH WANES SDOLCE CE ecru ceensccSerane, oso ste oi atas Denshare wie ueneceusi seit es ene gentilis-group
Thorax never with the median stripe, wings without spots (gregarius-group) ... 13
Key to the exulans-group.
Callusabsent, seeye lars cox rome ekes eioteme re seisoa eee cie adelaidae Ferguson; pseudobasilis Tayl.
Callus not reaching eyes, being separated by a pulverulent strip .............. 6
Cailus.~nmeachin gy (ey.esmanrein Sigh -iope rick t-tetcie ni otsss Sah ced tees Shere: ols chs: epdlemysfieh aw ot eibeee te ene 8
Body covered with a uniform pulverulent overlay, brownish-yellow (sand colour),
usually completely hiding the markings ....................2.-.. vetustus Walk.
Body, Not Somcoverecds ithe, markinasedenmede aa secs soca cee cies eo cieictere cca craicnel si rat
A somewhat yellowish species from N. S. Wales and Queensland ... ocultus Ricardo
Darks forms h srs ewes Aes eae eee neocirrus Ric. (Tasm.); dixoni Ferg.
(Vict.) ; geraltonensis Tayl. (Queensl.) ; and postponens Walker (N. S. Wales).
Eairs of trons lonsersthan halt themwidtheot GON Ss seers aide oi cies s scieiisk- yokes aia een ee tolane Pleurota
ANTENNAE, WICH OUES DC CECT ee «spe sepsncusits jsdeualisiey crane. eqersapiouerel obo cuonepeite depaxei een feuene wench shalePeus Zacorus
by Palpi-withwapical inferior tutte cis io tees uss es, sh ousuis.s seyse ss eusliavole le vairslevele sh elseueienelese cueueierene 6
Pallpim with OUtvaDICALSCULU cote c cicvecoteilore co etiotere tetra octome totelclinre ern otetey aialiaietareterre aisle mina means ions 10
Got Hindwinestwitht4 absent sey. cpitee ahaa. Sees SII AEG Oe. letretatoeenciere olate Ptochosaris
Eindwings} with) <4: Presents ays) sysyectereires ct ott thats Segal oes epeyete es UTR Aree mie eel ahaa s Ah cdaet teens 7
ds MOTCWINES with) 2 And 13 istal Ke) sii cscecvevsuaucinus, skenclecesorwleonegays. Sree w poueneacnousroncbensucxeue Pararsia
MOLewANeSsmwithearandy on SCDALTALOmeyctern ive crete re elore nel cece we geconeoueieieuscesevelclersnerersVeleuareden ores 8
SeeANtennae: Without Decten® Hei reehnctaereee chaveua totes te ce aseePene decane Wee Os abet Wel eS ee oes een ooeouagodmooee ING WhiGls sal. Soy
Body pitted all over, not striated; strongly constricted at level of coxa iii; with two
semicircular caudal plates, each bearing three fine setae. Dorsal setae 28 to 32
Eo a oly DIG Ct LG 1s & DICTS CRORE DL Can Ota Drea aca ecaa aT RT RCT RaeE Scenes N. kallipygos, n. sp.
Body striated all over, not pitted; of usual shape, or only slightly constricted at
CODEWOTIUS:f INSr CAWLEY TOMES eoneahy eG peer oles eicths tone cnaupancetine Chuaatooncic ach enlace mola tte cece 6
iPSendoshematiclorcans more on wlesssslobulan se ae seco ace ne co ee ete eee ff
Pseudostisniaic croncansrd enuiitelyarclaneaicem te se aleieayauuelel-) tiseasi-t icy: tetany icteneien , oancceoonoucooubsouModudoOUDS 10
Pseudostigmatic organs a broad leaf-shape. Scutum roughly hexagonal; corners
angular; posterior margin strongly convex, its lateral thirds at about 45° from
the middle third. Pseudostigmata almost in line with the posterolateral setae.
Dorsal setae 64, 264 long, arranged 2, 14, 14, 10, 12, 8, 4 .... N. edwardsi, n. sp.
Pseudostigmatic organs truly globular. Scutum roughly trapezoidal, corners
LeaRwN OG Kee NE Foes co ecOis Wolo cecad eo /O eRe ONS ob Or ae tnuo ORR ERC ChGtO nace REE DACRE eae 3 aeRO rE eeny Fae Te 9
Posterior margin of scutum rounded. Dorsal setae 32, 504 long, arranged 2, 6,
GRO Mec ler ernie ahaa OAD 20, Rhee ut nay ABs Rented MS eh SEN es chaz a. oo Ye N. coorongense Hirst 1929
Posterior margin of scutum flattened medially. Dorsal setae approximately 64, 404
NOME, Bisco 2 O. (55 Was Aone HO me whe Oe Sid WOW Socunacspccodooeucuonds
“Su soksigsn Eps yer el aioe ots SRR MSR NGS ATER Pe gee ES eat REE AEE Po ee Se N. petrogale Womersley 1934
Anterior margin of scutum four-fifths of length of posterior margin. Dorsal setae
HN, BO louis, eremennncl Oy .85' 35 Bos Gy 5° coocdooc N. antipodianum Hirst 1929.
SOLE ARSON OS AS MONS AG WAGE Goldoctosook soucrucnsessubuuoa buono ooo debe d 12
SEuULUM Wheat, Cir ISS BIG Ione IS WHS sana soocsnveseuodeeusoobsoodcss bole 13
Posterior margin of scutum evenly convex. Pseudostigmata in line with postero-
lateral setae. Dorsal setae 32, 40m long, arranged 2, 8, 6, 6, 6, 2, 2 ..........
Se chose or cen coer cette Dh ceee id SEaP knee Ou: Gace bk oar Set at Nee eee te N. dasycerci Hirst 1929
Posterior margin of scutum flattened in its middle third. Pseudostigmata well in
front of posterolateral setae. Only six segments in mid- and hind-legs. Dorsal
SUE AS i© HO, AOM ome, eieceinecs! BO, GO, (2), B 4 B CB) scocec N. impar, n. sp.
Secutum three-fifths as long as wide; roughly hexagonal; posterior margin strongly
convex, bluntly pointed in the centre; anterior margin projecting in the centre.
Pseudostigmata closer to the anterolateral setae than to the posterolaterals.
Dorsalesetaes220 5 0mlone arrnan aed Gs ont eran | eee ee N. lorius, n. sp.
Scutum not more than half as long as wide; posterior margin concave. Dorsal
Seiae se Wye lone. arceimsedl 2, Bo O53, OC). BB), B seccoccdodcoanbuuceosomoncunn
Ce Raa TROT OMTIRO Sol or ATR | Got Oe Ne tiotaeh eBay gus Ronen ay! arn Uae N. westraliense Womersley 1934
Genus SCHONGASTIA Oudemans, 1910.
Entomol. Ber., iii, No. 54, 1910, 86.
SCHONGASTIA JAMESI, n. sp. Figs. 30, 33, 36.
Body a rounded oval, flattened anteriorly, widest at level of coxa iii. Striations
coarse and moderately strong; very fine pitting on scutum, maxilla and coxae,
and over the anterior third of the venter. Colour bright orange. L, 278u;
W, 2324. Maxillary setae single, fine, with six long branches on the convex side.
Chelicerae very long, straight, slender; a minute sharp dorsoapical barb, with ten
92 TROMBIDIID LARVAE IN NEW GUINEA,
small saw-teeth in a row on the distal two-thirds. Ventral tooth represented by a
rounded thickening opposite the fourth and fifth teeth. Cheliceral sheaths long,
slender, reaching almost to the ends of the chelicerae, and bearing a short nude
curved seta on the base of each. Palpi rounded, slender, narrow at the base,
widest towards the distal end of ii. A long seta with long branches all over
on ii; a short seta with a few long branches on iii; on iv a long seta near the
base with six branches on the convex side, two short nude setae near the apex.
Palpal claw trifurcate, the dorsal and ventral elements long and sharp, with a
shorter, finer lateral element alongside them. Appendiculum with a rounded
point, bearing seven setae; one prominent, four finer, all with branches along one
side; two nude, the one stout, short and curved, the other fine and straight.
Scutum a rounded trapezoid. L, 50u; W, 854. Anterior margin sinuate; anterior
corners rounded; lateral margins slightly concave; posterior margin convex:
posterior corners rounded. Scutal setae 5, long, with long branches on all sides.
The three anterior in line; the PL in the posterior corners on the margins of the
scutum. The AM broken off short; AL, 37:54; PL, 474. Pseudostigmata just
behind the PL setae; 37u apart. Pseudostigmatic organs capitate, leaf-shaped,
with apparently no setules on the head. L, 37:54; stem, 12:54; head, 25u x 12-5u.
Ocular shield 7u from scutum. Eyes double, the anterior just in front of the PL
setae. Body setae approximately 68. (The dorsal details cannot be made out
easily, as the only available specimens are not well cleared and are all mounted
with the dorsum down. The figures are therefore imperfect.) Those of the first
dorsal row are stout, straight, blunt, with a few short spines along one side;
those of the first two ventral rows are slender, with long branches on one side;
the remainder, dorsal and ventral, have short branches on one side. Dorsum: setae
approximately 40, in rows as follows: 2, / 12, (8), (4), (6), 4, 2, 2. Venter: setae
28, in rows as follows: 2, 2, / 6, 4, 8, 4, 2. Legs relatively very long. i, 246u;
ii, 2094; iii, 2154. Coxal setae single, long, with many branches on the convex
side. The leg setae similar, but those on the distal segments have fewer branches,
those of iii having shorter and still fewer branches. The bases of the sixth
segments are markedly constricted, their distal portions markedly expanded.
All tarsi tapering, the third very long. A fine spur on tarsus i; that on ii short
and blunt; a fine nude seta, not at all prominent, on iii.
Two specimens from a bush-fowl (Megapodius duperreyi); one from a
bandicoot (Hchymipera cockerelli).
SCHONGASTIA BLESTOWEI, n. sp. Figs. 31, 34, 37.
Body a short rounded oval, widest at level of coxa iii. Striations moderately
coarse, strong and very wavy; pitting on scutum, maxilla and coxae. Colour
dull brownish-orange. Newly hatched, L, 1674; W, 1674; average, 2034 x 168u;
largest seen, 223u « 2074. Maxillary setae single, short, stout, with four long
branches on the convex side. Maxilla typically square. Chelicerae very long,
straight, slender, with sharp points. A minute dorso-apical barb and a row
of twelve denticles along the distal three-fifths. Ventral tooth apparently missing.
Cheliceral sheaths slender, as long as the chelicerae, with a long nude seta on
the base of each. Palpi rounded, projecting boldly forward. A long seta with
a few fine branches on the convex side on ii; a similar seta, but shorter on iii;
on iv near the base a short seta with a very few fine branches on the convex
side, near the apex two nude setae, one very short and stout. Palpal claw
trifurcate, the ventral element much the longest and stoutest, the lateral very
short and fine, almost vestigial. Appendiculum rounded, with six setae; one
BY C. E. M. GUNTHER. 93
stout with a few stout branches, three finer with short fine branches, and two
nude, one of them short, sharp and strongly curved. Scutum rounded, straight
anteriorly. bl, 62:54; W, 94u. Crest a sinuate overhanging ledge, two-thirds of
the way back; the posterior portion of the scutum at a much lower level than
Figs. 30-40.—30. Composite dorsal and ventral diagram of Schéngastia jamesi, n. sp.
31. Same of S. blestowei, n. sp.; 32. Walchia morobensis, n. sp.; 33. Dorsal scutum of
S. jamesi; 34. Same of S. blestowei; 35. Leewwenhoekia aiustraliense Hirst; 36. Cheliceral
fang of S. jamesi; 37. Same of S. blestowei; 38. Same of L. australiense; 39. Same of W.
morobeinsis; 40. Composite dorsal and ventral diagram of L. australiense.
the anterior. Crest very faintly marked in some specimens. Anterior margin
straight; anterior corners angular, projecting very slightly forward; lateral
margins slightly convex; posterior margin strongly convex, with a smooth
indentation in the middle; posterior corners about two-thirds of the way back,
angular, projecting laterally. Scutal setae 5, the AM 37:5u, stouter than the
others, with short branches on all sides, set well back from the anterior margin,
behind the AL; the AL 75u, slender, with long branches on all sides, well
forward in the anterior corners; the PL 50yu, slender, with branches on one side
only, in the posterior corners. Pseudostigmata half-way back, directed almost
horizontally, lying under the overhang of the crest, just anterior to the PL setae;
25u apart. Pseudostigmatic organs capitate, racquet-shaped, the heads covered
with fine short setules. LL, 374; stem, 12u; head, 254 x 154. Ocular shield
applied to the scutum from well in front of the pseudostigmata to behind the
PL setae. Eyes single, small, the posterior missing; just anterior to the pseudo-
stigmata, Body setae 108, of three forms: those of the last two rows of both
94 TROMBIDIID LARVAE IN NEW GUINEA,
dorsum and venter are short, stout, curved, with short spines along the convex
side; the remainder of the dorsum stout, with closely-set branches on the convex
side; the remainder of the venter slender, with a few branches on the convex
side. Dorsum: setae 64, in rows as follows: 2, 10, 8, 10, 8(10), 10(8), / 8, 8.
Row eight is on the posterior margin, often more ventral than dorsal. Venter:
setae 44, in rows as follows: 2, 2, 10(8), 8(10), 6, 6, / 6, 4. Row six is at the
level of the anus. Legs relatively very long; i, 270u; ii, 209u: iii, 250u. Leg
setae slender, with a few fine branches on the convex side. Coxal setae single.
Sixth segments not unduly constricted or expanded. Tarsi tapering. A short
stout spur on tarsus i, the dorsal nude seta prominent, set on a tubercle. The
spur on tarsus ii short, finer and sharper. A very fine nude seta on tarsus ili,
often broken.
Fifteen specimens collected from two men near the Suein River, Sepik District;
eight specimens from abandoned colonies in the ears of two bush-fowl (Megapodius
duperreyi) from the Bulolo River basin, Morobe District; six specimens from a
man at Bulolo.
There is a strong resemblance between this species and SNS. vandersandei
Oudemans, 1905. The differences are as follows:
S. vandersandei S. blestowei
Dorsal setae 50. 64.
Ventral setae 42. 44,
Dorsal setae arranged:
As UM. WO, a, ws 3s 2p NO OS UO, SCG), ClO. G;
2 palpal claws. on
Maxillary setae plain. With 4 long branches.
Key to the New Guinea Species of Schongastia.
(Constructed by Mr. H. Womersley.)
Ss Dorsalesetaewm Ovemtiamy D0) cies cisieus: cretion sl cy cpttevroichecet tous sy silensmetiecter terns) once) ayrcliey eisai isatverteve oie teeter os (ear 2
Dorsal setae 40, arranged 2, 12, (8), (4), (6), 4, 2, 2. 50u long .... S. jamesi, n. sp.
2. Dorsal setae 52, arranged 2, 10, 10, 10, 10, 8(10), 2(10). Ventral setae 42. Maxillary
setae plain. Palpal claw bifurcate .......... S. vandersandei Oudemans 1905
Dorsal setae 64, arranged 2, 10, 8, 10, 8(10), 10(8), 8, 8. 40 long. Ventral setae 44.
Maxillary setae with four long branches. Palpal claw trifurcate ..............
Bia o 19.0 CMS I RT SIS Ne ana areas LR ves a as Be lt S. blestowei, n. sp.
Genus WALcHIA Ewing.
Proc. U.S. Nat. Mus., xxx, 1931, 10.
WALCHIA MOROBENSIS, Nn. sp. Figs. 32, 39.
Body a broad oval, widest midway, the anterior fourth with a gradual
straight taper to a rounded point. Irregular folds radiating in all directions
from behind the pseudostigmata. No striations; pitting all over, not specially
marked on scutum, maxilla or coxae. Cephalothorax completely hidden below
the anterior point of the body. Colour a dirty cream. lL, 4254; W, 310u; largest
seen, 5354 * 38754. Maxillary setae single, long, fine, curved, with long fine
branches on the convex side. Chelicerae short, stout, almost straight, tapering
very sharply. Dorso-apical tooth single, small, sharp. Ventral tooth a small
swelling behind a shallow notch. Cheliceral sheaths almost as long as the
chelicerae, and relatively stout. Palpi small, strongly curved, ii angular. A long
nude seta on ii; a similar one on iii; on iv two short nude setae and a longer
one with a few fine short branches. Palpal claw bifureate, the two elements
curved, very long and slender, the ventral slightly longer and stouter than
the dorsal. Appendiculum small, rounded, with five setae; two long and stout,
BY C. E. M. GUNTHER. 95
with a few fine branches; two long and very fine, with a tew fine short branches;
and one short, nude, stout and pointed. Scutum not distinguishable in these
specimens. Pseudostigmata 53u back from the anterior margin of the body
(74u in the largest specimen) and 25 apart (this figure does not vary). An
oblique curved ridge lies around the anterior and medial aspects of each
pseudostigma. Scutal setae 4: a pair 14u in front of the pseudostigmata, 18u
long, curved, with two or three fine branches; and a pair 19u behind the pseudo-
stigmata, 30u long, curved, with five or six long fine branches. Pseudostigmatic
organs capitate, leaf-shaped, the head covered with setules. lL, 25u; stem, 6y;
head, 19u x llw. Ocular shield apparently missing. Eyes single, very indistinct
except in freshly-killed specimens; about 75u lateral to and 30u behind the corres-
ponding pseudostigma. Body setae 58, those of the dorsum and the first two rows
of the venter long, fine, with six to eight long fine branches on the convex side;
the remainder of the venter shorter, with fewer branches. Dorsum: setae 26, in
rows as follows: 2, 6, 6, 6, 4, 2. Venter: setae 32, in rows as follows: 2, 2, 8, 6, 6, 6, 2.
Row five is level with the anus. Legs relatively very short; i, 1254; ii, 111; iii,
165u. Only six segments in legs ii and iii. Leg setae long, fine, with a few fine
branches along the convex side. Coxal setae single. The sixth segment of i and
the fifth of ii short and stout; the fifth of iii is of typical shape. Tarsi bluntly
tapered, short. The dorsal nude seta on tarsus i prominent, the spur very long,
stout and curved; the spur on ii shorter but stouter. No prominent nude seta
on iii. On each tarsus two or three setae with only two fine terminal branches.
Four specimens from two Brown’s rats (Rattus browni); many from the
Brown bush-rat (Rattus ringens).
Genus LEEUWENHOEKIA Oudemans, 1911.
*s Gravenhage Ber. Ned. Ent. Ver., iii, 1911, 138.
LEEUWENHOEKIA AUSTRALIENSE Hirst. Figs. 35, 38, 40.
Trans. Roy. Soc. Trop. Med. Hyg., xix, 1925, 150.
A single specimen of this species, lacking the pseudostigmatic organs, was
taken at Bulolo from a Cassowary (Casuarius casuarius). I am indebted to
Mr. H. Womersley for its identification.
ACKNOWLEDGEMENTS.
My very sincere thanks are due to many people, to the Directors and
Managers of Bulolo Gold Dredging, Limited, for the encouragement they have
given me, and the excellent facilities they have provided for me to undertake
research work; to the many. members of the staff of the Company, in particular
Mr. G. M. Rio, who assisted me in obtaining specimens of all kinds; to Mr. A. T.
Simmons, my Senior Assistant, whose considerable photographic knowledge and
skill were always at my disposal; to Professor Harvey Sutton, Director of the
Sydney School of Public Health and Tropical Medicine, and to Mr. K. J. Clinton
of his staff, who searched out references for me and sent me negatives of them;
to Mr. BE. Le G. Troughton and Mr. J. R. Kinghorn of the Australian Museum, and
Mr. Tom Iredale, who identified mammal and bird hosts for me; to Dr. C. T.
Backhouse, of the New Guinea Public Health Department, who has advised me
and offered suggestions; to Mr. F. H. Taylor, School of Public Health and Tropical
Medicine, University of Sydney, and Mr. H. Womersley, South Australian Museum,
without whose assistance this paper would never have been completed.
96 TROMBIDILD LARVAE IN NEW GUINEA.
References.
bwinc, H. E., 1929.—A Manual of External Parasites. London.
FANTHAM, H. B., STEPHENS, J. W. W., and THEOBALD, F. V., 1916.—The Animal Parasites
of Man. London. Page 485.
GATER, B. A. R., 1932.—Parasitology, xxiv, p. 143.
GUNTHER, C. #. M., 1957.—Lab. J. Australasia. i, 4, p. 106.
—————,, 1958.—Med. J. Australia, ii, 6, p. 202.
Hirst, S., 1920.—Trans. Roy. Soc. Trop. Med. Ilyg., Xix.
1929.—Ann. Mag. Nat. Hist. (10), iii, p. 564.
Patton. W. S., 1931.—Insects, Ticks, Mites and Venomous Animals. II. Croydon.
Page 331.
PATTON, W. S., and Evans. A. M., 1929.—Insects, Ticks, Mites and Venomous Animals.
I. Croydon.
SAMBON, L. W., 1927.—Ann. Mag. Nat. Hist. (9), xx, p. 157.
WARBURTON, C., 1928.—Parasitology. xx, p. 228.
WoOMERSLEY, H., 19536.—Records S. Aust. Museum, v, 2 ps 79s
————, 1936a.—Jowm. Linn. Soc. London, Zool., xl, p. 112.
————,, 1937.— Records S. Aust. Museum, vi, 1, p. 75.
97
THE DIPTERA OF THE TERRITORY OF NEW GUINEA. VII.
FAMILY OTITIDAE (ORTALIDAE).
By JoHN R. Mattocnu, Arlington, Va.
(Communicated by Frank H. Taylor, F.R.E.S., F.Z.8.)
(Plates iv—v.)
[Read 26th April, 1939.]
This family is in many respects similar to the Trypetidae, the only almost
invariably dependable character for its separation therefrom consisting of the
lack of incurved anterior orbital bristles on the frons. The course of the subcostal
vein at its apex is also usually distinctive, the vein in the Otitidae normally
gradually approaching the costa and connecting with it at an acute angle, while
in the Trypetidae the vein makes an abrupt angular bend forward close to its apex
and is usually faint beyond the angle. All the New Guinea Otitidae lack the
presutural bristle.
There have been many species recorded from New Guinea and adjacent
islands, as the peculiar forms and distinctive colour markings of most of them
readily attract collectors. In the Australian region the family is represented
almost exclusively by the subfamily Platystominae, though some species of almost
cosmopolitan occurrence have been brought in, probably by commerce.
The late Dr. F. Hendel published many papers on the family, the most
interesting of them, from an Australian point of view, being that on the
Platystominae. This is the predominant subfamily in the Indo-Australian region,
more than half of the approximately 500 species occurring in the region, and in
1914 only 45 in North and South America.
I present herein a key to the New Quinea and Australian genera of
Platystominae based upon materials available to me and to some extent upon
data obtained from Hendel’s paper when the genus or species is not available.
In 1924 Enderlein published a paper in which he erected several new
genera and described some new species from this region. I have incorporated his
work herein.
Material collected in Papua and Dutch New Guinea by Miss L. HE. Cheesman
has been included in this paper for geographical reasons, thus rendering the
paper more valuable.
I have to thank the British Museum (Nat. Hist.) authorities for photographs
of the wings of the type-specimens of the species in their material, and Mr.
Frank H. Taylor for the other photographs of wings when the types belong to
the School of Public Health and Tropical Medicine, University of Sydney.
Subfamily ULIpIINnaer.
In this collection there is but one species of this subfamily. This is an almost
cosmopolitan species which occurs in adjoining islands and Australia.
J
98 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
PSEUDEUXESTA Hendel. (Gen. Ins., Fasc. 106, 1910, 30.)
PSEUDEUXESTA PRIMA Osten-Sacken.
Ann. Mus. Civ. Stor. Nat. Genov., xvi, 1881, 470 (Huxesta) —EHucxesta semi-
fasciata Malloch, Insects of Samoa, pt. 6, Diptera, fase. 5, 1930, 216.
Originally described from Celebes and known from many other localities,
including Hawaii.
There is a single specimen in the collection from Wewak, New Guinea (F. H.
Taylor).
Subfamily PLATYSTOMINAE.
The genus name Platystoma is preoccupied in Mollusca, but up to the present
no writer on the group has proposed a new name for the genus.
The group segregated here may be distinguished from others in the family
by the presence of short stiff setulae on the upper surface of the first vein, usually
extending from near the humeral cross-vein to its apex, the lack of the propleural
bristle, and the presence of at most three bristles between the suture and the
anterior lateral angle of the scutellum, i.e., one supra-alar and two postalars.
Hendel has attempted to separate the group from the Pyrgotidae by the shorter
basal two antennal segments and the presence of ocelli, but these characters do
not invariably apply, as some Pyrgotidae have ocelli, and short basal segments to
the antennae.
Key to the Genera.
1. Eyes quite densely haired; arista long haired; frons with two pairs of fronto-
orbital bristles; fifth wing-vein with stiff setulae along the entire extent of the
posterniorebasalecellon upper VSuULrace wees ices eel oieie ea aeiieiee inicio 2
Byes not distinctly haired; other characters not as above in toto .............. 3
2. Face below antennal foveae with two rounded or oval elevations .. Lasioxiria Hendel
Hace pwithoutssuch) elevationsig-s. -yonclorixeci sick susie oe cl kepentencat e Dasyortalis Hendel
Allefemora withssomevshone StOumvenLLal sSpINCS us icwelelesioel sues cei siekmieleieueneue eens 3a
At most one pair of femora with short stout ventral spines ................... 3b
3a. All femora with anteroventral and posteroventral spines; an extra cross-vein between
second and third veins; arista subnude (Samoa) ......... Apactoneura Malloch
Only mid and hind femora with biseriate ventral spines, the fore femora with
spines on anteroventral surface only; venation normal; arista long-haired
GSU Oa) ates ice ss ostace sesrausauay otis hershevenoverclisnel ace vedexsitonsiiens poy suet wen siteeeyroue Xenognathus Malloch
3b. Suprasquamal ridge with erect hairs near posterior extremity; stem vein of the
wing bare at base above; lower squama about twice as large as upper; no
fronto-orbital bristles on frons; arista bare or almost so (Australia) ......
Josgo odo OU modo Om n oS dor Oe ooo) Koodo natn sano nb oO ac Duomyia Walker
Suprasquamal ridge bare, or if haired then the stem vein of the wing is haired above
at bases onthe oLrher ‘characters are not allsasmapOve, cree ci cleicne crercncepelenencle t
4. Mesopleura, sternopleura and pteropleura with numerous short stout bristles .....
OTs OTL 019 GRO O Oca HERG CeOe Con OHO Ceo cise et Oleadby os4 Go to ho rnors cig biota Pseudocleitamia, n. gen.
The above sclerites of pleura without short stout bristles .................... 44a
4a. Elongate slender species, the abdomen slim, not widened at base or at middle and
usually quite noticeably laterally compressed; arista never long haired, if
noticeably haired at base then bare beyond middle, or extremely long and with
dense short white hairs on entire extent that give it the appearance of being
thickened; antennal foveae usually long and distinct; sternopleural bristle
always lacking; fourth wing-vein never setulose above along posterior basal
CEL reratteteresseterenetencce [scahets ae terete to) aieen tia ee Cree eee ona ewe aT aeMONe Love cette latevever on ehenetenenoneheretehs 5
Stouter species, the thorax sometimes much wider than long, the abdomen either
wide at base or centrally, never laterally compressed, if rather slender species
the arista is haired to apex; fourth wing-vein sometimes setulose in part
PMIGN GoD OOODOOMNCOUUUD.6 Oot to 0 Ott odo0 So cpennOOdunbad con dGos0 Dc ebo0GOOS 14
5. Third antennal segment with quite dense decumbent stiff black hairs; face more or
less’ produced’ above, recedine below Sa... sere cee sie renee oe Conicipithea Hendel
Third antennal segment not stiff haired; face not receding below ............... 6
10.
Nil,
12.
13.
13a.
14.
15.
16.
17.
18.
BY J. R. MALLOCH. 99
Antennae and aristae exceptionally long, the former longer than the face, the aristae
still longer and with a thickened appearance because of the presence of dense
short white hairs; humeral bristle lacking ................0c02-2-ecseeeeeee 7
Antennae usually not longer than the face, the aristae shorter and never with
dense short white hairs; humeral bristle present or lacking ................ 8
Fourth wing-vein making a wide shallow dip into the discal cell from inner to outer
cross-vein and angularly bent up just beyond that vein; cross-veins rather widely
SVE NEE NIEX|. Go Gio'o 6 Ox GO Ol DIDioro ia Charen G DIGIcROlO Et DOL OATIG Y Oee Cahora Philocompus Osten-Sacken
Fourth wing-vein not dipped down into discal cell from inner to outer cross-vein,
and not angularly bent upward just beyond outer cross-vein; cross-veins quite
closely placed, sometimes interstitial ................. Antineura Osten-Sacken
First posterior cell of the wing quite noticeably narrowed at apex, the fourth vein
either sloping forward from outer cross-vein or with its apex curved appreciably
SHOIOWEN COL orb Co Grou0 O/C COND DID DITO Oe DID LOIRE ROD OOO CREED ORG, out Cod Cie OfOnG EO DRONDSO, Dra (hen aaa Sr cre emeactotD 9
First posterior cell of the wing not narrowed at apex, the fourth vein either
straight or with its apex slightly downwardly sloped ...................+-.- 13
Frons deeply or rather closely pitted or punctured; parafacials wrinkled above;
facial carina prominent, in profile exposed at least as widely as parafacial,
rounded on dorsum; two fine pairs of fronto-orbital bristles generally visible
A Guat Uc eh POSE COON OFTEN Oc SICRE ERROR Cuca RCC NCPC RSES ch) ce cma as ee salen ae Rhytidortalis Hendel
Frons not distinctly punctured nor the parafacials wrinkled above, the facial carina
TOE Foporopaabaverae shal FoPNOMVKs) GHG ooigdmote oS poems oon ono MO Ob CMON oO cis an end Cob e.coG 10
Mesonotum as wide as long; frontal orbits with two pairs of bristles; mouth opening
very large, male with a beard of long downwardly-directed bristles on posterior
DOGCLON MOLI OWASW ys. crete tar tetas: opiates ie tairstiavetad ch ciret abe FU Sialis: /oufeieh wetgatie, © Pogonortalis Hendel
Mesonotum longer than wide; frons with at most one pair of orbital bristles .... 11
Penultimate section of fourth wing-vein about one-fifth as long as ultimate and
only as long as the outer cross-vein, the latter as long as ultimate section of
fit Vein ErOnst wrinkles. tyeaeiedy sich tie die selielchet oie) sade kl. Microepicausta Hendel
Penultimate section of fourth wing-vein longer, the outer cross-vein much nearer
to the apex of fifth vein and tip of wing than in the above; frons smooth .... 12
Inner cross-vein of the wing oblique, upper extremity much nearer to the base of
wing than the lower; face with some fine short hairs in centre ..............
ata alatnet anata tetas totcrattienedetakstare te ty ratevanase bene ler heeena eho tame a medete eS Plagiostenopterina Hendel
Inner cross-vein of the wing erect or almost so; face bare in centre ...........
BOR a i his aay, tr Gethin ten Ne nS a erin t a aan nN ERA LAL AN eS Elassogaster Bigot
IDTAOHANS Vee TAyyO) TVET Gry ChoomeENl oN 4onoooucdocuadudnoobununnoobacouOUODS 13a
Frons with but one pair of orbital bristles ................. Pseudepicausta Hendel
Inner cross-vein of wing more than one-third from apex of discal cell ...........
aera aWical ebrartes anerate satana corSeohe ele teurene tlota tata atts toc cten a ate aie ie Re eran Scotinosoma Loew
Inner cross-vein of wing not more than one-fifth from apex of discal cell ........
SE eR ISON SHR a ECan TaCRCR csr ec ON SRS COT IRE EAR OPEC IRENE RENEE fiir Euxestomoea Hendel
Sternopleura with a strong upper marginal bristle .....................-++-e0. 15
Sternopleura without a well-developed bristle ..................... 00. ee ee neee 16
First posterior cell of the wing narrowed at apex; second vein nearer to third than
to costa; head higher than wide in front (Australia) ............. Celetor Loew
First posterior cell of the wing not noticeably narrowed at apex; second vein nearer
to costa than to third vein; head seen from in front as wide as or wider than
TOUTES GT went Sich Grek TORCH OIEE O ON CRON BSC De SOG CHEST CeO ELERORG ENOL O ona Ree Scholastes Loew
Mid femur much stouter and distinctly longer than the hind one, with two series
Of Shortestnonaventrallibristle sii cus stave crashes cake ceusee) ieee vale ei s/ oy susuar si sues) buss sucaere 17
Mid femur not thicker nor longer than the other pairs, if slightly stouter then with
at most finenventraly bristles ace crscueds oe ciao cicus cath choustslees oc: otece wosveyede onsys saleersiteue 18
Antennal bases close together, separated by less than the width of the third antennal
segment; discal cell of the wing much narrower at base than at apex ......
POOR Or Hck By. OLDER IDO LECT or CLIONSTG GORATH DNCEO HE OR CECE eT OREO Brea Walker
Antennal bases widely separated, distance between them exceeding length of third
antennal segment; discal cell of the wing almost as wide at base as at apex ....
Mo Ae SEER a HAE Pb arete oes eee aroihat aesbavate awerte Si55s Mesoctenia Enderlein
Hind femur much stouter than the other pairs and armed below with short stout
black bristles or spines (Pacific Islands, Fiji, Samoa) .. Pseudorichardia Hendel
All femora about equally thick, hind pair without stout ventral spines ........ 19
100
21.
22a.
23.
bo
or
to
~
28.
29.
be
DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
Cross-veins of the wing quite close together, the penultimate section of fourth vein
not one-fifth as long as the antepenultimate one ..............-.0.0e000- 20
Cross-veins of the wing not exceptionally close together, the penultimate section of
fourth vein not less than one-third as long as the antepenultimate one .... 23
Frons with two pairs of strong orbital bristles; arista with very short hairs; fifth
abdominal tergite in the male not long-bristled at apex .... Huxestomoea Hendel
Frons without or with but one pair of orbital bristles except in Loriomyia; arista
rather long haired; fifth abdominal tergite of the male long-bristled at apex;
SCUAMNACS. "SINAT Gee etetevet cto rctone ns lcversi ciety) rersten ol tele ot tts) Aetonstonth a dictehe skciel eranalceie o)aretenet ebsites 21
The cross-vein closing the anal cell angled below middle, broken, the cell at apex
below forming a short point; two pairs of fronto-orbital bristles .............
Koo noado dO OUUC Oo UO GSC ODOD Gnd OOO OUOUSIOOb US ago Doo lOb aS Loriomyia Kertész
The cross-vein closing the anal cell rather angularly curved outward at middle,
the celll note pointed MDeloOws Qtr AOR ts cre ahetet lever ay ova) ot et olfol clot siclcn al olere arenctene ete ey = cls) te 22
Second wing-vein usually much bent forward at apex, unusually close to first near
costa, sometimes almost fused with it, its tip much closer to that of first than
to tip of third in costa; head of male frequently widened, but never with
Aeon ENE AE JooemaudoboudbudocuucobododuloUs oud obaboud ooo dUadoouE 22a
Second and first wing-veins never approaching each other apically; male with the
EVESTONMBVATIAD LY MIONS SCALES Were) chetote) euereucl sieiel creletoletenenerenenatersieeiey aie Laglaisia Bigot
Second wing-vein much closer to third than to first on apical section of latter; one
pair of strong orbital bristles present ...............-0000- Cleitamia Macquart
Second wing-vein at least as close to first as to third on apical section of former;
THO) Cyd ohizvl [HOKU fs coooocucosgucc ooo UCC ObUENUOUGQOON Cleitamoides, n. gen.
Anal cell closed by an angulate cross-vein, produced into a distinct, sometimes
elongate, point or lobe at lower apical angle; frons with only the outer verticals
pLesentianagdTonewpairsOfsOLEDILAlSee ere ieietaterel 1 sietek kel ede) otetel Neosophira Hendel*
Anal cell closed by a straight or slightly curved cross-vein at apex, not produced
into aepointuor lobe at lower apicalvangele =. semi eiaer-iisieicle octane cra eieieie eee 24
Extremely short stout species, the thorax broader than long, the mesopleura well
exposed when seen from above, the tergites of basal half of abdomen in female
usually more or less telescoped so that the abdomen is usually not longer than
wide excluding the ovipositor; first posterior cell of the wing almost invariably
RIN! CrP TAlWGl ENE BYOES ooocacbacdanc0duD Dodou ad DODO ya DDDD00NDS 25
More elongate species, both the thorax and abdomen longer than wide, the segments
of the latter not noticeably telescoped; first posterior cell of wing usually
MArrowed , AVICALLY sci cicecwlsse 6 sae casyaekePoyeh es Beet oberons che yelenerbelorsucreutyeloved yeionereieucispamere 30
Posterior basal cell of the wing longer and larger than the discal cell; wings more
or less folded lengthwise and crosswise centrally, usually held close against the
abaomenkands depressed: At aAplCeSereererelevorel ane clare scheuciel ciel a cucienctouchel storceb Renoir =netatele 26
Posterior basal cell of the wing shorter and smaller than the discal cell; wings not
GURKHA ia silo) Vo eye We eeiedio clacidinGiag Modnidicia Cominco Clinical G06 Gabo coc b 6.006 o 27
Antennal bases rather widely separated; fourth wing-vein ending in the wing-tip;
vein closing the anal cell sloping outward posteriorly so that the cell is rather
ACULELYBVOINTEAEDELOW ac (LDe Xena reuoieie cieicie cierenelcneicneians Asyntona Osten-Sacken
Antennal bases closer together; fourth wing-vein ending below wing-tip; vein closing
anal cell erect or sloping forward anteriorly, the cell transverse at apex ......
“SODESODOODODUO DOO OOOO DOO COU SOCEIU SOO ODOC DD OD ODOM dOD NS Naupoda Osten-Sacken
Frons with a pair of strong orbital and two vertical bristles; antennae short, inserted
at middle of eyes in profile; arista plumose; ultimate section of fourth vein
SlPHthyaCurvenouDwWaLd cyaceisccreccie ertekeie ste rere ner en tater a oreo Chaetorivellia de Meijere
Frons without distinct orbital bristles; antennae inserted below middle of eyes in
profile; ultimate section of fourth vein not bent upward ................... 28
Bases of antennae close together; discal cell of the wing much narrower at base
than atvapesrr et ee see ME oaks ee ree
AS*
" rR |
BY J. R. MALLOCH. pip ag ay 107
eu yy
Key to the Species. Nagel
1. No black streak emanating from the costal edge of the large brown mark over the
CRORES ib ab binlblnglbloe Go Ob odie a ORO eieibe bo bcd pala miro ae cle liturata (Walker)
A black or dark brown streak emanating from the costal edge of the large brown
mark over the cross-veins and extending narrowly round the costal margin to
DOOKIE O fate PHOUEUMG Ve len rtm eenetenen erento ne et Veh oneal stints, ctrauoterciorecicticdeteneuene tens ae wicre otaire 2
2. The basal brown mark on the wing not extending to the costa at apex ...........
5 Be Bald co apis SERRA SAC ICRE AED SEEGERS CRAB LAN CRC URS CCH ISG c eons OCs kc RAC oar CMP kerteszi Hendel
The basal brown mark extending to the costa on a large part of its apical half
DEE CM eM HNP Paneer e Ath ota taken h Beton wat ate hahabe 4 itn TAG, MNnealra Man asta ea here bts cite latifascia (Walker)
CLEITAMOIDES LITURATA (Walker).
Jour. Proc. Linn. Soc. Lond., v, 1861, 251 (Dacus).
Originally described from Dorey, and subsequently recorded from New Guinea.
CLEITAMOIDES KERTESZI Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 130—Cleitamia liturata Osten-Sacken,
Ann. Mus. Civ. Genov., xvi, 1881, 468; op. cit., (2) xix (xxxix), 1899, 559.
Described from New Guinea and known only from the original material.
CLEITAMOIDES LATIFASCIA (Walker). Pl. iv, fig. 7.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 114 (Dacus); Edwards, Trans. Zool.
Soc. Lond., xx, pt. 13, 1915, 415.
Originally described from Aru Islands and subsequently recorded from Dutch
New Guinea by Edwards. Papua: Kokoda, 1,200 feet, April, September and
October 1933 (L. E. Cheesman). (PI. iv, fig. 7.)
CLEITAMIA Macquart.
Suites a Buffon, Diptéres, ii, 1835, 440.
This genus, the species of which are usually distinguished by the conspicuously
black-marked wings with hyaline streaks or spots, is very well represented in
New Guinea and below I present a key to the species referable to it, some of
which are known to me only from descriptions. Hendel in his paper on Platy-
stominae (Abhandl. Zool.-botan. Ges., viii, 1914, 123) presented a key to 14 species,
which list is considerably enlarged herein.
Key to the Species.
1. Scutellum with four marginal bristles, the basal pair sometimes weak and hair-
Tei tecercis sn Sarseac eae aocanaielv cess eka rec TN ele aoe ek Renate ay ARM re tenet Soak sabe wensehraeepey oy cuicbendtcn av omesaine har Sys 2
Seutellum with six strong marginal bristles; fourth wing-vein beyond the outer
cross-vein usually markedly upwardly curved to before middle of apical section,
then sloping down to wing-margin .................. Giehased taectsaston boReacnEuaae ORs 12
2. Wing brownish-black, with three wedge-shaped hyaline streaks on the costa, one
before the apex of the subcostal vein that extends over the wing to second vein
near its furcation with third, two others between apex of subcostal vein
and that of first vein that extend backward over third vein, three hyaline streaks
on apical half, the anterior one extending diagonally from below the apex of
second vein to apex of the first posterior cell, the central one extending from
behind middle of the inner cross-vein to and including most of apical half of
second posterior cell, and the third extending from the lower half to inner
cross-vein over the discal cell to the hind margin of wing, angulate on fifth
vein, and a hyaline streak along the anal margin to apex of fifth vein ........
RR) A a Ae TES nO Bio aco CR AIG lolG. co Wololcith ciate o tib Sionted car Cie cies catharinae de Meijere*
*In 1915 (Tijdschr. v. Hnt., lviii, 129) de Meijere placed this species as a synonym
of tricurvata Walker, but there does not appear to be a great similarity in the descriptions
and I leave the matter as presented in the above key until a comparison of the types
is made.
108
10.
11.
12.
12a.
DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
Both the cross-veins of the wing enclosed in a large broad black mark or spot .. 4
Both the cross-veins of the wing not enclosed in a single large black mark or spot,
Or scoverecdapyasanuneay DlACK eS trea Ke rpemeieyedeckeveieley = cisicreveioiecchekeuele\sauoneucnedcreneleie 9
The large black spot over the cross-veins extending over the entire width of wing
fromthe COstanLOutne DIN deManeiniee ides clewakeweisicletehelre amabilis Osten-Sacken
The above black spot or mark not reaching the costal margin or only so as a mere
VAMC} 2 sexssyievcnens vogeitou coke Hee ewee oie MMT OUCR ode 25 WOLONS Takes acs acah Sus oe oie aus vance soot iain: Sipaeonebet Reh aoker eno 5
No black streak emanating from the apical border of the large discal spot, the
only dark mark beyond it consisting of a narrow costal streak that is not
connected nwithysthe mar ees tSDO ti mercuele eversiensie eiclioite\eve te (olla ive) GeTORcG Cid one eC nO Dao cROaaaare (ond Gt Grohe c io cling Hickok rosa oi magnifica Hendel
BREA DISCALIS Walker.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 117.
Described from Aru Islands and not subsequently reported.
BREA DISCIFERA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 270.
Described from Key Island from a single female.
Most nearly like magnifica, differing as noted in the key to species.
BREA FLAVIPES de Meijere.
Nov. Guin., ix, Zool., livr. 3, 1918, 371; Hendel, Abhandl. Zool.-botan. Ges., viii,
1914, 272.
Described from one female from Biwak Island, New Guinea.
Similar to magnifica in most respects, differing as noted in the key ae in
having the tibiae dark brown except their apices and the apical half of the fore
femora also dark brown.
Hendel suggests the possibility that this is discalis, though Walker says that
there is a ‘blackish line’ over the outer cross-vein, which would hardly equal the
broad black fascia present in flavipes.
BREA CONTRARIA Walker. PI. iv, fig. 21.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 117.— Maria caeruleiventris Bigot, Rev. et
Mag. de Zool., 1859, 311.
This species was originally described from New Guinea and recorded from
Aru Is. It has the legs more extensively black than any of the other species
BY J. R. MALLOCH. 125
and is readily distinguished from any of them by the wing markings. MHalteres
black-brown.
A large series of both sexes, Wewak, New Guinea (F. H. Taylor).
BREA MAGNIFICA Hendel. PI. v, fig. 22.
Abhandal. Zool.-botan. Ges., viii, 1914, 271.
Originally described from a single male taken in New Guinea.
Hendel states in his key that the “four hind legs” are entirely yellow, but
in his description he gives the bases of all tibiae as black-brown. The latter
statement is correct for most specimens of the male sex, but the apices of the
mid femora are in all females more or less distinctly blackened, and in a few
specimens the greater part of the mid femora is black. The different wing
markings are sufficient to distinguish it from any other species of the genus. The
costal edge between the apices of the third and fourth veins is narrowly browned,
which is not the case in contraria.
A large series of both sexes, Wewak, New Guinea (O82 H. Taylor).
BREA RALUMENSIS Enderlein.
Mitt. Zool. Mus. Berl., xi, 1924, 129.
This species was described from a single female from Ralum, New Britain.
It was merely distinguished from contraria by a few characters, of which the
following appear to be the most important: Mesonotum with three slender vittae
of yellowish-brown tomentum (white in contraria), fore coxae and fore femora
brown (yellow in contraria); of the brown basal fascia there is only a small spot
on the fork of the radius. :
It may be a variety of contraria, but I have seen no specimen that appears to
agree with it from New Quinea.
BREA BASILIS Enderlein.
Op. cit., xi, 1924, 129.
This species apparently falls with discalis and discifera in the foregoing key.
It differs from both in having the mesonotum black, with thick yellowish-grey
tomentum; there is no mention of vittae in the description. The legs are ochre-
yellow, mid and hind tibiae brown, and the fore tibiae somewhat brownish. Length,
7-5 mm.
North-east New Guinea.
I have seen no species that agrees with this one.
PTEROGENIA Bigot.
Rev. et Magas. de Zool., (2) xi, 1859, 312.
Species of this genus have been recorded from the Straits Settlements,
Sarawak, Borneo, Batchian, Molucca, Aru, Java, Formosa, Ceylon, the Philippine
Islands, New Guinea, and Australia. Hendel keyed 14 species and included 13
additional species described by Walker that he tentatively assigned to the genus
in his large paper on the Platystominae. The New Guinea and Australian species
may be distinguished as in the key given below.
A striking character of the species before me is the presence of short stiff
hairs on the upper side of the stem vein of the wing at its base as in Huprosopia.
Key to the Species of New Guinea and Australia.
1. Scutellum black, with the margin pale yellow 2
Scutellum entirely black or dark brown 3
126 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
2. The preapical dark fascia on the wing meeting the dark cloud over the outer cross-
vein; the small hyaline costal spot through stigma extending to third vein; palpi
MOKA EN EHO cogaoone FOodbe oo bonso Ss sobageanoD ooo dC DEO pectoralis Hendel
Preapical dark fascia on the wing not meeting the dark cloud over the outer cross-
vein; the small hyaline costal spot through stigma not extending over second
VEIN Palpi eEncirely. VSllO ws yer lee oneisie cele eels) =) «\-lleledelele lise) elo eee similis, n. sp.
3. Thorax entirely shiny black; aristae with very long hairs; palpi blackish-brown ....
WARIO CTOs Cid ao sob dino Daya Cod clan Uo dio gin si cd 0 OO Oona OG ‘.,..... fuliginosa Hendel
Thorax partly red or yellow; aristae moderately long-haired; palpi red, apices
aig Fear gays haere es on Big Biers gio oie DIO UDI Oa ODO d cadoomoG GoM wea odin occ Oo 4
4. Frons and mesonotum black-haired; face and lower occiput blackish-brown ......
ECC SEY. TAR. SEY cece. ctl ches aictciearectatecet tehate: PemetaveMaycRatehe (ehehet ot. nubecula Hendel
Frons and mesonotum golden-haired; face and lower occiput red .. latericia Hendel
PTEROGENIA PECTORALIS Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 316.
Described from Bogadjim (Stephansort), New Guinea. I have seen one
specimen from North-east New Guinea (Kaiser Wilhelmsland), and one, Papua:
Kokoda, 1,200 feet, August 1933 (L. H. Cheesman).
PTEROGENIA SIMILIS, N. Sp.
3, 9. Similar to pectoralis, but the wing pattern is different, the frons
narrower, the legs preponderantly yellow as in the variety of pectoralis described
by Hendel (Abhandl. Zool.-botan. Ges., viii, 1914, 316).
Type, male, Kuranda, Queensland (Dodd).
PTEROGENIA FULIGINOSA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 309.
This New Guinea species is not known to me except from the description.
Described from Maroka, New Guinea.
PTEROGENIA NUBECULA Hendel.
Op. cit., viii, 1914, 314.
Described from Burpengary, Queensland, and New South Wales.
I have two specimens from Kuranda, Queensland, sent to me by Mr. F. H.
Taylor. It may occur in New Guinea.
PTEROGENIA LATERICIA Hendel.
Op. cit., viii, 1914, 312.
This form was considered doubtfully distinct from nubecula by its describer.
I have seen no specimen that has golden hairs on the mesonotum, but occasionally
in this and related genera teneral specimens have the hairs yellowish instead of
black as in the mature individuals of the same species.
Queensland.
NEOHEMIGASTER, 0. N.
Hemigaster Rondani (nec Brullé), Ann. Mus. Civ. Stor. Nat. Gen., vii, 1875, 431.
This genus is distinguished from Pterogenia by the following characters: Base
of the stem-vein of the wing bare above, lateral angles of the clypeus more or less
produced downward and with a small rounded elevation on the dorsum, vertex with
four strong bristles, humeral bristle present. The humeral bristle is not always
present in Pterogenia, and while the antepenultimate section of the fifth vein is
either bare or setulose in that genus, in all species of Neohemigaster it is setulose.
The apex of the second abdominal tergite and usually to a lesser extent the base
of the third in all species of the latter is compressed in centre and furnished with
a sharp keel-like elevation.
BY J. R. MALLOCH. 127
This last character is met with also in Tropidogastrella Hendel, but in the
latter the third antennal segment is much longer, reaching to or beyond the
epistome, and the structure of the face and prelabrum is different. Despite the
removal of this genus so far from Pterogenia in Hendel’s key to the genera, it is
closely related to both the genera now under discussion.
I have proposed the new name Neohemigaster for Rondani’s concept, with the
same genotype.
NEOHEMIGASTER ALBOVITTATA Rondani.
Op. cit., vii, 1875, 431.
I identify as this species a male from Sandakan, Borneo, sent me some years
ago by the late C. F. Baker.
Although no species known to me from New Guinea is referable to this genus,
there may be such that are as yet unknown to me, and the acceptance of the genus
contrary to Hendel’s action, who placed the genotype in Pterogenia, appears to
justify the inclusion of the above data in this paper.
I have seen two additional species of the genus from Sibuyan Island.
CHAETORIVELLIA de Meijere.
Nov. Guin., ix, Zool., livr. 3, 1913, 376.
A monobasic genus, distinguished from its allies by the single pair of strong
orbital and vertical bristles, the very short antennae which are not half as long
as the face and inserted at the middle of the eye in profile, the plumose aristae,
lack of humeral, anterior notopleural, supra-alar, and prescutellar acrostichal
bristles. Scutellum haired, with four marginal bristles.
CHAETORIVELLIA TRIFASCIATA (Doleschall).
Natuurk. Tijdschr. v. Nederl. Ind., xvii, 1858, 121 (Ortalis)—Ortalis
punctifascia Walker, Jour. Proc. Linn. Soc. Lond., vi, 1862, 15.
A small glossy blue-black species, with black head on which there is a silvery-
white stripe round the eye-margins; antennae and palpi and lower half of face
brown. Pleura with a silvery central vitta. Basal two segments of all tarsi orange-
yellow. Wings whitish-hyaline, with three dark brown fasciae as follows: a short
one from the humeral cross-vein to the anal cell, a broad complete one filling the
area between the apices of the subcostal and first veins that encloses a small
hyaline spot on the costa at the middle of the stigma, and a third one much
narrower from the costa between the apices of first and second veins to fifth vein
and enclosing the outer cross-vein which sends an equally wide streak along the
costa to the apex of the fourth vein. -
Recorded from New Guinea, Djilolo, Molucca, and Amboina (type locality).
One female, Papua: Kokoda, 1,200 feet, August 1933 (L. E. Cheesman).
SCHOLASTES Loew.
Mon. N. Amer. Dipt., iii, 1873, 38; Hendel, Abhandl. Zool.-botan. Ges., viii, 1914,
248; Curran, Proc. Cal. Acad. Sci., xxii, ser. 4, no. 1, 1936, 23.
The robust habitus, haired aristae, strong orbital and sternopleural bristles,
the subtriangular, quite densely short-haired scutellum with its six marginal
bristles, and the almost invariable yellow sublateral lines on the mesonotum and
marginal yellow line on the scutellum readily distinguish this genus from others
in the family.
Hendel recognized 6 species, and in 1936 Curran described 3 additional species.
I give below a key to those species known to me, and notes on some others ee <
those that they are apparently most closely related to.
128 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
Key to the Species.
1. Supra-alar bristle lacking; mesonotum with almost invariably four pairs of dorso-
central bristles, the anterior one at or slightly in front of the suture; arista
of male with, that of female without, an apical palette; first wing-vein setulose
Onca aLt. OL tse basal naltsbelOwemcrierleietsterere crete riers nyo aeroieienee cinctus Guérin
Supra-alar bristle present; niesonotum with 3 or 2 pairs of short dorsocentrals,
all qpostsutubalisficess £5. dead ao Siete ee Restos ole op folleifols eR ERE EPEC ich Dare eam aoe nG Cece a ta by Cone caine ain ia eure: EO SiS tt Ue nM er SER Car, 12a
Wing never with such large basal mark, but with two or three smaller dark spots
OM -the) Cross=vVelnss and LAGU Sheds eter eterstel cue. comet at «ew ses ears eleven el cysy/sl ome lle ehewe 13
Preponderantly metallic-blue species; scutellum with 6 bristles; inner cross-vein
near) middlevof discal! Cello santas cere o Side ees coils ce arebee basalis Walker
Brownish-yellow species; scutellum with 2 bristles; inner cross-vein less than
OMS ove! rrroyen Eyoyese Ore Chisel CA ooodacnoudooonudnoouubeonDoSs decolor, n. sp.
140 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
13. Both the cross-veins brown-clouded; thorax and abdomen metallic-green, shagreened
and with fine yellow hairs; fore femora green, fore tarsi black .-.. laeta Walker
@uter cross-vein not dark-clouded .......5 22.5.0. s0s cece cnc e case e snes sevevcese 14
14. Wing with a dark brown costal spot above the level of the outer cross-vein and
two others proximad of it on the costa; squamae dark brown ............. 15
Wing without a dark costal spot above level of the outer cross-vein, with only
two dark costal spots; squamae pale ...........-..--+ee-- eee e rete eeee 16
15. Only the inner cross-vein dark clouded; legs entirely reddish-yellow .......... 15a
A short dark streak from the costa to and enclosing the inner cross-vein; bases of
fore: FemorayanG suhemtanrsioaplaGke wer erie fep-lene -l-ta)sleB- lV maculipennis Macquart
15a. Gena one-third as high as eye; prelabrum very exposed; scutellum bare except for
CHevmMaTreinalsPVIStlesmerereierere es eteley elton lone) reba luake doa -aaarol= macrocephala Hendel
Gena not more than one-fourth as high as eye; prelabrum quite prominently
exposed; scutellum strongly haired and with six marginal bristles ........
OG. Sr BO OC CHICO On OG OIG CUD Gy COCRO er oncacee Th ck OTOrOrS (orcad cen fulvipes, n. sp.
16. Dorsum of thorax, scutellum, and abdomen, glossy, bare, reddish-brown; pleura
WAGON AL O56 Boo Dato od co Oo dO Cg aoe GOING FO tho tigre 5 dd Gd Guo hi clo abet costalis Walker
Thorax and scutellum black, shiny, abdomen greenish-black ...................
Be SOOO Ot ood UO Oo Ore O hette COCOE COO ciao a Otho ornEn Ue trisignata van der Wulp
17. Wing with three dark brown costal marks; legs entirely yellow; scutellum bare ....
sisi © ete he Sea whe Aaa ceis thts fees EEGs TELSTRA LUE LEE SSAMA SARAIA Ge Bateret ats Seeheoai akg rufipes Hendel
Wing with four dark marks on the costa; tarsi more or less blackened ........ 18
1. Oye CHONG CEAROCUCEG! soo60neoo0KdUnCOU KD a DOO KaOO OU DOD OUND ODDUDOGCUC 19
Outer cross-vein not dark-clouded; basal dark wing-spot not extending to costa;
thorax and abdomen blue-black; legs yellow ........... pumicata van der Wulp
Gs eros pleura anaes seredaish=VellOwaerereiederei-icouseasanicietcncno lll) oten sol kekaia i Repol-l-l-holor- 20
Frons dark brown to black; mesonotum steel-blue, with a short yellowish-white-
dusted vitta over the upper half of each humerus extending to suture, and a
similar one along the upper edge of each pleuron; abdomen violet-black
Pogo GOD Oo OOS OCI ci ner Gite er Orcic Crone crcl oro oreo chare: the olceorc quadrilinea Walker
20. Apical and basal dark spots on the wing very large, the latter extending from
SUDCOStanLOMUHesanalaveinun erection eerie re t-iek ren Ean lel severa Hendel
Basal spot on the wing small, extending from posterior basal cell to inner cross-
veinsrapicaluspot slender, Giffuse))-)-\-cyejyeu-iel- donene ere ote cold ster taeniata van der Wulp
LAMPROGASTER (CERATOPELTA) PATULA Walker.
Jour. Proc. Linn. Soc. Lond., v, 1861, 247.—L. bispinosa Walker, op. cit., viii,
1865, 118.—Ceratopelta tricolor Bigot, Bull. Soc. Ent. Fr., viii, ser. 5, 1878, 35.
A reddish-yellow species with entirely pale legs and yellowish-hyaline wings,
the costal margin deeper yellow, the dorsum of abdomen usually largely steel-blue.
The frons, genae, mesonotum, scutellum, and pleura, generally with microscopic
black dots on parts of their surfaces. Antennae not extending to lower level of
eyes; arista short-haired to beyond the middle; vertex with four bristles.
Mesonotum black-haired, pleura largely yellow-haired, the hairs rather long and
dense. Bristles as follows: 1 humeral, 2 notopleurals, 2 postalars, 1 pair of dorso-
centrals and one mesopleural; the prescutellar acrostichals undeveloped. Scutellum
stout, convex, the two tubercles with minute black apices; some of the marginal
black bristles on small elevated bases; disc rather long-haired. First posterior
cell of the wing narrowed at apex; inner cross-vein slightly dark-clouded. Abdomen
broadly ovate, convex on dorsum, fifth tergite of male nearly twice as long as
fourth, and with rather long stiff hairs. Length, 12-14 mm.
Dutch New Guinea: Lake Sentani, August 1936, one male (L. E. Cheesman).
Originally described from New Guinea. Enderlein recorded it from Dutch New
Guinea and accepted the genus as valid. I incline to accept Ceratopelta as a
subgenus and so treat it here.
BY J. R. MALLOCH. 141
LAMPROGASTER (LIOLAMPROGASTER) GRACILIS Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 225.
This species, costalis Walker, and angusta Enderlein were placed in a new
generic concept by Enderlein, the characters used for the segregation being the
lack of hairs on the dorsum of the thorax and abdomen, and the slender form,
especially of the abdomen. The designated genotype is angusta. ‘This species is
unknown to me, was very briefly described, and the type locality is Ternate, so we
may ignore it here.
I have a male and female that I refer to gracilis. The female is considerably
darker than the male. In the latter the humeri, lateral margins of the mesonotum,
the scutellum and most of the pleura are tawny-yellow, with many microscopic
black dots, while in the female these parts are almost entirely blackish-blue. The
mesonotum is not entirely bare in the disc, but has a double series of microscopic
fine hairs down the centre, and there are some hairs on the sides. The face and
prelabrum are fulvous-yellow and speckled with black in both sexes.
As stated by Hendel, the occiput projects behind the eyes in profile more
than in the other species of the genus, being as wide above as the parafacial,
but whether this character is maintained in the other two species I am unable to
state.
The wings are yellowish-hyaline, with a more distinct yellow tinge along the
costa as far back as the third vein to its apex. The first posterior cell is not
narrowed at its apex.
Papua: Kokoda, 1,200 feet, May, Sept—Oct. 1933 (L. E. Cheesman). Originally
described from Astrolabe Bay, New Guinea.
Both my specimens lack the humeral and mesopleural bristles, and I can detect
only one pair of verticals.
LAMPROGASTER (LIOLAMPROGASTER) COSTALIS Walker.
Jour. Proc. Linn. Soc. Lond., v, 1861, 247; Osten-Sacken, Ann. Mus. Civ. Stor.
Nat. Gen., xvi, 1881, 472; Hendel, Abhandl. Zool.-botan. Ges., viii, 1914, 231.
Osten-Sacken states that Walker’s description is “recognizable”, but considers
that the species seems to be closely allied to superna Walker and quadrilinea van
der Wulp, the former of which was unknown to Hendel. I have not seen either
of those species.
Hendel states that the dorsa of the thorax and abdomen are bare and, as
Enderlein had apparently seen neither angusta Hendel nor costalis, it may be
assumed that he placed them in his new genus Liolamprogaster on the basis of
Hendel’s statement to that effect. Hendel makes no mention of the occiput being
convex and it may be assumed to be as in typical species of Lamprogaster. The
wing has three short brown streaks on the costa, the outermost one being above
the level of the outer cross-vein.
Hendel described a variety nuda which differs from the typical form in lacking
the two grey-dusted pleural vittae, in having the apex of the scutellum almost
transverse, and a slight dark cloud on the outer cross-vein.
Described from New Guinea. Recorded from Dorey (0O.S.), and Huon Gulf
(Hendel).
LAMPROGASTER (LAMPROGASTER) ZELOTYPA Hendel.
Op. cit., viii, 1914, 226—L. ventralis Walker, Jour. Proc. Linn. Soc. Lond., v,
1861, 248.
I give the above citation from Hendel’s paper on the group without comment.
142 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
A glossy fulvous-yellow species, with yellow or fulvous hairs and bristles,
and yellowish-hyaline wings, with a less markedly intense yellow costal border
than in gracilis, the yellow colour not extending very noticeably over the second
vein. There are no microscopic black specks on the head and thorax as in gracilis.
The upper occiput is much narrower in profile, the vertex has four fine dark
bristles, the mesonotum and scutellum are quite densely short-haired, the latter
has 4 marginal bristles, the humeral is lacking, but the mesopleural is present.
Dorsum of the abdomen rather densely short-haired.
Papua: Kokoda, 1,200 feet, August 1933 (L. E. Cheesman). Recorded pre-
viously from Dorey, New Guinea, and Australia.
The variety of this species listed in the key is from Cairns, Queensland.
LAMPROGASTER (LAMPROGASTER) GROSSA, N. SD.
¢. A large robust species of a general yellowish-brown colour, with fuscous
frons, the thorax appearing darker brown because of the presence of many minute
black dots visible only under a strong lens, the abdomen infuscated, especially
apically, and no trace of any metallic sheen. Wings yellowish-tinged, darker
basally, the inner cross-vein and the stigma brown-clouded.
Frons at vertex about two-fifths the head-width, almost parallel-sided and
about 1:25 times as long as wide, with many short pale surface hairs, the orbits
narrow, densely yellowish-grey tomentose, which tomentum is carried down on
the paratacials, narrowing below; vertex in type specimen with 6 fine black bristles,
the inner pair duplicated. Antennae hardly more than half the length of face,
third segment fully three times as long as wide; arista pubescent on basal half,
simple at apex; palpi longer than antennae, slender. Facial carina with sharp
edges, the foveae deep; prelabrum poorly developed, not heavily chitinous. Gena
about half as high as eye. Face and genae black dotted, the latter with blackish
marginal line; occiput narrowly visible above in profile; parafacial in profile wider
than third antennal segment.
Mesonotum in type specimen with the black dots lacking on four wide
contiguous vittae, the central pair not attaining posterior margin, rounded at
extremities; surface quite densely covered with short decumbent black hairs;
bristles as follows: 1 humeral, 2 notopleurals, 2 postalars, and 1 pair of dorso-
centrals. Scutellum slightly convex above and rounded in outline, with many
short black discal hairs and six marginal bristles. Pleura partly black dotted,
pale haired; mesopleural bristle of moderate length.
Wings large, veins brown, yellow clouds in cells of basal half. Fourth vein
near base of discal cell slightly angulate and with a short spur vein on its
anterior edge; inner cross-vein a little beyond middle of the discal cell; fourth
vein very slightly bent up beyond outer cross-vein. Squamae and halteres pale
brown. Legs rather stout, brownish-yellow, all the tibiae with a brown dorsal
line. Fore femora without posteroventral bristles. Abdomen short ovate, blackened
apically. Fifth tergite about as long as the third and fourth combined. Length,
13 mm.
Type, Dutch New Guinea: Cyclops Mts., Mt. Lina, 3,500 feet, March 1936
(L. E. Cheesman).
LAMPROGASTER (LAMPROGASTER) QUADRILINEA Walker. PI. v. fig. 29.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 111.—L. sepsoides Walker, op. cit., vii,
1864, 220; Hendel, Abhandl. Zool.-botan. Ges., viii, 1914, 242.
A metallic black-blue species, with three narrow black costal streaks, the basal
one not extending to costa, the middle one at the stigma and enclosing the inner
BY J. R. MALLOCH. 143
cross-vein, and the outer one above level of the outer cross-vein, a narrow black
edge from midway between apices of second and third veins to apex of fourth, a
narrow cloud over the outer cross-vein, and a spot on cross-veins at base of discal
cell that connects with a basally directed streak in basal half of anterior basal
cell. The mesonotum is closely piliferous-punctate, the very short depressed pile
black, and has a yellowish-white-dusted vitta over the upper half of each humerus
extending to the suture, and one on upper edge of the pleura; scutellum slightly
alutaceous, not punctate, bare on disc, with a few fine hairs and four or six
weak bristles on sides, the apex truncate. Mesopleural and humeral bristles
lacking. Legs black, mid and hind tibiae and tarsi largely brownish-yellow, fore
femora sometimes brownish at bases.
New Guinea: Wewak (F. H. Taylor). Thirteen specimens; two pairs taken
in copula. Western New Guinea: Njau-limon, south of Mt. Bougainville, 300 feet,
February 1936; Eastern Dutch New Guinea: Jutefa Bay, sea level, 100 feet,
February 1936, four specimens (L. HE. Cheesman).
Originally described from Aru Island, and recorded from Mysol, Waigou, and
New Guinea.
LAMPROGASTER (LAMPROGASTER) SEVERA Hendel.
Op. cit., viii, 1914, 240.
Originally described from New Guinea and not since recorded.
Scutellum bare.
LAMPROGASTER (LAMPROGASTER) MACULIPENNIS Macquart.
Dipt. Hxot., Suppl. ii, 1847, 89.
This Australian species may be found in New Guinea.
LAMPROGASTER (LAMPROGASTER) TRISIGNATA van der Wulp.
Tijdschr. v. Ent., xxviii, 1885, 231.
Described from New Guinea and not seen by Hendel. Unknown to me.
LAMPROGASTER (LAMPROGASTER) AUSTENI Sharp.
Zool. Res. on material from New Britain, etc., Cambridge, Arthur Willey, pt. iv,
1900, 391.—Lamprogaster xanthoptera Hendel, Abhandadl. Zool.-botan. Ges., viii, 1914,
225.
I have arrived at the above synonymy after a careful examination of a
long series of specimens from the Solomon Islands submitted to me by Sir Guy
A. K. Marshall of the Imperial Institute of Entomology and a comparison with
a specimen from New Britain, the type-locality.
There can be no doubt as to the correctness of the aeretrnietion: though
it is in only a few cases possible to see the large sack-like abdominal expansions
of the abdomen described and figured by Sharp in his paper. In one female,
however, these are widely exposed and agree well with Sharp’s figure.
LAMPROGASTER (LAMPROGASTER) RUFIPES Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 233.
Scutellum bare.
Described from New Guinea, Key Island.
LAMPROGASTER (LAMPROGASTER) PUMICATA van der Wulp.
Tijdschr. v. Hnt., xxviii, 1885, 230.
Described from New Caledonia. Unknown to Hendel and myself. May occur
in New Guinea.
144 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
LAMPROGASTER (LAMPROGASTER) BASALIS Walker.
Jour. Proc. Linn. Soe. Lond., v, 1861, 248—L. limbata van der Wulp, Tijdschr.
v. Ent., xxviii, 1885, 228.
I have before me two specimens that agree very well with the description of
this species, though they ‘have not the mesonotum, scutellum, and abdomen particu-
larly long black-haired as stated by Hendel.
The mark on the anterior half of the base of the wing up to and including the
inner cross-vein is quite dark brown, and beyond that point on the costal margin
back as far on to the field of the wing as the third vein and to the apex of the
latter there is a distinct yellow streak. The thorax and abdomen, except the apex
of the latter and the pleural sutures, are glossy metallic-blue. In the female before
me the legs, except the mid and hind coxae, are orange-yellow, while in the male
the femora all have a blackish streak on their basal half or less on ventral surface.
The vertex has 4 strong bristles; the humeral and supra-alar bristles are
lacking; the scutellum has six marginal bristles and, like the mesonotum, is rather
long black-haired on the disc. Inner cross-vein a little beyond middle of the discal
cell, the outer one twice its own length from inner one; fourth vein undulated
proximad of the inner cross-vein, highly arched just beyond outer one, then almost
parallel with third to its apex.
Known only from New Guinea. East Dutch New Guinea, Jutefa Bay, Pim, sea-
level to 100 feet, February 1936 (L. EH. Cheesman).
I have no doubt about the synonymy given above, though Hendel kept the
species separate. He did not have limbata before him and merely quoted van der
Wulp’s description.
LAMPROGASTER (LAMPROGASTER) DECOLOR, 1. Sp. PI. v, fig. 30.
Q. Very similar to zelotypa in general colour, the blue metallic sheen not very
conspicuous on the fulvous-yellow ground-colour, most evident on the pleura. The
main differences between the two lie in the presence of a brown cloud over the
base of the wing from costal margin to anal vein and extending to apices of first
posterior and anal cells, most noticeable on the cross-veins at the apices of these
cells, a faint brown cloud over inner cross-vein, the more approximated cross-veins,
which are usually separated by less than the length of the outer cross-vein. The
genae are also much darkened, usually dark brown. The vertex has four bristles
in both species, very small and fine in decolor, and in the latter there are but two
marginal bristles on the scutellum. The thoracic bristles are also darker than in
zelotypa though not black. Length, 7-11 mm.
Type and 7 paratypes, Wewak, New Guinea (F. H. Taylor).
LAMPROGASTER (LAMPROGASTER) STENOPARIA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 227.
This species has much in common with basalis Walker, but the wing markings
to the apex of the costal streak, including a conspicuous cloud over the outer
cross-vein, are dark brown.
Originally described from North Queensland and very possibly will yet be
found in New Guinea.
LAMPROGASTER (LAMPROGASTER) ELONGATA van der Wulp.
Tijds. v. Ent., xxviii, 1885, 228.
A common species in New Guinea though not in this collection. Recorded
also from Key Island and Molucca. Papua: Itikinumu Plantation (F. P. Dodd).
BY J. R. MALLOCH. 145
LAMPROGASTER (LAMPROGASTER) MACROCEPHALA Hendel.
Abhandl. Zool.-botan. Ges., vill, 1914, 230.
This species is described by Hendel as the most robust species known to him,
with an exceptionally large head. It must resemble grossa described herein, but
the parafacial is wider, about twice as wide as the third antennal segment, and
the gena is more than half as high as the eye. In addition to these differences
the scutellum is bare on disc, and the wing has a large black-brown mark on the
base and the inner cross-vein blackened.
Described from New Guinea and not known to me except from the description.
LAMPROGASTER FULVIPES, hn. sp. Pl. vy, fig. 31.
¢. Head brown, frons pitchy-black, shiny, with yellowish-dusted line on each
side widened in front and carried down over the parafacials, the latter and the
genae dark brown, the parafacials glossy on anterior edges. Frons subquadrate,
almost half as wide as head; vertex with four moderately strong bristles, the
short glossy upper orbits with a bristle; surface hairs short and dark. Face
produced slightly below, concave centrally in profile, with irregular transverse
striae on upper half. Antennae extending to below middle of face; aristae short-
haired to near middle; palpi reddish-yellow, slightly club-shaped, with some
fine black bristles on sides. Thorax metallic-blue, without vittae or dust on
mesonotum, the pleura slightly brown-dusted. Mesonotum and scutellum with
quite dense depressed stiff black hairs, longer on the sides. Humeral, both noto-
pleurals, the supra-alar and postalar bristles present, mesopleural fine but distinct;
scutellum short, thick, rounded in outline, convex on disc. Legs fulvous-yellow,
without exceptional structure or armature.
Wings yellowish, as usual more distinctly so costally, with a rather faint
blackish streak from over inner cross-vein extending towards costa, most marked
on the former, and a small dark brown mark on fork of second and third veins;
stigma brownish-yellow. Inner cross-vein close to middle of the discal cell;
venation as in pseudoelongata Malloch, second vein in type specimen with a few
setulae on upper side on basal half (Pl. v, fig. 31). Squamae and halteres
brownish-yellow. Abdomen deep metallic-blue, glossy, with rather long black hairs.
Length 7-5 mm.
Type, New Guinea: Marprik (J. R. Rigby and C. M. Deland). Type in the
collection of the School of Public Health and Tropical Medicine, University of
Sydney.
LAMPROGASTER LAETA Walker.
List Dipt. Ins. Brit. Mus., pt. iv, 1849, 805 (Chromatomyia).
Hendel placed this species in his key to the species of this genus, but stated
that he believed it belongs to Duomyia. It is an Australian species and he is
probably correct in his conclusion, though I have not seen the insect.
LAMPROGASTER (LAMPROGASTER) TAENIATA van der Wulp.
Tijds. v. Hnt., xxviii, 1885, 229.
Described from Molucca and not known to Hendel or myself,’ except from
description.
HKuUPROSOPIA Macquart.
Dipt. Hxot., Suppl. ii, 1847, 89.
In 1881 Osten-Sacken proposed the generic name Notopsila to supplant
Pachycephala Doleschall, the latter name being preoccupied, the genotype named
M
146 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
being mohnikei Doleschall. In 1924 Enderlein proposed for this same concept the
name Oncoscelia, again as a substitute for Pachycephala, apparently having over-
looked Osten-Sacken’s previous action. In 1931 I dealt with this matter briefly
and, in addition, singled out certain segregates of Huprosopia without proposing
the use of distinguishing names for any of them. Enderlein went farther than
Osten-Sacken and erected the genus Lepidocompsia for the reception of two New
Guinea species, impingens Walker and fusifacies Walker. The characters used to
distinguish this concept consisted of the presence of broad spindle-like scales on
the abdomen, and of long hairs on the entire extent of the aristae. He also proposed
a new genus, Tetrachaetina, for a new species, burgersiana, and E. brevicornis
Hendel, the distinguishing character being the 4-bristled scutellum. His new
species was from New Guinea (see under innocud, Nn. sp.).
It must be obvious that the proposal of new genera, on the basis of characters
such as those listed and used by Enderlein for his new concepts in a genus that
contains such a large number of species with all sorts of combinations of these
and similar characters, places no limit upon the number of genera that may be
suggested except the number of species involved. The application of such criteria
necessarily renders valueless such generic concepts insofar as indices to relation-
ships are concerned. I therefore do not make use of Enderlein’s genera herein.
Below I present a key to the species of Huprosopia from New Guinea.
Key to the Species.
1. Thorax dull brownish-black, with five golden-yellow vittae, three on the mesonotum
and one on each pleuron; the abdomen brownish-black, with a dorsocentral
Parawel-sidedebrigiit, VellOow wilttaie neces cl ocis chelaievatensranel ileus cieisicheetoncica ey wen cnelewenene »
ihhorax and sabdomen not vittate with brichteyellow mice cmc cede coin os ce ences 3
2. Wing greyish-hyaline with three narrowly separated black or brown fasciae on the
apical half that are fainter and slightly attenuated behind, the basal one
connected near the costa with a streak from base of wing in the subcostal cell
and the preapical one connected with an apical blackish spot; aristae of the
male slightly widened at apices; vertex with two bristles .. tigrina Osten-Sacken
Wing with numerous small fuscous spots basally, becoming more numerous to middle,
and from there to apex the membrane dark brown, with a few transverse
linear hyaline streaks in the field, two séries of the latter forming slightly
interrupted fasciae between the outer cross-vein and the tip; aristae of male
hair-like at apices; vertex with two bristles and two short fine hairs .....
SG. ORE Os CEG. Pit CRE R AR CCRC Ot Gsc, ACRE cio cuchioe aiohe ae soe ce ecrecatcT cso OL aR as aureovitta, n. sp.
Scutellum more or less distinctly emarginate or concave at apex; abdomen yellowish-
red in ground-colour, with ochre-yellow dusting; inner vertical bristles lacking,
outer pair very small; aristae haired, not spatulate at apices in male; scutellum
with G=mareinal: DTISGlESR SE. kre cite ene teetore ie Oneiie eetene touches rufiventris Hendel
Scutellum regularly rounded at apex; abdomen black or blackish-brown ........ 4
4. Wings dark brown, with many small hyaline or yellowish transverse marks in the
cells extending in most cases entirely across the cell, sometimes almost or
entirely divided centrally and then forming two series of small spots against
cs
the yeins; small species usually much less than 7 mm. in length .......... 4a
Wings either hyaline with entire or broken dark fasciae, or with brown or black
spots; species normally much more than 7 mm. in length .................. 7
4a. Only 3 or 4 hyaline marks in first posterior cell, which extend entirely across the
cell; fore femur (2) with 2 or 3 short stout preapical bristles on the postero-
ventral surface; fifth vein bare above; prescutellar acrostichals lacking; pleura
withoutiyellow=dustedizvittaen sat. eae iat oie cte Sree minuta, n. Sp.
More numerous hyaline marks in first posterior cell, mainly consisting of small
paired spots opposite each other against the veins; fore femur with some fine
bristles on the apical half or more of the posteroventral surface; prescutellar
acrostichals present; pleura with one or more golden-yellow-dusted vittae ... 5
BY J. R. MALLOCH. 147
5. Fifth wing-vein closely setulose on the entire extent of posterior basal and discal
cells above; pleura with a short golden-yellow vitta on upper margin and a
complete similarly coloured vitta on lower margin of mesopleura; vertex with
four bristles, the inner pair the Shorter ..................... setinervis, n. sp.
Fifth vein not setulose above on entire extent of posterior basal and discal cells:
pleura with a complete golden-yellow central vitta and a short one on upper
margin and a third one on upper edge of the sternopleura ................. 6
Bo WORDS Van MOWE GERM LOWISUIES) vo 6 coo ono oc no Dood obo O ODO mo OOD miliaria Hendel
WD. Wald [DUE TO GaPOvs loemswles scoooonuuogdcoonoodooboUDOGIG dubitalis, n. sp.
7. Face with a black or dark brown streak on each side, at least from the antennal
TOWOD, KO. WAG COMMONS “Goooocoocencouoonouaguc bon UDC ooorcosoumEooUHb goo DS 8
Face yellow or grey, without a black streak on each side from antennal fovea to the
EDISTOINC MMPI eer ee es eater reel ch ew epial atresia ep Moe ndc usin sticict ae ishiokze pcp a ate saa ci otredns ate 10
wm
No dark vitta over the middle of the discal cell of the wing; palpi black; scutellum
with 4 marginal bristles; abdomen of the male without yellow lanceolate scales ;
wing with two outstanding dark fasciae among the other markings, the inner
one wide on the costa and falling over the outer cross-vein, the outer one
narrower and not extending to the hind margin, the apex with a rounded black
spot, the basal half with numerous small dark spots in the cells ...........
Beeps EAN BOE ee es Sos MR ee amen ee Ie re ee es ae ee od bilineata de Meijere
A dark vitta extending over the inner cross-vein and the middle of the discal cell
of the wing, other characters of markings not as above ................... )
9. The dark fascia over the outer cross-vein connected with the preapical one before
attaining the hind margin of the wing; inner vertical pair of bristles lacking;
aristae of the male without an apical palette .............. impingens Walker
The two dark fasciae above referred to not connected behind; inner vertical pair of
bristles present; aristae of male with a lanceolate apical palette ...........
RE ee ahs eae REE ene enn chia) feb te TEIN ore Le et dante ric opne sUISneI eM SHER el Loken GRASS vale fusifacies Walker
10. Tarsi entirely black, or at most only the base of the mid metatarsus brownish .... 11
At least all the metatarsi except their extreme tips yellow .................... 3
11. The dark fascia over the outer cross-vein of the wing broken into small spots
costally ; legs except the tarsi yellow, the femora brownish marked on both sides
below at apices; mid metatarsi reddish-brown at bases; fore tibiae of male
with a small brush of short thick setulae at apex on the posteroventral surface
FORCE Orck a Ole chit vs EAC Onn cit AGE Ei A chee eA eR Oe race Pa ah ade ee cs oe penicillata Hendel.
The dark fascia over the outer cross-vein of the wing as in penicillata, but the
femora almost entinelys black rrge ery) poy i ens ee innocua, n. Sp.
The dark fascia over the outer cross-vein of the wing complete ................. 12
12. Mesonotum whitish-grey-dusted, with two broad blackish vittae .................
3.5/0 PRB OAC GIG ORES ELECT Sie tra Se Ain iro ARE RR ee Keir vie See Bee albolineata de Meijere
Mesonotum olive-grey-dusted, with seven narrow indistinct dark vittae
ORG: GO CORT CEA NE TE CR CR ORR ORE ONTO ecu penn Sa oeteE ERA cucCTS ee antck Cac Sache Mere protensa Walker
13. Abdominal tergites with pale brown preapical or central fascia; hind femora slightly
emarginate or concave below centrally ......................... potens Walker
Abdominal tergites with four brown discal spots; hind femora slightly thickened,
not emarginate or concave below centrally .............. ws. ventralis Walker
N.B.—There are several species that occur in Australia and in some of the
adjacent islands that may yet be found in New Guinea. It will thus be necessary
to take these into consideration in making identifications in the genus. One such
species that is closely similar to impingens occurs in the Solomon Islands and
may occur also in the territory now under consideration.
EUPROSOPIA TIGRINA Osten-Sacken.
Ann. Mus. Civ. Stor. Nat. Genov., xvi, 1881, 473.
The golden-yellow vittate thorax is not unique for this species in this genus,
there being several others with that character known to me, but, taken in
conjunction with the dark vittate wing, the characters readily separate it from
any other now before me.
Known only from New Guinea. I have seen specimens, but have none before
me at this time,
148 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
EUPROSOPIA RUFIVENTRIS Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 334.
This is the only species of the group with emarginate apex to the scutellum
known from New Guinea. I have seen one of the group from the Solomon Islands
and several from Malaya.
Described from New Guinea and not subsequently recorded.
EUPROSOPIA MINUTA, n. sp. PI. v, fig. 32.
°. The smallest species of the genus known to me, distinguished from all
the others by the blackish-brown wings with their transverse hyaline markings
in the cells (Pl. v, fig. 32).
Head brownish-yellow, occiput fuscous, with grey dust, frons red on each side
ot central stripe except in front, the orbits and triangle grey-dusted; antennae
yellowish-brown; face with a small dark spot on epistome below and slightly
mesad of each fovea, the prelabrum with a similar spot on each side; palpi orange,
with dark tips. Frons at vertex not depressed, about one-third of the head-width,
a little more than that in front, and about 1:25 times as long as its anterior width;
vertex with four bristles. Antennae about two-thirds as long as face, third
segment about three times as long as wide; arista very short haired on basal
fourth or less. Edges of facial carina not sharp. Gena about one-sixth as high
as eye.
Thorax dull black, quite densely grey-dusted, mesonotum with five dark brown
irregular vittae, submedian pair broken at suture and notched on inner edge
behind suture, the sublateral pair broken at suture. Pleura pale-grey-dusted, dull
black above; scutellum with a large dark brown discal spot. Hairs black, rather
strong on pleura. Bristles as follows: 1 humeral, 2 notopleurals (and some long
setulae at base of the posterior one), 2 post-alars, and a pair of dorsocentrals;
scutellum convex on disc, rounded in outline, with numerous dark discal hairs and
4 marginal bristles. Legs black, hind tibiae centrally sometimes brownish, all
metatarsi except the extreme apices whitish-yellow.
Wings brownish-black, marked as in Plate vy, figure 32. Stigma entirely brown,
nearly as long as the third section of the costa; fourth vein almost straight on
apical section, its tip almost imperceptibly turned up; inner cross-vein at about
one-third from base of discal cell; fifth vein bare above. Squamae brown. Halteres
yellow. Abdomen black, dull, grey-dusted at bases of the tergites. Genital cone
very broadly leaf-like. Length, 4 mm.
Type and 1 paratype, Papua: Kokoda, 1,200 feet, August 1933 (L. BE.
Cheesman).
EUPROSOPIA MILIARIA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 353.—Platystoma pectorale Walker, Jour.
Proc. Linn, Soc. Lond., vi, 1862, 13.—Euprosopia diminutiva de Meijere, Nov. Guin.,
ix, Zool. livr. 3, 1913, 368.
The above synonymy is that given by Hendel in his work on the Platystominae,
but I have some doubts as to the correctness of his deductions. Until I had the
opportunity of examining the present collection I considered there was but one
small species with the peculiar type of wing markings shown for miliaria by
Hendel (Pl. 2, fig. 41). Now I have four very similar species, three of which
are dealt with herein.
Hendel’s species I have been able to determine from his photograph of the
wing and his statement that there are four strong vertical bristles and three
BY J. R. MALLOCH. 149
golden-yellow-dusted vittae on the pleura. One specimen agreeing with these
characters, a male, is before me. It has a lanceolate apical aristal palette, and
there are some very short hairs or pubescence on the basal fifth of the upperside
of the aristae. Hendel gives the aristae as bare. The fifth ventral segment of the
abdomen is furnished with a clump of about 8 downwardly-directed black bristles
on each side at apex, a character found in two of the other closely allied species
of which I have males. The hairs on the underside of the basal section of the
stem vein of the wing are indistinguishable in miliaria, and there are no setulae on
the upperside of the fifth vein along the discal cell, but the latter may have been
rubbed off. The extreme apex of the first posterior cell is dark brown.
Originally described from Isle of Lakes in the Papuan region. One male. New
Britain (Dr. Heydon).
EUPROSOPIA DUBITALIS, nN. sp. Pl. v, fig. 33.
6, 9. Very similar to miliaria as above accepted, differing essentially as
follows: Vertex with but the two outer bristles present: basal section of stem vein
of the wing with short fine hairs below. Both species have a transverse series of
bristles on the hind margin of the mesonotum, the outer one on each side being
the posterior postalar, the others the dorsocentrals and prescutellar acrostichals.
Length, 5-6-5 mm.
Type, male, Aitape, Oct-Nov. 1936 (lL. E. Cheesman), allotype, Vanimo
(F. H. Taylor), New Guinea.
HEIUPROSOPIA SETINERVIS, n. sp. PI. v, fig. 34.
A smaller and darker species than either of the other two, with wing markings
more distinctive (Pl. v, fig. 34), and only two golden-dusted pleural vittae.
9. Face largely blackened, and the third antennal segment darkened above.
The latter is shorter than in the other two species and the arista is much more
distinctly haired, the longest hairs on the basal fifth being about half as long as
the width of the third antennal segment. Vertex with four bristles, the inner pair
the shorter. Gena about one-tenth as high as the eye. Mesonotum much darker
than in the other two species, the yellowish-grey-dusting less dense and the seven
dark vittae inconspicuous. Bristling as in miliaria, the hairs on dise of mesonotum
and on most of the pleura dark, those on the pteropleura and the margins of the
mesonotum and scutellum yellow. Legs black, basal two-thirds of all tibiae fulvous-
yellow, all metatarsi except their extreme apices whitish-yellow.
Wings dark brown, with many small hyaline spots, becoming short transverse
streaks in the cells apically (PI. v, fig. 34). First, third and fifth veins closely
setulose above, the fifth on the entire extent of posterior basal and discal cells,
third more widely setulose below almost to its apex; first posterior cell slightly
narrowed at apex. Halteres yellow. Abdomen shiny black, with less dense grey-
dusting than in the other two species, the dust most distinct across bases of the
tergites, each tergite with a large poorly-defined black mark on each side, hairs
and bristles black. Length, 5 mm.
Type, West New Guinea: Mt. Nomo, south of Mt. Bougainville, 700 feet,
February 1936 (L. EH. Cheesman).
This is the only species known to me in this genus in which the fifth vein
is setulose on the extent of the posterior basal and discal cells.
EUPROSOPIA BILINEATA de Meijere. Pl. v, fig. 35.
Nov, Guwin., v, Zool, livr, 1, 1906, 92; op, cit., ix, 1913, 367,
150 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
Originally described from New Guinea and not since recorded. One male
which I refer here agrees with the rather brief description. The frons has a
narrow brown central vitta, the face has a rather broad dark brown streak in the
lower half of each fovea that extends over the sides of the prelabrum. ‘The
antennae descend to lower level of the eye, and the aristae are long-haired on their
basal halves. There are but two vertical bristles. Thorax quite densely whitish-
grey-dusted, the mesonotum with two uniformly wide black vittae that extend
over the sides of the scutellum, pleura entirely grey-dusted. Scutellum with two
short and two long apical bristles. Abdomen entirely pale-grey-dusted, quite
densely covered with moderately long whitish-yellow hairs and without scales.
Legs with the exception of the yellowish basal halves of the tibiae entirely black.
Wings as in fusifacies, but the fascia proximad of the one over the outer cross-
vein is broken into numerous spots and the apical spot is but narrowly or not at
all connected with the preapical fascia; the markings are also paler than in
fusifacies and impingens.
Dutch New Guinea: Cyclops Mts., Sabron, 930 feet, April 1936 (L. E.
Cheesman); New Guinea: Marprik (C. M. Deland and J. R. Rigby) one female;
Papua: Mt. Lamington (Northern Division) one specimen, July 1927 (C. T.
McNamara).
EXUPROSOPIA PROTENSA (Walker). Pl. v, fig. 36.
Jour. Proc. Linn. Soc. London, vii, 1864, 228 (Platystoma).
New Guinea: Vanimo, Wewak (F. H. Taylor).
EUPROSOPIA POTENS (Walker). PI. v, fig. 37.
Op. cit., vi, 1862, 12 (Platystoma).
This species has the face yellow, the thoracic dorsum olive-grey-dusted, with
three, five, or seven, narrow dark vittae, and the abdomen with a pale brown
fascia near the apex of each tergite, usually quite indistinct. The wings are
hyaline, with a slight yellowish tinge, and numerous almost evenly distributed
pale brown spots. There is no noticeable anterior prolongation of the tegulae,
the scutellum has six bristles, the anterior pair rather high-placed. There are no
seales on the dorsum of the abdomen in either sex.
New Guinea, Key Is., Ternate, Gilolo, and Molucca. A long series from Wewak,
New Guinea (F. H. Taylor); four specimens, Dutch New Guinea, Cyclops Mts.,
Sabron, 930 feet, April-June 1936 (L. E. Cheesman).
EUPROSOPIA VENTRALIS (Walker). Pl. v, fig. 38, 39.
Op. cit., iii, 1859, 131 (Lamprogaster).
I have a female that I refer here, though the character of the maculation of
the dorsum of the abdomen is not distinguishable owing to its being crushed.
However, from the citation of other characters by Hendel, I am certain that my
identification of the species as the one he accepted as ventralis is correct. The
thorax and abdomen are darker in ground-colour, with the black interrupted vittae
on the former much more developed. The small black spot at the apex of the
subcostal vein is larger and more intense than in potens, and there is a short
blackish streak over the inner cross-vein that is not present in that species, there
being only a short transverse line through the vein. The preapical blackish fascia
on the wing in ventralis is also entire, the one over the outer cross-vein is almost
so and both are darker and more definitely fasciform than are the rather broken
markings in potens, In neither sex is the hind femur concave below, and the
BY J. R. MALLOCH. 151
mid and hind pairs are more noticeably browned apically than in potens. Though
it may not be constant, I may mention that in my specimen of this species the
inner pair of vertical bristles is much smaller and more incurved than in the
females of potens before me.
Originally described from Key Island, and subsequently recorded from New
Guinea by Hendel. One female, Dutch New Guinea; Cyclops Mts., Sabron, Camp 2,
2,000 feet, May 1936 (L. EH. Cheesman).
EUPROSOPIA IMPINGENS (Walker). Pl. v, fig. 40.
Op. cit., viii, 1865, 134 (Platystoma).—EHuprosopia fusifacies de Meijere, Nov.
Guin., v, Zool. livr. 1, 1906, 92; op. cit., ix, Zool. livr. 3, 1913, 367; Edwards, Trans.
Zool. Soc. Lond., xx, pt. 18, 1915, 416.
The black mark on either side of the lower edge of the face, and the con-
spicuous V-shaped black mark on the apical third of the wing, which has both
extremities widened, readily distinguishes this species from its nearest allies.
The tegulae are not at all produced forward and the aristae are long-haired on their
basal two-thirds. Abdomen with many yellow lanceolate scales on the dorsum.
Described from New Guinea. Two females, Kavieng, and Put Put, New
Ireland (F. H. Taylor), and four from Dutch New Guinea: Cyclops Mts., Sabron,
930 feet, May—June 1936 (L. E. Cheesman).
EUPROSOPIA FUSIFACIES (Walker). PI. v, fig. 41.
Op. cit., iii, 1859, 113 (Platystoma); Osten-Sacken, Ann. Mus. Civ. Stor. Nat.
Gen., xvi, 1881, 473—Huprosopia squamifera de Meijere, Nov. Guin., ix, Zool.
livr. 3, 1913, 368.
This species is very similar to the preceding, but differs in having the fasciae
of the wings as stated in the foregoing key to the species. Both sexes have
lanceolate scales on the dorsum of the abdomen.
Originally described from Aru Islands and subsequently from New Guinea. A
pair, Papua: Kokoda, 1,200 feet, April 19383 (L. E. Cheesman); Mt. Lamington
(Northern Division), five specimens (C. T. McNamara).
EUPROSOPIA PENICILLATA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 343; Edwards, Trans. Zool. Soc. London,
xx, pt. 18, 1915, 416.
Very like potens Walker, differing as specified in the foregoing key to species.
Described from New Guinea: Huon Gulf; Dutch New Guinea: Wataikwa
River. Unknown to me except from the description.
EUPROSOPIA AUREOVITTA, n. Sp. PI. v, fig. 42.
3; 9. Readily distinguished from any other species of the genus by the
dull brownish-black thorax with the three broad densely yellow-dusted mesonotal
vittae, the central one continued over the scutellum and the others sublateral and
continued down over the postalar declivities, and the single similarly-dusted vitta
on the pleura from below the anterior spiracle to the posterior margin of the
pteropleura. Wing dark brown, with hyaline spots in the cells, becoming sparser
and smaller apically (Pl. v, fig. 42).
Head brownish-yellow, with a yellowish-white-dusted line round the entire
eye-margins, centre of trons reddish-brown, face with a brown line from lower
part of each antennal fovea to epistome, occiput largely grey; third antennal
segment brown above; palpi brown at tips. Antennae extending about two-thirds
ot the distance to epistome; aristae short-haired on basal fifth or less, without an
152 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII,
apical palette in either sex. Outer pair of vertical bristles strong, inner pair short
and fine. Height of head barely greater than its greatest width in front; frons
slightly narrowed and a little depressed above, about 1:5 as long as wide; gena
about one-eighth as high as eye.
Thorax of male with the following bristles: 1 humeral, 2 notopleurals, 1 supra-
alar, 2 postalar, and 1 pair of dorsocentrals, the prescutellar acrostichals lacking;
scutellum with 4 bristles, the outer pair well in front of the apicals and rather
highly placed. In the female the humeral is minute and the notopleurals are
hardly larger, the posterior one being directed forward and upward. Tegulae of
male normal, those of the female rather noticeably produced forward. Hairs black,
yellow on central yellow vitta and on the pteropleura. Legs black, femora grey-
dusted, fore coxae and basal two-thirds or more of all tibiae brownish-yellow, all
metatarsi whitish-yellow except their apical fifth. Fore femur with a series of
posterodorsal bristles and a few finer bristles on the apical half of the postero-
ventral surface.
Wings as in Plate v, figure 42. No costal bristle at the break basad of the
humeral cross-vein, nor hairs on the underside of the stem vein on its basal
section; fourth vein slightly forwardly bent at apex, inner cross-vein oblique.
Halteres yellow. Squamae brownish-yellow, edge of the upper one with narrow
black line. Abdomen blackish-brown, dull, with a broad, complete dorsocentral
vitta of yellow dust, the hairs on latter yellow, on sides black. Length, 7 mm.
Type male, and allotype, Papua: Mafulu, 4,000 feet, December 1933 (L. E.
Cheesman ).
EUPROSOPIA INNOCUA, hn. sp. Pl. v, fig. 43.
d, 2. This species belongs to that group in which the aristae are pubescent on
their basal fifth or less, the scutellum has four bristles, and there are no lanceolate
scales on the dorsum of the abdomen in either sex. The entirely black tarsi are
distinctive.
Head brownish-yellow, the usual grey-dusted line against the eye-margins, face
sometimes brownish centrally. Antennae ferruginous, with the third segment
brown above; the palpi darkened at apices. Frons narrowed above, about 1:25
times as long as its greatest width, the latter exceeding one-third of the head
width. Vertex with 4 strong bristles. Arista of the male with a small broad
apical palette. Gena about one-fourth the eye-height.
Thorax brownish-black, pleura paler, mesonotum with greyish-brown dust and
7 inconspicuous dark vittae, the central one entire and most evident, the next pair
broken between suture and hind margin, the outer pair obsolete before suture;
mesopleura with a brown central mark. Hairs black. Bristles as follows: 1
humeral, 2 notopleurals, 1 supra-alar, 2 postalars (the outer one sometimes dupli-
cated in the female), 1 pair of dorsocentrals, and 1 pair of prescutellar acrostichals.
Scutellum with 4 bristles as in the preceding species. Suprasquamal ridge haired
in centre. Legs black, mid and hind femora usually reddish-brown in part, at
least the mid and hind tibiae reddish-brown except apically. Fore tibia of male
with a yellow subnude stripe on the anteroventral surface except at base and
apex, the posteroventral surface with dense short slightly lanceolate black bristles
on apical sixth. Posteroventral bristles on fore femora of female stronger than
in the male. Tarsi black.
Wings greyish-hyaline, with numerous brownish-black spots (Pl. v, fig. 43).
Stem vein with some fine hairs below on basal section, costa with a fine bristle
below at basal break; fourth vein bent forward at apex; inner cross-vein oblique;
BY J. R. MALLOCH. 153
outer cross-vein enclosed in a dark spot. Halteres yellow. Squamae brown, edge
of upper one fuscous. Abdomen black, densely olive-grey-dusted, usually with a
faint narrow dark apex to tergites 3 and 4 and a brownish central fascia on fifth
tergite. The hairs dense, short, and black, longer and yellow on centre and sides
of the basal composite tergite. Length, 11-13 mm.
Type, male, allotype, and 7 paratypes, Dutch New Guinea:
Sabron, 930 feet, May 1936 (L. E. Cheesman).
It is possible that this is Tetrachaetina burgersiana Enderlein, described from
the same colony, but there are so many important characters lacking in the brief
description of the species, and such probabilities that there are many closely related
forms in New Guinea that I have felt compelled to describe this species as new and
leave the question of the identity of Enderlein’s species to the future. His genus
in any event is not tenable, in my opinion.
Another species that should be considered in connection with this one is
penicillata Hendel. The very brief description given by Hendel states that the
scutellum and pleura are distinctly reddish, and the legs are reddish-yellow, with
the femora at apices below on both sides brownish-striped, and the tarsi black,
only the base of the mid metatarsus brownish. The fifth tergite of the male is
only a little longer than the fourth or third. His comparison is with potens
Walker, which his new species resembles very strongly. In the type male of
innocua the fifth tergite is about as long as the third and fourth together. The
dense short bristles on the posteroventral surface at tip of the fore tibia of the
male of the latter could hardly be termed as “‘Burste” as in penicillata.
Cyclops Mts.,
EUTHYPLATYSTOMA Hendel.
Abhandl. Zool.-botan. Ges., viii, 1914, 398.
EUTHYPLATYSTOMA RIGIDUM (Walker).
Jour. Proc. Linn. Soc. Lond., i, 1857, 32 (Platystoma).—Platystoma stellatum
Walker, op. cit., i, 1857, 32.—Platystoma punctiplenum Walker, op. cit., v, 1861,
268.—Platystoma parvulum Schiner, Reise Novara, Zool., ii, 1, Dipt., 1868, 286.
I have seen no specimens of this species from New Guinea, having only one
trom Celebes, the type locality, and another from Singapore, the last sent me by
C. F. Baker.
It may yet be found in New Guinea.
EXPLANATION OF PLATES IV-V.
Plate iv.
(Walker) o& 11.—Cleitamia excepta, n. sp. type. x3.
12.—Cleitamia delandi, n. sp. type. x6.
1.—Dasyortalis complens
co-type. x12.
2.—Dasyortalis complens (Walker). 2 13.—Plagiostenopterina (Plagiostenopter-
co-type. x12. ina) aenea Wied. X6 app.
3.—Dasyortalis complens var. separata, 14.—Plagiostenopterina (Plagiostenopter-
ina) enderleini Hendel. x6.
15.—Plagiostenopterina (Stenopterosoma)
orbitalis, n. sp. type. x12.
16.—Elassogaster evitta, n. sp. type. x 6.
sp. type.
n. var. type. x12.
4.—Antineura (Adantineura) kerteszi de
Meijere. x6.
5.—Pseudocleitamia setigera, n. sp. type.
« 12° 17.—Pseudepicausta apicalis, n.
6.—Euxestomoea bipunctata Hendel. x12.
7.—Cleitamoides latifascia (Walker )
type. x3.
8.—Cleitamia astrolabei Boisd. x6.
9.—Cleitamia cyclops, n. sp. type. x3.
10.—Cleitamia cheesmanae,n. sp. type. X 3.
N
x LA
18.—Rivellia rufibasis, n. sp. allotype. x 6.
19.—Rivellia dimidiata de Meijere. x12.
20.—Asyntona tetyroides (Walker). x6.
21.—Brea contraria Walker. x6.
154 DIPTERA OF THE TERRITORY OF NEW GUINEA. VII.
Plate v.
22.—Brea magnifica Hendel. x 6.
23.—Scholastes cinctus (Guérin). x 6.
24.—Scholastes aitapensis, n. sp. paratype.
x 6.
25.—Scholastes taylori, n. sp. paratype. x 6.
26.—Achiosoma nigrifacies, n. sp.
x 6.
27.—Achias brachyophthalmus Walker. x 6.
28.—Achias australis, n. sp. type.
type.
29.—Lamprogaster quadrilinea Walker.
x 6.
30.—Lamprogaster decolor, n. sp. paratype.
x 6.
31.—Lamprogaster fulvipes,- n. sp. type.
x 6.
32.—Huprosopia minuta, n. sp. type. x12.
33.—Euprosopia dubitalis, n. sp. allotype.
x 6.
34.—Huprosopia setinervis,n. sp. type. x12.
35.—Huprosopia bilineata de Meijere. x 6.
36.—EHuprosopia protensa (Walker). x6.
37.—Huprosopia potens (Walker). x6.
38.—Huprosopia ventralis (Walker) type.
2 Bie
39.—Huprosopia ventralis (Walker). A
small specimen identified by J. R.
Malloch. x3.
40.—Huprosopia impingens (Walker). x 6.
41.—Huprosopia fusifacies (Walker). x6.
42.—EHuprosopia aureovitta, n. sp. type.
> PY
43.—Huprosopia innocua, n. sp. type. x3.
Proc. Linn. Soc. N.S.W., 1939. PLATE Iv.
Otitidae from New Guinea.
Proc. Linn. Soc. N.S.W., 1939. PLATE V.
Otitidae from New Guinea.
155
THE DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII.
DOLICHOPODIDAE.
Par Vabbé O. Parent, Ambleteuse.
(Communicated by Frank H. Taylor, F.R.E.S., F.Z.8.)
(Thirty-one Text-figures. )
[Read 26th April, 1939.]
I. CAMPSICNEMINAE.
Sympycnus Loew.
Neue Beitr., v, 1857, 42; Smiths. Misc. Coll. 171 (Mon. Dipt. North Amer.),
Gen. xxxii, 1864, 185.
S. PLUMIPES, n. sp. Fig. 1-3.
6. Front bleu d’acier brillant. Face a épais satiné blanc, moins large que
larticle 3 des antennes. Cils postoculaires inférieurs pales. Antennes noires,
Particle 3 triangulaire arrondi, pas plus long que large, soie glabre, insérée au
milieu du bord dorsal. Mesonotum vert brillant, varié de cuivreux, 2 séries mal
distinctes de soies acrosticales réduites, 6 d.c., 2 scutellaires, 1 prothoracique noir.
Abdomen vert sombre métallique, segment 2 jaune rouge translucide sur la moitié
basilaire. Hypopyge noir & appendices peu saillants. Hanches jaunes, II noires,
toutes a vestiture noire. Pattes jaune rouge, tarses noirs, II 4 partir du milieu du
protarse. Patte I: tibia, face dorsale, un chéte postérieur long, tarse (fig. 1) 1 fois
% aussi long que le tibia, les articles 1 et 2 filiformes, le protarse un peu plus long
que le reste, 2 un peu plus long que les 3 suivants réunis, ceux-ci aplatis dorso-
ventralement, et un peu élargis; aux bords antérieur et postérieur avec une
plumosité noire. Patte Il: femur, un préapical. Tibia, face dorsale, 3 antérieurs, 2
postérieurs; face ventrale, 2 antérieurs. Tarse simple, un peu plus long que le
tibia, protarse un peu plus court que le reste. Patte III: femur, un préapical;
tarse plus court que le tibia, les articles 1 et 2 courts, 3 le plus long, un peu plus
long que les 2 suivants réunis; protarse (fig. 2), face ventrale, avec 2-3 longs cils,
2 avec un appendice vermiforme a l’apex. Ailes (fig. 3) teintées de brun, nervures
noires, 3 et 4 a peine convergentes a l’apex; transverse postérieure légérement plus
longue que la section apicale de la 5e. Balanciers jaunes. Cuillerons jaunes 4a cils
noirs. Long: 5 mm.
Femelle inconnue.
N. Guinea: Edie Creek (F. H. Taylor).
Il. CHRYSOSOMATINAE.
CuRYSOSOMA Guérin.
Voy. Coquille Atlas, vii, 1831, 25.
1. C. apruptum Walker, Jour. Proc. Linn. Soc. London, iv, 1860, 115 (Psilopus);
muticus Thomson, Hugenies Resa, Zool., i, Diptera, 1868, 509.
New Britain: Rabaul (F. H. Taylor).
156 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII,
2. C. ATROPURPUREUM, n. sp. Fig. 4.
9. Front vert bleu brillant, une soie orbitaire. Face a satiné blane 4 cétés
paralleles, étroite, large comme un tiers de travers d’oeil. Favoris blanes avec 3
chetes noirs prés de la bouche. Antennes noires, l’article 3 rouge brique, noir au
bord dorsal; soie ventrale de l’article 2 presque aussi longue que l’article 3; celui-ci
1 fois 4 aussi long que large; soie apicale longue comme téte, thorax et écusson
Figs. 1-7.—1-3. Sympycnus plumipes do, 1, tarse i; 2, tarse iii; 3, aile—4. Chrysosoma
atropurpureum 2, aile-—5-7. C. barbescens o, 5, hypopyge; 6, tarse i; 7, aile.
réunis. Mesonotum vert brillant, 3 acrosticales longues, 5 d.c., 2 scutellaires.
Abdomen trés brillant, 4 part le bord postérieur du segment 2 noir violacé; une
. seule série transverse de soies. Hanches noires a givré blanc, I a pilosité blanche;
au bord externe avec un peigne de 6 6pines noires; III avec un chéte externe noir,
robuste. Trochanters noirs. Femurs noirs, I et II étroitement jaunes 4 l’apex.
Tibia I jaune, II and III noirs. Tarses noirs. Patte I: tibia, face dorsale, 1 chéte
antérieur prés de la racine; tarse un peu plus long que le tibia, protarse presque
aussi long que le reste. Patte II: tibia, face dorsale, 2 antérieurs, 2 postérieurs,
3 chétes ventraux, tarse 1 fois 4 aussi long que le tibia, protarse égal au reste.
Patte III: tarse un peu plus court que le tibia, protarse égal aux articles 2 et 3
réunis. Ailes (fig. 4) sans tache; transverse apicale naissant a angle droit; trans-
verse postérieure droite. Balanciers jaunes. Cuillerons a cils pales. Long: 5 mm.
Male inconnu.
N. Guinea: Wewak (F. H. Taylor). N. Britain (Dr. Hosking).
3. C. BARBESCENS, nN. Sp. Figs. 5-7.
6. Front vert métallique brillant, avec, au coin postérieur, une plage de soies
folles noires, s’étendant jusqu’a l’avant. Face violacée brillante, sans poudré,
renflée, de largeur moyenne égale aux 2 d’un travers d’oeil. Palpes noirs a pilosité
dense, jaune blanc. Favoris longs, jaune blane. Antennes noires, l’article 2 a
BY O. PARENT. 157
chétes dorsaux et ventraux 1 fois % aussi longs que l’article 3, celui-ci légerement
plus long que large, ovale, tronqué a l’apex; soie apicale mais insérée au coin
dorsal, simple, pas plus longue que téte et mésonotum réunis. Mesonotum vert
brillant, 3 acrosticales longues, 2 d. c. a l’arriere, 2 scutellaires. Abdomen vert
doré brillant, les segments 3, 4 et 5 avec, a la base, une étroite bande noir mat, une
seule série transversale de chétes. Hypopyge (fig. 5) et ses appendices noirs, les
externes fourchus, a branche ventrale bilobée 4 l’apex. Hanches noires, a vestiture
blanche. Trochanters et femurs noirs, tibias jaunes, tarses I et II jaunes, noirs a
partir de l’apex du protarse, III entiérement noir, le protarse cependant un peu
rougeatre. Tous les femurs, face ventrale, a pilosité blanche, longue comme le
travers. Patte I: tibia, face dorsale, 2 chétes minuscules, tarse (fig. 6) un peu
plus long que le tibia, protarse plus long que le reste, un peu élargi; a la face
ventrale aplati et pelucheux, les autres articles aplatis latéralement, 2 épaissi,
échancré ventralement peu avant l’apex. Tarse II a peine plus long que le tibia,
protarse plus long que le reste. Patte III: tibia gréle, tarse sensiblement égal au
tibia, protarse sensiblement égal au reste. Ailes (fig. 7) sans tache, transverse
apicale formant arcature réguliére, transverse postérieure pratiquement droite.
Balanciers brun noir. Cuillerons blancs a large bordure noire et cils blancs.
Long: 5 mm.
Femelle inconnue.
N. Guinea: Aitape (F. H. Taylor).
4. C. COMPRESSIPES, nh. sp. Fig. 8, 9.
dg. Front vert métallique, brillant, une touffe dense de longues soies folles
noires au coin postérieur. Face a satiné blanc, a cotés convergents vers l’apex,
de largeur moyenne égale aux 2 d’un travers d’oeil. Favoris blancs. Antennes
entiérement noires, les soies de l’article 2 plus courtes que l’article 3, celui-ci
triangulaire, un peu plus long que large; soie simple, longue comme téte, thorax
et écusson réunis. Mesonotum vert sombre brillant, 3 acrosticales longues, 5 d.c.
dont les deux postérieures seules développées, 2 scutellaires. Abdomen vert sombre,
brillant, les segments noir mat, dans leur moitié basilaire, pilosité noire assez
longue, une seule série transversale de chétes. Hypopyge (fig. 8) et ses appendices
noirs, les externes fourchus. Hanches noires, I a pilosité blanche longue, 3 soies
apicales noires, III a pilosité blanche, une soie externe noire, robuste. Trochanters
jaune brun. Femurs noirs, tivia I jaune rouge, II jaune brun, III noir, tarses
noirs. Patte I: femur, face ventrale, deux séries divergentes de soies blanches,
de longueur décroissante vers l’apex, les basilaires au plus aussi longues que le
travers. Tibia inerme. Tarse un peu plus long que le tibia, protarse égal au reste,
tace ventrale, avec une série de chétules courts, les 4 articles suivants aplatis
latéralement et élargis, les articles 2, 3 et 4 d’égale longueur. Patte II: femur,
face ventrale, ligne médiane, sur les 2 basilaires, une série dense de soies fines,
blanches, rigides, aussi longues que le travers; ligne antérieure et postérieure, sur
la moitié apicale, une série de soies rigides, noires, au moins aussi longues que le
travers, les postérieures moins développées. Tibia, face dorsale, 2 chétules
antérieurs, 1 postérieur. Tarse un peu plus long que le tibia; protarse plus long
que le reste. Patte III: femur, face ventrale, une série de soies blanches peu
remarquables. Tarse plus court que le tibia, protarse un peu plus court que le
reste. Ailes (fig. 9) (les deux exemplaires sont immatures) brunies au bord
antérieur, les transverses apicale et postérieure nimbées de brun. Costa non ciliée;
transverse apicale naissant a angle légérement obtus; transverse postérieure
158 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII,
légérement sigmatiforme. Balanciers noirs. Cuillerons noirs a cils noirs. Long:
6 mm.
Femelle inconnue.
N. Guinea: Vanimo (F. H. Taylor).
5. C. FASCIATUM Guérin, Voy. Coquille, Zool. ii (2) i, 1838, 293 (Agonosoma).
New Guinea: Wewak, Aitape (F. H. Taylor).
6. C. FISSILAMELLATUM, n. sp. Fig. 10, 11.
6. Front violacé brillant, une soie orbitaire minuscule, arquée. Face verte, a
satiné blanc, de largeur moyenne égale aux 3 d’un travers d’oeil. Favoris blancs.
Antennes noires, article 2 a soie ventrale, un peu plus longue que l’article 3,
celui-ci 1 fois 4 aussi long que large; soie apicale simple, longue comme thorax
et écusson réunis. Mesonotum assez brillant, noir pourpre; flanquant extérieure-
ment les soies d.c. une bande longitudinale vert bleu; 4 acrosticales longues, 2 d.c.
a Varriére, 2 scutellaires. Abdomen plut6t terne, vert, les segments noir mat sur
la moitié basilaire, une seule série transverse de chétes, pilosité courte, dressée.
Hypopyge (fig. 10) et appendices noirs, les externes fourchus, la branche ventrale
plus longue que l’autre. Pattes entierement noires. Hanche I a pilosité blanche;
trois soies apicales noires, III avec plusieurs soies externes dont une noire. Patte
I: femur, face ventrale, sur le tiers basilaire, 4-5 soies noires rigides, longues 2
fois comme le travers, disposées en deux séries irréguliéres; au dela, deux séries
divergentes de soies blanches plus longues que le travers. Tibia: 3 chétes
postérieurs remarquables, 2 chétes dorsaux, quelques chétules ventraux. Tarse 1
tois # aussi long que le tibia, protarse presque aussi long que le tibia, un peu plus
long que le reste. Patte II: femur, face ventrale, a villosité blanche, un peu plus
longue que le travers. Tibia, face dorsale, une ciliation fine, droite, aussi longue
que le travers, se continuant sur tout le tarse; un chéte antérieur prés de la racine,
2 chetes postérieurs, 2 chétes ventraux. Tarse 1 fois 4 aussi long que le tibia,
protarse plus long que le reste; face ventrale, avec une série de chétules épais,
espacés. Patte III: femur, face ventrale, une pilosité blanche plus longue que le
travers. Tibia & nombreux chétes dorsaux. Tarse égal au tibia, protarse plus
long que le reste. Ailes (fig. 11) presque entiérement noires, une tache fenétre
dans la premiére cellule postérieure; une étroite bande blanche au bord postérieur.
Costa non ciliée. Transverse apicale naissant a angle obtus, transverse postérieure
fortement S-forme. Balanciers noirs. Cuillerons a cilSs noirs. Long: 7 mm.
Femelle semblable au male.
N. Guinea: Edie Creek (F. H. Taylor).
(jC ehULiEE: Ns SDs. 2%
9. Front vert métallique brillant. Face 4 satiné blanc, plane, a cdtés
paralléles, large comme les {$ d’un travers d’oeil. Palpes et trompe jaunes.
Favoris blanes. Antennes noires, chéte dorsal de l’article 2 long comme l'article 3,
celui-ci 1 fois 4 aussi long que large; soie longue comme thorax et écusson réunis.
Mesonotum vert métallique brillant, 3 acrosticales grandes, 2 d.c. a l’arriére, 2
scutellaires. Abdomen vert métallique brillant, sans bandes noires; une seule
série transverse de chétes, pilosité courte et rare. Hanche I jaune a pilosité
jaune, 2 soies noires a l’apex, II et III noires, III avec un vrai chéte externe noir.
Trochanter I jaune, II et III noirs. Pattes jaunes, femur III noir a l’apex, les
tibias confusément noirs a l’apex, III plus largement, tarses I et II noirs a partir
de apex du protarse, III entiérement. Patte I: femur, face ventrale, sur le quart
basilaire, 2 soies chétiformes noires, 1 fois 4 aussi longues que le travers. Tibia,
BY O. PARENT. 159
face dorsale, 1 antérieur, 2 postérieurs; face ventrale, 1 antérieur, 1 postérieur.
Tarse 1 fois 2 aussi long que le tibia, protarse sensiblement égal au reste. Patte IL:
tibia face dorsale, 2 postérieurs, 1 antérieur plus développé. Tarse un peu plus
long que le tibia, protarse plus long que le reste. Patte III: tarse sensiblement
1
Figs. 8-15.—8-9. Chrysosoma compressipes oc, 8, hypopyge; 9, aile.—10-11.
C. fissilamellatum ¢, 10, hypopyge; 11, aile.—12. C. futile Par. 2, aile-—13. C. latemacu-
latum 2, aile.-—14-15. C. nigrohalteratum co, 14, hypopyge; 15, aile.
égal au tibia, protarse égal au reste. Aile (fig. 12) sans tache, transverse apicale
naissant a angle droit et formant une arcature régulieére, transverse postérieure
légérement S-forme. Balanciers noirs. Cuillerons a cils blancs. Long: 5 mm.
Male inconnu.
N. Guinea: Edie Creek (F. H. Taylor).
8. C. Impressum Becker, Capita Zool., i, afl. 4, 1922, 173, fig. 138.
New Guinea: Wewak (F. H. Taylor).
9. C. INSULANUM, 0. SDP.
@. Front vert métallique brillant, une soie orbitaire. Face a satiné blanc
argent, a cotés paralléles, large comme les 2 d’un travers d’oeil. Favoris pales.
Antennes noires, soie dorsale de Varticle 2 aussi longue que I’article 3, celui-ci
triangulaire un peu plus long que large, soie apicale longue comme le thorax.
160 DIPTERA OF THE TERRITORY OF NEW GUINFA. VIII,
Mesonotum vert brillant, 3 acrosticales grandes, 5 d.c., 2 scutellaires. Abdomen vert
métallique; une bande noir mat a cheval sur les incisions, une seule série trans-
versale de chétes. Hanche I jaune, a soies terminales noires, II et III noires.
Trochanter I jaune, II et III noirs. Pattes jaunes, tarses I et II noirs a partir de
l’apex du protarse, III entiérement. Patte I: femur, face ventrale, une série de 5
soies jaunes, de longueur décroissante vers l’apex, les basilaires plus longues que
la demi-longueur du femur. Tibia face dorsale, moitié basilaire, 3 longues soies
noires, égales. Tarse presque 1 fois 4 aussi long que le tibia, protarse au moins
aussi long que le reste, muni de 2 chétes dorsaux antérieurs. Patte II: tibia face
dorsale, 2 chétes postérieurs minuscules, 3 antérieurs longs et robustes, face
ventrale, 3 chétes dont le proximal long et robuste. Tarse plus long que le tibia,
protarse 1 fois 4 aussi long que le reste, avec, a la face dorsale, un chéte court au
tiers apical et, face ventrale, des chétules remarquables. Patte III: tibia face
dorsale, 2 chétes antérieurs assez longs. Tarse égal au tibia; protarse égal au
reste, muni apres le milieu d’un chétule dorsal remarquable, les autres articles
comprimés et légérement dilatés. Aile sans tache; transverse postérieure
légerement S-forme. Balanciers jaunes. Cuillerons a cils jaunes. Long: 4 mm.
Male inconnu.
Duke of York Island, off New Britain (Dr. Hosking).
10. C. LATEMACULATUM, n. sp. Fig. 13.
2. Front vert métallique brillant, une soie orbitaire robuste. Face a cdtés
paralléles, verte, a satiné blanc, large au plus comme le demi-travers de loeil.
Trompe noire. Favoris blancs. Antennes noires, soie dorsale de l’article 2 plus
courte que larticle 3, celui-ci triangulaire un peu plus long que large; soie un peu
plus longue que le mesonotum. Celui-ci vert brillant, 3 acrosticales longues, 5 d.c.,
les deux derniéres plus développées, 2 scutellaires. Abdomen vert métallique, les
segments noir mat sur la moitié basilaire, une seule série transversale de chétes peu
développés. Hanches noires, I a pilosité blanche, et 3 soies apicales noires, III
avec un chéte externe noir, robuste. Trochanters et femurs noirs, tibia I jaune
rouge, II et III noirs, tarses noirs. Patte I: femur, face ventrale, a courte pilosité
blanche, tibia, face dorsale, un chétule minuscule prés de la racine. Tarse un peu
plus long que le tibia, protarse inerme, égal au reste. Patte II: tibia, face dorsale,
2 chétes antérieurs bien développés, 2 postérieurs, protarse plus long que le reste.
Patte III: protarse aussi long que le reste. Ailes (fig. 13) presque entiérement
noires, les nervures longitudinales 2 et 3 sinueuses a l’extrémité; transverse apicale
naissant a angle droit; transverse postérieure faiblement S-forme. Balanciers
noirs. Cuillerons noirs a cils noirs. Long: 6,5 mm.
Male inconnu.
N. Guinea: Vanimo (F. H. Taylor). ,
Remarque.—Cette espéce ne peut se comparer qu’a nigrilimbatum Meij. (N.
Guinea), marginale Walk. = anthracinum Beck. (N. Guinea et Kaiser Wilhelmsland)
et latefuscatum Par. (I. Samoa).
Elle se distingue: (i) de nigrilimbatum Meij. dont la femelle seule est connue
1, par la pilosité blanche des hanches I et de la face ventrale du femur I; 2, par
le tibia I présentant un seul chétule et non 3; 3, par le contour de la tache alaire.
(ii) de marginale Walk. 1, par la couleur des cils des cuillerons franchement
noirs et non brun clair; 2, par la forme triangulaire de l’article 3 des antennes;
3, par la couleur des tibias; 4, par lV’absence de chétes apicaux a la hanche I.
(iii) de latefuscatum Par. 1, par la couleur des tibias dont seul l’antérieur est
jaune; 2, par la transverse postérieure égale au manche de la furcea; 3, par la
tache de Vaile s’étendant jusqu’a l’apex.
BY 0. PARENT. 161
11. C. LucicENA Walker, Jour. Proc. Linn. Soc. London, iii, 1859, 91 (Psilopus).
New Guinea: Salamaua (F. H. Taylor).
12. C. NIGROHALTERATUM, n. sp. Fig. 14, 15.
6. Front vert métallique brillant, ume soie orbitaire folle. Face de largeur
moyenne égale aux # d’un travers d’oeil, épistome renflé, vert doré brillant, clypeus
a satiné gris jaunatre. Favoris jaunes. Antennes noires, article 2 a chéte dorsal
égal a l’article 3, celui-ci conique, 1 fois 4 aussi long que large; soie apicale, simple,
longue comme téte, thorax et écusson réunis. Mesonotum vert terne, 3 acrosticales
grandes, précédées de 3-4 minuscules. 2 d.c. postérieures, 2 scutellaires. Abdomen
vert doré, une bande noir mat sur les incisions, pilosité courte, une seule série
transverse de chétes. Hypopyge (fig. 14) noir, appendices noirs, les externes
tourchus a4 pilosité claire. Hanches noires a vestiture claire, I face antérieure
avec une série externe de soies plus robustes a l’apex. Trochanters et femurs
noirs; tibias jaune rouge, III progressivement brunis vers l’apex; tarse brun noir,
les protarses I et II plus ou moins rougeatres a la racine. Patte I: femur, face
ventrale, une série de soies jaunes, de longueur décroissante vers l’2pex, les deux
basilaires plus longues, longues comme les # de la longueur du femur. Tibia face
dorsale, 3 longues soies chétiformes; face ventrale, 1 soie chétiforme vers le milieu.
Tarse 1 fois # aussi long que le tibia, protarse égal au tibia; sur le tiers basilaire
légérement élargi, aplati ventralement et pelucheux. Patte II: femur, face
ventrale, une série de soies fines, rigides, pales, longues 1 fois 4 comme le travers.
Tibia, face dorsale, ligne antérieure, 3 soies chétiformes; face ventrale, 1 soie
chétiforme longue, au quart basilaire, une courte vers le milieu. Tarse 1 fois 4
aussi long que le tibia, protarse un peu plus long que le reste. Patte III: femur,
face ventrale, une ciliation claire comme au femur II, mais un peu plus courte.
Tibia, un chéte dorsal long au quart basilaire. Tarse un peu plus court que le
tibia, protarse égal au reste. Ailes (fig. 15) brunes plus intensément au bord
antérieur, sans taches nettes et bien délimitées; transverse apicale plutéot anguleuse,
transverse postérieure modérément S-forme. Balanciers noirs. Cuillerons noirs a
cils pales. Long: 6 mm.
Femelle semblable au male, l’article 3 des antennes plus développé, presque 2
fois aussi long que large.
N. Guinea: Wewak (F. H. Taylor).
13. C. papuAsINuM Bigot, Ann. Soc. Ent. France, Sér. 6, x, 1890, 283
(Spathiopsilopus).
New Guinea: Vanimo, Aitape; New Britain: Rabaul (F. H. Taylor).
14. C. pEXOIDES, n. sp. Fig. 16-18.
6. Front vert métallique, une soie orbitaire noire, arquée, minuscule. Face
verte au fond, a satiné gris blanc, a cétés convergents vers l’apex, de largeur
moyenne égale aux # d’un travers d’oeil. Trompe jaune. Favoris blancs. Antennes
noires, article 2 a soie ventrale 1 fois 4 aussi longue que larticle 3, celui-ci pas
plus long que large, triangulaire; soie presque aussi longue que le corps entier,
terminée par une palette (fig. 16) fusiforme, 3 fois aussi longue que large, noire
sur ses 2 basilaires, blanche au dela. Mesonotum vert bleu brillant, 3 acrosticales
grandes, 2 d.c. a l’arriére, 2 scutellaires. Abdomen brillant, cuivreux doré, la
moitié basilaire des segments noir mat, le segment 1 bordé de blanc a la marge
postérieure; une seule série transverse de chétes. Hypopyge (fig. 17) et ses
appendices noirs, les externes fourchus. Hanches I jaunes presque glabres, les
soies apicales jaunes; II et III noires, 4 vestiture pale. Trochanter I jaune, II et
162 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII,
IiI brun noir. Pattes jaunes, femur III noir sur le huitiéme apical, tarses I et II
noircis a partir de l’apex du protarse, III entiérement noir. Patte I: femur, face
ventrale, tout au long, avec une double ciliation rigide noire, le chéte basilaire de
chaque série remarquablement long, au moins double du travers, le chéte suivant
au plus aussi long que le travers du femur, les autres de longueur progressive-
ment décroissante vers l’apex. Tibia: un chéte dorsal trés réduit prés de la racine.
Tarse presque 1 fois 3 aussi long que le tibia; protarse égal aux 2 articles suivants
Figs. 16-22.—16-18. Chrysosoma pexoides 3%, 16, palette antennaire; 17, hypopyge; 18,
aile.—19-20. C. pulverulentum o&, 19, hypopyge; 20, aile.—21-22. C. trichromatum oc, 21,
hypopyge; 22, aile.
réunis. Patte II: tarse un peu plus court que le tibia, protarse égal au reste.
Patte III: tarse plus court que le tibia, protarse un peu plus court que le reste.
Ailes (fig. 18) teintées de rouille, plus intensément au bord antérieur. Costa ciliée,
transverse apicale naissant 4 angle droit, transverse postérieure légérement sigmati-
forme. Balanciers jaune pale. Cuillerons a cils pales. Long: 6 mm.
Femelle inconnue.
N. Guinea: Wau (F. H. Taylor).
Remarque.—Cette espéce est extrémement voisine de pexum Beck. décrite de
N. Guinée et lui est peut-étre synonyme. Cependant, si la description de Becker
est exacte, elle s’en sépare: (1) par la longueur de la soie antennaire ici presque
égale au corps entier, chez pexuwm a peine plus longue que téte et thorax réunis,
(2) par la couleur du tibia III jaune et non brun noir, (3) par la forme de
Vhypopyge, (4) par la ciliation ventrale du femur I. Ici le chéte basilaire de
chaque série tranche vigoureusement par sa longueur sur les suivants, chez pexum
il semble que la décroissance de longueur soit progressive.
15. C. PULVERULENTUM, nN. sp. Fig. 19, 20.
dg. Front vert métallique terni par un poudré jaunatre; une soie orbitaire
minuscule. Face verte, a satiné jaune. Trompe jaune. Favoris pales. Antennes
BY O. PARENT. 163
jaune orange, l’article 2 avec une soie dorsale un peu plus longue que 3, celui-ci
pas plus long que large; soie apicale, noire, simple, longue comme téte et thorax
réunis. Mesonotum bleu métallique terni par un poudré jaune, 3 acrosticales
longues, 2 d.c. a Varriére, 2 scutellaires. Métaépimeére jaune. Abdomen partie
vert, partie jaune, segment 1 entiérement métallique, 2, 3 et 4 largement tachés de
jaune sur les flancs; 5 presque entiérement métallique, le reste entiérement.
Hypopyge (fig. 19) vert, 4 appendices jaunes, les cornes de la capsule trés longues,
jaunes. Hanches jaunes, II et III tachées de noir a la face externe, toutes a
vestiture pale. Trochanters et pattes jaunes, tarse I progressivement noirci, II et
III avec les 4 derniers articles noirs. Femurs pratiquement glabres a la face
ventrale. Patte I: tibia aplati dorso-ventralement; face postérieure peu avant
l’apex, une soie fine, remarquable. Tarse extrémement gréle, 2 fois 4 aussi long
que le tibia, protarse presque 2 fois aussi long que le reste, l’article 5 déprimé, un
peu élargi. Patte II: tarse presque 2 fois aussi long que le tibia, protarse 1 fois
4 aussi long que le reste. Patte III: tarse plus court que le tibia, protarse un peu
plus long que le reste. Ailes (fig. 20) & nervures noires; costa non ciliée. Trans-
verse apicale naissant a4 angle un peu aigu, transverse postérieure droite; a
lextrémité de l’aile une tache brune, presque carrée, allant de la costa a la 4e
longitudinale et respectant l’apex de l’aile. Balanciers jaunes. Cuillerons jaunes
a cils pales. Long: 5 mm.
9. Semblable au male. En particulier pour le tarse I. Cependant la soie
orbitaire est robuste, le protarse III est sensiblement égal au reste du tarse, la
tache alaire est & peine indiquée.
N. Guinea: Edie Creek (F. H. Taylor).
16. C. TRICHROMATUM, n. sp. Fig. 21, 22.
6. Front vert métallique brillant; au coin postérieur un large buisson de soies
folles jaunes. Face vert métallique au fond, a satiné gris jaune, de largeur
moyenne égale presque aux 2 d’un travers d’oeil. Favoris clairs. Antennes jaune
orange, l’article 3 brun au bord dorsal, l’article 2 a soies trés courtes, 3 conique, a
peine aussi long que large; soie apicale noire, simple, longue comme téte, thorax
et écusson réunis. Mesonotum vert métallique assez brillant, une fascie médiane
entiére, bien délimitée, noir purpurescent; sur les flancs une fascie de méme
couleur, fragmentée, 4 acrosticales grandes, 6 d.c. dont les 2 derniéres seules bien
développées, 2 scutellaires. Fiancs sombres, a satiné gris blane. Abdomen
cuivreux doré, avec une large bande noire sur les incisions, une seule série trans-
verse de chétes. Hypopyge (fig. 21) noir a appendices noirs, les externes fourchus.
Hanches I jaunes, a pilosité jaune, et 3 chétes apicaux noirs, II et III noires, a
pilosité pale, III avec un chéte externe noir. Trochanters et pattes jaunes; tibia
III brun noir, a part le sixiéme basilaire; tarses I et II brun noir a partir de
lVapex du protarse, III entiérement noir. Tous les femurs, face ventrale, tout au
long, avec une pilosité pale, fine, érigée, longue comme le travers. Patte I: tibia,
face dorsale, 2 chetes antérieurs, 3 postérieurs, 2 ventraux. Tarse 1 fois % aussi
long que le tibia; protarse un peu plus long que le reste. Patte I: tibia, face dorsale,
3 antérieurs, 3 postérieurs, 2 ventraux; tarse sensiblement aussi long que le tibia;
protarse presque 2 fois aussi long que le reste. Tarse III un peu plus court que le
tibia, protarse sensiblement égal au reste. Ailes (fig. 22) blanches au fond, une
grande tache brun noir dans la moitié apicale, une autre beaucoup plus petite au
niveau de V’embouchure de la le longitudinale. Bord antérieur de l’aile moitié
basilaire, jaune rouille. Transverse apicale formant arcature réguliére, transverse
164 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII,
postérieure fortement S-forme. Balanciers jaunes clair. Cuillerons jaunes, noirs a
l’apex, a cils blancs. Long: 8 mm.
Femelle semblable au male, cependant tous les tarses brun noir, l’apex du
tibia II noirci.
Makada Is., off N. Britain (F. H. Taylor).
MEGISTOSTYLUS Bigot.
Ann. Soc. Ent. France, vii, 1859, 215.
M. LonGicornis Fabr. var. LONGISETOSUS Wulp, Tijds. v. Ent., xxv, 1882, 120, Tab. x,
fig. 7 (Psilopus).
New Britain: Rabaul (F. H. Taylor), Laup (Dr. H. C. Hosking).
Sciopus Zeller.
Isis, 1842, 831.
1. S. BASISTYLATUS, nD. sp. Fig. 23, 24.
og. Front vert métallique brillant. Face couverte d’un satiné blanc. Trompe
jaune. Favoris blancs. Antennes (fig. 23) jaunes, les articles 1 et 2 largement
noirs au bord dorsal, 3 au point d’insertion de la soie; article 3, 1 fois 4 aussi long
que large, piriforme; soie simple, insérée a la base du bord dorsal. Mesonotum
vert brillant, 2-3? acrosticales longues, 2 d.c. a l’arriére, précédées de soies fines
et courtes, 2 scutellaires. Abdomen vert brillant, une large bande noir mat ala base
des segments, une seule série transverse de chétes. Hypopyge noir (en mauvais
état). Hanches I jaunes, II et III noires, toutes a vestiture pale. Trochanters et
pattes jaunes, au tarse I, article 4 noir, 5 blanc; aux tarses II et III les 4 derniers
articles noirs. Tous les femurs pratiquement glabres 4 la face ventrale. Patte I
(fig. 24): tibia, face dorsale, un chéte a la racine. Tarse trés gréle, 2 fois 4 aussi
long que le tibia, protarse un peu plus long que le tibia, égal au reste, 2 fois aussi
long que l’article suivant; celui-ci un peu plus long que 3, lequel est plus long que
4 et 5 réunis; ces derniers aplatis dorso-ventralement, et élargis; 4 une fois 4 plus
long que 5, a plumosité noire ce qui lui donne un contour ovalaire, 5 blanc argent.
Patte II: tibia face dorsale, 2 chétes antérieurs dans la moitié basilaire, 1 postérieur
prés de la racine. Tarse un peu plus long que le tibia, protarse légérement plus
long que le reste. Patte III: tarse nettement plus court que le tibia, protarse
légérement plus long que l’article suivant, les articles 4 et 5 trés courts. Ailes sans
tache, €@ nervures noires. Costa non ciliée; transverse apicale naissant a angle
droit; transverse postérieure droite, fortement oblique. Balanciers jaunes.
Cuillerons noirs a cils jaunes. Long: 5 mm.
Femelle inconnue.
N. Guinea: Sauri, Wewak (F. H. Taylor). ‘
Remarque.—Cette espéce par lVinsertion basilaire de la soie antennaire est a
rapprocher de Jespece australienne décrite par Becker sous le nom de
S. anomalicornis. Elle s’en distingue par de nombreux caractéres: couleur des
antennes, forme et dimensions relatives de l’article 3 des antennes, les soies
acrosticales robustes, les deux derniers articles du tarse I de forme et de couleur
différentes.
2. S. occuttus Par., Encycl. Entom., Diptera, vii, 1934, 124; op. cit., vili, 1935, 75.
New Britain: Rabaul (F. H. Taylor). Décrit des Iles Salomon.
3. S. rEcrus Wied., Ausser. Zweifl. Ins., ii, 1830, 225 (Psilopus).
New Guinea: Edie Creek (F. H. Taylor).
LS Ke oN
j 25 » <
e |
BY Ol PARENT O\-ON htt! | fom) G5
Ys, Nu ase” sO/
III. DriaPHoRINAR. \G ean eo
ASYNDETUS Loew. SQ Ru
Berlin Ent. Zeitschr., xiii, 1869, 35.
1. A. LATITARSATUS Beck., Capita Zool., i, afl. 4, 1922, 83.
New Guinea: Wewak (F. H. Taylor).
2. A. PORRECTUS, Nn. Sp. Fig. 25.
6. Front entiérement terni par un satiné gris blanc; 1 soie orbitaire. Face
vue de face, vert métallique, tangentiellement & satiné blane. Palpes noir profond,
porrigés; vers l’apex, élargis en spatule, a pilosité noire, rude et chétes terminaux
noirs. Favoris blancs. Antennes noires, l’article 3 nettement triangulaire, presque
aigu a l’apex; soie presque basilaire nue. Mesonotum vert clair a givré blanc;
acrosticales petites, bisériées, 5 d.c. dont la médiane faible. Abdomen brillant,
cuivreux, a givré blane sur les flanes, 4 macrochétes anaux. Hanches noires,
toutes a vestiture noire; III: 1 chéte externe noir. Trochanters et femurs noirs,
Figs. 23-31.—28-24. Sciopus basistylatus &%, 28, antenne; 24, patte i—25. Asyndetus
porrectus 3, aile.—26. Diaphorus fulvifrons, aile.—27. D. lateniger, aile.—28. Paraclius
maculifer 92, aile.—29-30. P. strictifacies ¢, 29, hypopyge; 30, aile.—31. Thinophilus
taylori o&, aile.
166 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII,
tibias I et II jaune rouge, III noir, tarses noirs. Patte I: tibia, 4 chétes dorsaux
en une série; tarse a pelotes un peu hypertrophiées; pas de griffes. Patte II: tibia
face dorsale, 4 postérieurs, 3 antérieurs, tous robustes; pas de ventral. Tarse:
protarse un peu plus long que l’article suivant; pelotes normales, pas de griffes.
Patte III: tibia, face dorsale, 4 antérieurs, 4 postérieurs, tous robustes, pas de
ventral; protarse un peu plus long que l’article suivant, pelotes normales, pas de
griffes. Ailes (fig. 25) grises, nervures noires; la 4e simplement coudée. Trans-
verse postérieure en face de l’embouchure de la le. Balanciers jaunes. Cuillerons
a cils blanes. Long: 3,5-4 mm.
Femelle semblable au male.
N. Guinea: Vanimo (F. H. Taylor).
DrapHorvus Meigen.
Syst. Beschr. Zweifl. Insekt., iv, 1824, 32.
1. D. atuigaAtus Walker, Jour. Proc. Linn. Soc. Lond., i, 1857, 121.—Bulolo, N.
Guinea (F. H. Taylor).
2. D. FULVIFRONS, Dn. sp. Fig. 26.
g. Front a satiné fauve, large comme le tubercule ocellaire. Face a satiné
gris jaunatre. Favoris pales. Antennes noires, l’article 3 en demi cercle surbaissé;
soie a peine pubescente. Mesonotum brillant, vert bleu sombre, 5 d.c., acrosticales
bisériées, peu développées. Abdomen brillant, noir bronzé, 4 macrochétes anaux.
Appendices hypopygiaux externes noirs. Hanche I noire sur la moitié basilaire, a
vestiture noire, II et III noires, III avec un seul chéte externe. Trochanters
jaunes. Femur I jaune, II noir sur les 2 basilaires, III jaune, noirci sur la moitié
apicale, 4 part V’apex; tibias jaunes; tarses noirs a partir de l’apex du protarse.
Femurs sans vestiture remarquable. Patte I: tibia avec 2 chétes dorsaux. Pelotes
hypertrophiées, pas de griffes. Patte II: tibia, face dorsale, 2 antérieurs, 2
postérieurs, 1 seul ventral. Pelotes normales, des griffes. Patte III: tibia, face
dorsale, 2 antérieure, 4 postérieurs. Protarse a peine plus long que Il’article suivant.
Pelotes normales, des griffes. Ailes (fig. 26) teintées de rouille; nervures noires.
Balanciers jaunes. Cuillerons a longs cils noirs. Long: 5 mm.
Femelle inconnue.
N. Guinea: Edie Creek (F. H. Taylor).
3. D. LATENIGER, 0. Sp. Fig. 27.
6. Front gris, en son milieu compléetement oblitéré par la coalescence des yeux.
Face noire, a satiné gris blanc. Favoris jaunes. Antennes noires, l’article 3 demi-
circulaire, soie simple. Mesonotum vert bleu, assez brillant, malgré un léger
givré gris blanc; acrosticaux bisériés, bien développés; 5 d.c. Abdomen noir
bronzé, le segment 2 entiérement jaune, & vestiture noire, 4 macrochétes anaux
bien développés. Hanche I jaune, II et III noires, toutes a vestiture noire; III avec
un chéte externe noir. Trochanters et pattes jaunes, femur III noir sur sa moitié
apicale; tarses I et II legerement brunis a l’apex, III tombé. Patte I: femur, face
ventrale, une double série de soies presque aussi longues que le travers; tibia, face
dorsale, un chéte postérieur; face postérieure, une ciliation presque aussi longue
que le travers. Pelotes hypertrophiées, griffes absentes. Patte II: tibia, face
dorsale, 2 antérieurs, 2 postérieurs; face ventrale, un seul chéte. Pelotes normales,
des griffes. Ailes (fig. 27) de la forme ordinaire au genre. Balanciers jaunes.
Cuillerons jaunes a cils noirs. Long: 3, 5 mm.
Femelle inconnue.
N. Guinea: Aitape (F. H. Taylor).
BY O. PARENT. 167
4. D. maurus O.-S., Berl. Ent. Zeit., xxvi, 1882, 114. Z
New Guinea: Wewak (F. H. Taylor). ED
/ NS
5. D. sereNus Beck., Capita Zool., i, afl. 4, 1922, 72. poe
Makada Is., off New Britain (F. H. Taylor).
'
IV. DoLicHoPoDINAE. ea
ae
DoxicHorus Latr. Ce
Precis Caract. Ins., 1796, 159. 2
D. ziczac Wied., Analecta Ent., 1824, 40; Ausser Zweifl. Ins., 1830, 232.
Admiralty Is.: Lombrum (F. H. Taylor).
PaRACLIUS Bigot.
Ann. Soc. Ent. France, (3) vii, 1859, 215 and 227 (Paracleius).
1. P. MACULIFER, n. sp. Fig. 28.
©. Front vert bleu métallique brillant. Face a cotés paralléles, a épais satiné
blane, large comme un tiers de travers d’oeil. Cils postoculaires inférieurs blancs.
Antennes jaune rouge, l’article 3 noir sur la moitié apicale. Mesonotum vert
bleu, peu brillant; fossettes notopleurales noiratres, précédées d’une bande trans-
versale blanc de neige, interrompue au milieu; 6 chétes scutellaires, les moyens
trés robustes, les externes de moitié plus courts, les internes croisés. Abdomen
vert sombre brillant, les segments noirs a la base, et sur les flanes 4 givré blanc
argent. Hanche I jaune, II et III noires, toutes 4 vestiture noire. Pattes jaunes,
femur III avec un point noir a lV’apex, face antérieure; les tarses I entiérement
jaunes, II avec les derniers articles noircis, III entiérement noirs. Patte I: tibia,
face dorsale, 3 antérieurs robustes, 3 postérieurs faibles. Tarse a peine aussi long
que le tibia. Patte II: femur, 1 préapical. Tibia, face dorsale, 3 antérieurs, 3
postérieurs, face ventrale, un antérieur. Patte III: femur, épais, 1 préapical.
Tibia, face dorsale, 3 antérieurs, 4 postérieurs; face ventrale, tout au long, une
série dense de chétes fins. Protarse égal aux # de l’article suivant. Ailes (fig. 28)
grises, & nervures noires, une tache brune allant de la costa a la 3e longitudinale,
commencant peu aprés l’embouchure de la le et finissant a Vapex de la 2e.
Quatriéme longitudinale coudée au tiers apical, sa section apicale arquée convexe
vers l’avant. Balanciers jaunes. Cuillerons jaunes, a longs cils noirs. Long:
6 mm.
Male inconnu.
N. Guinea: Wewak (F. H. Taylor).
2. P. STRICTIFACIES, n. sp. Fig. 29, 30.
6. Front vert métallique. Face blanche trés étroite; en son milieu, réduite a
un filet 4 peine perceptible. Cils postoculaires inférieurs noirs. Antennes noires,
larticle 3 pas plus long que large; soie insérée au milieu du bord dorsal.
Mesonotum bleu vert métallique, brillant; une tache blanche peu marquée a l’avant
des fossettes notopleurales. Abdomen noir, les segments a leur base, a taches
latérales rectangulaires blane argent. Hypopyge (fig. 29) noir, bien développé, a
appendices noirs. Hanches noires a vestiture noire. Trochanters I et II jaunes,
III noir. Femurs noirs, tibias jaunes, III noir aux deux extrémités; tarses I et II
noirs a partir de l’apex du protarse; III entiérement. Patte I: tibia, face dorsale,
4 antérieurs robustes, 3 postérieurs faibles; face ventrale un postérieur, tarse un
peu plus court que le tibia. Patte II: femur, 3 préapicaux. Tibia, face dorsale, 4
postérieurs, 3 antérieurs, 1 proprement dorsal prés de la racine; face ventrale, 1
antérieur. Patte IJI: femur 3 préapicaux. Tibia, face dorsale, 4 antérieurs, 4
in =
AT™
f NN
Peaitin Gee
Yi =
2 Rp tow |}
fy)
ass“ SS
168 DIPTERA OF THE TERRITORY OF NEW GUINEA. VIII.
postérieurs, 1 proprement dorsal formant groupe avec les premiers de chaque
série; pas de chétes ventraux. Protarse a peine plus court que l’article suivant.
Ailes (fig. 30) hyalines 4 nervures noires. Segment apical de la 4e un peu avant
le tiers apical brusquement coudé a angle droit, la transverse apicale ainsi formée,
arquée convexe vers l’avant; la 4e longitudinale au dela du coude se prolongeant
en courte spuria comme chez les Chrysosomatinae. Balanciers jaunes. Cuillerens
jaunes a cils noirs. Long: 5 mm.
Femelle semblable au male.
N. Ireland: Put-Put; Kavieng (F. H. Taylor).
Remarque.—Cette espéce se place a coté de P. neglectus Beck. décrit de
Palmerston, N. Australia. Elle s’en distingue comme suit:
Article 3 des antennes brun rouge. Yeux non contigus au milieu de la face. Tibia III
entierement jaune. Femurs II et III avec un seul préapical. Quatriéme longi-
CUGCIN ALS EN ONMLOULCI UC Meters aici) see ee alel ave ov ete sic enl/aike\ cue pele felts eege eu ere Lous rebeuiens neglectus Beck.
Antennes entiérement noires. Yeux pratiquement contigus au milieu de la _ face.
Tibia III noir aux deux extrémités. Femurs II et III avec 2-3 chétes pré-
apicaux. Quatriéme longitudinale fourchue comme chez les Chrysosomatinae
ase doocondooog do obDO Ge OO EOE Sloop ooo oc aa dbo old co Goes old 6 Strictifacies, n. sp.
VY. HypROPHORINAE.
THINOPHILUS Wahl.
Ofvers Kongl. Vet. Akad. Forhandl., i, 1844, 37.
T. TAYLORI, n. sp. Fig. 31.
dg. Front vert métallique assez brillant. Face guére plus large qu’un tiers de
travers d’oeil, vert métallique; le clypeus brun fauve. Palpes jaunes a pilosité
noire. Favoris jaunes. Antennes noires, l’article 3 brun rouge a la base ventrale,
pas plus long que large; soie pratiquement glabre. Mesonotum vert brillant, deux
stries bronzées flanquant intérieurement les 2 séries de soies d.c., pas d’acrosticales,
5-6 soies d.c. dont la derniére seule bien développée, 2 scutellaires, pas de pro-
thoraciques. Abdomen brillant, entiérement bleu d’acier; lamelles hypopygiales
externes brunes. Hanche I noire, jaune a la face interne, a vestiture noire; II et
III noires. Pattes jaune rouge, les tarses noircis a partir de l’apex du protarse.
Tarse I un peu plus long que le tibia. Patte Il: femur, face ventrale, moitié
apicale avec 2 séries divergentes de chétes noirs rigides, 2 fois aussi longs que le
travers. Tibia, face dorsale, 2 chétes antérieurs, 2 postérieurs, ceux-ci plus réduits.
Patte III: protarse a peine plus long que l’article suivant. Ailes (fig. 31) teintées
de rouille, A nervures noires. Balanciers jaunes. Cuillerons a cils pales. Long:
3 mm.
Femelle inconnue.
N. Ireland: Kavieng (F. H. Taylor).
169
THE DIPTERA OF THE TERRITORY OF NEW GUINEA. IX.
FAMILY PHYTALMIIDAE.
By JoHN R. MALLocH.
(Communicated by Frank H. Taylor, F.R.E.S., F.Z.S.)
(Thirteen Text-figures. )
[Read 26th April, 1939.]J
This group was accorded family rank by Hendel, but it appears to me to be
composite in nature, the group containing Angitula Walker, Angituloides Hendel,
and Giraffomyia Sharp, being probably derived from a different stem from
Phytalmia Gerstaecker and Diplochorda Osten-Sacken. However, this is not the
place to deal exhaustively with the matter, there being three other genera referred
to the family, only one of which I am able to examine at this time, and none of
them belonging to the faunal region now under consideration. Below I present a
key to the genera covered by this paper, and keys to the species of those genera
that are known to occur in New Guinea.
Material collected in Papua by Miss L. EH. Cheesman has been included in this
paper for geographical reasons, thus rendering the paper more valuable.
Key to the Genera.
1. Scutellum with a pair of long, divergent, apical, finger-like processes, at the apex
of each of which there is a fine bristle; suture at hind margin of the meso-
pleura extending downward beyond the level of upper edge of the sternopleura
and appearing to cut into the former proximad of the middle; frons without an
anterior incurved pair of fronto-orbital bristles ...... Subfamily ANGITULINAE, 2
Scutellum without finger-like processes, with at most two fine divergent bristles at
apex; suture at hind margin of the mesopleura not extending downward into
the sternopleura; frons usually with a pair of fine incurved anterior orbital
HDI WO GRD EISCISS ease er ey scene nhac ison ome LOM eeteRe Subfamily PHYTALMIINAE, 4
2. Anterior margin of the pronotum with three moderately long forwardly-directed
processes, the central one with two fine apical bristles .... Angituloides Hendel
Anterior margin of pronotum without three processes as above .............+.-.. 3
3. Vertex with two quite strong bristles; inner cross-vein of the wing much beyond the
middleryot therdiscaly Celis cirs musger span: elemee eters fun esasveieusuens 2 oeyreas eis Giraffomyia Sharp
Vertex without distinct bristles; inner cross-vein at, or a little before, middle of
the GiScaleee ache LONER lenckse sare qetorsh ah ava iana tah hanson eha eta. she iaiehaile: cts Angitula Walker
4, Wirst, second, and third wing-veins closely placed, distance from costal to third vein
opposite the inner cross-vein rarely more than half as great as length of the
cross-vein; first vein ending in the costa much closer to apex of second vein
than to that of subcosta, and far beyond level of inner cross-vein; costa of male
thickened and elevated beyond middle .............. Diplochorda Osten-Sacken
First, second, and third wing-veins normally placed, the distance from the costal
to the third vein opposite the inner cross-vein distinctly greater than the length
of the latter; first vein ending in the costa about midway between apices of
subcostal and second veins, and almost directly above the inner cross-vein; costa
Ine Male InoOt thiCkenedMy weyers ie siecle cre er ele telsl none ecaeene Phytalmia Gerstaecker
170 DIPTERA OF THE TERRITORY OF NEW GUINEA. IX,
Subfamily ANGITULINAE.
There is but one of the three known genera of this subfamily as yet reported
to occur in New Guinea, the others being known from New Britain and the
Solomons. No species of the other two genera are as yet known from New
Guinea. A more extensive consideration of the extralimital species is included
in a report on the species of Phytalmiidae from the Solomon Islands now ready
for the press.
ANGITULA Walker.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 123; Hlaphomyia pt., Saunders, Trans.
Ent. Soc. Lond., v, ser. 2, 1861, 416; Edwards, F. W., Trans. Zool. Soc. Lond., xx,
eis By, gil, Ole
There are two species of the genus known, but one of them being in material
now before me. Edwards has given the following distinguishing characters:
Head dark bluish, submetallic, rarely with any reddish tinge except on front and face;
antennae almost entirely dark brown; a small, but sharply-defined dark brown spot
ALSEHSMEIP MOLTEN CULTS erosee excl es tetalse ere fate val io Saas ees ete erase ie Joe es aieeverensas longicollis Walker
Head bright reddish, with two narrow dark lines on the nape; antennae yellowish except
for the tip of the third joint which is dark brown; wings with a somewhat larger
but much fainter and ill-defined brown patch at the tip .......... cyanea Guérin
ANGITULA LONGICOLLIS Walker.
Jour. Proc. Linn. Soc. London, iii, 1859, 123; EHlaphomyia polita Saunders,
Trans. Ent. Soc. London, v, ser. 2, 1861, 416; Osten-Sacken, Ann. Mus. Civ. Stor.
Nat. Genova, xvi, 1881, 481; Edwards, Trans. Zool. Soc. London, xx, pt. 13, 1915, 417.
A glossy-black species with the fore coxae and basal fourth or less of all
femora whitish-yellow. The face, lower part of occiput, and the genae, yellowish
in male, less noticeably so in the female; third antennal segment sometimes
yellowish basally in male but usually black in female. Basal half of the costal
margin of wing narrowly black, and a narrow black margin along the costa
between apices of second and fourth veins (Fig. 1). MHalteres black. Basal
composite tergite of abdomen about as long as the others combined, with a pair
of short, sharp, upwardly-directed tubercles at basal angles and a more or less
conspicuous somewhat centrally divided elevation or hump a little proximad of
middle.
Female, Sauri, Wewak District (F. H. Taylor), Marprik (J. R. Rigby and
C. M. Deland), Territory of New Guinea; both sexes, Papua: Kokoda, 1,200 feet,
April, June, August to October, 1933; Dutch New Guinea: Cyclops Mts., Sabron,
930 feet, May, 1936; Western New Guinea: Njau-limon, south of Mt. Bougainville,
300 feet, February, 1936 (L. EH. Cheesman). Seventeen specimens. Previously
recorded from Aru, Dorey, and New Guinea. ;
ANGITULA CYANEA (Guérin).
Voy. de la Coquille, Zool. ii (2), 1838, 301, Pl. 21, fig. 11 (Nerius).
This species is not known to me. Described from New Guinea.
PHYTALMIA Gerstaecker.
Stett. Ent. Zeit., xxi, 1860, 169; Hlaphomyia Saunders, Trans. Ent. Soc: Lond.,
v, ser. 2, 1861, 413.
In the key presented below I have included all species Known to me but have
not included wollastoni Edwards, of which I have seen only the description and
figure. It differs from all the others in the genus in having the anterior notopleural
bristle well developed, and the aristae with the hairs almost as long below as above
BY J. R. MALLOCH. iU7/al
and. carried to, or almost to, the apices. The wing has a very narrow dark brown
costal streak from the apex of the subcostal vein to the tip. Originally described
from New Guinea, in the paper by Edwards cited under Angitula.
Key to the Species.
1. Brownish-yellow species, with all the femora of that colour, the hind tibiae largely
dark brown; both sexes with a short stout upwardly-directed and slightly back-
wardly-curved tubercle in centre of the anterior edge of the pronotum, the lateral
portions of collar low; a pair of small tubercles on the posterior margin of the
head below in male and female; male with a pair of stout black anteriorly-
directed thorns at the middle of the anteroventral surface of the fore femur,
and a series of microscopic decumbent black setulae from near them to apex
on same surface, the posteroventral surface with one or two decumbent
forwardly-directed short black bristles nearly opposite the two strong thorns,
and some microscopic black setulae in a series from them to apex; the long apical
ventral spur of mid tibia knobbed and slightly warped at apex in male, simple
and acute at apex in female; frons with a pair of hair-like incurved anterior
orbitals, and a very fine pair of slightly recurved orbitals well above middle;
genal process of male when fully developed about two-thirds as long as entire
insect, very slender; with a short preapical branch, black or dark brown, with
NAGUUEV EET OFS. ais iat co. c., OMe ONO icr CISION IS HIRE aonE RE eeae Meta cervicornis Gerstaecker
Black or pitchy-brown coloured species, with pale yellow scutellum and sometimes
yellow thoracic markings, the greater portion of the legs blackened or browned;
one species with a central tubercle on anterior margin of the pronotum, but the
lateral portions of the collar are more or less elevated and not forwardly pro-
duced; neither sex with a pair of tubercles below on posterior margin of the
head; fore femur of male if armed with strong central bristles has them either
on the posteroventral surface, or the bristles on the anteroventral surface are
close to the base; the long apical ventral spur in both sexes simple, acute at
ALD CONCERNS tote Sa ercn es crish cues Kecatishcvieh-shetetersculsitelialteits /5ls sey en eiayienes ohte Slice lacie) deials) Scar wirebabe leneceneher eva) sta 2
2. Anterior margin of the pronotum with a short central wart-like tubercle; fore femur
of male with a series of three or four strong closely-placed bristles beginning just
beyond middle of the posteroventral surface; femora brownish-black; mid and
hind pairs narrowly yellowish-white at bases; pleura without pale yellow
markings; epistome quite prominently protruded; genal processes of male about
as long as thorax, almost equally wide from base to beyond middle, from there
tapered to a point at apices; scutellum with the pair of apical bristles fine
FW aXe ESH GRO) Gh Eames sees a 5B Ich GORGE CLONE". CUR CRG DEERE RENTS) REMEDIES ety nig coer wallacei (Saunders)
Anterior margin of the pronotum emarginate in centre, without a central tubercle,
at most with a low transverse ridge centrally; fore femur with at least six
posteroventral bristles; pleura with yellow markings; epistome not protruded,
OT WOU Ss iS it live 1S OM speereans meen isner hors clones ome wetsseuchells ite eee RR MME wae Ome aeons er eG) chahe.e cite 3
3. Fore tibia of male with dense short stout spinules from near base to near apex on
the ventral surface, the fore femur stoutest at base, with strong bristles on both
the anteroventral and posteroventral surfaces, basally only on the latter, on
almost the entire extent of the anteroventral surface;:genal processes of male
about as long as the thorax, moderately stout, with a thumb-like projection on
the posterior side near middle; scutellar bristles as long and strong as the
Hosterion NoOtopleunaly Crow kek= scree steed © ia eyor se epee rats Sade ree ok biarmata, n. sp.
Fore tibia with only fine appressed hairs on the ventral surface in both sexes; fore
femur of male stoutest at middle, with six closely-placed bristles in a series
beginning just beyond middle; genal processes of male longer than the thorax,
expanded fan-like near base, and with a rather slender lobe from posterior
apical angle that is as long as the expanded portion; scutellar bristles repre-
sented by fine short hairs, not nearly as long as the posterior notopleural
LISELI ee ot a cette aici aoue Screen ere er eve tense stedotenniereycccusjouskew ens ene-ey al's alcicornis (Saunders)
PHYTALMIA CERVICORNIS Gerstaecker.
Stett. Ent. Zeit., xxi, 1860, 173, Pl. 11, fig. 4; Hlaphomyia cervicornis Saunders,
Trans. Ent. Soc. Lond., v, ser. 2, 1861, 414.
By a strange coincidence Saunders chose the same specific name for this species
as had Gerstaecker before him.
172 DIPTERA OF THE TERRITORY OF NEW GUINEA. IX,
The males before me have the head black, with an oval yellowish spot in front
of the ocelli, and a pear-shaped yellow spot on each side of the face close to the
lower margin, the tapered end of each close to the parafacials. The propleura and
basal half or more of the fore coxae are blackened. The genal thorns (Fig. 2)
are very long and slender, deep black, with the apices of the two branches white.
I have three typical males before me. Wing as in Figure 3. Length, 15 mm.
Papua: Kokoda, 1,200 feet, August, September, October, 1933 (L. E. Cheesman),
six specimens; Mt. Lamington (Northern Division), three specimens (C. T.
McNamara). The females are not as long as the males except the ovipositor is
included in the measurement. One female, New Guinea: Marprik (J. R. Rigby
and C. M. Deland). Recorded from New Guinea and Dorey.
PHYTALMIA PRISCA Enderlein.
Arb. morph. taxon. Entom. Berlin., iii, No. 3, 1936, 230 (Archiphytalmia).
Papua: Kokoda, 1,200 ft., June, 1933 (L. E. Cheesman), British Museum (Nat.
Hist.).
PHYTALMIA WALLACEI Saunders.
Trans. Ent. Soc. Lond., v, ser. 2, 1861, 414 (Hlaphomyia).
do. A much darker species than cervicornis, general colour black, part of the
trons, most of the genal processes, and the face yellow or yellowish-brown,
scutellum and thoracic sutures also of that colour. A yellow spot near the apex of
abdominal petiole, and the apices of tergites slightly paler than remainder of
tergites. Legs dark brown, bases of mid and hind femora and bases of all tarsi
yellow. Stigma brown, apex of wing faintly browned. Genal processes (Fig. 4)
much longer than in prisca, about as long as the thorax, flattened, width less than
that of frons, tapered on apical third, ending in a point. Anterior dorsal marginal
process of thorax much shorter than in cervicornis. Fore femur with postero-
ventral armature only, consisting of about three short curved bristles close to
middle. Longer mid-tibial spur sharp at apex. First posterior cell of wing not
noticeably widened at apex. Length, 12 mm.
Papua: Kokoda, 1,200 feet, June and August, 1933 (L. EH. Cheesman).
Originally described from the island of Dorey, Mt. Lamington (Northern Division),
two specimens (C. T. McNamara).
PHYTALMIA ALCICORNIS (Saunders).
Trans. Ent. Soc. London, v, ser. 2, 1861, 415.
A larger species than wallacei, with a greater amount of yellow on the head
and thorax, there being a broad hind marginal streak on the mesopleura, another
behind the wing base that extends to the lower margin of the metapleura, and a
number of marks on the mesonotum, as well as a streak in centre of the chitinous
rounded sclerite between the base of the abdomen and bases of the hind coxae.
The apices of the abdominal tergites are also quite noticeably yellow. The genal
processes of the male (Fig. 5) are longer than the thorax, much expanded, fan-like
on the basal half, with a slender lobe extending outward from the apical posterior
angle of the “fan” that is a little longer than the latter. These processes are pale
stramineous in colour, with reddish-brown streaks, the extreme tip of the slender
lobe black. Pronotum in both sexes emarginate in centre, behind the emargination
there is a slightly-raised transverse rounded ridge, and the collar on each side of
the emargination is in the form of a rounded ridge extending forward. Scutellum
with two hair-like apical bristles that are distinctly shorter and finer than the
posterior notopleural bristle. Fore femur in both sexes thickest centrally, much
BY J. R. MALLOCH. 173
Fig. 1.—Angitula longicollis Walker, wing of female.
Fig. 2.—Phytalmia cervicornis Gerstaecker, left genal process of male from the side.
Fig. 3.—Phytalmia cervicornis Gerstaecker, wing of female.
Fig. 4.—Phytalmia wallacei Saunders, left genal process of male from above.
Fig. 5.—Phytalmia alcicornis (Saunders), left genal process of male from above.
Fig. 6.—Phytalmia biarmata, n. sp., left genal process of male from above.
Fig. 7.—Phytalmia biarmata, n. sp., right fore femur and tibia, anterior view.
Fig. 8.—Diplochorda aneura, n. sp., head of male from in front.
Fig. 9.—Diplochorda aneura, n. sp., wing of male type.
Fig. 10.—Diplochorda myrmex O.S., wing of male.
Fig. 11,—Diplochorda myrmex O.S., wing of female.
Fig. 12.—Diplochorda trilineata de Meij., wing of male.
Fig. 13.—Diplochorda minor, n. sp., wing of female type.
174 DIPTERA OF THE TERRITORY OF NEW GUINEA. IX,
thicker in male than in female, and in the former with a series of about six
very closely placed slightly curved and forwardly-directed black bristles, the basal
one almost exactly at middle of the posteroventral surface. Mid-tibial spur simple
in both sexes. Length, 13-16 mm.
Papua: Kokoda, 1,200 feet, June and August, 1933 (L. E. Cheesman). Ten
specimens, both sexes. Original locality, island of Dorey.
Four males identified as this species by Dr. Smart were sent to me by him,
and without these I should have had some doubt as to the identity of the specimens
before me, because no long apical lobe is shown in Saunders’ figure of the genal
process. In some specimens in hand this apical lobe is bent back against the
“fan” and it may sometimes be broken off.
PHYTALMIA BIARMATA, Nl. SD.
6, 2. Similar in general colour and markings to alcicornis, but the yellow
vertical mark on the metapleura is not nearly as distinct and does not attain
the lower edge.
Structurally the main distinctions lie in the form of the genal processes of
the male (Fig. 6), in the shape and ventral armature of the fore femur of the
same sex, there being bristles on both the anteroventral and posteroventral
surfaces (Fig. 7), and in the much stronger apical pair of scutellar bristles in
both sexes. In other characters the species is much as in alcicornis, the mid tibia
having the apical ventral spur simple, acute at apex, in both sexes. The frons
has the anterior incurved orbital bristles well developed, usually stronger than in
most of the allied species, but the upper reclinate pair is not evident in any of the
seven specimens before me. Wing coloured as in the other species, with the stigma
dark brown and the tip more or less suffused with pale brown. In teneral
specimens the apical clouding is usually very indistinct or lacking. Length,
12-15 mm.
Type, male, allotype, and five paratypes, Papua: Mondo, 5,000 feet, February,
1934 (L. E. Cheesman).
DipeLocHorpsA Osten-Sacken.
Ann. Mus. Civ. Stor. Nat. Genova, xvi, 1881, 484; Hendel, Gen. Insectorum,
Pyrgotinae, fase. 79, 1908, 4.
Bezzi did not recognize this genus when he published his paper in 1924 (Rev.
Zool. Afric., xii, fase. 2, p. 225), so that it is not found in his key to the genera
included in the paper. He also omitted Angituloides Hendel, though in the copy
of the paper sent to me by Bezzi he pencilled it in the margin.
Key to the Species.
1. The dark brown costal stripe on the wing extending on the field to over the third
vein a little proximad of the inner cross-vein, running obliquely back to near
middle of that vein and entirely filling the first posterior cell, even spreading
renin aitt) oVer (2{-1C10) 010 CG o.cackeo 0 GIOIGG o.0 GIOIA Gg OO cick Glo olcod GEA db OO Maid” Oidiat cota ack 2
The dark brown stripe on the costal border of the wing not extending over the third
vein, or if it does then only at a point well beyond the inner cross-vein, and
neverwentinelyanilline; the first tposterior Cell) i OUD EIN VE LES bares opsey scrapie: esto el elroserroh onlay aua/fo\ etjeh ep tun: envelletuei/<) «litte 17. Spermatochnus Reinke.
VII. Order LAMINARIALES Oltmanns.
Chordaceae Dumont. and Laminariaceae Reichenb. do not occur here.
The stipe is distinct, at least when young, and paraphyses bear hyaline appendages in
the types so far recorded from New South Wales.
Splitting arises at the transition place or within its influence; fronds composed of hold-
fast, branching stipe and a few to numerous blades; no cryptostomata or tufts of hair;
paraphyses unicellular. No outgrowths develop as in Alariaceae except in Lessoniopsis
IRGUMKS, ceoesocnbosboeones pee SCA bee odo 6 bos GUD UD Deo MUlED eo Moa Eb Lessoniaceae S. & G.
Sori on the ordinary blades; stipe scorpioid-sympodial. This is the only section recorded
TGie ING Sewn WAGES sso pwooesaldicdods6eDaooOocOObS Macrocysteae Kuetz. (lim. mut.)
Stipe solid. Only genus recorded from New South Wales ........ 18. Macrocystis Ag.
Outgrowths arise at the transition place or within its influence ..:... Alariaceae S. & G.
Mature outgrowths confined to the blade. This is the only section recorded for New
SOuthe “Wiese rscetve ts nsisletnusae eidetne cna bopens fencer aucces sich ameooaweiia) aston se ntleee cece ai anle HEecklonieae Setchell.
Lamina pinnatifid, ribless and broad. Only genus recorded from New South Wales
OR GR ol CT ERC aE inno ic a teciubt Ga tones ER EAA! eG NG scko niet CUE aoN nena Eee 19. Ecklonia Hornemann.
1. SPHACELARIA Lyngb.
Branching pinnate; pinnae frequently opposite, irregular in length, but becoming shorter
near the tips of branches; articulations about equal in length and breadth ..............
a NEL OE ADEE OSE SACRO EERO RTCA Oe HINO ICICI A COPRONESORDACACIGS Ci aCe ERE IES 1. S. cirrhosa (Roth.) Ag.
Locality.— Harv. Aus.: Port Jackson.
Branching not pinnate; articulations longer than broad ...... 2. 8S. tribuloides Menegh.
Locality.—Nat. Herb.: Tuggerah Lakes, Harv. Aus.: Port Jackson, Kiama (also
Victoria).
5The Order Dictyosiphonales S. & G. is here regarded as extended to include those
members of the Spermatochnaceae with growth from a distinct apical cell. This
extension is suggested by Setchell and Gardner (1925, p. 587).
196 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
2. CLADOSTEPHUS Ag.&
Whorls of ramuli very close together and difficult to differentiate; joints of the ramuli
shorter than Droad “Vskie VS ere ein ss oye wee ears wid wie eres 3. C. spongiosus (Lightft.) Ag.
Locality.—Nat. Herb.: Tuggerah Lakes (also Victoria). C.S. & I.R.: Narrabeen. Herb.
Notes: Lake Macquarie.
Whorls of ramuli close but distinct; joints about as long as broad ....................
aaa MO Re NRO ES CR ORS CR OROTHAIO CROMER CR TERCRC EC 4. C. verticillatus (Lightft.) Ag.
Locality.—Nat. Herb.: Narrabeen (also Victoria).
3. STYPOCAULON Kuetz.
Frond notably stupose, to 20 cm. or more high and harsh and stiff; fruits occur 3 or 4
Rysfaeeeaeel aba) Wea Eboleils ogodocageosodeuugoonboea aoc 5. S. paniculatum (Suhr.) Kuetz.?
Locality.—Nat. Herb.: Kiama, Narrabeen, Newcastle (also Victoria). University :
Broken Bay. C.S.&I1.R.: Bondi or Long Bay—cast up.
4. LEATHESIA Gray.
Thallus of metallic-green, shining, irregularly globose, hollow sacs of up to 5 cm.
diameter ; paraphyses clavate, gradually and uniformly enlarging upwards ..............
PR ete teh eS CAS TCR ONCE CaS On re CERT CRCLCI El CIC RPE GET cl 6. L. difformis (Linn.) Aresch.
Locality.—Nat. Herb.: (also Victoria). C.S.&1.R.: Eden.
5. ASspERococcus Lamour.
Fronds attenuated at the base, swelling into elongated sacs, which may be constricted into
segments; sori dotted over the surface; paraphyses numerous .. 7. A. bullosus Lamour.
Locality.— Nat. Herb.: Eden, Twofold Bay, Botany Bay.
6. InEea Fries.
There is a disc-like attachment organ; frond oval or cuneiform; no hairs or paraphyses
GCCUT MDIANC SVERVAVATIA DIC antes teen aie teisiea aie ca adele checeueicuatoieiciccnee 8. I. fascia (Muell.) Fries.
Locality.—Nat. Herb.: Plant as Phyllitis fascia (Muell.) Kuetz. Farm Cove, Sydney,
Woolloomooloo Bay, Sydney. C.S. & I. R.: Plant as Phyllitis fascia (Muell.) Kuetz.
Sydney district, Maroubra, Wollongong, Kurnell, Manly, Bondi.
7. ScyTosrpHOoN Ag. (emend. Thur.).
Unbranched frond is intestiniform, sometimes articulately constricted; attachment by a
small disc; sporangia associated with paraphyses .... 9. S. lomentaria (Lyngb.) J. Ag.
Locality. Nat. Herb.: Huskisson, Jervis Bay. Lucas (1936): ‘North as far as Sydney’.
8. COLPOMENIA Derb. & Sol.
Thallus consists of pale brown bladders without stipes—attachment being by a broad
base; the cortical layer consists of 1 or 2 rows of cuboidal cells—the inner layer of larger,
TOUNTIAEARGECVIS serctoreis cis. see ree. e cseracanave, axoemerehe are siete e euevenate 10. C. sinwosa (Roth.) Derb. & Sol.
Locality.—Nat. Herb.: Middle Harbour, Sydney, Newcastle (also Victoria). University:
Watson’s Bay. C.S.&I1.R.: Botany Bay, Port Jackson (also Queensland and Lord Howe
Island). Muell.: Plant as Asperococcus sinuosus Bory., Tilba Tilba.
9. EcrocarPpus® Lyngb.
Plant tufted, usually about 30 mm. high and rarely, if ever, exceeding 1 cm-; usually
epiphytic; branching diffuse; articulations at the base half as long as broad, and in
the other parts four or more times longer than their breadth; plurilocular reproductive
structures egg-shaped or elongated, sessile or shortly stipitate; unilocular reproductive
structures (ess-shaped andisessile cyoc: 0s © cliciciece cll ele mpiensiet 11. #. simpliciusculus Ag.
Locality.—C.S. & 1.R.: Manly. D.T.: (also Queensland).
6 Notes in the Algal Section of the National Herbarium, Sydney, indicate that there
are intermediate forms between the two species listed below.
7Sonder (1880) lists Sphacelaria paniculata Lgb. as from Tilba Tilba. This species
is not mentioned by De Toni (1895). Sphacelaria paniculata Suhr. is a synonym of
Stypocaulon paniculatum Kuetz.
8S.&G. (1925) use chromatophore form-discoid or band-shaped, as a means of
distinguishing species of Hctocarpus. The writer has found both forms present in a single
filament of E. confervoides.
BY VALERIE MAY. 197
Plant tufted; when mature usually exceeds 2 cm. in height, and may be more than 30 cm.
long; branching alternate or secund, not opposite; plurilocular reproductive structures
very variable, but not cylindrical or obtuse-conical at maturity ....................4..
eM a RM he ae Ee abbas sero eh sated taka: Syatiaileevanepdubila @ 12. H. confervoides® (Roth.) Le Jol.
Some workers divide this species further as:
Plant always fixed; never possessing a terminal hair on the plurilocular reproductive
FSU EIGEN Xe) 16 ' erG OOkG DI O10 CHOI ORO Ce CEO Ent Ok a OTD: OF SEL rrtce ioaeEge EF. confervoides (Roth.) Le Jol.
Plant often free-floating and usually possessing a terminal hair on the plurilocular
GEVEOGUCEIVEKSEGUCEULE! sje s cele + © chebelolic leusle coslsiaieo ete ee cies EH. siliculosus (Dillw.) Lyngb.
Locality.—Nat. Herb.: Plant as EF. confervoides (Roth.) Le Jol., Port Stephens; Plant
as H. siliculosus (Dill.) Lyngb., Wollongong, Port Hacking. C.S.&I1.R.: Plant as
E. confervoides (Roth.) Le Jol., (also Queensland and Lord Howe Island). Bailey:
Plant as E. siliculosus (Dill.) Lyngb. (also Queensland).
10. PYLAIELLA Bory.
Branches usually opposite, and given off at wide angles; articulations once or twice
longer than broad; plant gelatinous, adhering to paper .. 13. P. littoralis (Linn.) Kjellm.
Locality.—C.S. & I.R.: South Head, Port Jackson.
11. BacrroPpHorA J.Ag.
Lower branches pinnately branched, becoming simple and somewhat attenuate on
ascending; fertile filaments occur near the apices .... 14. B. nigrescens (Harv.) J. Ag.
Locality.—Nat. Herb.: (also Victoria). C.S. &I.R.: Eden.
Branching absent or simple, never pinnate.
Distinct stipe present; branching alternate and rare or absent; apices attenuated
LS TR CSUR ORCU ER OES FSR CH TS Ta NCR ccs Chee INrr IC Der i a 15. B. fium (Harv.) J. Ag.
Locality.—Nat. Herb.: Twofold Bay (also Victoria).
No distinct stipe present; branching irregular and frequent; apices blunt ............
eee Rede h ree etic snals sep omeprosivatos hier (che daneyte” of oNsnistrayleyel ioe suichin- ia tenenc enous, 16. B. irregularis Tilden & Fess.
Locality.—Tilden & Fess.: Kiama.
12. CHNOoOSPORA J. Ag.
Fronds densely caespitose, of the same diameter throughout, except at the slightly
attenuated apices; branches forming acute angles .............. 17. C. pacifica J. Ag.
Locality.—Muell.: Plant as C. fastigiata J. Ag., N.S.W.
13. SporocHNusS Ag.
Receptacles borne on pedicels which are at least longer than the receptacle.
Receptacles linear-cylindrical, obtuse at each end; frond very lax and slender ........
PMS SOLEUS HR vtenen sat sas Pawan sheer aunt ay Seiweney aptwapepcee “cashed Ley cante wish aie fue ageratvay Sue's ae etertelyers 18. S. Moorei Harv.
Locality.— Nat.’ Herb.: Parramatta River, Port Jackson, (also Victoria).
Receptacles spherical or ovoid; frond terete ......... 19. S. radiciformis (R. Br.) Ag.
Locality.—Nat. Herb.: Botany Bay, Eden. Muell.: Tilba Tilba.
Receptacles borne on pedicels which are shorter than the receptacles; fronds cylindrical ;
branching repeatedly decompound ..................2-eeceeerceres 20. S. comosus Ag.
Locality.—Nat. Herb.: Botany Bay (label not attached), (also Victoria).
14. CARPOMITRA Kuetz. :
Plant much branched and irregularly dichotomous; thallus compressed; branches erect
with acute axils, attenuated at the base and obtuse at the apex; receptacles occur at the
thickened apices of the branch midrib ..................0.02e0ceee 21. C. costata Batt.
Locality.—Nat. Herb.: Plant as C. Cabrerae Kuetz., (also Victoria). C.S.&I1.R.: Plant
as C. Cabrerae Kuetz., Eden. Harv. Aus.: Plant as OC. Cabrerae Kuetz., Kiama.
15. Myriocito1a Kuckuck.
Branching alternate or irregular; every portion of the frond thickly clothed with long,
free, villous, hair-like, articulate filaments, which are branched at the base ..........
2099pc0000000000000000000008 Ree cecheed- ere 22. iM. Seuriws, (Harv) ikuckuck
Locality.—Nat. Herb.: Plant as Myriocladia Scurius Harv., (also Victoria). Harv. Aus.:
Plant as Myriocladia Scurius Harv., Newcastle.
®As the result of unpublished work on the variation of this species found near
Sydney, the writer considers E. siliculosus (Dillw.) Lyngb. should be included as a
variety.
10 Under the name C. fastigiata, J. Agardh included his C. pacifica and C. atlantica.
By rules of priority, C. pacifica must be accepted for our species.
198 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
16. ScyTOTHAMNUS H. & H.
Frond somewhat compressed or terete, the median part vaguely ramose, the ultimate
ramuli thins risid and "acuminate! ... see ee eee > ee 23. 8S. australis (J. Ag.) H. & H.
Locality.—Nat. Herb.: Manly, Bondi, (also Lord Howe Island).
17. SPERMATOCHNUS Reinke.
Apices of the filaments without peripheral filaments; branching dichotomous; branches
elongated; secondary branches few, the apices attenuate; sori not sharply differentiated
Fille eR eI PCE SCC CCE ONY 0. CICERO RES eOucn beth HELE CRMc Eee ARS 24. 8S. Lejolisii (Thur.) Reinke.
Locality.— Nat. Herb.: Plant as S. Lejolisii (Thur.) D.T., Port Stephens.
18. Macrocystis Ag.
Main stipes bear at their summits the young differentiating blades and along the greater
part of their length, at regular intervals, the mature, lateral blades, each with a pyriform
bladder at its base, which in turn is supported by a short, cylindrical stipe; blades rigid,
coarsely rugose and with spinulose margins .............. 25. M. pyrifera (Linn.) Ag.
Locality.—Nat. Herb.: Plant as M. pyrifera (Turn.) Ag., Long Bay, (also Victoria and
Lord Howe Island). C.S.&I1I.R.: Plant as M. pyrifera (Turn.) Ag., Bondi. Muell.:
Tilba Tilba.
19. EcKLONIA Hornemann.
Pinnae linear; triangular spines occur at the frond margins, and sometimes cover the
Whos Shines KE WOK oohog6bhasudooceboouobe coos 26. H. radiata (Turn.) J. Ag.
Locality —Nat. Herb.: Between Harrington and Farquhar Inlets, Tweed River, Rich-
mond River, Woy Woy, Urunga, Farm Cove, Clifton Gardens, Long Bay, Bermagui,
Jervis Bay (cast up), (also Lord Howe Island). C.S.&I.R.: Botany Bay to Long Reef.
Herb. Notes: Clarence River, Port Macquarie, Manning River, Forster, Port Stephens,
Newcastle, Tuggerah, Hawkesbury River, Port Hacking, Lake Illawarra, Nowra, Bate-
man’s Bay, Pambula. D.T.: (also Victoria). Sonder: Plant as #H. radiata Harv., (also
Queensland). (As Harvey treated EH. lanciloba as merely a variety of the plant under
discussion, this record for Queensland cannot be accepted as definite.) Muell.: Tilba
Tilba.
Pinnae linear-lanceolate, with spinose dentate margins; stipes slender ..................
BP aciin ial ieoahie Se SU LG AeTs fal eueledeee ie! Gieire: © a Sue taae ete BAe ewes errolbs, owe tape dee Leap. tere We. apexes 27. H. lanciloba Sond.
Locality.—C.S. & I.R.: Port Stephens, (also Victoria).
Tribe APLANOSPOREAE S. & G.
The Tilopteridales Kylin do not occur here (the aplanospores of these occur singly,
and unilocular zoosporangia giving rise to bi-ciliated zoospores are sometimes produced).
Fronds of moderate size, complanate; plants usually attached by a stupose base; growth
apical; reproductive structures formed from superficial cells and projecting beyond the
surface; aplanospores in groups of, usually, four, produced from a single mother cell;
no zoospores produced; gametangia usually in dense sori; distinct oogamy occurs; male
gametesswith ausinele) CiMUM Vs on ve ie) lac) ol de ciel ltt aeons VIII. Order DicryoTaLes Kjellm.
OnTy. amily; Hate cece ek tee Seas Ba ie eee eee date Ae EeE Bee Dictyotaceae Harv. (lim. mut.)
Fronds flabellate, zoned with conspicuous lines of innovation; growth in length by the
division of many marginal cells; thallus ecostate.
No independent tufts of paranemata on the frond; frond composed of several layers of
cells (distromatie in Chlanidote J. Ag.) ; reproductive organs may occur on both sides
of the thallus; sori entirely superficial at maturity.
Striae of cortical cells radiate fan-wise in pairs, as if twinned.
Sori naked and on the upper surface; sub-zonate; frond flat, fan-shaped and with
ODES ates lobes deiouele po tuahie''=(oiroign sh oi ee eR NUS IONS <4, 5 TROL eee Rees 20. Gymnosorus J. Ag.
Sori protected by a hyaline indusium; paraphyses present; frond stipitate ........
Sidve vee HORUS RORS c. drhe Aebehedeele tage: Wakes alae abche a oleh ch DSEE TRIAD SHRP PAS 21. Zonaria (Ag.) J. Ag.
Striae of cortical cells radiate fan-wise, singly; ultimate divisions of the frond fan-
shaped; thallus pleiostromatic; sori prominent; paraphyses present; indusium
F)) oY=(2¥ 4 | ewe tac SIO ONC ROM OL CECE OR COREE? Come eae okt Diaicaoi mera 5.5 Oo oe 22. Homoeostrichus J. Ag.
Independent tufts of paranemata on the fronds; thallus ecostate and flat; fronds
reniform and orbiculate, the edges involute or scrolled; lamina sometimes split into
lobes; thallus of two or more layers of parallelepipedal cells covered by a single
layer of coloured cells; reproductive structures formed in transverse zones; hairs and
reproductive structures on one side of frond only .............. 23. Padina Adanson.
BY VALERIE MAY. 199
Fronds erect, nowhere zoned with lines of innovation.
Terminal cells of the frond numerous and radiating fan-wise.
Fronds ecostate, sub-palmate, dichotomous; spores single or twinned, and evolved on
both faces of the frond; thallus of inner, empty angular cells in several layers, and
an outer zone of cubical cells scarcely smaller, but coloured ......................
COPS OUODODHC OO OOECOODOGIOOO DOD OOD OOOO OdeE Cae cag DGon 24. Spathoglossum Kuetz.
Frond prominently costate and dichotomous; thallus of an inner zone of rectangular,
empty, colourless cells, and an outer (cortical) of cubical and densely coloured
cells (monostromatic layer); reproductive structures on each face of frond; tetra-
spores collected in naked sori; paranemata occur apart from the sori, in clumps
PE ce Dee CR Ree Rear Weieev elie) col elie! suetten cles siren'ei-sy eliarey suey ex'epersy sy:er'e 25. Neurocarpus Webb. & Mohr.
Terminal cells of frond converging towards a central, apical, initial cell.
Frend ecostate; reproductive cells borne on frond proper (but on proliferations in
Glossophora J. Ag.).
Frond flat, dichotomous and composed of a median, monostromatic layer of large,
colourless cells covered on each face by a cortical layer of small, coloured cells;
hairs occur in groups on both surfaces .................... 26. Dictyota Lamour.
Fronds as above, but the central layer di- or polystromatic .... 27. Dilophus J. Ag.
Holdfast much and diffusely branched; frond erect; stem cylindrical or compressed,
especially in the upper part; cartilaginous and closely set throughout with patent
lateral branches; branches slender, flat, furnished with a midrib in the lower half;
ultimate divisions linear, spirally-twisted, alternately pinnate and _ bi-cuspidate;
reproductive structures on both surfaces, in diffuse sori, on the pinnules ..........
MST Uae eel oe ct SaeE sere ev eels Taklouatcostay ce tober er eee ie! Shere Ne et RR ee SS rer aie leu st aman 28. Lobospira Aresch.
20. GyMNosoRUS J. Ag.
Piantovaniesately, pales bEOwmM «4 seers ei cee eel oie 28. G. variegatus (Lamour.) J. Ag.
Locality. Nat. Herb.: Long Bay. C.S. & I.R.: (also Victoria and Queensland). Herb.
Notes: Tuggerah. Muell.: Plant as Zonaria variegata Mert., Port Jackson.
Plant very dark, turning black on being exposed or dried .............. 0.00. e eee eee eee
Ree re teataies icc ere l siccid bso ou seceiieicar ai a.va, op ay. ab ni aS eOMSN AOE RNY aro euetaceveon ena 29. G. nigrescens (Sond.) J. Ag.
Locality—Nat. Herb.: Cronulla, Long Bay, Narrabeen, Tuggerah, Port Stephens (also
Lord Howe Island). C.S.&I.R.: (also Queensland). Sonder: Richmond River, Ballina.
‘ 21. Zonaria (Ag.) J. Ag.
Stem terete or winged; thallus much divided, in general outline being flabellate; branches
end in deeply parted, basally woolly laciniae, whose segments are narrow-linear, trun-
cate, sparingly toothed or incised; no paraphyses occur in the sori ....................
3: ota LN Gai eGii OBS REIRERE SER RE ata CRORE CTE PTIC RC RE ee ive dea deer eon thy 30. Z. Turneriana J. Ag.
Locality.—Nat. Herb.: Eden, (also Victoria).
Frond (where unbranched) or branches cuneate-flabellate.
Frond stupose on under-surface; colour variegately pale brown ...:................
FSG enti ORG Oy ETON EOL Gn OIC Oct ten SEE REREAD SnCRE Fc RaURN Weck Pin i eo ana Sd EIS ine Rute 31. Z. Diesingiana J. Ag.
Locality. Muell.: N.S.W. Laing: (also Norfolk Island).
Frond rather erect, branching; margins coarsely crenate ........ 32. Z. crenata. J. Ag.
Locality.—Nat. Herb.: (also Victoria). C.S.&I.R.: Port Jackson, Maroubra, Bondi,
Port Stephens, (also Queensland).
22. HOMOEOSTRICHUS J. Ag.
Stem terete, stupose, much branched; branches end in narrow wedge-shaped, flat
segments, which are free from stupa (wool) .......... 33. H. Sinclairii (H.& H.) J. Ag.
Locality.—Nat. Herb.: Bulli, Kiama, Narrabeen, Tuggerah, Bondi, Newcastle, (also
Victoria). Herb. Notes: Lake Macquarie.
23. PapIna Adanson.”
Tissue subcoriaceous; frond fan-shaped and split many times, the base stupose ........
ARSENE MSR aA AIS sds BARRIER TAM BON eer 34. P. Fraseri (Grev.) J. Ag.
Locality. Nat. Herb.: Kiama, (also Victoria, Queensland, Lord Howe Island and
Norfolk Island). C.S.&1I.R.: Eden, Maroubra. Lucas (1936): ‘Generally around
Australia’. Muell.: Tilba Tilba.
U Setchell & Gardner (1925) give the reasons for the adoption of the generic name
Neurocarpus Webb. & Mohr. in preference to the more customary Haliseris Targ. Tozz.
2 Lucas (1935) says he is ‘inclined to follow Harvey in referring’ Australian species
of Padina ‘all to Pavonia’. Until definite proof of synonymy is forthcoming, it is
perhaps wiser to leave the species as they are labelled in the herbaria consulted.
200 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
Tissue thick, subcoriaceous below, delicately membranaceous above, highly reticulate;
plant attenuated at the base; the broad, fan-shaped upper part simple or cleft, the
frond or lobes being curled into funnel-shaped cups while growing; on the upper surface
deciduous, orange filaments fringe the concentric bands, these replaced by white, chalky
powder. on the; lower, surface iiss s355 see ae . peice 35. P. pavonia (Linn.) Lamour.
Locality.—Nat. Herb.: Port Jackson, Forster, (also Queensland, Norfolk Island, and
Lord Howe Jsland). C.S.&I1.R.: Long Bay. Herb. Notes: Tuggerah.
24. SPATHOGLOSSUM Kuetz.
Apices squared and sinuses conspicuously rounded; plant much branched ..............
TORAH) Hes ARNE Osi lehs 0 MENS PURI RRR Abels Han Srreva fares ctodehesabanetetanstaXatetohe taledetotereteMs 36. S. cornigerum J. Ag.
Locality. Nat. Herb.: Port Jackson, Port Stephens. C.S.&I.R.: Botany Bay.
25. NeEuRocARPUS Webb. & Mohr.%
There are no veins running from midrib to margins in the New South Wales species.
Spores form a linear band on either side of the midrib, leaving wide sterile margins;
muciferous glands arranged in recurved arches from midrib to margin; the tufts of
paranemata larger than in N. Muelleri ...... 37. N. acrostichoides (J. Ag.), nov. comb.
Locality.—Nat. Herb.: Plant as Haliseris acrostichoides J. Ag., Port Jackson, Port
Stephens, (also Queensland and Victoria).
Spores do not form a linear band on either side of the midrib.
Spores form a cloud-like patch, continuous from midrib to margin; muciferous glands
and tufts of paranemata scattered over the surface; axils rounded and margins entire
Sa ata cn aNe RST SESS TTR es nae eset OTe ee Se oS wee Seel arate Ertenereis 38. N. Muelleri (Sond.), nov. comb.
Locality.— Nat. Herb.: Plant as Haliseris Muelleri Sond., (also Victoria). Harv. Aus.:
Plant as Haliseris Muelleri Sond., Port Jackson.
Spores scattered over the frond.
Seements denticulatewes-- «.ccsece ccs ale 39. N. Woodwardia (R. Br.), nov. comb.
Locality.—Lucas (1913): Plant as Haliseris Woodwardia (R. Br.) J. Ag., Ballina,
(also Queensland).
DELINENUS ENtIGeG myst cheleistexs, sii & wpe otiecehers Pele tens 40. N. polypodioides (Desf.), nov. comb.
Locality.—Sonder: Plant as Haliseris polypodioides Ag., Ballina, (also Queensland).
(As Sonder treated N. Woodwardia as merely a variety of the plant under discussion,
this record for New South Wales cannot be accepted as definite.)
26. Dicryota Lamour.
Base of the plant not stupose or woolly, the attachment being by means of many long,
simple, thread-like fibres arising from the base of the frond and from the lower parts
of the principal rachides; apices of the much-elongated segments of the frond are
blunt.
Plant dark olive-green, the tips of the dichotomies lighter and flabellately expanded;
the branches of each dichotomy slightly diverge above a rotundate sinus; segments
often narrower near the base; margins of thallus have the internal stratum thicker
than the usual monostromatic; surface of the thallus (apices and margins excepted)
covered with small, dense and crowded hairs ....... 41. D. prolificans A. & E. S. Gepp.
Locality. Nat. Herb.: Long Bay, Tuggerah, (also Queensland and Lord Howe Island).
Lucas (1935): Narrabeen, Newcastle.
Membrane rather translucent, lighter in colour towards the extremities; segments of
the irregularly dichotomous frond linear-cuneate, much attenuated at the base,and quite
entines tronGdgwidthywaniable: .sthccsieee fies ote Geared be ES ote eae ote 42. D. radicans Harv.
Locality.—University: Port Stephens. Sonder: (also Queensland). Harv. Aus.:
(also Victoria).
Base of the plant stupose or woolly.
Apices of segments forked and furcate or rather rounded-obtuse; frond delicately
membranaceous, cuneate at the base, afterwards nearly linear; much and regularly
divided dichotomously, the segments being elongate-cuneate; ultimate branches approxi-
mately equal in length; frond width variable, if narrow, segments may twist spirally
and entangle; no proliferations occur on the surface; spores scattered over the disc of
the frond, leaving a clear border on the margins; cells elongated ...................
EASA RAO ROIS SSA CSIC On! SOL ORE een 43. D. dichotoma (Huds.) Lamour.
Locality.—Nat. Herb.: Botany Bay, Kirribilli Point, Port Jackson, Port Stephens,
(also Victoria and Queensland).
13 See footnote on page 199.
BY VALERIE MAY. 201
Frond decompound-dichotomous, densely striate—especially in the older portions;
cortical cells rectangular.
Fertile cells occur over the central area in almost linear, longitudinal, parallel lines,
Wwe WHY, LXE [RON SococacnnoadouvoCcoocGUGdoUnOUCGOuOGDOnUCD 44. D. robusta J. Ag.
Locality.—Nat. Herb.: Botany Bay.
Fertile cells occur scattered irregularly over the central area .............-++2+--+0--
NM e ee eee aire tastes outcte Melee snetereeecel wees 455 Di linearis (Ag) Grev:
Locality.—Muell.: Clarence River.
27. DiLoPpHus J. Ag.
Frond caespitose, attached by radicles, decompound-dichotomous, with linear, erect
segments; adult fronds marked with conspicuous, transverse wrinkles; margins thickened,
the inner stratum of the lamina there consisting of four layers; sori occur in broken,
THEVELEN Kay IVOKEST I Gg bic aid 6 OreOia a old CHE CLUES Io oo DIA Coho cid. tect cy Oro oir 46. D. marginatus J. Ag.
Locality.—Nat. Herb.: Long Bay, Tuggerah, (also Victoria).
28. Losospira Aresch.
Thallus wiry and spirally much twisted, the lower portion being fibrous; the quadrate
cells of the thallus surface converge towards the apices of each terminal tooth of the
FObebM UES A ois Go eo Gee O Chom a Oc oc101d OG Go Bicic Or jola oars 0G CRCACEO COLO 1: 6 Cac ig 47. L. bicuspidata Aresch.
Locality.—Nat. Herb.: Eden, (also Victoria).
Tribe CYCLOSPOREAE Aresch.
IX. Order Fucaues Kylin is the only order.
Frond differentiated into axial and lateral members, and consisting of holdfast, stem,
branches and leaf-like organs; vesicles and specialized receptacles may also be present;
oogonia monosporous; growing region at the apex of the rachis, being somewhat obscure
PA Mee he Ny eas Te ty eat Aten wae hice Rt cpiceanadeHe tel det Sostiranat s\bue tarstiona ees Sargassaceael4# (Decne.) D.T.
No differentiation of frond into axial and lateral members.
Frond not homogeneous; 2 to 8 oospores (4 in Australian species) produced per
oogonium ; holdfast dise-shaped .......................... Fucaceae (Lamour.) Kjellm.
Frond moniliform and branching; internodes inflated and carrying the conceptacles;
paranemata simple. Only genus recorded from New South Wales
Frond homogeneous; no special organs developed; conceptacles scattered over the whole
frond.
NONE VSOMGY Boe ceusiaies septic sscsrsveususoneoe Gbeue tere eect ene Durvillaeaceae4 Oltmanns (lim. mut.)
Frond hollow, cylindrical, containing fluid within, pinnately branched on all sides;
thallus of two layers of cubical, epidermal cells and three layers of polygonal to ovate
cortical cells, within these are long filaments bordering on the central, mucilaginous
TESTS sald Ce Oe CK roe OOD Sloe oOo Sie otcia Glo arc Splachnidiaceae Mitchell & Whitting.
Plant pale green to brown when mature; disc holdfast. Only genus ...............
Sree Ree SSCL! DORE ROTC PROTO Che ER See eee cnolcno CIC cmsiora clepto Stas oe elt 388. Splachnidium Grev.
SARGASSACEAE (Decne.) D.T.
Receptacles specialized from the frond segments.
Receptacles, or groups of receptacles, arise from the transformation of the upper part
of proper branches.
Stem abbreviated, not vesicular, giving off long branches; leaves flat modified branches
ONO SREHD ELOTCTGEG aa. 9 CIO CHE RONG ke GID SO- Eno CRORE CLG ORCL CF OROTES LO Dace Onc eh heme ot eciee ote ce cee 29. Sargassum Ag.
Stem elongated, exceeding the branches in height; leaves flat, marginal ..............
Bee eh Shea hia eto hoe ED SY Gc: Os) co Ne ees wigs dance ane mocanse ups eh ucistisioe darts cdr otwnere nates 30. Carpophyllum Grev.
Receptacles marginal, single, arising from the transformation of an entire ramulus or
proliferation.
Vesicles distinct from other organs and stipitate; leaves unspecialized, ramuli-form and
nou passing. Into branches, je.) leaves: not mid=GFibbedy ac. oss scien ai cis leieke che eheleeiae
STORIE Ce CANOE NCB to oH EO EOL CRONE (oC REE cn toate 31. Blossevillea® Decne. (orthog. mut.)
14 For greater clarity the key to the genera of this family is placed at the end of the
Order Fucales.
1 Gardner (1913) gives reasons for the adoption of the generic name Blossevillea
Deene. (orthog. mut.) in preference to the more customary Cystophora J. Ag.
202 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
Vesicles not distinct from other organs, but are inflations in the terminal leaves; leaves
alternate, mid-ribbed and with cryptostomata .............. 32. Cystophyllum J. Ag.
Receptacles not specialized from the frond segment.
Leaves peltate, fleshy, warted externally and spirally inserted round the stem; vesicles
ATE MNOGIILEG EAVES is oe crevalclie clotelol evens tome encucielieiclistens Sana ihenarcu-pe tctewars oiamemats 33. Scaberia Grev.
Leaves take form of a flattened stem; cauline vesicles present; leaves intermixed with
small ciliary processes that may develop into leaves ............-. 34. Phyllospora Ag.
DURVILLAEACEAE Oltmanns (lim. mut.).
Frond stipitate, flat, pinnatifid or subdigitate ................ 36. Sarcophycus IKuetz.
Frond terete, vaguely branched and parasitic on other algae .. 37. Notheia Bail. & Harv.
29. Sarcassum Ag.16
Leaves pinnatifid, the lower segments being broader, the upper narrower, often ramelli-
form; frond formed by the evolution and repeated division of a primordial, pinnate, leaf-
like axis, the parts of which, by transformation, bear proper leaves, vesicles and recep-
tacles; vesicles either minute, ellipsoidal swellings in the lamella and beaked (aristate),
or larger, terminal, rounded and unbeaked (mutic); receptacles terminal, smooth, at
length racemose on a ramulus .... This is the subgenus Phyllotricha (Aresch.) J. Ag.
Vesicles minute, ellipsoidal, aristate; common caulis compressed and rugged or nodose;
lower leaves pinnatifid, upper simple, sub-linear ...... 48. S. linearifolium (Turn.) Ag.
Locality.—Nat. Herb.: Richmond River (questioned by Lucas). Sonder: Ballina, (also
Victoria).
Vesicles spherical, mutic, large and numerous; leaves much divided, compound, at first
trichotomous, then more vaguely dichotomous-pinnate, all the segments (laciniae) being
filiform; primary caulis rounded, rachides of branches being angulate-rounded; petiole
bases persist as spines on the branches; laciniae warted (verruculose) from the
Presence ol Cry pLOStomMatay ea. 20 4 hs a cits Gite eee ene Sere 49. S. verruculosum (Mert.) Ag.
Locality.—Nat. Herb.: (also Victoria). C.S. &1I.R.: Maroubra.
Leaves entire or dentate-serrate, but not pinnatifid or pinnate; fronds not formed as
described above.
Frond an elongated, branching axis bearing simple leaves without cryptostomata ;
vesicles crowned by a mucro or leaflet, unarmed or dentate (this is subgenus Arth7o-
phycus J. Ag.) ; branches conspicuously angular; ramuli retrofract; leaves which act as
bracts often differ conspicuously from the others.
Receptacles terete, unarmed by teeth; midrib obvious in the lower leaves, but absent
in the upper ones; vesicles almost spherical.
Lower leaves very large, oblong-lanceolate, denticulate and crowded at the base
SiO Boitboraiicn hb Outs, GREG: RCE RCIDICHCRGIC HCA a CRDEC RENCE eer Tira ae 50. S. paradoxum (R. Br.) Harv.
Locality.— Nat. Herb.: Eden, (also Victoria).
Lower leaves flat, somewhat membranaceous and almost entire (without teeth on the
margins).
HMAC AVESRCLON SACO sNINGAT Gejeyeyco erehet aye imitans heveresloye! weiter = Gyaieuokereveepetarsaeseneliey ic 51. S. fallax Sond.
Locality.—Nat. Herb.: Clarence River. C.S. &1.R.: Bondi, Tuggerah Lakes. Sonder:
Richmond River, Ballina.
Meavesiishorter* Wanceolatey....« si-picveporeyae wlarelanaqe sysrol verse Slaraers 52. S. laevigatum J. Ag.
Locality.—D.T.: New South Wales.
Receptacles acutely angled and dentate.
Receptacles terete, angulate or two-edged, and beset with small scattered teeth; lower
leaves flat, coriaceous, obovate-obtuse and almost entire ..............202ceeceeeees
5 OND OOh.0 0.0 G15 Ghd OKO ORCIOIDIO CHCSCRRDICICT RRO EER RE IGI eci en ers 53. S. globulariaefolium J. Ag.
Locality.—J. Ag.: Illawarra, Port Jackson.
Receptacles triquetro-prismatic with prominent acute-angled edges. .
Reeeptacles without teeth; lower leaves obovate-lanceolate, flat, coriaceous, whole or
slightly or distantly dentate, upper leaves lanceolate-serrate .. 54. S. erosum J. Ag.
Locality. Nat. Herb.: Tuggerah Lakes, Port Jackson. C.S.&I.R.: Manly. J. Ag.:
Port Stephens.
>
1 Sonder (1880) lists S. Muelleri Sond. as from New South Wales. The writer has .
been unable to trace this species; it is not mentioned by J. Agardh (1888) nor by De
Toni (1895).
BY VALERIE MAY. 203
Receptacles toothed; stem branches quadrate with branches arising from the flat
sides; leaves membranaceous, the lower being very large, oblong, lanceolate, deeply
serrate and crowded at the base, the upper very narrow, linear and sharply serrated ;
vesicles near-spherical, possessing a wing-like border and tipped with a nerved and
Serrave del caimemrcree eevee Cicis ous india eneesy sion See aden gcse 55. S. lacerifolium (Turn.) Ag.
Locality.—Nat. Herb.: Ulladulla.
A short, common caulis bears several elongated, branching fronds; leaves simple and
usually bearing conspicuous cryptostomata; vesicles spherical, usually mutic and
petiolate. This is subgenus Husargassum J. Ag.
Mature, fertile branches bearing receptacles associated with and united to the petiolate,
vesicular leaves in the axils of the ordinary leaves; leaves usually serrate and costate.
WCAVESUMALEOW =e AI) cp epeneis strencletonsnel sce cher eis) oiehel eieire 56. S. angustifolium (Turn.) Ag.
Locality.—C.S. & I.R.: Port Jackson. J. Ag.: (also Queensland).
Leaves lanceolate-linear, acuminate ..................... 57. 8. carpophyllum J. Ag.
Locality.— Nat. Herb.: Botany Bay. C.S.&1.R.: Lake Macquarie, (also Queensland).
Mature fertile branches bearing receptacles not associated with or united to the
vesicular leaves.
Receptacles compressed, obovoid-oblong, slightly curved, the apex and outer margins
serrate or dentate; lower leaves oblong-elliptical, with slightly developed midribs,
coriaceous and somewhat serrate, the upper subcuneate falcate, the inner margin
entire, the outer very dentate, midrib not developed ........ 58. S. lophocarpum J. Ag.
Locality.—Nat. Herb.: Wollongong, (also Lord Howe Island). C.S.&I1.R.: Narrabeen,
Manly. Okamura: Bondi, Sydney.
Receptacles not serrate or dentate.
Receptacles completely confluent with the branching system which bears them
SPR He erate ce eee wig cal pails, Gud var oregano ele ayer aie eeretenm rea gina dalle eters 59. S. aquifolium (Turn.) Ag.
Uocality.—Sonder: Plant as S. obovatuwm Grev., Ballina.
Receptacles racemose and each with a distinct pedicel.
Receptacles verrucose and cylindrical; lower leaves lanceolate, costate with serrated
margins, the upper cuneate-obovate and dentate .............. 60. S. fragile J. Ag.
Locality.—C.S. & I.R.: Hawkesbury River, (also Queensland). D.T.: Port Stephens.
Receptacles lanceolate-conoid.
Cryptostomata almost or quite absent: leaves with a prominent, percurrent midrib,
lower leaves broad lanceolate, the upper narrow-linear and entire ..............
BW Seecoha IOU TRE EER GEG TRO CREAM CHEE RTE SRS ae eae EM ea ea 61. S. neurophorum J. Ag.
Locality.—Nat. Herb.: Wollongong, Thirroul, Twofold Bay, (also Lord Howe
Island). C.S.&I1.R.: Narrabeen, (also Queensland). University: Nelson’s Bay,
Port Stephens.
Cryptostomata inconspicuous or arranged in a series on either side of the midrib.
Mature vesicles ellipsoid-spherical, often apiculate and on petioles longer than the
vesicles; leaves serrate-dentate, lower broad-lanceolate, the upper narrow-linear ;
cryptostomata arranged in a series on either side of the midrib ................
Erte erect mea DE Yet fay brah tab al ohms aba atame veri aeita os at SPOT AP ERS Ey ofa dae best a RTE PTGT sires 62. S. leptopodum J. Ag.
Locality.—Nat. Herb.: (also Queensland). C.S.&I1.R.: Coogee, Bondi, Port
Jackson, Jervis Bay, (also Lord Howe Island and Victoria). Herb. Notes:
Bermagui, Port Hacking, Woy Woy, Forster, Urunga.
Vesicles spherical and petiole often shorter than the vesicle it bears.
Leaf serrations never acute.
Upper leaves lanceolate, serrate-dentate or uneven at the margins, with a series
of cryptostomata arranged on each side of the midrib; lower leaves broader and
VARTA Jor, FH CAV OuOSICOMMENE soa d5oacccuuonoGdo000e 63. S. spinuligerum Sond.
Locality. Harv. Aus.: Sydney, (also Victoria). Sonder: (also Queensland).
Lucas (1936): ‘On all the coasts of Australia except the North.’ Muell.:
Ballina.
Upper leaves small, entire or obsoletely dentate, obtuse, with two rows of small
glands; mid-rib conspicuous; lower leaves large, sessile, obtuse and whole
GELATO TY sO UTC Dy iste ce rou scray vc geristyron eos pra lor cueyie shen saeco see cc hepeoliscepa 64. S. Godeffroyi Grun.
Locality.—Muell.: Richmond River. Nat. Herb.: (also Norfolk Island). D.T.:
(also Queensland).
Cryptostomata often completely obsolete; leaves lanceolate-linear, the cauline
whole, the upper sharply acute and unequally serrate-dentate, the teeth often
being prolonged into spines; midribs smooth, percurrent ...............e++20--
Ach eac hts oMCL ours. esucriteneuop sony tie delpousaaren crletenemecacuenstusteheeceicl sicaeel cue 65. S. polyacanthum J. Ag.
204 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
Locality.—Nat. Herb.: Bondi, Little Coogee, Long Bay. C.S. & I.R.: Maroubra,
Jervis Bay, Port Jackson, Wollongong. J. Ag.: ‘Port Jackson et alius locis
New South Wales.’
30. CARPOPHYLLUM Grev.
Lower vesicles spherical-ellipsoid, terminated by a leaf or mucro; the upper piriform-
ellipsoid, mucronate; lower leaves of the young plant much pinnatifid and with uneven
MAL SING wares chara erate. Susdeee ther enmies oleae ce OReMe ere ciaro ere 66. C. phyllanthus (Turn.) H. & H.
Locality.—Muell.: Plant as C. Phyllanthus Grev., Sydney.
31. BLossEvILLBaA Decne. (orthog. mut.).%
Vesicles spring direct from the stem or primary branches.
Vesicles spherical, tmUtl@wacictesiepciereieneie ok oe ere slaieienciel ey cusienensue tees 67. B. uvifera (Ag.) Harv.
Locality.—Nat. Herb.: Plant as Cystophora uvifera (Ag.) J. Ag., Long Bay, Jervis Bay
(cast up), Eden, (also Victoria and Norfolk Island). C.S.&I1.R.: Plant as Cystophora
wuvifera (Ag.) J. Ag., Bondi.
Vesicles cylindro-elliptical, apiculate; stem filiform, the lower part being warted or
muricated with the remains of old branches .... 68. B. Cephalornithos (Labill.) Kuetz.
Locality.—Nat. Herb.: Plant as Cystophora Cephalornithos (Uabill.) J. Ag., (also
Victoria). Lucas (1936): Plant as Cystophora Cephalornithos (Uabill.) J. Ag.,
‘Victoria to Twofold Bay’.
Vesicles spring from ramuli of the last order.
Conceptacles occur in two linear series; vesicles, if present, mutic.
The whole plant sub-distichously pinnate, the pinnae being flattened, pinnatifid; stem
and branches flattened, pinnate along the edges; ultimate pinnules pedicellate, lanceo-
lates passinesinto) broad flat receptacles’; vesiclesisphenicall ss). 2. eiee rele ene eles eel
Sintedsa le tshe ie staal ete eee cee etehensye eiatisneiels Git s sis =, Sues aliate ak 69. B. platylobium (Mert.), nov. comb.
Locality.—Nat. Herb.: Plant as Cystophora platylobium (Mert.) J. Ag., (also
Victoria). C.S.&I1.R.: Plant as Cystophora platylobium (Mert.) J. Ag., Bondi.
Frond pinnately divided, the branches emerging from the flat faces of the rachis and
generally bent back near the base (retrofract); ramuli terete, not conspicuously
compressed.
Vesicles usually numerous, but occasionally absent; plant very variable; axils sub-
rounded; receptacles compressed and somewhat less torulose than usual for the genus
OE ONS ORO Oe SO Eo OR ea eR re icin ie one ae 70. B. retroflexa (Labill.), nov. comb.
Locality.—Nat. Herb.: Plant as Cystophora retroflexa (Labill.) J. Ag., Eden, Kiama,
(also Victoria). C.S.&I1.R.: Plant as Cystophora retroflexa (ULabill.) J. Ag., Bondi,
Thirroul. Muell.: Plant as Cystophora retroflexa (Lab.) Ag., Tilba Tilba, Sydney.
No vesicles occur; stem quadrate and robust (much thicker than in B. retroflexa) ;
pinnate rachides not as flat as in the above-mentioned species; bases of the pinnules
persist as small conical protuberances; receptacles elongated and slightly com-
TOTESSC eve ar cue poten reten sis) + ilshysirs oe: oil shes folgss ulon susie Queiene tele. ¢ 71. B. siliquosa (J. Ag.), nov. comb.
Locality.—Nat. Herb.: Plant as Cystophora siliquosa J. Ag., Jervis Bay, (also
Victoria).
Conceptacles scattered, i.e., not confined to two linear series.
Stem flattened, the rachis being dorso-ventrally compressed and giving off pinnate,
much divided branches from the sharp edges of the rachis, these plano-compressed
like the stem; pinnules warted at the base, thence to the apex closely set with
alternate filiform, setaceous, irregularly dichotomous ramuli; receptacles’. long,
cylindrical, pointed, warted and constricted at short intervals, i.e., nodoso-filiform ;
VESICLES TIA SEM Camels eucssteyeyoicie ce tees skevetere, eucusn s/eisrsvayarenene 72. B. spartioides (Turn.) Decne.
Locality.— Nat. Herb.: Plant as Cystophora spartioides (Turn.) J. Ag., Bermagui
River, Long Bay, Sydney district, Coogee, Kiama, Thirroul, (also Victoria and Lord
Howe Island). University: Plant as Cystophora spartioides (Turn.) J. Ag., Port
Stephens. Herb. Notes: Plant as Cystophora spartioides (Turn.) J. Ag., Illawarra.
Stem usually flattened laterally and, if so, the pinnae emerging from the plane faces.
Stem terete, bearing pinnae and pinnules, ete., from all sides; secondary stems
retrofract (bend downwards at point of insertion); tertiary branches bare on their
lower half, and densely beset above with tertiary ramuli, these latter closely covered
with filiform, setaceous, ultimate ramuli, especially towards the summits; vesicles
not known; receptacles nodose .................. 73. B. paniculata (Turn.) Decne.
Locality.—Nat. Herb.: Plant as Cystophora paniculata (Turn.) J. Ag., Long Bay,
Kiama, Jervis Bay (cast up), (also Victoria). C.S.&1.R.: Plant as Cystophora
See footnote on page 201.
BY VALERIE MAY. 205
paniculata (Turn.) J. Ag., Long Bay. University: Plant as Cystophora paniculata
(Turn.) J. Ag., Bondi, Port Stephens. Lucas (1936): Plant as Cystophora panicu-
lata (Turn.) J. Ag., ‘As far up as Sydney’. Herb. Notes: Plant as Cystophora
paniculata (Turn.) J. Ag., Illawarra, Tuggerah, Newcastle. Muell.: Plant as
Acrocarpia paniculata Aresch., Tilba Tilba.
Stem definitely flattened laterally, with branches arising from the plane faces; pinnae
retrofract ; vesicles present usually.
Vesicles elongate-ellipsoid, acute at both ends, occasionally absent; pinnules
slender, dichotomo-pinnate, the ultimate segments being filiform; receptacles fili-
form, distantly tortulose and ending in sterile beaks .. 74. B. polycystidea Aresch.
Locality Nat. Herb.: Plant as Cystophora polycystidea Aresch., Jervis Bay
(cast up), Long Bay (cast up), (also Victoria). Herb. Notes: Plant as Cysto-
phora polycystidea Aresch., Bateman’s Bay.
Vesicles spherical mutic; primary branches pinnated at intervals of about an inch
with closely-branched and decompound pinnae, these usually bare at the base
except for scars of broken, alternate branchlets; ultimate pinnules dichotomo-
pinnate, slender and almost setaceous; receptacles constricted and so appearing
bead-like, usually each terminated by a setaceous point ..................-0220000-
Ree E BATE Rom eet Sa UR ad cea Telbch sranarey ormet Oretieuae Sucve 75. B. monilifera (J. Ag.), nov. comb.
Locality.—Nat. Herb.: Plant as Cystophora monilifera J. Ag., Long Bay, Jervis
Bay, (also Victoria and Lord Howe Island). C.S.&I.R.: Plant as Cystophora
monilifera J. Ag., Bondi (cast up). Lucas C.S.&1.R. Notes: Plant as Cystophora
monilifera J. Ag., Illawarra, Sydney. Herb. Notes: Plant as Cystophora
monilifera J. Ag., Bateman’s Bay.
32. CYSTOPHYLLUM J. Ag.
Rachides densely muricated; lower leaves linear, entire, pointed and with a row of
cryptostomata on each side of the midrib; upper leaves filiform, with ovoid vesicle
swellings, like beads on a thread, the leaf continuing beyond the vesicle; receptacles
on the interior side of the terminal leaves, racemose, and each stipitate, cylindrical-
lancoid; plant frequents harbours .................. 76. C. muricatum (Turn.) J. Ag.
Locality Nat. Herb.: Port Stephens, Port Hacking, Port Jackson, Lake Macquarie,
(also Queensland and Lord Howe Island). C.S.&I1.R.: Botany Bay, Wallis Lake,
(also Victoria). Lucas (1913): Clarence River. Lucas (1936): ‘All round Australia’.
33. SCABERIA Grev.
Frond a dark colour and much branched, branching being irregular or alternate; lower
part of the stem and older branches denuded of leaves, smooth, filiform and flexuous,
the upper portion and all younger branches closely imbricated with small, vertically-
compressed leaves, which are smooth on the lower side and densely warted on the
upper side; the petioles of these are spirally inserted round the stem; vesicles spherical,
SSMS aime Wwemuscl cogocooncpoenadoogdoDdod OCD goUnOOdOOCDOOCDSOn 77. S. Agardhii Grev.
Locality.—Nat. Herb.: (also Victoria). C.S.&1I.R.: Bondi (cast up). D.T.: (also Lord
Howe Island).
34. PHYLLOSPORA Ag.
Attachment consists of a central, concave, margined disc, radiating from which are
numerous short, robust, simple, closely imbricating, obtuse fibres; the solitary stem
arises from the centre of the disc; branching pinnately decompound; stem and branches
strap-shaped, of approximately the same width throughout, plano-compressed, two-edged,
somewhat thicker in the middle, and densely beset throughout with irregular, marginal
leaves, which taper to each end and are toothed or more or less entire; whole plant
VeLYs tOUlit anal LeaBtherye vein onessos fevcyoneveusvousbavrerslel herpes Gnaverere yeas 78. P. comosa (Uabill.) Ag.
Locality.—Nat. Herb.: Woy Woy, Long Bay, Sydney, (also Victoria and Lord Howe
Island). C.S.&1.R.: Bondi. Herb. Notes: Pambula, Bermagui, Bateman’s Bay, Nowra,
Illawarra, Port Hacking, Botany Bay, Hawkesbury River, Woy Woy, Tuggerah, Lake
Macquarie, Newcastle, Port Stephens, Manning River, Port Macquarie. Muell.: Tilba
Tilba.
35. HormMosira Endl.
Stem triquetrous with interrupted wing expansions, which are more or less dentate;
nodes approximately as long as the vesicated internodes ..............0.0eeseeeeeeee
ST dG ODT ON RCE TO tne ea ict 5 SaPh Grok an RAS DLPRC CENT cy iG. Ouet Rac ae ecae 79. H. ? articulata (Forsk.) Zan.
Locality.—Nat. Herb.: Port Stephens, (also Queensland).
206 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II,
Frond dichotomously or irregularly branched, and consisting of a series of inflated,
vesicated internodes and filiform nodes; internodes act as vesicles and receptacles, they
vary greatly in size and shape according to the habitat, and this accounts for the
synonyms; attachment by means of a minute disc; thallus coriaceous ..............
PF arcee mae whe a hse ea we See, Siete Mie sheave cide shew rete) a ROS Retro aie wide 80. H. Banksii (Turn.) Decne.
Locality.—Nat. Herb.: Botany Bay, Lake Macquarie, Long Bay, Eden, (also Victoria).
cC.S.&1.R.: (also Lord Howe Island). University: Bondi. Herb. Notes: Bermagui,
Lake Illawarra, Forster, Port Macquarie. Lucas (1936): ‘As far north as Pt.
Macquarie’. Laing: (also Norfolk Island).
36. SarcopHycus Kuetz.
Holdfast a large disc; stem sub-terete at base, soon compressed, widening and flat-
tening and so becoming lost in the base of the lamina; lamina thick, simple, or once
or twice forked, the segments being strap-shaped and more or less copiously furnished
with lateral, lanceolate lobes or pinnate, which sometimes are again lobulate or forked
as the lamina, these taper to both ends and possess undulate margins; plant very large,
tough and leathery fearesttnewrs sistele obishsies ies |. BINNS kee 81. S. potatorum (Labill.) Kuetz.
Locality.— Nat. Herb.: Eden, Pambula. C.S.&I1.R.: (also Victoria).
37. NoTHEIA Bail. & Harv.
Cylindrical base of the plant inserted in a conceptacle of the host plant, Hormosira
Banksii (Turn.) Decne.; branches linear-fusiform, much attenuated at their insertion,
and tapering towards the apex, they arise from spore cavities of older branches; axis
composed of long, interwoven filaments, the periphery being of sub-horizontal, parallel,
radiating, slender, coloured filaments .................. 82. N. anomala Bail. & Harv.
Locality. Nat. Herb.: Port Stephens, Crookhaven Heads, Newcastle, (also Victoria).
University: Long Reef. Lucas (1913): Twofold Bay.
38. SPLACHNIDIUM Grev.
Main frond quite simple, linear-club-shaped, cylindrical, tapering to the base, truncate
at the apex; lateral branches similar to the primary, and spring proliferously from its
sides; there may be tertiary similar ramuli; whole plant very mucilaginous; attach-
MENE DyMMeanseonrawconical (GiSC) A. aecr. -- taaeseeie] ete oe 83. S. ruwgosum (Linn.) Grev.
Locality.— Nat. Herb.: Ocean coasts about Sydney, Crookhaven Heads, Newcastle,
(also Victoria). C.S.&I1.R.: Middle Harbour, Narrabeen, Bondi, Long Bay. lucas
(1936): ‘As far north as Newcastle.’ Muell.: Tilba Tilba.
SYNONYMS.
Under the name of each accepted species are listed those synonyms which
various workers have attributed to it. In each case a bracketed number then
follows. This number indicates the authority quoted far the acceptance of the
synonymy. The numbers and their corresponding references are: (1) De Toni,
G. B. (1895); (2) Harvey, W. H. (1858-63); (3) Harvey, W. H. (1846-51);
(4) Agardh, J. (1888); (5) Laing, R. M. (1900); (6) Laing, R. M. (1906);
(7) Lucas, A. H. S. (1909); (8) Herbarium Notes from the Lucas Collection,
C.S.&1.R., Canberra; (9) Newton, Lily (1931); (10) Lucas, A. H. S. (1913);
(11) Setchell, W. A., and Gardner, N. L. (1925); (12) Sonder, W. (1871); (13)
The generic name has been changed by the writer in the present paper; (14)
Grunow, A. (1874); (15) Sonder, W. (1880); (16) Kuckuck (1930).
1. SPHACELARIA CIRRHOSA (Roth.) Ag. Conferva cirrhosa Dillw. (3)
Sphacelaria cervicornis Ag. (1) fusea Huds. (1)
cirrosa var. cervicornis Ardiss. (1) intertexta Roth. (3)
fusca Ag. (1) marina Dillw. (3)
irregularis Kuetz. (ex parte) (1) pennata Huds. (1), (3)
japonica Martens (1) prebrevis Dillw. (3)
pennata Lyngb. (1) villosa Dillw. (3)
pennata Lyngb. (excl. var. B). (3) Stypocaulon bipinnatum Kuetz. (1)
racemosa Reinsch. (1) Ceramium cirrhosum Hook. (3)
rhizophora Kuetz. (1) cirrhosum Ag. (1)
Conferva cirrhosa Roth. (1), (3) pennatum Roth. (1)
BY VALERIE MAY.
Varieties include:
Sphacelaria fusca Harv. (9)
2. SPHACELARIA TRIBULOIDES Menegh.
Sphacelaria brachygonia Mont. (1)
caespitula Kjellm., non Lyngb. (1)
capensis Kuetz.? (1)
cervicornis Decne.? (1)
fulva Kuetz. (1)
Novae-Hollandiae Sond. (1)
rigida Hering. (1)
Ceramium fulvum Bertol. (1)
3. CLADOSTEPHUS SPONGIOSUS (Lightft.) Ag.
Cladostephus laxus Fl. Dan. (?) excl. syn.
(1), (3)
setaceus Suhr.? (1)
verticillatus var. spongiosus Farl.
Ceramium spongiosum DC. (1)
Fucus hirsutus Linn. (non Wulf.) (1), (3)
Conferva spongiosa Huds. (3)
spongiosa Lightft. (1)
(1)
4. CLADOSTEPHUS VERTICILLATUS (Lightft.)
Ag.
Cladostephus australis var. ponticus Sperk.
(1)
hedwigioides Bory ? (1)
Myriophyllum Ag. (1), (3)
spongiosus Kuetz., non Ag.-(1)
tomentosus Kuetz. (1)
Fucus hirsutus Wulf., non Linn. (1)
verticillatus Wulf. (1), (3)
Conferva ceratophyllum Roth. (71), (3)
Myriophyllum Roth. (1), (3)
verticillata Lightft. (1), (3)
Ceramium verticillatum DC. (1), (3)
5. STYPOCAULON PANICULATUM (Suhr.)
Kuetz.
Stypocaulon filare Kuetz. (1)
gracilescens Kuetz. (1)
hordeaceum Kuetz. (1)
virgatum Kuetz. (1)
Sphacelaria filaris Sond. (1)
gracilescens Dies. et J. Ag. (1)
hordeacea Harv. (1), (2)
Muelleri Sond. (2)
paniculata Suhr., non Hering. (1), (7)
scoparia Sond. (2)
(Stypocaulon) spicigera Aresch.
virgata H.& H. (1)
6. LEATHESIA DIFFORMIS (Linn.) Aresch.
Leathesia marina J. Ag. (1)
marina Endl. (3)
tuberiformis 8S. F. Gray (1), (3), (9)
Chaetophora marina Lyngb. (1), (3)
«
(1)
Nostoc marinum Ag. (1), (3)
mesentericum Ag. (1)
Clavatella Nostoc Bory. (1)
Rivularia tuberiformis Engl. Bot. (1), (3)
Corynephora .baltica Kuetz.? (1)
marina Ag. (1), (3)
Ulva mesenterica Bonn. (1)
Corynophloea baltica Kuetz. (1)
Tremella difformis Linn. (1), (8), (11)
207
7. ASPEROCOCCUS BULLOSUS Lamour.
Asperococcus rugosus B. bullosus Duby.
(1), (3)
tenuis Zan. (1)
Turneri Hook. (1), (3),
utricularis D’Urv. (1)
Encoelium buliosum Ag. (1),
Mac-Gregoryi Suhr. (1)
tenue Kuetz. (1)
utriculare Kuetz. (1)
Gastridium Opuntia Lyngb. (1), (3)
Ulva Turneri Dillw. (1), (3)
8. ILEA FAascrA (Muell.) Fries.
Phyllitis caespitosa Le Jol. (1)
fascia Kuetz., non Le Jol. (1), (11) ;
Phycolapathum cuneatum Kuetz. (1) ac
Laminaria caespitosa J. Ag. (1)
cuneata Suhr. (1), (3), (6)
debilis Ag. (3) f
fascia Ag. (1) iS
fascia Muell. (6) stp if
papyrina Bory (3)
Fucus fascia Muell. (1),
fascia Fl. Dan. (3)
Ulva fascia Lyngb. (6) ?
Petalonia fascia Kuntze (11)
Varieties include:
Phyllitis debilis Kuetz.
filiformis Batt. (11)
Zosterifolia Reinke (11)
Petalonia debilis Derb. & Sol. (1)
Fucus Phyllitis var. subsessilis Clem. (1)
Laminaria caespitosa J. Ag. (11)
debilis Ag. (1), (11)
papyrina Bory? (1)
Phyllitis Delle Chiaje Hydrophyt. (1)
ScYTOSIPHON LOMENTARIA (Lyngb.)
J. Ag.
Scytosiphon filum var. fistulosus Ag.
filum var. lomentarius Ag. (1)
filum var. y Ag. (3)
fistulosus Ag. (1)
lomentaria Endl. (3)
Chorda filum var. fistulosa Kuetz. (1)
filum var. lomentaria Kuetz. (1)
fistulosa Zan. (1), (3)
lomentaria Lyngb. (1), (11)
Ulva fistulosa Good. & Woodw. (1)
simplicissima Clem. (1)
Conferva fistula Roth. (1)
Solenia fuscata Bory (1), (3)
Asperococcus castaneus Carm. (1), (3)
Chlorosiphon Shuttleworthianus Kuetz. (3)
10. COLPOMENIA SINUOSA (Roth.) Derb.
& Sol.
Asperococcus sinwosus Bory. (1), (7)
Ulva cavernosa Forsk. (?) (1)
sinwosa Roth. (1), (11)
FEncoelium sinuosum Ag. (1)
sinwosum Kuetz. (12)
vesicatum Kuetz. (1)
Hydroclathrus sinuosus Zan. (1)
Stilophora sinuosa Ag. (1)
vesicata Harv. (1)
(7)
(3)
(11)
(1)
g),
qQ)
208
Nostoc mesentericum Delle Chiaje
Hydrophyt. Neap. (1)
Tremella cerina Clem. (1)
rugulosa Clem. (1)
Zonaria sinuosa Ag.
Varieties include:
Colpomenia tuberculata Saund. (11)
Scytosiphon bullosus Saund. (11)
11. EcrocarPus SIMPLICIUSCULUS Ag.
Ectocarpus irregularis Kuetz. (1)
12. ECTOCARPUS CONFERVOIDES (Roth.)
Le Jol.
Ectocarpus amphibius Harv. (1 a’)
confervoides var. siliculosus Auct. (1 a’)
corymbosus Kuetz. (1 a’)
gracillimus Kuetz. (1 a’)
siliculosus Harv. (9)
siliculosus Lyngb. ex parte (1), (11)
spalatinus Kuetz. (1 a’)
viridus Harv. (1 a’)
Ceramium confervoides Roth. (1),
(11)
confervoideum Roth. (1a’)
siliculosum var. atrovirens Ag. (1)
siliculosum Ag. (1a’), (3 a’)
Conferva siliculosa Dillw. (1a’), (3 a’)
siliculosa Dillw. (excl. synonyms) (11 a’)
Varieties include:
Ectocarpus amphibius Harv.
approximatus Kuetz. (1)
arachnoideus Zan. (1)
arctus Kuetz. (1 a’)
bombycinus Kuetz. (1)
ceratoides Kuetz. (1)
confervoides f. arcta Kjellm. (1 a’)
var. hiemalis Kjellm. (1 a’)
B. subulatus Hauck. (excl. synonyms)
Glave)
f. subulatus Collins, Holden & Setchell
(11 a’)
draparnaldioides Kuetz. (1 a’)
draparnaldiaeformis Kuetz. (1)
fasciculatus Kuetz., non Harv. (1)
flagelliformis Kuetz. (1)
flavescens Kuetz. (1)
fuscatus Zan. (1a’)
hiemalis Crouan (1 4a’)
intermedius Kuetz. (1 a’)
Kochianus Kuetz. (1)
leptocarpus Kuetz. (1)
macroceras Kuetz. (1)
nebulosus Zan.? (1)
nitens De Not. (1)
ochroleucus Kuetz. (1 a’)
patens Kuetz. (1)
polycarpus Zan. (1a’)
pseudosiliculosus Crouan (1 a’)
pygmaeus Aresch. (1), (11)
rigidus Kuetz. (1a’)
rufulus Kuetz. (1 a’)
(3 a’),
(11 a’)
KEY TO THE MARINE ALGAE OF NEW SOUTH WALES.
Il,
Ectocarpus siliculosus nebulosus Ag.
parvis Saunders (11)
spinosus Kuetz. (1 a’)
subulatus Kuetz. (1), (11 a’)
terminales Collins, Holden & Setchell (13 )
venetus Kuetz. (1)
vermicelliferus De Not.
verminosus Kuetz. (1 a’)
Corticularia arcta Kuetz. (1 a’)
fuscata Kuetz. (1 a’)
Naegeliana Kuetz. (1)
verminosa Kuetz. (1 a’)
13. PYLAIBLLA LITTORALIS (Linn.) Kjellm.
Pylaiella flexilis Rupr. (1)
nordlandica Rupr. (1)
pyrrhogon Rupr. (1)
saxatilis Rupr. (1)
Ectocarpus compactus Ag. (1), (3)
crinitus Croall ? (1)
ferrugineus Ag. (3)
firmus Aresch. (f. vernalis Aresch. et
var. rupincola Aresch.). (1)
littoralis Ag. (1)
f. protensus Lyngb. (11)
ochraceus Zell. Zweite Polarfahrt., non
Kuetz. (1)
Conferva littoralis Linn. (1), (3)
littoralis Linn. (in part). (11)
Varieties include:
Pylaiella littoralis Kjellm. ex parte (1)
f. compacta (Linn.) Kjellm. (1)
macrocarpa Foslie (1)
varia Kjellm. (1)
Ectocarpus brachiatus Ag. (1)
compactus Ag. ex parte (1)
firmus J. Ag. (1)
var. rupincola Aresch. (1)
f. vernalis Aresch. (1)
fluviatilis Kuetz. (1)
Landsburgii Dick. (1)
littoralis Wyatt (1)
var. brachiatus J. Ag. (1)
f. brachiatus Aresch. (1)
f. vernalis Kjellm. (1)
var. y compactus J. Ag. (1)
ramellosus Kuetz. ex parte (1)
siliculosus y firmus Ag. (1)
subverticillatus Kuetz. (1)
Vidovichii in Heugl. Reise non Menagh.
(1) ;
Spongomorpha castanea Kuetz. (1)
Ceramium compactum Roth. ex parte (1)
Spongonema castaneum Kuetz. (1)
14. BacTROPHORA NIGRESCENS (Harvy.)
Jee.
Cladosiphon nigrescens Harv.
nigricans Harv. (1), (7)
15. BAcTROPHORA FILUM (Harv.) J. Ag.
Mesogloia filum Hary. (1)
(1)
(1)
q)
18 The ‘fa’? within the number bracket indicates that this is claimed by the authority
quoted as a synonym of #. siliculosus (Dill.) Lyngb., which species he regards as distinct
from E£. confervoides (Roth.) Le Jol.
BY VALERIE MAY.
17. CHNOOSPORA PACIFICA J. Ag.
Chnoospora fastigiata var. pacifica J. Ag.
(11)
Sargassum piluliferum Collins, Holden &
Setchell (11)
19. SPOROCHNUS RADICIFORMIS (R.
Ag.
Fucus radiciformis R. Br. (1), (2)
21. CARPOMITRA COSTATA Batt.
Carpomitra Cabrerae Kuetz. (9)
Fucus Cabrerae Clem. (1), (3)
costatus Stackh. (9)
Sporochnus Cabrerae Ag. (1), (3)
Cabrera gaditana Schousb. (1)
22. MyrioGuoia scuRIUS (Harv.) Kuckuck
Myriocladia scuriws Hary. (11), (16)
23. ScyTOTHAMNUS AUSTRALIS (J. Ag.)
H. & H.
Chordaria australis J. Ag. (1)
24. SPERMATOCHNUS LEJOLISII (Thur.)
Reinke.
Spermatochnus microspermus Wuetz.? (1)
Stilophora Lejolisii Thur. (1), (9)
25. MAcCROCYSTIS PYRIFERA (Linn.) Ag.
Macrocystis angustifolia var. oocysta Ag.
(1)
communis Bory (1)
Dubenii Aresch. (1)
Humboldtit Ag. (1)
latifolia Bory (M. latifolius) (1)
latifrons Bory ? (1)
orbignyana Mont. (1)
pelagica Aresch. (1)
planicaulis Ag. (1)
pomifera Bory (1)
tenwifolia Post. & Rupr. (1)
Laminaria pomifera Lamour. (1)
Fucus hirtus Humb. et Bonpl. (1)
Humboldtii Bonpl. (1)
piriferus Linn. (excl. syn. Esper) (1)
piriferus Linn. (11)
Lessonia armata J. Ag. (1)
ciliata Post. et Rupr. (1)
Varieties include:
Macrocystis Dubenii Aresch. (2)
26. EXCKLONIA RADIATA (Turn.) J. Ag.
Fucus radiatus Turn. (1)
Laminaria radiata Ag. (1)
Capea radiata Endl. (1)
Varieties include:
Ecklonia exasperata (Turn.) J. Ag. (1),
(2)
flagelliformis J. Ag. (1)
lanciloba’® Sond. (2)
Richardiana J. Ag. (1), (2)
Fucus radiatus var. exasperatus Turn. (1)
Laminaria biruncinata Bory (1)
Cunninghamii Grev. (1)
flagelliformis A. Rich. (1)
Prieurii Bory (1)
radiata var. exasperata Ag. (1)
Br.)
209
Capea biruncinata Mont. (1)
exasperata Mont. (1)
flabelliformis H. & H. (1)
Pinnaria fastigiata Endl. & Dies. ? (1)
27. ECKLONIA LANCILOBA Sond.
Capea biruncinata y elongata Sond. (1)
28. GYMNOSORUS VARIEGATUS (Lamour.)
do ANE
Zonaria variegata Mert. (1)
Dictyota variegata Lamour. (1)
Spatoglossum variegatum Ixuetz. (1)
Padina lobata Mont. ? (1)
variegata Gaill. (1)
variegata Mont. (1)
Orthosorus variegatus Trev. (1)
Stypopodium fissum Kuetz. (1)
laciniatum Kuetz. (1)
29. GYMNOSORUS NIGRESCENS (Sond.)
do “ANE
Zonaria nigrescens Sond. (1)
Orthosorus nigrescens Trev. (1)
Spatoglossum nigrescens Kuetz. (1), (12)
30. ZONARIA TURNERIANA J. Ag.
Zonaria interrupta Ag. (1)
Phycopteris angustata Kuetz., non Dictyota
interrupta Lamour. (1)
interrupta Wuetz. ex parte (1)
Fucus interruptus Turn. (1)
32. ZONARIA CRENATA J. Ag.
Zonaria flava Harv., non Ag. (1)
var. tenwior Sond. (1)
3. HOMOEOSTRICHUS SINCLAIRII (H. & H.)
J. Ag.
Zonaria Sinclairii H. & H. (1)
Phycopteris Sinclairii Kuetz. (1)
Stypopodium Sinclairii Kuetz. (1), (2)
34. PADINA FRASERI (Grev.) J. Ag.
Zonaria Fraseri Grev. (1)
Pavonia var. fuscescens Ag. (1)
3d. PADINA PAVONIA (Linn.) Lamour.
Padina anglica Kuetz. (1)
Commersoni Auct. (2)
D’Urvillaei Auct. (2)
D’Urvillaei Bory ? (5)
Fraser Grev. (2)
gymnospora Kg. (5)
Mediterranea Bory’ (1), (3)
Neapolitana Kuetz. (1)
Oceanica Bory (1)
Dictyota Pavonia Lamour. (1), (3)
Ulva cucullata Cav. (1), (38)
Pavonia Linn. (1), (3)
Flabellaria Pavonia Lamarck (1)
Zonaria gymnospora WKuetz. (14)
Pavonia Ag. (3)
Pavonia Draparn. (1)
tenwis Kuetz. (excl. var.), non Z.
Pavonia var. tenuis Ag. (1)
Fucus Pavonicus Gmel. (1)
Pavonius Linn. (1), (3)
12 Following De Toni, this synonym has not been accepted.
*0 This synonym has not been accepted by the writer.
in the key.
R
See footnote to genus Padina
210
Varieties include:
Spatoglossum versicolor K. (15)
NEUROCARPUS ACROSTICHOIDES (J. Ag.),
nov. comb.
Haliseris acrostichoides J. Ag.
Muelleri Harv. (partim) (1)
38. NruRocARPUS MUELLERI (Sond.), nov.
comb.
Haliseris Muelleri Sond. (13)
polypodioides Harv. (1)
polypodioides Hary. (excl. syn.) (2)
39. NEUROCARPUS WoOODWARDIA (R. Br.),
nov. comb.
Haliseris Woodwardia (R. Br.) J. Ag. (13)
polypodioides var. denticulata Sond. (10)
Fucus Woodwardia Brown. (1)
Woodwardia Turner Hist. (12)
40. NBEUROCARPUS POLYPODIOIDES (Desf.),
nov. comb.
Haliseris polypodioides (Desf.) Ag. (13)
Fucus ambiguus Clem. ? (1)
membranaceous Stackh. (1)
polypodioides Desf. (1)
Ulva polypodioides DC. (1)
Dictyopteris elongata Lamour. (1)
polypodioides Lamour. (1)
42. DicTYOTA RADICANS Harv.
Dictyota intermedia Zan. ? (1)
zonata J. Ag. (1)
43. DicryoTa DICHOTOMA (Huds.) Lamour.
Dictyota acuta Kuetz. (1)
attenuata Kuetz. (1)
(Dictyopteris ?) areolata Schousb. (1)
(Dictyopteris ?) complanata Schousb. (1)
dichotoma volubilis Lenorm. (1)
elongata Kuetz. (1)
implexa Lamour. (1)
intricata Kuetz. (14)
latifolia Kuetz. (1)
ornata Zan. (1)
? setosa Duby. ? (1)
sibenicensis Zan. (1)
spiralis Mont. ? (1)
volubilis Kuetz. (1)
vulgaris Kuetz. (1)
Neurocarpus anniularis Schousb. (1)
areolatus Schousb. (1)
Fucus dichotomus Bertol. (1)
Ulva dichotoma Inti (Gla (8)
Dichophyllium dicholomium Isuetz. (1), (3)
vulgare Kuetz. (1), (3)
Zonaria dichotoma Ag. (1), (5)
Haliseris dichotoma Spreng. (3)
Varieties include:
Dictyota impleza Lamour. (3)
Dichophyllium implexwm Iuetz. (3)
45. DiIcTYOTA LINEARIS (Ag.) Grev.
Dictyota aequilis Kuetz. ?? (1)
angustissima Sond. (1)
ceylanica Kuetz. ? (1)
divaricata Kuetz. (1)
fibrosa Kuetz. (1)
Zonaria linearis Ag.
37.
(13)
(excl. synon.) (1)
*tDe Toni considers this is more probably Sargassum grande.
KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. IL,
47. LOBOSPIRA BICUSPIDATA
ry ~)
or co bo bo
ono oct e
BY VALERIE MAY.
Fucus Phyllitis var. subses-
silis Clem.
piriferus Linn.
Platylobium Mert.
polypodioides Desf.
potatorum Labill.
radiatus Turn.
radiciformis R. Br.
retroflexus Lapbill.
retroflecus Turn.,
Labill.
rugosus Turn.
rugosus Linn.
spartioides Turn.
trichophyllus Klein.
triqueter Delile
verruculosus Mert.
verticillatus Wulf.
Woodwardia Brown ..
non.
Gastridium Opuntia Lyngb.
Haliseris acrostichoides J. Ag.
dichotoma Spreng.
Muelleri Harv. Gontins)
Muelleri Sond. OURS?
polypodioides Harv. (excl.
syn.) Abs 3113
polypodioides var. denticu-
lata Sond. A SY ANE
polypodioides (Desf.) Ag.
Woodwardia (R. Br.) J. Ag.
Hormosira Billardieri Mont.
gracilis Kuetz.
obconica Kuetz. ..
Sieberi Decne.
triquetra Decne. :
Hydroclathrus sinuosus Zan.
Laminaria biruncinata Bory.
caespitosa J. Ag.
cuneata Suhr.
Cunninghamii Grev.
debilis Ag.
fascia Ag.
fascia Muell. Aes
flagelliformis A. Rich.
papyrina Bory? ,
Phyllitis Delle Chiaje
Hydrophyt.
pomifera Lamour.
potatorum Gamour.
Prieurii Bory
radiata Ag. ate 5
var. exasperata Ae.
Leathesia marina J. Ag.
marina Endl,
tuberiformis S. F. Gray
Lessonia armata J. Ag.
ciliata Post. et Rupr.
Macrocystis angustifolia var.
oocysta Ag. 0.0
communis Bory... ., 5,
bo
on
6
40
(Ju)
Aare wo
cow nore
co CO CO Co m1 or-1 WD 0 7
“1 co =I -1 Oo me OO cS bo fo Co ON
wn
bo
=r)
bo
rae. < ao 2)
bo bo
manrnwnn
bdoww we
SHH ke OI CO
hr or er)
Macrocystis comosa Ag. 78
Dubenii Aresch. 25
Humboldtii Ag. - og 240)
latifolia Bory (M. lati-
folius) 25
latifrons Bory ? 25
Orbignyana Mont. 25
pelagica Aresch. 25
planicaulis Ag. 25
pomifera Bory 25
tenuifolia Post. & Rupe 25
Mesogloia filum Harv. 15
Metachroma thuyoides Harv. 47
Moniliformia Banksii Bory 80
Labillardieri Bory 80
Sieberi Bory 80
triquetra Decne. so) 09)
Myriocladia Scurius Harv... 22
Neurocarpus annularis
Schousb. 43
areolatus Schousb. 43
Nostoc Marinum Ag. 6
mesentericum Ag. .. .. 6
mesentericum Delle Chiaje
Hydrophyt. Neap. 10
Orthosorus nigrescens Trev. 29
variegatus Trev. 28
Padina anglica Kuetz. 35
Commersoni Auct. 35
D’Urvillaei Auct. 35
D’Urvillaei Bory ? 35
gymnospora Kg. 35
lobata Mont.? 28
Mediterranea Bory 35
Neapolitana Kuetz. 35
Oceanica Bory 35
variegata Gaill. 28
variegata Mont. oo eae
Petalonia debilis Derb. &
Sol. 8
fascia Kuntze 8
Phycolapathum Aneation
Kuetz. 8
Phycopteris E ngustane inetes
(non Dictyota inter-
rupta Lamour.) 30
interrupta Kuetz., ex parte 30
Sinclairii WKuetz. 5.0) 3383
Phyllitis caespitosa Le Jol. 8
debilis Kuetz. BN Saye ats
fascia Kuetz. (non Le
Jol.) age 8
filiformis Batt. 8
Zosterifolia Reinke 8
Phyllotricha spartioides
Aresch. ste eda
Pinnaria fastigiata Endl. &
Dies.? 26
Platylobium Mer seni ENE, 69
214 KEY TO THE MARINE ALGAE OF NEW SOUTH WALES. II, ~
Pylaiella flexilis Rupr.
littoralis f. compacta
(Linn.) Kjellm.
macrocarpa Foslie
nordlandica Rupr.
pyrrhogon Rupr.
saxatilis Rupr.
varia WKjellm.
Rivularia
Bot.
Sargassum adenophyllium
Harv. ae Sis
angustifolium (Ag.) J. £
capillaceum H. & H.
densifolium var.
pressa Grun.
flexile Grev.
herbaceum WKuetz.
obovatum Grev.
obovatum Sond.?,
Harv. nec Grev.
paradoxzum J. Ag.
Phyllanthus Ag.
non
piluliferum Collins, Holden
& Setchell
Raoulii H. & H.
uviferum Ag.
virescens Fig. et De Not
Scytosiphon
var. lomentarius Ag.
var. y Ag.
fistulosus Ag. ..
lomentaria Endl.
Sirophysalis binodis Kuetz...
muricata Kuetz.
trinodis Kuetz.
virgata Kuetz.
Solenia fuscata Bory
Spatoglossum
Kuetz.
versicolor Ix.
nigrescens
AGARDH, J.,
BaILby, F. M.,
tuberiformis Eng].
subcom-
bullosus Senviail
filum var. fistulosus Ag...
6
1 -]
WCAAADMDwWwH wos
a -1
bo
co
or
oo
1888.—Species Sargassorum Australiae.
Brisbane, xi, 7-69, Pl. 1-17.
Dr TONI, G.
ENGLER, A.,
GARDNER, N.
Pl. 481.
GRUNOW, A.,
Godeffroy, iii,
HARVEY, W. H.,
————,, 1858-63
LAING, R. M.,
XXxili, 299-301.
—————,, 1905.—Appendix to the List of Seaweeds of Norfolk Island.
XXXvili, 424,
Inst.,
B., 1895.—Sylloge Algarum, Vol.
and PRANTL, K.,
Ibe) G83
SEPP, A., and E. S.,
.—New Fucaceae.
1906.—Some Marine Algae from N.S.W.
1874.—Algen
23-50.
1846-51.—Phycologia Britannica.
.—Phycologia Australica
Kuckuck, P., 1930.—Fragmente einer Monographie des Phaeosporeen.
Meeresuntersuchungen,
Mush, =Ayent
1900.—A List of the Seaweeds of Norfolk Island.
der Fidschi-, Tonga-
1-93.
and Synopsis.
und Samoa-
London.
Spatoglossum variegatum Stypocaulon gracilescens
Kuetz. nd Ls Kuetz.
Spermatochnus micr SORPIETEIE hordeaceum ranetee
Kuetz.? 24 virgatum Kuetz. 7
Sphacelaria br nonugonta Stypopodium fissum Eeneia
Mont. Chu eter bee 2 laciniatum Kuetz.
caespitula Kjellm., non Sinclairii Wuetz.
Lyngb. 2
capensis WKuetz.? 2 Tremella cerina Clem.
cervicornis Ag. iL difformis Linn.
cervicornis Decne.? Ce rugulosa Clem.
cirrosa var. cervicornis
Ardiss. 1 Ulva cavernosa Forsk. (?) ..
filaris Sond. 5 cucullata Cav.
fulva Kuetz. 2 dichotoma Huds.
fusca Ag. 1 fascia Lyngb. ash ee
fusca Harv. 1 fistulosa Good. & Woodw.
gracilescens Dies. et J. Ne 5 mesenterica Bonn,
hordeacea Harv. 5 Pavonia Linn.
irregularis IXuetz. ex nate 1 polypodioides DC.
japonica Martens i rugosa Linn.
Muelleri Sond. 06 5 simplicissima Clem.
Novae-Hollandiae Sond. 2 sinuosa Roth.
paniculata Suhr., non Turneri Dillw.
Hering. ads 5
pennata Lyngb. 1 Zonaria dichotoma Ag.
racemosa Reinsch. il flava Harv. non Ag.
rhizophora Kuetz. 1 var. tenuwior Sond.
rigida Hering. 2 Fraseri Grey.
scoparia Sond. og | gymnospora Kuetz.
(Stypocaulon) spicigera interrupta Ag.
Aresch. .. : 5 linearis Ag. (excl. aon)
virgata H. & HL. 5 nigrescens Sona. :
Spongomorpha castanea Pavonia var. fuscescens
Kuetz. : 113} Ag. '
Spongonema aatemenin Pavonia Ag.
ESUISEZ no Pavonia Draparn
Sporochnus Gannenae Ae 21 ie Hii, ;
Stilophora Lejolisii Thur. 24 Sinclair HH. & HH:
sinuosa Ag. 10 siuosa a Pres.
nesicata Elarv. 10 tenwis Kuetz. (excl. var.),
Stypocaulon iRevachomnarzaiere non 4. Pavonia var.
Kuetz. 1 tenuis Ag.
filare Kuetz. 5 variegata Mert.
References.
Stockholm.
1895.—Contributions to the Queensland Flora. Bot. Bull. Dept. Agric.
3, Fucoideae. Padua.
1897.—Die naturlichen ee seins
Univ. Calif. Publ. in Bot., iv, 317-374, Pl. 36 aa
xliv, 249-26
ae ee
Inseln. Jour. Museum
London.
Wissenschaftliche
Trans. Proc. N.Z. Inst.,
Trans. Proc, N.Z,
BY VALERIE MAY. 215
LAING, R. M., 1906.—Notes on the Occurrence of Phyllitis fascia (Muell.) Kuetz. in New
Zealand. Trans. Proc. N.Z. Inst... Xxxix, 220-221.
Lucas, A. H. S., 1909.—Revised List of the Fucoideae and Florideae of Australia. Proc.
LINN. Soc. N.S.W., xxxiv, 8-60.
, 1913.—Notes on the Australian Marine Algae. 1. Proc. LINN. Soc. N.S.W.,
XxXxXvili, 49-60, Pl. 1-5.
————, 1985.—The Marine Algae of Lord Howe Island. Proc. LINN. Soc. N.S.W., Ix,
194-232, Pl. 5-9.
——_——, 1936.—The Seaweeds of South Australia, Part 1, Introduction and the Green
and Brown Seaweeds. Adelaide.
Newton, Linty, 1931.—Handbook of the British Seaweeds. London.
OKAMURA K., 1904.—List of Marine Algae collected in Caroline Islands and Australia.
Bot. Mag. Tokyo. xviii, 77-96.
OLTMANNS, F., 1922.—Morphologie und Biologie der Algen. Jena.
SETCHELL, W. A., and GARDNER, N. L., 1925.—The Marine Algae of the Pacific Coast of
North America, Part 3. Melanophyceae. Univ. Calif. Pwbl. in Bot., viii, 383-898,
Pl. 34-107.
SoNpDER, W., 1871.—Die Algen des tropischen Australiens. Hamburg.
, 1880.—Algae Australianae hactenus cognitae, and Algae e manuscriptis
praecipue in Von Mueller: Fragmenta Phytographiae Australiae. xi, 1-42 and 105-107.
TILDEN, J. E., 1935.—The Algae and their Life Relations. Minnesota.
TILDEN, J. E., and FESSENDEN, A. P., 1931.—Bactrophora irregularis, a new brown alga
from Australia. Bull. Torrey Bot. Club, lvii, 381-388, Pl. 20-21.
TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. II.
A NEW NEOTROPICAL GENUS OF EMBIOPTERA.
By Consett Davis, M.Se., Lecturer in Biology, New England University College.*
(Twenty-one Text-figures. )
[Read 31st May, 1939.]
OLIGEMBIA, nN. gen.
Genotype: Oligotoma hubbardi Hagen, 1885, Canadian Entomologist, vol. 17,
p. 142.
Very small Embioptera, the males with the following characters: Winged, the
main veins greatly reduced in their development without reduction in number.
R, and main stem of Cu, strong; R.,; weak; remaining veins represented only by
their bordering pigment-bands and by rows of macrotrichia, sparse and little
obvious. These remnants of the main veins follow the course of those of the genus
Embia, Ry,; being clearly forked, the fork longer than the stem; M simple; anterior
branch of cubitus (Cu,.) simple, very weak. Mandibles slender, terminally
incurved and acute. Hind legs with first tarsal segment devoid of bladders.
Terminalia with tenth abdominal tergite divided by a longitudinal suture, obsolete
proximally; right hemitergite with a long thin process directed backwards; process
of left hemitergite complex; left cercus-basipodite well-developed, associated closely
with base of left cercus; no nodules on any of the segments of the cerci.
2 unknown.
Southern parts of the United States to South America.
The genus is closely allied to Diradius Friederichs 1934 (genotype D. pusillus
Friederichs 1934), from Brazil, in which, however, the process of the left hemi-
tergite is simply tapered, and the left cercus-basipodite of different form. The
species are superficially similar to those of Oligotoma; the forking of the trace
representing R,,; immediately differentiates them, and seems to rule out descent
from Oligotoma, just as the more complex terminalia and more complete reduction
in strength of the veins rules out the descent of Oligotoma from Oligembia. To
some extent the mandibles, hind tarsi, left cercus-basipodite, elongate process of
the right hemitergite and incomplete fission of the last abdominal tergite, suggest
some relationship to Oligotoma, but whether this is due to common descent from
a type possessing some or all of these characters, or merely to convergence, is at
present problematical.
Although one of the South American species referred by Enderlein to
Rhagadochir Enderlein 1912 is herein referred to Oligembia, the others do not seem
to be closely related. The genotype of Rhagadochir (Rh. vosseleri End.) is African,
and no South American species is actually congeneric with it; a new generic name
* A considerable part of the work embodied in this paper was performed when the
writer held a Linnean Macleay Fellowship in Zoology.
i)
218 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. II,
is required for this South American series, of which Hmbia trinitatis de Saussure
1896 is a typical example. This series agrees with Oligembia in having the process
of the left hemitergite complex, but differs in the complete fission of the last
abdominal tergite, number of hind tarsal bladders, and in having the first segment
of the left cercus echinulate, the veins R,,,; and M more strongly developed, ete.
OLIGEMBIA HUBBARDI (Hagen, 1885). Figs. 1-5.
Oligotoma hubbardi Hagen, 1885, Canad. Entomologist, vol. 17, p. 142.
6. Length 4 mm.; forewing 3-7 mm. x 1:0 mm. (dimensions of the type).
General colour pale yellowish-brown, head somewhat darker, eyes black, wings
very pale brown with hyaline streaks between veins or their traces. Head (fig. 1)
slender, eyes relatively large; sides of head behind eyes relatively straight, scarcely
converging. Mandibles slender, incurved distally, acute, the apex weakly bifid.
Antennae incomplete. Body sclerites, except the terminalia, as in Oligotoma.
Wings (fig. 2) with Se reaching to one-quarter the length of the wing; R, strong,
confluent subterminally with R.,,, the fused vein not quite reaching the termen.
R,,;, M and Cu,, represented only by pigment-bands and weak rows of macrotrichia;
R,,, with fork twice length of stem; M simple; Cu, very weak; A short but
distinct. No cross-veins apparent. Terminalia (figs. 3, 4, 5) with tenth tergite
divided incompletely by a submedian suture, obsolete proximally; right lobe (10R)
produced backwards and inwards to a slender evenly-tapered process (10RP),
curved outwards terminally. Three minute claw-like hooks placed dorsally on
10RP a little before the apex. 10RP more heavily pigmented and sclerotized than
remainder of 10R, and with a circular slot half-way along inner margin. Left
Figs. 1-5.—Oligembia hubbardi (Hagen), co. 1, Head, x 28; 2, Left forewing, x 13;
3, Terminalia from above, x 64; 4, Process of left hemitergite of tenth abdominal segment,
x 64; 5, Terminalia from below, x 64.
(9, ninth abdominal tergite; 10L, 10LP, left hemitergite of tenth abdominal segment
and its process; 10R, 10RP, right hemitergite and its process; LC,, LC,, first and second
segments of left cercus; RC,, RC,, segments of right cercus; LCB, left cercus-basipodite ;
H, ninth abdominal sternite (hypandrium).)
BY CONSETT DAVIS. 219
lobe (10L) (fig. 4) tapered backwards to a process (10LP), expanding terminally,
distal face concave. Right cercus of two subcylindrical segments (RC,, RC.), the
first somewhat thicker. Left cercus of two subequal segments (LC,, LC.), the first
slightly dilated distally on the inner side, but without nodules. Ninth sternite
(H) with a more membraneous concavity on the right side of the posterior margin,
and to the left of this a subquadrate lobe directed towards the base of the left
cercus. Left cercus-basipodite (LCB) tapered, directed backwards, bifid at apex,
basally apparently distinct from left cercus and not fused thereto as in other
species.
9 unknown.
Hagen’s type, from Enterprise, Florida (Museum of Comparative Zoology,
Harvard University) is in a very battered condition, as it was, indeed, when he
received and described it. The head is moderately well-preserved; the left fore-
wing is the only wing complete, the rest being much abraded. The abdomen,
broken off, was embedded in gum on a card, the terminalia almost entirely
destroyed. Preparation of the remains of the terminalia revealed the structure of
10RP, with its associated claw-like processes, and the tip of 10LP. These characters,
and the head and left forewing, were sufficient to identify the specimen with
certainty with another series in the Museum of Comparative Zoology, three males
(one much damaged) from Royal Palm Park, Florida (coll. Blatchley). One of
these was accordingly labelled plesiotype, and the figures (except fig. 2) and much
of the above description are from this specimen. In colour and dimensions this
series agrees with the type.
OLIGEMBIA ROSSI, Dn. Sp. Figs. 6-12.
6. Length 3 mm.; head, length 0-8 mm., breadth 0-6 mm.; forewing 3:1 mm. x
0-7 mm.; hindwing 2:3 mm. x 0-7 mm.
General colour pale ferruginous, head a little darker, eyes black. R,, R.,, and
stem of Cu pale brown; bands bordering veins or their traces very pale yellowish-
brown; thin lines bordering R, (Radiusnebenlinien or pseudo-radial lines) rose.
Head (fig. 6) relatively broader and more rounded than in O. hubbardi. Right
antenna with 14 segments, length 1:9 mm., probably complete; left broken.
Mandibles (fig. 7) slender, terminally incurved and acute, the tip of the left with
a weak longitudinal division; inner margin behind apex concave, with a tooth
half-way from apex. First segment of hind tarsi (fig. 8) without even the terminal
ventral bladder found in Oligotoma. Wings (fig. 9) much as in O. hubbardi, but
with a few weak cross-veins between costa and radius, and between radius and
sector. In the left hindwing the pigment-band representing R, is disconnected
basally from the stem R,,,. Terminalia (figs. 10-12) with tenth abdominal tergite
divided by an oblique suture, obsolete proximally. Right hemitergite (10R)
produced backwards to a tapered process (10RP) ending in two teeth (fig. 11), the
outer acute, the inner obtuse, shorter, and more dorsal. Base of 10RP with more
heavily-sclerotized areas in the form of two half-rings. Left hemitergite (10L)
produced backwards to a massive process (10LP; fig. 12), bifid, the inner or right
lobe slender, irregularly tapered, heavily sclerotized, the outer or left lobe obtuse,
membraneous, and placed somewhat dorsad. Right cercus of two subcylindrical
segments (RC,, RC.), the first somewhat thicker. Segments of left cercus
(LC,, LC.) similar to those of right, the first with the left cercus-basipodite (LCB)
fused to its base as a heavily-chitinized ring, produced inwards to a tapered horn
curving forwards. Hypandrium (H) tapered, truncate distally.
? unknown.
220 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. II,
Locality.—Barro Colorado Isd., Panama Canal Zone, coll. Dr. W. M. Wheeler;
in fungus.
This species is described from a single specimen in the British Museum of
Natural History, which I received mounted on two slides, one carrying the
terminalia, somewhat distorted, and one the other parts of the insect. The
exactitude of the locality and clarity of the taxonomic characters justify its
description, especially considering the morphological and geographic interest of
the record. The species is named after Mr. EH. S. Ross, of the University of
California.
Figs. 6-12.—Oligembia rossi, n. sp., &. 6, Head, x 60; 7, Mandibles from above, x 60;
8, Tarsus of right hind leg, viewed laterally, x 60; 9, Left fore- and hind-wing, x 20;
10, Terminalia from above, x 56; 11, Process of right hemitergite of tenth abdominal
segment, ~ 280; 12, Process of left hemitergite, x 280.
BY CONSETT DAVIS. 221
OLIGEMBIA BANKSI, n. sp. Figs. 13-20.
6. Length 4:8-6-2 mm.; head, length 0-8-1:1 mm., breadth 0-6-0:9 mm. Fore-
wing, length 3-8-4-6 mm., breadth 1:0-1:'2 mm.; hindwing, length 3-0-3-8 mm.,
breadth 1-0-1:2 mm.
General colour pale golden-brown, head darker, eyes black; wings very pale
brown with hyaline streaks. Head (fig. 13) relatively broader than in O. hubbardi,
the sides converging markedly behind the eyes. Greatest number of antennal
segments observed 15 (incomplete); greatest antennal length 2 mm. Mandibles
(fig. 14) similar to those of O. rossi, but with three terminal teeth on the left,
two on the right. Wings as in O. rossi, without anomalies. Hind tarsi (fig. 15)
similar to O. rossi. Terminalia (figs. 16-20) with longitudinal fission of tenth
abdominal tergite very incomplete; right lobe (10R) produced backwards and
inwards to a thin, flat tapered process (10RP), truncate distally, but apparently
smoothly tapered and acute from some aspects; inner margin of 10RP somewhat
Figs. 13-20.—Oligembia banksi, n. sp., ¢. 18, Head, x 20; 14, Mandibles from above,
x 40; 15, Hind tarsus, viewed laterally, x 60; 16, Terminalia from above, x 56; 17, Process
of right hemitergite from above, x 56; 18, Process of left hemitergite from above, x 56;
19, The same, from another specimen, viewed from a different angle, x 56; 20, Terminalia
from below, x 40. ,
Fig. 21.—Oligembia oligotomoides (Enderlein), ~ terminalia from above, x 13 (after
Enderlein, 1912).
corrugated, basally overlying an obtuse flap, similar to the structure present in
Oligotoma. Left lobe (10L) produced backwards to a bifid process (10LP), the
right lobe of which is flattened in a vertical plane, terminally subacute, but obtuse
from some aspects, curved to the left; left lobe of 10LP dorsiventral, spathulate.
Right cercus of two subcylindrical segments (RC,, RC.); first segment of left
cercus (LC,) clavate, inner margin lobed distally; basal part of inner margin
a little roughened by transverse furrows or creases, but without nodules. Second
segment (LC,) subcylindrical. Ninth sternite (H) produced backwards and to the
right in a blunt lobe, between which and the base of the left cereus are two
structures, one blunt, terminally outcurved, on the right, the other (LCB), probably
the true cercus-basipodite, on the left, i.e., at the base of the left cercus, and fused
222 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. II.
thereto; LCB curved upwards, ending in two small claws. Right cercus-basipodite
rudimentary.
? unknown.
Locality.—Villarica, Paraguay, coll. F. Schade. Holotype ¢ and series of
paratype gg, Museum of Comparative Zoology, Harvard University; paratype ¢
in the Macleay Museum, University of Sydney. Named after Mr. Nathan Banks,
Curator in Entomology, Museum of Comparative Zoology, Harvard.
OLIGEMBIA OLIGOTOMOIDES (Enderlein 1912).
Rhagadochir oligotomoides Enderlein, 1912, Embiidinen, in Coll. de Selys-
Longchamps, p. 61.
Enderlein described this species from two males, the locality being given as
South America. I have not seen the types (in the Berlin and Stettin Museums),
but there seems little doubt from Enderlein’s description and figures that the
species should be referred to Oligembia.
Enderlein’s description may be summarized as follows: g. Pale ferruginous-
yellow, head somewhat darker, eyes black, wings greyish-white. Length 41-4$ mm.,
forewing length 3:6 mm., hindwing 3:1 mm. Venation as in O. hubbardi and
O. rossi, but with R, apparently not confluent with R.,,; cross-veins apparently
stronger; R,,; simple in left forewing of the smaller example. Terminalia as in
figure 21 (after Enderlein) ; the projection from the base of the left cercus probably
represents the left cercus-basipodite fused to the cercus, as in O. rossi, O. bantsi
and the undescribed species mentioned below.
Discussion.
The possible affinities of Oligembia have been suggested in the generic
description. Other American genera which may have some obscure relationship
to Oligembia are Teratembia Krauss 1911, from the Argentine, and the genus to be
formed for Hmbia rujicollis de Saussure 1896, from Central America, which is refer-
able neither to Embia nor, as some authors have stated, to Oligotoma (cf., e.g.,
Friederichs, 1934). Both, however, are further removed structurally than is
Diradius, or even Oligotoma.
I have received details of two interesting species referable to Oligembia from
Mr. E. S. Ross. One is from Guatemala, the other from Tres Marias Isds., off the
west coast of Mexico; the latter is structurally similar to O. banksi. These species
will be described shortly by Mr. Ross, and the preparation of a key to the species
of the genus must await these descriptions.
It is probable that further collecting in the countries adjacent to Central
America will bring to light a number of further species of the genus Oligembia.
List of References.
ENDERLEIN, G., 1912.—Embiidinen, in Coll. de Selys-Longchamps, fasc. 3.
FRIEDERICHS, K., 1934.—Das Gemeinschaftsleben der Embiiden und Naheres zur Kenntnis
der Arten. Archiv fiir Naturgeschichte, Bd. 3, Hft. 3.
Hacen, H. A., 1885.—Monograph of the Embiidina. Canad. Entomologist, vol. 17, nos.
8-11 (London, Ontario).
Krauss, H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23 (Stuttgart).
pp Saussure, H., 1896.—Note sur la Tribu des Embiens. Mitt. Schweiz. entomol.
Gesellschaft, vol. 9.
223
A NEW SPECIES OF CHALCID (GENUS HURYTOMA) ASSOCIATED WITH
TEPPERELLA TRILINEATA CAM., A WASP CAUSING GALLING OF THE
FLOWER BUDS OF ACACIA DECURRENS.*
By N. S. Nose, D.Sc.Agr., M.Sc., D.I.C.,
Assistant Entomologist, Department of Agriculture, New South Wales.
(Twelve Text-figures. )
[Read 31st May, 1939.]
A detailed account of the life history of Tepperella trilineata, a wasp which
causes galling of the flower buds of Acacia decurrens var. pauciglandulosa in the
vicinity of Sydney, New South Wales, has already been published by the writer
(1938).
At that time it was pointed out that the species of Hurytoma under discussion,
hitherto undescribed, occurred so abundantly in these galls that it outnumbered
T. trilineata, the primary gall-former.
The unusual behaviour of the larva of a species of Hurytoma was commented
upon, and in the present paper the life history of this species is set out in detail.
The writer (1936) has already discussed the genus Hurytoma, and both
phytophagous and parasitic species in this genus are present in Australia. The
larva of H. gahani is first phytophagous, but later becomes a predator.
MoRrPHOLOGY.
Specimens of this species were submitted to Dr. A. B. Gahan, Senior
Entomologist of the United States Department of Agriculture, and in a letter dated
29th May, 1937, he informed the writer that it differed from any of the species
in the collections at the United States National Museum. He stated that it
ran close to Hurytoma mazzinii and also H. acaciae, two Australian species, but
was neither of these two. He concluded that the species was possibly new. The
writer has since compared specimens with all the available descriptions of
Australian species of this genus and has come to the conclusion that it is
undescribed, and a description of this species is included in the present paper.
EURYTOMA GAHANI, N. sp.
The Adult.
© (fig. 1): Length: Average, 2-6 mm.; maximum, 3:0 mm.; minimum, 2:3 mm.
Head black, evenly and coarsely reticulate and bearing short white setae.
Eyes red, this colour sometimes fading completely in mounted specimens. Mandible
(fig. 2C) brown. Antenna (fig. 2B) very dark brown, except the ring joint and
the base of the scape which is light brown. The scape extends a little beyond
the antennal groove, terminating level with the median ocellus.
* This contribution is one of ten papers on Australian Chalcidoidea submitted
to the University of Sydney in fulfilment of the requirements for the degree of
Doctor of Science in Agriculture.
224 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
Each segment of the funicle is very slightly wider than that preceding it.
The first segment of the funicle is a little longer than wide. The second segment
is a little shorter than the first and is exactly as wide as long. The third segment
of the funicle is slightly longer than the second and is very slightly longer than
it is wide. The fourth segment is approximately the same length as the third and
is very slightly wider than long. ‘The fifth segment is slightly shorter than the
fourth and is slightly wider than long. The club, which is approximately twice
as long as wide, is only very slightly wider than the last segment of the funicle.
Thorax black and, like the head, evenly and coarsely reticulate and bearing
short white setae. Wings hyaline; venation light brown, the postmarginal vein is
only slightly longer than the marginal vein, both being a little longer than the
stigmal vein (fig. 2D).
N.S.NOBLE
Fig. 1.—Hurytoma gahani, adult female (x 15).
Coxae and trochanters of all legs black. Coxae reticulate, more coarsely so
on the hind leg. Outer side of coxae of hind leg conspicuously grooved distally,
and in some mounted specimens the trochanter and base of the femur lie in this
groove. Femur of front and middle leg dark brown except distally, where it
fades to amber, tibia and tarsus amber. Femur of hind leg black except distally,
where it fades to amber, tibia and tarsus amber.
Abdomen black, rounded, not laterally compressed as is the case in many
species of Eurytoma reared from Australian plant galls. First five abdominal
segments smooth and shining, but at high magnifications fine reticulations can
be distinguished on these segments. Remainder of abdomen reticulate and dull,
and bearing a number of scattered white setae. No setae are present on the
first and second abdominal segments. A few short lateral setae borne in a median
position on the third segment. Setae on the fourth segment a little longer and in
a median single row laterally, but extending a little further up on to the dorsal
surface than in the third segment. Setae more numerous on the fifth segment,
being scattered irregularly over the distal half of the segment.
6: Length: Average, 25 mm.; maximum, 2°° mm.; minimum, 2:2 mm. In
general resembles the female, but is less robust. The abdomen is small and
globular, with a distinct petiole. The antenna of the male (fig. 2A) is con-
BY N. S. NOBLE. 225
spicuously larger than that of the female. The longest setae of the antenna are
approximately the length of the segments bearing them.
The type, allotype and numerous paratypes were bred by the writer from
galls caused by Vepperella trilineata on the flower buds of Acacia decurrens at
Lindfield, Sydney, New South Wales, in November, 1936.
The type, allotype and five paratypes of both sexes have been forwarded
to the British Museum of Natural History, South Kensington, London, and six
paratypes of both sexes have also been forwarded to the United States National
Museum, Washington, U.S.A.
Figs. 2, 3—EHurytoma gahani. 2: A, Antenna of male (x 36); B, Antenna of female
(x 36); C, Mandible of female (x 103); D, Stigmal knob of female (x 103). 3: A, B, C,
Ovarian eggs; D, E, Eggs after deposition (all x 103).
The Egg.
The ovarian egg (figs. 3, A-C) is just visible to the unaided eye. It is white
in colour and consists of an oval body bearing anteriorly a short pedicel with a
rounded end and posteriorly a very long slender pedicel which widens out distally.
The dimensions of the various parts of the egg are set out in Table 1. In general
features it bears a marked resemblance to the egg of Hurytoma fellis, a species
which has been studied by the writer (1936).
TABLE 1.—Dimensions of Egg of Eurytoma gahani (in millimetres).
{ )
|
Newly Deposited
Ovarian Egg. Egg.
Total
Length. Body of Egg. Anterior Pedicel. Posterior Pedicel. Body.
| Length. Width. | Length. Width. Length. Width. Length. Width.
Average 0:447 0-137 0-062 0-044 0-007 0-266 0-017 0-158 0-091
Maximum 0,492 0-142 0-066 0-050 0-007 0-310 0-020 0-172 0-096
Minimum 0-393 0:125 0:053 0-040 0-007 0-218 0-016 0-149 0-089
226 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
After deposition (figs. 3, D and E) both the long and the short pedicels may
become flaccid and twisted.
The Larva.
Based on mandible size and shape and the distribution of setae, five larval
stages are recognizable, there being one more stage than in Hurytoma fellis.
Stage I.—The first stage or primary larva (fig. 4) soon after hatching is
clear and translucent, but after feeding the region of the alimentary tract becomes
green. The smallest larva measured was 0:12 mm. in length and 0:06 mm. in
width, being almost invisible to the unaided eye. It consists of a rather prominent
head and thirteen clearly defined segments, the head being somewhat chitinized
and pale amber in colour. The larva is slightly dorso-ventrally flattened, and when
seen in side view is only very slightly arched. The head is slightly narrower than
the thoracic segments, the second segment being widest, the larva then tapering
gradually to the last segment.
Figs. 4-8.—Hurytoma gahani. 4, Ventral view of first-stage larva (x 180). 5, Ventral
view of second-stage larva (x 103). 6, Ventral view of third-stage larva (x 55). 7,
Lateral view of mature larva (x 20). 8, Front view of head of mature larva (x 635).
When viewed from beneath, the head is semi-circular in outline. The mouth
is ventral and is surrounded by a short rounded tubular structure formed from
the integument. In this respect it resembles closely the first stage larva of
Habrocytus cerealeliae which has been studied by the writer (1932) and, as in this
larva, this tubular outgrowth is most conspicuous when the larva elevates the
head when moving. The mandibles (fig. 9A) are triangular in outline, unidentate,
lightly chitinized and pale golden in colour, slightly curved and have the tips
overlapping, their average length being 0-007 mm.
Dorsally the head bears a pair of very minute truncate antennae, while
ventrally and a little to each side of the mouth one pair of minute setae are present.
There are no setae or papillae on any of the abdominal segments.
BY N. S. NOBLE. raya Th
Towards the close of the first larval stage the development of lateral tracheal
trunks, united anteriorly and disappearing posteriorly, gives the first indication
of the respiratory system.
Stage II—In general appearance the second-stage larva (fig. 5) resembles
the first stage fairly closely, being still more or less translucent with the
alimentary tract imparting a dark green colour to that region of the larva. It
consists of a head and thirteen segments, the head now being somewhat smaller
in proportion to the body segments, and being now no longer more heavily
chitinized than the latter. The smallest larva measured was 0:37 mm. in length
and 0:13 mm. in width.
The mandibles (fig. 9B), which are pale amber in colour, are unidentate,
very slightly curved and triangular in outline, their average length being 0-021
mm., the maximum being 0:023 mm., and the minimum 0-018 mm.
On the dorsal surface of the head there is a pair of truncate antennae, and
on the ventral surface there is a pair of large setae, there being a shorter pair
of setae on the front border of the head. Setae are present only on the three
thoracic segments. On the first segment there is a pair of very large ventral setae
and a smaller lateral pair, while on the second and third segments there is a pair
of smaller ventral setae and also a pair of lateral setae about the same length.
The respiratory system is now an open one. It consists of the two main
tracheal trunks, one extending along each side of the body, being united anteriorly
and posteriorly by transverse commissures. From the main trunks four pairs of
spiracular trunks pass out to open spiracles, one pair being situated on segments
two, four, five and six, the spiracles on segment two being much the largest.
A limited number of tracheae pass to the various organs.
Stage I1].—The third-stage larva (fig. 6) differs little in general appearance
from the second stage. It is now more white in colour and the contents of the
alimentary tract are dark green to almost black. The larva is very slightly dorso-
ventrally flattened and in side view is very slightly arched. The smallest larva
measured was 0:50 mm. in length and 0:19 mm. in width. The mandibles (fig. 9C)
are unidentate, triangular in outline, amber in colour, with the tips conspicuously
curved and overlapping. They average 0:035 mm. in length, the maximum being
0:040 mm. and the minimum 0-033 mm.
On the dorsal surface of the head is a fairly prominent pair of antennae, which
are more or less cylindrical with rounded ends, and pale amber in colour. Between
the antennae on the dorsal surface is a pair of fine setae, a second pair also being
dorsal and further back and more to the sides of the head. On the front margin
of the head and in front of and a little to the sides of the head, there is another
pair of setae, and ventrally just above the mandibles there is also a very short
pair of setae, while by far the largest on the head is a pair of ventral setae
situated below and to the sides of the mouth. There are thus five pairs of setae
of various sizes situated on the head.
Below the mandibles there is a large number of rounded sensory papillae
of various sizes, a more limited number being situated above the mandibles.
On the first three abdominal segments there are eight setae. One extremely
minute pair are dorsal and two large pairs are ventral and one pair are lateral.
From segment four to segment twelve, inclusive, there are two pairs of setae,
one minute pair being dorsal and a larger pair being lateral. On the thirteenth
segment the lateral setae are always wanting and only in some larvae examined
can the minute dorsal setae be distinguished.
bo
bo
6
NEW SPECIES OF CHALCID (GENUS EURYTOMA),
During the later period of the second stage, further spiracles develop, and in
the third stage there are nine pairs of open spiracles situated on segments two
to ten inclusive and there is now a very well developed respiratory system. The
first pair of spiracles are much larger than the succeeding ones.
Stage IV.—The fourth-stage larva is white in colour, cylindrical and arched,
and tapering gently towards both ends. The smallest larva measured was
0:96 mm. in length and 0:32 mm. in width.
The mandibles (fig. 9D) are triangular in outline, still only lightly chitinized
and amber in colour, slightly curved and average 0:064 mm. in length, the
maximum being 0:069 mm. and the minimum 0:059 mm. The antennae, apart
from size, are very similar to those of the third-stage larva, and the number and
distribution of the setae on the head is the same in the two stages. The
distribution and number of setae on the abdomen is, however, different. In the
fourth stage there are eight elongate amber setae on the ventral and lateral
surface of the first three segments, there being two small setae on each side of
the dorsal surface of these three segments.
On the remaining segments there are two pairs of large lateral setae and
one pair of minute dorsal setae on each segment. These setae become smaller
on each succeeding segment, those on the last segment being very minute. A well
developed open tracheal system, as in the third stage, is present.
Stage V—The fifth and last larval stage (fig. 7) is cylindrical and arched,
and tapers towards both ends, much more conspicuously than do any of the
preceding stages. The colour varies from white to light grey. The alimentary
tract is black, but this, being mainly masked by fat body, imparts a darker grey
appearance to this region of the larva.
It consists of a head and thirteen segments. The average length of the
mature larva is 3:32 mm., the maximum being 3-54 mm. and the minimum 2:97 mm.
The average width of the mature larva is 1:07 mm., the maximum being 1:15 mm.
and the minimum 0:94 mm.
The head (fig. 8) is of the typical generalized chalcidoid type, being more or
less hemispherical in outline. The mandibles (fig. 9E) are now much more heavily
chitinized, being brown in colour, somewhat triangular with a very broad base,
bidentate, with one very much longer curved and more heavily chitinized tooth.
The average length of the mandibles is 0-106 mm., the maximum being 0-116 mm.
and the minimum 0-092 mm. '
The head, as in preceding stages, bears a dorsal pair of cylindrical antennae
(fig. 9F) and five pairs of setae of various sizes, their distribution being as in
the third and fourth larval stages. Below the mandibles there are also four pairs
of minute sensory setae and four pairs of minute papillae, their distribution being
shown in figure 8. ‘
The number and distribution of the setae on the abdomen is the same as in
the fourth stage, i.e. there are ten large lateral and ventral setae (figs. 9, G, H,
and I) and two pairs of smaller dorsal setae on the first three segments, while
on the remaining segments there are two pairs of lateral and one pair of dorsal
and smaller setae. With the decrease in size of the posterior segments all these
setae are brought closer together and more or less form a median circlet.
A very profusely branching open tracheal system is present with nine pairs
of open spiracles, one pair on each of segments two to ten inclusive.
Intermediate measurements of the various larval stages of Eurytoma gahani
are given in Table 2.
BY N.
Ss.
NOBLE.
TABLE 2.—Dimensions (in millimetres) of the various Larval Stages of Eurytoma gahani.
Average Width
Stage of Larva. Length. Width. renal
Stage 1 .. .. Largest 0-30 0-11 0-063
Smallest 0-12 0-06
Stage 2 .. .. Largest 0-51 0-18 0:098
Smallest ()o8%7/ 0-13
Stage 3 .. .. Largest 1:04 0-32 0-180
Smallest 0-50 0-19
Stage 4... .. Largest 1:66 0-50 0-304
Smallest 0-96 0:32
Stage 5 .. .. Largest 3:54 ihorths) 0-443
Smallest 1:68 0-64
BIOLOGY.
Length of Life of Adults.
Newly-emerged adults of both sexes of H. gahani were placed in glass tubes
six inches in length and one inch in diameter.
One end of the tube was covered
with cheese cloth and the other was plugged with cotton wool which was kept
moistened with sugar and water solution.
These were held in the laboratory
until death; the length of life under these conditions is set out in Table 3.
TABLE 3.—Length of Life of Eurytoma gahani in the Laboratory.
Length of Life Number of Number of Length of Life Number of Number of
in Days. Males. Females. in Days. Males. Females.
1 4 3 15 2 2
2 21 4 16 1 3
3 19 26 17 = =
4 29 16 18 2 —_
5 21 18 19 2 —
6 31 10 20 — 1
a 27 25 21 1 1
8 38 24 22 1 il
9 18 44 23 — —_
10 12 20 24 — =
11 4 17 25 — 1
12 10 13 26 = 1
13 5 7 27 _ 2
14 2 1
Total 250 240
Average length of life of male wasps, 6:82 days; female wasps, 8:17 days.
Maximum
Minimum
”? ” ” ” ” ” 22
” ” ” ” ” ” 1 day >
”
93
”
”
27
”
1 day.
230 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
Under these conditions the average length of life was comparatively short,
but limited numbers of adults lived for more than two weeks, and a few females
lived for a period of three weeks or more, which is considerably longer than the
adults of the primary gall-former, Vepperella trilineata, lived under similar
eonditions.
Habits of Adults.
Adults are comparatively sluggish and do not fly readily, it being possible to
pick buds on which females are resting without disturbing them. However, they
can fiy quite well, and during November and December, 1936, on bright sunny
days, large numbers were to be seen flying around the galled tree, individuals
remaining on the wing for some minutes.
When confined in tubes in the laboratory, this species fed much more readily
on sugar solution than did the adults of Tepperella trilineata.
Percentage of Sexes.
Of a total of 1,605 adults which emerged from galls in 1936, 1,028 or 64-05
per cent. were females, and 577 or 35:95 per cent. were males. It will be seen that
females outnumbered males in a ratio of almost 2 to 1. It is worthy of note that
in Hurytoma fellis, the citrus gall wasp, studied by the writer (1936), of 4,889
adults, 3,122 or 63-86 per cent. were females, a percentage which is remarkably
close to that recorded for Hurytoma gahani.
Mating.
This species mated much more readily in the laboratory than did any of the
other species from the galls on Acacia decurrens. There is nothing unusual in
the procedure. The male spends a few moments on the dorsum of the female
vibrating the antennae in front of those of the latter, and fertilization follows, the
male invariably returning to the back of the female after coupling, but a second
contact was never observed. The time occupied ranged from 7 to 20 seconds,
the average being 11 seconds. Adults were frequently observed mating a few
minutes after emerging from the galls.
Oviposition.
Unlike Tepperella trilineata, the female of Hurytoma gahani at the time of
emergence from the galls has comparatively few eggs ready for deposition, and
even after being kept in tubes in the laboratory and fed for some days, the number
of well-developed eggs is still limited. Adults of Hurytoma gahani live longer
and are more vigorous than the adults of 7. trilineata, and it is probable that
Oviposition in the former species is a much more gradual process and extends over
a longer period. 1
At the time the first adults of Hurytoma gahani emerge all the flower buds
are very well developed, but it is several weeks before the tree blossoms, so that
these early emergents oviposit in advanced flower buds. During the greater part
of the emergence period of this species, however, the tree is in flower. It has
been pointed out that in globular flower-heads in which Tepperella trilineata has
Oviposited only the upper flowers open, and many females of Hurytoma gahani
oviposit in the fleshy green base of the unopened portion of the flower heads.
At the time the later adults of Hurytoma gahani emerge, viz. the last half
of December and early January, the tree has completed flowering, the normal
flowers have died and fallen, and the flower heads in which 7. trilineata has
BY N. S. NOBLE. 231
Oviposited are now present as very minute galls, and in these Hurytoma gahani
oviposits.
The tips of the antennae are held just above the surface of the plant tissues
to locate a suitable oviposition site. The abdomen is then brought down at right
angles to the normal position, the ovipositor is exposed and worked into the
gall until some stage of 7. trilineata is located, and then a single egg is deposited,
the process of oviposition being rather protracted. At the time the first adults of
Eurytoma gahani emerge, a limited number of eggs of Tepperella trilineata are
present in the buds, and the egg of EH. gahani in such instances is deposited
alongside the egg of 7. trilineata.
During the greater part of the emergence period of Hurytoma gahani,
T. trilineata is present in the first larval stage, and in large numbers of
dissections during December 1936, a single egg of Hurytoma gahani was found
adhering to the integument of a first-stage larva of T. trilineata, and in two
instances two eggs of H. gahani were found adhering to the integument of a
second-stage larva of 7. trilineata.
It is evident that the egg of H. gahani is always deposited alongside some
stage of T. trilineata, the exact stage of development of the latter species, at the
time of oviposition, apparently being of little significance.
Superparasitism.
In four instances it was evident that at least two eggs of Hurytoma gahani
had been laid in the cell occupied by Tepperella trilineata.
On 14th December, 1936, and again on 15th February, 1937, two eggs of
Eurytoma gahani were found adhering to the integument of a second-stage larva
of T. trilineata. In both cases the eggs were at distinctly different stages of
development.
On 17th July, 1936, two larvae of Hurytoma gahani, both in the fourth stage,
were found in a cell with a maturing larva of 7. trilineata. Both these larvae
were normal and active, but the larva of TZ. trilineata was very unhealthy in
appearance.
Again on ist September, 1936, two fifth-stage larvae of Hurytoma gahani were
found in the one cell accompanied by the dead remains of a fifth-stage larva of
T. trilineata.
Never more than one adult, however, was ever observed to emerge from a
single gall cell.
Larval Development.
The stages of Hurytoma gahani and Tepperella trilineata found in association
during a period of 16 months during 1936 and 1937 are set out in Table 4. It must
be remembered that as early as 16th May, 1936, gall cells were dissected in which
Eurytoma gahani had already devoured the larva of T. trilineata and was in the
last larval stage, and the number of such cells increased with each succeeding
dissection date. The figures indicated in Table 4 apply only to dissections in
which both species were still present in the cell, and this table does not give any
indication of the relative abundance of the two species.
Table 4 should be consulted in conjunction with Table 5, when considering
dissections during the second half of 1936, as the latter table indicates clearly
at the different dissection dates just what numbers of Jepperella trilineata still
remained in association with the larvae of Hurytoma gahani, the numbers of
ae, NEW SPECIES OF CHALCID (GENUS EURYTOMA),
mature larvae of the latter species present indicating the numbers of Tepperella
trilineata which had been devoured.
Though the eggs of the two species may be found in association, it was much
more usual to find the egg of Hurytoma gahani in the gall cell with the first-stage
larva of T. trilineata.
TABLE 4.—Stages of Tepperella trilineata and Eurytoma gahani found associated in Gall Cells on Acacia
decurrens during a period of Sixteen Months.
Stage of Larvae of Stage of Larvae of
Date of Number of Gall Tepperella trilineata Eurytoma gahani in
Dissection. Cells Examined. in Cell. the same Cell.
1935-36 Galls.
11/5/36 4 4 fourth. 1 second, 3 third.
1 1 fourth. 1 third.
16/5/36 3 3 fifth. 2 third, 1 fifth,
1 1 fourth. 1 third.
27/5/36 1 1 fifth. 1 third.
5/6/36 il 1 fifth. 1 third.
11/7/36 1 1 third. 1 second.
16/7/36 1 1 third. 1 second.
4 4 fifth. 3 fourth, 1 fifth.
9/8/36 9 9 fifth. 1 third, 8 fourth.
12/8/36 7 7 fifth. 7 fourth.
33 3 fourth 2 second, 1 third.
6/9/36 1 1 fourth. 1 third.
1936-37 Galls.
31/10/36 1 1 egg. 1 egg.
29/11/36 1 1 first. 1 egg.
13/12/36 1 1 first. 1 egg.
14/12/36 1 1 second. 2 eggs.
16/1/37 al 1 first. 1 first.
il 1 second. 1 first.
30/1/37 3 3 first. 3 first.
1/2/37 2 2 first. 2 first.
2 2 first. 2 eggs.
15/2/37 il 1 second. 1 first.
9/3/37 4 4 second. 4 first.
il 1 third. 1 third.
1 1 fifth. 1 fourth.
2/4/37 1 1 second. 1 first.
4 4 third. 2 first, 2 second.
20/4/37 9 9 third. 9 second. ,
7/5/37 1 1 second. 1 second.
8 8 third. 8 second.
7 7 fourth. 6 second, 1 third.
1/6/37 1 1 third. 1 second.
5 5 fourth. 5 third.
29/6/37 1 1 third. 1 second.
2 2 fourth. 2 third.
6 6 fifth. 5 third, 1 fourth.
15/7/37 13 13 fifth. 13 third.
6/8/37 14 14 fifth. 14 fourth.
13/8/37 18 18 fifth. 2 third, 16 fourth.
30/8/37 6 6 fifth, 6 fourth.
1 1 third. 1 second.
°
BY N. S. NOBLE. evo
In January and the beginning of February, 1937, the first-stage larvae of the
two species were sometimes found in association, but for the greater part of the
year the larvae of TJ. trilineata were one stage, and occasionally two stages,
ahead of the larvae of Hurytoma gahani with which they were associated, and the
size of the larvae of the former was always greatly in excess of the size of those
of the latter species.
k Ae)
en
ee
WA
Fig. 9—Eurytoma gahani: A, Mandible of first-stage larva; B, Mandible of second-
stage larva; C, Mandible of third-stage larva; D, Mandible of fourth-stage larva; H,
Mandible of fifth-stage larva; F, Antenna of fifth-stage larva. (x 180.) G, H, I, Setae
from first segment of mature larva (x 103).
Fig. 10.—Cross section of a fully-developed unilocular gall showing a maturing larva
of Tepperella trilineata in the cell together with a fourth-stage larva of Hurytoma gahani,
the latter larva being the smaller (x 7). Sectioned 14th August, 1936.
During the earlier part of the larval life the plant tissues fit closely up
against the integument of the larvae, and there is no room for movement. As the
two larvae feed upon the contents of the surrounding nutrient layer, their
alimentary tracts, which are blind sacs, become green in colour, and gradually
as the nutrient layer is devoured and the galls increase in size, the two larvae are
to be found in fairly large gall chambers in which there is room for movement,
and while it is more usual to find the small larva of E. gahani touching the larva
of 7. trilineata, the two larvae are sometimes found at opposite ends of the
chamber (fig. 10).
All stages of Hurytoma gahani, except the last larval stage, possess some
powers of locomotion, the second and third larval stages in, particular being able
to crawl along quite actively. With the increased space in the gall chambers
is correlated the further development of the respiratory systems in the two species
of larvae. This has been referred to when discussing the morphology of these
species.
The two species of larvae continue to develop normally together until the
late winter, when it is found that the majority of the larvae of T. trilineata have
reached the last larval stage. At this time the galls have also reached their full
size. However, larvae of T. trilineata, which are present in cells with the larvae
of #. gahani, are never able to pupate, and by the time the larvae of the latter
species reach the fifth or last larval stage, the larvae of TJ. trilineata have an
unhealthy appearance, and are sluggish and abnormal. Eventually the cells are
found to contain maturing larvae of Hurytoma gahani and the dead remains of
the larvae of TJ. trilineata, and finally all traces of the latter disappear, having
234 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
been devoured by the last-stage larvae of Hurytoma gahani, which reach maturity
and subsequently pupate in the cell formerly occupied by the two species. Factors
which bring about the destruction of the larvae of 7. trilineata are not clear.
It is possible that the exhaustion of the food supply may play an important
part, as examination of cells in which the larva of T. trilineata are dead shows
that the inner wall is hard and dry, the nutrient layer having completely dis-
appeared, this exhaustion of the food supply possibly being due to the extra
demands made upon it owing to the presence of two larvae. This exhaustion of
the food may cause the larva of 7. trilineata to become weak or even to die, and
hunger may be the factor which causes the larva of Hurytoma gahani to become
predaceous and devour the larva with which it formerly lived in harmony. On
the other hand, it is possible that the parasitic or predatory habit may develop
normally in the larva of Hurytoma gahani once it reaches the fifth stage, and it
may attack and destroy the larva of J. trilineata regardless of the state of the
food supply.
Many larvae of T. trilineata which had recently died, but in which the stomach
contents were still quite fluid, were mounted on slides and cover slips were super-
imposed and light pressure was applied. The integument became distended, but
there was no evidence of any break in the integument, which would be present
had the larva of Hurytoma gahani made a direct attack upon it. Continued
pressure of the cover glass usually forced the stomach contents out through the
anus. In more shrivelled specimens of dead larvae of 7. trilineata gaping ruptures
were present in the integument. These must have been made by the larva of
Hurytoma gahani, but it seems much more likely that these ruptures were made
after the death of 7. trilineata, as otherwise such ruptures should be present in all
the dead larvae.
In any case Hurytoma gahani behaves as a predator rather than a parasite,
and though many hundreds of cells were examined in 1936 in which both species
of larvae were present, it was only on very rare occasions that the larva of
Eurytoma gahani was actually observed feeding on the larva of T. trilineata.
Though the great majority of the larvae of 7. trilineata were devoured during
August, 1936, at each weekly examination of galls from May onwards occasional
maturing larvae of Hurytoma gahani were found in cells with dead T. trilineata
larvae of the last stage. Though at any particular period of the year the majority
of the larvae of Hurytoma gahani are at the same stage, a few cells may be found
in which the larvae of this species are more advanced.
In Table 5 are set out the results of a series of gall dissections during the
last six months of 1936 and also in August and September, 1937, and which
indicate the various stages of both Tepperella trilineata and Hurytoma gahani
present. Some maturing larvae of Eurytoma gahani were found as early as 16th
May, 1936, but it will be seen from Table 5 that in the dissections of galls on
3rd August and 9th August only six larvae of Hurytoma gahani were found alone,
while the larvae of the two species were still together in 90 cells.
On 22nd August, 1936, however, in 52 out of a total of 58 cells examined
it was found that the larvae of Hurytoma gahani had devoured those of
T. trilineata, and in 1936 and 1937 it was mainly during the last half of August
and the first half of September that the majority of the larvae of EH. gahani
devoured those of 7. trilineata and reached maturity. A remarkable increase in
the size of the larvae of Eurytoma gahani occurs during this time, larvae of this
species which have devoured the larvae of 7. trilineata increasing to twice the size
BY N. S. NOBLE.
235
TABLE 5.—Results of Dissection of Galls on Acacia decurrens showing Stages of Tepperella trilineata
and Eurytoma gahani present during the last half of 1936 and in the spring of 1937.
Cells
contain-
ing both Tepperella trilineata. Eurytoma gahani. Cells
No. of No. of T. tri- occupied
Date of Cells Emerg- | lineata by
dissection. |} Exam- | gence and Stage V other
ined. Holes. pe Larvae. | Pupae. | Adults. | Larvae. | Pupae. | Adults. | Species.
oma
gahani.
1936 Galls.
|
8-16/6/36 | 545 — 278 262 Sa Sy 5 — — —
26/7/36 | 36 — 20 15 — — 1 — — —
28/7/36 30 a 13 16 1 a — — — =
3/8/36 75 — 49 8 13 — 5 — — —
9/8/36 | 68 —_ 41 20 6 _ 1 — — —
18/8/36 82 —_ 26 — 21 — 35 —_ — —
22/8/36 85 — 6 8 19 = | > & — — —
30/8/36 | 136 oan 13 | 9 30. 1 | 83 — — —
6/9/36 MS | <= | 1a | 2 40 3 144 cs = 50
9/9/36 77 — 5 — 12 1 45 — — 14
13/9/36 98 1 Hl — 14 9 44 — —— 29
20/9/36 151 35 — — 2 10 69 — — 35
27/9/36 222 42 1 = 1 il | Tap = = 25
4/10/36 177 34 2 — 4 4 103 1 — 29
11/10/36 113 18 — ). GB 7 — 25
18/10/36 153 54 — 67 11 — 21
25/10/36 102 28 — — — —_— 39 31 —— 4
1/11/36 114 48 — 27 BY — 2
8/11/36 109 46 —= = — — 15 44 4 —
15/11/36 35 15 — — — — | 1 17 2 —
22/11/36 | 44 Ry MN ; oo 14 5 —
|
1937 Galls.
6/8/37 20 — 17 3 — —- — — — =
13/8/37 43 2s 23 10 4 = 4 = _ 2
30/8/37 57 — 23 5 15 — 6 ee == 8
13-16/9/37 516 — 11 _ 84 8 322 — — 91
First adult of Tepperella trilineata emerged on 7th September, 1936.
Masts yee 3s 3 5 bp », 12th October, 1936.
First ,, ,, Eurytoma gahani Fr ;, 30th October, 1936.
Tastes, es spss 5 ; 3 5 5th January, 1937.
The first adult of 7. trilineata of the following generation emerged on 19th September, 1937.
of larvae of the same stage which are still accompanied by the normal larvae of
T. trilineata. This great increase takes place in a very short space of time, and
it is evident that at this period the larva of T. trilineata provides an abundant
source of highly nutritious food.
All the available evidence points to the fact that after the larva of Hurytoma
gahani devours the larva of T. trilineata it partakes of no further food, but it is
evident that this species remains in the mature larval stage within the galls for
several months prior to pupation.
236 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
A number of larvae of Eurytoma gahani were taken from cells in August
after devouring the larvae of 7. trilineata and were measured, and they were just
as large as larvae of the same species removed from the galls several months
later. Moreover, it has already been pointed out that at the time the larva becomes
predaceous the inner wall of the gall cell or chamber is hard and dry.
Many larvae of Eurytoma gahani which were removed from galls on 2nd
August, 1936, and placed on cotton wool in petri dishes remained alive for periods
of two and three months and finally voided waste matter and pupated normally.
The smallest and the largest larvae of the various stages of Hurytoma gahani
measured are set out in Table 2. It will be seen that the growth in the various
stages is fairly regular, there being comparatively little overlapping in size in the
various stages, and that the larva almost doubles its size during the last larval
stage.
Dissection of the larvae of Tepperella trilineata which are in cells with
Eurytoma gahani shows that numbers of them contain also larvae of a parasite,
Megastigmus sp. As Hurytoma gahani devours the larvae of TJ. trilineata it
accidentally also becomes a predator of the larvae of Megastigmus sp. in those cells.
During 1936 and before any of the larvae of Tepperella trilineata had been
devoured, six twigs of galls were taken and every cell examined and the species
present recorded. Cells containing strange larvae were discarded, and the number
of cells in which T. trilineata occurred alone and with Hurytoma gahani were
recorded, and then all the larvae of TJ. trilineata were dissected in order to
determine whether Megastigmus sp. was present. The results of these dissections
are set out in Table 6.
TABLE 6.—Numbers of Larvae of Tepperella trilineata, Megastigmus sp. and Eurytoma gahani present in Galls
on Acacia decurrens at Lindfield, Sydney, in 1936.
| | |
| Cells
| | containing
| | | Total Cells Cells Cells Larvae of
| | Total Cells containing containing | containing Megastigmus
Twig Total Gall | containing | Larvae of Larvae of only Larvae | sp. within
No. | Cells. Larvae of Megastigmus Eurytoma Ofer | Larvae of
T. trilineata. sp. gahani. trilineata. | QT. trilineata.
Larvae of EB.
| gahani absent.
|
1 54 | 54 15 25 21 8
2 63 63 27 29 19 | 15
3 54 54 Qi. 26 15 | 13
4 136 136 50 78 36 sh mee
5 116 | 116 40 68 35 | 13
6 122 122 52 67 29 26
—_—-—— . —___—. | | | —
| |
Total 545 | 545 | 211 293 155 97
Knowing the habits of these three species, it is evident that though there were
originally 545 cells containing larvae of 7. trilineata, only 155 or 28:44 per cent. of
this species could have emerged as adults, while from the same galls, though 211
larvae of Megastigmus sp. were present, only 97 or 17:80 per cent. could have
BY N. S. NOBLE. Zor
emerged as adults, while of the 293 larvae of Hurytoma gahani present and which
occupied 53-76 per cent. of the cells, all would have emerged as adults, no larvae of
this species ever having been found parasitized, though many hundreds have been
examined. In the spring of 1937 examination of a further series of 545 gall cells
from the same tree showed that 362 or 66-42 per cent. would have yielded adults
of Hurytoma gahani, this remarkably successful species having increased in
numbers at the expense of Tepperella trilineata and Megastigmus sp. as compared
with 1936.
The preceding figures give an excellent idea of the relative abundance of the
three species of Chalcids in the galls. It is of interest to note that until the
larvae of 7. trilineata and Eurytoma gahani reach the last stage, the development
of 7. trilineata when associated with H. gahani was just as rapid as that of larvae
which were in cells alone, indicating that during this period the presence of the
larva of Hurytoma gahani has no visible adverse effect upon the larva of
T. trilineata. This is further borne out by the fact that development of galls in
which the two larvae are associated in the cells is just as rapid and normal as in
galls in which the cells were occupied by the larvae of 7. trilineata alone.
The association of these two species of larvae in the one gall chamber is a
remarkable and unusual one.
Kinsey (1920), who has made an exhaustive study of cynipid wasps, which
are the main gall-formers of the United States, in discussing inquilines in the
galls, pointed out that no struggle existed between these and the primary gall-
formers, that the larvae of the two species lived in closely identical environments,
but that they did not come in contact with one another or interfere with one
another in any way. Judged on this basis, Hurytoma gahani could not at any
stage be classed as an inquiline. In some respects during its early larval stages
its behaviour resembles that of an inquiline, but it is always a competitor and
becomes a predator in its last larval stage.
Triggerson (1914) recorded an unusual phenomenon in the case of a Cynipid
gall wasp, Dryophanta erinacei, in America. A second species of Cynipid, Synergus
erinacei, destroyed the larva of D. erinacei, and then tunnelled through the galls
to the various cavities and fed upon the occupants.
The occurrence of the parasitic and phytophagous habit in a single chalcid
species has been observed by a number of workers, but the behaviour of Hurytoma
gahani, in a number of respects, is unusual. It is the intention of the writer to
discuss phytophagy and parasitism in the Chalcidoidea in a later paper.
Pupation and the Pupal Period.
As with the other species studied in this gall complex, no waste matter is
voided during larval life, but some days prior to pupation the larva voids from
the anus a quantity of black and fairly solid waste matter. In the gall cells this
waste matter usually becomes broken to fine black particles which adhere to the
larva and later the pupa, but sometimes it remains as one long twisted black
strand adhering to the tip of the pupa. The quantity of waste matter voided
by the mature larva is considerable and much more than in any chalcid larvae
previously studied by the writer.
On first passing to the pupal stage, the pupa is a uniform white in colour,
but within twenty-four hours the head, thorax and wing buds become amber and
the pupae remain thus for approximately two weeks, when they gradually
commence to turn black, and some days before emergence the pupae are a
238 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
uniform black. The average length of the pupa of Hurytoma gahani is 2:46 mm.,
the maximum being 2-66 mm., and the minimum 2:19 mm.
From August until November, 1936, large numbers of mature larvae were
dissected from galls and placed on either blotting paper or cotton wool in petri
dishes, and fifty-eight of these pupated in a normal manner and eventually emerged
as adults. The pupal period under these conditions is set out in Table 7. It will
be seen that the pupal period ranged from 25 to 36 days, the average for male
wasps being 32-84 days and for female wasps 33:13 days. The first pupa was
found in a gall on 4th October, 1936, and the first adult of Hurytoma gahani
emerged on 30th October, 1936.
TABLE 7.—Pupal period of Eurytoma gahani in the Laboratory, 1936.
Pupal Period Number of | Number of
in Days. Males. Females.
25 | — 1
26 1 —
27 —_— —_
28 1 1
29 1 2
30 1 1
31 1 1
32 4 1
33 7 6
34 ba’ 8
35 3 7
36 3 3
Total ie A 31
|
Average pupal period of male wasps, 32-84 days ; female wasps, 33-13 days.
Maximum 29 ” ” ” ” 36 ” 39 be) 36 ”
Minimum ” ” ” ” ” 26 ” be) be) 25 3”
Emergence of Adults.
Adult wasps emerge by eating a cylindrical channel out to the exterior of
the gall. In figure 11 is shown graphically the daily emergence of 2,779 adults
of Eurytoma gahani from galls on Acacia decurrens in 1936.
It will be seen that emergence commenced on 30th October, 1936, and continued
until 5th January, 1937. Though the emergence period extended over ‘68 days,
it will be seen that by far the greatest numbers emerged during the second half
of November and the first half of December. This emergence period was
approximately twice as long as that of JT. trilineata from the same tree.
In figure 11 is also shown graphically the emergence of 1,058 adults of
T. trilineata and 1,559 adults of Megastigmus sp., an internal larval parasite of
Tepperella trilineata. While figure 11 indicates the emergence periods of the three
species, it does not represent their relative abundance, as it was not always
possible to obtain emergence records of the three species from the same galls, the
total period being so extensive that galls used in the early part of the emergence
period became so hard and dry that they were unsuitable for later emergence
BY N. S. NOBLE. 239
| eGo al a St ee ae
al oa a oN IB Ss a
14,0
ae HA a
SERIE Eee Eee
suena UeaRELMRMMIEEG ce
=| OATES 1 19 ESS
ALL CCS@ CC ee PEEP EEE PRES
7 u 1S 19 a 27
PTEMBER Gaze a an M a
SEPTEMBE 5 EMERGENCE DATES Dee Be
Fig. 11.—Graph showing daily emergence of Tepperella trilineata, Megastigmus sp.
and Hurytoma gahani in 1936-37, from galls on Acacia decurrens.
(1058) ZT. trilineata
(1559) Megastigmus sp. ------------
(2779) H. gahani —--—--—:: =
records. It will be seen that the first adult of Hurytoma gahani did not emerge
until eighteen days after the last adult of TJ. trilineata emerged and only six
days before the last adult of Megastigmus sp. emerged.
In figure 12 is shown graphically the emergence of 1,605 adults of Hurytoma
gahani, representing the total emergence of this species from one batch of galls
: ug
perience tt
sta ui ut pf
Oct. Neveenes vigiaitaec ae EC
EMERGENCE Dates
Fig. 12.—Graph showing daily emergence of 1028 females and 577 males of Hurytoma
gahani from galls on Acacia decurrens in 1936-37.
(1028) females
(577) males ------------
240 NEW SPECIES OF CHALCID (GENUS EURYTOMA),
in 1936, the emergence of the two sexes being shown separately. It will be seen
that while the two sexes emerged over approximately the same period, in the
early part of the emergence period males predominated, while later the females
were greatly in excess of the males.
During the later part of the emergence period, the galls shrivel, become black
and extremely hard, and fall from the tree, but it was found that adults of
Eurytoma gahani emerged from these fallen woody galls in a normal manner.
SUMMARY.
The morphology and biology of Hurytoma gahani, a new species, which occurs
in the galls on the flower buds of Acacia decurrens caused by Tepperella trilineata,
is described.
Like that of the primary gall-former, 7. trilineata, the life cycle of Hurytoma
gahani is annual.
The adults of Z. gahani emerge from the galls mainly during November and
December, some time after all the adults of 7. trilineata have emerged.
Of 1,605 adults of Hurytoma gahani which emerged in 1936, 1,028 or 64:05 per
cent. were females and 577 or 35:95 per cent. were males. The average length of
life of male wasps was 6:82 days, and of female wasps 8:17 days, but the maximum
length of life of male wasps was 22 days and of female wasps 27 days.
The egg of Hurytoma gahani is deposited alongside the egg, or more commonly
the first-stage larva, of T. trilineata within the minute acacia flower-buds or aborted
flower-heads.
The larva of H#. gahani, on hatching, lives with the larva of Tepperella
trilineata in the one cell, the development of the latter usually being at least one
stage more advanced than the larva of Hurytoma gahani.
Five larval stages occur, and these are described in detail.
The two species of larvae live phytophagously on the plant tissues, and the
larva of 7. trilineata reaches the fifth or last larval stage, but when the larva of
Eurytoma gahani is also present, the larva of 7. trilineata never pupates.
By the time the larva of H. gahani reaches the fifth stage, the larva of
T. trilineata is unhealthy in appearance and is eventually devoured by the larva
of #. gahani.
Possible factors concerned in the change from a phytophagous to a predatory
habit in the fifth larval stage of H. gahani are discussed.
Having devoured the larva of 7. trilineata, the larva of Hurytoma gahani is
fully-fed and may remain in the gall cells for several months before pupating. The
pupal period is approximately four weeks.
Of 545 gall cells examined in 1936, 293 or 53:76 per cent. were occupied by
the larvae of Eurytoma gahani and T. trilineata together, and within 114 of the
larvae of the latter species there were also larvae of Megastigmus sp., an internal
parasite, and all of these latter larvae would have been devoured when the larvae
of T. trilineata were eaten by those of EHurytoma@ gahani.
In the spring of 1937, examination of a further 545 gall cells from the same
tree showed that 362 or 66-42 per cent. were occupied by Hurytoma gahani.
Though several thousand cells were examined, no larvae of H. gahani were
ever found to be parasitized.
The presence of the larva of EZ. gahani does not affect the development of the
galls.
BY N. S. NOBLE. 241
Acknowledgement.
The writer wishes to acknowledge his indebtedness to Dr. A. B. Gahan, Senior
Entomologist of the United States Department of Agriculture, for his critical
opinion on the species under discussion.
Literature Cited.
KINsBy, A. C., 1920.—New species and synonymy of American Cynipidae. Bull. Am. Mus.
Nat. Hist., xlii, 293-317.
NoBuE, N. S., 1932.—Studies of Habrocytus cerealellae (Ashmead), a Pteromalid parasite
of the angoumois grain moth, Sitotroga cerealelia (Olivier). Univ. Calif. Publ.
Entom., v, 311-354.
, 1936.—The citrus gall wasp, Hurytoma fellis Gir. Sci. Bull. Dept. Agr. N.S.W.,
No. 53, 41 pp.
, 1938.—Tepperella trilineata Cam., a wasp causing galling of the flower buds of
Acacia decurrens var. pauciglandulosa. Proc. LINN. Soc. N.S.W., Ixiii, 389-411.
TRIGGBRSON, C. J., 1914.—A study of Dryophanta erinacei (Mayr.) and its gall. Ann. Ent.
Soc. Amer., vii, 1-34.
242
THE UPPER PALAEOZOIC ROCKS BETWEEN MOUNT GEORGE AND
WINGHAM, N. 8S. WALES.
By A. H. Votsry,* M.Sc., Lecturer in Geology and Geography,
New England University College.
(One Map; three Text-figures. )
[Read 31st May, 1939.]
The area examined lies on both sides of the Manning River between Mount
George and Wingham and adjoins the Taree District which was described in a
previous paper (Voisey, 1938).
Geological field-work was commenced in May 1937, following the receipt at
the University of Sydney of some excellent specimens of Linoproductus spring-
surensis forwarded by Mr. R. T. Cox of “Colraine’, Kimbriki. The occurrence of
fossils at Kimbriki has not been recorded previously, although their presence
has been known to local residents for many years.
The only references which have been found relating to the geology of this
locality are those by Benson (1916) and Woolnough (1911). The former recorded
Devonian rocks, serpentine and Permo-Carboniferous fossils from the vicinity of
Mount George, and the latter noted the presence of fossils in a railway cutting
at Killawarra. On Professor Sir T. W. HE. David’s map of the Commonwealth of
Australia (1932) the area covered by the accompanying map was marked as
Lower Carboniferous, with the exception of the north-western corner, which was
shown as Devonian.
Except where noted otherwise, the fossils mentioned in this paper have been
identified by Mr. H. O. Fletcher, Palaeontologist at the Australian Museum,
Sydney. They have been included in the Museum’s palaeontological collection. No
microscopical examinations of the rocks have been made so far, but it is hoped that
this work will be carried out in the near future.
Map 1 indicates the distribution of the principal rock types and thé positions
of the major faults. Parish maps were used in connection with geological mapping,
and the place names have been taken from these maps. Certain differences in
spelling are worthy of comment. Burrell Creek Post Office is situated near Burrill
Creek and the school near Bow Bow Creek is called “Bo Bo School’.
STRATIGRAPHY.
DEVONIAN.
Three areas of Devonian rocks are shown on the map and each of these consists
of a different association of rock-types.
* This paper was completed while the author was Linnean Macleay Fellow of the
Society in Geology.
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244 UPPER PALAEOZOIC ROCKS BETWEEN MT. GEORGE AND WINGHAM,
1. Jaspers and Quartzites.
Jaspers and quartzites outcrop around the head-waters of Woolshed Creek
and continue to the north and north-east beyond the limits of the map to Wherrol
Flat, where they are cut off by a belt of serpentine presumably injected along a
major fault-plane. They give rise to very rugged topography, the Riek land
culminating in Johnston’s Peak near Wherrol Flat.
The siliceous rocks range in colour from the reds and reddish-browns of the
jaspers to the pale greens and yellows of the quartzites. The last-named, however,
are more often white and translucent. The beds are riddled with quartz veins
and are very hard. They are extensively jointed and cracked.
Stratification is indicated by colour differences and slight variations in the
physical characteristics of the units. Most traces of original sedimentary charac-
teristics have been obscured by the silicification.
It is proposed tentatively to correlate the jaspers and quartzites with the
Woolomin Series of Benson (1913) on account of their similarity to some of the
beds of that series in the Tamworth District. The micaceous phyllites, purple
schistose tuffs, and altered spilites which are associated with the siliceous rocks
in that region, however, have not been found so far in the area now being
described.
The correlation suggested is open to question and the writer has recently
assigned similar beds in the Armidale District to the Carboniferous system, but
here again no definite evidence was available (Voisey, 1938bD).
2. Banded Claystones, Cherts and Tuffs.
Portion of a large block of Devonian rocks is shown to the east of Bow Bow
Creek and Killawarra. This block is bounded by heavy faults on its northern,
southern and western sides, so that the beds are brought into contact with those
of the Carboniferous and Kamilaroi Systems.
Outcrops are poor as the rocks have been reduced by erosion to comparatively
low hills covered by a fair soil. Much of the country has been cleared and is
now well grassed.
The beds are exposed by cuttings along the main Gloucester—Taree road
between Bow Bow Creek and Tinonee and also along the roads from Killawarra
Bridge to Bootoowaa, and from Wingham to Tinonee. Isolated outcrops are seen
in gullies and quarries. There are insufficient data to permit the elucidation of the
structures in detail, since the variations in the direction of strike, together with
the complicated faulting and folding observed in the limited exposures, point to
the presence of numerous fractured folds of small amplitude and on different axes.
The rock types are similar to those described by Benson (1913a) from the
Tamworth Series. Banded claystones and cherts comprise most of the sequence.
The bands vary from a fraction of an inch to several inches in width. In the fresh
rock they are alternately light bluish-grey and dark bluish-grey, but, on weathering,
they become white, yellow or light grey. The dark grey bands are usually the
wider ones. The rock is quite hard and splintery. It exhibits a conchoidal
fracture in places. Excessive jointing has broken the beds into small blocks, and
it is difficult to obtain unweathered material. Radiolaria have been recorded
from these rocks immediately to the south (Benson, 1916; Sussmilch, 1921, p. 239).
A characteristic variant of the claystone described above weathers to a dark
or light green colour and is useful in the identification of the series.
Interbedded with the claystones and cherts are thick beds of tuff which appear
in places to be intrusive into them. The tuffs are generally dark grey or dark
BY A. H. VOISEY. 245
green in colour. They vary in texture, composition and appearance, but are
generally hard, massive, and weather to a brown colour. Some of them could be
confused with the Carboniferous tuffs, but their association with banded claystones
and cherts is sufficient to distinguish them.
HILLVIEW
FAUT
Ly Rm b
& KULLATINE
B SERIES yay
a
a 6 4
a
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See Cs ES SSS
KANGHAT
FAULT
MANGHAT FAULT
H DINGO CREEK
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FAULT
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a AULLATINE SERIES
yay a a a
DEVONIAN. Aa
Spili
Sea Are AU Oe AAT a
Clay st
anaes Ld A
QO MILES >
Fig. 1.—Section along line A-B (Map 1). V/H = 1/1.
Fig. 2.—Section along line C-D (Map 1). V/H = 1/1.
Fig. 3.—Section along line H-F (Map 1). V/H = 1/1.
3. Spilites, Tuffs and Cherts.
A thick series of tuffs, cherts and spilites forms the Kanghat Range and its
foothills. These beds are bounded on the north by the Kanghat Fault which runs
from the west of Mount George to Hillview and beyond. Southward the series
has not been thoroughly investigated, but its continuity is interrupted by faults
before Kramback is reached.
In marked contrast with the claystones and tuffs described above, these beds
give rise to rugged topography as evidenced by Mount Kiwarriec and the Kanghat
Range, which attain heights of 2,000 feet. Steep slopes covered with talus and
dense vegetation seriously interfered with geological work in this area. Moreover,
elucidation of the sequence was rendered impracticable by the presence of strong
faults. Spilites, so wonderfully developed at the western end of Kanghat Range,
do not appear to intersect Burrill Creek which separates the Kanghat Range from
Mount Kiwarriec. Strikes are extraordinarily variable.
Pillow lavas were described from between Gloucester and Mount George by
Benson (1916). He stated that very dense, hard, fresh-looking subvariolitic spilites
with well-preserved pyroxenes but albitic felspars were exposed in railway cuttings
east of Bundook. These greenish rocks contain quartz and epidote which fill
numerous cracks and vesicles. q
The north-western extremity of Kanghat Range is an impressive feature
composed largely of spilites.
The northern slope of Bucklebore Mountain, which is a smaller range
branching east from the northern front of Kanghat, is a fault scarp which is
strewn with talus consisting of a great variety of tuffs. The most spectacular of
these is a green volcanic agglomerate containing irregular fragments up to several
inches across. This rock is associated with breccias and finer grained tuffs, some
246 UPPER PALAEOZOIC ROCKS BETWEEN MT. GEORGE AND WINGHAM,
grey and others green and blue in colour. These outcrop in the bed of Stony
Creek near Bucklebore Mountain and also on the adjacent slopes. The brecciated
character of some of the varieties is seen best on the weathered surfaces, the rock
becoming brown and greenish-brown on decomposition.
In the foothills of Mount Kiwarric in the south-east corner of the area fine-
grained dark blue cherts are interbedded with tuffs, breccias and spilites.
CARBONIFEROUS.
With the exception of the Upper Burindi Series, which has not been identified,
the same series are developed in this area as in the adjacent Taree District
(Voisey, 1938a). The Lower Burindi Series consists essentially of olive-green
mudstones and tuffs and the Kullatine Series principally of tillite and tuff. These
two series bear faulted relationships to one another and to the Devonian beds.
1. Lower Burindi Series.
The Lower Burindi beds outcrop between Charity Creek and Dingo Creek and
are excellently exposed by road cuttings between Mount George and Killawarra.
Rocky Falls Creek has revealed a thickness of more than 1,000 feet of sediment.
The northerly dip changes from 60 degrees to 10 degrees going up the creek, and
in places the strata are practically horizontal. Variable strikes along the course
of Charity Creek and its tributaries indicate faulting and perhaps folding in that
locality. Owing to scanty outcrops away from the creeks and the absence of any
marker beds, details of the structures could not be obtained.
Tuffs and tuffaceous sandstones interbedded with mudstones make up the
sequence. The tuffs range from dark grey to light bluish-grey in colour and vary
considerably in texture. Fine-grained conglomerate bands containing pebbles up
to the size of a pea occur in places, but the most common rock is a gritty water-
sorted tuff containing fragments of felspar reaching a millimetre or more in
diameter. Fine-grained tuffs, dark bluish-grey but weathering to brown, occur,
generally in bands a few feet in thickness separated by thin beds of mudstone.
The mudstones range in thickness from a few inches to ten feet. They are
olive-green or black in colour and are rarely laminated. They contain numerous
unidentifiable plant remains. These do not necessarily indicate a fresh-water
origin since they are associated with marine fossil beds elsewhere in the Manning
District, They have been recorded from the Burindi Series in the Hunter Valley
(Osborne, 1922, p. 164).
The mudstones decompose readily on exposure to weathering agencies and
are generally found as buff or light brown crumbling material from which fresh
specimens are difficult to obtain.
Dr. Woolnough (1911) recorded tuffs containing a lamellibranch , identified
tentatively by W. S. Dun as a Pachydomus of Permo-Carboniferous age from a
railway cutting west of Killawarra Station. There is little doubt, however, that
the beds belong to the Lower Burindi suite. Of the 200 feet of mudstones and
tuffs exposed by the cutting the most important unit is a greenish-grey tuff fifty
feet in thickness. An attribute peculiar to this rock and perhaps to several other
massive tuffs in the sequence is the weathering out of spheres of the rock a little
smaller than cricket balls. These cannot be satisfactorily explained in a similar
manner to ordinary spheroidal weathering since the spheres are surrounded by the
unfractured rock separated only by a small thickness of brown decomposed
material. No suitable explanation of the phenomenon can be offered. Woolnough
regarded the bed as the equivalent of his ‘“Pachydomus” horizon, but no fossils
were found during the recent survey.
BY A. H. VOISEY. 247
As the continuity of the sequence both upward and downward has been inter-
rupted by faulting, it is not possible to estimate the maximum thickness of the
series. There is evidence, however, of at least 2,000 feet.
2. Kullatine Series.
The Kullatine beds consist almost entirely of tillite. Tuff and mudstone bands
probably make up less than a quarter of the whole thickness of several thousand
feet.
The tillite is a massive hard bluish-grey mudstone containing scattered frag-
ments of a variety of rock types including granites, porphyries, felsites, andesites,
tuffs, sandstones, cherts and quartzites. The included pebbles up to half an inch
in diameter are nearly all angular, but those above that size are more or less
rounded. While most of the rock fragments are less than two inches in diameter,
occasional larger ones reaching a foot across have been found. A most abundant
and ubiquitous pebble is a purple andesitic rock which is similar in appearance
to types found in the tillites and fluvio-glacial conglomerates in the Upper beds
of the Kullatine Series of the Macleay District.
The tillite outcrops as hard rounded boulders on the hillsides or, when more
extensively weathered, in cuttings when it has changed to a buff or yellow colour
and resembles a decomposed mudstone. The weathered rock is easily recognized,
however, by virtue of the small fragments of felspar and other minerals and rocks
which give it a speckled appearance. It is rarely that the tillite is free from the
smaller angular pebbles. The larger ones are more sporadic in their distribution,
but when present they constitute a more conclusive test.
Occasional bands of dark grey tuff of slightly variable texture break the
continuity of the tillite in places, as on F. Richardson’s property about half a
mile south-east of Charity Creek Railway Station. Two hundred feet of them
are developed at the top of the sequence below the Kamilaroi strata.
Fine-grained rocks resembling mudstones may be variants, but no definite
banding was observed.
The tillite and its associates occupy a large proportion of the area mapped.
Excellent exposures are found in the railway cuttings between Mount George and
Karaak Flat. Since the beds are dipping at a fairly high angle in most places
where measurement is possible, the immense development of tillite is apparent.
An interesting occurrence is that on the first hill on the Mount George road
past its junction with the Wingham-Gloucester road at Killawarra. A band of
sediment 3 inches to 6 inches thick embedded in tillite was found to contain
crinoid stems. This band is exposed in a gutter on the south side of the road
about half-way up the hill. Exposures being continuous for some distance, there
does not appear to be any escape from the conclusion that the tillites here, at any
rate, were laid down under marine conditions. No other fossils were found in the
series.
The tillite is indistinguishable lithologically from that occurring at the top
of the Kullatine Series in the Macleay District (Voisey, 1934). It also resembles
closely the tillites of Currabubula and Limeburner’s Creek. It is probable, there-
fore, that the glacial beds were contemporaneous with part of the glacial stage of
the Kuttung Series.
KAMILAROI*: MACLEAY SERIES.
The Kamilaroi sediments overlie the Kullatine Series without any apparent
unconformity. Indeed, there appears to be a transition from the tuffs overlying
RST HNOASIE PSs hoon (BERNA SSS RINE REE SOLE ET ONE CR Ea vt a ee
* See David, 1932.—Terminology used here in order to avoid confusion, but regarded
by the writer as synonymous with “Permian”.
248 UPPER PALAEOZOIC ROCKS BETWEEN MT. GEORGE AND WINGHAM,
the tillite into banded mudstones which have been taken as the basal unit of the
younger series. Since the tuffs bear a marked resemblance to those lower in the
Carboniferous sequence they must be retained in it.
Continuous exposures of the junction between the Carboniferous and Kamilaroi
strata are found in the following places: (1), a creek just behind Kimbriki Public
School; (2), along the south bank of the Manning River immediately west of
“Colraine”’; (8), along the south bank of the Manning River south of Charity
Creek Railway Station.
In each of the above localities a good section of the sequence of the Macleay
Series was obtained. The variations in the thickness and nature of the sediments
are expressed by these sections, which are representative of the series in the
district.
1. Creek behind Kimbriki School.
Thickness in feet.
D. Mudstones EN er Ne eC ee Aim Mette conde Tei 100
Cc. Limestones, banded mudstones and tuffs .. .. 60
B. Tuff containing sponge spicules SEPE SAEED gest 110
A. Banded mudstones A in Ns cee rey =, ACCS MiP ee eric 220
MMOH WOW OKESE. ao /igia Y Glos soo) of. one 490
Beneath the Kamilaroi beds 200 feet of tuff were measured and then an
indeterminate thickness of tillite was found.
2. Along the Manning River in the neighbourhood of ‘“Colraine’’.
Thickness in feet.
eM CA CEOS! WHIUASEONE hea. Me ers), Ska rele ess 200
E. Linoproductus horizon RAL eee te CBMs Gel nee 8
D. Mudstones, sandstones and tuffs .. .. .. .. 200
C. Limestone with marine fossils l 120
B. Tuff containing sponge spicules {j eee Te
A. Banded mudstones LOPS TMP ES SOD SA. yank UGA LE MIDS WS 500
Tt AU AtHICKNESS| gaccmele icc ck chien CE, Vie 1,028
3. Along the south bank of the Manning River south of Charity Creek Railway
Station.
Thickness in feet.
10%, WUD KEEONEIS soehDKoKioRevess! 55° 65° 66 mo an 06 | oo 720
D and E. Tuffs and sandy mudstones with marine
fossils Seer ate 900
C and B. Marine fossiliferous limestones, argillaceous
in part interbedded with banded mudstones and
sandstones ER COROT RTO chen WroFo DP a ray eel Swe rete e Bit 560
AS Dark=erey; "MUdStOnes: 7. . sug cso). eo est sis ale 240 .
TOtalethickness® Wit eyts) wees meer 2,420
The various units grade into one another as, for example, in the last-mentioned
section, where the banded mudstones, tuffs with sponge spicules, and limestones
are interbedded. It is convenient to discuss the beds in the order in which they
occur near “Colraine”’. This may be regarded as the type-section.
A. The Banded Mudstones.
These are banded, dark and light-grey rocks weathering to grey, brownish-
grey, light brown and white. They possess a well-marked rhythm throughout and
lamination is particularly noticeable. A major rhythm of from two to six inches
BY A. H. VOISEY. 249
occurs. Some of the bands are crumbly, dark grey mudstones and others are
lighter in colour.
Lamination is more noticeable in the light sandy layers—that in the grey
mudstones is more obscure. A parting is present parallel to the lamination. In
many cases the banding is spectacular and the rock resembles the banded mud-
stones of the Tamworth Series, there being a definite contrast between the light
and dark bands. The widths of these bands vary from less than a millimetre
to several centimetres.
B. Sponge Spicule Tuff.
This rock is closely associated with both the mudstones and the limestones
and forms a link between the two. Behind Kimbriki School beds of the tuff share
in the rhythm of the banded mudstones and grade into them. In the same section
bands of it alternate with limestone. The rock is composed of what appear to be
felspar fragments embedded in argillaceous material and is in all probability a
water-sorted tuff. It contains abundant sponge spicules. These serve a useful
purpose, as the rock is very easily recognized by their presence.
On the road from “Colraine” to the cultivation the tuff beds are several feet
in thickness and pass upward into grey impure limestones which consist almost
entirely of the remains of crinoids, bryozoans and brachiopods in a matrix of
tuffaceous material in places and elsewhere of mudstone.
C. Limestones.
Nearly six hundred feet of calcareous sediments, about half of which might be
called limestone, are represented in the section south of Charity Creek. They pass
into the banded mudstones along the strike and these assume more importance
to the east. At ‘“Colraine” and near Kimbriki School the limestone is subordinate
to the argillaceous sediments. Mudstones, tuffs and sandstones are interbedded
with the limestones.
Among the thicker calcareous beds in the Charity Creek section is an
interesting bed of the banded mudstone about two feet in width and showing the
rhythms quite as clearly as the better-developed horizons around Kimbriki. This
establishes beyond any doubt the intimate relationship between the mudstones and
limestones and is in opposition to the otherwise plausible suggestion that the
former might be varves belonging to the Carboniferous glacial suite.
The limestones are generally dark grey in colour but weather to a yellow
spongy rock consisting of insoluble material with which the calcite composing the
fossils was mixed. Some of the limestone is coarsely crystalline resembling to
some extent the Cedar Party Limestone (Voisey, 1938a) with which it may be
correlated with confidence. Most of it, however, is finer in texture, more argil-
laceous and darker in colour.
D. Mudstones, Sandstones and Tuffs.
The limestones gradually pass upward into mudstones, tuffs and sandstones.
These are all dark grey in colour; the coarser beds are quite hard but the fine-
grained mudstones are easily weathered. Fossils are rare except in the Charity
Creek section, where several bands of marine forms have been found.
The beds grade into the overlying micaceous mudstones but are separated from
the main portion of them at “Colraine” and possibly in other places by a very rich
band of marine fossils called the Linoproductus horizon.
E. Linoproductus Horizon.
The horizon is beautifully developed in the neighbourhood of ‘“‘Colraine” home-
stead and has been exposed by the Manning River which has cut into its southern
250 UPPER PALAEOZOIC ROCKS BETWEEN MT, GEORGE AND WINGHAM,
bank, revealing the folded bed. The fossils may be collected from the horizon on
either limb of an asymmetrical syncline of small amplitude.
The rock containing the shells is micaceous mudstone, the fossils being internal
and external moulds coloured by limonite. The actual shelly material is also
present, but well-preserved specimens of the forms are difficult to obtain.
Linoproductus springsurensis is particularly abundant, but the suite of fossils
collected is as follows:
Fenestella fossula Lonsdale Linoproductus springsurensis Booker.
Fenestella spp. Linoproductus cf. cancriniformis Tschern.
Protoretepora ampla Lonsdale Aviculopecten squamuliferus (Morris)
Stenopora (small dendroid form) Aviculopecten multicostatus Fletcher
Zaphrentis cf. gregoriana De Koninck Aviculopecten sprenti Johnston
Trachypora wilkinsoni Eth. Aviculopecten parkesi Fletcher
Monilopora nicholsoni Eth. Conocardium sp. (large form)
Crinoid stems (large form) Merismopteria macroptera (Morris)
Martiniopsis subradiata cf. var. Stutchburia costata Morris
branztonensis Eth. Stutchburia obliqua Eth.
Terrakea brachythaera (Sowerby) Pleurophorus sp.
Spirifer tasmaniensis Morris Myonia sp. (? small new sp.)
Spirifer stokesi Konig. Nuculana sp.
Strophalosia gerardi King Nuculana, sp. nov.
Strophalosia jukesi Eth. Nuculana waterhousei Eth.
Terrakea fragile Dana sp. Pleurotomaria morrisiana McCoy.
(Specimens F 37896—F 38012, Aust. Museum Collection.)
F. Micaceous Mudstone.
This rock is light to dark grey in colour, soft and easily weathered. It
contains a large proportion of mica, which is very useful for identification
purposes, especially since the mudstone makes very poor outcrops but yields a
light grey micaceous soil. Joints are excessively numerous, resulting in spheroidal
weathering, which is particularly well developed in cliff sections beside the river
at “Colraine’’. Calcareous nodules or concretions are common.
The mudstone is almost massive in its occurrence, only rare narrow sandstone
bands breaking its continuity. The maximum thickness measured was 720 feet
south of Charity Creek Station, and here the section was interrupted by a
fault. It is probable that the total thickness is far greater than this.
Distribution, etc.
Owing to the intense folding and faulting which has taken place, the Kamilaroi
rocks have been infolded and infaulted into Carboniferous tillite. They outcrop
largely as isolated blocks between Bundook and Hillview, except in the Kimbriki
area, where they form the limbs of an anticline.
West of Woolshed Creek the micaceous mudstones are in contact with tillite,
the lower beds of the sequence having been removed by faulting. Similar beds
containing marine fossils were recorded by Benson (1916) from Somerset, where
they are faulted against Devonian spilites.
Another small area of mudstone occurs between Woolshed Creek and Mount
George. Marine fossils were found by Benson (1916) and Sussmilch in a
railway cutting which passes through these beds. They are principally in a band
of breccia several feet in width.
= BY A. H. VOISEY. 251
Numerous specimens of Taeniothaerus subquadratus were found in the mud-
stones about half-way along the cutting which is the first one east of the railway
bridge across the Manning River. Benson (1916) listed the following forms:
Deltopecten illawarrensis, Spirifer sp., Martiniopsis subradiata, Polypora?, to which
the writer adds: Spirifer cf. tasmaniensis Morris, Spirifer duodecimcostata McCoy,
Taeniothaerus subquadratus Morris (plentiful), Linoproductus springsurensis
Booker, Aviculopecten sprenti Johnston, Aviculopecten mitchelli Eth. and Dun,
Hurydesma cordatum Morris (fairly common), Platyschisma sp. indet. (Specimens
F37671-77, Australian Museum Collection. )
Two more outcrops of the micaceous mudstone, one of which was noted by
Benson (1916), occur between Mount George and Charity Creek. The first is an
infaulted block containing Linoproductus and bryozoa, at the bend of the road
about 4 mile on the Wingham side of Mount George station. A road-material
quarry on the north of the road exposes the beds. The second is revealed by
railway cuttings a short distance to the south of the first-named outcrop.
The mudstones are seen in cuttings at Charity Creek Station and are bounded
by faults which bring them into contact with Carboniferous rocks.
More complete sequences are found on the north and south sides of the tillite
which forms the core of the Kimbriki anticline, and are terminated by faults on
all sides. Between Kimbriki and Burrill Creek the tightly infolded Kamilaroi
beds alternate with tillite. Marine fossils occur in a number of places.
Although outcrops are very poor indeed, they indicate that a belt of rocks
of the Macleay Series runs along the courses of Bow Bow and Burrill Creeks
east of Burrell Creek Post Office, and continues northwards across the Manning
River to the railway line between Karaak Flat and Killawarra. The mudstones
and limestones with the usual marine fossils are seen in cuttings along the Karaak
Flat road. Kamilaroi limestones and their associates outcrop on the hill just
before Hillview School is reached.
The rock types belonging to the Kamilaroi suite are so distinct from any
others in the district that they are readily recognized whenever they are exposed.
The fact that they are easily weathered somewhat restricts outcrops, but at the
same time this property provides a useful clue in the location of the series as a
whole. The underlying Carboniferous beds are so hard that differential erosion
along the junction serves to separate the two series.
Since the beds are lithologically and palaeontologically related to those
around Yessabah on the Macleay River, they are included in the Macleay Series
(Voisey, 1934). ‘
PLEISTOCENE TO RECENT.
The high-level river-gravels and recent alluvial deposits are shown on the
map, but will be discussed in connection with the physiography in a subsequent
publication.
IgNrEous Rocks.
Serpentine.
A belt of serpentine running north-west and south-east outcrops alongside
the Nowendoc road between its junction with the Bundook road and the village
of Mount George. It narrows near Mount George and disappears just east of the
railway station. The fault which it partly occupies continues eastward, separating
Carboniferous tillite on the north from Kamilaroi micaceous mudstone on the
south.
252 UPPER PALAEOZOIC ROCKS BETWEEN MT. GEORGE AND WINGHAM, e
Further to the west, beyond the limits of the map, the serpentine lies between
Lower Burindi tuffs and mudstones and the Kullatine tillite. Both series of rocks
are slightly metamorphosed by the intrusion.
A possible contact between Kamilaroi beds and serpentine near Mount George
school is obscured by alluvium. This occurrence of serpentine intruding
Carboniferous tillite is the first direct evidence produced that it was injected at a
period later than the Drummond Movement at the close of Upper Burindi times.
It is of little consequence, then, that a well-exposed contact with Kamilaroi
beds has not been found, since no orogeny is Known in eastern Australia at the
close of Upper Kuttung time. The Lochinvar Movement (Carey and Browne,
1938) was not characterized by extensive faulting.
A stronger argument for a late Kamilaroi age is the fact that the serpentine
fault transgresses the trends of the rocks and earlier faults which must be
referred to the Hunter-Bowen orogeny. Evidence that the serpentine is pre-
Jurassic was produced by Benson (1918, p. 493). It will be shown in a subsequent
publication that it is overlain by Triassic beds near Broken Bago, in the vicinity
of Wauchope, N.S.W.
Carey and Browne (1938) referred the Peel Thrust and serpentine to the
Drummond Movement and suggested that there was a renewal of movement along
the thrust during the Hunter-Bowen Movement. On the other hand, they recognized
the alternative of assigning both thrust and serpentine to the Hunter-Bowen
Movement, and such a course was favoured by Carey (p. 605).
Following the evidence available in the field at Mount George it seems now
that there cannot be any reasonable doubt that the serpentine at Mount George,
and possibly in other areas, belongs to the Hunter-Bowen Movement of late
Kamilaroi times.
The physical characteristics of the serpentine are similar to those of the basic
rocks described in detail by Benson (1913a, pp. 669-693).
STRUCTURAL GEOLOGY.
The geological structures are indicated on Map 1 and in the sections (Text-figs.
1, 2). The principal points worthy of notice may be considered as follows:
1. Folds and Faults in Devonian Rocks.
The structures in Devonian rocks were not studied in detail. Little can be
written of the beds south of the Kanghat Fault except that they dip generally
north or south at high angles. Silicification has obscured most of the structures
in jasper and quartzite areas.
The banded claystones and tuffs have been tightly folded and most folds have
been extensively fractured. Owing to their incompetence the claystones have
suffered much more deformation than the more resistant spilites, agglomerates
and tuffs. As the soft Kamilaroi beds are affected to a comparable degree there
is no definite evidence to demonstrate that there was any folding of the Devonian
beds prior to the deposition of the Carboniferous rocks which, on account of their
resistance, are folded and faulted to a lesser extent.
2. The Kimbriki Anticline and Associated Folds.
This is the best developed folded structure in the area. It strikes in a
west-north-west—east-south-east direction and appears to pitch to the east-south-east.
The limbs dip at approximately 45 degrees and consist of Kamilaroi limestones
and mudstones, while the core is of Carboniferous tillites and tuffs. Near the
BY A. H. VOISEY. 253
nose of the anticline in the vicinity of “Colraine” several folds of small amplitude
occur. These strike generally north and south and pitch gently to the north.
A synecline and an anticline are exposed by cliff sections on the south bank of the
Manning River. These are asymmetrical and the axial plane is tilted to the
west. Overturning accompanied by extensive faulting has taken place about a
mile to the south. Faults have broken the folds and tillite reappears near
“Mulconda”’.
3. The Kanghat Fault.
The Kanghat Fault runs right across the area shown on the map from
west-north-west to east-south-east for a distance of about sixteen miles, and has
been traced much further to the west and to the east. It is particularly important
and has very well marked physiographical expression in the Kanghat Range and
Mount Kiwarric. These features, consisting mainly of hard Devonian rocks, rise
to approximately 2,000 feet in height and present steep escarpments towards fne
north.
The fault brings Devonian spilites, agglomerates, tuffs and cherts into contact
with Kamilaroi rocks at Somerset (Benson, 1916), Kimbriki and Mount George
and elsewhere with Carboniferous tillite. Therefore, it must have a throw which
exceeds a mile in amount, but no more exact measurement of this could be made.
4. The Hillview Fault.
This fault forms the northern boundary of the downthrown block which is
responsible for the valley through which Bow Bow Creek flows. It runs at a slight
angle to the Kanghat Fault and separates Devonian banded claystones and tuffs
on the north from the Carboniferous and Kamilaroi beds on the south.
5. The Killawarra Fault.
The Killawarra Fault runs in a north-south direction parallel to Bow Bow
Creek and passes just west of Killawarra Bridge. Owing to poor outcrops, its
position as indicated on the map is approximate only, but its presence is amply
demonstrated because it separates Devonian claystones and tuffs on the east from
Kamilaroi rocks on the west. It is probable that a number of smaller faults are
present in the neighbourhood of Killawarra Bridge.
6. The Charity Creek Fault.
This fault separates Lower Burindi from Kullatine beds north of Donkin’s
Mountain near Karaak Flat, and Lower Burindi from Kamilaroi beds near
Charity Creek station. It may continue westwards to Mount George, but as, in
such a case, it would bring tillite into contact with tillite, it would be difficult to
detect. Strike measurements can be made only rarely in tillite areas.
7. Other Faults.
Faulted relationships between Lower Burindi and Kullatine strata are
indicated north of Charity Creek, and two major faults are shown. There is no
doubt, judging from minor anomalies in strike and dip measurements, that faults
are excessively numerous throughout the whole area, and even the number of faults
shown on the map gives little indication of the shattering to which the rocks have
been subjected.
Age Relations of the Folding and Faulting.
The oldest group of faults are those which are genetically related to the
folding of the Devonian, Carboniferous and Kamilaroi beds. Especially in the
254 UPPER PALAEOZOIC ROCKS BETWEEN MT. GEORGE AND WINGHAM.
Devonian claystones are the faults in anticlines and synclines obvious results of
the extreme compression to which the beds were subjected. Numerous other
faults involving the incorporation of blocks of Kamilaroi strata in Carboniferous
areas almost certainly belong to the folding period.
The fault which is occupied by serpentine at Mount George cuts across the
folded rocks and faults associated with such folding and is therefore of later
occurrence. Its relation to the Kanghat Fault is not demonstrated in the area.
The group of very large faults, Kanghat, Hillview, Killawarra and Wingham,
also cut across earlier trends and are distinctly of later occurrence than the first
period of folding and faulting. They may be referred, tentatively, to the Hunter-
Bowen Movement, but there is not any evidence available to prove that they were
not of much later occurrence.
Acknowledgement.
I desire to thank Mr. R. T. Cox, of ‘‘Colraine”’, Kimbriki, for his hospitality
extending over a period of several months. It was he who was instrumental in
drawing attention to the important fossil beds at Kimbriki, and his careful
observations and local knowledge of the rocks have been very helpful.
References.
BENSON, W. N., 1913a.—The Geology and Petrology of the Great Serpentine Belt of
N.S.W. Part i. Introduction, ete. Proc. LINN. Soc N.S.W., xxxXviii.
, 1913b.—The Geology and Petrology of the Great Serpentine Belt of N.S.W.
Part iii. Petrology. Proc. LINN. Soc. N.S.W., xxxviii.
—_————, 1916.—The General Geology of the Gloucester District. Jour. Roy. Soc. N.S.W.,
Vol. 1.
Carbpy, S. W., and BROWNE, W. R., 1938.—Review of the Carboniferous Stratigraphy,
Tectonics, and Palaeogeography of New South Wales and Queensland. Jour. Roy.
Soc. N.S.W., lxxii.
Davin, T. W. E., 1932.—A New Geological Map of the Commonwealth of Australia.
OSBORNE, G. D., 1922.—The Geology and Petrography of the Clarencetown-Paterson
District, N.S.W. Parts 1 and 2. Proc Linn. Soc. N.S.W., xlviii.
SussmMILcH, C. A., 1921.—The Geology of the Gloucester District. Jour. Roy. Soc.
N.S.W., lv.
Voisny, A. H., 1934.—The Geology of the Middle North Coast District of N.S.W. Proc.
LINN. Soc. N.S.W., lix.
, 1938a.—The Upper Palaeozoic Rocks in the neighbourhood of Taree. Proc.
LINN. Soc. N.S.W., Lxiii.
, 1938b.—The Geology of the Armidale District. Proc. Linn. Soc. N.S.W., Ixiii.
WooLNouGH, W. G., 1911.—Preliminary Note on the Geology of the Kempsey District.
Jour. Roy. Soc. N.S.W., xlv.
THE LORNE TRIASSIC BASIN AND ASSOCIATED ROCKS.
By A. H. Votsry,* M.Sc., Lecturer in Geology and Geography,
New England University College.
(1 Map; two Text-figures.)
[Read 31st May, 1939.]
The first record of Triassic rocks in the neighbourhood of the Camden Haven
River appears to be that contained in a report by J. E. Carne in 1897. Carne
found well preserved plant-remains in clay-shales underlying a massive bed of
conglomerate at Perpendicular Point, a short distance south of the entrance of the
Camden Haven River. He located similar beds at Grant’s Head and Diamond
Head and erroneously correlated them with the deposits at Crowdy Head. The
rocks at the last-named locality are Carboniferous. Carne viewed the Broken Bago
Range from Wauchope and suggested that it was composed of Mesozoic rocks
underlain by Permo-Carboniferous coal measures as in the Sydney District.
Carne also referred to the Triassic beds in his paper on the Western Coalfield
(1908); Benson (1918) showed a large area of Triassic rocks south of Port
Macquarie on his sketch-map, and Osborne (1929, p. 449) remarked on Triassic
rocks in the Kempsey district. However, the suggested Mesozoic area south of
Wauchope was not shown on other maps and only the coastal headlands and
Oxley Island were marked as Triassic. The alleged occurrence at the last-named
locality will be discussed later.
The writer, in the course of his investigations, independently came upon
Carne’s fossil locality at Perpendicular Point and collected a number of well
preserved specimens which were exhibited at a meeting of the Linnean Society
in September 1937. Since then the Triassic rocks have been examined in a
number of localities and portions of the boundary have been mapped.
It has been decided to call the geological structure which the beds constitute,
the Lorne Triassic Basin. The rocks themselves will be discussed under the
name of Camden Haven Series after the river which drains the Basin.
The igneous rocks which intrude the Triassic strata, the Palaeozoic sediments
and the serpentine with which they are associated will receive brief mention.
However, the boundaries between these units have not been mapped in detail and
most of those shown on the map (Map 1) are approximations only.
STRATIGRAPHY.
TRIASSIC: CAMDEN HAVEN SERIES.
Distribution.
The Camden Haven Series, as mentioned above, forms the headlands of
Perpendicular Point and Camden Head, Grant’s Head, and portion of Diamond
Head. These occurrences are separated from one another by low swampy coastal
* This paper was completed while the author was Linnean Macleay Fellow of the
Society in Geology.
256 LORNE TRIASSIC BASIN AND ASSOCIATED ROCKS,
flats so that it is impossible to trace the beds from one headland to the
or towards the principal basin structure further inland.
GEOLOGICAL SKETCH-MAP
OR une
CAMDEN HAVEN
DISTRICT
ajelole
STACKING
” WAUCHOPE pig-SSS>), A
ree ; POINT
»6 &4 5 +7
.
[GEN ae
([MTHE “RocK
a
ott ON)
rin ey
PERPENDICULAR
cH POINT
—_ AACAMOEN HEAD
iN LAURIETON
a =.
wu oie ’ “oouy
TN LIN Fy aE UO
au ”
2 *
Af
JOHNS, RIVER
= DIAMOND
TR HEAD
LEGEND
RECENT
PLEISTOCENE
Sha ie TRIASSIC
) STEWARTS R
KAMILARO!
CARBONIFEROUS ee
DEVONIAN
LOWER PALAEOZOIC
IGNEOUS
BASALT [Xxx]
ALKALINE EXTRUSIVES <5
ALKALINE INTRUSIVE ES
hk HARRINGTON SERPENTINE Fe)
= POSSIBLE FAULTS ———
MANNING
RIVER OUNTAIN SUMMITS
RAILWAY
ROADS
iL YS
vex (MITCHELL'S
DXLEY'. ISLAND.
| WEST BROTHER
HERONS CREEK
BROKEN BAGO
WAUCHOPE
B BCOOPERNOOK
op
om |
"4
a 44a 46
Ay Wx ay Os
js a yy eN
a CARBONIFEROUS 4
hs AO Dy
aA 4
a 4 4 a 4 a 4
4
ao 4
4
No
( COMBOYNE
BASALT
Fig. 1—Sketch Section from Coopernook to Wauchope.
Fig. 2—Sketch Section from Comboyne to Camden Head.
RIVER
ALKALINE RocR
Toe —— Ie
V/H =
Niipsi= wWAls
other
BY A. H. VOISEY. 257
Conglomerates, sandstones and grits constituting the basal beds of the series
may be traced from Broken Bago, just south of the town of Wauchope, westward
towards the Comboyne Plateau. They then swing southward, running east of the
Comboyne to curve easterly just north of Upper Lansdowne. Thence the beds swing
to the north-east to the neighbourhood of Coopernook. Along the easterly rim
of the basin large intrusions of alkaline rock have interrupted the continuity
of the beds and have made alterations in the direction of dip. However, the
Triassic beds are exposed by cuttings alongside the Pacific Highway between John’s
River and Ross Glen.
Within the basin outcrops are poor, on account of the ease with which the
soft clay-shales and sandstones, which overlie the more resistant beds of the basal
stage, are weathered. Road cuttings between Kendall and Lorne expose the beds,
which, in places, are overlain by Tertiary lavas.
Lithology.
The basal beds of the Camden Haven Series may be seen to advantage almost
anywhere around the rim of the Lorne Basin. To the north-west of Lansdowne
they consist of massive conglomerates, the basal bed being upwards of fifty
feet in thickness and forming a frowning escarpment. The rock is made up of
boulders and pebbles of quartzites, jaspers, cherts, quartz, and other resistant
rock-types. Some of the boulders attain a diameter of two feet, but for the most
part, they are only a few inches across.
The conglomerate in this region, the southern rim of the Basin, is overlain
by coarse sandstones and grits which are stained reddish-brown and purple by
iron-oxides. These may be examined at various points along the road between
Coopernook and Vincent’s Lookout. The sandstones pass upwards into grey
shales containing plant remains, and reddish and purple clay-shales which resemble
those of the Narrabeen Series further south. A good section of these beds is
to be seen in the cuttings along the Vincent’s Lookout road shortly after the
railway line is crossed near Coopernook Station. An estimated thickness of about
three hundred feet cf sediment occurs here, but outcrops of the clay-shales are so
poor, and dips so slight, that no information regarding higher beds in the series
could be obtained.
In the road cuttings along the Pacific Highway just south of Ross Glen the
grey and purple clay-shales associated with bands of sandstone are well exposed.
Plant remains are said to have been found in them. It is probable that these
beds correspond with those on the Vincent’s Lookout road, but this is uncertain.
Probably the best section which has been examined is that shown by the
cuttings alongside the road to Wauchope which leaves the Pacific Highway near
Heron’s Creek.
Where this road descends to a creek near the railway tunnel through Broken
Bago, four miles by road from Wauchope, a thickness of approximately two
hundred feet of coarse grits and fine quartz-pebble conglomerates, interstratified
with purple and grey shales and sandstones, was measured. The coarse beds
are each several feet in thickness and constitute the bulk of the section. The
heavy conglomerate underlies the grits, but varies somewhat in its development
from place to place. The clay-shales and sandstones which overlie the more
resistant basal beds again give rise to very poor outcrops.
The Pacific Highway crosses the Camden Haven Series between Heron’s
Creek and the turn-off to Green Hills beach. Outcrops are scarce all the way,
but conglomerates and sandstones, probably belonging to the basal stage, are
v
258 LORNE TRIASSIC BASIN AND ASSOCIATED ROCKS,
exposed by a road-material quarry about 13 miles south of Port Macquarie near
the Green Hills Beach turn-off. Between this point and Broken Bago the Triassic
beds cross and overlie the serpentine which is so well developed in this district.
The highest known beds of the series outcrop in the neighbourhood of Lorne
and are exposed in road cuttings. These are clay-shales, generally grey in colour,
containing plant remains, and associated with sandstone bands. The exact position
of these beds in the sequence could not be determined on account of the low
dip and lack of continuous outcrops.
The Camden Head or Perpendicular Point occurrence, which is important
because it was the first outcrop of the Triassic rocks found, is somewhat anomalous
when studied in relation to the rest of the beds in the sequence. As described by
Carne, a massive conglomerate overlies purple and grey clay-shales containing
plant remains. This is the reverse of the sequence of beds elsewhere in the
area.
The section as exposed in the cliff face at Perpendicular Point is as follows:
Thickness in feet.
Conglomerate STEN aya VGOnh | Zao TTI eee aeRO tore Ret LO
Purple tclay=shale. gate. is Se UATE OPED See 110
Purple sandstonesiicah tireeiou ast He GoM ietAd) Pose te 2
Purple melay=snaley ype teat “cio wncay «seu ET toe 15
Grey clay-shales with plant-remains So a wie Re 5
Purple*clay-=shaley
He
fm es
ase eWER ce oe asses
ErvERGENCE Dates
Fig. 10.—Graph showing total emergence of 1,058 adults of Tepperella trilineata
and 7038 adults of Megastigmus acaciae from one series of galls on Acacia decurrens in
the spring of 1936.
Tepperella trilineata
Megastigmus acaciae -----------
276 NEW SPECIES OF MEGASTIGMUS,
Galls were collected on 17th October, 1935, from the same tree, and adults of
M. acaciae were then emerging in numbers. On 28th October, 1921, galls were
collected from Acacia decurrens at Wyong, and at this time adults of M. acaciae
were emerging freely.
In Table 5 are set out the results of the periodical dissection of galls in the
spring of 1936, showing only the various stages of M. acaciae present, after the
larvae of this species have eaten their way out of the larvae of Tepperella
trilineata.
Pupae were present on 6th September, 1936, and the last pupa was found on
18th October, 1936. The first mature larvae were found on 22nd August, but
mature larvae were found up to 4th October, which was slightly more than one
month before the last adult emerged.
In the spring of 1937, in dissections made from 13th September to 16th
September inclusive, 55 mature larvae, three prepupae, and 5 pupae of M. acaciae
were found in the galls from the same tree. The first mature larva of M. acaciae
was found on 30th August, 1937, the first pupa was found on 4th September, 1937,
and the first adults of M. acaciae emerged on 38rd October, 1937, only one day later
than the first emergence of this species in the preceding year, though the emergence
of its host Tepperella trilineata was twelve days later in 1937 than in 1936.
TABLE 5.—Results of Dissections of Galls from A. decurrens in the Spring of 1936 showing the Progressive
Development of M. acaciae after leaving the larvae of Tepperella trilineata.
Number Stage of M. acaciae present.
: of Cells
Date of Vacated or
Dissection. Occupied Remarks.
by other Mature
Species. | arvae. Pupae. Adults.
| |
22/8/36 a3 80 5 = — [eee M. acaciae larvae still within
30/8/36 ae 132 4 — — host larvae.
6/9/36 af 203 Sul 19 — J
9/9/36 a 63 8 6 = |
13/9/36 ar 69 23 6 = |
20/9/36 are 116 23 12 —
27/9/36 an 197 il 24 —
4/10/36 o8 148 1 25 3
11/10/36 cea 81 = 21 4 Some of the vacated cells during this
18/10/36 aa 132 — 13 8 period must have once been occupied
25/10/36 - | 98 — — 4 by M. acaciae.
1/11/36 eaes| 112 ; _ — 2
8/11/36 a 109 — —_— —_—
First adult of M. acaciae emerged 2nd October, 1936.
Last adult of M. acaciae emerged 8th November, 1936.
Percentage of Parasitism.
In May and June 1936, 545 larvae of J’epperella trilineata were dissected, and
211 or 38-71 per cent. were found to contain larvae of Megastigmus acaciae.
In a previous paper (1939) the writer discussed the biology of Hurytoma
gahani Noble, another species of Chalcid which is present in these galls on Acacia
decurrens. The larvae of this species are to be found in the same gall cells as
larvae of the primary gall-former, Tepperella trilineata, and ultimately the larvae
BY N. S. NOBLE. PHT
of EL. gahani devour the larvae of T. trilineata with which they are associated, and
destroy at the same time any larvae of M. acaciae which happen to be present in
these cells.
In the 545 cells mentioned above, though 211 larvae of M. acaciae were present,
all but 97 were also accompanied by the larvae of H. gahani and would later have
been destroyed; thus out of the 545 cells examined, adults of Megastigmus acaciae
would only have emerged from 97 or 17:80 per cent. of them.
In the spring of 1937 a further 545 gall cells from the same tree were examined,
the larvae of Hurytoma gahani at the time of examination having already devoured
the other occupants of the gall cells. It was found that Megastigmus acaciae would
have emerged as adults from only 71 or 13-03 per cent. of the gall cells, a decrease
of more than 4 per cent. as compared with 1936.
Effect of Parasitism on the Host and on Gall Development.
At times during the course of these investigations, minute galls were observed,
which were much less advanced than the majority of the galls on the tree, and
dissection of these frequently revealed minute host larvae, which were parasitized,
and which were much less advanced than unparasitized larvae of this species in
other galls. However, such minute galls were also found, in which very backward
larvae of T. trilineata were present, and were unparasitized.
On the other hand, maturing larvae of T. trilineata have been examined in
which well-developed larvae of M. acaciae were present, without having any
apparent effect on the host larva.
At various times unilocular galls were found in which mature larvae or pupae
of M. acaciae alone were present, and these galls were just as large and normal as
galls in which the primary gall-former, 7. trilineata, was present alone. Froggatt
(1892), in the case of Trichilogaster acaciae-discoloris, causing galls on Acacia
discolor, stated that, as a result of infestation by a small black chalcid, the galls
are changed to a shapeless, fleshy mass. In the case of T. trilineata it would
appear that, provided the larvae are permitted by the parasite to reach maturity,
the presence of the latter does not affect the size or shape of the gall.
SUMMARY.
The external morphology and biology of Megastigmus acaciae, a new species, ~
are set out.
M. acaciae is an internal parasite of the larva of Tepperella trilineata, a species
which causes galling of the flower buds of Acacia decurrens and, like its host, the »
life cycle of M. acaciae is annual.
Emergence of both species commences in the spring each year. Hmergence
of adults of M. acaciae commences after most of the host adults have emerged, the
main emergence taking place in October. Of a total of 1,559 adults which emerged
in 1936, 1,013 or 64:98 per cent. were males and 546 or 35:02 per cent. were females.
Adults of M. acaciae are short. lived, the average length of life of male wasps
in the laboratory being 5:46 days, and of female wasps 5-17 days.
Eggs of M. acaciae are found in first-stage larvae of T. trilineata, but it is
possible that they may be deposited in the eggs of the latter species and remain
unhatched until after the eggs of J. trilineata had done so, this being the known
habit of Epimegastigmus brevivalvus, an allied species studied by the writer.
The entire larval period of M. acaciae is spent within the haemocoele of the
host larva. For the greater part of the larval period, the development of the
parasite larva is very slow, the latter still being comparatively small and some
being only in the first stage, when the last host-larval stage has been reached. A
278 NEW SPECIES OF MEGASTIGMUS.
period of rapid development then follows and, before the larva of TJ. trilineata
can pupate, the larva of M. acaciae devours all of its internal contents, eats its way
out of the larval skin of the host, and later pupates in the cell formerly occupied
by the host larva.
There are five larval stages, all of which are described.
Of 545 larvae of J. trilineata dissected in 1936, 211 or 38-71 per cent. were
parasitized by WM. acaciae.
Acknowledgement.
The writer wishes to acknowledge his indebtedness to Dr. A. B. Gahan, Senior
Entomologist of the United States Department of Agriculture, for his valuable
observations on the species under discussion.
Literature Cited.
Froceatrr, W. W., 1892.—Notes on Australian Cynipidae with descriptions of several new
species. Proc. Linn. Soc. N.S.W., (2) vii, 152-156.
Nose, N. S., 1938a.—EHpimegastigmus (Megastigmus) brevivalvus Girault: A parasite
of the citrus gall wasp (Hurytoma fellis Girault) ; with notes on several other species
of hymenopterous gall inhabitants. Sci. Bull. N.S.W. Dept. Agr., 65.
, 1938b.—Tepperella trilineata Cam., a wasp causing galling of the flower buds
of Acacia decurrens. Proc. LINN. Soc. N.S.W., Ixiii, 389-411.
, 1939.—A new species of Chalcid (genus Hurytoma) associated with Tepperella
trilineata Cam., a wasp causing galling of the flower buds of Acacia decurrens.
Proc. LINN. Soc. N.S.W., Ixiv, 223-241.
279
A RECONNAISSANCE SURVEY OF THE VEGETATION OF THE
MYALL LAKES.
By T. G. B. Osporn? and R. N. Rogpertson.?
(Plates vi-vii; three Text-figures.)
[Read 28th June, 1939.]
The coastal dune and swamp sequences of New South Wales have been so
much disturbed in the neighbourhood of Sydney, and for many miles to the north
and south of it, that particular interest is to be found in the Myall Lakes district.
There the coastal vegetation has been very little disturbed and the series of plant
communities that it shows can be examined in an almost primitive state. The
same area also offers some interesting comparisons between the Eucalyptus forest
developed on recent sands and on hills of palaeozoic rocks. The junction between
Hucalyptus forest and sub-tropical rain-forest—locally called ‘brush’—can also be
studied. These features of ecological interest appear to justify our placing on
record the notes made on three reconnaissance visits to the area. Circumstances
will prevent our continuing the joint work.
Visits were made to the area in September 1934, June and September 1935.
The first two were with the Sydney University Rover Scouts. We are indebted
to all who took part in these camps for assistance in various ways which made
possible work in an otherwise sparsely inhabited district. We also desire to
express our thanks to certain members of the camps for technical help; to S. W.
Carey and H. Maze for access to their field-notes on the geology and physiography
of the area; to N. A. Kelly and N. C. W. Beadle for help in collecting, and to O. D.
Evans, of the Botany School, University of Sydney, for assistance in determining
some of the plants.
The Myall Lakes are an extensive series of coastal lagoons situated 32° 30’ S.
Lat., and 152° 25’ E. Long., about 50 miles north-east from Newcastle. At the
present day they communicate with the sea only indirectly, by means of the
Lower Myall River. This is a slow-moving, narrow, tortuous stream which extends
from the southern end of the Lakes to Tea Gardens on Port Stephens, eleven
miles away. Between the lakes and the Southern Pacific Ocean lies a belt of sand-
dunes, low heaths and swamps, varying in width from a few hundred yards at
Mungo to three miles or more at its northern end. From this there rise at
infrequent intervals low rounded hills of tuffaceous rock. To the west of the
lakes the country consists of broken hills and valleys—also of tuffaceous rock—
with, however, considerable swamp and heath areas.
Though the area has been inhabited by white men for over a century, much
of it, especially the dunes, heaths and swamps, is still in a primitive state. Much
1 Department of Botany, Oxford.
2Botany School, University of Sydney. The field work was carried out whilst the
writer held a Science Research Fellowship of the University of Sydney and (later) a
Linnean Macleay Fellowship in Botany.
280 VEGETATION OF THE MYALL LAKES,
of the forest has been influenced by timber-getting,? or has been partially cleared
for grazing, but sufficient remains to reconstruct the essential parts of the story.
PHYSIOGRAPHY.
During the Tertiary Period the area now occupied by the Myall Lakes, like
the rest of the East Coast of Australia, was subjected to the uplift which resulted
in the formation of the coastal tablelands. In this region the uplift probably
amounted to about 1,300 feet. The plateau of palaeozoic tuffs thus formed was
PALAEOZOIC ROCKS
UNSHADE D
RECENT SAND,
SILT »» SWAMP
Fig. 1.—Sketch Map of the Area. C.K. = Chinaman’s Knob on the Lower Myall
River; M = Mungo; B.P. = Bombah Point; V.H. = Violet Hill; S.G. = South Gibber.
rapidly attacked by streams which carved deep valleys into its surface. In a
subsequent general subsidence of some 400 feet, these valleys were drowned by
the sea and a typical rias coast was formed. The coast then presented a rugged
appearance with numerous off-shore islands. At that time landmarks like Mungo,
Violet Hill, Bombah Point and Chinaman’s Knob were all islands. The combined
action of coastal currents, waves and tides resulted in the formation of sandspits.
Under the influence of currents, these sandspits would develop on the south-
western side of the islands and, gradually extending southwards, link up with
each other. Thus there would be formed a continuous sandspit running from
2R. Dowson, who founded the Australian Agricultural Company’s Settlement at
Port Stephens, records that he ascended the Myall River in 1825 to visit a timber-camp,
and that “Cedar” (Cedrela Toona) getters had been operating in the district, under
licence, for some time previously. ‘‘Present State of Australia, etc.”’, Edition II, pp.
41-76, London, 1835.
BY T. G. B. OSBORN AND R. N. ROBERTSON. 281
island to island for twenty miles parallel to the coast. This cut off the Myall
Lakes as a large coastal lagoon studded with islands. With their appearance
above water, the sandspits became subject to the direct action of wind which
caused the sand to accumulate in dunes and to advance landwards across the
sandspits. Since the prevailing wind was an easterly, and since the coast-line ran
approximately NH-SW, the sand-dunes, advancing before the wind, did not advance
parallel to the coast, but developed en échelon.
Meantime, land was, and is still, being reclaimed from the lakes. The accumu-
lation of blown sand has caused a gradual shallowing. Sand-bars made their appear-
ance and, assisted by the water-weeds, were built above the water. There are no
recently-formed sand-islands in the lakes, but the extensive sand-bar in the lower
part of the Booloombayt Lake approaches within a foot of the surface. In certain
parts of the area—particularly on the Broadwater—the waves of the lake them-
selves have caused an accumulation of sand to form sloping beaches. The sand
thus raised above the water has come under the influence of the wind and has
formed dunes of varying sizes on the inland shore of the lakes.
Certain areas, Known locally as ‘moors’, extend for some miles without any
elevation whatever. Though known as ‘moors’ there is no accumulation of peat on
them, and they will be termed ‘heaths’ in this account. Their level nature and the
fact that they are bounded by fixed sand-dunes point to their being old lake beds
which, having been raised above the water-level, have gradually drained. (Possibly
the relatively recent 15-foot uplift recorded in places along the New South Wales
Coast may account for some of these heaths.)
While the chief reclamation of the lakes, particularly on the coastal side, has
been by sand, silt deposition has been important in some areas. Three main rivers
drain into the lakes, the Upper Myall River and Dirty Creek into Broadwater at
the south, and the Booloombayt Creek into the small lake of that name in the
centre. These streams have built silt flats of considerable areas. Silt deposition
is at present active at the outlet (on the Broadwater) of the Lower Myall River
and particularly so at the mouth of Booloombayt Creek.
Beyond the entrance of the Lower Myall into Broadwater, tide has very little
effect, and in the channel at Bombah Point which connects Broadwater and
Booloombayt, the effect of daily tides cannot be noticed. The mangrove, Aegiceras
majus, which tolerates a considerable amount of freshwater, grows with Casuarine
glauca in the upper reaches of the Lower Myall, but does not enter the lakes.
Floods are very important. The Myall Lakes present the interesting example
of a lake system which is drained at one end and filled in the centre. That is to
say, they are drained by the Lower Myall River in the south, and filled by the
Upper Myall River, Dirty Creek and Booloombayt Creek, but the largest lake—
Myall Lake proper—receives no streams of importance. During flood times the
rivers filling the lakes do so at a much greater rate than the small Lower Myall
River can drain them. Consequently, they may rise quite rapidly. The rising
waters of the Booloombayt meet the rising waters of the Broadwater and, being
unable to escape, are pushed away from the outlet into the Myall Lake. Thus
the lakes which drain Myall Lakes are also the lakes which flood it. If the floods
in the filling streams are also accompanied by spring tides on the Lower Myall
River, the northward flow of the water may be quite rapid, and a strong current
may run in the channel at Bombah Point. This channel is the only place in the
lakes which shows evidence of stream scour.
The salinity of the lakes varies periodically. Generally speaking, the water
is brackish, but following heavy rain in the surrounding ranges, it may be almost
x
282 VEGETATION OF THE MYALL LAKES,
fresh. The salinity increases greatly after periods of dry weather, especially if
such periods are accompanied by high tides in the Lower Myall.
CLIMATE.
The Myall Lakes lie in the coastal belt of New South Wales, just within the
region having a maximum summer rainfall. The two nearest stations on the
coast for which rainfall figures are available are Manning Heads and Newcastle.
Manning Heads is about as far north of the area as Newcastle is to the south.
The average annual rainfall at these two stations is 139-7 ecm. (5,505 points) and
116-1 cm. (4,571 points) respectively. The rainfall in the Myall Lakes area may,
therefore, be taken as about 127 cm. (50 inches) per annum. The average monthly
falls at Manning Heads and Newcastle are set out in the following table:
Average Annual Rainfall in Millimetres.
Jan. | Feb. | Mar. | April. | May. | June. | July. | Aug. | Sept. | Oct. | Nov. | Dec. | Year.
Manning
Heads | 123 156 146 142 137 123 112 87 84 80 94 113 1397
Newcastle 88 103 122 119 126 99 119 78 78 58 66 87 1161
160
150
140
130
120
/10
100
90
80
70
60
50
J F M A M J J A S (a) N D
Fig. 2.—Curves showing mean annual rainfall in millimetres at Manning Heads
(continuous line) and at Newcastle (broken line). Data from C.S. & I.R. pamphlet 42,
1933.
BY T. G. B. OSBORN AND R. N. ROBERTSON. 283
Occasionally very heavy falls of rain accompanied by severe flooding are
features of the summer months. Thus, in Newcastle, there are records of 25-4
or 27:94 cm. (10 or 11 inches) of rain falling within 24 hours. It will be noticed
(Fig. 2) that the late summer months, February-March, are the wettest months,
and that the spring, September—October, are the driest. The main flowering period
of the sclerophyllous shrubs is in the months August-September.
At Manning Heads the average annual humidity is 77%, the extremes being
83% in April and 71% in October. An effect of the high humidity is to be noticed
in the abundance of the epiphytic Dendrobium teretifolium on Casuarinas fringing
the slow-moving rivers. Epiphytes do not usually develop on Eucalypts, but a
young tree of Ficus rubiginosa was observed in a fork of a large Hucalyptus
tereticornis near the entrance to Booloombayt Lake, opposite to Bombah Point.
3
16) 90
wo 20 i a ag <
Y Hie rg eo eee x Zane 80
A TRissogserad= See es ees S
Smear Al UMS Sale. Ale hk Soa MORNIN TS
Fig. 3.—Curves showing mean monthly maximum (continuous line) and minimum
(broken line) temperatures at Manning Heads in °C., also mean relative humidity (as
per cent.). Data from C.S. € I.R. pamphlet 42, 1933.
The mean maximum and minimum temperatures at Manning Heads are given
below:
Mean Temperature at Manning Heads in Degrees C.
Jan. | Feb. | Mar. | April.| May. | June. | July. | Aug. | Sept. | Oct. | Nov. | Dec. | Year.
Maximum 26°2 | 25-9 | 24-7 | 22-5 | 19-7 | 17-7 | 17-0 | 18-1 | 20-5 | 22-4 | 24-3 | 25-3 | 22-0
Minimum L727) W295) 16285) V4 ae hO8 8:7 7:4 8-1 | 10-0 | 12-9 | 15-1 | 17-2 | 13-1
Night frosts are not unknown between June and August in the valley bottoms.
They may have an effect on the stunted vegetation of the large open heaths.
THE PSAMMOSERE.
The vegetation of the sand-dunes shows all stages from that of the first
colonists of bare beach to climax forest on fixed dunes. The climax is an associa-
tion in which Hucalyptus pilularis (the black-butt) is found with H. gummifera,
Angophora lanceolata, and one or other of the Banksias, B. integrifolia or
B. serrata. The sere is complicated by an admixture of certain lower-growing but
broader-leaved species, e.g., Cupaniopsis anacardioides, Clerodendron tomentosum,
in more favourable locations near the sea. It is part of an Indo-Malayan element
in the flora which, however, does not enter into the Climax. There are some
extensive blow-outs and white dunes to the south of the area, inland from
Broughton Island.
284 VEGETATION OF THE MYALL LAKES,
Strand Plants.
The strand consists of a clear white sand derived from the wastage of the
tuff rocks. Unlike the sands of the southern Australian coast, it has not a high
lime content. Cakile maritima, a doubtfully indigenous species, is the only true
strand plant.
Fore-Dune.
Dune building is begun by Festuca littoralis, a tussock grass, mingled with
which low mats of Senecio spathulatus may also occur. Spinifex hirsutus, which
also occurs, is not so important in dune formation as it is further south on the
Australian coast.
Fixed Dunes.
These are remarkable for the important role of such mat plants as Mesembryan-
themum aequilaterale, Scaevola suaveolens and Stackhousia spathulata, also for
the early appearance of woody plants such as Correa alba and Leucopogon Richei.
The mat plants may persist, binding the sand into rounded hummocks a metre
or more in height, long after wind erosion has removed the low dune on which
they had been growing.
The following is a composite list from the dune face and the crest of the first
line of dunes:
Festuca littoralis
Spinifex hirsutus
Scirpus nodosus
Dianella caerulea
Lomandra longifolia
Pelargonium australe
Oxalis corniculata
Mesembryanthemum aequilaterale
Correa alba
Acacia longifolia
Apium prostratum
Leptospermum laevigatum
Leucopogon Richei
Stackhousia spathulata
Monotoca elliptica
Convolvulus Soldanella
Cupaniopsis anacardioides
Pomax umbellata
Scaevola suaveolens
Senecio spathulatus
Kennedya rubicunda S. lautus
Euphorbia Sparmanni Sonchus maritimus
The height to which the taller of these plants will grow is dependent on
exposure. Thus Cupaniopsis, normally a small tree about 3 m. high, has been
observed growing in extensive mats, not more than 30 cm. high, on the edge of
a stable dune. The density of the vegetation appears to be dependent upon its
freedom from fire, rather than on actual exposure to wind-shearing. Dense
impenetrable thickets of shrubs and low trees occur on exposed faces of settled
dunes, pruned neatly to an angle of 25° with the horizontal. Such a thicket may
have the following composition:
Banksia integrifolia Leptospermum laevigatum
B. serrata Angophora lanceolata
Breynia oblongifolia Monotoca elliptica
Dodonaea triquetra Myrsine variabilis
Eugenia Smithii Notelaea longifolia
Clerodendron tomentosum
The lianes, Kennedya rubicunda, Hibbertia volubilis and Tecoma australis are
found intertwined with the woody plants. In such a dense thicket there is very
little ground flora. Occasional plants of Pomaxr umbellata and Commelina cyanea
occur, but are not important.
Fixed Dune Woodland.
Banksia-Angophora Forest.
Given sufficient shelter from the wind, the tree species quickly assume
dominance and a more open woodland community results. The dominants here
BY T. G. B. OSBORN AND R. N. ROBERTSON. 285
are Angophora lanceolata and one or other of the Banksia species. In some places
the twisted limbs and frequent branching of the Angophora give evidence of its
development under scrub conditions (Pl. vi, fig. 3). In such a woodland the trees
may be no more than 5 m. high. Under more favourable conditions the dominants
may be 20 m. or more.
With the dominance of the trees, two changes are to be noted. First, the
broad-leaved species of sub-tropical affinities disappear. This ‘brush’ element,
which is a characteristic feature of the dense dune scrub, is not conspicuous or is
wholly absent in the dune forest. Secondly, most of the shrub species associated
with the earlier phases are lost. Other shrubs come in, also Pteridium, Macrozamia
and various Cyperaceae. Grass is not a feature of the dune forests. This
Angophora-Banksia forest is a very characteristic community of the settled dunes
and intervening dune flats. It exists in all grades between a forest with close,
but not dense, canopy and very little undergrowth, to open scrub woodland with a
considerable undergrowth of shrubs. Finally, as a result of burning, there may be
extensive areas of scrub in which the Angophora is absent and the Banksias only
present in the shrub layer.
The following are some of the more important constituents of the under-
growth in the Angophora-Banksia forest:
Pteridium aquilinum Hriostemon lanceolatus
Macrozamia spiralis Gompholobium latifolium
Imperata cylindrica, var. Koenigii Goodia lotifolia
Schoenus ericetorum Leptospermum laevigatum
S. imberbis Halorrhagis tetragyna
Xanthorrhoea hastilis HI. teucrioides
Lomandra longifolia Monotoca elliptica
Persoonia lanceolata Styphelia viridis
P. salicina Pomax umbellata
Leptomeria acida Opercularia varia
With the destruction of the dominants a great wealth of shrubs comes in,
chiefly nanophyllous or microphyllous forms belonging to the Proteaceae,
Leguminosae, Myrtaceae or Hpacridaceae. These are given at some length in
Appendix I.
Dune Hucalyptus Forest.
On deep stable sands, whether of fixed dunes or inter-dune flats, a forest of
Hucalypts develops. Hucalyptus pilularis is the dominant and often occurs pure,
though there is commonly present H. gummifera. Occasional trees of Angophora
lanceolata persist, and Banksia serrata is generally present in the second tree-
layer. This forest has a rather open canopy, but the amount of shade, and conse-
quently the scarcity or density of the undergrowth, appear to depend largely on
the time which has elapsed since the last forest-fire. The dominants are generally
about 15 m. in height, with a secondary tree-layer—largely Banksia serrata—up to
half that height. When the forest is open, an upper shrub layer may reach 2-3 m.
It contains such species as Leptospermum stellatum, Calycothrix tetragona, Lepto-
meria acida, Persoonia salicina and Banksia aemula. Such a height is excep-
tional; most of the undershrubs do not reach more than a metre. Such plants are
Banksia spinulosa, Isopogon anemonifolius, Persoonia lanceolata, Conospermum
taxifoium, Acacia suaveolens, A. discolor, Hibbertia linearis, Eriostemum Crowei,
Bossiaea heterophylla, B. scolopendria, Gompholobium latifolium, Dillwynia erici-
folia, Hardenbergia monophylla, Trachymene linearis, Xanthosia pilosa, Leucopogon
ericoides, L. virgatus, Epacris pulchella, Styphelia viridis. Pteridium aquilinum,
occasional plants of Macrozamia and various Cyperaceous species occur, but grasses
are scarce or absent.
286 VEGETATION OF THE MYALL LAKES,
A variant of this type of forest is to be found under conditions that are
presumably less favourable. In it the height-growth of the trees is only about
8 m. and the canopy is more open. The conditions of the reconnaissance did not
permit the taking of many soil samples. Superficially, the soils were similar;
stable sands with some humus development in the upper layers. Here Hucalyptus
pilularis is less abundant to absent. #H. gummifera is more abundant and
E. micrantha is present in sufficient quantities for its white trunk and limbs to
give character to the forest. These last two species are characteristic of tree-
scrub and low scrub-forest on the Hawkesbury Sandstone near Sydney, and are
the hardiest Eucalyptus species in that area.
Apart from a change of the dominants, the vegetation appears to be essentially
similar. Trees of Angophora lanceolata and Banksia serrata are present and
Pteridium is an important constituent of the undergrowth. In one instance, this
forest community was traversed by a water-course. These, of course, are noticeably
absent on the deep sandy soils. The water-course, which was scarcely lower than
the surrounding area, was marked by a pure stand of Melaleuca linariifolia trees
3-4 m. high with twisted trunks and canopy tops. The soil beneath, which was
superficially sandy, had much Selaginella wliginosa.
Where the deep sands abut on hills of tuff rock, an ecotone forest develops.
This will be considered in connection with the vegetation of the hills. The water-
relations of such boundaries are presumably better than either the sands—where
the water-table must lie at some depth—or the hills themselves, which have a
shallow soil. On the other hand, the Hucalypt forests mentioned above appear
to be unfavourably influenced by a permanently high water-table. They do not
extend into the various swamps and heaths to be described below.
THE HyYDROSERE.
The communities to be considered here are of interest because a very full
series is available for study, extending from open water to a swamp forest of
Eucalyptus robusta. With silt deposition, the series can be traced to a high
eucalypt forest, though only vestiges of this remain.
The open water of the lake is fringed by a reed swamp, except where white
sand reaches the water’s edge, or where the shore is stony owing to tuff hills
rising directly from the lake. The water of the lake is brackish and has a pH
of 7-7-5 but all swamp soils tested are acid.
Submerged Phase.
So far as could be ascertained, the bottom of Booloombayt and Broadwater
Lakes is covered with submerged vegetation. The most abundant species is Najas
marina, which has been found to a depth of 10 feet. This extends towards the
shore to depths of about 2 feet. With it is associated Potamogeton tricarinatus,
Vallisneria spiralis, Myriophyllum sp., Ruppia maritima. Both Potamogeton and
Myriophyllum are very abundant locally at shallower depths, but we have had no
opportunity of considering the factors which influence their relative distribution.
In places outside the recognized channels, progress, even in a rowing-boat, is
difficult. On sandy bottoms in shallow water Chara sp. may be found growing
in water 1 foot, or less, in depth, to the complete exclusion of other species. This
has been observed on sandbanks at a hundred yards or more from the shore, as
well as near to the shore line.
‘Field determination made by B.D.H. Universal Indicator. The other pH deter-
minations were made with a quinhydrone electrode in Sydney. We are indebted to
N. GC. W. Beadle for these and other analyses of the swamp soils, made after his visit in
June, 1935.
BY T. G. B. OSBORN AND R. N. ROBERTSON. 287
Succession with Silt Accumulation.
Amphibious Phase.
The reeds extend from a depth of 4-5 feet—where they are scattered—to the
water’s edge. The width of this zone is variable, but it is widest where there
are long stretches of shallow water. The pioneer plant is Scirpus lacustris, which
establishes itself on the lake bottom, spreading out from the shore, in places for
as much as 25 yards. Nearer inshore, in 1-2 feet of: water, there is usually a
continuous densely-growing zone. On its landward side Scirpus becomes mingled
with Phragmites communis, which gradually assumes dominance. In the
Booloombayt Lake the reed swamp may be 10 feet in width, and it is still wider
in the lower part of Broadwater. Other plants in the amphibious phase are Typha
angustifolia, which often forms characteristic socies in the shallower water;
Cladium articulatum, C. Mariscus and Juncus maritimus. Triglochin procera
occurs in open patches of water in the shelter of the reed swamp, and Gratiola
pedunculata may form extensive submerged colonies as well as being present in
the emerged flora near the margin. It is in the Phragmites zone that both
Casuarina glauca and Melaleuca Leucadendron first make their appearance. These
are invariably small trees (up to 5 m.) generally with a leaning trunk and abundant
branches. They differ markedly in habit from the upright and taller trees which
form the next two zones in the Swamp Forest.
Swamp Forest Phase.
From the edge of the reed swamp to the junction with the stable sand or silt
flats there extends a characteristic swamp forest with a dense undergrowth of
sedges. This can be divided into two consocies in which Casuarina glauca and
Melaleuca Leucadendron are respectively dominant. The former lies nearer to the
lake.
Casuarina glauca Fringing Forest.
A closed forest of Casuarina glauca immediately succeeds the reed swamp.
The trees, unlike those near the water’s edge, grow erect to a height of about 15 m.
The ground beneath is covered with the litter of their fallen branches, and a dense
undergrowth of tussocks of Cladium junceum, the wiry stems of which stand about
40-50 cm. high. The water-table in this forest is high. Occasional openings in the
ground-cover support colonies of Cladium articulatum, with which Cotula reptans
and (©. coronopifolia occur. Other plants are Schoenus brevifolius and Lepyrodia
mucronata, the latter locally abundant. Many of the trees have a considerable
growth of the epiphytic Dendrobium teretifolium, but the epiphytic fern Platy-
cerium alcicorne, which is a feature of similar forests to the south of Sydney, was
not observed. The soil here consists largely of decomposing plant remains. The
loss on ignition is high, 68-69%; the pH is 5:3 to 5-6.
Melaleuca Leucadendron Forest.
This characteristic forest succeeds that dominated by Casuarina glauca, on the
inland side, and may occupy a much wider zone. Occasional trees, scattered in
the Casuarina zone, link the Melaleuca forest with the low-growing trees at the
water’s edge. An important factor seems to be a decrease in the humus content,
with a corresponding relative increase in the mineral matter. Melaleuca
Leucadendron can maintain itself on silt flats which have been cleared for poor
grazing land. There it regenerates freely from seed and the seedlings have to be
cut every two or three years to prevent the land reverting to forest. The under-
growth beneath the Melaleucas is very similar to that beneath Casuarina glauca;
Cladium junceum is the chief ground cover. The Melaleuca trees in this forest,
288 VEGETATION OF THE MYALL LAKES,
unlike those of the lake margin, are stout and upright. About 15 metres is an
average height, but trees of 20 m. and more are not unusual, with a diameter of
more than a metre at breast height. With their papery white bark, showing black
streaks caused by fires, and olive green-brown foliage, they are striking and
handsome trees. Occasional trees of Endiandra Sieberi occur, but otherwise, except
for some Casuarina glauca or Eucalyptus robusta at the margins, the Melaleuca
forests are a very pure community.
Eucalyptus robusta Forest.
On the landward side, where the Melaleuca forest approaches the stable sand
or tuff rocks, there is developed a forest of Hucalyptus robusta, the swamp
mahogany. Well-grown trees may be more than 20 m. high, with a rough fibrous
reddish bark and—for a eucalypt—broad, glossy green leaves. The soil here is
often very wet, with pools of standing water due to seepage and run-off from
the inland parts. Here, too, the soil commonly has a considerable admixture of
sand, washed down or blown on to the area from behind. The acidity may be
high—pH 4. The undergrowth is typically Blechnum serrulatum, either as a
carpet or rising in clumps from pools of standing water. Large tussocks of
Gahnia psittacorum occur with the Blechnum. The junction between the Hucalyptus
robusta—Blechnum swamp and stable sand is often marked by a pure ribbon-
community of Restio tetraphyllus. Many variants of this forest exist, but it
appears to be a very stable community, progression beyond which depends rather
on allogenic than on autogenic causes.
Where there is any considerable admixture of sand—e.g. where a stable dune
abuts on a Hucalyptus robusta forest—the trees can survive for a time, though
the undergrowth changes. Pteridium and Imperata replace the Blechnum. It is
probable that the Eucalypt is rooted in swamp conditions, only the upper layer
of the soil being changed. EHucalyptus robusta does not occur on deep stable
sand, though it may be found at the margins of small swamps which occasionally
occur as outliers in the stable dunes. Stunted trees also occur on some of the wet
sand heaths described below.
Eucalyptus Forest on Silt Flats.
Behind the swamp forest zones on either side of the Booloombayt Creek and
the Upper Myall River are extensive silt flats caused by the flooding of these
rivers and wash from the neighbouring hills. These flats have been largely
cleared of timber or the standing trees ring-barked and burnt. Occasional trees
of Eucalyptus saligna var. pallidivalvis (E£. grandis) are left as indicators of what
must have been a magnificent forest. Some of the standing trees here are 36-40 m.
high, rising 18 m. to the first branch. The sward now consists largely of Paspalum
distichum; occasional patches of Cladium junceum or pools with Ranunculus
aquatilis indicate the wetness of the soil.
Swamp Forest with Palms.
In the vicinity of Mungo there is an extensive area in which the palm,
Livistona australis, grows abundantly and regenerates freely in a mixed swamp
forest of both Melaleuca Leucadendron and Hucalyptus robusta. The soil
conditions are a very confused mixture of silt banks, humus masses and standing
water. The palm has a similar occurrence in patches of swamp forest along
the Hawkesbury Estuary nearer Sydney. It is an important constituent of the
subtropical rain-forest on the tuff hill at Mungo, described below.
BY T. G. B. OSBORN AND R. N. ROBERTSON. 289
Succession on Sandy Shores.
The sandy shores at the northern end of Broadwater show lines of Melaleuca
Leucadendron growing as regularly as if they had been planted. Apparently these
result from abundant germination of Melaleuca seeds from time to time in the
flotsam and jetsam cast up on the sand (PI. vii, fig. 9). Most of these crops
of seedlings fail to establish themselves, but, occasionally, they have survived.
When this happens and the sand builds up towards the lake, there is left a
regular row of young trees parallel with the shore. Except for these trees, the
sandy shore bears only occasional clumps of Juncus maritimus or Leptocarpus
tenax.
Rocky Shores.
Plants of the reed-swamp communities usually fail to establish themselves on
shores where the tuff hills come directly to the waterside. Scirpus lacustris may
be found in the water, but the succession does not advance. On the shore itself
there is an open community of Casuarina glauca, behind which the land rises
with the forest vegetation of the hills, or its modifications.
HEATHS AND SWAMPS.
The foregoing account of the psammosere and hydrosere has only incidentally
mentioned the heaths and swamps which are such a feature of the Myall Lakes
area. These are not directly connected with either of the two major seres, though
in some cases they may represent deflections of the successions.
The origin of the extensive level sandy plains, locally called ‘moors’, but which
we have termed heaths, is difficult to explain, except as the sandy bottoms of
former lake beds. Any method of gradual reclamation by vegetation does not
meet the facts, for the heaths are.sandy plains: their surface soil has no peat
and but little organic matter. An extensive heath, four or five miles long and as
much as half a mile wide, lies between the coastal dunes and the tuff hills
south-east of Booloombayt and Myall Lakes.
A soil profile in this is as follows:
Water-holding
Depth. Description. Loss on Ignition. capacity. pH.
0-3 inches .. Sand, discoloured dark brown to black 9-1% we &¢/eh 4-4
with organic matter.
3 15) Ss Yellow sandy loam. 4-05 to 3-53% 33:3 to 25:0 4-0 to 4:2
15 oD Clean white sand saturated with 0:13% 20°5 4-4
water at 16-17 inches.
The heath vegetation consists of a considerable number of shrubs and herbs.
Our lists, inevitably incomplete, include more than sixty species. Most of the
shrubs are leptophylls or nanophylls and few of them exceed 60 cm. in height.
There is also considerable local variation. That portion of the heath shown in
Plate vii, Figure 10, shows numerous scattered bushes of Banksia latifolia. With
it occur such plants as Conospermum tazifolium, Dillwynia ericifolia, Aotus
villosa, Melaleuca nodosa, Epacris obtusifolia, E. microphylla, Sprengelia incarnata
and various Cyperaceae and Restionaceae.
290 VEGETATION OF THE MYALL LAKES,
Dry Heath.
In contrast, other heaths are still drier, the surface soil is lighter in colour
and the vegetation resembles that of scrub on the inter-dune flats, but, as is
usual on the heaths, the individuals are all stunted in their growth. Throughout
the heaths as a whole there are to be found pure societies of this or that species
which—for no apparent reason—assumes local dominance. An extensive society
of Hakea pugioniformis was observed growing so thickly as to be almost
impenetrable, although it was less than a metre in height. A fire had burnt out a
part of the community, and the regenerating area was quite different floristically.
After such fires rhizomic plants, such as Hypolaena lateriflora, Leptocarpus tenaz,
Caustis fleruosa, and Schoenus ericetorum have an obvious advantage which they
share with Xanthorrhoea hastilis and X. minor.
Wet Heath.
Certain of the heaths may be classified as wet. This is a mere matter of con-
venience, and all gradations exist between the two ends of the scale. In the wet
heath there is a greater frequency of Cyperaceae and Restionaceae, Xanthorrhoea
minor is more abundant, and Sprengelia incarnata tends to be replaced by
S. Ponceletia. A comparison of the two floras can be made from the list in
Appendix II.
With increasing wetness there is an accumulation of humus which, if the high
permanent water-level be maintained for long, results in the formation of peat.
Eventually, a peat-swamp may be formed.
Peat Swamps.
Just as all gradations may exist between dry and wet heaths, so the distinction
between some wet heaths and swamps with a shallow peat layer is not easily
drawn. In extreme cases there is no difficulty. One swamp was found to have a
depth of more than five feet of dark brown, wet peat. The pH was about 4—field
test with B.D.H. Indicator. Scattered and stunted Hucalyptus robusta occurred
over the area, but they could not be termed dominant. The dominant was
Leptospermum Liversidgei, which grew as a slender bush to 2 m. The ground
cover was largely tussocks of Blechnum serrulatum, Hypolaena lateriflora was very
common, Restio tetraphyllus and Blandfordia sp. were both frequent. A feature
of this swamp was the sheets of Sphagnum between the tussocks of Blechnum.
As the depth of peat decreased, so did the height of the Leptospermum, and
Blechnum almost disappeared. The shrubs Hpacris pulchella and Sprengelia
Ponceletia appeared, with dense masses of Hypolaena fastigiata. Local societies of
Gleichenia dicarpa were almost impenetrable.
There remains to mention one swamp. This was almost surrounded by stable
dunes with typical Eucalyptus pilularis-Angophora woodland. It was a pure
society of Blechnum serrulatum, bounded at the margin by a belt of Restio tetra-
phyllus. The soil here had a loss on ignition of 89-7% and the pH was 3:7.
VEGETATION OF THE TUrr HILLS.
The vegetation of the hills composed of Carboniferous rocks differs markedly
from that of even the most settled dunes and sand flats. The local resident will
aptly refer to the ‘old’ country and the ‘new’. The former is of value for its timber
and as potential grazing-land after the forest has been cleared; the latter is almost
worthless. Extensive masses of tuff rock occur as islands in the lakes, form
occasional promontories by their shores, or rounded hills rising from the
BY T. G. B. OSBORN AND R. N. ROBERTSON. 291
surrounding sandy or swampy soil. In all cases there is a sharp break in the
floristic composition, and often in the actual vegetation type. To the west of
the lakes the ‘old’ rocks form part of the foothills to the coastal plateau. The hills
here are often steeper and more broken, but the forest types, so far as we have
seen, are essentially similar.
Two distinct and unrelated forest types are developed: the one a mixed Hucalyptus
forest; the other sub-tropical rain-forest. This is composed largely of species with
Indo-Malayan affinities, from which eucalypts are absent, except for the one species
—Hucalyptus saligna—present at the margin. The evidence available shows that
sub-tropical rain-forest develops only in sheltered areas where the micro-climate
is favourable and the soil-water relations are good. On one occasion, helped by a
party, a traverse was made along a rain-forest-eucalypt-forest junction. The
result showed clearly that the sub-tropical rain-forest, which grew thickly along
the south- and east-facing slopes of certain steep-sided valleys, hardly rose much
above the valley floor on the north- and west-facing slopes. Moreover, even with a
favourable aspect, it was absent from the ridges, for they are exposed to the
drying northerly and westerly winds. A more difficult problem in the distribution
of the rain-forest is to account for its presence on certain of the rock outcrops
near the lakes, and its absence from others.
The ‘Brush’ at Mungo, though only a few acres in extent, covers the low hill
in a distinctive sub-tropical rain-forest (Appendix III). In a depauperate form
it exists at Chinaman’s Knob and Bombah Point, but it is absent from an outcrop
of tuff rock about a mile north of Mungo and from the hills to the east of
Booloombayt Lake. The rocks are all tuffs of the Burindi Series, of essentially
the same composition. Under eucalypt forest they tend to develop a podsol;
in the Brush the soils are loamy with a considerable amount of humus. Deter-
minations of the water-holding capacities of the eucalypt forest soil averaged
about 40%, that of the rain-forest about 70%.
Eucalyptus Forest.
The forests consist of a number of species growing to about 20 m. with clean,
straight boles. The canopy is generally closed, though the shade cast is light.
The more important species are Hucalyptus maculata, EH. propinqua, H#. punctata,
E. umbra, E. acmenioides, E. microcorys and LE. siderophloia. With these, growing
to a lesser height are scattered Casuarina torulosa, Exocarpus cupressiformis,
Acacia decurrens and Brachychiton populneus. Undergrowth is sparse, but the
following shrubs were noted: Persoonia linearis, Acacia floribunda, A. Maideni,
Dillwynia floribunda, Pomaderris ellipticum and Monotoca elliptica. Much of the
soil is bare or covered with low perennial herbs or grasses and sedges.
The following list serves as an indication of the plants present; grasses,
unfortunately, have not been prominent at the seasons of our visits.
Carex paniculata Lomandra longifolia
Schoenus imberbis L. filiformis
Lepidosperma laterale Dianella caerulea
Imperata cylindrica, var. Koenigii Pomaz umbellata
Andropogon sp. Opercularia varia
Poa caespitosa Helichrysum elatum
At the head waters of small streams or other wet places, there are indications
of an invasion by Indo-Malayan types. Thus, the following were noted in one such
place: Trema aspera, Ficus aspera, Callicoma serratifolia, Melaleuca styphelioides,
Eugenia Smithii, Breynia oblongifolia. These were growing with large tussocks
of Gahnia psittacorum and amongst them Dioscorea transversa was climbing. We
292 VEGETATION OF THE MYALIL LAKES,
regard these plants as rain-forest indicators. Some are mesophyllous forms with
a leaf type quite unlike the microphyllous sclerophylls around them. The
presence of the liane, Dioscorea, is also significant. Lianes are not a feature of
the eucalypt forest, but they are abundant in the sub-tropical rain-forest.
Probably, all these forests have been modified by fire and by felling. Under
such conditions the more exacting ‘Brush’ plants would disappear.
Many of the hills formerly covered by eucalypt forest have been cleared, or had
the timber ring-barked to encourage a growth of grass, but the results can hardly
be satisfactory (Pl. vii, fig. 13). The majority of the tussocks seen in this
figure are Carex paniculata or other sedges. In places Pteridium and Imperata
are abundant. The trees regenerate freely (PI. vii, fig. 15) when they escape from
fires.
Marginal Forest.
Around the bases of the tuff hills where there is a junction of rock and sand,
there is some mingling of eucalypts characteristic of the ‘old’ country with trees of
the deep sands. MBoth types find better water-relations and grow to a great
size. Certain species of eucalypt—e.g. Hucalyptus paniculata and E. resinifera—
seem limited to these areas. We have also noticed EH. punctata, EH. umbra,
E. microcorys of the tuff forests and #H. pilularis and Angophora lanceolata of
the sands. Many of these trees were 30 m. in height, rising with massive trunks
for 12 m. to the first branch. Casuarina torulosa was common at such junctions
and Angophora subvelutina also occurred. The undergrowth consisted of tall-
growing Pteridium with Imperata. Such shrubs as Dillwynia floribunda, Gompho-
lobium latifolium and Dodonaea triquetra were present.
Sub-tropical Rain-Forest.
These forests are strikingly different from the mixed eucalypt forests. They
grow with a close canopy of dark green foliage, the leaves often having a
polished or glossy upper surface which contrasts markedly with the dull, grey
oOlive-green of the eucalypt. Most of the species have mesophyllous or even
macrophyllous foliage which casts a dense shade upon the forest floor. There
is a high percentage of lianes and ferns in the flora. Palm species, though few
in number, are a characteristic element.
Consideration of the list of plants compiled in the different ‘Brushes’ shows
that the forests are by no means of uniform composition. It is obvious that
they can be divided into two groups: (1) those in which Tristania conferta is a
characteristic tree, sometimes dominant; (2) those in which TJvristania is absent.
The first type is represented in the valleys of the hills, the second pe the
‘Brushes’ at lake level at Mungo and Chinaman’s Knob.
Sub-tropical Rain-Forest—with Tristania.
The rain-forests in the hills have probably all been exploited for timber for
many years. At the time of our visit the brush-box trees (Tristania conferta)
were being felled. Relicts, such as strangling figs or tall trees on less accessible
slopes, show that the general height growth of the trees was much greater than
at Mungo. The palm, Archontophoenix Cunninghamiana, formed definite societies
in the valley bottom. Livistona was less prominent than it was nearer the coast.
It is not proposed to describe the forest further here. The most interesting
point brought out by this reconnaissance was the clear evidence that the develop-
ment of rain-forest depends on local micro-climate rather than the underlying
BY T. G. B. OSBORN AND R. N. ROBERTSON. 293
rock. A second point is that, given the appropriate soil and water relations,
rain-forest is increasing its present areas. But the danger of fire is much more
serious to the isolated rain-forest community than it is to the eucalyptus forest.
There is no rapid regeneration of the grown tree from epicormic shoots.
Sub-tropical Rain-Forest at Sea-level.
In Appendix III is a list of species found in the small patch of rain-forest at
Mungo. It is limited to a low rounded hill of tuff which, so far as our comparison
with rock specimens collected elsewhere goes, does not differ significantly from
other tuffs that are not covered with rain-forest. This hill must have been
an island quite recently. It is so marked on some charts; and a belt of Eucalyptus
robusta swamp-forest fringes its southern and eastern sides. This isolation may
have preserved it from fire, and it appears to have been immune from timber-
getters. None of the trees are of any great height—20 to 25 m. The tallest of
them is out-topped by a number of gigantic Livistona australis which project 5 m.
or more above the general level of the trees like huge mops. Of the 78 species
included in the list, 27 are trees, all of which at some place or other rise to the
canopy. No dominant species can be recognized. Inside the forest the light is
subdued. The ground flora is chiefly ferns which grow amongst the cable-like basal
portions of the lianes. This life-form comprises 16% of the species recorded. The
better light-relations at the margins probably account for the greater frequency
of nanophanerophytes which occurs there.
The little patch of rain-forest on Chinaman’s Knob is much more open than
that of Mungo. The list is shorter, and the few species growing there which do not
also occur at Mungo are plants of the rain-forest margin, not of the established
community.
Ophioglossum coriaceum
Pteridium aquilinum
Imperata cylindrica, var.
Koenigiit
Festuca bromoides
Themeda Forskalii
Caustis flexuosa
Lepidosperma laterale
Schoenus ericetorum
S. imberbis
Leptocarpus tenax
Dianella caerulea
Lomandra longifolia
L. filiforme
Xanthorrhoea hastilis
Acianthus exsertus
Caladenia carnea
Glossodia major
Pterostylis sp.
Casuarina suberosa
C. stricta
Banksia serrata
B. integrifolia
B. aemula
Isopogon anemonifolius
Persoonia lanceolata
P. salicina
APPENDIX I.
Plants of the Dune Scrub.
Leptomeria acida
Olax stricta
Drosera auriculata
Boronia ledifolia
B. pinnata
Correa speciosa
Eriostemon lanceolatus
H. Crowet
Zieria laevigata
Tetratheca thymifolia
T. ericifolia
Billardiera scandens
Acacia longifolia
A. suaveolens
Aotus villosa
Bossiaea heterophylla
B. ensata
B. scolopendria
Dillwynia ericifolia
D. floribunda
Indigofera australis
Hardenbergia monophylla
Kennedya rubicunda
Platylobium formosum
Phyllota phylicoides
Ricinocarpus pinifolius
Dodonaea triquetra
Hlaeocarpus cyaneus
Hibbertia fascicularis
H. linearis
Leptospermum flavescens
L. laevigatum
Xanthosia pilosa
Trachymene linearis
Actinotus helianthi
Astroloma pinifolia
Brachyloma daphnoides
Epacris pulchella
H. microphylla
Leucopogon Richei
L. ericoides
L. virgatus
LL. lanceolatus
Styphelia viridis
Monotoca elliptica
Tecoma australis
Asperula oligantha
Opercularia varia
Pomax umbellata
Wahlenbergia gracilis
Dampiera stricta
Cassinia aculeata
294
VEGETATION OF THE MYALL LAKES,
APPENDIx II.
Plants of the Heaths.
Dry. Wet. Dry. Wet.
Selaginella uliginosa xe Acacia longifolia xX
Blechnum serrulatum x A. suaveolens ENG
Gleichenia dicarpa x A, juniperina 3X
Schizaea bifida x Aotus villosa x
Caustis flexuosa AY Dillwunia floribunda X x
Schoenus ericetorum aN D. ericifolia X
Costularia paludosa xX Platylobium formosum NX BN
Restio complanatus Sphaerolobium vimineum x
R. gracilis. . Bossiaea heterophylla xX
R. tetraphyllus aN x Phyllota phylicoides a
Hypolaena lateriflora x Pultenea incurvata xX
H. fastigiata x x Viminaria denudata x
Leptocarpus tenax x x Ricinocarpus pinifolius .. aX
Ayris operculata .. aE Pimelea latifolia xX Dx
Blandfordia sp. xX Callistemon lanceolatus x
Lomandra longifolia x Melaleuca nodosa xX x
Xanthorrhoea hastilis x M. thymifolia : x
X. minor : x Leptospermum flavescens. . Xx
Haemodorum sp. .. xX L. laevigatum x
Casuarina suberosa XS LL. scoparium var. xX
Banksia latifolia .. aXe L, Liversidgeti a x
B. serrata z sis x Trachymene Billardiert .. xX
Conospermum latifolium xX Epacris obtusifolia x xX
C. ericinum 4 He x E. microphylla x x
Isopogon anemonifolius x E. paludosa ee XS
Persoonia lanceolata x Brachyloma daphnoides x
P. salicina x Leucopogon Richei x
Hakea pugioniformis x L. ericoides x
Symphyonema paludosum x L. virgatus x
Leptomeria acida x Styphelia viridis .. xX
Olax stricta x Sprengelia incarnata ax
Drosera spathulata x x S. Ponceletia ae x
Boronia parviflora xX Mitrasacme polymorpha x
Eriostemum Crowei x Villarsia reniformis x
APPENDIX III.
Floristic Composition of the Brush at Mungo.
Chinaman’s Chinaman’s
Mungo. Knob. Mungo. Knob.
Aspidium decompositum x Oplismenus compositus x aX
Woodwardia aspera x xX Cyperus sp. x
Pellaea falcata .. xX Gahnia aspera .. x
Adiantum hispidulum x x Livistona australis x
Pteris tremula x aX Flagellaria indica x
Polypodium confluens x x Commelina cyanea D.<
P. tenellum A x Juncus pauciflorus x
Platycerium bifurcatum x Drymophila cuanocarpa x
Botrychium australe x Rhipogonum sp. ox
Podocarpus elatus x Smilax australis x
Gymnostachys anceps aN Dioscorea transversa x x
BY T. G. B. OSBORN AND R. N. ROBERTSON. 295
APPENDIx IIJ.—Continued.
Floristic Composition of the Brush at Mungo.
Chinaman’s Chinaman’s
Mungo. Knob. Mungo. Knob.
Alpinia caerulea xX Cupaniopsis anacardioides ENG aN
Peperomia leptostachya x Nephelium lciocarpum aN
Trema aspera .. nee x xX Nephelium sp. xe
Laportea photiniphylla X Alphitonia excelsa x xX
Cudrania javanensis xX Vitis clematidea XG x
Ficus sp. x V. antarctica x x
F., rubiginosa ot xX V. nitens x
Sarcopetalum Harveyanum ONS V. hypoglauca .. x
Stephania hernandifolia aN Elaeocarpus cyaneus x
Cocculus Moore x E. obovatus x
Mollinedia macrophulla xX xX Viola hederacea aN aN
Cryptocarya microneura Xx Scolopia Brownit NS
Clematis glycinoides Xx Passiflora edule Xx
Citriobatus multiflorus x P. Herbertiana 3 xX
Pittosporum undulatum xX Eugenia sp. .. Bs xX
P. revolutum xX Rhodomyrtus psidioides x
Acacia implexa DNS ONG Panax sp. x x
A. decurrens var. xX Myrsine variabilis x x
A. floribunda .. ees ah X | Sideroxylon australe x xX
Pultenea flexilis aN Cargillea australis x
Acronychia laevis X Notelaea longifolia X xX
A, Baueri x Lyonsia reticulata aX
Zieria Smithit .. xX Marsdenia rostrata x
Dysoxylum Fraseranum xX Solanum pseudocapsicum x
Breynia oblongifolia xX x S. stelligerum x NS
Croton Verreauxit se xX S. verbascijolium XxX
Omalanthus populifolius Se x Clerodendron tomentosum x
Poranthera microphylla ahs x Myoporum tenuifolium x
Phyllanthus Ferdinandi xX Morinda jasminoides .. Mie Xx
Elaeodendron australe Xx Asperula oligantha .. 23 x
Cupania semiglauca x x Siegesbeckia orientalis. . ae x
EXPLANATION OF PLATES VI-VII.
Plate vi.
1.—Fore dune vegetation of Festuca littoralis and Senecio spathulatus. Near South
Gibber. ‘
2.—Melaleuca Leucadendron swamp forest at margin of lake, looking towards the
water. Dense ground flora of Cladiwm junceum. Shores of Booloombayt Lake.
3.—Low forest of Angophora lanceolata on stable dune near sea; note distorted
limbs. Macrozamia spiralis at foot of trees to left. Undergrowth of Pteridium, Xanthor-
rhoea and Lomandra. Near South Gibber.
4.—Eucalyptus pilularis-E. gummifera forest on deep stable sand. Banksia serrata
in second storey (right foreground) and tall, shrubby undergrowth of Leptospermum
stellatum, Calythrix, ete. About one-fourth mile inland from landing opposite Bombah
Point.
5.—Livistona australis in swamp forest of Hucalyptus robusta, near to Mungo. Note
the palms are flowering and there is active regeneration beyond the figure. South of
Mungo.
6.—Mixed eucalypt forest on tuff hill. Xanthorrhoea arborea in centre, ground cover
of tussock grasses and Cyperaceae. Near ‘Cutler’s’, west of Booloombayt Lake.
7.—Sub-tropical rain-forest in steep-sided valley of tuff hills. A society of Archonto-
phoenix in centre. Sheltered valley to north-east of Booloombayt Creek.
296 VEGETATION OF THE MYALL LAKES.
Plate vii.
8.—Remains of Hucalyptus saligna, v. pallidivalvis on silt flat by Booloombayt Creek.
To the left is a swamp forest of H#. robusta. Near northern extremity of Booloombayt
Lake.
9.—Sandy shore at north end of Broadwater, east of Bombah Point. There is a
dense fringe of young Melaleuca Leucadendron in the middle distance; other small trees
occur between clumps of Juncus maritimus in the foreground. Tall M. Leucadendron
behind.
10.—Heath with scattered Banksia latifolia among leptophyllous shrubs and sedge-
like plants. Behind is a fringe of Melaleuca Leucadendron beyond which rises Eucalyptus
pilularis-Angophora lanceolata forest on a stable dune. About 2 miles south-east of
South Gibber.
11.—Peat Swamp, Leptospermum Liversidgei dominant, with occasional stunted
ELucalyptus robusta. Eucalypt-Angophora forest on stable dunes behind. About 1 mile
east of Bombah Point.
12.—Peaty Swamp with Blechnum serrulatum; to the left and behind are stable
dunes with Hucalyptus pilularis-Angophora lanceolata forest. About 1 mile east of
Bombah Point.
13.—Poor grass-land with tussocks of Carex paniculata on tuff hill, forming part of
the peninsula in Booloombayt Lake.
14.—Mixed eucalypt forest on tuff hill; the trees shown include #. maculata, H. wmbra
and H. microcorys. North-east of Booloombayt Lake.
15.—Natural regeneration of mixed eucalypt forest on tuff hill; poor grazing land
with tussocks of Carex paniculata. Near the northern extremity of Booloombayt lake.
Postscript, 14 July, 1939——There exists some doubt about the correct specific
name of the Melaleuca referred to in this paper as M. Leucadendron. R. T. Baker
(Journ. Roy. Soc. N.S.W., 1918, and Proc. Linn. Soc. N.S.W., 1913), after
comparison of the local plants with the Linnean type specimen, came to the
conclusion that they were so different as to warrant the description of two new
species, M. Smithii and M. Maideni. He questioned whether M. Leucadendron
really occurred in Australia. Nevertheless the Census of N.S.W. Plants (1916)
retains the three specific names—Leucadendron, Smithii and Maideni. In view of
the fact that there exists doubt as to the real specific designation, the name
Leucadendron which is widely used by local botanists for this plant has been
retained in this paper, though it is recognized that revision of the species may
be necessary.
Proc. Linn. Soc. N.S.W., 1939. PLATE VI.
Vegetation of Myall Lakes district.
Proc. Linn. Soc. N.S.W., 1939.
PLATE
VI.
Vegetation of Myall Lakes district,
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297
AUSTRALIAN COLEOPTERA.
NOTES AND NEW SPECIES. NO. xI. [Mostly Elateridae.]
By H. J. Carter, B.A., F.R.H.S.
(Plates viii-ix; one Text-figure.)
[Read 26th July, 1939.]
COLYDIIDAE.
In examining what seemed to be a new species of Byrsax, Mr. Zeck found
that its tarsal formula was 4-4-4. From the similarity of form, the other
members of this genus were then examined, with the result that Byrsazr
saccharatus Pase. and B. egenus Pasc. (= coxi Cart.) are seen to be similarly
furnished. Both of these are thus true Colydiidae, near the New Zealand genus
Tarphiomimus. So close must be this relation that for the present I would call
them (?) Tarphiomimus (Byrsax) egenus Pasc. and (?) Tarphiomimus (Byrsax)
saccharatus Pasc. The remaining members recorded under the genus, B. macleayi
Pase. and B. pinnaticollis Cart., have heteromerous tarsi.
The following is the new species mentioned above.
TARPHIOMIMUS (?) ZIG-ZAG, N. Sp.
Convex, oblong; pale brown above, reddish beneath.
Head wide, trilobate, each lobe subtruncate in front, exterior angles sub-
dentate: near base of outside lobes, in one example, can be seen a small conical
protuberance. Antennae short, stout, the three apical segments strongly clavate.
Prothorax widely, arcuately, foliate; externally fringed with about five wide
crenulations, the foremost almost level with apical lobe of head; posterior third
abruptly excised and narrowed; disk strongly raised, medial area concave,
bounded on each side by a pustulose ridge; the outline somewhat variable in the
three examples, the most cénspicuous features being two subconical pustules
overhanging head and two rounded ones at basal third. Hlytra of same width as
prothorax, and of almost equal width for the greater part; widely (subtruncate)
rounded behind, with wide lateral foliation, fringed by deep; blunt, crenulations;
discal regions with shoulders prominent and widely ridged, with a variable number
of conical pustules along sides; medial area with two strongly-raised ridges,
forming straight lines at base and on apical declivity, the middle parts forming
two wide zig-zags, the intervening area foveate-punctate, with squamose derm;
underside squamose-rugulose. Dim. 3 x 14—4 x 2 mm.
Hab.—N. Queensland: Mulgrave R. (H. Hacker).
One of Mr. Hacker’s many discoveries. The species is near 7. (?) saccharatus
Pase., but, besides being less than half its size, has the following distinctions:
(a) All ridges less spinose-pustulose, (b) Fewer crenulations to pronotal foliation,
(c) Elytral spinose ridges replaced by zig-zag elevations. The only evident sexual
character lies in the frontal tubercles noted in one example. Holotype in the
National Museum.
Y
298 AUSTRALIAN COLEOPTERA,
BUPRESTIDAE.
BUBASTES SUBNIGRICOLLIS, N. Sp.
Conico-cylindric, nitid. Head dark blue, prothorax, underside and legs blue-
black, tarsi coppery, elytra brilliant coppery, its suture narrowly more brightly
metallic, scutellum peacock-blue.
Head very lightly concave, with narrow frontal sulcus, uniformly, closely
punctate; eyes large, not prominent, width of head less than that of prothorax at
apex. Prothorax (3% x 5 mm.) very convex, widest near front, sides lightly arcuate,
apex subtruncate, front angles wide, base lightly bisinuate, hind angles less than
90°; disk closely and finely punctate, slightly flattened on basal half at middle,
with a well impressed medial sulcus, just traceable on apical half. Scutelluwm
small, with longitudinal depression. Hlytra of same width as prothorax at base,
lightly narrowed to apex; apices each finely bidentate, with small lunation between
teeth; striate-punctate, the seriate punctures distinct on basal half and at sides,
elsewhere indistinct; intervals lightly raised and nitid, their interspaces trans-
versely hatched and rugose. Prosternum with large, alveolate punctures,
metasternum and abdomen with finer and more distant punctures. Dim.17 x 5 mm.
Hab.—Western Australia: Wurarga (A. Goerling).
A single example sent by this observant naturalist is remarkable for its nitid
and bicolorous surface. While the general colour scheme somewhat follows that
of B. vagans Blkb., it differs greatly in (1) the colours more strongly contrasted—
nitid blue-black thorax and brilliant coppery elytra, (2) the strong transverse
ridges of the interspaces between the raised intervals of elytra. Holotype presented
to the Australian Museum.
Melobasis impressa Cart.—Further material of this, also of M. abnormis Cart.
sent by Mr. A. Goerling, together with a helpful field note, enables me to correct an
erroneous synonymy (Trans. Roy. Soc. S. Aust., 1937, p. 125). He writes: “I find
these” (impressa and abnormis) “always separate in places about 24 miles apart—
never together, and this is my experience for the last 3 years.” An examination of
four examples of each gives constant differences as follows:
abnormis (1923) impressa (1936)
Average dimensions, 12% x 5 mm. 152 xX 64 mm.
Upper surface subopaque, strongly
pubescent. nitid, almost glabrous.
Pronotum sulcate. often (in 3 of 4 examples) carinate.t
Elytra: costae more, punctures less defined. vice versa.
impressions subobsolete. well defined (as in description).
MELOBASIS BELLULA, N. Sp.
Hlongate-ovate; head coppery with greenish tinge, prothorax variably violet-
bronze (each predominating in different examples); elytra blue, with golden
markings, as follows: a wide basal band, having similarly wide, trilobed, extensions,
namely two lateral, extending half the total length, and a sutural of about half the
length of the lateral, and two triangular, subapical markings. Underside purple,
often bluish in part, legs and antennae blue.
Head glabrous, densely, finely punctate, eyes not protruding laterally beyond
thorax. Prothorax widest at base, thence gently, arcuately narrowed to apex,
lightly produced in front at middle, base lightly bisinuate, all angles rather wide,
the posterior subrectangular; disk with fine, not close, punctures and a smooth
medial line. Scutellum small, subecircular. Hlytra lightly widened at shoulders
and compressed behind them, narrowly and separately rounded at apex, marginal
1 Very unusual in the genus.
BY H. J. CARTER. 299
serrulation evident to apical third. Disk with well-marked subsutural concavity,
and a few punctate striae near this, otherwise seriate punctures confused with close
general punctures, these dense near base. Underside glabrous, sternal area with
round, abdomen with finer, shallow, oval punctures, rather widely spaced; apical
segment of g truncate between two spines, of 9 with oval excision between spines.
Dim. 6-7 X 2 mm.
Hab.—Western Australia: Wurarga (A. Goerling).
A lovely little species, of which 14 examples were received from the keen
naturalist squatter in a prolific Buprestid region, showing little variation in size
and markings. Holotype presented to the Australian Museum.
MELOBASIS SPINOSA, N. SD.
Narrowly ovate; very nitid greenish coppery-bronze, head green, pronotum
with green and coppery sheen; elytra greenish-bronze, purplish near apex; sternal
regions, legs and antennae green, abdomen coppery.
Head rather fiat, densely and finely punctate, width at eyes wider than that of
prothorax at apex. Prothorax: apex and base bisinuate, all angles subacute, sides
lightly narrowed in a feeble arch from base to apex, disk finely punctate, punctures
sparse and distant on basal half, closer (but clearly separate) at sides and apex;
medial fovea at base, no medial line. Scwtellwm small, subcircular. EHlytra of same
width as prothorax at base; basal half subcylindric, thence finely tapering to a
spinose apex, each elytron terminated by a triangular tooth, the margin between
tooth and suture with two small spicules; subapical margins strongly serrate; disk
finely seriate-punctate, intervals flat and impunctate. Prosternum densely punctate,
rest of underside more sparsely so; apical segment of abdomen strongly bispinose.
Dim. 8 x 3 mm.
Hab.—Queensland: S. Johnstone River (H. W. Brown).
Two examples, both, I think, male, given me by Mr. Brown some time back,
are unlike anything in the genus in the apical structure. Under the Zeiss binocular,
each apex appears trispinose. The elytral seriate punctures are regular and clear,
almost (but not) striate-punctate. Holotype presented to the Australian Museum.
MELOBASIS VIRIDISTERNA, Nl. SD.
6. Hlongate-ovate; nitid bronze and glabrous above (save for a fine frontal
pubescence); prosternum, tibiae, tarsi, antennae and parts of head metallic green,
rest of underside coppery and glabrous.
Head densely, very minutely punctate, width less than that of prothorax at
apex. Prothorax: apex bisinuate, anterior angles acute; base subtruncate, posterior
angles obtuse, sides nearly straight, lightly narrowed from base to apex; disk finely
transversely strigose, only at sides very densely and minutely punctate, without
medial line or fovea. Hlytra slightly wider than prothorax at base, feebly widening
behind middle, thence tapering to apex; subapical margins strongly serrate, the
serration continuous to extreme tip; very finely seriate-punctate, the intervals
almost flat, with subuniform punctures, especially on apical half, and some trans-
verse strigae. Prosternum forming a rectangular plate, with small triangular
process fitting into mesosternum; densely punctate, rest of underside irregularly
punctate, abdomen strongly bispinose at apex.
9°. Green colour apparently limited to antennae, tibiae and tarsi. Dim.
W112) <4 mom.
Hab.—N.S.W.: Cooma (W. Duboulay), 4 examples. Victoria: Kiata, 2 examples.
A species with an unusually fine surface sculpture, the pronotal consisting
chiefly of fine strigae, the elytral suggestive of uwniformis Cart. which, however, is
300 AUSTRALIAN COLEOPTERA,
more convex, with a strongly pilose underside. WM. viridiceps has a much more
strongly punctate pronotum. The flat prosternal plate is a well marked character.
Holotype presented to the Australian Museum.
Since the publication of my Revision of the Australian species of the genus
Melobasis? I have added 14 names for new species, tabulated below. Of these 9
appear to be peculiar to Western Australia, three to Queensland and two to New
South Wales. Thus Western Australia records 39 out of a total of 81 species,
nearly 50% of the Australian species. The genus also occurs in New Guinea,
New Caledonia, Fiji, Sumatra, Java, Timor, Borneo and Penang. In Australia it
frequents various Leguminous plants, especially the numerous and widely
distributed Acacias, while individual species are associated with Cassias, Daviesia.
Dillwynia and Viminaria.
Table of Australian Melobasis described since 1923.
is blytra swith? prominent: KCOSTASMEA eons «hte ee lets in hes Re ee Gets eee area 2
Elytras without “prominent weostaes beat ce: cpm syale. fous - lel euemedsta es chaieie cleieas eects chedere aie 4
2 ULYICGAg INT COLO OMS! gryctetuoh wesc ere mc deke} sized sa AO) eucien cos suens sa cpepeuanens Wassewhs cys Gieicye impressa Cart.
Phytera aere nig wasup accents vewewerses ats co collar Varnes gs eliecal Brera cee MSU e IO SULoNeNe MRC Mase otal ALOR eee Lay Oree Seen OMe: 3
3. Elytra purplish, lateral vittae and sutural mark golden .......... aurocincta Cart.
Elytra with defined areas of light and dark bronze ................... brown Cart.
4 MA y train colorous RONZed Rete yey ie ei Sate tee Cre eee eee een bie 5
Mlytrasmetallicreoppenyen Geen wOL DUG em cick ices eieieeieLeieieie eo cicienicisiene iene aeieioe 6
Bvtr an papatcenned! spose ike keke cacsouais vous Sisneeiga Gusveeya cet cin stents act bap opie eus jauciesheke.oanancieiswemeus 11
5. Pronotum punctate, underside bronze. (Sculpture finer than in igniceps Saund.)
CRRA hte ici CaCI CAIRO SR aA ER aR ICRA isch ok ini eae ea tesa marlooensis Cart.
SEO OCD OES ON A, CLOTS CUNO OOO ROT CREE OT TING CoOTO DIGECT OREN oO roe viridisterna Cart.
Gey Elyithal ApiGeS) SPIMOSC we cesnereye ce ckes cic dene. ny.s 0 siic evfes elahie sirens eyes iter elle felsic caster cei tes spinosa Cart.
IBD Nah eH Hopvexetsti=) LORD OOT EL) § Ryiocoto loathe oss mene oteecene Uicno cto oO broke omola Gita collet GialdeGasiomo a GoS 7
Tie ULYtTA se SUMIATC=DUNCTATC™ racine iter eer cis iciet otter ema eee eee cee renee wannerua Cart.
IDVRAE), bes bAhie FophVOUEHKS Sods onisodaceonedtadgcdenosooasouooRes S644 5001006500 8
Se WipperssuTtacesblue yw welytrasnicate-pumCtale mm acrs creceiloei-eateicl teks kine dolencets pavo Cart.
Wiese GUIOTAVCS OUINGIAWISS sooacssossoccdat nomen nsaoox ss dca HOdOD0 DD UNO ONOO DNDN 9
DN Wippersand lowerssuctacereneenmn (6=1/ sli] O12 s)) meni arene rere enema pusilla Cart.
EXLVitGa, VIOLACCOUS OL DUIDLE: eile ece ota Aictes serene Te Meese eRe anu ee een ot eee 10
10. Pronotum and underside blue-bronze (12 mm. long) ................ myallae Cart.
Rronotumuandsundersidessreens (On mims lone) eee eens cence parvula Cart.
11. Elytra striate-punctate (blue with gold vittae) .................. aurocyanea Cart.
IDNA, TOE, Ore CERO, Sica UO. Goce ocooguchacooponaucododuodoouUcOaES 12
Toeily tras ereeni with Olden! sviltlaley ar che ov: .eteren on eval serena Ee CR IERIE Ree radiola Cart.
Elytra blue, with trilobed basal and preapical mark gold .............. bellula Cart.
STIGMODERA (CASTIARINA) PUTEOLATA, 0. Sp.
Ovate, subconic. Head, prothorax, underside and appendages nitid bronze, the
last brassy, elytra dull brick-red with black markings as follows: an irregular
medial fascia, widened at suture, extending obliquely to sides, this connected along
suture with a wide, sagittate, preapical mark (in two examples narrowly produced
to extreme apex) and three small spots—the middle one behind the others—half-
way between the fascia and base.
Head widely excavate-canaliculate, with brassy reflections. Prothorax convex,
apex subtruncate, base bisinuate, sides nearly straight on basal two-thirds, thence
narrowed to apex, base without excisions; disk with exceptionally coarse punctures,
widely separated on basal half, closer and finer near front, rather strongly
pubescent on sides; medial channel wide and deeply impressed throughout. Hlytra
convex, subconical to apex, sides entire throughout, apices rounded; striate-
2 Trans. Ent. Soc. Lond., 1923, pp. 64-104, with two plates.
BY H. J. CARTER. 301
punctate, the strial punctures large, crenulating sides of intervals, these sharply
convex—the 2nd, 3rd and 5th more strongly so on apical half, each interval with
a line of well marked punctures. Underside glabrous, almost impunctate, very
nitid. Dim. 10-5-12 x 3-5-4-5 mm.
Hab.—Western Australia: Lake Ningham (H. W. Brown).
Three examples examined, two given me by this enthusiastic collector, show a
species somewhat like S. convexa Cart. in colour and in the entire margins and
rounded apex of elytra. It differs strongly in its subcylindric, coarsely punctate
prothorax and the more sharply convex elytral intervals and more conical form.
Holotype in the Australian Museum.
Stigmodera brevifasciata Cart. = bifasciata Saund.—Mr. F. E. Wilson has
called my attention to the tarsal claws of this species, which are characteristically
those of Themognatha. I find the same in its close ally, S. secularis Thoms. Both
species should thus be removed from the subgenus Castiarina to that of
Themognatha.
HLATERIDAE.
This family has received somewhat piecemeal attention from Australian
authors, Elston alone venturing to deal seriously with the larger groups. The chief
difficulties attending its study are (1) the absence from Australia of well-named
collections, (2) the sketchy descriptions of many of our species by Candéze the
great specialist in the family, and (3) the slight and elusive characters that
separate species and, sometimes, genera. The purchase of the Hlston collection
by the Australian Museum, with the helpful and industrious work of this author
in putting together and translating the descriptions of our species, was the induce-
ment to the undertaking of the present paper. The large amount of new material
available here indicates the need for further revisional work in this family. My
thanks are due to Mr. K. C. McKeown of the Australian Museum, Mr. Womersley
of the Adelaide Museum, Mr. HE. W. Salter of the Macleay Museum, Mr. Clark of
the Melbourne Museum, Mr. H. Hacker of the Queensland Museum, Mr. Campbell
of the Canberra Museum, as also to Messrs. F. EH. Wilson, J. EH. Dixon and J. C.
Goudie for the loan or gift of material. I would here wish to express my apprecia-
tion of the generosity of Mr. H. W. Brown and of Mr. Gurney, of the Department
of Agriculture, for their presentation of holotypes to the Australian Museum.
LACON BULLATUS, N. Sp.
Wide, oblong; opaque reddish-brown, with short pubescence, antennae and legs
red. r
Head concave, punctate, widened to the front, here rounded on each side;
antennae short. Prothorax subquadrate, length and breadth subequal, convex,
scarcely gibbous; apex emarginate, front angles wide; sides nearly straight for
the greater part, rather abruptly narrowed in front, sinuately widened at the
posterior angles, lateral border coarsely crenulate, irregularly bicarinate, the
exterior carina sometimes reduced to a row of nodules, the two carinae forming
the lateral outline of the truncate, divaricate hind angles; disk coarsely alveolate-
punctate; an ill-defined medial depression, and, in two examples (of four),
bi-impressed. Scutellwm transversely oval. EHlytra as wide as prothorax at base,
and less than twice as long (9:5); lightly convex, very lightly enlarged behind
middle; sutural region, in two examples, depressed; striate-punctate, the striae
wide and deep, seriate punctures large and close; intervals flat, except near base,
1st with a single row of punctures, 2nd and 8rd with a double row of punctures
302 AUSTRALIAN COLEOPTERA,
and transverse ridges, those exterior to 3rd studded with rows of rounded nodules.
Underside finely punctate; prosternum with a transverse ridge, tarsal sulci absent.
Dim, 17-20 x 7-8 mm.
Hab.—Western Australia: Lake Austin (H. W. Brown).
Four examples taken by Mr. Brown, who has generously given the type to
the Australian Museum. It is characterized by its unusual size and width and the
coarsely nodulose exterior elytral intervals. Holotype in the Australian Museum.
MyYRMODES (?) ELONGATUS, 0. Sp.
Elongate; subparallél; above, beneath and appendages brownish-red, sparsely
pilose.
Head quadrate, somewhat rounded in front, briefly narrowed at hind angles,
coarsely setose-punctate; antennae short, segment 1 very large, twice as long as
wide, 2-3 short and oval, 4-8 bluntly dentate, 9-10 oval, 11 elongate-oval, narrower
than 10. Prothorax convex, as wide as long (44 mm.), widest at apical third, apex
arcuate, front angles defined but wide, base subarcuate, sides entire, widely sinuate
behind, posterior angles acute, obliquely pointing outwards, without carinae, the
discal sculpture continuous to margins, without lateral sulcus; rather coarsely
punctate in middle, more finely at sides and base. Scutellum large, oval. Elytra
closely adapted to, but wider than, prothorax, shoulders obliquely truncate, sides
subparallel; striate-punctate, with large square punctures in deep, clear-cut striae;
intervals flat, closely punctate towards base, elsewhere with transverse, sometimes
undulate, rugae, with recumbent pile near sides and apex. Prosternum coarsely
and closely punctate, without sign of tarsal sulci; the rest of underside densely
covered with small punctures: tarsi rather slender, clothed beneath with tufts of
hair, post tarsi nearly as long as tibiae; segment 1 as long as 2-3 together, 2, 3, 4
successively shorter. Dim. 13-15 x 44 mm.
Hab.—Queensland: Clermont (Peak Downs) (Dr. K. K. Spence).
Three examples given me by their captor can only be referred to Trieres or
Myrmodes, to the former of which it is similar, so far as may be judged by the
figure in the Genera Insectorum, but the narrow tarsi forbid its inclusion here.
While differing from the monotypic M. akidiformis Cand. in its elongate elytra,
it may provisionally be placed here. Holotype in the Australian Museum.
GLYPHEUS CRUCIGER, 0. Sp.
Elongate, oblong. Head, metasternum, abdomen, and elytral markings black,
clypeus, prothorax (above and beneath), legs and ground colour of elytra orange-
red; elytra bearing a postmedial cross, with diamond-shaped widening at suture,
the seriate punctures and the apex, also antennae, black.
Head with usual concave clypeus and narrow border; antennae -sublinear,
extending slightly beyond base of prothorax; basal segments yellow. Prothorax
subquadrate, apex arcuate, the acute anterior angles embracing the head to the
eyes; sides feebly, arcuately, widening from the apex, sinuate before the long,
divaricate hind angles; these with a strong, central carina. Disk very nitid,
almost impunctate; a few white hairs at side. Hlytra as wide as prothorax across
the hind angles and more than twice as long; striate-punctate, the round strial
punctures emphasized by dark colour; intervals convex and impunctate. Dim.
7-8 x 2:2 mm.
Hab.—New South Wales: Dorrigo (W. Heron).
Three examples, alike in colour, differ slightly in size. One example sent to
Mons. E. Fleutiaux, others given, some time back, to Mr. A. M. Lea. It differs
BY H. J. CARTER. 303
clearly in pattern from recorded species while approaching G. alpinus Blkb. in size.
Holotype presented to the Australian Museum.
GLYPHEUS MILITARIS, Nl. SD.
Elongate, oblong. Head, underside (except prosternum), antennae and legs
(including tarsi) black; prothorax above and below sanguineous, with apical
border and hind angles black; elytra black with the following markings
sanguineous: an arcuate patch at each side on basal third, covering 3rd and 4th
intervals, widened and produced to sides, this narrowly connected with wide
preapical fascia, interrupted at the suture. Whole upper surface with long, upright,
black hairs. Underside glabrous, sparsely and minutely punctate.
Head less rounded in front than usual, with well-raised border and excavate
within; antennae short, segment 8 slightly longer than the rest, 4-10 subequal.
Prothoraz feebly widened behind middle, scarcely sinuate anteriorly, front angles
rounded off, sides more strongly sinuate before the long, acute, strongly divaricate
and carinate hind angles; disk with fine, sparse setae and long, upright hairs at
sides; a fine medial sulcus traceable for the greater part, except near apex. Hlytra
about as wide as prothorax, sides nearly straight, lightly rounded at apex; striate-
punctate, the seriate punctures large, black, intervals nearly flat except at base,
impunctate save for setae towards margins bearing long upright hairs. Dim.
12 x 5 (4+) mm.
Hab.—New South Wales: Lithgow district (H. HE. F. Bracey).
A unique example is a striking species of a similar colour to G. sanguineus
Hlst., but differs in its red pronotum with black hind angles, different elytral
pattern, narrower form and finer sculpture, especially of underside. In some
respects it must be near G. decoratus Cand., a species with black prothorax and
different elytral pattern. Holotype in the Australian Museum (K.58776).
A second example in the S. Australian Museum, taken by the late A. M. Lea,
at Wilmot, Tasmania, is probably the other sex. It is smaller (10 x 3 mm.) with
the lateral red patch smaller and disconnected from the preapical fascia, but is
otherwise like the Lithgow insect. There are many instances of this faunal
distribution (Tasmania and alpine New South Wales).
PSEUDAEOLUS*® BIMACULATUS, N. SD.
Opaque black above and beneath, including appendages; hind angles of
prothorax, tarsi, two ill-defined plagia on apical third of elytra, and the apical
regions, vaguely, red.
Head rounded in front, strongly pubescent; antennae, with segment 1 long
and curved, 2 and 3 small, equal, 4 longer than 5, 5-10 equal, subtriangular, 11
lineate oval. Prothorax sparsely pubescent, subcylindric, lightly narrowed in front
and subsinuate behind, hind angles directed slightly outward, bicarinate. EHlytra
of same width as prothorax, apices diverging, each truncate; striate-punctate, the
striae fine and clearly cut, the punctures scarcely discernible, intervals flat and
silky, pubescent at sides and apex. Dim. 7-8 x 2 (+) mm.
Hab.—New South Wales: Rockley (H. J. Carter); Queensland: Cairns (H. W.
Brown).
Four examples, two from each locality, differ from Ae. australis Cand. and
Ae. waggae Cand. in the non-fasciate elytra. If considered only as a variety of
P. australis Cand. it deserves a name. Holotype in the Australian Museum.
2Candéze considered that the Australian species of Aeolus should be placed under
a separate subgenus Pseudaeolus (Cat. Blat., 1891, p. 77).
304 AUSTRALIAN COLEOPTERA,
N.B.—Ae. waggae Cand. is stated to differ from Ae. australis Cand. in having
the hind angles unicarinate. Examples from the Bogan River correspond with
description, and are smaller, paler and more pubescent than examples determined
as Ae. australis (4 examples from Mundaring, W.A. (Carter), 4 from Cue, W.A.
(H. W. Brown) ); Candéze’s locality is Sydney. The species seem to have a wide
distribution.
PSEUDAEOLUS ZIG-ZAG, N. Sp.
Opaque, castaneous, mottled with black; head black, pronotum with medial
and apical regions black; elytra castaneous with ill defined postscutellary mark,
a zig-zag fascia at apical third and the apex black; underside subfuscous red,
abdomen darker; antennae, palpi and legs testaceous. A short, pale, pubescence,
thickest on the elytra.
Head: clypeus rounded, frontal sculpture obscured by pubescence, antennae,
segment 1 stout, 2 shorter than 3, 3 than 4, 4 longer than 5, 8-11 wanting.
Prothorax longer than wide, laterally convex, sides very lightly converging to the
front, feebly sinuate behind, hind angles scarcely divergent, unicarinate, disk
without medial sulcus. Scutellum elongate-ovate. Hlytra elongate-ovate, as wide
as prothorax and nearly twice as long; striate-punctate, the striae fine, and, except
near base and sides, obscured by the dense pubescence, as also the dark markings,
intervals flat. Dim. 7 x 2 mm.
Hab.—N. Queensland: Cairns.
A single example in the Elston Collection is clearly distinct from recorded
species. Holotype in the Australian Museum. I find a second example amongst
some unlabelled Elateridae—probably from Queensland.
PSEUDAEOLUS VAGEFASCIATUS, 0. SDP.
Elongate, parallel; upper surface varicoloured, with varied amount of red, sub-
opaque, with short, pale pubescence; in general head and prothorax dark brown,
the hind angles and basal area of the latter red, the elytra chiefly dark, with ill-
defined postmedial fascia and the apex red. Underside castaneous, legs and
antennae yellow.
Head minutely, densely punctate; clypeus rounded, antennae extending well
beyond the prothorax in g, scarcely beyond the base of prothorax in the Q,
segment 1 curved, 2 and 3 short, 3 longer than 2, 4-7 subconic, 8-11 successively
narrowed, 4-10 subequal in length, 11 lineate. Prothorax longer than wide
(4 x 3 mm.), lightly convex; apex arcuate, front angles rounded off, sides nearly
straight, hind angles well developed, lightly divaricate, with a long carina parallel
to and near the external border. Hlytra of same width as prothorax and twice as
long; sides parallel for the greater part; finely striate-punctate, the punctures more
evident in external half of elytra, intervals flat, finely transversely striolate, apices
subtrunecate. Underside densely, minutely punctate. Dim. 10-12 x 3 mm.
Hab.—New South Wales: Comboyne (H. J. Carter); Kurrajong and Epping
(Dr. K. K. Spence); N.S.W. (H. W. Brown).
One ¢, 3 2 before me, the ¢ with longer antennae and the red colour more
extended over the upper surface. It is the largest species of the genus recorded.
Holotype presented to the Australian Museum.
An examination of the types in the Macleay Museum shows the following
synonymy:
Melanoxanthus (Cardiophorus) froggatti Macl. 6 = M. (Cardiophorus)
fasciolatus Macl. ?.—I think these are the sexes of the same species. I have noted
this sexual colour difference in other species.
BY H. J. CARTER. 305
Elatichrosis (Chrosis) angusticollis Blkb. = EH. trisulcata Er.—Blackburn’s
description exactly fits Victorian examples that cannot be separated from Erichson’s
species.
MELANOXANTHUS.
This genus appears to be common in tropical Australia, though undetermined
in our collections. In form subconic or navicular, elytra short in proportion to
the prothorax, the hind angles of the latter strongly developed, divaricate and
carinate, the sculpture often coarse, the antennae serrate, sometimes widely so,
often ornately coloured, they are strikingly different from the Cardiophorinae.
In Mem. Soc. Roy. Liége, 1882, Candéze states “la distinction entre les deux genres”
(Megapenthes et Melanoxanthus) “est devenue absolument impossible”. Yet I
prefer to separate the Australian species of these genera known to me by the
different antennae. As with other of our northern species of Coleoptera, many
occur on both sides of Torres Straits. Thus I have identified Melanoxanthus
angularis Cand., M. ruficollis Cand. and (?) M. abdominalis Cand., described from
New Guinea, amongst Hlateridae labelled as from Cairns district by the late
F. P. Dodd. The following are, I believe, undescribed.
MELANOXANTHUS JUCUNDUS, n..sp. PI. Viii, fig. 2.
Head, antennae, underside and legs black, prothorax and tarsi red; elytra
black, with two white rectangular markings, forming a medial fascia, interrupted
at sides and suture, each sloping backward from suture to sides: sparsely
pubescent.
Head short, punctate, antennae not reaching base of prothorax, rather wide,
segment 1 tumid, 2, 3 small, 4-10 triangularly dentate, 5-10 subequal, 4 smaller
than 5, 11 oval. Prothorax about as long as wide, arcuately narrowed in front,
subsinuately widened at the acute, carinate, posterior angles. Disk moderately
convex, coarsely and evenly alveolate-punctate, short bristly hair showing laterally.
Scutellum large, triangular. Hlytra subconic, navicular, at base as wide as
prothorax at hind angles, thence narrowing to apex, here not quite covering
abdomen; striate-punctate, striae close, seriate punctures large and close, intervals
asperate and nodulose on basal half. Prosternum coarsely, metasternum more
finely punctate. Hind coxae angulately widened within, narrowed externally.
Dim. 4 x 14 mm.
Hab.—North Queensland: Townsville (Elston Coll.), Port Denison (Macleay
Museum), Wide Bay (Australian Mus.).
Four examples examined of this pretty little species. Holotype in the
Australian Museum.
Var.—Two of the examples have the apical area of the pronotum black.
MELANOXANTHUS BIARCTUS, nN. sp. PI. viii, fig. 4.
Of the same size and form as H. jucundus. Nitid black with dark pubescence,
elytra with two elongate-oval markings testaceous extending from behind the
shoulders to the apical fourth, near, but not touching, sides; legs black, tarsi red,
antennae with reddish tinge.
Head strongly punctate, clypeus rounded, antennae very similar to that of
jucundus, but 4-10 less widely dentate, more closely adjusted, 11 wider.
Prothoraz: length and breadth subequal, arcuately narrowed in front, hind angles
long, acute, slightly divergent and carinate, sides feebly widened near middle; disk
moderately convex, with large, round punctures, alveolate in middle, separate
306 AUSTRALIAN COLEOPTERA,
towards sides, a linear depression behind each hind angle, basal declivity steep.
Elytra at base as wide as prothorax at hind angles, thence navicular to apex, not
quite covering abdomen; striate-punctate, with series of large round punctures
between narrowly raised intervals, underside with dense silvery pubescence. Dim.
33-4 x 14 mm.
Hab.—North Queensland: Cairns (Macleay Museum); Coen R. (C. York)
(Hacker).
Five examples; two on a card include the holotype, a third in the South
Australian Museum, and two in the National Museum, Melbourne, from Cape York.
MELANOXANTHUS COLUMBINUS, nN. sp. PI. viii, fig. 3.
Narrowly ovoid, with short, rather thick pubescence. Head black, prothorax
above and below red, with a black patch at apex, narrowing to a point near the
middle; elytra nitid black, with two curved yellow maculae at middle, formed like
the wings of a bird at rest; these nearly meeting at suture and extending along,
but not reaching, sides for about one-third of their length; underside (except
prosternum) black, legs reddish, antennae dark red.
Head: clypeus rounded, forehead coarsely punctate, antennae not reaching
base of prothorax, wide, very much as in M. biarctus, 4-10 strongly dentate, 11
oval. Prothorax rather wider than long, arcuately narrowed in front, sides
nowhere widened, hind angles lightly divergent, bi-carinate and acute, embracing
the shoulders of elytra; disk moderately convex, closely, not contiguously, punctate,
the punctures large, round and umbilicate. Scutellum large, triangular. Hlytra
slightly narrower than prothorax at the hind angles, thence converging to apex;
striate-punctate, the striae wide, intervals flat (except near base), seriate punctures
large and close with rugose edges, giving the basal half an asperate, though nitid
surface; underside rather densely clad with silvery pubescence. Dim. 4% x 14 mm.
Hab.—North Queensland: Cairns. (Macleay Museum.)
Another interesting novelty from this rich collection. The elytral pattern
suggests a dove’s wing. Hence the name. Two examples on a card include the
holotype, marked with an arrow. A third is in the South Australian Museum and
a fourth, from Wyreema, Q., is in the Queensland Museum. Examples in the
South Australian Museum from Cairns differ in having the prothorax wholly black.
These are 92 and, like froggatti Macl., show a sexual coloration.
MELANOXANTHUS FLAVOSIGNATUS, n. sp. PI. viii, fig. 1.
Ovate; nitid black, hind angles of prothorax and wide medial, interrupted
fascia on elytra yellow, legs reddish, antennae reddish-brown.
Head short, punctate and pubescent, antennae short, 4-10 strongly dentate.
Prothorax gently narrowed from base to apex, a little sinuate before the extreme
point of hind angles—these lightly divaricate and embracing elytral shoulders.
Disk moderately convex, densely covered with subcontiguous, umbilicate punctures
and with short, bristly dark hairs. Scutellum large, oval. Hlytra slightly narrower
than prothorax at hind angles, gently narrowed from base to apex, the wide yellow
fascia extending to the sutural interval, not quite reaching sides; striate-punctate,
strial punctures small, intervals flat, except on basal half—here strongly asperate
with fine nodules and transverse wrinkles. Dim. 4 (vix) x 14 mm.
Hab.—Queensland: Wide Bay (Macleay Museum.) Holotype in the Macleay
Museum.
Var.—Two examples in the Australian Museum, from the same locality, are
clearly conspecific, but have the hind angles of the prothorax black.
BY H. J. CARTER. 307
MELANOXANTHUS INSOLITUS, nN. sp. PI. viii, fig. 6.
6. Elongate-oval. Head black, prothorax red, elytra black with yellow
markings as follows: a small round spot on each side at extreme base, an arcuate
diagonal macula on each, extending from behind shoulder to the 2nd elytral
interval, forming an interrupted fascia, a straight subrectangular macula at apical
third, forming a second interrupted fascia; prosternum red, strongly pubescent,
rest of underside black.
Head rather longer, but of similar structure to that of H. jucundus, antennae
4-10 dentate, 11 oval. Prothoraz arcuately narrowed in front, sides nearly straight
on basal two-thirds, posterior angles feebly divergent, acute and strongly carinate;
disk rather closely punctate, the punctures much smaller than in the other species
described here, sparsely clad at sides with pale pubescence. Scutellum large, oval.
Elytra at base as wide as prothorax and more than twice as long, sides nearly
straight, more widely rounded at apex than usual; striate-punctate, striae narrow,
seriate punctures moderately large and very distinct, intervals—especially on dark
areas—cancellately divided by transverse wrinkles, the basal area asperate and
subnodulose.
9. Of two examples on a card, what I take to be the other sex has the
pronotum dark brown, with the hind angles red, the yellow subhumeral mark
connected with the basal spot, and the two subapical marks oval. There is little
doubt of the two being conspecific. Dim. 5 x 2 mm.
Hab.—Cape York. (Macleay and the Queensland Museums.)
Less conical in form than usual, otherwise typical of the genus. A dual
carina at sides of pronotum—somewhat as in Cisseis (Buprestidae). Holotype
and allotype in the Macleay Museum.
MELANOXANTHUS LATIVITTIS, n. sp. PI. viii, fig. 7.
Elongate, subconic; very sparsely pubescent. Head, prothorax and underside
dull brownish-black, the prothorax with apical band and hind angles, also antennae
and legs, red; elytra with base brightly luteous, a wide vitta extending throughout,
gradually narrowing to apex, yellow, leaving the suture narrowly, the sides more
widely, brown.
Head deeply enclosed in prothorax, antennae with segments 2 and 3 small,
4-10 moderately serrate. Prothorax gently narrowed from base to apex, sides
feebly sinuate behind, hind angles unicarinate, closely adapted to elytral humeri,
disk rather finely alveolate-punctate. Hlytra elongate, subconic, more than thrice
as long as prothorax; striate-punctate, strial punctures rather small, intervals
lightly convex, except near base; those on dark areas rugosely wrinkled. Under-
side subglabrous, finely and closely punctate, epipleurae with larger punctures.
Dim. 4:5 x 1 (4+) mm.
Hab.—Queensland: Wide Bay.
Two examples in the Macleay Museum show a species more elongate and
narrow than usual. Type series in the Macleay Museum.
MELANOXANTHUS SEMIRUBER, Nl. sp. PI. viii, fig. 5.
Subconic. Head and antennae, prothorax and underside dull black, the hind
angles of prothorax, basal segments of antennae and legs red, elytra with basal
half chiefly red, this colour with undefined limits at base, the base,, suture and
apical half black; upper surface with short pubescence.
Head convex, antennae rather stout, submoniliform, 2—3 short, 8-10 tending to
triangular, 11 oval. Prothorax slightly longer than wide, sides nearly straight,
308 AUSTRALIAN COLEOPTERA,
lightly narrowed in front, hind angles acute, slightly divaricate and strongly
carinate; disk uniformly alveolate-punctate. Scutellum large, oval. Hlytra of same
width as prothorax and about twice as long, sides narrowed from base to apex;
striate-punctate, strial punctures fairly large and close, setigerous; apical half
finely rugose. Dim. 44 x 14 mm.
Hab.—North Queensland: Cairns (Macleay and the South Australian
Museums).
Of like form to H. biarctus and H. flavosignatus. Holotype in the Macleay
Museum.
MELANOXANTHUS RUFONIGER, n. sp. Pl. viii, fig. 11.
¢. Base of head, antennae (except basal segments), a wide median vitta on
pronotum, apical three-quarters of elytra subnitid black, rest of surface, above and
below, red or yellow; dull red on head and pronotum, base of elytra, underside and
legs pale yellow, with rather dense pubescence at sides of pronotum and elytra.
Head closely punctate, antennae not quite reaching base of prothorax, segments
rather widely triangular to scutate. Prothorax: sides converging from base to
apex, hind angles acute, unicarinate, and feebly divaricate, closely embracing
shoulders of elytra; disk closely punctate, the punctures tending to coalesce in
lines, becoming finer towards sides. Elytra twice as long as prothorax, cuneiform;
clearly striate-punctate, intervals nearly flat and finely granulate.
©. Whole of head and greater part of elytra orange-red, the latter paler near
base, the sides only black, elsewhere very faintly clouded.
Dim. 8, 3 mm.; 9, 4 mm. long.
Hab.—Queensland: Tambourine Mountain (A. M. Lea).
A pair, the sexes, in the South Australian Museum, give evidence of the
thorough field-work of my old friend. The name vitticollis is barred by the triple
use of this name in the genus. The elytra are evidently liable to colour variation.
Holotype in the South Australian Museum.
Australian species of Melanoxanthus known to me.
iP eerothorax black. wor Chiefiys (SO; cys ord eee acre ok Te eT ee en oe eee 2
Prothorax Tred jor Chietly SO. ae t hale ns eae ene cas hee PU Reon ote EE ci cease 8
Prothorax trivittate, medial area black, sides yellow .............. rufoniger, n. sp.
Zeperovhnoraxquwi Olly Ch cue tutus tone lick eeilos Reusch vom ai asta lee Re ACLe (Rde eae es RS re eee 3
IST NC EDS Ayla LoubaKey Ahorslles aHsel Ge WeMlOny Soocooboboconsobacdannudooudacdendds 5
% IDVhnERe! moeyoraeS, Nomex ITChiNE og oogoocbvadcuodooHeuboodcmooDdoenouO ON biarctus, n. sp.
IDK AMEN Tasha abayeKs) “inoKOVNS (Ojo IEE) HEISOE Gaonagdoddovooodnaooconaubocuonouaecanc 4
APM ASCIARNAT TOW). fp nicieiaiels: dapele tebe cawiachok. a ete MIOCeNes He COlLOrad Oi7 = ircreteuc ete ste ee Sos, esas ie de aernca ht seta mepeee mean eens florissantensis (Ck11.)
Lexerereraiitg aSObteloy boc OORh “Aeididia a Gaieidin Mtieeo Cee eto He oe REE ai b oOo oman ou Sem bis 2
Cubitus 2-branched; R,,, forked, occasionally simple; length 12 mm. or less. Trinidad
ARPES ot UR TEME Sted Ses eG. riot CRC CMCC OME RPC REMC G .O.nc Oho cceeencR Ea OCHA CHCA NERC ILC urichi (Sauss.)
Cubitus) 3—4-pranchedi- clearly tonked: lene tings jmaride 107s YU seen telene nel 3
Tenth tergite divided, the hemitergites separated by membraneous areas. Venezuela
Pigs b eee es ay oy 2: mal ones kes Ral eden oh Ms carahione Wectece reper een on owed pc a ARO ict omcpenrse rs te intermedia, n. sp.
Tenth tergite entire, sclerotization continuous from side to side. Brazil ............
es PoP SY ap nears fe hs lets Ne UE oe Hay MSU ours retest erie valve a emethe hc ciGr avails merch ate wamemae hegre hegre wre nobilis (Gerst.).
bo
Co
List of References.
COCKERELL, T. D. A., 1908.—Descriptions of Tertiary Insects. Amer. Journ. Science,
Series 4, 25.
ENDERLEIN, G., 1909.—Die Klassifikation der Embiiden, nebst morphologischen und
physiologischen Bemerkungen, besonders tiber das Spinnen derselben. Zool. Anz., 35.
, 1912.—Embiidinen, in Coll. de Selys-Longchamps, fase. 3.
GERSTAECKER, A., 1888.—Charakteristik einer Reihe bemerkungswerter Orthopteren. Mitt.
naturw. Ver. Neuwvorpommern und Riigen, Jg. 20.
GRIFFITH, W., and PIDGEON, W., 1832.—The Animal Kingdom arranged in Conformity
with its Organization, by the Baron Cuvier, with Supplementary Additions to Each
Order. Vol. 15 (Vol. 2 Insects). London: Whittaker Treacher and Co. (Plates
issued separately, 1831.)
Krauss, H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23. Stuttgart.
Dn SaussuRE, H., 1896a.—Two Embiidae from Trinidad. Journ. Trinidad Club, Port of
Spain, Vol. 2, No. 12 (February 1896).
———., 1896b.—Note sur la Tribu des Embiens. Mitt. Schweiz. entomol. Ges., Bd. 9,
Hft. 8 (July 1896).
NavAs, L., 1925.—Neuropteren aus Brasilien. Mitt. der Miinchner Entomol. Gesellschaft,
15.
381
TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. V.
THE GENUS DONACONETHIS ENDERLEIN.
By Consett Davis, M.Sc., Lecturer in Biology, New England University College,
Armidale.*
(Five Text-figures. )
[Read 30th August, 1939.]
DoNACONETHIS Enderlein 1909. ;
Zool. Anz., 35, p. 176. Genotype, Donaconethis abyssinica Enderlein, 190! 5 deSop
| oe Ore
Enderlein’s generic concept depends on the forking of the media. Since
venational aberrations are moderately frequent in the Order Embioptera, specimens
rightly referable to Donaconethis may occur with M simple, as a venational
anomaly, and specimens of other genera may likewise, in exceptional cases, have
M forked (cf. Navas 1923, concerning Embia ramosa). It is consequently desirable
to establish the genus on the more reliable characters of the terminalia, and at the
same time to give a more complete description of the genotype.
The following description is based on a specimen (4) in the Museo Civico di
Storia Naturale, Genoa, labelled ‘Bogos, Keren; 1870, Dr. Beccari’. It had been
identified as Donaconethis abyssinica by Navas, who (1928) has given a brief and
inaccurate description of the venational anomalies, without detailing the structure
of the terminalia. Hxamination of the terminalia showed the species to agree with
Enderlein’s description of the type (Berlin Zool. Museum), which is from Asmara,
Hritrea, only some 50 miles from Keren. The genus may therefore be re-defined
as follows:
Robust Embioptera, the males with the following characters: Winged, with
R,,, forked, M with a tendency to fork, not always manifest. Hind tarsi with one
metatarsal bladder. Terminalia with tenth tergite completely cleft longitudinally;
right hemitergite massive, with a posterior tapered process directed downzvards,
and an internal flap-like process. Process of left hemitergite bifid. First segment
of left cercus with inner margin produced into two marked lobes, each with 3-5
very large spiniform toothlets directed forwards.
The genus is differentiated from Hmbia and Rhagadochir, apart from the
variable character of venation, by the structure of the first segment of the left
cercus, with its two lobes bearing few but very large toothlets. It is different from
Hmbia, but similar to Rhagadochir (probably by convergence), in having the
process of the left hemitergite forked. It agrees with Dihybocercus severini
Enderlein (1912), the genotype of Dihybocercus Enderlein, from the Congo, in the
two lobes of the first segment of the left cercus, which, however, according to
* Part of the work embodied in this paper was carried out when the writer held a
Linnean Macleay Fellowship in Zoology.
382 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. V,
Enderlein’s figure, carry numerous small teeth in this species. Dihybocercus
spinosus Navas 1931, also from the Congo, is more closely related to Donaconethis
than is Dihybocercus severini. The structure and dentition of the first segment of
the left cercus in Dihybocercus spinosus are strongly reminiscent of Donaconethis,
and other parts of the terminalia (process of left hemitergite; posterior process of
right hemitergite; hypandrium; left cercus-basipodite) also show general resemb-
lance. The two hind metatarsal bladders, simple media (in the unique specimen),
and right cercus-basipodite of Dihybocercus spinosus suggest that it should be
placed in a new genus, as they differentiate it from Donaconethis (in the present
sense) just as the dentition of the left cercus differentiates it from Dihybocercus.
Dihybocercus berlandi Navas 1922, and D. gromieri Navas 1934, together with
another undescribed species from West Africa congeneric with the above, are related
neither to Dihybocercus nor to Donaconethis. A new generic name is required
here also.
DONACONETHIS ABYSSINICA Enderlein, 1909, l.c. Figs. 1—5.
3 (Keren, Eritrea; Genoa Museum). Length 10-9 mm.; head, length 3-1 mm.,
breadth 2-5 mm.; forewing 9 mm. x 3 mm.: hindwing § mm. x 3 mm. General
colour very dark brown. Head (Fig. 1) large, eyes small, sides of head behind
eyes at first slightly divergent, rounded behind. Antennae incomplete. Wings
(Fig. 2) with numerous cross-veins; Sc reaching to one-quarter the length of the
wing; R, confluent distally with R,.,,; R,,; forked, fork longer than stem; R,; again
forked in left hindwing (the anterior branchlet fusing distally with R,), and very
shortly forked in right hindwing. M simple in right forewing, shortly forked in
left forewing and right hindwing, more clearly forked in left hindwing. Cubitus
two-branched, with a vestige of a third branch in left hindwing and right forewing
(cf. Enderlein’s figure, 1912, fig. 7, of the right forewing of the type), and a
prominent third branch in the left forewing. Metatarsus of hind legs with only
the terminal ventral bladder, as in the African species of Hmbia. Terminalia
(Figs. 3-5) with tenth tergite completely cleft, right hemitergite (10R) posteriorly
produced downwards and inwards to a tapered process (10RP,), the parts internal
and anterior to which are more membraneous. Inner margin of 10R with a
sclerotized flap (10RP.), as in Hmbia, separated from 10R except posteriorly by
membrane; free edge of 10RP, roughened posteriorly. Left hemitergite (10L)
massive, inner margin produced backwards to a broad flat process (10LP),
terminally curved out and acute, roughened on internal edge, with a subterminal
broad, flat, acutely-ending process latero-dorsally to the left. In this detail, the
specimen differs from Enderlein’s figure and description of the type, which
indicate no lateral lobe for 10LP; it is probable that it has been broken or over-
looked in the type. Second segments of both cerci broken; first segment of left
cercus (LC,) very characteristic, inner margin dilated subterminally in a rounded
lobe, with 4-5 relatively large teeth curved slightly forwards, acute; LC, with a
more dorsal basal lobe, rounded, with 3-4 similar teeth. First segment of right
cercus (RC,) subcylindrical. Ninth sternite (H) produced backwards from the
right-hand side to an obtuse process (HP); space between HP and base of LC,
occupied by left cercus-basipodite (LCB), which has a long curved acute process
directed downwards and outwards.
Enderlein’s dimensions of the type male are: Length 11 mm., forewing 8 mm.
His description and figures (1909, 1912) tally with the above except for the
structure of the process of the left hemitergite.
9. v. Enderlein, l.c. Not of taxonomic importance.
BY CONSETT DAVIS. 383
Donaconethis abyssinica, 3, Keren, Eritrea.
7
1. Head, x 7. 2. Wings, x 7 (conventional lettering for venation). 38. Terminalia
from above, x 15. 4. Terminalia from above, and slightly to the left and behind, x 15.
>. Terminalia from below, x 15.
9, ninth abdominal tergite; 10L, 10R, left and right hemitergites of tenth abdominal
segment; 10LP, process of 10L; 10RP,, 10RP,, posterior and inner processes of 10R;
LC,, RC,, first segments of left and right.cerci (second segments missing) ; LCB, RCB,
left and right cercus-basipodites; H, HP, ninth sternite and its process.
All figures based on camera lucida outlines.
Note.—The genus Donaconethis must at present be considered monotypic.
Krauss (1911) rightly classes D. ehrenbergi Enderlein 1909 (Zool. Anz., 35, p. 178)
as a doubtful species. The type male (Berlin Zool. Museum), from Hgypt, has the
terminalia missing. Its exact locality is not known. The species is likely to
remain unrecognizable; it should never have been described. It may represent a
specimen of some species of Hmbia with a venational aberration; its size, colour,
and the form of the head, suggest H. savignyi Westwood. There is no evidence
that it is referable to Donaconethis in the present sense. Enderlein, in his
‘Nachtrag’ (1912, pp. 107-108, fig. 70) describes terminalia which may belong to
his type; according to his figure, these terminalia are exactly similar to those of
Hmbia savignyi Westw.
List of References.
FENDERLEIN, G., 1909.—Die Klassifikation der Embiiden, nebst morphologischen und
physiologischen Bemerkungen, besonders itiber das Spinnen derselben. Zool. Anz.. 35.
, 1912.—Embiidinen, in Coll. de Selys-Longchamps, fase. 3.
Krauss. H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23. Stuttgart.
384 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. Y.
NavAs, L., 1922.—Algunos Insectos del Museo de Paris. Rev. Acad. Cienc. Zaragoega,
Vol. vii.
, 1923.—Comunicaciones Entomolégicas. 6. Notas sobre Embiépteros. Ibid.,
Vol. viii.
, 1928.—Insectos Exéticos Neurépteros y Afines del Museo Civico de Génova.
Annali del Mus. Civ. di Stor. Naturale, Genoa, Vol. 53.
—, 1931.—Insectes du Congo Belge (Série VI). Rev. Zool. Bot. africaines
(Tervueren), Vol. 21, fase. 2.
, 19384.—Décadas de insectos nueyos (Década 25). Brotéria, Série trimestral,
Vols 3.) tases t-
385
THE GEOLOGY OF THE COUNTY OF BULLER, N.S.W.
By A. H. Voisry,* M.Sc., Lecturer in Geology and Geography, New England
University College.
(One map; two Text-figures. )
[Read 30th August, 1939. ]
The County of Buller lies in the Far North Coast District of New South Wales
and is limited on the north and west by the Main Divide which marks the boundary
between New South Wales and Queensland. The Richmond Range forms a natural
boundary on the east, but the southern boundary, though following creek divides,
is less clearly defined. The area is drained by the Clarence River and its tribu-
taries, the most important of which are the Maryland, Cataract and Boonoo Boonoo
rivers and Koreelah, Tooloom, Duck and Peacock creeks.
Woodenbong, Urbenville and Bonalbo are the principal towns in the County,
but other small centres are Legume, Liston, Amosfield, Wilson’s Downfall, Boonoo
Boonoo, Acacia Creek, Capeen, Koreelah and Tooloom. Drake, Tabulam and
Mallanganee lie just outside the southern border of the County on the road between
Tenterfield and Casino.
Most of the data used in the compilation of this report were collected during
the early part of 1938 and during a trip to Rivertree in February 1934.
It is unfortunate that several problems raised by the writer in his report on
Boorook and Drake (Voisey, 1936) still remain unsolved. The most important of
these refers to the basal beds of the Drake Series and their relationship to the
Emu Creek Series. A thick soil cover prevents a close examination of the meeting
place of the two series in the neighbourhood of the Lunatic Gold-Field, but
examination of the structures in the adjoining areas suggests that the junction
is a faulted one. The continuation of the boundary of the Emu Creek Series is
believed to run through thickly wooded and rugged country which is difficult of
access. An attempt to map it in May 1938 was frustrated by heavy rains leading
to a flooding of the streams.
The purpose of this paper is to bring together a number of somewhat scattered
observations made by previous workers and the writer. The outcrops of the various
rock types are shown on the accompanying map.
Previous Literature.
Most of the earlier observations made in the County of Buller are mentioned
in the reports of E. C. Andrews (1900, 1901, 1902, 1903, 1908). HE. F. Pittman
(1908) referred to the trachyte of the South Obelisk near Tooloom, and L. F.
Harper (1929) gave a short account of the general geology of the northern and
eastern parts of the county. The writer (1936) in connection with investigations
* This paper was completed while the author was Linnean Macleay Fellow of the
Society in Geology.
FEF
386 GEOLOGY OF THE COUNTY OF BULLER, N.S.W.,
on the rocks in the neighbourhood of Boorook and Drake, reported on the
stratigraphy and palaeontology of the southern part of the area and submitted a
map.
GENERAL GEOLOGY.
Summary.
The oldest rocks found in the area belong to the Emu Creek Series and are
believed to be Upper Carboniferous in age. They outcrop principally between
Emu Creek and the Clarence River.
ae To Brisbane
GEOLOGICAL SKETCH-MAP OF THE a
WOODENBONG +
COUNTY OF BULLER
N.S. W.
‘ 4 r 5 ~ UreEnivite:.
DIVIDE J 7 . WORTH G35
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we * H a C. es
ee tAcCACy
QUEENSLAND...
"
OBELISK EX |
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,
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UNOERCLIFFE = f
TABLE
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=o
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* AMOSFIELD ¢
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ea wicsons
yy
LEGEND ee
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SEDIMENTARY
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LOweR CLARENCE
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COAL MEASURES .
eo + . #3 To Gasino
_ 3 } % ao a eo
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PALAEOZOIC a fk TARO eases Seon
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DRAKE SERIES Coe ( ra " a a AS. ; } TABULAM
Emu CREEK senies [ih] ee
BASAL STAGE
IGNEOUS
BASALT
ALKALINE NTRS oy a : Be a | ‘ : i USS J es ; SCALE.
= . ea 5 =
GRANITE
FOSSIL LOCALITIES x MILES
. J | “i :
COUNTY BOUNDARY — -—- . ¥ : , é
SETTLEMENTS P]
ROADS
Map 1.
BY A. H. VOISEY. 387
The Drake Series, comprising more than 5,000 feet of volcanic rocks, passing
upwards into several thousand feet of marine sediments, belongs to the Kamilaroi
(Permian) System. It continues northwards from the neighbourhood of Drake to
Rivertree and beyond.
Nearly half of the County of Buller is covered by sediments of Jurassic age
belonging to the Clarence Series. These in places are overlain by Tertiary basalts
and are intruded by sills, plugs, and, perhaps, laccolites of alkaline rocks also of
Tertiary age.
Granite in Late Palaeozoic times invaded the Drake and Emu Creek Series,
but is unconformably overlain by the sediments of the Clarence Series.
CARBONIFEROUS.
The Emu Creek Series.
Mudstones and tuffs containing an abundant marine fossil fauna and outcrop-
ping at Jump-up Hill and along Hmu Creek have been described previously
(Voisey, 1936). They were traced northward to Pretty Gully by Andrews (1908)
and have been found to continue to Paddy’s Flat and beyond.
The beds are overlain unconformably by conglomerates and sandstones of the
Clarence Series and by Tertiary basalt between Pretty Gully store and Paddy’s
Flat.
The prolific Fenestellidae beds outcrop in cuttings along the Paddy’s Flat road
10 miles from Tabulam. At least 30 feet of strata are crammed with polyzoan
remains. Several small spirifers were found also. The matrix is olive-green
mudstone which weathers to a buff colour. Associated with the mudstones are
hard tuffs and tuffaceous sandstones. The beds dip in a north-easterly direction
at 45 degrees. They disappear beneath the Clarence Series about a mile from
Pretty Gully store but make their appearance beside the road again where the
descent is made to the Clarence River at Paddy’s Flat. The highest beds are
principally tuffs, tuffaceous sandstones and mudstones, but occasional bands of
conglomerate are present. The mudstones contain Fenestellidae horizons with
subordinate coarser bands of sediment. They underlie the tuffaceous group and
MARYLAND RIVER
GREAT
TABLE
MOUNTAIN
MARYLAND R.
RIVERTREE
CLARENCE
RIVER
TOOLOOM CK
LOweR
TOOLOOM
DUCK CREEK
BONALBO
S05." * .GASAL = STAGE (OF 25+
St LOWER CLARENCE . SERIES *
Ae OlOl MACNN GO:
5 Sofie
GREAT
TABLE
NTH OBELISK
p(Giraad cK
PADDYS FLAT
CLARENCE R
ie
“ DRAKE SERIES “ { emy leatlag Vasdies |
KONA) g t hogs fase
ae ieilen Ii
= 36 MILES
1.—Section from Maryland to Bonalbo. V/
2.—Section from Drake to Urbenyille, V/H
Wow
oo
ees
ila’
388 GEOLOGY OF THE COUNTY OF BULLER, N.S.W.,
comprise several hundred feet of the total of approximately 1,000 feet of rocks
exposed. The dip is generally to the south-east at 40 degrees.
The Emu Creek Series is overlain by the Lower Clarence Series in the northern
part of the County but reappears in the vicinity of Mount Barney just over the
Queensland border (Richards, Bryan and Whitehouse, 1932).
In his previous paper the writer (Voisey, 1936) discussed limestones, cherts,
etc., occurring near the junction of the Paddy’s Flat road with the main road from
Tabulam to Drake under the name of Plumbago Creek Series. It was suggested
that the beds might be related to the Drake Series. However, they seem to pass
northwards into the Emu Creek Series and hereafter will be considered part of
that series. Some of the sediments have been contact metamorphosed by the
adjacent granite. They are indurated black rocks, some possessing a rough parting
parallel to the lamination. The name slate, loosely applied to them, is somewhat
misleading since there is no evidence of any dynamic metamorphism.
KAMILAROI.
Since the limits of the Permian System are still in dispute and the use of the
term ‘Permian’ admits of a number of interpretations it has been decided to
follow the nomenclature suggested by the late Professor Sir T. W. E. David
(1932). In an earlier paper (Voisey, 1936), the Drake Series was considered as
Permian in age, but, until the controversy is settled, the better-defined name
“Kamilaroi” will be used. The writer regards “Kamilaroi”, ‘Permian’ and
“Permo-Carboniferous” as synonyms and is opposed to the division of the first-
named into Permian and Carboniferous sections.
Drake Series.
The Upper and Lower Divisions of the Drake Series continue north and north-
east of Boorook and are folded into anticlines and synclines along a meridional
axis. In the neighbourhood of Boorook beds of the Upper Division occupy a
synclinal structure which pitches gently in a northerly direction. The beds
continue northwards towards Undercliffe and Rivertree.
Andrews (1901) noted the presence of graphite produced by the intrusive
granite from dirty coal seams at a point eleven miles east of Wilson’s Downfall.
These coal seams occur with tuffs and contact-altered sediments, probably belonging
to the Upper Division of the Drake Series.
Altered tuffs and mudstones outcrop at Undercliffe Falls in contact with
granite. Andrews (1902) recorded ‘‘Permo-Carboniferous” fossils from this locality
and also from Cullen’s Creek at Rivertree (1908). The present writer in 1934
found a number of marine fossils in indurated mudstones near the old silver mines
at Rivertree. Owing to the lack of detailed mapping between here and Boorook
the stratigraphical position of the beds has not been determined. The: irregular
boundary of the granite and the contact alteration of the sediments which it has
produced add to the difficulty of mapping this rugged, well-wooded country.
North of Rivertree the Kamilaroi rocks are overlain by the Clarence Series
and Tertiary basalt.
Near the Queensland border, at Maryland Station, and running in a north-
westerly direction through the parish of Maryland, is a mass of sedimentary rock
about seven miles long and averaging about a mile wide. It is surrounded on all
sides by granite and has suffered intense contact metamorphism. The rocks are
principally indurated mudstones, sandstones and tuffs which contain numerous
Kamilaroi marine fossils including Linoproductus springsurensis and Fenestellidae,
BY A. H. VOISEY. 389
The fossil beds are located on the properties of Messrs. C. Bonner and W. E.
Barnard on portions 266, 37, 446 and 23, parish of Maryland, and portion 73,
parish of Ruby.
Good exposures occur along Maryland Creek in the portions named. So far
as the author is aware, this is the first record of the discovery. Mr. H. W. Scott,
Manager of the Stanthorpe branch of the Commercial Banking Company of Sydney,
drew the writer’s attention to the beds after having been shown the fossils by
Mr. C. Barnard some years ago.
Associated with the altered sediments are several bands of what appears to be
voleanic rock. This contains well developed phenocrysts of felspar and resembles
some of the lavas of the Drake Series. Microscopical examination will be necessary
to prove the suggested correlation.
The fossil beds dip in a south-easterly direction at high angles, reaching 80
degrees in places. Felsite (?) half a mile south of Maryland Station strikes 140°
and appears to be vertical. At Cundumbul andesite (?) strikes 120° and again
the dip is very steep. The general strike of the beds within the sedimentary area
is north-west—south-east, but, as in the case of the fossil beds, there are local
variations.
Other blocks of sedimentary rock surrounded by granite occur in the neigh-
bourhood of Maryland, one such being found about 7 miles from Liston on the
Rivertree road and another is exposed by a railway cutting just north of Dalveen
(Queensland). The last-named may consist of members of the Silverwood Series of
Devonian age (Richards and Bryan, 1924). The Maryland and Rivertree road beds
may be referred to the Drake Series and, geographically, are situated between
known outcrops of these rocks and those of the Fault Block Series (Richards and
Bryan, 1924).
The writer visited the Silverwood area and examined the members of the
Fault-Block Series before he was acquainted with the Drake sequence and for
various reasons disagreed from the arrangement of the succession tentatively put
forward by Richards and Bryan (1924). This paper (Voisey, 1934) was discussed
at a meeting of the Royal Society of Queensland and a number of other arrange-
ments and correlations were suggested (A.N.Z.A.A.S., 1935).
The most satisfactory method of dealing with the isolated occurrences appeared
to be by correlating the units with horizons in an adjacent area where the sequence
was known. Therefore, field-work was carried out around Drake and Boorook
(Voisey, 1936) with the resuit that such a sequence was obtained at a distance
of less than forty miles from Silverwood. On the evidence furnished by these
beds the writer had no alternative but to alter the arrangement which he had put
forward previously. ;
There appears to be little doubt that the lavas, tuffs, conglomerates and grits
of the Tunnel, Rhyolite Range and Hight Mile blocks belong to the Lower Division
of the Drake Series. Detailed petrological work on these beds is of the utmost
importance and will settle the correlation question.
The tuffs and mudstones of the Condamine Block suggested by Richards and
Bryan (1924, p. 65) to be contemporaneous with the volcanic beds discussed above
were regarded by Reid (1930), the writer (Voisey, 1934) and others to have
preceded them. However, at Boorook, similar beds also containing abundant
Trachypora wilkinsoni and Monilopora nicholsoni occur with other marine strata
above the lavas and tuffs of the volcanic suite. Beneath the Trachypora—Monilopora
zone at Boorook are richly fossiliferous sediments with some bands composed
almost entirely of the remains of Strophalosia and others of Fenestellidae or
390 GEOLOGY OF THE COUNTY OF BULLER, N.S.W..
lamellibranchs. The stage is suggestive of that composing part of the Wallaby
Block at Silverwood.
Although a close correlation between the individual units of the Silverwood
and Boorook—Drake areas cannot be made at the moment, it would appear from
the presence of abundant specimens of Tvrachypora, Monilopora, Fenestella,
Strophalosia and certain lamellibranechs occurring in zones in both areas that
correlation in a broad way is indicated. It seems, therefore, that the Condamine
and Wallaby beds are the equivalents at Silverwood of part of the Upper Division
of the Drake Series.
The position of the strata of the Hurydesma Block is still in doubt. The writer
(1934) attempted to show that they overlay the strata of the Condamine Block,
using as evidence certain similarities in lithology and the presence of Monilopora
in each block. If the rocks are so related the Hurydesma beds must belong to
the Upper Division of the Drake Series, possibly occurring immediately below the
main Trachypora—Monilopora zone. In such a case the somewhat forced palaeonto-
logical arguments indicating that the beds underlay the volcanic suite must be
disregarded. On the other hand, the horizon of abundant Hurydesma cordatum is
still regarded by most Australian geologists as indicating a position low down in
the Kamilaroi sequence, even though the genus has been found scattered through-
out the whole system. If we regard this horizon as occurring high up in the
Upper Division of the Drake Series it is somewhat surprising to find such a big
thickness of sediments and lavas between it and the base of the Kamilaroi system.
The lavas and tuffs of the volcanic suite cannot be placed in the Carboniferous
System since Andrews (1908) records several occurrences of definite Kamilaroi
fossils interbedded with them. The writer has seen similar fossils in the Lower
Division of the Drake Series beside Girard Creek (Voisey, 1936).
No beds directly underlying the lavas have been found in the Boorook—Drake
area. Neither Glossopteris nor Gangamopteris has been collected. The presence of
dirty coal seams at Undercliffe (Andrews, 1901) is indicative, however, of some
fresh-water deposits.
JURASSIC.
Clarence Series.
Sediments belonging to the Clarence Series occupy most of the north-eastern
part of the County of Buller, their boundary running diagonally across it from
the neighbourhood of Legume to Tabulam. Outliers occur to the west of this at
Kettle’s Lift, Pretty Gully and elsewhere.
Warping and faulting which took place, probably in Tertiary times, have
been responsible for the elevation of the sediments, the base of which rises
gradually from Tabulam at 400 feet towards Legume and to Warwick in Queens-
land where it is at approximately 1,500 feet. Outliers in the vicinity of Silverwood
attain a height of over 2,000 feet. The base of the Pretty Gully outlier lies at
about 1,100 feet.
Only the Lower Clarence Series is represented in the County and it may be
divided conveniently into two stages, the Basal Stage and the Coal Measures.
Basal Stage.
The lowest beds of the Clarence Series consist principally of conglomerates
made up of a great variety of well-rounded pebbles. Sandstones separate the
conglomerates and merge into them. Smaller lenticular sandstone bands occur
within the main conglomerate horizons which are usually about ten feet in thick-
ness, Fine-grained sediments are rare in the Basal Stage,
BY A. H. VOISEY. 391
Large tree trunks and numerous pieces of fossil wood are a distinctive feature
of the beds. They are seen to advantage in road cuttings just east of Tabulam
and alongside creeks in that locality. Magnificent examples have been found at
Warwick in Queensland just beyond the limits of the accompanying map.
The constitution of the outlier at Kettle’s Lift is noteworthy since it is a
remarkably good example of a consolidated soil or rubble which had covered the
land surface before inundation. The rock consists of granite soil in which are
set large rounded granite boulders which give the impression that they are
intrusive into the bed in which they lie. Similar rocks characterize the basal
beds of the Jurassic System in parts of the Northern Territory, notably at
Buldiva (Voisey, 1938).
Coal Measures.
The Coal Measures overlie the Basal Stage. In the County of Buller coal
seams were met at intervals from a point near the junction of the Bonalbo road
with the Tabulam—Mallanganee road to Urbenville. They are then hidden by basalt
but reappear near the junction of the Urbenville road and the New England High-
way and continue northwards into Queensland. Owing to the very gentle dip in
the north the coal measures outcrop over a much larger area than in the south of
the Clarence Basin near Coramba.
The beds consist of soft mudstones with subordinate sandstone and a number
of coal seams. Details of the properties and value of the coal in the region are
given by Pittman (1908). He recorded a workable seam nearly three feet wide
near Killarney in Queensland. Most of the seams, however, are of poor quality
and less than 2 feet in thickness. Alethopteris was found by Pittman near
Killarney.
Age of the Clarence Series.
A. B. Walkom (1918) discussed in some detail the relationship between the
Clarence Series and the Mesozoic rocks of Queensland. There seems to be little
doubt that the Coal Measures of the Lower Clarence Series can be correlated with
the lower part of the Walloon Series of Queensland. They are, therefore, Lower
Jurassic in age. The Basal Stage bears some lithological resemblances to the
Bundamba Series which consists also of massive sandstones, grits and
conglomerates. The age of this series is still in doubt since no recognizable fossils
have been found in it. Fossil wood, however, is extremely abundant in the Basal
Stage of the Lower Clarence Series and may give some clue which will lead to the
selution of the problem.
As there does not seem to be any evidence to the contrary, both the Basal
Stage and the Coal Measures are regarded as Jurassic in this paper.
PLEISTOCENE.
High-level river gravels occur alongside the Clarence River and are similar
to those of the Macleay, Manning and other rivers along the coast. On the hills
just west of Tabulam bridge they are about 70 feet above the river.
RECENT.
Beautifully terraced alluvial flats are prevalent beside the Clarence River and
are developed to a lesser extent beside some of its tributaries. The terraces in the
neighbourhood of Tabulam are particularly fine examples.
392 GEOLOGY OF THE COUNTY OF BULLER, N.S.W.,
IGNEOUS Rocks.
Granite.
E. C. Andrews (1903, 1905, 1908) has dealt adequately with the granitic rocks
of New England and part of the County of Buller and little can be added here.
The granite occupies a large area to the west of the County, its eastern
boundary running irregularly through Boorook, Undercliffe and Rivertree to pass
under the Clarence Series and basalt.
Professor Skeats (1930-32) suggested that the age of some of the granites
might be Mesozoic following verbal communications from Professor Richards, Dr.
Bryan and Dr. Whitehouse. There appears to be general agreement, however, that
the evidence upon which the suggestion was based admits of another interpretation.
It is highly improbable, therefore, that any of the granite in the area being
described is intrusive into Mesozoic rocks. Its age may be regarded as late
Palaeozoic.
Alkaline Intrusives.
A number of alkaline plugs, laccolites and sills occur in the north-eastern
portion of the County. They comprise the prominent hills North Obelisk, South
Obelisk, Edinburgh Castle and others. These were mentioned by Andrews (1903)
in his report on New England. Pittman recorded the presence of the alkaline rock
at the North Obelisk in 1908 (Pittman, 1908). He regarded its occurrence as being
that of a laccolite.
Sills of fine-grained trachytic rock intrusive into the Coal Measures of the
Clarence Series are exposed by cuttings on the Bonalbo road about 9 miles south
of Urbenville near the bridge over Lemon Tree creek. The sills, which attain
thicknesses up to ten feet in places, have slightly metamorphosed the sedimentary
rocks and, where they have followed the coal seams, have affected them consider-
ably. They are particularly well developed in close proximity to the coal, evidently
having found progress more easy in the softer rocks.
Basalt.
Sheets of basalt cap most of the ridges in the north and east of the area,
notably Pocupar or the Great Table Mountain, the Richmond, Tooloom and
MacPherson Ranges. Its base lies generally at a height of about 1,000 to 1,200
feet above sea-level, but this height varies considerably from place to place.
The basalt is post-Jurassic in age since it overlies the Coal Measures. It may
be assigned confidently to the Tertiary Era. 5;
STRUCTURAL GEOLOGY.
The Emu Creek Series has been folded on a general meridional axis and has
been extensively faulted. Details of the individual folds have not been ascertained.
The Drake Series is gently folded into anticlines and synclines at Boorook and
Red Rock, the axis of the folding being generally north and south. Further east
the folding has become more intense and, in places, the beds have assumed vertical
positions.
A faulted junction between the Emu Creek Series and the Drake Series is
indicated on the map and has been deduced from a study of the strikes in that
region. Outcrops there are very poor. The relationship between the two series
between Rivertree and Hmu Creek is in doubt since the country is difficult of
access and recent investigations were hampered by floods.
The Jurassic rocks have a general easterly dip in the south-eastern part of
the county. They flatten somewhat and turn slightly northward in the north-west
BY A. H. VOISEY. 393
region. These sediments unconformably overlie the Upper Palaeozoic rocks and
the granites.
PHYSIOGRAPHY.
The County of Buller comprises the basin of the Upper Clarence River, being
bounded by divides on the east, north and west, respectively the Richmond Range,
MacPherson Range and the Main Divide.
Basalt forms a capping on most of the ridges and was apparently poured out
over a surface which now stands at heights of between 1,000 and 1,200 feet above
sea-level. This surface tilts upwards to the west.
Deep gorges characterize the Cataract and Maryland rivers and many of their
tributaries which are working in the Palaeozoic rocks and the granites. The
Clarence Series has responded much more readily to erosion and the region which
it occupies is more or less undulating.
The alkaline intrusions around Urbenville are conspicuous features rising
steeply from the more open country.
Acknowledgements.
I desire to thank Mr. H. W. Scott of Stanthorpe for his hospitality and help
which have been given freely over a number of years.
Messrs. C. Bonner of Cundumbul Station and W. E. Barnard of the Summit
guided me to the Maryland fossil beds and gave me much useful information,
and to them also my thanks are due.
Bibliography.
ANDREWS, EH. C., 1900.—Report on the Rivertree Silver Field. Ann. Rept. Dept. Mines
and Agric. N.S.W., 1900, p. 192.
, 1901.—Note on the Occurrence of Graphite at Wilson’s Downfall. Ann. Rept.
Dept. Mines N.S.W., 1901, p. 170. f
, 1902.—Ann. Rept. Dept. Mines N.S.W., 1902.
——, 1903.—The Tertiary History of New England. Rec. Geol. Surv. N.S.W.,
Wil, i8its Be
————, 1905.—The Geology of the New England Plateau. Rec. Geol. Surv. N.S.W.,
viii.
—, 1908.—Report on the Drake Gold and Copper Field. Geol. Surv. N.S.W.,
Mineral Resources No. 12.
Davip, T. W. E., 1932.—Explanatory Notes to Accompany a New Geological Map of the
Commonwealth of Australia.
Harper, L. F., 1929.—Clarence Valley Development Investigation. Ann. Rept. Dept.
Mines N.S.W., 1929, p. 85.
PITTMAN, EH. F., 1908.—Coal Seams South of Maclean, Clarence River. Ann. Rept. Dept.
Mines N.S.W., 1908, pp. 164-166.
‘Rep, J. H., 1930.—The Queensland Upper Palaeozoic Succession. Qld. Geol. Surv. Pwo.
No. 278. ;
RicHARDS, H. C., and BRYAN, W. H., 1924.—The Geology of the Silverwood-Lucky Valley
Area. Proc. Roy. Soc. Queensland, xxxvi.
RicHArRDS, H. C., BRYAN, W. H., and WHITEHOUSE, F.. W., 1932.—Preliminary Note on the
Geology of Mount Barney. Proc. Roy. Soc. Queensland, xliv, 1932.
SxEats, E. W., 1930-1932.—The Age, Distribution and Petrological Characteristics of the
Granites of Eastern Australia. Proc. Roy. Soc. Victoria, 43 (N.S.), 1930.
Voiszy, A. H., 1934.—An Interpretation of the Silverwood-Lucky Valley Upper Palaeozoic
Succession. Proc. Roy. Soc. Queensland, xlvi. ;
, 1936.—The Upper Palaeozoic Rocks in the Neighbourhood of Boorook and
Drake, N.S.W. Proc. LINN. Soc. N.S.W., Ixi, Parts 3-4.
, 1938.—Notes on the Stratigraphy of the Northern Territory with Special
Reference to the Jurassic System. Jour. Roy. Soc. N.S.W., 1xxii.
Wavkom, A. B., 1918.—The Geology of the Lower Mesozoic Rocks of Qld. Proc. LINN.
Soc. N.S.W., xliii.
GG
THE GEOLOGY OF THE LOWER MANNING DISTRICT OF NEW SOUTH
WALKS.
By A. H. Voisry,* M.Se., Lecturer in Geology and Geography, New England
University College.
(One map; one Text-figure. )
[Read 30th August, 1939.]
This paper deals with the general geology of the Lower Manning River District.
The accompanying map embraces parts of the counties of Macquarie and Gloucester
which lie respectively to the north and south of the Manning River. The area
is drained by the Manning and its tributaries, Lansdowne and Dawson rivers and
Cedar Party, Dingo and Burrill creeks.
The principal towns are Taree, Wingham, Coopernook, Cundletown, Mount
George, Croki, Harrington and Kramback.
Previous Literature.
No detailed account of the geology of the region has been published, but there
are a number of references to some of the occurrences of rocks within it.
J. HE. Carne (1896) described the rocks of the principal coastal headlands,
mentioning particularly Diamond Head, Halliday Point (Black Head) and Wallaby
Point. He regarded the last two as Carboniferous in age, but they are placed more
satisfactorily now as Devonian.
W. G. Woolnough in 1911 described the Cedar Party Limestone and underlying
beds, suggesting a glacial origin for some conglomeratic material. His tentative
correlations with the sequence on the Macleay River are not likely to be
challenged.
Devonian and Kamilaroi beds were discussed by W. N. Benson (1916, 1918)
and the occurrence of serpentine in the neighbourhood of Mount George was
recorded.
References to the alkaline intrusions in the neighbourhood of Lansdowne
have been made by C. A. Sussmilch (1932), W. R. Browne (1933), R. O. Chalmers
(1934) and others.
The writer has described portions of the area more recently (Voiséey, 1938,
1939a, 19396).
STRATIGRAPHY.
DEVONIAN.
All the rocks of undoubted Devonian age in the Lower Manning District are
found south of a group of faults which will be referred to as the Manning River
Fault System. These faults separate Devonian from the Carboniferous and
Kamilaroi rocks which occupy the country to the north of the Manning River.
* This paper was completed while the author was Linnean Macleay Fellow of the
Society in Geology.
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396 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
The complete Devonian sequence was not elucidated owing, in a large measure,
to the complexity of the structures and the lack of sufficient outcrops. It may be
possible to sort out the Devonian succession after a detailed geological survey of
the area, but as the Carboniferous and Kamilaroi rocks were the chief concern of
the present writer it was not found practicable to devote the necessarily large
amount of time to this project.
Benson (1916, 1918) and Sussmilch (1921) were in agreement that the
Devonian sequence closely resembles that of the type-area in the Tamworth District.
The suite in each case consists of characteristic banded claystones, tuffs, spilites,
agglomerates and breccias.
The beds will be discussed under the headings of the principal localities where
they were examined.
Bundook.
Fresh-looking, dense, pale green spilites containing well-preserved pyroxenes
and albitic felspars are beautifully exposed by railway cuttings all the way from
Bundook to Somerset (Benson, 1916). They continue eastwards to the Kanghat
Range, where they are responsible for this imposing feature which rises to over
2,000 feet. The spilites continue in a westerly direction beyond the limits of the
map.
Between Bundook and Gloucester, railway cuttings reveal banded mudstones,
tuffs, cherts and breccias of Devonian age. Quite close to Gloucester they give
way to the Carboniferous suite (Sussmilch, 1921).
Kundibakh.
Two miles south of Burrell Creek Post Office, along the Gloucester road, mud-
stones and sandstones associated with hard bluish tuffs outcrop. They contain
fragmental plant remains. Although these beds resemble those of the Burindi
Series to some extent, they are included with the Devonian on account of their
association with definite Devonian rocks south of the Kanghat Fault. They dip
in a south-easterly direction at 40 degrees.
Two and a half miles south of this occurrence in the Kramback Cutting are
coarse tuffs dipping steeply in a direction 30 degrees. They are very like those at
Tiri and contain the same kind of large angular shaly fragments. Associated with
them are greenish-grey mudstones and other fine-grained blue tufts.
Banded mudstones and tuffs may be followed in road cuttings along the Pacific
Highway to the neighbourhood of Mongrani Cutting near Gloucester.
Bucklebore Mountain. :
This spur from the main Kanghat Range is composed largely of coarse tuffs-
associated with spectacular volcanic agglomerates or tuff-breccias. Fragments of
green tuffs up to several inches across are cemented into a very hard and beautiful
rock, Fresh specimens of this may be obtained from large blocks in the scree on
the south bank of the Manning River at the bend about a mile south of Charity
Creek Railway Siding. }
Mount Kiwarric.
The north-eastern slopes of Mount Kiwarrie are composed of hard blue tuffs and
grey cherts with some interbedded igneous rocks, probably spilites. These beds
dip in a southerly direction at about 70 degrees near the head of Stoney Creek, a
tributary of Bow Bow Creek. In this locality they are intruded by serpentine.
Tinonee.
Typical Devonian banded claystones with interbedded coarse tuffs are exposed
by cuttings along the Taree—-Gloucester road between Tinonee and Bow Bow Creek.
BY A. H. VOISEY. 397
At Tinonee punt approach they dip in a direction 320° at 47°. A quarry about a
quarter of a mile from Tinonee on the Old Bar road reveals a good section of the
claystones which here dip in a direction 175° at 35°.
Dips are so variable in this region that it has not been possible to determine
the details of the structures even after numerous measurements have been taken.
Examination of the sections revealed by the Brushy Cutting and railway cuttings
near Wingham shows how futile it would be to attempt to map the folds and faults
with a limited number of measurements. The soft beds appear to have been folded
and crumbled along a number of different axes.
The banded claystones and tuffs extend eastward from Wingham to the coast.
Black Head.
Rock Platforms at Black Head expose a splendid variety of green tuffs inter-
bedded with banded claystones. The suite is similar to that met around Tinonee
and is undoubtedly Devonian in age. The strata vary in strike but generally dip
in a north-easterly direction at about 45 degrees. Numbers of small faults displace
the individual beds and are seen to great advantage on the rock platforms. The
tuffs have been twisted about in places and are partly silicified, containing
numerous veins of quartz.
Red Head.
One of the best places to examine the banded claystones is at Red Head, about
a mile north of Black Head. Wave action has cleared away weathered material
and polished the rocks so that the banding is particularly well displayed in dark
and light grey shades. The strata here dip south at 55 degrees.
Wallaby Point.
Carne (1896) placed the Black Head (Halliday Point), and Wallaby Point
rocks in the Carboniferous system, comparing them with the beds at Cape Hawke
where he found Carboniferous marine fossils. However, they correspond more
closely with the known Devonian rocks and are included now in that system.
Interesting intraformational structures occur in some bands of sandy mud-
stone interbedded with tuffs. Before consolidation of the laminated mudstones
they were puckered and folded.
Fragmental plant remains are abundant in the tuffs but no identifiable
material was found. According to Carne (1896) grits and conglomerates are
present. He was impressed by the “‘concretionary weathering of some of the
sandstones”.
Doubtful Occurrences of Devonian Rocks.
Johnston's Peak.
Jaspers and quartzites are exposed by Little Run Creek west of the serpentine
belt at Wherrol Flat and are responsible for the presence of an elevated block of
country which rises to a sharp, peculiarly-shaped summit called Johnston’s Peak.
The higher portions of this rugged region were not examined, but it is assumed
that the siliceous rocks are continuous from Wherrol Flat to the neighbourhood
of Mount George (Voisey, 1939a).
No evidence was found to indicate the stratigraphical position or age of these
beds. Abutting serpentine at Wherrol Flat and Mount George, they are believed
to be related to it as the Woolomin Series of Benson (19130) is related to the
basic intrusives of the Nundle District.
398 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
Strathcedar.
On the road to Mooral Creek, about 24 miles from its junction with the
Wingham—Comboyne Road, oceur some rocks which bear a strong lithological
resemblance to those of the Devonian suite. They are included on the map with
the Carboniferous beds since they are surrounded by sediments of that age and are
some miles from any other known Devonian occurrence.
They outcrop alongside the road for less than a mile but, as exposures are poor,
their extent was not determined nor was their relationship to the adjacent
Carboniferous glacial beds ascertained. The rocks consist of cherts and tuffs
having, in part, a light green colour which is especially typical of the Devonian
beds near Bungay (two miles south of Wingham) and in railway cuttings east
of Wingham. Banded claystones are also present.
If the age of the rocks really is Devonian, this anomalous occurrence can be
explained only by very strong faulting.
Coopernook.
Alongside the road between Langley Vale and Coopernook Railway Station,
road-material quarries expose tuffs and banded claystones which resemble Devonian
rock-types. As in the case of the Strathcedar beds, the locality is so far removed
from other Devonian areas that doubt is thrown upon lithological correlations and
a Carboniferous age is preferred. The strata dip in a direction 98° at 55°.
Correlations.
Although the Devonian sequence has not been worked out on the merits of
the outcrops in the area under discussion, the rock types may be correlated, more
or less, with those of the Tamworth and Nundle districts (Benson 1913a, 19135).
Benson (1916, 1918) and Sussmilech (1921) were:agreed on this point after
examining the sections from Mount George to Gloucester.
Woolomin Series.
The jaspers and quartzites occurring between Mount George and Wherrol
Flat are correlated tentatively with the Woolomin Series (Benson 1913a). No
tuffs, slates or phyllites, however, were found to correspond with those in the
Nundle District. Since the siliceous rocks appear to be related to the intrusion
of serpentine, it is unsafe to place them on any fixed stratigraphical horizon.
Tamworth Series.
Benson (1918) assigned the spilites of Kanghat Mountain to the Middle
Devonian. The tuff-breccias and agglomerates of Bucklebore Mountain suggest a
position in the sequence analogous to the Upper Breccias of the Bowling Alley
(= Tamworth) Series at Nundle. Here the association of such breccias and spilites
was remarked upon by Benson (1913b).
By far the most widespread rocks of Devonian age are the banded claystones,
possibly containing radiolaria. They are referable to the Tamworth Series, some
of them belonging probably to the upper, banded, radiolarian claystones (Benson
1916), but their relationship to the spilites and tuff-breccias could not be
ascertained.
Baldwin Agglomerates.
The Kundibakh tuffaceous deposits could belong to the Baldwin Agglomerates.
Benson, however, recorded beds of this type from the Tamworth Series, and they
resemble some Carboniferous types, so that again correlation is doubtful.
BY A. H. VOISEY. 399
Barraba Series.
Beds referred to the Barraba Series by Sussmilch (1921) occur in the
Gloucester District and might be expected to outcrop to the east and north-east.
What appear to be members of this series are exposed by road cuttings between
Kramback and Nabiac, immediately to the south of the area shown on the map.
Palaeontology.
Numerous fragmental plant remains were found in the Devonian rocks, but
none were sufficiently well preserved to allow identification.
Mr. Les. Weller of Nabiac brought in several well-preserved specimens of
Lepidodendron australe from the neighbourhood of Wang Wauk, several miles
south of the area mapped. It was in this locality that the writer was shown the
same fossil by Dr. G. D. Osborne in 1933.
CARBONIFEROUS.
The Carboniferous beds have been divided into three series. These, with
approximate thicknesses, are.as follows (in descending order):
Feet.
Kullatine Series SS a RT cer ee em re Te ee Belo DO)
Upper BurindiSerieés-s2) 5 8s. se. ee Se ead) os 7 4,000
Lower Burindi Series .. .. ae ate) 4,000.4
The Kullatine Series is very variable in thickness and probably exceeds the
amount given above in some localities. The fact that it consists largely of tillite
in which bedding is poorly developed renders elucidation of structures very difficult,
and the presence of numerous faults has further interfered with stratigraphical
work.
The Upper Burindi Series has been examined only in the neighbourhood of
Taree (Voisey, 1938) and has not been located anywhere else, although it may well
occur in a number of other places.
The Lower Burindi Series is very well developed throughout the area. Its
downward limit has not been found, since faults intervene between the series and
the Devonian beds. The estimate of 4,000 feet is very conservative since sections
of strata which do not correspond with the measured thickness of about 2,500 feet
(Voisey, 1938) are known.
The Carboniferous beds are not differentiated on the accompanying map on
account of its small scale.
Lower Burindi Series.
Everywhere that Devonian and Carboniferous strata have been found in contact
in the area, faults have separated them. This would appear to be the case also
to the west of Gloucester, in the Copeland District, where C. A. Sussmilch (1921)
has reported a contact between Devonian and Carboniferous rocks.
The beds consist, for the most part, of mudstones and tuffs, the last-named
being very variable in character.
Along the Nowendoc Road between Mount George and Caffrey’s Flat, notably
beside the Nowendoc River, there are good exposures of the series together with
the tillites of the Kullatine Series. Beds of tuffs several feet thick are separated
by olive-green mudstones containing plant remains. The general dip is in a
direction 190° at 65°. Between Wingham and Wherrol Flat similar rocks are
exposed in road cuttings. Some of the hard, massive tuff bands may be traced
across the country for short distances, usually being cut off by faults.
Members of the Lower Burindi Series occupy most of the country between the
Manning River and Wherrol Flat.
400 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
At Tiri, where the road from Mount George to Bundook crosses the Manning
River, there is a light bluish-grey tuff, very hard and splintery, consisting of rock
fragments up to several inches in diameter set in a tuffaceous groundmass.
Occasional angular inclusions of grey shale up to two or three inches across are
found scattered through the beds. With them are quite large plant stems. These
are particularly abundant in the road cuttings on the northern side of the bridge.
None of those collected were sufficiently complete to allow identification.
Associated with the Kullatine Series, Lower Burindi beds cover a large area
in the watersheds of Dingo Creek and its tributaries, and continue for an undeter-
mined distance to the west.
Mention has been made already of the sequence in the Taree and Wingham-—
Mount George districts (Voisey, 1938 and 1939a).
At Cundletown banded olive-green mudstones dipping in an easterly direction
at about 30° outcrop in road cuttings. Further east, tuffs, sandstones and mud-
stones occur on Oxley Island.
Woolnough (1911) recorded Knorria from Carboniferous tuffs and mudstones
at Crowdy Head. These rocks have been quarried and brought south to Harrington
and used in the construction of the breakwater at the entrance to the Manning
River. During the quarrying operations a specimen of a fossil fish was found and
forwarded to the Government Geologist, who submitted it to A. Smith Woodward
for identification (Smith Woodward, 1900-1904). Having been led to the belief
that the beds in which the remains were found were Mesozoic, Woodward referred
the imperfectly preserved specimen to the genus Atherstonia. He named it
tentatively Atherstonia australis and suggested that the rocks in which it occurred
belonged to the Hawkesbury Series. The matrix in which the fish is preserved
is identical with the Crowdy Head tuffs and other Carboniferous types and there
is no chance of it belonging to the Triassic suite. Another fossil fish has been
presented to the Australian Museum recently. It is set in a similar matrix and
comes fxom the same locality as the supposed Atherstonia. The fish may belong
to the Crossopterygii, a Palaeozoic group.
A small area of mudstones and tuffs which are similar to the Crowdy Head
types occurs at Harrington. The beds are practically horizontal, a most unusual
disposition for Palaeozoic strata in this region.
Upper Burindi Series.
The Upper Burindi Series consists of mudstones, sandstones and the Taree
Limestone which contains Aphrophyllum hallense Smith, Lithostrotion stanvellense
Hth. fil., and Lithostrotion columnare Eth. fil.
The only part of the area in which the series is known to be developed has
been described previously (Voisey, 1938).
Kullatine Series.
The Kullatine Series has a wide distribution throughout the Lower Manning
District. Together with the Macleay Series it occurs in a number of places along-
side the Manning River between Tiri and Hillview. Its occurrence here has been
described already (Voisey, 1939qa).
Tillites and tuffs outcrop in association with the Lower Burindi Series beside
the Nowendoc River in the neighbourhood of Caffrey’s Flat. In this region the
Kullatine Series appears to pass conformably downward into the Lower Burindi
Series without any intervening Upper Burindi Series.
Beautiful examples of the glacial beds occur alongside the road which follows
the western branch of Dingo Creek north of Wherrol Flat. The fluvio-glacial
BY A. H. VOISEY. 401
character of massive conglomerates constituting part of the glacial stage is demon-
strated by the presence of numerous rounded boulders of igneous rocks cemented
together by material identical with the matrix of the typical tillite.
Further outcrops of tillite are exposed by the Bulga road which follows the
eastern branch of Dingo Creek. The rocks are seen to advantage on the ascent
to the Bulga Plateau from Bobin Flat. They were shown the writer at Bilen-
borough Falls by Dr. G. D. Osborne in 1938, and were mentioned by R. O. Chalmers
(1934, p. 175).
In the neighbourhood of Strathcedar tillites are intruded by serpentine.
A high ridge composed principally of glacial beds of the Kullatine Series runs
northwards from Khatabunda near Wingham to the Comboyne. The beds dip
under the Macleay Series which lies to the east.
It would appear that the glacial beds become thinner going from the west of
the area to the east. They exceed 2,000 feet in thickness in the neighbourhood of
Kimbriki and are no more than 500 feet at Taree. The light-coloured tuffs under-
lying the glacial stage near Taree have not been found west of Wingham (Voisey,
1938). They may have passed into darker tuffs resembling those of the Lower
Burindi Series, but this point has not been established.
Carboniferous lavas and tuffs have been described from the Gloucester District
by C. A. Sussmilch (1921). They have been correlated with the Kuttung Series of
the Hunter River. These rocks are shown on the map to the east of Gloucester,
forming the eastern limb of the Gloucester Syncline or Trough.
KAMILAROI: Macleay Series.
The only Kamilaroi beds which have been found outside the areas dealt with
previously (Voisey, 1938, 1939a) occur just south of the Comboyne Plateau and in
the neighbourhood of Tiri.
In the first case they overlie the Kullatine Series which occupies the ridge
west of the Wingham—Comboyne road and dip away in an easterly direction.
A road cutting near the last bridge over Killabakh Creek before the ascent to
the Comboyne Plateau (portion 32, parish of Marsh) reveals purple shales
containing angular pebbles. These shales closely resemble the Tait’s Creek Glacial
beds (Woolnough, 1911) which have been compared with the Lochinvar shales in
the Hunter Valley sequence.
About two miles south of the above-mentioned locality near Killabakh School
(portion 32, parish of Marsh) a road cutting exposes impure limestones. The
spongy weathered material derived therefrom yields well-preserved Kamilaroi
marine fossils. Those collected were identified by Mr. H. O. Fletcher as: Fenestella
spp., Crinoid stems, Spirifer sp. indet., Linoproductus springsurensis Booker,
Aviculopecten sprenti Johnston, Pleurotomaria cf. morrisiana McCoy (abundant),
and Phillipsia sp. (Specimens 38133-4 Australian Museum Collection.)
These limestones overlie the purple shales and tuffaceous rocks and are
followed by light grey micaceous mudstones.
Along the road from Mount George to Bundook, south of the bridge across the
Manning River at Tiri, road cuttings reveal micaceous mudstones, sponge-spicule
tuffs and other members of the Macleay Series. Marine fossils similar to those at
Kimbriki were found (Voisey, 1939a). The beds were associated with tillites
belonging to the Kullatine Series.
TRIASSIC: Camden Haven Series.
Conglomerates, sandstones and shales comprising the lower beds of the
Camden Haven Series outcrop to the north of the Lansdowne River. These
402 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
Triassic rocks form the southern margin of the Lorne Triassie Basin which was
described in an earlier publication (Voisey, 1939b).
PLEISTOCENE TO RECENT.
Raised river gravels occur at varying heights above the Manning River. They
may be referred to the Pleistocene period.
A large area of country has been reclaimed from the sea. This extends from
Taree to the coast, with the exception of some hills of older rock which rise above
the plain of recent accumulation. The lower beds are marine or estuarine sands
and muds with bands of shells. They pass up into river alluvium or swamp
deposits.
I@NEOUS ROCKS.
Serpentine.
Serpentine has been located in four places in the area: (1) Mooral Creek,
(2) Wherrol Flat, (3) Mount Kiwarric and (4) Mount George.
1. Mooral Creek.—Serpentine is seen from the Wingham—Mooral Creek road
and may be traced for several miles in a north-easterly direction from Strathcedar
Public School to the small village of Mooral Creek. It is intrusive into tillites
belonging to the Kullatine Series. One block of tillite was found caught up in
the basie rock near the Strathcedar School.
2. Wherrol Flat.—A belt of serpentine crosses Dingo Creek south of Wherrol
Flat Hall and, passing through the settlement, continues for some distance to the
north. Contact altered Carboniferous tuffs were found beside the intrusion.
3. Mount Kiwarric.—Serpentine occurs on the north-eastern slopes of Mount
Kiwarric at the head of Stoney Creek, a tributary of Bow Bow Creek. It is
intrusive into Devonian rocks. This occurrence and that at Wherrol Flat (Glen
Lewis) were referred to by Benson (1918).
4. Mount George—tThis belt of basic rock has been mentioned previously by
Benson (1916, 1918) and mapped by the writer (Voisey, 1939). Tillites of the
Kullatine Series, tuffs of the Lower Burindi Series and Kamilaroi mudstones
appear to be the contact rocks.
The Age of the Serpentine.
The age of the serpentine has been discussed in a previous publication (Voisey,
1939a) and will be dealt with also under the heading Structural Geology.
As has been pointed out, it is intrusive into Devonian, Carboniferous, and
probably Kamilaroi rocks and cannot be pre-Kamilaroi in age. The only evidence
previously brought forward to suggest that the rock is olderyconsists of a pebble
of serpentine in Kamilaroi beds and the presence of “Permo-Carboniferous” rocks
apparently overlying the Peel Thrust (Benson, 1913, p. 511). With reference to
the pebble, such evidence cannot be regarded as definite proof of a pre-Kamilaroi
age for the rocks of the Great Serpentine Belt since it may have come from quite
another locality. In the second case Benson admits that the beds are not clearly
exposed and direct proof is impossible. S. W. Carey (verbal communication)
suggests that the beds may be infaulted, and with this view the writer agrees.
That the serpentine is of late Kamilaroi age may be taken now as established
beyond reasonable doubt.
Alkaline Intrusives.
A large number of plugs of alkaline rock, including comendites, arfvedsonite-
anorthoclase-trachyte, bostonite, etc. (Browne, 1933), occur principally about the
BY A. H. VOISEY. 403
headwaters of Killabakh Creek and the Lansdowne River along the southern
margin of the Comboyne Plateau (Sussmilch, 1932; Chalmers, 1934; Voisey, 1939b).
STRUCTURAL GEOLOGY.
The structural features of the district may be considered in six sections:
1.—The Lorne Triassic Basin and Associated Intrusives.
2.—Folded Carboniferous and Kamilaroi rocks north of the Manning River
Fault System.
3.—Tightly folded Devonian rocks south of the Manning River Fault
System.
4—The Gloucester Syncline.
5—The Manning River Fault System.
6.—Serpentine Faults.
1.—Triassic sediments lie with a violent unconformity on the Palaeozoic beds.
The unconformable junction may be followed with ease from the neighbourhood
of the Comboyne Plateau to Coopernook. Basal conglomerates and sandstones
present a line of vertical cliffs which resemble, in a small way, those of the
Hawkesbury Sandstone in the Blue Mountains.
The strata dip at a low angle towards the centre of the Basin which lies to
the north of the area embraced by the map. West of John’s River, intrusions of
alkaline rock have lifted the beds and have the form of sills and laccolitic bodies
(Voisey, 1939b).
2.—South and west of the Triassic basin are Carboniferous and Kamilaroi
sediments which have been folded on a general meridional axis. These folds have
been broken extensively by faults (Voisey, 1938, 1939a).
Yielding Kamilaroi beds have been overfolded near Kimbriki, but the more
resistant Carboniferous beds have been extensively fractured and, in places, such
as Cedar Party, thrust over the Kamilaroi strata.
Two synclines and an anticline were mapped north of Wingham and Taree.
The anticline has given way along the Cedar Party Fault and the syncline on its
eastern side along the Dawson Fault. In each case the overthrusting has been
from east to west and Carboniferous beds have been pushed over those of the
Kamilaroi.
The exact position of the Dawson Fault has not been determined on account
of the exceedingly poor outcrops of Kamilaroi micaceous mudstones on the west
and Burindi mudstones and tuffs on the east. Similarly its probable continuation
along the course of the Lansdowne River has been inferred from the presence of
Burindi beds along the Koppinyarratt road to the Comboyne and the presence of
Kamilaroi sediments along the Killabakh Creek road. In most of the intervening
area Kamilaroi mudstones are suspected on account of the low ground, grey soil,
and lack of outcrops. The duplication of the Taree Limestone in the Upper Burindi
Series in and near the limestone quarries at Taree and the disturbed disposition
of the beds are evidence of the presence of the fault in that locality.
Between Wingham and Wherrol Flat, strikes are exceedingly variable and
indicate extensive faulting. One fault running east and west is shown on the
map. This is suggested by a change in the general direction of strike from north-
west—south-east to north—south. Again, however, there are many departures
from these general directions, and details of the faulting were not obtained.
The Kimbriki Anticline (Voisey, 1939a) is the most important of the folds
in the western part of the area. Along its nose the Kamilaroi beds are folded
into asymmetrical anticlines and synclines on a meridional axis. The tilt of the
axial plane of the syncline nearest to “Colraine’” is towards the west.
404 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
3.—The resistant spilites, agglomerates and tuffs of Devonian age constituting
the Kanghat and Kiwarric ranges have been folded, for the most part, on an east-
west axis. The less-resistant banded claystones and tuffs have been very tightly
folded into anticlines and synclines. The amplitude of these folds is small and
they have been broken at the crests so that many beds are vertical in disposition.
Splendid examples of the folding are to be seen in railway cuttings west of
Wingham and at the Brushy Cutting on the Wingham—Tinonee road. Examination
of these has been sufficient to convince the writer that any detailed interpretation
of structures, which might be based on the limited outcrops available elsewhere,
is likely to be quite unreliable.
4—The Gloucester Syncline has been described by C. A. Sussmilch (1921)
and is shown on this map in order to demonstrate its proximity to the beds of the
Lower Manning District. South and east of the syncline are regions where
meridional strikes predominate.
The geological structures between this syncline and the well worked out areas
of the Hunter Valley have been discussed by G. D. Osborne (1938).
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5.—The most important structural feature in the Lower Manning District is
the Manning River Fault System, which must rank among the largest fault
systems in the State. It comprises the Kanghat, Hillview, Killawarra, Wingham
and probably the Charity Creek faults. The principal fault in the group, the
Kanghat Fault, runs from the coast near Black Head for a distance of at least 30
miles to the west-north-west. At Tiri it is still very powerful, since Devonian and
Kamilaroi rocks are in contact with one another. It is to be expected, therefore,
that it continues westward for many miles into the Upper Manning District. The
displacement of the beds must have been very great indeed, since 7,000 feet, at
least, of Carboniferous beds have been faulted out, as well as quite that amount of
Devonian beds. In addition, the Kanghat Range is 2,000 feet higher than the
Kamilaroi beds beside the Manning River. Thus an estimate of a minimum
displacement of three miles is suggested. Lateral as well as vertical components
are involved and it is more than likely that the amount of movement was consider-
ably greater than the minimum calculated above.
The Kanghat Fault cuts across the strike of the spilites which were not found
along the Pacific Highway which follows Burrill Creek through the Kanghat—
Kiwarriec ranges. The accompanying map (p. 395) shows how clearly the fault
transgresses the strikes of the Kamilaroi and Carboniferous rocks.
Lying to the north of the Kanghat Fault is an area of Devonian strata bounded
by the Hillview, Killawarra and Wingham faults. Between the Kanghat and
Hillview faults is a sunken block through which portion of Upper Bow Bow Creek
flows.
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Section along line A-B on Map 1. V/H = 1/1.
BY A. H. VOISEY. 405
The Wingham Fault separates Lower Burindi and Kullatine beds from
- Devonian claystones in the neighbourhood of Wingham. It is obscured by alluvium
south-east of Kolodong, but there cannot be any reasonable doubt that it continues
for some distance to the east, since Carboniferous rocks lie north of the river and
Devonian rocks to the south. The displacements along this fault and Killawarra
fault are comparable in amount to that of the Kanghat Fault since they separate
Devonian from Carboniferous and Kamilaroi beds.
The Charity Creek Fault is probably part of the Manning River Fault System
but its throw is not so great as that of the other members mentioned above. It
separates Kullatine from Lower Burindi Rocks and runs from Charity Creek
railway siding to the neighbourhood of Killawarra siding.
6.—It is assumed by analogy with the Great Serpentine Belt of N.S.W. (Benson,
1913, etc.) that the serpentine in the Lower Manning District was introduced
along fault planes.
The serpentine near Mount George appears to follow a fault which separates,
in places, Carboniferous tillites from Kamilaroi micaceous mudstones. It cuts
across the strike of the Kamilaroi strata and apparently of smaller faults which
bring them into contact with tillites (Voisey, 1939a).
Actual contacts between serpentine and Kamilaroi beds are obscured and,
hence, there must remain a slight doubt as to whether the latter are intruded. It
does not seem to be possible, however, to reconcile the observed facts with the
supposition that the serpentine was faulted into its present position after being
injected prior to the deposition and folding of the Kamilaroi and Carboniferous
sediments.
At Wherrol Flat the serpentine fault separates jaspers and quartzites from
Carboniferous tuffs, ete. Owing to doubt as to the age and origin of the material
from which the siliceous rock was derived no estimate can be made of the order
of magnitude of its throw.
The serpentine at Mount Kiwarric is in Devonian beds but is cut off. by the
Kanghat Fault. It is probable, therefore, that the basic rock was injected before
the Manning River Fault System dislocated the strata.
Age Relations of the Folding and Faulting.
In the Gloucester District Sussmilch (1921) described an interesting sequence
from Devonian into Carboniferous beds. An examination of some of the country
between Gloucester and Copeland did not yield any evidence of a major orogenic
movement between the two sequences.
On account of the intensity of the pressure which affected the Kamilaroi
sediments, in a manner comparable to the crumpled condition, of Devonian clay-
stones in the Lower Manning District, it has not been found possible so far to
distinguish any orogenic movement between the deposition of these two formations.
The less distorted, but faulted, intervening sequence of the Carboniferous System
owes much to its massive and competent units.
Wherever met in the field in the area shown on the map, the boundary between
Carboniferous and Devonian strata was found to be a faulted one.
Genetically related to the folds in the Palaeozoic beds are the faults in the
crests and the troughs of such folds, e.g., the Cedar Party Fault and the Dawson
Fault. Many smaller related faults observed from time to time in the field have
not been mapped, but may be referred to this first group of movements.
The available evidence indicates that the faults containing the serpentine cut
across the folds and faults mentioned above. In turn, however, these are truncated
by the Manning River Fault System.
406 GEOLOGY OF LOWER MANNING DISTRICT, N.S.W.,
Since Triassic sediments overlie both folded Palaeozoic beds and serpentine
(Voisey, 19390) there can be no doubt that the folding and intrusions may be
assigned to the late Palaeozoic orogeny. In order to limit the possible age of the
Manning River Fault System it is necessary to consider similar structures in other
areas.
The Manning River Fault System may be compared in certain respects with
the Hunter Overthrust (Osborne, 1929), Mooki Thrust System (Carey, 1934) and
Peel Thrust (Carey and Browne, 1938). In each case doubts have arisen regarding
the ages of the movements. The question has been discussed by Osborne (1929,
p. 449), Raggatt (1929, p. 278) and Carey (1934, p. 373). No direct evidence was
available to these workers to determine whether the diastrophism affecting the
regions which they discussed was pre- or post-Triassic. Carey (1934, p. 373),
however, showed that the Mooki Thrusts, which were continuous with the Hunter
Overthrust, were parallel to the fold axes and in all probability belonged to the
same movement. Carey and Browne (1938) further developed this theme and
included with the Hunter—Mooki thrusts most other structures developed in the
Palaeozoic rocks and referred them to the late Palaeozoic orogeny, the Hunter—
Bowen Movement.
Now that the serpentine associated with the Peel Thrust has been shown to
intrude Upper Carboniferous and probably Kamilaroi rocks there is little doubt
that the writers mentioned above will welcome the opportunity to include not only
the Peel Thrust, but the Manning River Fault System in their well developed
scheme.
Further, if it is agreed that the serpentine belongs to the same orogeny, the
fact that this rock is overlain by Triassic sediments (Voisey, 1939b) must be
admitted as evidence of a pre-Triassic age for the Hunter-Bowen Movement.
Summary of Structural Geology.
1.—Devonian, Carboniferous and Kamilaroi rocks were folded on a general
meridional axis. All the observed folds were fractured generally at the crests and
troughs.
2.—Closely following on this folding fractures developed and serpentine was
injected into them.
3.—The Manning River Fault System displaced the rocks and all previously
developed structures for distances of the order of several miles.
4.—After extensive erosion, Triassic sediments were laid down upon the
upturned edges of the Palaeozoic strata and serpentine.
5.—The Triassic sediments were folded, faulted, and, later, intruded by alkaline
rocks in the form of laccolites and sills.
CONCLUSION.
An outline has been given of the stratigraphy of the Lower Manning District.
Certain structural features have been described, among them the Manning River
Fault System consisting of a group of large and important faults.
It has been suggested that the age of the serpentine is late-Kamilaroi, and
evidence produced in favour of this alteration in the accepted views.
The stratigraphical position of the alleged Atherstonia australis has been
changed from Triassic to Carboniferous.
Bibliography.
BENSON, W. N., 1913a.—The Geology and Petrology of the Great Serpentine Belt of N.S.W.
Part i. Introduction. Proc. LINN. Soc. N.S.W., xxxviii.
BY A. H. VOISEY. 407
Bunson, W. N., 1913b.—The Geology and Petrology of the Great Serpentine Belt of N.S.W.
Part ili. Petrology. Proc. Linn. Soc. N.S.W., xxxviii.
———., 1916.—The General Geology of the Gloucester District. Jour. Roy. Soe.
N.S.W., 1.
, 1918.—The Geology and Petrology of the Great Serpentine Belt of N.S.W.
Part viii. The extension of the Great Serpentine Belt from the Nundle District to
the Coast. Proc. LINN. Soc. N.S.W., xliii.
BROWNE, W. R., 1933.—An Account of Post-Palaeozoic Igneous Activity of N.S.W. Jour.
Roy. Soc. N.S.W., 1xvii.
CAREY, S. W., 1934.—The Geological Structure of the Werrie Basin. Proc. LINN. Soc.
N.S.W., lix.
CarEY, S. W., and Browne, W. R., 1938.—Review of the Carboniferous Stratigraphy,
Tectonics and Palaeogeography of New South Wales and Queensland. Jour. Roy.
Soc. N.S.W., |xxii.
CARNE, J. H., 1896.—Geology and Mineral Resources of the Coast between Port Macquarie
and Cape Hawke. Ann. Report Dept. Mines N.S.W., 1896.
, 1908.—The Geology and Mineral Resources of the Western Coal-field. Mem.
Geol. Surv. N.S.W., Geology No. 6.
CHALMERS, R. O., 1934.—The Mid-North Coast. Aust. Musewm Mag., v.
Davip, T. W. E., 1932.—A New Geological Map of the Commonwealth of Australia.
OSBORNE, G. D., 1929.—The Structural Geology of the Carboniferous Rocks in the Hunter
River District, etc. Proc. LINN. Soc. N.S.W., liv.
--, 1938.—On Some Major Geological Faults North of Raymond Terrace, etc.
Jour. Roy. Soc. N.S.W., 1xxi.
Raceatt, H. G., 1929.—Note on the Structural and Tectonic Geology of the Hunter Valley,
ete. Proc. LINN. Soc. N.S.W., liv.
SmItTH-Woopwarp, A., 1900-1904.—On Atherstonia australis and Ctenolates avus, etc.
Rec. Geol. Surv. N.S.W.,. vii, p. 88.
SussmitcH, C. A., 1921.—The Geology of the Gloucester District. Jour. Roy. Soc.
N.S.W., 1.
, 1932.—Relation of the Tertiary Alkaline Rocks of Eastern Australia to Late
Tertiary Tectonic Lines. Jour. Roy. Soc. N.S.W., xvi.
Voisny, A. H., 1938.—The Upper Palaeozoic Rocks in the neighbourhood of Taree. Proc.
Linn. Soc. N.S.W., Ixiii.
—, 1939a.—The Upper Palaeozoic Rocks between Mount George and Wingham,
N.S.W. Proc. LInn. Soc. N.S.W., Ixiv.
———_——_, 1939b.—The Lorne Triassic Basin and Associated Rocks. Proc. Linn. Soc.
N.S.W., Ixiv.
WooLNouGcH, W. G., 1911.—Preliminary Note on the Geology of the Kempsey District.
Jour. Roy. Soc. N.S.W., xv.
408
A NOTE ON THE SYNONYMY OF LEPTOPS (COLEOPTERA:
CURCULIONIDAE).
By KeituH C. McKeown, Assistant Entomologist, Australian Museum.
(Contribution from the Australian Museum.)
[Read 30th August, 1939.]
Family CuRCULIONIDAE.
Subfamily ENTIMINAE (= Leptopinae).
Tribe STENOCORYNINI (= Leptopini).
BARYOPADUS Pascoe (= Leptops Schoenherr, nom. praeoc.).
The above are changes in subfamily, tribe, and generic names rendered
necessary by the fact that the name Leptops Schoenherr for the well-known genus
of Australian weevils is preoccupied by Leptops Rafinesque, a subgenus of Cat-fish.
It is unfortunate that a name so familiar to entomological workers should be
displaced but, by the law of priority, there appears to be no alternative.
The genus Leptops was founded by Rafinesque in 1820 (Ichthyol. Ohiensis,
[Dec.] 1820, p. 64); the coleopterous genus, by Schoenherr, founded on the geno-
type robustus Olivier, 1807 (Curculio), in 1834 (Genera et species Curculionidum,
mt (QD), wey 1s ZO).
The genus Leptops must now be known as Baryopadus Pascoe (Trans. Ent. Soc.
Lond., 1870, p. 186), a genus erected for the reception of B. corrugatus, a species
which Lea (Ann. Soc. Ent. Belg., 1906, p. 318) proved conclusively to be a Leptops,
on these grounds: ‘This species, an unusually short, robust insect which certainly
looks somewhat aberrant for Leptops, was described as the type of a new genus
Baryopadus; but I am convinced that it belongs to Leptops. Pascoe briefly defined
the genus, stating that its most peculiar feature was the tarsi, but these are
exactly as in superciliaris and other species of Leptops. Its antennae, rostrum
and tarsi are almost exactly as in superciliaris, the sculpture of the elytra of the
same character, and certainly the two belong to but one genus; just as certainly as
superciliaris and squamosus are congeneric, and the latter is quite a normal
Leptops.” I consider that Lea’s contentions are sound.
Baryopadus is listed separately by Shenkling and Marshall in Junk’s Catalogus
Coleopterorum, pars 114, and reference to Lea’s paper has been omitted.
I am indebted to Mr. F. H. Taylor, School of Public Health and Tropical
Medicine, University of Sydney, for drawing my attention to the fact that Leptops
could not stand, and to Dr. E. J. White, of the British Museum of Natural History,
for supplying certain references.
409
THE DIPTERA OF THE TERRITORY OF NEW GUINEA. XI.
FAMILY TRYPETIDAE.
By JoHn R. Matitocn, Arlington, Va.
(Communicated by Frank H. Taylor, F.R.E.S., F.Z.8.)
(Plate xi; fifteen Text-figures. )
[Read 30th August, 1939.]
In this paper I present a review of this family on the basis of materials in
hand, the Australian species available to me, and the rather sparse literature of
the New Guinea region. I make no attempt to deal with the many Australian
species of the genus Dacus, sens. lat., but I present records of the few species of
the group now before me.
Below I give a synopsis of the various groups reviewed in the paper. While in
the main this will apply to the family in other faunal regions, there are several
segregates not represented in this region, and in its circumscribed form a strict
application of the synopsis will undoubtedly result in misleading associations of
some extralimital genera or species if applied to the latter. I have included
certain extralimital genera in my keys merely for comparative purposes or because
it appears to me that they may yet be found in this region.
I have to thank Mr. Frank H. Taylor for his kindness in supplying me with
most of the materials dealt with and for undertaking the final preparation of the
manuscript and making most of the figures to illustrate the paper. A few species
I have had the opportunity of examining in the collection of the United States
National. Museum, the wing of one type-specimen being figured for me by Mr.
C. T. Greene of that Institution. Some of the specimens belong to me; I have
also had the opportunity of including in this report data derived from a study
of specimens, belonging to tiie imperial Institute of Hntomology, taken in the
Solomon Islands, these latter forming the basis for a separate paper.
Key to the Subfamilies.
1. Ocellar and postvertical bristles almost invariably lacking, rarely represented by
microscopic hairs, the postocular cilia short, almost undeveloped; thorax without
the presutural, dorsocentral, and sternopleural bristles, humeral present in only
one or two species; antennae slender, the third segment rarely less than three
tmestas lone sas wilder ies yar bhenctay yaa Siok o Med sdaree setae: SUatataletane Sa wl aha tes Dacinae
Some or all of the above bristles present on head and thorax, postocular cilia always
distinct; third antennal segment usually distinctly less than three times as long
Ee Vfalna (100 (Ten A oe DECH ONCE PHCN DRO RORCRERORCRC HOR NC ENROL OIG DecR Ace ink CROLENT ENCES ee aCNE RS IGT) Chee 2
Costa of the wing with a deep cleft at apex of the subcostal vein, the costa with a
definite angle at anterior side of the cleft and at tip of the angle with a pair of
well-developed bristles; genus from this region with a pair of long strong erect
bristles in front of the ocelli on the interfrontalia .............. Schistopterinae
Costa of the wing with no, or a hardly perceptible, break at apex of the subcostal
vein, with or without a pair of bristles at that point; no genus with a pair of
long strong erect bristles in front of the ocelli on the interfrontalia ........ 3
lo
HH
410 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
3. Postocular cilia black or dark brown, fine at tips; scutellum with from two to ten
marginal bristles; sixth abdominal tergite of the female usually distinctly shorter
Or at leastimot loner thanwtnennitthenrctesc saicieieieaeesereie eters eine Trypetinae
Postocular cilia yellow or yellowish-white, stout and rather blunt at apices; scutellum
with two or four bristles on margin; sixth abdominal tergite of female usually
longer: than MLth ss srccnc cra ncesnetans tev eieie arn eresere: oye, 1, oe ORT Cosas eS Tephritinae
Subfamily DaAcInar.
I include two tribes in this subfamily, but Adraminii has sometimes been
given subfamily rank. The two tribes may be distinguished as below.
A. Posterior basal cell of the wing much wider than the anal cell, the vein on its
anterior side much curved up at its base so that the cell is almost as wide at
its base as at its apex; lobe of the anal cell usually longer than the free part
of the anal vein; pleurotergite without fine erect hairs ................ Dacinii
AA. VPosterior basal cell of the wing not, or very little, wider than the anal cell, the
vein on its anterior side not noticeably curved forward at its base; lobe of the
anal cell not nearly as long as the free part of the anal vein; pleurotergite
almost invariably with erect hairs on part of its surface .......... Adraminii
Tribe DaAcrInit.
I am not dealing in a complete manner with this tribe as there are so few
species in the New Guinea material before me. The few that are in the collection
include representatives of four subgenera: Callantra Walker, Chaetodacus Bezzi,
Zeugodacus Shiraki, and Bactrocera Guérin. Of these the first listed has been
considered as a genus by Hendel, but an intensive study of all the species from all
the faunal regions where the genus Dacus, sens. lat., occurs is essential to a definite
conclusion on the matter of generic and subgeneric segregations and this I am not
prepared to make at this time. I present below a key to the species now available,
with a full realization of the fact that there must be many more species in New
Guinea that are unrepresented in this collection.
Key to the New Guinea Species.
1. Abdomen elongated, with a slender basal petiole which has a short pointed tubercle
on each lateral basal angle, the apical bulbous portion of the abdomen in the
female prominently convex; wing with a broad dark-brown costal border that
extends to, or almost to, the fourth vein on its entire extent; scutellum short,
broadly rounded in outline, with two bristles (Callantra Walker) Tapeehe EN EBD
5 RB RS Ca ora oho ot Ceol ci. Ststh aic 5 ech mente oct) bic cacRo, heres atq Cuokeaen otc Ele smieroides Walker
Abdomen not elongate, more or less ovate, not petiolate, without distinct tubercles
at lateral basal angles on composite basal tergite, and only moderately convex
on apical half in both sexes; wing with a much narrower costal brown stripe,
or, if with a broad stripe, then with two or three brown fasciae on the disc;
scutellum more elongate and not evenly rounded in outline ................ 2
2. Scutellum with four marginal bristles (Zewgodacus Shiraki) .................. 3
Seas bhoten, Akdel Loy Ayo) Geena LOOKS) Ha de dous oooh ogdoadonddoceHoeauouoode 4
3. Prescutellar acrostichal and supra-alar bristles lacking ............ cucumis French
Prescutellar acrostichal and supra-alar bristles present .......... papuaensis, n. sp.
4. Wing with a broad dark-brown costal stripe that extends to third vein and from
which emanate three dark-brown fasciae, the basal one connecting with the anal
stripe, the second covering the cross-veins, and the third, which is usually
incomplete behind, lying between the outer cross-vein and the wing tip;
prescutellar acrostichals present; humeri and posterior notopleural calli orange-
Vellow NCBACtRoCenauG UELiN)) Vege. ne-yo -peteusbed holed oh eestohel teeta umbrosus (Fabricius)
Wing with a narrow dark brown stripe on the costal margin that does not extend to
third vein, and the field of the wing without dark fasciae beyond the anal stripe
(ORM CATO) LSteV4A0) hl pO CRORE > CREE ICRED OO CIC ClO Ea OID Gao od ch OD. cid thoi bb. Ia ele 5
5. Prescutellar acrostichal bristles present; humeri and posterior notopleural calli
orange-yellow ; outer cross-vein not clouded with brown ........ froggatti Bezzi
Prescutellar acrostichals lacking; lateral margins of the mesonotum from anterior
margin of humeri to wing bases ivory-white; outer cross-vein of the wing
roe Maconidhs Clloyitetsyel \yvaNed lyon] Gaocoaugnoonodouaggcosneunuc albolateralis, n. sp.
BY J. R. MALLOCH. 411
Dacus (CALLANTRA) SMIEROIDES (Walker).
Jour. Proc. Linn. Soc. Lond., iv, 1860, 154.
The genus Callantra was erected by Walker for the reception of this species.
Hendel has since placed in it another species, from New Britain, which I have
not seen. Dacus aequalis Coquillett, from Australia, also belongs to the group.
The Australian species Dacus bryoniae Tryon may belong here also, but the petiole
of the abdomen is not so long, and the dark-brown costal stripe is narrower than
in the other species.
Head brownish-yellow, the face with an elongate black spot in lower third of
each antennal fovea; third antennal segment almost entirely brownish-black.
Frons subquadrate, a little more than one-third of the head-width, with two pairs
of incurved infraorbital and one pair of stronger reclinate supraorbital bristles;
verticals four, strong. Antennae long, geniculated at apex of first segment, the
apical two segments pendulous, basal segment slightly shorter than second, the
latter about one-third as long as third; arista bare, a little longer than third
antennal segment. Gena narrow.
Thorax brownish-black, nearly all parts closely and minutely piliferous
punctate, but slightly shiny, humeri yellowish, a yellow streak on hind margin of
each mesopleuron that extends along the transverse suture on the mesonotum, but
they do not entirely meet in centre; another elongate yellow spot on the pleuro-
tergite, and the apical two-thirds of the scutellum yellow. The bristles all weak,
as follows: 2 notopleurals, 1 supra-alar, 2 postalars, 1 mesopleural, one very fine
short pteropleural, and 2 stronger scutellars. Mesonotal hairs short and mainly
yellow, those on scutellum similar.
Legs blackish-brown, tarsi yellow, apices of femora paler brown.
Wing greyish-hyaline, with a broad dark-brown costal stripe that extends over
the third vein on its entire extent but does not reach fourth except in basal third
of the anterior basal cell, fading out about middle of that cell apically and the
middle of the first posterior cell; anal streak paler brown, entire. Inner cross-
vein about one-third from apex of the discal cell; outer cross-vein slightly curved.
sloping outward above; lobe of anal cell almost twice as long as free part of anal
vein. Halteres yellow.
Abdomen coloured as thorax, with a central transverse yellow line at middle
and another at apex of the composite basal tergite or petiole, the latter not
extending to apical lateral angles, no yellow colour on sides; surface of the
remaining tergites in poor shape in the specimen before me because of dust, but
apparently there is a large yellowish mark in centre of apex of the penultimate
tergite, on which mark the hairs are orange-yellow, and the large oval depression
on each side of the ultimate tergite is greyish-dusted. The composite basal tergite
is narrower on basal half than in aequalis, more distinctly constricted at middle
where the yellow transverse line is, and the apical half forms the base of the large,
oval, prominently convex remainder of the abdomen, which is pear-shaped when
seen from above, and straight on ventral edge when seen in profile; sheath of
Ovipositor narrowly conical, not at all depressed, with more and longer hairs than
in aequalis, and these black and not yellowish in colour.
Length, 9 mm.
Originally described from Celebes. The specimen before me is from Dutch
New Guinea, Lake Sentani, Iffar, August 1936 (L. E. Cheesman). In British
Museum.
412 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
I have compared the specimen with the type-specimen of Dacus aequalis
Coquillett in the United States National Museum to obtain the above comparative
data. In a paper on the Trypetidae of the Solomon Islands now in the press I
have included a key to all the species of this subgenus.
Dacus (BAcTROCERA) UMBROSUS Fabricius.
Syst. Antliat., 1805, 274.
This species and several others closely related to it have been placed in the
subgenus Bactrocera Guérin, but there are no outstanding characters beyond the
two or more oblique dark-brown fasciae on the field of the wing to separate it
from Dacus, sens. lat.
This species extends in range from the Malayan region to Australia. I have
before me specimens taken by Mr. Taylor at Wewak, New Guinea, Rabaul, and
Lindenhafen, New Britain.
Dacus (ZEUGODACUS) CUCUMIS French.
Dacus tryoni var. cucumis French, Jour. Dept. Agric. Vict., v, 1907, 307.—
D. cucumis French, Tryon, Proc. Roy. Soc. Qsld., xxxviii, 1927, 207.
One female, Papua: Mondo, 5,000 feet, i-ii, 1934 (L. E. Cheesman). British
Museum. Previously recorded from New South Wales and Queensland.
Dacus (ZEUGODACUS) PAPUAENSIS, Nn. Sp.
6, 2. A rather small orange-yellow species, with the usual two black spots on
the face, the thoracic dorsum not blackened, with three ivory-white vittae behind
the suture, and the abdomen without black markings though the base of the
composite basal tergite is browned. Wing with a very narrow dark-brown costal
stripe to apex of third vein or slightly beyond that, the costal cells hyaline; anal
streak present.
Frons in male a little more than twice as long as wide, with three pairs of
incurved infraorbital and one pair of supraorbital bristles, in female wider and
with two or three pairs of infraorbitals; both sexes with four strong verticals.
Third antennal segment about three times as long as second.
Thorax with mesonotum slightly browned along inner edges of the postsutural
yellow vittae, the following parts lemon-yellow: Humeri, posterior notopleural
calli, three postsutural vittae, the central one not attaining posterior margin, the
entire scutellum, posterior half of the mesopleura, but little narrowed below, a
large double spot on the pleurotergite; postnotum black-brown. Scapular bristles
quite strong; in the male there is a dark hair-like setula or bristle near the hind
edge of each humerus, but in the female this is not distinctly evident. Supra-alar
and prescutellar acrostichal bristles present; scutellars four.
Légs yellow.
Wing as Plate xi, figure 1, the costal cells hyaline, and the dark-brown costal
streak ending just beyond the apex of third vein. First and third veins setulose as
usual, the fifth vein bare; free part of anal vein in both sexes nearly as long as the
lobe. Anal streak broad to near apex of lobe of anal cell, faint beyond it.
Abdomen ovate, no visible erect fringe of third abdominal tergite of the male,
the depressions on fifth tergite of that sex poorly developed, the fifth tergite of
female very distinctly depressed centrally on each side. Hairs pale brown.
Length, 7-8 mm.
Type, male, Bulolo, New Guinea (F. H. Taylor). Allotype, Wewak, New Guinea
(J. R. Rigby).
BY J. R. MALLOCH. 413
Dacus (CHAETODACUS) FROGGATTI Bezzi.
Dacus zonatus Froggatt, nec Saunders, Proc. Linn. Soc. N.S.W., xxxv, 1910,
868.—D. froggatti Bezzi, n.n., Dipt. of Fiji, 1928, 101.
One male, Lindenhafen, New Britain (F. H. Taylor). Originally described
from Russell Island.
Dacus (CHAETODACUS) ALBOLATERALIS, N. SD.
6, °. A brownish-yellow species, much like papuaensis in general colour and
markings, the mesonotum with three ivory-white postsutural vittae; along the
inner edge of the sublateral pair there is a blackish line. The mesonotum differs
from that of any of the other species listed in this paper in having the entire lateral
edges in front of the wing bases ivory-white, and in having also a pair of yellowish-
grey-dusted vittae extending from the anterior margin to near the posterior margin
between the postsutural vittae.
Head brownish-yellow, paler in front, the face with the usual pair of glossy
black spots in the foveae. Third antennal segment about 2:5 times as long as
second. Frons with two pairs of incurved infraorbital and one pair of reclinate
supraorbital bristles, and four strong verticals; ocellar spot black.
Legs yellow, normal in structure and armature.
Wing as Plate xi, figure 2, the costal streak dark brown, not extending over
second vein on to the field, ending near middle of apex of the first posterior cell;
inner cross-vein not clouded, outer cross-vein distinctly but narrowly clouded with
brown. First and third veins setulose as usual, fifth vein bare.
Abdomen elongate-ovate, brownish-yellow, with rather dense concolorous hairs,
the apical lateral erect fringe on third tergite of male dark brown. Male with a
central apical dark mark on the fourth and fifth tergites.
Length, 7-7-5 mm.
Type, female, Upper Watut, New Guinea (F. H. Taylor). Allotype, Papua:
Mondo, 5,000 feet, i-ii, 1934 (L. E. Cheesman). Type returned to Mr. Taylor,
allotype in collection of British Museum.
Tribe ADRAMINII.
I have some doubts about the propriety of segregating this group on the basis
of the cited characters, as there appears to me to be a great similarity between
them and those genera most closely allied to Huphranta Loew. This latter group
has consistently been well removed from Adrama and its allies by specialists on
the Trypetidae, but by making use of other characters than have been used for
group segregations it might be possible to bring these two groups together.
The haired pleurotergite is present in Adrama and in Euphranta, as well as in
a number of related genera, and there is a great similarity in the general habitus
as well as in the wing-markings of most of the genera involved. The lack of the
presutural bristle is to my mind rather an important character that links all of
them together, and it appears to me to be of more significance than the previously
used character of the spinose femora, there being other genera in which this last-
mentioned character occurs that are not at all closely related to Adrama.
As this is purely a faunal paper and not intended as a revisional one, I prefer
to leave some matters, such as this, in abeyance meanwhile, or to other and better
informed workers on the family.
Below I present a key to the genera of this group known to me, though one
of them is so known from the descriptions and figures only. Two of the genera
are not known to occur in New Guinea, but Neosophira does occur in Celebes and
it may yet be found there.
414 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
Key to the Genera.
1. At least the mid and hind femora with short stout ventral spines apically, usually
in two series; marginal cell of the wing just beyond the apex of the first vein at
least twice as wide as the submarginal cell at the same point; subcostal vein
rectangularly bent forward near tip, obsolescent beyond the angle; stigma not
half as long as the costal division in front of it; stem vein of the wing with short
stiff setulae above to near its extreme base .................. Adrama Walker
None of the femora spinose on their ventral surfaces; marginal and submarginal
cells of the wing just beyond apex of first vein subequal in width; subcostal vein
sloping forward at apex, rather faint beyond the curve; stigma much more than
half as long as the division of costa before it; none, or very few, setulae on the
upperside of the stem-vein of the wing basad of the level of the humeral cross-
NEGO ae he 14, 0 GaS. Oh BLE REL CRIECLO. Cod. colo -c CLAIROL DRASTIC ROR BRC AP ESRCDCUCuMEe A iohc Tas Sion aeO Ants cheer ers hats 2
2. Apical section of the fourth wing-vein more or less undulated and bent forward at
apex so that the first posterior cell is narrowed apically .... Neosophira Hendel
Apical section of the fourth wing-vein straight or almost so, the first posterior cell
MOS Lie LNYh WEHH COV GOWEN Ke NUNY <6 o.oo CoO Me Ded AIGOC.S DU diablas 6 ued ulate ol aailore Geo 6 3
3. A pair of fine erect bristles in centre of anterior margin of the mesonotum (central
scapular pair) the apices of which are fine and slightly curled; second wing-
vein undulated; section of fifth vein basad of the base of the discal cell not longer
than the cross-vein closing the latter; vein closing the anal cell slightly angled
below the middle, posterior lower angle of that cell hardly produced, the cell
much longer than the free part of the anal vein; pleurotergite bare ............
BAI RRORCURCR ORS Cer ChOe A ch 8 tics Gr 8 Cho BRC Ree PMC OLR MONE Curae aa Pseudosophira, n. gen.
No fine erect bristles in centre of anterior margin of the mesonotum; second wing-
vein straight; section of the fifth vein basad of the discal cell about twice as
long as the cross-vein closing base of latter; vein closing anal cell much angu-
lated at or above middle, the cell with a slender subtriangular lobe at lower
posterior angle, not nearly as long as the free part of the anal vein; pleuro-
terpite! aimed’ waite ovens weve wets Ss Pate ee Oem Ue PER ews ee dae Cyclopsia, n. gen.*
NEOSOPHIRA Hendel.
Abhandl. Zool.-Bot. Ges. Wien., viii, 1914, 138; Wien. Hnt. Zeitg., xxxiii, 1914, 73.
Originally Hendel placed this genus in the family Otitidae (Ortalidae), sub-
family Platystominae, but in the same year, as cited above, he included it in his
key to the genera of the family Trypetidae. I have not seen either of the two
species he placed in the genus, but there can be no doubt about the correctness of
his later decision.
From Hendel’s description and figures of the genotype, distorta Walker, I draw
the following data: The frons has one upper reclinate pair of orbitals and a very
weak incurved pair of infraorbitals, and one strong pair of verticals; the arista is
moderately long haired; mesonotum with 2 notopleural and 2 supra-alar (postalar?)
bristles, the other bristles lacking; scutellum with four marginal bristles. Stigma
of wing as long as the costal division before it and much longer than the one
between it and the apex of second vein; inner cross-vein beyond middle of discal
cell.
,
NEOSOPHIRA DISTORTA (Walker).
Trans. Ent. Soe. Lond., iv, n.s., 1857, 230 (Sophira). Originally described from
Celebes. May be found in New Guinea.
PSEUDOSOPHIRA, nN. gen.
The essential characters of this genus may be derived from the features given
in the foregoing keys to tribes and genera. As the genus is extralimital, all the
known species being from the Philippines, it appears essential to describe only the
venotype in order to establish the validity of the genus. This I take the oppor-
tunity of doing herein.
BY J. R. MALLOCH. 415
PSEUDOSOPHIRA BAKERI, NM. Sp.
6. General colour orange-yellow to ferruginous, shiny, frons dull, upper orbits
and vertex glossy. Frons with a large pear-shaped black mark, the narrow end of
which is on vertex, the other at anterior third of the interfrontalia; face black
centrally, the mark widened from between antennae to epistome. Second antennal
segment largely black, third bright orange-yellow, barely twice as long as wide,
rounded at apex; arista with the longest upper hairs longer than the width of
third antennal segment; palpi yellow. Head slightly wider than thorax, frons
one-third of the head-width and about 1:25 times as long as wide, parallel-sided;
upper orbits well defined, extending to middle, with a short fine yellow bristle at
lower extremity, one pair of fine erect infraorbitals only and these near anterior
margin; only the inner verticals present, strong and straight. Eye higher than
long, more narrowed below than above; gena narrow.
Thorax with three deep black spots on each lateral margin of the mesonotum
as follows: One above humerus, one behind humerus, and a very small one against
the hind side of the suture; pleura with a large glossy black spot on upper
posterior angle; postnotum immaculate. The single, central, pair of scapulars
long, luteous; anterior notopleural lacking, posterior one strong; posterior postalar
much shorter than the anterior, which latter is equal to the supra-alar; prescutellar
acrostichals minute; scutellum with four strong bristles and many short stiff
hairs; pleura without bristles: pleurotergite without erect hairs.
Legs orange-yellow, hind tibiae browned centrally. Fore femur with a series
of fine yellow bristles that begins at base rather long and runs out about middle
with very short hairs. Mid tibia with a strong black apical ventral spur.
Wing (PI. xi, fig. 3)* as in Colobostrella ruficauda Hendel, but the hyaline
streak between the cross-veins attains the costa, there is a hyaline marginal streak
from the apex of the second to beyond the apex of fourth vein, and the hyaline
spot is in the second posterior cell, not near the apex of first.
Abdomen glossy ferruginous yellow, the hairs concolorous.
Length, 8-5 mm.
Type, Kolambugan, Mindanao, Philippine Islands. Sent to me a number of
years ago by C. F. Baker when I planned a review of the Trypetidae of the
Philippines.
Subfamily TRYPETINAE.
Key to the Groups.
1. Arista plumose, or long-haired, the longest hairs rarely (Acanthoneura) less than
half as long as the width of third antennal segment; scutellum with six marginal
bristles, the intermediate pair sometimes very short ..... Ge este jleusye ieyisy seals Group I
Arista much shorter haired; if plumose then the scutellum has but four marginal
DDISELSS) Vii ee Reta tematic: teak roma Sue ool RESeaev che emai tie anaes, Siete, niche Panta Matene, oz claus 2
bo
Scutellum flattened, coarsely haired on its entire surface, and with eight or more
strong but unequal marginal bristles; hairs on upperside of the first wing-vein
carriedvalmost tor the basen ss sees aie aid ese saiaereie etoresalee alate Pee eee Group II
Scutellum with but four marginal bristles, rarely with two .............. Group III
Group I.
In this group there are three genera, in which the dorsocentral pair of bristles
are almost in line with, or even in front of, the transverse line between the supra-
alar pair. Of these but one, Diarrhegmoides, is in the present collection. The
others are Malayan, but may yet be found in New Guinea or adjacent island groups.
* The tiny spots all over the wing are dirt adhering to the wing membrane,—F.H.T.
416
or
5a.
DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
Key to the Genera.
Second wing-vein conspicuously undulated beyond level of apex of first vein; petiole
of second and third wing-veins sometimes setulose above; dorsocentral pair of
bristles well behind the supra-alar line; anterior supraorbital sometimes near
ANCELION -LOUntM (OL ELONS) qinyeserstorekel aici ccarey ce) sie ne aL oc FTE Rene oaeae ge he eee te III nae 2
Second wing-vein at most but slightly bent beyond level of apex of first vein; if it
is so, then the fifth vein and the petiole of second and third veins are bare above,
the face is noticeably convex, the anterior supraorbital is above middle of frons;
or the dorsocentral pair of bristles is close to, or in front of, the supra-alar
UR TTO: somes rosrcuestelens f= 'cnexexe ros) Cheus bene ee vevedlen okerte anges ages cuss sy 8 cade vce ac sales caeiar emausihe apo nareRORS EcICirone tiene 6
Second wing-vein with several short spur-veins at right angles to it on each side
that frequently connect with the first or third veins; fourth vein conspicuously
bent forward beyond middle of its apical section so that the first posterior cell
ISiveryamuch! nNarrowediinvavexOL Winky hee eeiecee cena seen Polyara Walker
Second wing-vein without any, or but one, short spur-vein; if the latter it is near
apex on the posterior side and it does not connect with the third vein ........ 3
Fourth wing-vein bent forward at its apex so that the first posterior cell is narrowed
in the wing tip; only one pair of infraorbital bristles present ..................
SS atmo netics SARA RAS ce SMe teea fel oh oh cren tarsi era crit matte s fal Fh ee ae ae Colobostroter Enderlein*
Face in profile strongly convex, receding below; antennae not half as long as face;
anterior pair of supraorbital bristles very strong, situated at about the anterior
fourth of frons; two supra-alar, two postalar, and six equally strong scutellar
bristles present; fifth wing-vein bare above; undulation of second wing-vein not
VEL PIMARKEd" ec cee ateteerteneraensis sre at Scrat sve ere Renita tel ana sche Themaroides Hendel
Face not at all convex in profile; anterior pair of supraorbital bristles at or above
middle lot frons: [AR cee PALE. SSSR ah BAe esenes oaths £ cen Rees iy 3) Seka ents Oaks a
Second wing-vein with a deep downward loop below apex of first; gena about three-
OWNS ENS lvkslal SGN (MOM) odoloonooosdcudooscnoodoago+ Exvicopterina Malloch
Second wing-vein merely undulated, not looped; gena not more than one-fourth as
1s h=3) clare non doe Be ene Cac ca bed ce Oren cae CRP CICRCaR OIE Sloane teste sy oe Mike is Gee eee es caciG. Geo trolgio 5a
Face vertical, epistome not projecting; antennae not half as long as face; ocellars
about as long as the postverticals; petiole of second and third wing-veins not
SCtulOse! (ADOVE™ seo coe cette ee che eect ie Gaels SencLa Sista tee Pseudacanthoneura, n. gen.
Face slightly concave centrally in profile, the epistome slightly projecting; antennae
descending to distinctly below middle of face in profile; ocellar bristles repre-
Sentedaby microscopic, Mains) 4h dipivesrsadeworsts > cy egedous Mice aseke k Ade ay Aas hag eee eed deh eis 5b
5b. One pair of infraorbital bristles present; intermediate pair of scutellar bristles very
short; petiole of second and third veins bare (Malayan) ...... Themara Walker
At least two pairs of infraorbital bristles present; all three pairs of scutellars long
and strong; petiole of second and third veins setulose above ..................
A ORG BCL Os MO CHDL ice SORE ICR RCE RHE TOR MER Cure tan Aira te mnaeennatce clei Neothemara Malloch
First, third, and fifth veins setulose on at least a part of their upperside ........ 7
Only the first and third wing-veins partly setulose above ....................... 11
First wing-vein exceptionally long, ending in the costal vein above level of upper
. extremity of the outer cross-vein, the distance between its apex and that of the
subcostal vein more than twice as great as that between latter and the humeral
cross-vein; face with a central vertical rounded Keel, narrowed above and not
continued between bases of the antennae; genae and lower occiput with numerous
rather long black bristly hairs; sternopleural bristle lacking ................
Hoo gnodcoopenovUoUonU Oo Gomes b po moodotD oO AO DOD ed ADO OOO Cheesmanomyia, n. gen.
First wing-vein not exceptionally long, ending in the costal vein well before level of
upper extremity of the outer cross-vein, the distance between its apex and that
of the subcostal vein not greater than that between the latter and the humeral
cross-vein; face not markedly keeled; gena with a few bristly hairs; sterno-
pleural’ bristle present. See. cie cht She ten ctatatie de Setote et sh eeiet ae an ctrele eluate fete Meenas 8
* This genus has but four marginal scutellar bristles, though Enderlein states that it
has six. J include it in Groups I and II.
10.
iL,
12.
13.
14.
15.
16.
We
the
BY J. R. MALLOCH. 417
Face quite prominently convex in profile, highest at centre, and from there receding
to epistome; vertex sharply carinate, the carina projecting behind; antennae
about half as long as face; mid tibia with no ventral submedian bristles and
with two equally long and strong apical ventral spurs; scutellum bare on disc
29 a0: 6)i6-'7S G00 tb eos Enea SM aeeh rola earths fee Hl Snir ve Ceri Mei a ROP iii SP a ON ti ae i ae Rabaulia Malloch
Face either almost flat and vertical, or, if slightly convex, not receding from middle
to epistome; vertex not sharply carinate; mid tibia either with one long and
one or more much shorter apical spurs or with a submedian ventral bristle .. 9
Antennae not half as long as face, the latter convex and more or less receding below;
anterior orbitals very strong, curved backward; hind tibia with two or three
submedian anteroventral bristles and the usual series of short anterodorsal
setulae; pteropleural bristle present; scutellum with the entire disc covered with
SHOVEL INE WHS) > Gua ot ee oreo bugs bio CRORIG: o oIGROVCL CoE EcReee one es eea ee Themarohystriz WHendel
Antennae more than half as long as face; anterior two pairs of orbital bristles
proclinate and inecurved; mid and hind tibiae without exceptional armature;
DLUcroOpleuURnaAlMbnISble™ laekiney BAe snatey es declare he hs cheese) Sancho oh eeed ata deal ee N cre dicreteehaci cis 10
Mid tibia with two long apical ventral spurs .......... Trypanocentra Hendel
Mid tibia with one long and one much shorter apical ventral spur ................
Od Dray OrONCRORSIEMO en EIA CORIO C0, Din GER CCR ich oR CREO RP CES EET rs aa ane ae Clusiosoma Malloch
Mesopleura with an outstanding bristle near lower edge centrally ; infraorbitals very
close together, the anterior pair incurved, the upper pair backwardly directed
SM Hes COMA NS wc Pel Se nalts eit a atta piseoteee Atte SRS ei sidl UAE Bs PENS Shin MES Hexacinia Hendel
Mesopleura without an outstanding bristle near lower edge centrally ; frontal bristling
TACHI “EISEN NONE ols aro Gices Wale Oot G DICT ORIEN OFELS IOs CECH ORG oto re To OrGT ONG OICHD ESE CnC SHE Me rCTONT fey oie nemenciT 12
Wing brown or black, with some hyaline incisions in the margin and three or more
STU MyaAlan emai SCAMS DW OLS chaste oie esectre aie sta e a foie ieeetemsitereucnel Shencareenckeleee seus, Ais 13
Wing hyaline or yellowish, with brown longitudinal streaks on costa and veins.. 17
Dorsocentral pair of bristles almost in line with the supra-alar bristles ........ 14
Dorsocentral pair of bristles much behind the line of supra-alar bristles ...... 15
Second wing-vein straight; fourth vein slightly arcuate on apical section; dorso-
central bristles slightly behind the transverse supra-alar line (Malayan) ......
0:0 GE Oe OO OOo id b OO OT Choe Ore O° OG OG. B'0 CIOS MERC ECECRE NCEE POR ENC CRO OIC eaonEr TE Diarrhegma Bezzi
Second wing-vein slightly undulated; fourth vein conspicuously arcuate on apical
section; dorsocentral bristles slightly proximad of the transverse line of supra-
Ura Oe SCLES MPA eet te ciate rato hciweecteney ENE iyo ile needa ve Ron ekeVeteie ta abot Diarrhegmoides, n. gen.
Setulae on the first wing-vein extending the entire length of the node above ....... S
Cher ASG COLONG or Cha ome o POte eee aed. clicks DORIS TRC 6, GEES CR CTEe Se ete EERE et ere nc an aa an Rioxaptilona Hendel
Setulae on first wing-vein not extending over node above ....................- 16
One pair of supraorbital bristles present, and usually only one pair of finer infra-
orbitals; mesonotum narrow, much longer than its greatest width; scutellum
with a few minute hairs on each side of disc; arista long haired ..............
Re Se ee ints Rocmesin ete A AH ROE SRS Dy Skt eto ae ol REE IN Geis etre oe Ste cae Termitorioxa Hendel
Two pairs of supraorbital ana two pairs of infraorbital bristles; mesonotum broad,
not much longer than its greatest width; scutellum bare; arista long haired
PICHON ICR RC ere eee aS cho] dice Alek enc. Orr PRE OGRA Loca Bah atch Goo tld ok SeeRC eee ee Rioza Walker
One pair of infraorbitals and two pairs of supraorbitals; arista short haired ........
Bo Pes Neetu ai ged ae visi ee Dee fe cee taal bg ft SN Acanthoneura Macquart
Inner cross-vein of wing at middle of the discal cell; presutural bristle lacking
UC OLEn ra Koyo’) li tacerolnedi ord CHEER n cach CRORCRE RCL Chet GES Garena. Gc CL Cae eey CLRSRS TOES ase e Sophiroides Hende}
Inner cross-vein before or beyond middle of the discal cell; presutural bristle present
SASS SIRES) CTaiciG a Mane ona aeaaa o BitaNo ke een ‘oasromteoNaro Aig: DRoloeced ip cip ay OEaLe aides chee MGI Res Sophira Walker
PoLtyara Walker.
Jour. Proc. Linn. Soc. Lond., iii, 1859, 122.
This genus was erected for the reception of a single species, described from
Aru Islands.
The head is broader than the thorax in the male, with the frons broader
than long, about two-fifths of the head-width, inner verticals much longer than
the
outer, postverticals and ocellars short, anterior orbitals two pairs, incurved,
anterior pair very short and close to the second pair, two reclinate upper pairs,
418 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
the anterior pair the longer; face slightly convex, with deep lateral infra-antennal
foveae; eye a little higher than long; antennae more than half as long as face;
aristae long-haired. Thorax with the following bristles: 1 humeral, 1 presutural,
2 notopleurals, 1 supra-alar, 3 postalars, 1 pair of dorsocentrals a little behind
the level of the supra-alars. a pair of strong prescutellar acrostichals, 2 or 3
mesopleurals, 1 sternopleural, 1 pteropleural, and 6 strong scutellars, the dise of
scutellum bare. Abdomen slender, with four evident tergites, first (composite)
and fourth longer than the others, all with lateral bristles, strongest on fourth
and on apex of fifth sternite. Mid and hind tibiae with a few anterodorsal and
posterodorsal bristles. Wing with some spur-veins on both sides of the second
vein, sometimes extending entirely across the cells, the vein slightly angulate at
bases of these spur veins; cross-veins separated by less than the length of the
inner, fourth vein much curved forward about apical third; anal cell with a
long apical lobe; first and third veins setulose above and below.
POLYARA INSOLITA Walker.
Op. cit., iii, 1859, 123.
Head orange-yellow, with a black spot between bases of antennae and another
between each antenna and eye; facial foveae white-dusted. Thorax testaceous
yellow, with grey dust, mesonotum with four rather obscure black vittae, pleura
largely black, with dense grey dust, the postnotum black. Legs tawny yellow. -
Wings (PI. xi, fig. 4) greyish-hyaline, with dark brown costal stripe and paler
markings in some of the cells and on the outer cross-vein. Halteres yellow.
Abdomen black, densely grey-dusted, with a testaceous-yellow dorsocentral
vitta on its entire extent that tapers behind.
Length, 7-5 mm.
Bulolo, Wau, New Guinea, three specimens (Dr. C. E. M. Gunther, F. H.
Taylor). Walker later recorded the species from Mysol, and Osten-Sacken in 1881
listed it from Ramoi and Dorey, New Guinea.
COLOBOSTROTER Enderlein.
Zool. Jahrb., Abt. fur Syst. Geog. und Biologie, xxxi, 1911, 445.
This is a rather exceptional genus and, though it is not known to occur in
New Guinea, and may never be found there, it appears necessary to present a
few notes on the genotype.
COLOBOSTROTER PULCHRALIS Enderlein.
Op. cit., xxxi, 1911, 445.
Has much the appearance of an Otitid, the posterior basal and anal cells of
the wing being much longer than usual in the Trypetidae, the anal cell having
but a short angular extension at lower apical angle; the frons has but one
infraorbital and one supraorbital pair of bristles, and one pair of verticals, the
inner. Specimens that I have seen have but four scutellar bristles despite
Enderlein’s statement that there are six; this difference from the description has
already been noted by de Meijere. A peculiar feature of the wing is the presence
of a short spur-vein on the posterior side of the second vein above the outer
cross-vein. The forward curve of the apical section of the fourth vein is not very
marked, but the apical section of the vein is biundulate, making the upward
inflection of the tip more apparent. The wing has three blackish fasciae, the first
over the inner cross-vein that does not extend beyond the fifth vein and has a
BY J. R. MALLOCH. 419
backward extension to almost the fork of second and third veins, the second one
extends over apex of second vein and encloses the outer cross-vein, over which it
connects with the third fascia on the apical margin of the wing.
Sumatra. I have seen it from the Philippine Islands.
THEMAROIDES Hendel.
Wien. Ent. Zeitg., xxxili, 1914, 77.
This monobasic genus was erected for the reception of an old species placed by
Walker in Helomyza. I have not seen the species, which must have been known
to Hendel, as the characters used by him for the segregation of the genus are
not given by Walker in the original description. Differs from Rabaulia in bristling
of frons, etc.
THEMAROIDES QUADRIFERA (Walker).
Jour. Proc. Linn. Soc. Lond., v, 1861, 246 (Helomyza).
Described from a female that is testaceous in ecclour, with the apical half
of the abdomen black, the black colour most extended on sides, the wings black,
limpid at the base and along the hind border, with a white subquadrate costal
spot opposite to which the black extends nearly to the hind border, veins black,
testaceous in the limpid part, discal transverse vein straight, parted by less than
half its length from the border, and by about its length from the prebrachial
(inner) transverse vein. Length 11 mm.
Dorey, New Guinea.
THEMARA Walker.
OTD. Gitte, ty IS, 38,
I have seen several species of this genus, but none from New Guinea.
The undulated second wing-vein, presence of setulae on the first, third, and
fifth wing-veins above and on the second and fourth below, the very small inter-
mediate pair of scutellar bristles, and the wing markings distinguish the genus
from most of its allies.
Enderlein held that this and Ptiolina van der Wulp were synonyms of
Acanthoneura Macquart, but Hendel did not accept his conclusions.
CHEESMANOMYIA, Nl. gen.
Generic characters.—Belongs to the same group as Themarohystrix Hendel,
but is distinguished from it and other closely related genera by the exceptionally
long first vein (Fig. A). As in other genera of this group the wings are largely
black or very dark brown, without pale spots, though there are pale longitudinal
streaks in some of the cells. The frons is much longer than wide, with the upper
orbits glossy, the bristles consisting of two anterior incurved and two posterior
reclinate pairs of orbitals, the outer verticals and the incurved postverticals about
half as long as the inner verticals. Face convex, highest at middle (Fig. B),
antennae extending to a little below middle of face, gena and lower jowls with
numerous fine black bristles (Fig. B). Thorax much as in Themarohystriz, but
there is neither a pteropleural nor a sternopleural present and the dorsocentrals
are well behind the transverse level of the supra-alars. Mid tibia with one
long and one short apical ventral spur and no submedian ventral bristle. First
and third wing-veins setulose on almost their entire extent above, less extensively
and more sparsely so below, fifth setulose basally above, and fourth with a few
widely separated setulae centrally above and below.
Genotype, Cheesmanomyia unica.
420 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
CHEESMANOMYIA UNICA, Nl. Sp.
2°. Head tawny-yellow, frons, antennae, and palpi brighter yellow, vertical
edge and upper occiput brown. Length of frons about 1:75 times its central
width, vertex rounded. The four pairs of orbitals about equally spaced, upper
anterior and lower posterior bristles longer than the others, the anterior two pairs
incurved, upper pairs reclinate, the upper one of latter a little shorter than outer
vertical, the latter about half as long as the inner, ocellars minute; postocular
cilia fine and black.
Thorax glossy brownish-black, the humeri and a line along upper edge of
pleura to base of wing bright yellow, mesonotum in type slightly shrunken because
of the teneral nature of the specimen, showing traces of a yellowish central anterior
marginal mark. Scutellum with the usual six bristles, the intermediate pair
shorter than the others.
Legs yellow, the coxae, femora except their extremities, and basal half of hind
tibiae brownish-black.
Wing (Fig. A) dark brown, paler at. base, in costal cell, along hind margin,
and with pale streaks in centre of discal, first and second posterior, marginal and
submarginal cells. Halteres yellow.
Abdomen coloured as thorax, with numerous black hairs and some fine apical
and lateral bristles on the tergites.
Length, 8 mm.
Type, East Dutch New Guinea, Jutefa Bay Pim., sea-level to 100 feet, February
1934 (L. E. Cheesman). Type in British Museum.
Genus dedicated to the collector in recognition of the fine collection before me.
I place in this genus also the species described by de Meijere, notes on which
are presented below.
CHEESMANOMYIA NIGRA (de Meijere).
Nov. Guin., v, Zool., 1906, 95 (Riozxa).
Similar in almost all respects to wnica, differing in having the costal margin
of the wing more rounded at middle, the costal cell yellow, the central portion
of the wing including the posterior basal cell, the posterior half or more of the
discal cell yellowish-hyaline, the dark colour fading out over the outer cross-vein,
and no subhyaline elongate streaks in the cells of the apical half. There are
also some minor differences in the leg colour-markings, but the type of unica is
teneral and has been attacked by mites or dermestid larvae so that minute
distinctions are difficult to draw between it and de Meijere’s description of his
species. |
Length, 6-7 mm.
New Guinea.
RABAULIA Malloch.
Ann. Mag. Nat. Hist., (11) iv, 1939, 257.
Generic characters.—Similar to Themarohystrix in structure, differing
markedly in the structure of the head (Fig. C), the face being quite prominently
conically produced, with the highest point a little below the middle in profile and
from that point roundly receding to the mouth margin which is not produced.
Antennae extending to middle of face. Eye higher than long, about six times as
high as gena. Intermediate pair of scutellar bristles shortest, the disc bare. First,
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
Fig.
BY J. R. MALLOCH.
=f
“ah
D UNOS {
7 Pfs \
ae
se
ae i a
N pei tense tee
A.—Cheesmanomyia unica, n. sp. Wing.
B.—Cheesmanomyia unica, n. sp. Head in profile.
C.—Rabaulia fascifacies Malloch. Head in profile.
D.—Clusiosoma puncticeps, n. sp. Head in profile.
E.—Sophira flava (Edwards). Wing.
F.—Acanthoneura acidiomorpha Hendel. Wing.
G.—Types of armature of node of stem vein of wing: 1. Pseudacanthoneura.
2. Chrysotrypanea.
H.—Cyclopsia inaequalis, n. sp. Wing.
I.—Pseudina bulolodae, n. sp. Head in profile.
J.—Ceratitis capitata (Wied.). Anal cell of wing.
K.—Ceratitella loranthi (Froggatt). Anal cell of wing.
L.—Tephrella sexincisa Malloch. Anal angle of wing.
M.—Spathulina acrolewca (Schiner). Anal angle of wing.
N.—Sphenella marginata Fallen. Anal angle of wing.
421
422 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
third, and fifth veins setulose above, both sections of last setulose, first vein not
exceptionally long. Mid tibia with two long and two short apical ventral spurs.
Genotype, Rabaulia fascifacies Malloch.
RABAULIA FASCIFACIES Malloch.
Op. cit., (11) iv, 1939, 258, Pl. xi, fig. 18.
A small shiny-black species, with black wings, the head largely yellow, the
face with a black central narrow fascia.
Rabaul, New Britain.
THEMAROHYSTRIX Hendel.
Wien. Ent. Zeitung, xxxiii, 1914, 78; Ann. Mus. Nat. Hung., xiii, 1915, 432.
This genus was erected for the reception of a species from the Indian
Archipelago, but without more definite locality given. The generic description
is quite full, but the description of the genotype is very short and rather inadequate
for accurate identification. The type species is unrepresented in the material
before me. Curran erroneously referred a species taken by the Whitney Expedition
on Mouo Island to this genus; I deal with this species under another genus in
the following text. Below I present a key for the identification of the species
known to me at this time.
Key to the Species.
1. Face with a black central mark; wings blackish-brown, without hyaline markings
and the anal angle hardly paler than the disc .................. suttoni, n. sp.
Face and frons entirely yellow; wings dark brown, broadly subhyaline on anal
Nyt eh. Bima don oo oD 0.0 CoC MOR 46 Chui od on cloiciesduoiges cio Goin el fn Gin S.c.o1O Om ee Cl OEcict Z
A WISSOrE ere pon Wake amare Jee WALI oooogomodood¢oodeooano 0G doimon > erinaceus Hendel
MesonotummwithufivierblachkeaviGtaeurenners ri rnel- ii leieieieiciel iterate flaviceps, n. sp.
THEMAROHYSTRIX ERINACEUS Hendel.
Op. cit., xiii, 1915, 433.
Hendel describes this species as having four black mesonotal vittae, the
submedian pair continued along the sides of the scutellum, the others along the
notopleural suture, and two similar vittae on each pleuron. The abdomen is
described as: “‘Seitenrand der Tergite Schwarzbraun, die Spitze im allgemeinen
etwas verdunkelt.” The wings are similar to those of flaviceps. Length, 9 mm.
In the original description Hendel states that the base of the second vein
and the fourth vein to about the middle are setulose. This character holds in
both the species before me, and in addition it may be well to add that the second
vein has the underside, except at apex, closely setulose and that there are setulae
on the underside of the fourth vein to beyond its middle. No doubt these features
ought to be taken as of generic import.
Indian Archipelago. Described from a female specimen.
THEMAROHYSTRIX FLAVICEPS, N. Sp.
9. Wing (Pl. xi, fig. 5): In this species the first, third, a part of fourth
centrally, and all of the fifth vein are setulose above, and the second on its entire
extent from its furcation with third, and a large part of third and fourth, are
setulose below. The apical pair of scutellar bristles is a little shorter than either
of the other two pairs. The head, thorax, and abdomen are pale testaceous-yellow.
The only dark marks on the head consist of a small ocellar spot and a small spot
below each eye; antennae and palpi yellow, the third segment of former slightly
darkened above. The thorax has five narrow black vittae on the mesonotum, the
submedian pair continued over the sides of the scutellum, the pleura each have
BY J. R. MALLOCH. 423
two similar vittae, one at middle of the mesopleura that extends to hind margin of
that sclerite, the other on the upper margin of the sternopleura that does not
extend as far back, and a black spot on the lower margin of the pteropleura.
Postscutellum with an irregular black transverse line; postnotum yellow. Abdomen
with a black central spot on each of the basal three segments and a black basal
fascia on each of the others, sometimes broken; genital cone black. Fore and mid
tibiae largely black. Fore femur in female with a posteroventral series of long
strong bristles and two series of much shorter bristles on the posterodorsal surface;
mid femur with two anterior series of bristles, the lower one the least extensive
and the stronger; hind femur with one or two strong bristles beyond the middle on
the anteroventral surface. Mid tibia with one or two anteroventral bristles and a
series of posterior setulae; hind tibia with two or three rather strong anteroventral
bristles and a series of anterodorsal setulae. Knobs of halteres dark brown.
Length, 8-10 mm. ;
Type and 3 paratypes, Bulolo, New Guinea (F. H. Taylor).
THEMAROHYSTRIX SUTTONI, D. Sp.
6, 9. This species is very similar to flaviceps, but differs in having a vertical
black stripe on the face that extends over the prelabrum, the mesopleural vitta very
rarely extends over the spiracle, there is no black spot on the pteropleura, there
usually is a central dark spot on the sternopleura, and the postscutellum is entirely
yellow. The wings (PI. xi, fig. 6) are hardly paler on the anal angle than on the
disc. The mid and hind femora are preponderantly black, instead of very narrowly
browned at bases as in flaviceps. Abdomen with a narrow black dorsocentral vitta
on the basal three tergites, the other tergites usually entirely black.
Structurally as flaviceps. Length, 6-8 mm.
Type, male, allotype, and 11 paratypes, Wewak, New Guinea (F. H. Taylor).
Occasionally the central dark spot on the sternopleura is lacking.
It appears worthy of note that in Themarohystrix and Neothemara the
scapular bristles are distinct, though rather weak and fine, while in Clusiosoma,
Trypanocentra, and Cheesmanomyia these bristles are undeveloped. This lack of
scapulars in the last-mentioned group of genera is associated with a slight but
evident concavity of the occiput which allows the head to fit more closely against
the thorax than it does in the other group, and sometimes this concavity is
emphasized by a backward extension of the vertex forming a slight flange, most
pronounced in Rabaulia. I do not make use of this cephalic character in my
generic key, though it may be of even more phylogenetic significance than those
I have used.
CLusiosoma Malloch.
Proc. Linn. Soc. N.S.W., li, 1926, 547.
This genus was described from Australia. I have several species before me
that I refer here and deal with them below though they do not all occur in New
Guinea. The genus is similar in general habitus and characters to Themarohystriz,
but it is readily separated therefrom on the characters of the frontal and scutellar
bristling. The upper pair of reclinate orbitals is much shorter than the second
pair, the infraorbitals are not very closely placed, they are equally long, very
distinctly shorter than the anterior supraorbital pair, and both are sloped forward
and slightly inward; the ocellars are minute, and the postverticals are much more
widely separated than in Themarohystrix. The preapical pair of scutellar bristles
is much shorter than either of the other two pairs, and there is no distinct ptero-
424 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
pleural bristle. The fore femur in the male is thicker than the other pairs, and
sometimes very strongly spined or bristled on the central part of the postero-
ventral surface and usually furnished with some short bristles on the anteroventral
surface. In the known males either the fore tibia or fore tarsus is modified. There
are no long strong bristles on the anteroventral surface of the hind femur beyond
the middle in any species as yet known to me.
Key to the Species.
Face with a brown spot on each side near lower margin; male with no modification
of apex of the fore tibia, but with a stout process at the apex of the metatarsus
that projects along the anterior side of the second segment and is covered with
minute black spines at its apex; wings greyish-hyvaline, with a brown border
on the costa, on second vein, on third vein beyond the inner cross-vein, on fifth
vein along the discal cell, and on fourth vein from before outer cross-vein to its
EN GXESS: Doin. &.6 Cucub lOO muon 0.010. Geo nia. cide 6 eAvoio els OIG OCICS Ol O1O DiOsONO.G-o-DId.b Oto puncticeps, n. sp.
Face yellow; fore tibia of male with a spongy swelling at apex on posterior side, and
the fore tarsus normal; wings quite evenly blackish-brown apically, usually
Hy aAlinevonmbasal wha fete she we cdase Secwe ve wiser eves ele ee MER Sh Teed eae oe ROR ITER ener 2
De SINE Si ese cae ete eds ee cena ee es Anomoea Walker
Fourth wing-vein straight proximad of the inner cross-vein ..................-. 17,
17. Wing dark brown on the costal half or more, with or without a hyaline or subhyaline
mark on the costa beyond the apex of first vein and with the hind margin more
or less broadly hyaline, the posterior edge of the dark portion usually irregular ;
lobe of the anal cell rather short, tapered to apex .............. Hemilea Loew
Wing either black with hyaline marginal and discal markings, or almost equally black
and hyaline, the black markings not confined to costal half .............. 18
18. Frons not less than twice as long as wide, the ocellar bristles quite short and fine,
not longer or stronger than the posterior supraorbitals; anal cell with long
vat Mole” oaodadd os oUpu cd bdoo Om amo ooo do coco OO O Pseudospheniscus Hendel
Frons much less than twice as long as wide, the ocellar bristles long and strong,
distinctly longer and stronger than the posterior supraorbital pair .......... 19
19. Postocular cilia yellowish-white; scutellum yellow, with black spots at bases of the
bristles; third antennal segment sharply angulate at apex above ............
OSU O NO oo COM D Out TO WO Oe eC eo oo Oe Sees roams Oedaspoides Bezzi
Postocularveilia and allyotherycephalic bristlessblackas- ieee ieee 20
20. Scutellum black and yellow; anal cell with an elongate apical lower lobe (fig. K)
£0 CHOON OA DO EF CUO OI ROLCEO OIC OL CEA Re EOICIGIO ICO OREO Gc loko naa OG Ceratitella, n. gen.7
Scutellum black; anal cell with a very short angular lower apical lobe ............
FOTOS OUI PORE OD OF ACO IHORR Pr RRP otcr a tore daira c mioec aolonere Spheniscomyia Bezzi
N.B.—It should be noted here that where I have given in parentheses ( ) the
locality of a genus listed in the above key it is not treated in the following text,
though there may be, in one or two cases, some reference to such a genus under
one of those that occur in New Guinea or Australia. There is a possibility that
some of these genera may yet be found in the region covered by this report.
EUPHRANTA Loew.
Mon. Europ. Bohrfl., 1862, 28—Lagarosia van der Wulp, Tijdschr. v. Ent.,
Xxxiv, 1891, 210.
* The characters cited for the segregation of this genus will suffice for use in this
region only.
7 See note, p. 465.
BY J. R. MALLOCH. 443
I am synonymizing the above two generic names after a careful comparison
of the type-species of each. Hendel, in his key to the genera in 1914, presents no
better character for the segregation of Lagarosia from its allies than the type of
wing markings, and a classification based upon this character is unreliable.
My examination of the genotypes discloses the fact that they are closely
related, having the same cephalic characters as well as the same thoracic bristling,
the presutural bristle being absent in both, while the wing venation and bristling
are the same. One important character, not mentioned by any writer on the
family except Hendel, that links both and segregates them from most related
genera known to me, is the presence of many erect fine hairs on the metapleura
above the central furrow. I consider therefore that the above cited synonymy is
warranted.
The long-haired aristae, four scutellar bristles, 2-3 infraorbital and 1 supra-
orbital, lack of the presutural bristle, very small ocellars, the setulose third
wing-vein, and metapleural hairs, will separate this genus from any other in the
Australian region.
But one species is as yet reported from Australia.
EUPHRANTA MINOR Hendel.
Ent. Mitt., xvii, No. 5, 1928, 362.
A small species, 4 mm. in length without ovipositor. Head yellow, frons
shiny, as wide aS one eye and 1:5 times as long as wide; two infraorbitals.
Longest hairs on aristae about two-thirds as long as width of third antennal
segment. Thorax reddish-brown, whitish-dusted, shiny, hind margin of mesonotum
and the scutellum bare, the latter paler yellow, flattened on disc. Mesophragma
(= pleurotergite) white-haired. Halteres yellow. Legs including the coxae yellow.
Abdomen rusty-coloured, shiny, yellowish-haired, the apical two tergites with black
Marginal bristles. Venation and markings of the wings as in Staurella cruz
Bezzi. The brown basal cross-band lacking, the one over the inner cross-vein as
in crux. There are some additional dark markings, including a straight fascia
over the outer cross-vein to the costa, but the tip of the wing has a white mark
that extends over the tips of third and fourth veins and is convex inwardly;
the posterior basal cell is brown, with only a small hyaline mark on the hind
margin; base of wing hyaline, the veins yellow.
Darwin (Palmerston), N. Territory, Australia. Type in collection of Deutsches
Entmologisches Institut.
EUPHRANTA SCUTELLATA Malloch.
Ann. Mag. Nat. Hist., (11) iv, 1939.
A larger species than minor, averaging 8 mm. in length, with thorax black
except on each side just behind suture, two large spots in centre of postsutural
area, and the apical two-thirds of the scutellum which are yellow. Legs pre-
ponderantly black. Wing with a large black-brown mark from base of stigma to
apex that extends back to middle of the discal cell, a large spot on costa just
beyond apex of first vein and the extreme apex whitish-yellow.
Solomon Islands.
XANTHOTRYPETA Malloch.
Op. cit., (11) iv, 1939, 250.
Generic characters.—This genus is similar to Huphranta in all characters,
but lacks the sternopleural bristle. The frons has two pairs of inwardly-directed
444 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
infraorbitals, the upper one twice as far from the lower as it is from the single
pair of reclinate supraorbitals, ocellars microscopic, the postverticals mere hairs,
outer verticals about half as long as inner pair, surface of frons shiny. Longest
hairs on arista about as long as width of third antennal segment, the latter
three times as long as wide, slightly tapered to the narrowly rounded apex;
face concave in profile, parafacials invisible centrally in profile, gena narrow.
Central pair of scapular bristles lacking, lateral pair distinct, presutural, acro-
stichal, sternopleural, and pteropleural bristles lacking, scutellum flat above, with
four strong bristles and the dise closely short-haired, metapleural (pleurotergite)
with the upper half above the impressed line furnished with numerous fine erect
hairs. First wing-vein setulose from well before node to apex above and at apex
below, third setulose to about midway from base to inner cross-vein above and at
base below; first posterior cell not narrowed at apex; anal cell with a subtriangular
apical lower angle or lobe.
Genotype, Xanthotrypeta bimaculata Malloch.
XANTHOTRYPETA BIMACULATA Malloch.
Ann. Mag. Nat. Hist., (11) iv, 1939, 250, Pl. x, fig. 13.
A reddish-yellow species, with an elongate shiny-black mark on each side of
anterior margin of mesonotum above the humeri, the frons darkened centrally, legs
yellow, the mid and hind tibiae largely browned, the wings yellowish, more
distinctly so in front, with a fuscous fascia from stigma to over the inner cross-
vein that is carried forward to connect with the large apical black-brown mark
beginning midway between the cross-veins and filling the apical third or more of
the wing except the hind margin as far in as the middle of the discal cell, a
small mark in margin of the second posterior cell near lower extremity of the
outer cross-vein, and a narrow lunate mark across the apex of the first posterior
cell, these excepted portions whitish-hyaline.
Length, 8 mm.
Solomon Islands. Type in Imperial Institute of Entomology.
CYCLOPSIA, nN. gen.
Generic characters.—Frons depressed down centre, with two pairs of rather
closely placed weak incurved infraorbital bristles on anterior fourth, and one pair
of stronger reclinate supraorbital bristles near upper third, only the inner verticals
present; ocelli extremely close together. Antennae extending to lower fourth
of face, third segment fully three times as long as second and its own width,
slightly tapered to the rounded apex; arista with the longest hairs not more
than half as long as width of third antennal segment. Face slightly receding
below, foveae rather deep, epistome not projecting; eye higher than long, more
narrowed below than above; gena narrow, the bristle weak. Thorax with the
following bristles: outer pair of scapulars, 2 notopleurals, 1 supra-alar, 2 postalars,
4 scutellars, the prescutellar pair of acrostichals widely separated, the mesopleural,
pteropleural, and sternopleural bristles rather weak, the acrostichal pair reduced
to short fine hairs. Scutellum flattened, subtriangular, disc minutely haired. Legs
normal, femora not spinose; mid tibia with a strong apical ventral spur. Wings
narrow, much as in Adrama, but the second vein is straight, about as far from
costa as from third vein just beyond apex of first, and the stigma is equal in
length to the costal cell. Abdomen elongate-ovate, basal composite tergite nearly
as long as the next two tergites combined, fifth tergite longer than fourth,
tapered to apex.
Genotype, Cyclopsia inaequalis, n. sp.
BY J. R. MALLOCH. 445
CYCLOPSIA INAEQUALIS, Nn. sp.
6. Head orange-yellow, dull on face, genae, and lower occiput, shiny from near
anterior margin of frons and becoming glossy behind and on upper occiput, the
frons with a large brownish-black mark from near anterior margin to ocelli
that is narrow in front and widens to fill entire width at ocelli, the vertex reddish-
yellow, upper occiput glossy-black except in centre; third antennal segment
brownish-black except extreme base; palpi yellow. Frons nearly twice as long as
wide; surface hairs microscopic, yellow.
Thorax brownish-yellow, distinctly shiny, the humeri and a broad streak down
the posterior third of the mesopleura to middle coxae lemon-yellow, the posterior
notopleural calli and scutellum pale-yellow; mesonotum with two broad brown
vittae along the inner edges of the humeri traceable on entire extent, darkest
in front and paler behind the suture, the intervening area grey-dusted and with
quite dense pale hairs; pleura blackened in front of the yellow central stripe
except on the propleura, and entirely black behind it, including the postnotum,
the latter slightly grey-dusted. All the bristles black; hairs largely pale, the
scutellar hairs black. Scutellars four.
Legs orange-yellow, mid and hind tibiae dark brown; fore legs missing. Mid
tibia with a series of very short posterodorsal setulae; no setulae evident on the
hind tibia, tarsi incomplete, the metatarsi long and slender.
Wing as Figure H, hyaline, yellow along the costa from the fork of second
and third veins, with a small deep brown transverse mark on the inner cross-vein
that does not extend to costa, and the entire apex dark brown from slightly
before the outer cross-vein and well before the apex of second vein, the inner
edge of the mark almost straight. First vein setulose from a little before node
to apex above, bare below; third vein setulose from base one-third of the distance
to inner cross-vein above and at extreme base below; lobe of anal cell elongate
triangular. Halteres yellow.
Abdomen glossy reddish-yellow, blackened from apex of composite tergite to
tip, with a subtriangular grey-dusted mark in centre of apices of third and
fourth tergites. Hairs quite dense, short, decumbent, and black; no bristles
present.
Length, 8 mm.
Type, Dutch New Guinea, Cyclops Mts., Sabron, Camp 2, 2,000 feet, May
1936 (L. HE. Cheesman). Type daimaged in shipping, the head mounted on same
card, fore legs missing.
This genus connects the Adraminii with the Huphranta group rather distinctly.
COLOBOSTRELLA Hendel.
Wien. Ent. Zeitg., xxxiii, 1914, 79; Ann. Mus. Nat. Hung., xiii, 1915, 428.
This genus probably belongs to the group with haired pleurotergite, but I
have not seen the genotype, which is described from Celebes. It may occur in
New Guinea.
In Hendel’s description the following bristles are given as lacking or
rudimentary: ocellar, postvertical, presutural, dorsocentral, and sternopleural.
He also lists the “Schietelborsten’”, but I am uncertain just what bristle he
refers to by this name. In his 1914 key he states that there is but one infraorbital
bristle, and in 1915 he states that there is an infraorbital and a supraorbital pair.
If Kambangania de Meijere is a synonym then there is a difference in the frontal
bristling, as de Meijere says that in his genotype there are four pairs of orbitals,
446 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
the anterior and posterior pairs being weak and hair-like. In both the genotypes
the second wing-vein is distinctly undulated, and the first vein enters the costa
much farther from the apex of the subcostal vein than the latter is from the
humeral cross-vein. In Xanthotrypeta the stigma and the costal cells are subequal
on the costal edges, and the second vein is straight. In Xanthotrypeta the inner
cross-vein is at or slightly before the middle of the discal cell, while in the other
two species it is about the apical third of that cell.
COLOBOSTRELLA RUFICAUDA Hendel.
Op. cit., xiii, 1915, 429.
A shiny reddish-yellow species. Mesonotum with a large glossy-black rounded
mark on each side between the humeri and the suture and two similar elongate
marks behind the suture that widen behind; pleura with two black spots, one at
the prothoracic spiracle and one before the mesopleural suture; postnotum with
two black stripes. Abdomen with a black mark on each side of each tergite. Wing
yellowish-hyaline, with a narrow black fascia from middle of stigma to over
second vein, a broader slightly-curved fascia from costa to middle of discal cell
just beyond the inner cross-vein that is narrowly connected on the costa with the
large apical black mark, the latter with a hyaline spot near apex of the first
posterior cell.
Celebes.
Possibly a synonym of Sophira bistriga Walker, described from Celebes.
PSEUDINA, nl. gen.
Generic characters.—Frontal bristling different from that of any allied genus,
the orbitals consisting of four pairs, the upper two pairs very small and evidently
the supraorbitals, the upper infraorbital pair at upper third of orbits and twice
as long as the anterior pair, both pairs slightly proclinate and incurved; ocellars
minute, shorter than the incurved postverticals; outer verticals much shorter than
the inner pair; face slightly carinate in centre, epistome not projecting; post-
ocular cilia dark and bristle-like; antennae normal; aristae pubescent. Thorax
with all bristles present, the four scapulars fine, dorsocentral pair distinctly
behind the supra-alars, prescutellar acrostichals strong; mesopleurals 2; scutellum
with one or two luteous hairs and four strong black marginal bristles. Wings
marked much as in Rioxa, the first vein setulose from near apex of node to tip
above, bare below, third vein setulose from base to near level of outer cross-vein
above and below, fifth vein bare; inner cross-vein about one-fifth from apex of
discal cell. Legs normal, fore femur with posteroventral bristles, mid tibia with
no central setulae, and a strong apical ventral bristle, hind femur without ventral
bristles, hind tibia with a regular series of short closely-placed anterodorsal
dark setulae. ;
Genotype, Pseudina buloloae, n. sp.
PSEUDINA BULOLOAR, Nl. Sp.
¢. Glossy brownish-yellow, face a little paler, small ocellar spot black;
mesonotum without dust or vittae; humeri, scutellum, and a streak along upper
edge of pleura lemon-yellow; abdomen with black mark on each side of each
tergite at curve; legs yellow: wings dark brown, with hyaline and yellowish
markings (Pl. xi, fig. 14).
Frons shiny, depressed centrally, a little longer than wide and slightly
narrowed in front, with a few microscopic pale hairs; profile as Figure I.
BY J. R. MALLOCH. 447
Mesonotal hairs short, dark, depressed and numerous. Scutellum short, flattened
above. Legs normal.
Wing-veins dark brown. Lobe of anal cell elongate; first posterior cell
parallel-sided at apex; stigma short, black-brown except a hyaline line across
base. Halteres yellow. Squamae brown, the fringe dark brown.
Abdomen broadly ovate, convex above, with blackish hairs and black bristles.
Fifth tergite longer than fourth, rounded at apex, with some quite strong apical
and lateral bristles.
Length, 6 mm.
Type, Bulolo, New Guinea (F. H. Taylor).
This species reminds one of the species of the Rioxa group, but there are
only four scutellar bristles, though a bristly hair on one side in the type-specimen
is in the position that the intermediate pair of bristles occupies and may represent
that pair, and the arista a merely short pubescent.
HeEmMILEA Loew.
Mon. Eur. Bohrfl., 1862, 32.—Ocnerus Costa, Atti Acad. Sci. Napoli, v (2), 1844,
102.
This genus is unrepresented in the New Guinea collection before me, but it
may yet be found here as there are species occurring as close as the Solomon
Islands and Fiji.
In a paper now in the press dealing with the Solomon Islands species I
present data on the species from this region so that it may be possible to identify
any such that occur in New Guinea if already described.
The genus extends from Europe to Japan and southward to the Solomons
with some closely-related species that have been removed to other genera in
Africa. All the known species have the costal half or more of the wing dark
brown, and the posterior half hyaline, the costa sometimes having a hyaline mark
close to the apex of first vein, and the hind edge of the dark portion being more
or less irregular in most species.
CALLISTOMYIA Bezzi.
Mem. Ind. Mus., iii, 1913, 124.
This genus contains four species, only one of which is known to occur in
the region under consideration. The genotype, pavonina Bezzi, occurs in India and
Formosa. I have examined specimens. The outstanding character of the genus
consists of the small stout spines on the apical halves or more of the antero-
ventral and posteroventral surfaces of the mid and hind femora. The genotype
has the following bristles on the head and thorax: 2 supraorbitals, 3 infraorbitals,
inner verticals long, outer pair short, postverticals short; 1 humeral, 1 presutural,
2 notopleurals, 2 postalars, a pair of dorsocentrals almost in line with the
acrostichals, 4 scutellars, 1 mesopleural, 1 pteropleural, 1 sternopleural, and a fine
propleural just below the humerus. Ocellars lacking. Scutellum flat, sub-
triangular. First and third wing-veins setulose, those on first vein carried to base
of the node. Venation closely similar to that of Sophira. Sixth tergite of
abdomen in female shorter than the fifth.
CALLISTOMYIA HORNI Hendel.
Hint. Mitt., xvii, 1928, 361.
Similar to the other species of the genus in general coloration, agreeing
with pavonina Bezzi in having a black spot on the lower centrai portion of the
448 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
face, and differing from it in the lack of a black fascia on the bases of the
abdominal tergites. Thorax brownish-yellow, the humeri and a vitta below the
notopleural suture lemon-yellow, the latter continued to base of the wing, scutellum
lemon-yellow, mesonotum with five black vittae posteriorly.
Darwin (Palmerston), N. Territory, Australia. Type in the collection of the
Deutsches Entomologisches Institut, Berlin-Dahlem, Germany.
CARPOPHTHORELLA Hendel.
Wien. Ent. Zeitg., xxxiii, 1914, 80; Ann. Mus. Nat. Hung., xiii, 1915, 448.
This genus was erected for the reception of a new species, magnifica, from
Formosa. It is the only species as yet assigned to the genus. The very striking
character of the 6 to 10 pairs of strong incurved equal infraorbital bristles
distinguishes the genus from its nearest allies. The species bear a superficial
resemblance to those of Gastrozona Bezzi and Callistomyia Bezzi.
There are two known species that may be separated as below.
A. Frons with 6-7 pairs of infraorbital bristles; wing with a subhyaline mark on costa
just beyond apex of first vein; mid and hind tibiae browned apically (Formosa)
OTC OSOMAIC OA one Oinitie Gna O Mich GEES Huts tec CACC REMC CRRA See IDeecacntaciacrere oar’ eto, Bic magnifica Hendel
AA. Frons with 10 pairs of infraorbital bristles; wing without a subhyaline mark on
the costa just beyond apex of first vein; legs entirely orange-yellow (Solomon
TSTDIVAS Masco oy stcucte sconce guste mosucnedel cage. sce ucleysNetals Mauamer ious utes trea sacmnitene setifrons Malloch
It is possible that setifrons will be found in some of the other island groups
in the same region.
CARPOPHTHORELLA SETIFRONS Malloch.
Ann. Mag. Nat. Hist., (11) iv, 1939.
The large number of closely-placed pairs of incurved infraorbital bristles in
this species will at once distinguish it from any other in this region.
Solomon Islands.
CRISTOBALIA Malloch.
Ann. Mag. Nat. Hist., (11) iv, 1939.
Generic characters.—Frons at vertex less than one-third of the head-width,
narrowed to anterior margin and more than twice as long as wide, with three pairs
of infraorbital and one pair of supraorbital bristles, the ocellar and outer vertical
pairs undeveloped; aristae very short haired, longest hairs about twice as long as
width of arista at base. Thoracic bristling complete, scutellars four. First and
third wing-veins setulose; inner cross-vein at middle of the discal cell.
CRISTOBALIA LUTEA Malloch.
Op: cit.) (11) Miv, 1939% 265; Pl. oxi) figs 22:
Described from the Solomon Islands.
ANOMOEA Walker.
Ent. Mag., iii (1), 1835, 80—Phagocarpus Rondani, Bull. Soc. Ent. Ital., iii,
ial, 17d
Most recent writers on the family have used Rondani’s name for this genus
under the belief that Chevrolat’s similar name had priority over that of Walker. It
has been conclusively proven that the part of Chevrolat’s Catalogue containing the
name Anomoea did not appear until 1837. Thus Walker’s name must be used for
the Trypetid genus.
The genus has been generally misinterpreted by writers on the family and a
number of species have been placed in it that do not properly belong to it, while
at least one species that belongs here has been placed in another genus.
BY J. R. MALLOCH. 449
The most striking character for the recognition of the genus is the down-
wardly bent antepenultimate section of the fourth wing-vein, a character met with
in the Otitid genus Rivellia Robineau-Desvoidy. The anai cell has a long narrow
apical lower lobe that is sometimes as long as the free part of the anal vein, and
the third antennal segment is about twice as long as wide, nearly attaining the
epistomal edge.
There are four species of the genus, as I interpret it, known to me; they may
be distinguished as in the key given below. All except the genotype, permunda,
may yet be found in New Guinea or on islands close to it.
Key to the Species.
PETAR CSE Ii eatwnye LOW pus ipcican cess oO ica oe es oxoal « averctee oka iae Sayeed onrrchimwowd a sheers O58 2
Inlay Wyihtin Gena aa Oe IdlR@k UNOS sonscosccubebeudavogub eu suuoaguaanabodD 3
2. Thorax largely, and the legs entirely yellow (Palaearctic, Formosa) .. permunda Harris
Thorax entirely, and the legs largely black ...................... nigrithorax, n. sp.
(st)
The small hyaline mark in the costal cell of the wing quadrate, extending to the
costal vein, the latter yellow along the edge of the mark (Solomon Islands)
518 BROLACERO EG at Oko ca DEAE Geneon Gian SOLS Lats oi 5lo "ca ROO NCES SAGE MONCH ce CREA RSE ER Ree quadrata Malloch
The small hyaline mark in the costal cell of the wing elongate, not attaining the
costal vein, the latter black along the edge of the mark (Fiji Islands) ........
O76 6, Beh ae na Eaeby Ciel OREN NSH? olitlen ORE RPGR Gl Oia SEO TORD EE ICIS a CrGer eS camer Roun eR Cec ORT curvinervis (Bezzi)
ANOMOEA NIGRITHORAX, N. Sp.
?. Head black, frons dull brown, with whitish-grey dusting, most evident on
the orbits, face brown, shiny below, with rather dense whitish-grey dust, gena
brown, occiput shiny black; antennae and palpi red. Frons at vertex fully one-
fourth of the head-width, slightly narrowed to anterior margin, and fully twice as
long as its central width; uppermost of the three pairs of incurved infraorbital
bristles at about two-fifths from upper margin, not much in front of and distinctly
laterad of the anterior pair of supraorbitals, the latter much longer than the
posterior pair; outer verticals about half as long as the inner pair; surface hairs
centrally rather numerous, short, erect and dark. Antennae elongate, nearly
attaining the epistome, third segment about three times as long as wide, rounded
at apex; arista pubescent. Gena not higher than width of third antennal segment,
with numerous short stiff black hairs, vibrissal angle more produced than in the
other species.
Thorax black, glossy, the mesonotum rather densely grey-dusted on disc, with
three black vittae on anterior half. Dorsocentral bristles slightly in front of the
transverse supra-alar line; secutellars subequal, the hairs on sides of scutellum
very minute.
Legs black, fore femora brownish on anterior surface, fore tibiae, mid tibiae
except their bases, and apices of hind tibiae, and all the tarsi orange-yellow.
Wing hyaline, with black markings as Plate xi, figure 15, the small hyaline
mark in the costal cell quadrate, extending entirely across the cell, the vein in
front of it black. Second vein not running for any distance closely alongside the
costal vein at its apex as in some of the other species, third vein with a distinct
arch beyond the black preapical fascia, inner cross-vein at about its own length
from outer; setulae on third vein extending to or slightly beyond the inner cross-
vein above. Halteres yellow.
Abdomen glossy-black, with narrow grey-dusted apical fascia on second and
third tergites. General shape broadly ovate, ovipositor sheath flattened, short
and broad.
Length, 4:5 mm.
Type, Edie Creek, New Guinea (F. H. Taylor).
450 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
SPHENISCOMYIA Bezzi.
Mem. Ind. Mus., iii, 1913, 146.
This genus is very similar to Tephrella Bezzi, differing essentially in having
all the cephalic bristles including the postocular cilia black, the latter short and
fine, and the scutellum with four strong bristles. There is a slight angular
production of the lower apex of the anal cell that is sometimes not evident in
Tephrella.
SPHENISCOMYIA SEXMACULATA (Macquart).
Dipt. Ezot., ii, Pt. 3, 1848, 222 (Urophora).
There is some question as to the distinctness of this species from atilia Walker.
The entirely yellow hind tibiae have been cited as a distinguishing character for
the latter. In both the specimens I have from this region the hind tibiae are
infuscated on their basal halves or more, and in the specimen in which the
antennae are present they are largely darkened.
Admiralty Island; Papua. Recorded by Hendel from Australia in 1928 (Ent.
Mitt., xvii, 364).
PSEUDOSPHENISCUS Hendel.
Suppl. Ent., ii, 1913, 82.
This genus contains species that rather closely resemble those of Anomoea,
but the fourth wing-vein is straight before the inner cross-vein. The frons is
usually about two or more times as long as its central width, and the ocellar
bristles are quite weak, contrasting markedly with those of Spheniscomyia. I
have not enough material to justify definite conclusions on the status of the genus
or the various species referred here, but it appears possible that some future
worker may subdivide the present concept. In the only New Guinea species I
have the frons is a little less noticeably narrowed than in some of the other
species, and the antennae are a little shorter than in such species as fossata
Fabricius, to which it is rather closely similar in most other features.
I present below a key to the three species from this region that are known
to me at this time.
Key to the Species.
1. The entire costal margin of wing from base to middle of apex of first posterior cell
black, the black pattern sending three branches to or almost to hind margin, the
first on the anal cell that is narrow and does not reach the apex of sixth vein,
the second very broad, tapered behind and covering the basal two-thirds of the
discal cell, the third in the form of an inverted V, with its inner arm over the
outer cross-vein and enclosing it and the outer arm ending near apex of the
Lounth kveln (CH is))* eee torsivevecce eters ey eed estate eo: Orehc colons tor te reeetone reno (eves weseiee bifidus Bezzi
Costal border not entirely black, the costal cell partly whitish-hyaline, and another
‘break in the dark mark beyond apex of first vein, the pattern not as above .. 2
2. Costal cell with two subquadrate whitish-hyaline marks; mesopleura except its
anterior margin lemon-yellow (Fiji) .................. mesopleuralis Malloch
Costal cell hyaline, dark brown along the anterior and apical edges; mesopleura
entirely Black Ais.) sea aes Se Ty, A I EEE BRD: AA oe taylori, n. sp.
PSEUDOSPHENISCUS TAYLORI, 1. Sp.
3, 9. Head entirely orange-yellow, the ocellar spot only dark. Frons at vertex
one-fourth of the head-width, hardly narrowed in front, and twice as long as wide;
with the usual bristles, the ocellars about as long as the posterior supraorbitals.
Antennae extending to lower third of face.
Thorax shiny black, humeri and propleura brownish-yellow, mesonotum rather
densely brownish-grey-dusted, with three faint linear dark vittae, the outer pair
BY J. R. MALLOCH. 451
most evident and along the lines of dorsocentrals. Apical scutellar bristles
much shorter than the basal pair, most markedly so in the male.
Legs orange-yellow, mid and hind coxae and femora and basal halves of hind
tibiae blackened. Posteroventral bristles on fore femora quite strong; apical ventral
spur on mid tibia strong; hind tibia with a series of weak anterodorsal setulae.
Wing whitish hyaline, with black markings as Plate xi, figure 16. Inner
cross-vein at a little more than its own length from outer; third vein setulose
to inner cross-vein above; first vein setulose from just before apex of node to tip
above, and at apex below. Halteres black.
Abdomen broadly ovate, glossy-black, with black hairs and bristles.
Length, 3-4 mm.
Type, male, Bulolo, New Guinea (F. H. Taylor); allotype, Papua: Ishurava,
3,000 feet, July 1933 (L. E. Cheesman); paratype, in poor condition, Wewak,
New Guinea (F. H. Taylor).
CerRATITIS McLeay.
Zool. Journ., iv, 1829, 475.
This genus is represented by but one species in this region, the widely distributed
Mediterranean Fruit Fly. It may be readily distinguished from all other genera
of the family by the characteristic diamond-shaped apical palette on the anterior
pair of supraorbital bristles of the male, the small black spots or short streaks
in the centre of the cells of the basal half of the wing, and the dense stubble-
like yellow bristles on the posteroventral and apical portion of the anteroventral
surfaces of the fore femora of the male. The characters cited in the foregoing
key to the genera will distinguish both sexes from other genera in this region,
though they cannot invariably be successfully applied for the distinction of the
genus in other regions.
CERATITIS CAPITATA (Wiedemann).
Anal. Entomology, 1824, 55 (Trypeta).
This species is distributed from Southern Hurope through tropical portions
of Africa and Asia as well as in the Hawaiian Islands, and tropical portions of
Australia. It has been introduced in commerce in some other sections of the
world, but has failed to establish itself permanently, notably in Florida. The
lack of continuous supply of suitable fruits for the larvae prevents its being more
than a passing menace except in strictly tropical countries.
In addition to the characters mentioned above, it may be worthy of note that
the stubble-like postvertical and lateral bristles on the head and the setulose node
of the first vein of the wing should be carefully considered as possible indices to
a closer affinity with the Tephritinae than with the Trypetinae.
I have seen no specimens from this region.
I figure the characteristic anal cell of this species (Fig. J).
OEDASPOIDES Hendel.
Wien. Ent. Zeitg., xliv, 1927, 63.
This genus is unknown to me, so that I have to depend upon Hendel’s
description for distinguishing data.
Despite the suggestive generic name the genus is apparently not very closely
related to Oedaspis Loew, the frons in the latter being much broader and more
convex, and the scutellum markedly convex and highly polished.
452 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
In his comparative data Hendel states that the third antennal segment is
sharply angled at the upper apical corner, the sixth abdominal tergite of the
female is shorter than the fifth, and the postocular cilia yellow and pointed. The
wings have several dark fasciae as in Oedaspis and Rhagoletis Loew. In some
respects the genus must resemble Chrysotrypanea described herein, but in the
latter the third antennal segment is rounded at apex, and the orbitals are 3 + 2
instead of 2 + 2, and the postocular cilia stubble-like and pale yellow.
There are two species that Hendel places in Oedaspoides.
OEDASPOIDES ESCHERI (Bezzi).
Boll. Lab. Zool. Portici, v, 1911, 21 (Oedaspis).
Described from Sydney, N.S.W.
OEDASPOIDES ACUTICORNIS Hendel.
Wien. Ent. Zeitg., xliv, 1927, 63.
Head pale yellow, with whitish dust on orbits, triangle, and face; bristles
reddish-yellow, behind pale-yellow. Thorax black, humeri, suture, pleura over
the fore coxae and in front of wing bases ochre-yellow, densely grey-dusted. Hairs
pale yellow, the bristles reddish. Scutellum yellow, undusted, and at the bases
of the two apical bristles black. Postnotum grey-dusted. Abdomen ochre-yellow,
the bases of the tergites with dark fasciae, broader laterally, centrally interrupted
on tergites 2 to 4. Genital cone as long as tergites 5 and 6 combined, glossy-
black, with dark hairs, other abdominal hairs whitish-yellow. Legs and halteres
yellow. Wings as in escheri; the hyaline fasciae are all narrower, not wider,
than the brown ones, and there is no hyaline dot at apex of first vein.
Sydney, N.S.W.
CERATITELLA, Nh. gen.
Generic characters.—Quite similar in general appearance to Ceratitis capitata,
but all the cephalic bristles and the postocular cilia are black, the anterior supra-
orbital bristles in the male are simple, the fore femora in the same sex have only
the normal bristles, the wings are not as wide at the anal angle, though the
markings are quite similar, especially in the basal cells, the lobe of the anal
cell is much as in the other genus but not as markedly sinuate, there is no
outstanding costal bristle at the apex of the subcostal vein, and the third antennal
segment is rather noticeably sharpened at the upper apex. In this last character
the genus appears to resemble Oedaspoides, as well as in the swollen and black
and yellow scutellum, but the black postocular cilia and the black dotted and
streaked basal portion of the wing are different from that of Hendel’s genus.
Genotype, Ceratitella loranthi (Froggatt).
CERATITELLA LORANTHI (Froggatt).
Proc. Linn. Soc. N.S.W., xxxv, 1911, 863 (Ceratitis).
dg. Head orange to brownish-yellow, with a lemon-yellow band across anterior
fourth of frons, the face and anterior portion of genae yellowish-white, glossy,
ocellar black spot small; antennae, aristae, palpi, and proboscis orange-yellow. All
bristles, including the genal one, black, central minute hairs on frons and genal
margins black, those on lower portion of back of head yellow. Orbitals 2 + 2, the
upper reclinate pair much shorter than the lower and not longer than the
moderately long ocellar pair; post-verticals shorter and finer than the latter, outer
verticals about half as long as the inner pair. Width of frons at vertex about
BY J. R. MALLOCH. 453
two-thirds its length and two-fifths width of head, slightly widened in front.
Face slightly concave in profile, epistome not protruded, centre flat, a slender
fovea on each side most evident below, lower margin transverse; eye vertical,
about 1:25 times as high as long, longest at middle opposite antennal insertion,
and about seven times as high as gena. Antennae extending to lower fifth of
face, with noticeable apical upper point; arista subnude. Postocular cilia very
short and setulose. Palpi spatulate; proboscis short and stout.
Thorax glossy black, the humeri, a large spot on each basal lateral angle of
the scutellum, the posterior portion of the mesopleura above a line from near
the spiracle to near the lower posterior angle, and most of the pleurotergite,
lemon-yellow; disc of the mesonotum with dense yellowish-grey dust on two
vittae from near anterior to near posterior margin, fused in front and behind,
with a short lateral spur on anterior edge of the suture, and a short vitta laterad
of the outer one behind the suture; hairs on the yellow parts and on dorsal vittae
yellow, on other parts mainly black, all the bristles black. All bristles present,
the dorsocentral and acrostichal pairs equally long, the former in line with the
supra-alar pair; scutellum convex and thick, with four strong bristles, the basal
pair in the yellow marks, the hairs fine and dark.
Legs entirely tawny-yellow. Fore femora with a series of black posteroventral
bristles; hind tibia with a series of short anterodorsal black setulae on basal
two-thirds or more.
Wing as Plate xi, figure 17, with black dots and streaks in cells on basal
third and the veins blackened, a broad brownish-black fascia from the stigma to
hind margin just in front of apex of anal vein, this connected on costa with a
broad costal band of the same colour that extends to wing-tip, filling apex of first
posterior cell, and very slightly notched below before apex and narrowly separated
from the costal vein along parts of its extent, and a third dark fascia that
emanates from the junction of the other two and extends obliquely to wing-
margin over both cross-veins. Costal spine very inconspicuous; first vein setulose
above from base of node to apex, and at apex below, third vein setulose from
base to beyond inner cross-vein above and below, fifth vein bare. Two streaks
from second vein to costa more intensely black than the other portions of the
cell, may sometimes contain vestigial spur-veins. Anal cell as Figure K. Squamae
white. Halteres yellow.
Abdomen shiny-tawny to srange-yellow, with black lateral marks on third and
fifth tergites and the apices of second and fourth narrowly whitish-grey-dusted,
hairs pale on the pale-dusted parts and base of second tergite, mainly black on
other parts. Fifth tergite with an apical series of fine black bristles.
Length, 4 mm.
Sydney, N.S.W., bred from Loranthus sp., Dec. 1938 (L. R. Clark).
ORTALOPTERA Edwards.
Trans. Zool. Soc. Lond., xx, Pt. 18, 1915, 419.
This genus is a peculiar one, with characters that make it difficult to associate
it with either Trypetidae or Phytalmiidae, though the cephalic and wing characters
strongly suggest the latter relationship. There are two pairs of orbitals, the supra-
orbital pair strong and reflexed, the infraorbital pair short, weak, and incurved.
The arista is long haired. The thorax lacks the humeral, presutural, prescutellar,
and propleural bristles, and has the scapular, notopleural, supra-alar, and meso-
pleural bristles strong, and the pteropleural and sternopleural bristles weak but
454 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
distinct. Scutellars four. Edwards states that the genotype has a preapical bristle
on the mid tibia, a character he states, erroneously, occurs also in Rioxa formosi-
pennis Walker. I have never seen a species of Trypetidae with a preapical dorsal
bristle on any tibia. The wing-veins are bare, another very exceptional character,
the second vein is undulated, and the anal cell is longer than the free part of the
anal vein, without an apical lobe, though longest on its lower edge, the vein closing
the cell slightly arcuate, and the inner cross-vein is far before the middle of the
discal cell.
ORTALOPTERA CLEITAMINA Hdwards.
Oyo, Olin, 20:5 Jeti, iB} allay, Zeit).
This species is quite similar to certain species of the genus Cleitamia, notably
in the wing markings. General colour uniformly dull-black, the head dull light-
ochreous-brown, with some darker mottling on the vertex, antennae and palpi
ochreous, third segment of former darker at apex. Legs blackish-brown, fore
femora, apices of mid tibiae, and the greater part of mid and hind tarsi more
reddish-brown. Wings dark brown, hyaline in costal, subcostal, posterior basal,
and anal cells, on a narrow fascia at middle that runs straight to fifth vein and
then curves apically, ending in hind margin below the outer cross-vein, a broadly
arched streak as wide as the fascia that is separated by a brown interspace about
its own width from the fascia, extending forward from fifth vein to second vein,
then running along the hind side of that vein and ending in the apex of the first
posterior cell, the anal angle also hyaline. Length, 10 mm.
Dutch New Guinea, Mimika River.
Subfamily TEPHRITINAE.
This group is usually distinguished from Trypetinae by the longer sixth
abdominal tergite of the female, the yellow stubble-like postocular cilia, yellow
postvertical, upper supraorbital, and outer vertical bristles, and the speckled wings,
on which the setulae of the first vein commence at the base of the node on its
upper surface. Frequently the pteropleural and posterior notopleural bristles are
yellow, and usually the surface of the thoracic dorsum has flattened yellow scale-
like bristles instead of fine hairs. The scutellum has never more than four bristles
and often has but two, the apical pair being absent or much shorter than the
basal pair. The dorsocentral pair of bristles are in most cases close to the suture,
thé arista is pubescent or bare, and the fifth vein is bare, while the third is rarely
setulose to beyond the inner cross-vein above. In one or two genera I have
included, the sixth abdominal tergite is not longer than the fifth. I include
Tephrella and Platensina here though they are generally placed in Trypetinae.
Key to the Genera.
1. Head on lower margin in profile much longer than at bases of antennae; proboscis
slender, chitinous, and geniculated at middle, without fleshy labellae, the apical
Section as lone as head on lower smaneineed-recieaeieeeiceicene Paroxyna Hendel
Head not or very little longer on lower margin than at base of antennae in profile;
jaye oVof(tes Kiwoybhe, \ypidoy tone Chokeeyl IRVINE, Gasdouuéancoo000d50050dnn 50000055 2
bo
Wing exceptionally broad, less than twice as long as wide, the widest point at outer
cross-vein, the anal angle undeveloped (PI. xi, fig. 21), ground colour brownish-
black, with some small hyaline wedge-shaped marginal incisions, the extreme
apex white, and sometimes some small hyaline dots in the field ..............
Paps arena Fat ice ACs oats car aOR ae ir BOER Rare eS acirez Fito ince ade hcintk cpeeh ae Platensina Enderlein
Wing either normal in width or slender, not less than twice as long as wide, widest
point usually near middle of discal cell, the anal angle usually well developed,
and not coloured and marked as above, or if but little more than twice as long as
wide and the markings and ground colour as above, then there is no hyaline
MArk At the SXtrEMEMCIP! . A rene steve cco: cee relhey oD eleren canes Rete oenrereteltehe Moen n eR OIE TEE aaa 3
BY J. R. MALLOCH. 455
38. Wing black or brownish-black, with whitish-hyaline incisions in the margin and at
most four small hyaline dots in the field ...................:.--60---+---- 4
Wing hyaline, with black or brown marks, sometimes fasciate markings broken by
numerous small hyaline dots, or yellowish-brown, with hyaline fasciae ...... 5
4. Wing more than 2:5 times as long as wide, the anal angle well developed; sixth
abdominal tergite of female about 1:25 times as long as fifth; apex of wing with
Bowhitertransverse /StreaMkesyinys sci. s lsdehesie) «fel eleaeders + cuetedencle si selere Spathulina Rondani
Wing not or very little more than twice as long as wide, without white mark at
extreme tip; sixth abdominal tergite of female not longer than fifth ..........
6 POOR D Oto Cano: 6 O10 DIE COROIGIG CCRC CRO IELG CCI cSne cir RSE ICRA ERO nares exicne a =areriee Tephrella Bezzi
5. Wing yellowish-brown, with hyaline markings, those on the dise consisting of three
fasciae from hind margin to near the second vein, converging in front; inner
cross-vein at or very close to middle of the discal cell; apical ventral spur on
mid tibia not longer than apical diameter of the tibia .... Chrysotrypanea, n. gen.
Wing not marked as above; inner cross-vein much beyond middle of the discal cell;
apical ventral spur of mid tibia much longer than apical diameter of the
TEL ODIET ts Hiker Buk PECL C HOES CoeeCalG tb. ce GIG Sonate GU CNOLE RGEG: SUCIC Ger foes Ieee Ieee OLS eR ORME ES SCRA RE Err ROARS Fer ke 6
6. Wing brown or brownish-black, with many small hyaline spots on entire area, the
base largely hyaline, with a black spot at base of the anterior basal cell that
extends over the fourth vein into the posterior basal cell; fore femur of male
thicker than the other femora; genital cone of female circular in cross section ;
third antennal segment more than twice as long as wide, distinctly angulate at
MPD CTL Pl CANICOLNER atalensacieiel ois ai chek rene elon sie eiiebereisueleue lets omeushe Camaromyia Hendel
Wing brown, with hyaline spots or with an apical star-like dark mark, or marked
with black along the costa and a black fascia from costa to hind margin over
the cross-veins, never with a black spot at base of the anterior basal cell that
extends over fourth vein into the posterior basal cell; fore femur in neither sex
‘much thicker than others; genital cone of female usually flattened, oval in
cross section; third antennal segment, if twice as long as wide, without upper
OLGA MecuTT Sl Cumawactewcicia cute eet elt eckenaarcchentie miloxeaen elec tera crore te maleratctay sir eeetey evarclaltetencusints 7
7. Wing markings consisting of a large star-like mark on apical half or less from which
emanate a few dark rays; scutellar bristles 2; infraorbitals 3 pairs ..........
ree reer Es ere a eo Uentin cues eh ean cael arte panies otieasey ahisyio. aie ertaneua he awl eeuacieedes Trypanea Schrank
Wing markings not as above, not confined to apical half nor star-like; scutellar
bristles 4, the apical pair sometimes short; infraorbitals 2 pairs .......... 8
8. Wing hyaline, with some brownish-black markings along the costa, a large mark at
apex which usually encloses one or two hyaline dots, and a similarly coloured
fascia from the costa to hind margin that encloses both the closely placed cross-
AYGUI TIS acy eset So AES Gacdrcrs Gn Sr GEM MCT PRO hc ao Rr al Sphenella Robineau-Desvoidy
Wing dark brown, with many indiscriminately arranged variably-sized hyaline spots
ONy CHE EN GIRE RARE Shame 5. Rea Tanimura er Gale Eis ans ecm le ltn cng seen mt als Tephritis Latreille
TEPHRELLA Bezzi.
Mem. Ind. Mus., iii, 1918, 151.
This genus superficially resembles Spheniscomyia Bezzi in structure, colour,
and wing markings, but may at once be distinguished from it by the presence of
but two scutellar bristles, the yellow postvertical and outer vertical bristles and
postocular cilia, the latter being stout, and stubble-like; the cross-vein closing the
anal cell is either straight or very slightly angled at centre so that the lower
posterior corner of the anal cell is not produced into a lobe.
I have recently described a species of this genus from the Solomon Islands,
and have another from Western Australia that I provisionally refer here. They
may be distinguished as below.
A. Wing (Fig. L) black, the costal cell with three whitish-hyaline marks, one against
the humeral cross-vein, a larger one before middle, and a narrower one near
apex, three pairs of whitish-hyaline marginal incisions, one just beyond the
apex of first vein, one in the second posterior cell, and one in the third
posterior cell below middle of the discal cell, and three small hyaline discal
spots, one in the first posterior cell beyond the outer cross-vein, one near apex,
and another before middle of the discal cell; pleura and lateral margins of
456 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
mesonotum and scutellum brownish-yellow, remainder of thorax black; cross-
Vein (closing thesanal) cell straienit ass jeeieiel. ere Reena eee sexincisa Malloch
AA. Wing black, costal cell whitish-hyaline on basal half, the six whitish-hyaline
incisions in the wing margin larger and longer than in sexincisa, the outer one
in the second posterior cell curved and extending forward to a little over the
third vein, the inner one to anterior extremity of the outer cross-vein, the pair
in third posterior cell widely separated, the basal one extending across the
discal cell near base, the other extending to fifth vein just before outer cross-
vein; thorax black, propleura brownish-yellow ; vein closing the anal cell slightly
aricked at Jig gle 5.5 5 3% ciate aerial. oleh anita she eae one rulio a aiatamoeraan aye australis, n. sp.
TEPHRELLA AUSTRALIS, N. Sp.
9. Head testaceous-yellow, slightly yellowish-grey-dusted, the ocellar spot
hardly darkened. Outer vertical, ocellar, and orbital bristles except the posterior
supraorbital, dark brown. Frons slightly more than one-third of the head-width
and about 1:25 times as long as wide, with three pairs of strong incurved infra-
orbitals and two pairs of supraorbitals, the posterior the shorter, the anterior
close to middle of frons; ocellars slightly behind the level of posterior edge of
anterior ocellus. Antennae short, extending to lower third of face, third segment
about twice as long as wide; arista pubescent. Gena not as high as width of
third antennal segment.
Thorax shiny-black, grey-dusted, pleura more distinctly so, the propleura
brownish-yellow, bristles brown, the scale-like mesonotal hairs pale yellow.
Legs yellow. Fore coxae each with a brown bristle near apex on anterior
side; fore femur with a series of brown posteroventral bristles; mid tibia with
an apical ventral brown bristle.
Wing brownish-black, whitish-hyaline at base to middle of costal cell and
on basal half of edge in front of the anal vein, the other whitish-hyaline markings
as in Plate xi, figure 18. Inner cross-vein at about its own length from apex of
discal cell; second vein slightly bent in the dark part between the costal hyaline
marks. Halteres yellow.
Abdomen glossy-black, abraded in type-specimen. Sixth tergite subequal to
fifth; sheath of the ovipositor elongate-conical, the ovipositor slender, spine-like,
yellow.
Length, 4 mm.
Type, Western Australia.
SPATHULINA Rondani.
Dipt. [tal. Prodr.. i, 1856, 113.
This genus is distinguished from its allies by the black wings with whitish-
hyaline marks, one at the tip distinguishing it from Tephrella (Fig. M; PI. xi,
fig. 19). The pair of dorsocentral bristles are at the suture quite noticeably in
front of the supra-alar line. Scutellars two. ;
SPATHULINA ACROLEUCA (Schiner).
Reise Novara, Zool., ii, i abt., B. Diptera, 1868, 268 (Tephritis).
This species is rather variable in wing markings and has been described
under several specific names. The distribution is very wide, from Africa through
Asia to Australia, including Guam, Fiji, ete.
Efflatoun records parceguttata Becker, which is accepted as a synonym of this
species, as having been reared from larvae feeding on Ceruana pratensis in
Egypt, and states that the larvae are known to live on Composites in South
Africa.
BY J. R. MALLOCH. 457
Shiraki, who records this species from Formosa, states that Schiner’s type-
specimen could not be found in his collection in Vienna, but there can be no
doubt that his species is the one dealt with above, regardless of whether there
may be some confusion in the matter of the relationship of forms described
under different names from other regions.
I have specimens before me from Townsville, Queensland; Canberra, A.C.T.
(F. H. Taylor).
The Canberra specimen has a hyaline dot near the apex of the discal cell of
the wing.
CHRYSOTRYPANEA, Nl. gen.
Generic characters.—This genus is an aberrant one in this subfamily, the
fasciate wings being like those of certain Trypetinae, though the yellow post-
vertical, outer vertical, and posterior supraorbital bristles, and thick yellow
postocular cilia clearly link it with the Tephritinae. Head higher than long,
face slightly produced below; frons more than one-third of the head-width, and
longer than wide, with hardly any central hairing, the orbitals 3 + 2, ocellars
long, in line with the posterior edge of the anterior ocellus. Proboscis stout and
short. Thorax with the normal bristles, the posterior notopleural yellowish-white
and pteropleural stout and white, the other bristles black; basal scutellars long,
apical pair microscopic. Legs rather stout, apical ventral bristle on mid tibia
not longer than apical diameter of the tibia. Wing normal in shape, inner cross-
vein at middle of discal cell, anal cell with triangular apical lower lobe; first
vein setulose from base of node to tip above and at apex below (Fig. G2); third
vein bare. Sixth abdominal tergite of female slightly shorter than fifth; sheath
of ovipositor conical, circular in cross-section.
Genotype, Chrysotrypanea trifasciata, n. sp.
CHRYSOTRYPANEA TRIFASCIATA, Nl. Sp.
9. Head dull orange-yellow, frontal orbits grey-dusted. Antennae extending
to lower third of face, third segment about 1:5 times as long as wide, rounded at
apex, hairs on basal segment yellow, on second black; arista subnude. The three
pairs of incurved infraorbital bristles equal in length, upper pair near middle, well
in front of the anterior pair of supraorbitals, the latter close to upper third and
about one-third longer than posterior pair. Gena about as high as width of third
antennal segment.
Thorax brownish-yellow, mesonotum except narrowly on lateral margins, and
the entire scutellum, glossy-black, lower part of pteropleura and the postnotum
black, greyish-dusted. Mesonotum thickly covered with depressed yellow scale-like
bristles. Metasternum bare.
Legs entirely yellow, hairs and bristles black, fore coxal bristles yellow. Fore
femur with a complete posteroventral series of bristles; no hind tibial setulae.
Wings (Plate xi, fig. 20) yellowish-brown, with a rather faint broad subhyaline
fascia from middle of costal cell to near hind margin and three narrow anteriorly
convergent hyaline fasciae beyond it from hind margin to near second vein, the
first from near apex of anal vein, ending in front of inner cross-vein, second
between the cross-veins, the third from near upper apex of second posterior cell
ending in submarginal cell above level of outer cross-vein; ground colour dark
along the edges of the hyaline fasciae. Halteres yellow.
KK
458 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
Abdomen glossy-black above, including the sheath of ovipositor, yellow below,
the dorsum with similar yellow scale-like armature to the mesonotum. Bristles
yellow.
Length, 3-5 mm.
Type, Seaford, Victoria, from gall on Dogwood.
PLATENSINA Enderlein.
Zool. Jahrb., xxxi, Abtl. Syst. Geog. und Biologie, 1911, 453; Hendel, Ann.
Mus. Nat. Hung., xiii, 1915, 461; Curran, Proc. Cal. Acad. Sci., xxii, ‘No. 1, 1936, 29.
This genus was originally erected for the reception of a new species, sumbana
Enderlein. Subsequently Hendel included six old and two additional new species
in the genus. Whether these are all distinct species is a matter of considerable
doubt as the general features of several of them are extremely similar. A
comparison of the figures of the wings of the genotype, platyptera Hendel, and
malaita Curran shows a remarkable resemblance in the shape and the markings,
and examination of a series of specimens may reveal whether they are valid species
or not. Each of the three species was described from a single female example.
The genus is distinguished from its allies by the broad wing, with the peculiar
type of markings, and the two bristles at the apex of the subcostal vein.
There are two specimens in my present material, one of them a female very
like malaita Curran, the other a male and quite distinct from that species in wing
markings.
PLATENSINA PARVIPUNCTA, 0D. SD.
og. Type specimen greasy, but apparently pale yellowish-brown or ferruginous in
general colour, the mesonotum darker except on lateral margins, the abdomen glossy-
black, yellowish at base; legs entirely brownish-yellow; wings dark brown, with the
following hyaline marks: the cell basad of the humeral cross-vein, extreme base
and a mark before middle of the costal cell, a narrow irregular streak from below
the latter to apex of the anal cell, a transverse mark from the costa to second vein
just beyond apex of first vein, two small triangles on hind margin, the basal one
close to the tip of anal vein, and a narrow apical margin from just before apex of
third to beyond apex of fourth vein. There is in the type specimen a slight short
narrow hyaline mark along the edge of the second posterior cell just above the
apex of the fifth vein.
Head in profile subquadrate, slightly higher behind, the frons a little longer
than wide, three pairs of incurved infraorbital and two pairs of reclinate supra-
orbital bristles, the upper one of the latter white and much shorter than the lower,
inner verticals as usual much the longest on head, luteous, postverticals short,
parallel and, like the postocular cilia, white, ocellars moderately long, brown. Face
vertical, not visible in profile except at epistome, with slight antennal foveae
separated by a raised line. Antennae a little more than half the length of face,
third segment not twice as long as wide, rounded at apex, downy; arista very
short haired; eye higher than long; gena about half as high as width of third
antennal segment. Proboscis short and thick; palpi moderately wide.
Thoracic bristles, yellowish, as follows: 1 humeral, 2 notopleurals, 1 pair of
dorsocentrals in line with the supra-alars, 1 pair of prescutellar acrostichals,
1 presutural, 2 mesopleurals, 1 pteropleural, 1 sternopleural, 2 long basal and
2 short apical scutellars. There are about four quite strong erect setulae or
bristles in a series on the propleura.
Legs slender, fore femur with a few rather long bristles on the postero-
ventral surface, mid tibia with one long apical ventral spur.
BY J. R. MALLOCH. 459
Wing as in Plate xi, figure 21. The usual two bristles at the apex of the
subcostal vein, first vein setulose to apex, third with a few microscopic hairs at
base above and below.
Abdomen narrowly ovate, fifth tergite longer than fourth, with a few bristles
apically on sides. Hypopygium small.
Length, 5 mm.
Type, Cairns, N. Queensland (Illingworth).
PLATENSINA DUBIA, Nn. Sp.
©. Very similar to malaita Curran, the bristling of the frons as in parvipuncta;
there is a small dark-brown mark between each antenna and eye not mentioned by
Curran in his description, and the third antennal segment is quite broadly rounded
at apex. Thorax brownish-yellow, mesonotum black except on lateral margins and
densely grey-dusted. Bristles as in parvipuncta, the apical scutellars about half as
long as the basal pair. Legs as in parvipuncta. Wing: Costal cell with a hyaline
spot before middle and another near apex as in malaita, but the stigma has a much
narrower hyaline mark at base than in that species, and the hyaline spot near the
base of the first posterior cell is much smaller than in malaita or sumobanda.
Abdomen glossy-black, without grey-dusting on any part of the dorsum, genital
cone as long as the three preceding tergites combined.
Length, 5 mm.
Type, Gordonvale, N. Queensland, in scrub (Illingworth).
One wing of the type-specimen is much damaged.
I take this opportunity to draw attention to the similarity between the genera
Platensina and Protephritis Shiraki. The author of the latter separated them in
his key by a very slight difference in the position of the dorsocentral bristles.
This difference is largely imaginary, and in fact it is my opinion that the character
has been to some extent overemphasized in the classification of the family. In any
event, both the genera, so far as my material shows, would fall in the same section
of Shiraki’s key. A very careful examination of the genotype of Protephritis
(Tephritis sauteri Enderlein) reveals that the only character that might be utilized
for its separation from typical Platensina is the narrower wing with, peculiarly
enough, its wider anal region. The first vein is setulose at apex below, but it is so
in dubia also, though not in parvipuncta, and though there are some setulae on the
third vein below almost to the inner cross-vein there are traces of similar setulae
on the third vein in dubia both above and below though the dark colour of the
vein and membrane as well as the setulae makes them difficult to see. It requires
ho vivid imagination to discern, from the similarity of the wing markings, that
both these generic concepts have had a common origin, and one may be pardoned
for accepting them as but subgenera. Of course the same attitude may be adopted
with regard to several other concepts in the same subfamily, many of them being
founded upon quite nebulous characters.
SPHENELLA Robineau-Desvoidy.
Mém. présentés Ac. Roy. Sci. Inst. France, ii, 1830, 773, Essai Myodaires.
This genus contains three palaearctic species, and one is recorded from
Formosa. Three species occur in Africa, one of them the genotype, which I have
also from Australia.
SPHENELLA MARQGINATA (Fallen).
Ortalides Sueciae (1) 1820, 7 (Tephritis).—Trypeta heterura Thomson, Eug.
Resa, ii, Zool, i. Insecta, 1868, 584.
460 DIPTERA OF THE TERRITORY OF NEW GUINEA. \XI,
A small dark species with dense grey-dusting on the thorax and abdomen, the
legs tawny-yellow, the wings (PI. xi, fig. 22) hyaline, with some marks along costal
margin up to the apex of the stigma brownish, the stigma darkest, a rather narrow
fascia from the costa to the hind margin enclosing both the cross-veins, and an
irregular marginal band from before apex of second vein round the wing margin
to beyond apex of fourth vein, black: there are also two faint dark spots on the
fifth vein about middle of the discal cell and one about middle of the anal vein
(Fig. N). The arista is almost bare, the third antennal segment reaches almost to
the slightly produced epistome and is slightly angulate at apex above, the frons
has two pairs of incurved infraorbitals and two pairs of reclinate supraorbitals,
the uppermost one of the latter short and pale yellow, the ocellars are long and
dark, the inner verticals are the longest bristles on the head and are dark while
the much shorter outer verticals, the parallel postverticals, and the postocular cilia
are yellowish-white. The dorsocentral bristles are almost in transverse line with
the supra-alar bristles, the presutural is present, as are also one mesopleural and
one sternopleural; the pteropleura has one or two long stiff outstanding setulae:
scutellum more or less yellowish and with four subequal black bristles. The cross-
veins of the wing are rather closely placed, separated by about the length of the
inner one.
Length, 3-4 mm.
Tallong and Scone, N.S.W.; Canberra, A.C.T. (F. H. Taylor). This Huropean
species occurs also in Africa and the Canary Islands. I have seen one specimen
that is evidently this species from Tonga.
The larvae feed on various species of Senecio, Centaurea, and Picris.
_ | believe this is Urophora ruficeps Mcq., Dipt. Exot., Suppl. 4, 1850, p. 288.
CAMAROMYIA Hendel.
Wien. Ent. Zeitg., xxxiii, 1914, 95—Malloch, Dipt. Patag. and S. Chile, Pt. vi,
fase. 4, 1933, 273.
This genus was erected for the reception of a widely distributed species, Dullans
Wiedemann, but several additional species from Africa and South America have
since been placed in it.
CAMAROMYIA BULLANS (Wiedemann).
Trypeta bullans Wiedemann, Aussereur. Zweifl. Ins., ii, 1830, 506—Tephritis
tenera Loew, Zeitschr. ges. Naturw., 1869, 8.—Acinia rufa Macquart, Dipt. Exot.,
ii, Pt. 3, 1843, 228.—Tephritis meleagris Schiner, Reise Novara, Zool. ii, i abt.,
B. Diptera, 1868, 272—Tephritis adspersa Coquillett, Invert. Pac., p. 30 (1904).—
Camaromyia bullans Hendel, Wien. Ent. Zeit., xxxiii, 1914, 95; Abh. Ber. K. Zool.
Mus. Dresden, xiv, 1914, 63.—Tephritis wolffi Cresson, Ent. News, xlii, 1931, 5.
In this species the scutellum has the apical pair of bristles about half as long
as the basal pair, the antennae of the male are dark brown to fuscous in colour,
with the apex of the second segment and base of the third yellow, and in the female
they are entirely yellow, with the aristae in both sexes thickened to near the
middle, yellow at extreme base, white to near middle, the apical portion dark
brown. The genital cone in the female is glossy-black, cylindrical, and tapered
to apex. Rarely in teneral specimens or in those that have been damaged this
cone may be flattened through pressure, so that care should be exercised to deter-
mine on the basis of other characters where such specimens fall in the generic
key. The wing is marked as shown in Plate xi, figure 23.
Illawarra and Botany Bay, N.S.W.; Brisbane, Queensland. The distribution
in the New World extends from the southern United States to Patagonia, and in
BY J. R. MALLOCH. 461
the Old World throughout most of the Palaearctic Region except Japan, and in
Australia. Possibly it may yet be found in intermediate points in the latter.
TEPHRITIS Latreille.
Nouv. Dict. Hist. Nat., xxiv (Tab.), 1804, 196.
This genus, as accepted here, has the wings brown, with many small hyaline
marks or spots indiscriminately arranged in the cells on almost the entire field,
the frons with but two pairs of infraorbital bristles, and the proboscis quite thick
and short.
There is but one species before me from this region which I re-describe below.*
TEPHRITIS PELIA Schiner.
Reise Novara, Zool., ii, i abt., B. Diptera, 1868, 271.
3, 2. Very similar to plebeia Malloch from New Zealand, with two hyaline dots
in the dark-brown stigma, and a hyaline spot at the apex of the first posterior cell
of the wing, but the genae are much narrower, not more than one-sixth of the
eye-height as against one-third in plebeia, there is no small hyaline spot in the dark
patch in the marginal cell below the stigma, there is a yellowish patch on each
side of the composite basal segment of the abdomen in the male that is not present
in plebeia, and the genital cone of the female is bright orange or fulvous-yellow
with a black tip, not entirely glossy-black.
Head testaceous-yellow, with greyish-white dust, most evident on the ocellar
triangle, the frontal orbits and parafacials, occiput broadly black centrally, with
grey dust; antennae, aristae and palpi yellow, the palpi brownish apically; infra-
orbital, anterior supraorbital, ocellar, and inner vertical bristles black, all others
and the short hairs yellowish-white. Gena about one-sixth as high as eye, eye
slightly oblique, higher than long; head in front about three-fourths as high as at
occiput; epistome projecting. Frons about 1:25 times as long as wide, parallel-
sided, and more than one-third of the head-width, all black bristles long and strong.
Third antennal segment about 1:5 times as long as wide, angulate at upper apex;
avista pubescent; palpi rather long and strap-like.
Thorax black, densely brownish-grey-dusted on dorsum and upper part of
pleura, grey-dusted below, the humeri, posterior notopleural callosities, and
scutellum more or less yellowish, a dark brown spot at insertion of each of the
acrostichal and basal scutellar bristles, all the bristles except the pteropleural and
scapulars black. SBristling complete, the apical pair of scutellars about half as
long as the basal pair. Surface hairs pale yellow and decumbent. -
Legs tawny-yellow. Fore tarsi longer than their tibiae, mid and hind pairs
shorter; fore femur with the posteroventral series of bristles complete, hind pair
with no anteroventral bristles.
Wings greyish-hyaline, with dark-brown markings (Pl. xi, fig. 24), the most
distinctive being the bipunctate stigma, and the peculiar hyaline spot at the
apices of the submarginal and first posterior cells. First vein setulose from base
of node below the humeral cross-vein to apex and below on apical third, third vein
with a few setulae at base above and sparsely setulose between base and inner
cross-vein below. MHalteres yellow.
Abdomen coloured as thorax, densely dark-grey-dusted, with faint traces of a
pair of brown discal spots on tergites 3 to 5 inclusive, sides of composite basal
tergite of male usually yellowish, hypopygium of that sex fulvous-yellow, the
*T have been unable to find «a species agreeing with the description of Tephritis
11-guttata Thomson.
.
462 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
genital cone of the female flattened, glossy-orange or fulvous-yellow, with black
apex, broadest above. Hairs yellowish-white, bristles at apex of fifth tergite in
male and sixth in female quite strong and black.
Length, 3-5-4 mm.
I am accepting as this species, which was originally described from Sydney, a
number of specimens from Illawarra and Botany Bay (Peterson); Tallong,
N. S. Wales; Canberra, A.C.T. (Taylor). This may be the species recorded by
Macquart as leontodontis De Geer.
TRYPANEA Schrank.
Briefe Donaumoor, 1795, 147.—Urellia Robineau-Desvoidy, Mém. présentés Ac.
Roy. Sci. Inst. France, ii, 1830, 775, Essai Myodaires.
This generic concept is a difficult one to maintain in cases where many species
are available, as I have shown in my paper on the Patagonian Trypetidae. I am,
however, segregating the single species now before me from Australia in Trypanea
as an index to its closest affinities in the Old World fauna. The stellate dark apical
wing-mark is quite characteristic in this species and is distinctive enough to
warrant this procedure tentatively, though there is little in the line of structural
features to justify the perpetuation of the segregation.
TRYPANEA GLAUCA (Thomson).
Hugen. Resa, ii, Zool. i. Insecta, 1868, 581 (Trypeta).
6. Very similar in wing markings to neodaphne var. gamma Malloch from
Patagonia, differing in the three incomplete branches of the brown mark over the
first and second posterior cells of the wing (PI. xi, fig. 25).*
Head testaceous-yellow, with pale-grey dust, centre of occiput broadly black;
antennae, aristae, palpi, and proboscis yellow, second antennal segment with a
small dark mark above. Head a little wider than thorax, in profile with the face
almost vertical, epistome slightly protruded and about two-thirds as high as at
occiput; eye oblique, at middle about two-thirds as high as its extreme length;
gena fully half as high as width of third antennal segment, the latter about 1:5
times as long as wide, its upper apex angulate; aristae subnude. Frons fiat,
about 1-25 times as long as wide, and almost parallel-sided, with three pairs of short
fine yellowish infraorbitals, the other bristles rubbed off, but scars of four verticals
and one pair of supraorbitals distinct.
Thorax black, densely whitish-grey-dusted, humeri and a spot below wing base
yellowish. Most of the bristles rubbed off, but those remaining and the short
hairs are yellow. Bristles as follows: 1 humeral, 2 notopleurals, 1 presutural,
1 supra-alar, 1 pair of dorsocentrals close to the suture, 1 pair of acrostichals,
2 postalars, 1 mesopleural, 1 sternopleural, 1 pteropleural, and a pair of scutellars
near base. :
Legs yellow. Fore tarsus shorter than its tibia, basal segment rather stout,
in dorsal view about four times as long as wide, all the segments except fifth with
a few long pale hairs on anterior edge, longest on basal segment; mid and hind
tarsi slender, longer than their tibiae, basal segment much more than four times
as long as wide.
Wing milky, veins yellow, dark brown in the dark markings. First vein
setulose from base of node to apex above and on apical half below, third vein with
a few setulae at base above and below. Halteres yellow.
“The tiny dots on the photograph are dirt, the three irregular patches on the fifth
vein are pieces of wing membrane.—F.H.T.
BY J. R. MALLOCH. 463
Abdomen coloured as thorax, immaculate, with yellow bristles and hairs.
Tergites subequal in length, with some lateral bristles on fifth.
Length, 3 mm.
Waterfall, N.S.W. (H. Peterson). This and other specimens from the same
collector sent me by the late C. F. Baker in general sweepings. Type locality,
Sydney. ;
ParoxyNna Hendel.
Flieg. Palear. Reg., in Lindner, xlix, Trypetidae, 1927, 146.
There are a large number of Old World species of this genus, but there is only
one known to me from the Australian region.
PAROXYNA SORORCULA (Wiedemann).
Aussereur. Zweifl. Ins., ii, 1830, 509 (Trypeta).
A very small species characterized by the long head, slender geniculated
proboscis, and slender hyaline wings with numerous small fuscous marks
(Pl. xi, fig. 26).
It is recorded from many tropical and subtropical countries in the Eastern and
Western Hemispheres, extending in the latter into the Patagonian region, though
in the Old World confined to the warmer section. It has been described under
several specific names in three genera.
I have four specimens from Tambourine Mt., Queensland (C. Deane).
Recorded from Fiji by Bezzi, and possibly occurs rather generally throughout
this region, though its small size may be responsible for its being overlooked by
most collectors.
Shiraki, in dealing with the Formosan Trypetidae, retained the species in the
genus Hnsina Robineau-Desvoidy despite Hendel’s having placed it in Paroxyna.
Subfamily SCHISTOPTERINAE.
This subfamily, as I accept it, contains five genera, only one of them occurring
in the region now under consideration, the others being African.
The distinguishing character consists of a deep cleft in the costal margin
of the wing at the apex of the subcostal vein, the apex of the section of the costa in
front of the cleft sharply angulate and with a pair of bristles that are usually quite
strong and conspicuous.
Bezzi distinguished two subfamilies in the group, segregating Schistopterinae
from Rhabdochaetinae by the fact that in the former there are no strong bristles
on the interfrontalia in front of the ocelli, while in the other group, to which the
sole representative we have to consider belongs, there are at least two strong erect
bristles in front of the ocelli, usually convergent and slightly forwardly directed
at their apices.
This same combination of cleft costa and interfrontal bristles is met with in
some other families, notably in the Milichiidae.
RHABDOCHAETA de Meijere.
Bijd. Dierk., 17-18 Afl., 1904, 109.
There are seven described species of this genus known to me, but only one is
from this region.
RHABDOCHAETA CROCKERI Curran.
Proc. Cal. Acad. Sci., xxii, No. 1, 1936, 28.
Described from the Solomon Islands and not known from elsewhere, though it
may be expected to occur on adjacent island groups.
464 DIPTERA OF THE TERRITORY OF NEW GUINEA. XI,
Unidentified Species from New Guined.
Ptilona bischofi Kertész, Term. Fuzet.. xxiv, 1901, 427.—Bezzi says this is not a
Ptilona.
Sophira bistriga Walker, Jour. Proc. Linn. Soc. London, iv, 1860, 160—See under
Colobostrella ruficauda Hendel, in text.
Trypeta brevivitta Walker, op. cit., viii, 1865, 124.—Genus doubtful.
Ptilona lateralis Kertész, Term. Fuzet., xxiv, 1901, 428.—A Rioza according to Bezzi.
Trypeta indistincta de Meijere, Nov. Guin.. ix, Zool. livr. iii, 1913, 364—Genus ?.
Acanthoneura sexguttata de Meijere, Nov. Guin., ix, Zool. livy. iii, 1913, 364.
Acanthoneura debeauforti de Meijere, op. cit., v, 1906, 94 (Riora).
Acanthoneura insignis de Meijere, op. cit., ix, Zool. livy. iii, 1913, 366——See under
Pseudacanthoneura septemnotata, n. sp. in text.
Riora (?) nivistriga Walker, Journ. Proc. Linn. Soc. Lond., v, 1861, 246
(Helomyza).
Themaroides (?) optatura Walker, op. cit., viii, 1865, 116 (Helomyza)—Czerny has
said this is the female of quadrifera Walker.
“Helomyza”’ ortalioides Walker, op. cit., viii, 1865, 116—A Trypetid.
Dacus speculifera Walker, op. cit., viii, 1865, 122—A Callistomyia ? according to
Bezzi.
Ptilona variabilis Kertész, Term. Fuzet., xxiv, 1901, 426.—Not a Ptilona according
to Bezzi.
Dacus biarcuatus Walker, Jour. Proc. Linn. Soc. London, viii, 1865, 122.—Allied
to Callistomyia according to Bezzi.
Addendum, by F. H. Taylor.
It has been suggested to me that a few remarks on the method adopted to
make the photographs of the wings would be of service.
First of all the wing is taken off the fly with a sharp pointed pair of forceps
and placed in absolute alcohol. It is then mounted direct into Euparal and
weighted down with a small bottle of mercury, a half-dram vial serves the purpose,
until the Euparal has set.
Any good type of projection lamp will serve as the illuminant for the camera.
The lens should be of 3:5 cm. focal length; no eye-piece is used. The plate or cut
film is “Process”. It is a great mistake to use any other type of plate or film as
it is essential to have complete control over the negative during development. The
developer used is the “‘Kodak” process formula, Hydroquinone-Caustie Potash. The
negative must not be overdeveloped.
Wings showing a lot of “pattern” are comparatively easy to photograph,
requiring from two to five seconds’ exposure at f. 6:3. Wings which have very
little or no ‘‘pattern” should have not more than one second exposure at the above
lens stop, should be slightly underdeveloped and then intensified. The mercury-
ammonia intensifier serves the purpose.
When the negatives are dry the background must be completely blocked out
with “Opaque’’, using a fine sable-hair brush to go round the wing. A hand lens
should be used to see that the “Opaque” does not encroach on the wing.
Any slow gaslight paper with a glossy surface will give excellent prints from
negatives produced by the above means.
There is no necessity to retouch the wings in any way, as the veins stand out
quite well.
Proc. Linn. Soc. N.S.W., 1939. PLATE XI.
New Guinea Trypetidae.
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BY J. R. MALLOCH. 465
EXPLANATION OF PLATE XI.
Fig. 1.—Dacus papuaensis, n. sp. Wing, type. x 6:5.
Fig. 2.—Dacus albolateralis, n. sp. Wing, type. x 6-5.
Fig. 3.—Pseudosophira bakeri, n. sp. Wing, type. 5.
Fig. 4.—Polyara insolita Walker. Wing. xX 5d.
Fig. 5.—Themarohystria flaviceps, n. sp. Wing, paratype. x 5.
Fig. 6.—Themarohystrix suttoni, n. sp. Wing, paratype. xX 6:5.
Fig. 7.—Clusiosoma biseriata, n. sp. Wing, paratype. x 6:5.
Fig. 8.—Clusiosoma puncticeps, n. sp. Wing, type. xX 6:5.
Fig. 9.—Acanthonewra nigriventris, n. sp. Wing, type. x 5.
Fig. 10—Neothemara formosipennis Walker. Wing. x 5.
Fig. 11.—Pseudacanthoneura septemnotata, n. sp. Wing, type. x 5.
Fig. 12.—Diarrhegmoides hastata, n. sp. Wing, allotype. x 6d.
Fig. 13.—Hexacinia multipunctata, n. sp. Wing, paratype. x 6:5.
Fig. 14.—Pseudina buloloae, n. sp. Wing, type. x 6:5.
Fig. 15.—Anomoea nigrithorax, n. sp. Wing, type. x 6:5.
Fig. 16.—Pseudospheniscus taylori, n. sp. Wing, type. x 6:5.
Fig. 17.—Ceratitella loranthi (Froggatt). Wing. x 6:5.
Fig. 18.—Tephrella australis, n. sp. Wing, type. x 6:5.
Fig. 19.—Spathulina acrolewca (Schiner). Wing. x 6:5.
Fig. 20.—Chrysotrypanea trifasciata, n. sp. Wing, type. x 6:5.
Fig. 21.—Platensina parvipwicta, n. sp. Wing, type. x 6:5.
Fig. 22.—Sphenella marginata Fallen. Wing. x 6:5.
Fig. 23.—Camaromyia bullans Wied. Wing. x 6°5.
Fig. 24.—Tephritis pelia Schiner. Wing. x 6:5.
Fig. 25.—Trypanea glauca Thoms. Wing. x 6:5.
Fig. 26.—Paroxyna sovorcula Wied. Wing. x 6:5.
Note re Ceratitella (pp. 442, 452 supra), added 6 September, 1939.—The
Formosan genus Paratrirhithrum Shiraki (Mem. Fac. Sci. and Agric., Taihoku
Imp. Univ., Formosa, viii, 1938, Hnt. No. 2, 137) differs in having the third antennal
segment tapered to the narrowly rounded apex, the apex of the subcostal vein
farther from the apex of the first and the latter running into the costal vein at a
much more acute angle, not almost rectangularly bent forward to join that vein,
while the third vein is much more arched on its apical portion, the apex being
distinctly more deflected. The scutellum is also entirely black, though this is
hardly a generic character.
LL
466
THE ASSOCIATION BETWEEN THE LARVA DESCRIBED AS TROMBICULA
HIRSTI VAR. BULOLOENSIS GUNTHER 1939, AND TROMBICULA MINOR
BERLESE 1904. (ACARINA: TROMBIDIIDAE.)
By Cart E. M. GuntHer, M.B., B.S., D.T.M. (Sydney), Field Medical Officer,
Bulolo Gold Dredging Limited, Bulolo, Territory of New Guinea.
(Three Text-figures. )
[Read 27th September, 1939.]
Previous work on Trombidiid Nymphs and Adults.
Apart from Hirst’s paper on the nymphal form of the “Harvest bug” (1926),
I have not had access to the original articles on the subject, but am indebted to a
paper by Warburton (1928) for the following information.
Brandis first, in 1897, bred nymphs from the European Harvest Bug, Leptus
autumnalis Shaw, in sterile earth; these were of the general Trombicula form,
and suggested 7. holosericeum.
Then, in 1906, Miyajima obtained nymphs of Microtrombidium akamushi; and,
in 1916, he and Okumara bred adults and established this larva as belonging to
the genus Trombicula.
Ewing is mentioned as stating that Leptus irritans has been bred to the adult,
and that the latter belongs to the genus Jrombicula also.
Meanwhile Bruyant obtained one nymph from Leptus autumnalis in 1910, but
there is some doubt about its identification with the adult Microtrombidium
pusillum Hermann, to which it was at first assigned.
Finally, in 1925, Hirst bred out a single female nymph from the harvest bug,
and definitely established it as belonging to the genus Jrombicula.
Apart from these, no other larval species has so far been linked up with its
corresponding adult, although both larvae and adults, separately, have been
thoroughly worked out.
TROMBICULA MINOR Berlese.
Redia, ii, fase. 2, 1904 (1905), 155.—T. hirsti var. morobensis Gunther 19388,
202, nom. nud.—T.. hirsti var. buloloensis Gunther 1939, 78. :
This larva occurs in great numbers in the Morobe District on the mainland
of New Guinea. Of approximately 3,000 larval mites taken in four years, it
numbered about 2,700; the remainder were distributed over 13 other species. It
has been found on nine hosts: Man, Bush pig (Sus papuwensis), Bandicoot
(Echymipera cockerelli), Bush turkey (Talegallus jobiensis), Bush fowl
(Megapodius duperreyi), Ground pigeon (Gallicolumba jobiensis), Cassowary
(Casuarius casuarius), Rail (Amaurornis moluccanus nigrifrons), and Rail
(Porphyrio melanotus).
The larva is shown in Figure 1, which is from my detailed description of the
species (1939). The probable association of this larva with endemic typhus in New
Guinea has been discussed (1938).
BY C. E. M. GUNTHER. 467
While investigating this larva, I was so fortunate as to breed out 23 nymphs,
and to obtain four specimens in intermediate stages. It was, however, Mr. H.
Womersley who, after checking my material, pointed out that, as far as can be
determined, these nymphs are identical with Trombicula minor Berlese 1904, which
I had not recognized. The credit, therefore, belongs to him for this discovery.
Preparation of breeding jars.—A wide-mouthed clear-glass jar with a ground-
glass stopper, of 4 ounces capacity, was used. Dry soil was finely crumbled and
placed in the jar to a depth of one-quarter of an inch. The open jar and its stopper
were then sterilized in an autoclave. When cool, sterile water was added drop by
drop until, by stirring with a glass rod, the soil was evenly moistened, care being
taken not to add enough water to cause caking of the soil or the formation of mud.
The stopper was smeared with a little sterile soft paraffin.
GS
Figs. 1-3. Trombicula minor.
Fig. 1.—Composite dorsal and ventral diagram, 7’. minor, larva.
Fig. 2.—T. minor, nymph. a, Dorsal view of palp. 6b, Dorsal view of chelicera and
cheliceral sheath. c, Lateral view of chelicera.
Fig. 3—ZT. minor, nymph. a, Crista. b, First tarsus.
Obtaining and checking larvae.—A freshly-shot bush fowl or other host was
examined with a hand-lens and all sections of skin bearing large larvae were cut
out and placed in white china pots with screw-on lids. These were allowed to
stand all night; by morning most of the larvae had detached themselves. The
largest were placed one at a time in a hollow-ground slide, covered with a cover-
slip, and examined with the low power. Once one is accustomed to the salient
characteristics of the species, only a few seconds are needed to identify each larva
and to determine whether it is sufficiently engorged to be worth trying out.
When checked they were dropped into the jar. By selecting a number of very
large larvae there is some chance of obtaining a few which are sufficiently engorged
to go on to the nymphal stage without seeking a fresh host for a further feed.
Some of the largest were often found hidden beneath the sections of skin; this I
believe to be an indication that they are ready to bury themselves and prepare for
metamorphosis.
Too large a number in one jar makes subsequent checking too complicated.
It was finally found that from 10 to 15 was a convenient number.
Only vigorous and active larvae were selected. It was found too tedious
inducing them to climb onto a needle-point and to hold on while being transferred
from the pots; a convenient method is to lay the pot on its side, chase a larva
468 TROMBICULA HIRSTI VAR. BULOLOENSIS AND T. MINOR,
out with a needle, and induce it to climb on to a rectangular coverslip held in its
path.
When the desired number had been tallied into the jar, the stopper was
inserted and the jar placed on a window-ledge where it would get as much direct
sunlight as possible. It was found that in jars kept in the shade, moulds covered
the soil in a few days. The heat of the sun, however, causes water from the soil
to condense on the shady side of the jar; if too little water has been added
originally, the soil becomes dry and caked, and more sterile water has to be
dropped in.
Behaviour of larvae.—Some of the larvae bury themselves in the soil imme-
diately; others climb the sides of the jar, usually becoming imprisoned in the
drops of water on its sides. At first the plan of freeing these latter with a bent
wire and dropping them back on the soil was followed, but as they invariably set
out to climb up the sides again, it was decided that they were probably in search
of another host. It was thought simpler to remove all such larvae on the second
and subsequent days. All larvae so removed were checked again under the
microscope.
It was found that even after being held in a drop of water for several days
most larvae would begin to walk about within a few seconds of being placed on a
piece of filter-paper to dry. The longest period noted was 20 days, mostly spent
in water; 4 such larvae, when dried and examined, although unable to move about,
or even to turn themselves over, still made feeble movements with their legs.
Some of the earlier batches had in their jars slices of apple, banana, paw-paw,
liver, or steak, transfixed with a toothpick and placed upright. Moulds grew
rapidly and made it impossible to breed out any nymphs, but it was noted that
even newly-hatched larvae were not particularly attracted to any of these
substances, and none gave any appearance of feeding on them. The method was
abandoned.
Breeding-time——F rom four batches a total of 23, comprising 7 living nymphs
and 16 dead nymphs, was collected; the periods ranged from 17 to 20 days from
the time they were placed in the jars. From two batches transitional forms were
obtained. From nine batches there was no result.
Assuming that the larvae, when they were put into the jars, were so nearly
engorged as to make no difference, this fixes the time for emergence of the nymph
under these conditions at from 17 to 20 days. Most of the dead ones were found
on the 19th and 20th days, and most of the living ones on the 18th day, which
makes me inclined to fix the average time at from 17 to 18 days.
There is, of course, no means of telling whether this is the usual time under
natural conditions—it is possible that the temperature and humidity inside the
jar are higher than is usually found in nature, and that they may therefore have
forced earlier development. It is unlikely that these conditions could have retarded
development. Hirst’s nymph took 33 days to emerge, but it had its habitat in a
much colder climate, and its hatching-time would reasonably be expected to be
longer.
When they first emerge, the nymphs are extremely soft and fragile, and
easily break up with even the most careful handling. They harden after several
hours, but in these breeding-jars they apparently do not live long. Once dead,
they shrivel rapidly. For these reasons, most of the present specimens were of
no use for detailed study when mounted.
Transitional stage—In one jar which had too little moisture, the soil became
absolutely dry. On the 24th day, since no nymphs had emerged, the soil was gently
BY C. E. M. GUNTHER. 469
crumbled and searched. One apparently dead larva was found, but on examination
it proved to be an intact larval skin, colourless and transparent, the legs and palpi
empty, but containing within the body a pupa-like mass. This mass was orange
in colour; its posterior margin had the shape of the posterior pole of a nymph,
and bore typical setae; anteriorly there was no projection of any cephalothorax;
but ventrally, outlines suggestive of immature folded legs were quite distinctly
visible.
From another batch three living nymphs and three specimens in transitional
stages were obtained. One of the latter group was much further advanced than
the one described above, and one had partly cast its larval skin. These specimens
leave no doubt that the larva, when ready for metamorphosis, withdraws inside
its own skin and there goes through the nymphochrysalis stage.
The Nymphs.—Berlese’s description (1904) is from damaged specimens, and
is therefore incomplete. However, my specimens agree with every point in
Berlese’s description, except that the fore-tarsus is slightly longer and wider; but
the ratio of the length to the width of the fore-tarsus (2:5:1) as laid down by
Berlese is retained. Berlese’s description, however, makes no mention of the
number of genital suckers, so the specimens cannot be definitely stated to be
adults; that they were not bred out, but were taken running free, makes the
assumption that they are adults rather than nymphs possible. This, however,
does not affect the validity of the comparison between my specimens and his, and
his name should therefore be used.
Description of the Nymph (Figs. 2, 3).—Colour, bright orange-red. Body oval,
widest at level of coxa iii, without any marked constrictions; covered with closely-
set fine setae bearing long fine branches on all sides. Total length, including
chelicerae, 6804; abdomen, length 500u, width 3254. Coxae i and ii set close together
at front of body, projecting partly beyond the margin; coxa iii two-fifths of the
distance back, and coxa iv half-way back, well in from the margin. Cephalothorax
projecting boldly forward. Chelicerae stout, long, sharply curved. No cheliceral
teeth. Cheliceral sheaths reaching almost half-way along the chelicerae; bulbous in
the middle third, which bears about five fine setae with a few branches; two fine
nude setae towards the apex. Palpi long, curved, widest at the distal part of segment
ii. A few fine setae with a few fine short branches on ii; on iii and iv, more similar
setae. Palpal claw single, long, stout, curved,and sharp. Two accessory bristles near
its base. Appendiculum long, rounded, bearing about 6 to 8 fine setae with fine
branches. Crista of typical shane; as in diagram; bearing a seta 28u long, with
fine branches on all sides, at the centre of each lateral margin. Greatest width
50u. Pseudostigmata at the anterolateral angles, 37-5u apart. Pseudostigmatic
organs filiform, 854 long, with 4 or 5 short widely-spaced branches on the distal
fourth. Eyes single, close to the crista, just lateral and posterior to the pseudo-
stigmata. Legs each with seven segments, covered with closely-set branched
setae. Two curved claws on each tarsus. Tarsus i typically long and expanded.
Lengths, excluding coxae, as follows: i, 4164; ii, 223u4; iii, 250u; iv, 292u.
Genital opening with its anterior end opposite the posterior ends of coxa iv.
Furnished with two pairs of large, roughly circular suckers. Setae: the general
body-setae almost straight, with many relatively long, fine branches on all sides.
On the cephalothorax the setae are of similar type, but are shorter, finer, and
slightly curved. On the palpi and legs the setae are thicker, very slightly curved,
and bear a few branches along the convex side only.
470 TROMBICULA HIRSTI VAR. BULOLOENSIS AND T. MINOR.
Acknowledgements.
My thanks are due to Mr. H. Womersley, A.L.S., F.R.E.S., of the South
Australian Museum, not only for his discovery mentioned above, but also for his
kindness in obtaining copies of references for me, and in checking this paper.
References.
BERLESE, A., 1904.—Redia. ii, fase. 2 (1905), 155.
GUNTHER, C. E. M., 1938.—The Probable Vector of Endemic Typhus in New Guinea.
Med. Journ. Aust., 6 August, 202.
, 1939.—Trombidiid Larvae in New Guinea. Proc. LINN. Soc. N. S. WALES,
Ixiv, 1939, 73.
Hirst, S., 1926.—On the Nymphal Form of the ‘Harvest Bug’ Trombicula (Neotrom-
bicula) autumnalis. Annals App. Biology, xiii, 140-143.
WARBURTON, C., 1928.—The Harvest Bug: An Account of the Present State of Our
Knowledge of the Larval Trombidiid Mites Attacking Man. Parasitology, xx,
228-236.
471
OBSERVATIONS ON THE LIFE HISTORY OF NHOSCHONGASTIA
KALLIPYGOS GUNTHER 19389.
(ACARINA: TROMBIDIIDAE.)
By Cart EH. M. Gunruer, M.B., B.S., D.T.M. (Sydney), Field Medical Officer,
Bulolo Gold Dredging Limited, Bulolo, Territory of New Guinea.
(Two Text-figures. )
[Read 27th September, 1939. ]
NEOSCHONGASTIA BIPYGALIS, Nom. nov.
N. kallipygos Gunther, Proc. Linn. Soc. N. S. Wass, lxiv, 1939, 83.
Owing to the regrettable use of the specific name kallipygos by Derrick, Smith,
Brown and Freeman (1939), before the species was described, a change of name
becomes necessary.
Life History.—As far as is known the life history of the trombidiid mites is as
follows:
According to Patton and Evans (1929) it is likely that the eggs are laid
singly in the ground.
The larvae are mostly parasitic on birds and mammals—the genus Hannemania
is confined to frogs. When ready for metamorphosis the larvae bury themselves in
the ground (this has been observed for Trombicula akamushi, Leptus autumnalis,
and Trombicula minor).
The nymph is reported to be parasitic on other arthropods, although there is
a possibility that it is a vegetable feeder.
The adult is supposed to live in decaying vegetable matter on the forest floor,
or in the sand and silt left by floods, and by assumption (Hirst, 1926), in the nests
of field mice.
Nowhere is there any mention of the adult or nymph being parasitic on either
birds or mammals, nor is there any record of ova being found cemented to fur
or feathers in the manner of louse ova.
The larvae of Neoschongastia bipygalis occur in New Guinea as parasites on
the following hosts: The brown bush rat (Rattus ringens), Brown’s rat (Rattus
browni), Monckton’s melomys (Melomys moncktoni), Stalker’s melomys (Melomys
stalkeri), the rufous melomys (Melomys ruber), an arboreal ‘‘mouse” (Melomys
sp.), Bandicoot (Echymipera cockerelli), and Bandicoot (Peroryctes raffrayanda).
On the first five of these it can be found in large numbers embedded around
the mammae, or in the penis, and on the bare parts of the hind legs; specimens
have also been taken running free in the fur. From the other three hosts only a
few specimens have been taken. It seems likely that the rats are the principal
hosts, the others being only casual hosts.
On each of the five principal hosts are to be found many ova cemented to the
abdominal hairs. Some are undifferentiated, but in those in late stages of develop-
ment the details of the contained larvae can clearly be seen through the shell.
472 LIFE HISTORY OF NEOSCHONGASTIA KALLIPYGOS,
They show the characteristic scutum, first tarsi, dorsal setae, chelicerae, and
caudal plates of the normal larva, Neoschéngastia bipygalis (Fig. 1, which is the
illustration of this larva from my detailed description, and Fig. 2b).
There is no possibility that these ova may have been laid in the nests of the
rats, and have become entangled in their fur, for they are definitely cemented to
bundles of 5 to 10 hairs at their bases, and the larva lies always in the same
relative position in the ovum.
Fig. 1.—Larva of N. bipygalis.
Fig. 2.—a, Undifferentiated ovum; b, Ovum in late stage, showing contained larva.
The adult female must certainly be a parasite of these hosts for as long
as it takes her to deposit her eggs. Nothing further can be assumed positively,
but the possibilities are:
1. That the adults live in the nests of these rats, and that the ovigerous
females deposit their eggs while the rats are sleeping. If this be so, then
investigation of nests should result in specimens of adults being taken.
2. That the ovigerous female is a normal parasite of the rats—which would
demand that it resembles, for instance, one or other of the two suborders of lice—
and that it lives either by sucking or by biting. In this case, adults should be
found on the rats.
In view of the fact that nobody knows what the adults of the larval genus
Neoschongastia look like, the question is not likely to be settled until the hymph
at least can be bred, although the finding of an ovigerous female bearing an ovum
of the typical shape and size would be conclusive.
I have tried with ten larvae to breed nymphs, using the technique which
was successful with Trombicula minor, but the larvae neither buried themselves in
the soil nor made any considerable efforts to crawl around; they just died.
So far I have been unable to obtain any rats’ nests, nor have I found any
promising adults on rats. For the present, therefore, all that can be done is to
describe the ova, and point out that their presence on the abdominal hairs of
various rats indicates for this species a radical variation from what we know of
the normal life history of the Trombidiidae.
BY C. E. M. GUNTHER. 473
Ovum (Figures 2a, 0b).
Location: Found cemented to the abdominal hairs of various New Guinea
rats: Rattus ringens, R. browni, Melomys moncktoni, M. stalkeri, and M. rubex.
Colour a dirty yellow to light brown. Bell-shaped, cemented to the hairs at its
base. The walls consisting of a lining layer, a clear centre, and an outer
laminated layer. The apex produced into a small conical tubercle. The larva
lying with its head away from the base, its chelicerae projecting into the conical
tubercle. The undifferentiated ovum is larger, with thick walls. As the larva
matures the shell shrinks and becomes thinner, the latter mainly due to shedding
of the outer laminated layer. Average measurements: Height, early, 541u; mature,
380u. Width at base: early, 5084; mature, 370u. Width across equator: early,
412u; mature, 270u. Thickness of shell: early, 1414; mature, 70u.
Acknowledgement.
Mr. H. Womersley, A.L.S., F.R.E.S., has been so kind as to check this paper
for me.
References.
DERRICK, SMITH, BROWN and FREEMAN, 1939.—WMed. Journ. Aust., 28 January, 150.
GuNTHER, C. EH. M., 1939.—Trombidiid Larvae in New Guinea. Proc. LINN. Soc. N. S.
WALES, Ixiv, 73.
, 1939a.—The Association between the larva described as Trombicula hirsti var.
buloloensis Gunther 1939, and Trombicula minor Berlese 1904, Proc. LINN. Soc. N. S.
WALES, Ixiv.
Hirst, 8S., 1926.—On the Nymphal form of the ‘Harvest Bug’ Trombicula (Neotrombicula)
autumnalis. Ann. Applied Biology, xiii, 140.
Patron, W. S., and Evans, A. M., 1929.—Insects, Ticks, Mites and Venomous Animals
of Medical and Veterinary Importance, Part 1, Croydon.
fe
S(vis
MM
474
TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X.
By Consrerr Davis, M.Se., Lecturer in Biology, New England University College,
Armidale.*
(Highty-three Text-figures.)
[Read 27th September, 1939.]
PART VI. THREE NEW ASIATIC GENERA RELATED TO EMBIA LATREILLE.
(Thirty-two Text-figures. )
Genus METEMBIA, Nn. gen.
Genotype, Metembia ferox, n. sp.
Indian Embioptera closely related to Embia Latreille (s. str.), but with two
ventral bladders on the first segment of the hind tarsi.
6. Wings as in Embia, with R,,; clearly forked, M simple, and Cu two-
branched, except for individual anomalies; terminalia with tenth abdominal
tergite completely cleft, right hemitergite as in Hmbia, with a short posterior
process directed inwards and downwards, and an inner flap-like process separated
from the remainder of the hemitergite, except posteriorly, by a membraneous
area. Process of left hemitergite simple, acute. First segment of left cercus with
two internal lobes, armed with large sharp teeth.
METEMBIA FEROX, nN. Sp. Figs. 1-3.
dg. Length 6:-5-8:-5 mm.; head 1:2-15 mm. x 0:9-1:1 mm. Forewing 4-4-6-0
mm. x 1:0-1:2 mm.; hindwing 4:0-5-0 mm. x 1:0-1:2 mm. Antennae incomplete.
General colour very dark brown, eyes black, longitudinal bands on wings smoky-
brown. Head (Fig. 1) with eyes small, sides behind eyes scarcely converging,
smoothly rounded behind. Wings as in generic description, fork of R,,, subequal
to stem, all veins well-developed; cross-veins variable, fairly numerous. Hind
tarsi with two well-developed ventral bladders on first segment, one on second.
Terminalia (Figs. 2-3) with ninth abdominal tergite (9) very short, slightly
asymmetrical; tenth tergite completely cleft longitudinally, right hemitergite
(10R) produced downward and inward to a tapered, acute process (10RP,); inner
margin of 10R with an elongate flap-like process (10RP,), separated from 10R
by membrane except at posterior end. Left hemitergite (10L) produced back-
ward from its inner margin to a slender process (10LP), acutely tapered, curving
outward very slightly. Right cercus composed of two subequal subcylindrical
segments (RC,, RC,), arising from a well-developed pad-like cercus-basipodite
(RCB). First segment of left cercus (LC,) with inner margin produced to two
rounded lobes, the basal one more dorsal, the distal more ventral in position; both
lobes furnished with a number of sharp, prominent teeth. Second segment (LC,)
subcylindrical. Ninth sternite (H) produced backwards to a short blunt lobe
(HP), between which and the base of LC, is the left cercus-basipodite (LCB),
acute, curved outwards.
* Part of the work embodied in this paper was carried out when the writer held a
Linnean Macleay Fellowship in Zoology.
BY CONSETT DAVIS. 475
9. Hight females, from the same locality as the males, are probably referable
to this species. They are not of taxonomic importance.
Locality —Nedungadu, Southern India, coll. P. S. Nathan, 13 males, and 8
females probably conspecific. Holotype male, 11 paratype males, and females,
Museum of Comparative Zoology, Harvard University; one paratype male in the
Macleay Museum, Sydney University.
METEMBIA IMMSI, n. sp. Figs. 4-8.
6. Length 14 mm.; head 2:0 mm. x 1:8 mm.; forewing 8 mm. x 1:8 mm;
hindwing, length and breadth as forewing. Antennae incomplete. General colour
mid-brown, head darker, eyes black. Wing-veins dark brown, bordered by pale
smoky-brown bands. Head (Fig. 4) as in the preceding species, but relatively
broader, the eyes relatively larger; left mandible with three acute teeth, right
with two, on inner face. Wings as in the preceding species, R,,; simple in the right
forewing of the type; cross-veins numerous, 2—4 from costa to R,, 4-6 from R, to
R»,3, 1-2 from R,,, to R,,;, 0-1 from R, to R;, 2-3 from sector to media, 0-1 from
media to Cu,.. R, dichotomizes terminally, one branch going to the costa, the
other to R.,;. Hind tarsi as in the preceding species. Terminalia (Figs. 5-8)
Figs. 1-3.—Metembia ferrox, n. sp., holotype ¢. 1. Head from above, x15. 2. Terminalia
from above, x 30. 3. Terminalia from below, x 30.
Figs. 4-8.—WMetembia immsi, n. sp., holotype ¢. 4. Head from above, showing outline
of mandibles, x 15. 5. Terminalia from above, x 15. 6. Process of left hemitergite from
above, x 30. 7. Left cercus from above, x 30. 8. Terminalia from below, x 15.
All original figures based on camera-lucida outlines, except figures 26-27, which
were prepared with constant reference to an ocular micrometer.
Conventional lettering for text-figures:
9, ninth abdominal tergite: 10L. 10R, left and right hemitergites of tenth abdominal
segment; 10LP, 10RP, processes of 10L, 10R; LC,, LC,, RC,, RC,, first and second
segments of left and right cerci; LCB, RCB, left and right cercus-basipodites; H, ninth
abdominal sternite; HP, process of H.
476 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
similar in general arrangement to the preceding species; 10RP, subobtuse; 10RP.,
more slender; 10LP broader, with a slight dorsal flange longitudinally (Fig. 6);
RCB smaller. First segment of left cercus (LC,) very characteristic; basal lobe
smaller, distal lobe strongly incurved, with stronger teeth; outer margin of LC,
convex. Left cercus-basipodite (LCB) subobtuse, directed backwards.
©. Unknown.
Locality.—Shimoga, Mysore, India: River Tunga, 1,865 ft., coll. P. S. Nathan,
1.vii—. A single male, well preserved, in the Museum of Comparative Zoology,
Harvard University (holotype). Named after Dr. A. D. Imms, to whom much of
our knowledge of Indian Embioptera is due.
Key to the Species of Metembia (¢).
1. First segment of left cercus incurved, external margin convex ........ immsi, n. sp.
First segment of left cercus not incurved, external margin concave ...... ferox, n. sp.
Genus PSEUDEMBIA, Nn. gen.
Genotype, Pseudembia paradoza, n. sp.
Indian Embioptera related to Metembia, but differentiated by the following
characters of the male terminalia: Left hemitergite with a simple posterior
process, acute or truncate, and with a dorsal lobe, shert and obtuse, arising from
the hemitergite laterodorsally on the right of the insertion of the posterior
process. First segment of left cercus with two internal lobes, the basal one small,
the distal one large, both covered wholly or partly with numerous small teeth.
PSEUDEMBIA PARADOXA, Qh. Sp. Figs. 9-14.
6. Length 11-12 mm.; head 1:8-2-2 mm. x 1-4-1555 mm.; forewing 9-0-9-5
mm. x 1:8-2:0 mm.; hindwing 8-0-8-5 mm. x 1:8-2-°0 mm. General colour (in
alcohol) mid- to pale ferruginous, eyes black, wing-veins golden-brown bordered by
pale-brown bands, with rather broad hyaline inter-venal lines. Head (Fig. 9)
broad, eyes rather large, sides behind eyes converging markedly. Antennae with
up to 22 segments, all except first very slender; total length up to 5 mm. Wings
as in HEmbia, the holotype with anomalies as follows: In both forewings, R, is
forked terminally; in the right hindwing there is an additional pigment-band, but
no vein, between Cu, and the cubital stem (Cu,). First segment of hind tarsi
with two large ventral bladders. Terminalia (Figs. 10-14) with right hemitergite
(10R) as in Hmbia, the posterior process (10RP,) short, acute, the inner process
(10RP.) elongate, slenderly tapered in front. Left hemitergite (10L) complex,
with a large laterodorsal lobe directed to the right, short and obtuse, and an
elongate posterior process {10LP), curving downwards terminally, irregularly
tapered, acute (Figs. 11, 12). Right cercus with two subcylindrical segments
(RC,, RC.), with a basal annular cercus-basipodite (RCB). First segment of left
cercus (LC,) complex, outer margin convex, inner margin with a small basal
lobe dorsally, furnished with small teeth; inner margin distally dilated inwards,
dilation with a large concavity for the accommodation of the basal lobe of the left
hemitergite; small teeth present on a blunt lobe dorsad to the concavity; ventral
parts of distal lobe smooth (Fig. 13). Hypandrium (H) produced to an obtuse
process (HP) to the right of the mid-line; left cercus-basipodite (LCB), between
HP and base of LC,, with a short blunt median process.
2. Unknown.
Locality—India: Namkum, Ranchi, Bihar, coll. W. B. R. Laidlaw, 1928
(holotype g and paratype ¢ in the British Museum).
BY CONSETT DAVIS. 477
PSEUDEMBIA TRUNCATA, Nl. Sp. Figs. 15-19.
do. Length 14 mm.; head 2:4 mm. x 2:0 mm.; forewing 12 mm. x 1:9 mm.;
hindwing 11 mm. x 1:9 mm. Antennae incomplete. General colour as in
Ps. paradoxa, darker, probably due to dry state of specimen. Head (Fig. 15),
wings, and hind tarsi (Fig. 16) as in Ps. paradoxa, wings without venational
anomalies. Terminalia (Fig. 17-19) resembling Ps. paradoxa, but with the distal
part of the inner margin of the first segment of the left cercus (LC,) smoothly
dilated, without any concavity, and evenly furnished with small teeth; basal lobe
of left hemitergite correspondingly smaller. Process of left hemitergite (10LP)
obliquely truncate terminally (Fig. 18).
%. Unknown.
Locality.—Shimoga, Mysore, R. Tunga, 1,865 ft.; coll. P. S. Nathan, 13.iv.—
(holotype g in the Museum of Comparative Zoology, Harvard University).
Key to the Species of Pseudembia (c).
1. Distal part of inner face of first segment of left cercus with a large concavity; left
hemitergite with a large obtuse basal lobe .................... paradoxa, Nn. sp.
Distal part of inner face of first segment of left cercus smoothly dilated; basal lobe
Ofmlettivnennitergitensraal lM Acai Sshucer arc oko eo. cuttodelis chekotentes cueholaiyis. truncata, n. sp.
Figs. 9-14.—Pseudembia paradoxa, n. sp., holotype ¢%. 9. Head from above, x 15.
10. Terminalia from above, x 15. 11. Left hemitergite from above, x 30. 12. Distal part
of left hemitergite viewed laterodorsally from the left, x 30. 138. First segment of left
cercus from above and slightly to the right. x 30. 14. Terminalia from below, x 15.
Figs. 15-19.—Pseudembia truncata, n. sp., holotype o&. 15. Head from above, x 15.
16. First segment of hind tarsus viewed laterally, x 30. 17. Terminalia from above, x 15.
18. Process of left hemitergite from above, x 30. 19. Terminalia from below, x 15.
478 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
Genus PAREMBIA, Nn. gen.
Genotype, Oligotoma valida Hagen, 1885, Canad. Entomologist, 17, p. 150.
Embioptera closely related to HEmbia Latreille, but with two relatively large
ventral bladders on the first segment of the hind tarsi. Venation and terminalia
not generically distinguishable from Hmbia.
Metembia differs from Parembia in the bilobed, strongly-toothed first segment
of the left cercus; Pseudembia differs in the complex form of the left hemitergite;
its left cercus has the first segment bilobed, as in Metembia, but the teeth are
small, as in Parembia.
PAREMBIA VALIDA (Hagen, 1885). Figs. 20-24.
Oligotoma valida Hagen, 1885, l.c—Hmbia major Imms, 1913, Trans. Linn. Soe.
London, Zool., xi, p. 1.
Under Oligotoma michaeli M’Lachlan, Hagen (l.c.) described a female from
Amballa, Kumaon Himalayas, introducing the name Oligotoma valida, and there-
after considering the specimen as O. michaeli. This female is in the Museum of
Comparative Zoology, Harvard University, with the label ‘O. valida Hagen*; fem.
of O. michaeli; Mon. Emb. 150’ in Hagen’s writing. The asterisk is Hagen’s
characteristic type designation. The specimen is conspecific with the species well
described from both sexes by Imms (l.c.) as Hmbia major. It is regrettable that
Hagen’s name must displace that of Imms, by priority; knowledge of the species
will, however, be due to Imms’s excellent description, although the name is
displaced.
Hagen’s specimen agrees in colour and size (18 mm.) with Imms’s series, and
has the characteristic number of hind metatarsal bladders (two). It is, of course,
no relation to Oligotoma michaeli; the male described from Amballa by Hagen
(1.c.) is not O. michaeli either, but is, in fact, a large, dark specimen of O. nigra
Hagen, the type series of which, smaller and paler, is from Egypt (Museum of
Comparative Zoology).
In view of the close proximity of Amballa to Imms’s localities, and of the
knowledge that the species is unlikely to show variation in such a short range,
since series from as far away as Mesopotamia and Bihar are scarcely more than
subspecifically distinct, there seems to be no alternative but to reject the name
major, even though Hagen’s type, being a female, has no taxonomic features apart
from the tarsal bladders and the exceptional size.
In the British. Museum of Natural History there are two well-preserved
_ Specimens (4, 9), labelled ‘Embia major Imms. Bhowali, Kumaon Himalaya, July
1912, A. D. Imms’. These are presumably intended as types, though not so labelled.
I name the ¢ allotype of Parembia valida (Hagen).
Full details of the morphology of the species, and of individual variation,
are given by Imms (le.). The accompanying figures (20-24) are from the
specimens mentioned above (British Museum), figure 20 from the female, the rest
from the male allotype. The occasional forking of the media, noted by Imms, is
demonstrated in Figure 22.
PAREMBIA MINOR (Mukerji, 1927). Fig. 25.
Hmbia minor Mukerji, 1927, Rec. Ind. Museum, xxix, p. 253.
Full details have been given by Mukerji (l.c.). The differences from P. valida
(EZ. major), as tabulated by Mukerji (l.c., p. 265) scarcely warrant more than
subspecific rank, but, as I have not seen the specimens, I am unwilling to reduce
BY CONSETT DAVIS. 479
the status. The size differences are significant, subspecifically at least, but the
structural differences listed seem to be based on a misapprehension. Mukerji
appears to base his comparison on Imms’s description, not on actual specimens,
of P. valida, and the differences noted in the compression of the ninth tergite
and curvature of the process of the left hemitergite seem likely to represent
merely a variation in method of preparation and in disposition of the structures
when figured. The smoothness of the tarsal bladders appears to be concerned, not
28
Figs. 20-24.—Parembia valida (Hagen) (= Embia major Imms). 20. 9, hind tarsus
viewed laterally, x 15. 21-24, allotype ¢. 21. Head from above, x 6. 22. Left forewing,
x 6. 23. Terminalia from above, x 15. 24. Terminalia from below, x 15.
Fig. 25.—Parembia minor (Mukerji), ¢%, terminalia from above (after Mukerji, 1927,
fig. 5B).
Figs. 26-27.—Parembia persica (M’Lachlan), ¢@ from Persia. 26. Terminalia from
above, x 11-5. 27. Terminalia from below, x 11:5.
Figs. 28-32.—Parembia persica (M’Lachlan), co from Baghdad. 28. Head from
above, x 15. 29. Left forewing, x 8. 30. Hind tarsus viewed laterally, x 15. 31.
Terminalia from above, x 15. 32. Terminalia from below, x 15.
480 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
with structural difference, but with the power of the microscope used. The inner
surface of the concavity of the first segment of the left cercus is not denticulate
in the specimen of P. valida (E. major) here figured (Figs. 23, 24), and the
‘ventral process’ (left cercus-basipodite of this paper) agrees in this specimen
with Mukerji’s description of P. minor. The number of antennal segments is an
unreliable criterion, being subject to individual variation and to breakage. All
the structural differences noted by Mukerji seem, therefore, to be open to question.
Figure 25, after Mukerji (l.c., Fig. 5B), represents a dorsal view of the male
terminalia of Parembia minor.
PAREMBIA PERSICA (M’Lachlan 1877). Figs. 26-32.
Embia persica M’Lachlan, 1877, J. Linn. Soc. London, Zool., xiii, 70, p. 382.
The type, from Shahrud, North Persia, is not in the M’Lachlan Collection
(British Museum), where all M’Lachlan’s other types of this Order are preserved.
It may therefore be assumed to be irretrievably lost. The following description is
from two males in the Paris Museum, from Bender-Bouchir, Persia (coll. Dr.
Bussiéres, 1905). These had been identified by Navas as Embia tartara de Saussure
1896, which is probably a synonym of P. persica (M’Lachlan) (v. infra). Navas
(1923, p. 9, fig. 1) has described these specimens, but his figures are inaccurate.
6. Length 9-5 mm.; length of forewing 8 mm., of hindwing 7 mm. General
colour rather pale brown, eyes black, wings mid-brown with hyaline intervenal
lines (M’Lachlan’s data are: Black, rather shiny; length 9:5-10-5 mm.). Venation,
tarsi, and terminalia as in P. valida (no venational anomalies); the first segment
of the left cercus (LC,) is slightly different in form, the longitudinal channelling
of the inner face, basad to the internal lobe, being less marked.
9 (of this series) unknown (cf., however, Silvestri, 1923).
Several series from Mesopotamia (Baghdad, coll. H. Scott; Amara, Basra, coll.
P. A. Buxton) are in the British Museum; they have been described by Hsben-
Petersen (1929a) and Silvestri (1923), and the terminalia adequately figured; the
number of tarsal bladders has been overlooked, and Esben-Petersen gives the
colour as blackish-brown (apparently following M’Lachlan), whereas, in members
of the same series seen by me, it was mid- to rather pale brown.
The males agree with the above description of P. persica, and there seems no
need to introduce the alternative name scotti (Hsben-Petersen), unless specimens
from M’Lachlan’s type locality should prove different from the present specific
concept.
Silvestri (1.c.) considers these specimens to be probably a subspecies of Hmbia
Savignyi Westwood; Hsben-Petersen (19296) denies this. In view of the difference
in the tarsi, considered here as generic, Silvestri’s view cannot be followed.
Embia tartara de Saussure 1896 (Mitt. Schweiz. entomol. Ges., Bd..9, Hft. 8,
p. 352), from Turkestan, is probably synonymous with P. persica in the present
sense. We owe our knowledge of the type of H. tartara to Krauss (1911, p. 67,
Pl. v, figs. 22, 22A), who studied it in the Geneva Museum. He notes that the
second segment of the left cercus is broken, its former attachment being evident;
de Saussure considered it as unbroken and originally one-segmented. Krauss’s
figures of the terminalia are from the dry, unprepared specimen, and show the
hemitergites as not quite tallying with the present figures (of P. persica); the
left cercus and cercus-basipodite, however, agree closely with the present figures.
The locality is probably closer to M’Lachlan’s type locality than any of those listed
here (Baghdad, Amara, Basra, Bender-Bouchir).
BY CONSETT DAVIS. 481
Key to the Species of Parembia (<¢).
1. Inner face of first segment of left cercus, basad to echinulate lobe, not markedly
channelled longitudinally. Pale to mid-brown. Mesopotamia, Persia, Turkestan
EME Ee eae festa one Lepaoe eae seaeh hie, mua ousousueNeaetiomeis bien elke alco ya) shen Ian eis persica (M’Lachlan)
= tartara (Sauss.), = scotti (Esb.-Petersen)
Inner face of first segment of left cercus markedly channelled longitudinally basad
to echinulate lobe. Dark brown to black. India ........................... 2
R, Iberian Copal sshd, B AWE ose .6 BiploD dia Om. ciololcibioia oro malolalowsiteckelavc o oo minor (Mukerji)
Wengihedi2 ios) Ime UI AONwEtima lavas’ sepscis alee sels clersiecieee sac valida (Hagen)
= major (Imms)
Note——The above may represent three subspecies, in which case P. persica
should be selected as type subspecies, by priority. EHmbia rabaulti Navas 1934
(Mem. Pont. Accad. Nuovi Lincet, Series iii, Vol. i, p. 224, fig. 101) may belong to
Parembia, and may be synonymous with one of the above. The poor description
does not allow any definite conclusion; the type (¢; Mus. Berlin) requires
re-examination.
DISCUSSION.
Apart from the hind tarsi, Parembia is generically inseparable from Hmbia
Latreille. Its separation on this character seems to be justified geographically,
and it facilitates the drawing up of a generic concept for Hmbia, and the con-
sideration of the relationships of the more advanced Metembia and Pseudembia.
It is not possible to state whether the number of hind metatarsal bladders of
Embia (one) or Parembia (two) is the more primitive condition. The Neotropical
genus Clothoda, the most generalized recent Embiopteron in other characters,
agrees with Parembia in this respect, but this cannot be used as a safe argument
for the primitive nature of two hind metatarsal bladders on an altogether different
line of descent. For instance, Embia and Parembia might possibly be derived from
an extinct Old World genus with only one hind metatarsal bladder, and with
generalized terminalia as in Clothoda.
The differentiation of Metembia and Pseudembia from Parembia has proceeded
along two rather divergent courses, and this prevents the use of less than three
generic concepts; it is impossible to consider the species of Pseudembia congeneric
with those of Metembia, but not with Parembia, while an attempt to group the
three as a single genus overlooks the close relation of Parembia to Hmbia,
and would include three series, two of which would be more divergent from the
third than the third would be from Hmbia.
Metembia has been derived from Parembia chiefly by modification of the
first segment of the left cercus, which is parallel to that found in Dihybocercus
or, perhaps more closely, considering the dentition, Donaconethis. Pseudembia
has the first segment of the left cercus also bilobed, as in Metembia, but with small
teeth, as in Parembia; its left hemitergite has been considerably modified from
the simple form common to Parembia and Metembia.
List of References.
ESBEN-PETERSEN, P., 1929a.—Embioptera from Baghdad. Ent. Mo. Mag., Series 3, Vol. 15,
No. 169.
, 1929b.—Further Remarks on Embioptera from Baghdad. Ibid., Vol. 15, No. 179.
HAGEN, H. A., 1885.—Monograph of the Embiidina. Canad. Entomologist, 17. (Wondon,
Ontario).
Imus, A. D., 1913.—On Embia major, sp. nov., from the Himalayas. Trans. Linn. Soc.
London, Zool., xi, 12.
Krauss, H. A., 1911.—Monographie der Hmbien. Zoologica, Hft. 60, Bd. 23 (Stuttgart).
M’LACHLAN, R., 1877.—On the Nymph-Stage of the Embidae, with Notes on the Habits
of the Family, ete. Journ. Linn. Soc. London, Zool., xiii, 70.
482 TAXONOMIC NOTES ON TIE ORDER EMBIOPTERA. VI-X,
MuxKergi, S., 1927.—On the Morphology and Bionomiecs of Hmbia minor sp. noy., with
Special Reference to its Spinning Organ. Rec. Ind. Musewm, xxix, 4.
NavAs, L., 1923.—Comunicaciones Entomolégicas. 6. Notas sobre Embi6pteros. Rev.
Acad. Cienc. Zaragoza, viii.
— , 1934.—Insecta Orientalia. Mem. Pont. Accad. Nuovi Lincei, Series III, Vol. 1.
DE SAUSSURE, H., 1896.—Note sur la Tribu des Embiens. Mitt. Schweiz. entomol.
Gesellschaft, Bd. 9, Hft. 8.
SILVESTRI, F., 1923.—Thysanura, Termitidae and Embiidae collected in Mesopotamia and
N.W. Persia by W. Edgar Evans, B.Sc., late Capt. R.A.M.C., and Dr. P. A. Buxton.
Trans. Ent. Soc. London.
PART VII. THE GENUS DICTYOPLOCA KRAUSS.
(Ten Text-figures. )
Genus DicryopLoca Krauss 1911.
Zoologica, Hft. 60, Bd. 23, p. 54—Genotype, Dictyoploca cercocyrta Krauss, l.c.
African Embioptera, the males with the following characters: Wingless; first
segment of hind tarsus with two ventral bladders; first segment of left cercus
echinulate, second segment distinct, subcylindrical.
This definition of the genus (sensu Rimsky-Korsakov, 1927) separates it from
Haploembia Verhoeff, which has the first segment of the left cercus smooth (cf.
Krauss, 1911, figs. 16A, 17B). It differs from the wingless species of Embia Latr.
(wrongly divided off as Monotylota) in the presence of an extra tarsal bladder,
and in the lack of an inner flap-like process to the right hemitergite of the tenth
abdominal segment.
The Australian genera Notoligotoma Davis and Metoligotoma Davis would
agree structurally with the above diagnosis (the former having the males winged
as well as wingless), except that they have the second segment of the left cercus
reduced or absent.
DicryopLoca CERCOCYRTA Krauss 1911 (1.c.). Figs. 1, 2.
¢ (after Krauss). Length 9 mm. General colour dark yellowish-brown. Head
large, elliptical, evenly narrowed behind eyes. First segment of hind tarsi with
two ventral bladders, the proximal one very large. Terminalia (Figs. 1-2) with
tenth abdominal tergite completely cleft; right hemitergite produced back to a blunt
hook-like process (10RP), directed inward and downward; process of left hemi-
tergite (10LP) obtuse, ending spathulately. First segment of left cercus (LC,)
incurved, internally truncate and echinulate. Second segment of left cereus (LC,),
and both segments of right cercus (RC,, RC.), subeylindrical. Process of ninth
sternite (HP) small, obtuse, directed to the left. Left cercus-basipodite small.
© unknown.
Locality—Port Elizabeth, South Africa; type in Hamburg Museum.
DICTYOPLOCA CAPENSIS (Hsben-Petersen 1920). Fig. 3.
Haploembia capensis Esben-Petersen, 1920, Ann. S. Afr. Museum, xvii, 6, p. 503.
3g (after Esben-Petersen). Length 10-11 mm. General colour dark brown.
Head somewhat narrowed behind, with almost straight lateral margins and rounded
hind angles. Hind tarsi as in preceding species. Terminalia (Fig. 3) with process
of right hemitergite (10RP) bifid, directed inward; process of left hemitergite
(10LP) essentially similar to the preceding species. Echinulate process of first
segment of left cercus (LC,) rounded, not truncate as in D. cercocyrta.
©. Length 17 mm. Colour, and hind tarsi, as in the male.
Locality.—Dunbrody, Cape Province. Location of types not stated.
BY CONSETT DAYIS. 483
Figs. 1-2.—Dictyoploca cercocyrta Krauss. o¢ terminalia from above and below (after
Krauss, 1911).
Fig. 3.—Dictyoploca capensis (Hsb.-Pet.). o& terminalia from above (after Hsben-
Petersen, 1920).
Wigs. 4-6.—Dictyoploca burensis R.-Korsakoy. o&: 4. Head from above. 5. First
two segments of hind tarsus, viewed laterally. 6. Terminalia from above (after Rimsky-
Korsakov, 1927).
Fig. 7.—Dictyoploca sjostedti (Silvestri). o& terminalia from above (from Enderlein,
1912, after Silvestri, 1910).
Figs. 8-10.—Dictyoploca rimskyi, n. sp. Holotype oc. 8. Head from above, x 15.
9. Terminalia from above, x 15. 10. Terminalia from below, x 15.
Magnifications for Figures 1-7 not given by respective authors. Figures 8-10 based
on camera lucida outlines. Setae omitted.
484 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
DIcTYOPLOCA BURENSIS Rimsky-Korsakov 1927. Figs. 4-6.
Revue russe d@’Entomologie, xxi, 3-4, p. 145.
é¢ (after Rimsky-Korsakov). Length 10 mm. General colour brown to black.
Head as in Figure 4; hind tarsi as in Figure 5. Terminalia (Fig. 6) with process
of right hemitergite (10RP) slender, acute, directed backward; process of left
hemitergite (10LP) tapered, acute, margins sinuous. First segment of left cercus
(LC,) incurved, inner margin rounded and echinulate distally. 9 unknown.
Locality—Bura Mountains, British East Africa. Location of type not stated.
DIcTYOPLOCA SJOSTEDTI (Silvestri 1910). Fig. 7.
Embia sjostedti Silvestri, 1910, Sjostedt’s Kilimandjaro-Meru Exped., Bd. 3,
p. 41 (Stockholm).—Haploembia sjéstedti (Silvestri), Enderlein, 1912, Coll. de
Selys-Longchamps, fasc. 3, p. 69, fig. 40.
¢ (from Enderlein, after Silvestri). Length 15 mm. General colour black,
legs and cerci brownish. Head little longer than broad, posterior angles rounded.
Hind tarsi as in preceding species (cf. Silvestri, l.c., Fig. 7). Terminalia (Fig. 7)
with only very slight differences from D. burensis, e.g. the first segment of the left
cercus (LC,) less incurved, the process of the right hemitergite (10RP) curved
inward terminally, and the process of the left hemitergite (10LP) straighter.
©. Length 15-6 mm.; general colour brownish-red.
Locality—Ngare-na-nyuki, Lower Meru, Tanganyika. Location of types not
stated.
Enderlein’s copy of Silvestri’s figure shows the first segment of the left cercus
of the male smooth. It may be assumed to be echinulate, since the species bears
very great resemblance on other characters to D. burensis. The differences, noted
above, may be due to the disposition of the parts when figured, and not to structural
difference; if this were so, D. burensis would fall as a synonym. The two species
are best considered as distinct pending further information.
DIcTYOPLOCA RIMSKYI, n. sp. Figs. 8-10.
d. Length (dry) 13 mm.; head 3-8 mm. x 2:9 mm. General colour very dark
brown to black. Head (Fig. 8) similar in general form to D. burensis, relatively
longer. Antennae very long (10 mm.), the left with 31 segments, the right with
30. Hind tarsi missing; presumably with two metatarsal bladders, as the species
is in its other characters closely related to the preceding. Terminalia (Figs. 9-10)
with the right hemitergite (10R) produced inward and downward to a short acute
process (10RP), inner margin sinuous. Left hemitergite (10L) produced back-
ward from its inner margin to a slender process (10LP), tapered, subacute. Right
cercus composed of two subcylindrical segments (RC,, RC.), arising from a pad-
like basipodite (RCB). First segment of left cercus (LC,) clavate, echinulate at
middle of inner face, where it is produced into a weakly-bilobed process, flattened
dorsiventrally. Second segment (LC.) subcylindrical. Process of ninth sternite
(HP) obtuse, placed to the right of the mid-line; left cercus-basipodite (LCB)
obtuse. 9 unknown.
Locality—Athi River, British East Africa, May 8-19, 1899, C. S. Betton; holo-
type ¢@ in the British Museum of Natural History. Dedicated to Dr. M. Rimsky-
Korsakov.
Key to the Species of Dictyoploca (0c).
ic inst scementuot Letts cercusmncunved struncatem eri enieeeneiecee cercocyrta Krauss
MITStSerImentnOtMerticercusmrolunged: anternallliveersenrer in enerelencienncnicieiekensnsieieiencnaienene 2
2 Process Of jleLt hemitergitevoDtusel jcc. +2 < cde Coe ie ean capensis (Esb.-Pet.)
Process (Of, left (hemitereite7SUDACUUC) sciences se) sieme eeicreneln oieoe eleenchanercrcusione rer icnenctewenen nenon ene 3
BY CONSETT DAVIS. 485
8. Process of right hemitergite short, directed inward .................. rimskyi, n. sp.
Process of right hemitergite long, directed backward ..................-.++++-+es+ 4
4. Inner margin of first segment of left cercus almost straight .... sjdstedti (Silvestri)
Inner margin of first segment of left cercus markedly concave .. burensis R.-Korsakoyv
List of References.
EINDERLEIN, G., 1912.—Hmbiidinen, in Coll. de Selys-Longchamps, fase. 3.
EXSSBEN-PETERSEN, T., 1920.—New Species of Neuropterous Insects from South Africa
(Ephemerida, Megaloptera, and Hmbiidina). Ann. S. Afr. Museum, xvii, 6.
Ikrauss, H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23 (Stuttgart).
Rimsky-Korsakov, M., 1927.—A New Species of Embia from British Hast Africa. Rev.
russe d’Hntomologie, xxi, 3-4.
SILVESTRI, F., 1910.—Embiidae, in Sjostedt’s Kilimandjaro-Meru Exped. (Stockholm).
(Not seen in the original.)
PART VIII. THE GENUS DIHYBOCERCUS ENDERLHIN, AND A NEW AFRICAN
GENUS RELATED TO IT.
(Twenty-five Text-figures. )
Genus DirHysocercus Hnderlein 1912.
Coll. zool. de Selys-Longchamps, fase. 3, p. 109 (as subgenus of Hmbia Latr.).
Genotype, Hmbia (Dihybocercus) severini Enderlein, 1912, l.c-—Raised to
generic rank, Navas, 1931, Rev. Zool. Bot. africaines (Tervueren), Vol. 21, fase. 2,
Dp. 134.
African Embioptera, the males with the following characters: Winged, R,,;
forked, M simple, cubitus 3-branched, the two lateral branches arising anteriorly
from the stem, pectinate. First segment of hind tarsi with two large ventral
bladders. Tenth abdominal tergite completely cleft; process of left hemitergite
complex, with a flat latero-dorsal lobe. First segment of left cercus with inner
margin produced in two lobes, both bearing numerous small teeth.
Three species: Uganda, Congo and Rhodesia.
Enderlein’s generic diagnosis depends on the lobes of the first segment of the
left cereus, a character found in unrelated genera also (Donaconethis End.,
Pseudembia Davis, Metembia Davis, and others). The above diagnosis delimits the
genus from these parallel genera. Additional points not recorded by Enderlein in
the genotype (e.g. number of tarsal bladders) are deduced from the structure of a
new Rhodesian species, very closely related to D. severini, described below.
The genus as here recognized differs from Donaconethis End. (sensu Davis
1939) in the number of tarsal bladders, dentition of the left cercus, and in the
simplicity of the media, which tends to fork in Donaconethis. Dihybocercus
appears to stand closest to Rhagadochir End. (s.str., i.e. congeneric, in a narrower
sense than Enderlein’s, with Rh. vosseleri End.). It is differentiated chiefly by the
form of the first segment of the left cercus, which has only one echinulate internal
lobe in Rhagadochir.
DIN YBOCERCUS SEVERINI Enderlein 1912. Figs. 1-2.
Hmbia (Dihybocercus) severini Enderlein, 1912, l.c—Dihybocercus severini
Enderlein, Navas, 1931, l.c.
6 (after Enderlein). Length 12 mm.; forewing 93-11 mm. x 2-6-3-2 mm.;
hindwing 9-10 mm. x 2-8-3:-4 mm.; head 24 mm. x 1:8 mm. General colour rust-red,
front of head and terminalia dark brown, legs brownish, wings brown with dark-
brown veins and hyaline streaks. Head relatively broad, flattened, sides behind
eyes somewhat rounded, weakly converging, hind angles rounded. Hyes prominent,
486 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA, VI-X,
fairly large. Wings (Fig. 1) as in generic description. Details of hind tarsi not
given by Enderlein, but presumably with two metatarsal bladders, as in the other
species. Terminalia (Fig. 2) with right hemitergite (10R) produced downwards
and inwards in a short, slender, subobtuse process (10RP,); inner process of 10R
not detailed by HEnderlein. Process of left hemitergite (10LP) long, sinuously
tapered terminally, with a flat basal lobe directed upwards and to the right.
First segment of left cercus (LC,) with two rounded echinulate lobes internally;
other segments of cerei (LC., RC,, RC.) subcylindrical. Left cercus-basipodite
(LCB) produced outwards, ending acutely.
a
Figs. 1-2.—Dihybocercus severini Iind., ¢. 1. Right fore- and hindwing, x 3.
Terminalia from above, x 14. (After Enderlein, 1912, Figs. 72, 71.)
Figs. 3-9.—Dihybocercus rhodesiae, n. sp., holotype ¢@. 3. Head from above, x 20.
4. Left fore- and hindwing, x 8. 5. Hind tarsus viewed laterally, x 20. 6. Terminalia
from above, x 20. 7. Process of left hemitergite from above, x 40. S. The same from
below, x 40. 9. Terminalia from below, x 20.
to
BY CONSETT DAVIS. 48
“A
° unknown.
Locality.—Belgian Congo: 311 km. from Kindia. Types (¢@) in Coll. de
Selys-Longchamps, Stettin Museum, and Musée du Congo, Tervueren; not seen by
the author.
DIHYBOCERCUS RHODESIAE, nh. Sp. Figs. 3-9.
6. Length 12-15 mm.; head 2-1 mm. x 1:8 mm.; forewing 7-6 mm. x 2:2 mm.;
hindwing 6-8 mm. x 2:1 mm. General colour very dark brown, wings with dark
smoky-brown bands bordering dark-brown veins, with hyaline streaks between.
Head (Fig. 3) relatively broad, eyes rather small, sides behind eyes at first
diverging, then smoothly rounded. Antennae incomplete. Wings (Fig. 4) as in
the generic diagnosis, but with R, or R,; tending to branch terminally in one or
more wings: in the holotype, R; is simple, but R, is shortly bifid in both forewings.
Hind tarsi (Fig. 5) with two well-developed bladders on first segment, one on
second. Terminalia (Figs. 6-9) with tenth tergite completely cleft; right hemi-
tergite (10R) triangular, posteriorly ending in an acute process (10RP,), directed
inward and downward. 10R with an inner subrectangular flap (10RP.), connected
posteriorly to 10R, anteriorly separated by membrane. Ventral to 10RP, is a
triangular membraneous lobe, partly concealed, chitinized only medially. Left
hemitergite (10L) with a long process (10LP), terminally acute, sinuously tapered,
with an irregular basal lobe dorsally and to the right (Figs. 7-8). First segment
of left cercus (LC,) similar to D. severini, the basal lobe placed more ventrally
than the distal lobe. Ninth sternite (H) produced backward, slightly to the right
of the mid-line, to an obtuse process (HP). Left cercus-basipodite (LCB) situated
between HP and base of LC,, directed outward, acutely tapered. Right cercus-
basipodite (RCB) small, subannular. 2 unknown.
Locality.—Rhodesia (Marshall Collection; British Museum of Natural History):
holotype @ and paratypes (%).
Closely related to D. severini. It is therefore admissible to assume similarity
in the hind tarsi, ninth sternite, and inner process of right hemitergite. It differs
from Enderlein’s description of D. severini in the narrower process of the left
hemitergite. In view of the possibility that this process may be viewed obliquely
in Enderlein’s figure, or inaccurately figured, it may be that it should be regarded
as a subspecies only; the possibility of absolute synonymy cannot be discarded
entirely. The present course seems the simplest way in which to place the
additional generic facts on record.
DIHYBOCERCUS CONFUSUS, n. sp. Figs. 10-20.
A pinned male in the British Museum of Natural History carries the following
labels: ‘Gulu, W. Madi, Uganda, 5,000 ft., V-1926, G. D. Hale Carpente1’;
‘Rhagadochir vosseleri End., det. Friederichs 1936’. The terminalia of the dried
specimen had not been prepared; preparation showed the determination to be
incorrect, and the specimen is therefore described as a new species, in the genus
Dihybocercus.
6. Length 9 mm.; head, length 2-0 mm., breadth 1:6 mm. Forewing 8 mm. x
24mm. General colour smoky-brown, prothorax and legs (especially femora) more
orange-brown, eyes black. Wing-veins dark brown, bands bordering veins smoky-
brown, lines between bands hyaline. Head (Fig. 10) with eyes large, prominent,
sides behind eyes slightly and smoothly converging, rounded behind. Antennae
incomplete. Wings (Fig. 11) with all veins strong, cross-veins numerous, fork of
R,,,; nearly twice length of stem. Stem of cubitus with two anterior branches
488 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
pectinately. Hind tarsi (Fig. 12) with two ventral bladders on first segment, one
terminal, one medial; second segment short, with a terminal bladder ventrally.
Terminalia (Figs. 13-20) with tenth abdominal tergite completely divided by a
longitudinal cleft; right hemitergite (10R) posteriorly curving downwards to a
short spiniform process (10RP,), directed outwards (Figs. 14-15), with a small
concavity and then a blunt projection outside the spine. Inner margin of right
hemitergite with a flat process (10RP.) separated from the body of the hemitergite,
except posteriorly, by membraneous areas (Fig. 14); process curving inwards
anteriorly. Left hemitergite (10L) produced backwards to a slender process
a
Figs. 10-20.—Dihybocercus confusus, n. sp., holotype @. 10. Head from above, x 15.
11. Left forewing, x 8. 12. Hind tarsus viewed laterally, x 15. 13. Terminalia from
above, x 15. 14. Right hemitergite from above, x 45. 15. Extremity of right hemitergite
viewed obliquely from above, right, and behind, x 45. 16. Process of left hemitergite
from above, x 45. 17. The same from below, x 45. 18. First segment of left cercus,
viewed from above and slightly to the left, x 45. 19. The same, viewed from above and
to the right, x 45. 20. Terminalia from below, x 15.
Figs. 21-25.—Odontembia spinosa (Navas), holotype ¢@. 21. Head from above, x 15.
22. Hind tarsus viewed laterally, x 15. 28. Terminalia from above, x 11. 24. Process of
left hemitergite viewed laterally from the right, x 15. 25. Terminalia from below, x 11.
All original figures based on camera lucida outlines.
BY CONSETT DAVIS. 489
(10LP), sinuously acute at apex, with a blunt irregular flap-like process latero-
dorsally to the left (Figs. 16-17). First segment of left cercus (LC,; Figs. 18-19)
with inner margin produced into lobes, one subapical, the other median, the latter
again subdivided by a shallow depression into two blunt lobes; all lobes echinulate.
Second segment (LC.) subcylindrical. Right cereus with first segment (RC,)
slightly dilated distally, second (RC.) thinner, subcylindrical. Ninth sternite
(H, Fig. 20) produced back to an obtuse process (HP) somewhat to the right
of the mid-line; to the left of this is a concavity, filled by the left cercus-basipodite
(LCB), which gives off an acute process towards the left. Right cercus-basipodite
(RCB) subannular, small.
Locality.—Gulu, Uganda. Holotype ¢ in the British Museum.
Key to the Species of Dihybocercus (<¢).
1. Posterior process of right hemitergite bifid ........................ confusus, Nn. sp.
Posterior process of right hemitergite simply tapered ..................200eeeeee 2
Ao JECOOESS OF liGar Increase loro“) oconccnconboonbes=yoodebbpoobDaoDO severini Enderlein
Process of left hemitergite narrower
Genus ODONTEMBIA, Nn. gen.
Genotype, Dihybocercus spinosus Navas, 1931, Rev. Zool. Bot. africaines
(Tervueren), Vol. xxi, fasc. 2, p. 134.
African Embioptera closely related to Dihybocercus, but with the two internal
lobes of the first segment of the left cercus each armed with 4-5 large, sharp teeth,
and the right cercus-basipodite produced backward, in the male. Other characters
as in Dihybocercus.
The structure and dentition of the left cercus are strongly reminiscent of
Donaconethis (sensu Davis 1939). The remaining characters agree most closely
with Dihybocercus, the venation and tarsal bladders separating these two genera
from Donaconethis. The right cercus-basipodite, small and subannular in
Dihybocercus and Donaconethis, appears to be partly fused to the first segment of
the right cercus in Odontembia, and is produced back to a free obtuse lobe.
The genus probably represents a direct specialization of Dihybocercus, notably
in the modification of the left cercus convergent to Donaconethis. One species:
Congo.
ODONTEMBIA SPINOSA (Navas 1931). Figs. 21-25.
Dihybocercus spinosus Navas, 1931, 1.c.
The following re-description is from Navas’s unique type (Musée du Congo,
Tervueren, Belgium):
6. Length* 10 mm.; forewing 7:5 mm. x 1:8 mm.; hindwing 6-5 mm. x 1:8 mm.;
head 1:8 mm. x 1:5 mm. General colour orange-brown, eyes black, wing-veins dark
brown, bordered by mid-brown bands. Head (Fig. 21) broad, eyes large, prominent,
sides behind eyes converging posteriorly. Venation as in the previous genus. Hind
tarsi (Fig. 22) with two large ventral bladders on the first segment, one on second.
Terminalia (Figs. 23-25) very characteristic; tenth tergite completely cleft, right
hemitergite (10R) produced posteriorly to an acute process (10RP,), directed
downward and inward. Inner margin of 10R with only a trace of a flap-like
process. Process of left hemitergite (10LP; Fig. 24) very complex, irregularly
tapered distally, flattened in a vertical plane, somewhat twisted, with a median
dorsal lobe directed forward. This lobe, the dorsal face of 10LP basad to it, and
the left face distad to it, are minutely nodulose. Right cercus with two sub-
* These dimensions do not agree with those given by Navas (l.c.) for the same
specimen.
NN
490 TAXONOMIC NOTES ON THE ORDER EMBLOPTERA. V1-X,
cylindrical segments (RC,, RC.); base of RC, partly fused to right cercus-
basipodite (RCB), the inner part of which is produced backward in an obtuse
lobe. First segment of left cereus (LC,) highly characteristie (the figure of Navas,
l.c., Fig. 70, is inaccurate), inner margin produced into two rather slender lobes,
the basal one placed more ventrally than the terminal one; basal lobe with two
very large, sharp teeth at apex, and two on distal face; terminal lobe with five
such teeth on anterior face. Second segment (LC.) subcylindrical. Ninth sternite
(H) produced to a blunt process (HP), curved to the left. Jeft cercus-basipodite
(LCB) produced backward, termination acute. 9 unknown.
Locality —Lulua, Belgian Congo, 1929, Dr. Walker; holotype ¢ in Mus. Congo,
Tervueren.
List of References.
Davis, C., 1939.—Taxonomic Notes on the Order Embioptera. v. The Genus Donaconethis
Enderlein. Proc. LINN. Soc. N.S.W., Ixiv, 3-4.
IENDERLEIN, G., 1912.—Embiidinen, in Coll. zool. de Selys-Longchamps, fasc. 3.
NavAs, L., 1931.—Insectes du Congo Belge (Série VI). Rev. Bot. Zool. africaines, Vol.
xxi, fasc. 2 (Tervueren).
PART IX. THE GENUS ENVEJA NAVAS.
(Six Text-Figures.)
Genus Envesa Navas 1916.
Mem. R. Acad. cienc. y artes de Barcelona, Vol. 12, No. 13, p. 23. Genotype,
Enveja bequaerti Navas, l.c.
Robust Embioptera, the males with the following characters: Mandibles huge,
projecting inwards, distally overlying labrum. Winged, with R,., forked, the fork
exceeding the stem; M simple; cubitus two-branched. All veins strong, cross-
veins rather numerous. First segment of hind tarsi with two very large ventral
bladders. Tenth abdominal tergite completely cleft by a longitudinal division
placed to the left of the mid-line; right hemitergite with a long posterior process;
process of left hemitergite complex. First segment of left cercus with a basal
echinulate internal lobe, otherwise smooth. Second segment of left cercus, and
both segments of right cercus, subcylindrical.
One species: Congo.
This remarkable genus has no close allies. It is perhaps most closely related
to Dihybocercus, from the same general region. It is immediately differentiated
from Dihybocercus by the extraordinary mandibles, and by the first segment of the
left cereus (with only one lobe); additional but less important differences are
found in the right hemitergite and the two-branched cubitus. EHnveja is not at all
closely related to Hmbia Latreille, as stated by Navas (l.c.).
ENVEJA BEQUAERTI Navas 1916 (l.c.). Figs. 1-6.
The following description is based on two specimens (¢) (Mus. Congo,
Tervueren), each labelled: ‘Enveja Bequaerti Nav.’; ‘Musée du Congo. Mufungwa
Sampwe, 1/16-xii-1911, Dr. Bequaert’; ‘Enveja Bequaerti Nav.; Navas S.J. det.’.
They may be regarded as cotypes (A and B); cotype B also bears Navas’s pink
manuscript label ‘Typus’, but there seems no need to distinguish it as holotype or
lectotype, as the two specimens are conspecific, and probably collected at exactly
the same time.
6. Length 17-5 mm. (A), 17 mm. (B); forewing 10-5 mm. x 2:5 mm. (A),
11 mm. x 3 mm. (B); hindwing 9 mm. x 2:5 mm. (A), 9 mm. x 3 mm. (B). Head
(B) 4:5 x 3-4 mm. General colour dark brown, head with ferruginous areas (as in
BY CONSETT DAVIS. 491
other members of the Order, but slightly different in position, probably due to
changes in the structure of the head associated with the development of the
mandibles; compare Figure 1 with that given by Davis, 1936, Fig. 42). Prothorax
orange-brown; wings with dark brown veins bordered by pale-brown bands, with
hyaline streaks between; margins of wings pale, tawny. Head (Fig. 1) relatively
very large, with a median anterior projection behind the clypeus, angular, and a
rhomboidal depression behind this projection; whole of head minutely granulate.
Eyes relatively small. Mandibles (Fig. 2) huge, incurved, each in the form of a
quadrant of a ring, distally truncate, roughened, overlying labrum. Maximum
Figs. 1-6.—Hnveja bequaerti Navas, 0. 1. Head from above. x 6. 2, Mandibles from
above, x 6. 3. Right forewing, x 6. 4. Hind tarsus viewed laterally. x 15. 6. Terminalia
from above, x 25. 6. Terminalia from below, x 25.
Figures 1 and 3 from cotype B, other figures from cotype A. All figures based on
camera lucida outlines. Setae omitted except in Figure 4,
492 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
antennal length 8 mm., with 18 segments. Wings (Fig. 3) with R,.; forked, fork
nearly twice as long as stem; M and Cu, simple. R, confluent subterminally with
R.,3;. The following venational anomalies occur: In both cotypes, R; is terminally
forked in the right forewing. In the left forewing of cotype A, R; and M become
confluent, and almost immediately separate again. The cross-veins are variable,
as shown in the following table:
Cotype A— Oa Lala ann [Relay dayne Tate ING IRI AIC hey
Right forewing .... — —_— — 1 — 1 —
Left forewing .. .. — — — —_— — confluent —
Right hindwing .. .. a 1 2 1 — 2 1
Left hindwing .. .. _— 1 —- 1 1
Cotype B—
Right forewing .. .. 2 3 3 2 1 1 2
Mekt. forewink, waa) se 1 3 3 2 1 2 2
Right hindwing .. .. 2 4 2 2 1 1 2
Heit -hindwineww eke 2 4 2 1 1 1 2
* In addition to terminal confluence.
This extreme variability is characteristic of the Embioptera, and justifies the
usual omission of details of position of the cross-veins. The above table shows
how small is the significance even of the relative frequency of the cross-veins, as
a great difference occurs between the two cotypes, which are structurally indistin-
guishable on other characters, and obviously conspecific.
Hind tarsi (Fig. 4) with ventral bladders very large, especially the more basal
bladder of the metatarsus. Terminalia (Figs. 5-6) with longitudinal division of
tenth abdominal tergite complete, placed to the left of the mid-line; right hemi-
tergite (10R) with outer margin produced backward and inward as a heavily-
sclerotized process (10RP,), slender, distally truncate, upper part of distal margin
concave, lower part furnished with minute teeth. Inner part of posterior margin
of 10R heavily sclerotized as a subrectangular plate (10RP.). Left hemitergite
(10L) produced backward from its right-hand part to a broad process (10LP),
sharply truncate distally, inner margin sinuous; 10LP with a subobtuse dorsal
lobe, as a continuation of its outer margin, directed backwards and a little to the
right, exceeding the main part in length. Right cercus with two subcylindrical
segments (RC,, RC.), arising from a small ventral subannular cercus-basipodite
(RCB). First segment of left cercus (LC,) subcylindrical, inner margin produced
near base to a blunt lobe, armed apically with small nodules; second segment
(LC.) subcylindrical. Ninth sternite (H) tapered back to an obtuse process (HP),
directed somewhat to the left; left cercus-basipodite (LCB) a flat plate between
HP and LC,, terminally obtuse. 9 unknown.
Locality —Mufungwa Sampwe, Belgian Congo; types in Musée du Congo,
Tervueren.
List of References.
Davis, C., 1936.—Studies in Australian Embioptera. Part i. Proc. LINN. Soc. N.S.W.,
Ixi, 5-6.
NavAs, L., 1916.—Neurépteros Nuevos o Poco Conocidos, Séptima Série. Mem. R. Acad.
cienc. y artes de Barcelona, Vol. 12, No. 13.
BY CONSETT DAVIS. 493
PART X. THE GENUS LEPTEMBIA KRAUSS.
(Ten Text-figures. )
Genus LEPTEMBIA Krauss 1911.
Zoologica, Hft. 60, Bd. 23, p. 71. Genotype, Leptembia hamifera Krauss,
1911, le.
Robust Hmbioptera, the males with the following characters: Winged, R, not
confluent with R.,,; R,,; forked, the fork longer than the stem; M simple; cubitus
three-branched, i.e. its anterior branch bifid. Tenth abdominal tergite completely
cleft longitudinally; right hemitergite massive, convex; process of left hemitergite
simple. First segment of left cercus with an internal echinulate forwardly-directed
process, longer than thick.
Two species: Hast Africa (Sudan; Zambesia).
I do not agree with Enderlein (1912), who includes this genus in Hmbia
Latreille. The left cercus immediately differentiates it. The right hemitergite
has not the characteristic form of Hmbia (s.str.), and the venational differences
appear to be significant: R, and R.,, are nearly always confluent in Hmbia, and the
cubitus is two-branched in most cases.
Krauss does not state the number of hind metatarsal bladders in the geno-
type. There are two in ZL. surcoufi (Navas), which I consider to be congeneric;
this probably applies to L. hamifera also, and offers a further point of difference
from EHmbia (s. str.).
LEPTEMBIA HAMIFERA Krauss 1911 (l.c.). Figs. 1-4.
6 (after Krauss). Length 15 mm.; forewing 10 mm. x 2:7 mm.; head
2:3 mm. x 1:8 mm. General colour pale ochreous, head darker, eyes black; wings
hyaline, with ochreous veins and narrow bordering lines; radius brown. Head
with sides behind eyes convergent, rounded behind. Antennae incomplete; eyes
small, reniform. Wings (Fig. 1) as in the generic description. Terminalia
(Figs. 2-4) with tenth tergite completely divided, right hemitergite (10R) massive,
swollen, with a rather short blunt process on the posterior inner angle. Process
of left hemitergite (10LP) acute, directed backward and curving to the left.
Right cercus with two subcylindrical segments (RC,, RC.); first segment of left
cercus (LC,) subcylindrical, inner margin subterminally produced to a slender
forwardly-directed hook, armed with sharp teeth (Fig. 4). Inner surface of LC,,
anterior to this hook, longitudinally channelled, with small teeth on the upper
part. Second segment (LC.) subcylindrical, more slender. Ninth sternite (H)
Se
Ri SSS
Ras3
Ru)
Rs A
Mm Gua Culb 4
Figs. 1-4.—Leptembia hamifera Krauss, ¢, after Krauss, 1911, Pl. v, figs. 23A-D.
1. Left forewing. 2. Terminalia from above. 3. Terminalia from below. 4. Left cercus
from below. (Krauss does not state the magnifications, but from his dimensions given
in the text they are here approximately x 4, x 12, x 12, and x 16 respectively.)
494 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. VI-X,
produced backward to an obtusely-tapered process (HP), curving to the left; left
cercus-basipodite (LCB) simple, apparently truncate; right cercus-basipodite
(RCB) small, with a peg-like extension posteriorly on the inner side. 9? unknown.
Locality—Sudan; type in the Vienna Museum (not seen by the author).
LEPTEMBIA SURCOUFI (Navas 1933). Figs. 5-10.
Embia surcoufi Navas, 1933, Broteria, Serie trimestral, Vol. 2, fase. 1.
Navas (l.c.) has noted the similarity to the genotype of Leptembia, without
accepting Krauss’s genus. The following description is from Navas’s unique type
(Muséum d’Histoire naturelle, Paris) :
6. Length 14:5 mm.; head 2:3 mm. x 1:9 mm.; forewing 11-5 mm. x 3:0 mm.;
hindwing 10:-5 mm. x 3-4 mm. Body and legs pale orange-brown, head black,
abdomen darker posteriorly; wing-veins dark brown, bordered by smoky-brown
bands. Hyes black, antennae dark brown. Head (Fig. 5) with eyes large,
prominent; sides behind eyes straight, converging strongly. Antennae incomplete.
Wings (Fig. 6) as in L. hamifera. Hind tarsi (Fig. 7) with two large ventral
bladders on first segment, one on second. Terminalia (Figs. 8-9) with tenth
abdominal tergite completely divided; right hemitergite (10R) large, convex, with
Figs. 5-10.—Leptembia surcoufi (Navas), holotype ¢%. 5. Head from above, x 7.
6. Left, forewing, x 7. 7. Hind tarsus viewed laterally, x 18. 8. Terminalia from above,
x 13. 9. Terminalia from below, x 13. 10. Terminalia from above after Navas, 1933,
Fig. 90.
Figures 5-9 prepared with constant reference to an ocular micrometer. Setae omitted
except in Figures 7 and 10.
a large oblique postero-ventral process (10RP,), the two ends of which are acute,
with a shallow distal concavity between. Inner margin of 10R produced forwards
to a process (10RP.), anteriorly separated from 10R by membraneous areas. Left
hemitergite (10L) smaller, inner margin produced back to a slender tapered process
(10LP), acute, curving outward distally. Right cercus composed of two sub-
cylindrical segments (RC,, RC.) ; cercus-basipodite (RCB) small. First segment of
left cereus (LC,) subeylindrical; inner margin produced near base to a forwardly-
BY CONSETT DAVIS. 495
directed echinulate lobe, broader than in L. hamifera. Second segment (LC.)
elongate-subcylindrical. Ninth sternite (H) produced backwards to a tapered
process (HP), between which and the base of LC, is the left cercus-basipodite
(LCB), embedded in membrane; LCB with a blunt flap directed upward near the
base of LC,, and with a terminal truncate portion adjacent to HP.
I publish without comment a tracing of the figure of Navas (l.c., Fig. 90), a
dorsal view of the terminalia of this specimen. 9 unknown.
Locality —Zambesia: Chemba, coll. I. Surcouf, Nov. 1928 (Mus. Paris).
Key to the Species of Leptembia (¢).
1. Echinulate lobe of first segment of left cercus subterminal ........ hamifera Krauss
Echinulate lobe of first segment of left cercus basal .............. surcoufi (Navas)
List of References.
ENDERLEIN, G., 1912.—Embiidinen, in Coll. zool. de Selys-Longchamps, fasc. 3.
Krauss, H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23 (Stuttgart).
NavAs, L., 1933.—Décadas de insectos nuevos. Década 23. Brotéria, Série trimestral,
Vol. 2, fase. 1.
496
ELEMENTARY HYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA.
By FRANK A. CRAFT, B.Sc.*
(Ten Text-figures. )
[Read 25th October, 1939.]
Introduction and Acknowledgements.—This paper is a preliminary attempt to
collect and evaluate some of the geographical facts disclosed by stream gauging
Statistics cover many of the largest rivers of the
region, and it is not anticipated that future information will affect the general
tenor of the conclusions reached herein.
The statistics employed were made available by the Hydrographic Branch
of the N.S.W. Water Conservation and Irrigation Commission. The writer’s thanks
are tendered to many of the officers of that. service, including Messrs. H. H. Dare
and G. Evatt (Commissioners), the late Mr. A. Morrison, and Messrs. V. T. England
and G. E. Robinson. The essentials of the paper were prepared in the University
of Sydney Department of Geography, which is under the direction of Professor
in south-eastern Australia.
J. Macdonald Holmes.
ed TASH T/T/
}
Text-fig. 1.—Locality map, with
key to stations enumerated in Table 1.
A number of stations have been
omitted because of shortness of record,
lack of continuity of record, or lack
of significance by comparison with
longer-established or higher-class
stations recording flows of similar
magnitude on the same river.
* This research was undertaken whilst the writer held a Linnean Macleay Fellowship
oy the Society in Geography.
BY F. A. CRAFT. 497
MEAN VOLUMES
Widths show
annual volumes
in millions of
acre feet
Text-fig. 2.—Map to show volumes discharged by the principal gauged streams,
Notice that many of the coastal streams have no significant gaugings, and are thus
represented by blank spaces.
Distribution of Flows and Catchments.
The principal facts are set out in Tables 1 and 2, and Text-figs. 2 and 3.
There is an apparent predominance of the south-eastern group of streams,
especially those flowing to the Murray. This is partly offset by the coastal rivers
Clarence and Fitzroy, and by the Macleay, Burdekin, Mary, and Burnet. Of the
latter group, the Macleay and Burdekin have not been gauged at all in their main
channels, and the others have only short records.. However, all except the Burdekin
are probably smaller, in average discharge, than those set out below (Table 2).
Attention is particularly drawn to the tremendous variations between maximum
00
498 ELEMENTARY TWYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA,
acre ft/sq.mile
2200
1000
600
400
200
100
50
29
7
de W.
ley arregzo
/ iS)
aS
i
ey,
a
Text-fig. 3—Map to show the distribution of the principal stream catchments, so far
as they are known. The inland limit of productive catchments is shown, whilst the
names inserted within this limit (Warrego, Balonne, ete.), with their enclosing lines, show
the approximate distribution of the main billabong and distributary areas.
and minimum annual totals, and the caution that must be used when discussing
matters on the basis of average values.
Although the greatest streams attain a fair average volume, this is mainly
due to the run-off from limited areas of headwater country. Many of the rivers
are only gauged low down on their courses, outside the main plateau zone, but in
every case where tributaries from the highlands are measured separately, they are
found to contribute a volume quite out of proportion to the ratio between their
catchment areas and those of the main streams. A few of the outstanding examples
are given (Table 3).
pe 1s Ne CNet, 499
In other words, we envisage a typical catchment of south-eastern Australia,
whether belonging to the coastal or Murray-Darling system, as consisting of a
limited area of headwater country with a high run-off, and a great area with a low
run-off. The catchments on which this paper is based cover rather more than
400,000 square miles, exclusive of the areic plains of the lower Darling. Of this
area, 12,600 square miles, or 3:-4% of the total, have a run-off greater than an
equivalent depth of 10 inches (25:4 cm.) per annum, and the proportion might
be considerably reduced if the upper Goulburn (Vic.), the Ovens and the Mitta
basins, aggregating 8,000 square miles, did not have to be included en bloc. The
portion with an equivalent annual depth of run-off greater than 3 inches is only
12:5% of the total considered.
In order to find why a few limited districts are so productive of water we
may consider the highest points in Australia, about Mt. Kosciusko, where the
Tooma and Swampy Plain (Murray system), and the Snowy and Tumut Rivers
rise. It has already been indicated that the district has a notable orographical
rainfall much in excess of that of the nearby valleys to the west, and of those
highlands slightly on the eastern or leeward side (Craft, 1934). It is also likely
that their summer evaporation is low, not only on account of altitude and lower
temperature, but also because of the daily formation of cloud due to local con-
vection. In the summer months, particularly on the hotter days, cumulus gathers
from 10 a.m. onwards, and by early afternoon it has covered 50% to 80% of the
sky, with a boundary sharply defined by the edge of the higher plateau (4,500
feet plus). Apart from thunderstorms, which help to keep the catchments moist,
this cloud has an obvious blanketing effect.
Similar conditions also apply to the Victorian heights at the heads of the
Mitta, Goulburn and Latrobe Rivers, and with other streams, such as the eastern
tributaries of the Shoalhaven, Wollondilly and Nepean Rivers, there is an almost
daily indraught of air in the warmer season. This affects the country to a
distance of 50 miles inland, and gives coolness, moisture, frequent mists on
the higher points, and much cloud.
Other convection centres occur at Gangerang (Blue Mountains), Moonbi
Ranges, Barrington Tops (Namoi-Hunter-Manning focus), and the Macleay-Dorrigo
and Nymboida scarps facing respectively eastward and northward on the north-
eastern coast of New South Wales. The phenomenon is, of course, well known
in tropical regions.
The foregoing are some of the more notable cases observed in the field, and
it is worthy of notice that all have considerable areas of swamp land, especially
those in the south-eastern highlands of the continent. In the more northerly
plateaus of New England and of eastern Queensland, the swamps tend to dry up
in their respective dry seasons, whilst in the isolated areas of higher run-off, like
the Nymboida (Clarence) and upper Brisbane valleys, the moist areas are mostly
in the rain-forests of slopes or scarps. Generally speaking, these latter cases appear
to be much less influenced by swamp or moist soil areas than those of the cooler
regions.
It is certain, from rain and stream records, that rainfall on the select areas
is higher than usual (cf. Text-fig. 3). This would probably be emphasized if
rainfall stations were not located consistently in valley settlements, to the exclusion
of the top country. It is also reasonable to suppose, as we have indicated, that
there is a lower evaporation in these major contributing places, giving an
additional reason for the existence of the swamps, and the effectiveness of the
500 ELEMENTARY ILTYDROGRAPITY OF SOUTH-EASTERN AUSTRALIA,
districts concerned for both high- and low-water run-off. The very presence of the
swamps must further tend to check evaporation and to conserve water.
Whilst we have definite information of the gathering grounds of the stream
water, the extent and nature of losses are very uncertain. Thus Balonne River—
the Queensland trunk stream of the Darling—appears to lose much of its water
by evaporation from swamps and distributaries before its “through” channel, the
Culgoa, joins the Barwon to form the name stream, Darling River. The Macquarie
and Lachlan both degenerate into many distributaries; 37% of the original volume
of the Lachlan passes Booligal, and only a portion of this finds its way to the
REGIMES
RELATIONSHIP
tuumn| Winter|Spring|SummerAutums
Maxima Minima
Text-fig. 4.—Regimes for the principal rivers of the region. Station numbers are
shown. Sach polygon contains 13 ordinates, from January to January. The ordinates
are percentages of yearly averages. The inset gives a summary of the types; for instance,
2a has summer and winter maxima, autumn minimum.
BY F. A. CRAFT. 501
Murray. The position is so well recognized that Lachlan water is excluded, as
inconsiderable, from River Murray agreements between the States and the
Commonwealth.
The main stream, Murray, appears to lose 20% of the water originally
contributed to it, the loss being estimated between the tributary gauges and the
confluence with the Darling. Streams like Wimmera, Paroo and Warrego, flowing
on the arid borderlands, do not contribute to the main rivers.
Stream Characteristics.
Regimes and their Classification.—The regimes disclose four principal stream
types, namely:
1. Queensland Type.—Summer maximum, low at other seasons, with
spring minimum.
2. Transition Type.—a. Barwon Subdivision; summer and winter maxima,
autumn minimum. 0b. Clarence Subdivision; summer and winter
maxima, spring minimum.
3. Sydney Coastal Type—Autumn or winter maximum, spring or early
summer minimum.
4. Victorian Type.—Winter or spring maximum, minimum in late summer
or autumn.
The letters ‘“a’ and “b” (Text-fig. 4) show the earlier and later incidence,
respectively, of phases in the northern and southern streams of the type.
This classification is brought out by the map (Text-fig. 4). The incidence of
maxima and minima for individual stations of types 1 and 4 is reasonably constant.
Thus the maximum flow of a river like the Murray is always found within
the range of the cooler season (Jun.—Nov.), with most occurrences in
September—October. Similarly, the maximum of a river like the Fitzroy always
occurs in summer. In contrast, the coastal streams of type 3 are likely to have
a maximum for a given year in almost any month. The Nepean and Shoalhaven
are characteristic: the regime laid down on averages is much less realistic than
with the other types, and is really a summation of chance storms.
The combination of summer and winter influences in the Transition type, 2,
is well shown by the Darling system, but it is not a constant factor (Text-fig. 5).
The Barwon at Walgett is dominated by winter flow in years above the average,
but summer flow is a little greater than winter in minimal years. With the
Namoi, the winter flow is the greater under all conditions, but the two rivers have
this much in common—summer flow varies much less than winter fiow. In this
area of approximately equal average rainfall at all seasons, the winter rain for
run-off comes mainly in 37% to 38% of the seasons. Summer run-off is, however,
more widely distributed in time.
In general, the only notable difference between the incidence of a rainy
season, on one hand, and major flow, on the other, is found in the south. Here
a prolongation of the winter rains into September and October gives a later
maximum flow than is shown elsewhere in the Victorian type. The effect of
melting snow trom the hills over 5,000 feet is a minor factor, and it does not
give the double maximum usually found under such conditions of climate. This
will be readily understood when the small area of appreciable snow storage is
remembered; this amounts to something of the order of 500 square miles, at
most, for the whole of south-eastern Australia, split up amongst a number of
rivers. This estimate excludes the forest country intermittently covered with snow
502 ELEMENTARY HYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA,
Bar won
2
e 3
on
Sa)
J
x
wo
g 4
en
Each division
Text-fig. 5.—Partial regimes for the transition rivers. In each case, the upper curve
is the regime for years above their annual average; the lower curve represents the
balance. Summer flows tend to predominate in a majority of years, but strong winter
influences in a minority of years give the observed higher winter maximum. Periods:
1.—above average, 15 years; below average, 26 years; 2.—above, 17 years; below, 28
years: 3.—above, 14 years; below, 385 years. Stations are: Barwon, 2; Darling, 15;
Namoi, 60 on Key.
in winter to a depth of a foot or more, liable to complete melting and replace-
ment within the winter itself. (See also Craft, 1934, 316, 317, 324).
In the warmer regions of more inconstant flow, the streams depend on the
greater rainstorms for their volume. Failure of these storms, even without
temporarily arid or drought conditions, will give a season of minimal flows. This
is very marked on the Queensland coast, where the large drainage areas give
enhanced flows. The Fitzroy has already been quoted in this regard, and a
comparison of its greatest and least flows with those of the Murray is instructive
(Table 2).
All told, the averages and diagrams based on them give a fair indication of
discharges and regimes for the south-eastern streams, but they should not be
relied on beyond a certain point for northern New South Wales, and for the whole
of Queensland. :
Variability of Flow.
The tables of figures give some idea of the differences met in the annual
totals of the various stations, and they lead to the consideration of the relative
importance of extremely low and high flows in stream economy. Some con-
sideration of seasonal and annual variability may be added.
Extremes of Flow.—Flows of exceptionally great magnitude were examined
on a monthly basis, the figure of 200% of the monthly mean being chosen rather
arbitrarily as the lower limit. That is, if the mean for a given month at a
given station were 100 units, and an individual record for that month was 205
BY EF. A. CRANT. 503
units, the whole 205 would be credited as an exceptional flow for that month. This
was done because the size of each average is largely determined by the greater
flows, which are few in actual number, and are usually well above the 200%
limit. On the other hand, the usual totals were considerably below the average.
Quartile and octile groupings were tried before the arbitrary figure was adopted,
but without success.
Having obtained all the exceptional flows for one month, the next month was
treated in a similar manner, and finally the twelve monthly totals were added
together. The gross figure thus obtained was expressed as the percentage of
the total flow of water recorded at the station for the whole period of gauging.
Thus a figure of 58% for the Warragamba indicates that 58% of the total water
recorded as passing that station did so in months 100% or more above their
respective monthly averages.
It was found that stations located at different points on the same river gave
very similar results, and that three distinct groupings appeared, namely:
a,—Streams of the south-eastern highlands, which owe a comparatively small
proportion of their totals to exceptional flows, the Murrumbidgee being the
northern limit of the type; b,—Streams of the central coastal region, between
Brisbane and Sydney, owe more than half their volumes to exceptional flows;
c,—Streams rising in the lower and drier highlands, or in the cyclonic storm
areas of the eastern coast of Queensland, owe the greater part of their flow to
exceptional months. The outstanding records are as follows (see also Text-fig. 6):
Percentages of Total Volumes due to months of Excessive Flow (more than 200%
of monthly means).
Group 1—less than 50%.—Uatrobe 8; Yarra 12; Snowy (Jindabyne) 18;
Murray (Albury) 20; Tumut 22; Mitchell, Ovens, ea. 25; Murrumbidgee
(Gundagai) 32; Glenelg (Sandford) 40.
Group 2—50% to 60%.—Clarence (Newbold-Gorge) 53; Brisbane (Lowood)
57; Yass 57; Warragamba 58; Hunter (Singleton) 59.
Group 3—more than 60%.—Namoi (Narrabri) 62; Shoalhaven (Welcome
Reefs) 62; Lachlan (Cowra) 63; Nepean (Penrith) 63; Macquarie (Dubbo) 64;
Barwon (Walgett) 65; Peel (Bowling Alley) 66; Darling (Menindie) 67; Fitzroy
(Wattlebank) 70; Colo 71; Lockyer Creek 76; Dawson (Taroom) 81.
A calculation was also made for exceptionally low recordings. In this case,
the amount of water passing does not have a great effect on the total, but the
number of months subject to minimal flow is of great importance, especially from
the economic standpoint. It was found that groups of very low recordings occur
at many stations, and the actual number less than 20% of their respective monthly
means was determined, and expressed as a percentage of the total number of
months for which readings have actually been made. Thus a figure of 10% for
the Mitchell indicates that 10% of months have recordings less than 20% of their
respective monthly averages. (Text-fig. 7.) ‘
Percentages of Months of Exceptionally Low Flow (less than 20% of means).
Group 1—less than 10% .—Uatrobe 0; Yarra 0; Snowy (Jindabyne) 1; Murray
(Albury) 1; Tumut 3; Ovens 8; Murrumbidgee (Gundagai) 8; Mitchell 10.
Group 2—20% to 40%.—Clarence 22; Hunter (Singleton) 27; Shoalhaven
(Welcome Reefs) 28; Brisbane (Lowood) 30; Warragamba 30; Glenelg (Sandford)
31: Namoi (Narrabri) 33; Lockyer Creek 33; Barwon (Walgett) 34; Nepean
(Penrith) 36.
504 ELEMENTARY HYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA,
MAXIMA Wha. MINIMA
7/7 /\ 62-81 Lu Me 77 /\4\ -81
TIT I]} 53-59 YN, Av} TMIfT 22-36
O-10
————s}
Text-fig. 6—Dependence of streams for volume on maximum flows. All flows over
200% of their monthly means were totalled, and the complete total thus obtained was
expressed as a percentage of the gross volume measured for the stream in the whole of its
record. In the first group, 62% to 81% of the gross flow was due to these individual
exceptional flows; in the second, 53% to 59%; in the third, 40% down to 8%.
Text-fig. 7W—Percentages of months with flows less than 20% of their respective
means. A figure of “10’’ shows that only 1 month out of 10 (= 10%) fell below the
mean for the month of record. Notice the close correspondence with Text-fig. 6. The
south-eastern rivers have few exceptionally low months; the inland and north-western
have many—up to four-fifths of the total number of months recorded.
Group 38—more than 40%.—Lachlan (Cowra) 41; Macquarie (Dubbo) 41;
Peel (Bowling Alley) 42; Colo 44; Darling (Menindie) 44; Fitzroy (Wattlebank)
70; Dawson (Taroom) 81.
These figures show conclusively that streams which rely on exceptional flows
to build up their monthly averages also have a large number of months which
contribute little to the discharge volume. There is a clear difference, on both
counts, between the south-eastern group and the remainder. Of that balance, the
rivers in the warmer northern section have the greatest number of months of
exceptionally low flows, and a high percentage of water derived from those of the
greatest magnitude.
In all this discussion the topographical factor should not be forgotten. Group 1,
in each of the above sets of figures, is associated with the highest of the plateau
country, but others of the higher and more abrupt plateaus also have a favourable
influence on stream discharges. This is brought out by the map of annual
variability.
Annual Variability (Text-fig. §)—This was calculated as percentage of varia-
4 are % : Standard Deviation
tion, according to the formula: Coefficient of Variation = ———————_——_——— x 100%.
Mean
When the probable error in calculating S.D. was greater than 15% of the S.D.,
BY F. A. CRAFT. 505
the result was discarded. In general, a 12-year record was the minimum necessary
to give a figure within the limit imposed. The accepted values are given in
Table 1.
In broad outlines, the map corresponds with the facts obtained by the study
of exceptional flows. The south-eastern rivers are the least variable, and are
followed by some members of the east coastal group, in country easily penetrated
by the inward drift of moist air from the eastern coast.
/
Witt kee
{if
ALLEL
VARIABILITY ! iy
RIVER im i]
119 Rainfall “Reliability |
after J. Andrews
PPT
40 Phtd daa
35
oft
IVE
(/
\ oS
35 Cann
emer Tl
eae a
ca
Pritikin
ns
PITEEL LWW
ns a
Vdeermgp prt
il Nf
Text-fig. 8.—Coefficients of variation for recorded catchments. The lowest figures
indicate the least variability, and the highest show the greatest variability. The value
of average figures varies accordingly, being greatest when variability is least. For
rainfall, the higher the figure attached to the isolines, the greater the “reliability” of
rainfall. In the south, there is a general correspondence between variations of rain
and river: in the north, it is probable that rivers depend more on concentration than on
erude amount of rainfall.
506 ELEMENTARY HYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA,
A zone of high variability extends along a NW-SE line from the Lachlan valley
to the Shoalhaven, recalling, in a shadowy manner, the southern Andes
(de Martonne, 1927). This feature is probably due, in part, to the occurrence
of lower and gentler topography here, associated with the northern limit of the
most constant and effective winter rains. At the same time, the south-eastern
highlands have a screening effect in winter, and there is a considerable flow of
descending air from the south-west. Towards the north, also, a similar feature
is repeated in the Queensland border country, to the north of New England
Plateau. In that case, the streams involved are Condamine River and Lockyer
Creek.
It is interesting to compare stream variability with rainfall ‘reliability’.
Using modal values, which exclude exceptionally low and high records, Andrews
(1932) obtained a map of which some details have been reproduced here (Text-
fig. 8). It will be realized, of course, that the river stations represent flows from
5000 cusec
intervals
Text-fig. 9.—Types of flood curves, drawn from daily discharges. 1 (Station 54,
Murrumbidgee, Aug.-Oct., 1916) shows two “flash’’ floods due to separate periods of
concentrated rainfall. 2 (Station 50, Murray, June-Oct., 1931) shows the most severe
flood phase recorded for that station; one major period of rain was experienced to give
a symmetrical curve. 3 (Station 50, July-Oct., 1917) gives a saw-toothed curve due to
heavy rainfall experienced at repeated intervals, and giving the greatest seasonal flow
recorded for the station. 4 (Station 15, Darling, Sept.-Dec., 1931) demonstrates the slow
rise and fall of a river of low gradient, derived from vast areas of country, with natural
equalizers in the form of distributary ‘deltas’. 5 (Station 79, Warragamba, May-June,
1930) shows ‘‘flash’”’ floods, one of extreme type, derived from a compact, relatively small
catchment in a period of heavy general rainfall.
BY F. A. CRAFT. 507
the higher, more rugged, and less settled country rather than the lower lands,
whilst the rainfall stations are located in valleys or on plains. For this reason,
the writer believes that rainfall “reliability” isolines for the south-eastern
highlands cannot be accurately drawn. A similar condition, of affairs might well
prevail for much of the Main Divide highlands.
On the whole, however, there are marked correspondences between the two
sets of values. Both show less variable conditions in the south-east than elsewhere;
both emphasize the NW-SE area of greater variability which has been described
above, with differentiation along the line of the highlands proceeding northwards.
In this respect they vary from Taylor’s earlier map of rainfall “reliability”, based
on departures from the average, which gives isolines concentric about the centre
of the continent. On the basis of what has been disclosed above, respecting the
distribution of exceptionally low and high flows, it will be agreed that Andrews’
map, empirical though it is, gives a more realistic picture than Taylor’s (1920).
Variation of Streams with Rainfall—The “station profiles’ are continuous
curves showing the height of the river at a particular station for each day. If
translated into terms of volume by reference to station rating curves, the quick
rise and fall which they show become still more apparent (Text-fig. 9). The
small portions published give some idea of conditions met.
With regard to the seasonal aspect, the writer made an investigation of
conditions on the upper Murray which, as we have seen, is one of the most constant
of the rivers, as well as one of the largest. For the Jingellic and Albury gauging
stations, there was a positive correlation between winter (May—October) rainfall
and winter flow (June—November), taking the actual totals of precipitation and
rainfall in each case. This correlation varied from 0-78 to 0-86, + 0-03 to 0-04,
with a period of 42 years for Jingellic and 55 years for Albury (1935, 131). (See
also Text-fig. 10.)
For the upper Murray catchments, then, the volume of rainfall is the main
factor determining winter flow. It must be borne in mind that the greatest’ run-off
takes place from alpine or forested areas, and that conditions are as normal as
they can be in the region. For the storage of snow, it corrects itself within the
season, thus causing no error of any consequence in the correlation.
In fact, there can be little delayed run-off, or carry-over from winter to
summer, and if such a conclusion is reached for a river ‘like the upper Murray,
it can hardly be departed from in the cases of the less constant rivers with lesser
facilities for water storage in the shape of swamp, marsh, or other moist soil
areas.
It should also be remarked that the station profiles establish this conclusion
independently. The quick rise to a crest, and the rapid fall from it for individual
rises or “freshes” show that there is little delayed run-off. In the cooler lands,
the seasons with monthly totals above the average (and, indeed, those below the
average, too) owe these to a whole series of “freshes’, separated by phases of
lower levels and smaller flows. The only divergences from this rule occur at those
rare times when there are closely-spaced rainstorms extending over a period of
weeks, or even months. In this respect, the major floods and inundations of the
River Murray are worthy of special notice. Relatively high levels have been
maintained at such times by exceptional incidence of rain. (Text-fig. 9, 3.)
In this cooler region, with its greater “reliability” of rainfall, exceptionally
humid periods are long, extending over a number of seasons: the group of years
1916 to 1918 is a case in point. On the other hand, invasions of semi-arid
508 ELEMENTARY HYDROGRAPHY OF SOUTH-EASTERN AUSTRALIA,
conditions are rare, but they may persist even through the winter season, as in
1902.
In the warmer regions, the exceptionally high flows are produced by severe
storms of limited duration, and the succeeding periods of low water are more
emphatic and prolonged than those in the more constant south. For example, the
first three months of 1917 showed the Fitzroy discharging 5,623; 2,558; and 3,560
units (x 10% acre feet) respectively. The discharge for April was only 81 units, and
the next four months were also below their respective averages.
tunit river = 10° ac.ft.
1 + rain —o-oinch
Text-fig. 10.—la shows the Murray at Albury in 1917. and rainfall at Batlow in the
Same year; 1b treats the same group in 1902. 2a shows the Brisbane River at Lowood,
and Esk rainfall station, in the middle valley of the river, for 1926-27; 2b is for the
same group in 1922-23. Note the logarithmic scale of the ordinates. There is,a general
similarity between rainfall and river curves, which appear to keep closer together in the
south. This is a suggestion pointing to future research.
The variations of flow in this warm country produced by varying intensities
of rainfall are suggested by Text-fig. 10, parts 2a, b. The rainfall station chosen—
Esk—in the middle Brisbane valley, has a record similar to those of other rain-
recording points of the catchment, and might be expected to be representative.
The periods of maximum and minimum river flow recorded were chosen, and the
corresponding rainfall curves drawn to match them. With (a), a rainfall of 49
inches was enough to give a river flow of 2,085,000 acre feet; with (b), a rainfall
of 32 inches gave a mere 80,000 acre feet, or 3-8% of the other. Such differences
BY F. A. CRAFT. 509
might appear fantastic if they were not discernible in all the rain and river
statistics of the summer rainfall type.
The portion of the run-off which is delayed by storage in the catchments is
used to supply the drought flow of streams, and is thus economically important,
even although it is small. There is no indication that it forms a considerable
fraction of the normal low-water flow—that is, in times when there is the usual
rainfall. It has been indicated that this is the case even in the cooler and higher
districts.
As an example, the Snowy at Jindabyne shows a tendency to decrease to a
volume of 5,000 to 6,000 acre-feet per month after two consecutive drought months
(rainfall less than 0-5 inch per month as shown by each of the three nearest
rainfall stations). This flow represents a depth of 0:13 to 0:16 inch for the
catchment involved, so that delayed run-off from this productive catchment is by
no means great. It must be noted that two successive drought months are a rarity
here, there is much cloud, and there are considerable areas of Swamp and moist
soil.
A sound conclusion appears to be that very little of the water which finds
its way into streams is delayed for any considerable time in the catchments—
say, for a period of a month or more.
References.
ANDREWS, J., 1932.—Rainfall Reliability in Australia. Proc. LINN. Soc. N.S.W., lIvii, 95.
CraFrt, F. A., 1934.—Regimes and Cyclical Volume Changes of the upper Murray and
Snowy Rivers, N.S.W. Proc. Linn. Soc. N.S.W., lix, 314.
, 1935.—The Relationship between Erosion and Hydrographic Changes in the
Upper Murray Catchment, N.S.W. Proc. LINN. Soc. N.S.W., Ix, 121.
MARTONNE, E. bE, 1927.—Regions of Interior-Basin Drainage. Geog. Rev., xvii, 397.
TAYLOR, GRIFFITH, 1920.—Australian Meteorology, Oxford.
TABLE 1.
Principal statistical details for the rivers of south-eastern Australia, showing lengths of records, areas of catchments,
run-off in acre feet per sq. mile (see also table on teat-fig. 3), mean run-off, and coefficient of variation, omitting
doubtful cases.
Notes.—x1, ana-branch of Murray, which rejoins the main river ; x2, excluding 1918, a year of high flow ;
x3, too low, cf. No. 61; x4, minor regulation by water supply dams, which now intercept a greater proportion
of flow ; x5, for comparison of flow and variability ; x6, principal Lachlan distributary ; x7, cross stream,
Murrumbidgee to Murray.
Flow.
Record. Catchment. Var.
“No. River and Station. ——_—__——— §q. miles. Per %
Start. Years. Acre feet. sq. m.
1 Avoca, Coonooer. . 33 ws 1890 35 1,029 63,000 61 80
2 Barwon, Walgett Ee hs 1886 45 53,500 1,122,000 21 78
3 Bell, Wellington oe be 1913 21 710 72,000 101 100
4 Belubula, Canowindra .. ate 1909 25 816 112,000 Nz 95
® Billabong, Cocketgedong a 1916 15 — 54,500 — 112
6 Brisbane, Lowood Ac D0 1910 22 3,950 655,000 166 81
i Broken, Goorambat si te 1887 47 . 730 223,000 306 95
8 Campaspe, Rochester .. Be 1886 48 1,350 208,000 154 —
9 Chichester, Dam ae aS 1913 14 76 130,000 1,710 —_—
10 Clarence, Tabulam ae ae 1917 16 1,724 526,000 305 89
11 an Gorge-Newbold he 1917 16 6,674 2,143,000 321 77
12 Colo, Upper Colo Ae A 1910 23 1,680 338,000 202 79
13 Condamine, Chinchilla .. wa 1925 7 7,366 177,000 24 —_—
14 Corang, Hockey’s an a 1925 9 — 42,000 — —
ELEMENTARY TWYDROGRAPHY
River and Station.
oo Nn ee
on
bo bo bb bo bo bo
rag
for)
eonoc,n
or ot Or Or Or Or ot
NO ork WN ©
or ¢
Darling, Menindie
Dawson, Taroom
Glebe
Dumaresq, Riverton
Edward, Deniliquin x1
Fitzroy, Wattlebank x2
Glenelg, Sandford
Goodradigbee, Brindabella
3 Wee Jasper
Goulburn, Murchison (Vic.)
Goulburn, Rosemount (N.S.W.)
Hawkesbury and Tributaries—
Short Records—
Hawkesbury, Richmond x3
Cox, Cedar Vale ,
Nepean, Pheasant’s Nest
> Wallacia x4
Wollondilly, Burragorang
Hunter, Moonan Flat
5 Muswellbrook ..
5 Singleton
Indi, Bringenbrong
Kiewa, Kiewa
Lachlan, Wyangala
+5 Cowra ..
55 Forbes . .
a6 Booligal
Latrobe, Rosedale
Lockyer, Tarampa
Loddon, Bridgewater
Macalister, Maffra
Macintyre, Boggabilla
Macquarie, Wellington
a Dubbo
5 Warren
Mitchell, Bairnsdale
Mitta, Tallangatta
Molonglo, Yarralumla
Mongarlowe, Charleyong
Murray, Bringenbrong ..
3 Jingellic
5 Albury
op Barham. .
a Mildura ; a3
Murrumbidgee, Cotter Junction
a Gundagai
5 Wagga
5 Hay
oh Balranald
Namoi, Old Cuerindi
35 Gunnedah
Narrabri
Nepean, Penrith
Nymboida, Bueearumbi
Ovens, Wangaratta
Peel, Bowling Alley
OF
SOUTH-EASTERN
TABLE 1.—Continued.
AUSTRALIA,
Record. Catchment.
Sq. miles.
Start. Years.
1885 49 221,675
1911 21 6,100
1924 8 8,500
1920 13 2,000
1898 36 —
1915 16 53,286
1900 20 3,300
1919 12 _—
1915 19 443
1882 52 3,966
1907 12 3,100
1926 5 4,600
1927 6 1,040
1924 10 274
1924 10 —
1926 7 1,813
1912 22 290
1907 27 1,630
1898 36 6,580
1908 13 493
1886 48 434
1920 14 3,200
1893 41 4,470
1893 41 7,550
1909 25 =
1901 19 1,475
1910 22 965
1882 52 1,856
1901 9 850
1925 8 9,050
1909 25 5,482
1886 48 7,690
1902 31
1890 32 1,770
1886 48 5990
1927 7 700
1925 8 —
1906 15 820
1891 42 2,520
1877 57 6,500
1905 29 —_
1877 56 92,000
1927 Gi 2,660
1887 46 8,400
1885 49 10,700
1887 47 17,520
1887 47 _
1916 17 940
1912 21 6,600
1892 41 9,800
1892 42 4,240
1922 11 1,888
1887 47 2,090
1916 17 130
Flow.
Acre feet.
2,386,000
328,000
540,000
215,000
1,570,000
3,450,000
599,000
116,000
315,000
2,384,000
134,000
925,000
314,000
154,000
219,000
320,000
92,000
310,000
685,000
442,000
554,000
519,000
540,000
577,000
215,000
693,000
66,000
201,000
292,000
474,000
605,000
710,000
574,000
686,000
1,079,000
51,000
81,000
1,140,000
1,897,000
3,657,000
4,126,000
8,095,000
486,000
2.723.000
2,830,000
2,239,000
2,133,000
182,000
431,000
517,000
958.000
969,000
1,191.000
66,000
BY F. A. CRAFT. Bilt
TABLE 1.—Continued.
Flow.
Record. Catchment. ———————————————___ FVar.
No. River and Station. ——___—_—_—_————._ §q. miles. Per Of
Start. Years. Acre feet. Sq. m.
65 Peel, Carroll Gap sys ets 1924 8 1,800 116,000 64 —
66 Shoalhaven, Warri at atc 1915 i 572 192,000 335 119
67 a Welcome Reefs .. 1910 22 1,066 ~ 352,000 330 106
68 Snowy, Jindabyne A se 1903 31 716 951,000 1,330 32
69 aa Orbost .. 5 Ae 1907 18 5,210 1,749,000 336 36
70 Stanley, Silverton BG Pe 1916 16 515 465,000 902 80
7k Swampy Plain, Indi... ae 1906 8 320 616,000 1,926 —
72 Ag as Khancoban .. 1927 7 228 436,000 1,912 —
73 Tambo, Bruthen ne Age 1906 19 1,040 212,000 204 62
74 Thames (England) x5 ye 1904 28 — 2,120.000 — 29
75 Thomson, Heyfield ag ate 1901 21 550 323,000 587 34
76 Tooma, Warbrook Ns a 1910 11 713 634,000 888 —
77 a5 Possum Point .. af 1927 7 189 415,000 2,200 —
78 Tumut, Tumut .. Aes Sve 1905 29 980 1,017,000 1,036 46
79 Warragamba, Nepean J. ae 1904 30 3,383 590,000 174 58
80 Willandra, Tocabil x6 .. a6 1921 13 — 113,000 — oo
81 Wimmera, Horsham wie os 1889 36 1,530 144,000 94 88
82 Yanko Ck., Offtake x7 ie 1902 26 — 205,000 — 89
83 Yarra, Warrandyte ma Si 1892 33 972 740,000 17 31
84 Yarrangobilly, Caves... x3 1911 20 _ 51,000 — 49
85 Yass, Yass Bee e: ef 1916 17 500 67,000 134 —
TABLE 2.
to
Largest streams gauged in Australia. Compare Text-fig.
Annual Flows.
Station Catchment Record Acre feet X 10°.
No. River. (Sq. mls.) Years.
Mean. Max. Min.
52 Murray in aie Ae 92.000 56 8.095 _ 24,452 1,320
20 Fitzroy .. ae a8 53.286 16 3.450 13,301 137
55 Murrumbidgee fe 50 10,700 49 2.830 7,712 384
15 Darling ae as oe 221,675 49 2.386 11,107 1
24 Goulburn .. See SA 3,966 52 2.384 6,202 567
11 Clarence .. te ns 6.674 16 2,143 6.066 532
69 Snowy a3 sve 0 5,210 18 1.749 2,972 776
63 Ovens ys Bis Ses 2,090 47 1,191 4.023 141
2 Barwon oe5 a a 53,500 45 emi 22: 3,866 16
45 Mitta Ae oO 60 1,990 48 1,079 3.370 238
78 Tumut wy Be Ae 980 29 1,017 2,387 283
61 Nepean he ite é0 4,240 42 958 2,947 67
512 ELEMENTARY HYDROGRAPHY OF SOUTILT-EASTERN AUSTRALIA,
TABLE 3.
Comparison of certain main stream catchments (including all headwaters) with gauged headwaters. Note the especial
productiveness of limited areas of the highlands.
Depth of Run-off.
Station River. Area. ———— —_—— ———
No. (Sq. miles.) Inches. Cm.
50 Murray .. an ne i sis 6,500 10°5 PAS'7/
30 Indi ss ste oF is ae 495 16°8 42-6
31 Kiewa ais ok we sia ee 454 23°9 60°7
io Swampy Plain .. ats a te 228 35°8 91-0
Ud Tooma te ee a'b te ns 189 41-0 104°2
54 Murrumbidgee .. ik as tee 8,400 6-1 15-5
23 Goodradigbee Be es te an 443 113983 33°38
78 Tumut a ae pie Re sts 980 19-3 49-0
69 Snowy Lf; shi Pe ats a 5.210 6°3 16:0
68 Snowy a is ia: ye Ee 716 24-9 63°3
29 Hunter .. vi; A ae 33 6.580 1:9 4°8
25 Hunter .. a eo Ae ee 290 6:0 15:2
59 Namoi vie ats te a Be 6,600 110%) oli
64 Peel a ele ahs 60 he 130 5 24-1
513
STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES.
By T. Harvey JOHNSTON and Patricia M. Mawson, University of Adelaide.
(Sixty-six Text-figures. )
[Read 25th October, 1939.1
The present communication is the fifth of a series dealing with the nematode
parasites of Australian marsupials, the earlier papers giving accounts based
largely on material from Queensland and Central Australia.
Twenty-five species are proposed as new and are distributed amongst eleven
genera, three of which (Cyclostrongylus, Parazoniolaimus, and Maplestonema) are
new.
Types of new species described in this report are deposited in the South
Australian Museum, Adelaide.
This investigation has been made possible by the Commonwealth Research
Grant to the University of Adelaide. We desire to acknowledge assistance in
regard to material from Professor J. B. Cleland; Messrs. L. Gallard, Narara;
A. S. Le Souef, Director, Sydney Zoological Gardens; and W. L. Rait, Adelaide.
Much of the material was collected by the senior author between 1908 and 1911
during his residence in New South Wales. The locality quoted as Lower Hawkes-
bury is in the vicinity of Milson Island and the township of Hawkesbury River.
List of Hosts and Parasites dealt with in this Paper.
Macropus rurus Desm.: Pharyngostrongylus alpha J. & M.; Zoniolaimus longi-
spicularis (Wood); Cloacina magnipapillata, n. sp.; C. longispiculata J. & M.
Macropus MAgor Shaw: Pharyngostrongylus alpha J. & M.; P. beta J. & M.;
Zoniolaimus longispicularis (Wood); Zoniolaimus sp.; Cloacina obtusa, n. sp.;
C. expansa, n. sp.; C. magnipapillata, n. sp.; Cyclostrongylus clelandi, n. gen., n. sp.
Macropus rospustus Gould: Pharyngostrongylus alpha J. & M.
MAcROPUS UALABATUS Less. & Garn.: Pharyngostrongylus alpha J. & M.: P. beta
J. & M.; P. epsilon J. & M.; Zoniolaimus ualabatus, n. sp.; Z. clelandi, n. sp.;
Z. setifer Cobb; Z. brevicaudatus Cobb; Parazoniolaimus collaris, n. gen., n. sp.;
Cloacina macropodis J. & M.; C. wallabiae, n. sp.; Cloacina sp.; Macropostrongylus
dissimilis, n. sp.; Cyclostrongylus wallabiae, n. gen., n. sp.; Cyclostrongylus
dissimilis, n. gen., n. sp.; Maplestonema typicum, n. gen., n. sp.
MACROPUS RUFICOLLIS Desm.: Pharyngostrongylus alpha J. & M.; P. beta J.& M.:
P. delta J. & M.; P. epsilon J. & M.; P. zeta J. & M.; P. eta J. & M.; P. brevis
Canavan; P. iota, n. sp.; P. macropodis Y. & M.; Macropostrongylus lesouefi, n. sp.;
M. wallabiae, n. sp.; Zoniolaimus communis J. & M.; Z. onychogale J. & M.;
Zoniolaimus sp.; Buccostrongylus australis J. & M.; Buccostrongylus setifer, n. sp.;
B. labiatus, n. sp.; Cyclostrongylus gallardi, n. gen., n. sp.; Austrostrongylus
wallabiae, n. sp.
Macropus PARMA Waterhouse: Pharyngostrongylus epsilon J. & M.; P. parma,
n. sp.
PP
514 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
MAcROPUS THETIDIS Lesson: Pharyngostrongylus alpha J. & M.; P. delta J. & M.;
P. epsilon J. & M.; P. zeta J. & M.; P. theta, n. sp.; Zoniolaimus sp.; Cloacina
bancroftorum J. & M.; C. similis J. & M.; C. thetidis, n. sp.; Cloacina sp.; Bucco-
strongylus buccalis J. & M.; Globocephaloides thetidis, n. sp.; Hypodontus thetidis,
Nn. sp.
TRICHOSURUS CANINUS Ogilby: Asymmetricostrongylus trichosuri, nN. sp.
PHARYNGOSTRONGYLUS Yorke & Maplestone.
The original species, P. macropodis, was described by Yorke and Maplestone in
1926. Monnig in the same year described australis, attributing it to a preoccupied
genus Spirostrongylus, but transferred it in 1927 to Rugopharynz which was shown
by Wood (1929) to be a synonym of Pharyngostrongylus. This latter author
described P. woodwardi in 1930. Canavan in 1931 added P. brevis. We described
two others in 1938 and recently added four more (1939). In the present report
three others are described and host records relating to nine of the known species
are mentioned.
PHARYNGOSTRONGYLUS THETA, nN. Sp. Figs. 1-2.
From stomach, Macropus thetidis, New England.
Male 4:8; female 4:5 mm. Head with six small papillae; buccal cavity 9u
long; followed by transversely striated chitinized vestibule 0-04 mm. long, 8yu
internal and 14u external diameter, with wall becoming narrowed suddenly just
before joining oesophagus. Oesophagus 0:56 mm. long, anterior part 0-37 mm.,
followed by a narrower portion around beginning of which is nerve ring, posterior
region widening into bulb before joining intestine. Cervical papillae not observed.
Excretory pore at level of nerve ring.
Male: Bursa with ventral lobes very small and separated from each other as
well as from lateral lobes; lateral and dorsal lobes continuous, dorsal longer.
Ventral rays parallel, cleft nearly to base; not reaching edge of bursa; externo-
lateral shorter than, and slightly divergent from, laterals; laterals reaching edge
of bursa, cleft three-quarters of their length; externo-dorsal long, thin, arising
from same root as laterals, diverging from them, not reaching edge of bursa;
externo-lateral, laterals and externo-dorsal each elevate bursa into slight papilla
at their termination. Dorsal ray long, bifurcating just before its mid-length, each
of the two slender branches reaching bursal edge and giving off a very short
lateral ray at about mid-length. Spicules 1:9 mm. long, half of body length, stout,
with striated alae extending nearly to tips. Gubernaculum present, 404 long; with
a pair of less chitinized leaf-like alae extending alongside the spicules.
Female: Body tapering suddenly behind vulva and again behind anus; tail
pointed, 0-2 mm. long, ventrally directed; vagina muscular, 0°35 mm. long; vulva
0:13 mm. in front of anus; ripe eggs not seen.
The species differs from P. australis in its shorter length, the form of the
vestibule, length of the externo-dorsal ray, width of the dorsal ray, absence of
median dorsal thickening of the bursa, relatively longer spicules, and the absence
of papillae on the bursa. It differs from P. brevis in its shorter length, absence of
leaf crown and cervical papillae, relatively shorter spicules, and in the relatively
larger narrower vestibule. It can be distinguished from P. alpha and P. beta by
the different dorsal ray, the form of the bursa (which is not deeply subdivided),
and the absence of bursal papillae.
PHARYNGOSTRONGYLUS IOTA, Nn. sp. Figs. 3-4.
From Macropus ruficollis, Ourimbah, Gosford district (L. Gallard).
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 515
About 9 mm. long. Head with external leaf-crown similar to that of P. gamma,
with six similar papillae. Vestibule 1 mm. long,
P. macropodis, and P. eta;
Posterior end of very narrow oesophagus
0-2 mm. wide; without striations.
obscured by granular material, hence length not determined.
Male: Spicules 2:9 mm. long, one-third of body length. Bursa deeply lobed,
papillated. Ventral rays cleft, not quite reaching edge of bursa; externo-lateral
divergent from laterals near tip and shorter than laterals; laterals extending nearly
=
Gittee| EGGequmenanscan
Te PCORBBRRRABECEt
Figs. 1-2, Pharyngostrongylus theta. 1. bursa of male; 2. head.
Figs. 3-4, P. iota. 3. dorsal ray of bursa; 4. anterior end.
Figs. 5-7, P. parma. 5. head; 6. bursa; 7. posterior end of female.
Figs. 2 and 5 to same scale; figs. 1, 3, 4, and 6.
Figs. 8-10, Cyclostrongylus wallabiae. 8. head; 9. anterior end; 10. bursa.
Figs. 11-13, C. gallardi. 11. head, lateral view; 12. posterior end of female; 13. bursa.
Figs. 8 and 11 to same scale; figs. 9 and 12.
2,
Ay
516 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
to edge; externo-dorsal stout, arising separately, not reaching bursal edge. Dorsal
ray bifurcating at half-length and its branches not quite reaching edge, each
branch giving off a short lateral ray at about mid-length.
Female: Vagina exceedingly long (1-4 mm.), wide, with very small eggs
(0:07 mm. by 0:04 mm.); vulva 0-85 mm. and anus 0-63 mm. from tip of tail; tail
long, tapering.
This form is very like P. macropodis, P. gamma and P. eta, differing from
them in the absence of striations on the vestibule and in general measurements.
It most closely resembles P. gamma, differing in having a relatively narrower
vestibule, a much longer vagina and a stouter dorsal ray whose lateral rays are
more robust and relatively shorter, and whose terminal branches are longer.
PHARYNGOSTRONGYLUS PARMA, Nn. Sp. Figs. 5-7.
From oesophagus, Macropus parma, Narara, Gosford district (L. Gallard).
Filiform worms, tightly rolled; male 7°3 mm. long; females 6-7—7-5 mm. Body
ending abruptly at anterior end and surmounted by six small papillae. Mouth
opening 10u in diameter; continuous with, and of same width as, buccal cavity
(14u deep) and vestibule. Posterior part of buccal cavity surrounded by thick
chitinous ring about 4u long; followed by vestibule 154 long, and with stout
chitinous walls 9u thick at anterior end, narrowing posteriorly and marked with
radial striations. Oesophagus 0:54 mm. long, of uniform width until suddenly
constricted near its posterior end and then widening into a terminal elongated
bulb; nerve ring surrounding it at level of constriction, 0-4 mm. from anterior end;
excretory pore near base of oesophagus.
Male: Bursa large, lobes not divided from one another. Owing to the close-
ness of the helix it is very difficult to roll the bursa into a position allowing the
dorsal ray to be seen in dorsal view. Ventral rays reaching edge of bursa; externo-
lateral ray stout, tapering at tip, not reaching edge; laterals cleft for half their
length, reaching edge of bursa; externo-dorsal arising separately, stout, tapering,
shorter than externo-lateral. Dorsal ray dividing near its base into two long
narrow branches reaching nearly to edge of bursa and each giving off near its
origin a short stout lateral branch. Spicules 0-96 mm. long, 1:7:-6 of body length;
narrow, with striated alae; tips curved, bluntly pointed.
Female: Posterior end tapering; tail bluntly pointed, 0-3 mm. long; vulva
0:15 mm. in front of anus; vagina fairly long, wide. Eggs in vagina 0:1 x 0:04 mm.
This species differs from other members of the genus Pharyngostrongylus
chiefly in its attenuate form and coiled habit, and in the structure of the vestibule.
PHARYNGOSTRONGYLUS ALPHA Johnston & Mawson 19388.
This parasite has been identified amongst collections taken from the following
hosts: Macropus rufus, from Wentworth (coll. W. L. Rait); M. major, Coonamble;
M. ualabatus, Lower Hawkesbury (coll. J. B. Cleland): M. rujficollis, Bathurst
district; M. thetidis, New England; and M. robustus (robustus), N.S.W. (coll.
A. S. Le Souef, Sydney Zoological Gardens).
PHARYNGOSTRONGYLUS BETA Johnston & Mawson 1938.
From Macropus udlabatus, Lower Hawkesbury (coll. J. 3B. Cleland);
M. ruficollis from Bathurst district, Ourimbah (Gosford district), and Sydney
Zoological Gardens; and M. major, Coonamble.
PHARYNGOSTRONGYLUS GAMMA Johnston & Mawson 1938.
From Macropus ruficollis, Bathurst district.
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 517
PHARYNGOSTRONGYLUS DELTA Johnston & Mawson 1938.
From Macropus ruficollis, Bathurst district, and from Sydney Zoological
Gardens; M. major, Narrabri; and M. thetidis, New England.
PHARYNGOSTRONGYLUS EPSILON Johnston & Mawson 1938.
From Macropus ualabatus, Lower Hawkesbury River; M. parma, Gosford
district; M. thetidis, New England; and M. rujficollis, Bathurst district.
PHARYNGOSTRONGYLUS ZETA Johnston & Mawson 1938.
From Macropus rujicollis, Bathurst district; and M. thetidis, New England.
PHARYNGOSTRONGYLUS ETA Johnston & Mawson 1938.
From Macropus rujicollis, Bathurst district.
PHARYNGOSTRONGYLUS BREVIS Canavan 1931. ‘
From Macropus rujicollis, Bathurst district; and M. ualabatus, Lower Hawkes-
bury district.
PHARYNGOSTRONGYLUS MACROPODIS Yorke & Maplestone 1926.
Specimens, probably belonging to this species, were taken from Macropus
rujicollis from Bathurst district.
CYCLOSTRONGYLUS, nN. gen.
Trichoneminae; with long buccal capsule, thick cuticular collar around mouth,
the inner surface of which is marked with parallel longitudinal striations
extending into the buccal cavity and resembling at first sight a leaf crown of
Many narrow elements; arising from this collar are four submedian and two
lateral papillae. Oesophagus varies in form in different species. Main stem of
dorsal ray soon bifurcates, each branch giving off a short lateral ray. Posterior
end of female resembles that in Cloacina. From stomach of marsupials. Type,
C. wallabiae, n. sp., from Macropus ualabatus.
The generic name is applied because of the circumoral cuticular ring or
collar. The genus differs from Coronostrongylus in the absence of a leaf crown;
and from Pharyngostrongylus in the shape of the bursa and in the absence of a
vestibule. We have assigned to this genus, in addition to the type, two species
C. clelandi and C. gallardi. A fourth species, C. dissimilis, has been placed here
provisionally, but it probably belongs elsewhere, its state of preservation preventing
us from giving a sufficientiy detailed account of it.
CYCLOSTRONGYLUS WALLABIAE, nN. sp. Figs. 8-10.
From Macropus ualabatus, Lower Hawkesbury (coll. J. ‘B. Cleland).
Worms of moderate size; male 8-5 mm. long; female 5-1 mm.; somewhat coiled.
Anterior end rounded, surmounted by wide thick mouth-collar, bearing four small
submedian papillae and a pair of small rounded laterals. Mouth opening round,
large, leading into a long cylindrical buccal chamber 0-04 mm. long, 0-15 mm.
internal diameter, with the walls about 7» thick anteriorly but diminishing
posteriorly; walls marked with transverse striations. At base of buccal cavity a
rather disc-like wider ring of chitin lying against anterior end of oesophagus.
Latter 0:07 mm. long in male, 1:11 of body length; wider than buccal capsule; and
consisting of two parts—the anterior portion longer and narrowing suddenly at
level of nerve ring, 0-55 mm. from head end of worm; the posterior part widening
to form a bulb. Excretory pore at 0-56 mm., just behind nerve ring; cervical
papillae not seen.
518 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
Male: Spicules short; 0-7 mm. long, 1:12 of body length; with very narrow
striated alae. Gubernaculum not observed. Ventral lobes of bursa short, separate
from one another; dorsal lobe with wide median cleft. Ventral rays long, cleft
nearly to base: externo-lateral, short, lifting wall of bursa; laterals cleft nearly
to base, reaching edge of bursa; externo-dorsal arising separately, nearly reaching
bursal edge. Dorsal ray long, bifurcating soon after origin; each branch tapering
and forming projection on edge of dorsal lobe, and giving off short lateral ray at
about mid-length.
Female: The only available specimen is rather unsatisfactory. Body tapering
suddenly behind region of vagina to end in long bluntly-pointed tail. Uteri parallel;
vagina short; vulva at 0:25 mm., and anus at 0-2 mm. from tip of tail. Hgg in
vagina 0-041 x 0:025 mm.
CYCLOSTRONGYLUS GALLARDI, n. sp. Figs. 11-13.
From Macropus ruficollis, Ourimbah, Gosford district (LL. Gallard).
Male 4-5 mm. long; female 5-6 mm. Head with characteristic cuticular collar
round anterior end, through which the hypodermis projects in six small rounded
papillae. Mouth small, circular, 10u diameter, leading to narrow buccal cavity,
17u long, followed by wide buccal capsule 30u long, 124 wide internally, 19u wide
externally. Striations of hypodermis (resembling a leaf crown) 7u deep and not
reaching top of buccal cavity. Oesophagus 0°53 mm. long, 1:8-11 of body length;
longer anterior region of uniform width, becoming constricted suddenly, then
widening into large spherical bulb before joining intestine. Nerve ring around
oesophageal constriction, 0-48 mm. from anterior end of worm; excretory pore
just in front of nerve ring; cervical papillae not observed.
Male: Spicules 1:9-2 mm., 1:2-4 of body length; slender; with wide striated
alae and blunt tips. Gubernaculum small. Bursa large, ventral part shorter than
dorsal; lobes all joined but marked off by shallow indentations. Ventral rays cleft
nearly all their length, reaching bursal margin; externo-lateral divergent from
laterals, extending nearly to edge; medio- and postero-lateral cleft for half their
length, a little shorter than externo-lateral; externo-dorsal arising separately and
not reaching edge of bursa. Dorsal ray bifurcating after about one-third to one-
quarter its length, each branch almost immediately giving off a very short lateral
ray before extending nearly to edge of dorsal lobe; these branches relatively long
and parallel.
Female: Body tapering gradually to posterior end; tail bluntly pointed,
straight, 0-3 mm. long. Vagina muscular, 0-4 mm. long; vulva 0:13 mm. in front
of anus. Eggs in vagina 0:08 x 0:04 mm.
This species differs from C. wallabiae in the different form of the buccal
capsule, papillae and dorsal ray of the bursa; from C. clelandi in regard to the
lips, bursal rays and the characters of the buccal capsule; and from C. dissimilis
in the form of the oesophagus and the dorsal ray. (
CYCLOSTRONGYLUS CLELANDI, hn. sp. Figs. 14-15.
From Macropus major, Coonamble (coll. A. S. Le Souef).
Slender worms, 10-11 mm. long, widest in anterior third, with fine annulate
cuticular striations. Head surrounded by large cuticular mouth collar through
which project four short cylindrical submedian and two very short lateral papillae.
Mouth large, circular; buccal cavity 0:065 mm. long, 0:05 mm. wide; with walls
marked by numerous longitudinal lines, at first sight suggesting a leaf crown of
numerous elements. Oesophageal region packed with granular material in all but
one specimen examined; oesophagus 1:7 mm. long in female, 1:6 of body length;
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 519
narrow; with small posterior bulb. Nerve ring, cervical papillae and excretory
pore not recognized.
Male: Spicules 1:7 mm. long, 1:6 of body length, stout, with wide striated
alae. Bursa large; ventral lobes joined, laterals separated from ventral and dorsal
by shallow indentations. Ventral rays long, parallel; externo-lateral long, only
slightly divergent from medio- and postero-laterals, all three of same length and
nearly reaching edge of bursa; externo-dorsal arising separately, long, thin.
Dorsal ray dividing before one-third length into two divergent branches, each
giving off a very short lateral ray just before its middle. Genital cone short;
accessory cone present.
Female: Body narrowing behind vulva to end in tapering pointed tail; vagina
short; vulva at 6-8 mm., anus at 3-8 mm. from tip of tail. No eggs were seen in
the only female found, which was immature, and about 11 mm. long.
CYCLOSTRONGYLUS DISSIMILIS, n. sp. Figs. 16-18.
From Macropus ualabatus, Milson Island, Lower Hawkesbury (J. B. Cleland).
Only one specimen, a damaged male, was found, but the unusual shape of the
oesophagus warrants the inclusion of a description of the worm which was 13-9 mm.
oSSmm
Figs. 14-15, Cyclostrongylus clelandi. 14. head; 15. bursa.
Figs. 16-18, C. dissimilis. 16. head; 17. oesophageal region; 18. bursa.
Figs. 19-22, Zoniolaimus setifer, enlarged from Cobb (1898, fig. 30). 19. lateral view
of head; 20. anterior view of head; 21. lateral view of anterior end; 22. posterior view
of bursa.
520 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
in length. Head very indistinct, with cuticle so swollen that it appears
asymmetrical. Only two short conical papillae observed. Mouth leads into a thin-
walled cylindrical buccal capsule, 0-015 by 0:02 mm., opening into oesophagus.
Latter 1 mm. long; 1:14 of body length; anterior half narrow and surrounded near
its posterior end by nerve ring, posterior half increasing in diameter so that it has
the form of a cone, with the base near the intestine. Excretory pore in vicinity of
junction of the two oesophageal regions.
Spicules 2-5 mm. long, 1:5:6 of body length, with striated alae. Gubernaculum
not seen. Bursa large; lobes well marked, distinct from one another. Ventral ray
long, thin, nearly reaching bursal edge, cleft for entire length; externo-lateral
arising with lateral but divergent from it after half length, and nearly reaching
edge of bursa; lateral cleft for half length, nearly reaching edge; externo-dorsal
short, stout, arising from base of laterals. Dorsal ray stout, short, bifurcating
about half length, each branch dividing beyond mid-length into two rays, the inner
being slightly longer and thinner.
As already stated, this species has been placed under the genus only pro-
visionally, since the condition of the solitary specimen has prevented a more
detailed account being given and a satisfactory assignment being made.
ZONIOLAIMUS Cobb 1898.
In a recent paper (1939) we rehabilitated Cobb’s genus, giving a diagnosis
and describing some new species. Labiostrongylus Yorke and Maplestone was
placed as a synonym and the numerous species described under that genus were
transferred to Zoniolaimus. Since the two species named by Cobb came from New
South Wales material, an attempt has been made to interpret his formula and
figures relating to them. In addition to describing two new species in this paper,
we give host and locality records for three already known.
ZONIOLAIMUS SETIFER Cobb 1898. Figs. 19-22.
From the “brush wallaby”’, Moss Vale. We have already indicated that
Macropus ualabatus is the species referred to. The following description is based
on the figures and formula given by Cobb (1898, fig. 30).
Length of male, 7°75 mm. Head with eight lips, the four submedian larger
than laterals, dorsal and ventral, and bearing each a long bristle (0:02 mm.) near
the bases. Buccal capsule cylindrical, about 0:02 mm. wide, with base 0:04 mm.
from top of lips. Oesophagus 1:23 mm. long, widening at about half its length into
an elongate bulbous portion, then narrowing into a constricted region followed by
a spherical bulb. Nerve ring at 0-4 mm. from head end and surrounding oesophagus
at about two-thirds its length; excretory pore near beginning of median swollen
portion of oesophagus, and about 0:52 mm. from anterior end of worm.
Male: Spicules thin, apparently 1-6 mm. long (i.e. 1:4-8 of body length). Bursa
large, all rays except externo-dorsal reaching edge. Ventrals parallel, cleft half
their length; externo-laterals arising with laterals, diverging from them near tip;
laterals cleft half their length; externo-dorsal thin, arising from base of laterals
but divergent from them. Dorsal ray bifurcating between one-third and one-half
its length, each branch giving off short lateral ray soon after its origin. Genital
cone present; accessory cone of two small bodies. The breadth of body of the
male at base of buccal capsule, 0-069 mm.; at nerve ring, 0:13 mm.; at posterior
end of oesophagus, 0:22 mm.; maximum width 0:28 mm.; width near bursa,
0-08 mm.
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 521
No particulars are given of the female, except a drawing of the anterior end.
The measurements given for the Z. setifer (setiferus in Cobb) agree with the
sizes indicated in the diagrams. This worm then is much smaller than most species
of the genus. We have not been able to identify it amongst our material.
ZONIOLAIMUS BREVICAUDATUS Cobb 1898.
Host not mentioned, but presumably from a “brush wallaby” (i.e. Macropus
ualabatus) from Moss Vale, where Cobb was for a time engaged in official parasito-
logical work.
The only information relating to this species is embodied in two figures, one
of the female genitalia and one of male apparatus, together with the formula for a
female worm. The diagrams are of little use in identification, as also are the
measurements of the female. In no specimen of Zoniolaimus examined by us,
however, are the spicules so short in relation to other parts of the male. They are
apparently 1:5 mm. long. The measurements of a female, according to Cobb’s
formula, are: length of body 7-5 mm.; length of buccal capsule 0:06 mm.; anterior
end to nerve ring 0-33 mm.; oesophagus 1:07 mm. (i.e. 1:7 of body length); vulva
from tip of tail 0-38 mm.; anus from tip of tail 0-23 mm.; maximum width of body
0:32 mm. The figures in Cobb’s paper (figs. 102 and 103) are said to be natural
size; the length of the female is given as 7-5 mm., but the length of the sexual
organs (as figured) is 30 mm. We suggest, therefore, that an error has occurred
either in reduction of the original figures, or perhaps of a decimal place in the
stated length of the worm. On the other hand, no such error has been detected
in the case of Z. setifer (Cobb 1898, fig. 30), where the measurements given agree
very well with the figures.
The spicules of Z. brevicaudatus as indicated in a diagram (which is stated
to be natural size) are of the same length as those of Z. setifer, but a comparison
of the figures given for the two species shows them to be much shorter than those
of the latter in relation to other parts of the male system.
ZONIOLAIMUS CLELANDI, n. sp. Figs. 23-25.
From the stomach of Macropus ualabatus, Lower Hawkesbury (coll. J. B.
Cleland).
Male 21 mm.; female 30 mm. long. Lateral lips very prominent, with a median
terminal papilla; submedian lips rounded, each with a long seta. Buccal capsule
0-1 mm. wide, 0:07 mm. long; base 0:15 mm. from tip of submedian lips.
Oesophagus 4 mm. long; 1:5 of body length.
Male: Dorsal lobe of bursa long. Dorsal ray long, giving off a fairly long
branch on each side, the main stem continuing for a distance somewhat greater
than the length of each branch, and then bifurcating into two rather broad
terminal rays reaching the edge of the bursa. Spicules 7-2 mm., 1:3 of body length.
Female: Tail long, tapering; vulva at 1-7 and anus at 0:9 mm. from tip of tail:
vagina narrow, twisted, 1:5 mm. long; eggs (in vagina) 0-12 by 0-07 mm.
The species resembles Z. longispicularis and Z. communis. It differs from the
former in the form of the lateral and submedian lips and in the presence of setae
on the lips, the thinner dorsal ray and the different form and position of the
branches of that ray. It differs from Z. communis in the form of the dorsal ray,
relative sizes of the lateral and submedian lips, length of setae on the lips, and in
the rather shorter spicules.
ZONIOLAIMUS UALABATUS, nN. sp. Fig. 26.
From stomach, Macropus ualabatus, Lower Hawkesbury (coll. J. B. Cleland).
522 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
Only immature females found; short, stout; 6-4-7 mm. long; 0:3 mm. maximum
breadth; body with fine longitudinal striations. Head differs from that of any
other known member of the genus in having the four submedian lips smaller than
the laterals. Submedians conical, each with short seta; laterals tall, wider distally
where they bear each a small median rounded papilla; a dorsal and a ventral lip
present, conical, as large as lateral lips. Buccal capsule 0-045 mm. wide; 0-051 long
from top of lips. Oesophagus 1:1-1-4 mm. long; 1:6-7 of body length; base
surrounded by a pair of sheath-like prolongations of intestinal wall. Nerve cord
at 0:35-0-4 mm. from head end; excretory pore just behind nerve ring; cervical
papillae not observed.
Body narrows suddenly behind vulva, and again behind anus to end in narrow
pointed tail, 0°3 mm. long. Anus 0:17 mm. behind vulva. Since the above account
was written two adult females, 20 mm. long, were found amongst the material
from the same host, the organs in these worms presenting the same proportions
as in the younger specimens.
ZONIOLAIMUS LONGISPICULARIS (Wood 1929).
This large species, originally described as a Labiostrongylus, has been identified
amongst material collected from M. rufus, Wentworth, South-Western New South
Wales, and from Balranald; and M. major, from Narrandera and Narrabri.
ZONIOLAIMUS COMMUNIS Johnston & Mawson 1939.
From Macropus ruficollis, Bathurst district.
ZONIOLAIMUS ONYCHOGALE Johnston & Mawson 1939.
From Macropus ruficollis, Bathurst district.
ZONIOLAIMUS SP.
Immature specimens and females, not identifiable specifically, were found in
Macropus thetidis, New England; M. major, Coonamble; M. ualabatus, Lower
Hawkesbury; and M. ruficollis, Ourimbah, Gosford district.
PARAZONIOLAIMUS, DT. gen.
Trichoneminae: Lips prominent, laterals largest, dorsal and ventral smallest.
Short cuticular projecting frill around head region just behind lips, followed by
slight constriction. Bursa large; ventral lobes separate; dorsal ray giving off a
pair of lateral branches and then bifurcating. Female with tapering pointed tail;
vulva a short distance in front of anus. From stomach of marsupials. Type,
P. collaris, n. sp., from Macropus ualabatus.
This genus is close to Zoniolaimus from which it differs in the possession of a
cuticular frill surrounding the head.
PARAZONIOLAIMUS COLLARIS, Nn. sp. Figs. 27-29.
From stomach, Macropus ualabatus, Lower Hawkesbury (J. B. Cleland).
Body long, stout; male 15-16-5 mm. long; adult female 20-30 mm.; young
females (devoid of eggs) from 11mm. long. Anterior end with eight lips; two laterals,
long, upright, each with small round terminal papilla; four submedian shorter,
stout, bent inwards, each bearing rounded papilla with upwardly-directed bristle,
the tip of which divides into two; distal end of each submedian lip dividing into
two short laterally-directed processes; ventral and dorsal lips short, conical.
Behind origin of lips arises a cuticular frill, with free outer edge, 0:03 mm. wide,
marked with circular concentric striations, parallel to its edge. Head in this
region 0-18 mm. diameter, and followed by somewhat constricted neck region
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 523
widening after 0:06 mm. to form body proper. Buccal cavity 0:07 mm. in diameter;
squarish in side view; lined by thick chitin; base 0:1 mm. from anterior end of
submedian lips. Oesophagus about 1:4:2 (or less) of body length; widening
towards its posterior end, to become surrounded by sheath-like granular prolonga-
tion of intestinal wall. Nerve ring surrounding oesophagus about 0:6 mm. from
Figs. 23-25, Zoniolaimus clelandi. 23. dorsal lobe of bursa; 24. ventral and lateral
lobes of bursa; 25. head.
Fig. 26. Z. walabatus, head.
Figs. 23, 24, and 25 to same scale.
Figs. 27-29, Parazoniolaimus collaris. 27. head; 28. anterior end; 29. half of bursa,
ventral and lateral lobes folded over dorsal lobe. All figures to same scale.
Fig. 30, Maplestonema typicum, head.
Figs. 31-32, Macropostrongylus lesouefi. 31. head, sublateral view; 32. bursa.
Fig. 33, M. wallabiae, head.
Figs. 34-36, M. dissimilis. 34. head; 35. bursa; 36. posterior end of female.
Figs. 30, 31, and 34 to same scale; figs. 32, 33 and 35.
524 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
anterior end of body; cervical papillae long, threadlike, about half-way between
nerve ring and frill; excretory pore about 0-2 mm. behind nerve ring.
Male: Bursa large, ventral lobes separate from one another, joined to lateral
lobes; dorsal lobe prolonged with rather large median indentation. Ventral rays
long, parallel, cleft nearly all their length. Externo-lateral ray short, about half
length of laterals; externo-dorsal two-thirds length of laterals with which it arises.
Laterals long, parallel, cleft nearly all their length. Dorsal ray very broad at
base; giving off at about mid-length a pair of lateral club-shaped branches, and
soon afterwards dividing into two club-shaped rays forming an arch reaching into
prolongations of the dorsal lobe. Genital cone with small button-like structure on
its tip. Spicules 4:05 mm. long in a male 16 mm. long, 1:4 of body length; with
striated alae extending nearly all their length, widening near distal ends. Spicules
difficult to trace in whole specimens, and have to be dissected out. Gubernaculum
0:08 mm. long, canoe-shaped.
Female: Body tapering to a pointed tail; intestine narrowing suddenly about
0-3 mm. from anus and surrounded by narrow band of tissue (glandular?) before
passing to anus; latter 0:7 mm. from tip of tail. Vagina thin, long; vulva about
0-35 mm. in front of anus; eggs 0:09 mm. by 0:07 mm.
MAPLESTONEMA, Nn. gen.
Since males have not been found, we cannot give a complete diagnosis.
Trichoneminae. Anterior end rounded; no mouth collar; six equal elongate
papillae around mouth; deep buccal cavity supported only by narrow ring of
chitinous substance near its base; oesophagus of uniform width. Male unknown.
Female with tail tapering to a point; vulva just in front of anus. From stomach
of marsupials. Type M. typicum, n. sp., from Macropus ualabatus, Lower
Hawkesbury. °
This genus differs from its nearest relatives Macropostrongylus and Cloacina
in the absence of a leaf crown, and in the possession of six equal oral papillae.
It differs from Buccostrongylus in the structure of the buccal capsule; and from
Spirostrongylus Y. & M. in the absence of the leaf crown and in the characters of
the buccal capsule. The generic name is proposed in recognition of Dr.
Maplestone’s contributions to Australian helminthology.
MAPLESTONEMA TYPICUM, nN. sp. Fig. 30.
From Macropus ualabatus, Lower Hawkesbury.
We have examined only two immature female specimens. They are small
and coiled; about 6-1 mm. in length. Flattened anterior end with six short thin
digitate papillae surrounding wide mouth; latter leading into large cavity, 40u
long, 354 in diameter. This cavity, at about three-fourths length, is surrounded by
ring of chitin 8u long, 5u thick. No leaf crown. Oesophagus 0:95 mm. long, rather
wide, slightly enlarged towards posterior end; surrounded by nerve ring at about
end of its anterior half (0-4 mm. from head); excretory pore just behind this
level, 0-47 mm. from head end. Body tapering gradually at posterior end, tail
pointed, tip curved dorsally. The vulva can just be distinguished, 0:25 mm. in
front of the anus. The latter is equidistant from the vulva and the tip of the tail.
MACROPOSTRONGYLUS Yorke & Maplestone 1926.
This genus was based on M. macropostrongylus Y. & M. (type) and M. australis
Y. & M. from Macropus sp. from North Queensland. Baylis (1927) added a third
species, M. yorkei, from the same region. Wood in 1930 described M. baylisi from
Macropus robustus woodwardi. M. macropostrongylus and M. yorkei were recorded
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 525
by us from Queensland wallabies (1939). We now add two new species from the
red-necked wallaby and one from M. ualabatus in New South Wales.
MACROPOSTRONGYLUS LESOUEFI, nN. sp. Figs. 31-32.
From stomach of Macropus ruficollis, Sydney Zoological Gardens.
Short worms tapering more towards anterior end. Male 6-2-8-4 mm.; female
about 10-7 mm. Anterior end with two large prominent lateral papillae, and four
small submedian papillae, the latter each with two short bristles. Buccal capsule
about 0:04 mm. long and 0:02 mm. in diameter in male; wall not regularly
chitinized but middle part (i.e. middle longitudinal layer) most strengthened; wall
ending anteriorly in six (perhaps eight) rounded knobs, presumably corresponding
to a leaf crown. Oesophagus about 0:95 mm. long (in male); comprising two
parts, a longer anterior, about the middle of which is the nerve ring, and a shorter
posterior portion, narrow at the beginning but widening to a bulb. Excretory
pore not detected; cervical papillae long, hair-like, at 0-25 mm. from anterior end
of worm.
Male: Spicules seem to vary in length in specimens otherwise identical, but
they are always short, 0-:36-0-7 mm.; stout; ends tapering, rounded; wide striated
alae extending nearly to tip. Bursa large; dorsal lobe longest; ventral lobes
short, joined ventrally. Ventral rays long, thin, cleft nearly all their length;
laterals and externo-dorsals arising from same root, long, thin; medio- and postero-
laterals longest, cleft half their length. Dorsal ray bifureating after half its
length, each branch giving off stout lateral ray from its mid-length. Genital cone
very small.
Female: Uteri parallel; ovejectors 0:15 mm. long; vagina about 0:25 mm. long;
vulva about 0-9 mm. and anus at 0:6 mm. from tip of tail.
This species closely resembles M. macropostrongylus but differs from it in the
length of the spicules and oesophagus as well as in the shape of the female tail
and in the characters of the head.
It is named for Mr. A. S. Le Souef, Director of the Sydney Zoological Gardens
and author of important works dealing with Australian vertebrates.
MACROPOSTRONGYLUS WALLABIAR, nN. Sp. Fig. 33.
From stomach, Macropus rujicollis, Bathurst district.
Male 8-4 mm., female 11:4 mm. long; cuticle marked with fine striations.
Anterior end blunt; mouth collar with six small rounded papillae. Buccal capsule
0:045 mm. deep and 0:025 mm, wide (internal measurement) except at anterior
end where walls bend outwards; walls much thicker in posterior half than in
anterior. Short leaf crown probably present, arising from anterior end of -capsule
but number and shape of elements indistinguishable. Oesophagus about 0:8 mm.
long, with wider anterior part and short thin posterior part ending in bulb. Nerve
ring appears to be around thinner part of oesophagus. Cervical papillae long,
threadlike, at 0:25 mm. from anterior end of worm.
Male: Spicules short, about 0-8 mm. long, 1:10 of body length, with wide
striated alae and bluntly rounded tips. Bursa large; ventral lobes small, not
joined ventrally and almost separate from lateral lobes; dorsal lobe wide, long.
Condition of specimen prevented disposition of bursal rays from being ascertained
accurately. Ventral rays short, parallel, almost to edge of bursa; externo-lateral
ray divergent from laterals for most of its length; laterals stout, cleft for half
their length and reaching almost to bursa; externo-dorsal arising separately, long,
stout, not reaching edge of bursa. Dorsal ray indistinct; two main branches
526 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
apparently reaching edge of dorsal lobe and each giving off a lateral ray at about
mid-length. Genital cone short.
Female: Ovejectors long, thin; vagina short, wide; vulva 0-8 mm., and anus
0-3 mm. from tip of tail. Tail long, tapering, ending in point. Hggs 0:13 mm.
by 0-07 mm.
This species closely resembles Spirostrongylus spirostrongylus Y. & M. 1926 in
the arrangement of the buccal capsule, but those authors do not indicate the
presence of oral papillae. It has been assigned to Macropostrongylus on account
of the buccal capsule, leaf crown, shape of bursa, general arrangement of rays, and
character of female tail; but it differs from other species of this genus in that
the lateral and submedian oral papillae are of equal size.
MACROPOSTRONGYLUS DISSIMILIS, i. Sp. Figs. 34-36.
From Macropus ualabatus, Lower Hawkesbury.
Rather plump worms; males 6-5 mm.; females, often coiled, 6-8 mm. long.
Anterior end truncated, bearing four small conical submedian papillae and two
very small laterals. Buccal capsule continuous from oral opening, 10u deep, 15u
in diameter, with chitinized walls. Oesophagus widening gradually towards base;
0-55 mm. long. Nerve ring at 0:19, excretory pore at 0-46, and threadlike cervical
papillae 0:1 mm. from anterior end of worm. Anterior part of intestine surrounded
by granular lobes.
Male: Bursa large; lobes not deeply separated from one another; rays all thin
and reaching nearly to edge of bursa; externo-lateral divergent from laterals;
externo-dorsal arising separately; dorsal ray stouter, bifurcating after half its
length, each branch immediately giving off a lateral ray almost as long as itself.
Genital cone small, pointed. Spicules 0:7 mm. long, 1:9 of body length, with wide
striated alae. Apparently two gubernacula, the larger of which is more anteriorly
situated and may be a chitinization of the spicule sheath.
Female: Body tapering suddenly at vulva; tail pointed, backwardly directed.
Ovejectors 0-3 mm. long; vagina 0:35 mm. long; vulva 0-29 mm. and anus 0:2 mm.
from tip of tail. Eggs 80u by 50u.
This species is placed in the genus with some reserve because of the absence
of a leaf crown and because the submedian papillae are larger than the laterals.
It seems related to M. yorkei which it resembles in many features but differs in its
much smaller size, in the shape of the buccal capsule, and in the absence of a leaf
crown, which we have recognized in our specimens of yorkei, though Baylis
regarded its presence as doubtful.
BuccostRoneGyLus Johnston & Mawson 1939.
Although the general appearance of the head of two species now to be
described, Buccostrongylus setifer and labiatus, does not at first sight suggest that
they belong to the same genus, they have essentially similar structure; the chief
difference being in the size of the oral papillae and lips. In these features they
represent extremes of which the type species of the genus, B. buccalis, is the mean.
There is also a difference in the formation of the leaf crown which in the type
is formed by the indented anterior edge of the buccal capsule, but in B. setifer by
an accessory projection inwardly from the anterior edge of the buccal capsule. In
the latter species there is also a difference in the form of the dorsal ray, the lateral
branches coming off before instead of after the bifurcation, but these variations
are not considered sufficient to justify the erection of a new genus.
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. yl
BUCCOSTRONGYLUS BUCCALIS Johnston & Mawson 1939.
This species has been found in Macropus thetidis from New England, the
nematodes possessing lips slightly more prominent and the spicules a little longer
than those described previously from Queensland material.
BUCCOSTRONGYLUS AUSTRALIS Johnston & Mawson 1939.
Specimens of this species were found in Macropus ruficollis from Bathurst
district. Previously recorded from two other species of Macropus from
Queensland.
BUCCOSTRONGYLUS LABIATUS, nN. sp. Figs. 37-38.
From stomach of Macropus ruficollis, Bathurst district.
Worms slender, short, usually coiled. Male 3-7-4:3 mm.; female 5-6 mm. long.
Cuticle marked with fine longitudinal striations. Cuticle of mouth collar raised
into six rounded lips, outgrowths of the subcuticular tissue between these form
six small rounded papillae; four submedian lips each with a bristle; two lateral
lips without bristle. Cuticle around mouth further raised into 6-8 peri-oral lips,
the ventrals being larger than the others.
Within the mouth is a long straight chitinized buccal capsule or vestibule. In
all specimens this is very indistinct, only its outline and posterior limits being
perceptible; its termination is 0:043 mm. from top of lips and about 0:01 mm. wide
(external), but the anterior end is not clear. It is not striated. Oesophagus thin,
0:65-0:75 mm. long, 1:7:5 of body length, terminating in large distinct bulb. Nerve
ring surrounding oesophagus at about half length; excretory pore just behind
nerve ring; cervical papillae not observed. Intestine without processes around
base of oesophagus.
Male: Spicules about 1 mm. long, 1:3-7—4:3 of body length; with very wide
striated curved alae; distal ends of spicules lying together, each surmounted by a
small dise of thin chitinous material. Gubernaculum probably present; genital
cone short. Bursa wide, much shorter ventrally than dorsally; lobes not separated
by deep indentations. Ventral rays parallel, nearly reaching edge of bursa and
cleft nearly all their length. Externo-lateral and externo-dorsal shorter than
laterals with which they arise, and lifting side wall of bursa; laterals reaching
practically to edge of bursa, and cleft for half length. Dorsal ray long, bifurcating
after one-quarter of its length, almost immediately afterwards each branch giving
off a short lateral ray and then continuing nearly to edge of bursa, the two branches
coming closer together near their distal ends.
Female: Body tapering rapidly but evenly from region of vagina to end in
blunt point. Ovejectors about 0-5 mm. long, narrow; vagina about 0:3 mm. long;
vulva 0:37 mm., and anus 0-3 mm. from tip of tail. Hggs in vagina about 0:09 mm.
by 0:05 mm.
This species differs from B. setifer chiefly in regard to the lips and papillae.
BUCCOSTRONGYLUS SETIFER, nN. sp. Figs. 39-41.
From stomach of Macropus ruficollis, Bathurst district.
Short worms, tapering to both ends, tending to be somewhat coiled. Cuticle
with fine longitudinal striations. Male 4:8 mm.; female 6-5-7 mm. long. Mouth
surrounded by six low rounded papillae, each with a tapering bristle, those in
submedian positions being very long, and the two laterals short. The buccal
capsule differs from that in other members of this genus in being much longer
(0:075-0:085 mm.) and in enclosing a wider cavity near its anterior end, where
the walls become narrowed to a fine rim around the mouth. This enlarged part is
528 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
0-015 mm. wide and about 0:02 mm. deep, while the succeeding portion is 0:01 mm.
in internal diameter. It differs also in having a definite leaf crown of a few
(4, perhaps 6) elements projecting from the wall of the anterior wide part of
the capsule.
Figs. 37-38, Buccostrongylus labiatus. 37. head; 38. bursa.
Figs. 39-41, B. setifer. 39. head; 40. bursa; 41. posterior end of female.
Figs. 38 and 40 to same scale.
Figs. 42-45, Cloacina expansa, 42. head; 43. bursa; 44. posterior end of female;
45. anterior end.
Figs. 46-48, C. obtusa. 46. head; 47. bursa; 48. posterior end of female.
Figs. 42 and 46 to same scale; figs. 43, 45, and 47; figs. 44 and 48.
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 529
The anterior end differs from that of pharyngostrongyles in that there is no
differentiation into buccal capsule and vestibule, the whole structure, referred to
above as buccal capsule, being a continuous cylinder. There are also no striations
on this structure. There is, as in other species of Buccostrongylus, a slight
inflation of the cuticle around the anterior end.
Oesophagus 0:1 mm. long; with two parts, a long wide anterior and a shorter
narrow posterior, the latter terminating in a slight bulb. Nerve cord not seen.
Excretory pore near posterior end of anterior portion of oesophagus.
Male: Spicules stout, 1-3-1:4 mm. long, 1:4 of body length; with wide striated
alae extending almost to the rounded tips. Bursa very closely resembling that of
pharyngostrongyles in being small and covered with papillae on inner surface of
ventral and lateral lobes. Lobes well separated from one another; dorsal widest
and longest. Externo-lateral and externo-dorsal rays shorter than laterals with
which they arise, projecting on wall of bursa. Dorsal ray with two lateral branches
at about its mid-length, the main stem continuing a short distance before dividing
into two rays reaching edge of bursa; lateral branches stout, entering into dorsally
projecting pockets of bursal wall. Gubernaculum not observed.
Female: Body ending in tapering pointed tail, about 0:38 mm. long; distance
from anus to vulva about 0:28 mm. Uteri long, straight; ovejectors narrow; vagina
wide, quite long; eggs (in vagina) about 0:12 mm. by 0:06 mm.
This species differs from other members of the genus in the length of the
buccal capsule, presence of a leaf crown, form of bursa, and shape of female tail.
CLoacina Linstow 1898.
This imperfectly characterized genus was known only from the type species,
CO. dahli, from a wallaby in New Britain. In 1938 we recognized representatives
amongst Australian material and, as a result, were able to give a diagnosis differen-
tiating it from Macropostrongylus and to add fifteen new species from Central
Australian kangaroos and wallabies. A study of material from Queensland has
permitted recognition of five additional species (1939). We now describe five
more new forms and record the occurrence of four known species from New South
Wales Macropods.
CLOACINA EXPANSA, hh. Sp. Figs. 42-45.
From Macropus major, Coonamble (coll. A. S. Le Souef).
Male 9-6 mm.; female 15-18 mm.; cuticle widened at level of base of lips,
inflated region thinning out to end near the level of the posterior end of the
oesophagus; buccal capsule 0:05 mm. diameter, 0:01 mm. long. Oesophagus 0:55 mm.
long; nerve cord at 0:3 mm., excretory pore at 1 mm. (i.e. about 0-35 mm. behind
end of oesophagus), and cervical papillae at 0:12 mm. from head end.
Male: Bursa as in C. longispiculata; spicules 5:8 mm., 1:1:7 of body length.
Female: Anus at 0:3 mm., and vulva at 0-4 mm. from tip of tail; eggs 0:14
by 0:07 mm.
This species closely resembles ©. longispiculata in general form, shape of
bursa, oesophagus, submedian papillae; shape of posterior end of the female; and
spicule:body-length ratio. It differs in the following features: slightly greater
length; greater extension backwardly of the widened cuticular region at the head
end; wider buccal capsule with thicker, shorter chitinous ring; absence of lateral
papillae; cervical papillae nearer anterior end; and the longer. narrower vagina.
The specific name is given because of the wide cuticular inflation anteriorly.
QQ
530 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
CLOACINA OBTUSA, nN. Sp. Figs. 46-48.
From Macropus major, Coonamble (coll. A. S. Le Souef).
Males 11:5-13 mm. long; females 18-22 mm.; not tapering markedly at anterior
end which is truncate; six large lips, submedians with small two-jointed papillae.
Buccal capsule 0:055 mm. wide; 0-015 mm. deep with base 0:04 mm. from top of
lips. Leaf crown of six elements arising from base of capsule and bluntly pointed
at distal ends. Oesophagus 0°75 mm. long, widening at base; surrounded by nerve
ring about its middle. Excretory pore just in front of posterior end of oesophageal
region; thus nerve ring is 0:36, and excretory pore 0:68 mm. from anterior end of
worm.
Male: Bursa large, lobes not deeply separated. Ventral rays together, extending
nearly to edge, cleft for most of their length; externo-lateral stout, tapering, almost
reaching to edge; laterals extending nearly to edge, cleft for three-fourths of their
length, tips separate; externo-dorsal arising separately, shorter than laterals.
Dorsal ray stout, bifurcating after one-third length, each branch ending in two
short processes, of which outer is shorter and stouter, neither reaching edge of
bursa. Spicules about 3-5 mm. long, 1:3 of body length. Gubernaculum absent.
Genital cone very short, rounded.
Female: Body tapering suddenly beyond vulva to end in pointed dorsally-
directed tail, 0:27 mm. long. Vagina about 0-8 mm. long; vulva 0:2 mm. in front
of anus; eggs in vagina 0-1 by 0:05 mm.
This species resembles C. macropodis in its head region but differs in its
greater length; blunt elements of the leaf crown; longer buccal capsule; and in
the spicule:body-length ratio. The specific name is given on account of the
blunt tips of the elements of the leaf crown.
CLOACINA MAGNIPAPILLATA, Nn. Sp. Figs. 49-52.
From Macropus major (type host), Coonamble (coll. A. S. Le Souef); and
M. rufus, Wentworth (coll. A. L. Rait).
Male 10-11 mm.; female 12-15 mm. long; head with six low lips, submedians
with long, two-jointed papillae, laterals each with small papilla; buccal capsule
0:032 mm. diameter, 0:01 mm. deep, base 0:02 mm. from top of lips. Elements of
leaf crown arising from base of capsule; sharply pointed, with tips incurved.
Oesophagus 0:75 mm. long (in male), wider at base but without definite bulb.
Nerve ring at 0:35 mm., excretory pore at 0:7 mm., and cervical papillae at 0:09 mm.
from anterior end.
Male: Bursa large; lobes not deeply divided except ventrals which are separate
from one another. Ventral rays long, cleft nearly all their length; externo-lateral
long; laterals cleft for three-fourths length, reaching nearly to edge of bursa;
externo-dorsal as long as, and arising with, laterals. Dorsal ray bifureating after
one-third length, each branch giving off a shorter lateral ray after half length,
neither reaching edge of bursa. Spicules 3-8 mm. long; 1:2-:7 of body length.
Genital cone small; accessory cone of two prominent processes. Gubernaculum
not seen.
Female: Posterior end tapering gradually from region of vagina; tail J:23 mm.
long, ending in point. Vagina long, twisted; vulva 0:35 mm. in front of anus.
This species resembles Cloacina curta and ©. wallabiae in the head region. In
general characters it suggests the latter species but differs from it in size; form
of the dorsal ray; spicule—body-length ratio; absence of definite oesophageal bulb;
and less sudden tapering of the posterior end of the female.
531
BY T. H. JOHNSTON AND PATRICIA M. MAWSON.
Figs. 49-52, Cloacina magnipapillata. 49. head; 50. posterior end of female; 51.
bursa; 52. dorsal ray.
Figs. 53-54, C. wallabiae. 53. head; 54. bursa.
Fig. 55, C. thetidis, head.
Figs. 49, 53 and 55 to same scale; figs. 51 and 52.
Figs. 56-58, Globocephaloides thetidis. 56. head,
view; 5S. bursa, dorsal view.
Figs. 59-62, Hypodontus thetidis.
61. bursa, lateral view; 62. dorsal ray.
Figs. 58 to 62, to same scale.
Figs. 63-64, Austrostrongylus wallabiae.
Figs. 65-66, Asymmetricostrongylus trichosuri,
lateral view: 457. bursa, ventral
59. head. ventral view: 60. head. lateral view;
63. head; 64. bursa.
65, head; 66. posterior end of female,
532 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
CLOACINA WALLABIAE, nh. sp. Figs. 53-54.
From Macropus ualabatus, Lower Hawkesbury district (coll. J. B. Cleland).
Only five specimens found; 4—6 mm. long; some rather coiled. Apparently only
four outer lips, the laterals being absent and their position marked by a pair of
small conical papillae; submedians each with long two-jointed papilla; inwardly
from outer lips and from lateral papillae are six distinct rounded inner lips;
inwardly from these latter, projecting beyond them, is the leaf crown of six finely-
pointed triangular elements, 0:04 mm. long, arising from base of buccal capsule;
latter 0-038 mm. in diameter internally, 0:01 mm. long, with walls 4y thick.
Oesophagus 0°55 mm. long, widening towards base to a more or less definite bulb;
nerve ring at about mid-oesophagus; excretory pore at level of three-fourths length
of oesophagus. Cervical papillae, long, threadlike, about 0:15 mm. from anterior
end of worm.
Male: Spicules about 0:9 mm. long, 1:4 of body length, thin, with very wide
striated alae. Ventral rays long, thin, cleft about half length; externo-lateral
stout, tapering; laterals thinner and longer; externo-dorsal arising with laterals,
shorter and divergent from them. Dorsal ray bifurcating near its origin, each
branch continuing nearly to edge of bursa and giving off shorter lateral ray after
about one-third of its length. Genital cone very short; accessory cone of two large
projecting lobes.
Female: Body tapering suddenly beyond vulva, which is 0-5 mm. in front of
anus; tail about 0:3 mm. long, ending in rounded point; vagina long, narrow; eggs
0-08 by 0-04 mm.
This species most closely resembles (©. robertsi in the general appearance of
the head but differs in the spicule—body-length ratio; shape of the dorsal ray;
length of vagina; and in the position of the excretory pore; as well as in the
rather different configuration of the head region.
CLOACINA THETIDIS, nN. sp. Fig. 55.
From Macropus thetidis, New England.
Only one female found, 6-5 mm. long. Lips not distinct; four submedian
papillae arising from elevations of mouth collar, each papilla consisting of two
thin joints; leaf crown arising from base of buccal capsule giving appearance of
six rounded inner lips, on two of which the inner edge can be seen projecting as a
pointed tip like the leaf crown elements in other species of Cloacina; similar
pointed tips presumed to be present on other lips though not seen. Buccal capsule
0-055 mm. diameter, of uneven height (0-008 mm.—0:01 mm.), base 0:034 mm. from
anterior end. Oesophagus 0:6 mm. long, wide, straight. Nerve ring at 0:26 mm.,
and cervical papillae at 0:09 mm., from anterior end.
Posterior end of body tapering to a dorsally-directed point; tail 0-2 mm. long.
Vulva. 0-35 mm. from tip of tail. Specimen is probably young, eggs being present
only in uterus, where they measure 0:11 by 0:08 mm. :
This species differs from all Known species in the wide shallow buccal capsule,
the long thin papillae at the anterior end, and the rounded ends of the elements
of the leaf crown.
CLOACINA stmMiILis Johnston & Mawson, 1939.
Females from stomach of Macropus thetidis, New England.
These nematodes very closely resemble C. similis and C. petrogale but, since
males are absent, it is difficult to place them exactly. The head differs from that
in these species in having a relatively wider buccal capsule, thinner papillae, and
less obvious lips, The distinct leaf crown, the presence of a lateral papilla, the
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 533
deep buccal capsule and the long, thin anteriorly-placed cervical papilla suggest
both these species. The posterior end has the characteristic short conical tail, long
vagina with rather small eggs, and anus equidistant from the vulva and the tip of
the tail. The positions of nerve ring and excretory pore agree most closely with
those in C. similis, but the oesophagus differs slightly in shape, the terminal bulb
being more distinct and larger.
The parasites may be placed provisionally under C. similis.
CLOACINA BANCROFTORUM Johnston & Mawson 19839.
This species was recognized amongst material from Macropus thetidis from
New England.
CLOACINA LONGISPICULATA Johnston & Mawson 1939.
We have identified the species from Macropus rufus from Wentworth, South-
western New South Wales (coll. W. L. Rait).
CLOACINA MACROPODIS Johnston & Mawson 1938.
From Macropus walabatus, Lower Hawkesbury district (coll. J. B. Cleland).
Our specimens differ a little from those from Central Australia, the oesophagus
being somewhat longer and spicules slightly shorter. The general features and
arrangement of parts, however, are similar in both and there does not appear
to be sufficient justification for the erection of a new species.
CLOACINA SP.
Two poorly preserved female specimens of Cloacina were found in the stomach
of Macropus thetidis, New England. Their condition has not permitted us to
make a definite identification.
GLOBOCEPHALOIDES Yorke & Maplestone 1926.
The genus was based on female specimens described as G. macropodis, from a
Northern Queensland Macropus sp. Recently (1939) we added two other species,
G. wallabiae and G. affinis, also from Queensland, and have been able to extend the
diagnosis on account of the finding of males. We now add another species,
G. thetidis.
GLOBOCEPHALOIDES THETIDIS, n. Sp. Figs. 56-58.
From the intestine of Macropus thetidis, New England.
Male 6 mm.; female unknown. Buccal capsule 60u long, 504 maximum width,
20u wide at base; dorsal tooth projecting 20u from base of capsule. Mouth opening
254 diameter. Oesophagus 0:58 mm., 1:10 of body length. Nerve ring and
excretory pore not seen. Spicules 0:045 mm., 1:13:3 of body length. Bursa with
ventral lobes separated in front, ventral and lateral lobes continuous, dorsal lobe
small and elongate. Ventral rays long, thin, separate, reaching edge of bursa;
externo-lateral stouter, slightly shorter than ventrals; medio-lateral stout, distal
part narrowing suddenly; postero-lateral slightly thinner than medio-lateral,
narrowing as in latter ray; medio- and postero-lateral not quite reaching bursal
edge; externo-dorsal thin, shorter than postero- and medio-laterals, raising edge of
bursa into papilla-like structure. Dorsal ray ending in two short, probably
bidigitate, processes.
The species differs from G. macropodis (female) in the size of the buccal
capsule, relative size of the dorsal tooth, and length of oesophagus; from G. affinis
(female) in the form of the chitinous support for the buccal capsule, and in the
relative size of the tooth; from G. wallabiae (male) in size, relative length of the
spicules, length of ventral rays, and form of the medio- and postero-lateral rays,
534 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES,
Hyropontus Monnig 1929.
This genus, belonging to the Ancylostomatidae, Necatorinae, is so far known
only from its type species, H. macropi Monnig, whose name should be emended
to H. macropodis. The host was Macropus rufus from Pretoria Zoological Gardens.
We add a second species, H. thetidis.
HyYPopONTUS THETIDIS, n. sp. Figs. 59-62.
From the caecum of Macropus thetidis, New England.
Male about 11 mm. long; female about 14 mm. Mouth collar with six very
small papillae; buecal capsule with two dorsal cutting plates anteriorly, ventral
margin notched. Dorsal gutter in buccal capsule, ending anteriorly in two short
lateral arms, narrowing posteriorly. Anterior end of oesophagus with three pointed
triangular teeth about 30 long, projecting into buccal capsule. Cervical glands
extending back about 0:5 mm. from anterior end. Oesophagus 1:05-1:1 mm. long,
1:10-11 of body length (in male). Nerve ring at 0-6 mm. from anterior end.
Cervical papillae and excretory pore not seen.
Male: Dorsal lobe of bursa longest; ventrals not joined in front. Ventral rays
short, together; externo-lateral short, tip diverging from laterals; laterals cleft at
tips, not quite reaching edge of bursa; externo-dorsal arising separately, tapering,
not reaching edge of bursa. Dorsal ray bifurcating soon after origin, each branch
giving off a shorter lateral ray just after its mid-length, neither branch quite
reaching edge of bursa. Prebursal papillae not seen. Spicules 0:87 mm., i.e.
1:12:6 of body length. Gubernaculum large, elongate.
Female: Vulva 0:3 mm., and anus at 0:1 mm. from tip of conical tail.
The species closely resembles H. macropodis whose males are 13-15 mm., and
females 17-20 mm. long. The relative measurements agree closely; the chief
differences between the two are the shorter gubernaculum, greater distance between
the vulva and the tip of the tail, and the lower position of the bifurcation of the
dorsal ray.
AUSTROSTRONGYLUS Chandler 1924.
This genus of Trichostrongylinae was based on A. macropodis Chandler from
Macropus bennetti from Zoological Gardens, Houston, Texas. We added (1938)
A. minutus from M. dorsalis in Queensland. We now give an account of another,
A. wallabiae n. sp.
AUSTROSTONGYLUS WALLABIAE, hn. sp. Figs. 63-64.
From the intestine of Macropus ruficollis, Bathurst district.
Worms very tightly coiled; tapering markedly at anterior end; cuticle with
6-8 longitudinal folds, marked with transversal striations, the cuticle between the
folds being unstriated. The folds begin just posterior to the dilated cuticle around
the head (0:08 mm. from anterior end) and extend in the female to the region just
anterior to vulva; in the male to within a short distance of bursa where they give
place to ringed striations; in the female there is little trace of striation between
the vulva and anus, but on the tail fine rings are definite.
The worms are characterized by regularly-placed masses of granular tissue,
forming a projection over the vulva, another a little anterior to the vulva, and
one in the dorsal lobe of the bursa where it obscures the dorsal ray.
There are probably four small papillae at the anterior end, in submedian
positions. Buccal capsule dome-shaped, 0:0832 mm. diameter at base, 0:022 mm.
long at centre, its thin chitinous walls with outwardly projecting ridge at their
base; walls continuous inwardly with floor of buccal capsule and cuticular lining
BY T. H. JOHNSTON AND PATRICIA M. MAWSON. 535
of oesophagus; dorsal tooth 0:02 mm. long, 0:01 mm. wide near base; ventral tooth
about 4u long. Oesophagus about 0-38 mm. long, widening slightly towards base.
Nerve cord at 0-2 mm., and excretory pore at 0:28 mm. from anterior end of worm.
Male: About 5-3-5-5 mm. long, 0-2 mm. maximum diameter. Spicules very fine,
proximal terminations hard to observe; probably between 0-4 and 0:8 mm. long.
Gubernaculum not seen. Bursa distinctive in having a very short dorsal lobe and
the two lateral lobes extended laterally, so that in their natural position (i.e. before
flattening) they fold together, the bursa then having the appearance of a ventral
outgrowth of the posterior end of the body. Lobes not asymmetrical. Ventro-
ventral ray bending ventrally; postero-ventral almost straight; externo- and medio-
laterals stout, tapering, with distal ends divergent from one another; postero-
lateral thin, long; externo-dorsal long, thin, arising from same base as laterals
but immediately separating from them. Dorsal ray short, thin, giving off a lateral]
branch at each side soon after its origin, the main stem dividing into two short
branches at distal end; the lateral branches may be asymmetrical.
Female: About 6:9 mm. long; body narrowing suddenly about 0-1 mm. from
posterior end to a tapering, pointed tail. Position of vulva (1:15 mm. from
posterior end) marked by presence of a projecting mass of granular tissue just
beneath its cuticle, probably a kind of protective flap, somewhat like that occur-
ring in Haemonchus. Vagina short; ovejectors muscular; uteri divergent but hard
to trace as specimens do not clear easily. Anus probably at beginning of narrow
tail, about 0:08-0:09 mm. from posterior end. ;
The species closely resembles A. macropodis (from Macropus bennetti, which
is the Tasmanian subspecies of M. ruficollis), but differs from it in the different
form of the bursa, dorsal ray, length of postero-lateral ray and greater divergence
of the externo- and medio-lateral rays. The characters of the head region, buccal
cavity and cuticular ornamentation are similar.
The species differs from A. minutus in its greater size, wider bursa, form of
the lateral rays, and relatively shorter dorsal tooth.
ASYMMETRICOSTRONGYLUS Nagaty 1932.
The name was proposed by Nagaty for Trichostrongylus asymmetricus Cameron
1926 (as type), 7. australis Wood 1930, and T. dissimilis Wood 1930, but no
diagnosis was given. The first was described from Macropus bennetti and the
other two from M. woodwardi, Wood also recording A. asymmetricus from the
latter marsupial. Lent and Freitas (1934, 252) consider the genus invalid.
ASYMMETRICOSTRONGYLUS TRICHOSURI, n. sp. Figs. 65-66.
From the oesophagus of Trichosurus caninus, Gosford district.
Only females were collected. Very thin filiform worms, about 4:5 to 5:1 mm.
long, with maximum breadth about 50u. Cuticle with fine longitudinal striations
and with more widely separated transverse markings. Anterior end about 17 in
diameter, apparently surmounted by six lips. Oesophagus 0:86 mm. long, of even
diameter. Vulva a narrow transverse slit, 1:68 mm. from posterior end of
oesophagus and at about mid-length of worm; uteri divergent; eggs large, 60u
long, 27u wide. Posterior end tapering, narrowing suddenly from anus to end in
blunt point; tail 0:06 mm. long.
The absence of males prevents our comparing the species with those described
from Australian marsupials. The type, A. asymmetricus (Cameron), is described as
having six papillae and no buccal tooth. If these papillae resemble the structures
536 STRONGYLATE NEMATODES FROM MARSUPIALS IN NEW SOUTH WALES.
which we refer to as lips, then our species could be placed under Nagaty’s genus,
as we have done.
Literature.
BayLis, H. A., 1927.—Some New Parasitic Nematodes from Australia. A.M.N.H.. (9),
20, 214-223.
, 1934.—Some Parasitic Worms from Australia. Parasitol... 26, 129-132.
CAMERON, T. W. M., 1926.—On a New Species of Trichostrongyle Worm from the Bennett's
Wallaby. J. Helminth., 4, 28-26.
CANAVAN, W. P., 1931.—Nematode Parasites of Vertebrates in the Philadelphia Zoological
Garden and vicinity, II. Parasitol., 23, 196-228.
CHANDLER, A. C., 1924.—A new Genus of Trichostrongylid Worm from the Kangaroo.
Parasitol., 16, 160-168.
Cops, N. A., 1898.—Extract from MS. Report on Parasites of Stock, Agric. Gaz. N.S.W..,
9, 296-521, and 419-454.
JOHNSTON, T. H., and Mawson, P. M., 1938.—Strongyle Nematodes from Central
Australian Kangaroos and Wallabies. Tr. Roy. Soc. South Austr., 62 (2), 263-286.
————,, 1938.—Some Nematodes from Australian Marsupials. Rec. South Austr. Mus.,
6 (2), 187-198.
, 1939.—Strongyle Nematodes from Queensland Marsupials. Tr. Roy. Soc. South
Austr., 63 (1), 121-149.
Lent, H., and Freitas, J. F. T., 1934.—Sobre dois novos generos da subfamilia Tricho-
strongylinae Leiper. parasitos de Tinamus solitarius Vreill. Mem. Inst. Osw. Cruz,
28, 247-257.
MOonnic, H. O., 1926.—Three New Helminths. Jr. Roy. Soc. S. Africa, 13 (3), 291-298.
, 1927.—On a New Physalopteran from an Eagle and a Trichostrongyle from
the Cane Rat with notes on Polydephis quadricornis and the genus Spirostrongylus.
Tr. Roy. Soc. South Africa, 14 (3), 261-265.
, 1929.—Hypodontus macropi, n. gen., n. sp., a Hookworm of the Kangaroo.
Rep. Dir. Vet. Serv. Pretoria, 15, 303-506.
NaGaty, H., 1932.—The Genus Trichostrongylus Looss 1905. Ann. Trop. Med. Parasit.,
26, 457-518.
YORKE, W., and MAaPLESTONE, P. A., 1926.—The Nematode Parasites of Vertebrates.
London.
537
ECTOCARPUS CONFERVOIDES (ROTH) LE JOL.
By VALERIE May, B.Sc., Linnean Macleay Fellow of the Society in Botany.
(Forty-six Text-figures. )
[Read 27th September, 1939.]
The Ectocarpales include the simplest known forms of the Melanophyceae
(Phaeophyceae). Therefore, in any discussion of the origin of a land flora from
marine plants, a knowledge of the life-history and cytology of these forms is
advantageous.
The Ectocarpaceae comprise filamentous forms which may bear sexual and
asexual reproductive structures on the same plant. As Knight (1923) indicated,
a more intimate knowledge of these forms may lead to a better understanding of
the problem of the origin of the alternation of generations among algae.
The life-history of Pylaiella litoralis Kjellm. has been investigated by Knight
at Port Erin, Great Britain (1923); that of Hctocarpus siliculosus (Dillw.) Lyngb.
by Berthold at Naples, Italy (quoted by Knight, 1929), by Knight at Port Hrin
(1929), by Kylin at Kristinberg, Sweden (1933), by Fgyn at Herdla, Norway
(1934), and by Papenfuss at Wood’s Hole, U.S.A. (1935).
The investigation reported here has been concerned with the variation in form
shown by E. confervoides, its host relationships, and particularly its cytology and
life cycle. The coastline examined in detail extends from Five Islands, Wollongong,
to Palm Beach, near Sydney, N.S.W.
SYSTEMATICS.
The Species.—A difference of opinion exists as to whether £. siliculosus should
be accorded the status of a species or should be regarded as a variety of
E. confervoides. Batters, quoted by Knight (1929), respects the species-distinction;
so also do Setchell and Gardner (1925), although they say: “We know full well
from our Own experience that it is difficult to draw a satisfactory line of demarca-
tion between the two species, but feel that the best we can do is to keep them
distinct and draw the line somewhat arbitrarily.” The distinction, if any, between
the two species is the usual presence of a terminal hair on the plurilocular
structure of H. siliculosws and its absence from that of H. confervoides.
If this distinction be accepted, both EH. confervoides and E. siliculosus occur
near Sydney, N.S.W. Forms corresponding to the typical EH. confervoides and
H. siticulosus were found, but as a complete series of variation exists between the
two extremes (Figs. 3, 6, 9, etc.), and since plurilocular structures terminated by
hairs may occur in the form which is usually non-haired (Figs. 1 and 2), there
seems to be no reason for regarding the form siliculosus as other than a variation
of H. confervoides. The life cycle of H. confervoides, reported in this paper, is in
agreement with that reported previously for EZ. siliculosus.
Vegetative Anatomy.—The plant is filamentous, growth being intercalary and
occurring usually at the base of the filaments (Fig. 3). Branching is irregular and
usually not opposite. It occurs by the development of a “blow-out”, usually at the
RR
538 ECTOCARPUS CONFERVOIDES,
upper end of a cell. The angle at which the branch emerges varies greatly; when
most acute (Fig. 3a), the branch tapers to a long, terminal hair, the cells of which
are elongated and possess but little protoplasm. The angle of branching becomes
more obtuse as fewer hairs are formed (Fig. 9a). Knight (1929) reports that at
Port Erin there is an increase in the angle of branching and a decrease in the
production of hairs during the course of a season, plants in the upper and lower
limits of the Hctocarpus-zone, however, maintaining the end-of-season form. At
Fig. 1.—E. confervoides showing associated plurilocular structures, which are either
hair-tipped or not. x 48.
Fig. 2.—As Figure 1, but reproductive structures are larger. a and b are from the
same plant. x 48.
Fig. 3.—a shows the habit of the hair-producing form, intercalary growing regions
occurring at the base of the hairs. a, b (haired plurilocular structure) and c (non-
haired) are from the same plant; d and e show variations of the non-haired form of
plurilocular reproductive structure. x 48.
Fig. 4.—An abnormal (bent) plurilocular reproductive structure. x 204.
Fig. 5.—An abnormal plurilocular reproductive structure, showing branching at the
apex. x 204.
Fig. 6.—This shows how a stalked, terminal plurilocular structure (b) may become
sessile and lateral (a) by sympodial development of a lateral branch. x 220.
Fig. 7.—Shows proliferation into the crumpled empty outer wall of a burst pluri-
locular structure. x 204.
Fig. 8.—a shows three cells which occurred in a single branch. In i the form of the
chromatophore is banded, in ii it is intermediate, and in iii discoid. b shows an almost
reticulate form of chromatophore. c and e show variation in the shape of the plurilocular
structures of a filament. d shows a constricted plurilocular structure which is abnormal,
due to failure of a central cell to divide. f shows a conical plurilocular structure, the
opposite in form to such as in Fig. 3b. (a, b, f x 196; c, d, e, x 48.)
BY VALERIE MAY. 539
Sydney relatively little of the acute-angled, hair-producing form has been found
at any time, and no evidence has been obtained of a seasonal change in appearance.
False cortex may occur in the basal portions of the plant. This is formed by
one or more lateral branches, each originating near the base of a cell, growing
downwards around the main axis (Fig. 9g). Where growth is dense, the loose
intertwining of the basal filaments gives a further measure of mechanical support.
The prostrate portion of the thallus is poorly developed.
The Vegetative Cell.—The size of the vegetative cell varies greatly (May, 1938,
and Fig. 17); the average measurements are 20-80u x 30u. Usually the lateral walls
are thicker than the transverse ones, but this difference is less obvious than that
between the outer and enclosed walls of the plurilocular reproductive structures.
Chromatophores occur in the parietal cytoplasm; these range from large band-
shaped and spirally-arranged forms (Fig. 80), to small, numerous, discoid ones
(Fig. 10a). Usually a single plant possesses one of these forms of. chromatophores,
but Figure 8a shows the transition in a filament from one extreme type to the
other. Closely associated with the chromatophores are round, highly refractive
Fig. 9.—a shows a wide angle of branching and very slight production of hairs; this
habit accompanies the broader form of plurilocular structure. Variation in the length of
the stalk of the plurilocular structure is shown. 0b, c, d and e show developmental stages
of a plurilocular structure. f is a mature plurilocular reproductive structure, in which
the apical tiers have divided actively. g shows false cortex; the laterals have arisen from
the basal end of the cells of the main axis and have grown down adpressed to the
filament. (a, x 48; b-g, x 204.)
Fig. 10.—a shows an extreme form of discoid chromatophores; as usual, the
pyrenoids are drawn black. b,c and d (apices of branches) show the habit of this form
of E. confervoides, i.e. broad angle of branching and very little suggestion of hair-
formation. The plurilocular structures possess usually not more than one stalk cell.
e shows one plurilocular structure in greater detail. The apical cells have not divided
as much, relatively, as those in Fig. 9f. (a, e, x 196; b, c, d, xX 48.)
Fig. 11.—This shows plurilocular reproductive structures which are associated with
forms as in Fig. 10e. a and b are from the same plant. x 204.
540 ECTOCARPUS CONFERVOIDES,
bodies, the “pyrenoids”. Usually these appear on the surface of the chromato-
phores, though they may be free except for cytoplasmic connections. Figure 27
shows the variation which may occur in any one cell. The chromatophore often
has a gap representing the former position of a pyrenoid. Knight (1929) and
later Mathias (1935) suggested that the pyrenoid body is a transformed portion
of the chromatophore.
Fig. 12.—This shows unilocular structures, sessile (a) or with one stalk cell (6b).
x 204.
Fig. 13.—a shows uni- and plurilocular reproductive structures occurring together.
b shows a series of unilocular structures, which vary in shape. ec is a surface section
of a unilocular structure; dense cytoplasm and many discoid chromatophores with
pyrenoids are shown. (a, c, x 204; b, x 48.)
Fig. 14.—This shows stages in the growth of the diploid germling. a is an older
plant than b. In athe upright (ii) and prostrate (i) portions of the thallus are clearly
differentiated. x 212.
Glistening droplets of fucosan, which stain red in hydrochloric acid-vanillin
(Knight, 1929), are usually present, especially near the nucleus. Non-staining
droplets (freshly-formed fucosan? (Knight, 1929) ) occur mainly near the
chromatophores, but as hydrochloric acid-vanillin disturbs the cell-contents, the
original positions cannot be stated with certainty. The size of these globules
varies, but they are usually somewhat larger than the ‘“‘pyrenoids”. They were
observed only in fresh material. Further work on the presence and relative
abundance of fucosan has been done by Knight (1929), who believes it is a storage
product and has correlated its absence with cell division. The nucleus occurs near
the centre of the cell (Fig. 16). The nucleolus may contain one or more clear
areas (Figs. 17a and 17b).
Reproductive Structures.—The plurilocular reproductive structures are very
much more common than are the unilocular. The plurilocular structures arise as
BY VALERIE MAY. 541
a short tier of cells occurring terminally or as a side branch. The densely cyto-
plasmic contents of the initials of the reproductive structures distinguish them
from the vegetative cells. In Figure 24, from c to b are vegetative cells, while
those from b to the apex of this same filament will later form a plurilocular
structure. Each densely cytoplasmic cell of such a filament divides by vertical
walls into first two (Fig. 18), then four (Fig. 20) cells. Further division is
irregular, and the position of the cross walls varies (compare Figs. 22 and 23).
Dividing nuclei were seen in longitudinal as well as transverse sections (compare
Figs. 21 and 25); this indicates that cell division occurs also in the vertical plane.
The mature plurilocular structure consists of numerous, small cells, approximately
4u square, each with very dense contents (Fig. 8f, etc.). The outer wall of the
whole structure is very much thicker than are any of the internal ones (Fig. 6).
It remains after the contents are shed and the inner walls mainly dissolved
(Fig. 7). Proliferation is common, i.e. new growth occurs at the base of the
empty case (Fig. 7).
Two extreme forms are found, one in which the plurilocular structure is
elongated, thin, cylindrical, and terminated by a fine hair. This form is stalked
and usually associated with acute-angle branching (Fig. 3). The other form of
plurilocular structure is short, thick, rather conical and not terminated by a hair.
This form is sessile and is usually associated with obtuse-angle branching (Fig. 8).
All gradations between the two exist. Both forms differ in the degree of division
in the topmost two or three tiers of cells (compare Figs. 9f and 10e). The size of
the mature plurilocular structure varies greatly.
Figure 6 shows how a stalked, terminal plurilocular structure (b) may become
sessile and lateral (a) through the growth of a lateral branch. The structures
shown in this figure are of a form which is approximately intermediate between
the extremes possible for this species. On rare occasions some portion of the
initial filament of the plurilocular structure may remain vegetative (Fig. 8d);
other abnormal examples show bending (Fig. 4) or branching (Fig. 5), which may
be due to injury.
Plants bearing unilocular reproductive structures are extremely rare, but those
that are found bear the structures abundantly. They are associated with the pluri-
locular structures on the same plant (Fig. 13a). They are oval in shape and
usually sessile, but they may possess a one-celled stalk (Fig. 12). Variations in
shape are shown in Fig. 13b. No burst or empty containers have been found.
The initial of the unilocular reproductive structures arises as a densely cyto-
plasmic cell (Fig. 28), in which a central vacuole is soon visible (Fig. 29). The
peripheral nuclei and plastids are at first indefinitely arranged (Fig. 30), but
later they become associated; each group contains a single nucleus and presumably
indicates a future zooid. At this stage the plastids are nearer the periphery than
are the nuclei (Fig. 31).
Hither type of reproductive structure is liable to occur in any season.
FIELD OBSERVATIONS.
Distribution.
General.—E. confervoides occurs in pools in the rock platforms of exposed
coastal headlands, and is never exposed to the air. These pools nearly all become
submerged at high tide and some extend downward at least to extra-low-tide
mark. During the season of most abundant growth, Ectocarpus was found inside
Sydney Harbour (Balmoral) and Broken Bay (near Church Point); these places
are more sheltered than the normal habitats.
542 ECTOCARPUS CONFERVOIDES,
E. confervoides has been found in all its forms on Hormosira Banksii, which
is at all times the most common host. Similar forms grow also on rocks and wood,
and on various other plants, including Ulva, Colpomenia, Ecklonia, Zonaria,
Dictyota, Sargassum, Blossevillea, Amphiroa and Corallina species. From this it
appears that Ectocarpus in the Sydney district is not dependent on any particular
host or hosts. Knight reports (1923) a definite host correlation in Pylaiella
litoralis through the season, while Papenfuss (1935) indicates the presence of an
E. siliculosus—host relationship which is obligate in the case of the sexual plant.
Seasonal.—During the course of a year there occurs a marked rise and fall in
the abundance of Hctocarpus. The maximum abundance occurs about March to
April. It is, however, fairly prevalent from January to June and it is possible
to find plants at all times of the year in pools which are exposed at low tide for
only a very short time. As conditions become favourable a progressive upward
migration occurs, the plants occupying positions which are exposed at low tide
for increasingly longer periods. As EH. confervoides increases in abundance, it
appears on any plants which happen to occur in suitable pools. Thus the seasonal
change is related to conditions of the pools and not to distribution of a host.
Later in the season the amount of Hctocarpus diminishes, the last remaining
plants being limited to: (1) Deep pools, in which tufts of Hctocarpus occur
occasionally; (2) Extensive, shallow, cliff-sheltered pools, in which Hctocarpus
grows lithophytically; (3) Pools exposed for very short periods at low tide. This
zone probably extends below the lowest tide mark, and is the only permanent
habitat of H. confervoides.
Local distribution may be affected by a storm, the plants on occasion being
smothered by sand.
As EH. confervoides grows both on rocks and on Hormosira Banksti, which is
plentiful throughout the year, the changes in its abundance are not connected with
substrate. As the permanent habitat is rarely, if ever, exposed between tides, it is
thought that seasonal migration may be connected with changes throughout the
year in the conditions experienced during exposure. WHctocarpus plants in pools
which are exposed during the day frequently exhibit a reversible plasmolysis, due,
no doubt, to increased salinity of the pool water.
Bursting of the Plurilocular Structures and Development of Zooids.
Plurilocular reproductive structures at all stages of development may be found
together. No factor could be correlated with the liberation of zooids, despite an
analysis of the habitat-factors during twenty-four hours of HE. confervoides plants
growing in a pool at Narrabeen headland. Artificial methods which cause bursting
are described by Knight (1929); these were not used by the writer.
The bursting of a plurilocular structure commences by a tear which appears
at the apex, and the contents are freed in sudden bursts through this. The internal
walls have previously been dissolved. After the zooids of the upper half have been
freed, the rate of liberation becomes more rapid for a time; later, however, the
rate decreases progressively. Usually about five zooids remain permanently .inside
the encasing wall. The rounded zooids within the plurilocular structure become
elongated during a laboured passage through the aperture; they then escape
rapidly and again assume their rounded form. These rounded, freed zooids form
a dense ellipsoidal or spherical mass at the mouth of the bursting structure. The
outer zooids of this mass soon become pyriform and active, cilia and an eye-spot
are now distinguishable in addition to the chromatophores and pyrenoids. Knight
(1929) reports that there are two chromatophores in each swarmer. Kylin (1933)
BY VALERIE MAY. 543
says there is usually only one. As cells of the adult plant may contain one to
humerous chromatophores (Figs. 8b and 10a) no importance need be attached to
the number in the zooid. Each zooid rotates before moving away, and it retains
this rotation throughout its motile stage. The motile zooids tend to radiate from,
not congregate about, the plurilocular structures. On loss of motility, the zooids
again become rounded. The time taken for these processes appears to vary. The
inside of the empty outer wall of a plurilocular structure shows highly refractive
protuberances; these mark the position of former main cross-walls. Very small,
‘circular structures, apparently of the same substance, are freed with the zooids.
The size of the zooids, before and after motility, is usually constant. A series
of them showing progressively greater size may, however, be found on occasion.
The greater size is due to the presence of a greater volume of cytoplasm than is
normal. It is suggested that the variation in size of these zooids depends upon the
irregularity in the divisions of the plurilocular structures before bursting, and is
in no wise connected with fusion. Equally large zooids may be found at the mouth
of or inside the plurilocular structures. The inequality of size of the divisions of
the unburst structure is shown in Figure 9e.
No sign of fusion of the zooids was ever observed, so that the zooids of the
plurilocular structures function as zoospores, reproducing the plant asexually.
The resting zoospore has a thin enveloping wall. On germination, the contents
pass out of this to form a rounded mass, from which a filament later arises. This
produces a branching system of prostrate and upright filaments (Fig. 14). In
some instances the substrate may be the parent plant, but it is thought that such
epiphytes do not develop to maturity. Sometimes a loosened zoospore may
germinate within the encasing walls of a plurilocular zoosporangium. Material
kept in the laboratory in tanks showed the development of unloosened zoospores
(aplanospores) from within the zoosporangium; the filaments grew freely through
the surrounding walls. A similar development in another species has been seen
under natural conditions. Kylin (1933) describes the development of #. siliculosus
in detail.
Host RELATIONSHIPS.
Parasitism has been reported in H. Padinae Sauv. by Sauvageau (quoted by
Williams, 1925); this suggested the advisability of an investigation of
E. confervoides from this point of view. Plants of Hormosira Banksii (Turn.)
Decne. and Colpomenia sinuosa (Roth) Derb. and Sol., on which H. confervoides
was growing, were examined in section. The methods used in fixation, staining,
etc., are described under the heading ‘‘Cytology”.
In Colpomenia the large, central cells were unaltered, but the arrangement of
the small, epidermal cells was disturbed by the filaments of the Ectocarpus. In all
cases the filaments of Hctocarpus appear to pass between the epidermal cells,
displacing them, but no case has shown the development of haustoria, and there
is no close apposition between the cells of the two plants (Figs. 32 and 33). We
may say, then, that HE. confervoides on C. sinuosa behaves as an epiphyte, the basal
portions of which are endophytic.
The results obtained in the case of Hormosira were rather more unusual. The
epidermal cells of this plant develop a thick, cuticle-like layer to their outer wall.
This layer is periodically shed, a new one replacing it (Fig. 37). A cast of the
cell detail of the plant surface is retained usually by the portion shed. Successive
layers may remain superimposed on the plant (Fig. 36). When epiphytes, often
including Hctocarpus, are present on the surface of the “cuticle” they are shed with
5A4 ECTOCARPUS CONFERVOIDES,
it (Fig. 37). However, Hctocarpus is able sometimes to continue growth through
the “cuticle” layers as they are produced (Figs. 34, 35). This character, as well
as re-infection, accounts for the continued growth of Hctocarpus on Hormosira
throughout the season. In portions of Hormosira bearing Ectocarpus, occasionally
there is no sign of the cuticle-like layer. In these parts, the large, inner, cortical
cells of Hormosira lie nearer the surface, and the epidermal cells are rather more
loosely arranged than usual. These portions may be termed Hctocarpus-galls
(Figs. 38, 39). No haustoria have been observed, nor is there very close associa-
tion of the cells of the two plants, so that parasitism does not seem indicated. The
presence of foreign filaments within the “cuticular” surface apparently suffices to
cause Hormosira to develop loose-celled galls, on which the “cuticle” layer is no
longer formed. Figure 38 shows the change from normal to a gall.
It appears that from both Colpomenia and Hormosira, E. confervoides gains
position but not nutrition, penetration of the outer layers of the host being
endophytic, not parasitic. This conclusion is supported by the abundant growth
of the same plant on rocks. Furthermore, parasitic algae are usually associated
(Setehell, 1914) with specific hosts; this is certainly not the case here.
CytToLoGy AND LirrE History.
Method.—Cytological details were obtained from the non-haired variety of
E. confervoides. This is the more common form in the Sydney district. The
plants examined were mainly epiphytes on H. Banksii; those growing on C. sinuosa
were found to possess the same number of chromosomes. Since the forms of
E. confervoides found on various hosts (e.g. Ulva, Colpomenia, Ecklonia, Zonaria,
Dictyota, Sargassum, Blossevillea, Amphiroa, and Corallina species) correspond
microscopically to plants growing on H. Banksii, it appears highly probable that
they are cytologically identical. A morphological difference has been reported as
accompanying a difference in the number of chromosomes, when this has been
_ found within the species H#. confervoides (Papenfuss, 1935).
After fixation in 1% chrom-acetic acid in salt water, the material was washed
well and then was embedded in paraffin. Sections for the study of host relation-
ships were cut at thicknesses up to 64; for nuclear detail the most satisfactory
thickness was 3u. Staining presented many difficulties. There is very little
differentiation shown by Hctocarpus when treated with the usual combinations of
stains. The cleanest and clearest staining obtained was that given by magdala red
and aniline blue, the sections being left for some days in the magdala red. Iron
alum-Haematoxylin-light green was the staining combination used for confirmation
of the chromosome number.
Observations.—In material treated as described above, the pyrenoid bodies and
the nucleus appear more prominently than they do in the living state. The
nucleus, except for the nucleolus, appears nearly uniform, and lightly-stained. The
single nucleolus stains most heavily at its periphery; inside this band there may
be one, two, or three colourless areas (Figs. 16, 17).
The cell detail is shown more clearly by the vegetative than by the repro-
ductive cells. In some cases interpretation of the cell contents of the chambers
of the plurilocular structure is almost impossible because of the small size, dense
protoplasm, and especially the uniformity of staining.
The diameter of the nucleus usually measures approximately 3-6u, that of the
nucleolus 1:8u. Serial sections 3u thick showed all necessary nuclear detail in the
one section.
BY VALERIE MAY. 5A5
The chromosomes are only slightly elongated, if not spherical. They are very
small, but it is possible to count them, especially when at the metaphase stage of
division.
The chromosome number in the normal vegetative cell (Fig. 15) and in the
plurilocular zoosporangium (Figs. 21, 22, 25) is 16, so that the asexual zoospores
also have 16 chromosomes. Meiosis occurs during the formation of the unilocular
reproductive structure, so that the daughter nuclei and the zooids each carry the
haploid number of chromosomes (Figs. 30, 31). The figures given here are
similar to those of Knight (1929).
Fig. 15.—Longitudinal section of a vegetative cell showing mitosis. x 1,360.
Fig. 16.—Longitudinal section of a vegetative cell showing a resting nucleus.
Nucleolus has two light areas. x 1,360.
Fig. 17.—Transverse sections of vegetative cells showing variation in size. The
peripheral arrangement of the chromatophores in the cytoplasm is illustrated. The
nucleolus contains one (a) or two (b) clear areas within it. x 1,360.
Fig. 18.—Transverse section of an initial of a plurilocular structure, after the forma-
tion of the first vertical wall. x 1,360.
Fig. 19.—Transverse section of an initial of a plurilocular structure, after the forma-
tion of the second vertical wall in one cell only. ‘This view is less common than that
shown in Fig. 20. x 1,360.
Fig. 20.—Transverse section of a plurilocular reproductive structure after the forma-
tion of the second vertical wall; one quadrant shows a nucleus dividing. x 1,360.
Fig. 21.—As Fig. 20. x 1,360.
Fig. 22.—Transverse section of a plurilocular reproductive structure at a later stage
than shown above, further vertical walls having formed. Nuclear division is shown.
x 1,360.
Fig. 23.—This figure shows a different order in the formation of vertical walls from
that shown in Figure 22. x 1,360.
546 ECTOCARPUS CONFERVOIDES,
Fig. 24.—A longitudinal section of an initial. of a plurilocular structure. at the
filament stage. The cells which are about to divide actively (from b to apex) can be
distinguished from the normal vegetative cells (c to b) by their dense contents, especially
cytoplasm. Wall formation is incomplete at a. x 1,360.
Fig. 25.—Longitudinal section of a plurilocular reproductive structure, in which
mitosis is shown. There are sixteen chromosomes. x 1,360.
Fig. 26.—Longitudinal section of a young plurilocular reproductive structuré. x 1,360.
Fig. 27.—A selection of chromatophores and associated pyrenoids from a single cell.
x 1,360.
Fig. 28.—Transverse section of an initial cell of a reproductive structure. It is
distinguished from a vegetative cell (see Fig. 24) by the dense cytoplasmic contents. As
the nucleus is resting, the cell could be the initial of a uni- or a plurilocular structure.
an Os ;
Fig. 29.—Transverse section of a unilocular structure showing three nuclei. Wacuole
formation is apparent. The proportion of cytoplasm to vacuole is much greater here than
in a more mature structure (compare Fig. 30b). In one nucleus chromosomes are visible.
It is unusual for division in a unilocular structure not to be simultaneous (compare with
Figs. 30 and 31). x 1,360.
BY VALERIE MAY. 547
From the above it appears that the plant is diploid (2n = 16); it reproduces
asexually by means of diploid zoospores which are developed from plurilocular
reproductive structures. Very rarely unilocular reproductive structures are
developed from this diploid plant; this development is associated with meiotic
division, so that the zooids produced are haploid, each carrying eight chromosomes.
Life History.—It has been shown above that the diploid plant gives rise freely
to diploid zooids (from plurilocular structures) and, very rarely, to haploid zooids
(from unilocular structures). Zooids from the plurilocular structures (zoosporangia)
develop asexually, i.e. are zoospores. Zooids from the unilocular structures have not
been observed by the writer. These zooids occur so rarely that their function
must be of relative unimportance in this life history. A survey of the relevant
literature (see below) suggests that their behaviour may be variable. Cytological
evidence suggests they could either (1) fuse, and then produce the usual diploid
plant, or (2) develop directly to a haploid soma (as yet not found in the field).
This soma would be another phase of the life history and would finally give rise
to cells capable of fusing and so reforming the normal diploid plant; asexual
reproduction of this hypothetical soma would, of course, be possible. If reduction
division followed the formation of a zygote, the result would be the same as if the
.20ooids had developed without fusion; but a case narallel to this is unknown
in the Melanophyceae so far.
It is unlikely that haploid plants occur within the district (Five Islands,
Wollongong, to Palm Beach) examined by the writer. The examination of a wider
area may disclose their existence, though material collected from some dozen places
between Sydney, N.S.W., and Brisbane, Qsld., appeared identical with that which
was found near Sydney.
No plants of H. confervoides which differ morphologically or cytologically
from those described in this paper have been found by the writer at any season,
and there appears to be no relationship between EH. confervoides and its substrate.
This differs from where (Papenfuss, 1935) an n and 2n soma have been found.
Further, there is no seasonal drift from host to host, as was found in Pylaiella
litoralis (Knight, 1923).
Kylin (1933) said: “Dass diese Pflanzen, wenn sie an der schwedischen
Westkiiste tiberhaupt lebensfahig sind, besonders selten vorkommen, kann gar nicht
Wunder nehmen, da unilokul4re Sporangien so selten sind’, and “Wegen einer
reichen vegetativen Vermehrung der diploiden Generation mittelst Schwarmer aus
diploiden plurilokularen Sporangien ist aber der Generationswechsel weggefallen,
und tibrig bleiben dann nur diploide Individuen.” These statements could well
apply to the Sydney district.
The life history described above may be expressed diagrammatically as in
Figure 44. The dotted line shows both methods of development possible for the
haploid zooids from the unilocular structures.
This diagram may now be compared with other published results of Ectocarpus.
Discussion —Knight (1923) has shown the life history of Pylaiella litoralis to
be one of fluctuating alternation with similarity of form. The diploid plant is the
Fig. 30.—a and b show longitudinal sections of vacuolated unilocular structures
undergoing simultaneous nuclear division, eight chromosomes appearing in each nucleus.
a is a surface section. Serial sections show seven peripheral nuclei in the next section
and two surface ones (as here) in the third. b is a more median section than a, and
shows the vacuole occupying a central position. ec shows an initial of a plurilocular
structure (ii) associated with unilocular structures (i). (a, b, x 1,360; c, x 216.)
Fig. 31.—As Fig. 30 a and b, but an association of nuclei with chromatophores is
suggested. x 1,360.
548 ECTOCARPUS CONFERVOIPES,
<0 As
Ba
1,
Nowses
BEER
=
a
Fig. 32.—e Longitudinal section of a fold in Colpomenia sinuosa. The epidermal zone
is disturbed by filaments of Ectocarpus, while the large central cells are unaltered.
b shows a surface section of this same fold and so more detail of the narrow epidermal
zone is obtainable. x 76.
Fig. 33.—This is the central portion of the tissue shown in Fig. 32b. The filaments of
Ectocarpus only are shown in cell detail. The loose arrangement of the tissues is clearly
shown. There is no sign of parasitism. x 316.
Fig. 34.—Penetration of the ‘cuticle’ of Hormosira Banksii by filaments of
Ectocarpus. x 204.
Fig. 35.—As Fig. 34, but the tip of the penetrating filament is flattened into a
“holdfast”. x 204.
Fig. 36.—Transverse section of the thallus of Hormosira Banksii showing shed
“cuticle” layers. x 264.
Fig. 37.—As Fig. 36, but epiphytic Hctocarpus is being shed with the ‘“‘cuticle’’. x 264.
Fig. 38.—Longitudinal section of a gall on Hormosira Banksii. As in Figs. 34, 35
and 39, the “‘cuticle’’ is shown as black. The large-celled, central tissue of Hormosira
protrudes towards the surface. Filaments of Ectocarpus and epidermal cells of
Hormosira are associated in the gall. The apparent difference in the thickness of the
“cuticle” on either side of the gall is due to the ‘cuticle’ having been torn loose in one
casey x) 60:
Fig. 39.—The edge of a gall is shown in detail; penetration of the “cuticle” by
filaments of Hctocarpus. is illustrated. x 264.
BY VALERIE MAY. 549
more prevalent and reproduces itself asexually by zooids which are formed in the
plurilocular zoosporangia. Reduction occurs in the first division of the unilocular
gametangium, whose haploid zooids either straightway fuse (Knight, 1929), and
presumably give rise to the diploid plant or, much more generally, form a haploid
soma (Knight, 1923). The plurilocular structure of the haploid soma gives rise to
gametes which either fuse, then give rise to the diploid plant, or develop asexually
to produce anew the haploid soma. Diagrammatically this may be shown as
Figure 40.
Papenfuss (1935) has summarized the contradictory reports of early workers
regarding the behaviour of zooids of H. siliculosus. Sauvageau (1896-7) and
Kuckuck (1891-1912) held that the zooids of the plurilocular structures were
asexual. Kuckuck (1891) and Reinhardt (1884) reported the zooids of the
unilocular structure as asexual. Oltmanns (1899) reported that sexual zooids were
produced from the plurilocular structures. Detailed work on this species has been
done by Berthold (quoted by Knight, 1929); Knight (1929); Kylin (1933); Fdéyn
(1934), and Papenfuss (1935).
Plants collected at Naples by Berthold were haploid, with eight chromosomes
(Knight, 1929). Their plurilocular structures produced gametes which usually
fused before further growth, but which could develop asexually. The culture
obtained from the products of the plurilocular structures contained small plants,
some bearing plurilocular structures only (plants, haploid, i.e. from the unfused
zooids?), others bearing pluri- and unilocular structures (plants developed from
zygotes?). It may be that reduction occurs in the diploid unilocular structure,
the zooids produced then giving rise to the usual haploid plants. Unfortunately,
work was not continued on these cultured plants; their cytology was not
investigated.
Knight (1929) reaffirmed the sexual nature of the zooids described by
Berthold, and determined the chromosome number (eight) of the plants which
grow freely near Naples.
Bjgrn Fgyn (reported by Fdyn, 1934) repeated and extended the investigation
of Berthold. Gametes from plurilocular structures of plants of different sex were
mixed and copulation occurred. Zygotes, with which were associated a few female
gametes, were then cultured. Plurilocular structures on the resultant plants gave
rise to asexual zoospores. Zooids from unilocular structures (which might occur
on plants which bore plurilocular structures) also germinated directly.
F¢éyn summarizes thus: ‘Hs ist bei dem neapler Material ein Genera-
tionswechsel vorhanden zwischen einer haploiden sexuellen Generation, die nur
pluriloculare Behaiter erzeugt, und einer diploiden, vegetativen Generation mit
zwei Sorten von Behaltern: pluriloculare mit diploiden Schwérmern und
uniloculare mit haploiden Zoosporen. Dass Gameten, die nicht zu Kopulation
kommen, sich parthenogenetisch entwickeln kénnen, hat schon Berthold gezeigt,
dass die sich direkt zu Geschlechtspflanzen entwickeln, wissen wir von Hartmann
(1929).”
It is highly probable that the diploid plant, readily obtained in culture, occurs
naturally at Naples. As Papenfuss (1935) says: “. . . it is evident that such
plants exist there. Both Berthold and Oltmanns observed “neutral” spores from
plurilocular sporangia, and Oltmanns states that these are generally larger than
the gametes, facts which indicate that these zoids were diploid zoospores.”
A diagrammatic scheme is shown in Figure 41.
The results obtained by Knight at Port Erin were that the plants were
diploid (sixteen chromosomes) and gave rise to asexual zoospores from the
550 ECTOCARPUS CONFERVOIDES,
plurilocular structures. Reduction occurred in the first division of the unilocular
structures, the zooids thereof (each with eight chromosomes) fusing after libera-
tion. The zygote produced the normal, diploid plant. Diagrammatically this may
be represented as in Figure 42.
The main difference between these two sets of results is that the prevalent
plant was haploid in one case and diploid in the other; also that the plurilocular
structures gave rise to potentially sexual zooids in one case and to asexual zooids
in the other.
Figure 45 is a theoretical scheme showing the range of development possible
in the complete life cycle of Ectocarpus confervoides. In certain localities, phases
of the life history may be absent. The form of the life history occurring at any
one place may be determined by the habitat there. This scheme would account
for the existence of conflicting reports.
Kylin (1933), at Kristinberg, found individuals of E. siliculosus (presumably
diploid), which bore plurilocular structures. The swarmers from these developed
directly to new individuals, which were morphologically the same as the parent
plant. Unilocular structures occurred extremely rarely and never in his cultures;
when present they either occurred alone or were associated with the plurilocular
structures. No haploid plants were found. Kylin says: “. . . erklare ich den
Wegfall des Generationswechsels mit einer vegetativen Vermehrung der vorhan-
denen diploiden Individuen mittelst diploider rein vegetativer Schwarmer aus
diploiden plurilokularen Sporangien.” As in the plant cycle as lived at Sydney,
the products of the unilocular structures are negligible, and Kylin says further
(1933): “Primar liegt meiner Meinung nach bei Hctocarpus siliculosus an der
schwedischen Westktiste ein Generationswechsel mit zwei einander morphologisch
gleichen Generationen vor. Wegen einer reichen vegetativen Vermehrung der
diploiden Generation mittelst Schwarmer aus diploiden plurilokularen Sporangien
ist aber der Generationswechsel weggefallen, und tibrig bleiben dann nur diploide
Individuen.” These results are shown in Figure 44.
Papenfuss (1935), at and near Wood’s Hole, found both haploid (eight
chromosomes) and diploid (sixteen chromosomes) plants. The haploid form was
represented only at Penikese Island, 20 miles from Wood’s Hole, while the diploid
plants occurred also at Wood’s Hole itself. The more common plant was the
diploid, and it bore both unilocular and plurilocular structures. Zooids formed in
the plurilocular zoosporangia were asexual. Meiosis occurred during the develop-
ment of the unilocular structures; the zooids produced from these gave rise to
the haploid soma. The haploid plant was inferior to the diploid in size, length of
cells, and size of plurilocular structures. These reproductive structures produced
gametes, all those from one plant being of the same sex. The male and female
gametes both varied greatly in size; so, as a result, did the zygotes. The zygote
developed into the normal diploid plant. Parthenogenetic development of either
gamete led to the re-formation of the haploid plant. This scheme is represented
diagrammatically in Figure 43.
Foéyn (1934) at Herdla, obtained results which are in agreement with those of
Papenfuss.
This life history differs from that reported by Knight (1929) in the behaviour
of the haploid zooids produced in the unilocular structures. Papenfuss suggests
that this difference is due to a misinterpretation by Knight. Kylin (1933) also
criticizes Knight’s work and thinks that the copulation described by her was
merely the blundering and sticking together of asexual zooids. Knight describes
fusions as being rare and associated with clump formation, the fusing zooids
BY VALERIE MAY. 551
both being motile and taking about 20 minutes to coalesce. In contrast, Papenfuss
states that the fusions between zooids from the haploid plurilocular gametangia are
numerous, the female zooids are non-motile at fusion, clump formation does not
occur, and the time of fusion is less than half a minute. He suggests Knight’s
observations were of abnormalities and that both localities present life histories
identical with that reported from the United States of America. Papenfuss reports
that the haploid plant was absent if the specific host were not present. This fact
may account for. Knight’s failure to find this form at Port Erin, if indeed it does
form part of the life history in Britain.
Reduction
Habloid
ae
4
\
’ eens
\ Fusions. 1
' \’
i Wa
A Oy
© ! :
a Te Qe;
Reduction Reduction 44
Reduchion, .
Fig. 40.—Pylaiella litoralis, Port~Erin (Knight). Haploid and diploid plants are
morphologically identical and are most abundant at different seasons.
Fig. 41.—Ectocarpus siliculosus, Naples (Berthold, Knight, and Fgyn).
The haploid
plant occurs naturally.
The diploid plants were produced in culture by Berthold and,
later, by F¢yn; if this soma occurs naturally, the life history is the same as that shown
in Figure 438.
Fig. 42.—Hctocarpus siliculosus, Port Brin (Knight).
Haploid plants absent (or
missed ?).
Fusion of haploid zooids questioned by Papenfuss (1935) and Kylin (1933).
Fig. 43.—Ectocarpus siliculosus, Herdla (Fgyn), Wood’s Hole (Papenfuss). The
haploid plants are smaller than the diploid, and they bear male or female gametes. No
fusion of zooids from unilocular reproductive structures was noted. The haploid plants
are absent if the specific host is not present.
Fig. 44.—Hctocarpus confervoides (= siliculosus), Kristinberg (Kylin), Sydney (May).
Unilocular reproductive structures are extremely rare, and the behaviour of the haploid
zooids is unknown. A haploid soma has not (yet?) been seen.
Fig. 45.—Hctocarpus confervoides (= siliculosus), theoretical scheme.
scheme includes all reported forms of the life history.
either sexually or asexually.
occur.
This theoretical
Any haploid zooid may develop
In certain localities a phase of the life history may not
552 ECTOCARPUS CONFERVOIDES,
Whether the Port Erin—Wood’s Hole life-histories are the same or not, all
reported life-histories of H. confervoides (including EH. siliculosus), including that
presented in the present paper, fit the scheme given in Figure 45.
Great differences exist in the proportion of haploid to diploid phases in the
life cycle—the relative importance of any phase varying with locality. At Naples
conditions favour the haploid plant (diploid not yet recorded as occurring
naturally); at Port Erin, Kristinberg, and Sydney, they favour the diploid (haploid
occurring rarely, if ever) and at Wood’s Hole and Herdla the balance between the
haploid and diploid phases is more even—both occurring relatively commonly. We
do not know yet what factor or factors control these relative proportions, except
that at Wood’s Hole the occurrence of the haploid phase is known to be dependent
on the presence of a specific host. In those localities where a haploid soma has
not been found, unilocular structures are very rare. Papenfuss (1935) says: “The
absence of the sexual generation of Ectocarpus in certain localities is due,
undoubtedly, to an effect of the environment which inhibits the formation of
unilocular sporangia. ... It is probable that a very slight difference in the environ-
ment may determine the absence of unilocular sporangia, for the writer found that
asexual plants growing on Spartina at Grassy Island bore plurilocular sporangia
only, while the plants which grew on Chorda in the same locality but in slightly
deeper water, bore both plurilocular and unilocular sporangia.”
The problem now existing is to find what conditions are responsible on one
hand for the production of an abundant crop of unilocular structures as against
where there is an almost complete inhibition of the formation of these reproductive
structures. In the first case, an alternation of haploid and diploid somas occurs
40",
36°55
gms./litre.
3s"
20°C.
Water
temperature.
Lge
30", 36°35
gms./litre.
Air
18°C. temperature,
25"
20"
5 36-15
it gms ./litre.
Salifity of|Water.
15 s | \\
15°C 1 35-95
' \ gms. /litre.
!
Depth 4 } '
youp4ticf 1! / ' d
Water, ! 1 , 1
above \ ! ,
Plants. , f ‘ \
Ai \
we PA b+ \ 35-75
3° 1 ; ! \ gms./litre.
lm 1 i : ' vA
n \ ! (\ /
2u ¥ Vv 1 Vey if.
Y OC) a Rao es eee as) Nee [on Aer Ente ie ol —4 AY +t
o" - Water not moving. Water not moving.
Oe Darhness| OSS “G55
WO, BY U2) eget, Sed Sy 6l ei BE 7192 10) SEM BAL 2) Sy APS Rey ir ia gtion i Eeemeey Bitre:
A.M. Yoon Midnight AM.
Fig. 46.—An analysis of the habitat factors for twenty-four hours (April 25-26, 1936)
of #. confervoides growing in a rock pool at Narrabeen headland, near Sydney.
)
BY VALERIE MAY. 553
(e.g. Wood’s Hole, Herdla, and probably Naples), while in the second case the
alternation of generations is overwhelmed and there remain no, or practically no,
haploid individuals (e.g. Port Erin, Kristinberg, and Sydney).
The only evidence we have as to the conditions favouring the formation of
unilocular structures on asexual plants is that given by Papenfuss (1935) and
quoted above, i.e. that slightly greater depth (or specific hosts?) favours the
formation of unilocular structures. The fact that F¢yn, at Herdla, Norway, has
reported the occurrence of haploid plants, and Kylin, at Kristinberg, Sweden, has
been unable to find these, suggests that the form of the life cycle is determined by
relatively local factors.
It would be most advantageous if one could compare the conditions under
which H#. confervoides thrives in those localities in which it has been studied. To
facilitate this comparison, there is given here, in graph form (Fig. 46), an analysis
for 24 hours of the habitat of H. confervoides on the coast near Sydney at the
season of its maximum prevalence.
SUMMARY.
1.—An investigation has been made of H. confervoides found growing on the
coast near Sydney, N.S.W.
2—A systematic examination led to H. siliculosus (Dillw.) Lyngb. being
regarded as merely a variety of H. confervoides (Roth) Le Jol.
3A seasonal migration up and down the rock platform is reported.
4—Host relationships have been investigated. H. confervoides has been shown
to be slightly endophytic in Colpomenia sinuosa and Hormosira Banksii. In the
latter, curious gall-formations are formed.
5.—A cytological investigation has been carried out on H. confervoides found
growing near Sydney. The chromosome numbers are 16 and 8; all plants found so
far are diploid; reduction division occurs in the unilocular structure. Asexual
zoospores from plurilocular reproductive structures may, under artificial conditions,
act as aplanospores.
6.—A discussion is given of the life cycle of H. confervoides as reported from
various localities. The conditions under which it flourishes near Sydney are
noted in order to facilitate comparisons.
Work described in this paper was performed by the writer while holding a
Caird Scholarship (1936) and a Science Research Scholarship (1937).
This investigation was carried out under the supervision of Assistant Professor
J. McLuckie, University of Sydney. Thanks are also due to Dr. L. Fraser,
University of Sydney, for her assistance and encouragement, and to Professor J.
Turner, University of Melbourne, for his criticism of the manuscript.
References.
Fern. B. Ruup, 1934.—Uber den Lebenscyklus einiger Braunalgen. Bergens Mus. Arbok.
Naturvidensk. rekke, Nr. 2, 1-9.
HARTMANN, M., 1925.—Untersuchungen Uber relative Sexualitat. 1. Versuche an
Ectocarpus siliculosus. Biol. Zentralb., 45, 449-467.
KNIGHT, MARGERY, 19238.—Studies in the Hctocarpaceae. ils The Life-history and
Cytology of Pylaiella litoralis Kjellm. Trans. Roy. Soc. Edin.. 53, 343-360, Pls. 1-6.
————,, 1929.—Studies in the Ectocarpaceae. 2. The Life-history and Cytology of
Ectocarpus siliculosus Dillw. Trans. Roy. Soc. Edin.. 56, 307-332, Pls. 1-6.
KYLIN, HaRALp, 1933.—Uber die Hntwicklungsgeschichte der Phaeophyceen. Lunds Univ.
Arsskrift., N.F. Avd. 2, 29(7), 1-102, Taf. 1-2.
MATHIAS, W. T., 1935.—Life History and Cytology of Phloeospora brachiata Born. Publ.
Hartley Bot. Lab., No. 138, 3-33.
Ss
554 ECLOCARPUS CONFERVOIDES.
May. VALERIE, 1938.—A Key to the Marine Algae of New South Wales. Part 1.
Chlorophyceae. Proc. LINN. Soc. N.S.W., 63, 207-218.
PAPENFUsSsS, G. F., 1935.—Alternation of Generations in Ectocarpus siliculosus Dillw. Bot.
Gaz.. 96, 421-446, Pls. 6-7.
SETCHELL, W. A., 1914.—Parasitic Florideae. 1.
Pls. 1-6.
and GARDNER. N. L., 1925.—The Marine Algae of the Pacific Coast of North
America. Part 3. Melanophyceae. Univ. Calif. Pwbl. in Bot., 8, 383-898, Pls. 34-107.
WILLIAMS, J. Luoyp, 1925.—The Phaeophyceae and their Problems. Brit. Ass. Adv.
Pres. Add. Sec. K. Southampton. 182-196.
Univ. Calif. Publ. in Bot.. 6, 1-34,
Sct...
559
A NOTE ON THE RE-EXAMINATION OF AUSTRALIAN SPECIES OF
CERATOPOGONIDAE (DIPTERA).
By J. W. S. MAcFIr.
(Communicated by Frank H. Taylor, F.R.ES., F.Z.8.)
(Three Text-figures. )
[Read 25th October, 1939.]
In 1889 Skuse described 17 species of Ceratopogonidae collected in Australia.
Thanks to the courtesy of Mr. A. R. Woodhill and Mr. Frank H. Taylor, I have
been permitted to re-examine one or both sexes of 6 of these species, namely those
named by Skuse Ceratopogon subnitidus, sydneyensis, marmoratus, molestus,
aeratipennis, and minusculus, and also the type material of Culicoides multi-
maculatus Taylor and C. townsvillensis Taylor.
Two of these species, namely C. marmoratus and C. molestus, are Culicoides,
and should be recognizable from the figures of the wings given by Skuse. The
descriptions of the others, published fifty years ago, are not sufficiently detailed to
enable the insects to be recognized now, or to be separated from other species of
the same genera. They are, indeed, insufficient to indicate to what genera the
insects belong, and thus Kieffer (1917) supposed all four to be Culicoides, whereas
in fact one is Forcipomyia, one Apelma, and two Dasyhelea.
The brief notes which follow may assist in the recognition of these species.
FORCIPOMYIA SUBNITIDA (Skuse).
Proc. Linn. Soc. N. S. WALES, xiv, 1889, 299.
This insect is a Forcipomyia, not a Culicoides as Kieffer (1917) supposed.
Dickinson and Hill (1916), and McEachran and Hill (1916) have referred to this
species in connection with their work on Onchocerca gibsoni, but as it is a
Forcipomyia this reference requires confirmation. The male (which is not known)
is more likely to show characteristic features, but the following details about the
female may assist recognition.
2. Head with palpi rather dark brown, third segment with deep pit of
moderate size. Antennae dark brown, segments forming an almost continuous
series: 4-14 from sub-spherical to flask-shaped, ranging from about 9 by 9 to
10 by 7 (maximum) units;* 15 about 15 (including nipple-like stylet of about
3 units) by 6 units. Thorax and scutellum very dark brown or blackish. Wings
unadorned, as shown in Skuse’s figure. Legs with femora and tibiae uniformly
dark brown, tarsal segments (excepting last which is infuscated) paler brown.
Knees not pale. No tibial spines. Without scales. T.R. about 2. Abdomen very
dark brown or blackish; without scales. Spermathecae two, highly chitinized,
pyriform, subequal; total length about 70u and greatest breadth 45z.
* The unit used is approximately 3-5u,
556 AUSTRALIAN SPECIES OF CERATOPOGONIDAER,
APELMA SYDNEYENSIS (Skuse).
Proc. Linn. Soc. N. S. WALES, xiv, 1889, 302.
This insect is now much damaged and lacks the hypopygium. It is a species
of Apelma, not a Culicoides as Kieffer (1917) supposed, but in its present condition
shows no clear means by which it might be distinguished from other known
species.
CULICOIDES MARMORATUS (Skuse).
Proc. Linn. Soc. N. 8S. WALES, xiv, 1889, 304.
This insect is a Culicoides, and should be readily recognized by the adornment
of the wings. The male (which is not known) may furnish additional diagnostic
characters. The following details about the female may facilitate recognition.
©. Head with palpi very dark, third segment longer than fourth and fifth
together, with a small sub-apical pit. Antennae brown: segments 4-10 from
sub-spherical to oval, ranging from about 10 by 10 to 11 by 8 units; 11-14 more
elongate, ranging from about 16 by 8 to 21 by 9 units; 15 about 31 by 8&8 units,
without stylet. The combined lengths of segments 3-10, 4-10 and 11-15 about 88,
73 and 105 units respectively. Wings densely clothed with macrotrichia which,
indeed, cover almost the whole surface. Adornment as shown in Skuse’s figure.
The pale spot just beyond end of costa is double; that enveloping cross-vein rather
small, covering only base of first radial cell. Legs with femora and tibiae uniformly
dark brown. Knees not pale. T.R. about 2:1. Fourth tarsal segments not cordiform.
CULICOIDES MOLESTUS (Skuse).
Proc. Linn. Soc. N. S. WALES, xiv, 1889, 305.
This insect is a Culicoides, and should be recognizable by the adornment of the
wings, and the cordiform fourth tarsal segments. The male (which is not known)
may furnish additional diagnostic characters. The following details about the
female may facilitate recognition.
°. Head with antennae brown: segments 4-10 from sub-spherical to shortly
oval, ranging from about 8 by 7-8 to 9 by 7 units; 11-14 slightly longer, ranging
from about 11 by 6-7 to 14 by 6 units; 15 about 21 by 7 units, without stylet.
The combined lengths of segments 4-10 and 11-15 about 57 and 72 units
respectively. Wings with macrotrichia rather scanty, mostly at tip. Adornment as
shown in Skuse’s figure, but in the specimen examined by me the pale spot
enveloping cross-vein larger, covering proximal half of first radial cell, and the
spot between branches of Cu more central, not abutting on Cu, Legs darkish
brown with paler knees. T.R. about 2:2. Fourth tarsal segments cordiform.
CULICOIDES MULTIMACULATUS Taylor. Fig. 3.
Aust. Zoologist, i, pt. 6, 1918, 169. ;
Thanks to the kindness of Mr. F. H. Taylor, I have had the opportunity to
examine two females of this species, the type and another specimen taken with it.
A few details may therefore be added to the original description (published in
1918) to assist in differentiation from other species now known.
The eyes are bare, narrowly separated above. Palpi relatively short, the third
segment inflated about middle, with a large, shallow pit, which is subdivided:
lengths of last three segments about 25, 8, and 11 units respectively. Antennae
with segments 4-10 oval to vasiform, ranging from about 11 by 8 to 12 by 7 units;
11-14 more elongate, subequal, 17-20 by about 7 units; 15 about 30 by 9
(maximum) units, without stylet, The combined lengths of segments 3-10, 4-10,
BY J. W. S. MACFIE. 557
and 11-15 about 102, 85, and 103 units respectively. Wings finely adorned, the
distribution of the pale spots as shown in diagram (Fig. 3). In addition to these
pale spots, certain parts of the wing are paler than the rest, namely, the area
immediately below R,,;, and narrow zones along veins M,, M., Cu, Cu,, and Cu..
Macrotrichia abundant, covering almost whole surface excepting radial areas, and
extending to base between M and Cu. Legs with all knees dark, and a narrow
pale band both a little above and a little below them. T.R. almost 2. Fourth tarsal
segments sub-cylindrical, not cordiform.
_ Fig. 1.—Dasyhelea aeratipennis (Skuse). Hypopygium, ventral view, to show ninth
segment and aedeagus only.
Fig. 2.—Dasyhelea minuscula (Skuse). Hypopygium, ventral view. A, ninth segment
(at lower magnification than other figures); B, side-piece and clasper; C, harpes;
D,. aedeagus (perhaps abnormal).
Fig. 3.—Culicoides multimaculatus Taylor, female. Diagram to show adornment
of wing.
DASYHELEA AERATIPENNIS (Skuse). Fig. 1.
Proc. Linn. Soc. N. S. WALES, xiv, 1889, 303.
This insect is a Dasyhelea, not a Culicoides as Kieffer (1917) supposed. The
following details may be added to the original description to facilitate future
recognition.
3, 2. Head with eyes densely hairy. Palpi brown, third segment about as long
as fourth and fifth together, without definite pit. Antennae rather dark brown.
In male, segments 4-11 gradually narrowing from about 9 by 11 to 10 by 7 units;
12-14 binodose, elongate, subequal, lengths about 20 units; 15 about same length,
without stylet. In female, segments forming an almost continuous series: 4-10
from sub-spherical to oval, ranging in one specimen from about 7 by 8 to 9 by 5-6
units; 11-14 subequal, about 10-11 by 5-6 units; 15 about 14 by 5-6 units, without
stylet. The combined lengths of segments 4-10 and 11-15 about 59 and 56 units
respectively. Thorax with scutellum yellow, bearing 5 bristles and one or two small
hairs. Wings well clothed with macrotrichia which, however, are not as dense as
is suggested in Skuse’s figure, but are distributed in the normal manner. Second
radial cell small, almost square in male, slightly longer than broad in female.
Legs with femora and tibiae darkish brown, and tarsal segments (excepting
last which is infuscated) almost colourless. T.R. in both sexes about 2:5. Abdomen
blackish. Spermatheca single, highly chitinized, collapsed in the specimen
examined, but probably oval. Hypopygium (Fig. 1) very dark brown. Ninth
sternite without bristles, prolonged posteriorly in middle line as a conical process
with an expanded and somewhat scoop-shaped end. Side-pieces short, broadest near
apex; claspers short, very dark. Harpes apparently similar to those of D. similis
C.I. & M., an irregularly-shaped transverse band on each side, with a rather feebly
chitinized posterior extension between, Aedeagus with lateral bars strongly
denticulated,
558 AUSTRALIAN SPECIES OF CERATOPOGONIDAE.
DASYHELEA MINUSCULA (Skuse). Fig. 2.
Proc. Linn. Soc. N. S. WALES, xiv, 1889, 299.
This insect is a Dasyhelea, not a Culicoides as Kieffer (1917) supposed. The
following details may be added to the original description to facilitate future
recognition.
go. Head with eyes densely hairy. Palpi darkish brown, short, third segment
without definite pit. Antennae darkish brown, with ample dark plume, and
finely sculptured segments: segments 4-11 ranging from about 8 by 10 to 9 by 6
units; 12-14 elongate but not clearly binodose, their lengths about 16, 15, and 11
units respectively; 15 about 18 by 6 units, without stylet. Thorax very dark
brown with traces of usual adornment. Scutellum yellowish, bearing 4 bristles.
Wings with both radial cells completely obliterated. Venation and distribution of
macrotrichia as shown in Skuse’s figure, but junction of R,.; squarer, more normal.
Legs rather pale brown, especially segments 1-4 of tarsi. T.R. about 2. Abdomen
very dark brown. Hypopygium (Fig. 2) with ninth sternite devoid of bristles,
prolonged posteriorly beyond aedeagus. Ninth tergite with a pair of large conical
processes posteriorly, and apparently no hairy processes. Claspers very highly
chitinized, much attenuated distally, almost claw-like. Harpes forming an
irregularly-shaped transverse band with a long posterior process, the end of which
is expanded and feebly chitinized. Aedeagus perhaps abnormal in the specimen
examined, asymmetrical, the chitinized parts in ventral view as shown in the
figure.
LASIOHELEA TOWNSVILLENSIS (Taylor).
Aust. Zoologist, i, pt. 6, 1918, 169 (Culicoides).
Mr. F. H. Taylor has kindly permitted me to examine specimens (females) of
this species, including the type. The insect, originally described (1918) as a
Culicoides, would now be placed in the genus Lasiohelea Kieffer 1921. It resembles
closely L. lefanui Carter, an African species, and may indeed prove to be conspecific.
Very similar if not identical forms have been taken in Malaya and elsewhere.
Several of the species of Lasiohelea differ to only a very slight degree. The
following additional characters of this species may therefore be helpful in
differentiating it from other species which may be found in Australia.
The eyes are bare. Palpi with third segment much inflated, with large shallow
pit: lengths of last three segments in one specimen about 15, 6, and 9 units
respectively. Antennae with segments 4-10 from disc-shaped to oval, ranging in
this specimen from about 6 by 8 to 8 by 6 units; 11-14 elongate, subequal,
17-18 by 5-6 (maximum) units; 15 about 22 (including nipple-like stylet of about
2 units) by 5 units. The combined lengths of segments 3-10, 4-10, and 11-15
about. 60, 50, and 93 units respectively. Wings as in L. lefanwi, but bare areas
along veins not quite so conspicuous. T.R. about 2. Claws and empodium normal.
Spermatheca single, of the same type as that of L. lefanwi, its diameter about 70.
References.
CLELAND, Dopp and FERGUSON.—Further Investigations into the Etiology of Worm Nests
in Cattle, 1916. Commonwealth of Australia.
DICKINSON and Hi.Lu.—Investigations into the Cause of Worm Nodules in Cattle, 1916.
Commonwealth of Australia.
McEacHrRAN and HiLu.—Investigations into the Cause of Worm Nodules (Onchocerca
gibsoni) in Cattle at Darwin, Northern Territory, Australia, Vet, Jowrn.. xxiii
(Giiss), BLOGs iis;
559
TAXONOMIC NOTES ON THE ORDER EMBIOPTHRA. XI-XIV.
By Consetrr Davis, M.Se., Lecturer in Biology, New Hngland University College.
(Fifty-one Text-figures. )
[Read 29th November, 1939. ]
PART XI: A NEW GENUS FROM THE CONGO.
(Seven Text-figures. )
Genus DINEMBIA, Nn. gen.
Genotype, Dinembia ferruginea, n. sp.
Fairly large Embioptera, the males with the foliowing characters: Winged,
R,,; forked, fork longer than stem; M simple; cubitus two-branched. Hind tarsi
with two relatively small ventral bladders on the first segment, one on the second.
Terminalia with tenth abdominal tergite completely cleft; right hemitergite large,
processes much as in Hmbia Latreille, but with the inner flap-like process
continuous with the hemitergite, not separated by membrane as in Hmbia. Process
of left hemitergite simple. First segment of left cercus produced inward sub-
terminally, process not prominent; relatively few, but large, sharp teeth, directed
forward, along the whole of the inner margin anterior to the subterminal
projection; teeth practically in a single row. Right cercus-basipodite large,
produced inward and backward, incompletely sutured off from first segment of
cercus.
Differs from Hmbia Latreille in the form and dentition of the left cercus; the
right cercus-basipodite; and the number of bladders on the hind tarsi. The
terminalia of the single species are throughout different from those of Hmbia
savignyi Westw., the genotype of Hmbia, and of its numerous fairly homogeneous
congeners. The separation of Dinembia is further justified by geographic
considerations, as species of Hmbia, relatively closely related to Hmbia savignyi,
occur in the same region, while no transitional species are known connecting
Dinembia with any of the true species of Hmobia.
DINEMBIA FERRUGINEA, nh. sp. Figs. 1-7.
6. Length 11:5-12 mm.; head, length 1:9 mm., breadth 1:6 mm.; forewing,
length 10-11 mm., breadth 2-:3-2:'5 mm. General colour ferruginous, head and
thoracic nota a little paler than the remainder; eyes black; wing-veins dark brown
bordered by brown bands. Head (Fig. 1) with eyes relatively large; sides behind
eyes converging, rounded posteriorly. A raised area, more or less semicircular, is
present in the middle of the epicranium. Antennae incomplete. Mandibles (Fig. 2)
with acute teeth terminally, and subterminally on the inner face, the left with
three, the right with two. Wings (Fig. 3) as in the generic diagnosis, cross-veins
vather numerous. Hind tarsi (Fig. 4) as in generic description. Terminalia
(Figs. 5-7) with right hemitergite (10R) massive, convex, posteriorly produced
inward and downward to an acute process (10RP,). Inner margin of 10R repre-
sented by a heavily-sclerotized strip (10RP.), directly continuous with 10R, with-
out separating membranes; free edge of 10RP. sinuate and posteriorly corrugated.
Left hemitergite (10L) small, inner margin produced backward as a rather short
560 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. XI-XIV,
process (10LP), obliquely truncate at tip, subacute; 10LP basally marked off from
10L by a clear boundary. First segment of left cercus (LC,) with inner margin
depressed in a shallow concavity medially, distally enlarged to a slight swelling or
process; entire inner margin anterior to process armed with large, sharp,
forwardly-directed teeth, nearly all of which are in a single longitudinal row.
Second segment of left cercus (LC.) shorter and thinner, subcylindrical. First
segment of right cercus (RC,) subeylindrical, basally separated from basipodite
(RCB) by an internal groove, not by a complete suture. RCB produced backward
Figs. 1-7.—Dinembia ferruginea, n. gen. et sp., o.
1. Head from above, x 12. 2. Mandibles from above, x 12. 3. Right forewing, x 2:7.
rc
4. Hind tarsus viewed laterally, x 22:5. 5. Terminalia from above, x 22:5. 6. Terminalia
from above, x 22:5 (different aspect). 7. Terminalia from below, x 22:5.
Fig. 3 semi-diagrammatic, remainder based on camera lucida outlines. All setae
omitted. Figs. 1-5, 7, from the holotype; Fig. 6 from paratype, viewed from a different
angle, stippling on 10RP, proportional to sclerotization.
on inner side, obtusely tapered. Second segment of right cercus (RC.) similar
to LC, Ninth sternite (H) with hind margin extended to a blunt subquadrate
process (HP). Left cercus-basipodite (LCB), between HP and base of LC,,
produced to the left into a sharp spine.
° unknown.
Locality.—Elisabethville, Belgian Congo, 11° 40’ S., 27° 34’ E.; holotype ¢
(numbered 2263) and paratype gj (2979) in the Museum of Comparative Zoology,
Harvard University.
Conventional lettering on Text-figures: 9, ninth abdominal tergite; 10L, 10R, left and
right hemitergites of tenth abdominal segment; 10LP. 10RP, processes of 10L, 10R;
10RP,, 10RP,, posterior and inner processes of 10R; LC,, LC,, RC,, RC,, first and second
segments of left and right cerci; LCB, RCB, left and right cercus-basipodites; H, ninth
abdominal sternite (hypandrium) ; HP, process of H.
BY CONSETT DAVIS. 561
PART XII: THE GENUS HAPLOEMBIA VERHOEFF.
(Fifteen Text-figures. )
Genus HAaPLoEMBIA Verhoeff 1904.
Abh. Leop.-Carol. Akad. Naturf. Halle, Bd. 82, p. 201 (as subgenus of Hmbia
Latr.). Raised to generic rank, Enderlein, 1909, Zool. Anz., 35, p. 188.
Genotype, Embia solieri Rambur 1842, Hist. nat. Névroptéres, p. 3131—
(Synonym, Dityle Friederichs 1907, Verh. Zool. bot. Ges. Wien, Bd. 57, p. 272.)
Rambur’s type (de Selys Collection) is a female, lacking head and legs
(Enderlein, 1912, p. 66). I follow the interpretation of Enderlein (l.c.) and Krauss
(1911) as to the identity of Rambur’s species, and the structure of the male. It
would be beneficial if a male specimen, agreeing with this concept and collected
near the type locality (environs of Marseilles), could be selected as an allotype for
this species, fixing it with certainty.
Medium to small Embioptera, the males with the following characters: Wing-
less; two ventral bladders on the first segment of the hind tarsus, one on the second.
Right hemitergite of tenth abdominal segment produced backward and inward to a
long process. First segment of left cercus somewhat clavate, but without nodules.
HAPLOEMBIA SOLIERI (Rambur 1842). Figs. 1-4.
Embia solieri Rambur 1842, l.c—Hmbia grassii Friederichs, 1906, Mitt. Zool.
Mus. Berlin, Bd. 3, p. 227.
6 (after Krauss). Length 8-9 mm. General colour dark brown, with or
without paler flecking. Head elliptical or slightly trapezoidal, eyes small, antennae
with 18-20 segments. Mandibles (Fig. 1) elongate, incurved. Hind tarsi (Fig. 2)
with two metatarsal (basitarsal) bladders. Tenth abdominal tergite (Figs. 3-4)
Figs. 1-4.—Haploembia solieri (Ramb.), <&, from Crete (after Krauss, 1911, Pl. iii,
figs. 17D, F, H and J respectively). 1. Left mandible. 2. Tarsus of right hind-leg
from inside. 3. Terminalia from above. 4. Part of same, further enlarged.
Figs. 5-6—Haploembia megacephala Krauss, ¢ (after Krauss, 1911, PI. ii, figs.
16A, B). 5. Terminalia from above. 6. Terminalia from below.
1As Verhoeff (l.c., p. 167) states that this species has two hind metatarsal bladders,
some of his material must have been determined correctly. However, his figure (Pl. iv,
fig. 26) of a male from Sicily, given as H. solieri (Ramb.), appears to be of a species of
Embia (perhaps H. ramburi R.-Kors.). Haploembia was therefore based on a partly
misidentified series.
TT
562 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. XI-—XIV,
deeply cleft, right hemitergite (10R) produced backward and inward from outer
margin to an elongate, acutely-tapered process (10RP,), sinuous, terminally directed
slightly either to the right or to the left. Basally, the inner margin of 10RP,
overlies an obtuse flap-like process (10RP.), similar to that in Oligotoma; I follow
Krauss (1911, explanation to Pl. iii, fig. 17J) in referring to this as a process of
10R, not as a ‘median plate’. Process of left hemitergite (10LP) elongate, narrowly
tapered, acute, rotated about axis. Right cercus composed of two subcylindrical
segments (RC,, RC,), the first thicker, curved inwards a little and slightly clavate.
Left cercus composed of similar segments (LC,, LC,), the first with curvature and
distal swelling stronger than in RC,. Ninth sternite produced back to an obtuse
lobe (HP), on the left of which is an elongate chitinous structure, possibly
homologous with the structure referred to in other genera as the left cercus-
basipodite.
9. See Enderlein (1912) and Krauss (1911). Not important taxonomically.
Note.—The species seems to have a wide distribution around the Mediterranean,
exclusive of Syria. Males agreeing with this concept are recorded from Crete
(figured in this paper, after Krauss), Dalmatia (figured by Krauss, 1911, and
Enderlein, 1912), the French Riviera (Friederichs, 1906), and Sicily (Grassi and
Sandias, 1893-4). Many of the records cited by Krauss (l.c.) are based on females
or larvae, and do not therefore prove the occurrence of this species.
HAPLOEMBIA TAURICA (Kusnezov 1903).
Embia taurica Kusnezov, 1903, Rev. russe Entomol., 3, p. 208—Haploembia
taurica (Kusnezov), Krauss, 1911, p. 53.
¢ (after Kusnezov, l.c.). Length 8-11 mm. General colour dark brown, shiny,
legs and antennae paler. Head subtriangular, eyes fairly large, subreniform.
Number of antennal segments 18-19. Tarsi as in H. solieri. Terminalia similar
to H. solieri, but with the process of the left hemitergite bent to the left in the
form of a hook.
9. See Kusnezov (l.c.). Not of taxonomic importance.
Locality.—South Coast of the Crimea, from Cape Sarytsch to the Bay of
Alushta, up to 150 metres above sea-level.
Although no figures exist, and no types seem to be extant, the species may be
listed as recognizable, at least being capable of differentiation from the other
known species. The selection and complete description of a neotype (¢) from the
type region would be very advisable.
HAPLOEMBIA MEGACEPHALA Krauss 1911. Figs. 5-6.
Zoologica, Hft. 60, Bd. 23, p. 53, Pl. ii, figs. 16-16B.
¢ (atter Krauss, lc.). Length 15 mm.; head 3 mm. x 2 mm. General colour
very dark rust-brown. Head very large, broadly elliptical. Mandibles elongate,
bidentate. Terminalia (Figs. 5-6) similar to the two preceding species; but with
the process of the left hemitergite (10LP) flat, terminally outcurved in an ovoid
knob. First segment of left cercus more clavate than in H. solieri.
? unknown.
Locality.—Syria (holotype ¢ in Vienna Museum).
HAPLOEMBIA ANTIQUA (Pictet 1854). Figs. 7-15.
Embia antiqua Pictet, 1854, Traité de Paléontologie ou Histoire naturelle des
animaux fossiles, 2nd edition, vol. 2, p. 370.—Pictet and Hagen, 1856, Neuroptera,
in Berendt, Die im Bernstein befindlichen organischen Reste der Vorwelt, vol. 2,
BY CONSETT DAVIS. 563
p. 56.—Oligotoma antiqua (Pictet), Hagen, 1885, Canad. Entomologist, 17, p. 176;
Krauss, 1911, Zoologica, Hit. 60, Bd. 23, p. 47; Hnderlein, 1912, in Coll. zool. de
Selys-Longchamps, fasc. 3, p. 95.
The following description is from an excellently-preserved female, in Baltic
Amber (as were the original specimens). It is in the Harvard University collection
(number 9306). It must be freely admitted that there is no certainty that it
belongs to Pictet’s species, or even to the genus Haploembia, but the present course
involves the least addition to the nomenclature of the Order compatible with the
facts observed.
The early descriptions do not fix the species, nor do any types appear to be
extant; the present specimen may therefore be referred to Pictet’s specific name.
As it is a female, the main generic characters are lacking, but the tarsal bladders
prove that the specimen cannot be referred either to Hmbia Latr. or to Oligotoma
Westw. If such a female were found in Europe to-day, it would certainly be
8 7
Figs. 7-15.—Haploembia antiqua (Pictet), 9. 7. Head viewed obliquely, from left,
below and anteriorly, x 25. Labial palp obscured. 8. Head viewed from behind and to
the right, x 25. 9. Four of distalia of antenna, x 25. 10. Pronotum from above and to
the right, x 25. 11. Right foreleg from below, inside and anteriorly, x 25. 12. Tarsus of
left foreleg from outside, x 25. 13. Left hind-leg from outside, x 25. 14. Tarsus of right
hind-leg, from inside and distally, x 25. 15. Terminalia viewed laterally, from the left,
x 25.
Figs. 1-6, magnifications not stated by Krauss. Figs. 7-15 based on camera lucida
outlines. Stippling in Figs. 11 and 15 to represent degree of pigmentation. The black
areas of Figs. 7 and 8 represent a mouth-secretion, obscuring certain structures. MXP,
maxillary palp; LR, labrum; CL, clypeus; 7, 8, 9, abdominal tergites; 10, tenth abdominal
tergite of 9; ? LCB, structure probably representing left cercus-basipodite; VII, VIII, IX,
abdominal sternites of 92; X, longitudinally-cleft tenth abdominal sternite of 9; G,
position of @ genital aperture.
>
564 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. XI-—XIV,
referred to Haploembia; this does not prove, however, that the genus, as defined
on the characters of the male (above), existed in Oligocene times.
Two points may be noted supporting the present classification. First, Hagen
(1885, p. 177) noted that the original specimens (wingless, length 10 mm., colour
as in the present specimen) had the last tergite asymmetrical, and concluded that
he was studying males; the males of the recent species of Haploembia are wingless.
Secondly, it would not be surprising to find such a highly-specialized type as
Haploembia in the Oligocene; a very highly-specialized Embiopteron (Burmi-
tembia) is known from Burmese Amber (? Miocene).
In view of the general entomological interest of this specimen, it is described
rather fully.
9. Length just over 9 mm.; length of head 1-6 mm.; breadth of head not
discernible, as only oblique views could be obtained. General colour (to judge
from the amber specimen) dark chocolate-brown, with paler areas, especially on
thorax and inner parts of legs; no trace of pattern on head. Head (Figs. 7-8)
ovoid, pilose, eyes subreniform, broadest behind, extending forward below insertion
of antennae, with some 200 ommatidia, and with a few setae interspersed. Antennae
some 3 mm. long, each with 19 segments exclusive of the subannular basal sclerite
fused to the head-capsule. Basal segments of same general relative sizes as in
recent Embioptera (Figs. 7-8); distalia (Fig. 9) subcylindrical, each slightly
swollen distally. Palps as in recent Embioptera, maxillary with 5, labial with 3
subeylindrical segments, terminal segment longest in each case. Whole of mouth-
region obscured by a secretion, such as is noted when living Embioptera are placed
in fixative (e.g. Carnoy). Pronotum (Fig. 10) trapezoidal, broader behind, with a
transverse sulcus in anterior third (cf. Hagen, 1885, p. 177); trace of a shallow
longitudinal furrow medially in front of transverse sulcus (i.e. on ‘prozona’), none
behind (on ‘metazona’). Forelegs (Fig. 11) as in recent Embioptera, with femora
somewhat swollen, tarsi three-segmented (Figs. 11-12), the first segment very
greatly dilated, plantar surface flattened, with spinning-hairs; second segment
small, basally embedded in first; third segment longer than second, more slender at
base, with two sharp claws distally. Second pair of legs slender, as in recent
Embioptera. Hind legs (Figs. 13-14) with coxae small, fused to thorax.
Trochanter small, oblique; femur greatly swollen, to accommodate flexor muscles;
tibia more slender, somewhat curved. Three tarsal segments, the first with two
ventral bladders, one medial, one terminal; second segment short, with a terminal
ventral bladder; third segment a little longer than first, slender, curved, with two
well-developed claws.
Mesonotum and metanotum subrectangular. Wings absent. First eight
abdominal tergites subrectangular, subequal, ninth shorter, transverse, tenth entire,
subtriangular; abdominal tergites except 9 and 10 paler than head and thorax.
Pleurites represented by dark longitudinal bars placed laterally on abdominal
segments 2-8. Abdominal sternites ii—viii subrectangular, viii large, with medial
and posterior sclerotized areas. Ninth sternite large, heavily-sclerotized. . 0 210-CLab CCE R CREE RON ERC cS ieialorreh ayaa cee berlandi (Navas)
Concaivity, between lobes shallows GEE e 9) yar ter-) ale) nestenenereneyetey Welton nan gromieri (Navas)
List of References.
NavAs, L., 1922.—Algunos Insectos del Museo de Paris. Rev. Acad. Ciene. Zaragoza, vil.
— , 1928.—Insectos Exéticos Neurépteros y Afines del) Museo Civico de Génova.
Ann. Mus. Civ. Stor. Nat. Genova, vol. 53.
, 1931.—Insectes du Congo Belge (Série vi). Rev. Zool. Bot. africaines, vol. 21,
fase. 2 (Tervueren).
, 1934.—Décadas de insectos nuevos (Década 25). Brotéria, Série trimestral,
>
Vols a, Lasc de:
PART XIV: THE IDENTITY OF EMBIA RUFICOLLIS DE SAUSSURE AND OF
OLIGOTOMA VENOSA BANKS.
(Seven Text-figures. )
De Saussure (1896) described a single male specimen as Hmbia ruficollis,
giving the locality as ‘America Centralis’. The only points of note in his descrip-
tion are the size (length 6-5 mm., wing length 5 mm.), the colour (dark brown
with orange-ferruginous pronotum), and the venation (R,,, simple, distinct only
at base; M, Cu, obsolete). The brief mention of the terminalia does not seem to
be based on a critical examination; it may be assumed to be as inaccurate as the
descriptions of the terminalia of other species (EH. trinitatis, EH. urichi) in the same
paper, which do not agree with the types.
Krauss (1911) briefly re-described the type (Muséum d’Histoire naturelle,
Geneva), as Oligotoma ruficollis, figuring only the head and prothorax (1911,
Pl. ii, fig. 10). His brief description of the terminalia (Supra-anal plate asym-
metrical, right process short, dagger-shaped, left hooked at the end; cerci only a
little asymmetrical, first and second segments of equal length) is valuable, although,
if the specimen described below is really conspecific, he has confused the right
process with the left. Krauss also gives a detailed locality (Bugaba, Central
America, 250-400 metres), presumably from the type label. Krauss’s reference of
the species to Oligotoma has been followed by all subsequent authors.
In the Paris Museum there is a single specimen (1) from Costa Rica (coll.
Paul Serre, 1920). It has been identified as Oligotoma ruficollis by Navas (1924).
I believe the specific identification to be correct, but the specimen is not referable
to Oligotoma. The new genus here proposed is based on this specimen, rather than
on de Saussure’s; if it should prove not conspecific, the present specimen, not de
Saussure’s name, should be retained as the genotype.
BY CONSETT DAVIS. 573
The specimen under discussion seems to be conspecific with two males
described and semi-diagrammatically figured by Friederichs (1934), as Oligotoma
rujicollis. Friederichs’s specimens were also from Costa Rica (Mojica, Guanacaste,
Rio Bianco: Farm La Caja, nr. San José; Mus. Hamburg).
Genus SAUSSURELLA, Nn. gen.
Genotype, Hmbia ruficollis de Saussure, 1896, Mitt. Schweiz. entomol.
Gesellschaft, Bd. 9, Hft. 8, p. 358.
Small Neotropical Embioptera, the males with the following characters:
Winged, R,,, simple, terminally subobsolescent; M and Cu,. simple, subobsolescent.
Hind tarsi with only one metatarsal bladder. Tenth abdominal tergite completely
cleft, right hemitergite with an elongate posterior process, but without any process
on the inner margin. Process of left hemitergite simple. Left cercus composed of
two subcylindrical segments, of equal length, the first very slightly thickened
distally, but without nodules.
The genus differs from Oligotoma Westw. in the right hemitergite, which lacks
the inner flap-like process characteristic of the latter genus. It is to be considered
as fairly closely convergent to Oligotoma, rather than as fairly closely related. It
differs from two other Neotropical genera (Diradius Fried., Oligembia Davis) in
the simplicity of the trace of R,,;, which is forked in these genera; they have the
tenth abdominal tergite only incompletely cleft, a further important difference.
Saussurella is probably most closely related to the Antillean genus (undescribed),
to which ‘Oligotoma’ hospes Myers belongs; this genus* may be ancestral. It is
much larger, with less obsolescent venation; its chief difference, however, lies in
the clavate, echinulate first segment of the left cercus.
SAUSSURELLA RUFICOLLIS (de Saussure 1896). Figs. 1-4.
Hmbia ruficollis de Saussure, 1896, 1.c—Oligotoma ruficollis (de Saussure),
Krauss, 1911, Zoologica, Hft. 60, Bd. 238, p. 42, Pl. ii, fig. 10; Navas, 1924, Brotéria,
Série Zooldgica, vol. xxi, fasc. 2, p. 63; Friederichs, 1934, Arch. f. Naturg., N.F.,
1si¥0l, By Jebtws & Ws Gules wake
6. Length 6 mm.; forewing 4 mm. x 1:2 mm.; head 1:1-mm. x 0:9 mm. General
colour dark chocolate-brown, head almost black, pronotum orange-red; wing-veins
dark brown, bordered by mid-brown bands. Head (Fig. 1) elongate, eyes somewhat
prominent, sides behind eyes rounded, converging behind. Antennae defective.
Wings (Fig. 2) with R, strong, R,,, distinct, the two veins not confluent terminally,
but joined by several cross-veins. R,,; simple, distal half represented only by a
row of macrotrichia; M and Cu, simple, subobsolescent, as the distal part of R,.;.
Stem of cubitus strong; anal short but distinct.
Hind tarsi with one metatarsal bladder. Tenth abdominal tergite (Fig. 3)
completely cleft by a median longitudinal division; inner edge of right hemitergite
(10R) straight, simple; 10R produced backward to an elongate process (10RP),
expanded distally, and curving to the right; left-hand margin rounded near tip;
outecurved portion acute. Left hemitergite (10L) produced backward from inner
margin to a simple, tapered, subacute process (10LP). Right cercus missing (in
the specimens described by Friederichs, l.c., with two subcylindrical segments).
Left cercus with two segments, the first (LC,) very slightly swollen distally,
without nodules; the second (LC,) thinner, of subequal length. Ninth sternite
(H) (Fig. 4) tapered backwards to an elongate process (HP), curved to the left;
* This genus will shortly be described by Mr. E. S. Ross, of the University of
California.
574 TAXONOMIC NOTES ON THE ORDER EMBIOPTERA. XI-XIV,
left cercus-basipodite (LCB) slender, obtusely tapered; space between HP and
LCB largely membraneous.
Locality—Costa Rica (Mus. Paris). The specific identification requires
checking against the type (Mus. Geneva).
Note.—Friederichs (l.c.) has described a female from Costa Rica, which he
believes to be referable to this species. It possesses no features of taxonomic
importance.
A
Cula Culb
Figs. 1-4.—Saussurella ruficollis (Sauss.), &, Costa Rica (Mus. Paris). 1. Head
from above, x 35. 2. Right forewing, x 10. 3. Terminalia from above, x 35 (right cercus
missing). 4. Terminalia from below, x 35. (Based on constant use of ocular micrometer.)
Figs. 5-7.—Saussurella venosa (Banks), holotype ¢, Santa Clara, Cuba (Museum of
Comparative Zoology, Harvard University). 5. Head from above, x 16:5. 6. Left fore-
wing, x 16:5. 7. Appearance of damaged terminalia from above, x 16:5. (Based on
camera lucida outlines. )
SAUSSURELLA VENOSA (Banks 1924). Figs. 5-7.
Oligotoma venosa Banks, 1924, Bull. Mus. Comp. Zool. Harvard, vol. 65, no. 12,
p. 421.
Banks’s type g, from Santa Clara, Cuba, is in the Museum of Comparative
Zoology, Harvard University. It is in such a battered state that a valid specific
description cannot be prepared; but it is sufficiently well preserved to prove with
certainty that it cannot be referred to Oligotoma. I refer it to Sauwssurella
provisionally; another possibility is that it belongs to the undescribed genus
containing ‘Oligotoma’ hospes Myers, or perhaps even to Anisembia Krauss, both
of these genera being known to occur in Cuba. The differential feature between
these genera (the left cercus) is missing in the type; the right hemitergite, as
preserved in the type, does not place the species, as this structure, and its process,
agree in general form in ‘Oligotoma’ hospes Myers (also from Cuba), and
Saussurella ruficollis (Sauss.).
Further collecting from the type region may clear this matter up; I submit
further details of the type as a step in this direction.
BY CONSETT DAVIS. 575
6. Length not discernible in broken type; forewing 4:0 mm. x 1:1 mm. Colour
(in balsam) black. Head (Fig. 5) similar in size and general form to SN. ruficollis.
Wings (Fig. 6) as in S. rujicollis, but with R,,, and M stronger, and cross-veins
strong, influencing the direction of the main veins. Terminalia (Fig. 7) much
battered; process of right hemitergite (10RP) apparently as in S. ruficollis;
process of left hemitergite obscured. Left cercus missing; first segment of right
cercus (RC,) subcylindrical, partly obscured; second segment broken.
The specimen is very much smaller than O. hospes Myers.
List of References.
BANKS, N., 1924.—Descriptions of New Neuropteroid Insects. Bull. Mus. Comp. Zool.
Harvard, vol. 65, no. 12.
FRIEDERICHS, K., 1934.—Das Gemeinschaftsleben der Embiiden und N&aheres zur Kenntnis
der Arten. Arch. f. Naturg., N.F., Bd. 3, Hft. 3.
Krauss, H. A., 1911.—Monographie der Embien. Zoologica, Hft. 60, Bd. 23 (Stuttgart).
NavAs, L., 1924.—Insectos de la América Central. Brotéria, Série Zoolégica, vol. xxi,
fase. 2.
DE SAUSSURE, H., 1896.—Note sur la Tribu des Embiens. Mitt. Schweiz. entomol.
Gesellschaft, Bd. 9, Hft. 8.
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577
THE GENERAL GEOLOGY OF THE DISTRICT EAST OF YASS, N.S.W.
By KATHLEEN SHERRARD, M.Sc.
(Plate xii; three Text-figures.)
[Read 29th November, 1939.]
The district of which the geology is described in this paper lies across the
common boundary of the Counties of Murray and King in New South Wales and
includes parts of the Shires of Goodradigbee and Gunning. It comprises the
whole of the Parishes of Manton, Mundoonen and Morumbateman, with the portions
in Bango, Jerrawa, Dixon, Nanima, Toual and Hume adjoining them, covering
in all about 150 square miles. Its western boundary is 3 miles east of the town
of Yass and 185 miles south-west of Sydney by road, and in part adjoins the
eastern boundary of an area described previously (Sherrard, 1936).
The general geology of the area shown in the sketch-map (Fig. 1) has been
investigated, particularly in regard to the nature of rock types, to the junctions
between sedimentary and igneous rocks, to the determination of the age of the
sedimentary rocks, and to the structural and age relationships of the sediments
to each other.
Acknowledgements.—The author wishes to acknowledge gratefully the courtesy
of Professor L. A. Cotton, M.A., D.Sc., in granting her facilities for study in the
Geological Department of the University of Sydney, and of Mr. R. A. Keble, F.G.S.,
Palaeontologist to the National. Museum, Melbourne, who has kindly advised her
in the determination of graptolites. She also wishes to express her appreciation
to Miss Irene Crespin, B.A., Commonwealth Palaeontologist, Canberra, and to
Dr. Dorothy Hill, M.Sc., Ph.D., of the University of Queensland, who have been
good enough to examine specimens for her. She is also grateful to Dr. Ida Brown,
D.Se., of the University of Sydney, for much helpful discussion.
Previous Literature.
No detailed description of the geology of the whole of this area has been
published hitherto. In the geological map of New South Wales published by the
Department of Mines in 1914, it is shown as composed of porphyry in its western
half with Silurian sediments to the east.
Some localities, especially Morumbateman (or Nanima) Creek and Jerrawa,
have figured in gold, bismuth, silver, copper, iron and other mineral mining
(Ann. Reps., 1888, 1907, 1916, 1921; Watt, 1897). Shearsby (1911) included the
north-western part of this area in his “Geology of Yass’. He named and described
the Bango Limestone Bed of the Silurian Series, named the igneous rock east
of it, “No. 1 Porphyry”, and called the sediments further east the “Jerrawa
Shales”, regarding them as the lowest member of the Silurian Series, no fossils
having then been obtained from them. In 1937 descriptions of graptolites from
this district were published (Sherrard and Keble, 1937).
UU
578 GEOLOGY OF DISTRICT EAST OF YASS,
GEOLOGICAL
SKETCH-MAP
OF
DISTReGy
EAS TO VASsS
SCALE
; ) ; 1 Mile
PARISH OF
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7m. W\A3 o ie
PARISH OF \ \o NE \ MM be ta N Neen : ni
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YASS \ © \ei\ 2%" PARISH OF \ MONDOONE Re
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'
So
o
Direct Counts,mill.per gm.
°
Ss r)
3° o
Plate Counts,mill.per gm.
0 15 28 51 85
Incubation, Days.
~
Fig. 2.—Multiplication of microorganisms and production of ammonia and nitrate
soil B without addition of organic matter.
n
604 CONTRIBUTIONS TO THE MICROBIOLOGY OF AUSTRALIAN SOILS. V,
experiment. In this soil, too, actinomycetes were rather scarce (max. 3 mill.
per gm.).
The curves for mineral nitrogen (chiefly or exclusively nitrate) are even more
clear-cut than in soil A. At 5°C. the nitrate content actually declines during
incubation, at 15°C. the process of nitrification is little active, but gains strongly
in activity with increasing temperature. The observation of Prescott and Piper
(1930), that differences in temperature between 11°C. and 34°C. have little
influence on the rate of nitrate production, can thus hardly be considered generally
valid. As to the decrease in nitrate content at 5°C., it is interesting to note,
although no exaggerated importance should be attached to this single observation,
that the disappearance of 10 parts per million (i.e. 107 per gm. of soil) of mineral
nitrogen has coincided with an increase in total bacteria equal to about 450 mill.
cells per gm. of soil, which quantity may be estimated to contain approximately
9y of organic nitrogen. The suggestion lies close at hand that disappearance of
per gm.
Direct Counts
100 mill.
15
per gm.
Plate Counts
100 mill.
S
NH,-*NO,-Nyp.p.m.
TUS 30
62 G4a.|.
72 LS Zoe Whe
40
20
0
15 30 7 15 30
Density of
mycelium %
? 15 30 nS 30 7
Incubation, Days.
Fig. 3.—Multiplication of microorganisms and production of ammonia and nitrate in
soil A with addition of 1% fungal matter. Densities of mycelium as in Fig. 4 expressed
as percentage of microscopic fields showing presence of fungal hyphae.
BY H. L. JENSEN. 605
nitrate at low temperature may be due simply to nitrate consumption by
multiplying bacteria, and not to a preponderance of denitrifying bacteria at this
temperature, as suggested by Lebrun and Radet (1933).
In both soils fungal mycelium was generally very sparsely represented,
except for a few isolated instances (soil A at 7°C. after 15 days, and soil B at
25°C. after 15 days) where densities of about 6% were observed. Otherwise the
density was at the most 1:1%, without any correlation with temperature or time;
these figures have therefore not been included in the graphs.
It thus applies to both control soils that incubation at increasing temperature
results in a stronger mineralization of the humus nitrogen but in a less
abundant microflora, especially bacteria capable of developing on agar plates.
Figure 3 shows the results from soil A with addition of mycelium. They
agree completely with those of former experiments in shorter intervals of time
(Jensen, 1936): numbers of bacteria, total as well as plate counts, show first
a rapid rise and then a gradual decline, at 37° C. approaching a constant level
already after 15 days. At each point of time, even after 7 days, we find an almost
Direct Counts
&
: { js = e\
a 's, (LIBRARY) 2
2 — ‘ py Br =
ie ats Sy,
ef
Eb gs
Firs
Ome
on iar
on i ~
zo 4 / Sei a Sl. samp os oe
° i Sse’ ar ay miei td = ea COIS Che ee Bie 1§°
/ hea Ree Nena rh re eee == o
| ees «oh ecm ID Vesa 225
, wHev?
200
ear?
o 50 —— iE Se eed eangee = 25°
a So ae Par Perret pinks BOP S Cea o
ante Vor Rees i eee aa,
z= | Ve a ae Se
50 ZA
lo}
=
a SS US
28 Si 85a.
o
Las SI od BEY Bee
>F 20
ae
£2 lo
AB
0 = ;
815 «38 51 B15 28 48 15 28 4815
Incubation, Days.
Fig. 4.—Multiplication of microorganisms and production of ammonia and nitrate in
soil B with addition of 1% hay.
606 CONTRIBUTIONS TO THE MICROBIOLOGY OF AUSTRALIAN SOILS. _ V,
perfect inverse relationship between temperature and numbers of organisms.
The growth ef fungal mycelium behaves similarly: maximal development, which
reaches its highest values at 7-15°C. and is least at 37°C., takes place during the
first 7 to 15 days and is followed by a decline which is slowest at 7°C. and most
rapid at 37°C. After the 30th day all densities of mycelium were very low
at all temperatures, and have therefore been omitted from the graph. The curves
for mineral nitrogen are here again almost complete reciprocals of the bacterial
numbers and the mycelial densities. At 7°C. there is hardly any formation of
mineral nitrogen during the first 30 days, but a definite increase takes place
during the last 32 days, when nearly all fungal growth has ceased and the numbers
of bacteria are falling. At 37°C., on the other hand, most of the mineral nitrogen
is produced after 30 days, at which time mycelial growth has already disappeared
and the numbers of bacteria have reached an almost constant level.
In soil B, which was exposed to a still lower minimum temperature, the results
are similar but even more striking (Fig. 4), in respect of both total counts, plate
counts, growth of mycelium, and production of mineral nitrogen, except that the
initial rise in bacterial numbers is somewhat more rapid at the higher tempera-
tures, especially 25°C., in the very early stages of decomposition (4 to 8 days).
In both soils with addition of organic matter, but especially B, actinomycetes
figured prominently in the plate counts at 25° and 37°C., but were less numerous
at 15°C. and very sparse at 5° and 7°C.
Very little accumulation of ammonia took place except at the lowest tempera-
ture, where the following amounts of NO, and NH,-N (in parts per million)
were found:
Soil A (7°C.)
Days NO,-N NH,-N
Soil B (5°C.)
Days NO,N NH,-N
0 31 0 | 0 30 8
30 (0) 45 | 15 37 37
62 48 25 | 28 33 43
94 147 13 51 50 48
| 85 63 55
Even at 5°C. nitrification thus goes on, although slowly and without keeping
pace with the ammonia production (cf. Schoénbrunn (1922), who observed the
same phenomenon even at 0°C.). The lack of nitrate accumulation in the
corresponding control soil without addition of organic material is thus not due
to complete inhibition of the nitrifying bacteria by the low temperature, but must
be ascribed to more complex causes—perhaps inactivity of microorganisms capable
of producing ammonia from the resistant humus compounds, or the accumulation
of an abundant microflora capable of utilizing the otherwise nitrifiable nitrogen
for cell synthesis.
From the direct counts of bacteria we may roughly estimate the quantities of
nitrogen present as bacterial substance, by assuming that 1,000 mill. bactérial cells
of average size represent 1 mgm. of protoplasm with 20% dry matter containing
10% N, i.e. 1,000 mill. bacteria represent 207 of nitrogen. If we regard all the
bacteria found after 4-7 days and onwards, as well as the mineral nitrogen formed,
as derived from the organic matter added (since it igs by no means certain that
the soil humus would be attacked to the same extent as in the control soils
without addition of organic material), we may tentatively account for the per-
centages of added nitrogen that have been transformed into bacterial protoplasm
plus mineral nitrogen in the two soils with addition of fungal mycelium and hay
at the different times and temperatures. This calculation is shown graphically
BY H. L. JENSEN. 607
in Figure 5; it is to be noted that soil A received 352 parts per million of N
in mycelial substance, and soil B 273 p.p.m. of N in hay. We see that at the end
of the experiment some 75-80% of the added nitrogen can be accounted for at 37°C.,
and of this only a very small fraction is represented by bacterial substance. At
5° and 7°C. only approximately one-half of the added N can be accounted for, and
a good deal of this, especially im soil B, is present as bacteria. The intermediate
temperatures occupy intermediate positions. In the early stages of the decom-
position the calculated amount of bacterial nitrogen far exceeds that of mineral
nitrogen at the lowest temperatures, but the ratio of mineral nitrogen to bacterial
nitrogen is widened with both advancing time and increasing temperature, yet at
each stage being narrower at lower temperature; if it had been possible to
calculate the amount of nitrogen in vegetative fungal mycelium, which is produced
most abundantly at low temperatures, and to add it to the bacterial nitrogen, it
would further have accentuated the general principle of increasing synthesis of
microbial substance with decreasing temperature.
% of added N.
Soil A. (Fungal Matter). Soil B.(Hay).
Fig. 5.—Calculated percentages of added nitrogen accounted for as bacterial sub-
stance + (NH,+NO,)N. Black parts of columns: nitrogen estimated as present in
bacterial cells. White parts: (NH,+NO,)N. y
Conclusions.
The results as a whole agree completely with what was previously found in
short-period experiments: the rapidity of decomposition of organic matter, as
measured by formation of carbon dioxide, nitrate and ammonia, increases with
increasing temperature, but the abundance of microorganisms decreases. When the
accumulation of soil humus is known generally to increase with decreasing tempera-
ture (cf. Waksman, 1936), the explanation must be sought not merely in the general
retarding influence of temperature decrease on biological processes according to
the law of van’t Hoff, but also to the fact that decreasing temperature causes
larger proportions of the transformed organic material to be converted into
608 CONTRIBUTIONS TO THE MICROBIOLOGY OF AUSTRALIAN SOILS. V.
microbial substance, certain constituents of which contribute to the humus of the
soil. In its relation to temperature the soil microflora as a whole thus seems to
conform to a general biological rule governing the size of populations; this has
previously been most clearly observed in plankton populations, which reach their
greatest density in cold sea-water (cf. Bélehradek, 1935). No doubt this
phenomenon has also something to do with the high numbers of bacteria sometimes
observed in frozen soil; a reinvestigation of this problem by means of direct
counting methods might prove fruitful. When no definite correlation is usually
found to exist between soil temperature and numbers of bacteria under natural
soil conditions, it must be remembered that a complicating factor is here
represented by the food supply in the form of residues of higher plants, the growth
of which in its turn depends on the temperature (Hggleton, 1938). It seems quite
likely, however, that the frequently observed spring and autumn maxima in
bacterial numbers (Taylor, 1936) may arise, if at these seasons there prevails a
soil temperature insufficiently low to check the growth of bacteria altogether
(such as might happen in winter time), yet low enough to permit the accumulation
of higher numbers of bacteria than in summer time.
Summary.
Two soils were incubated with and without addition of decomposable organic
material (hay and fungal mycelium) for about 3 months at 4 ranges of temperature,
from 5°C. to 37°C. Determinations were made at different time-intervals of the
abundance of microorganisms, by both microscopical and plate methods, as well as
of ammonia and nitrate. The rate of nitrate accumulation, from the soil humus
as well as from the added materials, increased with the temperature, whereas
the numbers of bacteria and the densities of fungi showed an inverse relationship,
becoming highest at the lowest temperature, i.e. the lower the temperature of
decomposition, the greater a proportion of nitrogen in the transformed organic
matter is temporarily locked up as microbial substance before eventually appearing
as ammonia and nitrate. At 5°C. the numbers of bacteria were occasionally
so high as to account for approximately one-third of the nitrogen present in the
added organic material.
References.
BELEHRADEK, J., 1935.—Temperature and Living Matter. (Protoplasma-Monographien,
No. 8. G. Borntraeger, Berlin.)
EcGGLeTon, E. W. G., 1938.—The Influence of Environmental Factors on Numbers of Soil
Microorganisms. Soil Sci., 46, 351-3638.
JENSEN, H. L., 1936.—Contributions to the Microbiology of Australian Soils. iv. Proc.
Linn. Soc. N.S.W., 61, 27-55.
LEBRUN and RADET, 1933.—Les reserves azotées du sol et leur mobilisation dans les sols
calecaires de Champagne. Ann. Agron., N.S., 3, 478-492.
Prescott, J. A., and Piper, G. R., 1930.—Nitrate Fluctuations in a South Australian Soil.
Journ. Agr. Sci., 20, 517-531.
RUSSELL, E. J., and HuTCcHINSON, H. B., 1913.—The Effect of Partial Sterilisation of Soil
on the Production of Plant Food. Journ. Agr. Sci., 5, 152-221.
SCHONBRUNN, B., 1922.—Uber den zeitlichen Verlauf der Nitrifikation (etc.). Cent. Bakt.,
li, 56, 545-565.
Taytor, C. B., 1936.—Short-Period Fluctuations in the Number of Bacterial Cells in Soil.
Proc. Roy. Soc. London, B, 119, 269-295.
WAKSMAN, S. A., 1932.—Principles of Soil Microbiology. 2nd Ed. (Williams & Wilkins,
Baltimore).
————, 1936.—Humus, its Origin, Chemical Composition and Importance in Nature.
(Williams & Wilkins, Baltimore).
XXXili
ABSTRACT OF PROCEEDINGS.
ORDINARY MONTHLY MEETING.
31st May, 1939.
Mr. H. C. Andrews, B.A., Vice-President, in the Chair.
Miss Marion W. Hutley, B.Sc., was elected an Ordinary Member of the Society.
The Chairman offered congratulations to Dr. H. G. Raggatt on attaining the
degree of Doctor of Science of the University of Sydney, and to Dr. C. J. Magee
on attaining the degree of Doctor of Science in Agriculture.
The Donations and Exchanges received since the previous Monthly Meeting
(26th April, 1939), amounting to 10 Volumes, 146 Paris or Numbers, 4 Bulletins,
4 Reports and 8 Pamphlets, received from 87 Societies and Institutions, were laid
upon the table.
PAPERS READ.
1. A New Species of Chalcid (Genus Hurytoma) associated with Tepperella
trilineata Cam., a Wasp causing Galling of the Flower Buds of Acacia decurrens.
By N.S. Noble, D.Sc.Agr., M.Se., D.1.C.
2. The Upper Palaeozoic Rocks between Mount George and Wingham, New
South Wales. By A. H. Voisey, M.Sc.
3. The Lorne Triassic Basin and Associated Rocks. By A. H. Voisey, M.Sc.
4. Taxonomic Notes on the Order Hmbioptera. ii. Description of a New
Neotropical Genus. By Consett Davis, M.Sc.
NOTES AND EXHIBITS.
Professor J. Macdonald Holmes sent, for exhibition, several plants collected
in the Lismore district.
ORDINARY MONTHLY MEETING.
28th June, 1939.
Mr. EH. Cheel in the Chair.
Letters were received from Dr. H. G. Raggatt and Dr. C. J. Magee, returning
thanks for congratulations.
The Chairman announced that the Royal Zoological Society of Victoria has
decided to offer a prize of £25 for an essay on any scientific aspect of the fauna
of Australia. The prize is open to all interested persons and essays should be
forwarded to the Hon. Secretary, Royal Zoological Society of Victoria, 80 Swanston
Street, Melbourne, C.1, on or before 30th December, 1939.
The Chairman announced that members were invited by the Biological Society,
Sydney University, to a symposium on “The Origin of Life’, on Wednesday, 12th
July, at 8 p.m., in the Organic Chemistry Lecture Theatre, University of Sydney.
The Donations and Exchanges received since the previous Monthly Meeting
(31lst May, 1939), amounting to 11 Volumes, 136 Parts or Numbers, 3 Bulletins,
4 Reports and 12 Pamphlets, received from 69 Societies and Institutions and 2
private donors, were laid upon the table.
XxX
XXXiV ABSTRACT OF PROCEEDINGS.
PAPERS READ.
1. A New Species of Megastigmus parasitic on Tepperella trilineata Cam., a
Wasp causing Galling of the Flower Buds of Acacia decurrens. By N. S. Noble,
D.Se.Agr., M.Se., D.I.C.
2. A Reconnaissance Survey of the Vegetation of the Myall Lakes. By
Professor T. G. B. Osborn, D.Se., F.L.S., and R. N. Robertson, Ph.D., B.Sc.
3. The Genus Adrama, with Descriptions of Three New Species (Diptera,
Trypetidae). By J. R. Malloch. (Communicated by F. H. Taylor, F.R.E.S., F.Z.S.)
4. A New Family of Lepidoptera. By A. Jefferis Turner, M.D., F.R.E.S.
NOTES AND EXHIBITS.
Mr. EH. Cheel exhibited specimens and drawings of grasses with notes thereon
as follows: (1) Cynodon.—Four species of the genus are recorded for Australia by
Bentham (F1. Aust., vii, 1878, p. 608), namely, C. dactylon, C. tenellus, C. convergens
and C. ciliaris. The three latter species are classed in the genus Microchloa by
Domin, and Brachyachne by the late Dr. O. Stapf and C. E. Hubbard of Kew,
England. The common “Couch Grass” of Australia is still retained in the genus
Cynodon by the Kew authorities and the species C. dactylon is noted for its
variability, but only one variety has been recorded in botanical literature, namely,
var. pulchellus (Bentham, l.c.). Specimens collected by HE. Cheel at Hillston in
November, 1926, and Inverell by Mr. Sommerlad in May, 1939, were exhibited which
may belong to the latter variety, but as there are no authentic specimens available
for comparison they are tentatively recorded under this varietal name. (2)
Brachiaria notochtona Stapf.—Originally described by Dr. Domin of Prague under
the name Panicum notochtonum, and recorded and illustrated by Maiden and Cheel
(Agric. Gaz. N.S.W., 1914, p. 1034) under Domin’s name, afterwards by Hughes as
Urochloa notochthona. (3) Brachiaria piligera (F.v.M.) Hughes var. intercedens
Cc. E. Hubbard.—Recorded and illustrated as Panicum intercedens Domin by Maiden
and Cheel (Agric. Gaz. N.S.W., 1914, p. 1035), and Panicum helopus Maiden, not
Bentham or Trin. (Agric. Gaz. N.S.W., 1908, p. 241). (4) Themeda arguens C. EB.
Hubbard, syn. Anthistria frondosa R. Br.—Darwin, F. H. Taylor, March, 1939.
ORDINARY MONTHLY MEETING.
26th Juxny, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
Dr. C. E. M. Gunther, New Guinea, and Miss Joan Johnston, Bexley, were
elected Ordinary Members of the Society.
The President announced that the proclamation protecting certain wild flowers
had been extended for another year from Ist July, 1939. Five species, Clianthus
Dampieri, Grevillea asplenifolia, G. Caleyi, Sprengelia incarnata, and Persoonia
pinifolia, have been added to the list this year.
The President drew attention to the following International Congresses to
which the Society has been invited to nominate representatives: 7th International
Botanical Congress, Stockholm, 17th—25th July, 1940; 18th International Geological
Congress, London, 31st July-8th August, 1940; 138th International Zoological
Congress, Paris, July, 1940. Any members who may be likely to attend any one
of these three Congresses are invited to inform the Secretary of their intention.
The Donations and Exchanges received since the previous Monthly Meeting
(28th June, 1939), amounting to 25 Volumes, 164 Parts or Numbers, 5 Bulletins
and 4 Pamphlets, received from 89 Societies and Institutions, were laid upon the
table.
ABSTRACT OF PROCEEDINGS. XXXV
PAPERS READ.
1. Australian Coleoptera. Notes and New Species. No. xi. By H. J. Carter,
B.A., F.R.E.S.
2. Observations on the Bionomics and Morphology of seven Species of the
Tribe Paropsini (Fam. Chrysomelidae). By D. Margaret Cumpston, M.Sc.,
Linnean Macleay Fellow of the Society in Zoology.
3. Hymenopterous Parasites of Embioptera. By Alan P. Dodd.
4. Miscellaneous Notes on Australian Diptera. vi. Dolichopodinae. By
G. H. Hardy.
NOTES AND EXHIBITS.
Mr. HE. Cheel exhibited fresh flowering specimens of Calythrix from cultivated
plants raised from seed obtained from Denman. The species is allied to C. tetragona
and has been regarded as a form of that species, but it is proposed to describe it as
a new species when investigations are complete.
Professor J. Macdonald Holmes showed some coloured slides of the Kyogle
and Broken Hill districts.
ORDINARY MONTHLY MEETING.
30th Aueust, 1939.
Mr. F. H. Taylor, F.R.E.S., F.Z.S., in the Chair.
The Donations and Exchanges received since the previous Monthly Meeting
(26th July, 1939), amounting to 7 Volumes, 117 Parts or Numbers, 1 Bulletin,
4 Reports and 7 Pamphlets, received from 69 Societies and Institutions and 1
private donor, were laid upon the table.
PAPERS READ.
1. The Geology of the Lower Manning District of New South Wales. By A. H.
Voisey, M.Sc.
2. The Geology of the County of Buller, New South Wales. By A. H. Voisey,
M.Sc.
38. The Diptera of the ‘Territory of New Quinea. No. x. Family
Ceratopogonidae. By J. W. S. Macfie, M.A., D.Sc., F.R.H.S. (Communicated by
F. H. Taylor, F.R.E.S., F.Z.8.)
4. Taxonomic Notes on the Order Embioptera. iii-v. By Consett Davis, M.Sc.
5. The Diptera of the Territory of New Guinea. No. xi. Family Trypetidae.
By J. R. Malloch. (Communicated by F. H. Taylor, F.R.E.S., F.Z.S.)
6. A Note on the Synonymy of Leptops (Coleoptera: Curculionidae). By
K. €. McKeown.
ORDINARY MONTHLY MEETING.
27th SEPTEMBER, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
Messrs. S. L. Allman, B.Sc.Agr., Sydney, T. Langford-Smith, Chatswood, and
A. J. Marshall, Newtown, were elected Ordinary Members of the Society.
The President announced that the Council is prepared to receive applications
for four Linnean Macleay Fellowships tenable for one year from 1st March, 1940,
from qualified candidates. Applications should be lodged with the Secretary, who
will afford all necessary information to intending candidates, not later than
Wednesday, 1st November, 1939.
XXXVi ABSTRACT OF PROCEEDINGS.
The attention of members was drawn to a meeting of the proposed Australian
Association of Scientific Workers to be held at the Botany School, University of
Sydney, on Wednesday, 4th October, 1939, at 8 p.m.
The President referred to the death of William Butler Gurney, Government
Entomologist, who had been a member of the Society since 1901.
The Donations and Exchanges received since the previous Monthly Meeting
(30th August, 1939), amounting to 16 Volumes, 129 Parts or Numbers, 6 Bulletins
and 2 Pamphlets, received from 69 Societies and Institutions, were laid upon the
table.
PAPERS READ.
1. The Association between the Larva described as Trombicula hirsti var.
buloloensis Gunther and Trombicula minor Berlese. By C. E. M. Gunther, M.B.,
Bisse avr
2. Observations on the Life-history of Neoschéngastia kallipygos Gunther
(Acarina, Trombidiidae). By C. E. M. Gunther, M.B., B.S., D.T.M.
3. Ectocarpus confervoides (Roth.) Le Jol. By Valerie May, B.Sc., Linnean
Macleay Fellow of the Society in Botany.
4. Taxonomic Notes on the Order Embioptera. vi-x. By Consett Davis, M.Sc.
NOTES AND EXHIBITS.
Mr. EH. Cheel exhibited samples of material known in the trade ase“Rice-Paper”,
which is used to make artificial flowers. A Sydney firm submitted the material for
identification with a view of extensive cultivation in Australia. With the assist-
ance of Dr. Samuel Record, Professor of Forest Products in the Yale University,
New Haven, Connecticut, it has been classified as Tetrapanax papyriferum (Hook.)
K. Koch. A closely related plant is cultivated in the Botanic Gardens, Sydney,
and a few private gardens under the name Fatsia japonica (Thunb.) Dene., and is
frequently mistaken for the true Rice-Paper plant listed in catalogues as Fatsia
papyrifera and Aralia papyrifera.
Mr. Cheel also submitted the following notes on recent classification of certain
species of Australian grasses: (1) Chamaeraphis spinescens of Maiden figured in
Agric. Gaz. N.S.W., September, 1900, is Chamaeraphis squarrosa Chase. Specimens
collected at Hillston in November, 1926, were exhibited; (2) Panicum reversum
F.v.M., of Maiden with an illustration (Agric. Gaz. N.S.W., September, 1897) is
Paractaenum novae-hollandiae Beaud. (Syn. Panicum paractaenum Kunth. vide
Royal Herbarium, Kew (England) authorities).
A series of cultivated specimens of nine species and varieties of Callistemon
were exhibited to show the fugacious nature of the chaff-like bracts which support
the individual flowers arranged in the spike-like inflorescence. The bracts in most
species are shed before the petals and filaments are expanded. In Callistemon
acuminatus the bracts are shed simultaneously with the petals and filaments. The
leaves of Callistemon viminalis are shed just before spring and renewal of foliage
takes place about three weeks after defoliation. The seed capsules and seeds are
fully matured in ten to twelve months. The other species are not fully developed
until about two and a half years.
Miss J. Vickery exhibited specimens, from the Broken Hill district, of
Trisetum pumilum Kunth., a small European grass already naturalized in South
Australia; Hragrostis barrelieri Daveau, a Mediterranean grass species which has
sometimes been confused with #. cilianensis; Statice Thouini Viv., a native of the
Eastern Mediterranean region which has appeared spontaneously in an irrigated
area at Broken Hill. It occurs in South Australia and had probably been intro-
ABSTRACT OF PROCEEDINGS. - XXXV1l1
duced from there; two forms of Atriplex spongiosum F. Muell. collected from the
same locality; Galenia secunda Sond., a native of South Africa, a species which
has only been collected previously in New South Wales near Newcastle and Mait-
land; Swainsona fissimontana J. M. Black, a native pea described from the Broken
Hill district.
The first three of the species exhibited do not appear to have been recorded
previously from New South Wales.
Dufay colour photographs of some aspects of the ground flora in the Wilcannia,
Broken Hill and Silverton districts, and a number of specimens illustrating some
of the more important and conspicuous herbaceous elements of the vegetation were
also exhibited.
Professor E. Ashby exhibited lantern slides and a specimen of wood illus-
trating the activities of beavers in the construction of dams, using Populus
tremuloides.
ORDINARY MONTHLY MEETING.
25th OctToser, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
The President reminded candidates for Linnean Macleay Fellowships, 1940-41,
that Wednesday, 1st November, 1939, was the last day for receiving applications.
The President referred to the death of Bishop Dwyer, who had been a member
of the Society since 1920.
The Donations and Exchanges received since the previous Monthly Meeting
(27th September, 1939), amounting to 18 Volumes, 70 Parts or Numbers, 7 Bulletins
and 2 Reports, received from 47 Societies and Institutions, were laid upon the table.
PAPERS READ.
1. Elementary Hydrography of South-eastern Australia. By F. A. Craft, B.Sc.
2. A Note on the Re-examination of Australian species of Ceratopogonidae. By
J. W. S. Macfie, M.A., D.Se., F.R.E.S. (Communicated by F. H. Taylor, F.R.E.S.,
F.ZS8.)
3. Strongylate Nematodes from Marsupials in New South Wales. By Professor
T. Harvey Johnston, M.A., D.Sc., F.L.S., and Patricia M. Mawson.
- NOTES AND EXHIBITS.
Mr. E. Cheel exhibited flowering specimens taken from cultivated plants:
Leptospermum emarginatum, Callistemon hortensis Hort. C. acuminatus,
Callistemon hybrid (C. acuminatus x C. lanceolatus), C. linearis, C. pinifolius and
C. pachyphyllus.
Mr. J. A. Dulhunty exhibited specimens and photographs of Macrozamia
Macdonnelli from Macdonnell Range, Central Australia. The species is confined
to this region, and is closely related to coastal types, but has much larger seeds.
It grows near permanent water and fresh springs, but not near the mound springs.
It has remained isolated in Central Australia on account of surrounding desert
conditions, which have evidently persisted since late Cretaceous or early Tertiary
time.
Mr. J. R. Kinghorn exhibited a specimen of Bufo marinus Linn., the Giant
Toad, introduced into Queensland cane-fields from Hawaii in 1934 to control the
cane borer. It was stated at a conference of sugar planters in Puerto Rico the
XXXVili ABSTRACT OF PROCEEDINGS.
same year that “if conditions in Australia and Fiji are at all comparable to those
in Puerto Rico, the white grub problem in those countries would be solved within
ten or fifteen years”. In a recent letter Dr. K. J. A. W. Lever, of the Department
of Agriculture, Fiji, stated that the toad was not introduced into Fiji until 1936,
and that among other insects in the stomach of one specimen examined were two
banana borers, Cosmopolites sordidus Chevyr., the first record for Fiji. No records
are yet to hand regarding its economic status in Queensland, into which State its
introduction did not go unchallenged. The Giant Toad is a very prolific breeder
and is now extremely plentiful in the Cairns—Gordonvale district and is spreading
rapidly over the country. The fear is that the toad may interfere seriously with
the endemic herpetological fauna.
The Secretary referred to the recent death of Mr. Fred Turner, at the age of
87. Mr. Turner had been a member of the Council from 1897 to 1912 and during
that period had been an active member of the Society. He was a member of the
Society from 1891 to 1923.
ORDINARY MONTHLY MEETING.
29th NovemMsBeER, 1939.
Professor J. Macdonald Holmes, B.Sc., Ph.D., President, in the Chair.
The President announced that the Council had reappointed Miss Ilma M.
Pidgeon, M.Sc., Miss Valerie May, B.Sc., and Miss Margaret Cumpston, M.Sc., to
Linnean Macleay Fellowships in Botany, Botany and Zoology respectively, for one
year from 1st March, 1940, and had appointed Mr. J. A. Dulhunty, B.Sc., to a
Linnean Macleay Fellowship in Geology for one year from ist March, 1940.
The Donations and Exchanges received since the previous Monthly Meeting
(25th October, 1939), amounting to 8 Volumes, 79 Parts or Numbers, 2 Bulletins,
7 Reports and 4 Pamphlets, received from 55 Societies and Institutions, were
laid upon the table.
PAPERS READ.
1. The General Geology of the District east of Yass, N.S.W. By Kathleen
Sherrard, M.Sc.
2. Taxonomic Notes on the Order Embioptera. Parts xi-xiv. By Consett
Davis, M.Sc.
3. Contribution to the Microbiology of Australian Soils. v. Abundance of
Microorganisms and Production of Mineral Nitrogen in relation to Temperature.
By H. L. Jensen, Macleay Bacteriologist to the Society.
NOTES AND EXHIBITS.
Professor Macdonald Holmes handed to the Society a set of about 160 photo-
graphs taken by Dr. Brough and Messrs. Beadle and Langford-Smith during the
excursion to the far west of New South Wales in August, 1939.
Dr. H. L. Kesteven exhibited a vertical projector designed for examination of
large sections and for use in place of a camera lucida.
XXX1X
DONATIONS AND EXCHANGES.
Received during the period 27th October, 1938, to 25th October, 1939.
(From the respective Societies, etc., unless otherwise mentioned.)
ABERYSTWYTH.—Welsh Plant Breeding Station, University College of Wales. Bulletin,
Series H, No. 15 (1939); “The Welsh Journal of Agriculture’, xv (19389); ‘“‘Ley-
farming and a Long-term Agricultural Policy”, by R. G. Stapledon (From Herbage
Reviews, vi, 3, 1938).
Accra.—Geological Survey Department, Gold Coast Colony. Report for the Financial
Year 1937-38 (19388).
ADELAIDE.—Department of Mines: Geological Survey of South Australia. Annual Report
of the Director of Mines and Government Geologist for 1937 (1938); Bulletin No. 18
(1939) ; Mining Review for the Half-years ended 30th June, 1938 (No. 68) (1938)
and 31st December, 1938 (No. 69) (1939).—Field Naturalists’ Section of the Royal
Society of South Australia and South Australian Aquarium Society. “South Australian
Naturalist”, xix, 2-4 and Supplement (1938-1939).—Public Library, Museum and Art
Gallery of South Australia. 54th Annual Report of the Board of Governors, 1937-38
(1938); Records of the South Australian Museum, vi, 2 (1938).—Royal Society of
South Australia. Transactions, |xii, 2 (T.p. & ec.) (19388); Ixili, 1 (1939).—South
Australian Ornithological Association. ‘‘The South Australian Ornithologist”, xiv, 8
(1938) ; xv, 1-3 (1939).—University of Adelaide. ‘The Australian Journal of Experi-
mental Biology and Medical Science’, xvi, 4 (T.p. & c.) (1938); xvii, 1-3 (1939).—
Woods and Forests Department. Annual Report for the Year ended 30th June, 1938
(19388). ;
ALBANY.—New York State Library, University of the State of New York. New York
State Museum Bulletin Nos. 314-316, 318, 319 (1938-1939).
ALGER.—Institut Pasteur d’Algerie. Archives, xvi, 3-4 (T.p. & ec.) (1938); xvii, 1-2
(1939).—Société d’Histoire Naturelle de VAfrique du Nord, Bulletin, xxix, 6-9
(T.p. & c.) (1938); xxx, 1-3 (1939).
AMSTERDAM.—Koninklijke Akademie van Wetenschappen. Proceedings, xli, 6-10 (T.p. &c.)
(1938); xlii, 1-2 (1939); Verhandelingen Afdeeling Natuurkunde, 2e Sectie, xxxvii,
5-7 (1938).—Nederlandsche Entomologische Vereeniging. Entomologische Berichten,
x, 222-227 (1938-1939) ; Tijdschrift voor Entomologie, Ixxxi, 3-4 (T.p. & c.) (1938);
Ixxxii, 1-2 (1939).
ANN ArRBoR.—University of Michigan. Contributions from the Laboratory of Vertebrate
Genetics, No. 7 (1938) ; Miscellaneous Publications of the Museum of Zoology, No. 40
(1938) ; Occasional Papers of the Museum of Zoology, T.p. & ec. for Nos. 296-342
(Vol. xiii) (1934-1936); Nos. 3878-390; T.p. & ec. for Nos. 343-390 (Vol. xiv)
(1936-19388) ; Nos. 391-402 (1938-1939).
ATHENS.—Zoological Institute and Museum, University of Athens, Acta, ii, 3-4 (1939).
AUCKLAND.—Auckland Institute and Museum. Annual Report, 1938-39 (1939); Records,
ii, 3 (1938).
BALTIMORE.—Johns Hopkins University. Bulletin of the Johns Hopkins Hospital, Ixili, 4-6
(T.p. & c.) (1938); lxiv, 1-6 (T.p. & c.) (1939); Ixv, 1-3 (1939).
BANDOBNG.—Dienst van den Mijnbouw in Nederlandsch-Indie. Bulletin of the Netherlands
Indies Vulcanological Survey, Nos. 84-86 (1938-1939); Publications of the Mining
and Geological Survey Department in the Netherlands Indies during 1900-1939 (1939) ;
Wetenschappelijke Mededeelingen, No. 27, le Stuk (1938); “On Polylepidina,
Orbitocyclina and Lepidorbitoides” by Dr. Ir. Tan Sin Hok (Batavia-Centrum, 1939).
xl DONATIONS AND EXCHANGES.
BASEL.—Naturforschende Gesellschaft. Verhandlungen, xlix, 1937-38 (1938).
BaTAviA.—Departement van Economische Zaken. Bulletin du Jardin Botanique, Serie iii,
Supplement Vol. i, Index; Supplement Vol. iii, 1 (1938); xvi, 1-2 (1938-1939) ;
“Treubia’”’, xvi, 4 (T.p. & c.) (1938); xvii, 1-3 (1939).—Koninklijke Natuurkundige
Vereeniging in Nederlandsch-Indie. Natuurkundig Tijdschrift voor Nederlandsch-
Indie, xecviii, 5-6 (T.p. & c.) (19388); xcix, 1-5 (1939).—Natuurwetenschappelijke
Raad voor Nederlandsch-Indie te Batavia (Netherlands India Science Council).
Publication, Nos. 14-16 (1939).
BERGEN.—Bergens Museum. Arbok, 1938, 1 (1938); Arsberetning, 1937-38 (1938).
BERKELEY.—University of California. Bulletin of the Department of Geological Sciences,
xxiv, 11-12 (1938-1939); Publications, Botany, xviii, 6-7 (1938); xix, 7 (1939);
Physiology, viii, 4 (1938); Zoology, xlii, 6 (1938); xliii, 9-10 (1939); Publications
of the University of California at Los Angeles in Biological Sciences, i, 10-12 (1939).
BERLIN.—Deutsch-Auslandischer Buchtausch. ‘Flora’, Neue Folge, xxxiii, 1-4 (T.p. & c.)
(1938-1939).—Zoologische Museum. Mitteilungen, xxiii, 2 (T.p. & c.) (1938).
BERLIN-DAHLEM.—Botanisch Garten und Museum. Notizblatt, xiv, 123-124 (1938-1939 ).—
Deutsches Entomologisches Institut. Arbeiten uber morphologische und taxonomische
Entomologie aus Berlin-Dahlem, v, 4 (T.p. & c.) (1938); vi, 1-3 (1939); Arbeiten
uber physiologische und angewandte Entomologie aus Berlin-Dahlem, v, 3-4
(T.p. & c.) (1938); vi, 1-2 (1939); Entomologische Beihefte aus Berlin-Dahlem, vi
(1939).
BERN.—N aturforschende Gesellschaft. Mitteilungen a.d. Jahre 1938 (1939).—
Schweizerische Naturforschende Gesellschaft. Verhandlungen, 119. Jahresversamm-
lung, 1938 (1938).
BIRMINGHAM.—Birmingham Natural History and Philosophical Society. List of Members,
1939 and Annual Report for 1938; Proceedings, xvii, 1 (1939).
BLOEMFONTEIN.—WNasionale Museum. Argeologiese Navorsing, i, 9-10 (1939); Soologiese
Navorsing, i, 8 (1939).
BomBay.—Bombay Natural History Society. Journal, T.p. & c. for xxxix, 3-4 (1938);
xl, 2 (Ep: & ec for xl, 1-2) (1938); 3-4 (1938-1939); xli, 1 (1939).—Haffkine
Institute. Report for the Year 1937; 1938 (1939).
Bonn.—Naturhistorischer Verein der Rheinlande und Westfalens. ‘‘Decheniana’’, xcvii
(A and B); xcviii, A, 1 (1938).
Boston.—American Academy of Arts and Sciences. Proceedings, Ilxxiii, 1-4 (1938-1939).—
Boston Society of Natural History. Proceedings, xli, 6-7 (1939).
BRISBANE.—Department of Agriculture. Queensland Agricultural Journal, 1, 4-6 (T.p. &c.)
(1938); li, 1-6; lii, 1-3 (1939).—Department of Mines: Geological Survey of
Queensland. “Queensland Government Mining Journal’, xxxix, Sept.-Dec., 1938
(T.p. & c.) (1938); xl, Jan.-Aug., 1939 (1939).—Queensland Musewm. Memoirs, xi,
3 (T.p. & c.) (1939).—Queensland Naturalists’ Club and Nature-Lovers’ League.
“The Queensland Naturalist”, xi, 1-3 (1939).—Royal Society of Queensland. Proceed-
ings, xlix, 1937 (1938); 1, 1938 (1939).—University of Queensland. University of
Queensland Papers, Department of Biology, i, 10 (1939); ‘‘Water Conservation in
Australia”, by H. H. Dare (John Murtagh Macrossan Lectures for 1939) (1939).
Brno.—Prirodovedecka Fakulta, Masarykovy University. Spisy (Publications) (Botanical
only), Cis. 263, 267 (1938); “The Profile of Equilibrium as a Basis of the Study
of River Terraces” by Jan Krejci (1939).
Brooktyn.—Brooklyn Botanic Garden. “Genetics”, xxiii, 6 (T.p. & c.) (1938); xxiv, 1-5
(1939).
BRUXELLES.—Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique.
Annuaire, 1939, 105m™e Année (1939); Bulletin de la Classe des Sciences, 5™° Sé6rie,
xxiv, 3-12 (T.p. & c.) (1938).—Musée Royal d Histoire Naturelle de Belgique.
Bulletin, xiv, 1-60 (T.p. & c.) (1988); Mémoires, Nos. 82-85 (1938); Mémoires, 2™°
DONATIONS AND EXCHANGES. xli
Série, Fasc. 13-14 (1938); Mémoires, Hors Série (Résultats Scientifiques du Voyage
aux Indes Orientales Néerlandaises), ii, 19; iii, 18-19 (1938).—Société Entomologique
de Belgique. Bulletin and Annales, Ixxviii, 3-12 (T.p. & c.) (19388); Ixxix, 1-5
(1939).—Société Royale de Botanique de Belgique. Bulletin, lxx, 2 (T.p. & c.); 1xxi,
1-2 (T.p. & c.) (19388-1939).—Société Royale Zoologique de Belgique. Annales, 1xviii,
1937 (19388); lxix, 1938 (1939).
Bupaprst.—‘Index Horti Botanici Universitatis Budapestinensis”’, iii (1938).
BuENos AIRES.—WMinisterio de Agricultura de la Nacion: Direccion de Propaganda y
Publicaciones. Publicacion Miscelanea, No. 43 (1938).—Sociedad Argentina de
Ciencias Naturales. Revista, ““Physis’’, xii, 44 (T.p. & c.) (1938).
BuITENzoRG.—N ederlandsch-Indische Entomologische Vereeniging. Entomologische
Mededeelingen van Nederlandsch-Indie, iv, 3-4 (1938); T.p. & ec. for ii-iv, 1937-1938
(19389) ; v, 1-3 (1939).
CaEN.—Société Linnéenne de Normandie. Mémoires, Nouvelle Série, Section Botanique,
i, 4 (Ep. &-e.) (1938).
CaiIRNS.—North Queensland Naturalists’ Club. “North Queensland Naturalist’’, vii, 56-58 ;
viii, 59 (all with Supplements) (19388-1939).
Ca.LcurrTa.—Geological Survey of India. Memoirs, |lxxii, 2 (T.p. & ¢.) (1938); Ixxili
(1939); Memoirs, Palaeontologia Indica, N.S. xxv, 1; xxvi, 1; xxvii, 1 (1939);
Records, Ixxii, 4 (T.p. & c.) (1938) ; xxiii, 2-3 (1938); Ixxiv, 1 (1989) ; Geographical
Index to the Memoirs, Vols. i-liv, Records, Vols. i-lxv and General Reports of the
Director for the Years 1897-1903 by T. H. D. La Touche (1938).—Zoological Survey
of India. Report for the Years 1935 to 1938 (19388) ; Memoirs of the Indian Museum,
xiii, 1 (1938); Records of the Indian Museum, T.p. & c. for xxxix; xl, 1-4 (1938).
CAMBRIDGE.—Cambridge Philosophical Society. Biological Reviews, xiii, 4 (T.p. & c.)
(1938); xiv, 1-3 (1939).—University of Cambridge. Abstracts of Dissertations
approved for the Ph.D., M.Sc., and M.Litt. Degrees during the Academical Year
1937-38 (1939).
CAMBRIDGE, Mass.—Museum of Comparative Zoology at Harvard College. Annual Report
of the Director for 1937-38 (1938); Bulletin, Ixxxii, 3-6 (T.p. & c.) (1938); Ixxxiii;
Ixxxiv (1939) ; Ixxxv, 1-3 (1938-1939).
CANBERRA.—Administration of the Territory of New Guinea. Geological Bulletin, No. 1
(1939).—Commonwealth Bureau of Census and Statistics. Official Year Book, No. 31,
1938 (1939).—Council for Scientific and Industrial Research: Divisions of Economic
Entomology and Plant Industry. Contributions (Economic Entomology), Nos. 128-
140; (Plant Industry), Nos. 101-109 (1938-1939).
Carn Town.—Royal Society of South Africa. Transactions, xxvi, 4 (T.p. & c.) (1938);
xxvii, 1 (1939).—WSouth African Museum. Annals, xxiv, 5 (T.p. & ¢c.); xxxii, 4
(1938); List of Papers published in Vols. i-xxx, together with an Index to Authors
and Subjects (1938).
CHANGSHA (formerly Peiping).—National Geological Survey .of China. Geological
Bulletin, Nos. 31-32 (1938).
CHICAGO.—Chicago Academy of Sciences. Bulletin, v, 6-8 (1938); “The Chicago
Naturalist”, i, 2-4 (Index) (1938).—Field Museum of Natural History. Botany,
Leaflet 22-23 (1938-1939) ; Zoology, Leaflet 14 (1938); Publications, Botanical Series,
xii, pt. 2, No. 3; T.p. & c. for xiii, pt. 2; xvii, 5; xviii, 3-4 (T.p. & c.); Title page
for xix; xx, 1 (1938-1939) ; Geological Series, vi, 21-22, vii, 4 (1938); Report Series,
xi, 2 (1938); Zoological Series, xiii, 11; xx, 30-37; xxii, 3-4; xxiv, 1-4 (1938-1939).
CHRISTCHURCH.—Canterbury Museum. Records, iv, 5 (1939).
CINCINNATI.—Lloyd Library of Natural History. ‘‘Lloydia’, i, 1-4 (T. p. & c.); ii, 1
(1939).
CLuUJ.—Gradina Botanica. Buletinul, xviii, 1-4, Appendix 1-2 (T.p. & c.) (1988); xix,
1-2 (1939).
xlii DONATIONS AND EXCHANGES.
CoLomsE0.—Colombo Museum. Spolia Zeylanica (Ceylon Journal of Science, Section B—
Zoology and Geology), xxi, 2 (1939).
CoLuMBUS.—Ohio State University and Ohio Academy of Science. “Ohio Journal of
Science”, xxxviii, 5-6 (T.p. & c.) (1938); xxxix, 1-4 (1939).—Ohio State University:
Ohio Biological Survey. Bulletin 35 (T.p. & c. for Vol. vi, Bulletins 30-35) (1938).
CoPENHAGEN.—Det Kongelige Danske Videnskabernes Selskab. Biologiske Meddelelser,
xiv, 3, 5-8 (T.p. & c.); xv, 1 (1939); Mémoires, Section des Sciences, 9™°® Série,
Dy (ez Cy LOL VIL EVA CI py sic.) Gi938))-
DuBLIN.—Royal Dublin Society. Scientific Proceedings, N.S. xxii, 6-14 (1939).—Royal
Irish Academy. Proceedings, xliv, Section B, 10-11 (T.p. & c.); xlv, Section B, 1-12 .
(1938-1939).
East LANSING.—Wichigan State College of Agriculture and Applied Science. Report of
the Division of Veterinary Science for the Year ended June 30, 1938 (no date).
EDINBURGH.—Royal Botanic Garden. Notes, xix, 95 (T.p. & c.) (1938); xx, 96 (1939);
Transactions and Proceedings of the Botanical Society of Edinburgh, xxxii, 3, Session
1937-38 (1938).—Royal Physical Society. Proceedings, xxiii, 1 (1939).—Royal Society
of Edinburgh. Proceedings, lviii, 2-3 (T.p. & c.); lix, 1 (1938-1939); Transactions,
lix, 2 (1938).
FRANKFuRT a.M.—Senckenbergische Naturforschende Gesellschaft. Abhandlungen, 440-443.
(1938) ; “Natur und Volk”, Ixviii, 6-12 (T.p. & c.) (19388); Ixix, 1-5 (1939).
GENEVA.—Société de Physique et d’Histoire Naturelle. Compte Rendu des Séances, lv, 3
CE:p: & c.) (1938) ; lvi,; 1=2 (1939).
GENOVA.—WMuseo Civico di Storia Naturale Giacomo Doria. sexin 1=9) (G938) 5) sexi d=9) F939) exexilis EK6
(1939).—Geological and Prospecting Service, U.S.S.R. Soviet Geology (formerly
Problems of Soviet Geology), viii, 5-12 (T.p. & c.) (19388); ix, 1-3 (1939).—JLenin
Academy of Agricultural Sciences in U.S.S.R.: Institute for Plant Protection. Plant
Protection, Nos. 16-18 (1938-1939); Institute of Plant Industry: Supplement 84 to
the Bulletin of Applied Botany, Genetics and Plant Breeding (1938).—Société
Entomologique de VU.R.S.S. Revue d’Entomologie de 1’U.R.S.S., xxvii, 3-4 (1938).
LikcEe.—Société Royale des_Sciences de Liége. Bulletin, 7™* Année, 3-12 (T.p. & c.)
(1938); 8me Année, 1-5 (1939).
Lispoa.—Universidade de !Lisboa, Faculdade de Ciencias, Instituto Botanico. Trabalhos,
iii (1935-1936). ‘
LiIvERPOOL.—Liverpool School of Tropical Medicine. Annals of Tropical Medicine and
Parasitology, xxxii, 3-4 (T.p. & c.) (1938); xxxiii, 1-2 (1939).
LIUBLJANA (Yugoslavia).—Prirodoslovno drustvo (Natural Science Society). Prirodo-
slovne Razprave, iii, 9-11 (1938-1939).
LONDON.—British Museum (Natural History). Great Barrier Reef Expedition, 1928-29.
Scientific Reports, v, 5 (1937); vi, 1 (1938); Mosquitoes of the Ethiopian Region.
Part 2. By the late Alwen M. Evans (1938); The British Rhaetic Flora. By T. M.
Harris (1938).—Geological Society. Quarterly Journal, xciv, 3-4 (T.p. & c.) (1938);
xev, 1-2 (1939).—Linnean Society. Journal, Botany, li, 337 (1937); 340 (T.p. & c.)
(1938); lii, 341 (1939); Zoology, xl, 271 (1937); 273-274 (1939); Proceedings,
150th Session, 1937-38, 4 (T.p. & c.) (1938); 151st Session, 1938-39, 1-3 (1939).—
Ministry of Agriculture. Journal, xlv, 7-12 (T.p. & c.); xlvi, 1-6 (1938-1939) ;
xliv DONATIONS AND EXCHANGES.
Register of Accredited Poultry Breeding Stations and Accredited Hatcheries 1939
(1938).—Royal Botanic Gardens, Kew. Bulletin of Miscellaneous Information, 1938
(1939) ; Hooker’s Icones Plantarum, Fifth Series, iv, 3-4 (T.p. & c.) (1938-1939).—
Royal Entomological Society. Proceedings, Series A, xiii, 7-12 (T.p. & ¢.); xiv, 1-8
(1938-1939) ; Series B, vii, 10-12 (T.p. & c.); viii, 1-8 (1938-1939); Transactions,
Ixxxvii, 6-23 (T.p. & c.) ; lxxxviii, 1-7; Ixxxix, 1-8 (1938-1939).—Royal Microscopical
Society. Journal, Series iii, lviii, 3-4 (T.p. & c.) (1938); lix, 1 (1939).—Royal
Society. Philosophical Transactions, Series B, ccxxix, 559-564 (T.p. & ec.) (1938-
1939); ccxxx, 565-568 (1939); Proceedings, Series B, cxxvi, 842-845 (T.p. & c.);
exxvli, 846-848 (19388-1939).—Zoological Society. Proceedings, eviii, Series A, 3-4
(T.p. & ¢.); Series B, 3-4 (T.p. & c.); Series C, 8-13 (T.p. & c) (1988); cix,
Series A, 1-3; Series B, 1-2 (1939); Transactions, xxiv, 2-4 (1938-1939).
Los ANGELES.—See under Berkeley, University of California.
Lunp.—K. Universitets i Lund. Lunds Universitets Arsskrift (Acta Universitatis
Lundensis), Ny Foljd, Avd. 2, xxxiv, 1938 (1938).
Lyon.—Société Linnéenne de Lyon. Annales, N.S. Ixxiii, 1926-27 (1928); Bulletin
Mensuel, 7®@ Année, Nos. 1-10 (Contents) (1938).
MapiIson.—Wisconsin Academy of Sciences, Arts and \Letters. Transactions, xxxi (1938).
MANCHESTER.—Conchological Society of Great Britain and Ireland. Journal of Conchology,
xxi, 3-5 (19388-1939)—Manchester Literary and Philosophical Society. Memoirs and
Proceedings, Ixxxii, 7-9; pp. i-lii (T.p. & c.) (1938); Ixxxiii, 1-5 (1938-1939).—
Manchester Museum. Museum Publication 115 (1938).
MANHATTAN.—American Microscopical Society. Transactions, lvii, 4 (T.p. & ce.) (1938);
Iviii, 1-3 (1938).
MANILA.—Bureau of Science. “Philippine Journal of Science’, Ixv, 1-2; Ixvi, 2-4
(Uti, Cs G)) 8 Ibaiah, ale4b (GM, Cs @hyys Ibaati aloth (Uubey We @)) 9 Ibebic, lech (Ubi Ae ce.)
(1938-1939).
MARSEILLE.—Faculté des Sciences de Marseille. Annales, 2° Série, x, 3 (T.p. & ec.) (1937);
xi, 1 (1938).
MELBOURNE.—‘‘Australasian Journal of Pharmacy”, N.S. xix, 226-228 (Index) (1938);
xx, 229-237 (1939) (From the Publisher).—Council for Scientific and Industrial
Research. Twelfth Annual Report for Year ended 30th June, 19388 (1938); Bulletin,
Nos. 121-129 (1938-1939); Journal, xi, 4 (T.p. & ¢c.) (19388); xii, 1 (with Supple-
ment), 2-3 (1939); Pamphlet, Nos. 85-90 (1938-1939).—Department of Agvicultiu7e
of Victoria. Journal, xxxvi, 11-12 (T.p. & c.) (1938); xxxvii, 1 (with Supplement),
2, 3 (with Supplement), 4 (with Supplement), 5-10 (1939).—Field Naturalists’ Club
of Victoria. ‘‘The Victorian Naturalist’, lv, 7-12 (T.p. & c.); lvi, 1-6 (19388-1939).—
McCoy Society for Field Investigation and Research. Reports, No. 3 (1939).—
Royal Society of Victoria. Proceedings, li (N.S.), 1-2 (T.p. & ec.) (1939).—Unviversity
of Melbourne. Calendar for 1939 (1938).
Mexico.—Instituto de Geologia: Universidad Nacional de Mexico. Memoria de la
Comision geologica del Valle del Mezquital, Hgo (1988).
Monaco.—IJnstitut Oceanographique de Monaco. Bulletin, Nos. 749-760 (T.p. &’c. for
Nos. 739-760) (19388); 761-775 (1939); Rapport pour l’Année 1937, 1938 (no date).
MoNTREAL.—ZJnstitut (formerly Laboratoire) Botanique de VUnviversité de Montréal.
Contributions, Nos. 29-31 (1937-1938); “Un Manuscrit Botanique Prélinnéen.
L’ ‘Histoire des Plantes de Canada’’’, par Frére Marie-Victorin (From Revue
Trimestrielle Canadienne, Septembre, 1936); “Le Président de l’Acfas pour 1937-38:
le Frére Marie-Victorin. Biographie et bibliographie’ par Marcelle Gauvyreau (From
Annales de VAcfas, iv, 114-189) (1938).
Moscow.—Kossino Limnological Station of the Hydrometeorological Service of U.S.S.R.
Proceedings, xxii (1939).—‘‘Microbiology”’’ (a Journal of General, Agricultural and
Industrial Microbiology), vii, 5-10 (1938).
DONATIONS AND EXCHANGES. xlv
MUNCHEN.—Bayerische Akademie der Wissenschaften. Abhandlungen, Mathematisch-
Naturwissenschaftliche Abteilung, Neue Folge, 45 (1939); Sitzungsberichte, 1938,
1-2, (T.p. & c.) (1938); “Georg Simon Ohm” by W. Ferlach (1939); “Richard von
Hertwig’’—Gedachtnisrede, by Karl von Frisch; “Wissenschaft und Volk’’—Festrede,
by J. Zenneck (1938).
NANTES.—Société des Sciences Naturelles de VOuest de la France. Bulletin, 5™e Série,
vii, 1937, 1-4 (T.p. & c.) (19388).
NAPLES.—Stazione Zoologica di Napoli. Pubblicazioni, xvii, 1-3 (T.p. & ce.) (1938-1939).
New DsELHI.—Imperial Agricultural Research Institute. Agriculture and Animal Hus-
bandry in India, 1936-37 (1939); Catalogue of Indian Insects. Part 24 (1939);
Scientific Reports for the Year ending 30th June, 1938 (1939); ‘‘The Indian Journal
of Agricultural Science”, viii, pt. 4, 4 Articles; pt. 5, 5 Arts.; pt. 6, 4 Arts.; ix, pt. 1,
@ ANCES fot 75 D> AWEESS jos Bo . 356
Metembia (Hmbioptera) .. .. .. 474 Saussurella (Hmbioptera ) Ge be DUS.
Neohemigaster (Otitidae) new name 126 Thalamarchidae (Lepidoptera) .. 335
ey
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PROCEEDINGS
OF THE
_ LINNEAN SOCIETY
Crease " 5 v ~
OF
NE EW | SOUTH Wat ES
- : “FOR THE YEAR —
1939. -
Par ‘ts I-II (Pages i-verrii; 1- -2i6).
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AND PAPERS READ IN MARCH-APRIL.
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The dear Society of of New: South Wales
LIST OF OFFICERS AND COUNCIL, es a ea
a President: — jp eee f
Professor J. Macdonald Holmes, B.Se., Ph. ID 5% Be MAREE:
( Vice-Presidents: age a $5 ae ¥
W. L: Waterhouse, D.Se. Aer. E. C. Andrews, B.A. 7
Cc. A. Sussmilch. Abe Cc. Roughley, “B.Sc, ~
\ . -
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CSuerebaby: 1h B. Walkom, D.Se. : seine ei
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¢. Anderson, M.A., D.Sc. ~~ ALF, Basset Hull. be uzee
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Professor E. Ashby, D.Se. F. H. Taylor. a eis ;
5 W. R. Browne, D.Sc. -E. Le G. Troughton. ~ ae es 5 ae
Professor A. N. Burkitt, M.B., B.Se. A. B. Walkom, D.Se. ~ per eS
~ E. Cheel. * _- H.S. BH. Wardlaw, D.Sc. Se ee ie
Profesor W. J: Dakin, D.Sc. ' -G. A. Waterhouse, D5 5. of 0 OSS OS Es oad Wag as by Pia
1902 - i poe) TGs 7 6 1-15 0.
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zak f p= ty Ap IT 5 = 3 ~
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2 Supplement e 6d. additional, “Supplement 1s. additional. Sous
* Supplement. 2s. 6d. additienal. - Boe Smulees 2s, 6d. additional. }
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2 oe A
~ i x =\
. BY J. R. MALLOOH. Sie : 465 Sic
Je hens _ EXPLANATION OF PLATE ES its DO irae pene repay ref
A Fig 1—Dacus: papuaensis, Qn. SD. _ Wing, . type. x 6: Bis ue ees : ae, ae
Fig. 2.—Dacus albolateralis, n. sp. Wing, type. x 6: 5. es pace PGE SS ae eae
| Fig. . 3.—Pseudosophira bakeri, n, sp. Wing, type x 5. Ga etre pepe Sh Gee ae GR 2
‘ s Fig. 4.—Polyara insolita Walker. Wing. x 5. 45x : GHe es
Serie Z a ). ‘Fhemarohystrix flaviceps, n. sp. Wing, paratype. x 5: Be re ite :
Fig. - 6.—Themarohystria suttoni, n. sp. “Wing, paratype. x 6-5... _ Za pe
- Fig. 7.—Clusiosoma biseriata, n. sp. Wing, paratype. ~x 65. Eee tes Z ASR Eee :
se 2 Rig. 8. —Clusiosoma puncticeps, Keo: “Wing, type. x 6:5. sc te i bine sa
‘ig. 9.—Acanthoneura nigriventris; n. sp. Wing, type. x 5. ~- ep staat, ees
“Fig. 0 eothemara formosipennis Walker.’ Wing. x 5. af | = eae
Piet tk —Pseudacanthoneura septemnotata, n. ‘sp. Wing, type. MSHS Lad Sey RT RM
- Fig. 12 .—Diarrhegmoides hastata, n. sp. Wing, allotype. x 65, PR ers pte PES
| ‘Fig. ‘Ear —Hexacinia. multipunctata, n. sp. Wing, paratype. x 6: 8. ‘ : é Beas
za Fig. 14.—Pseudina buloloae, n \sp... Wing, type. -x 6°5. Pee ae Seka ie cgi
, ee, 15.—Anomoea nigrithorax, n. sp. Wing, type. x 6 58 J - : ES Ny ea gee 1 PSS ape
‘ 16 .—-Pseudospheniscus taylori, n. sp: Wing, type. K 65. Serene oA ee : Sik :
Fig. ‘H.—Ceratitella loranthi. (Froggatt). Wing. x 6 8. 5 le tiene = Ee sey So eee
Fig, 18. —ephrella australis, n. sp. “Wing, type. x 6:5... e =! * : ae ae see
Fig. 19, —Spathulina acroleuca (Schiner). Wing. x 65. wees ates ee a a ie er fn
Fig. 20:—Chrysotrypanea trifasciata, he spi Wing, ‘tyre. X65; 2+ a ae : = Gates: ats
* Fig. 21.—Platensina parvipuncta, Nn. sp. Wing, type. pbeos 3G a pape e See
_ Fig. 22: ~—Sphenella marginata Fallen. » Wing. x 6:5. ep ce te ze SERS SNCS REE SA as oe ag
Fig. 23. —Camaromyia bullans Wied. Wing. x & ae an OSes Cat : os
ae 4, —Fephritis pelia Schiner, Wing. Fee inant oN Se : Nan : ot Rak
Fig: 25.—Trypanea glauca Thoms. Wing. x-6-5. 39 : ‘pie
os 26. Perk aronune sororcula Wied. - Wing. %-6:5- ee
PROCEEDINGS, , 1939, PARTS 3-4,
CONTENTS.
Taxonomic Notes on the Order Embioptera. ii. A New Neotropical Genus
of Embioptera. By Consett Davis, M‘Se. (Twenty-one Text-figures. )
A New Species of Chalcid (Genus Hurytoma) associated with Tepperella
trilineata Cam., a Wasp causing Galling of the Flower Buds of
Acacia decurrens.’ By N. S. Noble, DStyEte M.Sce., D.1.C. (Twelve
Text-figur es.)
The Upper Pdlaeozoic Hecke petwaen Mount Conrce and Winehan.. N. S.
Wales. By A. H. Voisey, M.Sc. (One Map and three Text-figures.)
The Lorne Triassic Basin and Associated Rocks. By A. H. Vesey: M.Sc.
(One Map and two Text-figures.). . ke
A New Species of Megastigmus ASS on Tepperene ees Can a
Wasp causing Galling of the Flower Buds of Acacia decurrens. By
N. S. Noble, D.Se.Agr., M.Sc., D.I.C. (Ten Text-figures.) “
A Reconnaissance Survey of the Vegetation of the Myall Lakes. By Prof.
, T. G@. B. Osborn, D.Sc., F.L.S., and R. N. Robertson, Ph.D., ee
(Plates vi-vii and three Text-figures.) aa Be 4
Australian Coleoptera. Notes and New Biatiese Now Xi. ~ (Mostly
Hlateridae.). Byokie = Ji: cae B.A., F.R.E.S. (Plates vili-ix_and
one Text-figure.) é
The Genus Adrama, with Beseriptone: of Three Nees Species! (Caiman:
Trypetidae). By John R. Malloch.. (Communicated by Frank H.
Taylor, F.R.E.S., F.Z.S.) (Two Text-figures.) .. _
A New Family of Lepidoptera. By A. Jefferis en M. D., “ER. E. S.
Hymenopterous Parasites of Embioptera. By Alan P. Dodd ;
Miscellaneous Notes on Australian Diptera. -vi. Dolichopodinge. By
G. H. Hardy
Observations on the Bipnemicn a Marnhiotoey of ‘Seren Sneciss of thé:
Tribe Paropsini (Chrysomelidae). By D. Margaret Cumpston,
__ M.Se., Linnean Macleay Fellow of the See in Zoology. (Plate X
and twenty-two Text-figures. ) Woe Rae Sy
The Diptera of the Territory of New Guinea. xe Gea ish Ceratapoeonnine:
-By J. W. S. Macfie, M.A., D.Se., F.R.E.S. (Communicated q Frank Hi.
Taylor, F.R.ES., F.Z.8.) (Two Text-figures.) . 3
Taxonomic Notes on the Order Embioptera. iii. The Genus Burmitembdia
Cockerell. By Consett Davis, M.Sc. (Six Text-figures.)
Taxonomie Notes on the Order Embioptera. iv. The Cats Clothodes
Enderlein. By Consett Davis, M.Sc. (Twenty-five Text-figures.) ~
Taxonomic Notes on the Order Embioptera. -y. The Genus Wonnconeis
Enderlein. By Consett Davis, M.Sc. (Five Text-figures.) .
The Geology of the County of Buller, N.S.W. By A. H. veer M.Sc.
(One Map and two Text-figures.) . : 5
The Geology of the Lower Manning District of New South Wales: By
A. H. Voisey, M.Sc. (One Map and one Text-figure. ) .
A Note on the Synonymy of Leptops (Coleoptera: Cnreilionidacy. By
K. C. McKeown . hs a. UNvny Nova pee ened ata en
The Diptera of the Territyty. of New ainea” xi. Family Trypetidae.
By John R. Malloch. (Communicated by Frank H. Taylor, F.R.E.S.,
F.Z.8.) (Plate xi and fifteen Text-figures. )
*
Pages.
217-222.
223-241
242-254
255-265 °
266-278.
279-296
297-330
381-334
335-337
338-344 ~
345-352
353-366
369-372
373-380
, 381-384
385-393
394-407 -
408
409-465
8 7.
367-368
: (Issued 15th December, 1989.)
: i Vol LXiv Se SE
Parts 5-6. .
ef PROCEEDINGS
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Pt New SouTH WALES
FOR THE YEAR z ae
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1939. AN) Cer
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Bats) Parts V-VI (Pages 466-608); xexiii-levii. Ree fae ARY)|
‘ CONTAINING PAPERS READ IN SEPTEMBER-NOVEMBER, & \ Pes } a
. ~~ ABSTRACT OF PROCEEDINGS, DONATIONS AND EXCHANGES, \— AN ye
LIST OF MEMBERS, AND INDEX. : Seca Zs “e aSy >
With one plate. XW 4 ®
ERlate xiii Ne 3
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LINNEAN SOCIETY
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C. Anderson, M.A., D.Sc. ‘A. F. Basset Hull.
R. H. Anderson, B.Sc.Aer. T. C. Roughley, B.Sc. _
E. C. Andrews, B.A. Cc. A. Sussmilch.
Professor BE. Ashby, D.Sc. ‘ F. H. Taylor. 2.
W.-R. Browne, D.Sc. | E. Le G. Troughton.
Professor A. N. Burkitt, M.B., B.Se. _A. B. Walkom, D.Sc.
E. Cheel. H. S. H. Wardlaw, D.Sc.
Profesor W: J. Dakin, D.Sc. G. A. Waterhouse, D.Sc., BE. “4
A. G..Hamilton. BWA
Professor J. Macdonald Holmes, B.Sc.,
Ph.D.
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Sedo sedis 1s Od. Seedy Yee Reet Oy s. d Ss. d. 8.(d.
has oe 3- 0 3 0 5 0 C28 1899... ~ | 12-6 12 0 10 0-| 10 6
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1878 ee 5 0 5 0 GEO ae eo. 1901 : eel OsG 90 SD. SOrss L7e7 One
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1 Supplement is. 6d. additional. _ ; “Supplement 1s. additional. : ie
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The Linnean Society of New South _ Wales
LIST OF OFFICERS AND COUNCIL, 1939-40. oe is
)
- GF = x. Js
President: »-
Professor J. Macdonald Holmés, B.Sc., Ph.D. bias ; bi.
‘Vice-Presidents: ; a
W. L. Waterhouse, D.Sc.Aegr. B. C. Andrews, B.A, ~~
Cy A. Sussmilch. Thee TOs Rous nleys B.Se..
Hon. iiecanGeBee G. A. Waterhouse, D.Se., B.E.
Secretary: A. B. Walkom, D.S@
L. Waterhouse, DuSe: PASE. Bee z ats
a : + A
A a _ Auditor: F. ea Ss oe: 2 z eae \
: 4 NOVICE.
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oF THE ProceEDives Ussuea Lath February, 1926]. rose 08.
as Ae ta es A oe m Seat we
ase
= By y William Macleay, FL. Ss. “(18811
=
PROCEEDINGS, 1939, PARTS 5-6.
CONTENTS.
Pages
The Association between the Larva described as Trombicula hirsti var.
buloloensis Gunther 1939, and YTrombicula minor Berlese 1904.
(Acarina: Trombidiidae.) By C. E. M. Gunther, M.B., B.S., D.T.M,
(Three Text-figures.) Moafarthe Shep a Weert Vo Tk ake ie ona ee AES Ee 2 Ne REO)
; %
Observations on the Life-history of Neoschdngastia, kallipygos Gunther
1939. (Acarina: Trombidiidae.) By C. E. M. Gunther, M.B., B.S., fe
DTM set aC Two ext hi Sires ys es 50 sis 8 a Ne a ee cd NCR re wae eb es fem ASS
Taxonomic Notes on the Order Embioptera, vi-x. By Consett Davis,
M.Sc. (Eighty-three TOXE-HEMTOS:) st) ae 474-495
Elementary Hydrography of South-eastern Australia. By Frank A. Craft,
B.Se. (Ten ‘Text-figures.) Ae Caley RR, < “cteey, tks cc bibs Seen Gee Ameo PLO aenL
Strongylate Nematodes from Marsupials in New South Wales. “By ~
Professor T. Harvey Johnston and Patricia M. Mawson. (Sixty-six
Text-figures. ) net ite tmgeleap ene Lapis yetnarn, eta Dee) ees] Real teens tne cae eee ate ey rteael
Ectocarpus confervoides (Roth) Le Jol. By Valerie May, B.Sc., Linnean
Macleay Fellow of the Society in Botany. (Forty-six Text-figures.) 537-554
A Note on the Re-examination of Australian Species of Ceratopogonidae
(Diptera). By J. W.S. Macfie. (Communicated by Frank Be Taylor, ce
F.R.E.S., F.Z.S.) (Three ‘Text-figures.). WAG of A) ACY SE eH Ea de 555-558
Taxonomic Notes on the Order Embioptera. xi-xiv. By a Davis,
M.Se; (hifty-onéesRexttisyres. i) 210.42. Save Bateees, cement mee rae 559-575
The General Geology of the District east of Yass, N.S.W. By Kathleen
Sherrard, M.Sc. (Plate xii and three Text-figures.) «ue rahe espero aec oh OM OOO.
Contributions to the Microbiology of Australian Soils. v. Abundance of
Microorganisms and Production of Mineral Nitrogen in relation to
Temperature. By H. L. Jensen, Macleay Bacteriologist to the Society.
(Hive. Mexistipunes.)* os? sone igs OOP Reece oe ge ee ee OT SOUS
Abstract of Proceedings .. .. Ree eed es Wh ages Ohm eee Seite >
Donations and Exchanges at i deg ete BIE ot art Dae sha toy Ecieenliy ;
Take de, Members cor os brane Te a ey ee K, eS Liv
Index Stil adage AAV IXV-
EIS ROL ePIQUCS tiert sone er laiap tases pene ek Se ots ts ie ea a ame eee Ixvii
List of New Family and Genera .. .. .. a DONE As a eee 5 OAXViL
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