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TRANSACTIONS 


OF THE 


BOYAL,. SOCIETY OF | VilGiORaLA. 


VOD: Is.< = PART: 


1890. 


CONTENTS. 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS AS 
AIDS IN THE DETERMINATION OF SPECIES, sy D. McAtrrnz, 
F.C.S., anp J. R. Remrrey. (With Plates 1, 2, 3, 4, 5, 6, and 6a) = 


THE VICTORIAN LAND PLANARIANS, sy Artnur Denpy, M.S8c., F.L.S., 
Demonstrator anD Assistant LecrurER IN BioLogy IN THE UNIVERSITY 


or Metzourne. (With Plate 7) . - - - - - = 


THE EUCALYPTS OF GIPPSLAND, sy A. W. Howitt, F.G.S. (With 
Plates 8, 9, 10, 11, 12, 13, 14, 15, 16) - = = = : : 


A NEW FAMILY OF HYDROIDEA, TOGETHER WITH A DESCRIPTION 
OF THE STRUCTURE OF A NEW SPECIES OF PLUMULARIA, 
py W. Banpwin Spencer, M.A., Prormssor orf BroLogy IN THE UNIVERSITY 
oF Mretgourne. (With Plates 17, 18, 19, 20, 21, 22,23) - - - 


EDITED BY PROFESSOR W. BALDWIN SPENCER, M.A., HON. SEC. 


} 


_ 


~' MELBOURNE. 


PUBLISHED FOR THE ROYAL SOCIETY 


PAGE 


81 


BY THE SPECTATOR PUBLISHING COMPANY LIMITED, 270 POST OFFICE PLACE. 


Aprit, 1891. 


ened, SOCOM PY OR VICTORLA. 


Patron : 


HIS EXCELLENCY THE EARL OF HOPETOUN, G.C.M.G. 


President : 


PROFESSOR W. C. KERNOT, M.A., C.E. 


Vice-PPresidents : 


Hed) WEE BRAGS: | J. COSMO NEWBERY, B.Sc., C.M.G. 


tbon. Treasurer : 


JAMES JAMIESON, M.D. 


‘bon. Secretaries : 


H. K. RUSDEN, F.R.G.S. 
PROFESSOR W. BALDWIN SPENCER, M.A. 


bon. Librarian : 


JAMES EK. NEILD, M.D. 


C. R. BLACKETT, F.C.S. 
J. BOSISTO, C.M.G. 
R. L. J. HLUERY, F.RB.S. 


G. 8. GRIFFITHS, F.R.G.S. 


xh W. HOWLED? BGs: 


A. H. 8. LUCAS, M.A., B.Sc. 


Council : 
PROF. ORME MASSON, M.A., D.Sc. 
| H. MOORS. 
PROF. R. T. LYLE, M.A. 
ALEXANDER SUTHERLAND, M.A. 
, C. A: TOPP, M.A., ULB. 
Ree StaWAY, Asks 


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TRANSACTIONS 


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VOR. PARI. 


1890. 


CONTENTS. 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS AS 
AIDS IN THE DETERMINATION OF SPECIES, sy D. McAtrring, 
F.C.8., anp J. R. Remrrey. (With Plates 1, 2, 3, 4, 5, 6, and 6a) : 


THE VICTORIAN LAND PLANARIANS, sy Artuur Denpy, M.Sc., F.L.S., 
DEMonsTRATOR AND AssiIsTANT LecTURER IN BioLoey In THE UNIVERSITY 
or Metsourne. (With Plate 7) - - : - - - - 


THE HEUCALYPTS OF GIPPSLAND, sy A. W. Howirr, F.G.S. (With 
Plates 8, 9, 10, 11, 12, 18, 14, 15, 16) - - = - - . 


A NEW FAMILY OF HYDROIDEA, TOGETHER WITH A DESCRIPTION 
OF THE STRUCTURE OF A NEW SPECIES OF PLUMULARIA, 
BY W. Batpwin Spencer, M.A., Proressor oF BroLtoay in THE UNIVERSITY 
or MetBournE. (With Plates 17, 18, 19, 20, 21, 22,23) - - = 


EDITED BY PROFESSOR W. BALDWIN SPENCER, M.A., HON. SEC. 


MELBOURNE. 


PUBLISHED FOR THE ROYAL SOCIETY 


PAGE 


81 


121 


BY THE SPECTATOR PUBLISHING COMPANY LIMITED, 270 POST OFFICE PLACE. 


ApRiL, 1891. 


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ARTICLE I.—Tue Transverse Sections or Pretriones or EUCALYPTS AS AIDS IN 
THE DETERMINATION oF Species, By D. McArping, F.C.S., anp J. R. Remrry. 
(With Plates 1, 2, 3, 4, 5, and 6.) 

(Read Thursday, November 14th, 1889.) 


I.—IntrRoDUCTORY. 


The Eucalypts form such a prominent feature in the Australian vegetation, and 
have such varied uses, that any addition to our knowledge of their characters is sure 
to be welcomed. 


The primary object of the present paper is to show how transverse sections of 
the petioles of Kucalypts may be used as valuable aids in the determination of 
species. Sections of thirty different kinds are here described and photographed, and 
they show unmistakably, along with a general resemblance, differences which are 
more or less constant, and readily recognisable for each species. 


Anatomical characters of the leaf have already been successfully used in the 
discrimination of species belonging to other divisions of the vegetable kingdom.* 
Of course such characters, depending on a single organ, and apart from the aggregate 
of characters, are apt to be more or less artificial ; but, when we consider that the 
parts shown in transverse section of the petiole are in organic connection with, and 
form an essential portion of, the vital machinery of the plant, it need not excite 
surprise that they should vary in the different species, and be, to a certain extent, 
characteristic for each. 


We know that the leaf is simply a lateral expansion or extension of the stem or 
branch, usually bearing a bud in its axil, and its tissues are, as a rule, continuous 
with those of the stem, so that in it we have an epitome of the parts concerned in 
vegetative life—a point deserving of special notice in this connection. Besides, the 
petiole, with which we are more particularly concerned, is capable of reproducing 
the entire plant from a small portion of it, as in the well-known instance of the 
ipecacuanha plant. The vegetative organs which, in some form or another, are 
absolutely necessary for the life of the individual, have been too little used in the 
discrimination of genera and species, while the reproductive organs have been too 
often almost exclusively relied upon. The anatomist (dealing with internal structure) 
and the systematist (often entirely occupied with external characters) must combine 
their results in order to arrive at a proper conception of the true system of nature. 


* See De Bary, Comp. Anat. of Phanerogams and Ferns, p. 298. 


2 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Perhaps one result of this investigation will be to direct attention to the 
distinctive nature of the tissues of the leaf in other groups of plants as well as the 
Eucalypts. This has already been done, for instance, in the Gnetaceae and Coniferae 
by Dr. C. EK. Bertrand* and Prof. M‘Nab.+ The latter confined his attention to the 
Coniferae, and, in addition to the general anatomic structure of the transverse section 
of the leaf, noted the distribution and number of the resin-canals, and the arrange- 
ment of stomata on the surface, as aids in his diagnosis. 


While we have likewise described and drawn the transverse section as a whole, and 
found the total characteristics of the section of any species to be of great value for 
identification, there are certain features very useful for that purpose, even when 
taken alone. Thus, the cortical cavities, whether many or few, large or small; the 
size and shape of the section; the relative thickness of the epidermis, &c.; but it is 
the woody-tissue forming characteristic figures which is the most striking part. 
This wood-pattern is fairly constant for each, so that the most enduring part of the 
entire section fortunately gives a clue to the affinity sought for. 


It would appear that even from an economic standpoint some reliable means 
are much needed for determining a given species of Kucalypt, from a readily accessible 
portion of the plant, such as the leaf. It is highly desirable, in the interests of 
trade, not to speak of science, that one species should not be confounded with 
another, for the timber has such specific variations that serious loss and mischief 
might in many cases ensue. 


Mr. Maiden, of the Technological Museum, Sydney, in his recently published 
work on the ‘“‘ Useful Plants of Australia,” writes on this subject, at p. 427, in very 
decided terms :—‘‘ Scarcely a branch of Australian economic botany is in a more 
confused state than that which pertains to the timber of the Eucalypts. The genus 
is, perhaps, the most difficult one in the world, intrinsically, and also because of 
accidental circumstances, t.e., difficulty of obtaining flowers and fruit, and irregular 
flowering seasons; moreover, the trees vary, according to climate and soil, to such 
an extent as to render a definition of the species rather expansive, and, as this 
difficulty often extends to the wood, timbers of totally different character are 
sometimes reckoned under the same species.” 


Such a state of matters calls for some remedy, and it is evident that the present 
investigation tends in that direction. The leaves being evergreen are a constant, 
and not an accidental circumstance. The deep-seated characters revealed by the 
section are not so variable as others more dependent on soil and climate; and a 
definition which is included in, and shown by, the transverse section of a petiole, 
can hardly be called expansive. 

* Anatomie Comparée des Tiges et des Feuilles chez les Gnetacees et les Coniferes. Paris, 1874. 


+ Proc. Roy. Irish Acad., Series II., Vol. Il., 1875-77. Remarks on the Structure of the Leaves of certain Coniferae, 
and a Revision of the Species of Abies. 


AS AIDS IN THE DETERMINATION OF SPECIES. 3 


In the masterly monograph on the Eucalypts of Australia and adjoining islands, 
the ‘ Eucalyptographia,” by Baron von Mueller, there are numerous references to 
the anatomic structure, both of the wood and the leaf-blade, although none of them 
are concerned with the petiole. In one instance (Decade 7) he has given transverse 
sections of Eucalyptus wood, accompanied by the remark :—‘‘ These microscopic 
sections are given to aid in the discrimination of mercantile Kucalyptus timber of 
doubtful origin, such as sometimes occurs in the trade.” Here we have a distinct 
recognition of the idea, and a practical expression of it, that the minute structure 
of the wood may be useful in determining species, and be serviceable from the 
timber merchant’s point of view. Similarly in the wood-pattern of the leaf-stalk, 
there are serviceable characters for the same purpose. 


It may be noted here that the existence of such a work as the ‘ Eucalypto- 
graphia’’ invests the present investigation with a special importance. There the 
different species of Kucalypts are fully described and carefully drawn, and we have 
the advantage of working out a genus from which we can select numerous well- 
defined species. 


The species selected on the present occasion are such as were conveniently 
obtainable from the Melbourne Botanic Gardens. Our best thanks are due to Mr. 
Guilfoyle, F.L.8., Director of the Gardens, for kindly supplying us with fresh 
specimens when required. Thirteen of these are Victorian, and as there are 38 
altogether, according to the ‘“‘ Key to the System of Victorian Plants,’’ we hope to 
deal with the remainder in a future paper. 


We are also much indebted to J. Bosisto, Esq., C.M.G., for supplying us with 
the leaves of some of the oil-yielding species from their native habitats, and for 
information contained in various papers read at different times before learned 
societies. 


Above all, we have to thank Baron von Mueller for verifying each of the 
species used in this investigation, and thereby enhancing the value of the work— 
the determination coming from such an undoubted authority on this special group 
of plants. 


The type sections were prepared and the photographs taken by Mr. Remfry. 


Since the work has been in hand for over four years (the first sections having 
been cut about September, 1885), it has been possible to show the structure of 
the leaf-stalk at different seasons, and even in different years; and, as over a 
thousand sections have been made, a fair idea of the incidental variation is likewise 
given. 


4 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


LIST OF FORMS INVESTIGATED, ALPHABETICALLY ARRANGED. 


Boranicat Name. Common Name. 
1. E. alpina, Lindley a8 a0 00 VY. Alpine Gum 
2. ,, amygdalina, Labillardiére .. 30 Vy. hee Tree 
3. ,, calophylla, R. Brown oo on Calophyllum-like Eucalypt 
4. ,, citriodora, Hooker .. o6 fe Lemon-scented Eucalypt 
5. ,, cornuta, Labillardiére 36 BO “Yate” 
6. ,, corynocalyx, F. v. M. 06 50 V. Sugary Eucalypt 
7. ,, diversicolor, F. v. M. a0 am “ Karri” 
8. ,, ficifolia, F.v.M. .. 3 ae Scarlet-flowered Eucalypt 
9. ,, globulus, Labillardiére i = V. Blue Gum Tree 
10. ,, gomphocephala, Candolle .. ute ‘‘ Touart ” 
11. ,, pachypoda, F.y.M... 00 ae Thick-stalked Eucalypt 
12. ,, gunnii,J.Hooker .. an a0 V. Cider Eucalypt 
13. ,, lehmanni, Preiss .. dc 30 Lehmann’s Eucalypt 
14. ,, leucoxylon, F. v. M... ne ae VY. Victorian Ironbark Tree 
15. ,, macrorrhyncha, F.v.M. .. 56 V. Victorian Stringybark Tree 
16. ,, maculata, Hooker .. 50 oo Spotted Eucalypt 
17. ,, marginata, Smith .. te KA “ Jarrah ”’ 
18. ,, megacarpa, F. v. M... 60 oe West Australian Blue Gum Tree 
19. ,, melliodora, Cunningham .. 56 V. Yellow Box Eucalypt 
20. ,, obcordata, Turezaninow .. bc “* Maalok ” 
21. ,, obliqua,l’Heritier .. . a V. Messmate Stringybark Tree 
22. ,, occidentalis, Endlicher ie ai Flat-topped Yate 
23. ,, punctata, Candolle .. Se oO Leather Jacket 
24. ,, rostrata, Schlechtendal aa a VY. Red Gum Tree 
25. ,, rudis, Endlicher Sa Fs 5 Swamp Gum Tree of Western Australia 
26. ,, saligna, Smith ae ie 30 Grey Gum 
27. ,, sStuartiana, F.v. M. .. ete ote V. Apple-scented Eucalypt 
28. ,, tereticornis, Smith .. ah =f VY. Flooded Gum Tree 
29. ,, tetraptera, Turczaninow .. no Four-wing-fruited Eucalypt 
30. ,, viminalis, Labillardiére He A V. Manna Eucalypt 


Thirteen Victorian species (V), out of a total of thirty-eight, recorded in ‘‘ Key to the System of Victorian Plants,” 
by Baron Ferd. von Mueller. 


IJ.—Mope or Preparation AnD Mountina oF SEcTIONS. 


From the fresh branches not less than five of the most vigorous-looking leaves 
were selected. They were taken from different parts of the branch, but never from 
the growing points. The petioles, with a portion of the lamina attached to each to 
show the direction of growth, were placed in methylated spirit, and after a few days 
were usually found in good condition for cutting. If still too hard they were boiled 
in water for a short time. 


The sections were taken from the basal half of the leaf-stalk—from a point 
nearer to its base than its junction with the blade. Those intended to be sketched 
by the camera lucida were cut by hand, the thinnest being selected from a large 
number taken from each petiole, and examined in a mixture of equal parts of 
glycerine and spirit. 


, 


AS AIDS IN THE DETERMINATION OF SPECIES. 5 


The sections for the permanent type-slides were cut with a microtome, after 
embedding in paraffin in the usual way. To clear the sections for these mounts, a 
mixture of glycerine and caustic soda solution was generally used. Warming in 
nitric acid was in some instances attended with brilliant results, while in other cases 
the sections were ruptured and distorted by its action. 


Most of the sections were photographed without any preparatory staining. 
Indeed, in some instances, especially in the case of petioles kept for many months in 
ordinary tank rain water (and some kept for over three years were not in the least 
decomposed or affected by fungus growths), the colour acquired by the specimens—a 
rich yellowish-brown tint—was itself a stain not to be surpassed for the purposes of 
actinic contrast. When this tint was not acquired, and in the case of fresh material, 
the sections were, if necessary, bleached by the action of free chlorine, and then 
faintly stained with the stain first proposed by Dr. Frances Hoggan.* It is prepared 
by adding pyrogallic acid to tincture of steel. This was found more easy of 
application than the iron stain, composed of pyrogallic acid and protosulphate of iron, 
recently recommended in the Journal of the Royal Microscopical Society,+ which, 
however, gave equally good results to the eye and on the photographic plate. 


The Hoggan iron stain was originally recommended as especially suitable for the 
treatment of cartilage, in which the desired depth of colour could be produced in a 
few minutes. 


We found that the time required for the proper treatment of the sections of 
petioles varied from five minutes to half an hour, the stain here taking a longer time 
to penetrate. 


The source of illumination was a clock-work petroleum Jamp with a one-inch 
wick, and the light was all that could be desired, but a blue glass modifier was used 
in every case, whether the object was stained or not. 


Of the mounting media tried, glycerine jelly was found the most suitable. 
Balsam was used in a few cases, but it was invariably found to render the epidermal 
layers too transparent, and consequently somewhat indistinct. It may be mentioned 
that it was found to be essential for purposes of comparison and identification that 
the sections should be quite thin, showing little more than one layer of cells in the 
cortical ground tissue. 


* Marsh, ‘‘ Microscopical Section-cutting,” 2nd Ed., p. 131, 
+ Journ. Roy. Micro. Soc., 1888, p. 157. 


6 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


III].—CuasstFicatTion oF Tissunrs. 


Before describing the sections, it will be well to settle the system of classification 
to be adopted for the tissues. 


Various methods have been proposed, and more or less generally used. Of these 
we will briefly glance at four of the most important, and indicate the one most 
convenient for our present purpose. 


One system which has been very widely used is the topographical of Sachs. In 
this the tissues are mapped out according to their relative positions—the dermal 
tissue, the ground or fundamental tissue inside, and the fibro-vascular bundles or 
fascicular tissue studding the ground tissue. This threefold division is certainly very 
simple and easily applied, but it is not scientific, for geographical position does not 
always reveal the essential character of a tissue. 


A second system is the developmental of Hanstein, and, at first sight, it seems to 
be thoroughly scientific, being based upon development. In this classification certain 
meristem layers form certain tissues, and these get special names. There is a three- 
fold arrangement of the primary layers, as in animals, viz., dermatogen, forming the 
epidermis ; periblem, forming the cortex ; and a central cylinder of plerome, forming 
vascular bundles and pith. But the objection to this system is that it does not 
always hold good, for, as instances, in perforations of the leaf in many aroids, and in 
splitting of the leaf into segments in palms, the original epidermis is replaced by 
another, derived from the underlying tissue. 


The morphological system of De Bary is purely descriptive, and, therefore, the 
safest to adopt in the present state of our knowledge. We know so little of function 
as yet that we can do little more than place together parts agreeing in structure, 
although they may have little else in common, or no physiological relationship. 
Parenchyma is thus one kind of tissue, sclerenchyma another, and so on, and this is 
the classification most convenient for present use. 


But convenience is only a make-shift, and sooner or later function and structure 
together will determine the true position of any system of tissues. ‘This brings us to 
the last system to be mentioned, viz., the functional of Schwendener and Haberlandt, 
in which a certain structure is associated with a certain function or functions. The 
function is here brought to the front, and such terms as bast, cambium, Wc., are used 
to denote tissues performing special functions, and not as is usually the case, tissues 
haying special positions. Certain tissues may haye a certain position by virtue of 
their function and consequent structure, but that is an accidental, and not an essential 
circumstance. Relative position and structure are not considered apart, but as 
dependent on function. As already stated, function is as yet so little understood that 


AS AIDS IN THE DETERMINATION OF SPECIES. 7 


the determination of it is often but a guess at the truth, but this guess can either be 
verified or proved erroneous, and so advance in this direction will be made. This 
mode of classification will be the final outcome of all our studies, and to show its 
superiority we cannot do better than take the fibro-vascular bundle as an example. 


The F.V. B.,* according to the ordinary view, and as the name bundle indicates, 
is a unity, and treated as such. It is composed of a variety of cells, usually having 
a definite relation to each other, and either hard and fibrous, or soft and 
parenchymatous or vascular. 


On the functional view, the F. V. B. is not a unity, but composed of at least two 
main elements—a part for mechanical support, or skeleton, and another part for 
circulation. The skeleton and the circulating tissues are often associated, just as the 
blood vessels have a certain relation to the skeleton in the animal body—the hard 
and firm to protect and support the soft and yielding parts. 


In describing the sections generally we will adopt a combination of the two latter 
modes of classification, giving the separate parts, along with their respective 
functions. Perhaps this might be called, for distinction’s sake, the bzomorphic 
system, as both structure and function are taken into account, and it is undoubtedly 
the most scientific of all, for the structure did not precede and the use follow, but 
most probably the necessity for the use arose and the structure was forthcoming. 
Since life is the cause and not the consequence of organisation, and as life may be 
regarded as the sum total of the functions, and organisation as the sum total of the 
structure of the plant or animal body, therefore structure is dependent on—is a 
manifestation of—function. 


The biomorphic classification of the tissues is based upon the structure, taken in 
conjunction with the function, the mechanism in connection with its use, and it is 
added mainly to show the importance of certain structures for purposes of 
classification. When itis remembered that in a transverse section of even a petiole, 
we have structures which serve for protection and support, for the manufacture and 
the transport of food materials, and in fact, for nearly all the vegetative functions of 
the plant, as distinguished from the reproductive, then such structures become 
invested with a higher meaning, and with a corresponding classificatory value. 


Adopting a convenient arrangement of parts, which can be seen at a glance in 
any of the sections, and which will afterwards be further subdivided, they will be as 
follows from the outside inwards :— 

1. Epidermis or protective tissue. 
2. Cortex, or principally starch-manufacturing tissue. 
3. Hard bast, or supporting tissue. 

Fibro-vascular bundle /4. Soft bast, or albuminoid-forming tissue. 


5. Wood tissue, or circulatory and supporting tissue. 


* BF. V. B. is used instead of repeating in full the expression, Fibro Vascular Bundle. 


8 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


With the much-debated question, whether the hard bast really belongs to the 
vascular bundle or not, we have at present nothing to do. These bundles of bast 
fibres always accompany the vascular tissue in these transverse sections, and while 
they are often absent in other cases, and may be unessential, yet as a matter of 
convenience, and without entering upon the general question, we will use the current 
expression of fibro-vascular bundle to include the hard bast and the soft bast, as well 
as the woody tissue. 


lV.—Sections Descripep GENERALLY. 
E. globulus taken as a type. 


As each section is photographed and accompanied by its appropriate description, 
it will only be necessary here to notice the general character of the sections. For 
this purpose we will take Eucalyptus globulus as a type, and compare the others 
with it. 


When an ordinary hand-cut transverse section is mounted direct in Schulze’s 
solution, the differentiation of the tissues is clearly shown. ‘Taking a general view 
of the section before entering into details, it is seen to be of an oval shape, one 
and a half lines broad, by one line thick, or one and a half times broader than thick. 
The epidermis appears as an orange-yellow, or it may be pale crimson border, edged 
by a continuous pale yellow line, this latter indicating the presence of a cuticle. 
Beneath the epidermis is the purple-coloured cortex, composed of cells with walls 
varying in thickness, and as the colour indicates, of cellulose. Next comes the 
hard bast, with its orange-yellow lignified cell walls, succeeded by the purple-coloured 
soft bast; then the clearly-marked bright yellow cells and vessels of the wood, 
traversed by narrow radiating lines, composed of elongated cells of a darker colour. 
These are the parenchymatous cells of the wood resembling medullary rays. Next 
there is a continuation of the soft bast on the other side of the wood, succeeded by 
the hard bast, and then the other tissues as above. In short, if we start from the 
curve of the wood, which is more or less central, forming a woody core, there is a 
succession of envelopes more or less thick. The soft bast surrounds the wood, and is 
wedged in between it and the hard bast, which is surrounded in turn by the cortex, 
and the epidermis envelopes all. 


Each of the above parts will now be specially dealt with in succession. 


1. Epidermis or Protective Tissue.—The cells of the epidermis are well-defined, 
and distinct from the underlying tissue. It consists of a single layer of cells, 
measuring in thickness 1-570in., and the breadth of each cell on an average is 
about 1-800in. (Fig. 1, a.) 


AS AIDS IN THE DETERMINATION OF SPECIES. 9 


The outer wall is moderately thickened to prevent excess of evaporation, and 
generally to provide against injury. In the ordinary unstained cell there may be 
distinguished outside of the round or oval cell cavity a distinct clear band externally, 
and a somewhat turbid-looking portion abutting on the cell cavity. As the outer 
band is coloured a pale yellow by Schulze’s solution, it represents a cuticle, which is 
continued right round the section, forming a slight convexity on the outside of each 
cell. Itis on an average from 1-3200in. to 1-2400in. in thickness, and shows no 
sign of striation. 


The turbid-looking portion of the wall is coloured a deeper yellow by Schulze’s 
solution, and may even pass into orange-yellow or pale crimson, according to the 
amount of colouring matter present. Hence it may be concluded that beneath the 
fine sheet of cuticle, which is of the nature of cork, there is a cuticularised layer, a 
sort of transition between cellulose on the one hand and cuticle on the other. The 
use of the cuticle and cuticularised layer is evident, principally for the purpose of 
preventing evaporation. It is very thick on desert plants. Plants in rainless regions, 
and Australian plants generally, are well provided with it. The sections of the 
Mallee scrub species, to be afterwards referred to, will show this clearly. 


The lateral walls unite the cells together, and are relatively thin. They 
terminate outwardly at the cuticle, and leave no gaps between. No contrivances for 
admitting air were found, although carefully looked for. The inner wall is likewise 
thin, and may be composed of cellulose, being coloured purple by Schulze’s solution, 
thus allowing nutritive substances to pass in and nourish the living cell. Or it may 
be, like the outer wall, coloured yellow, and thus cut off from nutritive supplies, so 
that no further growth or expansion can take place. In the one case the epidermal 
cell is living, and capable of further growth, in the other it has reached maturity, 
and become surrounded by a corky wall. 


From the relative thickness and breadth of each epidermal cell, it may be 
inferred that it has the form of a prism perpendicular to the surface, and the cuticle 
covering produced by each, forms a continuous layer all round the outside. 


2. Cortical Tissue, or starch-manufacturing tissue principally.—Immediately 
beneath the epidermis there is a single layer of cells, which may or may not have 
their outer and lateral walls cuticularised, and which form a more or less distinct 
outer border to the cortex proper. This may be called the Hypodermal layer 
(Fig. 2). 


The remaining cells are of irregular outline, with walls of various degrees of 
thickness. The cortical parenchyma contains chlorophyll, and it is here the 
manufacture of starch is carried on, as evidenced by the contents of the cells 


10 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


containing numerous starch granules. When the section is treated with iodine this 
portion becomes visibly violet, showing the presence of starch in abundance. 


As the hard bast is approached the walls usually thicken considerably, and the 
cell cavity is correspondingly diminished (Fig. 2a). The purple colouration by 
Schulze’s solution shows, however, that the cell walls are of cellulose. Here we are 
specially concerned with that form of thick-walled parenchyma, known as Collen- 
chyma, or collenchymatous parenchyma. 


Sometimes the walls are thickened at the angles, or often completely round. 
While the epidermis is a protective tissue, this is a supporting one, serving to 
strengthen the comparatively slender petiole. It is common in parts of plants, such 
as the leaf-stalks, where provision has to be made for increase of length as well as for 
strength, and so the cells must be living, and have thin places to admit the necessary 
nutriment—they are living mechanical cells. In the old and fully-formed leaf, the 
thickening may extend all round (as seen in Fig. 4). If the living protoplasm were 
then to disappear, and the walls become thickened and lignified, this tissue would 
pass into that of the hard bast. 


The cortical tissue is excavated by large and numerous cavities, and crystals are 
very frequent, both of which will now be specially noticed (Figs. 2 and 3). 


These cavities may be named according to their position, rather than that of 
their contents (which has yet to be accurately determined), and so we may speak of 
them as cortical cavities. In contrast to these cavities, which are not continuous 
lengthwise, and so vary in their number and arrangement at different parts of the 
petiole, there are in some species canals which are constant and continuous, and 
from their position inside the wood curve, they may be termed central canals. 


The contents of these cavities or canals cannot be called resins, for they are 
soluble, sometimes very readily in water ; nor can they be called oleo-resins, for the 
petioles yield no oil on distillation. They may be spoken of as kinoid, until their 
chemical nature is more accurately determined. 


The kinos of the Eucalypts have been, and are being, investigated by Maiden,* 
and he finds that they are divisible into groups according to their behaviour with 
water and spirit. These groups will be referred to in connection with classification. 


Cortical Cavities.—These cavities, usually roundish or oval in shape, occur at 
irregular intervals, and at some little distance from the epidermis (Fig. 2). They vary 
in size and in number. The largest is about 1-80in. in diameter. They are 
distinctly visible to the naked eye when held up to the light. The number is usually 
from 7 to 8. 


* Proc. Linn. Soc., N.S.W. Vol. IY., Series 2. 


AS AIDS IN THE DETERMINATION OF SPECIES. 11 


The contents are usually of a yellowish, but in some instances of a dark-red 
colour, readily dissolved by alcohol, and deeply stained by tincture of alkanet. But 
if allowed to harden by keeping in water for a lengthened period, neither alcohol nor 
ether affects them. 


Each cavity is bounded by much-compressed cells, with their flat faces towards 
the cavity. From the appearance presented by these intercellular spaces or excava- 
tions, they appear to be formed by the rupture and disorganisation of the cells at 
that particular spot, and are hence of lysigenous origin. 


In some species there are special canals, not cortical, but enclosed by the curve 
of the wood, which will be noticed in their proper place. 


Crystals.—Crystals of the well-known octahedral form are seen in great profusion 
scattered through the cortical cells (Fig. 8). They vary considerably in size, 
sometimes reaching 1-$00in. in length, and, judging from the usual tests, as well as 
from their crystalline form, consist of oxalate of lime. Numerous crystals, similar 
to the above, likewise occur in the soft bast, but they are much smaller on the 
whole. No species examined was entirely free from crystals, although in some 
instances they were very scarce. 


Longitudinal Section Although it is not the object of this paper to give a 
complete account of the histology of the petiole, it was thought necessary to 
examine longitudinal, as well as transverse sections, at least in one or two cases. 


A longitudinal median section of the petiole of E. globulus, taken through the 
shorter axis of the crescentic bundle, revealed the ordinary succession of the various 
parts. 


The epidermis, after prolonged staining with Schulze’s solution, stood out as a 
somewhat pale, lemon-yellow border. The breadth of each cell varied from 1-760in. 
to 1-830in., and the length was just a little less, or about 1-920in. 


The purple-coloured cortex exhibited much smaller cells towards its outer than 
its inner portions, the hypodermal layer usually quite distinct beneath the epidermis. 
Cortical cells adjoining the hard bast were often relatively large (Figs. 2a and 0). 


The cortical cavities had the same form as in transverse section, being irregularly 
round, or oval, or pear-shaped, and the size was about the same. Two adjoining 
cavities were measured, one of which was 1-190in., and the other 1-115in. in length. 
The F. V. B. showed the hard bast usually in two distinct layers (an outer and an 
inner), with intervening soft bast, and the wood with its numerous spiral and annular 


12 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


vessels (Fig. 5). The soft bast was carefully examined, and found to consist of 
cambiform cells and sieve-tubes (Figs. 6 and 7). The cambiform cells varied 
considerably in shape and size. Often they were brick-shaped, and even somewhat 
roundish ; at other times they were much more elongated and thinner-walled. 
Directly adjoining the wood the cells were clearly marked off from the latter, and 
sufficiently thin-walled in some cases to resemble cambium. 


The sieve-tubes are shown in longitudinal section. (Fig. 7.) The iron stain, 
as well as Schulze’s solution, serves to differentiate them. 


F1pRo-VASCULAR BUNDLE. 


This is a convenient collective term for the group of tissues already separately 
mentioned as hard bast, soft bast, and wood tissue, or if the bast and wood be 
simply contrasted, then phloem and xylem may be used. 


Since the bundles form the most striking feature of these sections, and are the 
parts from the form of which the species of Kucalypts are chiefly determined, they 
will be expected to receive a large share of attention and illustration. 


The special form of the bundles, or rather of the woody portion of them, will be 
considered in the next section devoted to the determination of species, so little will 
be said here upon that point. 


It is to be premised, first of all, that the xylem portion of a leaf bundle is, as a 
rule, towards the upper surface, and the phloem portion towards the lower surface, 
just as would naturally happen in a lateral expansion of these tissues of the stem. 
Also, that the upper or inner surface of the petiole has often a different contour to 
the lower or outer surface. In this instance the upper surface is flattish, while the 
under surface is rounded. But in cases such as the fig and walnut, where the petiole 
is cylindrical, the bundles are likewise arranged in a circle, and form a cylinder. 


As is well known, in most Eucalypts the blade of the leaf is not spread out 
horizontally, as is usually the case, but vertically in relation to the leaf-bearing axis. 
In the young condition, however, it has the normal position, and it is by subsequent 
twisting of the leaf stalk that the changed position is brought about. In the course 
of this twisting process, stomata are developed on the upper surface, in addition to 
those already existing on the under surface, and palisade parenchyma is developed 
beneath the lower epidermis as well.* But it appears that the bundle of the leaf 


* Bower and Vines, Practical Botany, Part I., 2nd Ed., p. 148. 


AS AIDS IN THE DETERMINATION OF SPECIES. 13 


stalk ig unaffected by the change, or at least not rendered symmetrical, so that in 
every example investigated it does not form a complete circle, but a curve open 
upwards, with the two ends approaching, but never meeting. 


A section of the base of the midrib of the young sessile leaf (Fig. 8) lkewise 
shows the curve open upwards, whereas a section of the young square stem of the 
saine plant (Fig. 9) exhibits a symmetrical quadrangle, corresponding with the 
outline of the stem, and continuous right round. 


An attempt to account for the generally different distribution of the wood in the 
stem and in the leaf-stalk is made by Herbert Spencer in his ‘‘Principles of Biology.’’* 
After noticing that there is a direct relation between mechanical stress and the 
formation of wood, and that the general arrangement in stems is that of a cylinder, 
he says :—‘‘ While axes are on the average exposed to equal strains on all sides, 
most leaves, spreading out their surfaces horizontally, have their petioles 
subjected to strains that are not alike in all directions ; and in them the hard tissue 
is differently arranged. Its transverse section is not ring-shaped, but crescent- 
shaped ; the two horns being directed towards the upper surface of the petiole. 
That this arrangement is one which answers to the mechanical conditions, is not 
easy to demonstrate; we must satisfy ourselves by noting that here, where the 
distribution of forces is different, the distribution of resisting tissue is different. 
And then, showing conclusively the connection between these differences, we have 
the fact that in petioles growing vertically and supporting peltate leaves—petioles 
which are therefore subject to equal transverse strains on all sides—the vascular 
bundles are arranged cylindrically, as in axes.” 


That this is only a partial explanation is shown by the fact that in 
many instances the cylindrical arrangement of the wood occurs where the 
distribution of forces is different from that of the stem, as in the leaves of 
fig and walnut, already mentioned. It is true, however, that in all the 
petioles of Eucalypts examined the crescentic form prevailed, and was not 
appreciably interfered with by the twisting of the leaf-stalk. In some cases, such as 
that of E. ficifolia, where the horns of the crescent may approach so very close as to 
make the wood practically a cylinder, the outline was not cylindrical, and there was 
less twisting of the leaf-stalk than in many other species. Indeed, in one petiole 
of this species the wood formed a compressed hemisphere, the two horns abutting, 
but as four central canals were present, this petiole was evidently somewhat 
abnormal. 


The bundle will now be considered under three separate divisions, viz., hard 
bast, soft bast, and wood. 


* Vol. II., p. 261. 


14 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


3. Hard Bast.—This tissue is very easily recognised in transverse section from 
its position and structure. It forms an irregular, interrupted ring of exceedingly 
thick-walled cells. It passes not only round the outside of the bundle on its lower 
surface, but curves round the upper surface, and after dipping towards the centre of 
the bundle, and forming a thickened mass, it continues in a graceful curve. 


Treated with Schulze’s solution, the bright, yellow girdle is made to stand out in 
bold relief. 


The hard bast, which has received various other names, such as sclerenchyma, 
bast fibres, prosenchyma, &c., is one kind of mechanical or supporting tissue—a 
skeleton in fact. This particular kind of tissue may occur elsewhere than in this 
region, wherever, indeed, a strengthening of the parts becomes necessary, but in 
order to prevent confusion the name of hard bast or bast-fibres will invariably mean 
with us the skeleton accompanying, supporting, and protecting the soft bast. 


4, Soft Bast.—The soft bast, all but completely enclosed by the hard bast, is a 
ring of tissue immediately adjoining and surrounding the wood. It consists of cells 
of much smaller diameter than those of the hard bast, and relatively thin-walled. 
In a section treated with Schulze’s solution, this tissue is strikingly shown as a 
purple patch, between the bright yellow of the hard bast on the one hand, and that 
of the woody tissue on the other, which it completely envelopes as with a mantle. 


The thin-walled cells, many of them with large cavities, and all with cellulose 
walls, have evidently a different function from that of the hard bast. ‘The soft bast is 
composed of two main elements—the cambiform cells and the sieve-tubes, both of 
which have already been dealt with in considering the longitudinal section. 


5. Woody Tissue.—The wood forms the central figure of the section, and with 
its graceful infolding at each side gives rise to characteristic patterns. It sometimes 
resembles the inverted volute of an Ionic capital, or simply a capital © lying flat, or 
to change the figure, when, with Schulze’s solution, the radiating lines are made 
to stand out dark upon the yellow back-ground, it resembles a caterpillar coiled up at 
either end, with its body divided into numerous segments by beaded rings: When 
the two horns curve round the central canals, as in E. maculata, there is something 
of an owl-like appearance about it, when viewed upside down. 


In a section treated with Schulze’s solution it is easy to resolve the woody tissue 


into three elements— 
(a.) Wood fibres. 


(b.) Wood parenchyma. 
(c.) Vessels. 


AS AIDS IN THE DETERMINATION OF SPECIES. 15 


The wood fibres, forming mainly the outer half of the woody curve, are 
recognised by their thickened walls and comparatively small cavity. They are on an 
average 1-3000in. in diameter. 


The wood parenchyma consists of small elongated cells, arranged in radiating 
lines so as to resemble medullary rays. They stain of a dark colour, and hence stand 
out clearly from the surrounding yellow. The radiating lines are usually just 
sufficiently equidistant to allow room between for a radiating row of vessels. ‘The 
average leneth of each cell is about 1-2000in. 


The vessels, conspicuous by reason of their large cavities, are arranged in radial 
rows, and form mainly the inner half of the woody curve. A larger or smaller number 
of vessels generally appear on the outer border, at the central and thickest portion of 
the wood. The diameter of the vessels varies considerably, the largest being about 
1-750 in., and the average diameter about half that. In a longitudinal section the 
vessels are seen to be spiral and annular. 


From the foregoing brief description of the parts of the F. V. B. in the petiole 
of E. globulus, it will be seen that the bundle here is different from the normal 
bundle. Usually the phloem and xylem follow each other in the same radius, the 
phloem being outside and the xylem inside, so that when a bundle is traced into the 
leaf stalk, the phloem portion is towards the outer or lower surface, and the xylem 
portion towards the inner or upper surface. In this instance, however, there is 
phloem not only on the outer but also on the inner side of the wood, and continued 
round, so that the wood is in the centre completely surrounded by the phloem. In 
most cases the phloem forms a narrow band, where it curves round to become 
continuous. Such a bundle, with the xylem completely surrounded by the phloem, is 
called concentric. With the normal arrangement of phloem and xylem, the form of 
the bundle is collateral, and when there is phloem outside and inside the xylem it is 
distinguished as bicollateral. According to De Bary,* the latter is the form of the 
bundle in all investigated species of Eucalyptus, and ‘“‘ Eucalyptus globulus decidedly 
belongs to this series.”” As far as the petiole is concerned in this, and we may add, 
in the other species investigated, the bundle belongs to the concentric type. 


Having seen the mode of arrangement of the parts of the F. V. B., we will now 
endeavour to explain the use of this arrangement and structure. 


The hard bast all round is evidently, from its very nature and position, a 
mechanical support and protection. 


The wood fibres in the centre likewise play the part of mechanical support, and 
the soft bast is safely placed between the hard bast and the inflexible wood. 


The cambiform cells of the soft bast have thin walls, to allow of the circulation of 
diffusible substances, but as the thin walls might collapse and thick walls would pre- 


* Comp. Anat. of Phanerogams and Ferns, p. 338. 


16 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


vent diffusion, a compromise has to be effected. The walls are thickened here and 
there, and diffusion occurs in the thin places. 

The sieve tubes, with their sieve plates, allow of the transport of indiffusible 
substances, such as albuminoids. Just as the blood in our blood vessels is carried 
bodily along, so is there a direct bodily transport of these indiffusible substances 
through the meshes of the sieve. 

The next step is to vessels proper in the wood tissue, where there is no longer 
even a sieve plate, but the transverse partitions are removed completely. In that 
case the walls want special strengthening to prevent collapse, and so there are all the 
admirable contrivances of annular and spiral vessels. The vessels technically belong 
to the wood, but they are circulating tissue. They are for quick transport, the 
quickest of all; the cambiform cells the slowest, working by the slow process of 
diffusion; and the sieve tubes intermediate. The fibrous cells, or wood fibres, 
especially the younger, have probably the task of conveying water, for they readily 
take it in and readily give it off, so that the I. V. B., with its varied cells, resolves 
itself into a contrivance for mechanical support on the one hand, and a means of 
circulation on the other. 

To show the importance of the soft bast, it may finally be mentioned that it is 
probably there albuminoids are manufactured, as well as conveyed to their destina- 
tion. It contains more albuminoid matter than other parts, and it is thickly 
bestrewn with crystals of oxalate of lime. The albuminoid matter thus produced is 
not living protoplasm, but it is a necessary preliminary to it. The exact composition 
of this raw material of life occurring in the soft bast is not known. It is quite 
possible, however, that any living cell favourably situated may manufacture living 
protoplasm when the proper material is supplied to it, for the final touch is the 
touch of vitality to convert the lifeless mass into the living protoplasm. 

Before glancing at the other transverse sections in a comparative way, the 
effects of the application of Schulze’s solution on the different constituents of the 
transverse section of EK. globulus may be briefly summarised. The cuticle of the 
epidermis is generally stained yellow and orange; the cuticularised layer of a ruby- 
red ; the cortical portion purple; the lignified cells of the hard bast, orange; the 
soft bast, purple; and the woody tissue, orange, with a tint of brown. ‘The contents 
of the cortical cavities seem to be unaffected, and the crystals are dissolved. 

In the other transverse sections, the epidermis is generally a well-defined layer of 
cells, with more or less thickened outer walls. In some this thickness is excessive, 
specially in E. tetraptera, E. obcordata, E. pachypoda, and E. uncinata. It is worthy 
of remark that these four are shrubs, or at most small trees, that the two former are 
confined to Western Australia, while the two latter belong to desert country, and 
constitute a portion of the Mallee scrub. 

There is a kino-like exudation often met with in some, such as /eucoxylon, 
lehmanni, occidentalis, and alpina, being quite a feature in the last form. The 


AS AIDS IN THE DETERMINATION OF SPECIES. 17 


hypodermal layer, noted in globulus, is decidedly absent in many, but indications of 
it in some, suchas grossa. In /icifolia there is a decided and well-marked hypoderma, 
usually consisting of fwo layers of cells. The cortex may be compared as to the 
number and size of cortical cavities in it. This is shown in Table I., so that it is 
unnecessary to dwell further upon it. In one case at least (E. tetraptera), the 
cortical cells are continued into the organic centre of the section by means of two 
narrow and adjoining lines of cells. 

The hard bast is more or less dense in different sections, forming usually an 
interrupted or broken ring. 

The soft bast, on the other hand, usually surrounds the wood completely, but it 
is sometimes discontinuous. 

The wood-curve may be continuous or discontinuous, with a thinner or thicker 
body, and longer or shorter horns, but, on the whole, so varied in character as to 
serve in many cases as one of the characteristic features of the section. 

Broken curves occur in all the species—in some they are the rule, as in /ehmanni, 
in many they are exceptional, as in globulus, which was the most constant in its 
features of all the types investigated. 

This will be the most appropriate place to compare the essential features in the 


transverse section of a young stem and a young leaf of E. globulus. The leaf being 


sessile, it was necessary to take the base of the midrib instead (Figs. 8 and 9). 


Youne Stem. Youne Lear. Oxp Lear. 
Base of Midrib. Petiole. 

Epidermis— 1 1 1 

Thickness. . — = eit 
1500 in. 1150 in. 570 in. 

Cortical Cavities— 

Number 14 at least 4 7 or 8 

Shape round round round 
i 1 1 

Size (largest) — — ae 
140 in. 210 in. 80 in. 

Hard Bast— Dense and continuous on out- | Very sparingly developed in both | Well developed and dense. 
side of F.V.B. In patches in- layers. 
side, and absent from corners. 

Soft Bast— Continuous outside and inside | Continuous round wood and well Continuous round wood. 
of wood, but thinnest at the | developed, particularly on inside 
corners. of crescent. 

Wood— Forming a square, with slight | Crescentic, with horns well | Crescentic, with horns curving 
inward depression on each side curved in. inward. 
of square. 

Vessels— Distributed mostly towards inner | Numerous, and distributed| Numerous, and distributed 
surface of wood, and moderately | towards inner part of wood. | mostly in upper half of wood. 
numerous. Largest towards ex- 
terior of wood. 

1 1 1 
Size (widest) = —— — 
830 in., an elongated oval. 830 in., elongated ellipse 700 in. 
1 1 1 
Average = about—— about —— 
2300 in. 2300 in. 1400 in. 


18 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


The above table shows a contrast in various respects between the young square 
stem and the midrib of the young sessvle leaf. 


In the stem—Ist. The epidermis is thinner. 
2nd. The number and size of cortical cavities is greater. 
3rd. The hard bast is much denser. 
4th. The wood forms a square, and not a crescent. 


The width of the vessels is about the same in both. The upright growing stem 
and the lateral growing leaf are necessarily unequally acted on by various forces, 
hence the symmetrical and stronger F. V. B. of the stem, as compared with that of 
the leaf. 


If the comparison is made between the young and the o/d leaf, with its twisted 
petiole, there are a few striking differences along with general agreement; but it 
will be seen that the differences are simply those between a young and tender organ, 
and the same arrived at maturity. In the old leaf, the epidermis is about twice as 
thick, the cortical cavities are increased and immensely enlarged, the hard bast is 
now strongly developed, and the vessels are a trifle larger. 


The twisting of the petiole seems to have produced no noticeable difference in the 
general arrangement of the tissues, particularly the vascular. The twisting 
of a leaf-stalk round a support, in the case of leaf-climbers, has been shown by 
Darwin to increase the growth. The pressure here has acted as a stimulus, but it is 
worthy of note that while in the free petiole the bundles form an open curve, in the 
clasping petiole they form a closed cylinder. 


The mere twisting of the petiole in Eucalypts has not produced any curving of 
the bundles greater than that met with in the young and sessile leaf, and even in 
those cases where the horns of the crescent most closely approach, as in ficifolia and 
calophylla, the leaf-stalk is less twisted than in ordinary cases. 


Further, the statement made by Mr. Darwin, on the authority of Dr. Masters, 
that ‘‘ the semi-lunar band of vessels is confined to petioles channelled along their 
upper surface,” is not countenanced by these researches, for it is in the most 
channelled leaf-stalks that the wood curve most approaches the complete ring. 


’* Darwin, ‘‘ On the Movements and Habits of Climbing Plants,” p. 43. 


AS AIDS IN THE DETERMINATION OF SPECIES. 19 


V.— CHARACTERISTICS OF HacH Species AS DERIVED FROM THE TRANSVERSE 
SECTIONS. 


Baron von Mueller, in his ‘ Eucalyptographia,” as well as in his humbler 
‘‘ Botanic Teachings,” has adopted two principal expedients for helping to determine 
the numerous species of Eucalypts, viz., the nature of the bark and the nature of 
the anthers, 


We now add a third, and although it has only been rigorously applied to thirty 
different kinds, and to a few more casually, there is every reason to believe that the 
principle will hold good throughout that extensive genus of plants. It is based upon 
the form and arrangement of the structures revealed in a transverse section of a 
well-developed and fully formed leaf stalk, taken in conjunction with external 
characters of the leaf. 


While the learned Baron has given a leading place in his classification to the 
two principles just mentioned, his fertile mind and wide knowledge have suggested a 
number of others which he has partially applied. Thus the size of the pollen-grains 
has been found to vary in different species, but to be more or less constant in each. 


Again, the number and distribution of the stomata have enabled him to form 
three series—Ist, according to the presence of stomata on the under surface only 
(hypogenous); 2nd, their presence on both surfaces, but less numerous above than 
below (heterogenous); or 3rd, their presence on both surfaces, but approximately equal 
in number above and below (isogenous). Then again the fruit has been suggested as 
a basis of classification, and each of these methods has its own special advantages, 
and its suitability for different purposes. 


The Carpologic system has this advantage, ‘“‘that any species might thus be 
defined from fruiting specimens alone, which latter, through the long persistence of 
the fruit, are always obtainable in collecting journeys, whereas flowering specimens 
can be got only at some period of the year, subject even to fluctuations and uncer- 
tainties.” (Huc. VIII.) 


The Cortical system is adapted ‘to the technic requirements of woodmen, who 
could not be expected to enter on a discrimination of the various species from such 
purely scientific differences, on which descriptive botany would rely.” (Huc. I.) Of 
course this system likewise suits the general seeker after a knowledge of these plants. 


20 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


The Anthereal system ‘‘ has proved the most convenient for easy-working with 
museum material, so long as it was the main object to ascertain the name of any 
species.” (Kuc. I. ‘“ Introduction.”) 


There is another system recently propounded which ought to be noticed here, 
viz., the ‘‘ Kino system ”’ of Maiden.* It is a chemical check, which he merely offers 
as a supplement to other systems. 


The three groups at present recognised are :-— 


1. Ruby group, with ruby-coloured kinos, soluble either in cold water or spirit ; 
E. macrorrhyncha, obliqua, and amygdalina, investigated by us, belong to this group. 


2. Gummy group, containing gum, and therefore imperfectly soluble in spirit, 
but soluble in cold water. £. leucoxylon and saligna belong to this. 


3. Turbid group, soluble in hot water or alcohol, but the solution becomes turbid 
on cooling. 


With regard to the present system, we consider that it has many advantages and 
few disadvantages. The Eucalypts being evergreens their leaves are readily obtainable, 
and where the leaf happens to be sessile the section of the base of the midrib may 
serve the purpose. The resemblance in habit of many different Kucalypts is often 
misleading and always confusing, and the basing of characters upon the internal 
anatomy, which is not so subject to fluctuation as the external, is an advantage. 


Again, the most persistent part of the petiole—the wood—1is often sufficient for 
purposes of discrimination, and it may be used, therefore, for the determination of 
museum material. 


It has, moreover, this great advantage, that it enables us in doubtful and difficult 
cases to decide whether the balance of evidence is in favour of specific identity or 
merely varietal distinction. 


It may be an objection that the above are not naked-eye characters, and that the 
system is suited rather to the laboratory than the field, but while less minute 
characters may be used for rough discrimination, the final test for specific distinction 
must be based upon essential characters that do not always lie upon the surface. 
Moreover, the internal structure has been hitherto too much neglected by systematists, 
just as anatomists have in like manner paid too little attention to the characters 
recognised by the former. If the whole truth is to be expressed by our classification, 
then all the features, external and internal, must be taken into account. 


* Pharm. Jour. XX., p. 221. 


AS AIDS IN THE DETERMINATION OF SPECIES. 21 


The accompanying drawings almost render description unnecessary, but as this 
is the main portion of the paper, the determining characters of each form examined 
will be briefly given. 


Before doing so, however, it will be necessary to fix upon some definite arrange- 
ment, and a geographical one may be followed, in order to see how far anatomical and 
ceographical relations agree. 


Table I. exhibits the thirty different forms investigated, variously arranged as far 
as the data will permit. It is hardly needful to state that the necessary information 
has been obtained from the ‘‘ Eucalyptographia,”’ and we have simply thrown it into 
tabular form. The only exception is the arrangement according to cortical cavities, 
central canals, and wood curve, which has been deduced from our own researches. 


Table II. starts with the forms arranged according to their geographical distri- 
bution, and places opposite each the characters respectively deduced from the 
transverse section of petiole, the leaves, stomates, fruit, anthers, pollen, and bark. 


The very different affinities shown by these various systems of arrangement 
only emphasises the fact that it is not by solitary characteristics affinities are deter- 
mined, but by the complex of characters, which go to the making up of an individual 
whole. 


The transverse sections will likewise show that along with a certain amount of 
variability there is sufficient constancy to give them a characteristic appearance for 
the different species. The most striking features are: Size and shape of section, 
relative thickness of epidermis, size and number of cortical cavities, frequency or 
scarcity of crystals, density and continuity, or the reverse, of hard bast, pattern of 
the wood, and size and distribution of the vessels. 


Since all these details are only necessary for complete description, the charac- 
teristic features ave given at the end as a sort of summary of characters, serving for 
all practical purposes. 

As regards the central canals, they occur in only a few of the investigated 


species, viz., E. calophylla, ficifolia, and maculata, with its variety citriodora. 


Two seems to be the normal number, but since each may divide in a forked 
manner, the number is sometimes increased to four, or even six (maculata). (See 
remarks in description of each species.) 


In stating the characteristic features of the various sections, it is often found 
necessary to speak of the relative sizes of different parts, such as the section of the 


. 


a THE TRANSVERSE SECTIONS OF PETIOLES OF BHUCALYPTS 


bo 


petiole, the epidermis, cortical cavities, central canals, and vessels, and in using the 
expressions “large,” ‘“ small,” or ‘‘ moderate in size,” it all depends upon what is 
considered an average size. 


While it is not advisable to lay down a hard and fast line, it is well to have a 
general understanding of the meaning of the relative terms. 


It may be stated generally that the average section is reckoned as being about 1 
line X 1 line or 2 line, and above or below that will be large or small respectively. 


The size of the section seems to be rather a constant and trustworthy feature. 
The absolute size is first given, then the relative breadth and thickness. 


The thickness of the epidermis only varies within certain limits, and cannot 


often be used as a characteristic, but when it is thicker than about 5 in., or thinner 


than ;1. in., it may be regarded as above or below the average. The cortical cavities 
1 


and central canals may be considered large up to ; in., moderately large up to 
1 
200 
given. 


in., and small beyond that. The size of the /argest in each species only is 


The vessels have a wide range of variation. In settling the average size it is 
largely a matter of judgment, and the largest size given in each case has to be taken 
into account. Roughly, when the largest size is ;, Im. or more, and the average not 
too low, the vessels might be described as “large,” while at ;3; in., or less, and a 
corresponding average, they would be “small,” and the intermediate would be 


‘moderately large,” or medium-sized. 


Of course the standard of measurement is confined to the petioles of Kucalypts, 
and has no reference to the absolute sizes of the parts mentioned in any other 
plants. 


The size of the cavities and canals varies in different parts of the petiole, and 
likewise the width of the vessels, so that too much importance must not be attached 
to the actual measurements given. The general results of these measurements may 
be given here. 


Size of section varies in breadth from } to 1% lines (¢efraptera), and in thickness 
from } line (séwartiana) to 13 lines (¢etraptera). 


Epidermis varies in thickness from ; in. (viminalis and stuartiana) to x in. 
1 


oe kas me se : 
(tetraptera). A very common thickness is 3; — gp mm. 


Cortical cavities vary from in. (diversicolor) to ~ in. (globulus), reckoning only 


the largest in each species. 


AS AIDS IN THE DETERMINATION OF SPECIES. 23 


ponte! canals vary among the four forms possessing them, from 5 in. ({ici- 
folia) to + in. (calophylla), taking the largest in each case for comparison. 


The vessels varied in width from 4, in. (/ehmanni) toy im. (gomphocephala), 
comparing only the largest in each species. 


Thus the largest section and thickest epidermis was found in ¢etraptera; the 
widest cortical cavity in globulus, although it is closely approached by cornuta ( {; n-), 
and the greatest width of vessel in MT gg but globulus, tetraptera, and 


citriodora almost equal it, with a width each of 5, in. 


The characteristic nature of the wood-curve has already been insisted on, and it 
may be added that the extent of development of the hard bast in the different species 
seems to be a very constant feature. 


I.—Forms ConFINED TO WESTERN AUSTRALIA. 


The following descriptions of the various sections are not merely based upon the 
type-sections photographed, but are drawn in each case from a considerable number 
of independent sections, of which camera lucida drawings were made. The usual 
method followed was to make outlines of several sections from the same petiole as 
that which supplied the type section, then from different petioles, and lastly from 
herbarium specimens, at least three years old, to test the capability of the system for 
determining museum material. 


1. E. occidentalis, Endlicher ; flat-topped Yate. 
' Shrub or tree, rising to 120ft. 
Leaves.—Of thick consistence, equally green on both sides. 
Size of Section.—1 line broad by ? line thick, or about 1} times broader than 
thick. 
Outline of Section.—Round to oval. 
Epidermis.—Thickness, 4,in.; breadth, ;4, — jy In. 
Cortical Cavities.— ;;1n., sieisal numbering from 8 to none, and therefore 
variable. 
Crystals.—Numerous. 
Hard Bast.—Interrupted ring, sometimes only 1 cell thick. 
Wood-curve (see Fig. 11).—Body thickened at centre, short horns, and sharply 
or gently inturned. 


Vessels.—Largest, ;4, im. in dia. 
1 


> 1500 
Comparatively large and numerous, and distributed pretty regularly. 


Average in. 


2. 


3. 


THE fRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Characteristic features : 
Section.—Average size. 
Cortical cavities.—Moderately large, generally few. 
Hard Bast.—Interrupted and thin. 
Wood-curve.—Body elongated, and short horns sharply inturned. 
Vessels.—Moderately large, numerous, and regularly distributed. 


E. cornuta, Labillardiére ; the ordinary Yate. 

Tree. —Of moderate size. 

Leaves.—Of thick consistence, and nearly equally green on both sides. 

Size of Section.—# line broad by 3 line thick, or about 13 times broader than 


thick. 
Outline of Section.—Oval, and somewhat irregular, flattened on upper surface. 
‘pidermi icknes 1 yh 2 
Kpidermis.—Thickness, 2,— J in. 


Breadth, ;*, in. 
Cortical Cavities.— 7 in. oval, numbering from 9 to 3. 
Crystals.— Moderately numerous. 
Hard Bast.—Pretty generally continuous, and several cells thick. 
Wood-curves (see Fig. 12).—Body slightly thickened at the centre, and short 
horns gently or somewhat sharply incurved. 
Vessels.—Largest, >, in. 
Average, about half that. 
Somewhat large, and most numerous towards upper portion of wood. 
Characteristic features : 
Section.—Relatively small. 
Cortical Cavities.—Large, numerous, often quite close together, and almost 
occupying breadth of cortex. 
Hard Bast.—Continuous and thick. 
Wood-curve.—Horns sharply incurved, and one or both often separated 
from body-curves. 
Vessels.—Moderately large, and aggregated towards middle and upper sur- 
face of wood. 


E. cornuta, var lehmann., Preiss. 

Tree.—Of moderate size. 

Leaves.—Of thick consistence, and equally green on both sides. 

Size of Section.—About 1 line broad by 3 line thick, or twice as broad as thick. 
Outline of Section.-—An irregular oval, elongated laterally. 
Hpidermis.—Thickness, <, — 4) in. 


. La 
Breadth, 3, in. 


4. 


AS AIDS IN THE DETERMINATION OF SPECIES. 25 


Cortical Cavities.— 4, in., oval to round, numbering from 11 to 3. 
Hard Bast.—Generally in isolated contiguous patches, a few or several cells thick. 
Wood-curve (see Fig. 13).—Slender elongated body, almost always broken, 
and with sharply incurved horns. 
Vessels.—Largest, 54, 1n- 
Average about , i. 
Small, few, and regularly distributed. 


Characteristic features : 
Size of Section.—Twice as broad as thick. 
Cortical Cavities. —Moderately large and numerous. 
Hard Bast.—Isolated contiguous patches. 
Wood-curve.—Generally broken, with slender body, and sharply imceurved 
horns. 
Vessels.—Few and small. 


E. obcordata, Turezaninow ; “‘ Maalok.” 


Tall shrub or small tree. 
Leaves.—Thick, broad, blunt, equally green on both sides. 
Size of Section._—About 1 line broad and thick, or as broad as thick. 
Outline of Section.—Round to oval, the greatest diameter sometimes dorso-ventral. 
Epidermis.— Thickness, 3 — go 19- 
Breadth, =, — wm: or half the thickness. 
Cortical Cavities. — 4, in. roundish, numbering from 10 to 6. 
Crystals.— Numerous. 
Hard Bast. —Very feebly developed, often consisting merely of isolated cells at 
distant intervals. 
Wood-curve (see Fig. 14),—With somewhat thickened body, graceful incurving, 
and moderate-sized horns. 
Vessels.—Largest, 4, in. 
Average, about half that. 
Small, not very numerous, in radiating lines, and mostly towards upper 
portion of wood. 


Characteristic features : 
Section.—Average size, as broad as thick. 
Cortical Cavities. —Large, and comparatively numerous. 
Hard Bast.—Feebly developed. 
Wood-curve.—With thickened body and graceful incurving horns. 
Vessels.—Comparatively small, not very numerous, and distributed mostly 
towards upper portion of wood. 


26 
5. 


6. 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


E. marginata, Donn ; Jarrah. 


Tree, averaging 100ft. in height. 
Leaves.—Somewhat paler beneath. 
Size of Section.—About 1 line broad by 3 line thick, or fully twice as broad as 
thick. 
Outline of Section. Laterally elongated, ovoid usually. 
Epidermis.—Thickness, 7 — 7 in. 
Breadth, 5,— im. 
Cortical Cavities. —-f, in., almost round, numbering from 9 to 3. 
Crystals.—Numerous. 
Hard Bast.—More or less continuous, and generally one or a few cells thick. 
Wood-curve (see Fig. 15).—Elongated laterally and slender, sometimes slightly 
thickened about the middle, incurving somewhat sharply, and horns 
usually relatively short. 
Vessels.—Largest, ,4, in. 
Average, about half that. 


Medium-sized, moderately numerous, and distributed pretty regularly. 


Characteristic features : 
Section.—Fully twice as broad as thick. 
Cortical Cavities.—Moderately large and numerous. 
Hard Bast.—Continuous ; a few cells thick. 
Wood-curve.—With slender, elongated body, and usually short slender 
horns. 
Vessels.—Medium-sized, moderately numerous, and regularly distributed. 


E. diversicolor, F. v. M.; Karri. 


Tree.—Very tall and straight. 
Leaves.—Elongated, much paler beneath. 
Size of Section.—About # line broad by 4 line thick, or about 14 times broader 
than thick. 
Outline of Section.—Oval to round, usually flattened on upper surface. 
Epidermis.—Thickness, ¢, in. 
Breadth, about half the thickness. 
Cortical Cavities.— 4, in., roundish, numbering from 7 to 2, or sometimes none. 
Crystals.—Few. 
Hard Bast.—Poorly developed, very discontinuous, often consisting merely of 
single isolated cells. 
Wood-curve (see Fig. 16).—Body may be either short and stout, or elongated 


and slender, with gentle incurving and somewhat stoutish horns. 


AS AIDS IN THE DETERMINATION OF SPECIES. 27 


Vessels.— Largest, 5 I. 
Average, 3, i. 
Comparatively small, not very numerous, generally distributed in 
radiating lines, absent from lower portion of wood. 
Characteristic features: 
Section.—Comparatively small. 
Cortical Cavities.— Small, and often few. 
Hard Bast.—Poorly developed: 
Vessels.—Medium-sized, not numerous, distributed in upper portion of 
wood. 


7. E. gomphocephala, De Candolle ; Tooart. 


8. 


A good-sized tree. 
Leaves.—Thick, shining, slightly paler beneath. 
Size of Section—About # line broad and thick, or of equal breadth and 
thickness. 
Outline of Section.—From round to oval. 
Epidermis.—Thickness, 7 — 7 1. 
Breadth, .4, in. 
Cortical Cavities.—, in., elongated oval, numbering from 4 to none. 
Crystals.—Very numerous. 
Hard Bast. Forming a pretty continuous ring, generally several cells thick. 
Wood-curve (see Fig. 17).—Body usually exceedingly thick, with large and 
stout horns, often well curved inward and approaching each other. 
Vessels.—Largest, 4, in. and several ;;; In. 
Average, o5 — jy In. 
Large and comparatively numerous, distributed mostly towards 
middle and upper surface. 

Characteristic features : 

Section.—Of equal breadth and thickness. 

Cortical Cavities.—Moderately large, but few. 

Hard Bast.—Continuous and thick. 

Wood-curve.—With exceedingly thickened body, and large and stout horns. 

Vessels.—Large, numerous, and distributed largely in upper half of wood. 


E. megacarpa, F. v. M.; West Australian Blue Gum. 
Tree.—Medium-sized. 

Leaves.—Of pleasant odour, and equally green on both sides. 

Size of Section.—1 line broad by } line thick, or twice as broad as thick. 


28 


Sh 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Outline of Section Generally oval and laterally expanded, sometimes roundish 
or angular, flattened on upper and under surface. 


Epidermis.—Thickness, 4, — 3 1 


Breadth, 4, — ym in., or half the thickness. 


Cortical Cavities.—#, in. round, numbering from 7 to 2. 


in. 


Crystals.—Very few. 
Hard Bast.—Generally continuous, but irregular in thickness, giving it a zig-zag 
appearance. 
Wood-curve (see Fig. 18).—Elongated, thickened at centre, with gentle 
inturning, and horns of medium length. 
Vessels.—Largest, 3 
Average, ae half that. 
Moderately numerous, wide variations in size, lower portion of wood 
comparatively free from them. 


Characteristic features : 
Section.—Flattened, about twice as broad as thick, tending to angularity. 
Cortical Cavities.— Moderately large. 
Hard Bast.—Generally continuous, but irregular in thickness. 
Wood-curve.— Slender, slightly thickened in centre, and short horns gently 
incurved. 
Vessels.—Moderately large and numerous. 


E. tetraptera, Turczaninow ; four-winged-fruited Eucalypt. 


Shrub, seldom exceeding 10ft. in height. 
Leaves.—Very thick and equally green on both sides. 
Size of Section.—1# line broad by 13 thick, or nearly 14 broader than thick. 
Outline of Section.—Circular to oval. 
ee eg ee wo in. 
Pred um 
Cortical Cavities.— j, in. round to oval, numbering from 4 to 2. 


in. or about 4 thickness. 


Crystals.—Numerous. 
Hard Bast.—Continuous except where wood-curve is broken, and usually several 
cells thick. 
Wood-curve (see Fig. 19).— Body thickened in middle, and gently incurved horns 
of medium size. 
Vessels.—Largest 
Average 


: rn in. and several ., in. 


Ae 
’ 300 nee 
Large, numerous, and distributed pretty regularly. 


AS AIDS IN THE DETERMINATION OF SPECIES. 29 


Characteristic features : 
Section.—Very large. 
Epidermis. —Very thick. 
Cortical Cavities.—Moderately large and few. 
Hard Bast.—Continuous, and usually several cells thick. 
Vessels.—Large, numerous, and regularly distributed. 


10. E. rudis, Endlicher ; flooded or swamp Gum of Western Australia. 
Tree.—Usually not very tall. 
Leaves.—Generally thin, and equally green on both sides. 
Size of Section.—About $line broad by 4 line thick, or 14 times broader than 
thick. 
Outline of Section.—Roundish, and flattened on top. 
EPS aay Tckneas, zp mM. 
Br Sea am in., or about half the thickness. 
Cortical Cavities.— ~ in., roundish, numbering from 9 to 2. 
Crystals.—Few. 
Hard Bast.—Very poorly developed, often just represented by straggling cells. 
Wood-curve (see Fig. 20), —Illongated, and with short or medium-sized horns. 
Vessels.— Largest, 0 in. 
Average, ay, In. 
Comparatively small, moderately numerous, and mostly distributed about 
middle. 
Characteristic features : 
Section.—Small. 
Cortical Cavities.—Small. 
Hard Bast.—Very poorly developed. 
Wood-curve.—With body elongated and short horns. 


Vessels.—Small, and mainly distributed in middle of wood. 


11. E. pachypoda, F.v. M. 
Shrub. 
Leaves.—Equally green and pale on both sides. 
Size of Section.—-About 1 lie broad and thick, or equally broad and thick. 
Outline of Section.—Round, sometimes slightly elongated. 
Epidermis.—Thickness, ¢,in.; oval, numbering from 4 to 2. 
ue about 4, in. 
Cortical Cavities.—i, in. 
Crystals.—Few. 


as 


30 THE TRANSVERSE SECTIONS OF PETIOLES OF BUCALYPTS 


Hard Bast.-—Ivregularly developed, discontinuous, many-celled, or only 1 cell thick. 
Wood-curve (see Fig. 21).—Body thickened, with the two short horns gently 
incurved, and approaching each other. 
Vessels.— Largest, 5 1 
Average, pe half that. 
Medium-sized, regularly distributed, but not crowded. 
Characteristic features : 
Section.—Average size, equally broad and thick. 
EKpidermis. — Relatively thick. 
Cortical Cavities.—Moderately large, but few. 
Hard Bast.—Weak and irregularly developed. 
Vessels.—Medium-sized, and very regularly distributed. 


12. E. calophylla, Brown; Calophyllum-hke Eucalypt. 

Tall Tree. 

Leaves.—Broad, acute, thick, more horizontal than vertical, and much paler 
beneath. 

Size of Section.—13 lines broad by 1} lines thick, or nearly 14 times broader 
than thick. 

Outline of Section.—Oval to round, and usually flattened on Sn surface. 

Epidermis.—Thickness, variable in same section from J, in. to = in 

Cortical Cavities.—Largest, ¢, in., round or oval, numbering from \4 to 3. 

Central Canals.—Normally two, oval, one4 in., other J in., or sometimes half that. 

Crystals.—Moderately numerous. 

Hard Bast.—Very sparingly developed, only in small isolated patches. 

Wood-curve (see Figs. 22 and 22a).—Generally somewhat slender, and of nearly 
equal thickness throughout; the horns often approaching each other. 

Vessels.—Largest, 2 a) in. 


Average n. 


’ mn i 
Comparatively large and numerous, and distributed in radiating lines 
mostly towards upper portion. 
Characteristic features : 
Section.—Large. 
Cortical Cavities.—Generally large and numerous. 
Central Canals.—Usually two ; very large, relatively to the others. 
Hard Bast.—Very sparingly developed. 
Wood-curve.—With moderately-thickened body and horns often 
approaching. 
Vessels.—Large, numerous, and distributed mostly towards upper portion 
of wood. 


AS AIDS IN THE DETERMINATION OF SPECIES. 31 


Remarxs.—While two is the normal number of central canals, there may be 
only one, or as many as four. 


The sections from one petiole showed only a single canal near the base, but the 
normal number (2) near the leaf-blade. The two main canals were also found in 
several instances to divide into four on passing into the midrib. Probably this is a 
normal occurrence in this species. 


The contents of the canals were tested with various reagents. When treated 
perfectly fresh they readily dissolved, but after long steeping in water, they became 
hardened and insoluble in the ordinary reagents. Under these circumstances they 
would not dissolve either when warmed in nitric acid or in potash and glycerine. 
Nitric acid gave a red tint, and potash a brown, but that was all the change observed. 


In the section of the young stem it is interesting to observe that central canals 
are absent, while the cortical cavities are present. The latter are very numerous, just 
as in some sections of the leaf stalk. The hard bast is not of equal thickness 
throughout, nor is it always continuous, although it is shown thus in the drawing for 
simplicity. Only the larger vessels of the wood are figured. 


13. E. ficifolia, &. v. M.; scarlet-flowered Eucalypt. 
Tree.—Seldom exceeding height of 50ft. 
Leaves.— Generally resembling preceding, but not so broad in proportion to 
length. 
Size of Section.— 14 lines broad by 1 line thick, or 1} times broader than thick. 
Outline of Section. Varying from round to oval to a much depressed semi-circle. 
Epidermis.—Thickness, 5, — J in. 
Breadth, 4 in 
Hypoderma.—Equal to enderms in thickness, and usually a two-celled layer. 
Cortical Cavities.—About 3, in., few in number, or absent. 
Central Canals.— Normally 2, ‘a occasionally 3 or 4; roundish. 
Largest, about 5, in. 
Crystals.—Numerous. 
Hard Bast.—In irregular patches, a few cells thick. 
Wood-curve (see Figs. 23 and 23a).—Generally slender, and with horns curving 
gently, and sometimes almost meeting. 
Vessels.—Largest, 3 in 


Average, abouts: mw} 


Comparatively a Ae numerous, and distributed towards upper 
and middle portions of wood. 


32 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Characteristic features : 

Section.—Large. 

Hypoderma.—Generally two cells thick. 

Cortical Cavities.—Small and few. 

Central Canals.—Normally two, but liable to variation; about same size 
as the largest of the cortical cavities. 

Hard Bast.—In irregular patches. 

Wood-curve.—Slender, and horns approaching each other, sometimes very 
closely. 

Vessels.—Comparatively large, numerous, absent from lower portion of 
wood. 


Remarxs.—Cortical cavities are certainly present in this species, but they are 
few in number, and many sections of a series show none. ‘They are likewise small, 
indeed the smallest of any species examined. 


The normal number of central canals is two, but occasionally there may be 
three or even four, as in one of the sections photographed. The occurrence of four 
canals is rather interesting in view of the fact that they were found in sections taken 
near the base of the leaf-blade. It would appear that while the normal number of 
two usually occurs in the body of the petiole, as the lamina is approached each 
divides into two before entering the mid-rib. 


Il.—Form ConFINED To VICTORIA. 


14. E. alpina, Lindley; alpine gum. 


Shrub. 
Leaves.—Very thick, broad, blunt, equally green on both sides. 
Size of Section.—About 1} lines broad and thick, or as broad as thick. 
Outline of Section.—Usually rounded, 
Epidermis.—Thickness, J, in. below, 7 in. above. 
Cortical Cavities. —4, in. roundish, numbering from 16 to 6. 
Crystals.—Very few. 
Hard Bast.—Well-developed, generally continuous, and several cells thick. 
Wood-curve (see Fig. 24).—With thickened body and gently incurved short horns. 
Vessels.—Largest, 4 in. 
Average, za in. 
Medium-sized and moderately numerous, principally occupying middle 


tract of wood. 


AS AIDS IN THE DETERMINATION OF SPECIES. 30 


Characteristic features : 
Section.—Large, as broad as thick. 
Cortical Cavities. —Moderately large, and numerous. 
Hard Bast.—Well-developed, and generally continuous. 
Wood-curve.—With thickened body and gently incurved short horns. 
Vessels.--Medium-sized, principally distributed in middle tract of wood. 


Tll.—Form Conrinep to New SoutH WaAtgs. 


15. E. punctata, De Candolle ; leather-jacket. 
Tree.—Attaining a height of 100ft. or more. 
Leaves.—Paler beneath. 
Size of Section.—About } line broad and thick, or as broad as thick. 
Outline of Section.—Round, with slight flattening on upper surface. 
Epidermis.—Thickness, 3; — jg 1. 
Breadth, about —,, in. 
Cortical Cavities.— 4, in., elongated oval, numbering from 8 to 1. 
Crystals.—Very few. 
Hard Bast.—Very sparsely developed. 
Wood-curve (see Fig. 25).—Nearly always found entire; body thickened, and 
horns very gently incurved and short. 
Vessels.— Largest, 4; in. 
Average, gy i. 
Relatively few, small and scattered. 

Characteristic features : 

Section.—Small, as broad as thick. 

Cortical Cavities.— Moderately large. 

Hard Bast.—Very poorly developed. 

Wood-curve.—Nearly always found entire, with thickened body and short 

horns. 
Vessels.—Few, small, and scattered. 


IV.—Forms ConFINED TO QUEENSLAND. 


16. E. maculata, var. citriodora, Hooker ; lemon-scented Eucalypt. 
Tree.—Only differing from maculata in the lemon-scented foliage. 
Size of Section.—1} line broad by 1 line thick, or 1} times broader than thick. 
Outline of Section.—Oval, somewhat irregular in outline, and flattened or 
depressed on top. 


34 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Epidermis.—Thickness, 5, — gp I. 
Breadth, ;4, 1. 
Cortical Cavities.— Largest, +, in., oval to round, numbering from 8 to 0. 
Central Canals.—Normally 2, oval and round; largest about the same size as 
cortical cavity. 
Crystals.—Moderately numerous. 
Hard Bast.—Very poorly developed, just represented at intervals by a few 
straggling cells. 
Wood-curve (see Fig. 26).—Usually of equal thickness throughout and slender, 
with very gently incurved horns, each about one-third body-length. 
Vessels.—Largest, =, in. 
Average, about 5, im. 
Numerous, large (about twice the size of those of maculata), and 
generally distributed. 
Characteristic features : 
Section.—Large. 
Cortical Cavities.—Moderately large, variable in number. 
Central Canals.— Normally two, and same size as cortical cavities. 
Hard Bast.—Very poorly developed. 
Wood-curve.—Of equal thickness throughout, with very gently incurved 
horns. 


Vessels.— Large, numerous, and generally distributed. 


Remarxs.—A petiole was noticed showing only one central canal near the base 
or point of attachment to the stem, but the normal number (two) towards the leaf- 
blade. Another petiole showed one only in all the sections examined. 


V.—Form Bertonerna to Soutn AUSTRALIA AND VICTORIA. 


17. E. corynocalyx, F. v. M.; sugary Eucalypt; sugar gum. 


Tree.—Finally tall, said to be the largest tree growing in South Australia. 
Leaves.—Shining, somewhat paler beneath. 
Size of Section.—About # line broad by } line thick, or 1} times broader than 
thick. 
Outline of Section.—Round to oval, usually flattened on upper surface. 
Epidermis.—Thickness, 5 in. 
Breadth, ;4, in. 


Cortical Cavities.-- 4, in., round or slightly oval, numbering from 4 to 18. 


AS AIDS IN THE DETERMINATION OF SPECIES. 35 


Crystals.—Few. 
Hard Bast.— Sparingly developed, sometimes consisting of isolated cells. 
Wood-curve (see Fig. 27).— Usually with slender, elevated horns, dipping inward. 
Vessels.---Largest, 5 in. 
Average, about 4, in. 
Rather small on the whole, comparatively few, somewhat scattered, 
and mostly absent from lower portion of wood. 
Characteristic features : 
Section.— Small. 
Cortical Cavities —Numerous, but comparatively small. 
Hard Bast.—Sparingly developed. 
Wood-curve.— Usually symmetrical and entire, with slender and very gently 
incurved horns. 
Vessels.—Comparatively small. 


VI.—Forms Brtoneine to Victoria, New SoutH WALEs, AND QUEENSLAND. 


18. E. melliodora, Cunningham ; honey-scented Eucalypt, or yellow box tree. 


Tree.—Middle-sized. 
Leaves.—Equally dull-green on both sides. 
Size of Section.—About 4 line broad and thick, or as broad as thick. 
Outline of Section.—Round or oval, and flattened on upper surface. 
Epidermis.—Thickness, 5 — a In. 
Breadth, about ;4, in. 
Cortical Cavities.—3, in., round, numbering from 4 to 1 or none. 
Crystals.—Very numerous, and frequently in groups. 
Hard Bast.—Continuous, and generally two cells thick. 
Wood-curve (see Fig. 28).—Always found unbroken, with thickened body and 
sharply inturned short horns. 
Vessels.—Largest, jj, in. 
Average, about =, in. 
Medium-sized, numerous, and equally distributed. 

Characteristic features : 

Section.—Small; as broad as thick. 

Cortical Cavities.—Small and few. 

Hard Bast. - Continuous, and generally a two-celled layer. 

Wood-curve.—Always found unbroken, with thickened body and short horns. 

Vessels. —Medium-sized, numerous, and equally distributed. 


36 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


19. E. tereticornis, Smith; flooded gum-tree. 


Tree,—Tall, handsome, seldom exceeding 100ft. in height. 

Leaves.—Kqually green on both sides. 

Size of Section.—About ? line broad by 3 line thick, or 14 times broader than 
thick. 

Outline of Section. eee aes round to oval. 

EKpidermis.—Thickness, ~, in. 


> 760 
ee 
Breadth, 5, — yj im. 
Cortical Cavities. —*, in., round to oval, numbering from 10 to none, but on an 


average ‘belat 5. 
Crystals.—Very numerous. 
Hard Bast.—Sparinely developed, discontinuous, in many places 1 cell thick. 
Wood-curve (see Fig. 29).—Body moderately thickened and horns gently 
incurved ; es found entire. 
Vessels—Largest, 4, 1 
Average, a half that. 
Comparatively small, moderately numerous, distributed loosely towards 
upper portion, and generally absent from lower portion of wood. 
Characteristic features : 
Section.— Small. 
Cortical Cavities. —Small. 
Hard Bast.— Sparingly developed. 
Wood-curve.—Symmetrical, and always found entire. 
Vessels.—Comparatively small, moderately numerous, and distributed 
loosely towards upper portion of wood. 


VII.—Forms Benoneine to New South Wates anp QUEENSLAND. 


20. E. saligna, Smith; grey gum-tree. 


‘Tree.—Tall. 
Leaves.—Tapering, much paler beneath. 
Size of Section.—% line broad by 4 line thick, or 14 times as broad as thick. 
Outline of Section.— Rounded, with flattened upper surface. 
Epidermis.—Thickness, 4, m. 

Breadth, about 5 1 
Cortical Cavities.— < in., round to eae numbering from 7 to 6. 
Crystals.—Numerous. 
Hard Bast.—Very poorly developed, and in many places entirely absent. 


AS AIDS IN THE DETERMINATION OF SPECIES. : 37 


Wood-curve (see Fig. 30).—Body thickened and elevated, horns generally not 
much incurved. 
Vessels.—Largest, 5, in. 
Average, about half that. 
Moderately large, numerous, and generally distributed. 
Characteristic features : 
Section.—Small. 
Cortical Cavities —Moderately large and numerous. 
Hard Bast.—Feebly developed. 
Wood-curve.-—With thickened body, and generally elevated horns. 
Vessels.—Moderately large, numerous, and generally distributed. 


21. E. maculata, Hooker; spotted gum. 


Tree.—Tall, handsome. 
Leaves. —Often very large and coarse, and equally green on both sides. 
Size of Section.—1 line broad by ? line thick, or about 1} times broader than 
thick. 
Outline of section.—Oval, flattened on upper surface. 
Epidermis.—Thickness, about ,5, in. 
Breadth, about half that. 
Cortical Cavities.—,5 in. oval to round, numbering from 6 to 2. 
Central Canals.—Normally 2, oval to round; largest, about 4, in., or generally 
the size of the cortical cavities. 
Crystals.---Numerous. 
Hard Bast.—In closely adjoining patches, generally a few cells thick. 
Wood-curve (see Fig.31).—Usually of equal thickness throughout, with very 
gently incurved horns, each about one-third of body-length. 
Vessels.—Largest, about 7, in. 
Average, 4, — gr im. 
Moderately large and numerous, confined almost exclusively to upper 
and middle portion of wood. 
Characteristic features: 
Section.—Of average size. 
Cortical Cavities.—Medium-sized, not very numerous. 
Central Canals.—Normally 2, about same size as cortical canals. 
Hard Bast.—In contiguous patches, a few cells thick. 
Wood-curve.—Of equal thickness throughout, with very gently incurved 
horns. 
Vessels.—Moderate in size and number, and absent from lower portion of 
wood. 


38 . THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Remarxs.—The number of central canals varies occasionally, due probably to the 
splitting up of the normal number (two). Thus, in nine successive sections taken from 
about the middle of the leaf stalk, there were four, two on each side; and in another 
petiole, the sections showed five, three on one side and two on another. And, as if 
to complete the series, a third petiole exhibited no less than six canals—three on 
either side, one of each being about the normal size, and the other two rather 
smaller. 


VIII.—Form Betoneine to Sours Austrauia, Victoria, anD New Sout WALEs. 


22. E. macrorrhyncha, F. v. M.; Victorian stringy-bark. 


Tree.— Tall. 
Leaves.—EHlongated, equally green on both sides. 


Size of Section. —1 line broad by % line thick, or about 14 times broader than 
thick. 

Outline of Section.—Oval, or nearly round. 

Epidermis.— Thickness, 5, in. 

Breadth, 7, — gq in. 

Cortical Cavities. — in., oval and round, numbering from 8 to 2. 

Crystals.—Few. 

Hard Bast.—Well-defined layer, several cells thick. 

Wood-curve (see Fig. 32).—Body exceedingly thick and short; horns stout, 
upright, or sharply inturned ; always found entire. 

Vessels.— Largest 


ae 
> qqg WD. 


Average 


tele 
Large and numerous; pretty equally distributed, but most thickly 
towards upper portion of wood. 
Characteristic features : 
Section.—Average size. 
Cortical Cavities.— Moderately large. 
Hard Bast.—Well-defined, and several cells thick. 
Wood-curve.—Always found unbroken, with much-thickened body, and 
short stout horns. 
Vessels.—Large, numerous, distributed mostly towards upper portion of 
wood. 


AS AIDS IN THE DETERMINATION OF SPECIES. 39 


IX.—Form Bertonerne to Tasmania, Victorta, AND New SoutH WALES. 


23. E. globulus, Labillardiere; blue gum. 
Tree.—Very tall. 
Leaves.—Thick, elongated, equally green on both sides. 
Size of Section.—A little over 1 line broad and 1 line thick, or slightly broader 
than thick. 
Outline of Section.—Oval, slightly flattened on upper surface. 
Epidermis.—Thickness, + in. 
Breadth, 5,— gq in. 

Cortical Cavities.— in., oval to round, numbering usually 7 or 8. 

Crystals.— Very numerous. 

Hard Bast.—Strongly developed, continuous, and usually dense. 

Wood-curve (see Figs. 32 and 33a).—Body thickened, particularly at the centre, 
and gently incurved horns, each about one-third length of body, 
and directed towards it at the tip. 

Vessels.—Largest, 4, in. 

Average, about half that. 

Comparatively large and numerous, radially arranged, and distributed 
mainly in upper half. A number of large vessels usually scattered 
about lower portions of wood. 

Characteristic features : 

Section.—Average size, slightly broader than thick. 

Cortical Cavities—Large, and numbering about 7 or 8. 

Crystals.—Very numerous. 

Hard Bast.—Well-developed and dense. 

Wood-curve.—-With thickened body, and horns curving gently inward. 

Vessels.—Large, numerous, and distributed mostly in upper half, but 
sparingly along lower margin of wood. 

Remarx.—In one petiole examined, all the sections showed an isolated bundle at 


one side of the ordinary curve. 


This species, however, shows as little tendency to broken and isolated wood- 
curve as any other examined. 


X.—Formus Betoncine to SoutrH AusTrRALiA, TasMANIA, VICTORIA, AND 
New Soutn Watgs. 
24. E. obliqua, L’ Heritier ; messmate. 
Tree.—Lofty. 
Leaves.—Very inequilateral at base, equally green on both sides. 


40 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Size of Section.— 1} lines broad by 1 line thick, or 14 times broader than thick. 
Outline of Section.—Oval to circular, sometimes flat on upper surface. 
Epidermis.—Thickness, ,-— 7, in. 
Breadth, about ;%, in. 
Cortical Cavities.—-;, n., roundish, numbering from 7 to 2. 
Crystals.—Few. 
Hard Bast.—Well developed, continuous, and many cells thick. 
Wood-curve (see Fig. 84).—Comparatively slender body, with short horns 
elevated or gently incurved. 

Vessels.— Largest, 4, In. 

Average, about half that. 

Large, numerous, and pretty regularly distributed, but most 


numerous towards upper portion of wood. 


Characteristic features : 
Section.—Large. 
Epidermis.—Thickish. 
Cortical Cavities.—Large. 
Hard Bast.—Well developed and dense, especially between the horns. 
Wood-curve.—With slender body and short horns. 
Vessels.—Large, numerous, and pretty regularly distributed. 


25. E. amygdalina, Labillardiére ; giant Eucalypt, Dandenong peppermint, mountain 

ash. 

Reputed to be the tallest of trees. 

Leaves.—Thin, equally green on both sides, with copious and transparent oil- 
dots. 

Size of Section.—About 4 line broad and thick, or equally broad and thick. 

Outline of Section.—Oval to round, with occasionally a flattened upper surface. 

Epidermis.—Thickness, = — 


= 

ag in. 
‘ 1 if = 

Breadth, 3, — win. 


aj I., oval or round, numbering from 7 to 2. 


Cortical Cavities.— =, 
Crystals.—Numerous. 
Hard Bast.—Sparingly developed, one or a few cells thick. 
Wood-curve (see Fig. 35).— Body excessively thick, with short stout horns elevated 
or slightly incurved; always found entire. 
Vessels.—Largest, |4, In. 
Average, about half that. 
Small, moderately numerous, on radiating lines, generally equally 
distributed, but scanty towards lower margin. 


AS AIDS IN THE DETERMINATION OF SPECIES. 41 


Characteristic features : 
Section.—EHxceptionally small, equally broad and thick. 
Cortical Cavities. —Small. 
Hard Bast.—Composed of few cells, but strongly thickened. 
Wood-curve.—Always found entire, with excessively stout body and short, 
stout horns. 
Vessels.—Small, moderately numerous, and pretty regularly distributed. 


Remarks.—In proportion to the size of the section, the wood-curve is the 
thickest of any yet investigated. This is of interest in connection with such a very 
tall tree, since the water must be raised so great a distance to reach the topmost 
boughs. It was also observed that the leaves from this tree did not, in the least, 
discolour the water in which they were kept for some months, although all other 
species examined did so, more or less. 


26. E. viminalis, Labillardiére ; Manna-Kucalypt. 


Tree.—Tall, and sometimes even gigantic. 

Leaves.—Thin, equally green on both sides. 

Size of Section.—Hither 1 line broad by ? line thick, or of equal breadth and 
thickness. 

Outline of Section.—Round to egg-shaped, or flattened on top, so as to become 
somewhat hemispherical. 


Kpidermis.— Thickness, 5, in. 
Breadth, as broad as thick, and sometimes broader. 
Cortical Cavities—,, in. in some sections, and only half that in others; 


roundish to oval ; numbering from 7, often 2, and sometimes absent. 

Crystals.—Numerous, and sometimes large. 

Hard Bast.—Moderately developed; slightly discontinuous; 1 sometimes, 
but mostly several cells thick. 

Wood-curve (see Figs. 36 and 36a).—Body straight and thickened, with short, 
sharply incurved, and usually broken horns. Occasionally a distinct 
isolated bundle at side of one of the horns. 


a 1 ees 
Vessels.— Largest, from ,5, — ji, I. 
. We os 
Average.—,4, in. 


Small, comparatively few or moderately numerous, mostly distributed 
towards upper portion of wood, and generally absent from horns. 
Characteristic features : 
Section.—Average size. 
EKpidermis.—Relatively thin, composed of cells at least as broad as thick. 
Cortical Cavities.—Medium size, often few. 


42, 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Wood-curve.—Straight and thickened body, with short, sharply incurved 
horns, often in detached parts. 
Vessels.—Small, and distributed on upper portion of wood, generally absent 
from horns. 


27. E. gunni, J. Hooker; swamp gum or cider Eucalypt. 


Tree.—Usually not tall. 
Leaves.—Equally dark green on both sides. 
Size of Section.—1} lines broad by 1 line thick, or 1} lines broader than thick. 
Outline of Section.—Oval to round, sometimes flattened on top. 
Epidermis.—Thickness, 5 — 7 i. 

Breadth, about ;*, in. 
Cortical Cavities.—,,, in., round or oval, numbering from 9 to 2. 
Crystals.—Few. 

Hard Bast.—Well developed, nearly continuous, and several layers of cells thick. 
Wood-curve (see Fig. 37).—Body thickened (thickness sometimes ;, in.), with 
short and sharply incurved horns directed towards body. 

Vessels.—Largest, 3, in. 
Average, ,2,n., or about half the largest. 
Moderately large and numerous, and pretty equally distributed with 
large ones at lower portion of wood as in globulus. 


Characteristic features : 
Section.—Relatively large. 
Cortical Cavities.—Large and moderately numerous. 
Hard Bast.—Somewhat dense. 
Wood-curve.—With thickened body and short horns directed towards it. 
Vessels.—Moderately large, numerous, and pretty generally distributed. 


XI.—Form Betoneinc to Sourn Avustrauia, Tasmania, Victoria, New SoutH 


WALES, AND QUEENSLAND. 


28. E. stuartiana, F. v. M.; apple-scented Eucalypt. 


Tree.—Moderate-sized. 

Leaves.—Kqually dark-green on both sides. 

Size of Section.—About 4 line broad by } line thick, or about 14 times broader 
than thick. 

Outline of Section.—Oval. 


AS AIDS IN THE DETERMINATION OF SPECIES. 43 


epi eres, Lnlgneees am in. 
ee 
Cortical Cavities.— 


i= — im IN., or sometimes as broad as thick. 


= in., oval to oe cis round, numbering about 6. 


Crystals.—Moderately numerous. 

Hard Bast.—Almost continuous, regular, generally two or three cells thick. 
Wood-curve (see Fig. a): —Body curved and moderately thickened (thickness 
Samieunpe zy in.), with short and sharply incurved horns. 

Vessels.—Largest, = in. 
Average, about half that. 
Small, numerous, and generally distributed towards upper and middle 
portion of wood. 
Characteristic features : 
Section.—Small. 
lpidermis.—Relatively thin, component cells often as broad as thick. 
Cortical Cavities.—Small. 
Hard Bast.—Regular, but not very dense. 
Wood-curve.—Moderately thick, and horns somewhat sharply incurved. 
Vessels Small numerous, and distributed towards upper and middle 
portion of wood. 


XIJ.— Form Betoneine to Sourn Avustrauia, Victorta, New SourH WALES, AND 
QUEENSLAND. 
29. E. leucoxylon, F. v. M.; Victorian ironbark. 
‘Tree.—Moderate size. 
Leaves.—Equally dull-green on both sides, with copious, pellucid oil-dots. 
Size of Section.—13 lines broad by # line thick, or twice as broad as thick. 
Outline of Section.—Roundish, flattened, or somewhat quadrangular. 
PL eae ppg aq in. 
Breadth =o Vide 


’ nS 1500 


Cortical Cavities.— ;, in. oval, numbering from 9 to 1, or none. 


Crystals.—Moderately numerous. 

Hard Bast.—Poorly developed; in many places entirely absent. 

Wood-curve (see Figs. 89 and 89a, b, c)—Body variable in thickness, and longer 
or shorter horns, gently incurved. 


Vessels.—Largest, 4 io in. 


Average n. 


1 
; = 
Medium-sized and numerous, radially arranged, and regularly distributed. 


44 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Characteristic features : 
Section.—Large, twice as broad as thick. 
Cortical Cavities.—Large. 
Hard Bast.—Scantily developed. 
Vessels.—Medium-sized, numerous, and regularly distributed. 


XIII.—Form Betoneinc To Western Australia, SoutH AUSTRALIA, VICTORIA, 
New South Wass, QuEENSLAND, AND NortH AUSTRALIA. 


30. EH. rostrata, Schlechtendal ; red gum. 
Tree.—Of moderate size, often attaining a height of over 100ft. 
Leaves.—Kqually green on both sides. 
Size of Section.—About 4 line broad and thick, or equally broad as thick. 
Outline of Section.—From round to irregular oval, generally with somewhat 
flattened upper surface. 
Epidermis.—Thickness, = in. 
Breadth, about ;4, in. 
Cortical Cavities.— ,,1n., roundish, numbering from 8 to none. 
Crystals. —Moderately numerous. 
Hard Bast.—Sparingly developed, discontinuous; one or a few cells thick. 
Wood-curve (see Fig. 40).—Thickened body, and stout short horns, usually 
gently incurved. 
Vessels.—Largest, ,4, 1. 
Average, ja, 1. 
Moderately large and numerous, mainly distributed in upper portion. 
Characteristic features : 
Section.— Small, equally broad and thick. 
Cortical Cavities. —Small and variable in number. 
Hard Bast.—Scanty. 
Wood-curve.—Moderately thickened, and short, stout horns. 
Vessels.—Medium-sized, numerous, and mainly distributed in upper 
portion of wood. 


XIV.—Forms Betoneine to West Austraia, SoutH AUSTRALIA, VICTORIA, AND 
New SoutH Watgs. 


We are indebted to Mr. Bosisto for specimens of the leaves of E. uncinata 
(Turezaninow) and EL. oleosa (F. v. M.), from the district between Dimboola and Lake 


AS AIDS IN THE DETERMINATION OF SPECIES, 45 


Hindmarsh. They constitute large portions of the ‘‘ Mallee Scrub,” and along with 
E. incrassata, Labillardiére, and its smaller variety, H. dumosa, are the only species 
of Eucalypt with the above Australian distribution, according to present knowledge. 


They are all shrubby, or at most somewhat arboreous, with leaves equally green 
on both sides. 


Only a few sections were made of wncinata and oleosa, but there is a decided 
difference between the wood-curve of each, so that they are thereby easily 
distinguished. (Figs. 41 and 42.) 


It is believed that the foregoing descriptions, with the accompanying drawings, 
when taken in conjunction with external leaf characters, will materially aid in the 
discrimination of the investigated species. Various specimens have been taken at 
random and tested, and referred to their respective types. 


As a very instructive example of this, no better could be given than the 
following :—One of us had a few leaves sent without any information as to their 
nature or locality, and sections were made in due course, and the following notes :— 
“The leaf looks like that of citriodora, but the characteristic odour is wanting. 
The first section shows two canals, and fairly numerous cortical cavities ; outline 
somewhat like citriodora. A second section from another petiole has very irrecular 
outline, but otherwise agrees with the first. A third section was cut from another 
petiole, which was still more like citriodora, a third canal tube appearing as in one 
of the type specimens of that species. I conclude that this specimen is either a 
variety of citriodora, or another very closely allied species.” The leaf belonged to 
E. maculata, thus justifying, from quite an independent source, Baron von Mueller’s 
determination of citriodora as a variety of that species. 


And, in the practical test to be presently described, the utility of the method 
will be more fully shown. But, apart altogether from the practical utility of this 
investigation, there is new light thrown on the histology of this important genus. 


M. L. Petit’ has described the structure of the petiole of Dicotyledons in 48 
families, including 300 genera and nearly 500 species, one of the families being the 
Myrtacez, to which the Eucalypts belong. 


He found the form of the petiole to be always convex below and concave on the 
upper face, whereas our observations show, in the twisted petioles of Kucalypts, that 
while this is often the case it is not invariably so. Thus, in obcordata and alpina the 
upper surface of the section is more convex than the lower, and in grossa and rostrata 
the section is round. The lower surface is generally convex and the upper flat. 


* Mem. Sci. Phys. and Nat. Bordeaux III. (1887). 


46 THE TRANSEVRSE SECTIONS OF PETIOLES OF EUCALYPTS 


As to the fibro-vascular system, it is observed that aggregation of the bundles 
generally occurs in woody plants, as we found to be the case, and that bicollateral 
bundles occur in the Myrtacez, among others. In the genus Eucalyptus, at any rate, 
the bundles are concentric. 


However, the importance of the structure of the petiole for taxonomic purposes is 
clearly established in this paper, and he naturally insists on the importance of the 
petiole for purposes of classification. 


A few of the facts recorded in the various suggestive and instructive papers on the 
Eucalypts by J. Bosisto, Esq., C.M.G., read at different periods before this Society,* 
may be noticed in connection with our present subject. He is led to the important 
conclusion that the volatile oil is the base of other products, such as resin-like 
substances, inasmuch as those species, great in the production of the oil, vigorously 
supply it to the atmosphere, and thus do not allow sufficient time for the formation 
of resinoid bodies, which require the absorption of oxygen by the leaf; and, 
conversely, those species less vigorous in oil production allow time for such a 
purpose, and so become well stored. 


This suggested to us that there might be some relation between the size and 
number of cortical cavities, and the greater or less production of oil or resinoid 
bodies respectively. Two of the chief oil-producing species are amygdalina and 
globulus, and of kino-producing species, Jeucoxylon and rostrata. On referring to 
the detailed description, amygdalina is found to have the smallest and fewest 
cavities of any of these, being even surpassed by viminaiis, which yields the least oil. 
Globulus has certainly large and moderately numerous cavities, but, on the other 
hand, Jeucoxylon is not far behind it, which yields kino to the extent of even 22 per 
cent. from fresh bark. 


We have observed that as a rule the notable producers of oil do not show 
numerous cortical cavities in their petioles, so that we may perhaps conclude that the 
production of kino in the leaf-stalk is not immediately dependent on the production 
of oil in the leaf-blade. It is in the leaf-blade alone that the oil is manufactured, as if 
was proved to be absent from the petiole, so that, contradictory as it may appear, it is 
in the leaf-blade, with its two surfaces equally exposed to sun and air, that the least 
oxidised constituent—the volatile oil—is made. ‘To prove the absence of oil from 
the leaf-stalk (at least in amygdalina, and presumably in the others), a simple 
experiment was made, which may be briefly described. 


Branchlets of fresh leaves were kindly supplied by Mr. Slater, of Mitcham 
Grove, such as he is in the habit of using for distilling his well-known oil. The 
largest and best leaves were selected, and 1000 petioles carefully snipped off and 


* See Trans. and Proceedings of Roy. Soc. of Vict., Vol. XII., &e. 


AS AIDS IN THE DETERMINATION OF SPECIES. AT 


weighed, amounting to a little over 200 grains. They were distilled by passing a 
current of steam through them for some time, but not a trace of oil, not even the 
smell of it, was obtained. 


Hence it would appear that the volatile oil is confined to the leaf blade, the 
flower-buds, and the fruit-capsules. 


The presence of central canals or reservoirs throughout the length of the petiole 
in calophylla, and its close ally ficifolia, maculata, and its variety citriodora, it 1s not 
easy to explain. When it is known whether they occur in any, and in what other 
forms, one may perhaps venture on an explanation. It is noteworthy that in 
calophylla the kino is a liquid of treacle-like consistence, and obtained in considerable 
quantity by tapping the tree (Kuc. Dec. X.), and that of maculata is readily soluble 
in hot water (Dec. III.) 


While weighing the leaf-stalks for the above purpose the weight of the leaf-blades 
belonging to them was likewise determined. The blades were sometimes imperfect 
from the ravages of insects or decay, so that the relative weight errs on the side of 
defect ; 1000 leaf-blades were found to weigh 48323¢rs., and the corresponding leaf- 
stalks 212ers., so that, on an average, each stalk has to bear a weight at least 23 times 
that of its own. 


VI. A Practicat Trsr. 


Tn order to settle how far the transverse section of the petiole alone was capable 
of determining species, we decided to submit the matter to a practical and very 
searching test. The names of the 30 kinds investigated by us were handed to Mr. 
Guilfoyle, and he selected specimens of leaves of szx of them. These were sent to 
us with numbers attached, while the names were retained by him. It will be seen 
that the test was really very severe, even more so than would occur in actual practice. 
In the first place the docality of the tree would be known, when met with in its native 
state, and by referring to the Table of Geographical Distribution (Table I.), the area 
of selection would be limited. In the next place, there are certain characters belong- 
ing to the leaf as a whole, which would help to settle specific nature. These two 
features are taken into account in the next section, dealing with a scheme for deter- 
mining species, but we thought it well to settle how far anatomic structure of the 
leaf-stalk, apart from other characters, could be depended on for specific distinction. 
This trial justifies us in our belief, that while sections of the leaf-stalk may be 
valuable aids in the discrimination of species, it would be unsafe to rely upon them 
exclusively. 


48 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


The result of this test was that four were named correctly and two wrongly, as 
shown in the following, sent by Mr. Guilfoyle :— 


YOURS. MINE. 

No. 1 E. cornuta Soe EK. cornuta 

ana ,, corynocalyx ie 5, corynocalyx 
ae ,, gomphocephala. .... ,», gomphocephala 
foetal ,, mMegacarpa ath ,, megacarpa 
LED », viminalis ae ,, occidentalis 

is 6 ,, melliodora ies ,», punctata 


It will not be necessary to say much about the first four, which were correctly 
named, but the two latter incorrectly named deserve further notice. The following 
remarks are meant to show the principal points which guided us in coming to a 
decision. 


No. 1. E. cornuta showed the characteristic features in the size and shape of the 
section; the large and numerous cortical cavities quite close together ; crystals 
moderately numerous; the wood-pattern continuous or often discontinuous at the 
horns, which are sharply incurved (as in Fig. 12), and the vessels distributed towards 
the middle and upper portion of wood. 


No. 2. E. corynocalyx showed numerous but comparatively small cortical cavities ; 
crystals rather few; relatively few hard bast cells ; symmetrical and generally entire 
wood-pattern, with slender, short, and gently incurved horns. (Fig. 27.) 


No. 3. E. gomphocephala showed few and moderately large cortical cavities ; 
wood-pattern, with very stout body and horns well curved in, and approaching each 
other; and the vessels large and numerous, and mostly in upper portion of wood. 
The large proportion of wood is a feature of Gomphocephala. (Fig. 17.) 


No. 4. E. megacarpa showed flattened section, tending to angularity, and nearly 
twice as broad as thick; hard bast irregular, and cells arranged in patches ; wood- 
pattern, with slender body, slightly thickened in middle, and short horns gently 
incurved. (Fig. 18.) 


No. 5. E. occidentalis (determined as E. viminalis). Since E. occidentalis is 
confined to Western Australia, and £. viminalis does not occur there, it is evident 
that the locality of the specimen would have prevented that mistake. 


As this particular specimen was somewhat puzzling to determine, it received 
special attention, and the following diagnosis of it was made by one of us :— 


Outline of Section.—Oval ; flattened on upper surface. 


Outer wall of Epidermis.—,,, in., relatively thin. 


AS AIDS IN THE DETERMINATION OF SPECIES. 49 


Cortex.—Consisting of rather loose tissue. 
Crystals.— Very numerous and in clusters. 
Cortical Cavities.—Five is a common number ; sometimes very large, about 
a il. 
Wood-pattern.—Always unbroken. 
Vessels.—Moderately numerous; distributed towards upper portion and 
middle of wood ; largest about {4 in. 
Body of curve is thickened about middle, and the two short horns curve 


gently and symmetrically upward and inward. 


The thinness of the epidermis, the number and relative size of the cortical 
cavities, the loose tissue of the cortex, the hard bast of few cells, but regularly 
distributed, the wood-pattern, and the distribution of the large and numerous vessels, 
seemed to point to viminalis. But the specimen turns out to belong to a tree which 
is exceedingly variable; ‘‘so variable,” as Baron von Mueller expresses it, ‘‘ as to 
change much of former ideas as regards the precincts of Hucalyptus species,” and 
therefore it would have been a mere accident to have determined it accurately from 
the construction of the leaf-stalk alone. 


No. 6. E. punctata (determined as E. melliodora). There is a general agreement 
between these two forms in the small size and round shape of the section, the 
thickness of epidermis, the number and size of cortical cavities, the hard bast composed 
of few cells, and the general features of the wood-curve. But in the former the 
vessels of the wood are relatively few, small, and scattered ; and in the latter twice 
the size, numerous, and equally distributed. Further, crystals are very few in 
punctata, but very numerous in melliodora. 


It is thus shown in a practical way how the minute structure of the leaf-stalk 
may be employed in the acknowledged difficult task of determining Eucalyptus 
species. As might be anticipated, this structure will vary according to differences in 
soil and climate, heat and moisture, but there is still a certain amount of constancy 
in the internal characters which renders their aid valuable. It is not the failure of 
the system adopted, but the imperfection of it, which prevents its wider application. 
Taking the characters of the leaf as a whole, and not merely sections of the petiole, it 
is believed that specific distinctions might be decided thereby. 


50 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


V1II.—Scueme For DETERMINING SPECIES. 


As our investigations proceeded it became evident that some scheme of arrange- 
ment might be devised, whereby the different species could be more or less completely 
separated, by taking all the characters derivable from the leaf. In framing this 
scheme we took the external leaf-characters principally from Baron von Mueller’s 
‘Kucalyptographia,’ where the most minute peculiarities are clearly noted, and 
combined them with such characters as were peculiar to the section of the leaf- 
stalk. 


It will be understood that this scheme is by no means meant to be final, since it 
is concerned with thirty species selected at random from the whole range of genera ; 
but it is merely given to show iow such ascheme might be constructed for any definite 
and restricted section of the Eucalyptus-species. Thus, when all the Victorian species 
have been investigated as to the structure of their petioles, it will be possible so to 
arrange them that the different species will be more or less clearly marked out. 


With this qualification, the scheme applicable to the thirty species will now be 
indicated, and may be generally represented as follows :— 


Section I.—Central Canals present. 
yolles Sy ,» absent. 


Section I. 
A. Cortical Cavities large — 
1. Hard Bast well developed— 
1. E. maculata. 
2. Hard Bast feebly developed— 
2. E. maculata, var. citriodora. 
3. EH. calophylla. 
B. Cortical Cavities small—— 
4. K. ficifolia. 


Szcrion II. 
A. Leaves equally green on both sides— 
1. Cortical Cavities large— 


a. Hard Bast well-developed— 


AS AIDS IN THE DETERMINATION OF SPECIES, 51 


A. Vessels of Wood relatively large— 


5. E. cornuta. 
6. Ki. tetraptera. 
7. KE. obliqua. 
8. E. gunnii. 
9. EK. megacarpa. 
10. E. macrorrhyncha. 
11. KE. globulus. 
B. Vessels of Wood small— 
12. K. alpina. 
13. E. viminalis. 


b. Hard Bast feebly developed— 
A. Vessels of Wood relatively large— 
14. E. leucoxylon. 
15. E. grossa. 
16. E. occidentalis. 
B. Vessels of Wood small— 
17. E. cornuta var. lehmanni. 
18. E. obcordata. 
2. Cortical Cavities small— 
a. Hard Bast well developed— 


19. KE. stuartiana. 
20. EK. melliodora. 
b. Hard Bast feebly developed— 
. 21. H. amygdalina. 
22. EK. rostrata. 
23. E. rudis. 
24, EK. tereticornis. 


B. Leaves unequally green on both sides— 
1. Cortical Cavities large— 

a. Hard Bast well developed— 
25. KE. gomphocephala. 
26. E. marginata. 

b. Hard Bast feebly developed— 
27. K. saligna. 
28. H. punctata. 


2. Cortical Cavities, small 
Hard Bast feebly developed— 

29, KE. corynocalyx. 

30. I. diversicolor, 


or 
bo 


THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


The first and most general division is based upon the presence or absence of 
central canals. 


Then such a limited Section as I. is comparatively easily disposed of. The 
cortical cavities are either large or small. 


Section I. 
A. Cortical Cavities large— 
1. Hard Bast well developed— 
1. E. maculata. 
2. Hard Bast poorly developed— 
a. Leaves, lemon-scented, and equally green on both sides— 
2. HK. maculata, var. citriodora. 
b. Leaves unequally green on both sides— 
3. H. calophylia. 


B. Cortical Cavities small— 
4. Et. ficifolia. 


In Section II. the first division may be based upon the leaves being equally 
or unequally green on both sides. 


Section IT. 


A. Leaves equally green on both sides— 
1. Cortical Cavities large— 
a. Hard Bast well-developed— 
A. Vessels of Wood relatively large— 


(1) Section small— 
5. HE. cornuta. 
(2) Section large— 
(a) Epidermis very thick— 
6. E. tetraptera. 
(0) Epidermis thickish and wood-curve slender— 
7. EH. obliqua. 
(c) Epidermis thinner and wood-curve thicker— 
8. EK. gunnii, 
(3) Section of average size— 
(a) Section twice as broad as thick— 
9. EH. megacarpa 
(6) Wood-curve always entire, and exceedingly 
thickened— 
10, E. macrorrhyncha, 


AS AIDS IN THE DETERMINATION OF SPECIES. 53 
(c) Wood-curve almost always entire, and ordi- 
~ narily thick 


11. E. globulus. 
B. Vessels of Wood small— 


(1) Section large and epidermis of average thickness— 


12, K. alpina. 
(2) Section of average size and epidermis thin— 


13, E. viminalis. 
6, Hard Bast poorly developed— 
A. Vessels of Wood relatively large— 
(1) Section large, twice as broad as thick— 


14. EK. leucoxylon. 
(2) Section of average size— 


(a) Epidermis relatively thick— 


15. E. grossa. 
(6) Epidermis of average thickness— 


16. E. occidentalis. 
B. Vessels of wood small— 
(1) Section twice as broad as thick— 
17. EK. cornuta, var. lehmanni. 
(2) Section as broad as thick—- 
18. E. obcordata. 
2. Cortical Cavities small— 
a. Hard Bast well-developed— 


A. Epidermis relatively thin— 


19. EK, stuartiana. 
B. Epidermis of average thickness— 


20. HK. melliodora. 
b. Hard Bast feebly developed— 


A. Wood-curve excessively thick— 
21. EH. amygdalina. 
B. Vessels medium-sized— 


22. HK. rostrata. 
c, Vessels comparatively small— 


(1) Epidermis thicker— 
23. EH. rudis. 
(2) Epidermis thinner— 
24. H. tereticornis. 


Section II, B. may be further subdivided according to the size of the cortical 
cavities and the development of the hard bast. 


54 THE TRANSVERSE SECTIONS OF PETIOLES OF EUGALYPTS 


B, Leaves unequally green on both sides— 
1, Cortical Cavities large— 
a. Hard Bast well-developed— 
A, Wood-curve exceedingly thickened— 
25. EK. gomphocephala. 
B, Wood-curve slender— 
26. E. mareinata. 
b. Hard Bast feebly developed— 
A, Vessels moderately large and numerous— 
27. EK. saligna, 
B. Vessels small and few— 


28. E. punctata. 
2. Cortical Cavities small— 
a, Comparatively numerous— 
29. K. corynocalyx. 
b, Relatively few and very small— 
30. E. diversicolor. 


VIII. Srectres ComMPARED AND CoNTRASTED. 


Before instituting comparisons between different species, it seemed advisable to 
give the characters for all the species as derived from the transverse sections, and 
then one was in a position to say where resemblances might be traced. Of course it 
must be borne in mind that out of 134 recorded species, only 30 different kinds are 
here considered, so that the range is rather limited for making perfectly just 
comparisons ; still, as far as it goes, it will be useful to take a comparative view, at 
least for some of the species. 


In the ‘“ Eucalyptographia,” the affinity between certain species (and even 
probable identity) is often pointed out, and we will now select some of the more 
important of these, in order to see how far we agree with, and wherein we differ from, 
Baron von Mueller, in his views of affinity, views which are based upon other 
characters, and are the result of prolonged, and careful, and exhaustive study of this 
special group. It will facilitate this comparison if we give a brief abstract of the 
allied species. In the following table (III.) the principal affinities are classified, and 
short reference is made to each :— 


Or 
On 


AS AIDS IN THE DETERMINATION OF SPECIES. 


TABLE III. 
SPECIES AND THEIR ALLIES (Accorpine ro Baron von MUELLER). 
SPECIES. ALLIED SPECIES. REMARKS. 
1. Globulus oo oe Alpina 
Megacarpa 
| 2. Rostrata 50 O° Viminalis “Instances occur when Rostrata merges almost into 
Tereticornis Viminalis, and completely into Tereticornis. It is also 
Rudis almost linked by exceptional transit-forms with E. 
rudis.” (Dec. 4.) 
3. Viminalis cc On| Rostrata ‘EK. viminalis is closely allied as well to E. rostrata as to 
Stuartiana E. stuartiana.” (Dec. 10). 
4. Stuartiana .. a Gunnii 
Viminalis 
| 
5. Ficifolia ae SI Calophylla 
6. Maculata ae Sl Citriodora “Citriodora can only be considered a variety differing 
merely in the exquisite lemon-scent of its leaves.” 
(Dec. 3.) 
7. Cornuta 20 O06 Lehmani ‘Specifically inseparable.”’ (Dec. 9.) 
8. Occidentalis .. an Cornuta ‘«The lines of demarcation between these three are not 
Obcordata always very clear.” (Dec. 6.) 


1. As regards E. globulus and E. alpina, it is stated E. alpina ‘stands to that 
species in nearest systematic affinity’ (Decade 2), and E. megacarpa likewise ‘‘ bears in 
some respects alliance to E. globulus” (Dec. 6). If the sections are compared there is 
a suggestion of resemblance between these three species, but in alpina the smaller 
vessels and more numerous cortical cavities distinguish it, while in megacarpa the 
cortical cavities are generally smaller. In both the comparatively few crystals contrast 
with the large number in E. globulus. 


2. Again, it is said of E. rostrata and E. tereticornis that “both might be regarded 
as forms of one species” (Dec. 9), and of E. rostrata and E. rudis that they are “also 
almost linked by exceptional transit-forms” (Dec. 4). It is further stated, ‘‘ On the 
whole this is one of the most easily recognised of all species; still instances occur 
when it merges almost into E. viminalis, and completely into E. tereticornis” 
(Dec. 4). 


On referring to the preceding scheme of arrangement it will be seen that rostrata, 
rudis, and tereticornis are grouped together, but viminalis does not seem to be very 
closely allied. On comparing the sections it is found that they exhibit resemblance 
in the following order :—Rostrata, tereticornis, rudis. 


It is likewise interesting to note that both E. rostrata and E. tereticornis have 
their leaves sometimes devoured by the same insect (Dec. 9). 


When rostrata and tereticornis are compared as regards the minute structure of 
the leaf-stalk (and it may be mentioned that the characters of each were drawn out 
quite independently), itis found that their close affinity, determined on other grounds, 
is borne out. 


56 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


Summarising the principal differences between them, as given in the ‘‘ Hucalypto- 
graphia,” and in the more recent ‘‘ Key to the System of Victorian Plants,” as well 
as those deduced from the transverse section of the petiole, they are as follows :— 


Rostrata. TERETICORNIS. 

Calyx-tube .. --| Nearly hemispherical .. go ..| Almost semi-ovate. 

Calyz-lid .. --| Hemispheric and sharp-pointed at top..| Elongate-conical—longer and blunter 
at top. 

Stamens G0 --| Outer inflexed before expansion ..; Outer straight before expansion (room 
for straightening in the longer 
calyx-lid). 

Section of Petiole— 
Crystals 60 -.| Moderately numerous .. 5¢ -.| Very numerous. 
Vessels bo --| Moderately large .. oe ce -.| Comparatively small. 


Such small differences completely justify teveticornis being regarded as merely 
a variety of rostrata, but the latter, being the most cosmopolitan of all the Eucalypts 
as far as Australia is concerned, might be expected to have undergone some 
modification of structure in order to adapt it to its wider environment. 


3. E. vinunalis is said to be closely allied to E. stuartiana as well as to E. 
rostrata (Dec. 10). The thicker epidermis of LE. rostrata, the generally smaller 
cortical cavities, the feebly developed hard bast, and the relatively larger vessels 
distinguish it. Stwartiana agrees, on the other hand, generally in the thinness of 
the epidermis, the development of the hard bast, and the small size of the vessels, 
but the cortical cavities are much smaller. 


4. When stuartiana and gunn are compared, the differences are clearly 
marked. In gunn the thicker epidermis, the larger cortical cavities, and the wider 
vessels form a contrast, but in the development of the hard bast, and the thickness 
and curving of the wood, there is general agreement. 


5. Ficifolia and calophylla are nearly allied, and it is said of the latter that it is 
‘the only species to which LE. ficifolia bears very close alliance” (Dec. 7). 


The sections reveal a very close general agreement indeed, the presence of two 
internal canals normally in each, showing this. Calophylla has a much thicker wood- 
pattern, and large and numerous cortical cavities, while in ficifolia they are very few 
and very small, but the greater size of the former tree, as compared with the latter, 
might account for this difference. 


6. Maculata and citriodora may be considered here, since both possess the 
internal canals. It is stated that ‘“citriodora can only be considered a variety of 
maculata, differing merely in the exquisite lemon-scent of its leaves” (Dec. 3). And 


AS AIDS IN THE DETERMINATION OF SPECIES. 57 


it is a striking corroboration of this that a study of the two sections leads to the 
same conclusion. Further, there is a remarkable resemblance between the relations of 
the sections of maculata and citriodora, and calophylla and ficifolia. There is the 
similar stout and slender wood-pattern respectively in both, although the cortical 
cavities are about equally numerous and equally large in maculata and citriodora. In 
ficifolia it would appear that the stunted habit of the tree had rendered large and 
numerous cortical cavities less necessary, and so they have dwindled down in size and 
numbers, whereas the variety of maculata has lost nothing of its stateliness. Such 
are some of the affinities which have been noted by Baron von Mueller, and which 
are borne out as well by the transverse sections of petioles. Let us turn now to some 
others which do not agree with our sections. 


The affinities of E. viminalis have already been discussed. 


7. E. lehmanni is said to be “ specifically inseparable from E. cornuta” (Dec. 
9), but a glance at the two sections would not suggest it. There is resemblance in 
the large and numerous cortical cavities, and in the much broken wood-pattern, but the 
vessels in cornuta are much larger and more numerous, and the wood-curve is consider- 
ably thicker. Altogether, the resemblances in the sections would not justify their being 
classed together as the same species, or the one as a variety of the other. 


How are we to regard a discrepancy of this sort? Are we to regard the deep- 
seated characters of the leaf-stalk as delusive ? External resemblances and allied 
internal anatomy do not always go together, for there may be fundamental difference, 
accompanied by superficial resemblance, just as there may be fundamental resemblance 
with superficial difference. We consider that the relationship may still hold between 
E. cornuta and E. lehmanni, the latter being a variety of the former, even in spite of 
seeming contradiction from the section, when it is remembered what aberrant and 
extreme forms are assumed by some species, and the extent of their variability. 
That this applies here will now be shown. In arranging our sections independently of 
external characters in the first instance, E. occidentalis was placed next to E. 
lehmannt, which naturally formed the last term of the present series. The section 
of the petiole of E. occidentalis exhibits a wood-pattern of such an irregular nature 
that it is difficult to say what it resembles exactly, and yet it is suggestive of 
resemblance to a number of forms. It is, in short, just such a form of section as 
might easily develop into several of the others, and so we were unable to correlate it 
with any. In considering the affinities of E. occidentalis in the “ Kucalyptographia ”’ 
(Dec. 6), much light is thrown on the present difficulty. 


First of all, we are informed that E. cornuta, E. obcordata, and E. occidentalis 
““seem to be the only three entitled to specific rank in the series of cornuta or 
orthostemoneae, and even the lines of demarcation between these three are not always 


58 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


very clear.” So this brings E. occidentalis into some sort of affinity with E. cornuta, 
and, by implication, with its variety, E. lehmanni. When the section of the latter is 
compared with E. occidentalis, there is undoubtedly a certain resemblance, but not 
directly, with E. cornuta. 


Again, it is found from extended observation and increased material, that E. 
occidentalis runs more or less into at least six named species (not reckoning two 
varieties of E. cornuta), viz. :— 


E. spathulata, Hook. 

E. macrandra, F.v. M. 
E.. cornuta, Labillardiére. 
E. obcordata, Turez. 

E. redunca, Schauer. 

. pachypoda, F.v. M. 


ty 


And the inference is that E. occidentalis is capable of and subject to a vast 
amount of variability. 


Nay, further, in the concluding sentence of the notice of this form, it is stated 
“ . occidentalis, in its scope as here considered, seems so variable as to change much 
of former ideas as regards the precincts of Eucalyptus-species, a similar playfulness 
of forms having been observed by me in FE. stricta and E. incrassata, the characters of 
shrubby Eucalypts proving generally less constant than those of the tall timber-trees 
of this genus” (Dee. 6). 


In such a sentence as that there is contained the essence of a volume on the 
“Origin of Species.’’ And when we consider that at least three species—E. glauca, 
E. pulverulenta, and E. perfoliata—have been based upon the young state of E. 
globulus (Dec. 6), it is not to be wondered at, but rather to be expected, that in such 
a variable genus of plants there would be striking resemblance in internal structure, 
as well as a certain amount of diversity. 


IX.—Conciupine REMARKS. 


If transverse sections of the petioles can be used as an important aid in the 
determination of species, then it is evident that this test may be applied where there 
is doubt as to specific identity. 


AS AIDS IN THE DETERMINATION OF SPECIES. 59 


Thus there is a remarkable resemblance, for instance, between the sections of 
the petioles of E. calophylla and E. ficifolia, and the question arises—Are they to be 
regarded as distinct species or not ? 


The principal differences between LF. ficifolia and £. calophylla, as given by 
Baron von Mueller in his “‘ Eucalyptographia”’ (Dec. 7), are as follows :— 


E. ficifolia. 
Tree.—Of less height. 
Bark.—Somewhat more deeply furrowed. 
Leaves.—Proportionately not quite so broad, but longer. 
Flowers.—Mostly larger. 
Calyces.—Assume a reddish hue. 
Fruits.—Less turgid. 
Seeds.—Much paler in colour, have a smaller kernel, and are provided with con- 
Spicuous appendicular membranes. 


If the leading specific differences of the same authority be compared, it will be 
found that the crimson filament and the pale seeds, with a long membrane, of E. fici- 
folia ave the principal offsets against the pale-yellowish, rarely pink filaments, and 
dark membraneless seeds of E. calophylla. 


Here the differences are comparatively small, but the characters, such as they 
are, being permanent, are considered sufficient to fix this as a distinct species. 


If we turn to the characters revealed by the petiole, the same remark applies. 


The broad differences separating ficifolia from calophylla are :— 


Slightly thicker epidermis, with a strong development of hypoderm, although 
there are indications of something similar to the latter in calophylla. 

Cortical Cavities.—Much fewer and smaller. 

Central Canals.—Smaller. 

Vessels.—About the same size, slightly larger, but weaker development of 
wood. 


Such permanent differences probably entitle E. ficifolia to specific rank, but it 
will be observed that the differences are just such as might arise from the same kind 
of tree, from any cause, becoming dwarfed and stunted in growth. 


Both belong to the furrowed bark series (Schizophloiz), have anthers opening by 
parallel slits (Parallelantherz), and pollen-grains of the same size. The fruits in both 
are urn-shaped, and their habitat is confined to Western Australia. 


60 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


To take just another striking example. £. citriodora is regarded on general 
erounds as a variety of E. maculata, and from the transverse sections of the petioles 
of both the same conclusion might be drawn. It is a suggestive fact that the 
resemblances and differences are mainly of a parallel kind with those of E. ficifolia 
and E. calophylla. But the differences are evidently less in degree, or rather the 
resemblances are closer, for they generally agree in thickness of epidermis, size, and 
number of cortical cavities, and size of central canals. But the vessels are about 
twice the size of those of maculata, while the wood itself is relatively much more 
feebly developed. 


On the whole the study of the transverse sections of petioles of well-developed 
and fully-formed leaves of Eucalypts has led us to the following conclusions :— 


1. Fresh species may be identified by means of such sections, combined with 
external characters of the leaf. The aggregate characters of the section are employed 
but chiefly those derived from the following parts:—Epidermis, hard bast, wood with 
its vessels, cortical cavities, and central canals. 


2. Herbarium material, by appropriate treatment, may likewise be used. 
3. The size and shape of the transverse section is often characteristic. 


4. The relative thinness or thickness of the epidermis is a more or less 
constant feature, and it is often indicative of the habitat of a plant, say of a desert 
species. 


5. The number, size, and arrangement of cortical cavities are very variable, but 
their relatively large size in some species is such a striking feature that it may be 
used for purposes of discrimination. 


6. The central canals are so decided and distinct, and occur in such a limited 
number (at least of thirty-two species and varieties examined), that they might con- 
veniently be used as a diagnostic character for a section of the Kucalypts. 


7. Crystals are always present, more or less, but they form too precarious a 
feature to be relied upon. 


8. The hard bast, whether dense or scanty, seems to be generally characteristic. 


9. The wood-curve is likewise a characteristic feature, with the relative number, 
size, and arrangement of vessels; but in some few instances it is too variable to be 
much relied on. 


10. The broken nature of the wood-curve, as found in some species, cannot be 
used as a distinctive character, like the invariably unbroken curve in others, because on 
fuller investigation unbroken curves are found in all. 


AS AIDS IN THE DETERMINATION OF SPECIES. 61 


11. The closeness of resemblance in the sections of two allied reputed species 
may lead to their being recognised merely as varieties; or, on the other hand, the 
differences between reputed varieties may be sufficiently great to suggest their 
distinction as species. 


12. Lastly, the general agreement among the various sections, and the absence of 
those clear distinctions which would mark off each species if quite independent, tend 
to the conclusion that the varied species of Eucalypts may have arisen through a 
process of evolution. After allowing for the changes which may have taken place 
through possible hybridisation, as hinted at in the “ Kucalyptographia”’ (Dec. 9), 
‘extreme forms,” ‘“ aberrant forms,’ and “transition forms,” so frequently referred 
to in that work, are not thereby accounted for. While the mere existence of 
transition forms does not prove that the transit has been accomplished through 
descent with modification, still permanent varieties or species, with such forms 
flanking them on every side as would be regarded as distinct species if isolated, would 
seem to have arisen thus. Hence the proper study of the Eucalypts, like that of the 
Platypus and Ceratodus, may add another page to Australia’s contribution to the 
evolution theory. But perhaps it is hardly necessary to formally state this conclusion 
in the face of the recent utterance at the Newcastle meeting of the British 
Association, 1889, by the distinguished President (Prof. Flower) :—‘ I think I may 
safely premise that few, if any, original workers at any branch of biology appear 
now to entertain serious doubt about the general truth of the doctrine that all 
existing forms of life have been derived from other forms, by a natural process of 
descent with modification.” 


Since this investigation is strictly comparative, we have endeavoured to preserve 
as much uniformity as possible, both in the sections made and the language used, 


Besides, we felt that an important principle was being tested here, and one 
which might receive a wider application, viz., that in many families of plants the 
intimate structure of the leaf-stalk might be made a means or an aid in the 
identification of species. Therefore it was necessary to select a sufficiently varied 
number of examples, as well as a fair proportion of the entire number of known 
species on which to base our conclusions. It will be conceded, we think, that the 
Eucalyptus formed a sufficiently critical genus to test, and that the number of species 
(30), forming nearly one-fourth of the whole, was fairly extensive. According to the 
latest ‘‘Census” by Baron von Mueller, the number of Australian species of Eucalypts 
is 184. Whatever conclusions may be drawn, the photographed sections, and the 
accurate outlines, particularly of the wood, ought to be a decided addition to our 
knowledge of this characteristic and peculiar form of Australian vegetation. 


62 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 


EXPLANATION OF PLATES. 


REFERENCE LETTERS TO ALL THE FIGURES. 


b. bast. 

ce. cuticle. 

cc. central canals. 

ce. cavity of epidermal cell. 
cp. cortical parenchyma. 
er. crystals. 

ct. cortex. 

ctc. cortical cavity. 

cw. cuticularised cell-wall. 
e. epidermis. 

h. hypoderma. 

hb. hard bast. 

k. kinoid substance. 

p. pith. 

sb. soft bast. 

sp. sieve plates. 

st. sieve tubes. 

vw. vessels of wood. 

w. wood. 

we. wood curve. 


PLATE 1. 


Fig. 1. Epidermal cells of 2. globulus, shortly after treatment with Schulze’s solution, showing also hypoderma (h) 
(x 114). 
Fig. la. Single epidermal cell of samc, with underlying cells (x 600). 
Fig. 2. Cortex of EZ. globulus, showing a cortical cavity (x 114). 
Fig. 2a. Cortical cells adjoining hard bast (x 114). 
3. Crystal in cortical cells of L. ficifolia (x 140). 
4, Cortical parenchyma bordering on hard bast, in vertical section (x 600) 
Fig. 5. Hard bast and adjoining tissue in vertical section (x 600). 
6. Cambiform cells of soft bast, in vertical section—comparatively elongated and thin-walled (x 600). 
Fig. 6a. Cambiform cells, from round to brick-shaped—the commonest form (x 600). 
7. Soft bast in vertical section, showing sieve-plates (sp) on radial side-walls (x 600). 
Fig. 8. Transverse section of base of midrib of young sessile leaf, to show not only structure of midrib, as far as the 
wood-curve is concerned, but mainly for comparison with section of petiole of mature leaf. 
Fig. 8a. Natural size of section. 
Fig. 9. Transverse section of quadrangular stem of young H. globulus for comparison with that of petiole. 
Fig. 9a. Natural size of section represented in Fig. 9. 
Fig. 10. Transverse section of stem of young EZ. calophylla for comparison with that of F. globulus. 
Fig. 10a. Natural size of section represented in Fig. 10. 


Norr.—All the preceding drawings belong to H. globulus, except Figs. 3 and 10. 


In Plates 6, Ga inclusive, the natural size of the section of each petiole is shown beside the enlarged section, and thus 
the amount of enlargement throughout is seen at a glance. 


Fig. 22a, 
Fig. 23. 


Fig. 23a. 
Fig. 24. 


Fig. 25. 


Fig. 26. 


AS AIDS IN THE DETERMINATION OF SPECIES. 


PLATE 2. 
E. occidentalis—Transverse section of petiole. 
(Glycerine jelly). 
E. cornuta— do. do. 
(Balsam). 


FE. cornita, var. lehmanni—Transverse section of petiole. 
(Glycerine jelly). 


E. obcordata— do. do. 
(Glycerine jelly). 

FE. marginata— do. do. 
(Glycerine jelly). 

E. diversicolor— do. do. 


(Glycerine jelly). 


PLATE 3. 


E. gomphocephala—Transverse section of petiole. 
(Glycerine jelly). 


E. megacarpa— do. do. 
(Glycerine jelly). 

EE. tetraptera— do. do. 
(Balsam). 

EL. rudis— do. do. 
(Glycerine jelly). 

E. grossa-— do. do. 


(Glycerine jelly). 
EB. calophylla— do. do. 
(Glycerine jelly and iron stain). 


PLATE 4. 
E. calophylla—Transverse section of petiole. 
(Balsam). 
E. ficifolia— do. do. 


(Glycerine jelly, nitric acid, and iron stain). 
E. ficifolia—Transverse section of petiole. 


E. alpina— do. do. 
(Glycerine jelly). 
E. punctata— do. do. 


(Glycerine jelly). 


E. maculata, var. citriodora—Transyerse section of the petiole. 
(Glycerine jelly and iron stain). 


PLATE 5. 


63 


E. maculata, var. citriodora—Transyerse section of another petiole, showing abnormal number of Central Canals 


(Glycerine jelly). 


I. corynocalyx—Transyerse section of petiole. 
(Glycerine jelly). 


E. melliodora— do. do. 
(Glycerine jelly). 

E. tereticornis— do. do 
(Glycerine jelly). 

E, saligna— do. do 
(Glycerine jelly). 

E. maculata— do. do. 


(Glycerine jelly 


64 THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS. 


PLATE 6. 
Fig. 32. EH. macrorrhyncha—Transverse section of petiole. 
(Balsam). 
Fig. 33. E. globulus— do. do. 
(Glycerine jelly and iron stain). 
Fig. 33a. E. globulus—Transverse section of petiole. 
(Glycerine jelly). 
Fig. 34. EH. obliqua— do. do. 
(Balsam), 
Fig. 35. E. amygdalina— do. do. 
(Glycerine jelly). 
Fig. 36. E. viminalis— do. do. 


(Glycerine jelly). 


PLATE 6a. 

Fig. 36a. E. viminalis—Transverse section of petiole. 

(Glycerine jelly). 
Fig. 37. EH. gunnii— do. do. 

(Balsam). 
Fig. 38. LE. stuartiana— do. do. 

(Glycerine jelly). 
Fig. 39. E. leucoxylon— do. do. 

(Glycerine jelly). 


Fig. 39a, b,c. E. lewcoxrylon—Outlines of three sections from different petioles, invariably showing broken wood-curve. 


Fig. 40. E. rostrata—Transverse section of petiole. 
(Glycerine jelly). 


Trans. PLS. Victoria Plate. |. 


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latency 0 repeats 
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On tHE Victor1aAN Lanp Puanarians, spy AntHuR Denpy, M.Sc., F.L.S., Demon- 
STRATOR AND AssisTANT LicturER In Bronogy aNnD FELLOW oF QUEEN’S 


CoLLEGE IN THE University or MELBouRNE. 


(With Plate 7.) 


(Read May 8th, 1890.) 


INTRODUCTION. 


The present paper may be regarded as a sequel to my memoir on the Anatomy 
of an Australian Land Planarian, already published in the Transactions of this 
Society.* Having fully described, in the memoir referred to, the anatomy of one 
species, which may be taken as a type of the whole group, it remains to name, 
briefly describe, and where possible figure the other Victorian species. 


There are, as I have pointed out in my previous memoir, two genera of 
Australian land Planarians, Geoflana, with many small eyes, and Rhynchodemus, 
with only two larger ones. Both of these genera are found in Victoria and it would 
doubtless have been desirable to have described in detail the anatomy of a type from 
each ; as, however, I have only seen a single specimen of Rhynchodemus, and that 
only recently, I have been unable as yet to do this. The gap thus caused is, however, 
to a great extent filled by the researches principally of Moseley and von Kennel, to 
which frequent reference is made in my earlier paper. 


In their ‘‘ Notes on Australian Land Planarians, with Descriptions of Some New 
Species ” (Part I.),+ Messrs. Fletcher and Hamilton enumerate eighteen Australian 
and Tasmanian species. Of these, seventeen were found in New South Wales, one 
in New South Wales and Queensland, one in New South Wales and Victoria, and one 
in Tasmania only. In the present paper I propose to describe fifteen Victorian 
species, Viz.: 

. Geoplana cerulea, Moseley sp. 
. quinquelineata, Fletcher and Hamilton. 
. munda, Fletcher and Hamilton. 
. Spenceri, Dendy. 
. ad@, X. sp. 
. lucasi, n. sp. 


SR YE 
QAAHRAO 


* Transactions of the Royal Society of Victoria, 1889. 
+ Proceedings of the Linnean Society of New South Wales, Vol. II. (Series 2), p. 349. 


66 ON THE VICTORIAN LAND PLANARIANS. 


7. G. m‘mahont, n. sp. 

8. G. alba, n. sp. 

9. G. hoggi, n. sp. 
10. G. sugdeni, n. sp. 
11. G. mediolineata, n. sp. 
12. G. quadrangulata, n, sp. 
13. G. walhalle, n. sp. 


14. G. fletcheri, n. sp. 
15. Rhynchodemus victoria, un. sp. 


Of these fifteen species the first three occur also in New South Wales and have 
been already described by Moseley and Fletcher and Hamilton. The twelve 
remaining species are, so far as is yet known, exclusively Victorian, but it is more 
than probable that some of them will sooner or later be discovered in one or other 
of the adjacent colonies. Still it is evident, when we consider that out of twenty- 
nine known Australian species, nearly equally divided between the colonies of 
Victoria and New South Wales, only three have been found in both colonies, that 
the land Planarians, however widely they may be distributed as a class, do not enjoy 
wide specific areas of distribution; or, in other words, that in different districts of 
the same country we may expect to find different species of Planarians. In spite of 
the occurrence of one or two comparatively widely ranging species, such as Geoplana 
alba, which I have had from M‘Mahon’s Creek, Warragul, Macedon, and Croajin- 
golong, this expectation is justified by my own observations. 


With regard to the question of specific distinctions I have come to the conclusion 
that we may safely rely on a combination of the following characters (1) the colour 
and pattern, (2) the position of the external apertures, (3) the general shape of the 
body. Although I have examined considerable numbers of the same species, as, for 
example, in the case of Geoplana spenceri and G. hoggii, I have not found any 
important variations in these respects. Perhaps the most variable species are the 
common yellow Planarians which I have named Geoplana sugdeni and G. mediolineata. 
These two species agree fairly well in the general shape of the body and in the 
position of the external apertures, but the former has none of the stripes present in 
the latter. ‘The two species are, however, connected by an intermediate variety with 
imperfect stripes. Under these circumstances I have assigned all specimens with 
any stripes at all to G. mediolineata and all those without any to G. sugdent. It 
must, however, be remembered that although in G. mediolineata the number of 
stripes may vary yet the arrangement is always identical, and this is the important 
point. In the most perfectly striped examples which I have seen we find a single, 
fine, dark median stripe, a lighter stripe at some distance on each side of it, and 
outside this again on each side an indication of a stripe at the anterior extremity of 


ON THE VICTORIAN LAND PLANARIANS. 67 


the body only (Figs. 3, 8a), All these stripes may be more or less suppressed, the 
first to disappear being those on the outside and the last the one in the middle; or 
we may with equal justice assume that the parent form had no stripes and that the 
first to appear was the median one and the last the outside ones. The observations 
of Fletcher and Hamilton on the markings of very young specimens of Geoplana 
quinquelineata, which will be found quoted in the description of that species, seem to 
indicate that the latter assumption is the correct one. So it is in most of the species; 
the markings, if there are any, may be more or less strongly emphasised in different 
individual specimens, but fundamentally the pattern is the same in all. I have 
pointed out* the same fact in the case of Peripatus leuckartii. 


We now know a good deal about the general habits of land Planarians. They 
are What I have elsewhere+ termed ‘‘ Cryptozoic” animals, living for the most part 
under logs and stones, or the dead bark of trees. They prefer moderately damp 
situations and appear to be much more abundant in the autumn, after rains, than in 
the drought of summer. When at rest in their hiding places they commonly lie 
coiled up with the anterior extremity in the centre of the coil (Fig. 12). Asa rule 
they seem to venture abroad in search of food at night only, or in very damp weather, 
but I have more than once found Geoplana sugdeni crawling about in broad daylight, 
once on a stone near the top of Mount Macedon, in a decidedly dry situation. 
Geoplana lucasi, again, was obtained by Professor Spencer at a height of 4000 feet 
on the top of the coast ranges in the Croajingolong district. 


Still there can be no doubt that land Planarians require a very considerable 
amount of moisture for their existence. Thus I once found a considerable number 
of specimens which had escaped from the collecting box dried up on the floor of a 
room, having apparently exhausted all their supply of moisture in the production of 
their slimy track. 


In this connection I may mention that when a living land Planarian is placed 
in loose dry earth, it forms a cyst for itself by cementing together the particles of 
earth with its slimy secretion. Within this cyst the Planarian lies completely 
hidden, but if the cyst be torn it will crawl out perfectly clean and free from earth. 
This habit of forming cysts of earth may be a protection against drying up and may 
perhaps account for the disappearance of land Planarians in the heat of summer. 


Land Planarians crawl with an even, gliding motion, which I believe to be 
largely due to the action of the numerous strong cilia on the ventral surface, for I 
have seen a minute fragment of the worm, snipped off with a pair of scissors, 
gliding away over a smooth surface by itself, much as in the case of detached parts 


* Proceedings of the Royal Society of Victoria ; 1889, p. 50, et seq. 
} Victorian Naturalist; December, 1889. 


68 ON THE VICTORIAN LAND PLANARIANS, 


of the common mussel described by McAlpine.* Cilia are probably present on the 
dorsal surface also, but very small and much obscured by slime. In crawling the 
horseshoe-shaped anterior extremity of the body, on which the eyes are mostly 
situate and which has usually more or less of a reddish tinge, is uplifted to gain a 
more extended view, and the path of the animal is marked, like that of a snail, by a 
slimy track. 


They live upon the juices of insects and other small animals, which they extract 
by suction, the sucker-like pharynx being inserted in some soft part of the victim 
and the latter held fast by the intensely sticky slime secreted around it by its 
captor. Mr. C. Frost informs me that on one occasion when out collecting he placed 
a living land Planarian in a box with a live Cicada and that when he opened the box 
again to show the Cicada to a friend he found the insect quite flat and empty, all the 
inside having been sucked out by the Planarian. Hence the land Planarians are 
certainly carnivorous and they must be able to find an abundant supply of food 
amongst the innumerable cockroaches, beetles and other small animals which make 
up so large a proportion of the cryptozoic fauna. 


Land Planarians are found breeding in the autumn and winter months and I 
have been able to observe the method of copulation in Geoplana mediolineata, at 
Upper Macedon on April 7th of the present year. The two individuals were 
precisely similar in colour and markings and of about the same size. 


They were lying beneath a log in such a manner that the posterior portions of 
théir ventral surfaces were applied together, the tail of the one pointing in the 
opposite direction to that of the other. The genital atrium in each case was 
expanded to form a sucker and the two suckers being applied together held the 
worms in position. The orifices of both male and female copulatory organs were in 
each case somewhat protruded and it follows from the position of the animals that 
the male opening of the one must come into close contact with the female opening of 
the other and vice versé. The most important factor in bringing this about is the 
use of the common genital atrium as a sucker, in the hollow of which lie the male 
and female openings. . Thus the method of action of the copulatory organs, 
whose minute anatomy I have described in the case of Geoplana spenceri, 1s 
made clear. 


The eggs are laid in cocoons, several in each. I was fortunate enough to obtain 
recently a specimen of Geopflana hoggii with a cocoon in the uterus, which proves 
clearly that the cocoon is an internal structure and not, as in the case of the earth- 
worm, an external structure formed by the skin. In the case observed the body of 


* Transactions and Proceedings of the Royal Society of Victoria, Vol. XXIV., Part 2, p. 139. 


ON THE VICTORIAN LAND PLANARIANS, 69 


the worm was seen to be greatly distended just behind the genital opening, and 
sections showed the presence of a fully formed cocoon occupying the whole of the 
ereatly dilated uterus, and squeezing the other internal organs to one side. The 
cocoon itself was crowded with closely packed yolk-cells, whose nuclei and outlines 
were still visible. In older cocoons the yolk disappears as the embryos increase in 
size until at last the young worms come to occupy the whole of the cavity. Finally 
the young escape through simple rupture of the wall of the cocoon or through a 
definite circular opening. After having been laid for some time the cocoon appears 
as an oval or nearly spherical body of a shining black appearance. In the specimen 
which contained the cocoon in utero the yolk glands were, as might have been 
expected, very largely developed, and there was some evidence in support of the 
suggestion which I made in my previous memoir to the effect that the shell of the 
cocoon is secreted by certain glands opening into the small chamber which receives 
the contents of the united oviducts before they enter the uterus. To this chamber I 
therefore propose to apply the name “ shell-gland chamber.” 


The brilliancy of colour and markings in the land Planarians are so well known 
that I need scarcely do more than allude to them. Blue, green, yellow, brown, black 
and red may be found in various combinations and generally arranged in longitudinal 
bands or stripes symmetrically disposed on the two sides of the body. It is difficult 
to account for these varied and brilliant markings, which seem, as I have already 
pointed out, to be tolerably constant for each species. Wallace proposes* to divide 
the colours of animals into four groups which he terms Protective, Warning, Sexual 
and Typical. I would suggest that the brilliant colours of land Planarians may be 
“warning” colours. There are many butterflies which have been shown by Wallace 
to be brilliantly coloured and at the same time inedible by birds and there is good 
reason for believing that the brilliant colours serve to warn the birds of the 
objectionable character of the butterflies and thus protect the latter from being 
pecked to death. In the same way I think it possible, though not as yet by any 
means proved, that the colours of Planarians may serve to protect them from being 
eaten by birds by rendering them readily recognisable. 


But it requires to be shown first that land Planarians are inedible by or 
distasteful to birds. I have made two experiments which seem to indicate that this 
is the case ; (1) I tasted two species myself and found that the mere application of 
the tongue to the slimy surface of the animal was sufficient to produce an exceedingly 
unpleasant sensation, something like that caused by putting a piece of velvet ora 
lump of alum in the mouth. (2) I threw a living specimen of Geoplana spenceri to a 
number of hens. The hens, not being native birds, would, of course, not recognise 
the worm, and they at once attacked it, broke it up and took it in their mouths. 


* «Tropical Nature, and other Essays,” p. 172. 


70 ON THE VICTORIAN LAND PLANARIANS. 


Instead, however, of swallowing the pieces they dropped them again. This 
experiment, though but a solitary one and of course in need of confirmation, tends 
to show that land Planarians are unpalatable to birds as well as to human beings. 


In my paper on the anatomy of Geoplana spenceri I have already suggested that 
the unpalatable character of these worms may be due to the presence of the rod-like 
bodies in the slime with which they are always covered. 


In concluding my introductory remarks I have much pleasure in expressing my 
indebtedness to my wife for her valuable assistance in collecting specimens; to 
Professor W. Baldwin Spencer for numerous Planarians from various localities and 
especially for an exceptionally interesting collection from Croajingolong, including a 
species of Rhynchodemus, which genus is now for the first time recorded from 
Victoria; to Mr. H. R. Hogg, for many specimens of Planarians from Macedon and 
for his kind hospitality and assistance whilst I was collecting in that district; to 
Mr. J. Bracebridge Wilson, for Planarians from the Otway Forest, and to Mr. Henry 
Dendy, of Walhalla, for assistance in collecting in that locality. 


DESCRIPTION OF VICTORIAN SPECIES. 
Genus Geoplana. 


This genus, as I have already had occasion to point out, is distinguished from 
the only other known genus o¢ Australian land Planarians by the presence of 
very numerous minute, unicellular eyes, which occur principally on the lateral 
margins of the anterior end of the body and are usually, if not always, continued 
round the edge of the horseshoe-shaped anterior extremity. Frequently, also, the 
eyes occur more sparsely scattered along the sides of the body to the extreme 
posterior end. 


1. Geoplana cerulea, Moseley sp. 


1877. Ccnoplana cerulea, Moseley, Quarterly Journal of Microscopical 
Science, Vol. XVII., N.S., p. 285. 


1887. Geoplana cerulea, Fletcher and Hamilton, Proceedings of the 
Linnean Society of New South Wales. Series II., Vol. 2, p. 361, 
Pls, Higa ds 


“Entire body of a dark Prussian blue colour, somewhat lighter on the under 
surface of the body and with a single, narrow, mesial, dorsal, longitudinal stripe of 


ON THE VICTORIAN LAND PLANARIANS. (fal 


white. Length 5 em., extreme breadth 4 mm., mouth central; generative aperture 
8mm., posterior to the mouth. Parramatta, near Sydney. Under the bark of a 
species of Eucalyptus.” (Moseley, /oc. cit.) 


A number of specimens brought in spirits by Professor Spencer from Croajin- 
golong appear to belong to this species. According to Professor Spencer the colour 
of the living worms was cobalt on the ventral and dark olive green on the dorsal 
surface, exactly as in G. spenceri but with a median, dorsal, yellow line. The spirit 
specimens still show very plainly the narrow median dorsal line, and they also show 
indications of a narrow, median, ventral light line in the posterior part of the body, 
apparently not observed in the living animals. They also still exhibit traces of a 
reddish anterior tip. 


According to Messrs. Fletcher and Hamilton (Joc. cit.) there appears to be a 
certain amount of variation in the colouration of this species. Thus these authors 
have found specimens without any red tip and with the dorsal median stripe varying 
from a dirty white to a distinct yellow, changing to white in spirit. These obser- 
vations make it probable that the Croajingolong specimens are correctly identified as 
G. cerulea, though the opening into the peripharyngeal chamber appears to be a 
little further back than Moseley places it. In shape this Planarian closely resembles 
Geoplana spencert. 


Localities —Sydney, Parramatta, Ryde, Springwood, Mount Wilson, Hunter 
River (New South Wales); Cairns (N. Queensland) ; Croajingolong (Victoria). 


2. Geoplana quinquelineata, Fletcher and Hamilton. 


1887. Geoplana quinquelineata, Fletcher and Hamilton, Proceedings of the 
Linnean Society of New South Wales. Series II., Vol. 2, p. 366, 
Pl. V., Figs. 4, 5, 15, 16. 


‘Under surface whitish. Ground colour above presents considerable variations, 
pale yellow or nearly orange, dull olive-green, ochreous-brown, reddish-brown, 
sometimes almost brick-red. The dorsal surface divided into six longitudinal bands 
by five longitudinal lines, also varying in colour, sometimes a darker and more 
intense tint of the ground-colour, from dark brown almost black to warm brown or 
red, their margins irregular when viewed with a lens, arranged as follows: usually a 
very fine dark line occupies the median line, external to which on each side is a 
narrow band of ground colour ; outside of which again on either side is a line of 
brown or red usually slightly broader and better defined than the mesial line; each 


72 ON THE VICTORIAN LAND PLANARIANS. 

of these again is bordered by a band of ground colour one and a-half times or twice 
as wide as the inner stripe on each side; beyond each of which is the outermost 
brown or red line of the same width as the first on each side but sometimes narrower, 
and each of these is followed by a narrow band of ground colour extending outwards 
to the lateral margin of the body. At the anterior extremity the lines blend in the 
red tip. The ground colour, and the reddish tint of the anterior extremity usually 


disappear more or less completely in spirit, while the bands become brown or 
sometimes black. 


Largest living specimen 10 cm. long. In two contracted spirit specimens 42 
and 23 mm. long respectively, the apertures of the mouth are 20 and 12 mm. 
respectively behind the anterior extremity; in a third specimen 26 mm. long the 


genital orifice is 4 mm. anterior to the hinder extremity. In none of our specimens 
are both apertures visible. 


Young specimens on emerging from the cocoon are 2.5 to 4 mm. long. In 
these and sometimes in larger ones the colour of the anterior portion of the body is 
more intense. In very young specimens also the lines are brighter, but the 


outermost one on each side is only faintly indicated, or absent.’’ (Fletcher and 
Hamilton, /oc. cit.) 


Messrs. Fletcher and Hamilton state that this is one of the commonest species 
in New South Wales, and they also record it from Sandhurst, Victoria. I myself 
collected four specimens near Sandhurst, all of which were found under stones on an 
old gold-field near the Back Creek Cemetery. The ground colour of the dorsal 
surface was, in the living worms, brownish yellow. The five dark lines were placed 
nearly equidistant from one another, running all down the body. All five were 
rather thin, the middle one black and the others chestnut brown. The ventral 
surface was greyish cream coloured. 


I have also received two specimens from the Otway Forest, sent to me in spirit 
by Mr. J. Bracebridge Wilson. The latter are very large, the largest measuring 
60 mm. in length and 5 mm. in breadth even in spirit. 


Localtties.—Near Parramatta, near Springwood, near Capertee, Guntawang, 


Beaudesert Hills, Biraganbil Hills (New South Wales); Sandhurst, Otway Forest 
(Victoria). 


ON THE VICTORIAN LAND PLANARIANS. 73 


3. Geoplana munda, Fletcher and Hamilton. 


1887. Geoplana munda, Fletcher and Hamilton, Proceedings of the Linnean 
Society of New South Wales. Series II., Vol. 2, p. 369, Pl. V., Fig. 8. 


‘‘Undersurface greyish in centre, yellowish towards the margins. Above 
there is a narrow median dorsal line of pale olive brown, bounded on either side by 
a very fine dark line, external to which is a broader band of a slightly darker brown, 
and this is bordered externally by a very dark brown line which gradually merges 
into a rather broad band of very dark brown which fades gradually towards its outer 
margin. 


“‘This pretty little Planarian retains its colours in spirit very well but the under- 
surface becomes quite white. The single specimen obtained measured when alive 
and crawling, 2°5 cm. long, and 3mm. broad. In spirit it measures 15 mm. long, 
4mm. broad, the mouth 6 mm. behind the anterior extremity, and the generative 
aperture 2 mm. behind the mouth.” (Fletcher and Hamilton, Joc. cit.) 


As I have not seen this species in the living condition I quote the above 
description of Fletcher and Hamilton. Mr. J. Bracebridge Wilson sent me sixteen 
specimens in spirits, from the Otway Forest, which agree excellently with the above 
account, but I could not find the genital aperture. The species was described by 
Fletcher and Hamilton from a single specimen. 


Localities —Hartley Vale (New South Wales) ; Otway Forest (Victoria). 


4. Geoplana spenceri, Dendy. 


1889. Geoplana spenceri, Dendy, Transactions of the Royal Society of 
Victoria. Volo. Part, p50; Piss 7, 8; 9) 40: 


For the description and figures of this species I must refer the reader to my 
former paper. 


Localities —M‘Mahon’s Creek, Warburton, Walhalla (Victoria). 


5. Geoplana ade, n. sp. (Fig. 7). 


The body is nearly oval in section, flattened ventrally, tapering rather more 
oradually in front than behind. ‘The opening into the peripharyngeal chamber is 


74 ON THE VICTORIAN LAND PLANARIANS. 


situate in about the middle or a little behind the middle of the ventral surface. The 
eround colour of the dorsal surface is pale yellowish brown. ‘There is one very fine, 
median, dark brown stripe, and a very broad lateral dark brown stripe on each side of 
it and separated from it by a fairly wide interval of ground colour. The lateral 
stripes are rather ill-defined at their outer edges, where they touch a band of the 
ground colour splotched with darker brown. The ventral surface is pale yellowish 
brown, slightly mottled, or white. The largest of the three specimens which I have 
seen was about 40 mm. in length and 3 mm. in greatest breadth when crawling. 


I have called this beautiful Planarian after my wife, who has greatly assisted me 
in my search for cryptozoic animals. 


Localities —Macedon, Warburton (Victoria). 


6. Geoplana lucasi, n. sp. 


The body (in spirit) is very broad and much flattened, especially on the ventral 
surface ; very blunt behind and tapering more gradually in front. The opening into 
the peripharyngeal chamber is rather behind the middle of the ventral surface and 
the genital aperture about halfway between it and the posterior end of the body. 
The dorsal surface, in the living animal, was of a creamy white colour, with a narrow 
dark brown median stripe and on each side of the stripe numerous close-set, narrow, 
discontinuous, wavy longitudinal streaks of brown over all the remainder of the dorsal 
surface. There is no record of any markings on the ventral surface of the 
living animal. 


I received three specimens of this worm in spirit from Professor Spencer, from 
Croajingolong. The largest measures (in spirit) about 40 mm. in length and 8 mm. 
in greatest breadth, and came from a height of 4000 feet on the top of the coast 
ranges. I have named the species after Mr. A. H. S. Lucas, M.A., B.Sc. 


Locality.—Croajingolong (Victoria). 


7. Geoplana m‘mahont, n. sp. 


Body (in spirit) strongly convex on the dorsal surface, flattened on the ventral, 
tapering gradually towards the anterior end and much more suddenly towards the 
posterior. Opening into the peripharyngeal chamber situate at about the junction of 
the middle and posterior thirds of the body. Genital aperture nearer to the posterior 


ON THE VICTORIAN LAND PLANARIANS. 75 


end than to the opening of the peripharyngeal chamber. The ground colour of the 
dorsal surface is yellow (pale or bright) and there are two strong brown stripes, one 
on each side of the middle line, separated by a considerable interval and meeting at 
the anterior and posterior ends. The ventral surface is cream-coloured. A specimen 
in spirit measured 23 mm. in length and 4:5 mm. in greatest breadth. 


Locality —M‘Mahon’s Creek, on the Upper Yarra (Victoria). 


8. Geoplana alba, n. sp. (Figs. 10, 11). 


Body broad and much flattened, strap-shaped; when at rest often crenated at the 
edges, the crenations disappearing when the animal is fully extended; sub-triangular 
in transverse section, the apex of the triangle with a very wide angle; tapering 
very gradually in front and unusually suddenly behind, so that the hinder end of 
the body is blunt, especially when the animal is at rest or in spirit. The opening of 
the peripharyngeal chamber is near the junction of the middle and posterior thirds of 
the body and the genital opening nearer to it than to the hinder end of the body. 
There are no stripes and except for the pinkish anterior tip the entire body is of a 
very pale and nearly uniform tint. Ihave noted specimens from M‘Mahon’s Creek 
as “cream-coloured or white’ and specimens from Macedon as ‘ peach-coloured or 
yellow flesh”’ and “brownish flesh-coloured all over, dorsally and ventrally, with 
beautiful peach-coloured tip.’ Specimens from Macedon measured when crawling 
about 65 mm. in length and 4 mm. in greatest breadth, but I have larger specimens 
from M‘Mahon’s Creek and from Warragul. 


Localities—M‘Mahon’s Creek, Warragul, Macedon, Croajingolong (Victoria). 


9. Geoplana hoggit, n. sp. (Figs. 4, 5.) 


Body almost elliptical in section but flattened beneath, long and narrow, tapering 
gradually towards the anterior extremity and more suddenly towards the posterior. 
Opening into the peripharyngeal chamber nearly in the middle of the ventral surface 
and genital aperture about one-third of the distance between it and the posterior end 
of the body. The ground colour of the dorsal surface is rather pale, translucent 
yellow, or greenish yellow. There are four stripes, two on each side of the middle 
line and extending throughout the entire length of the body. The two stripes 
nearest the middle line are separated from one another by only a very narrow band 
of ground colour and are usually of a green colour with a tinge of indigo; they may, 


76 ON THE VICTORIAN LAND PLANARIANS. 


however, be grey or greenish grey. The two remaining stripes, one on each side, 
are separated by wider intervals from those nearest to the middle line and are of a 
very dark brown, almost black colour. The relative breadth of the stripes appears to 
vary a good deal. The anterior extremity of the body is of the usual brownish pink 
colour, into which the stripes merge. The ventral surface is of a uniform yellow 
colour, a little paler than the ground colour of the dorsal surface. The largest 
specimen which I have seen alive was about 125 mm. long and 5 mm. in greatest 
breadth when crawling (Fig. 5). Usually, however, specimens are only about 70 or 
80 mm. long when crawling. 


I have seen great numbers of this species under logs and stones at Macedon and 
I have great pleasure in calling it after Mr. H. R. Hoge, on whose property it is 
particularly abundant and who first brought it to me in a living condition. 


Locality.—Macedon (Victoria). 


10. Geoplana sugdent, n. sp. (Figs. 12, 13, 14). 


Body very narrow and much elongated; approximately oval in section but 
somewhat flattened ventrally, more nearly cylindrical than in any other species of 
the genus with which I am acquainted; tapering gradually to each extremity. 
Opening into the peripharyngeal chamber a little in front of the middle of the 
ventral surface. Genital opening only a little behind the middle, separated from the 
opening into the peripharyngeal chamber by an interval of about 10 mm. (in spirit) 
and from the posterior end of the body by an interval of about 18mm. The colour 
of the dorsal surface is bright canary yellow all over except the reddish brown 
anterior tip; the ventral surface is of a paler yellow colour. There are no stripes 
at all. Length when crawling about 70 mm., greatest breadth only about 2 mm. 


This species is rather remarkable for its habit of wandering about in broad 
daylight, to which I have already referred in my introductory remarks. I have much 
pleasure in naming it after the Rev. E. H. Sugden, B.A., B.Sc., the Master of 
Queen’s College in the University of Melbourne. 


Locality.—Macedon (Victoria). 


11. Geoplana mediolineata, un. sp. (Figs. 1, 2, 3, 3a). 


Body long and narrow, oval in section but not very much flattened; tapering 
very gradually towards the anterior and more suddenly towards the posterior end. 


ON THE VICTORIAN LAND PLANARIANS. 77 


Opening into the peripharyngeal chamber somewhat in front of the middle of the 
ventral surface. Genital opening at about the junction of the middle and posterior 
thirds of the body. The ground colour of the dorsal surface is bright canary yellow. 
The stripes vary considerably in the extent to which they are developed. The most 
typical condition appears to be that represented in Figs. 1 and 2. Here there is a 
single, narrow, very dark brown or almost black, median dorsal stripe. At the 
anterior end the brownish-pink tip is continued into two short, dusky brown stripes 
on each side of the middle line; the one nearest the middle line being the longest. 
At the posterior end also an ill-defined dusky stripe seems to be always present on 
each side of the middle line. Specimens with stripes answering to the above 
description are very abundant at Macedon. In a slight variety from Warburton and 
Walhalla, of which I obtained six or seven specimens, the stripes are less developed, 
even the median one being present only at the anterior end of the body, though 
longer than the others. In a third variety, on the other hand, from Macedon, there 
are three continuous stripes (Figs. 3, 3a), the innermost of the two lateral stripes on 
each side extending all the way down the body and becoming continuous at the 
posterior end with the rudimentary lateral stripes mentioned as existing there in the 
typical form. The ventral surface is pale, nearly white. When crawling, examples 
of this species are about 90 mm. in length and hardly 3 mm. in greatest breadth. 


Localities —Macedon, Warburton, Walhalla (Victoria). 


12. Geoplana quadrangulata, n. sp. (Figs. 6, 6a). 


Body almost quadrangular in section but rounded off at the angles. Dorsal 
surface a good deal broader than the ventral and connected therewith by inwardly 
sloping lateral surfaces. Both the dorsal and ventral surfaces are flattened. The 
opening into the peripharyngeal chamber is situate a little behind the middle of 
the ventral surface, and the genital opening is about half way between it and the 
posterior end. The dorsal surface is of a dark reddish brown colour, slightly mottled, 
with a narrow median stripe of very dark brown, and a dark brown anterior tip. At 
the junction of the dorsal with the lateral surfaces there is, in two out of three of my 
specimens, a single row of small, pale spots, very distinct in spirit specimens. The 
lateral surfaces are also reddish brown, but much paler than the dorsal surface. The 
ventral surface is white, but owing to the slope of the sides of the body the latter 
appear as a brown stripe on each side of a median white band (Fig. 6a). Length 
when crawling about 27 mm., greatest breadth about 1.5 mm. 


Locality.—Macedon (Victoria). 


78 ON THE VICTORIAN LAND PLANARIANS. 


13. Geoplana walhalle, n. sp. 


This species agrees with Geoplana spenceri in shape, and in the uniform dark 
olive green colour of the dorsal surface. 'The ventral surface, however, instead of 
being blue, is of a light, speckled brown colour. The anterior tip is dark brown. 
The opening of the peripharyngeal chamber is situate near the middle of the body, 
but slightly in front, and the genital opening is about half way between it and the 
posterior end, if anything a little nearer to the posterior end. Length of two 
specimens when crawling about 37 and 50 mm. respectively. 


I found two specimens of this Planarian at Walhalla, Gippsland, Victoria, one 
crawling on the top of a stone (in the day-time), and one under a log. 


Locality.—Walhalla (Victoria). 


14. Geoplana fletcheri, n. sp. (Figs. 8, 9). 


Body much flattened ventrally, convex dorsally ; a good deal broader behind than 
in front ; tapering gradually to the anterior, and much more suddenly to the posterior 
extremity. Opening into the peripharyngeal chamber a little behind the junction of 
the iniddle and posterior thirds of the body. Genital opening somewhat nearer to the 
posterior extremity of the body than to the opening into the peripharyngeal chamber, 
and hence very near the posterior end. The ground colour of the dorsal surface is 
canary yellow, not quite so bright as in G. sugdeni, with a tendency towards the 
formation of two brown lateral stripes, continued backwards for some distance from 
the brownish pink anterior tip. In one specimen (Fig. 9), the ground colour was 
slightly mottled with brown, and, in addition to the two partial stripes already 
mentioned at the anterior end, there was a faint, narrow, median, brownish stripe 
running along the posterior half of the dorsal surface. The ventral surface is pale 
yellow. Length when crawling about 60 mm., greatest breadth about 3 mm. 


This species at first sight resembles G. sugdeni, but may be readily distinguished 
by the general shape of the body, and the position of the apertures. I have named 
the species after Mr. J. J. Fletcher, B.A., as a slight recognition of his valuable work 
on the Australian land Planarians. 


Locality.—Macedon (Victoria). 


ON THE VICTORIAN LAND PLANARIANS. 79 


Genus Rhynchodemus. 


This genus is distinguished from the preceding principally by the possession 
of only two, multicellular eyes, situate near the anterior extremity, and on the dorsal 
surface. Although apparently not uncommon in New South Wales, five species being 
described by Messrs. Fletcher and Hamilton (Joc. cit.), only a single specimen has as 
yet been found in Victoria, and that in the Croajingolong district, not very far from 
the New South Wales border. The species is, however, a new one. 


15. Rhynchodemus victoria, nu. sp. (Figs. 15, 15a). 


Body (in spirit) much flattened, especially on the ventral aspect, not tapering 
evenly to the anterior extremity but with a slightly developed neck, which seems, 
indeed, to be characteristic of the genus (vide Figs. 15, 15a). The opening into the 
peripharyngeal chamber is very distinctly margined and situate a little behind the 
middle of the ventral surface ; the genital opening is about half way between it and 
the posterior end of the body. The eyes are very near the anterior extremity (Fig. 
15, 2). Professor Spencer informs me that the principal colour of the dorsal surface 
in the living animal was French grey or “‘elephant’s breath.’ At the anterior end, on 
the dorsal surface, the following stripes are visible :—A narrow dark median stripe, 
dying out about half way down the body and edged on each side by a creamy white 
stripe of about the same width and dying out a little before the dark one. Just 
above each lateral margin of the body is another narrow creamy white stripe, soon 
dying out. The two white stripes of each side unite near the anterior extremity and 
at their point of union the eye of that side is situated (Fig 15, ¢). The ventral 
surface in the living animal was lighter grey, with a single, median, creamy white 
stripe dying out just behind the genital aperture, and a similar stripe very near the 
margin on each side also dying out towards the posterior end. Length in spirit 
about 26 mm., greatest breadth about 3 mm. 


I received a single spirit specimen of this interesting Planarian from Professor 
Spencer, who collected it at Croajingolong. Professor Spencer supplied me with the 
description of the colours of the living animal, but the arrangement of the stripes I 
was obliged to make out in the preserved specimen. 


Locality.—Croajingolong (Victoria). 


80 ON THE VICTORIAN LAND PLANARIANS. 


Derscrietion oF Puate VII. 


Figures 1, 2.—Geoplana mediolineata, n. sp. Dorsal aspect. Fully extended. 
Typical form. Painted from life; natural size. Macedon. 


Figure 8.—Geoplana mediolineata, nu. sp. Dorsal aspect. Fully extended. 
Variety with three complete stripes. Painted from life; slightly enlarged. Macedon. 


Figure 8a.—Geoplana mediolineata, n. sp. Dorsal aspect. Anterior extremity 
of the same specimen as that from which Figure 3 is taken; enlarged to show the 
arrangement of the stripes. Painted from life. 


Figures 4, 5.—Geoplana hoggii,n. sp. Dorsal aspect. Fully extended. Painted 
from life; natural size. Macedon. 


Figure 6.—Geoplana quadrangulata, nu. sp. Dorsal aspect. Fully extended. 
Painted from life ; twice the natural size. Macedon. 


Figure 6a.—Geoplana quadrangulata, n. sp. Ventral aspect. Not quite fully 
extended. O, opening of peripharyngeal chamber ; g.a., genital aperture. Painted 
from life ; twice the natural size (same specimen as in Fig. 6), 


Figure 7.—Geoplana ade, n. sp. Dorsal aspect. Fully extended. Painted from 
life; natural size. Macedon. 


Figure 8.—Geoplana fletcheri, n. sp. Dorsal aspect. Pretty fully extended. 
Painted from life ; slightly enlarged. Macedon. 


Figure 9.—Geoplana fletcheri, n. sp. Slight variety. Dorsal aspect. Fully 
extended. Painted from life; one and a half times the natural size. Macedon. 


Figures 10, 11.—Geoplana alba, n. sp. Two specimens. Dorsal aspect. Pretty 
fully extended. Painted from life. Natural size. Macedon. 


Fieures 12, 18, 14.—Geoplana sugdeni, n. sp. Dorsal aspect. Figure 12 
represents the worm at rest, coiled up with its anterior end in the middle, slightly 
enlarged. Figure 13, partly extended, natural size. Figure 14, fully extended, 
natural size. Painted from life from three specimens. Macedon. 


Figure 15.—Rhynchodemus victorie, n. sp. Dorsal aspect; e, eye. Drawn from 
a spirit specimen, twice the natural size. Croajingolong. 


Figure 15a.—Rhynchodemus victorie, nu. sp. Ventral aspect of the same 
specimen as represented in Figure 15. O, opening into the peripharyngeal chamber; 
g.a., genital aperture. 


Fig | 


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Trans. Royal Society, lictorta 1890 Plate 7 


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ARTICLE III.—Tur Evcatyrets or Grppsuanp, sy A. W. Howrrt, F.G.S., F.L.S. 
(With Plates 8, 9, 10, 11, 12, 18, 14, 15, K(S)\s 


(Read Thursday, July 10th, 1890). 


CONTENTS. 


I.—Inrropuction .. a ee Be ec . ao 83 
Il.—Vanrertes or Typrs—GENERA Ee Be a 35 D0 84 
III.-—Distrinution or Typzs .. ie 26 Ss a ac 104 
4A.—As To AREAS... Se aa Ase se aie 104 

B.—In Autirupr Apove Sea Lrven es on ee np 107 

C.—As to GronocicaL Formation ee da 50 a 108 
TV.—Inrnvence or Crimate anp GEoLoGicAL ForMATIOoN ON THE DisrripuTion or Typrs 108 
V.—InFuvence or SerrnemMmNnt oN THE Eucanyprus Forrsts .. He oc 109 


LIST OF EUCALYPTS OF GIPPSLAND. 


RENANTHERA— PoRANTHERA— ORTHANTHERE— 
EK. pauciflora. EK. leucoxylon. K. pulverulenta. 
K. stellulata. K. melliodora. K. stuartiana. 
K. amygdalina. EK. polyanthema. EK. viminalis. 
E. piperita. KK. odorata. K. tereticornis. 
K. eugenioides. EK. hemiphloia (albens). _E. gunnii. 
EK. muelleriana. K. botryoides. 
E. capitellata. EK. goniocalyx. 
K. macrorhyncha. K. globulus. 
EK. obliqua. 
K. stricta. 


I 


sieberiana. 


D 
blo 


THE EUCALYPTS OF GIPPSLAND. 


TABLE OF BOTANICAL, ABORIGINAL* AND LOCAL NAMES OF THE GIPPSLAND RUCALYPTS. 


| E. paucitlora 30 | Bundagra aD 36 | Mountain White Gum. 
| E. stellulata ue | Yimbit | Black Sally, Muzzlewood. 
Ei. amygdalina Chunchuka | Peppermint Gum. 
3 (Gi) Katakatak or Yertchuk .. 
» (e) Wang-ngarat 
E. piperita | Yangura White Stringy- bark. | 
E. obliqua Katakatak | Messmate. 
Ii. capitellata Dumung Mountain or Red Stringy-bark. 
i. muelleriana Yangura Yellow Stringy-bark. 
E. macrorhyncha Katakatak or Yurokat Mountain Stringy-bark. 
TPES) {White ron-batl, Wooly But, | 
E. leucoxylon Yirik or Bwurawi Tron-bark. | 
KE. melliodora Dargan | Yellow Box. | 
| E. polyanthema Den or Dern | Red Box. 
E. odorata. . Dargan | Yellow or Grey Box. 
E. hemiphloia Den or Dern Grey Box. 
KE. pulverulenta Bindirk Silver Leaf Stringy-bark. 
E. stuartiana But-But | Apple Tree or Apple Box. 
E, yviminalis (a) Binak | White Gum. 
| * (vb) Cabbage Gum. 
Ii. tereticornis Yuro.. Red Gum. 
E. gunnii .. Gura-Binak Swamp Gum. 
E. botryoides Binak Snowy R. Mahogany. 
E. goniocalyx Baluk Spotted or Bastard Gum. 
| E. globulus Baluk or Wang-ngarat} . Blue Gum. 
I. eugenioides Yangura | White Stringy-bark. 


* The majority of these native names are taken from the Muk-thang dialect. Muk-thang. or “excellent speech,” 
was spoken by the Brabolung Kurnai, who lived on the Mitchell, Nicholson, and ‘'ambo Rivers. 


+ Wang-ngara, in the Nulit dialect, spoken by the Brataua and Tatung, who dwelt between the Lakes and the 
sea, and in South Gippsland; wang means “bark,” and ngara “‘a string” or ‘‘ tough,” hence ngarang ‘“‘a sinew.” The 
application of such a term seems more appropriate to KE. amygdalina than to E. globulus, for the bark of the former is 
extremely tough, and can be detached from the bole in long strips. The bark of E. globulus is not so tough, but at times 
hangs from the tree in long strings, in reference to which, perhaps, the name is given. 


+ Yuroka was the name given by the Krauatun Kurnai, who lived at the Snowy River and spoke Thang quai, or 


“broad speech,” to the mountain stringy bark, E. macrorhyncha. 


Tur Evucarypts or Grepsuanp, By A. W. Howitt, F.G.S., F.L.58. 


INTRODUCTION, 


So much has already been done by Baron von Mueller towards bringing into 
order the numerous varieties of the recorded Eucalypts, that it only remains to work 
out their local distributions, as well as the effects produced by soil and climate. This 
attempt I have now made as regards the Gippsland Eucalypts. 


The difficulties which have met me in this enquiry have been greater than I at 
first anticipated, as it has necessitated a series of investigations, spread over a 
number of years, and covering the greater part of Gippsland. Even now, after 
examining the whole of the district more or less carefully, I find that in order to 
complete my work with even a fair degree of accuracy, it would be necessary to again 
visit certain localities, my earlier observations of which are wanting in that minute 
examination which later investigations have shown to be absolutely necessary. I am 
unable to revisit the localities referred to, and have therefore confined my remarks 
more especially to Central and West Gippsland, touching the North-eastern part very 
lightly, and scarcely referring to Kast Gippsland at all. 


I regret that this should have been unavoidable, for it is in the country between 
the Snowy River and Cape Howe, and south of the coast range, that one would most 
probably find that the New South Wales species meet and mingle with those most 
general in Gippsland, 


It is my pleasing duty to thank Baron von Mueller most heartily for the unending 
kindness with which he has, throughout the course of my enquiries, responded to 
my constant requests for information, for the readiness with which he has 
examined and named the collections which I forwarded to him, and thus resolved 
difficulties which I met with, and for most kindly making available to me the 
specimens in his museum. I am much indebted for the kindness with which Mr. 
Luehmann has given me his valuable aid in comparing my samples with those of the 
departmental herbarium, with which he is so fully acquainted. 


To Dr. Wools I am under great obligations for valuable information as to New 
South Wales species, and for samples of the same. 


84 THE EUCALYPTS OF GIPPSLAND. 


Also to My. J. E. Brown, F.L.S., of Adelaide, to whom I addressed myself for 
information as to South Australian species. 


Mr. John O’Rourke, of Woolgulmerang, Mr. David O’Rourke, of Buchan, and 
Mr. 8. C. Holme, of Eagle Vale, have all most kindly made collections of the Eucalypts 
srowing in their respective neighbourhoods. 


Typrs oF KUCALYPTS GROWING IN GIPPSLAND. 


RENANTHERE.—In the following notes on the Types of Hucalypts in Gippsland, I 
have endeavoured to avoid repetition of the descriptions which have been 
given by Baron von Mueller with such admirable clearness and precision in 
the “ Eucalyptographia,” and desire only to add such particulars as have 
presented themselves to me, or have special reference to the local occurrence 
of these Eucalypts in Gippsland. 


E. pauciflora.—This Euealypt is extremely constant in character, whether 
found in small isolated colonies in the littoral tracts, as at Providence Ponds and 
Morwell, or forming forests over large areas in the Gippsland Alps up to an elevation 
of 5000ft., as on the Wonnongatta Plains, at Omeo, Woolgulmerang, and Delegate. 


It appears to be essentially an Alpine species, yet able to maintain itself, to 
some extent, in localities but little elevated above sea level. 


E. stellulata—This is also an Alpine species, ascending almost if not quite to 
the same elevation as E. pauciflora, but does not descend, according to my observa- 
tions, lower than 7OOft. at Dargo and Ensay. No varieties occur, as far as my 
observations go. 


E. amygdalina.—This is one of the most variable, and at the same time, 
naturally most widely spread of the Gippsland Eucalypts. 


I have observed the following well-marked and constant varieties :— 


(a). The ordinary narrow-leaved variety.—This is the type described and figured 
in the ‘Eucalyptographia;” it generally grows throughout this district on all formations, 
trom the sea level up to about 4500ft. 


(b). The broad-leaved variety. In the mountains, and more especially in some 
of the Plutonic and Metamorphic areas, as at Dargo and the Wentworth and Omeo, 
there occurs a form of Amygdalina which is to some extent distinct from the typical 
form referred to. I have not observed it at a lower elevation than 700ft. at Dargo, 


THE EUCALYPTS OF GIPPSLAND. 85 


and it grows upon Mount Livingstone at about 8000ft., which is, probably, near its 
upper limit. According to my observation it does not exceed 100ft. in height, and is 
more frequently under 50ft. Its bark is wrinkled, approaching to fibrous, and 
persists up to the smaller branches. 


The seedlings and young saplings have opposed sessile lanceolar leaves, which 
are, however, much broader than the ordinary form, approaching at times pointed 
ovate. 


The leaves when scattered are broadly foliate and unequal-sided. The umbels, 
buds, and flowers are those of the typical form, but the fruit is much larger, and 
almost always ovate top-shaped, with a flat or slightly convex margin, and a brown 
or brownish-red tint. The valves, as in the ordinary form, are sinall. 


However much this tree resembles the ordinary form of this Eucalypt, it is 
clearly to be distinguished from it, because the two varieties very commonly grow 
together, each maintaining its own character. 


In other places they may be found forming independent colonies. While the 
common variety grows especially in the damp gullies and on the shady sides of the 
ranges from the sea level up to about 4000ft., this form of Amygdalina (4) grows 
preferably upon the sunny slopes from 7O0Uft. to 4000ft. (See Pl. 8.) 


(c.) This variety is restricted to barren sand ridges of the littoral tracts, for 
instance, in South Gippsland, between Merriman’s Creek and Warrigal Creek, 
together with Banksia serrata, Acacia oxycedrus, and other sand-hill vegetation. It 
does not exceed 30ft. in height, and has a marked drooping habit in its branches and 
foliage, while the bark is wrinkled and persistent up to the small branchlets. 
The form of the leaves distinguishes it from variety (a), for they are long and narrow 
lanceolar or falcate, the venation is so little spreading as to resemble in some respects 
that of KE. pauciflora or E. stellulata; the flowers and fruit are typical of E. 
amygdalina, to which I have assigned the tree. (See Pl. 10, Figs. 6 to 12.) 


(d.) This is the most widely-spread variety of E. amygdalina, and at the same 
time that which departs most from the typical form. It grows most freely upon the 
rather poor sandy and clay lands of the littoral tracts, but I have also observed it in 
the mountains, for instance, where poor sandy tracts occur, as well as on the quartz 
grits and conglomerates at Wild-horse Creek, Wentworth River, on the Upper Silurian 
sediments, between Toongabbie and Walhalla, the Silurian sediment in the Tambo 
Valley Road, the Upper Devonian formations of the Insolvent Track, the Devonian 
porphyries at Gelantipy, and the Silurian formations at Delegate River. 


It rarely grows more than 100ft. in height, but is generally a rather small tree, 
often stunted. The bark classes it with the stringy barks, for it is fibrous and 


86 THE EUCALYPTS OF GIPPSLAND. 


persistent up to the smaller branches, somewhat resembling that of E. obliqua, but 
thinner, more fissile, and lighter in colour. For roofing purposes the bark is worth- 
less, and the timber of no value for splitting or sawing, having the soft, veiny 
character of some types of Amygdalina. 


The seedlings have opposed, narrow, lanceolar leaves, with, occasionally, tufts of 
hairs and frequently wavy margins. 


The opposed character of the leaves is not maintained beyond the first two or 
three pairs, and the leaves then become ovate lanceolar, resembling in their pointed 
and unequal-sided form those of E. obliqua, though rarely as large. They are thick 
in consistence, of a dull green, and not shiny ; in the Jatter trait resembling those of 
HK. sieberiana. 


The umbels have numerous buds, with the typical form of E. amygdalina, 
to which also the shape of the calyx tube, the short style, and depressed lid belong. 
The fruit is ovate top-shaped, with a flat and slightly convex margin and small deltoid 
valves. 


The tree is found at a height of 100ft. above sea level at Merriman’s Creek and 
the Bairnsdale to Buchan-road, to 2500ft. at the Upper Wentworth River. I have not 
observed it on the mountain plateaux, even where they descend to the latter height, 
and conclude that it is a littoral species which ascends the coast ranges. (See Pl. 9.) 


(e.) This is the Wang-ngara* of the Gippsland blacks. It is found in the 
eastern part of Gippsland, but, according to my observations, not so commonly as 
the other varieties of this type. It grows along the rivers and streams, and in moist 
valleys, where it takes the place of EK. viminalis (a). It has a smooth, tall, but 
comparatively slender bole, with a scanty, often rather spreading, head, in which there 
is frequently a marked absence of foliage. The bark is persistent, and wrinkled only 
on the lower part of the bole, above which it becomes smooth and almost white. It 
is of extreme toughness, whence the aboriginal name, 


The seedlings and young saplings have sessile, rather long, lanceolar, opposed 
leaves, resembling those of the normal Amygdalina, but which in the older trees 
become narrow lanceolar-falcate, attenuated at the stalk and pointed. The venation 
is rather indistinct, the marginal vein considerably removed, and the lateral veins 
very longitudinal. 


The umbels are on stalks as long or longer than the bud and stalklet, the stalklet 
slender and longer than the bud, the lid small and depressed, with a slight point. 


* This native name has a reference to the extreme toughness of the bark of this tree. Wang—a band; ngara is 


connected with ngarang—a sinew. 


THE EUCALYPTS OF GIPPSLAND. 87 


Buds numerous, 3 to 20. Flowers normal. Fruit, ovate truncate, with slightly 
contracted orifice, compressed rather narrow rim, and small weak valves. 


Compared with samples, for which I am indebted to Dr. Wools, of Sydney, this 
appears to be the White River gum of New South Wales, Eucalyptus radiata 
(amygdalina). This seems to be one of those eastern forms of vegetation which are not 
found any further to the westward than the Mitchell River, though this tree 
individually does not extend beyond the Tambo River. 


I have observed it at an elevation of 50ft. at Jimmie’s Point backwater, 200ft. at 
the Tambo crossing, 300ft. at the Murrendel River, and at Wangrabell on the Genoa 
in Kast Gippsland, at an elevation, judging from memory, of not more than 500ft. 
(See Pl. 10, Figs. 1 to 5.) 


(f) (or E. regnans).—This Eucalypt, though possessing a specific title, belongs to 
K. amygdalina, and is less removed from the typical form than the varieties which I 
have designated (d) and (e). Under its common name of black-butt it is found in 
the western part of Gippsland on the Mesozoic carbonaceous formations, where it 
especially flourishes. It reaches 300ft. in height, and according to the statements of 
some observers* to 400ft. and above that height. 


The young seedlings of this Eucalypt are at first like those of the typical 
Amygdalina, but with somewhat broader, lanceolar, opposed leaves. These are soon 
replaced by broadly lanceolar, scattered, unequal-sided, pointed leaves, very like those 
of E. obliqua. The saplings so much resemble those of this Eucalypt in other 
respects that at first sight they might be confused. The leaves of saplings of E. 
regnans, however, are thinner in texture, rather lighter in tint, not so pointed nor 
quite so unequal-sided as in E. obliqua. 


The flowers and fruit connect this tree with E. amygdalina, and do not differ 
from the typical form more than do those of the varieties (d) and (e). 


It occurs over a wide area in South and Western Gippsland, chiefly on the 
carbonaceous formations, together with E. obliqua, and E. globulus, from the sea 
level up to about 1200ft. It is also found in the mountains, as at Walhalla, 1200ft., 
and at Tucker Creek, Wentworth River, 2500ft. 


E. piperita and E. eugenioides.—In accordance with the list of typical Eucalypts, 
given at p. 81, I should now describe E. piperita and eugenioides in sequence, 
but it will be more convenient to speak of these together, since their near alliance 
renders it necessary to point out the distinctions which may be drawn between them. 

Eucalypts referable to these types grow more or less plentifully throughout the 
whole of Gippsland, ascending from the sea level to 3000ft. above it. 


* Amongst others Mr. J. Rollo, formerly a sawmiller at Yarragon. 


88 THE EUCALYPTS OF GIPPSLAND. 


In the “‘Kucalyptographia’’ Baron vonMueller says, in speaking of H. eugenioides, 
that the distinctions between E. piperita and H. eugenioides are not yet clearly made 
out, and that, perhaps, Bentham’s view, that both should be regarded as forms of one 
species, may have to be adopted.* And, in referring to EH. Piperita he describes 
its fruit as truncate or globular ovate, contracted at the narrow-edged orifice, with 
valves perfectly enclosed. 


This description accurately fits the sample from New South Wales, which, by the 
courtesy of Baron von Muelier, I was enabled to examine in the collection of the 
Department of Botany of Victoria. But it does not apply so aptly to the fruit of 
E. piperita as Ihave found it in Gippsland. Occasionally I have met with examples 
of this Eucalypt with truncate-ovate narrow-rimmed fruit, as, for instance, at the 
Tambo River; but the general form of the fruit, especially in the western part of thé 
district, is extremely variable, as will be seen from the following particulars. 


In order to study the possible differences which might exist between E. piperita 
and EK. eugenioides, I collected 26 samples from various parts of Gippsland, and 
compared the fruit as one of the readiest means of reaching some definite conclusion ; 
for I had already found that a diagnosis, based upon the general characteristics of the 
aged trees, saplings, seedlings of the umbels, buds and flowers, led to no definite 
result, except to raise very strong doubts as to the distinctions between the so-called 
separate species being maintainable. Of the 26 samples, 3 had truncate-ovate 
fruit, 16 truncate-globular, and 7 truncate-spheroidal. 


In 10 examples the rim was sharp, and in 16 blunt, but the bluntuess of the rim 
was not always associated with a much-truncated form of fruit and a wide orifice; and 
in several cases I noticed on the same tree two forms of fruit, one truncate-ovate, 
with a comparatively narrow sharp rim, and another which was much truncated and 
more globular, and with a wide orifice. 


The samples which I thus examined were, six from the country east of Bairns- 
dale, seven from the neighbourhood of Toongabbie, and the remainder from isolated 
places throughout the district, from the coast line to an elevation of 30U0ft., at the 
sources of the Wentworth River. 


If any conclusion is justified from these comparisons, I should say it is that the 
greater number of samples having a truncate globular fruit, with a contracted aperture, 
and a narrow sharp rim, are to be found in Eastern Gippsland, while those few, which, 
in their much truncated fruit, with wider, blunt rims, and wider apertures, may be 
assigned to Hugenioides, occur in the western parts, as, for instance, at Drouin and 
the Agnes River. 


* Eucalyptographia Tenth Decade. 


THE EUCALYPTS OF GIPPSLAND. 89 


It is in Western Gippsland, namely, near Drouin and at the Agnes River, 
that I found those samples which were most near to the typical forms of KH. eugenioides, 
and in which the valves were distinct, but yet only slightly exserted. 


The conclusion to which I am led is that the suggestion thrown out by 
Bentham, and noted by Baron von Mueller, is correct so far as concerns Gippsland, 
namely, that E. piperita and HK. eugenioides are near varieties of the same type. 
But when comparing the extreme forms found in South-western Gippsland with the 
typical E. piperita from New South Wales, to which the examples from near the 
Tambo River must be assigned, the conclusion is arrived at that the differences are 
such as to have justified Dr. Wools in regarding E. piperita and HK. eugenioides, 
as they occur in New South Wales, as distinct. 


An examination also of numerous individual trees in different localities where 
these Eucalypts flourish as one of the principal forest trees, for imstance, at 
Merriman’s Creek, Toongabbie, the Macalister River, Budgee Budgee, the Went- 
worth, and the Tambo, has shown me that in all these localities trees can be found 
growing side by side, having fruit which is either truncate ovate-globular with a narrow 
aperture, or compressed globular, much truncated, and with a wider aperture. The 
seedlings and saplings growing in such localities, with the aged trees bearmg such 
fruits as above referred to, are indistinguishable from each other, and I have come to 
the conclusion that, so far as concerns Gippsland, possibly excepting perhaps its 
extreme eastern part, there are no strong features to separate these EKucalypts into 
Piperita and Eugenioides. If, however, samples are compared of the New South 
Wales Piperita with the Gippsland samples, which agree with the definition of 
Eugenioides, then it will be found that there are good and distinctive characteristics. 


I have felt some difficulty in deciding to which type the Gippsland form should 
be assigned, but on consideration I think that, in the majority of cases, the form of 
the fruit and the seedings with ovate-crimped leaves, point to E. piperita rather than 
E. eugenioides (*). I have, therefore, assigned them to that species, though there 
are a few localities such as the Agnes River and at Drouin, where Kucalypts occur, 
which can rightly be referred to H. eugenioides. 


E. muelleriana.—This Eucalypt has an extensive range in the western half of 
Gippsland. It is a littoral species, and is principally found between the Hoddle 
Ranges and the sea coast. There it forms the bulk of the forest, growing upon sands 
and sandy clays, from Monkey Creek, 20 miles from Sale, to Shady Creek, west of 
Alberton, in an east and west direction, and from Carrajung southwards to the coast. 
The area thus covered by this tree is about 300 square miles. It also occurs in lesser 


* The seedlings of the New South Wales variety, for which I have to thank the courtesy of Dr. Wools, bear out 
this view. 


90 THE EUCALYPTS OF GIPPSLAND. 


colonies on the ridges extending from the Tertiary tracts up to the high ranges forming 
the spurs of the mountains. I have not observed it west of Toongabbie, where it ascends 
the hills of Upper Silurian sediment for about 6 miles northwards to 1000ft.in elevation. 
I have also seen it growing extensively on the hills across which the road, known as the 
Insolvent Track, runs from the Stockyard to Cobannah Creek. ‘The formations here 
are Upper Devonian, resting upon sediments which may be either Devonian or Upper 
Silurian. Its range north and south in this locality is at least 25 miles, and its 
highest elevation probably over 1200ft. I have noted a third locality where this tree 
occurs under precisely similar conditions, extending northwards on the spurs of the 
mountains, skirted by the Tambo Valley-road. ‘There it grows for several miles on 
the Silurian sediments, northwards from the edge of the tertiary marine beds, and 
reaches an elevation of at least 1000ft. I have little doubt that it will be found in the 
intervening localities, and perhaps further to the eastward; but of this I have no 
direct evidence. 


It appears to grow to the largest size on the sands and sandy clays of South Gippsland, 
where it forms most valuable forests. Its maximum height is 170ft. or thereabouts, 
but more frequently 100ft. to 150ft. The bole is straight and rather massive, with mode- 
rately spreading branches, and a fibrous and dark-grey bark, which is more deeply and 
coarsely fissured than that of E. piperita, in fact, resembling the bark of E. capitellata, 
where that species grows to a good size in favourable localities. The bark is 
persistent up to the small boughs, which are more or less smooth. The leaves of the 
aged trees are lanceolar, falcate, and more or less inequal-sided, rather dark green in 
colour, equally shining on both sides, and usually three to five times as long as broad, 
with a sharp apex. 


The seedlings have narrow lanceolar opposed leaves of a dark green, shining but 
paler on the under side. In the earlier stages they are frequently more or less beset 
with small tufts of hairs. I have noticed that the leaves are still opposed in young 
plants 2ft. to 3ft. in height. In young saplings, and those some feet in height, the 
leaves are rather broad lanceolar, or ovate lanceolar in shape, less shiny on the lower 
page, much dotted with transparent pores, and rather thin in substance. A marked 
feature in the saplings of this Kucalypt, and one by which it can be distinguished 
almost at a glance from those of other stringybarks, is that the broadly lanceolar and 
pointed leaves have a tendency to assume a horizontal position, rather than a vertical 
one, and this gives the saplings a shining appearance. ‘The stems of these saplings 
and young trees are somewhat smoother than those of K. piperita, E. capitellata, or 
K. macrorhyncha. 


The umbels are usually solitary, and there is a marked tendency in this Eucalypt 
for them to become strongly panniculated. The buds are from 3 to 12 in most 
of the umbels. The stalk is frequently slightly flattened, and not much longer than 


THE EUCALYPTS OF GIPPSLAND. 91 


the buds, and the stalket nearly as long as the calyx tube, the lid semi-ovate to 
hemispheric, smooth and occasionally slightly pointed, the stamens (rather sparse) are 
large and reniform like those of EH. capitellata. Fruit almost hemispherical to 
approaching semi-ovate, the rim flat or even slightly inverted, not wide, valves deltoid, 
small, and inserted, or more rarely slightly prominent; four-valved, less frequently 
three to five valved. 


The timber of this tree is usually rather darker in tint than that of E. piperita. 
It is fissile, free from gum veins or shakes, clear in the grain, and enjoying a great 
reputation for durability. It is used for fencing and sawing, and, according to Mr. 
Macalpine, of Tarraville, who has lived for 40 years in South Gippsland, fences are 
still standing at Woranga with posts split from this Eucalypt, which have been from 
30 to 40 years in the ground. I have myself observed posts of this timber standing 
in fences at Woodside since 1859. The local name of this tree is ‘‘ yellow stringy- 
bark.” 


This Kuealypt, therefore, is to be placed between E. eugenioides and E. capitel- 
lata. It resembles both, but the dissimilarities are more marked than the resemblances. 
The characteristic distinctions are quite as constant as those which distinguish those 
two species, and the occurrence of these species over so large an area, as well as in 
independent lesser colonies, negatives the probability of its being a mere hybrid. The 
distinctions which I have now noted as separating this Eucalypt from its nearest 
congeners are such as to have led me early in my enquiry to regard it as a species 
distinct from either. I hesitated, however, to definitely state this until I had an 
opportunity of comparing my samples with those in the collection of the Government 
Botanist. Having been enabled to do this through the courtesy of Baron von Mueller, 
and having been most kindly aided in the comparison by Mr. Luehmann, I feel that, 
being fortified by the opinion of our greatest authority, the venerable author of 
_“« Euealyptographia,” I may establish this Hucalypt as an independent species under 
the designation of Eucalyptus muelleriana. 


E. capitellata.—This tree occurs in small colonies, scattered over a great part of 
Gippsland. It cannot, strictly speaking, be called one of the littoral species, for I 
have not seen it growing at a lower elevation than 500ft., as at Drouin West, 75Uft. 
at Darlimurla, and above that elevation between Bruthen and Buchan. Thence it 
ascends the mountains to 1200ft., near Walhalla, and 2000ft. on Mount Elizabeth, 
near Noyang. It varies but little in character, yet in places the fruit approaches that 
of E. macrorhyncha in the somewhat protruded vertex and to HK. muelleriana when 
the margin is but slightly convex. I have referred to the peculiarity of its seedlings 
in comparing those of the stringy barks generally, after speaking of those of E. obliqua. 


E. macrorhyncha.—This is essentially a mountain species in Gippsland, and the 


92, THE EUCALYPTS OF GIPPSLAND. 


lowest elevation at which I have found it growing is at Glen Maggie, 200ft. above sea 
level, upon Upper Silurian sediment. In the valley of the Macalister it grows 
extensively, ascending the mountains near Mount Wellington to 3000ft. On the 
Insolvent Track it appears at 1000ft., and thence extends through the mountains to 
the sources of the Wentworth River, reaching an elevation of 3000ft. Similarly on 
the Tambo River it commences at S00ft., near Noyang, and extends to 8000ft. at 
Omeo. Further to the East at Turnback 1000ft., Jingalala 2500ft., and Bonang 
3000ft; it is also found extensively on the Buchan, Snowy, and Deddick Rivers, 
extending towards the high mountains in New South Wales. It grows especially 
upon dry ranges, on Plutonic, Metamorphic, and Sedimentary formations of Silurian 
and Devonian age. Ihave not observed it anywhere in the Tertiary tracts. 


E. obliqua—This Eucalypt is principally found in the western and south-western 
portions of Gippsland, where it, in many places, forms the whole of the forests, or is 
in others mixed with E. goniocalyx, EH. viminalis, E. gunnii, and EH. globulus. It 
appears to be essentially a littoral form, but ascends the mountains to considerable 
elevations in the cool, shady, moist gullies on the southern slopes. For instance, in 
the great Dividing Range, where the Nicholson River rises, E. obliqua follows up the 
damp gullies on the south side, and forms part of the forest on the summit, together 
with E. sieberiana (0), E. viminalis (a), and E. amygdalina(b). It occurs also in Kastern 
Gippsland, as, for instance, at Buchan, Gelantipy, Bonang, and Bendoc. It varies but 
little in character, although the form of the fruit is in some cases, as, for instance, 
near Port Albert, in the sandy coast country, not quite so truncate-ovate as in the 
typical forms, yet in all cases the peculiar unequal-sided ovate lanceolar or eyen- 
cordate lanceolar and pointed form of the leaves always marks the saplings and large 
seedlings from those of any other species. 


Having now referred to the various types of the stringy-bark groups, it is con- 
venient to mention the distinctions between their seedlings and saplings. 


The seedlings of E. piperita, E. eugenioides, and EH. capitellata are beset on 
stems and leaf-stalks with numerous tufts of hairs, which also line the edges of the 
leaves. 


The leaves themselves are more or less hairy, except in that form of H. capitellata 
growing in the mountains, as at Osler’s Creek, where they are smooth. Those of E. 
piperita and E. eugenioides are, at this stage, universally hairy. The seedling 
leaves of both E. piperita, E. eugenioides, and EH. capitellata are at first ovate and 
opposed, but in the former I have often observed them to be ovate-pointed, or even 
lanceolar and smaller than those of H. capitellata, which are always ovate. In 
neither species are the leaves shiny. 


In E. macrorhyncha the seedlings are also more or less beset with tufts of hairs, 


THE EUCALYPTS OF GIPPSLAND. 93 


giving the stems a rough appearance, but ina less degree than the last-named species. 
The leaves, at first opposed, are lanceolar in form, and slightly shiny. The 
seedlings of E. muelleriana are as characteristic as those of any other species known 
tome. ‘The stem and stalklets are slightly tufted with hairs, or are even smooth, the 
leaves rather long, lanceolar, pointed, and opposed throughout, even in seedlings of a 
foot or more in height, while their extremely shiny upper surface distinguishes this 
form from all the other species of this group, being more marked even than in E. 
obliqua, from which the persistent opposition of the leaves readily distinguishes it. 


The seedlings of EB. obliqua are usually free from hairs, but are very commonly 
warty, and the leaves are lanceolar, shining on one side, and thinner in texture than 
those of E. macrorhyncha. They become scattered somewhat sooner than those of 
E: macrorhyncha, and very much sooner than those of E. muelleriana, and soon 
show the marked unequal-sidedness which is so characteristic of this tree. 


The saplings of these Eucalypts may also readily be distinguished from each other. 


Those of E. piperita remain rough up to 10ft. in height, the leaves then 
become unequal-sided, ovate-lanceolar, or ovate-pointed, having the upper surface 
slightly darker green, and more shining than the lower. 


E. capitellata soon produces unequal-sided cordate leaves, fully twice the size of 
those of E. piperita, and of a lighter shade of green, moreover, they hang more vertically, 
and are consequently more equally tinted on both sides. In size, and the inequality of 
the sides, they resemble the sapling leaves of E. obliqua, but are readily distin- 
euished by not being attenuated as those of Obliqua are. 


The saplings of E. muelleriana are distinguishable from all the others by having 
opposed leaves, even up to two or three feet in height. The leaves are lanceolar and 
unequal-sided, but in a less degree than others of the group. The upper page is 
very shining, and the lower much duller and paler in hue. The apex is more or less 
acute, and the lateral veins are more numerous and less spreading than in K. 
capitellata. Even in saplings from 8ft. to 10ft. high, the leaves have a general 
tendency to assume a horizontal position, thus producing a peculiar shining 
appearance of their upper pages, which is characteristic of this tree when young. 


The saplings of E. obliqua have somewhat large, very unequal-sided leaves, 
broadly lanceolar, or even cordate, and always attenuated, thus being, as I have 
pointed out, distinguished from EH. capitellata, whose sapling leaves are not 
attenuated. 


E. stricta.—The only locality in Gippsland in which this Eucalypt is found is, 
as far as I am aware, on St. Pancras Peak, a rocky mountain between the Buchan and 
Snowy Rivers, probably 4000ft. in height. 


94 THE EUCALYPTS OF GIPPSLAND. 


Baron von Mueller refers to it in the ‘‘ Eucalyptographia, Tenth Decade,” on 
the authority of Dr. Wools and Rey. R. Collie, as growing on the elevated parts of 
the Blue Mountains, particularly at some of the summits. In Gippsland it is locally 
called ‘‘ Mallee,” from some fancied resemblance to the growth of that species, 
growing in a number of slender saplings, from one thickened stump-like butt. 


This variety agrees in almost all respects with that figured by Baron von Mueller, 
and described by Sieber as E. rigida, except that the fruit, in my example, has no 
prominent rim, and is rather hemispheric than truneate-ovate. 


E. sieberiana.—There are two well-marked varieties of this Eucalypt which I 
distinguish as (a) and (b). EH. sieberiana (a) occurs extensively on almost all 
formations, in parts of Gippsland, up to an elevation of 3000ft., near Grant and the 
sources of the Wentworth River, and at 4500ft. on Mount Wellington. It ‘is 
characterised by a very rough deeply-fissured bark, which is persistent on the stem 
and larger limbs only, hence its local names of ‘‘gum top,” or ‘silver top ;” its name, 
‘white ironbark,” only refers to the colour of the wood. It grows especially on 
the dry tops of the mountain ridges, and upon their sunny slopes. 


E. sieberiana (b) occurs only in the mountains above the limit of E. sieberiana 
(a), sometimes as low as 2500ft., but in other places, as on the summit of the Great 
Dividing Range at the sources of the Livingstone Creek, where K. sieberiana (a) 
ceases at 3000ft., and KE. sieberiana (6) commences at 3500ft. It extends on the 
summits of the higher mountains, ¢.g., the Bowen Mountains, near Omeo, and the 
Dargo High Plains to about 4500ft. 


I estimate the height to which the tree attains as not exceeding 200ft. The bark 
is fibrous, and rather like that of E. obliqua, but perhaps more flaky ; it is persistent 
upon the bole, the upper part of which and the branches are smooth, but with much 
detached bark, pendant from the forks and from the termination of the persistent 
bark. 


The seedlings of these two trees have much the same features, but that of the 
(a) variety is much darker, and the stems more purple or reddish in tint. The fruit 
also is usually smaller and darker, but otherwise no marked difference can be observed 
between the seedlings of these varieties. 


The timber of the (5) variety is of a light colour, long in grain, and remarkably 
fissile, yet elastic. It is not a heavy wood, and it seems to me should be valuable for 
many purposes. About 20 years ago, at Omeo, I made a set of swingle-bars for a 
four-horse team from this timber, which stood work remarkably well, and one of 
which is still in existence after much hard usage. I have also seen palings split from 
this tree over 6ft. in length, which were so clean, that after being planed up, were 
used successfully as weatherboards. Locally the tree is called ‘‘ Woolly-butt,” from 
the character of the bark, and also ‘‘ Mountain Ash.” 


THE EUCALYPTS OF GIPPSLAND. 95 


E. odorata—This tree has in many respects a superficial resemblance to EK. 
melliodora, with which it was for a long time locally confounded in Gippsland. 


Of late it has received the local name of ‘‘ Grey-box”’ from the splitters and 
sawmillers. 


It grows principally on the Miocene limestones in the littoral tracts of North 
Gippsland. 


The difference between KE. odorata and E. melliodora was long apparent to me, 
from a careful comparison of the trees growing in the Mitchell River district, and 
especially from distinctions which have been apparent to the timber men there. 
The wood of this Eucalypt is much browner in colour than that of E. melliodora, 
and while the timber of the latter can very rarely be split into posts or rails, that 
of the former, although it is difficult to split ‘‘ on the quarter,” is, when once the log 
is opened, ‘‘ backed off” with great ease. The principal differences upon which a 
rapid diagnosis may be made lie in the greatly superior height of E. odorata, in 
its freer growth, the rhytiphloious bark, the smooth upper portion of the stem and 
limbs, and the somewhat larger fruit, with a narrow compressed rim, and more deeply 
sunk orifice. Finally, the outer stamens are all provided with fertile anthers, while 
those of E. melliodora are anantherous. 


The timber of this tree is most durable, and is one of the most serviceable of 
the Eucalypts of Victoria, especially for work which is exposed to damp. 


This tree grows to 200ft., or in exceptional cases to perhaps 250ft. in height. 


I have observed a small colony of E. odorata growing in South Gippsland, near 
Four-mile Creek. The occurrence of this tree in the Miocene limestones of North 
Gippsland falls in with the statement made by Baron von Mueller that it occurs 
upon limestone areas at St. Vincent’s Gulf. 


E. leucoxylon.—This tree does not form forests in Gippsland, as in other parts of 
Victoria, but occurs scattered over a wide extent of country, from sea level up to 
2000ft. It grows upon various formations, as, for instance, at Toongabbie, on recent 
Alluviums, Tertiary clays, and Upper Silurian. At Bairnsdale, upon Miocene and later 
Tertiary beds; at Glen Maggie, upon Upper Silurian sandstone ; at Upper Freestone 
Creek, upon Upper Devonian conglomerates; at Noyang, upon Paleozoic Plutonic 
rocks ; and near Buchan, on Tertiary sands and clays. 


I have not observed it further to the westward than Toongabbie, and it varies 
but little, if at all, in character throughout Gippsland. 


E. melliodora.—This is also of wide distribution, from about Traralgon, in South 
Gippsland, to Jingalala, in North-east Gippsland, and at all elevations up to 2000ft., 
and on all formations. Its characteristics are also constant. 


96 THE BUCALYPTS OF GIPPSLAND. 


E. polvanthema.—Of this type there are two varieties, which, however, are not 
sufficiently marked to justify me in separating them, as 1 have done in other cases. 
Where it occurs in the littoral districts, as, for instance, at the Lakes’ Entrance, or 
river flats at Heyfield or Bruthen, it has full foliage of a rather dark green colour, 
and the leaves somewhat thin in texture. The tree grows to some size, but in many 
cases, as Baron von Mueller has already pointed out, become so hollow as to form a 
mere shell. 


The second variety is found in the hill country, and ascends from about 100ft. 
above sea level, as at Heyfield, to an elevation of 2000ft., as at the Wellington River and 
at the Tambo River (Fainting Range). This mountain variety is a much smaller 
tree than the lowland form ; the leaves are thicker in texture, frequently pruimous, or 
even mealy. At first sight the tree resembles somewhat EH. hemiphloia (variety 
Albens) in its bark, and ash coloured, and sometimes rather lengthened ovate leaves. 
But it is readily distinguished by the form of the buds, by the outer filaments being 
anantherous, and by the fruit. The seedlings and young saplings of both have much 
in common. 


E. hemiphloia—This species is extensively represented in Gippsland as a 
mountain form. It occurs, for instance, in the valley of the Tambo River, north of 
Fainting Range, where it forms the principal part of the forest, from about 750ft. at 
Numlamungie to 2500ft. at Tongeo Gap. It is found at Turnback, at the Snowy 
River, at Deddick, and, more rarely, at Tubbut. 


Its characteristics accord entirely with the diagnosis given in the ‘‘ Kucalypto- 
graphia,” with the exception that the umbels are formed by buds of comparatively 
large size. The fruit is proportionately large. The bark, also, extends frequently far 
up the branches, so that when the leaves are not markedly elongated, this tree 
resembles, as I have already said, at first sight, the mountain form of H. 
polyanthema. Yet, so far as I have observed, the two species are sharply marked off 
from each other. 


This form of E. hemiphloia appears to me to be that variety called E. albens. 


E. pulverulenta is found in many places in Gippsland, though it nowhere forms 
the bulk of the forests, or it is found scattered widely among other Eucalypts. In 
South Gippsland, and near Boolarra, it grows to a maximum height of under 50ft., but 
is of a smaller growth in other parts, as, for instance, at Osler’s Creek, Providence 
Ponds, and Buchan. The peculiarity of this variety, as found in Gippsland, to which 
Baron von Mueller has drawn attention in his ‘“ Kucalyptographia,” lies in the 
lanceolar or falcate form of the opposed leaves of the aged trees, the ovate or 
rounded leaves being confined to the saplings, or young trees. 


THE EUCALYPTS OF GIPPSLAND. 97 


This tree is worthless for timber, and I have never seen it used for any purpose 
except for fuel, in default of better. The local name, “silver-leaf stringy-bark,” 
refers to the pulverulent or ashy character of the foliage, and to its fibrous bark. 


Tt occurs from near sea level up to an elevation of 700ft. at Darlimurla, nearly 
the same at Buchan, and 1000ft. at Osler’s Creek. (See Pl. 15, Figs. 1 to 4, 9, 10, 
13, 32, 33, 34.) 


A few other remarks remain to be made when I compare E. pulverulenta, 
HK. stuartiana, and the mountain form of E. viminalis. 


E. stuartiana.—This species is well marked, and is one of the most persistent in 
character of any of the Eucalypts of Gippsland. Wherever I haye seen it I have 
found it to be a tree with somewhat large and spreading limbs, with a scaly, wrinkled 
bark, which is persistent up to the small branches. 


The wood of this tree is valueless for splitting, sawing, and even for fuel. Its 
general appearance has caused it to be confused with E. hemiphloia, under the 
designation of ‘ white box,’’ under which name I have known it to be cut for sale, at 
least at one sawmill in Gippsland. It is found growing over almost the whole of the 
district, from a little above sea Jevel up to a considerable elevation in the mountains, 
as, for instance, up to 2300ft. on the track from Dargo to Omeo. It is found on all 
formations, but I have observed it especially on the Tertiary clays of South Gippsland, 
and on the Metamorphic and Plutonic areas of Tubbut, Dargo, and Jingallala. 


FE. viminalis——My observation has shown me that there are at least three 
Kuealypts, which may be assigned to the type of Eucalyptus viminalis. 


(a.) The typical form of K. viminalis in Gippsland is the so-called ‘‘ white 
gum,” or ‘‘river gum,” which grows along the immediate course of streams. It 
may, for instance, be seen along the Glengarry, Thompson, Mitchell, and other rivers. 


It accords well with the description of the species given in the ‘‘ Kuealypto- 
graphia,’ hence I need not refer to it further here, more especially as I shall have 
to draw attention to it in distinguishing the varieties. 


The typical form grows from near sea level to at least 4000ft., as on some small 
streams rising in Mount Livingstone. It is especially found following the river 
courses, and ascends to its highest elevation without extending to the hills on either 
side. (See Pl. 15, Figs. 23 to 31; Pl. 14, Figs. 7, 8, 9.) 


(o.) This Eucalypt is sub-alpine, and appears some 7OOft. above sea level, as at 
Dargo and Noyang, but somewhat higher on the Wellington River, and at Gelantipy. 
It also grows about Morwell, where, together with EK. pauciflora, it forms part of the 


98 THE EUCALYPTS OF GIPPSLAND. 


forest, just as it does throughout the alpine and sub-alpine localities, which are its 
special habitat. In the highest tracts, as at Dargo High Plains, it grows to a height 
of over 100ft. It has a rather massive bole, wlth moderately spreading limbs, and 
fairly full foliage. ‘The bark is smooth and very white, excepting near the ground, 
where it more or less persists; it has frequently, when about to dehiss, a decided 
‘‘coppery” tint upon the bole and limbs. The wood is somewhat soft, not very 
fissile, and resembles that of the lowland form, except that it has a more reddish or 
pinkish tint. The leaves are lanceolar, slightly faleate, and more or less attenuated 
at the stalk, the marginal vein is usually but slightly removed, the lateral veins 
numerous, not very marked, and inclined at about an angle of 40dee. with the midrib. 
The umbels are axillary or solitary, and the stalklets about as long as the buds. The 
buds are ovate, most commonly three in number, and arranged in the cruciform 
manner so characteristic of E. viminalis. The lid is semi-ovate, smooth, and 
occasionally pointed, but is not mamillated, as is the case with KE. stuartiana. Judging 
by the examples which I have examined, I think that the buds of this variety are 
more broadly ovate, have shorter stalks, and more rounded lids than those of the 
jowland form. The fruit is semi-ovate, with a somewhat wide and more or less 
convex margin, and with rather strong deltoid and protruding valves. 


These characteristics are those of the typical E. viminalis, but the seedlings and 
young saplings have peculiarities which raise doubts whether indeed this Eucalypt 
should not rather be referred to HE. stuartiana. 


The seedlings have round or ovate opposed leaves, which are closely sessile, 
rarely they are ternary in verticels, the stems as well as the leaves are mealy, and 
thus resemble very strongly, as also in other respects, the young plants of EK. 
pulverulenta as it grows in Gippsland, rather than those of KE. stuartiana. 


Even when as high as 8ft. or 10ft., the saplings still have pulverulent leaves of 
an ovate form and opposed position, and the grown trees themselves occasionally 
show a reversion to this structure at the ends of their pendant branches. In some 
localities, as for instance at Dargo, this tree grows together with K. stuartiana, the 
latter being in its typical form. When the seedlings and saplings of these trees are 
thus compared, those of HE. stuartiana are found to be much less mealy, to be of 
thicker consistence, and more pointed than those of this variety of E. viminalis, in 
which the opposed condition of the leaves is continued much longer than in E. 
stuartiana. There can be no doubt that E. viminalis and E. stuartiana ave nearly 
allied, and it becomes necessary now to enquire to which of these this Eucalypt 
stands nearest. EK. viminalis differs from E. stuartiana, as I have observed them 
to be in Gippsland, by having much smaller limbs as compared to the bole. The 
leaves of the former are smaller, as a rule, more attenuated at the stalk, of thinner 


THE EUCALYPTS OF GIPPSLAND. 99 


“consistence and lighter colour. The marginal vein is less distant, the lateral veins 
more numerous, nearer together, and more obscure. The angle formed by the lateral 
yeins, with the direction of the midrib, is greater in KE. viminalis than in E. 
stuartiana. 


The mean of a considerable number of measurements gave 10deg. more for 
the former than the latter. In the greater number of cases the umbels of EK. 
viminalis are three in number, arranged in a cruciform manner, while those of 
E. stuartiana are more numerous and not so arranged. The buds of EK. viminalis 
are more ovate, with a rounded, or at most, minutely pointed lid; those of 
E. stuartiana are distinctly pointed, or even mammelated. The stalklets of E. 
viminalis are, as a rule, shorter, particularly in the mountain form, although in 
some cases those of the lowland forms are as long, or longer, than those of EK. 
stuartiana. 


The fruit of E. viminalis is more ovate than that of E. stuartiana, with a rim, 
which is always more or less convex, or frequently strongly so. 


Especially is this the case in the lowland form along the river courses, but is 
less so in the mountain form. 


In the mountain form the fruit is usually more hemispherical than in the 
lowland variety, with a convex vertex, and the valves somewhat weaker, although 
protruding. It is in those examples which grow at the highest altitudes, as, for 
instance, the Dargo High Plains, 4500ft., that I have observed the form of the fruit to 
resemble that of E. stuartiana, and in these the fruit is semi-ovate, the rim not very 
wide, and the valves, although exserted on the whole, having their insertions placed 
a little below the level of the rim. Yet, on examining the fruit from a number of 
trees, I observed that there was a considerable variation in that of the same tree. 
While some agree with this description, others have the protruding convex rim and 
exserted valves of the typical E. viminalis. (See Pl. 15, Figs. 14 to 22; Pie 
Figs. 1 to 6, 10 to 18.) 


In the variety which I am now considering, it must be noted that the habit of 
growth, and the character of the wood, is that of E. viminalis, and not of EK. stuartiana. 
Although the cortical character is not of much value, the character of its bark places 
it among the Leiophloiz. 


This tree is the manna-producing Eucalypt of the mountain country. The 
manna is produced as plentifully, in the same manner and of the same kind, as that 
produced by the typical EK. viminalis.* 


* When travelling through the Morwell district, where this tree forms part of the forest, some school children, 
whom I requested to point out the ‘“ manna gum,” indicated this tree, saying that in December the ground under 
the tree was white with manna. 


100 THE EUCALYPTS OF GIPPSLAND. 


I must note, in this connection, however, that I have found small quantities of 
manna indistinguishable from that of E. viminalis, either by appearance or taste, 
attached to slight injuries on the leaves of saplings of KH. stuartiana at Toongabbie. 


The differences between this Eucalypt and the typical form of E. viminalis lie 
almost entirely in the form of the leaves of seedlings and young plants, and in their 
pulverulent character. In general appearance these certainly resemble the young 
plants of Stuartiana, but even more those of EK. pulverulenta, as found in 


Gippsland. 


Having to choose between EH. viminalis and E. stuartiana, I have, after weighing 
all these considerations, assigned it to the former, notwithstanding the strong 
presumption which arises to the contrary from the extreme departure of its seedlings 
from the typical form. 


It seems not only to connect E. viminalis and EK. stuartiana, and thus to 
strengthen the alliance which, as Baron von Mueller points out, exists between these 
Kucalypts, but also to connect these two with E. pulverulenta, in some variety of 
which I have observed the fruit to have a protruding margin and exserted valves. * 


(c.) A somewhat peculiar form of E. viminalis grows between Toongabbie and 
Walhalla, from about 1000ft. to 2500ft. above sea level. It does not exceed 100ft. in 
height. The bark is somewhat rugged, and persists over the bole, but on the 
branches is smooth and of a reddish brown tint, the foliage is plentiful, and of a 
somewhat ashy-grey tint. The leaves are Janceolar to falcate, the veins rather 
indistinct, but agree with those of EK. viminalis. The umbels, buds, blossoms, and 
fruit are also of this type, but with this difference, that the umbels have numerous 
buds, and only rarely three arranged in a cruciform manner. 


The timber of this tree is of no use except as fuel. I have not observed it 
erowing in any other locality. 

E. tereticornis.—This tree, the well-known ‘“‘Red-gum” of Gippsland, is 
essentially a littoral species. 


It grows mainly on the recent alluviums, river flats, ancient lake basins, 
and on the lower terraces of the Tertiary formations, up to an elevation of 
150ft. or more, rarely 200ft., above sea level. The western limit is about Traralgon, 
and it extends eastwards, almost to Buchan, and northwards to Glen Maggie, 
Glenalladale, and Bruthen. 


* The difference in the young plants of the lowland and mountain forms of this Eucalypt are little, if any, greater 
than those which I observed exist in the young forms of the two varieties of E. leuacoxylon,which grow in the neighbourhood 


of Heathcote. 
The smooth-barked variety, locally known as spotted box has, in its young form ovate, opposed, somewhat mealy 


leaves. The rough-barked form—the Ironbark—has opposed leaves only in very young seedlings. 


THE EUCALYPTS OF GIPPSLAND. 101 


In only one instance have I found it growmg in the mountains, viz., at 
Glen Falloch, where it occupies a basin of soft shale of Upper Devonian age, from 
700ft. up to 1500ft. above sea level. The soil of this basin, which is derived from 
the soft shales, resembles that of the lower districts where E. tereticornis thrives 
best. 


The slight distinctions which separate it from EH. rostrata are constant throughout 
Gippsland, although the terete form of the lid varies ; some forms being much more 
attenuated than others. Yet in all the characteristic arrangement of the anthers is 
constant. 


E. gunniu.—tThis type is very widely spread over Gippsland, not only in horizontal 
range, but also in elevation above the sea level. I have observed a lowland and a 
highland form, and each of them has a dwarf variety. 


Lowland form (a).—This form has been fully dealt with by Baron von Mueller, 
and I have only to add that it occurs throughout the littoral country. In the damp 
climate of West and South-Western Gippsland it grows to a considerable height, say 
150ft., with a straight clear bole, and was there cut by saw-millers, in one instance 
at any rate, as ‘‘blue-gum.’”’ In Central and Eastern Gippsland it does not grow to 
so great a height, but maintains its other characteristics. 


(6).—This dwarf variety grows in poor, boggy country in the low-lying tracts, but 
also occurs in the drier hills at Foster. It usually does not grow higher than 4ft. to 
5ft., but at Foster it is found from 18ft. to 20ft. in height. The bark is smooth in 
texture and ashy grey in colour, which becomes lighter in the upper branches. 
Generally, when in its dwarf form it has a large butt level with the ground of several 
feet in diameter, from which rise numerous shoots. 


In the dwarf form the leaves (excepting in the upper shoots) are somewhat 
broadly ovate, and are opposed and sessile. Thetexture is thick and leathery, of a 
dull, rather dark green colour. In the taller examples the leaves become scattered, 
ovate lanceolar, somewhat attenuated at the stalk, and accuminate. They are 
equilateral, slightly shining, and of a rather brighter tint than the sessile leaves, and 
have the marginal vein distinctly removed, the lateral veins numerous and rather 
spreading. Very often the terminal leaves are opposed. 


This Eucalypt flowers and fruits when in a completely dwarf state. The umbels 
are mostly axilliary, and of a bright yellow to orange colour, as are also the stalks and 
young shoots, ‘The stalklet is angular and wrinkled, sometimes rounded, about 
twice as long as the sessile buds, which are 3 to 7, and much crowded together. The 
fruit sessile in clusters of 3 to 7, semi-ovate, margin slightly compressed, valves small, 
not exserted, stalk slightly flattened. 


102 THE EUCALYPTS OF GIPPSLAND. 


The Tall Mountain Form (c).—This much resembles some of the lowland varieties, 
which grow upon dry tracts of land; but the leaves are shorter, more ovate, smoother, 
thicker in consistence, and rarely have the wavy margin which is characteristic of the 
tall lowland form. 


Its lower limit is probably about 600ft. above the sea level, but I think it possible 
that the tall lowland form intermingles with it at that elevation, or less. 


Dwarf Highland Form (d).—I have observed this form of EK. gunnii growing 
extensively in the swampy flats at the source of the main branch of the Livingstone 
Creek, at an elevation of about 3000ft. 


The description given of the dwarf lowland form applies in many respects to this 
also. It does not exceed 2O0ft. in height; the bark is smooth, persistent at the butt, 
and smooth and greenish on the branches. The leaves are ovate, and at first 
opposed and sessile, or nearly so, finally scattered, of a dull green. The umbels are 
axillary, or solitary, of sessile crowded buds. Fruit, semi-ovate rim, rather broad 
and slightly convex, the valves barely exserted. The young twigs and umbels are all 
slightly mealy. This form, however, differs from the corresponding lowland one in 
the leaves being shorter and broader when they become scattered, in the darker 
green of the foliage, and the smaller size and mealy character of the buds. The fruit 
also is of a smaller size. 


E. botryoides.—This, compared with the other species of Gippsland, is one of 
the eastern types of Eucalypts. It spreads along the coast line westward to the sandy 
tracts known as Bole Bole, between the Gippsland Lakes and the sea, where it 
becomes stunted and worthless as a timber tree, though on the northern shores of 
the lakes, at Lake Tyers, and at the Snowy River, it grows to a large size, and is a 
valuable timber. At the latter locality it is known as ‘‘ mahogany.” 


On the northern shore of Lake King it is to be found growing to about 100ft. in 
height, and I have observed a small colony at the very extreme end of the long narrow 
delta through which the Mitchell River enters Lake King. ‘This is probably the most 
westerly point at which this tree grows, and, with Rubus rosifolius, which is found 
in one gully at Mount Taylor, is marked the western limit of the east coast flora in 


Gippsland. 


E. goniocalyx las a wide range in Gippsland, especially in the western parts. 
It grows well in the deep shady gullies of the southern slopes of the mountains, where 
it reaches some 2O00ft. to 250ft. in height, with a tall, massive bole. In its typical 
form it occurs in the valley of the Thompson River, on the Upper Wellington, near 
Grant, on the southern slope of Fainting Range, at Gelantipy, and elsewhere, up to 
4000ft. above sea level in favourable localities. 


THE EUCALYPTS OF GIPPSLAND. 103 

It is very commonly termed ‘‘Blue-gum,” and as such, has, to my knowledge 
been cut by sawmillers. At Walhalla it is used in preference to H. sieberiana or EK. 
capitellata, as being the best procurable in the district for props m the mines, and, so 
far as my experience goes, may be placed after EK. globulus as a useful timber tree 
for work that is not placed in or on the ground—as framing or planking. 


The typical form of E. goniocalyx seems not to be able to cross from the cool 
southern slopes to the warmer and drier northern sides, but there is found in such 
places a peculiar divergent form. 


On the south side of Fainting Range HE. goniocalyx ascends to the summit at 
about 2000ft., while on the northern face of the mountain, and at about 2500ft. above 
sea level, there is a peculiar variety of this type. The seedlings and young plants 
have opposed, ovate, sessile leaves, of a rather light tint of green, not shining, and 
without the peculiar and characteristic rank odour of the leaves of the young plant of 
the common form. 


The tree is usually under 50ft. in height, often with a short bole, and scanty 
limbs and top. The bark is distinctly wrinkled, and the branches only are smooth. 
The leaves are finally scattered, long lanceolar or falcate Janceolar, and more attenuate 
at the stalk than is usually the case in the typical form. The marginal veins are 
somewhat removed, and the lateral ones slightly spreading. The umbels, flowers, 
and fruit accord well with the general character of this Mucalypt. 


E. globulus is much more widely distributed in Gippsland than might be 
expected. It varies but little, and the variation is, 1 think, principally in the more 
or less smoothness of the fruit. It grows especially well in the cool and moist 
districts of the Strezlecki and Hoddle Ranges, more particularly on the southern 
slopes, to the very shore of Corner Inlet. It is more rarely found on the northern 
side of these mountains, as also scantily on the foot-hills of the main ranges—as, for 
instance, about Toongabbie, Freestone Creek, and the Tambo River. It grows in the 
gullies on the north-side of Lake King, near Jimmie’s Point, at Lake Tyers, and in 
other places towards the eastern boundary of the colony. In the Gippsland 
mountains, it is found here and there in isolated colonies, even ascending to 4000ft. 
on the north-eastern slopes of Mount Livingstone. 


104 THE EUCALYPTS OF GIPPSLAND. 


DiIsTRIBUTION OF THE Eucatypts. 


In deciding how the various types of Eucalypts are distributed throughout 
Gippsland, the first point which attracts notice is that the greater number fall into 
one or the other of two groups. One group essentially belonging to the mountains, 
and the other to the lowlands. Besides these, there are a few which are spread 
more or less over the whole district, whether littoral or alpine. 


Certain types, peculiar to the littoral tracts, are found, which thence extend up 
the river valleys, and moist, cool gullies at their sources on the southern slopes of 
the mountains. They then cease, and are replaced on the warm, dry northern 
slopes, and on the more elevated, cool, sub-alpine tracts, either by other types, or by 
other varieties of the littoral forms. 


A few instances will make my meaning more clear. I commence with the best- 
marked westerly example, that of the valley of the Macalister. In it E. viminalis, E. 
piperita, E. obliqua, and E. goniocalyx afford instances. 


The lowland form of EK. viminalis, which is the ‘river-gum” of Gippsland, 
follows up the Macalister River, growing only on the banks, or on the flooded flats, 
to an elevation of 3000ft. at Lake Karng, and at an elevation of 1000ft. at the 
Wellington River. The mountain form of E. viminalis (b) oceurs on the open, grassy 
spurs flanking the river, and then is found here and there, until it becomes plentiful 
on the table-land, through which flows the Caledonia River. 


E. piperita, which forms extensive forests along the foot of the hills, follows up 
the valley of the Macalister, growing on the flats above flood level, but gradually 
ceases on approaching Glen Falloch. 


EK. macrorhyncha commences at Glen Maggie, on the dry Silurian ridges, extends 
all along the stony ranges flanking the valley, and reaches an altitude of about 3000ft. 
on the track leading up from the Wellington to the Snowy Plains. In the mountain 
gullies, having a southerly aspect, which descend from the mountain at Lake Karng 
towards the Wellington River, E. piperita again appears, together with EH. viminalis 
(a), and K. goniocalyx, which all reach, in this spot, an altitude of 3500ft. above 
sea level. 


The high mountain ranges to the westward of the Macalister, and the still 
higher alpine tracts to the west of the Mitchell, above the Dargo junction, and again 
those to the west of the Snowy River, above its junction with the Buchan, 
precipitate the westerly rains, and divert the rainfall from the valleys on the eastern 
side of the mountains. 


THE EUCALYPTS OF GIPPSLAND. 105 


Somewhat similar seems to be the effect produced by the coast ranges upon the 
sub-alpine plateau of Omeo and the Dargo basin. 


At the sources of Cobbanah Creek, and at the Budgee Budgee Mount, similar 
observations can be made. 


E. piperita and E. obliqua ascend the sources of Granite Creek to the saddle 
separating it from Bulgaback Creek at 500ft. 


They then cease, and on the dry north side are replaced by E. macrorhyncha, 
which then extends as the sole stringy-bark to about 1200ft. in the mountains leading 
to Grant. On following these mountains, however, HE. obliqua re-appears in the 
south gullies of Mount Ewing, at an elevation of 4000ft., which is its limit in these 
mountains. 


In proceeding from Dargo to Omeo, by way of the Wentworth River sources, 
instructive observations can be made as to the distribution of the different types of 
Kucalypts. 


In Dargo itself, which is essentially one of the mountain areas, E. viminalis (0) 
occurs at its lowest limit of 700ft., growing plentifully over the open grassy hills of 
Plutonic rocks. EH. viminalis (a) occurs in the river courses, following them up from 
the littoral tracts. At the source of Teapot Creek, near Mount Steve, is to be found 
an outlying colony of E. amygdalina (f) the Black-butt, of South Gippsland, together 
with E. piperita and EK. obliqua at an elevation of 2500ft. The summit of the ridge 
is crested by E. sieberiana (a), and in the creeks falling into the Wentworth River, 
the Eucalypts are essentially lowland forms, with the examples of EK. amygdalinas 
(a) and (6) which occur locally at Pheasant Creek. These lowland forms, for 
instance, H. viminalis (a), E. amygdalina (a), E. piperita, KE. obliqua, K. melliodora, 
E. polyanthema, E. stuartiana, follow up the sources of the Wentworth River towards 
the Great Dividing Range. 


On the range along which runs the Wentworth track to Omeo, I observed that 
K. melliodora ceased at Wild Horse Creek at about 1500ft., EH. macrorhyncha at 
2400It., KE. amygdalina (b), which here grows plentifully at one place, and at an unusual 
elevation of 2400ft. HE. polyanthema gradually decreases in number, diminishes 
in size, until at 2300ft. it ceases with a few dwarfed trees. At the same place EH. 
stuartiana also ceases abruptly on the south side of the ridge, and with a diminution 
of size. 

At 3000ft. K. piperita disappears at the extreme source of Wild Horse Creek, 
without any change of size. At the same point E. viminalis (a) also ceases. It 
appears that the elevation above the sea level has less to do with the disappearance of 
these trees than the change of climate from the cool moist gullies on the southern 
slopes to the cold yet drier northern side of mountains. 


106 THE EUCALYPTS OF GIPPSLAND. 


On the great Divide itself HK. sieberiana (a) ends abruptly at 3000ft., and BE. 
sieberiana (b) commences at 3500ft., here also grows E. obliqua to great size, but 
ceases at 3100ft. at the descent into the Upper Livingtone Creek, where the mountain 
types of Eucalypts commence, viz., E. gunnii (0), H. stellulata, E. pauciflora, E. 
viminalis, and E. amygdalina. 


In descending from the Omeo plateau towards Tongio, I observed that BH. 
hemiphloia, variety albens, commences at 2500ft. This Eucalypt grows preferen- 
tially upon the Plutonic and Metamorphic formations of the dry valleys of Tongio 
and Ensay, the Upper Snowy (in Victoria), and of the Deddick and Tubbut Rivers. 
In the descent from Omeo one finds E. melliodora at 2000ft. In passing from the 
deep valleys of Ensay to the coast ranges, which may be regarded as commencing at 
Mount Elizabeth, I observed that E. hemiphloia ceased at 1000ft. at Hnsay, but this 
elevation must probably be decreased considerably, as I believe this type grows on the 
Tambo at Numlamungie, approximately 700ft. above sea level. The same remarks 
apply to E. stellulata, on the summit of Fainting Range. I have noticed that E. 
polyanthema, E. goniocalyx, K. piperita, and E. obliqua re-appear at their upper limit 
in this locality, and it is about here that the littoral types touch and intermingle 
with the mountain forms. It is here to be noted, as at other places to which I have 
referred, that it is the lowland types which slightly cross the limit set them by the 
summit of the cool mountains, and descend to some little extent in the warmer slopes, 
rather than the mountain types, which descend the moist southern side. 


At Noyang, on the Tambo Valley road, there occurs a tract of Plutonic and 
Metamorphic rocks, and here there is, to a certain extent, a re-appearance of the 
sub-alpine types intermingling with a greater number of the lowland Eucalypts. 


Further down the road E. muelleriana appears, growing on the Silurian for- 
mations from the upper limit of the Tertiary marine beds at 7OOft. to 1300ft. 
I observed only one or two scattered examples growing in the forest of E. piperita on 
the Tertiary sands near Monkey Creek. 


I might instance other examples in the mountain country, in the sources of the 
Buchan River—at Murrendel, at Woolgulmerang, and at Bonang, but the above will 
suffice, and my observations in these localities, although made with sufficient care to 
satisfy me as to the general results, want the precision which I have endeavoured to 
give to the cases which I have noted. My notes on the eastward of the Snowy River, 
in Croajingolong, were made many years ago, and fall into line with those I have 
given, but as they were less precise even than those made between the Tambo and 
Snowy Rivers, I prefer not to rely upon them. 


The observations which I have now recorded as to the distribution in the 


THE EUCALYPTS OF GIPPSLAND. 107 


mountainous and littoral tracts of Gippsland, of the several types of Eucalypts, seem 
to me to show that elevation above sea level, rainfall, and aspect have had more to 
do in their distribution than have the geological formations, or than have the different 
soils produced therefrom. 


The range of mountain and littoral types has, it seems, varied from time to time ; 
that is to say, the mountain types have at times spread into or over the littoral tracts, 
while at others the littoral types have spread into the mountains. 


The manner in which E. piperita, E. obliqua, E. goniocalyx, E. polyanthema, 
and others climb up the southern slopes, and there meet with the subalpine forms, 
and others whose habitat is in the dry valleys within the coast range, shows that the 
distribution of these forms is regulated by climate. 


It would only require that the conditions which now prevail on the southern 
slopes should extend over the drier mountain pleateaux; in other words, that the 
rainfall should be greater there than it is now for those Kucalypts to extend still further 
northwards from the lowlands. 


I have been led to suspect, from the study of the Gippsland Eucalypts, that 
varieties have arisen, not only through the impulse of the favouring conditions of 
climatic change, but also that to the same cause is due an emigration from the 
lowlands to the highlands, and vice versa. 


The instance of E. goniocalyx is significant. It is at present almost entirely 
confined to the cool, moist littoral regions, where the soil is good, and the cool, 
humid gullies of the southern slopes ; it does not, in its typical form, extend across 
the watersheds into the warmer and comparatively dry northern slopes. Its place is 
there taken by a dwarf variety having marked differences. 


Were the climate to become so much altered that the same conditions obtained 
throughout the district as are now found, for instance, at Dargo, Ensay, or Glen 
Falloch, 1 conclude that the lowland form of E. goniocalyx would disappear, and the 
dwarfed mountain form might take its place. The species would no longer be 
represented by a tree reaching 200ft. to 250ft., with a smooth-barked massive bole, 
but by a straggling tree with, often, a short gnarled trunk, a wrinkled strongly 
persistent bark, scanty foliage, and a young form, in which the leaves, although 
opposed, are not pointed-ovate or broadly lanceolar, nor haying the powerful odour 
which characterises the lowland form. 


The existence of small colonies of mountain species in the lowlands, as, for 
instance, the before-mentioned E. pauciflora and E. viminalis (6) points, I think, to 
survivals from a time when the climate was much colder than it is now. ‘The 
oscillations of level which have affected the coast line of the southern half of this 


108 THE EUCALYPTS OF GIPPSLAND. 


continent may be as well studied in Gippsland as in any part that I have seen from 
Shoalhaven to beyond Adelaide. These must: certainly have produced variations of 
climate, extending back beyond the Cainozoic period. 


The Gippsland Alps have not been submerged below a contour line of some 
800ft. to 1000ft. above sea level, not only during that period of time, but that land 
surface must have been continuous backwards to the time when the Mesozoic coal 
measures of Gippsland were formed. 


The lauraceous and other plants which have been found in the Miocene drifts 
of Gippsland, indicate, as does also the fauna of the marine limestones of that district, 
a warmer climate than of the present day. 


Lake Karng at Mount Wellington, if it be a moraine lake, points, on the 
other hand, to an alpine climate, descending to within at least 3000ft. of the sea 
level. Such changes of climate have evidently been attended by a corresponding 
change in the Tertiary flora, in which that element, which is now characteristic 
of Australia, has gradually predominated. Such changes of climate may, as it 
seems to me, also account in part for the great number of recorded types of 
Eucalypts and their varieties, and of which no less than 35 occur in Gippsland. 


Geological formation, as producing variation of soil, has no doubt influenced 
the present distribution of the Eucalypts, but its effects cannot be made out so 
clearly as those produced by climate, but the broad features can be readily seen by 
anyone travelling through Gippsland. LE. tereticornis grows almost entirely on lands 
which have been at one time lake or estuary beds, or in the alluvial flats of rivers. 


The stringy-bark Eucalypts preter the Tertiary sands and sandy clays. H. odorata 
grows mainly on the Miocene limestone, but this partiality to particular formations 
is not so apparent when all the Eucalypts are considered. Still, in looking over 
the whole of Gippsland, I observed some marked cases which it would be well to note. 
A good instance is afforded by E. amygdalina regnans (0), which, in Gippsland, 
grows almost wholly upon the Mesozoic coal measures. E. hemiphloia appears to be 
confined to the Plutonic and Metamorphic areas of the Tambo and Snowy Rivers. A final 
instance may be taken from the Gelantipy tableland, to the west of the Snowy River, 
which shows how certain Eucalypts grow preferentially upon certain formations. 
This tableland is formed by a great thickness of Devonian and Plutonic rocks, 
overlaid by more or less connected sheets of Tertiary basalt. 1 observed that on the 
former grow especially KE. piperita, E. globulus, E. sieberiana, and E. amygdalina, 
and on the latter formation E. stuartiana, E. melliodora, EK. polyanthema, and E. 
macrorhyncha. 

The annexed table has been compiled from observations which I have made in 
almost all parts of Gippsland, and shows the distribution of the Eucalypts on the 
various formations. 


THE EUCALYPTS OF GIPPSLAND. 109 


INFLUENCE OF SETTLEMENT ON THE Eucatyptus Forests. 


The influence of settlement upon the Eucalyptus forests has not been confined 
to the settlements upon lands devoted now to agriculture or pasturage, or by the 
earlier occupation by a mining population. 


It dates from the very day when the first hardy pioneers drove their flocks and 
herds down the mountains from New South Wales into the rich pastures of 
Gippsland. 


Before this time the gramminivorous marsupials had been so few in comparative 
number, that they could not materially affect the annual crop of grass which 
covered the country, and which was more or less burnt off by the aborigines, either 
accidentally or intentionally, when travelling, or for the purpose of hunting game. 


These annual bush fires tended to keep the forests open, and to prevent the 
open country from being overgrown, for they not only consumed much of the 
standing or fallen timber, but in a great measure destroyed the seedlings which had 
sprung up since former conflagrations. 


The influence of these bush fires acted, however, in another direction, namely, 
as a check upon insect life, destroying, among others, those insects which prey upon 
the Eucalypts. 


Granted these premises, it is easy to conclude that any cause which would 
lessen the force of the annual bush fires, would very materially alter the balance of 
nature, and thus produce new and unexpected results. 


The increasing number of sheep and cattle in Gippsland, and the extended 
settlement of the district, lessened the annual crop of grass, and it was to the interest 
of the settlers to lessen and keep within bounds bush fires which might otherwise be 
very destructive to their improvements. 


The results were twofold. Young seedlings had now achance of life, and a severe 
check was removed from imsect pests. The consequences of these and other 
co-operating causes may be traced throughout the district, and a few instances will 
illustrate my meaning. 


The valley of the Snowy River, when the early settlers came down from Maneroo 
to occupy it, as for instance, from Willis downwards to Mountain Creek, was very open 
and free from forests. At Turnback and the Black Mountain, the mountains on the 
western side of the river were, in many parts, clothed with grass, and with but a few 
large scattered trees of Hi. hemiphloia. 


110 THE EUCALYPTS OF GIPPSLAND. 


The immediate valley was a series of grassy alluvial flats, through which the 
river meandered. After some years of occupation, whole tracts of country became 
covered with forests of young saplings of E. hemiphloia, pauciflora, viminalis, 
amyedalina, and stellulata, and at the present time these have so much increased, and 
grown so much, that it is difficult to ride over parts which one can see Ie the few 
scattered old giants were at one time open grassy country. 


Within the last twenty-five years many parts of the Tambo valley, from Ensay up 
to Tongio, have likewise become overgrown by a young forest, principally of E. 
hemiphloia and macrorhyncha, which extend up the mountains on either side of the 
valley. This dates especially from the time when the country was fenced into large 
sheep paddocks, when it became very important that bush fires should be prevented 
as a source of danger to the fences, and even when fire occurred the shortness of the 
pasturage checked the spread. 


Similar observations may be made in the Omeo district, namely, that young forests 
of various kinds of Eucalypts are growing where a quarter of a centuryago the hills were 
open and park like. In the mountains, from Mount Wellington to Castle Hill, in 
which the sources of the Avon River take their rise, the increase of the Eucalyptus 
forests has been very marked. Since the settlement of the country, ranges, which 
were then only covered by an open forest, are now grown up with saplings of E. 
obliqua, E. sieberiana, and others, as well as dense growths of Acacia discolor, A. 
verniciflua, and other arborescent shrubs. These mountains were, as a whole, 
according to accounts given me by surviving aborigines, much more open than they 
are now. 


In the upper valley of the Moroka River, which takes its rise at Mount 
Wellington, I have noticed that the forests are encroaching very greatly upon such 
open plains as occur in the valley. I observed one range, upon which stood scattered 
cigantic trees of E. sieberiana, now all dead, while a forest of young trees of the same 
species, all of the same approximate age, which may probably be twelve years, 
srowing so densely that it would not be easy to force a passage through on horseback. 
Again, at the Caledonia River, as at the Moroka, the ranges are in many parts quite 
overgrown with forests not more than twenty years old. The valleys of the Wellington 
and Macalister Rivers also afford most instructive examples of the manner in which 
the Eucalyptus forests have increased in the mountains of Gippsland since the country 
was settled. The forest in these valleys, below 2000ft. above sea level, is principally 
composed of Eucalyptus polyanthema, E. macrorhyncha, with occasional examples of 
EK. melliodora and E. stuartiana ; while E. viminalis occupies the river banks and moist 
flats. I noticed here that E. melliodora and E. macrorhyncha formed dense forests 
of young trees, apparently not more than twenty-five years old. In some places, 
moreover, one could see that the original forest had been composed, on the lower, 


THE EUCALYPTS OF GIPPSLAND. 111 


undulating hills and higher flats of a few very large EH. melhodora, with scattered trees 
of E. polyanthema and HK. macrorhyneha. At the present time the two latter have 
taken possession, almost to the exclusion of E. melliodora. In other places E. poly- 
anthema or EK. macrorhyncha predominate ; but, on the whole, I think the latter will 
ultimately triumph over its rivals, unless the hand of man again intervenes. 


Such observations may also be made in Western and Southern Gippsland, but, 
of course, with reference to different species of Kucalypts. 


In the great forest of South Gippsland many places can be seen where there are 
substantially only two existing generations of trees; one of a few very large old trees, 
the other of very numerous trees which are, probably, not older than 30 to 40 years, 
and, in most cases, certainly not half that period. The older trees of this second 
erowth do not, I suspect, date further back than the memorable ‘“‘ Black Thursday,” 
when tremendous fires raged over this tract of country. . It may also be inferred, from 
the constant discoveries during the process of clearing of blackfellows’ stone 
tomahawks, that much of this country, now covered by a dense scrub of gum 
saplings, Pomaderis apetala, Aster argophylla, and other arborescent shrubs, that the 
country was at that time mainly an open forest. 


I might go on giving many more instances of this growth of the Eucalyptus 
forests within the last quarter of a century, but those I have given will serve to show 
how widespread this re-foresting of the country has been since the time when the white 
man appeared in Gippsland, and dispossessed the aboriginal occupiers, to whom we owe 
more than is generally surmised for having unintentionally prepared it, by their 
annual burnings, for our occupation. 


The age of the new forests does not, however, depend merely on the general 
observation that they have sprung up since the settlement of the country in 1840. 


I have been enabled to make some direct observations, which show the size of 
certain trees of known age, and which will serve as comparison for the general growth 
of the forests. 


In 1864 the discovery of auriferous quartz reefs in the Crooked River district, 
caused a township, which is now called Grant, to be formed on the summit of the 
mountains, near the sources of Good LuckCreek. In part of the Government reserve, 
upon which the warden’s quarters and police camp stood, and which was cleared of 
timber, a few young E. amygdalina trees grew, and were permitted to remain. One 
of these was lately kindly measured for me by Mr. W. H. Morgan, M.M.B., who 
found it to be 56ft. high and 10ft. in girth 3ft. above the ground. ‘This tree is an 
example of very many others of the same species now growing on the surrounding 
ranges. At Omeo, in the Government reserve, a number of young E. viminalis are 


112 THE EUCALYPTS OF GIPPSLAND. 


now 60ft. high, which in 1863 were only small saplings under 5ft. in height. On the 
road from Sale to Port Albert, which was formed somewhere about 1858-59, there 
are numerous places where E. viminalis and E. muelleriana and other species are now 
growing, upon the ditches formed at the sides of the road. Those, for instance, at 
Lillies Leaf are on an average about 30ft. high. 


These instances show how the occupation of Gippsland by the white man has 
absolutely caused an increased growth of the Eucalyptus forests in places. I venture, 
indeed, to say with a feeling of certainty, produced by long observation, that, taking 
Gippsland as a whole, from the Great Dividing Range to the sea, and from the 
boundary of Westernport to that of New South Wales, that, in spite of the clearings~ 
which have been made by selectors and others, and in spite of the destruction of 
Eucalypts by other means (to which I am about to refer), the forests are now more 
widely extended and more dense than they were when Angus M‘Millan first descended 
from the Omeo plateau into the low country. 


I have spoken just now of the destruction of Eucalypts by other means than the 
hand of man, for clearing his holdings, and the following are the facts I have gathered 
concerning the subject :— 


About the year 1868-4 I observed that a belt of Red-gums which extended across 
the plains between Sale, Maffra, and Stratford were beginning to die. Gradually all 
the trees of this forest, as well as in other localities, perished. At that time my 
attention was not drawn to the investigation of the cause. Later, however, probably 
about 1878, I observed the Red-gum forests of the Mitchell River Valley to be dying, 
just as those at Nuntin and elsewhere had died years before. I then investigated the 
subject, and found the trees were infested with myriads of the larve of some 
one of the nocturnal Lepidoptera. These devoured the upper and under epidermis 
of the leaves, thus asphyxiating the tree. Some 75 per cent. of that forest died that 
year, and subsequently almost all the surviving trees died also. Since then I have 
observed the same larvee at work, some of which, when kept until they had passed through 
their several metamorphoses to the perfected insect, were pronounced by Professor 
M‘Coy to be examples of Urubra Iugens. Whether this insect has in all cases been 
the agent in destroying the red-gums I cannot affirm. Probably not wholly, but Iam 
satisfied that the greater part of the Red-gum trees which have died in Gippsland 
from obscure causes have been killed by its agency. 


The inference may be drawn from the above observations of forests having been 
killed by infesting insects, that each species of Eucalypt, or at any rate each group 
of allied species, will have attached to it some particular insect which preys upon it 
rather than upon any other Kucalypt. 


THE EUCALYPTS OF GIPPSLAND. 113 


If this is so, we ought to find some one tree selected for destruction out of a 
number of species, and it is the case with the Red-gum, for it falls a victim to Urubra 
lugens, whilst its neighbours the White-gum (EK. viminalis), the Swamp-gum (EK. 
gsunni), and the Yellow-box (E. melliodora) are untouched and in vigorous 
health.* 


I feel little doubt that this will explain why it is that in many parts of the 
country, at all elevations above sea level, certain tracts of dead forest are to be found. 
Twenty-five years ago I noticed that during the course of three years all the White- 
oums (HE. viminalis) in part of the Omeo district died, whilst E. pauciflora and E. 
stellulata remained alive. 


I have said that in my opinion the increased growth of the Eucalyptus forests 
since the first settlement of Gippsland has been due to the checking of bush fires 
year by year, and to the increase thereby of the chance of survival of the seedling 
Kucalypts, and to the same cause we may assign the increase of the leaf-eating insects 
which seem in places to threaten the very existence of the Red-gum. 


Bush fires, which swept the country more or less annually, kept down the 
enormous multiplication of insect life, destroymg myriads of grasshoppers and 
caterpillars, which now devastate parts of the Gippsland district, spoiling the oat 
crops, and eating the grass down to the ground. 


The ravages of the larvae of Lepidoptera are at present greatly aided by the 
sickly state in which many of the Red-eum forests in Gippsland now are. The 
long-continued use of the country for pasturage, and the trampling of the surface of 
the ground by stock, has greatly hardened the soil, so that rain which formerly, in 
what I may call the ‘‘ normal state’? as regards Eucalypts, soaked in, now runs off. 
In the course of successive droughty seasons the soil of such places becomes 
thoroughly dry and hard, so that the Red-gum is deprived of much moisture which 
it otherwise would have in reserve. The trees are wanting in vigour, and thus 
unable to withstand the attacks of insect pests. 


The effects produced by man’s interference with the balance of nature, by settling 
new countries, is not only of great scientific interest, but is also of importance in 
showing us how and why it is that the labours of the graziers and farmers are being 
carried on year by year under the increasing attacks of insect pests. 


The subject is a tempting one, but to pursue it further would be foreign to the 
subject of these Notes, which is the ‘‘ Eucalypts of Gippsland.” 


* I have observed, however, in some localities E. melliodora and E. piperita have been slightly attacked by 
Urubra lugens. 


OF GIPPSLAND. 


EUCALYPTS 


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THE EUCALYPTS OF GIPPSLAND. 


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EXPLANATION OF PLATES. 


Puate 8. 


Eucalyptus amygdalina (b). 


Lower leaf of sapling, Mount Livingstone. 
Lower leaf of sapling, Dargo. 
Upper leaf of sapling, Wentworth River. 
Leat of aged tree, Wentworth River. 
Seedling, Mount Livingstone. 
Buds, natural size. 
Section of fruit. 

Anthers x 24 linear. 
Anthers x 6 linear. 
Fruit, natural size, Mount Livingstone. 


PLATE 9. 


E. amygdalina (d). 


Lower leaf of sapling, Stradbroke. 

Lower leaf of sapling, Wild Horse Creek. 
Leat of young tree, Dargo, 

Leaf of aged tree, Tambo River. 

Leaf of aged tree, Carrajung. 

Seedling, Bruthen Creek. 

Anthers x 24 linear. 

Filaments and anthers x 6 linear, Stradbroke. 
Cluster of buds, natural size, Stradbroke. 
Fruit, natural size, Dargo. 


Puate 10. 


E. amygdalina (e). 


iB 
2. 
3. 
4. 


Terminal shoot of young sapling. 
Cluster of fruit. 
Buds. 


Seedling. 


THE EUCALYPTS OF GIPPSLAND. 117 


5. Leaf of aged tree, Tambo River. 
6,7. E. amyedalina (c), Leaves of aged tree. 
8. Section of fruit. 
9. Cluster of fruit. 
10. Buds. 
11. Anthers x 6 linear. 
12. Anthers x 24 linear. 


Puate 11. 
E. muelleriana. 
1. Seedling, Insolvent Track. 
2. Seedling, Toongabbie. 
Seedling, Shady Creek, South Gippsland. 

4. Spray, with buds and flowers, Woodside. 

5, 6. Anthers x 24 linear, Woodside. 

7,8. Anthers x 24 linear, Toongabbie. 

9,10. Anthers x 24 linear of E. eugenioides, Agnes River. 
11,12. Anthers x 24 linear, E. piperita, Toongabbie. 
18, 14. Anthers x 24 linear, Wild Horse Creek. 

15. Section of fruit of E. muelleriana, Woodside. 
16. Cluster of fruit of EK. muelleriana, Woodside. 


ise) 


Pratt 12. 
FE. nuelleriana. 
1. Leaf of sapling (8ft.), Daraman. 


2. Leaf of sapling, Insolvent Track. 
3. Leaf of sapling, Woodside. 
4. Leaf of aged tree, Four Mile Creek. 
5. Leaf of aged tree, Woodside. 
6. Leaf from top of sapling, Tambo River. 
7. Leaf of aged tree, Toongabbie. 
Prate 13. 
1. Leaf of sapling of E. piperita, Toongabbie. 
2. Leaf of sapling of E. capitellata, Ostler’s Creek. 
3. Leat of sapling of EK. obliqua, Wallialla. 
4. Leaf of sapling of E. macrorhyncha, Dargo. 
5. Leaf of sapling of E. eugenioides, Drouin West. 


118 THE EUCALYPTS OF GIPPSLAND. 


Fruit of E. piperita. 
6. Bruthen. 
7. Fainting Range. 
8. Tambo River 
9. Wild Horse Creek. 
10. Stockyard. 
11, 12. Monkey Creek. 
13. Groggingee. 
14. Bruthen. 
15. Bulgaback. 
16. Insolvent Track. 
17. Bruthen. 
18. Toongabbie. 
19. Insolvent Track. 


E. eugenioides. 
20. Agnes River. 
21. Drouin. 


E. muelleriana. 
22. Tambo River. 
23. Insolvent Track. 
24. Toongabbie. 

25. Woodside. 


E. capitellata. 
26, 27. Lilies’ Leaf. 
28. Mirboo North. 
29. Ostler’s Creek. 


E. macrorhyncha. 
30. Drouin West. 
31. Fanwick. 


> 


32. Dargo. 


Prats 14. 


1. Seedling, E. piperita, Toongabbie. 
Seedling, E. capitellata, Ostler’s Creek. 
Seedling, E. macrorhyncha, Bulgaback. 
4. Seedling of E. eugenioides, Agnes River. 
5. Seedling of E. obliqua, Agnes River. 


co be 


THE EUCALYPTS OF GIPPSLAND. 119 
Puate 15. 


1, 2,3, 4. Anthers x 24 linear, K. pulverulenta, Boolarra. 
5, 6, 7,8. Anthers x 24 linear, EK. stuartiana, Lilies’ Leaf. 

9. Pair of leaves of aged tree, E. pulverulenta, Monkey Creek. 
10. ‘Terminal leaf (alternate), E. pulverulenta, Monkey Creek. 
11. Leaf of aged tree, E. stuartiana, Toongabbie. 

12. Seedling, EK. stuartiana, Toongabbie. 
13. Seedling of E. pulverulenta, Monkey Creek. 


Buds and Fruit of E. viminalis (6). 
14. Squirrel Forest. 
15. Omeo. 
16. Morwell. 
17. St. Pancras Peak, Woolgulmerang. 
18. Highteen Mile Creek, Dargo High Plains. 
19. Fraser’s Plain. 
20. Dargo High Plain. 
21. Grant. 
22. Woolgulmerang. 


E. viminalis (a). 
23. Monkey Creek, Port Albert Road. 
24. Alberton. 
25. Coal Creek. 
26. Wentworth River. 
27. Tucker Creek. 
28. Wild Horse Creek. 
29. Sources of ‘Tucker Creek. 
30. Woolgulmerang. 
31. Upper Wentworth River. 


E. pulverulenta. 
32. Monkey Creek, Port Albert Road. 
33. Boolarra. 
34. Ostler’s Creek. 


E. stuartiana. 
35. Lilies’ Leaf. 
36. Stradbroke. 
37. Cuidmundie, Dargo. 
38. Insolvent Track. 
All natural size, 


120 THE EUCALYPTS OF GIPPSLAND. 


PuatE 16. 
E. viminalis (6). 

1. Lower leaf of sapling, Dargo. 

2. Pair of upper leaves, sapling, Dargo. 

3. Leaf of young tree, Dargo Plains. 

4. Leaf of aged tree, Dargo Plains. 

5. Leaf of aged tree, Omeo. 

6. Young plant, Omeo. 

7,8, 9. Anthers x 24 linear of E. viminalis (a), Alberton. 
10, 11, 12. Anthers of K. viminalis (6), Cuidmundie, Dargo. 
13, 14, 15. Anthers x 24 linear, E. viminalis (0), Squirrel Forest. 
16,17, 18. Anthers x 24 linear, E. viminalis (6), Omeo. 


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ARTICLE IV.—A New Famity or HyprompEa, TOGETHER WiTH A Description 
OF THE STRUCTURE OF A New Species or Prumutaria, By W. Batpwin Spencer, 


M.A., Proressor or Bronocy in THe University oF MELBOURNE. 


(Read Noy. 12th, 1890.) 


The following deals with two hydroid forms obtained by Mr. J. Bracebridge 
Wilson, M.A., from the neighbourhood of Port Phillip. One of these is so distinct 
from any hitherto described that it must be taken as the type of a new Family, to 
which the name of Hydroceratinide is given, the other is a new and somewhat 
curious species of the genus Plumularia. The paper is, therefore, divided into two 
parts—(1) On the Hydroceratinide, a new family of the order Hydroidea, and (2) On 
Plumularia procumbens, a new species of the genus Plumularia. 


(1) On tHe Hyproceratinip®, 4 New Faminy oF THE OrpER Hyprorpea. 


The form in question undoubtedly calls to mind, in the general appearance of 
the dried specimens, one of the two genera which were placed in a distinct family— 
the Ceratellade—by Dr. Gray,* and, when this paper was read before the Royal 
Society of Victoria, I provisionally referred it to this family.f Dr. Gray had doubtfully 


* Norz.—Up to the time of reading this paper I had only the necessarily 
somewhat imperfect descriptions (since taken from dried specimens only) of Dr. Gray 
and Mr. Carter to be guided by together with the figures of the former. Those of 
Dehitella bore a general resemblance to the specimen in question which was 
placed provisionally in that genus as a new species. Through the courtesy of Dr. 
EK. P. Ramsay I have since been able to examine specimens of Ceratella and Dehitella 
from the Australian Museum, Sydney, and have received from there specimens 
obtained from the New South Wales coast, and from Lord Howe Islands by Mr. 
Whitelegge, to whom I am much indebted for kind assistance and information. The 
examination of these specimens has shown that the form with which this paper deals 
differs in such important points not only from the Hydractiniide but also from 
the Ceratelladz that it must be placed in a separate family and I desire to here record 
my indebtedness to the authorities of the Australian Museum, Sydney, for the 
courteous assistance received from them. 


* Proc. Zool. Soc., Nov., 1868. 


122 A NEW FAMILY OF HYDROIDEA. 


placed the family in the group Porifera. Mr. Carter subsequently had the opportunity 
of examining both Dr. Gray’s specimens and others of allied forms from New 
Zealand and the Cape, and rightly referred them all to the Hydroidea, placing them 
in the family Hydractiniide, This classification was adopted by Dr. v. Lendenfeld, and 
also, at first, by Mr. Bale in his valuable contribution to the literature of Australian 
zoology—the ‘Catalogue of Australian Hydroid Zoophytes.”* Subsequently, Mr. 
Bale had the opportunity of examining spirit-preserved specimens with the hydranths 
and soft parts present, and, finding that these differed very considerably from those 
of the Hydractiniide in the presence of irregularly distributed capitate tentacles, 
&e., rightly separated them once more from the Hydractiniide, and adopted the 
name of Ceratelladz for the family.| I was unaware of this short paper of Mr. 
Bale’s until my attention was kindly drawn to it by Mr. Whitelegge, of the 
Australian Museum. 


Whilst Dehitella in its general form (in the dried specimen) is somewhat like 
the specimen obtained by Mr. Wilson, there can be little doubt that the two are 
markedly distinct, even so far as the skeleton goes. Dehitella has most clearly what 
have well been called hydrophores', and agrees closely in this respect and in the 
general formation of its skeleton with Ceratella ; in their soft parts we may 
reasonably suppose that a corresponding agreement exists. Now the soft parts of 
the Ceratella are known,§ and they differ very strongly from those of the form with 
which this paper deals, so that we are probably correct in assuming that a similar 
difference exists between the latter and Dehitella. There is, on the other hand (as 
will be shown subsequently), quite as marked a distinction between the new form 
and any member of the family Hydractiniide as exists between the former and the 
Ceratelladx, so that it is necessary to create a new family for its reception. 


Ihave not so far, though numerous sections have been cut, been able to 
detect any reproductive elements, and therefore the description is incomplete, but will 
quite sufficiently serve to distinguish it from other forms. 


Family Hydroceratinide. 


Hydrophyton, consisting of a mass of entwined hydrorhiza, with a skeleton in 
the form of anastomosing chitinous tubes; the surface is studded with tubular 
hydrotheecx, into which the hydranths can be completely retracted. Hydranths 
sessile and connected with more than one hydrorhizal tube, claviform with a single 
verticil of filiform tentacles. Defensive zooids present with a solid endodermal axis 
and nematocysts borne at the distal end. 


* Catalogue of Australian Hydroid Zoophytes. W. M. Bale, 1884. 

+ Bale, Proc. Linn. Soe., N.S.W., Vol. III., pt. 2, p. 748; also Brazier, Proc. Linn. Soc., N.S.W., new series, Vol. I. 
page 575; Whitelegge, loc. cit., p. 578. 

+ Bale, Proc. Linn. Soc., N.S.W., 1888, p. 749. 

§ Bale, loc. cit. 


A NEW FAMILY OF HYDROIDEA. 123 


Clathrozoon wilsont, n. gen. et. n. sp. 


Hydrophyton irregularly sub-dichotomously branched, expanded in one plane fan- 
shaped. Main stem somewhat flattened and ridged, arising from an expanded base, dark 
brown in colour, with the surface showing a series of tortuous grooves. Smaller 
branches cylindrical. The whole composed of a number of branching and 
anastomosing tubes, with chitinous walls complete, except those of the most external 
ones. Hydrothece, which have the form of tubular spaces with chitinous walls, 
project slightly from the surface of all the branches, irregularly placed on 
the main stems, spirally on the branches. The whole, except the external 
openings of the hydrothec, completely enclosed in a thin transparent chitinous 
layer, from which arise very numerous cylindrical tubes enclosing the defensive 


zooids, and which forms also a funnel-shaped collar, projecting beyond the lips of the 
hydrothece. 


Locality—Near Port Phillip Heads, Victoria. Mr. J. Bracebridge Wilson. 


The description of the species is the same as that of the genus, and I have much 
pleasure in dedicating it to Mr. Wilson. 


The specimens were obtained from two spots, each within a distance of five 
miles of Port Phillip Heads, that is, in Bass Straits, close to the Victorian shore. 
They were dredged in water of from twenty to twenty-two fathoms, and were placed 
directly into strong alcohol so that, like all received from Mr. Wilson, they are in 
excellent histological preservation. The polypes are, of course, in a state of retraction, 
and though very many sections from various parts of the hydrophyton have been cut, 
nowhere as yet have I been able to detect the presence of reproductive organs, or of 
individuals modified in connection with these, and though, therefore, unable to give 
any account of the reproductive organs, I have thought it advisable to describe and 
figure the animal carefully so far as can yet be done.* 


The largest colony secured by Mr. Wilson measures 10in. in height, by 4in. in 
greatest width, and at first glance recalls to mind, to a certain extent, one of the 
dark coloured fan-shaped gorgonid forms. A cursory examination, however, at 
once shows that it does not belong to this group of animals. 


If the whole colony be secured, it is found to be attached by a broad flattened-out 
base, attached to some solid structure; from this arises a single large stem, perhaps 2in. 
in thickness, slightly flattened out in one plane, and distinctly ridged (Fig. 1). From 
the edge at either side of the plane lateral branches are given off, varying much in size; 


* That the animal is not at all common is shown by the fact that, though during this summer (1890-91), Mr. Wilson 
has been kind enough to spend a considerable amount of time in dredging, with the special object of procuring more 


specimens, not a trace of this hydroid has been brought up in the dredge, though the same ground which previously 
yielded it has been visited. 


124 A NBW FAMILY OF HYDROIDEA. 


from these other branches are given off on either side, which again divide in a roughly 
but not constantly dichotomous manner, the smaller branches being cylindrical in 
shape. All the branches in the living and spirit-preserved specimens usually le in the 
one plane, but when dried they often become slightly twisted, and thus thrown out of 
the plane. There is thus a considerable resemblance in general appearance between 
the form Clathrozoon on the one hand, and Dehitella and Ceratella on the other, 
especially between the two first mentioned, owing to the rounded branches of 
Dehitella. If, however, we come to examine the structure of the two more minutely, 
we find that the differences are very marked; whilst both have the skeleton in the 
form of a horny network, that of Clathrozoon has more the appearance of being 
composed of a series of anastomosing tubes, and rather less of the appearance of an 
open meshwork than is the case in the Ceratellade ; but, what is of much greater 
importance, it presents on its surface a large number of circular openings at the 
extremities of slightly projecting chitinous tubes, which form true hydrothece. 
These are very distinct from what Mr. Carter and Dr. Gray aptly described as scoop- 
like projections of the chitinous network of the Ceratellade, though they 
unfortunately gave to them the name of hydrothece, that of hydrophore being 
more correct and suggestive of their real function, as at most they can but afford a 
support for the proximal part of the hydranth. 


Skeleton (Figs. 4, 5, 6, 7, 8, 9, 11, 12, 18, 16). 


When the branches of spirit-preserved specimens, with the soft parts present, 
are viewed under the lens, the surface is seen to be covered with a great number of 
tortuous grooves, filled with light yellowish coloured material—the ccenosarcal 
tubes. The edges of the grooves are formed by the chitinous perisare of a dark-brown 
colour (Fig. 6), and arranged in a spiral manner are circular projections, the external 
opening of chitinous cylinders forming the hydrothec and containing the retracted 
polypes: These hydrothece are encircled by the tortuous grooves, and supported by 
extensions of the ordinary perisarc. The whole surface is covered over by an 
extremely thin and delicate colourless layer of perisarc common to the whole branch. 
This layer is not usually recognised until sections are cut, but the whole surface is 
seen to be studded with small cylindrical tubes, which are really formed from this 
thin layer and the spaces in which are continuous with the tortuous grooves below 
the latter (Figs. 7, 8, 9). 


Sections show also that this thin layer rises up somewhat from the general 
surface, and is attached to the lips of the hydrothece ; beyond the margin of the 
latter it is continued on so as to form a very thin collar-like extension, acting as an 
operculum. The arrangement is represented in the figures, especially in Fig. 13, 
which is meant to be a diagram showing the relationship of a hydrotheca to the 


A NEW FAMILY OF HYDROIDEA. 125 


perisarc, as seen in a very thick section cut transversely to the length of a branch. 
This operculum-like structure is very thin and liable to be torn away, but is present 
in all well-preserved and cut specimens. Sometimes it projects as a stiff collar, 
sometimes (Figs. 4, 16) it is thrown into folds, and at others is withdrawn into the 
hydrotheca. With only specimens in which the polypes are completely retracted to 
examine, I cannot say how much of the body of the polype is covered by this thin 
collar when the animal is fully expanded. 


When the soft parts are dissolved away by potash the whole branch appears to 
consist of a meshwork of tubes with chitinous walls (Fig. 11), which anastomose so 
freely that the skeleton appears, in surface view, to consist of an irregular chitinous 
network, which has a considerable superficial resemblance to the skeleton of a horny 
sponge, though this resemblance is even more strongly marked in the case of the 
Ceratellade. On cutting sections, however (Figs. 7, 8, 9), the tubular arrangement can 
be recognised. The structure is essentially identical in the branches and branchlets, 
whatever be the size, the only difference consisting in the greater number of tubes 
entering into the composition of the larger branches as compared with the smaller 
ones. The tubes (Fig. 7) run roughly parallel to the length of the branch, continually 
branching and anastomosing. The spaces which they contain vary much in calibre. 
Towards the exterior the chitinous walls are much stronger and thicker than in the 
interior, and the most external series are incomplete, forming grooves rather than 
tubes. The thin external layer of the branch, previously alluded to, touches the 
chitinous lips of these grooves (Figs. 8, 9), and thus a complete inclosure for the most 
external-lying ccenosarcal tubes is formed. 


Sections also show that the larger circular openings, visible on the outside, lead 
down into tubular spaces, the walls of which are formed of chitinous material similar 
to that of the tube walls with which they are connected. These form the hydrothece, 
and the spaces within them are continuous with one or more of those within the 
tubes surrounding them (Figs. 4, 7,12). The thin external chitinous (?) layer always 
passes up to be attached to the rim of the hydrothece. The cylindrical structures 
(P’) on this thin layer are very simple in form, open at both ends, and serve during 
life to contain the defensive polypes which are directly connected with the external 
layer of ccenosarcal tubes. (Fig. 5). 


Measurements of the Skeleton. 
Diameter of branch taken, ‘7 mm. 


Number of tubes, as seen in longitudinal section, entering into the 
composition of a branch of this size, 7—9; as seen in transverse 
section, 40—50. 


Thickness of the tube, varying, but averaging about ‘07 mm. 


126 A NEW FAMILY OF HYDROIDEA. 


Thickness of wall of tube, 0525 mm. at the exterior, some of those in the 
centre being not more than ‘00525 mm. 


Hydrotheca.— Transverse section, -175 mm. — °1225 mm. 
Hydrotheca.—Longitudinal section, *525 mm. (average). 
Soft Parts. (Figs. 8, 4, 5, 10, 12, 14, 15). 


The chitinous tubes are filled by the ccenosarcal tubes which branch and 
anastomose freely. No one of the latter tubes is more prominent than any 
other. ‘he polypes are distributed over the whole surface, having apparently no 
definite arrangement on the larger stems or branches, but, in the smaller ones, 
a very distinct spiral arrangement (Figs. 6,11). One corresponds to each of the 
hydrothees, seen in the skeleton, and is capable of complete retraction within the 
latter. When thus retracted the opening is protected by the thin collar-like projection 
formed of the outer layer of perisarc mentioned above. 


Each polype has the typical hydroid form. It is somewhat tubular, with a 
conical hypostome, from the base of which arises a single circlet of solid tentacles, 
which vary in number from six to ten, and are provided with minute nematocysts, 
the threads of which are short, stiff, and unbarbed. When the tentacles are retracted 
they curl over towards the mouth, much in the same manner as do those of 
Pedicellina, amongst the Polyzoa. 


The body of the polype is formed of the typical layers—an ectoderm of somewhat 
columnar cells, an endoderm of larger cells less defined in shape, and between the 
two a very strongly marked layer of mesogloea (.00875 mm. in thickest part). From 
the bases of the ectoderm cells pass off long processes (Fig. 14), much more 
strongly marked than is usual in hydroid forms. In its greatest breadth one of 
these fibres measures (0058 mm. ‘They give rise to a circular band of what are 
evidently in function, ‘muscle fibres.” In figure 14 these are represented as seen 
when an oblique longitudinal section of a polype is cut.* Possibly some of them 
may have lost their connection with the ectoderm cells from which they have been 
derived. Hach has a very definite outline and contents, which, when stained, have a 
somewhat granular appearance. ‘They all lie external to the mesoglea, and form a 
very definite band round the body of the polype, the position of which is represented 
in the diagram (Fig. 12). 


Sections, transverse and longitudinal, show that the basal ends of the polypes 
are continuous with more than one (sometimes as many as four or five) of the 


* These bear a considerable resemblance to those described by Weismann as occurring in the ceenosare of Plumularia 
echinulata. See Entstehung der Sexualzellen bei den Hydromedusen, Pl. VIII., Fig. 9b. 


A NEW FAMILY OF HYDROIDEA. 127 


ceenosarcal tubes. In this they resemble the polypes in the group Hydrocoralline. 
The cavities of the polypes and of the meshwork of tubes are hence directly 
continuous. The tubes are formed of the two primary layers with, if present 
at all, an extremely thin layer of mesoglea between them. The endoderm is always 
unilaminar and distinct ; the ectoderm is composed of smaller cells, the nuclei, but 
not the outlines, of which are clearly marked. It appears to be frequently more than 
one cell in thickness, and to be irregular in outline, spirit specimens showing 
projections (Fig. 10) which come in contact with the chitinous walls. Probably 
during life there is very little space between the hard and soft parts. Within the 
ccenosarcal tube are frequently seen large globular structures containing darkly 
staining portions (Fig. 10. x.) 


The whole of the external layer of ccenosarcal tubes is studded over 
with an enormous number of small defensive polypes of very simple structure 
(Figs.8, 5,15). One corresponds to each of the cylindrical structures which rise up 
from the outer thin perisare layer, and consists of a stalk and ahead. The former 
is directly continuous with the ccenosare tube, and consists of an internal axis, the 
nature of which is difficult to determine. It is solid, and contains no prolongation of 
the tubular canal of the canosarc, but appears to be continuous with the endoderm, 

‘though I cannot as yet make out the cellular structure. It is very much shrunken 
in spirit specimens. The outer layer is thin and continuous with the ectoderm of 
the ceenosare (Fig, 15). In spirit-preserved specimens it has the appearance of a 
thin layer of granular protoplasm with nuclei, the diameter of which is greater than 
the thickness of the protoplasmic layer, in which the outline of cells cannot be 
distinguished. No trace of muscle elements can be distinguished. 


The head consists of a little mass of nematocysts, with the remnants of the cells, 
which have given rise to them, and the nuclei of which can be clearly seen. Each 
nematocyst is fusiform in shape, and the whole form a little group lying close to the 
open end of the cylindrical tube, through which the threads can doubtless be ejected. 
None of the nematocysts have the threads put out, and their exact form cannot be 
therefore described. 


In relative size and structure these defensive polypes resemble more than 
anything else the machopolypes of the Plumulariidz, and have no resemblance to the 
defensive polypes of Hydractinia or Podocoryne, whilst none have as yet been 
described in the Ceratellade. 


In figure 3 is represented a diagrammatic restoration of a branch of the colony 
only the soft parts being drawn. The upper surface is supposed to have been cut 
away, and the network of ccenosarcal tubes is shown branching and anastomosing. 
The connection of the alimentary polypes with the tubes is drawn, and the small 


128 A NEW FAMILY OF HYDROIDEA. 


defensive polypes are shown arising from the outermost layer of ccenosarc. The hard 
skeleton parts represented in figure 11 occupy the spaces between the tubes in figure 3, 
the polypes corresponding in position to the large circular openings leading down 
into the hydrothece. The general relationship of the polypes to the skeleton and the 
ccenosarcal tubes is represented diagrammatically in figure 12. 


A ffimties of the Hydroceratinde. 


Clathrozoon differs in important points from any hydroid hitherto described, 
and it is somewhat difficult to determine its affinities, more especially in the 
absence, as yet, of any knowledge of its reproductive elements. 


At first glance it would appear to be related to the Ceratellade, but this is simply 
in consequence of the superficial resemblance in the skeleton of the two groups ; 
each consists of a branching mass of entwined perisarcal tubes, and here the 
resemblance ends, for, whilst the branching network of tubes may be compared with that 
constituting the skeleton of the Hydractiniide and the Ceratellade, there are present two 
structures entirely wanting in the members of these two families, (1) the hydrothecz, and 
(2) the external layer of thin perisarc, with its projecting cylindrical tubes. The first 
of these structures are quite unlike those of any other hydroid in their simple 
shape, the thickness of their walls, the relation of these to the surrounding 
perisarec tubes, and the number of openings leading through the wall into the 
enclosed space. At the same time, if the cavity in the scoop-like projection, formed 
of a small network of perisarcal tubes in the Ceratellade, were to become deeper 
and to penetrate the substance of the branch, and if the branches of the network 
bounding the cavities thus produced were to ‘‘run together’ and thus give rise to a 
tubular structure, in which apertures were left, we should have produced a structure 
similar to the hydrothece of Clathrozoon. ‘The second of these structures is, 
apparently, not present in any other hydroid, and the manner of its origin is difficult 
to conceive. There is no such external layer of ccenosare investing the colony as is 
present in the Hydractinude, and which might be supposed to secrete such a layer. 
On the contrary, the surface of the colony shows a series of much branching tortuous 
perisare tubes, each incomplete externally, and the whole covered in by this thin 
continuous layer, which does not give the idea of having been formed as a separate 
outer covering for each most external tube, though it must apparently have been pro- 
duced in this way. The little cylinders arising from it enclose each, it is important to 
notice, a defensive zooid, which arises directly from the ccenosarcal tube immediately 
below. In one or two of the sections cut transversely near to the end of a growing 
branch, the perisare tubes appear to have a thin imnermost lining distinguishable 
from the rest of the perisarc; possibly this may be comparable to this outer layer, 
but at all events the latter, as shown. in sections, passes continuously from lip to lip 


A NEW FAMILY OF HYDROIDEA. 129 


of the outer grooves, and has nothing to do with any layer lining the latter internally. 
That it is connected in development with the soft structures in these there can be 
little doubt if only on account of its relationship to the protective zooids to which 
they give rise. 


The extension of this layer beyond the mouth of the hydrothece so as to form, as it 
were, an operculum for these, is a curious feature, and one not met with, so far as I am 
aware, in any other hydroid. This particular part is very flexible, being capable of being 
thrown into folds (Fig. 16), or even of being pulled back within the outer rim of the 
hydrotheca by the retreating zooid. Taken altogether the skeleton, though in certain 
respects showing a resemblance to the Hydractiniide and Ceratellade, differs essentially 
from that of these forms in the two important points dealt with above. 


In dealing with the soft structures we find a most curious combination of 
characters, each one characteristic of hydroid forms, belonging to groups perfectly 
distinct from one another. 


The network of ccenosarcal tubes resembles, to a certain extent, that of the 
Hydractinide, Ceratellade and Hydrocoralline, but even here we have to note the 
entire absence of an external continuous layer, characteristic certainly of the first 
and third, and, probably, also of the second group. 


The alimentary polypes are sessile, and distinctly “ claviform,” that is, have 
tubular bodies with a conical hypostome and a single circlet of simple solid tentacles, 
in which points they resemble the genus Clava. Those of the Ceratellade*, on the 
other hand, have scattered capitate tentacles, and in the Oa Eat they are 
provided with a strongly developed hydrocope. 


The gastrozoids again resemble those of the Hydrocoralline, and differ from all 
others amongst the Hydrozoa in being connected with several of the ccenosarcal 
tubes. 


The defensive zooids, or dactylozooids, resemble more than anything else, certain 
individuals characteristic of the Plumulariide, to which the name of ‘« machopolype ” 
has been applied... They consist of a solid stalk bearing a number of nematocysts at 
its free end, each zooid being enclosed in a distinct protective case or nematophore. 


The structure of the gastrozooids thus calls to mind the genus Clava, that of the 
dactylozooids the family Plumulariide, and the relationship of the gastrozooids to 
the coenosareal tubes, the sub-order Hydrocoralline. This combination of characters, 
together with the nature of the skeleton, serves to render the Hydroceratinide distinct 
from any family of Hydroidea yet known, 


* Bale, loc. cit. 


130 A NEW FAMILY OF HYDROIDEA. 
2. A New Species oF PLumuuaria. 


This form was dredged by Mr. Wilson in Port Phillip, and differs, as far 
as I can ascertain, from any yet described. In (1) that the nematophores are 
perfectly independent of the hydrothec, (2) that no intrathecal ridge is present, 
(3) that the hydrothece are cup-shaped, with smooth untoothed margin, and are set 
at some distance apart from one another, the form in question shows the features 
characteristic of the group to which Allman gave the name of Eleutheroplea. 


The arrangement of the hydrothece would prevent it from being placed in any 
of the three divisions—Isocola, Anisocola, and Monopyxis—into which Kirchenpauer 
proposed to divide the genus. 


The species may be described as follows :— 
Plumularia procumbens, n. sp. 


Hydrocaulus upwards of 6in. in length. The whole colony procumbent with 
large polysiphonic branches running in a roughly horizontal direction. From 
one side of these principally arise smaller polysiphonic branches, all lying in one plane. 
From the sides of the branches arise numerous pinne (at largest }in. in length) 
irregularly arranged; in addition to these, hydrocladia (pinnules) may arise direct 
from the hydrocaulus. Two pinnules, alternate, arise from each joint of the primary 
pimne. Pinnules composed of alternate small and large joints, the latter only 
bearing hydrothece and nematophores. Nematophores bithalamic with simple 
terminal aperture, one beneath each hydrotheca, two at the level of the mouth of the 
hydrotheca, all independent of the latter. Two nematophores in the angle between 
the pinnule and main stem of the pinna; nematophores scattered irregularly in great 
numbers over the surface of the polysiphonic stem and branches. 


Colour.—Light-brown stems. 


Hab.—Port Phillip, Mr. J. Bracebridge Wilson. 


The colony reaches a considerable size, and from the fact that the main branches 
run in one direction (Fig. 20) with the smaller ones arising principally from one side, 
it is inferred that in all probability it is procumbent in habit. The branches of the 
hydrocaulus are all polysiphonic and strong, the pinne and hydrocladia, which arise 
from them, being very small indeed in comparison. The two latter are given off all 
round the branches, and reach at most the length of jin., whilst the main branch 
may be 6in. in length. 


Skeleton. 
(a) Structure of large branches (Figs. 24, 25, 26, 27, 28). 


A NEW FAMILY OF HYDROIDEA. 131 


Under the lens the tubes making up the branches can be clearly seen, the 
surface being marked by darkish brown lines, due to the edges of the perisarcal 
tubes seen in optical section (Fig. 25). The tubes on the exterior run parallel 
to one another along the length of the stem, branching very rarely. From the 
surface arise irregularly, and on all sides—(1) large pinnate shoots, the proximal 
parts of which are covered with one or more layers of dark-brown perisare, within 
which only one tubular cavity is contained; (2) smaller branches (hydrocladia), 
corresponding to the pinnules in structure ; (8) a great number of nematophores, 
or protective cases, for the minute defensive zooids which are characteristic of the 
group. 


In transverse section (Figs. 27, 28) the branch is seen to be made up of a great 
number of tubes—as many as 40-50 in a branch of average size—the number varying 
with the size of the branch. 


Each tube has a definite and thick perisarcal wall, which shows clear indications 
of arrangement in layers. In places the cavities within the tubes are seen to be (Figs. 
24, 27, 28) in communication with one another. A striking feature of both trans- 
verse and longitudinal sections is the presence of a distinct central tube, always clearly 
recognisable, both on account of its size and the slightly yellow colour of its walls 
when compared with the surrounding ones (Fig. 24). This central tube, which, from its 
relations to the other parts, is probably to be regarded as homologous with the main 
stem of a monosiphonic form, passes along all the branches of the colony, and from 
it arise every one of the pinne and hydrocladia, though, as will be shown shortly, 
these may be also connected with the other tubes which go to form the polysiphonic 
stem, Professor Allman has figured* in Aglaophenia coarctata a connection existing 
between the various tubes of a polysiphonic stem, and this is most clearly seen in the 
species under consideration. The connection is, however, somewhat different from 
that obtaining in 4. coarctata, which is thus described by Allman :—‘‘ Communication 
is effected by very short processes, which are given off from the component tubes, 
those of two juxtaposed tubes meeting one another and inosculating in such a way 
as to suggest the conjugation of a zygnema.” In longitudinal section (Fig. 24) the 
various tubes are seen to be arranged so that they run parallel to the central one, 
and at intervals their walls are pierced by apertures. Where the pinne and 
hydrocladia pass through, the walls of the latter are connected with those of the 
stem-tubes, and apertures are formed opening into the cavities of the latter, 


(6) Structure of the pinne, etc. (Figs. 21, 22, 23, 25, 26). 


The origin of these from the stem is shown in figure 25, their structure in 
figures 21, 22, and 26. 


*« Challenger” Reports, Hydroidea, Part I., Plumulariide. 


132 A NEW FAMILY OF HYDROIDEA. 


The basal portion of each pinna is strengthened by the development of a very 
strong layer of dark brown coloured perisarc, continuous with that of the tube walls. 
This thick external layer ends abruptly just before reaching the distal end of either 
the first or second joint (Fig. 25). Each jot beyond the first one or two carries 
two pinnules. There appears to be a slight variation in the most proximal joints ; 
sometimes the first, sometimes the first and second, differ from the rest, in bearing 
each only one pinnule. 


The pinnules are alternate, and consist of a varying number of joints, which are 
alternately shorter and longer, the latter only bearing the hydrothece and 
nematophores (Figs. 21, 26). This arrangement is constant in all specimens which 
IT have examined, In other Plumularie the pinnules of which are composed of 
alternately longer and shorter joints, such, for example, as P. setaceoides, goldsteint, 
delicatula,* the shorter ones always bear a nematophore. This is absent in 
P. procumbens. The hydrothece are cup-shaped, with a smooth margin, and are 
placed on the side facing the central stem of the pinna. The most distal pinnules 
carry one hydrotheca each, the proximal as many as six. The cavity is separated 
from that of the jomt by a septum pierced by a circular opening, which lies 
near to the external wall. There is no trace of an intrathecal ridge. 


The nematophores are three in number on each of the larger joints; one is 
placed below the hydrotheca, two at the level of its upper margin. Tach is 
bithalamic with the terminal chamber cup-shaped, and the proximal one somewhat 
canaliculate. The walls are thin (Fig. 22), except where the division into the two 
parts is formed, at which spot they thicken considerably, and give rise to a circular 
ridge projecting upwards into the distal chamber. ‘The opening is single and terminal, 
and each nematophore is only attached by its proximal end, where the walls are thin, 
and may be thrown into slight folds. 


The walls of the pinnule joints show internal ridges, which are always more 
prominent on the side facing the central stem of the pinna, and thin away towards 
the opposite surface. They are always arranged thus—(1) In the larger joints 
there is a ridge close to each extremity, with a third one corresponding in position 
to the septum of the hydrotheca; this varies much in development, being sometimes 
searcely noticeable. (2) In the smaller joints there are uniformly two ridges. (8) 
In the projection from the joint of the pinna bearing the pinnule there is always one 
ridge. Taken altogether the result is that each line of division in the pinnule has 
one ridge immediately on either side of it (Fig. 21). 


In the axil of the pimnules there are present—(1) Two nematophores correspond- 
ing in structure exactly to those described above, (2) between these a curious 


* Bale. Catalogue of Australian Hydroids, Pl. XI. 


A NEW FAMILY OF HYDROIDEA. 133 


structure formed of the perisarc, having the shape of a cone with the apex cut off 
(Fig. 21). The space within the latter communicates by the narrow end with 
the exterior, and by the broader with the cavity of the pinna joint. Into it 
cells of the ectoderm may enter to a slight degree, but more usually it appears 
to be unoccupied (in spirit-preserved specimens), and I am quite unable to 
attach any meaning to it, though it is a perfectly constant structure. It has 
nothing to do with the reproductive structures. Possibly it may serve as a means 
of allowing of the ingress and egress of water to and from the perisarcal tubes. 
Any space between the ectoderm and the perisarc in the very numerous tubes which 
compose the colony must presumably be filled by liquid. The openings leading into 
the hydrothece and nematophores from the stem are small and narrow, and quite 
filled up by the soft parts. When sudden contraction takes place part of the soft 
portions must be withdrawn through these openings and occupy space within 
this perisarcal tube previously, presumably, occupied by fluid. If there be 
some means of expelling this fluid then the sudden contraction of the polypes and 
machopolypes is rendered more easy. It may be that these openings serve this 
purpose. The openings are guarded, as it were, by two machopolypes. 


Soft Parts (Figs. 17, 18, 19, 24). 
(a) Larger branches. 


These are all polysiphonic, The ccenosareal tubes of which each is composed 
may be divided into two divisions—(1) a central one, (2) others varying in number 
and surrounding this. The tubes very rarely branch in such a way that two 
running longitudinally arise from a common one, though (Figs. 24, 27, 28) they 
frequently are united with one another by short transverse branches passing through 
openings in the perisarcal walls. Hach consists of ectoderm and endoderm 
containing a cavity. From the outermost series arise a great number of minute 
machopolypes or defensive zooids. The central one gives origin to all the branches 
passing out into the pinne and hydrocladia, with which the branches are irregularly 
studded. As they pass from the centre to the external surface they are connected 
with a varying number of the surrounding ccenosarcal tubes, a feature which is 
especially marked in the case of the pinne (Figs. 17, 24). ‘This arrangement is 
clearly seen when sections are cut, and has not, so far as 1 am aware, been noted before. 
Bale,* in speaking of the structure of the stem and branches in the Plumulariude, 
says that in most polysiphonic species ‘‘ the primary jointed stem is slender (the 
requisite strength being given by the compound stem, which is only developed as the 
zoophyte increases in size), and the branches spring, not from the jointed stem, but 
from the supplementary tubes which grow up in contact withit. For example, in 


* Genera of the Plumulariide, with observations on various Australian Hydroids. Proc. R. 8. Victoria, 1886. 


134 A NEW FAMILY OF HYDROIDEA. 


Aglaophenia longicornis we find at the back of the original slender-jointed stem a 
stouter secondary tube, and from this spring, at regular intervals, the alternate 
pinnately arranged branches.* . . . fa 28 2) Keeper mr amind the 
hydrorhizal origin of the polysiphonic atin we see thatin A glaophenia longicornis, for 
example, every one of the main pinne is equivalent to a separate shoot of such 
species as A. parvula, a fact which is further illustrated by the presence, near the 
base of the stem in the latter species (and, indeed, in many others), of a long 
oblique joint similar to that which exists near the base of each pinna in A. longicornis. 

: I have not hitherto met es any species with branches springing 
ly ai the jointed stem and the added tubes.” 


It will be seen at once that an important difference exists in this respect between 
the species now described, and those examined by Mr. Bale, and, so far as I am 
aware, any other investigator. Not only is there a very distinct connection between 
the soft and hard parts of all the tubes of the polysiphonic stem, but the central 
one, though distinguishable from the rest, has the same fundamental structure as 
the latter so far as its walls are concerned, and shows no traces of joints.+ The 
question naturally arises What elements are we to consider as entering into the 
structure of the polysiphonic stem in this form ? 


We may regard it as composed of— 


(1.) A central tube equivalent to the hydrocaulus of a monosiphonic form, 
which is surrounded by a series of added but modified hydrorhizal 
elements, or 


(2.) A number of hydrorhizal elements forming branch-like structures, and 
giving off pinne, or 


(8.) A number of hydrocauli in close apposition to one another. 


The last is the most improbable, since, if it were the case, we might expect pinne 
to be given off from all or any of the tubes composing the stem, whilst they all arise 
primarily from the central one. The same objection applies to the second, and the 
distinction which undoubtedly obtains between the central and all the other tubes 
seems to point to the fact that the former is the fundamental portion, the latter being 
secondary structures. At the same time a hard and fast line of distinction between 
hydrocaulus and hydrorhiza cannot possibly be drawn. In some forms of 
Plumulariide we find the pinne arising directly from the hydrorhiza, in others they 
arise from the sides of a hydrocauline structure which grows upwards from the 


* The italics are mine. 


+ At the free extremity of each branch it is continued directly on into a jointed stem forming the centre of a pinna, 
and may probably be regarded as having lost its jointed nature subsequent to its being completely enclosed by the 
surrounding tubes of the polysiphonic stem. 


A NEW FAMILY OF HYDROIDEA. 135 


hydrorliza. Sometimes the structure bearing the pinne, or the central stem of the 
pinne itself, may be strengthened by the addition of tubes clearly growing up from 
the hydrorhiza. These tubes, in some monosiphonic forms, may be feebly developed, 
whilst in typical polysiphonic ones apparently homologous structures may be constant 
and greatly developed. In the former case the distinction between hydrocaulus and 
hydrorhiza is clear enough, but then if the true polysiphonic form be investigated, we 
find that the supplementary structures grow around the primary jointed stem, and (1) 
finally (as in A glaophenia longicornis) give rise to the pinnate branches, just as does the 
hydrocauline tube in such a form as P. falcata, the jointed stem bearing no branches; 
or (2) they form (as in P. procumbens) an enclosing mass for the original tube which 
alone gives off the pinne, though these may be connected with the hard and soft parts 
of the enclosing branches. Thus what must be regarded as homologous structures, 
may either (1) be feebly developed, and retain their original hydrorhizal nature ; or (2) 
be strongly developed and (a) give rise to pinne, and, as it were, usurp the function of 
the original hydrocauline tube which they support, or (6) assume an intermediate form, 
the original tube which they inclose alone giving rise to pinne, with which, however, 
as well as with the former they are in organic connection. 


(b) Pinna, etc. 


There is little to say with regard to the structure of the soft parts contained in 
the pinne ; the hydranths have the form typical of the genus Plumularia, with the 
body divided into two parts by a central constriction, the distal part bearing a single 
circlet of solid tentacles at the base of a broad hypostome, the proximal half being 
somewhat globular and presenting no special feature. 


The machopolypes of the main branches and the pinne are of precisely similar 
structure, corresponding to those of other forms which Lendenfeld has distinguished 
as ‘“‘guard animals with corticating capsules.”* There is no trace of any with 
adhesive cells such as are found in the genus Aglaophenia. 


Each machopolype consists of a proximal tubular part lying in the proximal 
half of the nematophore and a distal swollen part, which contains rounded 
nematocysts. I have been unable to study the living form, and have only seen 
spirit specimens, in which the soft parts are of course much contracted ; in these, 
lines running from the head down the stalk probably indicate muscle fibres, the 
machopolype being capable of great extension. 


In figure 17 is represented a restoration of the soft parts of a small portion of 
one of the polysiphonic stem, together with one of the hydrocladia and pinne which 
arise from it. 


* Zeitsch. f. Wissen. Zool., Vol. XXXVIIL., p. 338. 


136 A NEW FAMILY OF HYDROIDEA. 
(c) Reproductive structures. 


The only specimen bearing reproductive structures was a male colony. The 
gonothece (Figs. 18, 19, 23) are simple and pear-shaped, with a large terminal 
opening and short stalk springing from the axil of a pinnule. Each contains one 
gonophore (Fig. 18), which in longitudinal section is seen to arise from the 
blastostyle and to fill nearly the whole cavity. The blastostyle in the spirit- 
preserved specimen examined was much shrunken with a terminal swelling (D) below 
the opening of the gonotheca. ‘The cell-layers could not be distinguished. The two 
prominent parts of the gonophore are the mass of sperm cells (sp), which stain deeply, 
and the spadix (Fig. 19, end.) Outside the sperm cells a very thin layer of ectoderm 
can be distinguished. I failed after long searching to recognise any trace of 
reproductive elements in the ccenosarcal tubes or blastostyle, or any appearance of 
the formation of more than one gonophore in each gonothece, though in 
P. echinulata Weismann states that very often a second gonophore may be found 
before the contents of the first have passed out.* In P. halecioides also it seems 
that two may be present at the same time. 


* Entstehung der Sexualzellen bei den Hydromedusen, p. 180. 


+ Loc. cit., p. 184. 


DESCRIPTION OF PLATES. 


Plates 17, 18, 19, and 20 refer to Clathrozoon wilsoni. 


Prats 17. 


Figure 1.—The skeleton of a dried specimen of Clathrozoon wilsont, life size, 
from a photograph. 


Figure 2.—Skeleton of part of a colony of Clathrozoon wilsoni, drawn from a 
spirit specimen. 

Puate 18. 

Figure 3.—Restoration of the soft parts. The hard skeleton parts are entirely 
omitted. Only the end of one of the branches of a colony is represented, but this 
is typical of the structure of the whole. The upper surface of the branch is 
supposed to be cut away to show the connection of the gastrozooids with the 
ccenosarcal tubes. The outermost of the latter are studded with the defensive zooids. 
The whole is much magnified, the actual size of the branches being represented in 
figures 1 and 2. 


Figure 4.—Represents a longitudinal section of a small portion of a branch to 
show the connection of a polype (retracted) with the ccenosarcal tubes. In the 
figure the polype is connected with three of these. (A) The perisare walls are shown, 
and the thin external layer forming at the mouth of the hydrotheca an operculum 
P. Outline drawn with the camera under Zeiss A. oc. 2. 


Figure 5.—Transverse section of a small portion of the outermost part of a 
branch to show a defensive polype, connected with one of the outer ccenosarcal tubes, 
which is connected again with a deeper lying one. The defensive poly pe is enclosed 
by the nematophore. LE. is one of the most external tubes, the outer wall of which is 
formed of the thin layer (P.) of perisare, on which lies an accumulation of foreign 
substances, spicules, &c. Outline drawn with camera under Zeiss A. oc 2. 


Puate 19. 


Figure 11.—A small branch much enlarged showing the skeleton only, the soft 
parts having been dissolved in potash. The hydrothece are shown arranged spirally 
and projecting with circular margins slightly from the surface. The network of 
chitinous tubes is seen to represent somewhat in appearance the clathrate horny 
skeleton of certain sponges. The somewhat prominent lines on the surface corres- 


138 A NEW FAMILY OF HYDROIDEA. 


pond to the dark curving ones in figure 6. The thin external layer with the 
nematophores is only shown at the edges, in reality it covers the whole surface. 
Letters as before. x 50. 


Figure 12.—A diagrammatic drawing to show the relationship of the hard and 
soft parts as seen at the external part of a longitudinal section of a branch. A 
gastrozooid is shown partially expanded. Hy. the walls of the hydrotheca. C. 
ccenosarcal tube. Ma. protective zooid arising from the outermost ccenosarcal tube. 
P. the thin external layer of perisarc. P’. the continuation of the latter to form a 
collar beyond the opening of the hydrotheca. P”. the nematophore.  T. tentacle. 


Figure 13.—A semi-diagrammatic drawing of a hydrotheca as seen in a thick 
transverse section of a branch very much enlarged. The walls of the hydrotheca are 
supported by numerous extensions of the perisarcal network, and the openings into 
the internal-lying end of the hydrotheca are shown. ‘The perisare tubes have 
branched and anastamosed to such an extent that their walls form a network, and 
the tubular structure is not so evident as it is in the more deeply lying parts. 
Letters as before. 


Figure 14.—The basal part of a gastrozooid cut obliquely to show the strong 
band of muscular fibres derived from the ectoderm together with the thick layer of 
mesoglea. Ect. ectoderm. End. large granular endoderm cells. M. thick mesog- 
lea layer. Mus. muscle fibres, some in connection with the ectoderm cells, from the 
basis of which they arise, others cut at a deeper level, at which their connection with 
ectoderm cells is not seen. Possibly some have lost their connection with ectoderm 
cells. Drawn under Zeiss F. oc. 2. 


Figure 15.—A defensive zooid highly magnified. It consists of a stalk and head. 
The former is in connection with a ccenosarcal tube one wall of which, as seen in 
longitudinal section is shown. The centre of the stalk is solid and continuous with 
the endoderm, though no cellular structure can be determined. Outside this is a 
thin layer of ectoderm in which nuclei are scattered. The head consists of nemato- 
cysts at the bases of which remnants of the cells in which they have been formed 
can be seen with their nuclei. ct. ectoderm. End. endoderm. M. mesoglea. 
N. nematocyst. Drawn under Zeiss apo. 4.0 mm. apert. 0.95 oc. 12. 


Figure 16.—The collar-like operculum surrounding the margin of a hydrotheca 
seen from above. The collar is thrown into folds. Drawn under Zeiss F. oc. 2. 


Pruate 20. 


Figure 6.—A terminal branch, much enlarged to show the circular openings of 
the hydrothecx, within which the polypes are withdrawn, and also the general spiral 
arrangement of the hydrothece. The surface is covered with tortuous grooves, 


A NEW FAMILY OF HYDROIDEA. 139 


bounded by dark lines, indicating the edges of the perisarc, and is studded with 
nematophores seen at the edges of the branch. Hy. Hydrothece. P. nematophores. 


Figure 7.—A longitudinal section of a small branch, showing the skeleton. The 
tubes of which the branch is composed are seen to be very irregular, but to run, 
especially towards the central part, in a direction generally parallel to the length of 
the branch. E. spaces or grooves, immediately beneath the thin external layer. 
Hy. hydrothece. P. thin external layer of perisarc. PP’. the continuation of P. 
to form an operculum at the mouth of the hydrothece. PP’. the nematophores. 
x 36. 

Fioure 8.—A transverse section of a small branch, to show the tubes of which it 
is composed. The tubes vary in size, and open into one another. The outer ones 
are incomplete externally, forming grooves, the lips of which are usually touched by 
the thin external Jayer of perisare. ‘Two hydrothece are cut through. The perisare 
is thicker towards the outer than in the inner part of the branch. Letters as in 
Fig. 7, x 70. 

Figure 9.—A small portion of the external part of a branch very much enlarged 
to show the roughly concentric layers of which the perisare is formed. Letters 
as in Fig. 7. 

Figure 10.—Small portion of a ccenosarcal tube with the perisare walls from 
the interior of a branch. Ect. the ectoderm in which the outline of the cells cannot 
be clearly distinguished, and which varies in thickness in various parts coming in 
contact, in certain places, with the perisarc walls. End. the unilaminar endoderm, 
the cells of which are larger than those of the ectoderm. x. globular structures of 
unknown significance containing darkly staining parts which lie apparently within 
the cavity of the tube. Drawn under Zeiss F. oc. 2. 


Plates 21, 22, 23 refer to Plumularia procumbens. 


Puate 21. 


Figure 17.—Restoration of the soft parts only of Plumularia procumbens. The 
polysiphonic stem is shown in section with the transverse connections between the 
various tubes which compose it. Down the centre runs the main tube from which 
arise all the lateral branches—pinne and hydrocladia—which are in connection with 
a varying number of the surrounding tubes. The most external ones give off 
numerous machopolypes, and on the pinne are shown the groups of polypes, each 
consisting of one gastrozooid and three machopolypes. One blastostyle is shown 
with a gonophore, arising from the angle between a pinnule and the main stem of the 
pimna. x 30. 


Figure 18.—Longitudinal section of a male gonangium with its contained 
blastostyle and gonophore. In the centre of the gonophore lies the manubrium. Bi’. 


140 A NEW FAMILY OF HYDROIDEA, 


blastostyle. D. swollen distal, end of blastostyle. Sf. sperm. G. walls of 
gonotheca. 


Figure 19.—Transverse section of a male gonangium and gonophore. On the 
left side between the gonophore and the wall are seen traces of the much compressed 
blastostyle. End. endoderm of manubrium. Ect. ectoderm outside sperm cells (sp.) 


Pruate 22. 


Figure 20.—Portion of a colony of Plumularia procumbens showing the poly- 
siphonic stem and the pinne arising irregularly from this, x 1}. 


Figure 21.—Much enlarged portion of a pinnule or hydrocladium to show the 
alternate longer and shorter joints. The latter bears no hydrotheca or 
nematophores ; the former bears a hydrotheca with the nematophores at 
the level of the mouth of the former, and one in the median line 
below. The thickenings in the walls of the pinnule are shown in their positions 
and the two nematophores in the axil between the pinnule and the main stem of the 
pinna, and at A, the conical structure opening to the exterior. N'. upper pair of 
nematophores. NN. lower median nematophores. N*. nematophores in the axil of 
the pinnule and pinna stem. A. conical process in the axil leading from the interior 
of the pinna to the exterior. 


Figure 22.—Much enlarged view of a nematophore seen in optical section, and 
showing the two chambers. 


Figure 23.—Much enlarged view of a male gonangium. 


Figure 24.—Semi-diagrammatic drawing of a longitudinal section of the poly- 
siphonic stem of the same to show the relationship of the hard and soft parts and the 
distinctness of the central tube with its walls slightly yellower than those of the 
surrounding tubes. C. central tube. H. central stem of pinna. H/’. hydrocladia. 
L. lateral tubes. N.nematophores. T. transverse connections uniting the various 
tubes. x 80. 


Prate 23. 


Figure 25.—Much enlarged view of the termination of a polysiphonic stem, 
showing the numerous nematophores on the stem and the pinne &c., arising 
irregularly. The basal parts of the pimne are strengthened by the formation of a 
thick perisare wall continuous with that of the tubes forming the stem. x 20. 


Figure 26.—A highly magnified portion of a pinna. 


Figures 27 and 28.—Transverse sections of the polysiphonic stem to show the 
component tubes—skeleton only—with the large central one, from which in figure 28 
a pinna is arising. The external tubes are studded with nematophores. 


Trans, PS Victoria. Plate 17 


CLATHROZOON WILSONI. 


Trans, PRS. 


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42, 


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Trens. PS. Vicforla. Flate 12 


Th 
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WB Spencer, del perce 


Trans, US. Vicloria. Flate C0 


= 
4 
: 


ve 


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(~) Vieloria Flate Cf 


Trans 


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Trans. PS Victoria Flale Ce 


Fig 23 


—_ 


Kress aN 
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WB. Spencer del. 


v 


Teens. LeiS. Victoria Plate 23. 


W.B. Spencer del Yi C Troedel & C? Lith Melb. 


" i A 
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Key 


avy 


TRANSACTIONS 


h 


OF THE 


ROYAL SOCIETY OF VICTORIA. 


VOL: PART II. 


1891. 


CONTENTS. 


ON THE OCCURRENCE OF THE GENUS BELONOSTOMUS IN THE 
ROLLING DOWNS FORMATION (CRETACEOUS) OF CENTRAL 
QUEENSLAND, sy R. Erueriper, Junr., PALEONTOLOGIST TO THE 
GroLoaicAL Survey or New Sourn Wates, SypNEY, AND ARTHUR 
Smith Woopwarp, F.Z.S., &c., oF THE DrparTMENT oF GEOLOGY, 
British Muszum (Nat. Hist.), Lonpon. (With Plate 1) - = - 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY), sy W. Batpwin 
Spencer, M.A., Proressor or Brotoay in THE UNIVERSITY OF 
Metsourne. (With Plates 2, 3, and 3a.) - : : - - 


ADDITIONAL OBSERVATIONS ON THE VICTORIAN LAND 
PLANARIANS, sy Artuur Denpy, D.Sc. (With Plate 4) : : 


LAND PLANARIANS FROM LORD HOWE ISLAND, sy W. Batowin 
Srencer, M.A., Proressorn or Brotogy IN THE UNIVERSITY OF 


Metsourne. Parr I.—Description or Species. (With Plates 5 and 6.) 


EDITED BY PROFESSOR W. BALDWIN SPENCER, M.A., HON. SEC. 


J" MELBOURNE. 


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TRANSACTIONS 


OF THE 


RON SOCIETY OF “ViCTORiLA 


VOR: PART II. 


1891. 


CONTENTS. 


ON THE OCCURRENCE OF THE GENUS BELONOSTOMUS IN THE 
ROLLING DOWNS FORMATION (CRETACEOUS) OF CENTRAL 
QUEENSLAND, sy R. Erneriper, Junr., PALEONTOLOGIST TO THE 
GroLogicaL Survey oF New South Watses, SypDNEY, aND ARTHUR 
Smith Woopwarp, F.Z.S., &c., or THE DEPARTMENT oF GEOLOGY, 
British Museum (Nar. Hist.), Lonpon. (With Plate 1) - 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY), sy W. Batpwin 
Spencer, M.A., Proressor oF Biology IN THE UNIVERSITY OF 
Mexpourne. (With Plates 2, 3, and 38a.) 2 2 z 2 - 


ADDITIONAL OBSERVATIONS ON THE VICTORIAN LAND 
PLANARIANS, sy Artuur Denny, D.Sc. (With Plate 4) s 2 


LAND PLANARIANS FROM LORD HOWE ISLAND, sy W. Batpwin 
Spencer, M.A., Proressor or BrioLogy IN THE UNIVERSITY OF 


Mesourne. Part I.—Description or Species. (With Plates 5 and 6.) 


EDITED BY PROFESSOR W. BALDWIN SPENCER, M.A., HON. SEC. 


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FEBRUARY, 1892. 


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ARTICLE I.—On tox OccurRENCE oF THE GENUS BELONOSTOMUS IN THE ROLLING 
Downs Formation (CRETACEOUS) OF CENTRAL QUEENSLAND, BY R. ETHERIDGE, 
JunR., PALEONTOLOGIST TO THE GEOLOGICAL SuRvEY oF New Sours Watgs, 
Sypney, anp ArTtHUR SmitH Woopwarp, F.Z.S., &c., of THE DEPARTMENT OF 
Grotocy, British Museum (Nat. Hist.), Lonpon. (With Plate I.) 


I. Iyrropvuction. 


The fine specimen about to be described was entrusted to our care by Mr. 
George Sweet, of Brunswick, Melbourne, by whom it was obtained when on a 
collecting tour in Central Queensland, during the year before last (1889); together 
with many other very interesting fossils, which one of the present writers hopes some 
day to have the pleasure of working out. 


The principal fossil exhibits a long, slender fish, with deep narrow ganoid scales 
and feeble fins, bent upon itself at about the middle point, and wanting the greater 
part of the head. The remains are preserved on counterpart slabs, one side being 
shown, reduced one-half in Plate I., Fig. 1, while various details are illustrated of 
the natural size in the accompanying Figs. 2-7. 


The information afforded by this specimen is supplemented by four other 
fragments in a similar matrix, numbered M. 31, M. 26 A, M. 28, and M. 80 respectively. 
The first exhibits an imperfect cranium, much fractured and imbedded in hard rock. 
In the second the remains of the gill arches are preserved. No. M. 28 shows part 
of the operculum, supraclavicle, supratemporals, and adjoining scales in counterpart ; 
and No. M. 80 isaconnected series of six large vertebral centra, bearing parts of their 
arches. Taken together, the specimens make known nearly all the more important 
features in the skeleton of the fish; and it is at once obvious that we are concerned 
with an unusually large species of the well-known Upper Mesozoic ‘“ Ganoid ” 
Belonostomus*, and with which we have much pleasure in associating the name of 
Mr. Sweet as B. sweets. 


Species that are apparently allied have already been recorded from the Upper 
Cretaceous of Western Europe, India, and Brazil; and the present discovery is of 
great interest as extending still further the ascertained geographical range of the 
genus during Cretaceous times. 


* L. Agassiz, Poiss. Foss., 1884, II., Pt. 2, p. 140. 


2 ON THE OCCURRENCE OF THE GENUS BELONOSTOMUS IN THE 


2. Previous Notices oF FIsH-REMAINS IN THE Roxiiinc Downs Formation. 


The first record of the existence of fish-remains in the immense expanse of 
rocks, now termed by Mr. R. L. Jack, Government Geologist of Queensland, the 
‘* Rolling Downs Formation,” is due to the late Mr. Charles Moore, of Bath, England, 
who found numerous fragments of teeth and scales in the Wollumbilla blocks 
submitted to him by the late Rev. W. B. Clarke, M.A. He regarded the teeth and 
certain of the scales as those of Hybodus, and other scales as representing the genus 
Lepiodotus.* Subsequent researches have so far failed to reveal further traces of these 
genera. 


The next reference to Australian Cretaceous fish with which we are acquainted 
is the brief record by Mr. R. Etheridge, F.R.§., of the caudal portion of the vertebral 
column and several scales of Asfidorhynchus in the Hughenden beds,+ Central 
Queensland, associated with Ammonites, and other fossils of Cretaceous age. 


After a lapse of some years, Mr. R. L. Jack, whilst engaged with General 
Fielding in the exploratory traverses for the Queensland Trans-Continental 
Railway, discovered at Kamilaroy, Leichhardt River, a bed of magnesian limestone, 
containing, with other fossils, sharks’ teeth and small vertebre.{ The associated 
fossils clearly proved this bed to belong to that portion of the great Rolling Downs 
Formation extending from Cloncurry to Hughenden. These remains were 
determined by one of us to be the teeth of Ofodus appendiculatus, Ag., and the 
vertebree those of a small Teleostean fish. Subsequent to this these teeth were 
described and figured,|| together with a portion of the vertebral centrums of a large 
Lamna from the Walsh River beds of the Rollimg Downs Formation. This interesting 
specimen forms a portion of the collection of the Queensland Museum, Brisbane, and 
was kindly communicated by Mr. C. W. de Vis, M.A., the Curator of that Institution. 
For the Selachian of which these bones formed a portion, the name of Lamna 
daviesii was proposed. ‘The old genera, Otodus and Lamna have now been united, { 
and in consequence the teeth before mentioned must in future be known as Lamna 
appendiculata. What relation they may bear to the vertebrie of L. daviesii remains 
for the future to prove. 


No other remains of Fish have been described from the Rolling Downs 
formation. 


* Quart. Journ. Geol. Soc., 1870, XXVI., p. 238. 
+ Quart. Journ. Geol. Soc., 1872, XXVIII., p. 346. 


t Reports on the Geological Features of Parts of the District to be traversed by the proposed Trans-Continental 
Railway. Queensland Parl. Papers, 1885 (pp. 22, feap., Brisbane, by Authority, 1885), p. 8. 


§ R. Etheridge, Jun. Appendix to R. L. Jack’s Report, loc. cit. 
|| Proc. Linn. Soc. N.S.W., 1888, III (2), Pt. I., p. 156. 
4; A.S. Woodward, Cat. Foss. Fishes Brit. Mus., 1889, p. 392. 


joy) 


ROLLING DOWNS FORMATION (CRETACEOUS) OF CENTRAL QUEENSLAND. 


3. Belonostomus sweett, sp. Nov. 


The state of preservation of the large fossil does not permit any precise estimate 
of the original proportions of the fish. Judging, however, by the analogy of the 
allied Brazilian species, the trunk cannot have been less than 0°9 in length, with a 
maximum depth of 0-14 in the abdominal region ; while the head, with the opercular 
apparatus, may have added about 0-4, making the total length approximately 1:3. 
The individual under consideration is thus and by far the largest member of the 
genus hitherto discovered. 


(a.) Head and Opercular A pparatus.—As shown by the fragment M.31, the cranium 
is well ossified in the occipital, otic, and prefrontalregions. The exoccipital extends 
considerably into the lateral wall of the brain-case, and is bounded in front by a large 
pro-otic element, separated only by suture, extending downwards to the base of the 
cranium, and exhibiting near its hinder border a large oval foramen, evidently for the 
exit of the glosso-pharyngeal nerve. The membrane bones of the cranial roof are 
thick; and there is a robust parasphenoid bone, expanding in front of the orbit. The 
jaws are not preserved, and the only element of the suspensorium exhibited is the 
hyomandibular, which lies beneath the opercular apparatus of the left side in the 
large fossil. As usual in Belonostomus, this bone is lamelliform, with a much 
expanded, squamous, inferior moiety, and a narrow, more robust, superior portion, 
from which at the hinder border would arise a short, stout process for the articulation 
of the operculum. Externally, remains of large suborbital membrane bones 
(Fig. 1, so.) are conspicuous between the orbit (orb.), and the preoperculum (p.0f.) ; 
these being ornamented with coarse tuberculations rarely fused into irregular ruge. 
The preoperculum (f.0f.) is a deep triangular bone, tapering, though notably 
robust, above, and terminating in a truncated expansion below. Its upper extremity 
reaches a point not far below that of the operculum, and the length of its inferior 
border exceeds half the height of the bone. The operculum (of.) is approximately 
quadrate in form, with a somewhat truncated and rounded postero-superior 
angle. Its maximum depth and breadth are nearly equal; the upper border 
is somewhat turned inwards, and the articular pit (a) for the reception of 
the process from the hyomandibular is especially prominent near the antero- 
superior angle. The sub-operculum (s.of.) is comparatively small, deepest and 
truncated in front, gradually tapering to a posterior apex at the postero-inferior angle 
of the operculum. All these bones are superficially ornamented with prominent 
tuberculations of ganoine, which are partly fused into irregular radiating series, but 
still more conspicuously arranged in concentric lines. 


(b.) Branchial Apparatus.—As shown by the small fossil M. 26 A, the gill-arches 
are slender, and shaped like those of modern Teleosteans, being a series of narrow, 


4 ON THE OCCURRENCE OF THE GENUS BELONOSTOMUS IN THE 


elongated lamin, —-shaped in transverse section. To each arch is affixed a close 
series of long, slender, compressed appendages, only superficially calcified, and 
apparently to be interpreted as supports of the gill-filaments. 


(c.) Axial Skeleton of the Trunk.—The vertebral centre (Figs. 2 and 3) are well 
ossified throughout, and the slender neural and hemal arches, with their spines seem 
to be fused to them. They are deeper than long, and so far as can be determined 
from impressions of the terminal coneavities (Fig. 3), the notochord was completely 
constricted, no central perforation of the bone being distinguishable. A secondary 
development of longitudinally-fibrous bone completely surrounds the primitive 
double-cone of each centrum externally, and imparts to the vertebra the robust 
appearance well shown in Fig. 2. 


(d.) Appendicular Skeleton.—Of the fins, only fragmentary remains of the 
pectoral and caudal are preserved in the large fossil (Fig. 1). The rays are all robust, 
laterally compressed, undivided for some distance proximally, but soon branching 
and marked by numerous articulations. Of the supporting elements, nothing can be 
discerned, and even of the membrane bones accompanying the pectoral arch there 
remains little evidence. It is clear from the small fossil, M. 28, that there was a 
pair of large supra-temporal bones externally ornamented with tubercles fused into 
radiating and somewhat reticulating ruge. The same specimen also exhibits a small, 
triangular, supraclavicle, adjoining the truncated postero-superior angle of the 
operculum, and ornamented with tubercles of irregular size, partly fused into 
concentric lines. Of the clavicle and pectoral arch itself, however, there are no 
fragments sufficiently worthy of note. 


(e.) Squamation.—As usual in Belonostomus one series of flank scales is 
excessively deepened, these being abruptly truncated below, but slightly rounded 
and reflexed forwards at the upper extremity. A restoration of one example 
from the anterior abdominal region is given, of the natural size, in Fig. 4. This 
scale is about five times as deep as broad, crossed at its flexure by the lateral line ; 
and the overlapped portion is relatively narrow. Immediately posterior to the 
hinder margin of the overlapping scale is an area of nearly smooth ganoine, bounded 
by a nodose longitudinal ridge. A parallel and more prominent longitudinal ridge, 
separated from this, and from the hinder area by a furrow, divides the scale into two 
nearly equal halves, and the posterior half is much ornamented. This ornament 
consists first of large irregular tubercles, passing behind into small, nearly parallel, 
though sometimes bifurcating transvere ridges, at right angles to the posterior 
border. ‘The scale immediately below the principal flank series is much deeper than 
broad, and then follow about four small vential scales, equally broad, but their depth 
not exceeding half their breadth. One of the latter is shown, somewhat restored, in ~ 
Fig. 5; its overlapped superior border, with the large articular spine, is conspicuous, 


ROLLING DOWNS FORMATION (CRETACEOUS) OF CENTRAL QUEENSLAND. 5) 


and there are some superficial ruge in the lower half of the scale parallel with its 
inferior border. The squamation above the principal flank series is partly shown in 
the hinder half of the trunk, and some of the scales are well preserved (Fig. 6). 
There are at least two series between the upper extremity of the principal scale and 
the dorsal azygous series, both comprismg imbricated rhomboidal scales, well 
ornamented with ruge of ganoine, and each with a prominent oblique ridge in the 
middle of its exposed portion, almost diagonal; the ruge are partly concentric 
with the hinder and inferior borders, partly at right angles to the former. Towards 
the extremity of the tail the flank scales gradually become less deep in proportion 
to their breadth, and at the origin of the caudal fin, all the scales of each ventral 
row are of nearly equal size (Fig. 7), rhomboidal, and closely resembling the 
ordinary dorso-lateral scales, except that the diagonal has become more prominent, 
and few of the rugz are concentric with the borders. 


4,—Sprciric DETERMINATION. 


In the absence of definite information as to the proportions of the species now 
described, it is necessary to refer exclusively to the scales for diagnostic characters. 
It seems, however, almost certain that we are concerned with a much less slender 
fish than the typical Jurassic species, Belonostomus tenutrostris, B. sphyrenoides,* &c.; 
while neither of these, so far as we can discover, exhibit so conspicuous and elaborate 
a superficial ornamentation. It thus suffices to refer only to the known 
Cretaceous species, which may be enumerated as follows :— 


Belonostomus attenuatus, Dixon, Geol. and Foss., Sussex, 1850, p. 368, Pl. XXXV., 
f. 4 [Portion of mandible], Chalk, Sussex. 


Belonostomus cinctus, Lu. Agassiz, Poiss. Foss., 1844, Vol. IL., Pt. IL., p. 142, 
Pl. LXVIa, Figs. 10—13; F. Dixon, op. cit., p. 367, Pl. XXXYV., Fig. 3; 
A. 8. Woodward, Quart. Journ. Geol. Soc., Vol. XLIV., p. 145, Pl. VIL, 
Figs. 7—13, and Proce. Geol. Assoc., Vol. X., p. 805.—Chalk; S.E. England. 
(Mandible and scales. ] 


Belonostomus comptoni, Agassiz, A. 8. Woodward, Proc. Zool. Soc., Nov. 18th, 
1890. Aspidorhynchus comptoni, Li. Agassiz, Edin. New Phil. Journ., 
1841, Vol. XXX., p. 83, and Comptes Rendus, 1844, Vol. XVIIL., 
p. 1009.—Upper Cretaceous; Serra de Araripe, North Brazil. {Imperfect 
fishes. | 


* L. Agassiz, Poiss. Foss., II., Part 2, p. 140; A. Wagner, Abth. Math. Phys. Cl. K. Akad. Wien, 1863, IX., 
p- 689. 


6 ON THE OCCURRENCE OF THE GENUS BELONOSTOMUS IN THE 


Belonostomus crassirostris, O. G. Costa, Pal. Regno Napoli, Pt. II., p. 33, 
Pl. IL., Figs. 1, 2. Belonostomus gracilis, O. G. Costa, ibid., p. 35, 
Pl. Il., Fig. 8.—Upper Cretaceous; Pietraroja, near Naples. [Imperfect 
fish. ] 


Belonostomus (?) indicus, A. S. Woodward, Rec. Geol. Surv. India, 1890, Vol. 
XXIII., p. 28. Upper Cretaceous (Lameta beds) ; Dongargdon, Nagpur, 
India. [Imperfect skull and mandible. | 


Belonostomus lesinensis, F. Bassani, Denkschr. math.-naturw. Cl. k. Akad. 
Wiss. “Wien, “1882; Vol OULV qt) 198.0 Ply a. Pao MOx? Tipper 
Cretaceous; Isle of Lesina, Dalmatia. [Imperfect fish.] 


Of these species B. attenuatus, and B. ? indicus, are not strictly comparable, 
being known only by parts of the head; but the absence of ornamentation on these 
fossils renders most improbable any intimate relationship with the Queensland fish. 
The feeble character of the ornament of B. cinctus, which is known by scales, as 
well as jaws, also excludes this species from comparison. 8B. crassirostris, and B. 
sleinensis are small slender fishes, apparently as much elongated as any of the 
Jurassic species. Indeed, the only form which seems to approximate at all closely 
to the species now under consideration is the large B. comptoni from Brazil. The 
few proportions that can be compared are very similar, and the superficial 
ornamentation in adult fishes is equally conspicuous. The principal flank scales of 
B. comptoni, however, never appear to exhibit the prominent, fine, transverse 
striations, so characteristic of the hinder margin of all the flank scales of B. sweeiz, 
and we thus venture to regard the latter as specifically distinguished by its superficial 
ornament. 


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ROLLING DOWNS FORMATION (CRETACEOUS) OF CENTRAL QUEENSLAND. 


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DeEscRIPTION oF FiGurReEs. 


Fig. 1.—Portion of fish, with remains of opercular apparatus. 
op. operculum. 
p.op. pre-operculum., 
s.op. sub-operculum: 


orb. orbit, half nat. size. 


Fig. 2.—Portion of a vertebra, side view, with parts of the neural and 


hemal arches. 
Fig. 3.—The same, end view. 
Fig. 4.—Restoration of a scale from the anterior abdominal region. 
Fig. 5.—A ventral scale, somewhat restored. 
Fig. 6.—Scales from above the hinder principal flank series. 


Fig. 7.—Scales of one of the ventral rows at the origin of the caudal fin. 


ARTICLE II.—On tHe Srructure or CERATELLA Fusca (Gray), By W. BaLpwin 
Spencer, M.A., Proressor or Bionogy In THE University or MELBOURNE. 
(With Plates 2, 3, and 3a.) 


(Read Thursday, June 11th, 1891.) 


IT have to thank Dr. Ramsay and the Trustees of the Australian Museum, 
Sydney, for the opportunity of examining the structure of this interesting hydroid 
form. The specimens examined came from Bondi on the New South Wales coast 
and from Lord Howe Island, where they were collected by Mr. Whitelegge of the 
Australian Museum, whom I have to thank for kind assistance. The Lord Howe 
Island specimen had the zooids beautifully expanded. 


Dr. Gray* was the first to describe and figure Ceratella and the closely allied 
genus Dehitella from specimens in the British Museum. He had dried specimens 
only at his disposal and his description necessarily refers only to the hard parts 
and these having the form of a horny network somewhat resembling in general 
appearance the skeleton of a horny sponge, led him to place the two forms 
provisionally amongst the sponges. For their reception he constituted the family 
Ceratellade. Five years later Mr. H. J. Carter+ published a paper entitled 
“Transformation of an Entire Shell into Chitinous Structure by the Polype 
Hydractinia, with short Descriptions of the Polypodoms of five other Species.” In 
this he refers to Ceratella fusca and Dehitella atrorubeus and describes two new forms 
belonging to the former genus under the names of C. procumbens and C. spinosa. 
Both of these came from South Africa the former from the Cape of Good Hope and Natal 
the latter from Natal. In the same paper he describes a new genus Chitina with a 
single species C. ericopsis which came from New Zealand. Reference to these will 
again be made after the anatomy of Ceratella fusca has been described, meanwhile 
it is sufficient to note that Mr. Carter’s investigations of a species of Hydractinia 
(H. levispina) with a skeleton composed of a horny network which incrusts and eats 
its way into univalve shells led him to re-examine the two forms placed by Dr. Gray 
in the family Ceratellade and in consequence of his finding undoubted traces of 
thread-cells in the dried specimens both of these and of the two new species 
of Ceratella mentioned above, he rightly recognised them as belonging to the 


* Proc. Zool. Soc., Nov., 1868. 
+ An. and Mag. Nat. Hist., Jan., 1873. 


ON 'THE STRUCTURE OF CERATELLA FUSCA (GRAY). 9 


Hydroidea and not to the sponges in which group Dr. Gray had provisionally placed 
them. At the same time it may perhaps be well to note that the finding of 
thread-cells in dried specimens with a skeleton in the form of a horny network 
is not in itself absolute proof of their belonging to the Hydroidea inasmuch as at the 
present time sponges are known to exist the substance of which is pierced by hydroid 
erowths so that it would be possible to find thread-cells in the dried skeletons of 
sponges. At the same time Mr. Carter was perfectly right, as events have proved, in 
removing the Ceratellade from the Porifera though the subsequent discovery by 
Mr. Bale of the nature of their soft parts has shown that they cannot be placed, 
where Mr. Carter put them, in the family Hydractinude. 


The next notice of these forms occurs in the Proceedings of the Linnean Society 
of New South Wales for 1886 (p. 575) when Mr. Brazier recorded the occurrence of 
Ceratella fusca from various localities near Sydney such as Bondi Bay and Coogee. 
In the Proceedings of the same Society for the year 1888 (p. 745) Mr. Bale for the 
first time gave some description of the soft parts and showed that the zooids were 
formed on a very different type from those of the Hydractiniide. The latter have a 
single circlet of filiform tentacles surrounding the hypostome whilst those of Ceratella 
are irregularly distributed over the body and are capitate. Mr. Bale accordingly 
removed Ceratella from its position amongst the Hydractiniide assigned to it by 
Mr. Carter and placed it in a distinct -family to which he gave the name Ceratellide. 
He apparently overlooked the fact that Dr. Gray had already adopted the name of 
Ceratellade for the family including his two genera Ceratella and Dehitella, so that 
this name given in 1868 must now be retained. With a more abundant supply of 
material I have been enabled to work out the structure in greater detail than was 
possible to Mr. Bale to whom we owe the first description of the soft parts and 
the determination of the fact that Ceratella belongs to a family distinct from the 
Hydractiniide. 


DeEscRIPTION OF THE STRUCTURE OF CERATELLA FUSCA. 


I have endeavoured so far as possible to give a complete account of the anatomy 
of both soft and hard parts the only figures yet published being those of the external 
form given by Dr. Gray* both of which suffice to clearly identify the genera. 


Skeleton. 


The colonies of Ceratella procured on the New South Wales coast measure from 
14—5 inches in height and are of a rich brown colour. The largest specimen which 
Ihave seen is the one procured by Mr. Gabriel which came from Flinders Island 
in Bass Straits where it had been washed ashore. ‘The figure given by Dr. Gray 


Maca Clits 


10 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


represents fairly well the macroscopic characters of the skeleton but conveys the idea 
of one which has been much water-worn and has lost many of its smaller branches. 
The branching is much richer and closer than is represented by him and the 
projecting hydrophores are more distinct and regular. At the same time there is a 
certain amount of difference in the growth of various colonies some of which are 
more bushy in appearance than others. That secured by Mr. Gabriel has the 
branches more distinctly arranged in one place than is the case with the others. 
The whole colony may be described as follows:—The colony arises from a much- 
branching root-like base encrusting foreign objects. The root-branches unite to 
form a strong stem common to the colony which is flattened in the same plane as 
that in which the branches of the colony, generally, expand. The common stem 
may have the appearance of being formed of intertwined branches and from it arise 
irregularly larger or smaller branches the former being more or less flattened in the 
same plane with itself. 


From the larger arise irregularly on either side smaller branches which again 
branch until a somewhat bush-like or fan-shaped colony is formed the whole being 
more or less flattened in the plane of the maim stem. Except the main stem close 
to the root branches and the latter all the branches may bear  bracket-like 
projections—the hydrophores—which are arranged in a roughly spiral manner and 
are especially abundant on the smaller branches except the growing ends which are 
somewhat swollen and flattened in a plane at right angles to that in which the 
branching of the colony takes place. 


In addition to considerable variations in the general form of the colony some 
appear to have the hydrophores so arranged that they le along the two opposite sides 
only of the branches whilst in others they are arranged all around. The more 
bush-like the growth is, to the greater extent does the latter obtain and vice versa. 
Usually there is only one main stem arising from the root-branches but at times one 
or more smaller ones may arise independently. (Fig. 1.) 


The skeleton when examined by the lens has much the same appearance as that 
of Hydractinia and differs considerably from that of Clathrozoon and more still from 
that of the polysiphonic stem characteristic of certain species of Plumularia. It forms 
in the larger branches a meshwork of chitinous tissues so similar at first sight to 
that of certain horny sponges that as Mr. Bale says ‘‘a portion broken off and 
examined separately might well be mistaken for sponge tissues.” ‘This however is 
only true with certain limitations for, if the soft parts are present, the distinction 
between the two is readily seen as is also the case when the hydrophores are present. 
Apart from this also nothing comparable to the layer of cells secreting the sponge 
skeleton is present nor are the chitin fibres of the two similar in their minute 
_ structure. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). el 


The meshwork is extremely irregular in the larger branches as is shown in the 
sections represented in figs. 9 and 11. There seem to be two not clearly 
distinguishable portions present (1) large and strong fibres (2) smaller ones which 
form connecting bars and often have the appearance of thin web-like plates which 
are especially well developed on the hydrophores. Fig. 5 represents a medium-sized 
branch, from which the soft parts have been removed by potash, seen by reflected 
light. At times the fibres seem to run for some distance parallel to the long axis of 
the branch though this is much more strongly marked in some branches than in the 
one figured. There are no definite hydrothece present within which the zooids can 
be completely retracted but the branches are studded sometimes only at the sides 
sometimes all over with little bracket-like projections which give a characteristic 
‘serrate appearance to the branches, very different however from that which is 
produced by the hydrothecx of the Sertularians. Mr. Bale has aptly suggested that 
the term ‘‘ hydrophores” (originally applied by Allman to the calyces of Halecium) 
should be used to describe these structures which form merely supports for the 
hydroid zooids. Each one may perhaps be best likened to a very concave scallop 
shell with ribs formed by the strong fibres continuous with those of the branch whilst 
the spaces between them are filled up by a thin fenestrated web of chitin. In some 
hydrophores the ribs are more strongly marked than in others and project as small 
points around the margin. (Figs. 5 and 6.) The growing ends of the smaller 
branches usually contain two or three longitudinal fibres connected by transverse 
bars, often somewhat web-like, and each of these growing ends is clearly 
distinguishable (1) by its being flattened in a plane at right angles to that in which 
general growth takes place and (2) by the entire absence of hydrophores and zooids. 
It may be added that the longitudinal arrangement of the fibres in the branches is 
more clearly noticeable in specimens with the soft parts present than in those in 
which the latter are absent since the soft parts conceal from view largely the 
connecting and the deeper-lying fibres and thus prevent to a large extent the network 
structure from being seen. The whole skeleton also in living specimens is 
completely enclosed by the soft parts though only a thin layer of tissue is present 
over the external surface. (Figs. 9, 10and11H.) There is no protective covering 
for the reproductive structures. 

Soft Parts. 


The structure of these has, as yet, been only briefly described once and that by 
Mr. Bale, whose short account refers only to the external form of the hydroid zooids. 
He pointed out, as stated before, that these possessed irregularly scattered capitate 
tentacles and that hence they differed considerably from those of Hydractinia. 

Amongst the specimens from the Australian Museum is one collected by 
Mr. Whitelegge on Lord Howe Island with the zooids fully expanded and others 
with the soft parts well preserved. 


12 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


(1). Hydroid zoords (Figs. 2, 4, 6, 7, 9, 13).—These may be found on all the 
branches, large and small except at the growing ends. Often also they are absent on 
the larger main branches and are always fewer in number on these than on the 
smaller ones (Fig. 4). Each zooid, in a well preserved spirit specimen, reaches a 
length of about 1-4 m.m. and in the general form of the body resembles, as Mr. Bale 
says, those of Coryne. The body (Figs. 4 and 6) is somewhat elongate with a 
terminal almost conical portion, at the apex of which lies the mouth opening. The 
basal portion which is seated upon the hydrophore is broad, this is followed 
by a shghtly contracted portion, then comes a slightly swollen part which gradually 
diminishes in size towards the mouth end. Over the surface are scattered irregularly 
the capitate tentacles from 10-14 or perhaps even more in number (Figs. 4 and 6), 
and one or two of these are frequently placed close to or upon the basal region. 


The minute structure is generally that which is typical of hydroid forms and is 
represented in Figs. 2 and 7. The ectoderm (£ct.) is unilaminar over the general 
surface the cells being in close apposition each with a large nucleus and except in 
the capitate ends of the tentacles there are no thread cells present. At the ends of 
the tentacles the ectoderm is swollen out and apparently forms a mass of cells in 
which large nematocysts are present with barbed threads (Fig. 7). The nematocysts 
here and elsewhere seem to be all of the one size. The ectoderm lies on a thin layer 
of mesogloea scarcely visible in extended zooids but more prominent in retracted 
ones. There cannot be detected any fibrous muscular elements such as form so 
distinct a feature around the basal region of the zooids in, for example, Clathrozoon. 
The endoderm consists of large vacuolate cells each one subtending the base of, as a 
general rule, at least three ectoderm cells. The protoplasm appears to be always 
concentrated at the inner ends where the nuclei are placed and where in preserved 
specimens the cell outlines are completely lost. In zooids which are feeding 
(Fig. 7) this inner end of the cell is filled with minute food particles the digestion 
being evidently, in part at least, intracellular. 


The ectoderm is continuous at the base with the layer which covers externally 
the whole colony whilst the endoderm is continuous with that of two or more of the 
coenosare tubes. 


(2.) Gonophores.—I have only been able so far to find the male gonophores 
which are present on three colonies secured at Coogee on the New South Wales 
coast. Hach of these colonies carries numbers of minute somewhat pear-shaped 
structures which are only from one-third to one-quarter of the length of the hydroid 
zooids and which are seen when rendered transparent or cut into sections to be 
medusoid in nature. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 13 


These gonophores arise directly from the cenosarc and are not carried by modified 
zooids or blastostyles. 


They may be very numerous indeed especially on the medium-sized branches 
where their number in one specimen far exceeds that of the hydroid zooids. Two 
are represented as seen by reflected light in figure 6 and in all specimens examined 
the gonophores are at the same stage of development. I have been unable to detect 
any indication of the formation of reproductive elements in the hydrophyton. 


The gonophores much resemble in structure those figured by Weismann* in 
Pennaria cavolina or Cladocoryne floccosa. In essential structure the transverse section 
of the gonophore of the former is identical with that of a similar section of a 
Ceratella gonophore as shown in figure 8. The longitudinal section again of the 
gonophore of Cladocoryne or of Pennaria as figured by Weismann agrees almost 
precisely with that of Ceratella represented in figure 12. In the latter the 
manubrium is well developed and surrounding this lie the reproductive elements 
which in longitudinal section (Fig. 12) form a horseshoe-shaped mass and in transverse 
section aring. External to the latter isa thin layer of ectoderm (ect.') which comes 
in contact with the external layer of ectoderm (ect.) at the part corresponding to the 
mouth of the medusa bell where the former layer dips inwards. (Fig. 12, M.) This layer 
must correspond to the sub-umbrella ectoderm of the medusa and the special point 
mentioned indicates also the position at which, in development, the “ glockenkern ”’ 
of Weismann grew in by proliferation of the ectoderm cells. I have been unable to 
find any gonophore younger than the stage figured though many have been cut in 
section, the manubrium being in every case well developed. 


Between the two layers of ectoderm lies the endoderm with four radial canals 
seen clearly in transverse sections (Fig. 8) whilst in longitudinal sections (Fig. 12) 
the indication of a ring-shaped space around the distal end can always be detected. 


Hach gonophore may be connected with more than one of the ccnosare tubes 
and its ectoderm is continuous with that which covers the colony externally. 


(3.) The Hydrophyton—This may be divided into two parts (1) the external 
layer common to the whole colony and (2) the branching network of tubes. 


The external layer is formed entirely of ectoderm cells (Figs. 3 and 12) and is 
only one cell thick though it may come into contact with the ectoderm of the tubes 
lying immediately beneath it. It is especially well marked in the younger branches 
and may be worn away to a greater or less extent in older ones though typically it 
forms a covering for the whole of the colony (Figs. 9 and 13). It is directly 


* Die Entstehung der sexualzellen bei den Hydromedusen. Pl. XVII., Figs. 1-5 and Fig. 7; Pl. XVIII., Fig. 1. 


14 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


continuous with the ectoderm of both the hydroid zooids and the gonophores, and 
has in many respects a close resemblance to the superficial layer of ectoderm as 
described and figured by Professor Moseley in Millepora.* In the latter the exact 
relationship of the superficial ectoderm to the zooids could not be ascertained but 
in Ceratella where the latter are not retracted imto spaces within the skeleton its 
direct connection with the ectoderm of the zooid can easily be seen in sections. 
Figure 8 represents a small portion of the layer as seen under a high power. The 
outlines of cells cannot be definitely distinguished in the specimen in question 
though a somewhat light space with a fairly distinct outline surrounds the thread 
cells. The inner ends of the cells are in contact with the ectoderm of the tube 
beneath and the layer thins out just where it passes over the projecting point of a 
portion of the skeleton. In younger branches (Fig. 14) the cells of the layer are much 
more definite in form and outline being each cubical with a distinct nucleus whilst 
comparatively very few thread-cells are present. 


This superficial layer is only known to exist m the Hydrocoralline, the 
Hydractiniide and, now, in the Ceratellade. In the last mentioned the soft parts of 
only Ceratella fusca ave known as yet but the skeleton of Dehitella is so closely 
similar to that of the former that we may with much probability infer that a close 
agreement exists in the nature of their soft parts. The ccenosare tubes form a 
richly branching network of tubes occupying all the spaces in the chitinous 
meshwork which forms the skeleton. In Figures 9 and 10 this is represented 
diagrammatically by the grey colour the former being a longitudinal and the latter 
a transverse section of a branch. Throughout the whole system the endoderm is 
never more than one cell thick whilst the ectoderm is very irregular. Very often the 
endoderm cannot be recognised or else it forms an indistinct layer which stains more 
darkly than the ectoderm and contains no space, a result probably due to the action 
of reagents. At other times (Figs. 8, 11, 12, and 14) a distinct tubular space 
can be distinguished. The number of tubes varies naturally according to the size of 
the branch. Figure 13 represents a longitudinal section through a portion of a small 
branch with a smaller offshoot which formed part of a specimen brought by 
Mr. Whitelegge from Lord Howe Island. The general appearance of a part of the 
same specimen viewed as a solid object is represented in Figure 4. This particular 
specimen has the branches much finer than those of the others and the skeleton and 
ccenosarc tubes somewhat more regular in arrangement, whilst the hydrophores 
are not very strongly developed. Up the small offshoot pass the main skeletal ribs 
united by cross bars which are thin and almost web-hke and up the centre runs a 
single ccenosare tube (B) which is connected with at least three of those in the larger 
branch. This tube consists of an internal layer of endoderm (Fig. 18 a, end.) and 


* On the Structure of a Species of Millepora occurring at Tahiti, Society Islands. Phil. Trans. R.S. London, 
1876, Vol. CLXVII., p. 117. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 15 


an irregular external layer of ectoderm (ect.) the former beg continuous with that of 
the zooids. The whole is covered by aunilaminar ectoderm (£). <A few thread cells 
are present. Up the layer branch the tubes run more regularly than usual and three 
or four may be traced for a considerable distance running parallel to its length but 
eiving off lateral branches. In sections both transverse and longitudinal of Ceratella 
these connecting bars or webs crossed by ccenosare tubes form a very characteristic 


feature (Figs. 11 and 138. C). 


As stated above there is a strongly-marked difference between the endoderm and 
ectoderm. The former (Fig. 3) is regular and takes stain somewhat more readily 
than the latter, which is often very irregular and several cells thick, though most 
often the outlimes of cells cannot be recognised, and a structure resembling a 
syncytium is formed. In the latter are found (1) nuclei, (2) thread cells, (3) bodies 
surrounded by a clear space and staining evenly and deeply (Fig. 3A). The 
thread cells are apparently confined to the ectoderm, though of this I cannot feel 
absolutely sure, and are found in great abundance in the inner parts of the branch 
whence they must migrate to the surface if they are to be of service to the colony. 
It is a somewhat curious fact that they are as a rule present in far greater numbers 
in the ectoderm of the coenosarc tubes than in the most external layer. Figure 3 
represents a small portion of the latter on a part of a colony where the 
gonophores were numerous and here thread cells were present in greater numbers 
than elsewhere. Of the nature of the third-named structures it is difficult 
to be certain but it is probable that they are ectoderm cells in which thread 
cells are being formed. ‘There is at all events a curious agreement in appearance 
between them and the structures which Professor Moseley has described as developing 
thread cells in Millepora.* He says “the thread cell appears to be developed out of 
the nucleus of the ectodermal cell, the ectodermal cell becoming much enlarged and 
forming a wide chamber, in which the process of development takes place. The 
ovoid nucleus becomes enlarged together with the cell, but not at all in the same 
proportion the cell always appearing as a wide cavity around it. The nucleus as it 
enlarges has a rounded nucleolus developed at one end of it.’ The nucleolus has 
large granules developed within it, whilst the nucleus becomes finely granular. In 
the next stage one large coil of the thread appears in the nucleus.” 


The earlier stage seen in Millepora when the nucleus with nucleolus at one 
end of it lies in the cell which forms a clear cavity around it, corresponds exactly to 
that represented in figure 3A.c. in the case of Ceratella. Though a complete series of 
stages could not be obtained still those drawn in figure 3A. will serve to show that in 
all probability Ceratella resembles Millepora closely in the formation of thread cells. 
In figure 3A.a. the cell is small and the nucleus but little larger than that of an 


* Toc. cit., p. 129. 


16 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


ordinary ectoderm cell though stained very deeply and having a homogeneous 
appearance ; in b. the cell has increased in size, the nucleus is much larger, and has 
a clear space all around it between it and the cell wall; this is clearly marked in c. 
and d. where, in the former, a nucleolus is present and in the latter two darker thread- 
like lines possibly indications of the commencing formation of the thread; in ec. what 
is evidently a very young thread cell is seen—it is somewhat darkly stained without 
a definite thick wall such as is seen clearly in later stages, and down the centre is a 
lighter line corresponding to the thicker attached part of the thread. It has also the 
shape of the thread cell but there is no trace of the clear space present in earlier 
stages, a certain amount of stained protoplasm being attached to it. Inf. and g. two 
later stages are shown in which the thick cell wall is present and the coiled thread 
can be clearly seen. ‘These thread cells evidently resemble closely in structure the 
three-barbed ones described by Professor Moseley in Millepora. 


The only other point to notice in regard to the ccenosare is the structure of the finer 
erowing branches which are somewhat flattened out. A longitudinal section of one 
of these is represented in figure 14. Up the centre runs a ccenosare tube with a large 
cavity and clearly-marked endoderm the ectoderm being as usual irregular. From 
this central tube short branches are given off (D) which run outwards towards the 
external layer with which, as at the point x, they may come into direct contact. At 
this point the cells of the two layers are well marked, and in all probability this 
shows us the earliest stage in the formation of a zooid. It has already been noted 
that the ectoderm of the latter is in direct connection not with that of the ccenosare 
tubes but with the common external layer and this method of formation would 
explain this otherwise somewhat curious fact. ‘The endodermal process grows out 
into a bud—the early stage of a zooid—carrying with it the external ectoderm layer 
which thus, as further growth takes place, naturally gives rise to that of the zooid 
itself. At the same time the ccenosarc tube branches as the stem increases in size 
and thus the zooid, if the branching be near the base of the latter, will become 
connected with two or more tubes. 


AFFINITIES OF THE CERATELLAD®. 


When Dr. Gray first described these forms there were only two specimens 
available neither of which possessed the soft parts. The hard parts whilst agreeing 
in important points differed from each other sufficiently to be regarded by him as 
species of two distinct genera Ceratella and Dehitella. 


Mr. Carter, with more material at his disposal, recognised the fact that they 
were hydroids and owing to similarities in their skeleton and that of Hydractinia 
placed them in the family Hydractiniide, thus abandoning Dr. Gray’s family 
Ceratelladee which had been created under the assumption that the two forms were 
allied to the sponges. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 17 


Undoubtedly in many respects Ceratella and Dehitella call to mind the 
Hydractiniide, but it is doubtful if even our knowledge were confined to that of the 
structure of the hard parts whether Mr. Carter’s classification could be upheld. ‘The 
one point of resemblance—and at first sight it is the most striking feature—is that 
the skeleton of both consists of a very irregular branching chitinous network. In the 
Ilydractiniide however this has the form of an encrusting network with at most very 
feebly developed branches arising from it; these may more correctly be described as 
spines and they do not appear to carry any zooids. In the Ceratelladx the whole 
colony consists of a much-branching structure arising from a comparatively small 
encrusting root-portion which may itself be made up of branches more or less 
entwined. In addition to this all the branches bear hydrophores or special 
developments of the network to support the hydroid zooids. These are never 
present in the Hydractiniidze but always in the Ceratelladee. Now that the soft parts 
are known there can be no doubt about separating the two families. The hydroid 
zooids are quite different those of Ceratella being provided as are those of Coryne 
with scattered capitate tentacles whilst there is no trace of protective zooids such as 
are present in Hydractinia and Podocoryne. In addition to this the gonophores 
arise directly from the ccenosare and not from modified zooids. ‘The most important 
points of agreement lie in (1) the existence in Hydractinia and Ceratella of a 
common external layer of ccenosare which covers over the whole skeleton mass 
whether this be encrusting or branching in nature; (2) the presence in both of a 
network of ccenosare tubes forming the hydrophyton. It may however be noted 
that in both these points we find a similar agreement to exist between Ceratella and, 
for example, Millepora amongst the Hydrocorallinz as between the first named and 
Hydractinia. 


The presence of this external layer which, in the Hydrocoralline and Ceratella 
at all events, consists simply of a layer of ectosarc is very difficult to explain. 
Professor Moseley* has represented it in Millepora as if it formed the outer layer of 
the surface ccenosare tubes though even in this case it passes over all the 
parts (occupied by the calcareous skeleton) which on the surface he between the 
tubes, and is very different in appearance and in the relative size of its cells from 
the ectoderm which elsewhere forms the onter wall of the tubes. In Ceratella it is 
perfectly independent of the tubes all of which have their own ectoderm covering 
though at the surface this comes in direct contact with the outer layer. I am not 
aware of any determination in Hydractinia of the exact relationship of this outer 
layer though very probably it will be found to agree with that of Ceratella. 


It is not apparently connected in any special way with the formation of the 
chitinous network as this ies deep within the structure of the branch, and the only 


* Loe. cit., Pl. 3., Figs. 10 and 16. 


18 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


purpose which it can apparently serve is that of a covering layer which prevents 
foreign objects from passing in between the meshes of the network and interfering 
with the general welfare of the colony. It is strange however to note, if this be its 
function, that most usually the internal ccenosare contain a far greater number of 
thread cells than this external layer does in Ceratella. 


In Millepora Professor Moseley was unable to determine its exact relationship to 
the zooids but in Ceratella by its means all the ectodermal structures lying on the 
external surface are brought into direct continuation with one another. 


It may be noted in passing that though in the genus Clathrozoon* the branches 
of the colony are formed of a somewhat similar network of soft parts there is nothing 
present resembling this external layer the whole branch being in this instance covered 
with a thin protective perisare, 


Taking both the hard and soft parts we find the following points of agreement 
to exist between the Hydractiniide on the one hand and the Ceratellade on the 
other though it must be borne in mind that we only know as yet the structure of the 
soft parts in one member of the latter family. 


(1.) The skeleton has the form of a branching chitinous network. 


(2.) The hydrophyton consists of a network of freely branching and 
anastomosing ccenosarcal tubes. 


(3.) The zooids arise directly from this network and no true hydrothece 
or gonothece are formed. 


(4.) A common external layer is present enclosing the whole colony. 
The two differ from one another in the following points :— 


(1.) Hydractiniide form encrusting masses with at most spmulose branches 
arising from the surface which do not bear zooids. The Ceratellade 
always form freely branching masses either erect or procumbent: the 
basal part which serves to attach the colony being alone of an 
encrusting nature whilst even this has the form of intertwined 


branches. 


(2.) The Ceratellade always possess hydrophores or special developments of 
the skeleton which serve asa support for the basis of the hydroid- 
zooids and nothing similar to which is found in the Hydractiniide. 


(3.) The hydroid zooids Ceratellade possess scattered capitate tentacles 
those of the Hydractiniide being filiform and arranged in a single 
circle beneath the mouth. 


* Trans. R.S., Victoria, 1890, p. 121. Pl. 18, Fig. 3; Pl. 19, Fig. 12. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 19 


(4.) The gonophores of the Ceratellade arise directly from the ccenosare 
and are not developed on special zooids as in the case of the 
Hydractinide. 


Whilst the poimts of agreement detailed above serve to show a general 
resemblance between the members of the two groups those of difference are of 
sufficient importance to justify their separation into two distinct families. 


As stated previously Dr. Gray’s name Ceratelladz will be retained and the 
following gives the characters of the family (modified from Dr. Gray’s and Messrs. 
Carter and Bale’s descriptions) and the list and characters of the genera and species 
yet known. 


Family Ceratellad@ (Gray, Proc. Zool. Soc., 1868, p. 575). 


Forming branching colonies. Skeleton in the form of a chitinous network with 
slight bracket-like or tubular projections (hydrophores) serving as a support for the 
bases of the gastrozooids. 


Hydrophyton a network of branching anastomosing tubes the whole enclosed by 
a common ectoderm layer. 


Gastrozooids naked. 
Gonophores medusoid : fixed and arising directing from the hydrophyton. 


Genus. Dehitella. (Gray.) 


Colony dichotomously branched, expanded growing in a large tuft from a broad 
creeping base. Stem cylindrical, smooth; branches tapering and cylindrical. 
Hydrophores shghtly tubular and on the smaller branches divergent nearly at right 
angles from the stem. 


(1.) Dehitella atrorubens. (Gray.) 


The description of the species is the same as that of the genus. It is known at 
present simply from that given by Dr. Gray* who states that the genus “is 
distinguishable from Ceratella by the greater thickness and cylindrical form of the stem, 
by the more tufted and irregular manner of growth and by the tufts of spicules (oscules 
or cells) being more abundant and equally dispersed on all sides of the branches and 
branchlets.” The ‘“oscules or cells” of Dr. Gray must be the structures which, 
following Mr. Bale, have been described above as ‘ hydrophores.” 


Locality. —Delagoa Bay, Africa. 


* Proc. Zool. Soc. 1868, p. 579. Fig. 1. 


20 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


Genus. Ceratella. (Gray.) 


Colony irregularly branching; more or less expanded in one plane; growing 
from a creeping base. Main stem flattened, branches rounded and beset with 
bracket-lke hydrophores. 


(2.) Cevatella fusca. (Gyay.) 


Colony branching and fan-shaped ; expanded in the one plane; erect. Skeleton 
consisting of alight or dark-brown chitinous network; the main stem broad and 
flattened; branches numerous with the bracket-shaped hydrophores arranged on 
them in a roughly spiral manner and formed of ribs continuous with the fibres of the 
stem and united by thin perforated laminz the ribs projecting at the outer margin. 
All the spaces within the chitinous network filled by a much branching hydrophyton 
and the whole enclosed by an external layer of ectoderm. Gastrozooids seated on 
the hydrophores, erect, with capitate tentacles tregularly scattered (10-14). 
Gonophores medusoid, fixed. 


Localities.—Coogee, Bondi (N.S.W.), Broughton Island, Flinders Island, Lord 
Howe Island. 


(3.) Ceratella procumbens. (Carter*). 


Colony procumbent, thickly branched on the same plane; the larger stems 
chiefly on one (the lower) side, hard, flexible, of an ochre-brown colour, tinged here 
and there with purple. Trunk short, solid, compact, compressed vertically, soon 
dividing irregularly or subdichotomously into round branches which are confined to 
the lower surface, ending in branchlets with sub-clavate ends, that appear on the 
upper or opposite side, not reuniting or anastomosing. Hydrophores consisting of 
a little semitubular plate, extending outwards and forwards from the side of the stem 
on the proximal border of an aperture in the latter; scattered thickly over all the 
branches, but most prominent on the branchlets ; frequently represented by the little 
hole alone in the stem where the projecting portion has been worn off; scanty on the 
lower side of the main stems. Minute structure ; composed of clathrate chitinous 
fibre throughout, whose meshes are subrectangular; hydrophore formed of the 
semitubular scoop-lke plate mentioned supported on its proximal side by an extension 
of the clathrate structure of the stem and bordering the little hole also above 
mentioned, which extends into the centre of the stem; surface of the larger stems 
bluntly microspined. Size of largest specimens 11 inches long by 5 inches broad, 
and about 1 ineh thick or vertically. 


Locality.—Cape of Good Hope, Natal. 


* Ann. and Mag. Nat. Hist., 1873. Transformation of an entire shell into chitinous structure by the Polype 
Hydractinia, with short descriptions of the Polypidoms of five other species (Pl. 1). The descriptions of C. procumbens, 
C. spinosa and Chitina ericopsis are taken with only slight alterations from this paper. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 21 
(4) Ceratella spinosa. (Carter.) 


Colony procumbent; thickly branched hard flexible of a dark rich red-purple colour. 
Main branches round, brownish, covered with small, smooth, often subspatulate erect 
spines. Stem dividing subdichotomously into purple branchlets, which terminate in 
abruptly pointed extremities. Hydrophores the same as in the foregoing species; 
most prominent in the round branchlets to which they give, en profil, a serrate 
somewhat sertularian appearance, the teeth of which are inclined forward. Minute 
structure: Main stems composed of clathrate chitinous fibre, of which the meshes are 
more or less oblong, passing into prominent longitudinal lines on the branchlets 
where they terminate on the backs of the semitubular plates which respectively form 
the floors of the hydrophores, to which they thus give support. Size of specimen, 
which is merely a branch 43 inches long by 2 broad. 


Locality.—Port Natal. 


Mr. Carter adds that ‘‘the spines on the surface distinguish this from the 
foregoing species, add to which its longer and more pointed branches, longitudinally 
ridged clathrate fibre and rich red-purple colour.” 


Genus. Chitina. (Carter.) 


Colony erect, bushy, fragili flexible, fawn coloured. Trunk long, hard, 
irregularly round, composed of many stems united clathrately and obliquely into a 
cord-like bundle, which divides and subdivides irregularly into branches which again 
unite with each other in substance (anastémose) when in contact and finally form a 
straggling bushy head. Hydrophores long clathrate tubular, terminating the ends 
of the branchlets, or prolonged from some of the proliferous tubercles which beset 
the surface of the trunk and larger stems. Minute structure : Composed of clathrate 
chitinous fibre throughout, whose network is subrectangular and massive in the stems, 
where there is no difference between the centre and circumference, with the exception 
that the fibre is stouter in the former or oldest part; hydrophores composed of several 
longitudinal fibres or ridges lattice-worked together transversely into a tubular form, 
somewhat contracted at the extremity, in the centre of which is an aperture of the 
meshwork a little larger than the rest. Height of specimens about 14 inches, trunk 
about 1 inch in diameter; hydrophores averaging 1-3rd of an inch long by 
1-60th of an inch in its broadest part and an aperture 1-90th of an inch in 
diameter. 


(5) Chitina ericopsis. (Carter.) 
The description of the species is the same as that of the genus. 


Locality.—New Zealand. 


22 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


DeEscrRIPTION OF PLATES. 
PLATE II. 


Fig. 1—Ceratella fusca. Life size. The specimen of which this is a drawing 
was washed up on Flinders Island, Bass Straits. The main stem of the colony 
springs from a root-like structure made up of intertwined branches. On the left side 
arises from the roots a very small independent stem. 


Fig. 2.—Transverse section through a portion of the wall of an expanded 
gastrozooid. Externally is the layer of ectoderm consisting of cubical cells. The 
mesogleea is an extremely thin layer and the endoderm consists of large vacuolate 
cells with granular protoplasm aggregated at their inner ends which face into the 
gastral cavity. The nuclei are conspicuous and placed at the same end. Camera. 
Zeiss H, oc. 2. 


Ect. ectoderm. End. endoderm. WM. mesoglea. 


Fig. 8.—A small portion of the external surface of a branch in the region in 
which gonophores are numerous to show the external ectoderm containing thread 
cells and a portion of one of the ccenosare tubes. In the latter the endoderm forms 
a definite layer of darkly-stained, small cubical cells. Surrounding this is the 
ectoderm in contact with the external layer and containing developing thread cells. 


E. external layer of ectoderm. Ect. ectoderm of ccenosare tube. End. 
endoderm. A. developing thread cells. Sk. skeleton. Camera. Zeiss H, oc. 2. 


Fig. 8a.—Developing thread cells found in the ectoderm within the branches. 
a. an ectoderm cell in which the nucleus is slightly larger than usual and appears 
homogeneous. b. the nucleus has increased in size, stains very darkly, lies at one end 
and is surrounded by a clear space. c. the nucleus begins to show a darker spot 
within it. d. two darkly-staining thread-like structures are present. e. the nucleus (?) 
does not stain so deeply, and is not surrounded by a clear space but has a small 
amount of protoplasm clinging to it; within it at the somewhat pointed extremity can 
be seen a light line indicating the larger terminal part of thethread. f. the wall 
of the thread-cell and the thread itself are clear. 9. The fully developed thread-cell. 


PLATE III. 


Fig. 4.—Portion of a small branch with the zooids expanded. The skeleton is 
covered by the soft parts but the dark lines indicate the external parts of the chitinous 
network which show through the soft structures. 


ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 238 


Fig. 5.—Portion of the skeleton of a somewhat larger branch showing the 
chitinous network of which it is composed and the little bracket-like hydrophores. 
(Ayyy x12: 


Fig. 6.—Highly magnified small portion of a branch seen partly by direct and 
partly by transmitted light. Two gastrozooids are shown each of which is placed upon 
a hydrophore. The latter shows prominent ribs which project beyond the margin 
and are connected by a thin fenestrated web of chitin. Two male gonophores arise 
from the ccenosare and they and the gastrozooids are quite naked. The whole branch 
is covered by a thin external layer of ectoderm. x 20. 


G. gastrozooids. Gon. gonophore. £. external layer of ectoderm. Hy. hydro- 
phore. Hy.' web connecting the ribs of the latter. 


Fig. 7.—Transverse section across the body of a gastrozooid. The tentacles 
are solid with swollen ectoderm ends filled with thread cells. The zooid has been 
feeding and the endoderm cells are full of little food particles. /.—Remnant of 
small crustacean on which the zooid is feeding. It lies close against the endoderm 
on one side and the food particles are passing into the interior of the cells. Outline 
drawn with Camera, Zeiss H, oc. 2. 


Fig. 8.—Transverse section across a gonophore. Mn. endoderm of the 
manubrium. Sf. sperm cells in the ectoderm of the latter. Ect. ectoderm of the 
medusa. . radial canals. Ect’. ectoderm of the sub-umbrella surface. Outline 
drawn with Camera, Zeiss E, oc. 2. 


PLATE IIIA. 


Fig. 9.—Semi-diagrammatic drawing of a longitudinal section through a 
small branch. The skeleton is coloured brown the soft parts grey. E. external 
layer of ectoderm. Gon. gonophore. G. gastrozooid. Hy. hydrophore. Sf. 
general network of skeleton cut across in various directions. Outline drawn with 
Camera, Zeiss A*, oc. 2. 


Fig. 10.—Semi-diagrammatic drawing of a transverse section across a good-sized 
branch. Letters as in figure 9. Ect. ectoderm of endosare tubes. End. endoderm. 
Outline drawn with Camera, Zeiss A*, oc. 2. 


Fig. 11—More highly magnified portion of a branch cut in transverse section. 
The ectoderm of the gastrozooid is directly continuous with the external layer of the 
branch and the base of the zooid is continuous with two of the ccenosare tubes. 
At C. is represented the characteristic feature of the latter crossing over five 
connecting strands of the chitinous network. C. points at which the soft parts 


24 ON THE STRUCTURE OF CERATELLA FUSCA (GRAY). 


cross thin connecting strands of the skeleton. &. external layer of ectoderm. 
Iict. general ectoderm. G. gastrozooid. Hy. hydrophore. Sk. general skeleton. 
Outline drawn with Camera, Zeiss A*, oc. 2. 


Kig. 12.—Portion of a longitudinal section of a branch from which arise two 
gonophores. The latter are cut in longitudinal section. &. external layer 
continuous with the ectoderm of the gonophore. Ld. endoderm of the manuubrium. 
Ect. ectoderm. Ect'. ectoderm of sub-umbrella layer of the medusa. G. 
eastrozooid. M. point at which the ectoderm dips in corresponding to the mouth 
of the medusa. RR. radial canals. Outlme drawn with Camera, Zeiss C, oc. 2. 


Fig. 18.—Longitudinal section of a branch from which another small one arises. 
In this specimen the skeleton has more than usual a more or less definite 
arrangement into ribs which run parallel to the length of the branch and are 
connected by transverse bands. Outline drawn with Camera, Zeiss A*, oc. 2. 


Fig. 18a.—A small portion of the small branch in figure 13 more highly 
magnified to show the single caenosare tube passing along the centre. The ectoderm 
is irregular. Letters as before. Drawn under Zeiss F, oc. 2, * 


Fig. 14.—Portion of a terminal branch devoid of zooids. Up the centre runs 
a single tube with an internal unicellular layer of endoderm and an irregular ectoderm. 
‘he endoderm gives off hollow processes which at certain parts (x) come into direct 
contact with the external ectoderm (Z). Further growth of these will probably give 
rise to the gastrozooids the external layer of the colony thus forming their ectoderm. 
Drawn under Zeiss H, oc. 2. 


> 


KER. 


icforia [89 Flat 


— 


Trans PS. 


RUS Cr 


CERATELLA 


err ded 


WB. Spencer &.R 1s 


(bbe PRE 
©. Lroedel & C 


‘Lith Mell, 


o 
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ARTICLE III.—Apprrionan OpsErvAtTIONS ON THE VicTorRIAN Lanp PLANARIANS, 
By ArtHuR Denpy, D.Sc. (With Plate IV.) 


(Read June 12th, 1891.) 


Since my last paper ‘‘On the Victorian Land Planarians”’ was read before this 
Society I have been able to collect a considerable amount of further information 
concerning this interesting group of worms, and the present observations are intended 
to bring our knowledge of the group up to date by describing species or varieties 
hitherto unknown and especially by giving full details as to the variation in colour 
and markings and as to the distribution within the colony of those species which 
have already been described. 


In my previous memoir I recorded fifteen Victorian species ; this number has 
now been brought up to twenty-two, the additional seven species being Geoplana 
dendyi, Spencer, G. frosti, Spencer, G. howitti, Dendy, G. ventropunctata, Dendy, 
all of which are new to science since I last wrote; with G. swlphurea, Fletcher and 
Hamilton, and G. sanguinea, Moseley, hitherto recorded only from New South 
Wales, and Bipalium kewense, Moseley, an introduced species recorded by Fletcher* 
from near Hltham. The genus Rhynchodemus has not again been met with. 


G. howitti and G. ventropunctata are now fully described and figured for the first 
time, and I have also taken the opportunity of giving figures of several other species 
or varieties which I had not been able to figure previously. 


The question of the distinctness of the different ‘species’? remains where it 
was, but I hope that the observations concerning the variation in pattern and colour 
recorded in the present contribution will be of assistance in ultimately settling it. 
These observations are given systematically under the headings of the different 
species, and I have thrown out hints as tothe possible relationship of the different 
forms, which may or may not be followed by future workers. 


I have also been in communication with Professor L. von Graff, of Gratz, who is 
engaged in the preparation of an elaborate monograph of the whole group and wrote 
to me for specimens of our Australian Planarians. Iam glad to have beeu able to send 
Professor von Graff a large number of our species, which he intends to examine 


* Linnean Society of New South Wales, February 25th, 1891. (Zoologischer Anzeiger, April 20th, 1891, p. 139.) 


26 ADDITIONAL OBSERVATIONS ON 


anatomically, and when the results of this anatomical mvestigation are combined with 
the observations of Australian zoologists upon the living animals we may hope to 
arrive at a fair idea of the relationship of the various forms. 


In the systematic part of this paper the species are arranged in what appears to 
me to be the most natural order, commencing with the forms without stripes. 
Fifteen of the species thus appear to fall into five groups, within each of which the 
species are all closely related. The remaining seven species do not to my mind fall 
into any of these groups and are also very distinct from each other. The following 
is the complete list up to date, the related species being bracketed together in 
groups :— 


1. Geoplana alba, Dendy. 
2. 3 sanguinea, Moseley. 
3. “i spenceri, Dendy. 
4, FA cerulea, Moseley. 
Lis, $5 dendy1, Spencer. 
6. 3 walhalle, Dendy. 
he , frosti, Spencer. 
S i sugdent, Dendy. 
9. mediolineata, Dendy. 
| 10. rr quinquelineata, Fletcher and Hamilton. 
ue me m'mahont, Dendy. 
12. , sulphurea, Fletcher and Hamilton. 
(rey - hoggit, Dendy. 
(ela: - quadrangulata, Dendy. 
ena mi, ventropunctata, Dendy. 
16. “ munda, Fletcher and Hamilton. 
ie ae ade, Dendy. 
18. 4 fietcheri, Dendy. 
19. Ms lucast, Dendy. 
20. 53 howitti, Dendy. 


21. Fhynchodemus victoria, Dendy. 
22. Bipalium kewense, Moseley. 


With regard to the distribution of the species within the colony, I have been 
able to collect a considerable amount of information; and, for the benefit of 
collectors, to whom it may be of service to know what localities have been explored 
and what species found in each, I give the following table of distribution. I at 
first thought of giving also a list of the months of the year in which each species 
has been found, but this appears to me to be superfluous. Land Planarians may, 
I believe, be found at all times of the year by diligent searching, but they seem to 


THE VICTORIAN LAND PLANARIANS. 27 


be much more abundant in spring (or early summer) and autumn than in the great 
heat and drought of the summer or the cold and excessive moisture of the winter 


months. 


Toorax.—Geoplana cerulea. 


HEIDELBERG. 


G. quinquelineata; G. munda. 
Eiruam.—Bipalium kewense. 
Croypon.—G. alba; G. mediolineata; G. sulphurea; G. munda; G. ade. 


Fern Tree Guiiy.—G. alba; G. mediolineata; G. sulphurea; G. munda; G. 
ade; G. m‘mahoni; G. ventropuncttata. 

Warracui.—G. alba; G. sugdeni. 

Between LinypaLe and Sevitte.—G. m‘mahoni. 

Warsurton.—G. sfencerz; G. mediolineata; G. ada. 

M‘Manon’s Creek (Upper Yarra).—G. alba; G. m‘mahoni ; G. spencert. 

Between Marysvitte and the Source or tHe Yarra.—G. alba; G. spencers; 
G. dendyi; G. walhalle; G. frosti; G. mediolineata; G. m‘mahont ; 
G. sulphurea; G. munda. 


WaLHALLA.—G. spenceri ; G. mediolineata; G. walhallea ; G. sulphurea. 


Upper Wetuineton River.—G. alba; G. sulphurea; G. quadrangulata, vay. 
wellingtoni ; G. lucasi; G. howttti. 


Croasincotone.—G. caerulea; G. dendyi; G. alba; G. lucasi; G. sulphurea; 
Rhynchodemus victoria. 

CASTLEMAINE.—G. sanguinea. 

SaNDHURST.—G. quinquelineata. 

Batuarat.—G. alba; G. quinquelineata ; G. munda. 

Creswick.—G. sugdeni; G. mediolineata; G. quinquelineata; G. hoggi; G. 
quadrangulata; G. munda. 

Macepon.—G. alba; G. sugdent; G. mediolineata; G. hoggiu; G. ade; G. 
quadrangulata; G. fletchert. 


Orway Forest.—G. sulphurea; G. quinquelineata; G. munda. 


From this it will be seen that, so far as Planarians are concerned, a very large 
proportion of the colony is unexplored, and we may expect considerable additions to 
our Planarian fauna in the near future. 


Bipalium kewense is undoubtedly an introduced species, whose natural habitat is 
unknown. It was obtained from the Kew Botanical Gardens near London, and 


28 ADDITIONAL OBSERVATIONS ON 


described by Professor Moseley. Since then it has been found in various parts of 
England and also in Sydney,* and still more recently, as I have already noticed, Mr. 
Fletcher has recorded its occurrence at Eltham, and likewise in Samoa. Good figures 
of this interesting Planarian are given by Bell in his ‘‘ Note on Bipalium kewense, 
and the Generic Characters of Land-Planarians.”’t 


Concerning Rhynchodemus and Bipalium I have nothing further to add, and we 
may pass on to the systematic observations on the 20 species of Geoplana. As the 
present memoir is merely a continuation of my earlier paper ‘On the Victorian 
Land Planarians,” published in the Transactions of this Society for 1890, I have not 
thought it necessary to give constant references to that paper, to which I would 
refer the reader for further information and references. 


1. Geoplana alba, Dendy. 


This is one of the most widely distributed and abundant of our Victorian 
Land Planarians. Since the publication of my description and figures Professor 
Spencer has recorded the species}—on the occasion of the Field Naturalists’ 
Expedition to the Yarra Falls—and has figured two specimens which are of a rather 
darker colour than usual and thus approach G. sanguinea. As already noted in my 
original description the species varies a good deal as to the depth of colouration, from 
almost pure white to peach-coloured or yellow flesh. I may add that the eyes are 
very small and difficult to make out. In addition to the localities already mentioned 
I have now obtained the species from Croydon, Fern-Tree Gully, Ballarat (abundant 
under stones close to the edge of the lake, Mr. Avery), and the Upper Wellington 
River. 


2. Geoplana sanguinea, Moseley.§ 


This species has not hitherto been recorded from Victoria, but I have now 
received seven specimens collected by Mr. T. S. Hall, M.A., at Castlemaine, under 
fallen bark and stones. The specimens were received by me in alcohol, with the 
following note as to the colours of the living worm :—* Rich Indian red above, 
paler below.’ The specimens (in spirit) are about 25 mm. long, and 4 mm. 
broad, much flattened on the ventral surface but pretty strongly arched on the dorsal. 
The anterior end of the body tapers off gradually, the posterior end terminates much 


* Pletcher. ‘Remarks on an introduced Species of Land-Planarian, &c.,” Proc. Linn. Soc., N.S.W., May 25, 1887. 
+ Proc. Zool. Soc. Lond., 1886, p. 166, Plate XVIII. 

t Proceedings of the Royal Society of Victoria, 1891, p. 88. 

§ Quarterly Journal of Microscopical Science, Vol. XVII., N.S., p. 285. 


THE VICTORIAN LAND PLANARIANS. 29 


more abruptly. The peripharyngeal aperture is situate at about the junction of the 
middle and posterior thirds of the body and the genital aperture nearer to it than to 
the posterior end. 


The eyes are, as in G. alba, very small and difficult to make out. 


Geoplana (Cenoplana) sanguinea was very imperfectly described by Moseley as 
follows :—‘‘ Closely resembles C. Coerulea, with the exception that it is coloured of 
a uniform light red, which is lighter upon the under surface of the body. Actual 
length when living 7 cm.; breadth 4 mm., Parramatta, near Sydney. Amongst 
earth at the roots of a Eucalyptus stump.” (Loc. cit.) 


It seems probable that Fletcher and Hamilton’s G. rubicunda* is identical with 
G. sanguinea, a conclusion at which I understand Mr. Fletcher has himself now 
arrived. My G. alba is also evidently closely related to G. sanguinea and may have 
to be considered merely as a variety of that species. 


G. sanguinea (as represented by the Castlemaine specimens), G. rubicunda and 
G. alba all agree in the general shape of the body, in the position of the apertures 
and in the curious indistinctness of the eyes. 


The Castlemaine specimens of G. sanguinea are all markedly smaller than the 
average size of G. alba, but Moseley’s examples seem to have been of about the same 
size as the latter. 


3. Geoplana spenceri, Dendy. 


This species has again been met with by Professor Spencer} on the occasion of 
the Field Naturalists’ expedition to the Yarra Falls, in a locality intermediate between 
the Upper Yarra district and Walhalla, whence it had been previously recorded. 
Though extremely abundant in these parts it does not seem to occur in other localities, 
so that its distribution appears to be curiously limited in extent. 


4. Geoplana cerulea, Moseley. 
@isy.,, Wie. %) 
In my previous memoir on the Victorian Land Planarians I recorded this species 


from Croajingolong, where it was collected by Professor Spencer. Since then 
I have only met with a single specimen and that in a somewhat remarkable 


* Proceedings of the Linnean Society of New South Wales.”’ Series II., Vol. IL, p. 370. 
+ Loc. cit. 


30 ADDITIONAL OBSERVATIONS ON 


situation, viz., in the earth around the roots of a chrysanthemum which 
was given to me by Mr. G. W.: Officer and which was taken out of the ground in 
Toorak, near Melbourne, in June, 1890. This specimen when alive was of a very 
dark Prussian blue colour on the dorsal surface and paler blue on the ventral. 
There was a narrow median dorsal stripe of yellow, and an indistinct median 
ventral very pale blue stripe traceable back nearly to the genital aperture. There 
was no different colour at the anterior extremity. In spirit the specimen measures 
about 35 by 2°5 mm.; the peripharyngeal aperture is very slightly behind the 
middle of the body and the genital aperture at rather more than one-third of the 
distance from the peripharyngeal opening to the hinder end of the body. The eyes 
are easily visible with a lens. ‘This specimen, although now preserved in spirit for a 
year, has preserved its blue colour remarkably well. It is impossible, of course, 
to determine how it was imtroduced into Mr. Officer's garden at Toorak, and 
it is interesting to note in this connection a remark made by Messrs. Fletcher 
and Hamilton* concerning the same species to the effect that the specimens usually 
found by them have an orange-red tip (as appears to have also been the case in the 
Croajingolong specimens) but that ‘‘ on three different occasions we have found on 
the pavement in Hyde Park alongside the enclosure at Captain Cook’s statue a 
number of blue Planarians (about fourteen altogether), which are without the red tip, 
and in which the median stripe varies from a dirty white to a distinct yellow, 
changing to white in spirit. . . . . Theenclosure referred to has probably been 
stocked with these Planarians from the Botanic Gardens, but we do not know from 
what locality. The differences in living specimens in the two cases seem to be 
constant, and are sufficiently marked to make one a variety of the other, if not to 
separate them as distinct species.’ ‘They consider that the red-tipped variety is 
probably the typical form, although Moseley does not mention the red colour of 
the anterior extremity. It is curious that the ‘ introduced” Toorak specimen, if 
I may use the term, should exhibit exactly the same peculiarity as the ‘‘ introduced”’ 
Sydney specimens, and this is an argument for supposing them to belong to a 
distinctly marked variety whose natural habitat is not known, but which is 
characterised by the absence of any red colour at the anterior extremity. } 


5. Geoplana dendyi, Spencer. | 


This species is evidently very closely related to Geoplana cerulea, being 
distinguished from it perhaps only by the presence of the median dorsal line of blue 


* Loe. cit. 


+ On the evening on which this paper was read another specimen of this variety was found on the floor in the house 
at Toorak from the garden of which the first specimen was obtained almost exactly twelve months ago. Mr. Officer kindly 
brought this second specimen to me alive, so that owing to this remarkable coincidence I am able to give a figure of 
the worm in its living condition. The second specimen agrees so closely with the first that no special description is 
necessary. 


t) oc: cit. 


THE VICTORIAN LAND PLANARIANS. 31 


in the middle of the yellow stripe. Some of the specimens brought by Professor 
Spencer from Croajingolong (in spirit), which otherwise resemble G. c@rulea, have 
the dorsal light band thus divided into two by a dark line, and I find that I had 
accordingly placed them in separate bottles away from those which | definitely 
identified with cwrulea. Probably, therefore, these Croajingolong specimens are also 
referable to G. dendyz, so that we have the two closely allied species, cwrulea and 
dendy1, inhabiting the Croajingolong district. The Croajingolong specimens appear 
to be more flattened than those described by Professor Spencer. 


6. Geoplana walhallea, Dendy. 


Only a single specimen of this species has been obtained since it was first 
described, and that by Professor Spencer, who found it in the country lying between 
Marysville and the source of the Yarra along the Wood’s Point Road, and has 
described and figured it in the Proceedings of the Royal Society of Victoria.* The 
genital opening, as figured by Professor Spencer, is much nearer to the peripharyngeal 
opening than in the type specimens. 


7. Geoplana frosti, Spencer.t 


This species, as pointed out in the original description, is obviously very closely 
related to G. walhalle, from which it is distinguished only by the presence of two 
light yellow stripes one on each side of the mid-dorsal line and by the absence of the 
brown speckles along the mid-ventral line. I do not feel disposed to lay any stress 
on the latter character. Professor Spencer has figured an interesting connective 
form in which the dorsal yellow stripes are absent throughout the greater part of the 
length of the body. 


T have identified} a small specimen which I found near Mount Wellington, 
Gippsland, with this species. In life the ground colour of the dorsal surface was 
very dark indigo blue, so dark that the exact colour was difficult to determine, with 
two narrow stripes of whitish separated by a very fine, dark, mid-dorsal line. The 
ventral surface was pale brown flecked with darker brown. Even in the spirit- 
preserved specimen a light mid-ventral line, devoid of specks, is distinctly visible, 
and the opening into the peripharyngeal chamber is situate in about the centre of 
the body and the genital aperture (?) only a short way behind it. The specimen 
(in spirit) measures 12mm. in length by a little under 3mm. in greatest breadth. 


* Loc. cit. 
{ Loc. cit. 
t Victorian Naturalist, June-July, 1891, p. 44. 


32 ADDITIONAL OBSERVATIONS ON 


8. Geoplana sugdent, Dendy. 


T have received specimens of this species from Creswick, collected by Mr. Fiddian, 
and have also obtained more specimens from Macedon, whence it was originally 
recorded. At Macedon I have again observed it crawling about in broad daylight. 
Professor Spencer informs me that he has found this species at Warragul. 


9. Geoplana mediolineata, Dendy. 


I identify with this species specimens obtained from Fern Tree Gully, Croydon 
and Creswick, and Professor Spencer has figured* a variety of the species from the 
country lying between Marysville and the source of the Yarra along the Wood’s Point 
Road. As Professor Spencer has pointed out, specimens in which the lateral stripes 
are well developed make an approach to Geoplana quinquelineata ; on the other 
hand, the species seems also to merge into G. sugdeni. Hence although typical 
specimens of G. sugdeni and G. quinquelineata appear very different indeed it seems 
not impossible that they may have to be united with G. mediolineata as varieties of 
one species. G. mediolineata occupies an intermediate position between the other 
two, not only as regards the stripes but also in the shape of the body, being not 
usually so flattened as G. guinquelineata and less cylindrical than G. sugdenti. 


In G. mediolineata the median stripe is always much darker in colour than the 
others (if they be present). In this it agrees with G. quinquelineata and differs from 
G. m‘mahoni. 


10. Geoplana quinquelineata, Fletcher and Hamilton. 


This species seems to be characteristic of the Sandhurst district and in addition 
to the localities mentioned in my previous memoir I have now to record it from 
Ballarat, Creswick and Heidelberg. In some of the Creswick and Ballarat specimens 
the lateral stripes show a strong tendency to disappear and it is difficult to say 
whether the specimens should be called quinquelineata or mediolineata. The genital 
aperture is very difficult to observe but appears to me to be rather nearer to the 
peripharyngeal aperture than to the hinder end of the body, while the peripharyngeal 
aperture is more easily visible and situate about the middle of the ventral surface. 
Hence G. sugdem, G. mediolineata and G. quinquelineata agree pretty closely in the 
position of the apertures. 


= Loc; ictt: 


THE VICTORIAN LAND PLANARIANS. 33 


11. Geoplana m‘mahoni, Dendy. 
(BIVLV., Haga) 


Since the publication of my previous memoir I have met with several interesting 
specimens of this species at Fern Tree Gully. The ground colour in the living worm 
was bright canary yellow on the dorsal surface, paler on the ventral. Some 
specimens had (like the original type) only the two stripes on the dorsal surface, both 
broad and black, or nearly so. Others had, in addition, a much narrower median 
dorsal stripe of the same colour, and yet others were intermediate between these two, 
the median band being very narrow and discontinuous. The paired stripes are, 
in this species, the characteristic and constant ones, and not, as in G. mediolineata 
the least persistent; they are always much more prominent than the median 
stripe. The position of the genital and peripharyngeal orifices in the Fern Tree 
Gully specimens agree in one specimen with that described for the type, though 
in another the peripharyngeal aperture is almost central. Ido not set much value on 
slight differences in this respect, as the position of the apertures must depend to a 
certain extent upon the state of contraction of the specimen. 


Professor Spencer* records the species from the country lying between 
Marysville and the source of the Yarra along the Wood’s Point Road. 


Thave also a slight variety of this species from between Lilydale and Seville. 
The colour when alive was bright yellow all over except for the brown anterior tip 
and two strong dorsolateral stripes (one on each side) of brown starting from the 
anterior tip and dying out about one-third of the way down the body, and also a very 
short, thin, median dorsal stripe of brown starting from the anterior tip 
but soon dying out. When alive the specimen measured about 60 mm. 
in length. In spirit it is rather broad and flat and the peripharyngeal aperture is 
situate shghtly in front of the middle of the body and the genital aperture not very 
far behind it, much nearer to it than to the posterior end of the body; obviously, 
however, the anterior half of the body is much more contracted than the posterior, 
thus bringing the apertures forward. 


The occurrence of the Fern Tree Gully variety with the median stripe is 
interesting as showing how an even-striped form may be derived from an odd-striped 
form by disappearance of the median stripe, and as pointing out a possible relationship 
between G. mediolineata (and its close allies), and G. m‘mahoni. 


* Loc. cit. 


34 ADDITIONAL OBSERVATIONS ON 


12. Geoplana sulphurea, Fletcher and Hamilton. 
(Geoplana sulphureus, Fletcher and Hamilton, Joc. cit.). 


This species was found by Professor Spencer in the country between Marysville 
and the source of the Yarra, alongthe Wood’s Point Road, and is identified and 
figured by him in the Proceedings of this Society.* I have in my collection a 
number of specimens from other parts of Victoria, viz., the Otway Forest (two very 
large specimens), Croydon, Walhalla, Croajingolong, Fern Tree Gully, and the 
Upper Wellington (a number of very small specimens). Some of these specimens 
have been in my possession for a long time but the original description is so short 
that I had not ventured upon an identification. Neither Messrs. Fletcher and 
Hamilton nor Professor Spencer mention the position of the external openings. In 
spirit specimens I find the peripharyngeal aperture situate in about the centre of the 
body and the genital aperture at about one-third of the distance between the 
peripharyngeal aperture and the posterior end. 


In G. sulphurea the outer stripes are broader than the inner, in G. hoggii, which 


é 


comes very near it, the reverse is the case. 


The ground colour in G. su/phurea is yellow. The inner stripes are dark brown, 
or sometimes greenish grey, the outer ones are darker, usually black or nearly so. 
In one of my Wellington specimens the two inner stripes are so close together that 
in the spirit-preserved specimen they appear as one, so that the specimen appears to 
have three stripes of equal width. In an interesting specimen from Fern Tree 
Gully all four stripes are extremely thin and discontinuous and almost entirely absent 
from the posterior part of the body; the outer stripes, however, are still distinctly 
stronger than the inner ones. 


13. Geoplana hoggit, Dendy. 


Thave little to add to my original description of this worm. I have again 
collected it at Macedon, where it is very abundant, and have also received typical 
specimens from Creswick, collected by Mr. Fiddian. The form certainly comes 
very near to G. sulphurea, and had I realised what G. sulphurea was really like at 
the time when I wrote my description I should possibly have considered it as a 
variety of the latter. G. hoggii, however, differs from G. sulphurea, as pointed out 
above, in having the inner stripes broader than the outer ones, the green colour being 
at the same time more pronounced; hence it may perhaps stand as a fairly 
well-marked variety, though probably not a distinct species. 


* Loc. cit. 


THE VICTORIAN LAND PLANARIANS. 35 


14. Geoplana quadrangulata, Dendy. 


I have again collected this very beautiful and distinct little Planarian at 
Macedon, where it is by no means uncommon, and I have also received a specimen 
from Creswick, collected by Mr. Fiddian. These specimens all exhibit in a more or 
less marked degree the pale spots along the junction of the dorsal and lateral 
surfaces ; these spots are merely the foreshadowings of the characteristic mottled 
appearance of the Mount Wellington variety. 


14a. Geoplana quadrangulata, var. wellingtont, nov. 


This pretty little variety was obtained in abundance under logs near the foot of 
Mount Wellington and its occurrence has already been recorded by me in the “ Victorian 
Naturalist.” * The worm is arather difficult one to collect as it crawls into the crevices 
of the rotten wood in a very provoking way and readily breaks to pieces. 


When alive the ground colour of the dorsal surface was pale brown, with a 


median dark brown line and on-each side of it numerous thickly scattered speckles 
of dark brown. 


The lateral surfaces were very pale brown thickly flecked with dark brown, and 
the ventral surface was white, devoid of speckles. All the specimens obtained were 
a good deal smaller than the typical form of the species from Macedon usually is. 
More than a dozen specimens were collected. 


15. Geoplana ventropunctata, n. sp. 
(Pl. IV., Figs. 2, 2a.) 


I obtained this very beautiful little species in abundance under rotten logs at 


Fern Tree Gully, on the occasion of the Field Naturalists Club’s excursion to that 
locality in March last. 


When at rest the body is very broad and flat (Pl. IV., Fig. 2a), but when 
crawling, which is done very actively, the body becomes greatly elongated and very 


narrow, measuring about 20 mm. in length anda little under 2 mm. in greatest 
breadth. 


The eyes are arranged as usual on the horse-shoe shaped anterior extremity and 
sides of the body. 


* Loe. cit. 


36 ADDITIONAL OBSERVATIONS ON 


The opening of the peripharyngeal chamber (in spirit) is somewhat behind the 
middle of the ventral surface and the genital aperture about one-third of the way 
between it and the posterior end of the body. The protruded pharynx (in spirit) is 
cylindrical. 


The ground colour of the dorsal surface is really nearly white, but almost entirely 
obscured by the abundant markings, which are arranged as follows:—(1) A rather 
narrow, nearly black median stripe with irregular margins. (2) On each side of the 
black stripe and extending to the lateral margin of the body are a great number of 
small, closely set, irregular longitudinal streaks of various shades of brown, in some 
specimens a good deal lighter than in others. Each side of the body, between the 
dorsal and ventral surfaces, is occupied by an irregular stripe of very dark brown, 
made up of a series of splotches of pigment more or less run together. The anterior 
extremity is dark brown. 


The ventral surface is white, very beautifully spotted all over with small, distinct 
and isolated specks of dark brown. 


When the animal is alive the lateral stripe is visible from the ventral surface 
but not from the dorsal ; in spirit it is just visible from the ventral surface. 


In general appearance and size this species closely resembles Geoplana 
quadrangulata var. wellingtoni, but we may note the following points of distinction :— 
(1) The body is not so distinctly quadrangular in section and the sides do not slope 
inwards nearly so much, so that the ventral surface is much wider. (2) There is a 
distinct, though irregular lateral stripe of a very dark colour, instead of the sides of 
the body being lighter in appearance than the dorsal surface as in G. quadrangulata 
and its variety. (8) The ventral surface is, in all specimens which I have seen (a 
considerable number), very distinctly spotted with brown; while in all specimens of 
G. quadrangulata which I have seen it has no spots at all. 


It a curious fact that while this species was found abundantly at Fern Tree 
Gully in March, in company with large numbers of Geonemertes australiensis, 
yet we could not find a single specimen of either of these worms when we visited the 
spot a few weeks later in May. 


16. Geoplana munda, Fletcher and Hamilton. 


This species has proved to be one of the commonest and most easily recognisable 
of our land Planarians. Since writing my last memoir on the subject I have had 
specimens from Croydon, Fern Tree Gully, Heidelberg, Creswick and Ballarat. At 


THE VICTORIAN LAND PLANARIANS. 37 


Croydon, on December 17th, 1890, I found more than fifty specimens of this species 
under a single log, all agreeing closely in colour and markings. 


I was at first much puzzled at not being able to find the genital aperture in this 
species. I could not find it in the Otway Forest specimens recorded in my previous 
memoir, nor could I find it in the specimens collected at Croydon in December, 1890, 
though I carefully examined a considerable number. When, however, I came to examine 
specimens collected at Creswick in March, 1891, I found it at once in ten out of eleven 
specimens, the eleventh being a very small one. The Croydon specimens were fully 
of the average size and the obvious conclusion seems to be that the genital aperture 
is visible only at certain times of the year (autumn). With this we may associate the 
fact, recorded in my last memoir, that Geoplana mediolineata copulates in the beginning 
of April. Possibly all our land Planarians breed in the autumn. 


The peripharyngeal aperture in G. munda is nearly central and the genital 
aperture only a short way behind it, as originally described by Fletcher and Hamilton. 


Professor Spencer* has also recorded the species from the country lying between 
Marysville and the source of the Yarra along the Wood’s Point Road, and has 
given an excellent coloured figure of the living worm. 


I have now to mention a slight variety of the species which I found at 
Heidelberg and which was again obtained by Mr. Fiddian at Creswick. The 
Heidelberg specimens, three in number, are thus described in my notes on the living 
animals :—‘“ In size and shape closely resembles G. munda, the ground colour is also 
yery similar, on the dorsal surface a slightly mottled olive brown; ventral surface 
pale yellow. In the mid-dorsal line a fine, very pale brown band, edged on either 
side by a fine dark brown line which forms a margin to the ground colour. No other 
stripes.” The Creswick specimens presented exactly the same peculiarity, viz., the 
absence of the dorso-lateral dark stripes; they were collected in May, and show the 
genital aperture distinctly. 


17. Geoplana ade, Dendy. 
(Pl. IV., Figs. 3, 3a.) 


I have again collected this very handsome Planarian at Macedon and have also 
found it at Croydon and Fern Tree Guliy. ‘The genital aperture, which I had not 
been able to distinguish when I first described the species, is situate only a short way 
behind the peripharyngeal and a long way from the posterior end of the body ; it 
appears to vary in distinctness with the time of the year, as in G. munda. 


¥ Loc. cuts 


38 ADDITIONAL OBSERVATIONS ON 


My original description and figure did scanty justice to the beauty of this 
species, partly because the specimens were not so fine as those which I have since 
obtained. 


The two specimens from Croydon were about 65 mm. in length and 4 mm. in 
width when crawling. The ground colour of the dorsal surface was light, mottled 
brown, and the paired stripes were very broad, of a dark greeny brown colour, with 
a fine, well-defined, very dark outline on each side. One of the specimens shows a 
fine, ight-brown mottling on the ventral surface, except in the mid-ventral line, the 
other only shows a trace of this mottling at the anterior end. 


At Fern Tree Gully, on March 14th, 1891, a number of fine specimens were secured 
which again showed some interesting variations in colour. The ground colour of the 
dorsal surface was very pale, yellow brown, generally, at any rate, more or less 
mottled, but only very slightly. The ventral surface was very pale yellow brown, 
often shehtly mottled and sometimes with two broad bands of distinct, slightly 
mottled brown one on each side of a narrower median band of almost pure 
white. In some specimens the three stripes on the dorsal surface were coloured 
as in the specimens originally described and figured. The most striking variety, 
however, is that represented in Figs. 3, 3a., Pl. IV. In this specimen the ground 
colour of the dorsal and ventral surfaces was very pale brown very slightly 
mottled, with slght imdications of a lighter median stripe on the ventral 
surface. The two broad stripes on the dorsal surface, mstead of being simply 
brown, or purple brown as in some specimens, were of a dark brown colour with very 
minute blue specks thickly scattered all over. Viewed as a whole these stripes 
appeared of different tints according to the light thrown on them, but the general 
impression was dark olive green. 


When at rest G. ade is very broad and flat,and the green variety closely 
approaches G. frosti in appearance. The broad, dark bands are, however, edged on 
the outside with ground colour, and do not extend to the lateral margin asin G. frosti. 
In other words, what appears as ground colour in G. frost: appears as a definite stripe 


in G. ade. 


18. Geoplana fletchert, Dendy. 
(ELLY jelio.iO5) 


I have again found this species at Macedon but have not seen it from any other 
locality. I take this opportunity of emphasising the fact that this Planarian, which 
at first sight might easily be mistaken for one of the common yellow forms, is really 
very distinct indeed. The much flattened ventral surface, sometimes becoming 


THE VICTORIAN LAND PLANARIANS. 39 


strongly concave in spirit, and the markedly posterior position of the apertures, the 
genital being close to the hinder extremity of the body, readily distinguish the 
species. 


In one of my specimens the copulatory organs are partially protruded, and 
exhibit the very remarkable peculiarity that while the female copulatory organ is 
single there are two distinct male organs. The appearance and arrangement of these 
parts 1s shown in Figure 6. Whether or not this condition is constant I cannot say, 
but I am inclined to think that the species possesses anatomical peculiarities which 
would well repay investigation, and which may even necessitate the erection of a new 
genus for its reception. The eyes are arranged as is usual in Geoplana. 


19. Geoplana howitti, Dendy.* 
(PRIN. Big. 5.) 


Body (in spirit) much flattened on the ventral surface, strongly convex on the 
dorsal, much broader behind, where it terminates rather abruptly and bluntly, than 
in front, where it tapers gradually. Peripharyngeal aperture (in spirit) well behind 
the middle of the ventral surface, only 8mm. from the hinder extremity of the body. 
Genital aperture about 4mm. behind the peripharyngeal. Length of body (in spirit) 
about 25mm., greatest breadth 4mm. ‘The eyes are arranged as usual in the genus 
but are difficult to make out owing to the dark pigment around them, so that I had 
to cut a slice off the side of the head end before I could find them. 


When alive the ground colour of the dorsal surface was yellowish white ; in the 
mid-dorsal line a fairly broad band of ground colour, on each side of this a stripe of 
about equal width of dark purplish brown, outside this a rather broader band of 
ground colour thickly flecked with dark purplish brown and edged on the outside by 
a fine line of dark purplish brown, outside this fine line a very narrow edge of ground 
colour. 


It is noteworthy, as showing a tendency towards variation in pattern, that in the 
mid-dorsal band of ground colour, just in one place near the posterior end, there are 
a few small flecks of dark purplish brown, as shown in the figure. The horse-shoe- 
shaped anterior extremity is, during life, dark purplish brown, and all the dark bands 
unite at each end of the body. 


The ventral surface in life is pale yellowish white or grey, with no markings. 


I found a single specimen of this Planarian beneath a log near the bank of the 
Upper Wellington River, at the foot of Mount Wellington, Gippsland, on the occasion 


* A brief preliminary diagnosis of this species was given in the Victorian Naturalist for June-July, 1891, p. 43. 


40 ADDITIONAL OBSERVATIONS ON 


of an expedition made to that locality in company with Mr. A. W. Howitt and 
Mr. A. H. 8. Lucas in December, 1890. I have much pleasure in naming the species 
after the leader of the expedition. 


In the shape of the body and the markedly posterior position of the apertures 
Geoplana howitt: resembles G. fletcher:. 


20. Geoplana lucasi, Dendy. 
(PL: -TY,;, Hig. 94") 


I found a single specimen of this interesting species under a log near Mount 
Wellington, Gippsland, on the same occasion and in the same locality as G. howitti. 
As I had not before seen this Planarian alive I was very glad of the opportunity of 
making careful notes of the appearance of the living animal, andI am also able to 
give a figure of the natural colour. 


In life the dorsal surface is white, with dark grey or black markings arranged as 
follows :—There is a rather narrow median stripe of black and the remainder of the 
dorsal surface is thickly flecked with small specks and longitudinal dashes of dark 
grey. On either side of the median black line these specks and dashes are absent, 
or nearly so, leaving a very narrow band of almost clear ground colour, then they 
appear comparatively large and very close together and more in irregular longitudinal 
dashes which seem to be formed each of a number of smali dots. Towards the 
margin of the body the dots and dashes get smaller and scarcer, ‘The horse-shoe- 
shaped anterior extremity is reddish brown. The ventral surface is greyish white, 
with no markings. 


When crawling the worm measured about 60 mm. in length. 


The specimen after preservation in spirit closely resembles the spirit specimens 
from Croajingolong originally described. The eyes appear to extend (in abundance) 
for an unusual distance down the sides of the body, if not along the entire length of 
the animal, but it is difficult to be certain on this point owing to the resemblance 
between the eyes and the smaller specks of pigment. 


In concluding these observations I desire again to express my indebtedness to 
those gentlemen who have kindly assisted me in collecting specimens of Land 
Planarians, viz., the Rev. W. Fielder, Mr. Officer, Mr. Avery, Mr. Fiddian, and Mr. 
W. Mann, of the Melbourne University ; Mr. H. R. Hogg, Mr. Hennell, and other 
members of the Field Naturalists’ Club of Victoria. 


32> 


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THE VICTORIAN LAND PLANARIANS. 41 


Description oF Prats LY. 


Fig. 1—Geoplana m‘mahoni, crawling, dorsal surface. From Fern Tree Gully. 


Fig. 2.—Geoplana ventropunctata, crawling, dorsal surface. From Fern Tree 
Gully. 


Fig. 2a.—Geoplana ventropunctata, at rest, dorsal surface. From Fern Tree 
Gully. 


Fig. 3.—Geoplana ade, variety with green stripes; crawling; dorsal surface. 
From Fern Tree Gully. 


Fig. 3a.—Geoplana ade, same specimen as represented in Fig. 3; at rest ; dorsal 
surface. 


Fig. 4.—Geoplana lucasi, crawling, dorsal surface. From Upper Wellington 
River. 
Fig. 5.—Geoplana howitti, crawling, dorsal surface. From Upper Wellington 


River. 


Fig. 6.—Geoplana fletcherz. Ventral surface of posterior end, showing copulatory 
organs protruded. From Macedon. 


Fig. 7.—Geoplana cerulea. Variety with blue tip. Dorsal surface. From 
Mr. Officer, Toorak. 


Norr.—All the figures are enlarged. The actual measurements are given in the 
text. ; 


ARTICLE IV.—Lanp Puianartans From Lorp Hower Isnanp, sy W. Batpwin 


Spencer, M.A., Proressox or BroLoay in THE University oF MELBOURNE. 


Part [.—Description oF Species. (With Plates 5 and 6.) 


(Read Thursday, June 11th, 1891.) 


The following paper deals with an interesting collection of land Planarians 
which were obtained by Mr. Thomas Whitelegge for the Australian Museum during 
a visit paid by a collecting party, despatched by order of the Trustees of the Museum 
to Lord Howe Island in 1887. 


The material was first placed for examination in the hands of Mr. J. J. Fletcher, 
to whom we are indebted for the description of the various species of land planarians 
found in New South Wales. Mr. Fletcher being unable to devote the necessary 
time to their elucidation kindly offered, with the consent of the trustees of the 
Museum, to place the material at my disposal. 


The specimens are excellently preserved, and I have had the advantage of the 
short notes made by Mr. Whitelegge at the time of collecting them giving some 
little information with regard to their colour and length. The specimens all came 
from under the leaves of palm trees. 


On the Australian continent two genera of land planarians are well-known, viz., 
Geoplana and Rhynchodemus. Of the former 35 species have been described, 
and of the latter six species, five from New South Wales, and only one as yet from 
Victoria. The latter is known only from one specimen which I collected in 
Croajingolong, near to the New South Wales border, and to which Dr. Dendy has 
given the name of R. victorie. In addition to these two genera, the introduced form 
Bipalium kewense has been recorded by Mr. Fletcher from both New South Wales 
and Victoria. 


Thus in Australia the genus Geoplana is the predominant one. New Zealand 
has as yet been scarcely worked for land planarians and from the Polynesian region so 
far as | am aware, the only land planarians recorded come from the Samoan Islands, 


LAND PLANARIANS FROM LORD HOWE ISLAND. 43 


from which place Grube has described two species of Rhynchodemus, viz., 
R. bistriatus and R, quadristriatus. 


Lord Howe Island lies far away from the nearest mainland, in the north of what 
it is now proposed to call the Tasman Sea at about one-third of the distance between 
the Australian eastern coast and the most northerly point of New Zealand. It lies in 
about Lat. 32° S. and Long. 158° EH. and in the line of the comparatively shallow 
soundings which indicate probably the existence of an ancient land connection 
between New Zealand and the north of the Australian continent. It is interesting 
hence to note that as far as our, at present, limited knowledge extends the genus 
Rhynchodemus would appear to be more common as we go northwards on the 
mainland, whilst there is only one species recorded from Victoria, five are known in 
New South Wales, and it will be of interest to see whether a knowledge of Queensland 
forms confirms this relative distribution of the two genera Geoplana and 
Rhynchodemus. Had a species of Geoplana been at any rate at all plentiful on Lord 
Howe Island it would have hardly escaped the notice of so careful a collector as Mr. 
Whitelegge though at the same time it must be remembered, judging by experience 
in Victoria, that forms commonly met with at one special time may at another be 
few and far between. Still there is not in Mr. Whitelegge’s collection a single 
example of Geoplana. 


The collection proves to contain eight species all, so far as can be ascertained, 
new to science. Jam however unable to refer to the description of R. bistriatus and 
R. quadristriatus described by Grube from the Samoan Islands. It is just possible 
that these may be identical with two of the species now to be described but taking 
into account the distance which separates the two islands and the fact that even 
Victoria and New South Wales, though so close together, have very few species 
indeed of land planarians in common it seems most likely that the species of 
Rhynchodemus will be distinct on the Samoan and Lord Howe Islands. 


The most interesting part of the collection consists of two species which 
must be referred to a new genus for which the name of Cotyloplana is proposed in 
consequence of the presence of a distinct sucker-like structure on the ventral surface 
anteriorly. 


In Part IT. of this paper I propose to describe the anatomy of this genus. The 
figures which accompany the paper are drawn from the spirit specimens and to 
preserve the relative dimensions proportional compasses have been used: at the 
same time it must be remembered that the form of these soft bodied creatures often 
changes very much when they are placed in spirit; still the markings and relative 
position of the pharyngeal and genital apertures may, together with colour markings, 
be taken as discriminative of the species. 


44 LAND PLANARIANS FROM LORD HOWE ISLAND. 
The following is a list of the forms described :-— 


Genus. Cotyloplana, gen. nov. 
1. C. whitelegger, sp.n. (Figs. 1, 2, 3, 4.) 
2. C. punctata, sp.n. (Figs. 5, 6, 7, 8.) 


Genus. Rhynchodemus.  (Leidy.) 


3. R. fasciatus, sp.n. (Figs. 9, 10.) 
R. laterolineatus, sp.n. (Figs. 11, 12, 13.) 
R. grandis, sp.n. (Figs. 14, 15, 16, 17, 18, 19.) 
R. mediolineatus, sp.n. (Figs. 20, 21, 22, 23.) 
R. dubius, sp.n. (Figs. 24, 25.) 

t. fletcheri, sp.n. (Figs. 26, 27.) 


We ED) Ub 


Cotyloplana, gen. nov. 


Body flattened. A sucker is present on the ventral surface close to the anterior 
extremity. Hyes two. 


Cotyloplana whiteleggei, sp.n. (Pl. V., Figs. 1, 2, 3, 4.) 


Anterior end somewhat spathulate with the antero-lateral margins of the body 
crenate and a median semicircular projection with smooth margin. yes two ; 
dorsal ; one at each side of the base of the semicircular projection. A sucker is 
placed on the ventral surface at the anterior extremity with its longest diameter at 
right angles to the long axis of the body. 


The dorsal surface is of a brown colour and the posterior part is covered with 
dark mottligs which become restricted anteriorly to form a broad median band 
which stops short of the anterior extremity. A dark band les across the anterior 
extremity and is continued backwards on each side for about one-fifth of the length 
of the body where it merges into the mottlings which cover the whole of the posterior 
part of the dorsal surface. 


Ventral surface mottled. 


Pharyngeal opening 12 m.m. from posterior end. Genital opening 5 m.m. from 
to} co) i co) 
posterior end. Length in spirits 24 m.m. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


LAND PLANARIANS FROM LORD HOWE ISLAND. 45 


The sucker placed on the ventral surface at the anterior end is distinctive of 
this genus and the somewhat spathulate form of the head together with the crenate 
antero-lateral margins are characteristic of the species. It is possible that this 
crenate appearance may be due to the presence of tentacular structures retracted in 
the spirit specimens but Mr. Whitelegge makes no remarks in his notes of the 
presence of any such nor do I think that they are anything more than crenations. 


I have much pleasure in naming the first species of this genus described after 
Mr. Whitelegge, and am now engaged in studying its anatomy an account of which 
will form Part II. of this paper. 


Coiyloplana punctata, sp.n. (PI. I., Figs. 5, 6, 7, 8.) 


Body flattened with the posterior half somewhat wider than the anterior half. 
Sucker on the ventral surface close to the anterior end, circular in outline, margin of body 
smooth. Eyes two, placed close to the anterior extremity. Dorsal surface except 
the lateral margins mottled with brown spots and with a median light line which may 
or may not extend the whole length. Ventral surface mottled except along the lateral 
margins and around the sucker, and somewhat lighter than the dorsal surface. 


Pharyngeal opening 9 m.m. from the posterior extremity; genital opening 
4 m.m. from the posterior extremity. Length whenalive 50 m.m. Length in spirits 
42 m.m. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


This species differs considerably from C. whiteleggei in the shape of its body 
whilst both agree in their notably mottled appearance on both dorsal and ventral 
surface though there is in the latter no indication of a median light line such as is 
present in C. punctata. This varies slightly being in one of the specimens figured 
(Fig. 5) continued to the posterior extremity whilst in the other (Fig. 6) it only 
passes along slightly more than one-half of the length of the body and there are 
indications of another light line on the left of the median one. ‘The margins of the 
anterior part of the body are, in spirit specimens, curved over ventrally (Figs. 7 and 8) 
making the dorsal, surface distinctly convex and the ventral concave. 


The two forms agree however in the presence of a ventral sucker anteriorly 
though in C. punctata the margins of this are not so strongly marked as in 
C. whitelegget. 


46 LAND PLANARIANS FROM LORD HOWE ISLAND. 
Genus Rhynchodemus. (Leidy.) 
Rhynchodemus fasciatus, sp.n. (Pl. V., Figs. 9, 10.) 


Dorsal face marked by a median broad blackish-brown band tapering suddenly 
anteriorly ; at either side of this are two dark bands separated by light lines the inner 
of the two former being broader than the outer. The edges of the upper surface are 
light coloured. The dark bands unite together some little distance in front of the 
posterior end leaving a distinct light margin. Eyes two placed close to the anterior 
end where the two outer dark bands unite together on each side. 


Ventral surface of dun colour with broad darker band in the median line and a 
narrow dark line on either side. Dark bands not nearly so prominent as on the 
dorsal surface. 


Pharyngeal opening 12 m.m. from the posterior end. Genital opening 9 m.m. 
from the posterior end. Length when alive, 50 m.m. In spirits 29 m.m. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


The bands as described above are probably much more distinctly marked in 
spirit than in living specimens. Mr. Whitelegge notes the colour as blackish brown 
on the dorsal surface with two light lines on the laterals, the ventral surface being dun 
colour. There are seen very clearly in spirit specimens five dark bands as shown in 
the figure (10) dorsally and three bands on the ventral surface though the latter are 
faint when compared with the former. A characteristic feature is the way in which 
the broad median land suddenly narrows at the anterior extremity whilst posteriorly 
it is broad and merges into the lateral ones. 


Rhynchodemus laterolineatus, sp.n. (Pl. V., Figs. 11, 12, 18.) 


Body much flattened; pointed at both extremities. Hdges of body with 
strongly marked dark bands tapering at both ends. Two dark lines along the body 
leaving between them a median narrow line of ground colour. 


Ventral surface with two dark lines one on either side of the median line and 
uniting anteriorly and posteriorly before reaching either extremity. Close to the 
two lateral dark bands is a dark line on each side; the two unite together anteriorly 
but posteriorly merge into the lateral bands. The dark bands on the ventral surface 
may be broad and as many as six be present. 


Pharyngeal opening 11 m.m. from post end. Genital opening 6 m.m. from the 
posterior end. Length of animal when alive 88 m.m. Length in spirit 25 m.m. 


Locality —Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


LAND PLANARIANS FROM LORD HOWE ISLAND. AT 


This species is marked by its very distinct bands of dark colour along the edges 
of the body. The latter is much flattened, broad in the middle and tapering to both 
ends ; there is no difference in the thickness of the body at any part, and the lateral 
margins are very distinctly marked. Whilst the dorsal surface is the same in all the 
specimens the ventral varies. Figures 12 and 13 serve to show the two extremes. 
The important dark bands consist (1) of two, one on either side the median line and 
(2) of two, one close to each of the lateral margins each of these falling into the 
lateral band before the posterior end is reached. 


In addition to these there may be present two more bands one on each side 
intermediate between those already described. In addition to varying in number 
ventrally the thickness of the bands may vary considerably, with the exception of the 
outermost one which always remains thin. ‘Thus in figure 13 the specimen drawn 
has four thick bands and the two lateral thin ones, whilst in figure 12 the specimen 
figured has only two thin median and the two thin lateral ones. In both cases the 
dorsal surface resembled the one drawn in figure 11. 


Rhynchodemus grandis, sp.n. (Pl. VI., Figs. 14, 15, 16, 17, 18, 19.) 


Dorsal surface with the ground colour fawn-brown, marked with streakings and 
spots of darker brown. The anterior end with the margins light-coloured and two 
dark bands, one on either side, which gradually become less marked posteriorly. 
They enclose between them at the front end a median light line, and the streaks 
show a tendency to form two dark lines one on either side the median line which 
remains light-coloured. Eyes two, one on either side in the lateral light lines close 
- to the anterior somewhat bluntly pointed extremity. Ventral surface of a lighter 
fawn-yellow colour, spotted with a prominent median line of dark spots. Pharynx 
35 m.m. from the posterior end. Genital opening 16 m.m. from the posterior 
end. Length when alive 6-7 inches, width 2-2 inches. 


Locality.—Lord Howe Island. (Coll. T. Whitelegge.) 


In spirit specimens the lateral edges of the body become curved towards the 
ventral surface so as to produce a distinct: concavity ventrally, but this only extends 
for a short distance. 


The specimen figured (Pl. VI., Figs. 14, 15) represents the animal very much 
contracted after the action of spirit, but this is probably one of the largest examples 
of the genus yet known. Some two or three of our Australian land-planarians of 
the genus Geoplana, notably G. dendyi and G. hoggii, reach a length when crawling 
equal to that of R. grandis, but the width of the body when fully expanded is 
nothing like so much as five-eighths of an inch. 


48 LAND PLANARIANS FROM LORD HOWE ISLAND. 


In Mr. Whitelegge’s collection are some specimens which are in all probability 
young forms of the species. These are interesting as showing, what Professor 
Moseley* has already drawn attention to, the curious fact that the markings are 
often more definite in young than in old and full-grown examples. Two young speci- 
mens are represented in figures 16,17,18, and 19. The first of these shows dorsally 
three stripes of dark colour, (1) a median one and (2) two lateral ones. In the older 
form these stripes, as it were, break up into a series of streaks and spots, but the 
two lateral ones persist anteriorly, whilst the median one becomes more obscure and 
represented by two lines of darker streaks. Ventrally also three dark but not so 
prominent stripes are present each composed of closely placed spots. 


The second shows dorsally the lateral stripes strongly marked only anteriorly, 
the median one being much fainter, whilst ventrally the lateral ones are only seen at 
the anterior end, and the median one is much as in the adult. In both of the young 
specimens figured only the pharyngeal opening is visible, the genital opening not 
being apparently developed presumably on account of the immaturity of the 
specimens. 


Rhynchodemus mediolineatus, sp.n. (Pl. VI., Figs. 20, 21, 22, 23.) 


Dorsal surface with a median dark stripe which may or may not extend the 
whole length of the body and on either side of which is a dark stripe anteriorly. The 
lateral edges are marked by dark lines. Two eyes close to the anterior end. 
Ventrally are two dark stripes one on either side the median line uniting anteriorly. 
Pharyngeal opening 12 m.m. from the posterior end. Genital opening 6 m.m. from 
the posterior end. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


This species varies somewhat in the development of the stripe just as does the 
species Geoplana mediolineata, which is distinguished by its median stripe. Two 
specimens are figured. In the first of these (Figs. 20, 21) the three stripes are only 
present at the anterior end dorsally whilst ventrally two extend for the whole length 
and enclose the pharyngeal and genital openings uniting together at both ends. 
In the second (Figs. 22, 23) the anterior dorsal end is darker than in the first and 
the dorsal median stripe extends the whole length whilst ventrally the two stripes 
are only present for not quite one-third of the length. The genital opening in the 
latter was indistinguishable. 


Rhynchodemus dubius, sp.n. (Pl. VI., Figs. 24, 25.) 


Dorsal surface with ground colour of pale cream colour, anterior end with four 
dark lines extending back not quite one-fourth of the length of the body the two 


* Trans. R. 8. London. The Anatomy and Histology of the Land Planarians of Ceylon. Vol. 164, 1874, p. 110. 


LAND PLANARIANS FROM LORD HOWE ISLAND. 49 


middle ones being more prominent than the outer ones and enclosing anteriorly 
a median light line of ground colour. The dark lines fuse at the anterior extremity 
leaving the margins of the body light coloured. The two eyes are placed in the dark 
lines where the four have fused close to the anterior end. The posterior three quarters 
of the body are marked by irregular, undulating, disconnected, dark lines the more 
prominent of which seem to forma broken up continuation of the two inner of the 
stripes. A median portion nearly one-third of the width of the surface is light 
coloured and there is present in this a median thin dark line made up of slightly 
discontinuous parts. The streaks have a tendency to form four lines at the very 
posterior end. Ventral surface pale cream colour with no streaks. Pharynx 36 m.m. 
from the posterior end. Genital opening 12 m.m. from the posterior end. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


The length of the animal when alive is 4-5 inches. The spirit specimens are all 
much coiled and vary somewhat in marking especially in the distinctness of the four 
stripes anteriorly and in the development of the thin dark median stripe. In one or 
two this is very difficult to detect and it may be very irregularly developed. It is not 
apparently at all prominent during life. The characteristic features are the lines 
giving place to streaks posteriorly and the entire absence of markings on the ventral 
surface. 


Rhynchodemus fletcheri, sp. un. (Pl. VI., Figs. 26, 27.) 


Dorsal surface with median light line and two broad black bands one on either side 
of this. Lateral portions of body and ventral surface light coloured. Ventral surface 
with two lateral dark lines and median broad punctated band not extending quite to 
the anterior or posterior ends and showing indication of division into two lines. 
Anterior extremity bluntly rounded with: eyes dorsal and close to the anterior edge. 
Pharyngeal opening 8 m.m. from the posterior end; genital opening 3 m.m. from 
the posterior end. 


Locality.—Lord Howe Island. (Coll. Mr. T. Whitelegge.) 


The animal when alive measures 25 m.m. in length the spirit specimen 
measuring 19 m.m. In the latter the pharyngeal opening has the form of a transverse 
slit with a light margin lying in the middle of the median dark. band; the genital 
opening is distinct and more noticeable than the pharyngeal and has a light- 
coloured circular margin the dark band being divided in its region into two by a 
median light line. 

The body in spirit specimens is somewhat flattened and band like the anterior end 
blunt and rounded the posterior more pointed. 

The median dorsal line swells out slightly on the head and does not quite reach 
the posterior end. 


50 LAND PLANARIANS FROM LORD HOWE ISLAND. 


DEscRIPTION oF PuLaTEs. 
Puate V. 


Fig. 1.—Cotyloplana whiteleggei, dorsal view. x 8. 
Fig. 2.—Cotyloplana whiteleggei, ventral view of the same. x 3. 


Fig. 3.—Cotyloplana whiteleggei, enlarged view of the dorsal surface of the 
anterior extremity to show the semicircular end with the crenated antero-lateral 
margins and the two eyes. x 7. 


Fig. 4.—Cotyloplana whiteleggei, enlarged view of the ventral surface of the 
same specimen as figure 3, to show the sucker with its slit at right angles to the long 
axis of the body and prominent margin. x 7. 


Fig. 5.—Cotyloplana punctata, dorsal view. x 2. 


Fig. 6.—Cotyloplana punctata, dorsal view of a larger specimen in which in 
addition to the median light line which does not extend the whole length of the 
body there is an indication of another light line at the side of the median one. x 1}. 


Fig. 7.—Cotyloplana punctata, ventral view of the same specimen as figure 6, 
showing the sucker anteriorly. x 1}. 


Fig 8.—Cotyloplana punctata, enlarged ventral view of the anterior extremity 
of the specimen represented in figure 6 to show the sucker. In figures 6, 7, 8, the 
lateral margins are seen to be strongly contracted so as to produce at the anterior end 
a very concave surface ventrally and convex dorsally. 


Fig. 9.—Rhynchodemus fasciatus, ventral view. x 3. 

Fig. 10.—Rhynchodemus fasciatus, dorsal view of the same. x 3. 

Fig. 11.—Rhynchodemus laterolineatus, dorsal view. x 2. 

Fig. 12.—Rhynchodemus laterolineatus, ventral view of the same. x 2. 


Fig. 18.—Rhynchodemus laterolineatus, ventral view of another specimen, in 
which the dark bands ventrally are strongly developed. x 3. 


LAND PLANARIANS FROM LORD HOWE ISLAND. 51 


Prats VI, 


Fig. 14.—Rhynchodemus grandis, dorsal view. Actual size of spirit specimen. 


Fig. 15.—Rhynchodemus grandis, ventral view of the same. Actual size of spirit 
specimen. 


Fig. 16.—Rhynchodemus grandis, young specimen, dorsal view. Actual size of 
spirit specimen. | 


Fig. 17.—Rhynchodemus grandis, young specimen, ventral view of the same. 
Actual size of spirit specimen. 


Fig. 18.—Rhynchodemus grandis, young specimen, dorsal view. Actual size of 
spirit specimen. 


Fig. 19.—-Riynchodemus grandis, young specimen, ventral view of the same. 
Actual size of spirit specimen. 


Fig. 20.—Rhynchodemus mediolineatus, dorsal view. x 38. 
Fig. 21.—Rhynchodemus mediolineatus, ventral view of the same. x 3. 


Fig. 22.—Rhynchodemus mediolineatus, dorsal view of another specimen in 
which the median line passes along the whole length of the body. x 3. 


Fig. 23.—Rhynchodemus mediolineatus, ventral view of the same, the two lines 
only being present at the anterior end of the body. 


Fig. 24.—Rhynchodemus dubius, dorsal view. x1}. 
Fig. 25.—Rhynchodemus dubius, ventral view of the same. x 1}. 
Fig. 26.—Rhynchodemus fletcheri, dorsal view. x 3. 
Fig. 27.—Rhynchodemus fletcheri, ventral view of the same. x 3. 


Norrt.—The blue tint in figures 14, 15, 16 and 18 should not be present. 


Vol. Hl. Plate 5. 


Trans. RS. Victoria 


= a naeemaneniaenel storia tlio Soo re 
Seer pndedann prt Manan simanern ene te wree n= 


W.B.Spencer del 


i 


LORD HOWE ISLAND - LAND PLANARIANS 


19 


Voll. Plate oO. 


18 


Trans. RS. Victoria 


19 


OI 
NI 


LORD HOWE ISLAND - LAND PLANARIANS. 


WB. Svence 


TRANSACTIONS. 


VOLUME Il. 

Part I.—6s. 
THE ANATOMY OF MEGASCOLIDES AUSTRALIS (THE GIANT 
EARTHWORM OF GIPPSLAND), sy Prorssson W. Baupwin Spencer, M.A. 


Plates 1 to 6. 
Part I1.—12s. 6d. 


1.—RECORDS OF OBSERVATIONS ON SIR WILLIAM MACGREGOR’S ~ 
HIGHLAND PLANTS FROM NEW GUINEA, sy Baron Von Muzzuzr, F.R.S. 

2.—THE PREPARATION OF AULKYL-SULPHINE, SELENINE, AND 
PHOSPHONIUM SALIT'S, sy Prorgssor Orme Masson, M.A., D.Sc., ann J. B. 
Kirxuanp, F.C.S. 

3.—IHE ANATOMY OF AN AUSTRALIAN LAND PLANARIAN, sy 
Artuur Denpy, D.Sc. Plates 7 to 10. . 

4—ON THE ORGANISATION OF AUSTRALIAN TRIBES, sy A. W. 
Howirr (with Map). 

5.—THE ANATOMY OF AMPHIPTYCHES URNA, sy Proressor W. 
Batpwin Spencer, M.A. Plates 11 to 18. 


VOLUME Il. 
Part I.—17s. 6d. 
1.—THE TRANSVERSE SECTIONS OF PETIOLES OF EUCALYPTS 
AS AIDS IN THE DETERMINATION OF SPECIES, sy D. McAupine anp 
J. KR. Rempry. Plates 1 to 6a. 
2.—THE VICTORIAN LAND PLANARIANS, sy Arraur Denny, D.Sc. 


Plate 7. 
3.—THE EUCALYPTS OF GIPPSLAND, sy A. W. Howirr. Plates 8 to 16. 


4.—A NEW FAMILY OF HYDROIDEA, TOGETHER WITH A DES- 
CRIPTION OF THE STRUCTURE OF A NEW SPECIES OF PLUMULARIA, 
BY Prorgessor W. Batpwin Spencer, M.A. Plates 17 to 23. 


VOLUME Ill. 
Part U.—7s. 6a: 


MONOGRAPH OF THE VICTORIAN SPONGES, sy Artuur Denpy, D.Sc. 
Part I., THE ORGANISATION AND CLASSIFICATION OF THE 
CALCAREA HOMOCGILA WITH DESCRIPTIONS OF THE VICTORIAN 
SPECIES. Plates 1 to 11. 


Ca 


hah sc) 
700 Vice 


ine 


Oy 


+ An {DA 


OEM TY 


3 2044 106 


BOUND JAN 1973