vsteriom maoeree : siete temnstinmrion in reece etme Peta metate pep ns 3 Tip aal Nh alone Cited THE RMRKOCE EW NGS OF TILK LISMEAN SOCIETY @ i el OF Nise Sours WWONES FOR THE YEAR WO 0 VOL. LIT. WITH FIFTY PLATES and 372 Text-figures. SYDNEY: PRINTED AND PUBLISHED FOR THE SOCIETY BY THE AUSTRALASIAN MEDICAL PUBLISHING CO., LTD., Seamer Street, Glebe, Sydney, and SOLD BY THE SOCIETY. 1927-1928. CONTENTS OF PROCEEDINGS, 1927. PART I (No. 210). (Issued 15th April, 1927.) Pages Presidential Address delivered at the Fifty-second Annual Meeting, 30th March, 1927, by E. W. Ferguson, M.B., Ch.M., D.P.H. a raeturteyts i-xxviii Elections and Announcements .. .. PB Poe! Wren bne XXViii Balance Sheets for the Year ended 31st Tacomber: 1926 SA Cle Ges mer 1 ee0.9D.05-5:0.0] Joseph James Fletcher RMT SEL ENN Maia eke pi Mis Ae iee bars inate git cera use h ery AM ORR NT LL CLD PART II (No. 211). (Issued 11th July, 1927.) Notes on Australian Diptera. No. x. By J. R. Malloch. (Communicated by Dr. HE. W. Ferguson.) (Twelve Text-figures.) .. .. .. .. .. 1- 16 The Influence of certain Colloids upon Fermentation. Parts iv-vi. By R. Greig-Smith, D.Sc., Macleay Bacteriologist to the Society. (Two Text-figures. ) ER ee Lesage 7 Pender A ta) comets 17- 24 A Note on Reproductive Pitansiene in some Lizard? By H. Claire Weekes, B.Sc., Linnean Macleay Fellow of the Society in Zoology. -° (Three Text-figures. ) Eb gates Ce, ent ee ae agent em are 25- 32 Notes on Australian Mosquitoes (Dinterat Culicidae). Part i. The Anophelini of the Mainland. By I. M. Mackerras, M.B., Ch.M., B.Sc., Linnean Macleay Fellow of the Society in Zoology. (Three Text- figures. ) cia hEAaS ; 33- 41 The Interpretation of the Radial Field be tne Wing in ne IN Gamibectous Diptera, with Special Reference to the Tipulidae. By Charles P. Alexander, Ph.D. (Communicated by Dr. EH. W. Ferguson). (Ninety- two Text-figures.) Face eine Se ree y Nene cect aoe fovea Dade seus 42- 72 The Anatomy of Cheilanthes Delee: By May M. Williams, M.Sc., Linnean Macleay Fellow of the Society in Botany. (Twenty Text-figures.) .. 73-. 84 The Geology of the Country between Lamb’s Valley and the Paterson River. By G. D. Osborne, B.Sc. (Plate i and two Text-figures.) .. 85-103 A New Deltopecten from the Illawarra District, N.S.W. By John Mitchell. j (CRIA TC RITE) etamete eer in crmeml crept senmenreC oe ct are Vater cote be a eal Ree 104 The Fossil Estheriae of Australia. Pantene: By John Mitchell. (Plates ii-iv.) SP ahaa re ldcaage 105-112 A Note on a Dicotyledonous Fossil ood fom Ulladulla, New South Wales. By C. Barnard, B.Se. (Plates v-vi and six Text-figures.) .. 113-121 On a Case of Natural Hybridism in the Genus Grevillea (N.O. Proteaceae). By C. T. Musson and the late J. J. Fletcher, M.A., B.Sc. (Plate vii.) 122-132 The Physiographic and Climatic Factors controlling the Flooding of the Hawkesbury River at Windsor. By Lesley D. Hall, B.Se. (Plate viii and nine Text-figures.) SC TARSTAT MERAY Recta eRe Ae Noy VEN Be ey Boe Lao be 309812 iv. CONTENTS. New Gall-forming Thysanoptera of Australia. By Dudley Moulton. (Communicated by W. W. Froggatt.) (Plate ix and fourteen Text- figures. ) . Biker Pncamd Os cee coe Stee An Ecological Study of ine igen GE Mount Wilson. Part iv. Habitat Factors and Plant Response. By John McLuckie, M.A., D.Sc., and Arthur H. K. Petrie, M.Sc.. (Twenty Text-figures.) Two New Species of Setaria from Western Australia. By Dr. aA S, Hitchcock. (Communicated by W. M. Carne.) SEVACEU Ty olelstin NO 2i'2))): (Issued 25th October, 1927.) The Vegetation of the Kosciusko Plateau. Part i. The Plant Communities. By J. McLuckie, M.A., D.Sc., and A. H. K. Petrie, M.Sc. (Plates x-xix and eight Text-figures.) SE AE Aad Siac Seah Australian Coleoptera: Notes and New Species. No. v. By H. J. Carter, B.A., F.E.S. (Six Text-figures.) Pca Tears iho ES eet WN AG The Gasteromycetes of Australasia. vii. The Genera Disciseda and Abstoma. By G. H. Cunningham. (Plates xx-xxii.) The Gasteromycetes of Australasia. viii. The Genus Mycenastrum. By G. H. Cunningham. (Plate xxii, figs. 5-8.) The Gasteromycetes of Australasia. ix. Keys to the Genera andl Snecies of the Lycoperdaceae. By G. H. Cunningham .. sige wae The Xerophytic Structure of the Leaf in the Australian Pecteccene: Part i. By A. G. Hamilton. (Plates xxiii-xxv and twenty-seven Text-figures. ) Australian Hesperiidae. Part i. Notes and Descriptions of New Forms. By G. A. Waterhouse, D.Sc., B.E., F.E.S. (Plate xxvi.) Notes on Australian Mosquitoes (Diptera-Culicidae). Part ii. The Zoogeography of the Subgenus Ochlerotatus, with Notes on the Species. By I. M. Mackerras, M.B., Ch.M., B.Sc., Linnean Macleay Fellow of the Society in Zoology. (Hight Text-figures.) eh ations Notes on Australian Diptera. No. xi. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) (Twenty-three Text-figures. ) : Notes on Australian Diptera. No. xii. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) (Two Text-figures.) .. BRU! Vie ee lier Descriptions of New Species of Australian Coleoptera. Part xix. By A. M. Lea, F.E.S. sveas estan Totals «ster Seasys Additional Flora of fhe Gambari Plateau, 1926. "By HK. C. Chisholm, M.B., Ch.M. On the Phylogeny of some “Diptere: SBrachvecea: Ba G. H. Hardy. (Two : Text-figures. ) 7 : Further Notes on a New Giaeuincation of AYetealiad Robbersies (piptere: Asilidae). By G. H. Hardy. (One Text-figure.) PART IV (No. 213). (Issued 15th December, 1927.) Notes on Australian Diptera. No. xiii. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) (¥ifteen Text-figures.) Pages. 153-160 161-184 185-186 187-221 222-234 235-244 245-246 247-257 258-274 275-283 284-298 299-335 336-353 354-377 378-379 380-386 387-398 399-446 CONTENTS. We Pages. Notes on Australian and Exotic Sarcophagid Flies. By G. H. Hardy. (Eleven Text-figures. ) Sh!) TEE ee Be) Diag wea ey BNC. oP aa -459 Notes on Australian Marine Algae. iv. The Australian Species of the Genus Spongoclonium. By A. H. S. Lucas, M.A., B.Se. (Plates SO QRIED OO Cs no INS cabe IRAE MIG Olay cro’ ava eth ow to AS Os, aumee tO ec TAU Studies in the Goodeniaceae. i. The Life-history of Dampiera stricta (R.Br.). By P. Brough, M.A., B.Sc., B.Se.(Agr.). (Plates xxxvi-xxxvii and fifty-eight Text-figures.) .. .. Svat | eR aduekey ey RO aL ERT Gh Oe) we EEL 498 Placentation and other Phenomena in ihe Scincid Lizard, Lygosoma . (Hinulia) quoyi. By H. Claire Weekes, B.Sc., Linnean Macleay Fellow of the Society in Zoology. (Plates xxxviii-xl and twenty-three Text- figures. ) Bik Oe OLR Ee: ON LIE ite MOE ee Notes on Australian Marine Aleaes v. By A. H. S. Lucas, M.A., B.Sc. @Blatesw xlizxivilig ss. 555-562 Mosquito Control in the Municipality, of cane Cove: New South Wales. By B. Bertram. (Communicated by Dr. I. M. Mackerras.) (Plates xlix-l, and one Text-figure.) aig ne See te ao 0o-D09 A New Dendrobium for New South Wales ead DiceeIond By Rev. H. M. R. Rupp. (Four Text- -figures. ) Sais Ree iss 0 tats aychod ee inet al rake. SD OSDIEL PART V (No. 214). (Issued loth February, 1928.) ADStract OM PhOCCCHIME Sica mein fiat Mean him cat Nie loose Ak apres SU ha xliii-liv Donations#andsHxchansesm enna 5) Winey mt en tenn eT On aunt a tapes lv-lxxiii List of Members Ooo NEG) erro ne WenGDL Monee Gipsy motets tt Gar pts eb oO-chelb.o-ayvbi Index 1xxix-xcVv vi. CONTENTS. LIST OF NEW TRIBAL AND GENERIC NAMES PROPOSED IN THIS VOLUME (1927). Page. Anthracomyia (Callophorinae, Diptera) .. .. .. .. .. .. .. .. pas Galt) Apinocis (Curculionidae) Maen Ng Ute Sn ae Oise Seraph RSet pay Vena yc Ramm PLE Asilini (Asilinae) Rb Bae tae ie ake eikrc rete -aae Uicaetinrs a i DR cacao ta Sian Nd else BIEN) Choleothrips (Kladothripinae) Bye eC eM ari tae A Dr Re etc aa AU lel ore ae Ngan! TILER IHOKCOM SON as (COMBO oboe, IDEN) 56 oo Go Go lod oo of bo oo 7H IHUSRCOTON IG (CMOS ioMmuoT, IDE) og bo of 05 oo vou. oo ‘o0 co, oo Gai EGDRTANUSOASIINAC)) ais RR pe eR, ere ree te use aca: oc eG Wines em OO ILEMIGOOaPIS (CURGWTOIICI®)) oo “oo \ido. Ge oe oo do OB oo 00, 66 “oo B70 Melanina (Sapromyzidae) Seems, ease, Weegee | Ries ect Mii Ses Vr at ele RET Ommatiini (Asilinae) OAT Uehara itis Ma inte COs OR et ee Me. SRD OS RU a i ee SOLO) LUTE OGS. (AEXOUE TO ONIGENE Arcee” ae a ou hub) ERA Dome vcig NEpou Memos COG SEMtUSU LUO CDIDECK AN meas am cee puta any lees Uaten costeeeanye CP aiNCRN I Out ar mann) LIST OF PLATES. PROCEEDINGS, 1927. i.—Geological Map of Lamb’s Valley-Paterson District. ii.—Deltopecten rienitsi and species of Estheria. lii-iv.—Species of Hstheria. v-vi.—Fossil wood from Ulladulla, N.S.W. vii—Species of Grevillea. viii.—Cracks in flood silt deposits. ix.—Kladothrips, Choleothrips and Dolerothrips. x.—Topographic map of the Kosciusko Plateau. xi-xix.—Vegetation, etc., at Mt. Kosciusko. xXx-xxii.—Australasian species of Disciseda, Abstoma and Mycenastrum. xxili-xxv.—Sections of leaves of Hakea. xxvi.—Australian Hesperiidae. XXVil-xxxiv.—Species of Spongoclonium. xxxv.—Species of Callithamnion. XXXV1-XXxVili—Dampiera stricta. XXXVili-xl.—Placentation in Lygosoma (Hinulia) quoyi. xli—Codium difforme (?), C. globosum and Avrainvillea erecta. xlii-xliii—Species of Caulerpa. xliv.—Hormosira articulata. xly-xlviii—Species of Chondria. xlix-l—Views in the Municipality of Lane Cove. CORRIGENDA. Page 194, line 19, for sanguisorba, read sanguwisorbae. Page 562, line 15, for coerulescens, read caerulescens. £4 Gi Oy gh : ‘ ral THE PROCEEDINGS OF THE TSN EAN SOCin RY OF News Sowrd, | VW ALES . WEDNESDAY, 30TH MarcH, 1927. The Fifty-second Annual General Meeting, together with the Ordinary Monthly Meeting, was held at Macleay House, 16 College Street, Sydney, on Wednesday evening, 30th March, 1927. ANNUAL GENERAL MEETING. Mr. A. G. Hamilton, Vice-President, in the Chair. The Minutes of the preceding Annual General Meeting (31st March, 1926) were read and confirmed. A letter of apology from the President (Dr. E. W. Ferguson) for his unavoid- able absence through illness was read. A letter of greeting to the meeting, dated Cambridge, England, 22nd February, 1927, was read from the Secretary, Dr. A. B. Walkom. PRESIDENTIAL ADDRESS. The past year has been one of more than usual activity in scientific affairs in Australia: The Australasian Association for the Advancement of Science and Australian National Research Council held their meetings in Perth in August last; quite a number of Australians have attended the third Pan-Pacific Science Congress in Tokio, and that important body “the Council for Scientific and Industrial Research’? has been constituted. The activity of members of the Society in conducting their own lines of research is emphasized by the fact that the volume of proceedings was larger than usual and, in addition, there were eleven papers in hand for 1927 before the close of 1926. The Australasian Association for the Advancement of Science held its 15th meeting in Perth during August, 1926. This was the first occasion on which the Association had ventured to hold its meeting at Perth, some doubt having been felt as to the possibility of holding a successful meeting in a centre which has been considered so remote. The unparalleled success of the 18th meeting in every A ii. PRESIDENTIAL ADDRESS. respect, shows that such doubt need no longer prevent Perth taking its place among the regular centres at which meetings are held. It was with very great regret that we learnt of the death a few months ago of the President of the Association, Edward Henry Rennie, M.A., D.Sec., Professor of Chemistry in the University of Adelaide, who was a native of Sydney, a graduate of the University of Sydney, where he obtained his M.A. in the same year (1876) as the late J. J. Fletcher. Professor Rennie also received the B.Sc., from the University of London in the same year (1879) as the late J. J. Fletcher. The Third Pan-Pacific Congress was held in Tokio, Japan, in November, 1926, under the auspices of the National Research Council of Japan and was attended by upward of 130 delegates from overseas. The countries represented were those bordering or having interest in the Pacific and included the United States of America, Australia, Canada, France, Great Britain, Hawaii, Japan, Netherlands, Netherlands East Indies, New Zealand, Philippine Islands, and for the first time, China and Russia. The subjects discussed at the Congress included all branches of physical and biological Sciences and a very full programme was carried out. At this meeting a Pacific Science Association was formed and a constitution adopted under which future Pacific Science Congresses will be held at intervals of not less than two years nor more than five years. The next meeting is to be held in Java in 1929. Amongst the delegates who attended were the following members of this Society: Mr. R. H. Cambage, C.B.E., President of the Australian National Research Council, Messrs. E. C. Andrews and G. H. Halligan and Professors L. A. Cotton, T. Griffith Taylor and W. N. Benson (New Zealand). The Great Barrier Reef Committee have completed their boring operations at Michaelmas Reef, Oyster Cay, near Cairns. The boring party landed during April, 1926, and operations ceased about the end of August. The boring results have yielded a rich harvest of information and have shown that the total thickness of the coral at Oyster Cay is about 427 feet. The material on which the coral rests is quartz sand, coloured green by the presence of glauconite and containing fragments of shells of molluscs and of foraminifera. The nature of the underlying quartz sand suggests that it was formed in shallow water conditions. This quartz sand was penetrated to a depth of 600 feet and practically all coralline material above it was loosely coherent, necessitating the use of casing right through. During the year several pieces of physiographical and geographical work had been completed and a report on the Barrier Reef Plankton Collections had been prepared. The Committee has decided to assist the expedition which will be sent cut during the coming year by the University of Cambridge under the leadership of Mr. fF. A. Potts, M.A. This expedition proposes to study the marine zoology and botany of a portion of the Reef. A highly successful appeal for funds to institute Cancer Research at the University of Sydney has brought the large sum of over £127,000. As members already know, the Council decided to perpetuate the memory of the late J. J. Fletcher by the institution of an annual “J. J. Fletcher Memorial Lecture”. The lecture, which is to be limited to some branch of natural history, is to be delivered at the invitation of the Council, and for the first lecture, in 1928, I am sure all will agree that no more fitting choice could have been made than Sir Baldwin Spencer, one of Mr. Fletcher’s oldest and closest friends in Australia, who has kindly consented to deliver the lecture early in 1928. In PRESIDENTIAL ADDRESS. ili. addition, it is intended to erect a small tablet in memory of Mr. Fletcher as soon as the opportunity offers. The concluding part of Volume LI of the Society’s proceedings has been issued. The complete volume (657 plus xciv pages, 48 plates and 227 text-figures) contains thirty-five papers from twenty-nine authors, including several representing first contributions by some of the younger members of the Society. The Society’s research staff contributed four papers. Exchange relations with scientific societies and institutions were normal, the receipt for the session numbering 1,821, as compared with 1,409, 1,457 and 1,450 for previous sessions. The year has been marked by the large number of applica- tions received from Societies and Institutions in other parts of the world to be placed on our exchange list. As many as possible of these have been acceded to, and the following names have been added to the exchange list during the year: Biologische Wolga-Station, Saratow, Russia; Botanic Gardens, Rio de Janeiro; Botanical Laboratory of the University of Montreal; College of Agriculture, Los Banos, Philippine Islands; Dominion Museum, Weliington, New Zealand; Institut des récherches biologiques a l'Université de Perm, Russia; Marine Biological Laboratory, Woods Hole, U.S.A.; Siberian Institute of Agriculture and Forestry, Omsk; and Instituto Botanico, Universidade de Coimbra, Portugal. The vacancies on the Council caused by the resignations of Mr. J. H. Campbell and Professor H. G. Chapman, and the death of Mr. J. J. Fletcher were filled by the election of Mr. A. H. S. Lucas, Professor A. N. Burkitt and Dr. C. Anderson respectively. As a result of representations made by Professor Sir Edgeworth David and Professor A. C. Seward of The University of Cambridge, the International Educa- tion Board (founded by John D. Rockefeller, Jr. in 1923) awarded to Dr. A. B. Walkom a Fellowship in Science to enable him to pursue his studies in palaeo- botany under Professor Seward during 1927. The Council has granted Dr. Waikom twelve months’ leave of absence to allow him to take advantage of this award; and has appointed Dr. G. A. Waterhouse as Acting-Secretary during Dr. Walkom’s absence. I have much pleasure in offering the Society’s heartiest congratulations to: Dr. P. D. F. Murray on attaining his Doctorate in Science in the University of Sydney. Mr. A. F. Basset Hull on his election as a Corresponding Member of the Academy of Natural Sciences of Philadelphia. Dr. A. B. Walkom on his election as General Secretary of the Australasian Association for the Advancement of Science in succession to Mr. E. C. Andrews. Mr. E. C. Andrews on the invitation extended to him to deliver the Silliman Lectures at Yale University in 1927. e Mr. R. H. Cambage on his election as President of the Australian National Research Council and as President-elect of the Australasian Association for the Advancement of Science. Dr. Margaret O’Dwyer on attaining the degree of Doctor of Philosophy of the University of London. During the past year the names of twelve members have been added to the roll, and two names have been removed from it, five members have resigned and we have lost five members by death. The number of ordinary members on the roll is now 168. Death has continued to take heavy toll among members, the iv. PRESIDENTIAL ADDRESS. losses for the past year including Miss E. E. Chase and Messrs. H. E. Finckh, J. J. Fletcher, Charles Hedley and Sir Hugh Dixson. Eleanor Emily Chase, who died at Roseville on 17th May, 1926, was born in Victoria and was educated at St. Catherine’s Church of England Girls’ School, Waverley and the University of Sydney. She entered the University in 1914 and obtained the degree of Bachelor of Science, with honours in Zoology and Physiology, in 1917, gaining at the same time Professor Haswell’s prize in Zoology. She was appointed demonstrator in Zoology on graduation, and in 1923 was appointed lecturer. During the five years that she was a member of the University staff she won the warm regard of her colleagues and of a large number of students by her conscientious devotion to her duties as well as by her charming personality. Her opportunities for carrying out research were limited, but she contributed one paper on “‘A new avian trematode” to our proceedings in 1920. She accompanied two important collecting expeditions during recent years, one to Barrington Tops, N.S.W., and the other to the Capricorn Group, Q. She had been a member of this Society since 1921 and was also a member of the Royal Zoological Society of New South Wales. In addition she was a Vice-President of the Sydney University Science Society, a member of the board of directors of the Women’s Union at the University, and secretary to the committee of the National Council of Women on sex education. The sudden death, at such an early stage in her scientific career, of one who had done promising zoological work and had endeared herself to those with whom her work brought her into contact, is a distinct loss to biological science. Hugh Dixson, who died at Colombo on 11th May, 1926, was born in George Street, Sydney, on 29th January, 1841. He was educated at Timothy Cape’s Academy at Paddington, and while still a youth he joined his father, who was a tobacco manufacturer, the business later becoming probably the greatest of its kind in Australia. He was deeply interested in church affairs and was a generous benefactor to the Baptist Church in New South Wales, having, with his wife Dame Emma Dixson, originated almost every existing trust fund connected with the Baptist Union, including the Aged and Infirm Ministers’ Fund, to which he gave £10,000. For some time he was president of the Young Men’s Christian Association and was a liberal supporter of the Boy Scouts. He was knighted in 1921. His general interest in science was manifested in his continuous membershio of scientific societies; he had been a member of our Society since 1887 and of the Australasian Association for the Advancement of Science since 1898. He was particularly well known for his interest in amateur gardening, his pet hobby in this respect being the growing of orchids. Herman Edward Finckh, who died at Mosman on 31st May, 1926, was born at Moore Park, Sydney, on 26th May, 1864. His earliest recollections were walks on Sunday mornings, across what is now the Golf Links, where he used to watch the aboriginals cooking over their camp fires. When ten years of age, he and his younger brothers and sister were taken to Heilbron, Germany, to be educated; he remained there for eight years, after which he toured Europe and America for two years. On his return to Sydney he went into partnership with his father, who carried on business as a jeweller in George Street, eventually taking over the business himself. He retired about fifteen years ago and devoted himself to natural history work. His earliest interest was horticulture and later on the breeding of birds and small animals, in which he was very successful. In 1904 he decided to take up marine work—an interest that grew from a desire of PRESIDENTIAL ADDRESS. Vv. his daughter (now Mrs. C. A. Messimer) to have a salt water aquarium. He began with one small tank, but later on when Mr. E. R. Waite resigned from the Australian Museum, Finckh bought his tanks. From that time onwards his tanks increased in number and he spent considerable time in studying the life histories of the Australian fishes and also many exotic species that he imported from time to time. His aquaria were well known to the naturalists of this State and he was always ready to show them to anyone who was interested. He was a recognized authority on the care and management of aquaria and during the past two years was engaged upon a book dealing with these matters and also on the life histories of some fish. It is hoped that this book will be published shortly. At the time of his death his fish numbered about 5,000 mature specimens. Finckh joined this Society in 1908; he had also been on the Council of the Royal Zoological Society of New South Wales, of which he was a Vice-President for many years; he did very efficient work as Hon. Treasurer of the Naturalists’ Society of New South Wales for many years; he was also a member of the Aquarium Society, of the Wild Life Preservation Society and of the Gould League of Bird Lovers. His keen interest in and love for nature made him a very enjoyable companion and he never spared himself in his performance of his duties in connection with Natural History in New South Wales. Joseph James Fletcher was the eldest son of the late Rev. Joseph Horner Fletcher. He was born in Auckland, N.Z. in 1850 and came to Queensland in 1860. He was educated at Ipswich Grammar School, at Newington College (of which his father was then Principal) and at the University of Sydney, gaining his B.A. degree in 1870 and his M.A. degree in 1876. In 1870 he joined the senior staff of Wesley College, Melbourne, and in 1876 went to England to study Biology at the University of London, where he obtained the B.Sc. degree in 1879, being one of the first two Australians to take a science degree from that University. Before returning to Sydney he spent some time in study at the University of Cambridge and there wrote his first paper in collaboration with J. J. Lister. This paper was published in the Proceedings of the Zoological Society of London for 1881. On his return to Sydney in 1881 he joined the staff of Newington College, where he had as a colleague R. T. Baker, until lately Curater of the Technological Museum, Sydney. He joined this Society in 1881 and was elected to the Council on 31st January, 1883. He soon attracted the notice of its founder, Sir William Macleay, who invited him to become its director and librarian. He entered upon his duties on the first day of January, 1886, and from that time devoted all his energies to the work of the Linnean Society of New South Wales. How he carried out his life work can be judged by the prominent position this Society takes in the scientific world. For 33 years he guided its affairs, edited its proceedings and when, in March, 1919, he retired from the position of Secretary, he was chosen as President, an office he worthily filled for two years. He remained on the Council until his death at Hunter’s Hill on the 15th May, 1926. His member- ship of the Society, with one exception, had been longer than that of any other member of the Society. The high degree of excellence reached in the performance of his duties is known to all workers in natural science in Australia. The PRocrEDINGS since 1886 and up to the time of his retirement may justly be said to be a monument to his capacity, his zeal and his devotion to duty. Authors of papers well know that he was ever ready to advise them and if necessary to make suggestions, which would tend towards the improvement of a paper in some detail and having set Vi. PRESIDENTIAL ADDRESS. a standard his watchful eye saw to it that such standard was maintained through- out the series. In all his doings he not only commanded our respect, but our affection as well and he served as an inspiration to many a student. Many of the leading members of the Society at the present time owe a deep gratitude to him for the valuable advice and instruction that he was always ready to give. Fletcher had a profound reverence for the founder of this Society, Sir William Macleay, and at all times instilled into our members the great debt.we owe to him. On the 14th June, 1920, to commemorate the one hundredth anniversary of the birth of Sir William Macleay, he delivered an important address entitled “The Society’s Heritage from the Macleays’’. In this he dealt with Alexander Macleay and his two sons, William Sharp and George, and it furnishes a most valuable record of what members of that family did in the cause of natural science. He had almost completed the remaining portion dealing with Sir William Macleay. Fletcher, no doubt, felt the removal of the office of the Society from Elizabeth Bay to 16 College Street, but he did nothing to oppose this step, for he foresaw that the new home nearer the centre of Sydney would increase the usefulness of the Society. His published papers include 36 in These ProceEepines together with one in collaboration with A. G. Hamilton and another with C. T. Musson, who has also presented for publication an important paper on Grevillea hybrids, based on the careful notes made by Fletcher over a period of several years. This paper will appear in 1927. In January, 1900, Fletcher presided over the Biology Section at the Melbourne Meeting of the Australasian Association for the Advancement of Science. In 1921 he was awarded the Clarke Memorial Medal by the Royal Society of New South Wales. He was a trustee of the Australian Museum and a member of the Royal Zoological Society of New South Wales. After his death Mrs. Fletcher felt that the desk, presented to her husband on his retirement trom the position of Secretary in 1919, should find a place in the Society’s rooms, so she graciously presented it to the members. It is now in the office and will be used by the future secretaries of the Society. An appreciation of Mr. Fletcher by one of his oldest friends, Sir W. Baldwin Spencer, appears at the conclusion of this part. Charles Hedley, who died at his home, ‘“Nukulailai’, Muston Street, Mosman, on the morning of the 14th September, 1926, was born at Masham Vicarage, Yorkshire, on the 27th February, 1862. On account of his health his school life was limited to two years at Eastbourne College, but he was an extensive reader and received instruction from his distinguished father, Rev. Canon T. Hedley, a Fellow of Trinity College, Cambridge. To avoid the English winters he was sent each year either to the south of France or to Italy, and at these places he began to find his first enjoyment of nature. At Mentone he purchased a book by A. Moquin-Tandon on Conchology. This book on land shells adopted what was then a modern view, that in the Mollusca the animal should be studied as well as the shell it formed. He has often spoken of this book as the one that gave him a stimulus which he carried throughout his zoological career. Here, when out collecting, he met George French Angas, a former Secretary of the Australian Museum, who was engaged in a similar occupation. Angas later gave him a letter of introduction to Dr. G. Bennett of Sydney. He left England for New Zealand in 1881, intending to learn sheep farming there, but very soon found that the wet climate of New Zealand did not suit his PRESIDENTIAL ADDRESS. Vii. health. The conditions under which he worked were far from satisfactory, so he came to Sydney in September, 1882. Shortly after his arrival he met Dr. G. Bennett, to whom he was immensely drawn. He wrote to his father, “I have again been to dinner with Dr. Bennett. Fancy speaking to a man who has talked with Cuvier, who is an intimate friend of Owen, who knew or knows Darwin, Hooker, Huxley, Lyell, Wallace, Thomson, Rolleston, Balfour, Gunther, all the distinguished men of science who have lived in the last half-century!” A trip to Hay to find if the dry inland air would relieve his asthma, was not successful, so he went to Queensland. He lived first at Nerang and afterwards took up an oyster lease at Stradbroke Is., Moreton Bay. Here, as in after years, he found he always had better health when living close to the sea. Though he was able to visit the Queensland Museum on many occasions he felt himself isolated from congenial companionship. In 1884 he was fruit growing at Boyne Island, Port Curtis, where he gathered information from the aboriginals for his first paper, “Uses of some Queensland Plants” (Proc. Roy. Soc. Queensland, 1888). Here when driving in a sulky he met with an accident, smashing his left elbow, and when he recovered he found he could no longer do any laborious work and so he left Boyne Is. in 1888 and for about two years lived in Brisbane. He occupied himself in collecting and doing voluntary work at the Queensland Museum. He found his first new species, a slug at Burleigh Heads and described it as Limax queenslandicus with figures and was pleased that his drawings caused such favourable comment. He also published a list of the Land Shells recorded from Queensland. On the ist January, 1889, he was appointed a supernumerary officer of the Queensland Museum and on 2nd May, 1889, he became a Fellow of the Linnean Society of London, and in July, Hon. Secretary of the Royal Society of Queens- land. In 1890 at the invitation of the Administrator, Sir William Macgregor, he visited British New Guinea, and reached some hitherto unexplored regions. He spent some time at the St. Joseph’s River, Milne Bay, and made important collections. Fever forced him to return to Brisbane though he wished to remain. He came to Sydney towards the end of 1890 and resided there until his death. On the 1st April, 1891, he commenced duty at the Australian Museum as assistant in charge of Landshells. On ist January, 1896 he became conchologist and on 20th December, 1908, Assistant Curator. On the death of Robert Etheridge, Junr., in January, 1920, he was appointed Acting Director until his appointment on 14th February as Principal Keeper of Collections. He resigned on 30th March, 1924, to become Scientific Director to the Great Barrier Reef Committee. Hedley’s connection with our Society began on the 25th June, 1890, when he was elected a corresponding member. On 29th April, 1891, he became an ordinary member; he served on the Council from 1897 to 1924 and was President, 1909-1911. He contributed to this Society forty-four papers—the first in 1890—and five others of which he was a joint author. These papers dealt chiefly with Mollusca, of which he described numerous new species. His papers on Zoogeography,.a subject in which he was keenly interested, are very important and he has made note- worthy contributions to the study of the distribution of plants and animals in the South Pacific. He also wrote a few papers on Ethnology. In all, he wrote nearly two hundred papers which have been published in Australia and abroad. Hedley’s papers were remarkable for the clear way he put his facts and for the interest he excited in everything he wrote. His public lectures were always crowded and, speaking in a simple way, with frequent humorous touches, he always carried his audience with him. Vill. PRESIDENTIAL ADDRESS. He was an original member of the Australasian Association for the Advance- ment of Science, was President of Section D at the Brisbane Meeting in 1909 and had attended most of the meetings since its inception and had assisted the Association in many ways. He had been President of the Royal Society of New South Wales (1914), the Royal Zoological Society of New South Wales and the New South Wales Naturalists’ Club. He was a member (1893) and Vice President since 1923 of the Malacological Society of London, a corresponding member of the Zoological Society of London (1922), a corresponding member of the Academy of Natural Sciences of Philadelphia (1893), Honorary Member of the New Zealand Institute (1924), Honorary Fellow of the Royal Society of South Australia and corresponding member of the Royal Societies of Queensland and of Western Australia. In 1916 he was awarded the David Syme Prize and in 1925 the Royal Society of New South Wales presented him with the Clarke Memorial Medal in recognition of his services to Australian Zoology. In addition to his writings Hedley was a keen explorer. He was always ready to join any expedition or trip to a place he had never visited before. He had explored most of Eastern Australia. He had visited the Gulf of Carpentaria with Dr. W. E. Roth, had led two trips to the Torres Strait Islands besides many smaller ones in Queensland and New South Wales. He was deeply interested in deep sea dredging and organized expeditions to explore the depths of the ocean. In 1905 and 1906 he was successful in obtaining a large collection of fish and invertebrates from a depth of a mile from the ocean bed off Sydney Heads—a feat never before attempted in Australian waters except from a man-of-war. With W. L. May he was the first to explore the 100 fathom zone off the Tasmanian coast and in company with Dr. J. C. Verco he lifted off Cape Borda the first deep sea bottom of South Australia. He was one of the few scientists to put on a diving dress and descend to a depth of 40 feet below the surface of Sydney Harbour. Of later years his chief interest was the study of the Great Barrier Reef, and his knowledge of it surpassed that of any other scientist. He had travelled over most of it and in his many trips he had landed at a number of the islands of the Reef area. He was the first civilian to make a trip by aeroplane over a portion of the Reef. His presence on the Pan-Pacific Excursion to the Reef in 1923 added greatly to the enjoyment and profit of those who were privileged to travel in the S. S. “Relief” from Mackay. Hedley did not confine his trips to Australia alone. He visited and collected in New Guinea, Ellice Group, New Caledonia and from all of these places he obtained valuable material. In 1896 he joined the expedition sent out by the Royal Society of London under Professor Sollas to bore the atoll of Funafuti, Ellice Group. He remained on the island for about 10 weeks and succeeded in amassing an interesting collection, particularly of invertebrate and ethnological objects, together with much valuable scientific information. An account of this work was given in “The Atoll of Funafuti’ (Australian Museum Memoirs, iii, 1896-1900), to which Hedley contributed the general account and the sections of ethnology and mollusca. Of later years he desired to go further afield to see other parts of the world, so in 1922 we find that he was in Western Canada and Alaska and in 1925 he visited Africa to see the Great Rift Valley. In the last few years the two men whose names will always be remembered in connection with Australian Zoology have passed away—the late Professor W. A. Haswell and the late Charles Hedley. Both in their own way have done more than any other two men to advance Zoology in Australia. Haswell will always be remembered for his accuracy and PRESIDENTIAL ADDRESS. ix. care of detail and he has amongst zoologists a world-wide reputation for his Text Book of Zoology. Hedley was known for his hospitality, being always the first to welcome any visiting biologist, to make them feel at home in Australia, and to place himself and his knowledge entirely at their disposal this all in addition to the reputation he had for his scientific writings. Hedley was held in the highest esteem by those who were his contemporaries and he was an ideal companion during a walk through the bush or along the sea- shore. He was of the utmost help to those younger than himself and many of the members of this Society will remember with gratitude the advice that he was ready to give them. He was always willing to listen to any biological or geological problem that presented itself-and never grudged the time spent in helping others in their work. By nature he was kindly and courteous and he was the best of friends. Zoological Science in Australia has lost a great man, who could ill be spared, but he has left behind him a monument of hard and patient work and others will arise to carry on the work he has so ably begun. The assistance he gave to young naturalists and to institutions has heen great. During his lifetime he gave many books to this Society and to the Australian Museum and by the wish of Mrs. Hedley, her husband’s books are being divided between these two institutions, so our library will be increased by the addition of many important books. During the end of April until August, 1926, he had been supervising ths sinking of the bore on Michaelmas Reef, Oyster Cay, near Cairns, and returned to Sydney about the middle of August to make preparations to visit Japan in connection with the Third Pan-Pacific Science Congress. He had to cancel his arrangements as he did not feel too well, though no serious consequences were expected and it was thought that a few weeks’ rest would restore him to health. His sudden death on the morning of the 14th September, 1926, was a great shock to all his friends. His remains were cremated and the ashes taken by Mr. E. C. Andrews and in the presence of the other Australian delegates to the Third Pan- Pacific Science Congress, distributed on the waters near the Great Barrier Reef, which he loved and knew so well. The year’s work of the Society’s research staff may be summarized thus: Dr. R. Greig-Smith, Macleay Bacteriologist to the Society, has continued his investigations into the activity of the mineral colloids such as fuller’s earth, kaolin, silica, aluminium hydrate upon fermentation. The possible assistance given to the alcoholic fermentation by their aiding the diffusion of carbon dioxide has been reported upon when it was shown that the colloids have an action of their own quite unconnected with the physical elimination of carbon dioxide. It has been shown that agar-fibre acts like the mineral colloids in accelerating the fermentation of solutions of sugar by yeast provided that a sufficient amount is present. The possible stimulation of enfeebled yeast cells by the mineral colloids led to the determination that when yeast cells are heated to just short of the lethal temperature they have a different action upon saccharose than normal unheated yeast. In presence of a mineral colloid the normal yeast inverts less saccharose and generally consumes less sugar while the heated yeast inverts the same amount of saccharose and consumes more sugar. It would seem that heating the yeast partly diminishes its invertase-secreting function. During the gum fermentation of saccharose by Bac. vulgatus it was noted that the non- reducing sugars decreased to a minimum then increased and again diminished. This led to the discovery of a substance intermediate between gum-levan and x. PRESIDENTIAL ADDRESS. levulose. Its presence can be shown but it has not been possible to prepare it in the pure state or in pure solution; it is always accompanied by levulose. Work is being prosecuted in the direction of the reason for the activity of the mineral colloids in accelerating fermentation. Miss May M. Williams, Linnean Macleay Fellow of the Society in Botany, has continued her investigations into the Cytology and Phylogeny of the Siphonaceous Algae, part 2 of which, dealing with Oogenesis and Spermatogenesis in Vaucheria geminata was published in part 2 of the proceedings for 1926. She has, further, been studying gametogenesis in Bryopsis plumosa with encouraging results. The establishment of a marine aquarium in the laboratory has enabled her to observe many interesting phases of gametogenesis. With the exception of the formation of gametes by vacuolization instead of by cleavage, the details of gametogenesis in Bryopsis plumosa are very similar to those in Codium tomen- tosum. She is investigating the problem as to whether reduction in the number of chromosomes in the nucleus occurs during gametogenesis, as in Codium tomentosum, or at the first division of the zygospore following on fertilization. As opportunity offers she is also continuing her search, as yet unsuccessful, for the reproductive organs of Caulerpa. In continuation of her work on the anatomy of certain ferns, Miss Williams has completed ready for publication a paper on “The anatomy of Cheilanthes vellea’, showing that this species exhibits, both in external morphology and internal anatomy, well marked adaptations to its xerophilous habitat. During the coming year she proposes to continue her investigations into gametogenesis in Bryopsis plumosa and to undertake a critical examination of the gametangia of Hctocarpus. Dr. I. M. Mackerras, Linnean Macleay Fellow of the Society in Zoology, has continued his investigations on the Diptera, having during the past year devoted most of his attention to the Culicidae. The results of his work are to be submitted in a series of papers under the title “Notes on Australian Mosquitoes”, parts i and ii being ready for presentation. Part i, “The Anophelini of the Mainland’, includes keys and figures which should make the recognition of the males, females and larvae of all species occurring on the mainland relatively easy. New life histories are described and notes are given on the status, habits and distribution of the species. Part ii deals in a similar way with the mainland and Tasmanian species of Ochlerotatus. In addition to completing his work on the mosquitoes Dr. Mackerras proposes to resume his studies of the comparative morphology and distribution of the genera of the Tabanoidea and to proceed with the study of other families of Diptera Brachycera. Seven applications for Linnean Macleay Fellowships, 1927-28, were received in response to the Council’s invitation of 29th September, 1926. I have pleasure in reminding you that the Council re-appointed Miss May M. Williams and Dr. I. M. Mackerras to Fellowships in Botany and Zoology respectively and appointed Miss Ida Alison Brown and Miss Hazel Claire Weekes to Fellowships in Geology and Zoology respectively for one year from 1st March, 1927. On behalf of the Society I have pleasure in wishing them a very successful year’s research. Miss Ida Alison Brown graduated in Science at the University of Sydney in March, 1922, with First Class Honours and University Medal in Geology and Second Class Honours in Mathematics, also being awarded the Deas-Thomson Scholarship in Mineralogy and a Government Science Research Scholarship. The PRESIDENTIAL ADDRESS. xi. latter scholarship was, however, relinquished by her in order to take up the position of Demonstrator in Geology, which she has held until her present appoint- ment to a Linnean Macleay Fellowship. Since graduation she has carried on research in geology and has published four papers, two in the Journal of the Royal Society of New South Wales and two in our own proceedings. The first of these papers, “Notes on hornblende and bytownite from hypersthene-gabbro, Black Bluff, near Broken Hill’, is a petrological study, and the other three are the result of field work in the districts of Milton and Moruya. For her work as a Fellow Miss Brown proposes to continue her work on the geological history of the South Coast district of New South Wales, studying in particular the geological age, conditions of sedimentation, mutual relations and tectonic history of the sedimentary rocks, as well as the relationships, petrogenesis and correlation of the associated igneous intrusions, commencing in the Moruya district and working south to Bodalla, Narooma, Mount Dromedary, Cobargo and Bega. Miss Brown comes to us with the strongest recommendations from Professors David and Cotton and she is the first woman to be appointed as a Fellow to do field work in Geology. Though her proposed researches involve arduous work in the field we may look forward to a satisfactory and successful year’s work. Miss Hazel Claire Weekes, who graduated with First Ciass Honours in Zoology at the University of Sydney in 1925, is the first woman to have been awarded the University Medal in Zoology at graduation. She was also awarded a Government Science Research Scholarship. In 1925 she commenced research work on reptilian embryology and published, in conjunction with Professor Harrison, a paper “On the occurrence of placentation in the Scincid lizard, Lygosoma entrecasteauxvi’. This paper appeared in our proceedings for 1925. These researches have been continued and a large amount of material has been accumulated, two investigations, into the reproductive phenomena in Lygosoma quoyi and the development of Amphibolurus barbatus being almost complete. This line of work gives promise of extremely important results on the morphological side of zoology and Miss Weekes proposes to continue her studies on reptilian embryology during her tenure of a Fellowship, and we wish her a most successful year’s research. I wish to bring under your notice, more particularly those of you who are entomologists, an important book written by a member of this Society, Dr. R. J. Tillyard, M.A., F.R.S., and published in Sydney by Messrs. Angus and Robertson, who have presented our Library with a copy. This book is entitled “The Insects of Australia and New Zealand”. In this work, Dr. Tillyard opens with the classi- fication of insects and gives a short account by which the 24 orders can be recognized from one another. The derivations of the names of the orders and the higher divisions are a help in understanding the various kinds of insects placed therein. A census of the insects of the world, Australia and New Zealand shows the large number of different species already known. More than one-third of Australian insects belong to the order Coleoptera and in New Zealand slightly more than one-half belong to the same order. Over 470,000 different insects have been described from the world and of these 37,000 (about 8%) are found in Australia and 8,000 (under 2%) in New Zealand. The number is being added to each year and it will not be long before 50,000 insects are known from Australia. The orders Plectoptera, Perlaria and Trichoptera are proportionately better represented in New Zealand than in Australia. Chapter ii deals with a general account of the external morphology, more detailed accounts being given in the chapters dealing with the X11. PRESIDENTIAL ADDRESS. various orders. In this chapter Dr. Tillyard explains the modern views on wing venation and gives an instructive account of the latest system of nomenclature and notation for the veins of the insect wing. Chapter iii gives a general outline of the internal morphology of insects, giving a short account of the alimentary, excretory, respiratory, circulatory, nervous and reproductive systems as well as the organs of sense. In Chapter iv a concise account of the complete life cycle of an insect is given under the headings: the egg or embryonic stage, the larva or growing stage, the pupa or resting stage and the imago or sexually adult stage. Chapters v-xxviii deal with the twenty-four orders in more detail, and treat of the suborders, superfamilies, families and in some cases subfamilies mentioning typical genera and species in each group. The whole is well illustrated with details of structures, particularly wing venation and figures, both coloured and black and white, of important species. The subclass Apterygota contains three orders of insects which are entirely wingless: (1) Thysanura (Bristle-tails, Silver-fish). In their early stages these are very similar to the adult and very little work has been done on this order. Only a few species are represented, but it is pointed out that many new forms will probably be found. (2) Protura. These small insects have not yet been found in Australia or New Zealand, but a short account of them is given so that they may be recognized when found. (3) Collembola (Spring-tails). These small and curious insects like the Thysanura and Protura are wingless, but they have no very near relations amongst the insects. It has even been suggested by some authors that they belong to a separate class distinct from Insecta. The subclass Pterygota contains all the winged insects, though some few of them do not possess wings. They are divided into two large groups. (A) Eeto- pterygota in which the wings develop as external buds during the larval stages and there is no true pupa. (4) Plectoptera (May-flies). Delicately formed insects, usually small, always found near water, in which their early stages are passed. The hindwings are often very small. About twenty species are known from Australia and New Zealand. (5) Odonata (Dragonflies, Damselflies). ‘These insects also as far as is known pass their early stages in water. They are carnivorous and both nymphs and adults feed upon mosquitoes in their various stages. Dr. Tillyard deals with this group very fully. (6) Orthoptera (Cock- roaches, Mantids, Phasmids, Locusts, Grasshoppers, Crickets). In this order the mouth parts are typically mandibulate, the larval forms closely resemble the adults except for the absence of functional wings. The order includes five very distinct superfamilies, which are considered as distinct suborders or even distinct orders by some writers. The order contains some well known insects as cock- roaches and grasshoppers and also some with very strange shapes. (7) Isoptera (Termites, White Ants). These insects are more nearly related to cockroackes than to the true ants. They are abundant in Australia especially in the north, but only four species are found in Tasmania and three in New Zealand. They cause many thousands of pounds loss each year by their attacks on houses, fences, and railway sleepers. (8) Dermaptera (Harwigs). These are not very numerous in Australia and only three species have been recorded from New Zealand where a common species introduced from Europe is becoming a serious pest to fruit- growers and gardeners. (9) Perlaria (Stone-flies). These insects form a small, but well marked order about equally represented in Australia and New Zealand. Their larvae are aquatic and are a valuable food for trout and freshwater fishes. (10) Embiaria (Webspinners). A small order resembling Termites. Only six PRESIDENTIAL ADDRESS. xiii. species are known from Australia and none from New Zealand. (11) Zoraptera. Only six species of this order have been described, none of which is found in Australia and New Zealand. (12) Copeognatha (Psocids, Book-lice). Chiefly very small insects, some of which are a pest in libraries and museums. (13) Anoplura (Lice). Both biting and sucking lice are included in this order, the Mallophaga (Biting lice, Bird lice) are represented by 88 species parasitic upon birds and marsupials, whilst only four native species of Siphunculata (Sucking lice) are known, though many introduced species occur. (14) Thysanoptera (Thrips). Small elongate insects usually infesting blossoms. This order is well represented in Australia about 14% of the known species occurring there. (15) Hemiptera (Cicadas, Plant Hoppers, Scale Insects, Bugs). The insects of this order are generally harmful, nearly all the Homoptera, and the majority of the Heteroptera being plant feeders causing destruction to vegetabie foods. Some few Heteroptera are beneficial, feeding on other insects. Scale Insects, Plant lice and other Hemiptera are responsible for the greater part of the total damage done to our crops and fruit. The division (B) Endopterygota, to which the remaining orders belong, have larvae in which the wings develop internally and have a true pupa or resting stage. (16) Coleoptera (Beetles). This is the largest order of living insects, comprising over 40% of the known insect fauna. They are an easily recognized group, the forewing being specialized as a hard horny covering for the hindwing. Many species are injurious owing to their attacks upon timber, [fruit and grain. A few are useful as scavengers and others are predatory on scale insects and aphids. The order is well represented in both Australia and New Zealand. (17) Strepsiptera, a small order of minute insects parasitic upon the orders Hymenoptera and Hemiptera (Homoptera). No species of the order have so far been found in New Zealand. (18) Hymenoptera (Ants, Bees, and Wasps). This is one of the most distinct of the Orders of Insects, usually with four stiff membranous wings, though in some groups many of the species are wingiess especially in the females. In many species the ovipositor of the female is often specialized as a sting. Some few species may be considered injurious insects and some ants and wasps are obnoxious, but generally the order may be looked upon as very beneficial to man. Parasitic Hymenoptera play a great part in the main- tenance of the balance of insect life, whereby many injurious species of other insects are prevented from overruning the world. Ants are useful as scavengers. (19) Neuroptera (Alder-flies, Lacewings). Most of the species of this order are delicate looking insects. Many of the larval forms have prominent jaws. The pretty antlions belong to this order, and also the delicate Psychopsis which are often mistaken for moths. (20) Mecoptera (Scorpion-flies). A small order with only twelve species in Australia and one in New Zealand. The perfect insects are diurnal, mostly inhabiting damp cool places. Some are predaceous, killing many small insects. (21) Diptera (Two-winged flies). In this order, except for ihose species that are wingless, the forewings are only developed, the hindwings being reduced to a pair of small club-like appendages called halteres or balancers. ‘rom New Zealand almost as many species have been described as from Australia, but this is chiefly due to the small amount of attention this group has received in the latter country until very recently. In the last two or three years many new species have been made known from Australia and though the number of flies, given by Dr. Tillyard as 2,120 when he wrote his book, is only about 4% of the world’s total of flies, if a census were now taken the percentage would be nearer Xiv. PRESIDENTIAL ADDRESS. six. It is probable that not half the flies have yet been described from Australia. Flies are undoubtedly the most important order of Insects considered in relation to man. They are discussed from their medical aspect in another portion of this Address. Besides their importance as carriers of disease, many species cause great destruction to trees, fruit and vegetables. Some few flies are certainly beneficial; the robber-flies prey on other insects. The larvae of Hover-flies prey on aphids and larvae of other groups are parasitic upon the larvae of other insects. (22) Siphonaptera (Fleas). This order is highly speciailzed and wingless. They cause irritation by their biting and are carriers of disease. (23) Trichoptera (Caddis-flies). This order is related to the Lepidoptera, in fact they are often mistaken for moths, but their wings are covered with dense hairs and rarely with seales. The early stages are passed entirely in water, the larvae living in portable cases or fixed abodes, often very curiously shaped. The larvae form one of the important articles of diet for freshwater fishes. In New Zealand the order has been more extensively studied than in Australia, from the latter country many more than the sixty species already described will be made known. (24) Lepidoptera (Butterflies and Moths). This is the best known order of insects on account of the striking beauty of many of the adult forms. The perfect insects do little damage, and are useful in the fertilization of flowers, but the larvae cause an immense amount of destruction. Chapters v to xxviii are all designed on the same plan, and consist of sections dealing with Morphology, Life History, Distribution, Fossil History, Economics and Classification. The illustrations are copious, clear and in most cases original. Each chapter concludes with references to the more important papers to be consulted for further details. Dr. Tillyard gratefully acknowledges the help he has received from various entomologists in the various orders in which they specialized. The chapter on the fossil record and origin of the Australian and New Zealand Insect Faunas shows us what has been accomplished in the space of a few years. Before Dr. Tillyard began to study fossil insects very few species had been recorded, but his enthusiasm inspired several collectors, with the result that a large number of specimens had been found and described. The number is still increasing and Dr. Tillyard has already received a large number of new specimens to study. The concluding chapter is devoted to the collection, preservation and study of insects and contains very valuable information. A glossary of technical terms is provided as an appendix. The chief importance of this valuable book to us is that it deals entirely with the insects of Australia and New Zealand. In the vast amount of original matter it contains it has a world-wide importance. Very few general entomological works are aS comprehensive and still fewer as up to date. The modern lines of research are included up to the date of writing. This is the second general entomological work produced by a member of this Society, Mr. W. W. Froggatt’s excellent “Australian Insects’ having been out of print for several years. Our congratulations are due to all concerned in the production of this book, to author, to artists, to printer and to publishers. PRESIDENTIAL ADDRESS. KV. MEDICAL AND VETERINARY ENTOMOLOGY IN AUSTRALIA.—A REVIEW. In the address from this chair last year the retiring President, Mr. H. J. Carter, gave a résumé of the evolution and development of entomology from early times to the present day. In his address Mr. Carter omitted any consideration of one important economic line of modern development—the relation of insects to the carriage of disease both in man and animals. This branch of entomology was deliberately omitted in order that I might deal with it in fuller detail than would be possible in Mr. Carter’s more general address. It would be, of course, manifestly impossible to traverse adequately the whole of this subject in the time at our disposal tonight. It is my purpose to restrict my remarks mainly to advances made by Australians in this particular field and at the same time to give a rapid survey of the special problems that confront Australian workers in the lines of medical and veterinary entomology. The whole science of medical entomology is of quite recent development and may be said to take its origin from the discovery by the late Sir Patrick Manson in 1878 of the role played by Culex fatigans in the transmission of Filaria bancrofti. This discovery established the principle of development of a metazoan parasite in an insect host. The existence of a corresponding, in this case sexual, development of a protozoan parasite in an insect host was shown by Ross’s discovery in 1898 of the life history of the parasite of malaria. Ross was unable from the lack of material to follow out all the stages in the malarial parasite, but was able to do so in the case of the allied Proteosoma of sparrows. Since that time it has been shown that a considerable number of parasites both of man and animals pass portion of their life cycle—generally the sexual cycle—in the bodies of insects. Another aspect of medical entomology later came into prominence when it was shown that bacterial agents of disease could be conveyed through the medium of insects, particularly of flies and fleas. The transmission in this case is purely a mechanical one and there is no question of the cyclical development of a parasite. The discoveries made by the protozoologist, pathologist and sanitarian in the mode of transmission of insect-borne diseases naturally led to further study of the insects themselves. Ross’s discovery of the vector of malaria and the American Commission’s discovery of the transmission of yellow fever by Aedes (Stegomyia) aegypti undoubtedly stimulated study of the mosquitoes as a whole and greatly enhanced our knowledge of the group. Similarly, the discovery of the role played by the common house fly—Musca domestica—in the transmission of typhoid, dysentery and similar diseases led to more intensive study of the Diptera as a whole, particularly of the house frequenting species. The discovery that trench fever as well as typhus and European relapsing fever was spread by the common body louse considerably increased our knowledge of the habits and bionomics of this insect. In similar fashion the study of fleas followed on the revelation of their spread of pestis bubonica and of ticks on the part played by them in the transmission of piroplasmosis and allied diseases in cattle and other animals, though consideration of ticks and mites and their relation to disease is rather outside the scope of the present address. Examples could be multiplied, but enough have been quoted to show the necessity for systematic study and classification of the insect vectors both actual and potential. I propose to discuss the advances made in Australia in the systematic study of certain groups of Australian insects which are, or which may XVi. PRESIDENTIAL ADDRESS. contain, species of economic importance from the medical and veterinary aspect as well as to outline the advances made in the study of the diseases concerned, particularly from the point of view of their relations to their insect hosts. I have excluded from my review ali consideration of the Arachnida and diseases borne by this Class, though such consideration is generally nee aEd ee as falling within the province of the medical entomologist. Viewing the Class Insecta as a whole it will be seen that only certain groups of insects are concerned in the transmission of disease, and that these are such as by their habits of life history come into more or less close association with man or animals. Practically all insects of medical or veterinary importance fall into the orders Diptera, Siphonaptera, Hemiptera and Anoplura. Diptera: Within recent years considerable activity has been shown in the study of Australian Diptera, hitherto one of the more neglected orders of Australian insects. Harly describers of Australian flies included Desvoidy, Macquart, Walker, Schiner, Thomson and Bigot. Unfortunately, many of these early descriptions are worthless and the species practically unidentifiable except in cases where the types are still available for comparison. From 1888 to 1890 F. A. Skuse contributed a series of eight papers with two supplements to These ProcEEDINGS on the Diptera of Australia. His work was, however, confined to the Nematocera, with the exception of two small papers on Acalyptrate flies of economic importance. The only groups of medical interest dealt with are the Culicidae or mosquitoes and a few blood-sucking midges comprised in the families Ceratopogonidae ana Simuliidae. Between 1914 and 1918 Arthur White published a series of papers on Brachycera Orthorrhapha dealing mainly with Tasmanian species, but including also papers on mainland species. His writings included descriptions of new Tasmanian Tabanidae. Since 1920 numerous papers on Australian Diptera have appeared, mainly from the pens of Hardy, Malloch, Bezzi, Mackerras, Hill, Ferguson, Alexander and Tonnoir. : Culicidae: Skuse (1888) first studied the mosquitoes systematically and described 19 new species. This was in continuation of his work on Australian Diptera and was not undertaken from the medical standpoint. The greater interest shown in the systematic investigation of mosquitoes following on Ross’s discovery of the transmission of malaria, and in which such men as Giles, Blanchard, Theobald, Dyar and Knab, Edwards, Christophers, ete., played a leading part, commenced in the ’nineties and has been continued to the present day. In this general study of the group, Australian species, of course, were included, mainly in the works of Theobald. In this connection full credit must be given to the unremitting efforts of Dr. T. L. Bancroft of Burpengary and later of Hidsvold to secure, either by capture or by breeding, representative collections of mosquitoes from the districts in which he was resident. In 1908 Dr. Bancroft published a census of Queensland mosquitoes in which some 32 species are listed. Though this comprised only about one-third of the species now known the work was the only list available for many years and proved invaluable to Australian workers. The next advance in the systematic study of Australian Culicidae followed on the establishment of the Australian Institute of Tropical Medicine in Townsville and the appointment of an entomologist to that institution. During the years 1912 to 1920 Mr. F. H. Taylor, the entomologist to the Institution, published a PRESIDENTIAL ADDRESS. XVil series of papers in which a large number of new species of mosquitoes are described. These included not only species from Australia, but also from New Guinea. About this period the scale classification introduced by Theobald broke down by its own weight and was replaced by the more rational structural system first proposed by the Americans and now adopted by Edwards of the British Museum. The resultant changes in generic appellations caused a period of some confusion in the nomenclature of Australian mosquitoes, which was increased by the rather considerable specific synonymy that existed. Through the joint efforts of Mr. F. W. Edwards, of the British Museum, and of Mr. G. F. Hill, then entomologist to the Tropical Institute at Townsville, the confusion was finally cleared up and the issue in 1924 by Edwards of his synonymic list of adult mosquitoes of the Australasian Region has placed in our hands an authentic list for the use of all future workers in this group. Larval characters: While the adult Australian Culicidae are now fairly well known much yet remains to be done on the identification of the larvae. Descriptions of most of the common species have been published by Cooling, Taylor and Hill, while in some instances the larvae of extra-limital species have been described by workers outside Australia. The latest worker in this field—Dr. I. M. Mackerras, Linnean Macleay Fellow in Zoology—has already a paper on the Anophelini ready for publication and a second on the Culicini nearly completed. Fieldwork: Work on Australian Culicidae has not been confined to the systematic description of new species. The work of Dr. T. L. Bancroft in collecting and breeding out species in Southern Queensland has already been mentioned. Similar work was carried out in New South Wales by Dr. J. B. Cleland largely in connection with the animal experimental station on Milson Island, Hawkesbury River. In his numerous journeys about the State Dr. Cleland also carefully collected and recorded the species of mosquitoes encountered and encouraged his officers to do likewise, with the result that it is now possible to map out the distribution of the Culicidae in New South Wales with some degree of accuracy. In North Australia much of the early work of collecting was carried out by G. F. Hill, particularly during his residence in the Northern Territory and later in Queensland and New Guinea. In Northern Queensland Taylor, Priestley, Breinl and Cooling all carried out extensive collecting. Taylor was responsible for a series of mosquito surveys of Northern Queensland towns and also undertook a survey of the mosquito population of the irrigation areas on the Murray River in Victoria. Recently, series of mosquito surveys have been made of Queensland towns mainly by Dr. Hamlyn Harris. Surveys have been made at various times in and around several of the capital cities, notably Brisbane and Adelaide. Mosquito eradication work: Only brief reference can be made to campaigns that have been instituted for the eradication of mosquitoes in various parts of Australia. The most complete and the best sustained appear to be the measures instituted by the Health Department in Brisbane, which were initiated by Dr. Elkington in 1912. Other centres in which anti-mosquito measures have been put into operation include Adelaide, Toowoomba, Kyogle and various suburban municipalities around Sydney. In New South Wales powers are given under Ordinance 41 of the Local Government Act, 1906, to enable local authorities to compel householders to LB xviii. PRESIDENTIAL ADDRESS. prevent the breeding of mosquitoes in or around their properties. This Ordinance is not in general use, but can be applied to any Municipality or Shire by proclamation. The Ordinance compels householders to keep cisterns, tanks, etc., properly screened or covered, to empty any receptacles that may contain water, to rectify defective water spouting, etc., to oil or stock with fish permanent and ornamental collections of water and generally to take such measures as may be necessary for the prevention of mosquito breeding. The more extensive work of ditching, draining, etc., must, of course, be undertaken by the local authority in each district. The stumbling block to the thorough carrying out of anti-mosquito measures is always the financial one and though in many cases something is done, the result often falls far short of expectations and it is often difficult to ensure that adequate maintenance work is continued. It is to be pointed out here that, whereas in tropical and sub-tropical Australia the eradication, or at least control, of the mosquito is a question of public health importance, in the more temperate portions of the continent this is not the case and it is merely a question of abating a nuisance. Mosquito-borne Diseases: Three distinct mosquito-borne diseases occur in Australia—Malaria, Dengue Fever and Filariasis. Malaria was at one time undoubtedly much more prevalent in tropicai Australia than it is to-day and while endemic foci probably still exist, many of the outbreaks recorded of recent years have been due to the reintroduction of the disease during the rainy season. In southern Australia only sporadic cases have occurred, some half-dozen or so being on record. (New South Wales 7, Victoria 1, Western Australia 1). While, however, the disease is a relatively rare one even in the tropical belt of Australia, the vector, the Anopheline mosquito, is widespread and has been recorded by various observers (Hill, Taylor, Ferguson, Cleland, etc.) from almost every portion of the continent. Much uncertainty exists as to the exact species of Anopheles that is responsible. The common and widespread species, A. annulipes, occurs throughout the temperate region, but appears to be, if not replaced by, at least associated with, a closely allied species, A. amictus, in northern Australia. Do the comparatively slight morphological differences between these two indicate, as Hill suggests, a possible difference in their readiness to act as vectors for the plasmodium? Or is there any difference in the avidity with which they will attack man? Reference might be made in this connection to the researches of Roubaud and others into the man or cattle attacking races of A. maculipennis of southern Europe and their relation to the incidence of malaria. That A. annulipes can carry malaria is shown by the sporadic cases in New South Wales. There are, of course, other species in tropical Australia, notably A. bancrofti and A. punctulatus, which may be responsible for the conveyance of malaria in these regions. It is to be noted that in Australia no species has been actually proved to be a vector by experimental feeding on malarial patients and afterwards finding the developing sporozoites on dissection of the mosquito, though Heydon in 1923 proved by experiment that A. punctulatus was an efficient carrier at Rabaul. Clearly the factors governing the incidence of malaria, even in the tropical portions of Australia, are not fully known and require investigation. The fact of Australia’s comparative immunity may depend on questions of sparseness of population or, as mentioned above, on relative unsuitability of the insect vector. Dengue Fever: It is now definitely established that dengue fever is conveyed through the medium of infected mosquitoes; the great part played by Australian workers in the elucidation of the aetiology of the disease was the proof of a PRESIDENTIAL ADDRESS. . xix. particular mosquito—Aedes (Stegomyia) aegypti—-as vector. Graham working in Syria first definitely proved that dengue was conveyed by mosquitoes and, though his results appeared to incriminate Culex fatigans, it was admitted that his stocks of this species probably contained individuals of Ae. (Steg.) aegypti. Experiments by Ashburn and Craig were not more conclusive. In 1906 Dr. T. L. Bancroft of Queensland definitely succeeded in transferring dengue by means of Ae. (Steg.) aegypti in two instances. This positive result was overlooked for some years and left some doubt as to whether other methods of infection could be absolutely excluded since Bancroft was working in a dengue district. In 1916 Drs. Cleland, Bradley and McDonald of Sydney, in a series of well planned experiments, definitely proved Ae. aegypti to be the vector. These observers brought down Ae. aegypti from the northern rivers of New South Wales to Sydney, where this species does not occur, and by feeding them on volunteers succeeded in reproducing the disease in four instances, the diagnosis being confirmed by inoculation experiments in other volunteers. Their results have been confirmed since by workers in other parts of the world, notably in the * Philippines. The Philippine Commission found that Ae. aegypti did not become infective until eleven days after feeding on an infected patient. This is against the whole evidence of the epidemiology of the disease, which indicates that the mosquito may be infective during the first three days after feeding on a patient. This was shown furthermore to be the case experimentally by Chandler and Rice in Texas. It appears from a study of the Philippine Commission’s report that no experiments were carried out with infected mosquitoes under seven days after being infected and it may well be that there are two methods of infection—a mechanical method of transference of infected material within the first three days of infection of the mosquito and a developmental method in which the parasite undergoes some change in the mosquito, which does not become infective for eleven days. Further work is required on these points. The causal organism of dengue itself yet remains to be discovered. Dengue is endemic in northern Australia and invades southern Queensland and northern New South Wales at irregular periods. When the disease makes its appearance up to 90% of the population of a town may be infected. Possibly the periodicity of the appearance of the disease may be associated with mass immunity of the population from a previous epidemic. The fact that the vector disappears from a locality during the colder months in the more temperate portions of its habitat, passing the winter in the egg stage, accounts for the disappearance of the disease with the onset of cool weather. Until the 1926 epidemic in New South Wales dengue had only been recorded from towns along the north coastal rivers, but in 1926 towns along the north-western slopes and on the north-western plains were heavily infected. Enquiry showed the presence of Ae. aegypti wherever dengue was present and revealed the fact that this species of mosquito was much more widely spread inland than had been previously known. Whether the inland spread was a recent one or whether the presence of the mosquito had been merely overlooked could not be determined. Filariasis: The third great mosquito-borne disease—filariasis—is widespread, at any rate in certain of the Queensland coastal districts. The discovery of the parent worm—Filaria bancrofti—was made by the late Dr. Joseph Bancroft of Brisbane in 1876. The fact that the mosquito was the vector was discovered by Sir Patrick Manson at Amoy, in China, in 1878, but the full details were not worked out; this was largely done by Dr. T. L. Bancroft in Brisbane in 1899. Xi. PRESIDENTIAL ADDRESS. Filaria has been proved to be carried by a number of different mosquitoes, the commonest being the night feeding mosquito, C. fatigans, and it was with this species that Dr. T. L. Bancroft successfully worked in Queensland. Further work by Miss M. J. Walker in Brisbane in 1923-4 confirmed Dr. Bancroft’s results with C. fatigans. Both observers obtained partial development in C. annulirostris; other species of mosquitoes yielded negative results. In the Pacific Islands the common vector as shown by Dr. Manson Bahr (1912), is Ae. (Steg.) variegatus, but this species does not touch Australia; furthermore, the island disease is non- periodic and is associated with numerous cases of HElephantiasis, whereas the Queensland disease is definitely nocturnal in periodicity and Elephantiasis is extremely rare, while lymph varix, chyluria, etc., are not uncommon. A consider- able field, therefore, yet awaits the investigator in Queensland into the aetiology of the disease, work in which both the pathologist and the entomologist might be suitably employed. Tabanidae: This family, familiarly known in Australia as March Flies, are abundantly represented, close on 300 species being known. Many of the better known forms were described by Macquart and Walker in the early part of last century. Ricardo, in a series of papers in the Annals and Magazine of Natural History from 1900 to 1917, reviewed many of the older described species as well as described many others as new. Australian workers were thus able to place correctly many species whose identity would otherwise have been uncertain. F. H. Taylor (1913-1920), of the Australian Institute of Tropical Medicine, Townsville, in a series of six papers, four of which were published in These PROCEEDINGS, added numerous species, mainly from northern Australia. During the years 1919-20 additional species were added by Ferguson, Ferguson and Henry, and Ferguson and Hill. These authors also discussed the somewhat extensive synonymy that had grown up in the family. Studies on the life histories of Australian Tabanidae were published by T. H. Johnston and M. J. Bancroft and by G. F. Hill, but the life history of only some half-dozen species is as yet known. In connection with the work on Onchocerciasis extensive collections of Tabanidae have been made in various parts of Australia in response to appeals made by the various committees appointed to investigate this disease. These collections have led to a great increase in our knowledge of the distribution of these insects as well as to the access of new species. Diseases conveyed by Tabanidae: While no disease has been definitely proved to be conveyed by Tabanidae in Australia, strong suspicion falls on these flies as the probable vectors of Onchocerca gibsoni, the causal organism of bovine Onchocerciasis. This nematode disease is widespread in the Northern Territory, Queensland and New South Wales and is responsible for severe economic loss. While the causal organism is known, the mode of transmission is as yet unascer- tained, though various facts point to the vector being a flying insect. HExtensive feeding and other experiments with Tabanidae carried out at Kendall yielded negative results, which could not be regarded as conclusive. Dissection in a few cases showed the presence of larval filariae in the proboscis of Tabanidae. Similar larvae had been found by Johnston and Bancroft in Queensland and named Agamofilaria tabanicola. These authors regarded the larvae as probably immature forms of some species parasitic in a native animal or bird. Reference might be made here to certain suggestive experiments recorded by Dr. Cilento of Townsville. In the one observation, Tabanidae were seen to bite two cattle on the brisket; the PRESIDENTIAL ADDRESS. XX spots were marked and later worm nodules found to have developed there. In the second case the crushed up heads of several Tabanids, in which nematodes were seen in the proboscis, were injected into the brisket and were followed by the development of worm nodules. The value of these experiments was to a certain extent impaired by the fact that they were carried out in a district in which the disease is naturally common and other modes of infection could not be excluded. The whole question of the transmission of Onchocerciasis was further com- plicated by the discovery that two other species of Onchocerca—O. gutterosa and O. lienalis—occur in Australian cattle and in no case is the vector known. There is no evidence that Tabanids have ever been associated with the spread of anthrax in Australia, as appears to have been the case in other countries. Other blood-sucking Diptera: The Leptidae, though usually non-blood-sucking flies predaceous on other insects, contain a single Australian genus of blood- sucking species, Spaniopsis, which is confined to this country. Some five or six species are known, but they are of academic interest only, as they are not known to be associated with any disease. Simuliidae or Buffalo gnats are represented in Australia by fourteen described and a number of undescribed species. The family was revised in 1925 by Tonnoir. Ceratopogonidae: Minute midges belonging to the genera Culicoides and Leptoconops are widespread in Australia and are commonly termed sandflies. They are vicious “biters’, raising irritating papules which are generally more irritant after twenty-four hours or longer. The various species found in Australia have been by no means thoroughly investigated, though some half-dozen have been described. Psychodidae: A single species of Phlebotomus has been described from northern Queensland by G. F. Hill. It is not Known whether it is associated with any disease, but short duration fevers analogous to three day or Phlebotomus fever are known to occur in the tropical regions of Australia. Muscidae: Two blood-sucking species of Muscidae occur in Australia, both introduced. Stomoxzys calcitrans—the stable fly—is widespread throughout the continent and, though usually confining its attention to cattle and horses, will on occasion attack man. It has been suspected as a possible vector of Onchocerca gibsoni, but extensive experiments with calves failed to prove any causal relation. S. calcitrans has been accused, at various times, of transmitting infantile paralysis, anthrax and surra, but there is no evidence that this species has ever acted as vector of these diseases in Australia. ‘The stable fly is, however, known to be the intermediate host of Habronema microstoma, a nematode parasite of horses in Australia. The life history of this parasite and its allies—H. muscae and H. megastoma—have been worked out by Hill, Bull, and Johnston and Bancroft. Haematobia exigua (Lyperosia exigua), a close ally of Stomoxys calcitrans, has been introduced into northern Australia and has spread from the Northern Territory into the Kimberley district of Western Australia. The attacks of this insect cause considerable irritation and the formation of intractable sores, leading to marked loss of condition in the cattle attacked. The presence of the fly is thus of serious economic importance and is the subject of special investigation by the Commonwealth Government. Non-blood-sucking Diptera: The vast number of Diptera are non-blood-sucking and only a few are of interest as actual or potential carriers of disease. Certain flies by habits of breeding or by predilection for certain food are attracted to Xxil. PRESIDENTIAL ADDRESS. human dwellings and come into close contact with man. Species that breed in excreta and that are attracted to food stuffs are especially dangerous: Practically all the important species are contained in the families Muscidae, Calliphoridae and Sarcophagidae. Muscidae: Musca domestica, the commor house fly, is par excellence the species responsible for the spread of disease, particularly such diseases as typhoid, infantile diarrhoea and dysentery. Since the discovery of the role of this species in spreading typhoid fever, a discovery that followed on the Commissions of Enquiry into the typhoid of the Spanish-American and South African Wars a vast amount of evidence has accumulated incriminating this species and an extensive literature has been compiled of its habits, bionomics, etc. While we thus have a considerable mass of information on these points most of the evidence has been obtained by study of the species in other regions and mainly in temperate climates. Further information is required as to the bionomics of M. domestica under Australian conditions, though in essentials the life history will be found to be the same in all countries. There are, however, questions of possible aestivation in the height of summer—it is a well known fact that flies are less abundant in the summer than in spring or autumn; questions of the relative abundance in different localities and States, to mention only two of the many obscure but important aspects of the bionomics of the house fly under Australian conditions. Such questions may be of paramount importance in the study of disease. Why is infantile diarrhoea more common in a hot, dry summer? Is this related to an increase in the fly prevalence during such seasons? What is the relation of its local incidence to that of house flies? It is freely stated that the seasonal curve of this disease closely follows that of the prevalence of flies. As a matter of fact, there is no adequate data on which the latter curve could be constructed for any part of Australia. To answer these and similar questions fly counts spread over a number of years are necessary. Such fly. counts are unfortunately not available, with the exception of a short series made by Dr. J. B. Cleland some years ago in Sydney; their institution and maintenance over a series of years is becoming a matter of urgent importance. Prevention of Fly Breeding: Though the principles of the prevention of fly breeding are well known, but little has been done to minimize the evil. Adequate powers exist under various by-laws and local government ordinances to regulate the storage and disposal of manure, the disposal of garbage and rubbish, the care of stables, dairies, the construction and care of privies, etc., but though these regulations may be, and generally are, enforced, many exceptions exist. I have personally seen conditions existent in country towns which were a disgrace to the community. The control of these conditions is, of course, a matter for the sanitarian. The entomologist has done his share in pointing out the conditions regulating fly breeding; he cannot do more. Too often, however, the efforts of the municipal sanitary or health inspector are nullified by the apathy or even active opposition of the local council. Better results might be obtained if all health inspectors were directly under the control of the central health authority and not servants of local councils. Conditions are as a rule better in the larger towns and cities and the advent of the motor has helped to diminish the fly prevalence by the decrease in the number of horses and the consequent lessening of the use of stables in the cities. In some degree the fly prevalence in a community may be measured by the typhoid incidence. Certain towns, particularly where water carriage of sewage exists, are always free from the disease. This does not PRESIDENTIAL ADDRESS. Xxili. necessarily mean a lessened fly prevalence, but that the fly has not the opportunity to come in contact with infected material. In other towns typhoid recurs annually. That typhoid fever is diminishing with yearly fluctuations in New South Wales is shown by the figures for the yearly incidence for the last ten years. To obtain a proper indication of the spread of typhoid by flies it would be necessary to deduct cases due to other causes, such as direct contamination of food, milk, etc., at the hands of typhoid carriers. TABLE I.—TyPHOID FEVER. Year. | Population. Cases. Deaths. ee eee — —— —, 1917 1,886,701 1,091 103 1918 1,928,174 | 810 112 1919 2,000,173 857 | 106 1920 2,099,763 1,016 | 132 1921 2,128,786 | 949 | 129 1922 2,174,688 | 706 99 1923 2,211,106 873 104 1924 2,256,649 | 768 97 1925 2,306,081 | 533 80 1926 2,349,000 674 | — | Several other species of Muscidae closely related to the house fly have been described from Australia; the nomenclature of these is by no means settled, since some extend beyond Australian limits. The most important is, however, Vivaparomusca ventustissima, the well known bush fly. This species is widely distributed throughout Australia, and though it does not enter houses it will persistently attack man in the open, being especially attracted by moist surfaces, such as the eyes, nostrils, lips, or by open sores. Its prevalence varies greatly in different years and there is reason to believe that the species is associated with the spread of ophthalmic infections, such as conjunctivitis (“Sandy blight”) and trachoma. It may also be the transmitting agent in cases of Bung-eye. This species was extraordinarily abundant in the summer of 1923-24 and according to the evidence of the school medical services this season was associated with an unprecedented number of cases of ophthalmia in country schools. An account of the bionomics of this species in Queensland was published by Johnston and Bancroft. Calliphoridae and Sarcophagidae: These two families may be briefly considered together since in both cases the habits are similar. They are largely of importance because of their habit of attacking meat and depositing their larvae and eggs thereon, thus rendering it unfit for human consumption. The more severe economic loss occasioned through the blowing of sheep will be considered under myiasis. Both families are strongly represented in Australia. The Sarcophagidae have been studied by Johnston and Tiegs and by Johnston and Hardy and in a series of papers by these authors some 25 species are recorded from Australia. The Calliphoridae have until lately been in a state of some confusion as far as the nomenclature is concerned, despite attempts by Patton and by Hardy to elucidate the family. I have recently received, however, a paper by Malloch on XXiv. PRESIDENTIAL ADDRESS. the family, which will be presented to this Society during the current year and which will place the Australian species on a sound classificatory basis. The question of the correct nomenclature is of importance, as Malloch found that under several of the commonly accepted names two or more species have been included. Differences of chaetotaxy and of male genitalia have been largely neglected in the past, but these may be of great importance in determining specific status. The bionomics of the Sarcophagidae have been largely studied by Johnston and Tiegs and by Johnston and Hardy, and the latter author has also devoted considerable time to the study of the bionomics of the Calliphoridae in Queensland. Bionomic studies of the Calliphoridae were also made by J. L. Froggatt in his investigations into the sheep-blowfly problem. Reference may here be made to the series of experiments carried out by W. B. Gurney into the range of flight of Australian blowflies. This observer found that marked blowflies could be captured up to ten miles from their point of liberation. Myiasis: By myiasis is understood the development in man or animals of the larval and pupal stages of dipterous parasites. Such myiasis may be more or less accidental or may be, as in the case of the bot flies, a constant phase in the life history of the particular species of fly. Both the common species of blowfly— Calliphora stygia and C. augur—may on occasion give rise to accidental myiasis, generally in the nature of the blowing of open wounds. Cases of intestinal myiasis are also known, the fly concerned being Fannia canicularis, a common introduced species. Much more important than these cases of human myiasis is the condition of myiasis in sheep due to infestation mainly of the crutch with one or more of the common blow or blue bottle flies. The condition has become so serious during recent years that considerable economic loss has been occasioned, not only through death of affected animals, but also through deterioration of the wool through constant yarding, etc., for the purpose of jetting and crutching or other remedial measures. In New South Wales a special combined Committee of the Department of Agriculture and the pastoralists has been investigating the condition for several years and experimental stations have been established in various parts of the country, but no certain remedy has been discovered; the best results appear to have been obtained by jetting and crutching under pressure, but this entails constant care and treatment at intervals. Efforts to find.a deterrant which would adhere to the sheep for any length of time have met with little success. Attempts have been made to control the fly by means of liberating parasites, notably Mormoniella brevicornis, but though success has been claimed in certain districts this has not been the universal experience. More assistance might be obtained by more careful attention to clearing up possible breeding places, particularly of carcases, refuse around shearing yards, ete. In this connection the flight experiments of Gurney become of importance as showing the extent of country that may be infested by one dead sheep. Some six or more species ot fly have been incriminated of attacking sheep, but some are probably merely secondary invaders. The status of Ohrysomyia albiceps, for instance, as a sheep maggot fly has been disputed, some authorities suggesting that it is predaceous on the larvae of other flies present in the wool. It is probable, however, that this species does actually attack the sheep, though it may also act as a predator. The Oestridae or bot flies are represented in Australia by four introduced and one native species. The habits of the introduced species appear to be identical with their habits in Europe. Further information is, however, required in PRESIDENTIAL ADDRESS. : XXV. respect to the time of the year at which infestation occurs, as, according to information gleaned by Mr. Clunies Ross in Western Australia, this appears to be different in Western Australia from what it is in New South Wales. The one native species, Tracheomyia macropi, is an inhabitant of the trachea of kangaroos; only the larval and pupal stages are known; the adult does not appear to have been seen. Parasitic Flies: The Hippoboscidae are represented in Australia by three introduced and a fairly large number of native species, most of which are as yet undescribed. The introduced Hippobosca equina and H. camelina occur in Western Australia, but are not known to carry any parasitic disease in Australia. Both species are unrecorded from eastern States. The sheep ked, Melophagus ovinus, is widely introduced. The native species mostly belong to the genus Ornithomyia and are parasitic on birds; there are, however, three or four species of Ortholfersia which are parasitic on marsupials (kangaroos and wallabies). The Nycteribiidae or bat flies are represented by a number of species belonging to the genera Nycteribia and Cyclopodia; the species have recently been mono- graphed by A. Musgrave. Streblidae are known to occur on Australian bats, but no species have so far been described. Siphonaptera: Australian fleas have been mainly investigated through the researches of Dr. Karl Jordan and the late N. C. Rothschild. Some 35 species are known, mainly parasitic on native rodents and the smaller marsupials. In many instances the species are not restricted to one host, but may occur on a wide range, including both rodents and marsupials. Bat fleas occur, but have not been thoroughly studied. The Sarcopsyllidae are represented by some half-dozen species, including the well known Echidnophaga gallinacea, the stick-fast flea which has been the cause of considerable economic loss in poultry in Western Australia. It is generally assumed that this species was introduced into Western Australia, but it was certainly present in that State for several years before it attacked the poultry and it is possible that the species is a native of Western Australia. E. gallinacea was originally described from Ceylon, but it was already present as a pest in that country and may well have been introduced from Western Australia. Undoubtedly the home of the genus Echidnophaga is in Australia, to judge from the number of species there represented. EH. gallinacea occurs also in South Australia, but not commonly, whereas in Western Australia almost every animal is affected and even children are attacked. In addition to the native species of Siphonaptera, several introduced species occur in Australia, of which the most important are the rat fleas, parasitic on the introduced black and grey rats—R. rattus and R. norvegicus—and in particular the so-called Indian rat flea—Xenopsylla cheopis—the vector of plague from rat to rat and from rat to man. The association of this species with the transmission of plague was first suggested by Simond in 1898, but it was Dr. Ashburton Thompson of Sydney who, during the 1900 outbreak, clearly showed on epidemiological grounds that the bubonic plague could be spread only through the medium of such an insect as the rat flea. His conclusions were fully verified experimentally by the Indian Plague Commission, of which Professor C. J. Martin, formerly of Sydney and Melbourne, was a member. The question of the distribution of Xenopsyllia cheopis in Australian ports is of some importance. The species is known to occur abundantly on rats in Sydney, Brisbane and other New South Wales and Queensland ports and in Perth, Western XXvi. PRESIDENTIAL ADDRESS. Australia. In Sydney about 45% of the rat fleas belong to this species and it shows a distinct seasonal prevalence, being most abundant during the plague epidemic months, February to May. The species occurs in Adelaide, but I have no knowledge of its relative prevalence; whether it occurs in Melbourne, apart from specimens taken on ship rats, appears uncertain. It seems to be absent from Tasmania. It is noteworthy that Melbourne, Adelaide and Hobart have always escaped infection at times when plague was rampant in other Australian ports. The number of fleas captured from rodents in Sydney is shown on the following table: TABLE II.—FLEAS FROM RODENTS. MICROBIOLOGICAL LABORATORY, 1909-1926. Name 1909 1910) LOTT | 1912) 1913) 1974 TQ |) ALB. ||) TLS) L7 | 1918 2 eee pepe re ij Xenopsylla | . | OBOE 65 | oo) |l-ileat 701 | 1,105 641 213 233 22 300 197 | 67 Leptopsylla | musculi 514 541 | 1,065 442 113 eal 156 108 60 | 63 Ceratophyllus | fasciatus 210 266 375 PANG) 31 94 72 76 57 | 47 Ctenocephalus | canis or felis.. 10 8 mal 14 3 2 4 8 1 1 Pulex irritans .. 1 aL 1 — — — — — — | — Pygiopsylla rainbowi — — = = as a= = — pees | = Echidnophaga myrmecobii = = ==> = = — cae = = | = | Total ILS PAD |) dS |) Gee) WSUS | 360 700 484 492 | 315 | 178 | | | Name 1919 1920 | 1921 | 1922 | 1923 | 1924 1925 | 1926 Pee % eS = | Xenopsylia | | cheopis 64 302 612 | 1,268 895 539 304 del || 9,215 || 44-55 Leptopsylla | musculi 7 202 780 NG, 672 639 689 362 | 7,541 || 36°48 Ceratophyllus fasciatus 30 169 503 542 376 284 309 107 || 3,767 || 18:22 Ctenocephalus canis or felis.. 1 6 18 29 if 4 2 2 135 0-65 Pulez irritans .. == 1 2 4 2 4 — 16 0-08 Pygiopsylla | rainbowi = — — — | =: 1 —— — 1 0-005 Echidnophaga | | myrmecobii — — — 1 a — — 1 0-005 Z. pas | ee Total 102 680 | 1,915 | 2,601 | 1,954 11,469 | 1,308 802 |/20,676 ||100-000 | | | Hemiptera: The great order of the Hemiptera or bugs calls for little mention. The common bed bug—Cimez lectularius—is introduced and is now widespread throughout Australia. It is not known to carry any disease in Australia, but its PRESIDENTIAL ADDRESS. ; XXVIi. presence is regarded as evidence of dirty and insanitary conditions. In Australia we are fortunately free from such blood-sucking Hemiptera as Conorhinus and its allies, which carry Chagas disease in South America. Anoplura: The three species of human lice occur in Australia as well as the common lice of domestic animals. The three great louse-borne infections of man— Typhus, Relapsing Fever and Trench Fever—do not now exist in Australia, though it is probable that typhus did occur in the early days of colonization. Reference might be made to the occurrence in recent years of a typhus-like disease in Adelaide. The disease is characterized by many of the features of typhus, though in a milder degree, and the serum of patients gives the typical agglutination reaction with Proteus X19. The disease is probably a member of a group of closely allied diseases which includes typhus. The interesting point from the entomo- logical aspect is that the disease does not appear to be infectious, but is probably conveyed through the medium of some insect, or possibly acarine, parasite; research has, however, failed so far to reveal the mode of transmission. A similar, if not identical, disease has recently been recorded as occurring on farms in the vicinity of Toowoomba, Q., and it is probable that cases elsewhere may have been overlooked or confused with typhoid fever. _. Other diseases exist in Australia, of which the aetiology and mode of transmission is still unknown. Some of these may perhaps be insect- or mite- borne. Mention has already been made of short-period coastal fevers in the tropical zone; two other diseases as yet unelucidated might be mentioned— Sarona Fever and Mossman River Fever. The latter at any rate appears to be allied to Japanese River Fever and, like it, is probably carried by some species of mite. : The above review of medical and veterinary entomology in Australia does not pretend to be exhaustive. Ample has, however, been said to show the importance of the subject and something of the problems that still await elucidation. Hymenoptera: Though not containing any disease-carrying insects, the Hymenoptera (bees, wasps and ants) are of interest to the medical and veterinary entomologist from two points of view—firstly, many of the species will attack human beings, inflicting severe stings; and secondly, several of the smaller Hymenoptera are parasitic on flies of economic importance. Stings from certain wasps, bees and ants are of common occurrence, but are rarely recorded in medical literature. Cleland, in his paper “On Injuries to Man due to Insects’, has collected a number of records. The more common stinging ants belong mainly to the Ponerinae and include bull ants, soldier ants and jumpers. A common stinging species is the greenhead (Chalcoponera metallica). Several instances are on record where injured people have been attacked by ants and portions of their faces or limbs eaten away. The parasitic Hymenoptera of interest to us mostly belong to the Chalcidoidea. Mormoniella brevicornis (Nasonia brevicornis) has already been mentioned; it is parasitic in the pupae of blowflies and attempts, largely unsuccessful, have been made to control the sheep-blowflies by its use. Other species have been suggested for the same purpose, but have not been tested out on the same scale. Attempts are now being made in Western Australia to establish the English blowfly parasite (Alysia manducator). The Australian Hymenoptera have been fairly extensively studied; the wasps by Dodd, Girault, Turner and others; the bees by Cockerell, and the ants by Wheeler. Lately J. Clark, formerly of Western XXVIii. PRESIDENTIAL ADDRESS. Australia and now entomologist to the National Museum, Melbourne, has taken up the study of the ants and has published several papers on the Ponerinae. In conclusion, I desire to express my appreciation of the cordial co-operation accorded me by my colleagues on the council and in particular by the permanent officials—Dr. A. B. Walkom and Dr. G. A. Waterhouse. I also wish to thank Mr. Carter and Dr. Mackerras for their help in revising the manuscript of this address; the latter has been of great assistance in checking all references at a time when I was unable to do so. The following letter was sent to Their Royal Highnesses the Duke and Duchess of York on the occasion of their visit to Sydney: “We, on behalf of the Members of the Linnean Society of New South Wales— a Society founded in 1874 to encourage the study of Natural History in Australia— desire to offer to Your Royal Highnesses this brief record of our loyalty to the Throne and of the pleasure evoked by the visit of Your Royal Highnesses as the representatives of our revered Sovereign and Her Majesty the Queen. May we be permitted to offer our respectful greetings and sincere wishes for an enjoyable visit, and for the welfare of Your Royal Highnesses during your return journey to Great Britain.” It was with deep regret that we learnt of the death last’ week of Professor A. A. Lawson, D.Sc., F.R.S., F.R.S.E. Professor Lawson was the first occupant of the Chair of Botany in the University of Sydney, being appointed to that position in 1913, when the Chair of Biology was divided, the late Professor W. A. Haswell remaining as Professor of Zoology. The late Professor Lawson worked hard to bring the School of Botany to its present high state of efficiency and had only recently been elected a Fellow of the Royal Society of London. Professor Lawson was a member of the Council of this Society in the years 1922-1924. Dr. G. A. Waterhouse, Hon. Treasurer, presented the balance sheets for the year ending 31st December, 1926, duly certified as correct by the Auditor, Mr. F. H. Rayment, F.C.P.A., Incorporated Accountant; and he moved that they be received and adopted, which was carried unanimously. No nominations of other Candidates having been received, the Chairman declared the following elections for the ensuing Session to be duly made:— President: Professor L. Harrison, B.A., B.Sc. Members of Council: C. Anderson, M.A., D.Sc., Professor A. N. St. G. H. Burkitt, M.B., B.Sc., H. J. Carter, B.A., F.E.S., Sir T. W. E. David, K.B.E., C.M.G., D.S.0., B.A., D.Se., F.R.S., A. G. Hamilton and A. H. S. Lucas, M.A., B.Sc. Auditor: F. H. Rayment, F.C.P.A. The following resolution was carried unanimously: That the nerinere of the Linnean Society of New South Wales assembled at the Fifty-second Annual General Meeting desire to express their warm appreciation of the services rendered to the Society by the retiring President (Dr. E. W. Ferguson) during his year of office and their deep sympathy with him in his long illness and trust that he will make a speedy recovery. “LOINSBVILL, AIBIOUOFL ‘USNOHYALVM ‘AIVNUBLE ISTZ Vv ‘KoupAg “LOVIPNW “Vd0U ‘LNGWAVU H ‘peonpord setjtanoag ‘166. ‘Advenaqeaq yt ‘AvupAg ‘1091100 PUNO] pue poulWexy TL TL 9FF SF TE TE 9b Ss } 218 = St 8/20) | 0 SI T¢é | 0 0 008 IT 4 86 9 LI 96 9 6 O06 6 &I LP ; (t) GYR 1h "* 7BILOWUZY, 9A, 0} suOTIdIIOsqns “ [tS She Oak = Ce eee Sila (ROC SBIE dULOoUul SNe AO) o/V SsdiqsMoT[ay “ Cacia: ae OT 61 IST (Sore MA 0 Sit a yINnos MON JO JUSTIUIAGAOH Aq poseyoind G T 08 SSUIpse001g JO soldod QO, sUuIpnpour) setVg “| b 6 «OOF 8 8 16S se o. o. 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PXSXOXSIE ‘TaINSevII], ATCIOUOFL ‘ASNOHYALVM ‘V ‘D G89'TS ‘LZ6L ‘Adenuee ysTzZ ‘AaupAG sooq uolyIny, “ CORTE punyoy “ yseteyur “ GZ6T Worl soueleg A Vac OY) @ © WH 1 T GE GGSh 6 LI 926 DS F BS F GT 680°STS b GI 6&2 ae @ @ © G OF Ser TE GT 60T 0 0 008°FT ‘DIS oS: WW a "+ puey uy yueg Ssulaeg JUSUIUIIAO ‘S.LUSSV Oo) sulyueg [elo1eurwmi0gn :Yysep) suvO'Ty YI[VaMUOMIUIOD “I0IPNV ‘LO6T ‘Atenaqoaq WIL ‘AoeupAg “Wd0U ‘LNAWAVY 'H ‘pesonpoid setjlunoeg bv GT S89°TS b CT 6E0'T € i 1 6 6 & «(0G a 0 ce 1) 3) J091100 puUNO] pue peurMexy L@6T 0} SouRTeg “ i ysep Ajjed “ Siieaneenn) pue snzeieddy “ sosuedxy “ soseM pure solie[eg OJ, "926. “Haquiacaq 34SLE papuy 4e9A “LNNODOV AWOONI b GT 680'STS "9261 ‘laquisceq ye ve LAAHS AONV IVE “LNNODODV ADOTOISLOVE ** 92761 ‘taquIe00q ISTE 1B 0/W ouLODUT ‘* - pastpeyides ouloouy poiefnuINndDy Pere WM JIG Aq poyyeonbeq JUNOUTY ‘SUILLITIGVIT cue re 1 ee * i i} ; hy } 1 ey) } dt} . yee c I ia \ ae beats i ic < Bt ay ‘ Cin (ass 4 , t = Ei eetary | i y i we i ny { ee a } eal , a a. 9c ant le + 4 s* } a Sora 1 Vey ‘ ibis * a i ‘ c ; ty ‘ Ma ' 4): y Mh “Wek ae o y he : ; ae 1 ¥ Ve. be . _* 7 i ( ie a aks | Z i ‘ i 7 x ; ah 42 ; a ¥ bs t on rs) wah OE A Se A 4 F , * 7 ta) | . © x k i? ¥ ‘ j Lots . aks : ) ie ioe. } ; 7 a fF ae = i y JOSEPH JAMES FLETCHER. Joseph James Fletcher was born in Auckland, New Zealand, in 1850. His father, the Rey. J. Horner Fletcher, was then headmaster of what afterwards, under his charge, developed into the ‘Auckland College’. He was both a scholar and a theologian. Later on, for reasons of health, he resigned the head- mastership and was appointed to the charge of a church at New Plymouth and, after the outbreak of the Maori War in 1860, was transferred by the Methodist Conference to Australia, first to Brisbane and then to Ipswich, where his son gained a scholarship in the Grammar School. He was then appointed Principal of Newington College Sydney, and there Fletcher passed most of his school days. From school J. J. Fletcher went to the University of Sydney, where he took his B.A. in 1870 and subsequently his M.A. degree in 1876. He does not seem to have distinguished himself especially in the class lists, nor had he the physique necessary for strenuous athletic work, but the following extract from The Sydney Morning Herald of January 25, 1868, shows not only that he was a fellow student of men who afterwards held prominent positions in the Commonwealth, but that he must have had qualities that attracted the attention of that fine scholar and experienced Professor, Dr. Badham. It reads as follows: “The Duke of Edinburgh in New South Wales—Dramatic performance at the University. Mr. Cooper’s (later Chief Justice of Queensland) impersonation of Phormio was very heartily appreciated and so, too, was the Geta of Mr. (later Sir Hdmund) Barton and the Nausistrata of Mr. Fletcher. This gentleman’s impersonation of the angry and jealous wife elicited much merriment. Altogether Phormio was a decided success”. Writing many years later Fletcher remembers how, “when the play was over and we had been recalled and got our bouquets and as the curtain went down finally, Dr. Badham came up out of.the prompter’s box and expressed his satisfaction at the way things went off and gave me a word of commendation, having to speak a foreign tongue in a big hall, in a falsetto voice’. He adds, “that made up to me for all the grind of rehearsals. I did not get home to Parramatta till after midnight, but I knew that my mother would sit up to hear whether I nad got a bouquet and an encore, or had disappointed Dr. Badham’’. This little episode occurred during his last year at the University. It is perhaps rather difficult to recognize in the ardent naturalist of later years the Nausistrata of ‘“Phormio”. After taking his degree he decided to devote himself to teaching, and accepted a position in Melbourne on the staff of Wesley College, the Headmaster of which was then Professor M. H. Irving, who had resigned the chair cf Classics in the University to devote himself to school work. We know little of his work in Melbourne except that, during the time he spent there, he came once more under the influence of the distinguished head of a Public School. It was, however, during this transitional period that he became interested in Natural Science, and, in 1876, he resigned from Wesley College and left for London. This was the time when Huxley was perhaps at his zenith—the year of his famous American addresses. At South Kensington in Huxley’s lecture room and laboratory it was possible for a student to listen to the leading exponent and protagonist of the evolution theory, and at the same time gain by practical experience a first c Xexexive J. J. FLETCHER. hand knowledge of plant and animal morphology. The latter is now a matter of everyday experience in modern universities, but at that time anything like true biological training was in its infancy. In the South Kensington laboratories Fletcher met and worked with G. B. Howes, who later on succeeded to the Professorship, and Jeffrey Parker, who migrated to New Zealand as Professor of Biology in the Otago University. In those days, when the field of scientific knowledge was comparatively limited, a Chair of Biology included teaching in both Zoology and Botany, mainly from the morphological side. Whilst in England he ~ studied hard and systematically. There was then no such thing as recognition of work done in Australian universities and, in order to gain the B.Sc. of the London University, he had to start again, complete the full three years of work and pass all the examinations necessary for admission to the degree. To start again, however, is perhaps not strictly true because in Sydney, under Dr. Badaam, his training, fortunately for himself, had been mainly on the literary and classical side—a training that stood him in good stead in later years. He not only worked in London but came into contact with F. Maitland Balfour, who, at Cambridge, was laying the foundation in England of the science of Embryology. Struck with his keenness and capacity Balfour invited him to visit the University as his guest and there he spent three months amongst a band of students including Milnes Marshall, Haddon, Lister, Adam Sedgwick, McBride, and others who in after years occupied Chairs of Zoology and Biology in many British universities both at home and in the Dominions. It was perhaps the most inspiring and fruitful time in the history of Biological Science. Darwin, Huxley, Hooker and Wallace were all at work, the “Challenger”, laden with wonderful material, had returned after its three years’ cruise of investigation in southern and tropic seas and in study, field and laboratory scores of eager students, relieved from the dead weight of the special creation theory, were working under the stimulus of an entirely new outlook on the world of life. It is difficult for students of the present day to realize the excitement of those times when everything was new and stimu- lating and when, further still, it was possible for one man to have a good all round knowledge of, at all events, the salient features of different branches of Science, small departments of which now occupy fully the time of many investigators. Imbued with the idea that to an Australian the study of problems concerned with the Australian fauna and flora was a duty of paramount importance, he set to work and, before leaving England in 1881, published in conjunction with J. J. Lister who was then a demonstrator in comparative anatomy in the Cambridge University, his first paper entitled “On the conditions of the median portion of the vaginal apparatus in the Macropodidae’. The authors based their results upon the scanty material then available in Cambridge and at the Zoological Gardens, London, some of which had already been investigated by workers, such as Owen and Everard Home, with indecisive results. In those days it was almost impossible to devote one’s life to scientific work unless endowed with private means, which Fletcher was not. Lack of pence, the attractions of his home country, the hope to be able to do something towards the elucidation of its fauna and flora whilst earning enough by other work to make this possible, drew him back to Australia, where he spent the rest of his life. Before leaving England, being fully aware of the imperfections of the Australian libraries in regard to scientific literature, he set to work and compiled a “Catalogue of Papers and Works relating to the Mammalian orders, Marsupialia, J. J. FLETCHER. XXXV. and Monotremata”’. The value of this, in those early days, especially to investi- gators in Australia, was much enhanced by his inciusion of references to all the new species described since the earlier works of Gould and Waterhouse. This was published in Sydney in 1881. Immediately on arrival in Australia, personally and with the aid of friends up country whom he interested in the work, he collected much more material which served as the basis for further investigations into the structure of the reproductive organs of Marsupials, and for the publication of three additional papers in 1881 and 1888. His first three memoirs embody the results of pioneer investigations into a matter of peculiar interest in regard to the anatomy of Marsupials and are of permanent value. It is much to be regretted that in those days there was no opening in Australia for a young unendowed zoologist. No post was available, either for teaching or for carrying on systematic research under modern laboratory conditions. Fletcher was obliged to return to school work and thus Australia lost the services of one who would have been a brilliant anatomist and an inspiring university teacher had the opportunity presented itself. He rejoined the staff of Newington College; was acting Headmaster for a short time and then became one of the senior teachers. “As a teacher’’ says one of his old pupils, Professor Scott Fletcher, now Professor of Philosophy in the Queensland University, he “showed great originality and achieved quite remark- able success. He had his own ideas on the subject of education, and evidently believed that a boy at school should be guided in the development of his moral character as well as taught to acquire knowledge. . . The roars of laughter that at times rang out from Fletcher’s class-room were not only the envy of adjoining “forms” but were ample evidence that the well known austerity of his rule was not unrelieved by a genuinely human touch that stirred both laughter and loyalty . . . his method of imparting knowledge was no less original and effective’. This, be it remembered, was forty years ago, before the days of Diplomas in Education, and of attempts to teach teachers how to teach. “He made it a rule’, says his old student ‘‘never to tell his pupils anything which they could find out for themselves. The spirit of research which he himself had learnt from Huxley he passed on to his successive classes. No matter what the subject was, he set his scholars to work gathering the raw material of fact which his own master-hand was later to round off into systematic knowledge. There is perhaps one word only in which may be summed up both his discipline and his instruction —sinecerity. He hated all humbug and shams, but he loved all that is true or beautiful or good in nature, in literature and in human character”. From 1881-1885 Fletcher worked at Newington College, but during these four years two things happened that determined the future course of his life. First, he joined the Linnean Society of New South Wales, and there came into contact with Sir William Macleay, its founder and benefactor, and secondly he married, and in his wife found a companion who, with quiet, ceaseless and unselfish sympathy, devoted herself to him and to his life’s work. Those of us who have had the privilege of their private friendship, understand what this meant to him and to us. These were the early days of the Linnean Society. Macleay was evidently impressed with the enthusiasm and capacity, and probably also, the ideals of Fletcher in regard to Natural History work in Australia, and in 1885 offered him the position of Director and Librarian of the Society. In reply to Fletcher’s acceptance of the position, Sir William wrote to him a short but characteristic XXXVi. J. J. FLETCHER. note dated April 14, 1885. It runs as follows: ‘‘My dear Sir, I was much pleased by your letter of yesterday, accepting my offer re ‘Linn. Soc.’. I shall now arrange | that the first charge on the £10,000 I leave as an endowment to the Linnean, shall be the salary of the Director, at present I presume my promise will be sufficient security. I hope that the New Year will see our house completed. At all events I should wish your duties to commence then. Yours, William Macleay”. On January 1, 1886, Fletcher entered upon his duties, and henceforth devoted his life to the work of the Society, to the furtherance of the study of Natural History in Australia, and to the carrying out of what he conceived to be the aim and objects of Sir William, and later also of Lady Macleay, with both of whom he always remained on terms of the most friendly mutual trust and confidence, which found expression in their selection of him as executor under both their wilis. From 1886 to 1893 he acted as Director and Librarian; in 1893 the title of his post was changed to that of Secretary in which capacity he acted until his retire- ment in 1919. He was an ideal Secretary and, if the Society owes the possibility of the present extent of its usefulness to the munificence and public spirit of Macleay it owes almost an equal debt to the loyal and tireless zeal of Fletcher. No task, however great or however small, that he thought touched upon the honour of the Macleays or the welfare of the Society was left undone, no matter what it cost him in time and thought. His width of scientific knowledge, his literary ability, his wonderful acquaintance with work published in regarec to Australian Natural History, and the early settlement of the Continent, together with his long practical experience in the field, both as regards Zoology and Botany, were of inestimable value to the Society and its members during the thirty three years in which he held office and, it is not too much to say, largely guided its destinies. During his term of office he edited thirty-three volumes of proceedings with meticulous care. Every word of every manuscript was carefully read through and even references were verified before it went to the press, often indeed, in the case of younger workers, before it was submitted to the Society, and many of them gladly recognize that they owe him much for hints and suggestions derived from his wide knowledge and experience. Realizing, so far as he himself was concerned, the urgent need of studying the land and fresh-water fauna before it passed away or became profoundly modified by the opening up of the country and the introduction of alien forms, he decided to work upon such material as he could study during leisure hours without the necessity of recourse to a fully equipped laboratory. He started upon the earthworms, a lowly group about which, in Australia, absolutely nothing was known, though, in Europe, Darwin, in what is now regarded as a classic work, had demonstrated their great practical value to the agriculturalist. From 1886-1894 he published six papers in which he showed the unexpected richness of Australia in this group. He described some seventy new species belonging to nine genera, five of which, as determined by him, were new and confined to Australia. His work was not simply systematic, but included careful field observations in regard to habits and distribution, and the results of anatomical investigation. “On one occasion, when trying to estimate the number of worms in a given area”, he says, “when the length of the furrows was 80 yards, I walked behind the plough and counted all the worms I could see, either in the furrows or sticking out of the overturned clods, and I found that for a number of furrows the average number J. J. FLETCHER. XXXVii. of worms under these circumstances was about 50 per furrow . . . these would give nearly 10,000 worms to the acre’. At the same time he was working, together with Mr. A. G. Hamilton, on the specific identity and distribution of Peripatus, and was investigating the Land Planarians, studying them in their living conditions. Of the latter only four species had previously been described, one by Darwin and three by Moseley. Hight new species of Geoplana were added and six of Rhynchodemus, a genus not before known from Australia. He then turned his attention to Amphibia, more especially those to be found near Sydney and in the County of Cumberland, where he was able to watch them in their native state. His first paper dealt with their oviposition and habits; the dates and places of spawning; the form of the spawn and the dependence of this, in regard to its developing, upon the nature of the season. He drew attention to the fact that certain species had developed the faculty, some in the adult and others in the larval state, of accommodating themselves to the varying climatic conditions of the dry parts of Australia. To those of us who knew him and his methods of patient inquiry, the following sentences, quoted from one of his papers, explain much. He says: “My most instructive round in one of the suburbs of Sydney included a visit to an old quarry, a brickyard, a deserted tanyard and three waterholes in paddocks used for watering cattie; these five spots were frequented during some period of the year by at least eleven species of frogs’. “That our frogs’, he says, “aestivate during hot and very dry periods there can be no doubt. During such times one hears no croaking and sees very little or nothing of the frogs, while logs and stones no longer afford sufficient moist shelter. In March, 1885, a very dry month, after just sufficient rain to moisten the ground, hearing croakings emanating from what, under more favourable conditions, is the bed of a pond, I turned up the soil with a stick and soon unearthed half a dozen specimens of Pseudophryne bibronii which were in this manner trying to survive the drought. . . . P. australis is a lively perky little frog, very partial to damp shelves and cracks in the Hawkesbury Sandstone and breeds earlier. . . . P. bibronii on the other hand is much less active, usually makes little or no effort to escape when uncovered in its hiding place, ‘shams dead’ when placed on its back and falls to the bottom like a stone when thrown into water; I have never found it except on the ground, under stones, logs, etc.; I have found the ova every year for seven successive years, once in April only, thrice in May only, once in June only and twice in both April and June”. These records and many others made by Fletcher are reminiscent of the simple observations of a naturalist that, when recorded by White of Selbourne, made him famous. Fletcher learnt to distinguish all the commoner frogs around Sydney by their call. Sitting in the evening on his verandah at Hunter’s Hill, enjoying with him the beauty of the fairy like scene of the Parramatta River, framed with the delicate tracery of the trees in his garden, watching the ferry boats gliding to and fro with long reflected lights of white and red and green, he would listen for them, and when, from a pond close by, the shrill piping of the little Hyla ewingi was heard, supported later by the slow-timed, dignified croak of its larger relative Hyla cerulaea and the calls of two or three other species, he would tell us which note belonged to each. At these times, while we could hear them croaking in the water, he very much enjoyed repeating, by way of warning, a sentence penned and published in an unlucky moment by a well known Professor of Natural Science who had never worked in the field, “In Australia the Hylas inhabit the tops of the lofty gum trees”. XXXViii. J. J. FLETCHER. He devoted in all seven papers to a careful investigation into the distribution and habits of Australian frogs, and to the descriptions of new genera and species, aided in this and other work by friends such as Messrs. Sidney Olliff, C. T. Musson, W. W. Froggatt, A. M. Lea, A. G. Hamilton, T. G. Sloane and others who recognized in him an ardent naturalist and were themselves as eager as he was to elucidate the Australian fauna. His papers on the Batrachia are not only models of accurate records of distribution but contain valuable original observa- tions, such for example as those on the warning colouration of Notaden bennettii, the Catholic frog. The following, written privately but not published, shows his broad outlook on problems concerned with the origin of the Australian fauna: ‘I feei satisfied that the Tasmanian frog fauna is the most primitive assemblage of genera and species (i.e. of frogs) we know of and that not only the genera but also the species (with perhaps one or two exceptions) were differentiated in Antarctica. Both in the case of Marsupials (extinct especially) and frogs and other things, I cannot help thinking that there was much more differentiation in Antarctica than we have been disposed to allow. Australia was a residuary legatee but the legacy was of course subsequently increased by endemic differentiation. The chief obstacle in the way seems to be the absence of intermediate forms of so many groups. If the creatures were developed in the centre or on the Hast Coast (of Australia) from forms which passed through Tasmania and Victoria, where are they now? Or is it that we cannot recognize them when we see them?” In January, 1900, he presided over the Biology Section at the Melbourne meeting of the Australasian Association for the Advancement of Science, and chose for the subject of his address “‘The Rise and early Progress of our knowledge of the Australian Fauna”. He devoted to its preparation all his spare time during the preceding eighteen months. “I can promise you’, he writes, “that there is one President with his coat and weskit off and his pantaloons tied round with string just below his knees—mentally perspiring—I hope to some purpose, if there were not about 1,500 books that I want to see and don’t know how to find”. The result was the compilation of a record of great value to all students interested in the historic aspect of Natural History in Australia. “I have often’’, he says, ~ “wondered why no one seems to have attempted an historical sketch of the Fauna such as I contemplated. Idiot that I was and am, I attempted to step into the breach. Already I am wiser and sad and no longer wonder . . . the history of the collections is most lamentably and grievously and sorrowfully depressing. The collectors (in Australia) were full of enthusiasm, but the British zoologists did not come up to the scratch. One is reminded of poor old W. B. Clarke taking home his fossils—hawking them round the United Kingdom, going down on his knees, begging and praying the British Palaeontologists to describe them—getting nothing but kicks and cold shoulders. Determined to get them worked up, he at last carts them off to Belgium, to De Koninck, who helps him out of the difficulty”’. In 1893 he edited the Macleay Memorial Volume, containing thirteen papers on zoological, botanical and ethnological subjects, written by Australasian workers, and himself contributed the biographical sketch. Writing in September of that year he says: “We have got to the end of the lane at last, and the volume will be published next week. I cannot say that I am proud of the sketch or that it does justice to the theme. It cost an awful lot of trouble but the absence of journals, letters and documents of that sort and the non-survival of hardly a contemporary J. J. FLETCHER. XXXix. with anything but shadowy recollections left me with but a small basis to work on”’. Times were then very straightened, financially, for the Linnean, as for all other scientific societies in Australia, and he writes: “‘The situation at present may be summed up in very few words—we hope soon to sell more copies and in the meantime we have got an overdraft’. The latter caused him much anxiety. His whole life was centred in the Society: indeed he was quixotic in a way that some- times made it difficult for his colleagues on the Council to help him as they were only too anxious and ready to do. The following years were filled with routine work, and the endeavour to deal with and solve, in a way satisfactory to the Society and in accordance with the intentions of Sir William Macleay, serious legal and financial difficulties that arose in connection with the foundation of the Research Fellowships and the appoint- ment of a Bacteriologist. During all this time, however, he was working when- ever opportunity offered, in close contact with friends and colleagues in the Society—J. H. Maiden, A. H. S. Lucas, R. H. Cambage, H. J. Carter, C. T. Musson, Henry Deane and others—each of whom was interested in some special branch put recognized in Fletcher a naturalist of broad outlook and wide sympathies. As time passed by he found it increasingly difficult, as a private worker with no laboratory or assistance, to indulge in the rather expensive hobby of collecting and maintaining a “spirit” collection that required constant supervision, and therefore he devoted his energies more and more to botanical work, and to the study of certain characteristic features of the Australian flora. Mr. C. T. Musson, his friend and companion on many expeditions, in collaboration with whom he worked for many years, says: “of late his time was chiefly devoted to Botanical matters. He was especially keen about native things, the sandstone plants coming first. He was always emphasizing the fact that this was a dry country and that the plants had to be prepared, even down to the water’s edge for droughty conditions. The amount of detail he got together when studying a subject was remarkable. To give an example, when working at a Grevillea, he covered 50 or 60 quarto sheets with detail, hundreds of figures merely dealing with lobing of the leaves. . . . His knowledge of the literature of our Fauna and Flora was profound and his memory extraordinary”. During his work on Australian Acacia phyllodes, the results of which were published in his Presidential Address in 1920, he brought together, as every naturalist visitor to his house knew well, a vast amount of material in specimens and notes. These led him eventually to the conclusion that “The so-called phyllodes of the Australian phyllodineous Acacias are not simply flattened petioles which have lost their blades . . . on the contrary they are the flattened primary leaf axes or common petioles of bipinnate leaves which have lost ‘their pinnae. . . . I propose to call them Euphyllodia or Euphyllodes in the sense that they are something more than is implied in the accepted definition of phyllodes”’. Another important piece of work was carried out in conjunction with Mr. Musson on shoot-bearing tumours of HEucalypts and Angophoras, published in 1918. Mr. Musson writes: “About eighteen years ago during a walk at the Hawkesbury Agricultural College, we met with an extensive crop of seedlings of Hucalyptus sideroxylon. On digging some up Fletcher remarked, on observing the remarkable woody growths at the base of the stem, ‘A mallee in miniature’. In their joint memoir the tumour was shown to originate in the axil of the cotyledons, or in a few pairs of leaf axils immediately above them, from proliferating cambium al J. J. FLETCHER. material. The late Mr. J. H. Maiden first suggested a bacterial origin and in this conclusion the authors concurred, the tumours, according to them, being due to infection by some parasitic soil organism. In some species, spoken of as ‘refractory’, the growth slows down, a mild attack runs its course without injury to growth. In the mallee gum the concrescence of the nodular growths is complete; they enclose the tap and other roots and intercept water that they -contain at the expense of the seedling stem; the so-called ‘mallee root’ is not a root, but, in its extreme form, a great tumour, from which apparently, though in reality only enclosed by it, stems and roots arise’. A very characteristic sentence in one of his letters shows the way in which he thought about such problems: ‘‘When the mallee scrubs have been cleared away what are the soil organisms going to do? Are they going to send in their resignations and die out, or are they going to adapt themselves to attacking the introduced plants that have supplanted them?” After referring to Fletcher’s work on Grevillea hybrids, for which he had fortunately prepared notes sufficient to allow of its completion by Mr. Musson, the latter says: “He took his last walk with me a fortnight before passing away. We sat in the park near the beautiful Gordon Gully, and discussed various matters, chiefly dealing with Nature he loved so well”. The secretarial work of the Society, made even unnecessarily arduous by his personal supervision of the minutest detail, began to tell upon him. Writing at the close of 1918 he says: “I have not had a holiday since Easter, 1915, and my eyes and brain are very tired, and I am retiring from the Linnean on 31st March, 1919, and have enough proof and indexing to keep me busy, so I enjoyed a week’s loaf visiting my Grevillea hybrids. . . . I began to realize that thirty-three years was going to be about as much as was good for me. So I decided to give notice of my retirement. . . . I am normal again and looking forward to finishing up properly, to leaving my work up to date and then having a holiday”. He then refers appreciatively to the generous treatment accorded to him by the Council; he himself, with characteristic modesty, had asked for a year’s retiring allowance. At the general meeting in March, 1919, the President, Professor H. G. Chapman, expressed the deep appreciation of the Society of the distinguished services that he had rendered to it. ‘‘No Society’, he said, “has received better service than that given by our Secretary. The welfare of our Society has been the sole care of his industry”. Dr. T. Storie Dixson, an old friend and past President who had known Sir William Macleay in the early days, referred to the Secretary’s loss as in many ways irreparable, especially by reason of the complete understanding that existed between him and the founder in all matters concerning its policy. Mr. A. H. S. Lucas, another past President, old friend and companion in the field, handed over to the President a portrait to be hung in the Hall; Mr. C. Hedley on behalf of the members presented a desk and chair to him, whilst others bore testimony to the services rendered not only to the Society but to themselves personally in connection with their work. To one of Fletcher’s retiring disposition it was a rather trying ordeal but he felt deeply the genuine expressions of appreciation and gratitude. He writes: “My comrades gave me a very cordial and handsome send-off . . . half a dozen speeches and a resolution passed. The warmth and enthusiasm of the proceedings fairly astonished me as I had no knowledge beforehand of this part of the ceremony (referring to the desk J. J. FLETCHER. xli. and chair) and they pretty nearly knocked me off my perch, but I managed to hang on and say what it was needful for me to say without being overcome’’. He was elected President for the years 1920 and 1921. In his first address he dealt with the two main forms of climatic conditions with which men on the land are concerned. He pointed out that the man in the northern hemisphere has learnt his lesson and can live in harmony with his environment. The winter conditions when he must house and feed his stock are so regular that he can arrange his programme by the almanac. The man in Australia has yet to learn how to adapt himself to Nature’s second method for giving the land its needed rest and sweetening by means of what he aptly called a periodic “drought sleep’. We have manuals of Faunas and Floras, of fodder grasses and minerals and so on, but how is it, he asked, that we have no manual of drought problems to teach man how, with the aid of knowledge gained from scientific investigation, to insure against damage by drought. In this address he included as a supplement the results of his research, spread over many years of field work, into the so-called Phyllodes of Acacias. At a special general meeting held in June, 1920, to commemorate the centenary of the birth of Sir William Macleay, he delivered an address on “The Society’s Heritage from the Macleays’. In regard to this he wrote: “I will show my Macleayan things that I am using as the basis for my address for William Macleay’s centenary on June 13th next. Some original drawings of Lewin, W.S.M.’s (William Sharp Macleay) original sketches, one of ‘an animal caught by Mr. Huxley in the tow net in Torres Straits’, portraits, letters, etc. Lady Macleay gave me these when she went to England about 25 years ago. I looked over them, saw they were interesting, iocked them up, wondering how I could use them. Now I know what they are and what they mean, and I am up to my neck in it. When I was proposed as President I did not want it. Then I thought of the centenary and how I could use the material for an address—‘The Society’s Heritage from the Macleays’.” The address, which occupied 68 pages of the Proceedings, contains a most valuable record of the lives and work of the three senior members of the family, Alexander, William Sharp, and Sir George Macleay; of the collections they brought together; of their scientific contemporaries; of their 97 years’ connection with the parent society in London; of their 51 years’ connection with the Australian Museum. It might more correctly be entitled: ‘Australia’s Heritage from the Macleays”’. It was only his inside knowledge of the family, gained as the result of the complete trust placed in him by Sir William and Lady Macleay, who gave him access to their private journals and papers, that made it possible for him to compile such a valuable historical record of early days not only of the Society but in tke Colony. The most pleasing feature to him was the presence of Admiral Dumaresq, of H.M.A.S. “Melbourne”, then in Sydney, a grandson on his mother’s side of Alexander Macleay. The Admiral was deeply interested in the relics shown, and at his invitation Fletcher spent some interesting hours with him on his Flagship, showing him letters and papers and discussing the early days of the Macleays, within sight of the ancestral home garden at Elizabeth Bay. In his Presidential Address for 1921 he referred to a subject in regard to which he felt very keenly, that a grave injustice was being done to the memory and generosity of the Macleays, and to the public interested in Natural History. Under the heading of “Is all well with the Macleay Museum at the University?’ he certainly showed that it was far from well and that the University was not either in letter or in spirit carrying out its share of the bargain. It was the only time D xlii. J. J. FLETCHER. Fletcher entered into a newspaper controversy, but he felt that “one of Sir William’s great enterprises, potentially so fructifying, if properly managed has become bankrupt”, and he was quite right. When it was over he wrote, “very busy and very tired and in need of a holiday. At all events what I have done I have done from a sense of duty”. During his thirty years at Elizabeth Bay he had accumulated a very valuable collection consisting especially of marsupial material, amphibia, earthworms, and Peripatus. It included all the material upon which his zoological work was based. In 1923 he spent months in overhauling, rearranging and labelling it and finally presented everything to the Australian Museum. It pained him not to be able to present it to the Macleay Museum, but he was not prepared to place it, as he wrote rather scathingly, “in a room, placed under an iron roof, no blinds to the windows, the curator not a zoologist”. After retirement from active work at Elizabeth Bay he spent his spare time in carrying on botanical work on Acacias, Grevilleas, and Loranthaceae, often again in company with Linnean friends of long standing—Messrs. J. H. Maiden, R. H. Cambage, G. H. Halligan and C. T. Musson. Especially was he fond of exploring botanically the Hawkesbury sandstone and rarely missed a weekly tramp along the upper reaches of Lane Cove, the beauty of which, as seen in later years, from his own verandah, was a never failing source of pleasure by day and night. He writes in 1922, when he was a free man, “Of late the sunsets, sunrises, golden smokes, golden mists and reflections have been particularly beautiful. It is true that more and more houses are going up, and more and more bush is going, but I return thanks daily that though A may own this bit of ground and house, and B that bit, yet none of them, nor all of them own the Lane Cove, or the reflections, or the landscape”. He naturally felt the removal of the Linnean offices to the new premises in College Street, and whilst it was in progress wrote: ‘‘Before the Society can vacate Elizabeth Bay and remove the Library, a new one will have to be built. Then, if possible, the Bay property will be offered for sale. You can imagine what a wrench all this is and promises to be to me. It will certainly be more convenient for members and for meetings and is perhaps to be regarded as inevitable, but it is a little sad for the small remnant of the old brigade to cut ourselves adrift from the memories and traditions of the bit of the old historic garden and our associations with Sir William, and the old surroundings”. As the result of an accident four years ago he was forced to abstain from anything like strenuous exertion, though still retaining his association with the Society, and keen interest in his own work and that of his friends, who looked forward to his being able to enjoy some years of well earned rest in surroundings that appealed to him, both because of their scientific interest and of their beauty. But it was not to be, and on Saturday, May 15, 1926, without any warning, he passed away suddenly. It may be truly said that he lived for the Society and the carrying on of the Macleay tradition and, as the resolution of the Council records, “happily lived to see its present high position with an already honoured tradition behind it and an ever increasing activity in scientific research of the highest standard well established and portending a prominent future, with which his name will ever be inseparably associated’’. W.B.S. ABSTRACT OF PROCEEDINGS. SPECIAL GENERAL MEETING. 30th Marcu, 1927. Mr. A. G. Hamilton, Vice-President, in the Chair. Pursuant to notice the Honorary Treasurer moved the following addition to Rule vi: The Honorary Treasurer is authorized to accept from any ordinary member, who is not in arrear, the sum of Fifteen Guineas in lieu of further annual subscriptions. The motion was seconded by Professor Harrison and carried unanimously. ORDINARY MONTHLY MEETING. 30th Marcu, 1927. Professor L. Harrison, B.A., B.Sc., President, in the Chair. The Donations and Exchanges received since the previous Monthly Meeting (24th November, 1926) amounting to 61 Vols., 603 Parts or Nos., 24 Bulletins, 12 Reports and 14 Pamphlets, received from 160 Societies and Institutions and 7 private donors were laid upon the table. PAPERS READ. 1. Notes on Australian Diptera. No. x. By J. R. Malloch. (Communicated by Dr. E. W. Ferguson.) 2. The Anatomy of Cheilanthes vellea. By May M. Williams, M.Sc., Linnean Macleay Fellow of the Society in Botany. 3. A New Deltopecten from the Illawarra District, N.S.W. By John Mitchell. 4. The Fossil Estheriae of Australia. Part i. By John Mitchell. 5. The Geology of the Country between Lamb’s Valley and the Paterson River. By G. D. Osborne, B.Sc. 6. Note on a Dicotyledonous Fossil Wood from Ulladulla, N.S.W. By C. Barnard, B.Sc. 7. On a Case of Natural Hybridism in the Genus Grevillea (Proteaceae). By C. T. Musson and the late J. J. Fletcher, M.A., B.Sc. NOTES AND EXHIBITS. Miss H. Claire Weekes, B.Sc., Linnean Macleay Fellow of the Society in Zoology, contributed a preliminary note on placentation in some lizards. Definite placentation amongst lizards has been described in Chalcides tridactylus and C. ocellatus by Giacomini (1891) and (1906) respectively; in Tiliqua scincoides by Flynn (1923); and in Lygosoma (Liolepisma) entrecasteauxzi by Harrison and Weekes (1925). The occurrence of omphaloplacentation and allantoplacentation in the Scincid lizards Lygosoma (Hinulia) quoyi, Egernia whitei and E. striolata and of B xliv. ABSTRACT OF PROCEEDINGS. omphaloplacentation in TJ. scincoides is here recorded for the first time. In Hinulia quoyi the allantoplacentation is highly specialized. In the classic C. tridactylus, T. scincoides and L. entrecasteauxi the foetus obtains its food from the parent by means of the glandular activity of the modified uterine epithelium and the absorbing and phagocytic powers of the enlarged chorionic ectoderm cells. In other words it is the epithelial tissues which play the important part in food transition. In H. quoyi the epithelial tissues partly degenerate and there is a concentration of maternal and foetal capillaries in close apposition. Hence it can be stated that the type of allantoplacentation found in H. quoyi more closely resembles that found in the Marsupialia than does any hitherto recorded in a Reptile. In H#. whitei and LE. striolata the allantoplacentation resembles that of H. quoyi but offers sufficient variation to be of interest. Detailed accounts of these phenomena are in course of preparation. SPECIAL GENERAL MEETING. 27th Apri, 1927. Professor L. Harrison, B.A., B.Sc., President, in the Chair. The minutes of the Special General Meeting of 30th March, 1927, were read and confirmed. The President pointed out that the addition of Rule vi as carried and confirmed at the Special General Meetings provides for Life Membership of the Society. ORDINARY MONTHLY MEETING. 27th Aprin, 1927. Professor L. Harrison, B.A., B.Sc., President, in the Chair. Mr. W. A. L. Bredero, Orange, Mr. T. G. Campbell, Manly, Mr. W. Dixson, Killara, Miss M. L. Garde, Neutral Bay, and Mr. K. C. Richardson, B.Sc., Sydney, were elected Ordinary Members of the Society. The President announced that. Messrs. A. F. Basset Hull, R. H. Cambage, C.B.E., F.L.S., H. J. Carter, B.A., F.E.S., and Dr. E. W. Ferguson had been elected Vice-Presidents; and Dr. G. A. Waterhouse, Hon. Treasurer for the Session 1927-28. The President drew attention to the Fourth International Congress of Entomology to be held at Ithaca, New York, in August, 1928. The Donations and Exchanges received since the previous Monthly Meeting (30th March, 1927) amounting to 7 Vols., 71 Parts or Nos., 7 Bulletins, 2 Reports and 3 Pamphlets, received from 52 Societies and Institutions and 3 private donors were laid upon the table. PAPERS READ. 1. Two New Species of Setaria from Western Australia. By A. S. Hitchcock. (Communicated by Mr. W. M. Carne.) 2. The Influence of certain Colloids upon Fermentation. Parts iv, v and vi. By R. Greig-Smith, D.Sc., Macleay Bacteriologist to the Society. 3. Notes on Australian Mosquitoes (Diptera, Culicidae). Part i. The Anophelini of the Mainland. By I. M. Mackerras, M.B., Ch.M., B.Sc., Linnean Macleay Fellow of the Society in Zoology. 4. The Physiographic and Climatic Factors controlling the Flooding of the Hawkesbury River at Windsor. By Lesley D. Hall, B.Sc. ABSTRACT OF PROCEEDINGS. xlv. NOTES AND EXHIBITS. Mr. C. T. Musson exhibited specimens of the common introduced snail Helix aspersa from Gordon, Sydney, and also for comparison specimens from England. He remarked that he could see little difference in their texture. Mr. John Mitchell exhibited a very small cylindro-conical stone from an aborigines’ camp and workshop on the seashore south of the Bellambi jetty. In general contour it resembles the stones of this character optained from the western parts of New South Wales, but differs from all of these in its small size (four inches long) and from most of them in being smooth and having a rounded base (Mem. Geol. Surv. N.S.W., Ethnol. Ser. No. 2). The stone in question, it is plain, has been made from a thin pebble of some igneous rock, ground into its present shape. It is sub-two-sided; one side is flat, the other convex; each end is rounded. He was not aware of any previous reference having been made to the discovery of a similar stone fashioned by the aborigines of the east coast of Australia. Mr. J. Mitchell also exhibited a fragment of fossil fish belonging to the genus Elonichthys, recently obtained by him from the insect beds near Belmont, N.S.W. Very few fossil fish have been found in the Newcastle Coal Measures. The first was Urosthenes australis Dana; the next was not found till 1912, when he secured a few specimens, and now the present specimen. The latter specimens belong to the genus Elonichthys, which seems to be the genus best represented in the Newcastle Coal Measures. ORDINARY MONTHLY MEETING. 25th May, 1927. Professor L. Harrison, B.A., B.Se., President, in the Chair. Mr. J. W. F. Armstrong, Bogan River, N.S.W., and Mr. C. G. Oke, St. Kilda, Victoria, were elected Ordinary Members of the Society. The President announced that a movement had been started to provide a suitable memorial to the late Professor A. A. Lawson, the first Professor of Botany in the University of Sydney. The President announced that the Society had that day vacated the Hall at Elizabeth Bay which it had occupied since 2nd January, 1886. The Library had been removed to the Macleay Museum, University of Sydney, where it would remain until it could be housed in its new home. The Donations and Exchanges received since the previous Monthly Meeting (27th April, 1927) amounting to 25 Vols., 370 Parts or Nos., 31 Bulletins, 7 Reports and 19 Pamphlets, received from 73 Societies and Institutions and 2 private donors were laid upon the table. PAPERS READ. 1. The Interpretation of the Radial Field of the Wing in the Nematocerous Diptera, with Special Reference to the Tipulidae. By C. P. Alexander. (Communicated by Dr. E. W. Ferguson.) 2. New Gall-forming Thysanoptera of Australia. By Dudley Moulton. (Communicated by Mr. W. W. Froggatt, F.L.S.) 38. Note on Reproductive Phenomena in some Lizards. By Miss H. Claire Weekes, B.Sc., Linnean Macleay Fellow of the Society in Zoology. xIvi. ABSTRACT OF PROCEEDINGS. 4. An Ecological Study of the Flora of Mt. Wilson. Part iv. Habitat ; Factors and Plant Response. By J. McLuckie, M.A., D.Sc., and A. H. K. Petrie, M.Sc. NOTES AND EXHIBITS. Mr. David G. Stead referred to an extraordinary occurrence of large sharks in the following note: Several species of large sharks are known to occur in Port Jackson. Some of these penetrate but a short distance from the sea and only one kind travels far up into the head waters. On the 24th instant a launch party under the charge of Mr. Charles Messenger was fishing along the eastern channel of the harbour entrance when they met with a large school of sharks. Hight of these were captured and were seen by me to-day. They were all of the species Carcharinus brachyurus Gunther, the Whaler or Mullet Shark, and ranged in size from about 7 feet 6 inches to 10 feet. Apparently all of those present in this school were of the same species. This appears to be the first record of the occurrence of the Whaler in school formation. Both the Grey Nurse, Carcharias arenarius Ogilby (with which the present specimens were confused in the daily press accounts) and the well-known Blue Pointer are known to occur in very large schools on “outside” grounds, but the Whaler is usually more diffused— existing singly or in pairs ({ and 2). Mr. Messenger, who is a highly experienced shark catcher, is of the opinion that had several boats been present not iess than one hundred sharks might have been taken. The Whaler is the most dangerous of our man-eating sharks, penetrating our estuaries, even up into fresh water. It commonly attains to 10 feet in length and is of great girth. The occurrence of this large school of Whaler sharks is probably an aftermath of the schooling season for Sea Mullet, Mugil cephalus Linnaeus. Dr. C. Anderson communicated the following note:—At a meeting of this Society held on 27th June, 1888 (These ProceEepines, 1888, p. 894), Dr. J. C. Cox exhibited “a Tertiary fossil from Wildhorse Plains, which he believed to be identical with Thylacodes decussatus Gm., a living Port Jackson species”; this name is synonymous with Vermetus decussatus, a marine mollusc with a vermiform shell. By some unfortunate mistake this note led to the tentative recognition of a new genus of fossil marsupial, ? Thylacodes Cox, which is listed in Roger’s “Verzeichniss der bisher bekannten fossilen Saugetiere” (Ber. d. naturw. Vern. f. Schwaben u. Neuburg, Augsburg, 1896) in the family Phalangistidae, and in Trouessart’s “Catalogus mammalium tam viventium quam fossilium’’ (Vol. II, 1898-9, p. 1156) in the family Phalangeridae, sub-family Thylacoleontinae, along with Thylacoleo carnifex Owen, the so-called Marsupial Lion. In the Supplement to this latter work (1904-5, p. 846) this curious mistake is repeated but the sub-family is transferred to the family Dasyuridae. ORDINARY MONTHLY MEETING. 29th Jung, 1927. Mr. R. H. Cambage, C.B.E., F.L.S., Vice-President, in the Chair. The Chairman offered the congratulations of the Society to Dr. W. G. Woolnough on his appointment as Acting Federal Geologist. The Chairman announced with pleasure that the Government had recently issued a Proclamation protecting certain of the wild flowers. The Donations and Exchanges received since the previous Monthly Meeting (25th May, 1927) amounting to 21 Vols., 106 Parts or Nos., 7 Bulletins, 7 Reports ABSTRACT OF PROCEEDINGS. xlvii. and 2 Pamphlets, received from 69 Societies and Institutions and 2 private donors were laid upon the table. PAPERS READ. 1. The Gasteromycetes of Australasia. vii. The Genera Disciseda and Abstoma. By G. H. Cunningham. 2. The Gasteromycetes of Australasia. viii. The Genus Mycenastrum. By G. H. Cunningham. 3. Additional Flora of the Comboyne Plateau, 1926. By E. C. Chisholm, M.B., Ch.M. 4. Further Notes on a new Classification of Australian Robberflies (Diptera, Asilidae). By G. H. Hardy. 5. The Phylogeny of some Diptera Brachycera. By G. H. Hardy. NOTES AND EXHIBITS. Mr. A. J. Nicholson exhibited from the Macleay Museum Collection a bilateral gynandromorph of the butterfly, Papilio androgeus from S. America. Mr. A. Musgrave exhibited, from the Australian Museum Collection, a remark- able aberration of the female of Papilio aegeus from New South Wales. In the specimen the red spots on the hindwing were much enlarged and drawn out te about four times their usual size. Dr. G. A. Waterhouse exhibited the following butterflies: (1) Mosaic gynandromorphs of (a) Troides priamus pronomus from Cape York in which the female markings predominated, (bv) Papilio aegeus ormenus from Darnley Is. showing about equal proportions of male and female markings; (2) specimens of Papilio oberon from Santa Cruz Is. recently caught by Messrs. E. Le G. Troughton and A. A. Livingstone, and suggested that as they resembled Papilio aegeus from Eastern Australia so closely, they may have been introduced into the Santa Cruz Group. Dr. Waterhouse also exhibited fossils from Brookvale, near Manly, consisting of Estheria coghlani and a beetle. The latter, the first record of a beetle from the Quarry, was recently found by Mr. W. H. Hatcher. Mr. David G. Stead exhibited two extraordinary fishing lines: (1) A crocodile line as used by the Malays of the Malay Peninsula, Southern Siam, Sumatra and Borneo, for the capture of the short-snouted crocodile (Crocodilus porosus). The line itself is formed of a thin, strong rotan (Mal.) cane, to which the unusual hook is fastened—by the middle of the shank—by means of a multi-strand snood of ramie fibre. The strands of the snood are quite separate so as to prevent the crocodile from biting through the line, which becomes entangled in the teeth. After the crocodile swallows the baited hook, the tension of the line on the middle of the hook causes it to lie right athwart the gullet. (2) A baitless and barbless hooked fishing line, known as rawai (Mal.) used for the capture of sharks and rays and great eels by Chinese (Hokkien) fishermen. The line is set chiefly at the edge of tidal flats on muddy and sandy bottoms. Mr. E. Cheel exhibited specimens of Hremophila longifolia, infested with the aecidial stage of a rust-fungus (Uredineae) collected at Thackaringa, Broken Hill, by Mr. A. Morris. The cylindrical orange-red coloured pseudoperidia with white tips somewhat agree with those described as Roestelia polita by Berkeley which according to McAlpine (Rusts of Australia, p. 98) is an Uromyces. The only record so far as he could ascertain of a Myoporaceous plant being found infested with xviii. ABSTRACT OF PROCEEDINGS. a “rust-fungus” is that of Cunningham (Trans. N.Z. Inst., 1924, p. 35) on Myoporum laetum. Mr. A. F. Basset Hull exhibited 103 examples of 40 species, 23 genera of abnormal Loricates, showing specimens having 5, 6, 7 and 9 valves; others with damaged and repaired valves, or with one side repaired, and the aperture on the other side closed by enlargement of the adjoining vaive. The greater number of these had been obtained since his exhibit before the Society in May, 1925. Dr. I. M. Mackerras exhibited a series of Diptera Brachycera, showing South American affinities. Mr. R. H. Cambage recorded a series of flights of the flying squirrel Petauroides volans, which in six successive glides covered a distance of 590 yards. A resident at Milton, in the ’seventies, while near his house in the twilight, saw a squirrel leave the top of a Hucalyptus tree 100 feet high and glide to the foot of another 70 yards away. This it immediately climbed and from its summit glided to the next at 80 yards. It lost no time in ascending three more trees at distances of 110, 120 and 90 yards apart respectively, and from the top of the last it glided to another 120 yards away, which it climbed and in which it remained, this evidently having been its objective. While climbing the trees it uttered its peculiar squealing call notes as if to give a friendly warning of its approach to any of its kindred that might be in the tree. It is possible the squirrel landed on the ground a few yards short of some of the trees, but its total journey of a third of a mile shows that these nocturnal marsupials may wander a considerable distance from their homes to which they return by the morning. Archdeacon F. E. Haviland exhibited a device for use in centering ana mounting microscopic objects. It consists of a wooden slab recessed, into whicn fits a brass slab with a central hole and recessed for cover glasses. It is claimed that the object is held in its intended position on the slide and air bubbles are avoided. Mr. G. P. Whitley exhibited specimens of the Surf Fish, Iso rhothophilus, collected by Messrs. F. A. McNeill and A. A. Livingstone at Long Bay baths on 5th May, 1927. These fishes, which live in the outer breakers of the surf, occurred in thousands in the baths, where they had evidently been stranded after the Easter cyclone. Numerous isopod parasites were clinging to the fishes or swimming freely amongst them, whilst some copepods were netted with the fishes, and had evidently become detached from them. These crustaceans have been identified by Mr. H. M. Hale as: One young female Irona, five stages of juvenile Cymothoid isopods, and numerous Caligus sp. The collectors noticed some of the fishes in a school turning sideways and sinking to the bottom, where many were eaten by rock-pool fishes. Subsequent observations made at intervals by Mr. Whitley showed that the turning of apparently sickly fishes was not usually performed by those carrying parasites, and that taken as a whole the fishes fell on their left or right sides, but single specimens turned to right or left consistently. The reason for this action is still unknown. The fishes were plentiful until the end of May, but on 5th June, practically all had disappeared. The majority probably returned to the ocean in the waves which had broken over the baths during the stormy weather meanwhile. X-ray photographs of three specimens, made by Surgeon Lieut.-Commander W.E. J. Paradice, R.A.N., were also shown. The vertebrae numbered 13 + 29 to 30 ABSTRACT OF PROCEEDINGS. xlix. (excluding hypural). Iso flos-maris, known in Japan as the “Flower of the Wave,” has 18+ 25 (Jordan and Starks). Dr. McLuckie exhibited specimens of Chert obtained from the Rhynie Chert bed, Scotland, discovered in 1913 by Dr. Mackie, containing the petrified remains of very simple early Devonian plants. Fragments of the plant remains, sections and photographs of sections were also exhibited. The fragments had been separated from the main Chert mass by heating and suddenly cooling in cold water. He gave a brief account of the plant remains petrified in this Chert, discussing the extremely simple vascular structure and organization of Rhynia and Hornea which were leafless and rootless. Absorption from the soil was carried on by the rhizoids which develop from the creeping rhizome. The aerial branches forked, bore stomata (and probably chlorophylliferous tissue) and terminal sporangia, and had a very simple organized central vascular cylinder, consisting of spiral or annular tracheids. In Rhynia and Hornea we have the most simply organized vascular plants known. The sporangial structure of Hornea with its central sterile tissue and characteristic dome-shaped spore-bearing zone suggests a moss-like character (¢.g. Sphagnum) and a certain analogy is apparent between the Mosses and these simple vascular plants, which show a combination of characters which have been stressed by different botanists to show their Pteridophytic, Thallophytic or Bryophytic affinity. The Rhyniaceae may be a synthetic group related to Pterido- phytes and Bryophytes and retaining some characters of their original Algal ancestry. The discovery of the Rhyniaceae and the excellent elucidation of their structure by Lang and Kidston during recent years has given us a knowledge of the remarkably simple and probably the most primitive of vascular plants. ‘They throw a certain amount of light upon the probable origin of the sporophytic generation of land plants. ORDINARY MONTHLY MEETING. 27th JuLy, 1927. Mr. H. J. Carter, B.A., F.E.S., Vice-President, in the Chair. The Chairman referred to the great loss the Society had sustained by the death of Dr. EH. W. Ferguson on 18th July and read the following resolution passed by the Council and sent to Mrs. Ferguson on behalf of the Society: “The Society places on record its very deep regret at the death of Dr. E. W. Ferguson. It realizes the debt it owes to the late Dr. Ferguson, who had been a member of the Society since 1908, a member of the Council since 1921, its President during 1926. His death is a loss to the members of the Society and to the naturalists of Australia by whom he was held in the highest esteem and respect. The Society expresses to Mrs. Ferguson and her family their very sincere sympathy with them in their sad bereavement’. Mr. M. F. Albert, Elizabeth Bay; Miss M. V. McHugh, Potts Point; Rev. H. M. R. Rupp, Paterson, N.S.W.; and Mr. W. L. Waterhouse, M.C., B.Sc.Agr., Roseville were elected Ordinary Members of the Society. The Chairman offered the congratulations of the Society to Mr. A. H. K. Petrie, M.Sc., on his appointment to an 1851 Exhibition Travelling Scholarship. The Donations and Exchanges received since the previous Monthly Meeting (29th June, 1927) amounting to 3 Vols., 105 Parts or Nos., 3 Bulletins and 20 Reports, received from 53 Societies and Institutions and 2 private donors were laid upon the table. 1. ABSTRACT OF PROCEEDINGS. PAPERS READ. 1. Australian Coleoptera: Notes and New Species. No. v. By H. J. Carter, B.A., F.E.S. 2. The Gasteromycetes of Australasia. ix. Keys to the Genera and Species of the Lycoperdaceae. By G. H. Cunningham. 3. Notes on Australian Diptera. No. xi. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) 4. Descriptions of New Species of Australian Coleoptera. Part xix. By A. M. Lea, F.E.S. 5. The Vegetation of the Kosciusko Plateau. Part i. The Plant Communities. By J. MeLuckie, M.A., D.Sc., and A. H. K. Petrie, M.Sc. NOTES AND EXHIBITS. Dr. G. A. Waterhouse exhibited bred specimens of (1) Ogyris oroetes from the following new localities: Clermont, Queensland (EK. J. Dumigan), Brisbane, Queensland (L. Franzen), and Belltrees, near Scone, N.S.W. (G.A.W.); (2) the three subspecies of Ogyris amaryllis from all the States of Australia except Tasmania; (3) specimens of Ogyris aenone taken near Cairns by Mr. A. N. Burns. Mr. W. L. Wearne exhibited a piece of cedar timber in which a portion of a bed-post was embedded. The annual rings showed that this had been in position for about fifty years. Mr. A. F. Basset Hull drew attention to the recent issue of “A Monograph of the Australian Loricates’” and presented a copy to the Society on behalf of the Royal Zoological Society of New South Wales. ORDINARY MONTHLY MEETING. 3lst AuGUST, 1927. Mr. R. H. Cambage, C.B.E., F.L.S., Vice-President, in the Chair. The Chairman referred to the death on 6th August of Dr. R. Greig Smith, Macleay Bacteriologist to the Society and read the following resolution passed by the Council: “That the Council places on record its very deep regret at the death of Dr. R. Greig Smith, who was the first Macleay Bacteriologist to the Society, occupying that position for nearly thirty years. During the whole of his residence in New South Wales he had devoted himself assiduously to his research work and had assisted in many ways the advancement of science in Australia. His death is a loss to members of the Society and his presence will be missed from its meetings. The Society expresses to Mrs. Greig Smith its very sincere sympathy in her sad bereavement”. The Chairman also referred to the death of Mr. Thomas Whitelegge, at one time a member of the Society and for several years a member of Council. Mr. W. D. Francis, Brisbane, Queensland, was elected an Ordinary Member of the Society. The Chairman announced that Mr. A. G. Hamilton had been elected a Vice- President and Mr. A. J. Nicholson, M.Sc., a member of Council. The Chairman announced that the Société de Physique et d’Histoire Naturelle de Genéve offers a prize for the best unpublished monograph on a genus or family of plants, the closing date being 31st March, 1930. The Donations and Exchanges received since the previous Monthly Meeting (27th July, 1927) amounting to 31 Vols., 191 Parts or Nos., 20 Bulletins, 3 Reports and 8 Pamphlets, received from 98 Societies and Institutions and 2 private donors were laid upon the table. ABSTRACT OF PROCEEDINGS. li. PAPERS READ. 1. Notes on Australian Diptera. No. xii. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) 2. Notes on Australian Mosquitoes (Diptera, Culicidae). Part ii. The Zoogeography of the Subgenus Ochlerotatus with Notes on the Species. By I. M. Mackerras, M.B., Ch.M., B.Sc., Linnean Macleay Fellow of the Society in Zoology. 3. The Xerophytic Structure of the Leaf in the Australian Proteaceae. Part i. By A. G. Hamilton. 4. Australian Hesperiidae. Part i. Notes and Descriptions of New Forms. By G. A. Waterhouse, D.Sc., B.E., F.E.S. NOTES AND EXHIBITS. Dr. I. M. Mackerras exhibited a series of Australian Tachinidae in illustration of Mr. Malloch’s paper. Mr. A. G. Hamilton showed a number of lantern slides to illustrate the xerophytic structure of the leaf of the Australian Proteaceae. Dr. G. A. Waterhouse exhibited the new subspecies described in his paper and a number of coloured lantern slides of Australian Butterflies. Mr. David G. Stead exhibited a photograph showing bees collecting bitumen from the coating of wood pipes at Yarrangobilly (N.S.W.). Mr. Stead invited the attention of the Society to the great destruction of Koalas (Native Bears) which had taken place in Queensland as a result of the short open season of one month (August) declared by the Queensland Government. Already many thousands of skins had actually been exported and thousands more were in store in Sydney and Brisbane. On his motion it was resolved that the Commonwealth Government be requested to refuse all applications for permits to export such skins in the future in accordance with their proclamation of 5th December, 1923. Mr. G. P. Whitley exhibited a sample of marine growth from off Long Reef, New South Wales. This growth had been reported from Broken Bay, the ocean off Long Reef, and local estuarine waters, where it had occurred as a kind of scum at varying depths. It had proved annoying to fishermen by clinging to their lines, becoming concentrated into lumps as the lines were pulled out of the water. It has been suggested that the presence of this organism might have a deleterious effect on marine animals and that its occurrence in such large quantities might have been due to the lengthy dry weather period just experienced. It was suggested that the organism is a marine alga. Mr. A. H. S. Lucas exhibited specimens of the English primrose and cowslip and also what was probably a hybrid between them. He pointed out that the hybrid was found growing in a habitat between the two parent forms. ORDINARY MONTHLY MEETING. 28th SEPTEMBER, 1927. Mr. A. F. Basset Hull, Vice-President, in the Chair. The Chairman referred to the death of Mr. Daniel Frederick Cooksey on 16th September, 1927. He had been a member of the Society since 1926. The Chairman drew attention to the cable from England announcing the death of Professor A. Liversidge, who had been one of the original members of the Society and had served on its Council during 1875 and 1876. The Chairman announced that the Council is prepared to receive applications for four Linnean Macleay Fellowships tenable for one year from ist March, 1928, lii. ABSTRACT OF PROCEEDINGS. from qualified candidates. Applications should be lodged with the Acting Secretary, who will afford all necessary information to intending candidates, not later than Wednesday, 2nd November, 1927. The Donations and Hxchanges received since the previous Monthly Meeting (31st August, 1927) amounting to 9 Vols., 87 Parts or Nos., 2 Bulletins and 3 Pamphlets, received from 44 Societies and Institutions and 3 private donors were laid upon the table. PAPERS READ. 1. Studies in the Goodeniaceae. Part i. The Life History of Dampiera stricta R.Br. By P. Brough, M.A., B.Sc., B.Sc.Agr. 2. Notes on Australian Diptera. No. xiii. By J. R. Malloch. (Communicated by Dr. I. M. Mackerras.) 3. Notes on Australian Marine Algae. Part iv. The Australian Species of the Genus Spongoclonium. By A. H. 8. Lucas, M.A., B.Sc. NOTES AND EXHIBITS. Dr. I. M. Mackerras announced that the late Dr. E. W. Ferguson had bequeathed his fine collection of Amycterids (Coleoptera, Curculionidae) to the Macleay Museum, University of Sydney and that the collection had been transferred to the Museum. ORDINARY MONTHLY MERTING. 26th OctToBErR, 1927. Mr. H. J. Carter, B.A., F.H.S., Vice-President, in the Chair. Rev. E. Norman McKie, Guyra, N.S.W., was elected an Ordinary Member of the Society. Candidates for Linnean Macleay Fellowships, 1928-29, were reminded that Wednesday, 2nd November, 1927, is the last day for receiving applications. Mr. D. G. Stead mentioned the movement that had been proceeding for some time for the appointment of a Royal Commission of Inquiry by the Commonwealth Government, to make a close investigation into the general status of the aborigines throughout Australia. Upon his motion, seconded by Mr. I. V. Newman, it was resolved to write to the Prime Minister in support of the proposal. The Donations and Exchanges received since the previous Monthly Meeting (28th September, 1927) amounting to 12 Vols., 95 Parts or Nos., 13 Bulletins and 2 Reports, received from 56 Societies and Institutions and 1 private donor were laid upon the table. PAPERS READ. 1. Notes on Australian and Exotic Sarcophagid Flies. By G. H. Hardy. 2. Placentation and other phenomena in the Scincid Lizard, Lygosoma (Hinulia) quoyi. By H. Claire Weekes, B.Sc., Linnean Macleay Fellow of the Society in Zoology. NOTES AND EXHIBITS. Mr. D. G. Stead drew attention to the feeding habits of the large Black Shag, Phalacrocorar carbo, in the lower waters of Sydney Harbour. After many years’ observation it was concluded that normally this species lived almost exclusively upon bottom-frequenting fishes, especially the Frog Fish, Batrachus dubius, which ABSTRACT OF PROCEEDINGS. liii. was often obtained from a depth of about 26 feet. Catfish, Cnidoglanis megastoma, and Flathead, Platycephalus spp., were also captured. Mr. Stead also drew attention to the presence (in waters adjacent to Sydney Heads) of the Wafer Worm, Leptoplana australis, a species of dendrocoelous turbellarian worm which was destructive to oysters. Mr. EH. Cheel exhibited specimens of two species of plants of the Selagineae group of the family Scrophulariniaceae as follows:—(1) Hebenstreitia dentata Linn. This is quite common in the neighbourhood of Newcastle and has evidently been brought from South Africa in ballast. (2) Selago corymbosa Linn. Hawkesbury Agricultural College, C. T. Musson. Probably introduced from South Africa in agricultural seeds. It is interesting to note that Oenothera biennis (Evening Primrose) is also quite common at Newcastle associated with Oenothera odorata and Hebenstreitia. Mr. T. H. Pincombe exhibited Cleithrolepis granulatus found (July, 1927) in sewer tunnelling at the head of Tambourine Bay, Sydney, in a similar deposit to that at Brookvale. Dr. G. A. Waterhouse showed a lantern slide of the pupa of Liphyra brassolis and gave some notes on its life history. ORDINARY MONTHLY MEETING. 380th NoveEMBER, 1927. Professor L. Harrison, B.A., B.Se., President, in the Chair. The President extended a welcome to Dr. A. B. Walkom on his return from ' England. Mr. Bert BertRAM, Greenwich, Mr. F. A. Crart, Ashbury, Professor T. G. B. Ossorn, Adelaide, and Miss Doris A. SELBy, Gordon, were elected Ordinary Members of the Society. The President announced that the Council had reappointed Miss H. Claire Weekes and Miss Ida A. Brown to Linnean Macleay Fellowships in Zoology and Geology respectively for one year from 1st March, 1928. The President offered congratulations to Dr. R. J. Tillyard on his appointment as Chief of the Biological Research Station at Canberra; to Mr. C. A. Sussmilch on his appointment as Principal of the East Sydney Technical School and Assistant Superintendent of Technical Education; also to Mr. C. Barnard, B.Sc., on his appointment as Assistant Botanist to the Council of Scientific and Industrial Research. The President announced the receipt of a formal acknowledgment from the Secretary to the Prime Minister of the resolution carried at the last meeting. The Donations and Exchanges received since the previous Monthly Meeting (26th October, 1927) amounting to 216 Vols., 298 Parts or Nos., 14 Bulletins and 6 Reports, received from 75 Societies and Institutions and 1 private donor were laid upon the table. PAPERS READ. 1. Notes on Australian Marine Algae. No. vy. By A. H. S. Lucas, M.A., B.Sc. 2. Mosquito Control in the Municipality of Lane Cove, New South Wales. By B. Bertram. (Communicated by Dr. I. M. Mackerras.) 3. A new Dendrobium for New South Wales and Queensland. By Rev. H. M. R. Rupp. liv. ABSTRACT OF PROCEEDINGS. NOTES AND EXHIBITS. The President (Professor L. Harrison) exhibited examples of a new species of the primitive Annelid Stratiodrilus from the gill cavities of the Madagascar crayfish Astacoides madagascariensis. Through the courtesy and kindness of the Consul-General for France, M. Nettement, and the Governor-General of Madagascar, specimens of this crayfish were forwarded to Miss Lucy M. Wood, B.A., who desired to examine them for Temnocephaloid parasites, and who was successful in obtaining these. The genus Stratiodrilus was established by the late Professor W. A. Haswell, F.R.S., in 1900, for a species obtained from the Tasmanian crayfish Astacopsis tasmanicus. In 1913 he described a second species from the Australian crayfish Astacopsis serratus. In 1921 a third species was discovered in Uruguay by Dr. E. H. Cordero, which has not so far been described. The present species makes the fourth. The discovery is of considerable interest, as it sheds some light on the origin of the northern and southern crayfishes, a subject which has formed the basis for classical discussions at the hands of Huxley, Ortmann, Géoffrey Smith, Matthew and others. It is now established that both Temnocephala and Stratiodrilus occur in South America, Australia and Madagascar, chiefly as ectoparasites of crayfishes, while neither occurs in the northern hemisphere. Yemnocephala has no close relations, but the only known relative of Stratiodrilus, Histriobdella homari occurs upon the Norway lobster, Nephrops norvegicus. The suggestion is tentatively made that both northern and southern crayfishes have been derived from Nephrops-like marine ancestors, but that the transition from marine to freshwater conditions was. in the northern hemisphere, too sudden for Histriobdellid parasites to survive it; while in the southern hemisphere a more gradual transition has allowed survival. Temnocephala would appear to have developed entirely as a freshwater parasite, possibly derived from a Rhabdocoele ancestry. Mr. A. Musgrave exhibited a coloured drawing of an Argiopid spider, Poecilopachys bispinosa (Keyserling), made by Miss Joyce Allan of the Australian Museum, from a specimen collected by Mr. B. Bertram at Lane Cove, Sydney. During life the colour of the spider was observed to undergo changes similar to those in the octopus, the colour ebbing and flowing along the fore-border of the abdomen and the abdominal spines, and producing a definite flush. The abdominal spines, too, underwent a change, being quite smooth at times, while at other times they would be papillose. The spider is not uncommon in the vicinity of Sydney. It has been recorded from Gayndah, Queensland, and the Island of Upolu, Samoa. DONATIONS AND EXCHANGES. ly. DONATIONS AND EXCHANGES. Received during the period 25th November, 1926, to 30th November, 1927. (From the respective Societies, etc., unless otherwise mentioned.) ABERYSTWYTH. Welsh Plant Breeding Station, University College of Wales.—Advisory Bulletin No. 2 (1927); Bulletin, Series H, Nos. 5-7 (1927); “Self and Cross- fertilisation in Lolium perenne L.”, by T. J. Jenkin (From Journ. of Genetics, xvii, 1, Aug., 1926); “The Welsh Journal of Agriculture’, iii (1927). ACCRA. Geological Survey of the Gold Coast.—Report for the Period April, 1925-March, 1926 (no date). ADELAIDE. Department of Mines: Geological Survey of South Australia—Annual Report of the Director of Mines and Government Geologist for 1926 (1927); Mining Review for the Half-Years ended June 30th, 1926 (No. 44) (1926); December 31st, 1926 (No. 45); June 30th, 1927 (No. 46) (1927). Field Naturalists’ Section of the Royal Society of South Australia.—‘The South Australian Naturalist’, vii, 4 (1926); viii, 2-4 (1927). : Public Library, Museum and Art Gallery of South Australia.—Forty-third Annual Report of the Board of Governors for 1926-1927 (1927); “List of Books on Ornithology in the Public Library of South Australia and other Adelaide Libraries” (1926); Records of the South Australian Museum, iii, 38, (1927). Royal Geographical Society of Australasia, South Australian Branch.— Proceedings, xxvii, Session 1925-26 (1927). Royal Society of South Australia.—Transactions and Proceedings, 1 (1926). South 205 Gunnii . 205 INDEX. Bovistella nigrica .. -255 pusilla aera rosea 50. ASD scabra . 255 verrucosa 254 Brachycome cardiocarpa var. alpina 217-8 decipiens : mir eesee lO scapiformis 195, 197-8, 217 Brachypremna on 58 candida .. ao Bee 9 Be Cacia ‘ 388, 394 bella 5 5 Oo fenestrata .. 394 fulva SOO: maculata co etl pulchella .. 394 ruficornis 50 Oe! victoriae Brn gated . 394 Brunella vulgaris ou od) Brunonia 5 5 Rae er Bryopsis plumosa Hel eek BR x Bulbine bulbosa 50 Ye Bursaria spinosa . 160 Cabasa so oe! rufithorax .. o94 Caiusa 5 0 AeA surcoufi . 5b) BR Calamites .. .. 90-1 Calendula . . 484 Caligus xlvili Callicoma .. 114, 120, 162, 176, 181- 2 serratifolia 175-6, 181 Calliphora ee nee 300-3 ACCEPTA .. 307, 311, 314, 316 APICALIS 306, 312-3 ASSIMILIS 5 OS Bil7 augur 306, 309-11 AURIVENTRIS = 30K. a5 AUSTRALICA . 806, 314 CENTRALIS 5 5 SG, aBlal CLARKI 5 atl, silils Balko dispar . 306, 312 elliptica 5 Bets) erythrocephala .. 303, 306, 312-4, 319 fulviceps ee . 302 FUSCOFEMORATA 306, 309-11 hilli . 306, 309 lateralis : 55. BILD) MACLEAYI 306, 310-1 METALLICA 5 BOM, Bally MINOR . 007, 314 oceaniae Sp eee ly) ochracea OOD 08 ochracea form NIGRI- THORAX 56 oo GU, CLE PLEBEIA 5 De Ass, B37 pubescens - 312 ROBUSTA 306, 313- 4 rufiventris » oly) Suri. Soden ate Calliphora stygia .. XXiv, 305, 308- 9 tessellata u oS tibialis 305, 308, 315-6 villosa AN eee oly) XANTHOCERA .. . 306, 313 Callistemon Sieberi 194-5, 198-9, 204, 206, 208-9, 211-2 Callithamnion 460-463, 467, 469 angustatum . Abt angustatum Sak Pasa O brounianum .. 461, 464 brounianum . 464 conspicuum ‘ 460-1 crispulum .. 461, 469 dasytrichum 55 Atel dasyurum . 461 dasyurum ego LOG debile . 461, 469 formosum Me ecg UI | hirtum .. 461, 465 latissimum . 461 latissimum 56° 400 paradoxum ~ Aueil paradozum .. . 466 plumigerum .. 460-1 scopula . 461 scopula . 468 stuposum . 461 superbiens 460-1 tingens 460-1 violaceum . 461 violaceum . 468 wollastonianum 5 AuGal wollastonianum . 465 Calogyne 3 é we AW Calolimnophila Se SETS Caltha introloba 2lGer2ies Calvatia 5 YS aurea Pectin Sear a BG caelata 253, 255-7 candida .. 253, 255-7 candida var. rubro- flava 256-7 cyathiformis . 256 favosum . 256 Fontanesti . 256 gigantea 253, 255-7 lilacina 253, 256-7 maxima .. : 256 occidentalis bo PADD olivacea .. ao SMO primitiva ao ADD rubro-flava po 7A sinclairii .. 256 Campanula Hae OA: Campbellomyia ia) ORO Campolene CYANEA 5 BVA nitida P Bie ABA Carcharias arenarius 5 xdhial Carcharinus brachyurus xlvi Cardiothorax australis var. , PANE consimilis Nido Carex breviculmis .. Gaudichaudiana Cassinia aculeata 217-8 . 212 192, 194, 196, 198-9 Castiarina DEUQUETI a 225 DILATATA 226-7 FLAVO-VIRIDIS bo PAT FOSSORIA Per a20 Casuarina .. aerate! Catastoma 66 De anomalum .. 256 circumscissa sot 2D debreciensis .. a6 CANS hyalothrix o. 256 hypogaea ce ZS Muelleri s5 D8 pedicellata .. 256 purpurea ss CASO) subterranea S256 Catosperma 472 Caulerpa Xe 2 BRR, 558 9 abies So BN) Brownii.. 6 DY) cactoides So oo BY) clavifera . 5dd, 559 cupressoides 556 fastigiata Se DDS flexilis co. HRY) Hedleyi Pe 6a) hypnoides 56 BD) laetevirens 56 ERG ligulata eS Muelleri so BBL) Pickeringii 50 DY) sedoides so DOD trifaria 56 Say tristicha 55 DD Webbiana form _ tor- mentella SF 559 Caviceps : 435, 442 flavipes . 442 Celmisia longifolia .. 195, 215, 217-8 Ceramium clavulatum .. 555 Ceratocheilus 57, 69 australasiae . 68-9 edwardsi . 68-9 flavirostris 36 to 6. ised) Ceratolauxania . 400, 408 TASMANIENSIS .. 408 tetanocerina 408-9 Ceratolimnobia 54-5, 62 Ceratopetalum .. 114, 120, 161, 167-8, 172-4, 176, 184 apetalum priors awa LMS) Ceratophyllus fasciatus xxvi Cerdistus 387, 390-3 fulvipubescens 392 Cerodonta 423 australis 423 robusta 423 VITTIGERA 423 Cerozodia 50 Chaetogaster 3i5)33 INDEX. Chaetogaster violacea .. 353 Chalcides ocellatus .. xii, 27, 32, 500 tridactylus xliii, xliv, 25, 27-8, 30, 32, 499, 500, 503, 506-7, 537, 546-550, 553 Chalecoponera metallica xxvii Chamaclaucium uncin- atum 5 aid Chantransia as . 460 Cheilanthes | TRS ts TSN 803 emGllerrn os ov (eh tis 0 1 gracillima aor o lanuginosa .. Ts TH, TD) lendigera (35 microphylla Ua, U5) persica U5 5 US) tenuifolia 73-5, 77, 79, 81, 83 vellea x, 73-5, 77, 79, 83-4 Chiloglottis Gunnii 3) LOS Chionea = su tete boys Chloromerus » 430 GRACILIS 431-2 MACULIFEMUR 431-2 NIGRIFEMUR 431-2 pallidior AL ASE A Silt purus E 431433 purus form MACU- LIFERA . 431, 433 purus form purus 431, 433 purus form vaRIANs 431, 433 TRIM ACULATA esl, 48333 Chloropisca .. 429 MONTICOLA . 430 notata 429-30 ‘SUBNOTATA 429-30 Chlorops Badia a. Chlororhinia 1 329.7332 viridis bo Oe Chlorotachina 1 BDS flaviceps Sade CHOLEOTHRIPS 5 Aly) GEIJERAE 5 155-6 Chondria 555, 560-1 caerulescens . 560, 562 curdieana 562 dasyphylla e560 fusifolia 50 BOAL IRIDESCENS 50 Boll RAINFORDI . 560 sedifolia 560 tenuissima BaD 1 Chrysobothris 5 mastersi 2 eo Chrysomyia ae 325-6 albiceps .. 5 DA BAY incisuralis = BAD, B40 megacephala 327-8 micropogon 327-8 putoria bo BAe ? rufifacies bo BAY Chrysopasta 56 OZ Chrysopogon so Owes albopunctata > O94 Txexsxye Chrysopogon crabroni- formis 50 OS fasciatus 50 OS mulleri so OD nigriscens so OD pallidipennis BOOD punctatus oo OS queenslandi 50 OD rubripennis 56 BOB rufulus 5 OD splendissimus st 395 Chrysorutilia ? 348, 352 Cimex lectularius XXVi Cinnamomum ee Sala Cisseis careniceps .. .. 228 SUB-BIFASCIALIS 29229 viridipurpurea ype Cladochaeta 5 Cladolipes . 53 simplex .. so OS Cladophlebis PLoS Cladura 54 Claytonia australasica Veper Alar Cleithrolepis granulatus lili Clesthenia .. . 384 Clinopogon 395-6 Clydonodozus ao Oy! angustifasciatus :. .. 54 Clytocosmus 58 skusei 58 Cnemoncosis ‘ 57 Cnidoglanis megastoma lili Codium A 5 555-7 adhaerens 5 D5 Dae) bursa Be) ga BOIS difforme .. . 557, 559 GLOBOSUM 558 lineare so DDT mammillosum DDS ovale Sis cache Rone od ee Oe. tomentosum .. x, bdl,959 Codula 2 sa oe fenestrata ao oes limbipennis .. 394 ? quadricincta so aA! ? vespiformis So UE Coelochondria .. . 56 DUK!) Colobanthus subulatus so HAlis Comesperma retusum 195, 204, 209 Comptosia OOD Conosia 54 inronatal en. os: Conospermum Shien PAS Coprosma Nertera .. so Daley Coptorhynchus ALBIVARIUS 354 jansoni .. 3b4 OCULARIS Soon: TRIVITTATUS ODD Cordyline stricta 56, alts Correa Lawrenciana 56 US) Cossonus 367, 376-7 Craspedia Richea .. 195, 198, 204, 209, Paley’ Richea var. alpina 217-8 1xxxvi. Crocodilus porosus .. xlvii Crouania . 461 Crypteria ; cow eh Cryptochaetum 5 ela curtipenne 50 OR iceryae 422-3 LATIMANA a2 Oy monophlebi 422- 3 Cryptolabis ao HO Cryptopogon 5 BOG Ctedonia a 50 Ctenacroscelis .. 58 Ctenocephalus' canis xxvi felis xxvi Ctenolimnophila. 53 bivena 53 decisa 53 Ctenophora 3 57 Culex annulirostris Ox australis . 288 fatigans oe XV, XX, DGD-8 fergusoni . 565 flavifrons so CRS) occidentalis oo CAS procax ao cee rubrithorax Ameer tE)CL Culicada vandema .. .. 289 wilsoni 56 A) Culicoides .. 2 Xe Cyanonedys .. 394 Cycloderma ohiense 56) ADO platyspora oe 256 Cyclophorus confluens ao BUR serpens 5 DHS Cyclopsidea 55 (Gee Cylindrotoma .. 60-2 nigriventris .. 60 splendens so ED Cynomyia .. 50 ‘axdil Cyphogastra 50 BR browni 55 Cs farinosa 510 PR macfarlani See ere 2, pistor 5 LS venerea .. Sa Les vulnerata oad, Cyttaromyia . 60-1 Dactylolabis ae aio FAY) Dampiera 472-3 493, 495, 497 Brownii .. em Ashio stricta 471, 473. sth 493-6 Danthonia robusta .. 5 PALA Dapanoptera .. : 68 Dasylirion filifolius 272 Dasymallomyia 54 Dasymolophilus 56 Dasypogon 387 albopunctata 394 nitidus 397 princeps 397 rubrithorazr 394 salinator 397 spintha 394 INDEX. Dasypogon suavis OOK venno . 394 Dasythamnion . 460 Dasyurus viverrinus .. 550 Daviesia Cee ee 196, 199 ulicina .. 196,198 Dawsonia superba Se OLS Deltastoma . 435, 442 unipunctata .. . 442 Deltopecten . 104 obliquatus : . 104 RIDNELS Tes oh las) see Os Dendrobium . 570 Becklerii . 570 Mortii Later . 510 TENUISSIMUM a eae) Depressa . 399, 400 ALBICOSTA . 401 atrata : 400-2 STRIATIPENNIS Sette hess Aa Deromyia 395-7 Desmometopa m-atrum .. 8 VARIPALPIS .. 7 Dexopollenia chrysothrix 324 Dianella tasmanica .. 195 Diapontomyia .... .. 381 Diaspasis AN mee tattay eet | : S04 DiCKSOMLa eee en meee 10) Dicranomyia so. oo (OES _ diva aT CON VaR PR aed ta keke) doddi 64, 67 THONG, 65 50 on WO punctipennis Rey bere 14 OM tarsalba Per reve batires YT OK Dicranophragma i TAT AUM Ey OS Dicranoptycha 63, 69 germana 68-9 Dicranota .. 48-9 bimaculatay |. sane ee Dictenidia 57 Dictyosphaeria ‘favulosa BR 6 sericea . Pee eee Gey MON ae) Didelphiy Smee ene o Digenea simplex .. .. 555 Diotmephawe eae OS Diplotoxa = Wee eho 4 microcera 434 TASMANIENSIS 434 versicolor é .. 4384 Dipodium punctatum 55 BUS Discaria australis .. .. 197 Disciseda 235-6, 253- 4 anomala 239, 254-6 australis . 240, 254 candida .. 238, 254-6 cervina : 238, 254-6 circumscissa.. .. .. 256 debreciensis .. .. .. 256 hyalothrix 237, 254-6 hypogaea 240, 254-6 Muelleri Le 255-6 pedicellata . 2387, 254, 256 verrucosa au . 240, 254 DISCODOlA en oe ere nO Discobolo australis .. tesselata Per ike, (0 Dispar PPR NS Go BUD Dizgonomyza é 426 Dolerothrips (?) GEIJERAE 57-8 Dolichopeza 59, 60 cinereas 22 |. See mailagasva. > 2) Wasa queenslandica a eae OS, Doryphora sel an eee 161, 167-8, 172-6, 184 sassafras ; io abs Drapetes tasmanica Apaear sky) Drimys aromatica var. pedunculata 192, 194,198 Drosera Arcturi bo Chilis} peltata . 199, 204, 209 Drosophila Oates albostriata ampelophila .. Be 4 biarmipes iol eee 7 brunneipennis 4 buscki slo coes 3 BINIG@MA oc Sei Soe Ro flavohirta as 3 fuscithorax 4) ee hydei 3 immigrans 3 inornata 3 Ch tae 4 lativittata sig A regi eRe melanogaster 4 mycetophaga ae 2 NICHOLS ONiIia a aner ee <4 3 6 3 3 3 3 6 3 6 5 Co bo nigrovittata .. Hi NITIDITHORAX nat oe ea as obsoleta .. poecilothorax polypori repleta PERSIA Fes: SERRATA) 36 7.) aces setifemur 6 he SUBNITIDA Bol coteneecenede oe Cle SYDNEYENSIS me Gs Dryandra : 114, 258, 2 Dysmachus : a Echidnophaga gallinacea xxv myrmecobii XXVi Egernia striolata xliii, xliv, 25, 31, 499, 500, 553 whitei xliii, xliv, 25, 31, 499, 500, 520, 530, 553 Elaeocarpus ; 5 Wal4! Elephantomyia 53, 63 supernumeraria .. .. 53 westwoodi ..:°°.. J. 538 ote ener mens. 0S) OEP 56 6 i rey) Elliptera 63, 69 AStISIMALICa) =e nO CIAUSA ay ci Se OD. illini weet Sao.) ie ee 9) jacoti APG Rarattec ic. (UC) Elliptera omissa the Daahi69 tennessa ore net A68-9 zipanguensis wa? Seb 9, Elonichthys ALG Empeda a orev ea Toes ae Ey OG Empedomorpha atom okt) empedoides .. .. .. 56 Enhypnon laticeps .. .. 231 TLONCHBATIGNE 565 ina oo ezeul Eothrips BURSARIAE 5 Jus) Kotipula .. Ree air Epacris heteronema . 209 paludosa 194-5, 205-8 petrophila 215, 217-8 serpyllifolia 204, 206-8, 211-2 Ephydroscinis .. . 485, 437 australis Beene EAS Epilobium confertifolium 216-7 glabellum 194-5, 197, 199, 212 Epiphragma setae oo: , OX") Epitriptus fe BT dtotieee Eremophila longifolia xl vii Erethropogon 395-6 Eriocera 53, 55 fultonensis .. D2-3 gibbosa . 52-3 subrectangularis.. .. 53 velveta 52-3 wilsoni ~. Da-o Erioptera 46, 54, 56 lutea ate So OO Erythraea australis 197 IDOI, 955 oo oon Jia) ? BELLAMBIENSIS .. .. lll BELMONTENSIS 110-1 coghlani xlvii, 105-8 forbesi 107-10 GLABRA a Id GLENLEENSIS : 108-9 IPSVICIENSIS 107, 110-1 LATA cen re 6 Ld) LENTICULARIS 5 LOY) LINGUIFORMIS are pel ulbll mangaliensis 105, 107-8 minuta A een O09 NOV OCASTRENSIS 109-10 OBLIQUA .. . 109 striata 5 alk TRIGONELLARIS Be oo, LOY WIANAMATTENSIS 108-9 EKuamphibolia 351-2 Eucalyptus 114, 161-2, 164-5, 180, 182-4 albens : Bi AS amyegdalina var. nitida 184, 196 Blaxlandi 165,168, 172, 174, 179, 180, 182, 184 coriacea 114, 191, 194, 196-7, 200-1, 203, 212, 215, 219 goniocalyx 165, 167-8, 172, 174, 179, 180, 182, 184 INDEX. Eucalyptus Gunni .. 192, 194, 196-7, 200, 203, 219 haemastoma 161, 173-4, 176, 179, 180, 184 haemastoma var. mi- crantha oo. aUaxs Ural ley} hemiphloia 5 CABS meliodora MGA tS. eer} piperita 161, 165, 168, 171-4, 176, 179, 180, 182, 184, 200 pre-coriacea .. 5 Jlite! sideroxylon é Xxxix stellulata .. 192,194, 196-7, 200, 203 viminalis 196-7, 203 Euchondria . 560 EUCOMPSOMYIA ae AD LATIFRONS 325-6 SEMIMETALLICA 325-6 Eugenia australis 5 Or) coolminiana .. .. .. 379 Euglochina SRN bee ey OF! Euhippelates 435-6 pallidiseta 30. 40 Euhomoneura . 419 ornatipennis . 419 EKuphrasia Brownii 5 195, 204-5, 217- 8 Euphumosia 5 KDR, 3783 calliphoroides .. 324 eristaloides . 324 papouana .. 324 papua 323-4 variegata : aN . 324 Hurhamphidia .. .. .. 69 niveitarsis .. 58-9 Hurina 2» 442 Eusargassum .. .. .. 560 HUSTACOMYIA ..) 45.25 337, BREVISETA Fy 1 OREO RT ERR OE EUTHYRIDULA oo etl rugosa is 444. EKutolmus D0) ail Eixeretoneura 5 Gxsil Fagus .. MEAS heya weles: Fannia canicularis wie XXIV Ficus eugenioides 5. Os) henneana Botait oe be axthee) Fieldia 5 AL AG australis . 174 Filaria bancrofti XGV I EXLOXS Finlaya an . 298 alboannulatus eb 65 notoscriptus uke 565 queenslandis AG 298, 565 INOS, oso 56 oa. oo GOA) atribasis Sybil lucies 350-1 flavipennis .. .. °..+ 350 mirabilis i Dae 350 speciosa .. ; 349, 351 IDOVASAANOUIE, Go 5a oo oo Zhe! Hranklandiay) {sens ae 2D 8 Ixxxvyii. Galium umbrosum .. 194-5, 197-8, PAT Gastrodia sesamoides .. 198 Gaurax . 4385, 437, 444 APICIPUNCTATA . 444 atrisetaiiye, Sera loos sea se Geaster , ‘ 253-4 affinis a OCA Ae RO VAN CIICT Aeneas. eS) Tee OSG arenarius A rare eae argenteus cae SRN eo 6 asper aed Sano australis Set eee eee Berkeleyi Lay BAS Sch eee FA biplicatus Sevens 256 Bryantii : 254, 256 CACSDULOSUSH ee ee 6 COLCEUSOAR, 05 eee a6 campester 255-6 Clelandii chy, oe ee coriaceus ives See ED O coronatus dit) ZG delicatus 50 CAMO Drummondii 255-6 dubius bend NOR en 27215 6 ellipticis SU eh tht aaeerrqa ie LH OPA MOOUS So 60 oo PALS fenestriatus 5 255-6 fimbriatus 5 CA ADT floriformis 255-6 VOTMMCTUUIS a5 66 ao AXE granulosus 6d.) ace CAND Hariotii Sa) Wane yes Bee hungaricus 56 og 7D hygrometricus .. ... 256 involutus iE) lie Su bee Gs lageniformis ein 22 16 lignicola at Psa ye ola MerAS Me) limbatus Bete st aie 15) IGUOVOHE. ac 90. 40. 06 ZG MAMMOSUS ey ee MOAERLOULOLLS ae) eee O MinimuUs iS, eae e256 minus 255- 6 mirabilis 255-6 Morganii » 256 orientalis ee cat ioe aD pectinatus 254, 256-7 plicatus .. . 254, 256 pseudomammosus e256 Readeri BG) roeL CAO rufescens neous oar c) _saccatus Paes barat 700) Schimideviiw a. sea) oO simulans Se preteen te DD. Smithiis a) cee eaneiee DD striatulus Bede eon aes SHACTUST Roe subiculosus .. .. .. 255 tenwipes 256 triplex "255-7 7 tunicatus Me Wits d ot eure Ty ummobilicatus .. .. «. 2d velutinus 1xxxviii. Geaster violaceus so ZB Geijera parviflora .. 157, 159 Geoplana : XXXVii Geranium dissectum 195, 197-8 Geranomyia Ry ears TON. picta 66-7 tonnoiri .. 66-7 NGI bo sae og foo, We victoriae 66-7 @itomidesiees n\n) ecco 7 CONVERGENS .. rk Glaphyropyga australasiae 392 Globularia .. 484 Glossopteris 109-11 Glycine clandestina eg9 Gnaphalium purpureum 379 Gnophomyia Poti Vena Buses CPs): Gonomyiae oh oe 2514-60 Gonops geniculatus 390 Goodenia .. .. .. 472,493 cycloptera ne ehO'5 hederacea 198 Goodia lotifolia 379 Gracilaria taenioides 555 Grapholostylum 352 decorum 48. 352 dorsomaculatum eh eas Die Grevillea X6:O0b:¢; xd, 114, 122-3, 125, 258, 260 SCAM MMOIE, oo 06, a0 122, 124-6, 128-32 acanthifolia var. querci- foliae) ss. 5- Veo at teal! australis 195, 215-7, 259 buxifolia ne 125-6 Gaudichaudii 122-5, 129-32 lanigera 2) See 6 laurifolia 122, 124- 6, 128-32 parviflora Bo AAG phylicoides . 126 punicea .. ; 126 sericea 125-6 sphacelata . 126 Griphoneura . 429 Gryllotalpa . 455 Guioa semiglauca no Ue Gymnastes 51, 54-5, 69 ornatipennis.. .. 55 Shirase yee OD Gymnobaris pA RUM 751: Gynoplistia <3. gee O bella ia 2 aie VOR ALIEA DO dimidiata 3.8, OA ee DL RIAU TAS Terese g se oa hiemalis ieee | Waren Rab HASvOMItIC’, 2. “ac ieesol EVADLOmMastix, 42.6, neous Habronema megastoma xxi microstoma REX muscae 5 OS! Haematobia exigua AA >.©.4 Hakea 5 A425 8, 260 ambigua PN (fe INDEX. Hakea amplexicaulis . 269 arborescens : 50 AAD} auriculata . 260, 269 Baxteri . 265 Brownii . 264 Candolleana .. .. .. 266 ceratophylla . 260, 265 clavata . 268 conchifolia Sn enone corymbosa 5 ADIL, AZ IL cristata .. . 269 cucullata 260-1, 272 cyclocarpa : » AIL, AOS dactyloides 5 ILS, ABO, AU epiglottis . 259 eriantha ye 20 eucalyptoides a orAtal falcata 5 ADT ferruginea . 269 flabellifolia See 04: florida 5 CADE glabella .. . 269 Hookeriana Beet ee ZO incrassata . 260, 264 lasiantha 55 ALD laurina 271-2 linearis . 269 lissocarpa BE Big cA) Macreana 195, 198-9 macrocarpa . 259, 263 marginata 268-9 megalosperma .. 268 microcarpa 199, 211 Morrisonianum .. 267 multilineata .. A 262, 270 neurophylla 5 MA nitida aA ee OTS obtusa . 262, 268 oleifolia . 5 A orthorrhyncha . 259 pandanicarpa 267-8 petiolaris 271-2 plurinervia a BUA pugioniformis . 259 pycnoneura . 267 Roeii .. 264 ruscifolia 269-70 saligna . 270 stenocarpa 3) AUC trifurcata MMA LED gh PAS) undulata 2 2603 20Al varia : 6 ZAG varia var. intermedia 273 Victoriae aa AUC vittata . 259 Halimeda > DDT incrassata > jaz ODUNTIAN en) se 5 atl POlYAACEYLIS! |) eID DI tuna | 555, 557 Haliseris , . 560 acrostichoides . 560 Muelleri.. . 560 Harrisomyia 53 jo Ut Hebenstreitia dentata .. Saini Helichrysum baccharoides 194-5 bracteatum Ro di. 1} rosmarinifolium .. . 194 scorpioides 195, 197-8 semipapposum 197-8 ee aa Ae 5 aril lascus : 5 OY Helipterum incanum 217-8 Helius us 63, 69 uniformis i | Ee OS venustus 68-9 Helix aspersa .. . xlv Helobia Re os ae) 8 Helosis 484 Hemarthria compressa wie 204-5, 215, 217 Hemicistela testacea » 2e2 Hemipyrellia 55 OrAl) cyaneomarginata . 320 fergusoni 5 Al) ELE NDELONSY.ZAU) 4) ene 8 HU DOMCOOMNHIS Go 40 oc 8 Hesperilla .. 275-6 andersoni 2s chrysotricha . 279-80 chrysotricha chryso- tricha . 280 chrysotricha LEUCOSPILA 280 chrysotricha PLEBEIA .. 281 erypsargyra .. sil: crypsargyra crypsargyra 281 erypsargyra HOPSONI .. 282 eyclospila 278-81 donnysa.. 278-80 donnysa AURANTIA 5 UY) donnysa donnysa o ang) donnysa FLAVESCENS .. 279 donnysa GALENA .. . 280 idothea » BUS picta 281-2 Heterangaeus 48, 50 gloriosus Semis Liter: cts Heterolimnophila .. .. 50 Hexatomia: ise 2) eS megacera syayl.) Vet eS Hibbertia linearis var. obtusifolia 195, 197-8 Hinulia quoyi xliii, xliv, 25, 30-1, 499, 500, 553 Hippelates .. 485, 437 ABBREVIATA . 437, 440 ATRICORNIS 437-8 atriseta .. 437-8 bancrofti .. 437 FERGUSONI 437-8 NIGRIDORSATA 437, 439-40 UNIMACULATA 437, 439-40 Hippobosea camelina . XXV equina 5 LOY Histiopteris Ai trees alte incisa . 162,181 Histriobdella homari liv Holorusiays.) .2 ant LOS Homoneura 12, 400, 419 - apicinebula 13, 420 armata . 13-5 ASYMMETRICA . 13-5 atrogrisea 12, 419 barnardi iB}; 1s) eidsvoldensis Biehl tees OL ka} FERGUSONI .. 420 FLAVOFEMORATA . 420 fumifrons 5 Rear ate eeaeaa a Ls) GORDONI .. 13-4 ILLINGWORTHI .. 13-5 indecisa se lord ornatipennis . 419 PERTHENSIS . 13-5 preapicalis 13, 15 proximellay 82 se es signatifrons .. .. .. 13 TESTACEA ‘ . 419 Hoplanthemistus albo- fasciatus oo. 7%! conifer . 234 Honistomyila 2.25 '.. .. 50 leucophaea .. . 56g DOS Hormosira articulata . 560 Hornea : : 5 Sabb Hovea longifolia 5 NG, sus) Hudsonia .. peel nl PGs) Hybrenia angustata 5 RY: ILLIDGEI .. >, oe pilosa j . 234 Hydreoclathrus cancellatus 555 Hyla cerulaea .. XXXVii ewingi F XXXVI1i Hymenanthera dentata 198, 217 Hypericum japonicum 198-9 . 555 . 229 Hypnea seticulosa .. Hypocisseis suturalis Hypolaena lateriflora .. 199, 203-5, 209, 212 Idioglochina .. .. .. 67 TaKoryowe, 6 be “oo oe DY) Idotasia ae 5 OU) llex 5 > Atal Incurviseta .. 400, 402 AFFINIS .. 402, 404 BISERIATA .. 403, 406 FLAVICEPS .. 402, 405 FLAVIPALPIS .. 403, 407 FULVOVIRIDIS .. . 403, 407 LATIFRONS : 403-5 maculifrons 402-4, 406 TASMANIENSIS . 403, 406 VIRIDANA 403, 407-8 VIRIDULA . 403, 408 VITTIGERA . 403, 405 WILMOTI . 402, 404 Ipsichora so a) BIMACULIBASIS so Oho) desiderabilis 369-70 INDEX. Ipsichora TIBIALIS Irona .. Ischnothrix australasiae .. connexa.. Ischnotoma Iso flos-maris rhothophilus Isopogon Isotrogus bilineatus castelnaui TRREGULARIS Jania rubens Juncus pallidus pusillus .. Kladothrips AUGONSAXXOS rugosus .. Kreyssigia multifior a Kunzea Muelleri 57369 xlviii 52-3, 63 52 52 DS 5, dbrbs< xIviii P2518 5.6 BUT oo BUT 5 UO .. 555 co UY) > IY 153 “153-4 153-4 . 378 195, 199, 216-7 Lacerta agilis .. 503-4, 506 Laosa .. Mae OS Laphria . 094, 396 Lasiothalia 460-1 hirsuta A 460-1 Laurencia obtusa 555 rigida 555 Leaia .. 105 Lechria 62 singularis 62 sublaevis 62 Lecteria . 54-5 Leiomyza 445 LEPIDOBARIS 370 METASTERNALIS 371 Leptoconops xxi Leptogaster 389 aestiva 390 antipodus 390 australis 390 autumnalis 390 bancrofti 390 dissimilis 390 fumipennis 390 occidentalis 390 pedanus .. 390 vernalis .. ‘ 390 Leptoplana australis liii Leptopsylla musculi XXvi Leptosiphon 484 Leptospermum ppel99) lanigerum 194-5, 198-9 stellatum 196, 198-9 Leptotarsus Bas SUR'S macquarti ao BN Leschenaultia 42 Lestophonus sig AAIl Leucadendron 8258 Leucophenga 2 1xxxix. Leucophenga MINUTA .. 2 Leucopis ave 5 APA Leveillea jungermanni- oides OD Libnotes 64, 66 STSCI 4 se Se 66 OQOWCHA. 65> oo sy on OB TC LATS CY, cone ade ee OS ROSIN grein wwe. EE LOG subaequalis .. .. .. 66 thwaitesiana Cuneeetab6 undulata a ae. Borie ad) WiCiN OM aa eS aerea NOS TE reer ae iT angusticollis A MeO apasioides ys al eo Coeruleaicy yc 5) ee commoda 231 cyclocollis 231 elata 231 gilesi 231 illidgei 231 major 231 meridiana 231 monticola 231 nitida 230 nitidissima 231 nodulosa 230 pallipes .. 230 planata 231 puncticeps 231 splendens 231 subcanaliculata 230 sylvicola STE 5 eb rad Be tasmanica 230 truncata 231 umbilicata : ag 2D) Limax queenslandicus se wall Limnophila 50, 53, 62 Limnophilella ... 50 imoniays we ee. | ee amabilis Ler IRE Al ae oe tl PINAL TK eee Me ete en eee Os! BOOTS) 64 oo oo oo BO Eeenclorsibon 55° 4 so (87 basispina Sek Sea OM bifasciata ite ae SPO CalifornmiCa ae nO cinctipes Yeu Na es 67 esakii cS scat Ne SRSA eee ok ONG fallax Ar Mums me ts) Li'sch bY Natl HAV IDES celeste eee Ord fumosa 66-7 immatura Liay > jaan eae Ont) indigena SEAN Sea aise PONE! insularis ee Sete ot tr Bay LIVUS CAM ae ay, ere Seen ON) TMEKCWINKGOSNY o5. ac oc al THOT OOWUORE, 855 oo 60 WY parietina Ae SLE Oe RPA, Go oo bo ho quadrinotata Stan Git sciophila SP ectal aa Ot solitaria Sete tay ilk. fai xe. Limonia sponsa Se RS NONE: triocellata PUNY 2 Lo escn 3 PLS (BEYONCE, sa oo oo, Ol tristigma NAN ms ob ae Peer’ OV tristigmata 66-7 trivittata ORE dees SUL Lindsaya linearis .. .. 81 MMNGRO OAV, co oo bo til Linum Be uebeTEs cs ets oaks ore marginale 194-5, 198 Liogma Ales . 60-1 glabrata 2 Rom es ee Gill nodicornis Lat Lol etait geet batt () Liolepisma entrecasteauxi, xliii, 25-6, 499, 500, 546, 553 Liphyra brassolis .. .. liii Lipophleps ees eb leetay Sh 15)5) Ib OW ME oo) Gea doo sau, Be Liriomyza oper He Ny42 6 PALLIDICENTRALIS .. 427 OMG, 56° “Bev e0 oa Aa TRICOLOR eee sk CLA Lissanthe montana 195, 216-7 Lobelia . «. 484,495 trigonocaulis Oe Be. Be Lomatia 4 alas, eal longifolia 196, 198-9 Longuriv .. AS Loranthus pendulus 50. BUS) Lotus australis 197-9, 204 corniculatus ~ LOT; 199 Lucilia 303, 316, 318, 320-1 caesar i 321-2 GRO oo oo da loo Sul cyaneocincta fDi: cyaneomarginata .. 320-1 fergusoni Bre ene Vig os OAL) FLAVICORNIS 321-2 nosocomiorum hee 321-2 pallifrons gate Pa Seat eee AL SCLICALA Coe Lutzia halifaxi FER ee dt COMED) Luzula campestris .. 204, 212 Lycoperdon oe. AEDS asperum 254-5, 257 QUST Alera e 257 BOUUSTO acs 2 EL Ae POVAIStOIdes!);, ee oe candidum PM Ll ns hrAD CEPACTOTFANE .-)) > eee Colensoi Mo Oe foc PANT coloratum i 11 BS. COmpActim, =) | See ec DS COOKE. 50) eee coprophnilum.. Peas COLIN os MERIT cruciatum day vee aD depressum .. .. 253; 257 dermozanthum ..... 257 fUUOSIIVE 2) et eee OLN Fontanesti. .. ..° .. 257 furfuraceum Pee by hilt gemmatwum .. 2.215.. 257 PiPanteum (7). | eae. edt ENDEX. Lycoperdon glabrescens 245-5 Gunnii 254-5 WOCHUBUG o6 566° on. 06 ABU hungaricum .. .. .. 257 lilacinum Se ccatevemieres e 2 Dyl) macrogemmatum so ZANT microspermum .. .. 257 natalense eA aes TG OCU 06 o0 ‘on oo Gadd mvenGlbeat G5 6k oo) CU novae-zelandiae .. .. 257 perlatum 5 253,257 piriforme 5 ADB, Ze piriforme var. flavum 257 polymorphum . 2538, 257 pratense id chen PEAR e ON pseudopusillum .. .. 257 purpuraceum ae cee (DOW OURGOHE oo a5. oo ADY pusillum . 258, 255, 257 TFOLLCOMETHT 56 900 60, HDT retis A sf Leet a BT: rubro- flavum | Riera 45) | scabrum Bie 254-5 semi-immersum .. .. 257 Sinclairii Dele Pleas eke Sl spadiceum .. .. 253, 257 stellatum a NE PODS subincarnatum 5 A, CADE substellatum at 257 tasmanicum ROR ao ea tephrum Prarie poss? ca violascens BUSTA NEMO ay LeU Wrightii ae 2 YG Lycopodium clavatum on ALT Selago .... PAT Lygosoma entrecasteauxi xi, xliii, xliv, 25-30, 499, 500-1, 503-7, 525-6, 543, 546-53 quoyi xi, xliii, 25, 27-31, 499-501, 503-7, 525-6, 543, 546-53 IMachimusiy eee SO Macrochile 5 Soe a plete he Nee Ally Macromastix. 2 phe sae DS COStALIS He...) cna BS See eS Macrotaeniopteris .. .. 108 Mandalotus Bie cron: eae Oe) ARMICOXIS ice ppeney breeehere iT campylocnemis .. .. 356 CaLnInatipesi i aE So HourseoreNbI 55 55 oo BHT mirabilis oo RE) Geo Dyer >) See obo STERNOCERUS SRE ay or CLG Viet VEUIS) heer), |) Meio OO: Maria bide as Seto 4 Megistocera ee sadrratn axe) longipennis 58-9 MeESISTOMAStIX. arlene OO Melanagromyza yess esa ALBISQUAMA Melanagromyza phaseoli 424-5 -TRISPINA 424-5 MELANINA .. - 400, 412 AENESCENS! (5.0 cele MAJOR 412-3 PLEBEIA 412-3 QUADRISELIATA 412-3 Melanterius oe ee OA: Melinda Ae bow hOB Melophagus oy inus BEPXOXGY, Menyanthes Peat, prod aeKe Merimna atrata Rie Sic ee eae Meromyza Ms oo, CIS Mesodina .. 22) Ba Aae275 Metalaphria é 395- 6 aurifacies Li Saas 96 australis a Ce OOL6 Metallea 2. | :)) sah o e829 gracilipalpis .. 329-30 illingworthi . 329-30 INSULARIS 330-1 nigribarba 330-1 PUNCTICEPS 330-1 robusta 329-30 Microcalliphora 325-6 annulipes 2150s hae nem a O flavifrons eee so AD VOUOYNES 56 60 00 oo S28 Vari pes! :c..We eee 6 Microchrysa io oO Microtipula say) eee eee Microtis porrifolia .. .. 378 Microtragus 6. DE Oe. arachneias se Oe arachne var. sticticus 234 CEUSTUWLOLLS tS: echinatus aia t he 234 Microtropeza "'952- 3 Miltogramma:.. .. .. 335 Mischoderus .. . pee er! 45) Molophilus “46, 54, 56 froggatti Brod Diemer tim 83 Monophlebus.. .. 423, 446 Monospora ee the eae O) Mormoniella brevicornis xxiv Morphomyia .. .. .. 339 tachinoides .. .. .. 340 Motasingha shes) Levey Rape ie AHO dominula at) Src: drachmophora Pree. atts: monticola shai. | Saicet nee Mugil ae . xivi Musca nate - eo Oe domestica xv, xxii, 302, 314 Mycenastrum 245, 253-4 bovistoides) Ys) eee chilense cele rosie MR we OI clausum Rr siar corium 245, 254-5, 257 leptodermeum a 257 olivaceum 1/5 Soiree Ot phaeotrichum erie Ane radicatum Sint Late) Ciena ON SPUUULOSTTI weld ethene ti Mycodrosophila Siesl (ie 1 ARGENTIFRONS i if Myctides balaninirostris 366 Myoporum .. 484 laetum xl viii Myosotis australis Pei Scicer tly Myrica ies age ele: Myzomyia .. oo-4 amictus .. 34-5, 37 annulipes 5 OOD) mastersi chit MR haa O10) punctulatus . 33-4 Nasonia brevicornis xxvii Neoaratus 385, 390, 392-3, 397 inglorius : 393 Neocalliphora j 304, 308 Neocerdistus 390-2 Neocladura ae eite ent Bye Neoculex fergusoni so BOD Neocyrtopogon 383, 395-7 Neoderus .. .. . 45 patagonicus .... .. 45 Neodioctria 396 Neohesperiila .. .. .. 275 Neoitamus Ad an Bol, Bol Neolimnobia .. .. .. 68 Neolimnopfiila Se atpan aye Neomeris dumetosa 56 BOO Neopollenia . 3804 Neosarapogon 395-8 Claripennis) 2. 3. .. 39 froggatti Bae HS elitacas oneself nigrinus fey Meh Aerts teen ts 91: princeps 397 Neospades chrysopysia 56 eve) CUPRICAUDA .. 228 eOuGH: 65 bod oe ae. 24s lateralis te 228-9 NIVEO-SPARSA ae oo | AS Nephrops norvegicus eo Ibhy Nephrotoma dts 58, 60 INGEOWOZE 46.) bo a0 oo OY) Nipponomyia 47, 49 kuwanai nbc abe ah eT a) novem-punctata .. .. 50 SOMATA, | “go ao oo ON) symphyletes .. 49, 50 trispinosa Ree eee AP) () Notaden bennettii .. xxxviii Nothoderus Se rece iat ene) 92:5) australiensis fe rey Notiosomus 5 Se INSULARIS eM OO Nusa : . 394 Nyctozoilus pemionaivencis 232 TAYLOR | 32 1 ao CB Ochlerotatus . 284, 286, 288 aculeatus . 295 albirostris . 288 andersoni ~ 291 antipodeus .. .. .. 288 burpengaryensis .. . 294 E INDEX. Ochlerotatus camptor- SARCINUS 56) 50 on Zab clelandi .. yee tine 294 cunabulanus.. .. .. 292 flavifrons .. 289, 565 imMpRimens Meme eos luteifemur ney ae IO MACLEAYANUS At oe Oe yl nigrithorax Pete eR age moans oo. oo do oo ZAYB normanensis 50. ZNO purpureiventris -. 294 rubrithorax ao Ae sagax j be 292 stricklandi oo XD) theobaldi 5 oo OD theobaldi form &EIDS- VWORDIWSHS oo oo oo AD vigilax . 296, 565 vittiger oo Pe) Ochromeigenia 5 60 OO @immONONGleS 46 oo 9 oo Bests Ochromyia 56 0 6 ON 2? hyalipennis oo. oo alts Oenothera biennis .... lili OCOPANE, oo ba 06 | oo lb Oestrophasia Pay Ese: Lave al) Ogyris aenone.. .. .. 1 amaryllis OUEST E LT Ae 1 OTOeCTES We le ue fe 1 Olearia flor bunda PAILT( megalophilla 194-5, 198, 200 myrsinoides .. 192.195, 198 Ommatius as x 390 Onchocerca eibsoni- XX, XOX gutterosa Hig Sine aan? a lienalis 66 Oc Onesia 301- 2,316 Ophiodesma a Leo sate & Ophiomyia . 424, 426 lantanae . 426 Opseostlengis .. .. .. 395 insignis She (bau. LORD Oreisplanus 275-6 Oreomyrrhis andicola 195, 198-9. 203, 206, 212, 217-8 pulvinifica 5. Ake ONCE, 55 of oo oo We alpinay tases. ar ee O64 IGN Ae es, ere eee ats OE damped i G4 excessiva 5 63-4 fORIMOSICOLA NEE nO joana a 63-4 TAIAWEMEBIESNIS 55 6a) WE TOGWURIGINIORISHIS Fo oo 06 (eh punctipennis 63-4 Orimargula 63, 68 australiensis 5 56 ASG) Orites lancifolia 195, 216-7 (ORMNORIEY 55 “co c co DO Ornithodes ca. Wnt Poet Oropeza NS ALAS OO Ovinus mylittae 55 DUS KCI Oxylohium ellipticum var. alpinum 192, 194-8, 200, 208 (HOUIOORNADION oe o6 oo ord) OVAOCKIOEIE, 556 co co da bis Pachylophus . 428 ALIENUS .. 428-9 lutea 428-9 SECUNDUS 428-9 IEAGUTENOINE) a6.) oo oo os CD Palpostoma 337-8 APICALIS Silat yal Lee oo, desvoidyi OOO testacea .. 56, asaxe: Panax sambucifolius 194- 6, 198 Papilio aegeus .. xlvii aegeus ormenus xlvii androgeus xlvii oberon . ao xlvii Paracalliphora ero Paragymnastes 51, 54-5 haASCIpPeninilSee see DD Parahippelates - 435, 437 Paralauxania 400, 408-9 ATRIMANA 409-11 elevata 409, 411-2 FLAVIPALPIS . 410, 412 FLAVIPENNIS 3 409-11 fulviceps . 409, 411 NIGRIMANA ab 410-2 SCRIPTA ae 409, 411-2 Paralimnophila Besa pares Kona!) Paramenia : 5 aby Paramphibolay s..5) so len ene Paranomina . 400, 402 - unicolor aot ae Gh RaTraracusmeacwaee . 390, 393 MACLOStYAUS = VoLe Ooo Paratricyclea .. .. 303,322 TaORKEhieWagees Meee pts.) th LOR SUIRGOWNT 55 oo oo, oo RS Paritamus Lat Chere Pectinotipulina Rhy Mest taarss Pedicia ; EA 49, 50 Pelecorr hynchus EO OL! Pentachondra pumila .. 217 Pentarthrum : 5 BU australe PA ols, Sao FOVEICEPS aM 374-5 FOVELVENTRE 4. 9.2 2 ole huttoni ne 372-3 INTEROCULARE eo OD MiUillimMetOnie MOS nepeanianum 5 Ba nigrum 373-5 ORTHODOXUM .. 373-4 SMPMCIKCOIEIU oo co oo OD zealandicum .. : 372-4 Penthoptera TER OES) eae E183 Perameles .. 28-30, 499, bad, 546, 550- 3 Peringueyomyina .. .. 45 barnardi RA TEE EA 5 Peripatus XXXVii xcil. Peripheroptera 64, 67 CUCORPO® oo o6 60 05-2 WY HOVEOUNINOG, so oo oo Wd TOSIOSY | So gs Seige ton | oo oO Persoonia re ee onset) La yt ROO) od! be a6 oo Jet chamaepeuce 197-8 Fuanyoeenine, 66 bo oo Zo) INM@BTENIS og. oo a0 oo BUY) salicina 176-7 Petaloxylon porosum .. 113 scalariforme URLS Petauroides volans xlviii Petrophila Te ae ey TaD OS linearis .. . st EO An) Pezohelaeus denticollis . 5 OW) WnEUS Aeneas Beet) Phacelodocera BUSA LEDS Phalacrocerd eee le nOO formosae Pata Bare toO OCCICENntaliShey ce COO replicata . 60-1 tipulina . 60-1 Phalacrocorax carbo tees BL Phebalium ovatifolium .. 194-5, 216-7 Phellus . 388, 394 FIBMCUS 56°00 ob . 65 Soe piliferus SA aioe. Phenicia j 320-1 CUI, oo ca ao 40, Call Sericatan ey. Bian te eo2r IPnerocerawae i | eos Philonicus 385, 391 Philydrum lanuginosum 378 Phlaeophagosoma .. .. 376 corvinum fee, oA Dee OTG chulrpAvbea, 26° 56 on. oo. UD pedatum ee OT IAN OKO = 55 be oo 2x Phumosia .. 2 a2Z0 3823 ANAS eee eee Oe} Phyllolabis 50, 53 Phyllotheca Fiche cas) eLOS australis OM LE cee Ope) Phyllotricha He Niaak eigk One) Ey Mmatopsisi. mee ees Pimelea alpina 216-7 axiflora 5 ARYA TUS a, ale! axiflora var. alpina .. 217 SLATI CA es a coand, eae MELO. ligustrina 366 Bley aaa 2 ligustrina var. hyperi- cina j 195, 198 Piophila contecta 8 latipes ...2 tt A 8 Pittosporum rev olutum ong Plantago varia 195, 197-8, 212 Elatycephalus... Assit. oli Platycerium grande Se Loue PLATYINA ; 435-6 WEBULIBER AM Wee Us 1436 Platyiimnopia.. sail aie Platyphasia sete ob Me ABS INDEX. Pleonosporium ey re 4 Ob) brounianum .. . 464 Plusiomyia Ata eeaeeminis in: | LNs: felix eee ber oies (LL ede 8 Poa caespitosa .. .. 192, 195, 197-8, 204-6, 209, 212, 215, 217-8 Podocarpus alpina 195, 215-7 Podolepis longipedata .. 195, 198, 218 Podoneura Se TG Poecilohetaerella . 400, 408 Poecilohetaerus . 400, 408 decora Ne . 408 punctifacies 66. oon COS schineri aba OO RERAYS Poecilopachys bispinosa liv Pollenia 303, 318-9, 328 auronotata .. .. 303 HIRTICEPS Sieh larat sd hhs VESTS moretonensis .. .. 335 rudis ee Mee els waa aa eee As [tet ruficornis Se) ee Ero D tasmanensis.. .. .. 335 viridiventris aS 335 Polyangaeus “48, 50 maculatus J RB es Teg IPO ANE. 66 - oo “oo. oo 0) inornata arse > Uae Meena sty () Polymoria red eect) () ‘Polyporus mylittae ETS Polystichum aculeatum .. 195, 215, 217 Pomaderris Disk eae ee thes LL Poranthera microphyila 195, 198 Prasophyllum fuscum-.. 203 Prionocera Sch aeewe | eth OS IETPIOMOUB, oo. 6a oo ac Be Prodiaphania .. .. .. 351 testacea PHA tal Gin) Promachus 390-1 laciniosus wc (eat eer Oli PROMUSCa Sh yo eee Oe Prostanthera cuneata .. 194-5, 216-7 Proteosoma 7 MONEY ek PES OKAVE Protipuiay s.:, '/2c, £590 eee Protomiltogramma ooo Protoplasa sie Sehyeish ab ae Prunella yulgaris 197-8 Psaronius .. 51, 55, 69 abnormis oe 51 brevitibia ee Weaee? Seta: MATTCUS aes ts ee IL: ODIITEKATIS |e eae obscurus Par bA act ede, Aun etiay Ul trianguliferus nM alas etal Pselliophora Sa? 57 Pseudolimnophila 50) 53 Pseudopalpostoma .. .. 339 Pseudophryne australis xxxvii joniorwonahin 45% ; XXXVii Pseudoskusea concolor 5.0 PAD Psiloconopa Renae Hob okt Psilostoma incisuralis Bi OC Psilozona .. 232 Ove Pteridium .. 165, 167, 172, 184 Pterochionea .. .. 54 Pterohelaeus .. .. .. 230 WOHMOHHIS 556 60 co on 2A) sueriniy s. | aye oO) puer Sk eee ZOO CU POGUHTOS oo oc oo atl) ventralis id Eee 23 0 Pterostylis acuminata .. 198 coccinea BTM. 43) Le mutica sic Gs See Pterycota.. i. oo eee Ptilogyna 58, 60 Ptiloniesiay 3.) 2) eee Oe aunonotata 25 eels Pinlostena 4-0) sae eS Ptychoptera lenis .. .. 70 Pulex irritans .. XXvVi Pygiopsylla rainbowi xxvi Quercus a a aaa alt Questopogon 395-7 QOuintinia ~. 3. fa ee 20 Sieberi 3: 3. aS Rachiopogon 395-7 Radinoderus 54 hen Ranunculus anemoneus PALL dissectifolius che PeeereaevetlaT. Gunnianus 217-8 lappaceus i) Se Lg Millani MS hire aca “dle Muelleri nie 217-8 rivularis . 216, 218 Raoulia catipes 216-8 Rattus norvegicus .. .. XXV rattus . XXV Restio australis ae 203, 206-7, 209, 212, 218 56 Rhabdomastix .. Rhabdotoitamus el ROL Rhacopteris aoe 55 HRA Rhagadolyra .. .. 400, 413 handlirschi .. .. .. 413 Rhampholimnobia .. .. 69 Rhamphophila ha ee O Rhaphidolabis .. 46-7, 49 CAYUGA ch lie | a major er caro CL polymeroides pdllibe Richea Gunnii.. . 194-5, 204, 207-8, 215, 217-8 Roestelia polita xvii Rubus parvifolius .. 196,198 rosifolius Bes, Sette seei9 5: Rumex acetosella .. 194-5, 197- 8, 212 Rutilia 342, 345, 348, 350, 352 aneentiterd 5. <<. .. 349 GeCOnameesy see ise. Pe sab2 desvoidyi 345-6, 349 erichsoni 348-9 formosa .. 347-9 inornata . 847, 349 splendida 347-9, 352 vivipara .. 345-6, 349 Rutilodexia Pace ee lame aay. angustipennis po. 6g De Sambucus xanthocarpa .. 378 Sanmvalwmi ss a se eld Sapromyza , 8, 400, Agile 3, 415, 418 AVICOLA , 416 barnardi mes Pelanee skh, Phy BREVICORNIS .. .. .. 10 brunneovittata .. .. 12 flavimana ae rag kee Seoretiy PLL! FLAVODORSALIS Sena ewe alle) HIEROGLYPHICA ..... 415 maculithorax LN eee Dy magnicornis .. .. .. 9 magnifica Beth tak, hiccty a weil) IMUNRDAI Ve cel wos ee ll occipitalis adeel FAP ammo te U7 OCELLARIS Oe estan kali PETERSENI 414-6 PLUMISETA 414-6 regalis 416-7 RIPARIA .. 9-10 sciomyzina .. .. 10, 12 Stismaticas le se wl STRAHANI 417-8 suffusa Osha et 415-6 TENUICORNIS .. .. .. 8-9 TONNOIRI pay eealeg menage: BLY unicolorata .. .. 10-11 WRENN cas gucah «0 sane LO WHIPS HOIS 456 o0° +04 dy Sarcophaga 300, 305, 334, 447, 450, 455 albiceps . .. 448, 455 alpha ROSS eee ey AS antilope . 447-8 ANTILOPOIDES 448 aurifrons 447- 8, 452- 3 bancrofti Ai suan deta | ieee bi 15315) beta 448-9, 453 carnaria Bee iti alte DD, ceylonensis 452-3 communis Rael ey SAS CHASSIMEAI eS Fat ate 2452 INDEX. Sarcophaga crinata pig. GID) doleschali . 448, 452 Guubxeuene Sa ene 448, 452-3 Ctaiorr ga cas, Mba errr 2 exuberans eens es V4? fergusoni ne hice sh DD favinenul Smee wea eo flavipalpis .. ». 448, 452 floridensis .. .. .. 458 froggatti Bea Novel blades ee aE fuscicauda .. 448, 454 gamma 1. 458,455 haemorr hoidalis. pais we eats: HaLDaAxXeeo ese se a ab! howensis as 448-9 hudsoni aie athe g pswhe Al JAVANA crac. 2c! aw oe 448 KARNYI .. 448, 454 knabi so oa AIR, ale knabi Re ee aw eR hate de BOC a kohla seioeea es 452-3 lineatocollis .. .. .. 448 luzonensis Sete 452-3 marshalli hee ae eae nah 2, milleri 455-6 misera 447- 8, 451-3 MMAtICOlOT a een e456 ochideawen ae. ow of 245) omega ; 447, 453, 455 orientalis ee wae 4S pallinerviste =.) ei.) ae 458 pectinata SGM ok ADO peniculata .. Pee 4 5S peregrina 447- 8, 451, 453-5 sarracenoides aa 452 scopariiformis eel Avera D2 securifer Roma vere LAAT, shermani oe LOTR dein: 7 synia tm Unie Feet PAS taenionata .. 448 tryoni 450- iL, 453 tuberosa . 447, 452 zeta Seon pts th aarti BS) Scaevola : . 472, 484 Hookeri Meni Ser hte OD Scamboneura 59-60 plumbea 59-60 Schizomeria Ree GAA) Le Weel? () Scleroderma bovistoides 257 chilense PAA i OO Tf COLUMN uae dee Lehre leptodermum ie cae Asi | olivaceum Bra ae) SRD phaeotrichum 5 Om) BGI EEADI radicatum Sie DUNES ee neta TT SOUOMOSUT of oo. oo Dt Selago corymbosa .... liii Selliera ad eer erne tas. ANE aLALT 2, SEMES WAU AGueee nee 339 AUSTRALIS " 340- il ING/NAKCONINGIS! 65° oo | oo axial HY ALIPENNIS 341-2 NIGRICORNISW einen Oa NITIDIVENTRIS nid eiyee OAL xelii. SEMISUTURIA PAHANGEN- SIS ae a ts Wee 4a TRIANGULIFERA : 341-2 SEMMNMOUTS co oo o0 oa ioe Senecio lautus .. .. .. 195 pectinatus aR Sore tat aL Senostoma Be he SOD Sepimentum RA iba ett On lee) HIRTICEPS ee he TS ONS NS Setaria tic, CRN ote bh rand Bee 3) BUCHANANI i 185-6 @ARINETS posh) Waseem Oe Gils. VAG CIS een ee ete eee 1 Sherardia arvensis .. 489 SHEFVIOGSSE go 66) oo) oo. AE WENO, oo 66 oo bo. 246 MELBOURNENSIS .. .. 445 Sigmatomera 5 oo BL Signeta Sieh i aed hes PAPA ntymbophonae. ee seen. Siphonaptera XXV Siphunculina ; 435-6 breviseta Se Pas 43 G SLUMS eye Malek niece ee RA Solenobaris we oO CRYPTORHYNC HOIDES 50 a edentata Lise erent VOLO, Spaniopsis Dav Seating PON XOX Spermothamnion .. 460 Sphagnum xlix, 194- 5 Spirogyra .. .. ba Che Spongoclonium "460-2 , 469 angustatum Pais 463, 467 brachygonum aa sor 46 brounianum .. 463-6 conspicuum ae 460-3 ? crispulum . 463, 469 dasyurum . 463, 466 ?? debile . 463, 469 fasciculatum 461, 463-6 formosum ee iictotl | Lone ol INTO, 55 soo oo oo CGS latissimum . 463, 467 paradoxum . 463, 466 pastorale Nt Ue caus TER EL OL plumigerum .. ee iO scoparium i 461, 463, 468 scopula . 463, 468 violaceum .. 463, 468 wilsonianum 461, 463, 465-6 wollastonianum 463, 465-6 Stackhousia monogyna .. 199 pulvinaris ; 416-7 Steganopsis . 399, 400 melanogaster ae, ret OO Stegomyia aegypti .. xv, xix Stellaria flaccida .. .. 195 pungens 195, 197-8, 203 Stenopogon Be aE E ha Ms ithe tc) Stereoborus EEE Ped eRe BONG Stenmingomiyayeene ea OO: Stibadocera Ser ee eee MG! metallica Ste nays ROL Stibadocerella... 9.5 =. 61 XCiv. Stibadocerodes!.. 2. =. 61 australiensis acer aes (GEL tasmaniensis BR ok Be FOL: Stigmodera balteata 5 LAAT bonvouloiri .. .. .. 225 elancula Bion ai Gata) Gath ead) COMUNE, so bo Go. ao. AAAS DEUQUETI 225-6 DILATATA Naame ie 226-7 dimidiata Reet NPE High OPN) DUCALIS Swine 223-4 flavo-picta ie eS PLAVO-VIRIDIS A EE ONT: FOSSORIA eae 226-7 horni Bil tthe eed ete oO kershawi Be ay LeU O MIRANDA rege: 224-5 Manila «2 Wes eeec26 oleata SO evel, ns, meee princeps Berets tre Nba ran) recta et Oe eee oth Tectipenmis; =. 2. 2.) 225 Sexplaciataye ey yeaa 2o SPENCE ie) sn ee ICANT ss | cask (Aten geEeeaO GTHCOLOTiapsiek eae Dee eee 2 UIPIRONNIB, 66 ou oe Be unimaculata so. oo PKS Wilko oo oc 228 Stilbomyia 342, 344. 5 GOStANISH ae Lent on hea oa: opulenta mle Rees sept A hy Stilpnogaster . 387, 391 Stomatorhinia 5 A), Bax australis ayey ese 333 cribellata Seen en See a4: GISCOlOTA ee ee 4 hunaitas Sse a RE R39 VATE) Cee 333 PALLIDA " 339- 4 subapicalis 332-4 xanthogaster so oo Bet Stomoxys calcitrans ae EXON SRO HII So 6g aq. Jhhy Stylidium graminifolium 194-5, 197-9 lineare : 204-6, 209 Styphelia longifolia .. 495 SIRAMIMEONMIBAB, 55 wa of BIR terrae-reginae Pa Beye OO Swainsonia coronillifolia 379 Maemopteris; 22. weeeeewl0s8 Tanyderus vel Met eos pictus cel, Pei die verse ay any PLemnld pic p ie.) eens Tanyptera siawen,. somneese eon: fumipennis .. .. 57 Tapeigaster BRUNNEIFR ONS 16 TVATACULOCELAN 2 aes mee dens-leonis 194-5, 197-8, 217 Tasiocera.§.. 3. oe CARL Taraxacum INDEX. Telesto caecilius 66. ie AG Telicota Ben ead Rails nian OS) Telopea Se | cothe enamine a: COLI T speciosissima Biter ses) JL Temnocephala Lecter ete MLV Tetratheca thymifolia .. 379 Teucholabis 54-5, 63 Thamnocarpus .. . 460 Thaumastoptera Nar OO Galiceatas.) 0 a0 Re eS Themognatha bonvouloiri 225 DUCALIS 223-4 MIRANDA ‘ 224-5 princeps nee see. CAS) rectipennis .. .. .. 225 Thereutria 395-6 amaricus oe eee Lee OWO luctuosa BO eno eh Sola, GOO DWI, oo ao co oo aXe UKM 646 oo oo BOO Thinnfeldia Hy or POS Thrypticomyia 64, 67 doddi see Ste AY OT Thylacodes decussatus xlvi Thylacoleo carnifex xlvi Thyridula go o6 2a, 440) atroapicata .. .. .. 441 BRUNNEIFRONS ee 441-2 centralis 441-2 TUL OS Ai ei vets maw a ee 4:4) ‘Tiliqua scincoides xliii, dhhy, 2H, Wes, ~ axDil, 499, 500, 520, 524-5, 537, 542, 546, oe 550, 553 Timareta ns : 55 OI) (RInemylay .. Mee see uD 0) Tipula 57-9 omissinervis Seis Uuentateecas) Tipulodina oon ee BRS Todea lai) Se G2 HO, barbara .. ae 181-2 SraSCTIv aie) Nee ee eels ANNINEAUIS bo. oo oa «oo adil Tonnoiromyia tasmani- CNISIS! ice eth eLOS: Toxidia 275-6 crypsigramma Hey erh Bash PANEL malindeva .. .. .. 277 DELON AIG os Bese tere onKt Sexcouttata .500 See ea eenee Toxorhina 63, 69 magna 68-9 Tracheomyia macropi .. xxv Trachysaurus rugosus 499, 500 TPAD EZULESirie ace aR CHILD eliena ee ofaeeeee2i6 eliena eliena ome a Ae eliena monocycla 50 PAG jacchoides an, BAe eINO ACCHUS. 5 ..k ec eee ecu DPoizalioides! ..) ee. eee eo Trentepohlia A OR-O Trichocera cee MATS AO annulata Pie ree oes A Trichodolichopeza .. .. 59 AVENOMOINOMIS 55 oo ao Hal Trichoneura 4 55, 62 Vul Saris. - 0) ee eee) Trichopsidea) —2e) ea aseeocH Tricimba >. 435,442 carinata.. . 442, 444 CARINIFACIES .. 443-4 CONVEXA .. : 443-4 POLLINOSA Bt Po oc, 414183 scutellata 443-4 SIMILATA 8 443-4 Tricyphona 47, 49, 50 brevifurcata .. .. 49 constans 5.5) 1) Se me () formosana’ 5. eee gmundensis .. .. .. 50 INCOMES o5 cs so BY littoralis oo DERE EEG novae-zelandiae .. .. 46 OOO, 65 560 co oo BO opaca el ree 0 protea te CHO, 4) rainieria oS Schineriaa = ts) eee 0) tipulinay a). 250 ee ee) Trigonometopsis 400, 412 binotata : 5 aula Trigonometopus . 400, 402 fuscifrons .. 402 ‘Pramicra: \.3 > 4 e= eee 0 Triogma-: . 30. eee Ol! EXCUlD ENA An ee ene ee OL kuwanai Pant tics weal: (0) trisulcata Sa Sas Wee Oe Troides priamus i pro- nomus é xlvii Trypaneoides .. .. 400,418 Typha angustifolia oo BS Udotea argentea .. .. 556 orientalis sol EO OO Ula en a Ri EDO Ulex Europaeus’ : OS eee bg Unionella ae, 111 Uromyces F : xl vii Urosthenes australis oo oNlhy Utricularia dichotoma var. uniflora . 199, 212 Valonia confervoides .. 556 IMOVANSSL 65660 06 oa DDD Vaucheria geminata PAS x Velleia ice MEARIZ Velleya montana . 198, 212 paradoxa 197-8 Vermetus decussatus . xlvi Veronica Derwentia ; 192, 194, 198, 200 Verreuxia .. .. : . 472 Viola betonicifolia .. 195, 198, 217, 379 Wahlenbergia gracilis .. 195, 197-8,379 Warnenias 25.5 .. ' 4. 460 Weinmannia .. .. .. 120 Xenocalliphora 50 00 Baht? INDEX. XENOHOMONEURA ..._... 419 TESTACEA Syst? ehscn | te 4a Xenolimnobia 54-6, 62 camerounensis .. 55-6 Xenopsylla cheopis xxv, xxvi Xenotipula ay ie te COD XCV. Xerotes longifolia .. 197-8 Xipholimnobia 54-5, 62 terebrina cae UN es eel tT) Xylotrupes Lt, Coa ADD VAN ENNACOMONIEY 55 60 oo BO Zelandotipula .. .. =. 58 NOTES ON AUSTRALIAN DIPTERA. No. x. By J. R. MALLOocH. (Communicated by Dr. HE. W. Ferguson.) (Twelve Text-figures. ) [Read 30th March; 1927.] In this paper I present a revised synoptic key to the species of the genus Drosophila Fallén, with descriptions of some new species, a synopsis of the species of the genus Homoneura van der Wulp, descriptions and records of some species of the genus Sapromyza Fallén, and descriptions of some other acalyptrate Diptera, most of which have been received from Dr. H. W. Ferguson. Family Drosophilidae. Genus MycoprosopHILa Oldenberg. This genus is distinguished from Drosophila by the extremely short anterior pair of postsutural dorsocentral bristles, which, like the basal pair of scutellar bristles, are almost indistinguishable and by the humped up thoracic dorsum. All the known species are very similar in colour, glossy black on dorsum, with yellow abdominal markings and pale yellow on venter and sides of thorax. The lies occur commonly on the undersides of fungi in which the larvae feed. I have before me a series of specimens belonging to a species which is evidently undescribed and one injured specimen which may possibly belong to another species. MYCODROSOPHILA ARGENTIFRONS 0. SD. Male and female—Head black, yellow on centre of frons from ocelli to anterior margin and on lower half of occiput, the face brownish, bases of antennae yellowish; orbits shining, rest of frons dull, when seen from in front densely silvery; proboscis yellow below, fuscous above; palpi fuscous. Thorax glossy black on dorsum, with a variable amount of yellow on anterior margin, sometimes in the form of two rudimentary vittae; scutellum when seen from in front brownish or yellowish dusted apically; pleura pale yellow, black on upper margin; post- notum black. Abdomen pale yellow, with a black fascia across hind margin of each tergite which is carried forward on the median line on tergites 3 to 5 and connects with a similar fascia on anterior margin leaving two yellow spots on each, the lateral margins of tergites wholly black. Legs pale yellow. Wings hyaline, with a deep black mark on costa before apex of first vein and a faint cloud extending from it over cell to second vein. Halteres black. Head a little broader than thorax; frons at vertex nearly twice as wide as length at centre; all bristles, except the anterior reclinate one on each orbit, long; eyes almost bare; facial carina widened and flattened below; clypeus convex. Thorax quite conspicuously convex, the dorsal surface rather densely fine haired. Third costal division over half as long as second. Length, 2-3 mm. Type male, allotype, and 5 paratypes, Coramba, N.S.W., 15.2.25. A 2 NOTES ON AUSTRALIAN DIPTERA, X. Genus LEUCOPHENGA Mik. LEUCOPHENGA MINUTA DN. SP. Male.—Head testaceous, occiput and face, except sides, infuscated, frons slightly darkened above, but all these parts with dense white dusting so that in some positions they appear pale; palpi and antennae testaceous; cephalic bristles, except on vibrissal angles, yellow. Thorax testaceous yellow, densely white dusted, almost silvery when seen from certain angles, with evidences of a rufous vitta along each side of dorsum; a brownish vitta along centre of pleura; scutellum testaceous yellow; postnotum brown. Abdomen brownish, when seen from in front with quite dense silvery dusting on dorsum. Thoracic and abdominal hairs and bristles luteous. Legs testaceous yellow. Wings hyaline, a narrow fuscous cloud extending from apex of posterior basal cell obliquely to apex of first vein. Halteres missing in type. Frons about twice as long as wide, parallel-sided, all bristles well developed; face slightly carinate on upper half; antennae normal; cheek linear; vibrissae short; palpi slender. Both sternopleurals long. Legs slender, no outstanding setulae on mid tibiae. First posterior cell of wing not narrowed apically; third costal section over half as long as second. Length, 2 mm. Type, Cairns District, Queensland (Dodd). Distinguished from other Australian species known to me by the uniformly silvery white dusted dorsum, markings of the wings, and its small size. Genus DrosopHiLa Fallén. As I have described a number of species of this genus since I published my key in the first paper of this series (These PROCEEDINGS, 1923, p. 615) I deem it expedient to present now an enlarged synopsis which includes 22 species, all at present known to me as occurring in Australia. I have found it necessary to draw up this key for my own convenience in identifying material and hope that it may prove as useful to other students of the group as it has to me for that purpose. There must be many Australian species of the genus unknown to me. Most of those herein included are similar to the general run of species of the genus throughout its range, but some, and especially nicholsoni, are aberrant, though not entitled, in my opinion, to subgeneric segregation. I have not attempted to figure the genitalia of either sex, some of which possess striking specific features, nor have I attempted to determine the structure of the eggs of the species. Some of the eggs are furnished with filaments at one end which vary in form and in number with the species and they may sometimes be as readily distinguished as any of the other stages, and in some closely allied species even more readily than the adults. Key to the Species. 1. Wings with conspicuous fuscous markings in addition to those over the cross veins OLiatlapex OL Ursticostale divAsion! Ara ame acke eee i Ore lstorede oe iene rere ae 2 Wings without fuscous markings except sometimes faint clouds over the cross veins or at apex Of, MITSE) COSLALIGIVISION ec eteriellieckdiceie ot ek teiee nei ncnen mer tet 3 2. Wing with a large brownish or fuscous spot at apex of second vein, the dark cloud at tip consisting of a brownish suffusion along the apices of third and fourth veins, more or less coalescent in first posterior cell; mesonotum dark brown, with three linear yellow vittae, the median one not reaching anterior margin; scutellum yellow in centre, dark brown on sides of disc; pleura whitish-yellow, contrasting sharply with the dark brown mesonotum .... mycctophaga Malloch. 10. It, 12. 13. 14. BY J. R. MALLOCH. 3 Wing without a dark spot at apex of second vein, the dark cloud at tip consisting of a broad curved brown patch which extends from middle of third section of costa to just over third vein and over disc of wing to beyond fourth vein, but leaves a hyaline spot in apex of first posterior cell; mesonotum brown, with two poorly defined paler vittae which are carried over lateral margins of scutellum, the centre of latter brown; pleura not noticeably paler than mesonotum .........,. SHccage Sorey sab anatis gohehan oiataretrinetotauen tebe wobacdnDoDoaDDODODCODDDCODOCS. MOOT MEW er Fore femora with a comb-like series of microscopic setulae on apical third or more offanteroventral surftacevepacvne theo oot accel sverelse no etalalevelguahateneuelauatevecstetcnelic s, « 4 Fore femora without a comb-like series of microscopic setulae as above .......... 5 Fore femora with short closely placed setulae on more than the apical half of posteroventral surfaces, the longest one, at apex, not longer than the femoral diameter; third section of costa not less than one-third as long as second; facial CATIMA MTN ALT OW wv cere encusuet er eet Onste eh eh ove ias rede nchatie: suse cyai teen einstabe: wistelstie setifemur Malloch. Fore femora with four or five widely spaced bristles on the entire length of each posteroventral surface, the longest one, at middle, as long as or longer than the femoral diameter; third section of costa about one-fourth as long as second; facial carina much broadened below .................. immigrans Sturtevant. Thoracic dorsum with a minute but conspicuous dark brown or fuscous dot at base of each hair and bristle and sometimes with additional brown or fuscous dots on parts causing aggregations which assume the appearance of larger irregular spots, the ground colour of thoracic dorsum never testaceous yellow ....... 6 Thoracic dorsum with or without dark or pale vittae, not copiously marked with piliferous spots or dots, if faintly marked with piliferous dots then the ground colounsofethoraxsismtestaccousmyellowarrsen orc ook Eine eileen 9 Third costal division of wing almost as long as second; outer cross vein about one- third as long as apical section of fifth vein ............ poecilothorax Malloch. Third costal section of wing not over one-third as long as second; outer cross vein much more than one-third as long as apical section of fifth vein ............ a Facial carina practically absent except between bases of antennae, where it is sharp andwlineanr- eyes valmostibarces fair sole eyes ie, cus sievelleeteusii=, 16) 6 eueiisi eels obsoleta Malloch. Facial carina conspicuous below, where it is rather broad and usually longitudinally suleate; eyes with dense stiff microscopic hairs ....................20200- 8 At least the first three tergites of abdomen with a yellowish spot on each side on the part that is) incurved on) iventer ...5..5.25..0855.-2000e0- -repleta Wollaston. None of the abdominal tergites with yellowish ROS as above .... hydei Sturtevant. All hairs and bristles on insect luteous; thorax not vittate ...... flavohirta Malloch. AMllgnairseandebristleseruscoussonmplackishwmeerirre crane recieicr el eicieneieieerene cian 10 Sides of face, frontal orbits, and two narrow submedian vittae on mesonotum which extend over its entire length and on to sides of scutellum, densely white dusted, the whole forming two continuous white lines on a black ground, and very cConspicuousrsternopleuralsie2ieenr eect oleeioiene clones eicieieien. albostriata Malloch. Thoracic dorsum with or without dark vittae, not white vittate .............. 11 WNaoreee Clorrsibon GlisinbeMhy AAI sooccoccupbaoonodUndLonb OUD OUdOKOL SHO HOU OL 12 MHOLaAcCiCndorsummentirelys witholtenvittalemerri etnies bara iaieieieraie aici reir ee cioione 16 Thoracic dorsum with five dark vittae, the intervening spaces pale grey dusted; wing with a deep black spot and two fine bristles on’ costa before apex of first vein; third costal section almost as long as second ............ nigrovittata Malloch. Thoracic dorsum with four or six dark vittae, the intervening spaces inconspicuously MAleerdusted ert pas Ge «Al epee a Reet UAE toys cherokee ORE SD. ceie tere rk et 13 Arista with but one long hair above at base, no long hairs below; face without a carina on lower portion; third costal section not over one-fourth as long as second, and shorter than penultimate section of fourth vein; sternopleurals 3 NM eeu rare ey crea ey encvapeorscaliey sti eic iattome tan en sie Wetemcnten sisia’ «itettetianer olsen vatabee «sees MIChOlSON?, Nn. Sp. Semeh nici eu AKioieh aaices 14 Palpi fuscous; face with a vestigial carina only on: upper part, not carinate below; pleura with two dark vittae; third costal division over one-third as long as second and distinctly longer than penultimate section of fourth vein; sterno- LSU SHA eereaeswencce ct caetistyetot ose uo siascivsl ea oa eR Reerc ia ol Me meitone | anie vous) GUase Meta s buscki Coquillett. Palpi testaceous yellow; face with a very conspicuous carina which is continued below middle, its lower portion broadened ..............00c ce cccccsccrccers 15 4 NOTES ON AUSTRALIAN DIPTERA, X. 15. Submedian thoracic vittae narrowed at posterior extremities, but continued to the hind margin of mesonotum, no dark central mark in front of scutellum; the two central series of hairs located on the inner margins of the submedian dark 550 Valter ee A er UR Seat yey eR cy en One ois eSU en OST tes ence te ees EAE lativittata Malloch. Submedian vittae not reaching posterior margin of mesonotum; a dark mark on centre of hind margin of latter; the two central series of hairs entirely within the pale central vitta, the next two series on edges of the dark submedian WIC! | Val soh patie seicvenp weeps Sa tensute vena aistie vay ohana ahve) ikat su alccuraiha Wonte Devtentene beret a ewe nai csi re Wat be enigma nN. Sp. 16. Facial carina not developed except weakly on upper part between bases of Fey oli s$ ob 02 (2 yu Meee Bree Pa aE Croce carr, UREN EG hy tot Ho APR Cn OeNe Se PP CREATEN.S tote tastes er CRA atetins 1! GG. aT Facial carina well developed and broadened on lower part of face .............. 18 Teepe BY ony feb. cao WON 5 eb ISLerO Dy Reigtols: aeoe tie MCIORIO cuclOke Gi O-G ON IS Gee ORs crcl wala Gidc Juscithorax Malloch. Thorax testaceous yellow, sometimes with faint dark dots at bases of the bristles andehairs: ‘On: (GOnSUMe oc ls ereie. scsncieshe lente rsner cue ae velscs hers sosuenauads inornata Malloch. 18: Thorax morejor less shining pla chy kore crckeuescueneney veka sicaielci aed ciel estonia tiscali ane Noten 19 Thoraxyshinine testaceousyellows wieicacccuimenercietey acess aiareteas ds IONS Rance maleate 21 19. Third costal section distinctly more than half as long as second and longer than penultimate section of fourth vein (3:2); frons reddish or yellowish brown except on orbits and triangle, which are shining black, the anterior reclinate orbital bristle laterad of the proclinate one ................. sydneyensis, n. sp. Third costal section about one-third as long as second and about as long as, or very little longer than, penultimate section of fourth vein ...................... 20 20. Frons dark brown, the orbits and triangle dull black; anterior reclinate orbital bristle well above the proclinate one; thorax shining, but not glossy .......... MPEP Ie aria citi, LI SCO pee ce hence era NR LORU MUS ctrciie Tie neaiotenn ter stiey suis pie ee eicireweitopier eran ee ae sare subnitida n. sp. Frons black, the orbits and triangle shining, anterior reclinate orbital bristle but little above level of the proclinate one; thorax glossy ...... nitidithorax, n. sp. 21. Fore metatarsus of male with a comb of short black bristles on apical half, the second. Ssesment without a "combyeeiiiy is = jens sale ee) clens oncie = ampelophila Loew. Fore metatarsus and second segment each with a comb of black bristles from base fYa) Dione tha WMI GooaecuccoosuogausucUdangd oan RoODOOSoOKaobOOUS serrata, nN. Sp. [Drosophila brunneipennis Malloch described in These PROCEEDINGS, 1923, p. 617, has inadvertently been omitted. In the previous key loc. cit. p. 616 it is placed next to D. melanogaster Meigen = D. ampelophila Loew.-—Ed.] DROSOPHILA NICHOLSONI, Nn. sp. Male and female.—Testaceous yellow, shining. Frons opaque brownish, the orbits, sides of triangle, and anterior margin testaceous, not shining; third antennal segment largely fuscous; palpi and proboscis testaceous. Dorsum of thorax slightly brownish and greyish dusted with six brown vittae, the submedian pair of moderate width and complete, the intermediate pair much narrower and connected with the submedian pair behind suture, the sublateral pair broad, rather indistinct and broken at suture; pleura and metanotum largely brown; scutellum brown in centre, narrowly yellow on sides. Abdomen shining, apical tergites slightly darkened. Legs testaceous yellow. Wings greyish hyaline, veins not clouded. MHalteres yellow. Anterior reclinate bristle about one-third as long as posterior one and almost in transverse line with the proclinate one; postvertical bristles long interfrontalia with a few hairs anteriorly; facial carina distinguishable only on upper part; arista with one long hair on upper side at base and some short pubescence beyond, which is only visible under a high magnification; vibrissa single. Thorax with two humerals, about eight series of intradorsocentral setulae, the submedian two series on margins of the pale central vitta, and 3 sternopleurals. Legs normal. Second section of costa about four times as long as third, the latter not longer than penultimate section of fourth vein, ultimate section of fifth vein subequal to penultimate section of fourth and about twice as long as outer cross vein. Length, 2-5-3 mm. BY J. R. MALLOCH. 5 Type male, allotype, and 2 paratypes, Perth, W.A., 15.11.1924 (Nicholson). This species is readily distinguished from any other known species in the genus either from Australia or elsewhere by the presence of but one long hair on the upper side of the arista. This character was used as the distinguishing feature of the American genus Cladochaeta by Coquillett, but the present species differs from that genus in many characters and is so obviously merely an aberrant Drosophila that I retain it in this genus, while noting that it apparently weakens the claim of Cladochaeta to generic recognition. DROSOPHILA NITIDITHORAX, Nn. SD. Male.—Deep black, dorsum of thorax and of abdomen almost glossy. Face whitish dusted and, like the cheeks, partly brownish yellow; frons except the orbits and triangle velvety black; antennae black; palpi and proboscis dusky testaceous yellow. Thorax without markings, the pleura not so conspicuously shining as dorsum. Abdomen slightly yellow at base. Legs dusky testaceous yellow, femora almost entirely fuscous. Wings greyish hyaline, veins unclouded. Halteres brownish yellow. Frontal bristles strong, anterior reclinate orbital half as long as posterior one and slightly but distinctly above level of the proclinate one; interfrontalia with quite dense short black setulose hairs; facial carina nose-like, rounded above on the lower part; rays of arista about 4+ 2; vibrissae strong. Intradorsocentral setulae in 8-10 series; sternopleurals 3. Legs normal. Third costal section not longer than penultimate section of fourth vein and about one-third as long as second section; outer cross vein at about 1:5 its own length from apex of fifth vein. Length, 2-5 mm. Type and paratype, Perth, W.A., 15.11.1924 (Nicholson). A robust black species which is most closely related to subnitida deseeipea below. DROSOPHILA SUBNITIDA, Nl. SD. Female.—Distinguished from the preceding species by the brown colour of the frons, the opaque frontal orbits and less shining dorsum of thorax. There are no outstanding structural distinctions, but the anterior reclinate bristle is larger and farther from the proclinate one, the third section of costa is a little longer and the insect is less robust. Length, 2 mm. Type, Sydney, N.S.W., 6.1.25. This species has somewhat the appearance of fuscithorax Malloch, but the latter has no carina on lower part of face and differs in other respects. DROSOPHILA SYDNEYENSIS, Nn. Sp. Female.—Black, dorsum of thorax and abdomen almost glossy. Frons brownish red, orbits and triangle shining black; face yellowish on sides, slightly white dusted; cheeks yellowish; antennae yellowish or rufous, third segment fuscous; palpi and proboscis yellowish. Thorax as in nitidithorax, but the pleura as conspicuously shining as mesonotum. Abdomen with bases of basal two or three tergites yellowish. Legs as in nitidithoraz. Wings hyaline. Halteres yellow Frons with a few hairs in front; anterior reclinate orbital bristle short, in transverse line with proclinate one; facial carina well developed and nose-like. 6 NOTES ON AUSTRALIAN DIPTERA, X. Thorax as in subnitida. Legs normal. Wing venation differing-from that of nitidithorax and subnitida in having the third costal division well over half as long as second, usually about, or even full, three-fourths as long as it, and twice as long as penultimate section of fourth vein, the latter subequal to ultimate section of fifth, and about twice as long as outer cross vein. Length, 2 mm. Type and three paratypes, Sydney, N.S.W., 3 and 5.1.1925, and 2.4.1925. A less robust species than nitidithoraz. DROSOPHILA ENIGMA, 0. SD. ; Male and female.—Very similar to lativittata Malloch in colour and general structure. Differs from it in being paler, the ground colour being testaceous yellow, the dorsum of thorax greyish dusted, and with paler vittae which are narrower, the submedian pair separated by a wider space which covers four instead of two series of the short hairs, and the other characters of the markings as stated in the key. The abdominal markings consist of a dark brown fascia on hind margin of each tergite which is narrowed or interrupted in centre, widened each side of median line and again at the lateral curvature, the fasciae rather indistinct on the lateral incurved portions of the tergites. As in lativittata the outer cross vein is faintly clouded and the penultimate section of fourth vein is about half as long as ultimate. Length, 3 mm. Type male and allotype, Sydney, N.S.W., 22.7.23, and 23.9.24. Paratypes, two females, Toronto, N.S.W. DROSOPHILA SERRATA, Nn. Sp. (Text-figure 1.) Male.—Shining fulvous yellow, very similar to ampelophila Loew which it closely resembles in many respects. The type specimen is rather immature, but the thorax is not vittate and the abdomen has a faint dark uninterrupted apical fascia on each tergite. The legs are yellow and the wings yellowish hyaline with unclouded veins. Halteres yellow. Bristles and hairs fuscous. Anterior reclinate orbital bristle about one-third as long as posterior one and distinctly above the level of proclinate one; eyes quite densely stiff-haired; face distinctly carinate. Thorax with six series of intradorsocentral hairs; prescutellar acrostichals not differentiated; both humerals strong; only two sternopleurals well developed. Two basal segments of fore tarsus with a comb-like series of short stiff Text-fig. 1. Drosophila serrata, two basal segments of fore tarsi of male from in front. black bristles on anterior side, the comb on basal segment bipartite (Fig. 1). Third section of costa about half as long as second and a little less than twice as long as . penultimate section of fourth vein, the latter about one-third as long as ultimate section and subequal to ultimate section of fifth vein; outer cross vein at about twice its own length from apex of fifth vein. Length, 1:75 mm. Type, Eidsvold, Queensland, 2.4.24 (Bancroft). BY J. R. MALLOCH. 7 There are several described species of the genus with the two basal segments of fore tarsi armed with comb-like bristles, but none of these have the armature as in this species so far as I am aware. I described one, biarmipes, from India, but in it the combs are confined to the apical parts of each segment and do not extend along the whole length of the anterior surfaces as here. Genus GiTonipES Knab. The species described below falls most readily into Gitonides, but it differs from the genotype in having the frons much narrower anteriorly and the first posterior cell of the wing quite noticeably narrowed apically. GITONIDES CONVERGENS, 0. Sp. Head brownish testaceous; upper half of occiput fuscous, lower half white dusted; upper extremities of frontal orbits, ocellar spot and clypeus, fuscous; face slightly white dusted; palpi brownish, paler at apices. Thorax brownish testaceous, dorsum when seen from in front with a broad brownish centrai vitta which is faint in front of the suture, where it is sometimes divided centrally and which is divided between suture and hind margin, a broad branch curving to each side and between the two pairs of dorsocentrals, and a narrower central one continuing to hind margin, the disc laterad of the anterior and posterior portions of vitta white dusted, between these pale markings and lateral margins there is a broad brownish vitta; humeral angles testaceous; scutellum when seen from in front with a brown central line which broadens out and covers apex, a fainter brown mark on each basal angle and a less distinct dark mark on disc each side of the dark central line, the latter surrounded by whitish dusting. Abdomen testaceous, all tergites except the basal two largely or entirely black. Legs testaceous, femora browned, tibiae dark at apices, the mid pair most conspicuously so. Wings hyaline. Halteres yellow. Frons at vertex about one-third of the head width, much narrowed anteriorly, at front margin not half as wide as long in centre; proclinate orbital bristle well above middle of frons, the anterior reclinate bristle quite small and about midway between the others; arista bare; face slightly carinate; antennae normal, inserted at middle of profile. Thorax with two pairs of postsutural dorsocentrals, the anterior pair short, about eight series of intradorsocentral setulae, one humeral and two sternopleurals; scutellum convex. Abdomen broad and short. Legs stout, normal. Inner cross vein at two-fifths from apex of discal cell; outer cross vein at less than its own length from apex of fifth vein; ultimate section of fourth vein over three times as long as penultimate section; first posterior cell quite noticeably narrowed apically. Length, 3 mm. Type, Hidsvold, Queensland, 1924 (Bancroft). Family Agromyzidae. Subfamily MILIcHIINAE. DESMOMETOPA VARIPALPIS, 0. Sp. Female.—Head black, whitish-grey dusted, with the usual opaque black M-shaped frontal marking; cheeks yellowish below; palpi testaceous, with conspicuous irregular black spotting. Thorax black, slightly shining, evenly greyish dusted and without vittae. Abdomen greasy in type, black, and probably less dusted than thorax. Legs black, tarsi yellowish, darker at apices. Wings hyaline. Knobs of halteres yellow. 8 NOTES ON AUSTRALIAN DIPTERA, X. Each orbit with the two upper bristles directed outward over eyes, the two anterior bristles incurved; arista hair-like, almost bare; palpi large, a little longer than head, lanceolate, broader than cheek, their apices rather pointed, bristles short. Thorax with two pairs of postsutural dorsocentral bristles. Legs normal. Wings as in m-atrum Malloch. Length, 2-5 mm. Type, Bourke, N.S.W., 6.5.26. I know no species of this genus which kas the palpi coloured and shaped as has this one, these organs being in all others unicolorous or yellow with dark apices. Family Piophilidae. PIOPHILA CONTECTA Walker. This species I previously listed as latipes Meigen. (These ProckEpines, 1925, p. 316). Dr. O. Duda considers that contecta Walker is a distinct species, having two humeral bristles instead of only one, and the second segment of the fore tarsus about 1:5 as long as wide, not about as wide as long. Besides the specimen already recorded by me I have seen another female specimen from Wahroonga, Sydney, N.S.W., 26.1.26. I have before me what appears to be an undescribed genus of this family but have only one female specimen so defer describing it meantime. Family Sapromyzidae. Genus SaproMyza Fallén. In presenting my synopsis of the species of this genus (These PROCEEDINGS, 1926, p. 33) I stated that undoubtedly there were many species still unknown to me and as evidence of this furnish descriptions of several that have been received since I completed the key. Under the description of each of these I have included notes which will serve to associate them with their most closely related forms in the key, but unfortunately there must yet be many undescribed species which can only be distinguished from those dealt with to date by a careful comparison with the complete descriptions or with the type-specimens. I erect one new subgenus in the present paper for the reception of a very striking species from Sydney, but the others I retain in Sapromyza sens. str., though several of them are rather aberrant from the genotype. It will be necessary to publish a full key to the species later, but whether this duty may fall to me or another worker time will decide. Subgenus HENDELOMYZA, n. subg. Characters: Face concave in profile; basal segment of antenna as long as, or longer than, second, with some fine hairs below apically; sternopleura with but one bristle; thorax without presutural dorsoventrals. In other respects similar to Sapromyza. SAPROMYZA (HENDELOMYZA) TENUICORNIS, n. sp. (Text-fig. 2.) Female.—Head fulvous yellow, shining; ocellar spot fuscous, a fuscous line along inner margin of each orbital stripe which curves round anterior margin of latter and becomes wider there, almost connecting with the black spot between each antennal base and eye; some white dusting on sides and upper margin of frons; lower central part of face fuscous; parafacials white-dusted below the black BY J. R. MALLOCH. 9 spot; third antennal segment brown, darker apically; arista black, yellowish at base; proboscis and palpi black. Thorax shining fulvous yellow, with two sub- median vittae and one near each lateral margin white-dusted; pleura entirely white-dusted; scutellum paler yellow than mesonotum. Abdomen glossy black, yellowish on disc basally, where it is slightly grey-dusted. Legs yellow, apices of fore femora and tibiae infuscated. Wings honey yellow. Halteres brown. Text-fig. 2. Head of Sapromyza (Hendelomyza) tenuicornis, from side. Head in profile as in Figure 2; entire frons shining; anterior orbitals rather far from lateral margins; ocellars rather weak; arista subnude; head wider than high; proboscis stout. Thorax with but two pairs of postsutural dorsocentrals and one pair of prescutellar acrostichals; intradorsocentral setulae in four series in front of suture; scutellum convex, with four bristles; prosternum almost bare; mesopleura and sternopleura each with one bristle. Abdomen stout. Fore femur without preapical anteroventral comb; tibiae with preapical dorsal bristle. Inner cross vein almost below apex of first vein and at middle of discal cell. Length, 7-5 mm. Type, Bayview, Sydney, N.S.W., 19.12.25. A very characteristic species which might eventually be placed in a separate genus, though I prefer to consider it as a subgebus at present. It must be noted that magnicornis Malloch, with which tenwicornis has some characters in common, has two sternopleural bristles and the head quite differently shaped. This new species does not fit into any caption of my recently published key, the only other species having the antennae longer than the head being magnicornis. SAPROMYZA RIPARTA, ND. SD. Male and female—Head dull ochreous yellow; frons brownish in centre, ocellar spot fuscous; orbital stripes densely yellowish-grey dusted; a black or brown spot between each antenna and eye; antennae pale brown or yellowish, third segment and arista black; proboscis yellow; palpi black. Thorax subopaque ochreous yellow, rather densely greyish dusted, with two conspicuous brown submedian vittae which become wider behind, and traces of two sublateral vittae of the same colour behind suture; mesopleura and anterior part of propleura fuscous; scutellum brownish yellow, paler at anterior lateral angles and between apical bristles, and with two black apical spots. Abdomen ochreous, shining, with central part of each tergite darker and the apices paler. Legs testaceous yellow, apices of all femora, tibiae and tarsi, and bases of all tibiae, black. Wings yellowish hyaline. Halteres yellow. 10 NOTES ON AUSTRALIAN DIPTERA, X. Head almost normal in form, the face slightly receding below; orbital stripes receding from eyes anteriorly; frontal bristles all distinct; third antennal segment about 1:5 as long as wide; arista very short pubescent; proboscis stout. Thorax with three pairs of postsutural dorsocentrals, the anterior pair short and well behind suture; mesopleura with one bristle; sternopleura with two bristles rather close together; prosternum with a few very short hairs. Fore femur without anteroventral comb; mid tibia with two long apical ventral bristles; all tibiae with preapical dorsal bristle. Inner cross vein below apex of first vein and at middle of discal cell. ‘Length, 7-7-5 mm. Type male, allotype, and one paratype, Clyda R., Nov., 1925 (H. J. Carter). This species will run to caption 11 in my key to the species of the genus, but it is distinguished from magnifica Malloch by the unspotted wings and grey orbital vittae and from all the others falling under caption 10 by the entirely opaque frons. SAPROMYZA BREVICORNIS. 1. SD. Male and female.—Head black; frons velvety, the triangle and orbital stripes glossy; parafacials and sometimes the sides ef face yellowish, the former white dusted; cheeks yellow below, black above; antennae fuscous, yellowish at bases, arista black; palpi and proboscis black. Thorax shining fulvous yellow, some- times darkened a little on disc of mesonotum. Abdomen glossy black, yellow at base. Legs black, coxae, trochanters, bases of femora, of tibiae and of tarsi of mid and hind legs, yellow. Wings brownish hyaline. Halteres yellow. Head of normal form, the face centrally vertically convex; frontal bristles normal, the anterior orbital distant from eye; antennae short, third segment not much longer than wide; arista with very short pubescence. Thorax with three pairs of postsutural dorsocentrals, the anterior short pair well behind suture; scutellum convex; mesopleura with one bristle; sternopleura with two; prosternum with a few hairs. Abdomen robust. Fore femur without an anteroventral comb; mid tibia with an unequal pair of apical ventral bristles; preapical dorsal bristle present on all tibiae. Wing venation as in riparia. Length, 5-6 mm. Type male, allotype, and two male and one female paratypes, Sydney, N.S.W., Sept,-Oct., 1925. This species runs to caption 10 in my key, kaving the head black, with para- facials yellow, but is readily distinguished from sciomyzina Schiner by having the frons largely velvety instead of shining, and the third antennal segment not much longer than wide, instead of twice as long as wide. SAPROMYZA URBANA, Nl. SD. Male.—Entirely testaceous yellow, shining, the frons not conspicuously shining, and with undifferentiated orbits. Wings hyaline. Halteres yellow. Anterior orbital bristle not much in front of middle of frons, shorter than the ocellars; surface of frons with microscopic black hairs; antennae short; arista broken in type so that it is not possible to determine the nature of the hairing if any. Thorax with three pairs of postsutural dorsocentrals, the anterior pair rather weak, but in this character the species is about intermediate between the two groups defined in caption 9 of my key; hairs on thorax much weaker than in unicolorata Malloch, the median two series on dorsum most conspicuous. Legs slender, the fore femur with only two or three of the posteroventral bristles on apical half well developed, the anteroventral preapical comb present but weak. BY J. R. MALLOCH. 11 Inner cross vein below apex of first vein; penultimate section of fourth vein not over half as long as ultimate section. Length, 3:75 mm. Type, Sydney, N.S.W., 8.10.25. An inconspicuously coloured species with no outstanding external structural characters. It differs from any Australian species except wnicolorata Malloch in being entirely testaceous yellow, and is a less robust species than it, with weaker hairing, and different venation. The hypopygia are distinct but I have only the type-specimens of each and do not care to dissect these, unless compelled to for lack of other material later. An error occurs in caption 22, first section, of my key. The inner cross vein is beyond, not proximad of apex of first vein in unicolorata. This feature is correctly reported in the description of the species. SAPROMYZA MARIAB, n. sp. (Text-figure 3.) Male and female.—Fulvous yellow, distinctly shining. Frons dull, the orbital stripes and triangle shining; ocellar spot black; parafacials white dusted; antennae, palpi, and proboscis, yellow, arista fuscous. Dorsum of abdomen largely black or fuscous. Legs yellow, apices of fore and hind femora and tibiae, fore tarsi from before apex of basal segment, and mid and hivd tarsi from before apex of third segment, black. Wings luteous hyaline. Halteres yellow. Frontal bristles all well developed, anterior orbital distant from eye; third antennal segment fully 1-5 as long as wide, rounded at apex; arista subnude; head Text-fig. 3. Head of Sapromyza mariae from the side. in profile as in Figure 3. Thorax with three pairs of postsutural dorsocentrals, the anterior pair short; mesopleural hairs stronger than usual, one or two of. them quite bristle-like; scutellum normal. Hypopygium stout, the forceps much shorter and stouter than in flavimana Malloch. Fore femur without preapical antero- ventral comb; mid tibia with two long apical ventral bristles; preapical dorsal bristle weak on hind tibia. Inner cross vein almost below apex of first vein and close to middle of discal cell. Length, 6-6-5 mm. Type, female, allotype, one male and one female paratype, St. Mary’s, N.S.W., 12.8.24. This species will run to flavimana Malloch in my key, but the latter has the frons entirely shining, the face flat and dull, and the fore femora more largely black, ete. 12 NOTES ON AUSTRALIAN DIPTERA, X. SAPROMYZA OCCIPITALIS Malloch. Hight specimens, Sydney, N.S.W., October and November, 1925. SAPROMYZA SCIOMYZINA Schiner. One specimen, Sydney, N.S.W., 25.10.25. SAPROMYZA BRUNNEOVITTATA Malloch. Two specimens, Sydney, N.S.W., 18.10.25. SAPROMYZA STIGMATICA Malloch. One specimen, Millgrove, V., Dec., 1925 (F. E. Wilson). SAPROMYZA MACULITHORAX Malloch. Four specimens, Sydney, N.S.W., July, August, and November, 1924-25. SAPROMYZA VARIVENTRIS Malloch. A male of this species is darker than the type female, the spot at base of antennae on the parafacials being black, and the pale parts of the legs more brownish yellow. The thoracic vittae are also broader, and the abdominal markings are less regular. Locality, Nevertire, N.S.W., 25.3.26, the same day and month as type, but a year later. Genus HoMONEURA van der Wulp. In one of my recent papers (These PROCEEDINGS, 1926, p. 551) I stated that I would present in my next paper .a synopsis of the Australian species of this genus known to me, and though I am confidednt that my material contains but a small portion of the native species I feel that I ought to provide a synopsis of those already described in the interests of students of the family. This synopsis contains only 14 species, some of them so closely allied that their separation as distinct species has been based largely upon the structure of the male hypopygia, figures of some of which I present herein. I have previously referred to the importance of the male hypopygia as distinguishing characters of the species in this family and hope that an examination of the figured examples will create an interest on the part of some Australian student that will result in a comprehensive study of the family on this basis. One of the species figured exhibits an asymmetry of the inferior forceps which is unique in my experience in this family, but it appears to be a perfectly normal specimen in other respects. Key to the species. 1. Wings with quite conspicuous brown or fuscous clouds or spots, the cross veins and the japex of second vein tallways Clouded iti. sievelsiohelclelin ai ie) +) -edetcel +) ished titel-(-1 2 Wings clear or yellowish, at most the cross veins slightly clouded, none of the LONLILUIGINAL Veins ClOUGER Atta DICES micah hickaicLolonieyaasiehel Malet p Rohe Mn Meter hels 7 2. Thorax with only two of the three strong pairs of dorsocentrals behind the suture, the other pair in front of suture; wing with conspicuous fuscous markings, the most prominent consisting of a broad oblique fascia, the outer edge of which is at apex of second vein, extending over fourth vein but not to margin of wing, and enclosing a clear spot in first posterior cell; face largely fuscous, white below; a black spot between each antenna and eye; arista plumose; dorsum of thorax and abdomen largely fuscous; legs bicoloured, testaceous and GATICE DOW Eee serayenciote ease iere toy svete entiea sls sacha wekeus ekeael oLebeuane heiedodersyedous atrogrisea Malloch. Thorax with three strong pairs of postsutural dorsocentrals, or if there are but two such ‘pairs there are no presuturals Present 6 oi. cue eee lee clele wieie a) sis elec) elelelele|islivje 3 10. 11. 12. 13. 14. 15. BY J. R. MALLOCH. 13 Frons opaque fuscous; both cross veins of wings and apex of second vein with fuscous clouds; arista short plumose .....................-. fumifrons Malloch, Frons yellow or brownish yellow; in addition to the wing spots mentioned above there are two other spots present, at or near apices of third and fourth veins ...... 4 Spots on apical part of wing at extreme apices of the veins; arista with very short MUDESCEN CEM calit spony Canney ener eee a payee Mee tire e cl ti ls aaa eae ea apicinebula Malloch. Spots on apical part of wing not all at extreme apices of veins; arista plumose... 5 Tips of palpi black; thoracic dorsum with a dark mark along inner side of humeral callosities and two narrow dark vittae along inner margin of lines of dorso- COIMETGABDIS Weve ha atatiau'e' aoute vor een ewemepe ay deoedahas \ De ee yee . Gp Ea Oe pete SS Creer aoe The relative THE ANATOMY OF CHEILANTHES VELLIA. 78 NES Oy PT NTO ee) see eet ae ere y Xo iS, SER AAA aul act Gaeed/ \\ 4 BOO er Oli: ogc ckre ler eels BO aan semeeas nape cage ore ce e@ 6) C | A RIE Se tS LS SEnOw AS Sd one JAA a N Y rrU fe Ay, \) ey © Wwe loner aw Ome oe ES Be = HD) iS) SURE a) ROan the localities known as Summer Hill and Lennoxton. Just near the latter place they are displaced by two faults, a small one throwing west and the other, the important Lennoxton fault, throwing here to the south-east. As a result of the 1Proc. Roy. Soc. N.S.W., 1926, p. 213. BY G. D. OSBORNE. 87 latter fault the outcrops of the uppermost beds of the Kuttung Series have suffered a lateral displacement of two miles and a half in a direction perpendicular to the strike of the beds. The topmost horizon of the Volcanic Stage is a green albitic rock of the nature of a pumiceous keratophyre. The upper limit of the stage has been placed here because the keratophyre is followed by conglomerates and tuffs which form the Lower Portion of the Glacial Stage. These clastic rocks possess a lithology which is quite characteristic, and differs from the lithology of the clastic rocks of the Volcanic Stage. Two sections may be taken to indicate the variety of units in the Volcanic Stage. The more important, which is found near Lennoxton, is as follows, ascending stratigraphically: Thickness in feet. Purple) tuffisiiwathy pebbles. 9-)5 2s 0 ee 4 ee) DO Toscanite (Mt. Gilmore type) .. .. .. .. 30 Cherts with plant stems a LO Pastene Gc qla Nira tna Toscanite, albitized (No. 74 5)2 4 Sul Eietne bk ch bti” sts) Daciter@Nowi43) een ee oe 5, Yaa) Rake ep do. ACTA Cutis a GINO san 2) mee cere en Une uae an Ba () Felspathic tuffs Ss ce teeth, saat Ween) wmosee LOO Potash rhyolite (No. 741) RON UD ARE DN ec RS 34 yes) BrecciavViGNoniea nme) Wavy eee eel Ato ge Eh LAE E25) Felsite (No. 739) .. . Ean SAMI: aes mates O Green kKeratophyre (No. 746) Bie OM ket aatar poses dite O Total ase Sere ene 9.0 The second section is found at Summer Hill on the right bank of the Paterson River near the boundary between the Cessnock and Bolwarra Shires and ascending stratigraphically, is as follows: Thickness in feet. Bluish¥cure L@No: COG) iinet nie es ecte! esta oO Coarse banded green tuff (No. 707) .. .. .. 20 Tuffaceous conglomerate (No. 708) .. .. .. 10 Breccia ius ocd ies het isan h cr oe olenrc ane ci Mauve dacite (No. 713). Be Bone IO Banded green Keratophyre (No. 709) he apuaten a 1 e0) MOC Tie 2. eee eee 20D Some horizons are common to both localities and these can be traced fairly easily through the intervening country. The rocks described in the sections just given comprise a series quite compar- able with the Volcanic Stage sections to be found further east. There is not a great variety of type, but it should be remembered that in the present case only part of the Volcanic Stage is dealt with. Of the lavas already detailed, only four can be correlated directly with units from the districts to the east. These are those numbered respectively 745, 746, 739 and 741. The particular features of the more important of the horizons in the Volcanic Stage will be considered under the heading of Petrography. 1 Numbers refer to specimens in the collection of the Dept. of Geology, University of Sydney. 88 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. Glacial Stage. The Lower Portion. On the eastern and northern sides of the area, this division of the Glacial Stage (equivalent of the Mt. Johnstone Beds of Sussmilch), consists entirely of clastic rocks, tuffs predominating. The majority of the tuffs are contaminated with detrital sediment, becoming in places very pebbly. Conglomerates and sand- stones are associated with the tuffs, but so far no definitely glacial rocks hav2 been found, although in this portion of the Glacial Stage to the east, one horizon of varve-rock has been recorded, viz. from Glenoak, at a position about 200 feet above the base of the Glacial Stage. On the south-western margin of the area now being described, however, there are important glacial and fluvio-glacial deposits. Thus to the north of Hudson’s Peak and Drinan’s Mt., Browne has shown that the Volcanic Stage is followed by the grey-granite conglomerate and then a series comprising acid tuffs, varve-rock and tillitic conglomerate, culminating in a coarse conglomerate consisting of a tuffaceous matrix and many pinx aplite pebbles. This conglomerate is followed by the Paterson toscanite. The Paterson toscanite divides the Lower Portion of the Glacial Stage from the Main Glacial Beds, but between the Moonabung Plateau and Eelah the toscanite is missing from the sequence, and along this belt it is difficult to draw the line between the two divisions mentioned above. Still it is quite clear from what has been said that there is a distinct difference between the rocks under the Paterson toscanite on the north-east, and their stratigraphical equivalents on the south-west. This matter is of some interest and importance from the standpoint of palaegeography and will be discussed under that heading. Paterson Toscanite and Dellenite. The rocks which come under this heading immediately underlie the Main Glacial Beds in all cases except one. In this instance a very thin flow of toscanite is found sandwiched in with the conglomerate and tuffs which have been described under the last heading. The occurrence of this was first pointed out to me by Dr. W. R. Browne, the unit being found on the bridle track from Hillsborough to Webber’s Creek Falls, just a little to the south of Wildman’s Gap. This occurrence is of no great importance, stratigraphically, because of its extremely limited extent. Concerning the main lava-horizon, it is to be noted that this comprises more than one flow in the Moonabung area and also to the west of Paterson. At the base of the main mass on the track to Bell’s house there is a small decomposed outcrop of pitchstone, seamed with haematite veins. This is identical with a small flow found in precisely the same stratigraphical position at Westbrook, near Singleton. Whether this is a glassy phase of the Paterson toscanite, or bears to the latter a relationship analogous to that shown by the glassy andesites to their associated lithoidal types is not known. The maximum thickness of the main mass is about 150 feet, but the varia- tions in the thickness are very marked. One cannot determine exactly the number and extent of the subsidiary flows, but it is quite clear that these exist. Thus near Bell’s house the interposition of conglomerate between two flows of toscanite is seen. The conglomerate wedges out to the south and the two flows coalesce. In a number of places a similar state of affairs exists, and in four isolated localities the presence of two flows without any intercalated sediments has been found. To BY G. D. OSBORNE. 89 the west of the bridle track not far from the Falls a dense, almost felsitic lava is found resting on the main flow. This is an albitized rock and recalls many of the features of the albitized hornblende andesites of Bridgeman. To the north of Webber’s Creek Falls there are two important flows, which are both toscanitic in character. In the neighbourhood of Paterson on the northern side of Webber’s Creek there are a number of interesting varieties of the lavas. One rock, purplish in colour, shows, under the microscope the presence of a pumiceous groundmass indicating that it is definitely a volcanic rock. This unit is associated with two flows of toscanite, which resemble one another. There are certain features connected with the toscanite in Webber’s Creek just a little upstream from the Falls, which puzzle one when endeavouring to interpret their significance. Here there seem to be strings of igneous rock penetrating the glacial sediments. A similar set of features was seen in the bed of Dunn’s Creek, east of Paterson and commented upon in 1922. Professor Browne has remarked upon the features in Webber’s Ck. and suggested that the toscanite may have been a sub-aqueous flow disturbing the sediments with which it was associated. From an examination of the toscanites over wide areas during the past five years I feel fairly sure that they are essentially extrusive rocks, and that the peculiar features seen in Webber’s and Dunn’s Creeks are probably best explained by the suggestion of Browne. The hypothesis that the rocks are sill intrusions raises obstacles that are difficult to remove. The glaciated pavement discovered in 1921 (see These ProcerepInes, 1921, p. 259) is upon the surface of the toscanite. Main Glacial Beds. Succeeding the Paterson toscanites there is a group of sedimentary rocks which constitutes the Main Glacial Beds, horizons of glacial origin occurring right throughout this series. These rocks are characterized by the fact that the individual units do not persist for any great distance. They outcrop upon the Moonabung Plateau and have been protected from rapid denudation by reason of the existence of the basin structure there. On account of the lack of constancy of the units, it is difficult to find a representative section of any considerable length from which to obtain a fair indication of the stratigraphical succession. In addition to this I have not been able to examine the area as fully as desirable, and hence the stratigraphical detail is not fully known. However, by considering the succession at a number of places and correlating the data, a good idea of the general features of the sequence is obtainable. The rocks immediately on top of the flows of toscanite, etc., vary somewhat, and comprise varve-rock, tillite, fiuvioglacial conglomerate and tuffaceous con- glomerate. Careful tracing of the rocks shows that the tuffaceous conglomerates which are developed at the Bald Hill, north of Bell’s house, are the lowest, stratigraphically, of the supra-toscanite units. These rocks will be referred to as the Bald Hill Series, and their maximum thickness is about 350 feet. They are present to the north of the Bald Hiil, and swing round at the head of Webber’s or Moonabung Creek, outcropping in Cabbage Tree Brush. They are also found on the southern slope of Mt. George and above Lennoxton, but they are practically absent along the stretch of low country to the west of Paterson and also to the north-east of the glaciated pavement. The rocks are fairly coarse, there being en abundance of pebbles of quartz and fine-grained acid rocks like felsites. The pebbles are well-rounded in most L 90 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. cases and the deposit is reasonably well sorted. Current-bedding is seen in most places, and the matrix, which is definitely tuffaceous, contains a certain amount of relatively fresh felspar and biotite. Sometimes the tuffaceous conglomerates pass into tuffs. The latter type of deposit is found resting on the toscanite to the east of Mr. M. Boland’s farm. Here there is a section leading up to the plateau which, starting at the top of the toscanite and proceeding upward, stratigranhically, is as follows: Thickness in feet Acid tuffs with pebbles eet ids sapere ee megs e100) Varve-rock bit aaEtE ore aie re ae meek. O) Conglomerate with current bedding .. .. .. 150 Tuffs with scattered pebbles Dae 40) Tuffaceous conglomerate 5 RES Be as Mey eee NiO. Ui Moy oz Nae Pema ise he oe URGXG) The varves here are somewhat coarse in texture, and they show contem- poraneous contortions. Further to the east of the point where the above section is found there is a series commencing with conglomerate in which the average size of the pebbles is much less than in the rocks of the Bald Hill Series. This conglomerate contains pebbles of chert, slate, free quartz and felsite. It is followed by varve-rock which shows a peculiar kind of fracture, whereby large flaggy pieces become detached from the underlying rock leaving a surface having a type of confused subconchoidal fracture. This kind of disintegration coupled with the dip of the rocks has had a definite effect upon the development of minor ereeks in this region, erosion being facilitated in the direction of dip. Following the varve-shale are some sandy rocks which may be glacial in origin, and these are succeeded by tuffaceous conglomerate in which are some bands of tuff. The pebbles in the conglomerate average about six inches in diameter. The next unit is a mass of tillitic material containing many angular and subangular fragments which have been irregularly accumulated. The tillitic material is succeeded by coarse acid tuff which is ferruginous and varies a little in texture. Then comes a series of purple shaly rocks reminding one of the Lochinvar shales of the Permian system, but probably representing glacial shales, similar to rocks of the same general appearance near the pavement which are definitely glacial. The shales are followed by coarse conglomerate and this is the highest unit examined in the section which is summarized as follows: Thickness in feet. Conglomerate aes eae BAN Cuca aetadins hea) Saree Peo lO WAT VESHMer ch ita 7 crcl tet Be SEE cl ees ee Be ane 80 Sandy, Locks possibly selaciailin sa eis eae 50 AMbuRENeLeYoyots| CLossk=lWopoMNY . G5. oo oo co oo oO) Tillitic deposit bie Yeas Divan y Wentay . Aeweye cede, ic. ommme OO Coarse’ ‘acidtufi, «:) 32 “eee eer eet (0.0 Purple shales, possibly glacial .. .. .. .. 150 Goarsescongslomeraten..-) ci) each ann Ee OL Notal 22. (se. ware elas If a traverse is taken from the Bald Hill towards the east crossing the basin, we find that the Bald Hill Series is succeeded by a fine cherty tuff carrying excellently preserved remains of Rhacopteris and Calamites. This is exposed on the right bank of Moonabung Creek at the foot of the long spur leading down from BY G. D. OSBORNE. 91 the Bald Hill. Then comes some very acid tuff, which is immediately followed by a white plant-bearing tuff. In this Rhacopteris is again abundant throughout and Calamites stems are limited to thin zones. This horizon is only about 25 feet thick, and forms a dip slope to the north and north-west of Sherwood’s house, which leads up to a ridge running to the edge of the plateau overlooking Lamb’s Valley. The white rock stands out well and forms a useful guide for picking up, from a distance, the general geographical details of the western side of the basin. Following the second Rhacopteris-tuff horizon there are some more con- glomerates, and these are followed by rocks which appear to be the Lochinvar Shales. These are overlain by Permian conglomerate. On the east side of the Permian rocks rocks are found which do not fit in with the section on the western side. Thus there are some varves which are limited to the eastern side, and there is only one Rhacopteris-bearing horizon. The varves are probably to be placed on the top of the Bald Hill Series. Varves of the same stratigraphical position occur at the head of Webber’s Creek in Portion 44, Parish of Wolfingham, resting with associated tillite on the Paterson type of toscanite. The Carboniferous rocks in the section just described are as follows: Thickness in feet. Bald Hill conglomerate Bis. vi Aublea lew chic & Wks aa nOR DN) WEARS thatol TOONS Go loo +906) boo ool oo) bo wll) JRA DOKGOV OFA abute, IN, U6 5 Bo be 00 100 bo. SH) Coarse tuff AR Sa Rae aaa eT iota Ree Mis 0 TY CRO GGFES eblit, INOS 7 Go 60 oa 60 Go oo 7) Conzglomerateeery Gijon, os Doe Wie rte) oreeu en ea00 MOEAIE: (Ra EA ayy: Considering next the succession in the neighbourhood of the glaciated pave- ment and Webber’s Creek Falls, we find that immediately on top of the toscanite at the pavement there are varves with pebbles and a very minor amount of tillite, while at the Falls the first rocks to succeed the lava are tillites and conglomerates. Following the varves and tillitic conglomerates come some olive-green to brown mudstones with scattered plant stems. Then comes another series of varves which are almost purple or brown in colour, and relatively free from contemporaneous contortions. These are well exposed in Bell’s Creek, which runs just to the north of the pavement and joins Webber’s Creek above the Falls. These varves swing round from this locality and then die out as we continue across to the northern side of Moonabung Creek; but they are found on the eastern side of the basin in a number of places. Therefore this second series of varve-shales is well developed, being fairly widespread in the area of the basin. A little north of Bell’s house we see an occurrence of varve-rock which, as regards stratigraphical position, is of interest. 'The glacial rock is associated with conglomerate which can be followed down the small creek just to the north of Bell’s. This conglomerate clearly separates two flows of toscanite and hence the varve-shales are sandwiched in between the lava horizons. From the genera! field evidence I think it very probable that these varve-shales are lower stratigraphically than those at the glaciated pavement and in Portion 44. The stratigraphy of the rocks on the Moonabung Plateau, ascending strati- graphically, is summarized as follows: 92 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. Carboniferous. Thickness in feet. (Maximum values. ) Main toscanite unit Nee ha hepa bis ig quam lSXt) Varve rock and conglomerate a Bell’ Sioa seas 90 Subsidiary flows of toscanite, cte. .. .. .. 100 Bald Hill Series .. . ieeaeye © 3.0.0 Pavement varve-rock and tillitic deposit sg abaxt) Mudstone with plant stems s eaahece ee ee Se 90 Rhacopteris tuff No. 1 Syd fa Scy pagans, ey ee anes 30 Acid, ferruginous tuffs Buel Sure ke Dre ee 80 Rhacopteris tuff No. 2 Ch BW WC 3 A ee 25 Purple varve-rock Brel aneeD eth ely Le eel 0 Conglomerate Ba Near ie alien at Usa ae ami Dey) Coarse acid tuff ... slye se st bees enero LOO) Purple shales, possibly elesien Pee Nee e amris Sy eben oy GEER) Coarserconslonierates ape eet ene 70 TPO tai ae em apo Permian. Shales (probably the Lochinvar Shales) 5% 50 Amygdaloidal basalt .. .. oi 20 Tuffaceous sandstones and conclameratas sa. PAY) TRO EALMIE ea trses Secreta GO This -gives a thickness of 1,475 feet for the Main Glacial Beds, which is distinctly less than that obtained at Seaham, but many of the values for thickness given here are only approximate. It is necessary now to consider the rocks west of Paterson and between Lennoxton and the Permian area on the south. Along the left bank of Webber’s Creek for some miles west of Paterson it is possible to gather some information about the succession. Just near the Paterson Park there are two bands of varve- rock with associated sediments, and one can generally find evidence of the existence of the same two horizons as one goes west. Associated strata comprise fine white tuffs, coarse red tuffs and coarse conglomerates with tillitic phases, in one of which an erratic about five feet in diameter was found. The second set of varves thickens considerably to the west and is found well developed towards the Falls, attaining to a maximum of 150 feet. As one goes up Smith’s Creek to the north one finds definite tillite along with the varve rock, and to the south of Lennoxion above the Paterson River the following section in the Main Glacial Beds is found: Thickness : in feet. Conglomerate, probably equivalent of Bald Hill Series Ae MP8 $ ae Sap EE 90 Wellow. Shute) seme + cal eh a ORS 80 Coarse tuffaceous UBIO. SO ERED oo ANAKD Tillitic deposit ye : 20 Normal conglomerate, Rvith! pine mpiite Henoles 80 MoOcalumerer a ion e AL It will be seen that the varve-rocks have disappeared from this section. BY G. D. OSBORNE. 93 Proceeding from the Falls towards Rosebrook the varves are seen to be strongly developed, the horizon being the equivalent of the purple varves on the Moonabung Plateau. On the eastern fall of the Rosebrook ridge and to the north of Drinan’s Mt. there are, of course, at least two horizons of varve-rock. Associated with the glacial beds just east of the Falls there are some siliceous tuffs which are not seen elsewhere. Outliers of Permian Age. Apart from the large area of Permian rocks in the south-east of the area, there are a number of outliers. Most of these are only a few acres in extent, but a larger one is to be found to the east of the Falls (see map). It is probable that there exist other small outliers which are not shown on the map. The rocks constituting these outliers comprise units which are sometimes representatives solely of the Lower Marine Series; as for example the Lochinvar Shales and the amygdaloidal basalt. At other times there are conglomerates which remind one of the Upper Marine conglomerates south of Paterson. The height above sea-level of the base of the outliers on the Moonabung Plateau is fairly constant, and is in excess of the height of the same horizon on the east side of the Falls by about 340 feet. These data confirm the existence of the Lennoxton fault and to some extent give a measure of the throw in this locality. STRUCTURAL GEOLOGY. The greater part of the area consists, structurally, of a basin which has been broken by a large fault on its eastern side. The examination of the dips shows the existence of this basin quite clearly, and physiographically the structure stands out well, as the toscanites, particularly the main one, have on account of being resistant units, dominated the topography. The section given in Text-figure 1 shows the structure of the Moonabung area. The Moonabung basin is of the same general nature as the other basins in the district to the west, viz. the Cranky Corner and Mirannie Basins, and it is separated from the latter by a comple- mentary structural feature. This is a plunging anticline, out of which Lamb’s Valley has been carved. The anticline is really the northern end of the Lochinvar Dome, the northerly dip of the beds being the measure of the pitch of this portion of the dome. Just as the Lochinvar Dome is elongated in a more or less meridional direction, so the Moonabung Basin shows an elongation in that direction, and the plan of the outcrop of the rim of the basin (which consists chiefly of toscanite), is an ellipse, the length of the major axis of which is about five miles, and of the minor axis not more than three miles. The eastern portion of the area, which is separated from the Moonabung Plateau by the Lennoxton Fault, forms the western side of the Paterson anticline. This structure was described in a former paner in 1922, although much of the detail of this portion of the region was not known then. It will be seen by inspection of the dips to the west of Paterson that the toscanite is dipping in a general southerly direction for some distance, and there is a change in the dip further west, the beds becoming flat near Lennoxton. The structure in the last-named locality is shown by considering Text-figure 2 in conjunction with the map. The gentle dip of some of the beds and the advanced state of the dissection have brought about the existence of both outliers and inliers of certain horizons. S VALLEY GEOLOGY OF PATERSON-LAMB 94 ‘( 93e[q) dew uo g-V 9UIT—'T wInsy-}x9L “(1 91¥[q) dew uo q-D surq—zZ svinsy-1xay, Seas 12479 Jo worysey EME F \ ! - LINVI NOLXONNIT ¥) 4499qRA 40 bUngeLcoly ie ese ee SNIVHO a us ae 2 Qa 3) osl- Sn a) | i 1 | 1 j aj uerxso/ 22 7Ue2s0) WAntiy \ OSL ! abeye je17e}9 Jo abeys BUEION : “ Ault Sal 9) spag 1e7>¢/E) wey ‘. 1 221190) NéIW IY worysoy 42M0 7) ! | l | ! | ) | | ) t ' YDS. Ysgg Im LTAWI NOLXONNGT YIAIY NOSYFILV SNIVHD [ J T ] oc 8 ov ° 9 v o0s- 4 \\ = = Shee TIAL a at 0 SPPg (©1285 Urey) \ ? 7 A J 003 1 ~~ 17¢; ur ' i (aVAy uossazeg) 22/42/Jagq PUP a,1Ue>S0/ LAI OA) seh ers [019€/9 Jo; | o0z! ' y ! | ! i} ' | uorzsey 4amo7! | 1 ' ! | A | IKIY INOLSNHOL MNVILWId INNGYNOOW AJ1IVA S.ONYT BY G. D. OSBORNE. , 95 In addition to the Moonabung Basin and the eastern region near Mt. Johnstone, both of which have been already considered, there is a third region which comes up for consideration. This is the area in the south-east which is given over to Permian rocks. The detail of the structure of this area is not yet known and we can only refer to the general structural features. The junction of the Permian and Carboniferous systems from Eelah to the north can be followed fairly readily as has been shown by W. R. Browne, by noting the outcrop of the Lochinvar shales. These appear, however, to cut out as one goes north from the neighbour- hood of Rosebrook, except that they are found in the Permian outliers in a number of places. However, they are definitely missing from the sequence near Paterson. A consideration of the strata in the field has led to the position of the junction of the two series being placed as shown on the map. Now it will be seen that the Permian rocks lie in a plunging syncline, or, to borrow a term used by Prof. Browne, form a “gulf” in the Carboniferous area. This syncline is complementary to the Paterson anticline on the north-east side, and to the eastern margin (now faulted) of the Lochinvar Dome, on the south- western side. But associated with these relationships we have the rather abrupt change in the dip direction of the strata in the neighbourhood of the S.W. end of the Lennoxton fault. Hereabouts one finds on the S.E. side of the postulated position of the fault, the beds turning round to strike in sympathy with the Permian syncline. On the N.W. side of the fault line, however, the beds dip in accordance with the Moonabung Basin. These facts emphasize the irregular nature of the folding. Faulting. The most important fault in the area is the Lennoxton fault. This has been followed from a point a little to the south of Wildman’s Gap to Vacy on the Paterson-Gresford road. The fault is clearly shown by the outcrops of the various horizons, and it is manifested physiographically also. Above the river at Lennox- ton there is a parallel fault associated with the larger one, the former throwing to the west. From a consideration of the structure to the east of Webber’s Creek Falls it is clear that the Lennoxton fault is normal in character, throwing in general to the east and south-east. The throw of the fault is difficult to estimate, and it increases as one goes north, but in the neighbourhood of Lennoxton it is between 2,000 and 2,500 feet. It is rather singular that this dislocation is absent along the track from Hudson’s Peak district to the Falls. On the S.W. side of the track at Wildman’s Gap there is an interesting fault which has been described by Browne. This and the Lennoxton fault are almost collinear, but careful consideration of the problem and detailed field examination seem to prove clearly that the two are unconnected. The fault in Kilfoyle’s creek is not a large one and may easily die out north- eastwards, but the other dislocation seems to be of fair magnitude near the Falls, and one would expect to find it crossing the track to Wildman’s Gap. But this it does not do, and it can only be surmised that the fault does not extend any further than is shown on the map. Just at the limit of the map in Portion 9 Parish of Wolfingham there is a number of small outcrops of the Paterson toscanite, and these seem to be the displaced equivalents of the main mass outcropping on the Moonabung Basin. They are of a lower altitude and an examination of their general features of occurrence suggests that they are the remnants of the toscanite 96 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. flows, which thin out very definitely as one comes S.H. from the Moonabung Plateau, and that here we have a small displacement along the fracture of the Lennoxton fault, the amount of displacement increasing as one goes north. Beyond Lennoxton the fault turns to the east, and near Vacy is hidden by thick alluvium, but it looks as if it carries on and becomes the fault described as F, and shown on the Clarencetown-Paterson map (see These PROCEEDINGS, 1922, Plate xxvi), since the latter possesses the same features of strike, magnitude, etc. A very striking effect of the fault is the displacement of the higher lavas of the Volcanic Stage from their alignment at the foot of Mt. Johnstone to the right bank of the Paterson River near Lennoxton. In addition to the large fault just described, there are a number of smaller ones. One already mentioned throws to the west. Another occurs on the east side of Lamb’s Valley above Mr. Boland’s farm, where the displacement of the toscanite is clearly seen. Further, in many places on the Moonabung Plateau the beds are standing on edge, indicating faulting, although very few details can be obtained regarding the nature of the movements. Frequently also on the Moona- bung Plateau strong jointing is observed, and this feature is no doubt the result of faulting movements. Finally near Paterson along the Webber’s Creek road there are small faults displacing the junction line between the Permian and Carboniferous Series. All the faults are normal and belong to a general group which includes those described from the Paterson-Seaham region and the series of normal faults mapped in the Singleton district. All these normal faults are probably of late-Palaeozoic age for reasons given in two earlier papers (These PRocEEDINGS, 1922, p. 525, and 1926, p. 401). PHYSIOGRAPHY. The area being considered is part of the northern margin of the valley of the Lower Hunter River. Dissection has proceeded to a fairly advanced degree, and the aspect of the topography on the whole is that of late-maturity, although there are exceptions where some of the smaller creeks are concerned, and also some- times the same creek will show both youthful and mature aspects in different parts of its extent. Thus in the case of Webber’s Creek we find an interesting assemblage of varying physiographic features as we pass upstream. The physiography of the area is intimately bound up with the geological structure, and thus it is convenient to maintain the division used in the chapter on the structural geology, taking the Moonabung Plateau as one part and that constituting the remainder of the region as the other. The faulting which has occurred does not manifest itself in the presence of initial fault scarps, because the fault-scarp-formation antedated the peneplanation and subsequent uplift, which were in turn antecedent to the present cycle of erosion. However, the manner in which the strata were arranged by the Lennoxton fault coupled with the arrangement due to folding has had a marked influence upon the topographic evolution. The peneplain surface in the area of the map was probably not so regular as was the case in some parts of the adjacent country, as for example from Mt. Johnstone towards Mt. Gilmore. What are probably remnants of some of the original shallow valleys and rounded hills are to be seen in certain parts of the Moonabung Plateau, it being fairly clear that Mt. Johnstone and Mt. George and BY G. D. OSBORNE. , 97 the Bald Hill as seen now have not suffered much lowering of height due to the erosion which followed the uplift. The respective heights of these, viz. 1,130, 1,466 and 1,050 feet give some idea of the height of the plateau in this region at the completion of the Kosciusko uplift. In two or three places one can see examples of valley-in-valley structure, generally on a small scale, the original broad valleys developed in late Tertiary time, being cut into by small streams, which in these cases are the rejuvenated representatives of the older streams. The adjacent area of the Paterson-Clarencetown district and the area under consideration belong to the same physiographic unit (part of an uplifted peneplain), and there is as one goes from the west towards the south-east from the present area, a decrease in the general height of the plateau, this probably being due, as mentioned by Browne in the paper on the Gosforth district, to an original slope in the surface of the plateau when uplifted. There are a number of outliers on the surface of the Moonabung Plateau. These are remnants of the Permian rocks which at one time covered much of the area now forming the surface of the plateau. These rocks were at one time continuous with the Permian rocks south and west of the Hunter River at Gosforth. The denudation of much of the capping of Permian rocks was accom- plished in pre-Kosciusko times, and thus the uplifted peneplain was characterized by the existence of relatively isolated patches of Permian rocks scattered about on the Carboniferous basement, these being subsequently somewhat reduced in size by Pleistocene erosion. As the physiography is affected by the nature of the rocks it is interesting to note the varying resistance offered by the different units to erosion. The most resistant rocks are the toscanite and dellenite (Paterson type). These are respon- sible for many striking dip slope-escarpment elements which are wholly or partly made of these rocks. The toscanites of the Moonabung Plateau produce the ring- like outcrop which bounds the plateau along almost the whole of its extent. The precipitous cliffs on both sides of Lamb’s Valley, which are inaccessible in places, are made of the toscanite. The conglomerates in the Lower Portion of the Glacial Stage stand out much more strongly than the tuffs and varve-rocks. A good illustration of this is to be seen on the bridle-track to the Falls. Here one crosses two bands of coarse conglomerate separated by tuff, and the former produce steep “pinches” on the track while the tuff has been eroded rather rapidly from off the surface of the lower conglomerate thereby allowing for the presence of a gently sloping section of track along to the base of the upper mass of conglomerate. The Main Glacial Beds as a whole offer only a medium degree of resistance to denudation, the Bald Hill Series being the exception. The rocks of this series are fairly well cemented conglomerates and tuffs and they are generally found standing out forming fairly rugged features as at the Bald Hill. The varves and mudstones break up rather easily and the tillitic conglomerates, on the whole, disintegrate readily. In the area of the Volcanic Stage rocks it will be noticed that a broad valley has been eroded by the Paterson River, but while this is a reflection of the advanced state of the denudation, it also emphasizes the fact that the lavas of that stage, on account of their lack of any great thickness in all cases, have not resisted erosion and along with the easily disintegrated conglomerates have been rapidly removed. M 98 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. The most important stream in the area is the Paterson River, but we are only concerned with the extreme margin of its valley in this area. ‘The physiography of the Lower Paterson has already been described by the writer in another paper, but it is interesting to record the presence near Lennoxton and Summer Hill of terracing along the Paterson. The exact cause of the production of these is not known, and while they may indicate the occurrence of small uplifts late in the history of the river, they may be due to uninterrupted erosional activity. Dismissing, then, the Paterson River, we see that the next most important stream in the area is Webber’s or Moonabung Creek,’ generally called by the latter name in its upper portion. This stream joins the Paterson River some two and a half miles south of Paterson and its valley for some distance upstream is heavily alluviated. From the point of confluence to the west for a distance of about four miles, the creek is flowing in a direction more or less parallel to the strike of the rocks, and because of this it has been able to erode a fairly wide valley along this belt. The northern limit of the valley just west of Paterson is the outcrop of the Paterson toscanite, and to the south the boundary is, in part, made by the sandstones and conglomerates of the Upper and Lower Marine Series. Thus the Main Glacial Beds and the Lower Marine cherts, etc., have been extensively removed. Further along the valley, one finds that the trend of the creek and the direction of strike of the rocks are no longer more or less parallel. Eventually, one reaches the barrier of toscanite at Webber’s Creek Falls, where, due to the irregular folding and the Lennoxton fault, we find the creek flowing directly across the strike. The falls are about 90 feet in vertical range and form an imposing sight in winter time immediately after rain. They are carved out of toscanite almost entirely. Above the Falls, Webber’s Creek presents a valley, different altogether from that seen on the lowland to the east of the Falls. Now we find that the stream and its tributaries are not able to erode quite so rapidly and on account of the centroclinal nature of the dips on the plateau there is not any striking widening of the small valleys in any particular direction. The presence of the barrier of toscanite at the Falls has brought about the deposition of alluvium over a relatively wide area upstream, and this has been contributed to by the direction of the dip of the strata just above the Falls being directly opposed to the direction of fiow of the creek. The alluvium so accumulated produces swamp-like areas in the wet seasons and the aggradation has prevented, in some measure, the deepening of the channel of Webber’s Creek to the north-west of the Falls. The tributaries on the north side of Webber’s Creek in the region to the east of the Falls have developed much more extensively than those on the south, and this is due, partly, to the southerly-directed dip of the rocks in the major portion of the northern area. Thus Smith’s Creek, and the two to the east of it, have fairly broad valleys, and the extensive erosion has brought about the existence of both inliers and outliers of certain units. Professor Browne, in discussing the physiography of the Gosforth district, has suggested that in the evolution of the present Hunter River which began with the epeirogenic movements at the close of the Tertiary, there were two main stages of 1[t should be noted that there is another Webber’s Creek, viz. in the Glendonbrook district. BY G. D. OSBORNE. 99 erosion consequent upon two uplifts. The former stage consisted of denudation of Permian sediments and the production of certain river and creek systems, which were superimposed upon the underlying Carboniferous terrane when the second uplift took place. With regard to the physiography of the Moonabung area, as a whole there is nothing to show whether or not there were two main stages in the late Tertiary uplift, but there is evidence of rejuvenation of the ancient streams having occurred. PALAEOGEOGRAPHY. The palaeogeography and geological history of the Gosforth district and its environs have been ably dealt with by Dr. Browne, and much of what he has written will apply to the Moonabung area because this is intimately related geologically to the former region. However, there are one or two points connected with the present district which may be considered here: The extent of the Paterson lavas and the nature of the sediments in the Lower Portion of the Glacial Stage and their probable former extent in the region being discussed. It is quite clear that the toscanite and delienite flows were very widespread when one remembers that they have been found from Raymond Terrace to at least as far as Mt. Dyrring, north of Singleton. On the north their limitation is not yet known, but while they are found close to the base of the Permian along from Seaham towards Moonabung, they are definitely missing from the sections east of Rosebrook and near Helah, and probably they do not occur in the Gosforth region, although there are some toscanite flows in the glacial beds recorded by Browne for the west of the Hillsborough district. The remnants of the thin margins of the toscanites are to be seen between Drinan’s Mt. and Wildman’s Gap and the flows on the Plateau above the Gap thin out east and south. That the thinning is rather abrupt is suggested by the fact that at the Falls the lavas are about 90 feet thick while a little to the east on the other side of the Lennoxton fault there is no sign of the igneous rock in the succession. Thus in short at a time just prior to the accumulation of the Main Glacial Beds there developed the interesting group of toscanites and dellenites, the flows spreading over a vast area covering the underlying sediments to a depth of about three hundred feet at Paterson where we find the greatest development of the rocks. The area occupied by the igneous rocks was bounded on the south (in this particular region) by a line running from near Wildman’s Gap towards the east. With regard to the rocks constituting the Lower Portion of the Glacial Stage one notices the constancy of the basal conglomerate, but for the bulk of the remainder there is a distinct difference in facies between the rocks which are found right throughout the Clarencetown-Seaham district and to the north of Moonabung on to Mt. Dyrring, and their stratigraphical equivalents in the region extending from just north of Drinan’s Mt. to Eelah, and also in the Gosforth district. The rocks of the former areas consist of tuffs with subordinate con- glomerates which occur in bands. The congiomerates are not coarse-grained, as a rule, and are always well cemented. The tuffs possess a brown, sometimes chocolate, colour and have a lithology which is characteristic. The rocks of the second group are characterized by the prevalence of pink-granite conglomerates and the general lithology is just as typical as, and quite distinct from, that of the other series. One can see the intermingling of the two types of sediment as one 100 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. goes from north of Drinan’s Mt. along the base of the Plateau. The pink-granite type of conglomerate is seen on the track to Bell’s, but it loses its individuality as we proceed to the north, and at the head of Lamb’s Valley and on the northern slope of Mt. George we have the tuffs and more finely-textured conglomerates of the group which is so well developed in the Paterson region. Further, at Gosforth, the rocks of the Main Glacial Beds comprise pink-granite conglomerates, but such sediments are practically absent from the Moonabung Plateau, although imme- diately following the Paterson toscanite there are conglomerates (the Bald Hill Series) which display the general facies of the Paterson-Singleton group. Browne has pointed out the probability that the area, which provided the granitic pebbles, which are so prevalent in the conglomerates right through the Kuttung Series in the Gosforth district, was situated to the south, and with this I am in accord, but from a consideration of the data to hand regarding the distri- bution of the two types of sediment, which are found in the Lower Portion of the Glacial Stage through the areas to the north of Gosforth, I would suggest that the following course of events characterized the development of the Lower Portion of the Glacial Stage. While the conglomerates and other sediments of the present Gosforth district were accumulating in post-Voleanic Stage time in the southern portion of the large Upper Kuttung lake, volcanic activity was manifesting itself by ejecting fragmental material which was widely spread. The material falling in the Gosforth district, was, taken as a whole, distinctly coarser, and less contaminated with detrital sediment, than that which accumulated throughout the large area from west of Singleton to Clarencetown. Over this latter region there was being piled up a series of tuffaceous sandstones and occasional conglomerate, the latter indicating grand flood periods in the cycie of erosion. The nature of the sediments in this region and the presence of current bedding suggest that these were developed in a large delta. It is probable that this delta in the great Kuttung freshwater lake, flanked the north-western shore, the areas providing the detritus for the delta formation being composed of a terrane, different from that of the area to the south, where granitic rocks abounded. A line which would effect a broad division between the two types of sediments in the Lower Portion of the Glacial Stage could be drawn on the map, and the actual physical boundary would pass under the Moonabung Plateau. PETROGRAPHY. The petrography does not need to be fully discussed here, because the general petrological features of the rocks correspond very closely with those of the rocks of the Clarencetown-Paterson region, which have been described in an earlier paper (These ProceEepincs, 1925, pp. 112-138). There it is pointed out that, in the region mentioned, there is a great variety of lavas ranging from intermediate to acid types, and embracing andesites, dacites, keratophyres, toscanites, dellenites, rhyolites and felsites. Some of these are vitrophyric, and some, particularly the more acid, are tuffaceous. Associated with the lavas are some acid albitic tuffs and flow breccias. In connection with these rocks it is also shown that on account of albitization having affected them it is difficult to make out the magmatic relationships and to work out problems of petrogenesis. On the other hand, it is possible to recognize only a broad sequence of flows throughout the area. Amongst the salient petro- logical features shown by these rocks, when considered as a whole, are the BY G. D. OSBORNE. 101 following: evidence of the operation of late magmatic processes effecting albitiza- tion and kaolinization; autobrecciation; devitrification; spherulitic structure. Coming now to the rocks of the Moonabung-Paterson region we note that many of the rocks correspond in general features to rocks from the more eastern district. The sequence which is found in the upper part of the Volcanic Stage near Lennoxton is as follows: Toscanite, albitized toscanite, dacite, potash rhyolite and keratophyre. Specimen 745 is a toscanite from Lennoxton, which in hand specimen shows a general brown colour with lighter streaks due to the presence of elongated inclusions. Free quartz is very abundant and a certain amount of felspar is visible. Microscopically, one sees much phenocrystic quartz and some andesine which has suffered albitization, together with a little orthoclase and some biotite. These are set in a crypto-crystalline groundmass which exhibits flow structure rather well. Specimen 743 from Lennoxton is a dacite which consists of phenocrysts of quartz, which are often well crystallized, and andesine, set in a rough-feeling groundmass which is a devitrified pumice. The next flow after 743 is a potash rhyolite of which 741 is a specimen. This is always of a red colour due to the presence of haematite which has developed by devitrification of a glassy rock. The haematite occurs in patches and the structure of the pumiceous groundmass is well displayed by the outline of the iron oxide patches. The felspars are clear and not albitized, and in addition to fairly abundant orthoclase there is some oligoclase. Specimen 740 is from the felsite at Lennoxton which is near the top of the Voleanic Stage. The rock is light in colour, and has the rough feel characteristic of trachytes. In thin section it is seen to be almost entirely a devitrified pumice, in which are set phenocrysts of corroded quartz, albite (which is probably of deuteric origin), and subordinate biotite. Specimens 710 and 713 are from near the Paterson River at Summer Hill, being just at the top of the Volcanic Stage. These are phases of the same lava, the general nature of the rocks being dacitic. Some of the felspar is completely albitized but remnants of original andesine can be made out. The horizon from which these examples were taken is characterized by the variation which is found along the strike. The green keratophyre which, as shown in the stratigraphy section, is generally at the top of the Volcanic Stage, possesses fairly constant petrographic characters, although there is a great variation in the colour of the rocks from place to place. In hand specimen the white felspar phenocrysts stand out well, and these are seen under the microscope to be albite. The groundmass is strongly pumiceous, and at times there are examples of autobrecciation. These rocks may be called tuffaceous soda rhyolites or keratophyres. As examples of the tuffs of the Volcanic Stage we may take Specimens 706 and 742. The former is from near Summer Hill on the Paterson River, and is a dark-blue rock which is really a flow-breccia, consisting of fragments of felspar and quartz, and also of dacitic rocks included in a pumiceous groundmass or matrix which in places shows flow structure. No. 742 is a quartz tuff which consists of quartz, albite orthoclase and biotite cemented by haematite and kaolin. In addition to the mineral fragments there are occasionally angular pieces of cherty rocks. 102 GEOLOGY OF PATERSON-LAMB’S VALLEY DISTRICT. While considering the tuffs of the Volcanic Stage, brief mention can be made of the tuffs which make up such a large proportion of the Lower Portion of the Glacial Stage. Specimens 705 and 712 are typical of these tuffs, both being from the Summer Hill locality. These are similar in general features, although differing in detail, the former, for example, containing much more in the way of rock fragments. Both rocks consist essentially of pieces of quartz, and plagioclase (often showing albitization), and fragments of glassy and cryptocrystalline rocks. Paterson toscanite and associated lavas. As was the case in the other areas, it is convenient to treat the rocks embraced under the above heading as a separate group. In addition to the toscanite, and the closely allied dellenite, we find in association, especially where there is more than one flow, soda rhyolites and certain slightly tuffaceous rocks. Probably the most important feature of this group for the present area, in comparison with the same group in the Paterson area, is the occurrence below the main mass of toscanite of a pitchstone, which shows a certain amount of devitrification. Specimen 730 of this unit is of a reddish colour and possesses an irregular fracture. Phenocrysts of felspar and biotite can be seen quite clearly in hand specimen. Under the microscope the phenocrysts comprise quartz, andesine, biotite and magnetite. The first of these is somewhat angular in piaces, but generally corroded. The andesine varies in grainsize but maintains a tabular habit. It is fairly fresh and any alteration seems to be the result of ordinary weathering. 'The mica is notably altered, being bleached and strongly resorbed at times, and the majority of sections show a pleochroism from golden yellow to deep brown. The groundmass is strongly haematitic due to devitrification, but the greater part is still glassy, and exhibits flow structure. The absence of pyroxene and amphibole phenocrysts is of interest and suggests that the rock is distinct from the pitchstones in the lower part of the Volcanic Stage. The rock also differs from many of the rhyolitic pitchstones which are found near Glenoak, and which contain no visible biotite. A chemical analysis is needed to discuss the relation- ship of this rock to the associated toscanites, but it is probable that a fair amount of orthoclase exists in the base. Specimens 259 and 260 are from a spot about three miles west of Paterson where there seem to be at least two flows in association. The former is a toscanite, possessing a fawn colour, while the latter is a dellenite and possesses a dark blue colour. Wo. 259, when examined microscopically, shows individuals of quartz, orthoclase and strongly albitized plagioclase with occasional biotite, set in a groundmass which appears to have been devitrified. No. 260 differs a good deal from the former and shows the presence of much biotite with quartz and the two felspars, in a groundmass which exhibits excellent examples of fluidal fabric, and which possesses some pumiceous patches and a little tuffaceous material. There is no doubt of these rocks being of extrusive origin, and hence the importance of this evidence in relation to the problem of the mode of occurrence of the Paterson toscanite suite. Near Bell’s and elsewhere there are definite cases of the existence of two flows. Specimen 737 is from the upper flow just north-east of Bell’s house. It differs from the main mass in that there is more phenocrystic felspar and less quartz. The general features of the groundmass are similar in both cases. Amongst the sedimentary rocks (excluding primary tuffs) there are many iuffaceous sandstones. No sections of these have been made, but macroscopic BY G. D. OSBORNE. 103 examination gives some information about their constitution. Generally there are grains of quartz and felspar and tiny chips of fine-grained rocks cemented by argillaceous material, with a minor amount cf haematite. Sometimes the haematite is strongly developed and characteristic red rocks result. Then again, in a few isolated instances there are examples of rocks which possess a siliceous cement. Concerning the conglomerates one has to note that the matrix is often arkosic, and may have been derived entirely from detritus, or more generally may contain a certain amount of fragmental material derived from volcanic centres. In the case of the Bald Hill Series, biotite is quite an important constituent. The general nature of the pebbles of the conglomerates has been indicated in the discussion of the stratigraphy and palaeogeography. EXPLANATION OF PLATE I. Geological Map of the Lamb’s Valley-Paterson District. A NEW DELTOPECTEN FROM THE ILLAWARRA DISTRICT, N.S.W. By Joun MircHe tt, late Principal of the Technical College and School of Mines, Newcastle, N.S.W. (Plate ii.) [Read 30th March, 1927.] DELTOPECTEN RIENITSI, n. sp. Plate ii, figs. 1 and 2. Spec. chars. Equivalvular, very inequilateral, suboblique, outline suboblong. Right valve strongly convex, ears apparently subequal, transversed by numerous radii, lati-transverse folds of the anterior ear strongly arcuate, and distinct finer striae numerous; radials of the body fine, increased by interpolations, and before the ventral margin is reached are grouped into distinct fasciculi, consisting of six to ten radii in each bundle, the transverse striae are fine and echinate the radials where these are crossed by them; the wider growth lines have scalloped or wavy edges. Beak prominent, incurved, pointed and reaching beyond the hinge line. Left valve flattish, radials less numerous and convex and less distinctly fasciculated than those of the right valve; the beak, too, is much less prominent than is that of the right valve; the two valves are distinctly agape along the hinge line, resilium large. The anterior ear protrudes beyond the anterior end of the shell, and is strongly emarginate. Dimensions: Length 7:2, width (depth) 4:5 cm. This Deltopecten resembles D. obliquatus Ethr. and Dun. (Mem. Geol. Survey, N. S. Wales. Pal. No.5, 1906) in several features but it differs from that species in having a large resilium, fasciculated radials, more apparent on the right valve than on the left; and less oblique in shape. Loc.—lllawarra District. Horizon.—Upper Marine beds. Permocarboniferous. Dedicated to Mr. H. G. Rienits, of Mt. Victoria, N.S.W., who allowed me the privilege of describing this fine specimen and who also kindly presented the type to me. THE FOSSIL ESTHERIAE OF AUSTRALIA. Part i. By JoHN MitTcHELL, late Principal of the Technical College and School of Mines, Newcastle, N.S.W. (Plates ii-iv.) [Read 30th March, 1927.] Introduction. The earliest record (Cox, These PROCEEDINGS, 1880, p. 276) of the occurrence of fossil Estheria in Australia was made by Dr. J. C. Cox from the Moore Park Diamond Drill bore; and to this first specimen Dr. Cox gave the name ZFstheria coghlani, after Mr. John Coghlan of the Diamond Drill Company, who was directing the work of sinking the bore referred to, but he neither described nor figured the species. The species was subsequently described by the late R. Etheridge, Junr. (Mem. Geol. Survey, N. S. Wales, 1888, Pal. No. I, pp. 6-8, Pl. i, figs. 1-10). The next reference to the occurrence of fossil Estheriae in Australian rocks was also made by R. Etheridge Junr., who in 1892 referred some specimens of this genus, obtained from Denmark Hill, near Ipswich, Queensland, to HE. mangaliensis Jones (Jack and Etheridge, Geol. and Pal. Queensland and N.G., 1892, p. 387). In 1909 I recorded the discovery of Estheriae in the Newcastle coal measures (Notes and Exhibits, These Procreprnes, 1909, p. 411-12). In 1925 I referred to the presence of Estheriae in the Belmont chert (tuff) beds. (Descriptions of new species of Leaia, These PROCEEDINGS, 1925, p. 438.) During the year 1890 I collected several specimens of HEstheriae from the Wianamatta series near Glenlee, but did not record the find at the time. It will be seen by the above record that the geologic range of Estheria has been considerably extended since 1892, which will be obvious from the following list of the series of rocks from which they have been collected to date, viz.: 1. Wianamatta Series, about 700 feet thick (Clarke) (but probably exceed 1,009 feet in the vicinity of Cobbitty). ‘ 2. Estheria Shales, about 610 feet thick (David). 8. Newcastle Coal Measures, 1,100 or more feet thick (David). To complete the actual stratigraphical range of these fossils, the intervening series between the Wianamatta and the Newcastle Coal Measure must be included, as: follows: 1. Wianamatta series, about 700 feet thick (Clarke). 2. Hawkesbury Sandstone, about 1,000 feet thick (Wilkinson). 3. Narrabeen Shales, about 650 feet thick (David). 4. Estheria Shales, about 610 feet thick (David). 5. Newcastle Coal Measures, about 1,100 feet thick (David). The total thickness of these together exceeds 4,000 feet; but that does not by any means represent the full geologic range of these fossils in New South Wales as far as present knowledge discloses, for there are at least two gaps in the portion N 106 FOSSIL ESTHERIAE OF AUSTRALIA, i. of the geologic record shown above, and these represent a considerable length of time even from a geologic point of view. These gaps occur between the Wianamatta beds on the one hand, and the Hawkesbury Sandstones on the other, and again, between the Hstheria Shales and the Newcastle Coal Measures. That the gap between the close of the Hawkesbury Sandstone Series and the commencement of the deposition of the Wianamatta Series thereon represents a considerable length of time is shown by the extensive weathering the former had undergone before conditions arose to admit of the formation of the latter; and that the break between the Newcastle Measures and the subsequent deposition upon them of the Mesozoic measures represents a great length of time, is shown by the great changes in the fossil Flora ushered in with the Mesozoic deposits lying immediately upon the Newcastle measures. The length of this lapse of time is further emphasized when the denudation of the lower measures before une upper series began to be laid upon them is also considered. The Mode of their Occurrence. In the lower portion of the Hstheria Shales and in the Wianamatta Series they occur in thin bands of impure clay ironstone. In-the Newcastle Measures at Belmont and at Warner’s Bay, they are found in cherts (tuffs). Judging by the fossils associated with them, it would appear that in each case they were dwellers in fresh, or slightly brackish waters. Those from Belmont and Warner’s Bay occur as casts only; but those from Merewether Beach, Newcastle, from the Estheria Shales and the Wianamatta beds often have tests preserved. Those obtained from the Estheria Shales and the Wianamatta Beds are black and lustrous, but those from the Newcastle beds (Merewether Beach) are of a dun colour. It is not uncommon to find specimens with two valves conjoined, but never free from the matrix, so far as I am aware. The variety of forms of Hstheria obtained from the Newcastle Coal Measures is remarkable. From Victoria, South Australia, West Australia and Tasmania, the occurrence of fossil Estheria, so far as I am aware, remains to be recorded. Largely owing to imperfect preservation my attempts to obtain satisfactory microscopic enlargements of the ornamentations of the interspacial areas of the Estheriae:- dealt with in the present paper have not been successful; therefore I decided not to make any special reference to these particular features of this interesting genus so well represented in the Upper Permian rocks of the Newcastle Coal measures of New South Wales. ESTHERIA COGHLANI Cox. Plate ii, figs. 3, 4, 5. Proc. Linn. Soc. N.S.W. 1880, p. 276 (1881); Etheridge, Junr., Mem. Geol. Surv. N.S.W., 1888, Pal. No. 1, Pl. i, figs. 1-10. To Mr. Etheridge’s description of this species nothing remains to be added. He was of the opinion that among the drawings and specimens examined by him there was a second species. On comparing his figures 1, 3, 6 with figures 8 and 9 that opinion seems to have good evidence to support it. After a careful study of a large number of the specimens from the Hstheria beds, my view on the point in question agrees with that of Mr. Etheridge, but available evidence is not yet quite conclusive. BY JOHN MITCHELL. 107 The range through geologic time of H. coyhlani was considerable, for at least one specimen of it was obtained by me from the Wianamatta formation at Glenlee, thus affording evidence of its persistence throughout the Triassic formations as far as represented in New South Wales. ESTHERIA IPSVICIENSIS, n. Sp. Plate iii, figs. 1-4. Estheria mangaliensis Etheridae (nec Jones), Jack and Eth., Geol. and Pal. of Queensland and N.G., 1892, p. 387. The late R. Etheridge Junr. described this species but did not figure it. He referred it to HE. mangaliensis Jones. His description of it is as follows: ‘Valves broadly subovate, hardly convex; dorsal margin straight, about half the length of the valves, terminated at the anterior end by the umbones; anterior, posterior and ventral margins fully and broadly rounded, the anterior shorter than the posterior, rendering the valves narrower at the former of the two ends; umhbones depressed; ridges twelve in number, but probably two or three more exist on each umbo, strong and well marked; interspaces wide, depressed, or perhaps very slightly concave, especially towards the ventral portion of the valves; reticulation not preserved. Length about three-sixteenths of an inch.” “Observations: This little fossil, the first Hstheria found in the secondary rocks of Queensland, appertains to the group represented by such species as E. mangaliensis, E. Forbesi, etc., and in fact is so very close to the former in its general features, that I am constrained to consider it as identical, notwithstanding the absence of the reticulated surface in our fossil. It is particularly like Professor Jones’ Pl. 2, fig. 16.” In the above description and observations there appear to be some inaccuracies which require correction; and to enable me to make these corrections I have through the courtesy of Mr. B. Dunstan, Chief Govt. Geologist, Dept. of Mines, Brisbane, before me the specimens used by Mr. Etheridge when making his description and determination of the Hstheria under review. In the first place the valves of the carapaces of this Hstheria are said to be hardly convex, instead of being strongly so, when not flattened by external pressure. The interspaces are neither wide nor depressed, but narrow and convex, and flat near the ventral margin. Owing to the gradual way in which the dorsal margin merges into the posterior margin it is difficult to give the exact ratio which the dorsal margin of the Ipswich Estheria bears to the total length of its valves: but the following measurements taken with care will result in a fairly accurate estimate of the ratio being arrived at: 1. Length of dorsal margin and of valve 4: 7 (No. 55 in Coll. Mitchell). 2. Length of dorsal margin and of valve 5:12 (Type, Geol. Mus., Brisbane). 3. Length of dorsal margin and of valve 4: 9 (No. 53 Geol. Mus., Brisbane). It may be noted here that in the case of three specimens of H. mangaliensis Jones (Mon. Fossil Estheriae, 1862, p. 78, pl. ii, figs. 16, 20 and 21), the ratios of the lengths of the dorsal margins and lengths of valves are 3:5, 1:3 and 7:18 respectively, exhibiting much variation. These proportions between the dorsal margins and the lengths of the respective valves do not support the identity of the Ipswich Estheria with the one from Mangali. The anterior and posterior ends of the Ipswich Estheria are protrusively rounded, and in this respect differ from the Mangali species. The umbones are depressed only when distorted by pressure: ridzes visible on mature Ipswich LOPES) are twenty-two or more. 7 108 FOSSIL ESTHERIAE OF AUSTRALIA, i. I consider this Ipswich Hstheria to be a new species, and dedicate it to the locality or measures from which it was obtained. It differs from H. mangaliensis (1) in having a more ovoid form, (2) a greater number of growth ridges, (3) in the individual specimens being more uniform in outline, (4) in having more protrusive anterior and posterior margins. From E. forbesi it is easily distinguished. The illustrations of specimens of the species which accompany the present paper, so clearly show the important features of the species that the writer thinks it unnecessary to give further detaiis except as to dimensions, which are as follows. Plate iii, fig. 3, is from a specimen dealt with by Etheridge, who also examined the specimens shown on plate iii, fig. 4. 1. Length 5:0: width 3:0 mm. (Type, Geol. Mus., Brisbane). 2. Length 5:5: width 4:0 mm. (No. 27 Geol. Mus., Brisbane). 38. Length 6:0: width 5:0 mm. (No. 55 in Coll., Mitchell). Loc.—Denmark Hill, Ipswich, Queensland. Horizon.—Upper ‘Triassic (Jack and Etheridge, Dunstan, Walkom and Tillyard). ESTHERIA GLENLEENSIS, n. sp. Plate ii, fig. 6. Spec. chars.: Carapace transversely oval, dorsal margin mildly sagged, the other margins rounded, the anterior strongly so; beak prominent about five- eighths anterior, concentric striae nine or ten in number distinct, widely spaced; the whole carapace convex. Dimensions: Length 4:0; width 3:0, mm., approx. This species is easily distinguishable from #H. coghlani. In some resvects it resembles H. mangaliensis Jones (Mon. Foss. Estheriae, 1862, pl. ii, fig. 16), but differs from that species in (1) having many less growth ridges, (2) having a more truncate posterior margin, (3) a more protrusively rounded anterior margin, (4) being of smaller size, and in having wider spaces between the growth ridges; also in having a less variable outline. The horizons in which the Mangali and the Glenlee Hstheriae are found do not differ much in point of geologic time, therefore their identity would not have been surprising, if such had been proven. Loc.—The species was obtained from a cutting on the Great Southern Railway near Glenlee Homestead. Horizon.—Wianamatta series. The fossils found associated with this Hstheria consist of other Hstheriae, plants belonging to the genera Taeniopteris, Macrotaeniopteris, Thinnfeldia, Cladophlebis and Phyllotheca, all of which go to show that the Wianamatta Estheriae dwelt in fresh water. ESTHERIA WIANAMATYENSIS, n. Sp. Plate ii, figs. 7, 8. Spec. chars.: Carapace small convex, transversely subelliptic; beak sub- central; ridges six or seven only visible, interspaces relatively wide; anterior and posterior margins protrusively rounded dorsal margin arcuate, ventral margin mildly rounded. Dimensions.—Length 3:0; width (depth) 2:0 mm. BY JOHN MITCHELL. 109 This may represent an immature specimen, but even if that be so, its tumid, almost centrally placed beak and transversely elliptic shape, separate it from other Australian species, and also from H#. minuta Alberti. Loc. and horizon.—As for E. glenleensis. ESTHERIA NOVOCASTRENSIS, n. sp. Plate iii, figs. 5, 6. Spec. chars.: Carapace, outline subquadrate, dorsal margin straight, anterior and posterior margins truncate, ventral margin widely and gently rounded; con- centric striae about twenty in number, fine, evenly spaced; test appears to have been of delicate texture, and is much crinkled; beak anteriorly situated and prominent. Dimensions.—Length 8; width 6mm. Another L=9 and width 6 mm. (These dimensions are greater than for any other fossil Hstheria from the Newcastle Series. ) I know of no species with which this can be either compared or contrasted with advantage, though in the number of striae H. forbesi Jones, and the present form approximate. Loc.—Merewether Beach, a short distance S.W. of the outflow of the New- castle sewerage; between low and high tide levels. Horizon.—A few feet below the Dirty Seam of coal of Newcastle Coal Measures, associated with various species of Glossopteris, and with Phyllotheca australis. Upper Permian. ESTHERIA LENTICULARIS, n. sp. Plate iii, fig. 7. Spec. chars.: Carapace lenticular, small, smooth; beak subanterior, incon- spicuous; concentric striae very fine six or seven in number, interspaces increase in width as they approach the ventral margin. Dimensions.—Length 2; width 1:8 mm. The smoothness of the carapace and its small size are the two leading features of this Hstheria; the fineness of its concentric striae is also very noticeable. The only Australian Hstheria, which may be compared and contrasted with it, is H. wianamattensis. They are both of small size and have few concentric striae on their valves, but the species here dealt with has a more prominent and anteriorly situated beak than the other one has. The fineness of the striae and smoothness of the carapace of the present species strongly contrast with the similar parts of FE. wianamattensis. It is not improbable that the Wianamatta species descended from the mere ancient one from the Newcastle coa! measures. Loc. and horizon the same as for HE. novocastrensis. ESTHERIA TRIGONELLARIS, Dn. Sp. Plate iv, fig. 6. Spec. chars.: Outline subtriangular, convex, dorsal margin slightly sinuate, short; the other margins well rounded; beak about two-thirds anterior, very prominent, elevated; concentric folds distinct, fairly regularly spaced, from the end of the dorsal margin, the upper part of the posterior margin is depressed along its edge. The description above is made from a mould of a left valve. Dimensions.—Length 7:0; width 5:0 mm. Loc. and horizon the same as for H. novocastrensis. ESTHERIA OBLIQUA, n. Sp. Plate iv, fig. 1. Spec. chars.: Transversely suboblong, convex, posteriorly obliquely protrusive, dorsal margin long, straight anterior margin short, sharply rounded and gently 110 FOSSIL ESTHERIAE OF AUSTRALIA, i. sinuate near the beak, posterior margin truncate; beak anterior and prominent; concentric folds, strongly developed, twelve visible; but probably had sixteen or more; they are strongly geniculated where they cross the umbonal fold, and as they near the ventral margin, they are reduced to striae and are closer together. The ornamentation apparently is made up of small globular bodies. Dimensions.—Length 7:0; width 5:0 mm. The specimen described has the valyes in apposition, the right being under the left as may be observed by an examination of figure which represents the type. Loc. and horizon the same as for H. novocastrensis. ESTHERIA LATA, n. Sp. Plate iii, figs. 8, 9. Spec. chars.: Obliquely subflabellate, convex. smooth near the umbonal area; dorsal margin straight, half as long as the length of the valves; anterior margin distinctly rounded, posterior margin rounded and obliquely sub-protrusive, ventral margin widely rounded. Concentric striaé. Fourteen visible, fine and fairly distinct, and regularly spaced; beak inconspicuous, subanterior. Dimensions.—Length 7-0; width 6-0 mm. This is a very distinct species. easily separated from all other Australian forms discovered up to the present time; also it ranks among the largest of the fossil Estheriae from Australian palaeozoic rocks. In some respects it resembles some forms of EH. forbesi Jones (Mon. Foss. Hstheriae, Palaeontological Soc., 1862, p. 109, Pl. iv, figs. 8-9) in a general way; but specifically it is a distinct type. Loc. and horizon.—Merewether Beach, near the Newcastle Sewerage outlet; just below the Dirty Coal Seam, Newcastle Coal Measures, Upper Permian. ESTHERIA BELMONTENSIS, n. sp. Plate iv, fig. 5. Spec. chars.: The carapace subquadrate, flattish, dorsal margin straight, relatively long. Under the dorsal line there is a flat area which resembles a hinge plate, and which is not usually observed in members of the Estheria group; anterior subtruncate, and the posterior one widely and mildly rounded; ventral margin gently rounded, beak anterior, and inconspicuous, concentric striae, nine- teen or twenty in number, distinct and fine. Dimensions.—Length 6:0; width 5-0 mm. This species in some features bears a strong resemblance to EH. ipsviciensis, which may be a descendant of the older Permian type. Loc.—The chert (Tuff) quarries near Belmont, Parish of Kahibah, County Northumberland, New South Wales, associated with several species of Glossopteris, Leaia and Insects. Horizon.—Upper Permian. ESTHERIA GLABRA, nn. Sp. Plate iv, figs. 2, 3. Spec. chars.: Left valve testless, transversely subelliptic; convex; test was apparently thin and delicate; dorsal margin very gently curved, anterior and posterior margins rounded, ventral margin mildly rounded; beak, three-fifths anterior, prominent; concentric ridges, only three or four clearly visible, but traces of others can be seen with the aid of a good lens. Dimensions.—Length 4:0; width 2:0 mm. Although a large part of the cast of the valve above described has a smooth appearance, there is slight evidence that the concentric striae on the original test BY JOHN MITCHELL. P 1h lal were more numerous than are at present visible. Its much elongated subelliptic shape separates it from other Australian Hstheriae. The sparsity of its visible striae is another distinguishing feature. The type is a unique specimen. Loc. and horizon the. same as for EH. belmontensis. ESTHERIA LINGUIFORMIS, n. sp. Plate iv, fig. 4. Spec. chars.: Carapace obliquely flabellate, and flattened along the borders of the postero-ventral margins. Dorsal margin straight and long, anterior margin short and rounded; posterior one wide and gently rounded; beak anterior, incon- spicuous; concentric striae about eighteen in number, obliquely directed towards the postero-ventral margins, fine and compacted near the umbo and towards the postero-ventral margins, intermediate of these two areas they are distinct or ridged. Dimensions.—Length 5:0; width 4:0 mm. The above description of the type is made from a mould of a nearly perfect right valve. This species, like EH. belmontensis, bears some resemblance to H. ipsviciensis, so much so, indeed, as to make the assumption that the former is directly ancestral to the latter, not an unreasonable one. The distinguishing features of this form are (1) its anterior beak, (2) long straight dorsal margin, (3) narrow anterior margin, and (4) wide posterior margin. Loc. and horizon the same as for H. belmontensis. EstHEeRIA (?) BELLAMBIENSIS, n. sp. Plate iv, figs. 7, 8. Spec. chars.: carapace sub-oblong, very inequilateral. Dorsal margin very long and straight, anterior and posterior margins gently rounded, or subtruncate; ventral margin subparallel to the dorsal one; beak, anterior, inconspicuous; con- centric striae arranged in two sets—a wide apart set, and between each pair of these, finer ones occur, very numerous; the vaives are convex. Dimensions.—Length 10:0 mm.; width 6:0 mm. approximately. If this fossil is an Hstheria, it exceeds in size all other Australian species of the genus. In the character of its growth lines it resembles some Unionella; but of three specimens known, each has a length of approximately 10-0 mm., and appears to be mature. This length is much less than any mature Unionezila possesses. The straight hinge line of the present fossil clearly separates it from molluscans of that group. In shape, size and surface ornamentation H. bellam- biensis resembles the H. striata group. The tength of the carapace of the species under discussion exceeds that of all other Mstheriae known to me from palaeozoic rocks. Locality—The north side of the railway line connecting the South Bulli (Bellambi) Colliery with the staiths at Bellambi roadstead, associated with various species of Glossopteris. Horizon.—About 150 feet below the seam of coal worked in the South Bulli Mine, and in stratigraphical position near to the Belmont Insect and Phyllopoda beds. Upper Permian. My hearty thanks are extended to Dr. C. Anderson, Director of the Australian Museum, Sydney, for placing at my disposal for examination a number of recent Hstheriae. To Mr. W. S. Dun, Palaeontologist, Department of Mines, Sydney; and to Mr. Booker, of the same Department, I tender sincere thanks for valuable aid extended to me while preparing the present paper. I am thankful to Mr. H. G. 112 FOSSIL ESTHERIAE OF AUSTRALIA, i. Gooch, Photographer for the Department of Geology, University of Sydney, for some excellent photos of specimens dealt with in this paper, and lastly I am indebted to my friend T. H. Pincombe, B.A., of New Lambton, for the privileges of examining the Estheriae collected by Mrs. Pincombe and himself. I wish to point out that in my paper on ‘Descriptions of New Species of Leaia’’ (These PROCEEDINGS, 1925, pp. 4388-447) I have made a mistake in orienting the valves of the carapaces. I find that all right valves are designated left and the left valves right. EXPLANATION OF PLATES II-IV. Plate ii. 1. Deltopecten rienitsi, n. sp. right valve. 2. Deltopecten rienitsi, n. sp. left valve. 3. A right valve of Estheria coghlaini Cox somewhat pressed into the left valve. From Cremorne bore. x 8. Coll. Dept. of Mines, Sydney. 4. Estheria coghlani from Dent’s Creek bore. x 10. Coll. Mitchell. 5. Estheria coghlani from Glenlee (Wianamatta Series). x 14. Coll. Mitchell. 6. Estheria glenleensis, n. sp. x 12. Coll. Mitchell. 7. Estheria wianamattensis, n. sp. xX 12. 8. Estheria wianamaitensis, n. sp. x 14. Plate iii, 1. Estheria ipsviciensis, n. sp. Left valve. x 8. Coll. Mitchell. Presented by the Dept. of Mines, Brisbane. 2 Estheria ipsviciensis, n. sp. Left valve. x 10. A good specimen. Coll. Dept. of Mines, Brisbane, No. 53. 3. Estheria ipsviciensis, n. sp. Left valve (depressed). x i0. This valve was one dealt with by R. Etheridge Junr. as H. mangaliensis. Coll. Mines Dept., Brisbane. 4. Estheria ipsviciensis. The photograph shows two individuals on the same stone. They were examined by R. Etheridge Junr. (loc. cit.) x 10. Coll. Dept. of Mines, Brisbane. : bo 5. Estheria novocastrensis, n. sp. Left valve. x 5. Coll. Mitchell. 6. Estheria novocastrensis, n. sp. Left valve. x 5. Coll. Mitchell. 7. Estheria lenticularis, n. sp. x 12. Coll. Mitchell. 8. Estheria lata, n. sp. x 6. Coll. Mitchell. 9. Estheria lata, n. sp. Left valve. x 5. Coll. Mitchell. Plate iv. 1. Estheria obliqua, n. sp. Left valve. x 10. Coll. Mitcheil. 2. Estheria glabra, n. sp. Left valve. x 12. Coll. Mitchell. 3. Estheria glabra, n. sp. A mould of right valve showing a more ovoid form than Dives. 45 3 He 4. Estheria linguiformis, n. sp. Right valve. Coll. Mitchell. 5. Hstheria belmontensis, n. sp. x 7. Coll. Mitchell. 6. Estheria trigonellaris, n. sp. Left valve. x 7. Photo from a mould. Coll. Mitchell. 7. Estheria (7?) bellambiensis, n. sp. x 6. 8. Estheria (7?) bellambiensis, n. sp. A pair of fragmentary valves joined along the hinge. x 6:5. Coll. Mitchell. (The photographs by H. G. Gooch, J. A. Booker and J. Mitchell.) A NOTE ON A DICOTYLEDONOUS FOSSIL WOOD FROM ULLADULLA, NEW SOUTH WALHS. By C. BarnarpD, B.Sc., Demonstrator in Botany, University of Sydney. (From the Botanical Laboratories, University of Sydney.) (Plates v and vi, and six Text-figures.) {Read 30th March, 1927.] Introduction. The subject of this communication is a piece of fossil wood of a dicctyledon. It was found by Miss Brown of the Geology Department, University of Sydney, in a silica quarry at Bannister Head, near Ulladulla, New South Wales. The author published a brief descriptive note of this fossil in connection with Miss Brown’s paper on the Tertiary Formations on the South Coast of New South Wales. It seems desirable that a fuller account of this interesting specimen, supplemented by figures and photographs, should be recorded in order that its systematic position may be ascertained. Two fossil Angiosperm stems, with structure well preserved, have previously been described from Australia. Sahni“? has published a description of two stems from the Tertiary of Queensland. One, Petaloxylon scalariforme, from Mt. Meershaum, near Nerang, is peculiar in that the chief conducting elements are large scalariform tracheids. The medullary rays are 1-3 seriate, twenty-five to thirty cells in height and pursue a sinuate radial course. The other, Petaloxylon porosum, has essentially the same structure except that true vessels are also present. Nobes™ records the discovery of four petrified stems from some Tertiary Brown Coal deposits in South Australia. The preservation of these was so poor that no description was published. A great number of leaf impressions have been described by Httinghausen® and Deane.” “” These remains, which have mostly been derived from Tertiary 1The silica beds, in which the specimen was found, were formerly believed to be of Permo-Carboniferous age and the silicification was thought to have been effected by the intrusion of volcanic dykes (Harper). ® 4° Miss Brown®) has lately proved that these strata are of Tertiary age and has shown on reliable geological evidence that Silicification has been effected by later Tertiary basalts. These “silica rocks’ occur in patches, associated with clays and sandstones, in the Milton-Ulladulla district on the South Coast of New South Wales, overlying beds of Upper Marine age. At Bannister Head there is a slight angular unconformity between the later sediments and the underlying Permo-Carboniferous strata; and also at Pattimore’s Lagoon deposit, as well as at Bannister Head, remnants of the basalt flows are evident in the form of capping sheets. Petrographic studies by Miss Brown of the olivine basalt composing these lavas have established the correlation between the flows in this region and other Tertiary basalts of the State. Though the exact age of these ‘“‘Tertiary Olivine Basalts’” has not been definitely determined, it is generally held (Sussmilch)@” that they belong to the Upper Miocene or Pliocene period. The deposition of the underlying silica beds must then be assigned to the Lower Tertiary Period. O 114 DICOTYLEDONOUS FOSSIL WOOD FROM ULLADULLA. deep leads, come from the same period as the Ulladulla fossil and give an indica- tion of the Angiosperm flora existing at that time. . Ettinghausen has described fruits as well as leaf impressions of Casuarina, Persoonia, Grevillea, Hakea, Lomatia, Dryandra, Callicoma, Ceratopetalum, Pomaderris, Eucalyptus, Santalum, Myrica, Quercus, Alnus, Acer, Aralia, Cinna- momum, Fagus and Hlaeocarpus from Vegetable Creek, near Hmmaville, New South Wales. These, it will be observed, include many endemic genera as well as representatives of the Malayan flora. The same author has described many types from Dalton, near Gunning, New South Wales. Deane® ™ has identified a number of leaf impressions from the clay beds at Mornington, Berwick, and Wonwron, Victoria; R. M. Johnston® “ describes similar impressions from the Lower Tertiary of Tasmania. These remains have, with few exceptions, all been referred to existing genera. In some cases the resemblance between fossil forms and living species is so close that the affinity has been expressed in the specific name given to the fossil. Hucalyptus pre-coriacea from the Lower Tertiary, for example, is almost identical with the existing species “‘coriacea.’”’ From this evidence it will be observed that the flora of the Lower Tertiary was very similar to that existing at present. Text-figure 1. Representation of portion of the transverse section (slightly diagrammatic), showing the seriation of the vessels and fibres; illustrating particularly the thickness of the walls of the vessels and fibres. x 280. BY C. BARNARD. 115 Description. Material. The specimen consists of a fragment of secondary wood preserved by the agency of silica. It measures roughly 8 cms. by 4 cms. The end, which is cut transversely, shows regular and well developed annual rings. The curvature of these indicate that the piece of wood was about two and a half inches from the centre of the stem and that the stem had a minimum diameter of five inches. The structure of the wood is well preserved. Unfortunately the specimen does not show any phloem or bark. Microscopic Description. Diagnosis: The wood has a fine texture. Annual rings developed. Vessels numerous, circular, in radial series or isolated; bordered or scalariform pitting, mostly porous perforate, tertiary bands present, slightly stratified, average diameter 0-1 to 0-075 mm.; average of 50 per sq). mm. Wood fibres form the ground tissue of xylem, thick walled, size variable, arranged in regular radial series. Wood parenchyma cells abundant, rectangular, vertical height, 0:04 mm., width 0:25, occurring in vertical series. Medullary rays numerous, diffuse, biseriate, rarely uniseriate, 10-15 cells in height, heterogeneous, cell walls thick with simple oval or circular pits. General: The vessels are of medium size and are evenly distributed throughout the wood. The wood fibres compose the bulk of the wood and are very thick walled. The vessels in the spring have a diameter up to 0:16 mm. These become gradually smaller till at the end of the annual ring in the autumn the average diameter is 0:04 mm. Parenchyma cells are abundant, diffuse and mostly situated at the end of the annual rings, almost forming metatracheal bands. The medullary Tays are very uniform in height. The vessels and wood fibres are arranged in regular radial series. Details of Elements: In transverse section the Vessels show an approximately circular configuration. They occur singly or in pairs or in radial rows up to ten in number. In these latter cases the tangential walls are flattened (Text-fig. 1 and at 0 in Fig. 1, Plate v). The average diameter is 6-075 mm. The average diameter of the spring elements is 0-13 mm. and the autumn average is 0:05 mm. The walls are thick. In longitudinal section the sculpturing on the walls consists of regular series of small oval bordered pits in horizontal rows (Text-fig. 4c and Fig. 2, Plate v). The borders of the pits are narrow. The large vessel in the centre of Fig. 2 Plate v shows this type of pitting very well. In some cases the coalescing of the pits gives rise to a close scalariform sculpture. This feature is apparent in the large vessels in Fig. 3 Plate vi and appears, in fact, to be the dominant type. The internal spiral bands of thickening, termed tertiary thickenings, are also present in many of the vesséis. The average length of the vessel segments is 0:6 mm. The two segments, illustrated in Fig. 3 Plate vi, are typical and each of these has a length of 0-6 mm. The majority are of the porous end-wall type (Text-figs. 4c and 6 and Fig. 2 Plate v and Fig. 3 Plate vi). The septa in these elements are short and distinct; they are almost at right angles to the longitudinal walls of the vessel. Each is perforated by one large pore. A few vessels exhibit a number of elongated pores on the end-wall. These are examples of the scalariform perforate type. In some 116 DICOTYLEDONOUS FOSSIL WOOD FROM ULLADULLA. eases the so-called “imperfect perforation’ is present. The end-walls in vessels, which show this feature, are very oblique and numbers of bordered pits occur on them together with one or two large perforations (Text-fig. 4 a@ and db). Vessels . with end-walls of this nature are longer and have a smaller diameter than the neighbouring vessels with the porous type. No tyloses were observed. The vessels appear to be more or less stratified or storied. 2 Text-figure 2.—Representation of portion of the radial longitudinal section showing the vessels in detail. An indication of a close scalariform sculpturing is apparent on the lateral walls of several porous end-wall types of vessels. x 80. Text-figure 3 represents a portion of the tangential longitudinal section showing the medullary rays in detail together with vessels and fibres. On the left there is a series of parenchyma cells with the original thickness of the walls preserved. x 165. The wood fibres vary considerably in diameter and length. The average diameter is 0:02 mm.-0-01 mm. Very often the tangential diameter is greater than the radial. In general the walls seem thin (Text-fig. 2), but this appearance is due to the fact that it is really the junction line between contiguous fibres which represents the wall. In places where the preservation of the structure iS more perfect and the true thickness of the wall is shown it presents a very characteristic appearance. The nature of the fibres is seen at a in Fig. 1 Plate v. The lumen BY C. BARNARD. 117 represents only one-third or one-fourth of the diameter. No pitting could be observed in the longitudinal aspects of these elements. They are regularly seriated in a radial direction. The wood parenchyma cells are seen to best advantage in the longitudinal sections (Text-figs. 3, 4 and 5 and Fig. 3 Plate vi). They occur in vertical series and are most abundant in the region of the autumn wood. There are as many as forty cells in ome series. The average vertical height of each cell is 0:040 mm. and the average width in tangential and radial aspect is 0-025 mm. The pitting on these cells was not observed. The walls are comparatively thick. In some instances black carbonaceous material is apparent in the cell cavity. A Text-figure 4.—Illustrating the types of end-wall found in the vessels in radial longitudinal section. In a and 6 the end wall is of the imperfect perforate type. At c is shown a typical porous perforation in a vessel, which shows multiseriate pitting on the vertical wall. x 280. The medullary rays are numerous and diffuse, heterogeneous and without exception uniseriate or biseriate. The vertical height of the ray is also a definitely characteristic feature. They are relatively short. The biseriate type of ray is predominant and in tangential section generally contains 20 to 30 cells (Text-figs. 3 and 5 and Fig. 4 Plate vi). These rays are therefore about 10 and 15 cells in height. The two rows of cells, comprising the width of the ray in tangential view, alternate. The uniformity of the width of the ray is one of the most interesting features of the stem. The individual cells have a vertical height of 0:02 mm. and are approximately 0:07 mm. in radial length (Text-fig. 6). In 118 DICOTYLEDONOUS FOSSIL WOOD FROM ULLADULLA. tangential view they appear rounded with an average diameter of 0:02 mm. A large amount of black carbonaceous matter is present in the ceil cavity (Fig. 4 Plate vi). In places the pits on the walls of these cells may be distinguished in the radial longitudinal section. They are more or less rounded and simple. The walls of the ray cells contiguous to other ray cells are thick and are pitted in the same manner. These pits could be observed in section as well as in surface view (Text-fig. 6). Text-figure 5.—Representation of portion of the tangential longitudinal section of the autumn wood showing an abundance of wood parenchyma series. x 165. Systematic Position. Our knowledge, at present, of the systematic anatomy of the dicotyledonous stem is meagre. On this account the affinities of a fossil stem may be satisfactorily determined, only when very distinctive features are observed. Fliche,” Lignier,“ Stopes and Fujii,“® Stopes,°® Krausel,“® Bailey,™ and Edwards, have described dicotyledonous stems from the Cretaceous and Tertiary in other parts of the world. Hach of these authors has named the fossils described, after the woods of the living genera, which they most closely resemble. In this way the affinities of the specimens have been indicated. In the case of the Ulladulla fossil it has been found that the structure indicates an affinity with a certain Natural Order and not with one particular genus. There is a very close resemblance between the woods of the various genera of this Natural Order. On this account it is not possible to select one genus, which has a preeminent affinity with the fossil. The writer therefore has not followed the precedent established by the authors quoted above, but deems it wisest only to indicate the apparent systematic position of the specimen. The characters of every Order upon which information is available“ have been carefully considered. Representatives of certain orders show similarities to the fossil but differ in important details. Types of the Schizandreae group of the Magnoliaceae, for example, possess a very similar combination of wood structures, BY C. BARNARD. 119 but differ in the fact that the medullary rays characteristically have a great vertical height. Certain genera of the Natural Orders Bixineae, Euphorbiaceae, Anarcardiaceae, and Rutaceae have somewhat similarly constituted woods. These particular genera, however, are not represented in the present-day Australian flora. As a most striking resemblance is evident between the wood of the fossil and the woods of an Order, which is widely distributed in Australia, it seems that the similarities referred to above may be disregarded. The writer has examined figures, descriptions or actual sections of repre- sentative woods of most of the natural orders found in Australia. The Saxifragaceae alone possess the same type of wood structure as that exhibited by the fossil. The combination of wood structures, which are characteristic of this Text-figure 6.—Diagrammatic representation of a radial longitudinal section. All the features depicted may be clearly observed in certain places in the sections. The heterogeneous nature of the medullary ray is shown and the nature of the pitting on the various elements. x 280 approx. order, seems to be identical with the combination of structures present in the fossil. The regular radial seriation of the vessels, the occurrence of scalariform perforate end-walls in the vessels, as well as the narrow, heterogeneous, and uniform medullary rays are characteristic features of the woody genera of this order. For these reasons the writer tentatively places the Ulladulla specimen in the Natural Order Saxifragaceae. I am indebted to Mr. Welch, of the Technological Museum, for allowing me to examine photo-micrographs of the woods of certain representatives of this order, 120 DICOTYLEDONOUS FOSSIL WOOD FROM ULLADULLA. which I could not easily obtain in the living state. Weinmannia, Ackmana, Schizomeria, Quintinnia, Callicoma, and Ceratopetalum show a remarkable resemblance to the fossil. In the case of Ackmana the structures were almost identical. In conelusion, I wish to thank Professor A. A. Lawson for advice in the preparation of the text, and Mr. Welch for the above-mentioned assistance. I am indebted also to Dr. Carl Boesen and Mr. R. Murray, B.Sc., for the photo- micrographs reproduced. Summary. 1. The specimen described was obtained from the “Silica” beds at Bannister Head, near Ulladulla, on the South Coast of New South Wales. These beds are of Lower Tertiary age. 2. The specimen is a piece of silicified secondary wood. 3. The structure of the wood is that of a typical dicotyledon, and shows a very close agreement with that of the Natural Order Saxifragaceae. The author tentatively places the specimen in this Order. I have endeavoured to represent the nature of the individual elements accurately though a certain latitude has been taken in making the drawings. In Text-fig. 2, for instance, the medullary rays have been omitted in this radial longitudinal representation in order that the vessels may be seen more clearly. Further a uniform state of preservation is not present throughout the specimen; and irregularities in preservation render it impossible to depict the true character of all the elements in a drawing with the camera lucida. The less obvious details of structure in the various elements may not all be observed in one place in the section. For these reasons it was thought advisable to draw together features which could be definitely recognized into two diagrammatic figures (Text-figs. 1 and 6). References. ® Barttey, I. W., 1924.—The Problem of Identifying the Wood of Cretaceous and later Dicotyledons. Annals of Botany, Vol. 38. ® Brown, IpA, 1925.—Some Tertiary Formations on the South Coast of New South Wales—with special reference to the age and origin of the so-called Silica rocks. Proc. Roy. Soc. N.S.W., Vol. LIX. @ DEANE, H., 1902.—Geol. Survey Victoria, Vol. I, Part I. (4) —_______. 1902.—-Notes on Fossil Leaves from the Tertiary Deposits of Wingello and Bangonia. Records of the Geol. Survey, N.S.W., Vol. VII. ©) ETTINGHAUSEN, C. VON, 1888.—Contributions to the Tertiary Flora of Australia. Memoirs Geol. Surv. N.S.W. Pal, Series No. 2. ® Epwarps, W. N., 1925.—Report on Fossil Wood from Somaliland. Pal. Section, Botanical Abstracts, 1925. @ FLIcHE, P., 1905.—Note sur des bois fossiles de Madagascar. Bull. Soc. Geol. France, Ser. 4, Vol. 5. () Harper, L. F., 1916.—Annual Report, Dept. of Mines, Sydney. (9) ________, 1918.—Annual Report, Dept. of Mines, Sydney. ao) ________. 1924,__Dept. of Mines, Sydney, Geol. Survey. Bull. No. 10. Silica. GD JOHNSTON, R. M., 1885.—Proc. Roy. Soc. Tasmania. G2) ________, 1 §89.—-Proc. Roy. Soc. Tasmania. G3 KRAUSEL, K., 1924.—Reference in the Palaeobotanical Section of the Botanical Abstracts, 1924. “4 LIGNIER, 1907.—Vegetaux fossiles de Normandie, Bois dive. Mem. Soc. Linn. Normandie, Vol. 22. 45) Nopes, DorotHy, 1922.—A Preliminary Note on Fossil Woods from some Australian Brown Coal Deposits. Vrans. and Proc. Roy. Soc. S.A., 46. BY C. BARNARD. PAL a6) SAHNI, B., 1920.—Petrified Plant Remains from the Queensland Mesozoic and Tertiary. Queensland Geol. Survey Publication, 267. G7) SOLEREDER, H., 1908.—Systematic Anatomy of the Dicotyledons. Trans. Boodle and Fritsch, 2 Vols. a8) Stopes, MARIE C., and Fusir, K., 1909.—Study on the Structures and Affinities of Cretaceous Plants. Phil. Trans. Roy. Soc. London, Series B, Vol. 201. ao) Stopes, Marig C., 1915.—The Cretaceous Flora. Part 2, Lower Greensand Plants of Great Britain. Cat. of Plants of the Mesozoic in the Brit. Museum. @o SUSSMILCH, C. A., 1923.—Presidential Address, Proc. Roy. Soc., N.S.W., Vol. LVIII. EXPLANATION OF PLATES Vand VI. Plate v. 1. Photo-micrographic representation of portion of the transverse section. The vessels are clearly seen and in places the wood fibres are visible. Fibres are well shown at a. The cellular structure of the numerous and narrow medullary rays is not distinguishable. These cells are filled with carbonaceous material. x 200. Photo-micrographic representation of radial longitudinal section. The principal feature is a large vessel showing a large terminal porous perforation and multi- seriate pitting on the lateral wall. The wood fibres may be seen and also indications of the medullary rays, which are poorly preserved in this portion of the stem. x 200. bo Plate vi. Photo-micrographic representation of a radial longitudinal aspect showing two large vessels with porous perforations. Medullary rays are seen crossing the vessels. On the lateral walls of the vessels portions of the scalariform type of sculpturing are discernible. x 200. 4. Photo-micrographic representation of the tangential longitudinal section. This shows the medullary rays. At aa series of wood parenchyma is evident. x 200. (J) P ON A CASE OF NATURAL HYBRIDISM IN THE GENUS GREVILLEA [N.O. PROTEACEAE]. By C. T. Musson and the late J. J. FLrercHer, M.A., B.Sc.? (Plate vii.) [Read 30th March, 1927.] In the Abstract of Proceedings dated 30th July, 1913, is given a short account of a case of hybridism between two species of Blue Mountain Grevillea by the late Mr. J. J. Fletcher. He contended, with many facts, much detail and a large range of specimens, that G. Gaudichaudii, R.Br., consists of a series of transitional forms between G. laurifolia, Sieb., and G. acanthifolia, A.C. That the entire series known as G. Gaudichaudii is a series of variable naturally related forms, explain- able only as being hybrids between the two other species mentioned. That the two parent-species are markedly contrasted in most of their morphological characters, in their habit: of growth, in being members of two different plant associations, consequently in their habitats; cross-pollination being possible, how- ever, by reason of comparative proximity, and because the racemes of both are of the same pattern (elongated, secund and centripetal); moreover, the conditions favouring cross-pollination arise only at or close to the boundary between their respective habitats; consequently they are usually found in company with one or other, or both the parent-forms. G. Gaudichaudii has no specific characters; being of mixed origin, the characters are inherited, being blends or mixtures of those of the parent-forms. They are the first Australian, Proteaceous. wild hybrids recorded. They are not infertile, but they rarely reproduce themselves, because likely to be overlooked by visiting birds (the natural agents in pollination) or are likely to be pollinated from one of the parent-forms. (C.T.M. and J.J.F.) Historical. During the stay of the French corvette Uranie, engaged in a scientific voyage round the world, in command of Captain Freycinet, in Port Jackson, in November and December, 1820, Gaudichaud, the botanist of the expedition, made a fruitful excursion to Bathurst. Among the most important botanical additions to his collection was a rare, undescribed Grevillea, probably the only plant of its kind seen by him. It was obtained on the Blue Mountains, at “Vallée de Jamison.” ‘This paper is the outcome of an examination of extensive notes on the subject left by the late J. J. Fletcher and has been prepared for publication at the request of Mrs. Fletcher. Having had the opportunity to assist in the field work, knowing Mr. Fletcher’s views, having examined the species in the field and worked over the collected specimens, I can endorse fully the detail and conclusions given. Except where indicated, this paper is copied directly from Mr. Fletcher’s notes.—C. T. Musson. BY C. I. MUSSON AND J. J. FLETCHER. 123 But Gaudichaud did not go far enough from the Western Road to see the Jamison Valley which, at that time and for long afterwards, was inaccessible from the main road. What he means, we may fairly well conclude, was the little valley and its tiny rill of water visited by C. Darwin.* (It seems quite probable that Gaudichaud when at The Weatherboard on his way to Bathurst teok advantage of the short time at his disposal to take the (probably) one walk that presented itself, and which was later taken by C. Darwin. This is an interesting conjecture, and is quite likely correct, for in those early days there were no side roads opened up and any visitor would doubtless be directed, when the coach stopped at The Weatherboard, the old name for Wentworth Falls, to the one track, apparently between what is now known as King’s Tableland, and the more westerly spur at the end of which now exists the Wentworth Falls Hotel. The tiny creek runs approximately south from the township and falls over the cliff as described by Darwin. Gaudichaud could not have collected his plant in the Jamison Valley; but on the high ground overlooking it; somewhere along the valley mentioned above.—C.T.M.) On his return to Paris, Gaudichaud gracefully presented a portion of his specimen to Robert Brown, who subsequently described it in the Suppl. Prod. (1830) under the name of G. Gaudichaudii, R.Br. In the meantime the scientific records of the voyage of the Uranie had been in preparation and Gaudichaud wished to include 2 description of his new Grevillea in the botanical part of the work, which was eventually published in 1826. This description, the earliest to be published, is usually quoted as if it were R. Brown’s. From a comparison, internal evidence shows it is evidently Gaudichaud’s own description that he gives. Brown may or may not have sent him a copy of his proposed description. But as Gaudichaud’s specimen was not exactly a duplicate of the one he had parted with, and he wished to figure it, he evidently described his own specimen, adopting R. Brown’s name. Forty years later Bentham redescribed G. Gaudichaudii more fully than had his predecessors (Fl. Aus., V, p. 488); but unfortunately for those who came after him, he apparently did not see R. Brown’s specimen, nor specimens like them and in drawing up his description he omitted to make provision for any but his own. The consequence is that both the status and the identity of G@. Gaudichaudii are left in doubt. If we are to take Bentham’s description as the standard for deter- mining G. Gaudichaudii, then the specimens of R. Brown are not that species, and we are given no clue as to how they are to be disposed of. It seems remark- able that Bentham apparently did not himself realize this anomaly. Modern Details. At the meeting of this Society in July, 1910, in response to an invitation issued at a previous meeting asking members who had collected, or who had in their possession specimens of G. Gaudichaudii, four members brought specimens, some 2“Tn the middle of the day (1844) we baited our horses at a little inn called The Weatherboard. The country here is elevated 2,800 feet above the sea. About a mile and a half from this place there is a view exceedingly well worth visiting. Following down a little valley and its tiny rill of water, an immense gulf unexpectedly opens through the trees which border the pathway, at a depth of perhaps 1,500 feet. Walking on a few yards, one stands on the brink of a vast precipice, and below one sees a grand bay or gulf. . . . About 5 miles distant in front, another line of cliffs extends, which thus appears completely to encircle the valley.’-—Darwin’s Naturalist’s Voyage Round the World, 1889, p. 523. 124 NATURAL HYBRIDISM IN GENUS GREVILLEA. of them from the Botanic Gardens Collection. The joint collection then exhibited was, almost certainly, the best at the time in Australia. Three collectors had obtained plants which answered to the descriptions of Brown and Gaudichaud; but no plant was produced which corresponded with Bentham’s description. Since ‘then I have devoted my brief holidays to the further study of these plants under natural conditions, and have now (1915) a much better collection than that exhibited in 1910; but I have not yet found a single plant to which Bentham’s description will apply. Nevertheless I raise no doubt as to the correctness of Bentham’s descriptive details, though I think one of his inferences was made under a misapprehension, due to want of knowledge not determinable from the examina- tion of herbarium specimens alone; and that this is open to correction. I believe I am now in a position to offer a solution of the difficulties which arise from the conflicting descriptions. The Conflicting Descriptions. The three descriptions mentioned, together with a note by Mr. J. H. Maiden, which was not intended to be descriptive but to put on record some observations of the late Mr. W. Forsyth! on living plants, comprise all the literature about G. Gaudichaudii available.” Brown refers to some MS. notes of Allan Cunningham’s, at the end of his description in which the species is referred to under the MS. name G. acanthifolia var. quercifoliae. Unfortunately Cunningham’s notes were not published. There is no mention of the species in his “Specimen of the Indigenous Botany of the Mountainous Country between Sydney and Bathurst” (Field, 1825), though G. acanthifolia was first described in this paper; or in any other of his published writings as far as I know. Dr. Woolls and Baron von Mueller, as far as I can ascertain, never found any occasion to refer to it. In order, therefore, to make clear how some specimens I have now collected come in, in an important way, I preface an account of these with a brief statement of the whole case, based chiefly upon a comparison of the descriptions of G. Gaudichaudii by Brown, Gaudichaud and Bentham, supplying necessary comments. Though not first in chronological order, I begin with R. Brown’s description. One minor correction needs to be made, otherwise the description is satis- .factory as far as it goes; having no knowledge of the habit of G. Gaudichaudii, he naturally took the spikes to be erect. The plants are prostrate, as pointed out in Mr. Maiden’s note, and the spikes are more or less horizontal as in G. laurifolia; and, as in that species, frequently rest upon the ground. From a comparison of the descriptions of G. Gaudichaudii and G. acanthifolia, it is evident that R. Brown considered Gaudichaudii to be distinguishable from acanthifolia by the scattered appressed hairs on the underside of the leaves, by their simpler lobing, by the presence of an intra-marginal vein, by the racemes not being so dense and by the perianths having less clothing (sericeous as compared with very villous). The term sericeous, however, in the specimens I have seen applies only to the white silky hairs; but besides these there is some hairiness tinged with the colour, dark crimson, of the perianth as in G. laurifolia. If the white silky hairs could be removed the perianth would not be glabrous. 1 These PROCEEDINGS, 1904, p. 749. 2 Written between 1913 and 1918. BY C. T. MUSSON AND J. J. FLETCHER. 125 From my point of view, the condition in question is the result of a mixture of the corresponding characters of G. lawrifolia and G. acanthifolia when these two species are crossed. One other point, the lobes of the pinnatifid leaves are described as entire, a character in which R. Brown’s specimen differed from that described and figured by Gaudichaud. Portions of plants showing this character may be procured without difficulty, but in all plants of the Gauwdichaudii group (see ii below) that I have seen, if all the leaves are examined, some of them will be found to offer indication of secondary lobing. Brown’s and Gaudichaud’s specimens may, there- fore, have been different portions of the same plant, and yet offer the differences recorded. Finally R. Brown definitely recognized that the racemes and flowers were not exactly like those of G. acanthifolia. Turning to Gaudichaud’s description (he saw both species in the living condition), it is evident he did not copy the descriptions of Brewn, but drew up his descriptions independently. He recognized, like Brown, the differences in the indumentum of the leaves, in the lobing of the leaves, in the clothing of the perianth (sericeous in one case, tomentose in the other), but he used the wrong adjective in both cases in describing the pistils; the styles are glabrous in both cases, but the ovaries are villous in both cases. A very interesting and important omission, however, is that of the presence of the intra-marginal vein. If he had had the opportunity of seeing the leaves of G. laurifolia (which he apparently did not collect), its presence might have struck him. From this omission, and the mistake about the pistils, as well as in other small details, it seems clear to me, that R. Brown did not write this description, and that in all probability Gaudichaud did not see a copy of R. Brown’s before his own was published. He gives a good figure of a portion of a stem or branch with nine leaves, having 5, 7, 8 and 9 lobes; and two spikes which are evidently not exactly like those of G. acanthifolia; whilst the ovary is correctly figured as villous (Frey. Voy. Bot., p. 443, and Plate 46). Turning now to Bentham’s description it appears that the plants to which it applies are not known to local collectors; it may be that they are a second cross between one of the ordinary forms and a hybrid. Some Indirect Evidence. In the neighbourhood of Sydney it is easy to find plants of two or more different species of Grevillea flowering at the same time and fruiting freely, growing close to each other under conditions apparently quite favourable to cross- pollination by nectar-seeking birds. Nevertheless transitional forms between such species have never been reported. They do not seem to be produced in the cases examined, apparently for reasons given below. For some years I have had an excellent opportunity of periodically inspecting an extensive crop of thousands of specimens of the two species G. sericea and G. buczifolia, the former more numerous than the latter, crowded together on a ridge overlooking the Lane Cove River, 200 to 300 yards wide, it terminates abruptly on the east. Half a mile west the Hawkesbury sandstone is overlaid by Wianamatta shale, with a corresponding change in vegetation. This ridge was swept by a destructive bush fire on 2nd January, 1909, a phenomenally oppressive day with hot westerly wind. In due course, after rain had fallen, seedlings came up in great profusion, especially so Grevilleas, which grew rapidly, got ahead of the more slowly growing plants and temporarily took charge of the area. So 126 NATURAL HYBRIDISM IN GENUS GREVILLEA. numerous were they that one could walk down one side of the ridge and up on the other or zig-zag in any direction and yet keep one hand on one or more plants all the time. The two species mentioned were flowering side by side, their branches overlapping, so that the racemes of one were sometimes only a few inches from the other. Seven capsules to a raceme were quite a common occurrence. The plants are so different that they are readily distinguishable at sight at any stage of growth. I was interested in the renascence of the vegetation on this circum- seribed spot, having had the Grevilleas continuously under observation from the time they were seedlings, yet I never succeeded in finding a single plant that was not certainly determinable as one or the other. There appeared no evidence whatever of any kind of successful hybridization, nor was there, as far as I have observed, in a fresh crop of seedlings that came up. I am therefore led to conclude that the Honey-eaters cannot cross-pollinate them. Elsewhere G. punicea and G. buaxifolia, G. sphacelata and G. sericea; and on the lower part of the Blue Mountains G. nhylicoides and G. parviflora, may be found growing together under conditions which seem to be favourable for crossing, but apparently without any such result. It may be that the pairs of species enumerated are infertile, inter se; that is a matter for experimental investigation. There is another possible explanation, which may he the correct one. Reference to the Flora Australiensis shows that the species of every pair referred to are placed in different sections of Bentham’s Table; in other words the racemes are of different patterns or there are structural peculiarities of some sort present in one and not in the other. The result probably being, that a nectar-seeking bird visiting the flowers of one species may carry the pollen away from flowers on one part of the head, their position not matching with that of the receptive stigmatic surface of the other species. The result would be that cross-pollination of other flowers in the same or in other racemes of one type could take place, whilst in other species with raceme types differing it could not be effected. Experimental investigation into these interesting details is much to be desired. At present we have little or no data for consideration. (It has been observed that Honey-eaters commonly make a practice of com- mencing with the lower flowers of a raceme, working upwards. This would favour cross-pollination in the case of laurifolia and acanthifolia, as in both species the flowers open centripetally. In the case of sericea and buzifolia, one opens centrifugally, the other centripetally, a fact which would tend to prevent crossing.— C.T.M.) Some Detail as to the Three Species from Fresh Specimens, 1913. G. laurifolia (Plate vii, fig. 1.) G. laurifolia (Plate vii, fig. 1) belongs to the xerophytic plant association which successfully occupies the poor soil of dry situations in the Hawkesbury Sandstone series (approximating to the Bunter Sandstone of the Trias). It certainly occupies some very dry positions on the ridges or on more level areas on the top of the tableland, where the ground must be so sunbaked and hard in droughty summers, that when heavy rain falls comparatively little can be stored as it runs away so rapidly. On the other hand mountain mists, which are not infrequent, may be helpful. These plants are prostrate in habit, with several radiating procumbent stems arising from a thickened base. These stems are often 8-10 teet long, wiry and flexible, and readily made up into a small coil (except when very old); they are BY C. T. MUSSON AND J. J. FLETCHER. sey well branched and very leafy, forming carpets lying close to the ground. In very old plants the basal thickening forms a large knob and the stems arising from it may be an inch in diameter or more for some feet from the base. The leaves haye a characteristic venation and indumentum, and cannot be mistaken for any other local plant. They are distinctly thicker than those of G. acanthifolia. Petiolate, entire, they vary a good deal in shape and size, according as they are well exposed to the light, or shaded by grass, shrubs or trees. They may be ob-lanceolate, long and narrow, short and broad or broadly ovate, even almost circular, and mucronate. Glabrous above when adult, very young leaves and shoots are thickly coated with a mixture of silky white and ferruginous or reddish appressed hairs lying very close together. Those of the upper leaf surfaces are soon lost. Except the midrib the under surface is thickly coated with silky white hairs lying close together and doubtless of use in checking trans- piration as well as serving to protect the stomata from dust, or soil washed down by rain. The veins are very conspicuous, nearly parallel on each side of the midrib. They end distally in a characteristic well-marked intra-marginal vein. The perianth tube, viewed from outside, has much more colour than in G. acanthifolia, and this is all the more evident because most of the appressed hairs clothing the tube are dark crimson or ferruginous, only a few white hairs being mixed with them. The hairs appear as if plastered down, not merely appressed. Racemes of very young unopened buds, with the bracts in situ, may have the globular limb, and that part of the limb not hidden by the bracts, ferruginous or rusty; or they may be turning crimson, though with a distinctly ferruginous tint on the globular limbs. The bracts are yellowish, coated with yellowish or rusty and white hairs. The rhachis is also thickly coated with short crimson, ferruginous or rusty appressed hairs. As the tube dries the colour some- times becomes almost magenta. In still older buds in which the bowed style has not yet begun to protrude from the flowers, the tubes of the perianths, and the pedicels, are more distinctly crimson, but the globular limbs are still ferruginous, to the naked eye contrasting in colour. The rhachis may have more evident crimson hairs mixed with ferruginous or rusty hairs; while the bracts may be yellowish, or tinged with crimson near the base or over the greater part of their surface. In still older racemes, in which the bowed styles of the lowest flowers are protruding, there is still a noticeable contrast between the colour of the tubes, and of the globular limbs; and so much of the inner surface of the limb as is exposed, is seen to be edged with dark crimson, in still older flowers changing to purple. This may be confined to the free edge of the split perianth leaving a yellow gutter between, or the whole of the exposed inner surface may be purple, becoming darker as the flowers mature; eventually fading to some shade of dark red in dried flowers. In mature flowers the globular limb and tube still show the difference— crimson—ferruginous. The pedicels are same colour as the perianth—rusty. In some racemes the flowers remain ferruginous without change, in others one-half longitudinally is crimson, the other ferruginous. Stipes of the ovary is longer than in G. acanthifolia. Styles lighter crimson, stigmatic disc green, sometimes crimson. Freshly exposed pollen is bright yellow and floury, contrasting strongly with the crimson. Hairs on the-ovary and the stipites not so numerous as in G. acanthifolia, usually white mixed with crimson, or they may be nearly all crimson with just a few white. I think the hairs of the tomentum are correctly described as appressed all over (on tube and limb). The perianth and globular limb split on the lower 128 NATURAL HYBRIDISM IN GENUS GKEVILLEA. side (Bentham), the latter nearly to the base to allow the exit of the pollen- carrying disc, while the two laminae of the limb usually cohere on the upper side. When exposed in this way the inner surface is purple or there is a purple stripe on each side with an intervening longitudinal yellowish area along the coherent margin extending for some distance below the revolute limb but not to the base. The purple colour is evanescent, changing to dark crimson. G. acanthifolia. (Plate vii, fig. 6.) é This species is tolerant to any amount of water applied to the roots; it belongs to a mesophytic assemblage of plants which flourish in wet swampy areas mainly caused by soakage from springs. Such areas are noticeable from a distance because of the absence of trees, and their green appearance. ‘They are often mentioned by early explorers as they offered chances of feed for their horses or bullocks when there was nothing to be had elsewhere. They occur at different levels, frequently on the slopes of shallow valleys or bordering creeks,’ sometimes they surround small islands of drier ground on which a few trees may occur. They are to be found only in the upper portions of the tributary valleys of the Grose and Cox rivers. Further down the valleys are enclosed between precipitous cliffs, and this, with absence of sun, profoundly alters the conditions for plant life. In very dry seasons these areas dry up on the surface and are often burnt over. If the Grevilleas are only well scorched, the portions above ground die, but after sufficient rain they again send up shoots from the thickened base. G. acanthifolia also flourishes on the banks of creeks, close to the water; and it is not unusual to see some of the main roots actually trailing in running water. It occurs also in depressions near and along the course of creeks, supplied from the overflow after heavy rains. It sometimes occurs in unusual situations. I have seen one flourishing on the side of an apparently dry embankment leading to a bridge crossing a creek, and growing close to a plant of G. laurifolia. Possibly when rain falls the embank- ment is capable of absorbing more moisture than one might expect; perhaps much more than the sun-baked virgin ground which had never been stirred by spade or plough, but in which Jauwrifolia can flourish. Notes on Fresh Specimens, March and November, 1918. Leaves: Trifid leaves sometimes subtend an inflorescence. Have seen 3-19 lobes; intermediate numbers commonest. There is an intra-marginal vein (or perhaps an epidermal thickening) to the lobes, but it is not visible on the under- surface; nevertheless, when held up to the light, it is visible like the ordinary veins (anatomical examination is wanted here). Seedling leaves, and leaves of side shoots, also the lowest leaves near the ground, of adult plants have relatively much more lamina, and are more easily pressed flat, not being so rigid. Shoots: Young shoots, and unexpanded young leaf-masses, are coated with white silky hairs on both sides but not the upper surface of the young leaves, as in G. laurifolia. This is net mentioned in the Flora Australiensis. Spikes: Not truly secund at first, when young there are bracts all up the rhachis (or all round). That is on the back, or the inner side not exposed and facing the stem. As the flowers expand, they reach out towards the light; but even then there are bracts on the back. 1This is what A. Cunningham means when he says of this species that its habitat is “wet, peaty bogs on the Blue Mountains.” BY C. T. MUSSON AND J. J. FLETCHER. 129 Flowers: In very young spikes, before the styles protrude, the flowers, like the exposed surface of the bracts and the rhachis, are silky white, due to the hairs, and show no colour, or very little. The bracts are greenish or yellowish green on their inner surfaces. The bowed styles are rich pink; before they appear a little colour shows in the perianth, but it is masked by the silky hairs. In older spikes, it is to the massed styles the colour of the spikes is chiefly due, as seen from a distance, a fact not usually recognized. As the flowers mature, the colour of the styles fades to a lighter pink. At any time, viewed from outside, the perianths show but little colour. But when the styles are nearly ready to straighten, and afterwards, the inside of the perianth, viewed from front or above, is a rich purple (sometimes looking almost black), fading to »yurplish red in dry (herbarium) specimens. It fades considerably and what is left appears as longitudinal streaks (about ten). In herbarium specimens the colour of the inside of the perianth is perhaps more noticeable than in the fresh state; possibly due to disarrangement and flattening of the silky hairs in the process of drying. The perianth limb looks greenish outside, notwithstanding the coating of white silky hairs, this silky indumentum being most conspicuous. The hairs are appressed, projecting and rather tufty on the revolute limb; after the stigmatic disc has been released they appear as a very noticeable tuft on each side of the expanded revolute limb. The tube of the perianth of young flowers in bud, bracts and rhachis all appear of the same colour when fresh. Flower pedicels are greenish (like rhachis and bracts) and coated with white hairs, when fresh. The pollen masses when freshly exposed on the stigmatic surface are pink, those of G. lauri- folia and the hybrid (G. Gaudichaudii) are bright yellow. The stigmatic discs are light green, fading to yellowish green. ; ni The Hybrids (Plate vii, figs. 2-5). Fresh flowers November, 1913. With the exception of one plant, I have not seen spikes and flowers of any of the Gaudichaudii series, that were not readily distinguishable from those of acanthifolia. But I have had the great advantage of examining fresh as well as dried flowers. Plants of Section i have flowers and spikes like G. laurifolia, a little lighter in colour in some, but still some shade of crimson, with the same notice- able contrast between the tube and the globular limbs of the perianth (crimson as compared with ferruginous), but with a noticeable increase in the white silky hairs on the tube giving this a sericeous appearance. The inner surface when exposed purple. Plants of Section ii show a good deal of difference in the amount of colour in the perianth, some having very little (not more than in acanthifolia) when growing covered up in the shade, except as regards the purple inner surface, when the styles are hardly darker than those of acanthifolia. In others there is more diffused colour, lighter than in laurifolia, the exposed inner surface purple, when the limb and tube split. The pedicels are green as in acanthifolia, but what readily distinguishes them from that species is the admixture of white and crimson hairs on the limb, and white and ferruginous hairs on the globular end. The tomentum as a whole is also more copious and longer on the globular end. Even in dried specimens the contrast is strikingly obvious. The rhachis and bracts are also distinguishable from their rusty appearance due to the admixture of white and rusty or ferruginous hairs. This admixture of the different kinds of hairs on the flowers, rhachides and bracts is perhaps one of the best examples of mixed characters in these hybrids; apparently analogous to the case of hybrid roses between parents having either glandular or non-glandular hairs, mentioned Q 130 NATURAL HYBRIDISM IN GENUS GREVILLEFA. by Kerner.1 The tomentum, as a whole, is more copious than in laurifolia, but ~ less so than in acanthifolia; the hairs are somewhat longer than in laurifolia, not quite so long as in acanthifolia. The hairs on the ovary are more numerous, and the tuft is denser than in lauwrifolia, being very -like acanthifolia, but in many cases there are a few crimson hairs mixed with the white. Classification of Hybrids (G. Gaudichaudii). The series of hybrids met with, comprises recognizably different types of individual plants. The series, as known to me (J.J.F.) is divisible into two sections according as the plants have entire mixed with pinnatifid leaves, or all leaves are pinnatifid, as in G. acanthifolia the number of leaf lobes is not constant. With this difference in leaf character there are correlated certain differences in flower character. Fresh flowers are only available during the summer months, whereas plants may be seen in leaf through the year, therefore the leaf characters most readily catch the eye. I have had specimens, illustrating a series of stages commencing with laurifolia and ending near acanthifolia, whilst the reverse could also, neces- sarily, be illustrated. A short account of various types will show how the characters of the parent species are blended, also indicating something of the variations to be seen, pointing conclusively to their hybrid nature. Section i: Prostrate plants with procumbent stems. Entire leaves altogether of the laurifolia type, mixed with pinnatifid leaves with lobes numbering up to 9, all the lobes entire. Flowers indistinguishable from laurifolia, or with more white appressed hairs on the tube of the perianth. Habit like that of laurifolia. A. Entire leaves most numerous with pinnatifid leaves usually having not more than three-lobes (very rarely four). Flowers and inflorescence indistinguishable from those of laurifolia. B. Entire leaves in a minority, pinnatifid leaves, up to five lobes; venation and indumentum of laurifolia; tube of perianth with more white hairs. C. Like B, but indumentum reduced to'a remnant of scattered appressed hairs occurring singly, so that underside of leaves is almost glabrous, much as in some plants of A. D. Entire leaves more reduced in number mixed with pinnatifid leaves, having 2-7 or any intermediate even number of lobes, indumentum well developed in some specimens. Section ii: Prostrate plants with procumbent stems, stiffer than in laurifolia, and not forming such leafy carpets. All leaves pinnatifid, with from 3-15 lobes (maximum and minimum not found on same plant). Some leaves with entire lobes, but in every plant seen, some bilobed. Three and four lobed lobes may occur, occasionally with bilobed on the same leaf. Indumentum very variable, well 1 The cellular structures produced from the epidermis of the stem and leaves which are differentiated as hairs, bristles, scales, glands et cetera, classed together as under the name of indumentum, are very constant characters in most species of plants. Hybrids exhibit the most varied combinations of the indumenta of their parents. In the majority of cases the characteristics of the two stocks in this respect are mixed, but less frequently they are united, and in the latter case the shape, size and number of hairs tra are intermediate between those of the appendages in the two parent species.’’— Kerner and Oliver, Nat. Hist. of Plants, p. 564. “Where one parent rose bears only non-glandular and the other only glandular hairs, the hybrid is sure to be clothed with a mixture of the two kinds of hairs.’’—Ibid., p. 564. “The colour of the flowers in hybrids is usually the result of a fusion of the colours in the parent species; less frequently it is a mixture of the original colours.’—Jbid., p. 567. BY C. T. MUSSON AND J. J. FLETCHER. ~ Bil developed and much reduced on the same plant. Intermediate in extent on others, or reduced generally, on the leaves to a functionless remnant of appressed hairs, singly scattered; recognizable but vestigial. No plant seen with under surface of leaves entirely glabrous. Fresh flowers with more white silky hairs on tube of perianth, hiding the colour and giving dried flowers a greyish appearance. On the revolute limb of the perianth the hairs are tinged with ferruginous or reddish colour. Capsules hardly distinguishable from those of acanthifolia. E. Leaves with from 3-11 lobes, the maximum of indumentum for this section, but it varies in amount on leaves of the same plant. F. (Here is G. Gaudichaudii R.Br.). Leaves with from 3-11 or 5-15 lobes, with a maximum of bilobing; indumentum recognizable but vestigial, reduced to a few scattered hairs. Perianth with the tube sericeous, the hairs on the revolute limb tinged with ferruginous or reddish. This is the type of hybrid most frequently met with. G. Leaves with 7-13 lobes (or any intermediate even number), with most (but not all) leaves having a maximum of secondary lobing; some tri- lobed, rarely four lobed. No five lobed lobes seen. Remarks on the Various Types of the Series. A. If the pinnatifid leaves are removed, it will pass as a specimen of G. laurifolia. If it were the only member of the series Known, it might be regarded as a sport, perhaps due to bud variation. Fine colonies of G. laurifolia carpeting considerable areas of ground may be found too remote from plants of G. acanthifolia for birds to pass directly from one to the other, but in such cases the plants show no tendency whatever to produce lobed leaves. Fourteen plants . of this type seen; from the conditions under which they were growing, I believe them to be seedlings from ovules of G. laurifolia fertilized by pollen of G. acanthifolia. One fine plant was growing in the midst of a carpet of G. laurifolia, and, except in one instance, the others were growing quite close to, side by side with and the branches overlapping, or a little lower down a slope than, one or more plants of G. laurifolia. In some cases they were the only hybrids to be found in the locality. In one case only was a plant solitary, and this must have been a case either of a seed having been removed further than usual from the parent form, or more probably was a plant whose former associates had been removed by fire or accident. B. Six plants have been examined. The finest example was growing on a grassy slope, well exposed to the sun, just below, several plants of G. laurifolia with plants of G. acanthifolia a few yards away at the bottom of the slope. Another was one of a row of four contiguous plants; the two middle ones were examples of type C. The remaining one of the four a fine example of type F. Two others were growing close to plants of G. acanthifolia and the sixth quite close to a group of plants of that species. C. Two plants only seen, the two referred to above. Both old, very dry and quite alike. Dried leaves appear almost glabrous, but the scattered hairs readily seen on fresh leaves. They had a very distinctive appearance. The leaves, even when fresh, were incurved at the edges in an unusual manner. The facies of these two plants suggested the idea that they were suffering from excessive trans- piration due to the loss of the indumentum. 132 NATURAL HYBRIDISM IN GENUS GREVILLEA. D. Three plants seen, all, I believe, seedlings from G. laurifolia. One was growing in the midst of a carpet of G. laurifolia, another was beside a plant of that species, the branches overlapping. The third was growing in a grassy glade, near some other hybrids, but with plants of both G. laurifolia and G. acanthifolia close at hand. BE. Two plants seen, both remarkable for the well developed indumentum and for its variable amount. One plant showed great variety of lobing in the leaves. The other was overshadowed by a plant of G. acanthifolia, and hampered in symmetrical growth by other plants. A well marked intra-marginal vein present. But for the indumentum, this plant was quite of the F type. F (= G. Gaudichaudii, R.Br.). The commonest type met with, about fifty plants seen. Not only is this the type most frequently produced, but in my opinion it is the reciprocal hybrid. Solitary plants were seen in the midst of carpets of G. laurifolia; others were seen growing close to, even overshadowed by, a plant of G. acanthifolia. Others were growing on slopes between G. laurifolia above and G. acanthifolia below. On the whole they are most frequently situated near plants of G. laurifolia. Mr. Forsyth noted this close association with G. laurifolia, but without realizing its significance. The reason, as one can see, is that when the birds: travel up the valleys visiting G. acanthifolia in the swampy lower parts first, and come to the last of them, they very naturally visit G. laurifolia on the slopes above, if there is a display within sight. On the other hand, after visiting the Banksias, Lambertias, and other plants on the ridges and upper slopes they work down over the laurifolia areas until they reach the wetter lower slopes where acanthifolia flourishes; they may then pass direct from the former species to the latter. G. Five plants seen, two of them fine plants, one with stems seven feet long, growing in the midst of a carpet of G. laurifolia; another near a plant of type B, close to plants of both parent species. A fourth was growing between plants of the two parents. The fifth, a solitary plant, growing further from the parent forms than usual; but there was evidence of interference with the surface. Summary. Grevillea Gaudichaudii, R. Br. is a hybrid. The parents are G. laurifolia Sieb. and G. acanthifolia, A.C. The forms described by R. Brown, Gaudichaud and Bentham are representatives of naturally related forms, the result of hybridization; and fill places in a graded series between the parents. These plants are only found near one or both parents, along the Blue Mountains from Wentworth Falls to Blackheath. (The area west of this has not been searched.) The characters of G. Gaudichaudii, R. Br. are blends or mixtures of those of the parent forms.—C.T.M. 2 EXPLANATION OF PLATE VIL. 1. Grevillea laurifolia, Sieb. 2-5. Various forms of Grevillea Gaudichaudii. 6. Grevillea acanthifolia, A.C. 1The Spinebill chiefly. THE PHYSIOGRAPHIC AND CLIMATIC FACTORS CONTROLLING THE FLOODING OF THE HAWKESBURY RIVER AT WINDSOR. By Lestry D. Hatt, B.Se., Science Research Scholar in Geography, the University of Sydney. (From the Department of Geography.) (Plate viii, and nine Text-figures. ) [Read 27th April, 1927.] Introduction. Floods of the Hawkesbury River at Windsor have been part cf man’s experi- ence ever since the first farmers came and settled the rich alluvial flats along its banks in 1794. Records show that in recent years these floods have decreased considerably both in height and frequency, but the cause of the decrease is not definitely known. It may be due either to dam building on the headwaters of the river, or to an actual diminution in precipitation. In the following paper the effect of the Nepean dams on the floods of May and June, 1925, has been investi- gated in an effort to find a definite relationship between flood waters, water conservation and climatic conditions over the catchment area of the river. The term “catchment area” is used throughout to denote the entire area drained ‘by the stream irrespective of special regions reserved for water supply. So far as I am aware no work of this nature has been done for the Windsor district. Josephson, 1885, discusses the history of the floods of the Hawkesbury River, but makes no attempt to give their causes or to enter into the details of rainfall. David and Guthrie (1904), have investigated the nature of the Hawkes- bury River silts and their results are mentioned in this work. Information as to the position and capacity of the dams and the amount of water stored during the flood months, were kindly supplied by the Metropolitan Board of Water Supply and Sewerage; while other details concerning rainfall and run-off for the whole Windsor catchment area were contributed by the Water Conservation and Irriga- tion Commission. Thanks are especially due to Mr. French of this Commission for making these facts available and for his helpful suggestions and kindly assistance. Rainfall figures were given by the Weather Bureau and flood details were obtained from copies of the Windsor and Richmond Gazette of various dates, for which my thanks are due to the Editor who gave me access to his files. GENERAL DESCRIPTION OF THE HAWKESBURY RIVER. Three hundred and thirty-five miles in length, the river with its several large tributaries, drains all the immediate country to the north, west and south of Sydney, an area of approximately 8,000 square miles. It rises 20 miles from Goulburn. where it is known as the Wollondilly, flows generally northwards, and after receiving water from the Cookbundoon, Wingecarribee and Nattai streams, is Joined by Cox River from the western mountain region. From here it is known R FLOODING OF HAWKESBURY RIVER AT WINDSOR. 134 *SU0I7DIO ayo Jumy @ * $0772. — : S v ed “ a F NS ¢ x DE ~~. AE Sf os lo Mpajet : ee rae N . = CL uscd at, 2 Ni duties s EER G je isavod Vp Le ; fv) * + NOJLLAS c) b, Uy ;.. N5/ ue ei 4, \ 4) 2 5) s - oe f=a) Y, fy ef ford aes fs (=) z < = Zz, = ra) SHOALHAVEN ‘NOSMV 1 i : ® at eh £ ~ “MSBATU Go oe ; ‘SOA IW oS C8Ces <. 9109 HivaHoviad é ie KS \ ee J ye UY UV S.LN&A WHILVO SVAOWVIOVHUV MS ey io Vales S 49 NO TV VINO L IIA “16 Oe DN ; LNAOW ROO “Y ° %, yn AUVW @ MOLT en is : saAvo NVIONS.L é 53 Oo vary Ne eh 0 rks Dae men nncta, — }D oo One, S 2, veumtl é § 4¥O1VUVAL om i ey HN a ie ?®@ Nb usyaaegs TWLAY ne oe “he : r aoe fee a, ve BY LESLEY D. HALL. 5 as the Warragamba and flows through a deep gorge till joined by the Nepean near Mulgoa. The main river is now known as the Nepean and continuing northwards, is joined by the Grose a little above Richmond and by South Creek at Windsor. After the Grose junction it is called the Hawkesbury and is joined by two large streams, the Colo and the Macdonald, before reaching Wiseman’s elbow, where it turns eastward and finally enters the sea at the beautiful drowned estuary of Broken Bay. A consideration of the map, Fig. 1, will show that the headwaters of the river above Windsor may be divided into three systems, namely, the Wollondilly-Cox, the Nepean and the Grose, each of which has its own definite catchment area. The Wollondilly-Cox has a catchment area of 3,383 square miles including all the country drained by the Wollondilly, Cookbundoon, Wingecarribee, Nattai, Cox and Warragamba rivers. Part of the western warp, it is all highland, but varies eS Sys Roe WY, 2 RG Weanametlha =x) Permocarb = Hele rian Slates E-3] Shale. eel Oerces. fe] herts Limnestones Hawkesbur Devonian = Tgneous (u] [SCLC ES. WA Quar tj tes etc. <4 J eecieet Text-figure 2.—Sketch map showing the approximate geology of the catchment area of the Hawkesbury River above Windsor. somewhat geologically. The upper Wollondilly flows through a series of Palaeozoic rocks, so that its gorges are less striking than the huge canyons which have been cut in the Hawkesbury sandstone by the Cox. The lower Wollondilly, Nattai and Warragamba have also cut deep gorges in the sandstone. Thus the northern part of the catchment area is of a very rugged character making communication difficult. Within the area there is a comparatively small population and only a few large towns. Settlement has collected in three regions. On the Upper Wollondilly, beyond the limits of the sandstone, there is good agricultural land which supports a farming population. Goulburn, population 11,950, is an important inland town on the Great Southern Railway. Taralga is another large town in this district where grazing, dairy-farming and fruit growing are the chief industries. Good workable soil and a less rugged topography, have led to settlement in this area. 136 FLOODING OF HAWKESBURY RIVER AT WINDSOR. In the Bundanoon-Mittagong district is a series of small towns along the Southern Railway, well within the sandstone area and important only from the tourist and residential aspect. Among these are Bowral (2,640), Moss Vale (2,030), and Mittagong (1,440). Round Sutton Forest is some good grazing land due to the presence of basalt and the intrusive rock of the Gib at Bowral is important commercially. On the headwaters of the Cox are several towns the most important Of which is Lithgow (12,940). Here river erosion has caused the sand- stone to be worn away and the coal measure series to be exposed. Coal is mined at Lithgow and is the cause of the industrial prosperity of that centre. Other towns on the Cox catchment area are Mount Victoria, Katoomba and Wentworth Falls, all of which are tourist resorts. Except for these regions, juvenile dis- section and barren sandstone soils have prohibited settlement on the Warragamba catchment area. The Nepean.—On the headwaters of this stream 354 square miles of unin- habited country have been reserved for Sydney water supply. The catchment area is practically all Hawkesbury sandstone drained by the Nepean, Avon, Cordeaux and Cataract rivers. The maximum elevation is only 2,000 feet, so the river gorges are by no means as rugged as those of the western warp. Still the district does not invite close settlement and the small towns are mostly confined to the southern railway line. The presence of juvenile gorges at the headwaters of the streams and the absence of any close settlement were two factors in determining the choice of this site for the location of the water supply dams. The Grose has a catchment area of 250 square miles; a sandstone region of juvenile dissection and part of the western warp. Its deep canyons, wide gullies and barren hill tops prohibit all settlement except for towns such as Springwood, Lawson and Blackheath along the western railway, which are important tourist resorts. The waters from these three highland areas are discharged into a com- paratively flat region of Wianamatta Shale and lake silts; undulating: grassy country with hills not more than 200 feet above sea-level, which contrasts strongly with the sandstone highlands surrounding it on three sides (Taylor, 1923a). The Nepean leaves the southern warp at Menangle and meanders through the “fossil lakes” of Camden and Wallacia before again entering the uplifted region where it joins the Warragamba. The Camden district, therefore, is only liable to be flooded by Nepean water, which comes from a smaller drainage area than that which affects Windsor. The combined Warragamba and Nepean water is dis- charged on to the flats again at Penrith, causing floods here before it is joined by the waters of the Grose. The floods on the lowlands of Richmond and Windsor are caused by waters draining a total catchment area of approximately 4,840 square miles. At Cattai the river enters the northern warp and the flood waters are once more contained within the river valley. History oF Froops at WINDSOR. The Hawkesbury River is recorded to have flooded for the first time in 1799, doing much damage and causing great distress among the people of the young settlement. This flood ushered in a series from 1799 to 1801 and then the river was normal till 1805 when another series of floods commenced. The records of these early floods are not accurate and no attempt was made to ascertain to what height the river rose above normal. In 1808 there was another flood and the frequency and destructive power of these floods was the cause of much anxiety BY LESLEY D. HALL. “(PEZ6E ‘IOTAVT, UO paseq) roOATY AanqsayMeE ay} Aq poulvip AI}UNOD 9Y} JO 91N}eU OY} SUIMOYS weIseIP YooIq y—¢ eInSY-}xX9, OU POH 129g = em ; es Sr rT BRS Sty Sm = yy = PVPs} ne E jo us Suess aS ~*~ 243 casa (2S poe YY WORLS J/f VA Lat? Yyrl 4} ALITT —— Uy Vii) y Yy / Wy 2L/) Uy I, V pote, / Sip Nil) ay BLY é é Ye / YY Wie BRL € yy YU i elon GZ SU ee ee ge a Oe vA LEY, ey yy Be LD OO Prominin Yy We Ui de Z il Wy / & Y] Aly —— =n dy WSU 138 FLOODING OF HAWKESBURY RIVER AT WINDSOR. to the infant colony. Thus we find that the town of Windsor owes its origin directly to the necessity of constructing large granaries at higher levels in order to protect the produce from inundation. During 1811 a severe drought was experienced and was followed directly by another flood. Situated under the shadow of the great warp, the Windsor district does not receive a very high rainfall and droughts are fairly frequent, while the rain falling on the mountains will often cause floods of the river. These unsuitable conditions and the growth of the settlement made it imperative that the mountains should be crossed and more extensive pasture lands discovered. Between 1816 and 1819 three large floods occurred, then we have record of a series of smaller floods occurring at intervals until 1857 which marks the beginning of a wetter cycle. Three floods are recorded for 1860 followed by a small one in 1863 and a very large one in 1864. Three years SSE = —S= TES eg cena op 3 Sane a4 , ilbers } Ene eros gees © 1 See Se BEES An on 6 a = = ingula “-——~e= Text-figure 4.—Windsor Peninsula surrounded by flood waters, June, 1925. (Sketch from a Daily Guardian photograph.) later came the largest flood known to white men when the water rose 63 feet above summer level of the river, entered the town and left only two parts of it exposed as islands. The people had hardly recovered from this disaster when, in 1870 the river rose 15 times and flooded the flats five times. This was a record wet year at Windsor and the climax of the rainfall which had been increasing since 1857. From 1870 to 1879 floods occurred of smaller magnitude than the preceding ones, after which a drought period set in so that the river did not flood again till 1889. , For the next few years a good rainfall was recorded, but at the close of 1893 a drought began which lasted about fourteen years, although there were floods at Windsor almost every year between 1893 and 1900. Since that time the rainfall has been steadily decreasing and though some floods have occurred their height has been much less. In 1904 the river rose over 40 feet, a record which has not been equalled since. Dry years followed in which the rainfall for the year was below the average until 1910, when it started to increase and a small flood of 21 feet occurred. 1911, 1912 and 1913 had small floods without much rain in BY LESLEY D. HALL. 139 the Windsor district, then in 1915 heavy rainfall throughout the Hawkesbury watershed caused a rise in the river of 25 feet. October, 1916, witnessed a high flood of 35 feet 6 inches, followed by five years of drought which were broken by heavy rains in 1921, when the river rose 20 feet. From this time onwards the rainfall has been better, the flood of 1922 being a fairly high one. There is no doubt, however, that floods of the Hawkesbury have decreased considerably during the last twenty-five years. . In May, 1925, the water rose 25 feet, that is, about 2 feet over the Windsor Bridge, and a great many of the low-lying places were covered. The water only broke over the banks of the river in very low spots and, running up the gullies, inundated a good deal of land. In the flood of June the water was 15 feet above Windsor Bridge, or 37 feet 3 inches above summer level of the river, which is the biggest flood experienced since 1904. Many people on the lowlands were driven from their homes and it is estimated that damage amounting to between £40,000 and £50,000 was done in the Windsor district and approximately £30,000 round Richmond. All the country round Cornwallis, Freeman’s Reach, Pitt Town Bottoms, Wilberforce lowland, the Peninsula and the flats along South Creek were one vast sheet of water dotted here and there with the tops of houses and trees. Windsor was a complete island as the water backed up over the roads at the southern end of the town. The following is a list of the floods which occurred between 1795 and 1925 compiled from various sources: Height Height | Height above a above | above Year. Month. summer Year. Month. summer Year. Month. summer level, feet. | level, feet. level, feet. 1795 Jan. — 1857 Aug. 372 1889 May 383 1795 Aug. — 1860 Feb. 2632 1890 Mar. 38% 1799 Mar. 50 1860 Apr. 362 1890 Mar. 34k 1800 Mar. — 1860 July 342 1890 June 223 1801 Mar. — 1860 Nov. | 36 1891 June | 353 1805 Feb. — 1861 Apr. 274 nW23 a 123 ©) 6 263% 1805 Mar. — 1863 — — 1893 | Mar. 283 1806 Mar. 48 1864 June 48 1894 Mar. 318 1806 Cet. 3 1864 June 324% 1895 Jan. 302 1808 Nov. 20 1864 July | 36 1897 | Suly 22% 1809 May 48 1866 June 26 1898 Feb. 313 1809 Aug. 474 1866 | July 274 1899 Aug. 22 1810 July - 1867 Apr. 2 1899 Aug. 263 1811 Mar. — 1867 June 63 1900 July 46 1812 Mar. — 1869 May 362 1904 July 40 1816 June +52 1870 Apr. 45 1908 Aug. 15 1817 Feb. — 1870 May 358 1910 July. 21 1819 June 46 1871 May | 363 1911 Jan. 25% 1820 June — 1872 — = 1912 July 22 1821 Sept. — 1873 Feb. 413 1912 Aug. 24 1826 Jan. — 1875 June 38% 1913 May 264 1826 - Sept. — 1876 Sept. = 1913 May 20 1830 Apr. — 1877 May 30 1915 Jan. 25 1831 Apr. — 1877 May 20 1916 Oct. 354 1832 Mar. -= 1878 Feb. 262 TOI elle = 1833 | Apr. — 1879 | Sept. 433 1922 | July 31 1857 | July | 32h 1879 Sept. 342 1925 | May 25 1925 June 374 140 FLOODING OF HAWKESBURY RIVER AT WINDSOR. This list of floods records all those mentioned in the following references: (1) 1799-1819: Articles in the Nepean Times for June, 1925, entitled ‘126 Years Ago.” (2) Tebbutt: Catalogue of the floods and freshes of the Hawkesbury River and South Creek at the Peninsula, Windsor, New South Wales. 1855-1903. (3) “Results of Meteorological Observations at Mr. Tebbutt’s Observatory. 1898-1915.” (4) Results of Rain and River Observations. 1903-1908. (5) Windsor and Richmond Gazette. 1905-1925. (6) Josephson, J. P., 1885: ‘‘History of Floods in the Hawkesbury River.” Proc. Roy. Soc: N.S.W., page 97. RELATION OF FLOOD HEIGHTS TO YEARLY RAINFALL. Floods in the Windsor district come at all seasons and have been known to occur in almost every month although the winter months, May, June and July, are the most common (see graph, Text-fig. 5). No flood has been recorded for 7 a Floocls. S u Number of O Jan. Feb. Mar. Apr May June. July. Aug. Month OF Year. ept. Oct Nov. Dee. Jan. Text-figure 5.—A graph showing the number of floods occurring in each month of the year from 1795 to 1925. December and very few in October or November. Floods are caused by heavy Tain falling on the watershed of the river and are not affected by precipitation at Windsor. A fall of rain on the southern drainage area sufficient to cause floods is usually due to a cyclonic disturbance whose influence is felt all along the coast; thus it often has rained or is raining at Windsor during the rise of the flood waters. Cases have been known, however, when the river rose without any rain having fallen in the immediate district. The graph, Text-figure 6, shows the floods at Windsor in order of decreasing magnitude, with rainfall at Windsor for the corresponding years superimposed. It is obvious that the two lines bear no relation to each other. The third line shows the rainfall over the Nepean and Warragamba catchment areas, calculated as an average from the four stations, Goulburn, Taralga, Cordeaux and Picton. In this the relationship is more apparent as the rainfall curve is composed of a series of maxima and minima, with a general decrease in the height of the maxima, which corresponds to the decrease in height of the floods. The minima mark those years when the heavy rainfall was more coastal and all the flood waters came from the Nepean. The association between the rainfall and the flood line is not very close, for a flood does not depend on BY LESLEY D. HALL. 141 the amount of annual rainfall, but on a very heavy fall over a short period. Constant precipitation may give a high annual total with not enough at any one time to cause a flood, while flood rains followed by droughty conditions will result in a low yearly average. If heavy rain falls at a time when evaporation and percolation factors are high the run-off may not be sufficient to cause a flood. WATER CONSERVATION ON THE NEPEAN. The great flood of 1867 occurred during a time when floods were much more frequent than they are at present and when the waters over the whole catchment area were uncontrolled. Since that time schemes for the conservation of water have been carried out on the Upper Nepean. The locality was chosen as being the place nearest to Sydney which was high enough and comparatively unin- habited; not from any direct rainfall considerations. The first project was the building of a tunnel from Pheasant’s Nest to Broughton’s Pass, which diverted water from the Nepean and Cordeaux rivers to the Cataract. The water of both streams was carried along, partly by tunnel and partly in an open canal to bo 50. 50 Floods at Wendsor, in order of greatest magnitude. i Rain at Windsor. Rain on the Nepean and Cordeaux Catchment 20 Height of Floods in feet. (average of % Stations, Goulburn, Taralga, Cordeaux, Reton 40 . 5 RIGO HWY KG eWY CSN HBS Qh HM so Ww: x = gi? SONS SSR eee SONS Ses SSeS eee IRS ~m & ®& © % Gg & mn & BS OH © & & DH & & wm BH & OWweewo Qa = oS SS Sp SNS SSS OO Sas Se SS Sse eS SS SS SS ST OS Seo ee Text-figure 6.—A graph showing the relation of flood heights at Windsor to the yearly rainfall. In this figure the continuous graph represents the floods at Windsor, the dot and dash graph the rain at Windsor and the broken line the rain on the Nepean and Cordeaux Catchments. 142 FLOODING OF HAWKESBURY RIVER AT WINDSOR. Prospect and so to Sydney. Then the Cataract dam was built and stored water first in 1906. It was filled for the first time in 1911. In time of flood or fresh only a fraction of the flow of the Nepean River can be diverted to Sydney and the same might have been said of the Cataract River before the completion of the dam. In dry weather, however, practically the whole flow of the Cordeaux om x Beton Bargo. : a upton, ams, Pwversiggs $5655.55 54 Ms a _ wee -"No. I Se oan ane, a ) Cat ae QW ne Dam ‘ @ CATCH MEN AREA. S @ Letter ox ae Sherbroa EAE Text-figure 7.—Sketch map of the catchment area of the Nepean River showing the position of the water conservation dams. above Pheasant’s Nest and the Cataract above Broughton’s Pass is diverted, to the great disadvantage of settlers on the Nepean, who are thus deprived of water which would have otherwise reached their land. To assist them compensa- tion weirs have been built along the Nepean, and are replenished from time to time by water released at Pheasant’s Nest and Broughton’s Pass. The catchment area of the Cataract Dam is 50 square miles and, when full, it backs up the water to a depth of 150 feet and stores 20,743 million gallons. Construction of dams on the Cordeaux and Avon rivers is now almost complete and during the flood rains of May and June, 1925, they stored a great deal of BY LESLEY D. HALL. 143 water. As soon as these dams are finished one is to be constructed at Lupton on the Nepean proper, and with the four dams in working order a continuous flow of 108 to 110 million gallons of water per day will be able to be maintained to Sydney as well as the coastal supply to Mt. Kembla and Wollongong. In 1871 there were only two rainfall observing stations in the catchment area but at various times since then others have been established. The following is a list of these recording stations: | Catchment Area. Rain Gauge Stations. No. of Years. Yearly Average. Sherbrookciaeananeeeeeae 32 59-16 Madden’s' Plains) 2.5... | 17 58-47 Cataract. etter boxe. Secale oars tenes 16 49-43 Mount ebleasaniteeorycriarnK 174 57-13 Cataracty anime wrrieeeers 20 34-82 Broughtonispeassi esse 36 33-16 COndeauxe Weyer sic shessty cuss 53 61-01 Cordeaux Gauge Weir .. 15 42-04 Nepean, TROMSESIMENOD, | “Gaoococcsuo0eed 34 57-69 Mattar om Sgn ape tecsusroton! sieve aac 28 33-61 Bar eo Mrarsspses io ere Sere sors ols 22 30-22 WV BOTIE seer sewer cceteh cts ronsene shes 28 27:23 The average rainfall on the Cataract catchment area of 50 square miles is 48-69 inches. On the Nepean catchment area, which includes 35 square miles of Cordeaux drainage and-55 square miles of the Avon, the rainfall is less, the average being only 41:98 inches. Therefore, though the Cataract Dam has a smaller catchment area than the Avon it receives a greater amount of water. One inch of rain falling over one square mile of country is equivalent to 14:52 million gallons of water. A great deal of this water is lost by percolation and evaporation so that only a small percentage runs over the surface and into the river. Measure- ments of the amount of rain falling on the catchment area of a river will give the actual number of gallons which fell, while from measurements of the velocity of the stream the number of gallons discharged can be obtained. From these two sets of figures the actual amount of water lost by percolation and evaporation can be found and the run-off expressed as a percentage of the rainfall. Between 1887 and 1906 on the Warragamba catchment area the average rainfall was 32:45 inches and the mean estimated run-off was 16%. The run-off is found, to be a variable factor depending on climatic conditions and whether the rain falls after a wet or a dry season. On the Cataract catchment area for the 25 years since 1900, the average rainfall per annum was 50-56 inches and the average discharge was 13,358 million gallons or 33-64%. An inch of'rain over the 50 square miles of the Cataract catchment area is equivalent to 50 x 14:52 x 10° or 726 million gallons of water. Of this about one-third or 242 million gallons is available to be stored in the dam. The average fall of 50 inches of rain over the whole area will only produce 12,100 million gallons of water to be stored and, as this is only about half the capacity of the dam it seems evident that its catchment area is not 144 FLOODING OF HAWKESBURY RIVER AT WINDSOR. large enough. Yet the Avon Dam with about equal available water is twice as big as Cataract with a total capacity of 47,159 million gallons. The heavy rains of May and June, 1925, were not sufficient to fill the Avon and Cordeaux dams which would seem to be too large for their catchment areas. In this connection it is necessary to remember the purity of the water which flows into the Avon Dam, an important factor in a country where settlements are to be found on most of the rivers. Tue ACTION OF THE DAMS DURING THE 1925 Froops. Heavy rains were experienced on the Nepean catchment area during May and June, 1925, the total precipitation over the whole area for the two months, as ealeulated from four rainfall stations on the Cataract catchment and three on the Avon and Cordeaux, being 37:08 inches. Of this 22-84 inches fell during May as compared with the 14:24 inches which fell in June. At the time of the May fall, however, the ground was dry and a great deal of the water was lost by percolation and evaporation. For this month the average run-off over the whole area was 63:°6% of the rainfall, while during June when the ground was still moist the average run-off was 76:9%. On the Cataract catchment area the mean precipi- tation for the month of May was 25:24 inches and the run-off was 66% of the rain- fall. There were 5,470 million gallons of water stored at the beginning of the rain and the increase was 6,263 million gallons. The dam did not overfiow during the May flood and the water continued to rise during the rest of the month owing to run-off from the hills which continues for a good while after rain has fallen. At the beginning of the heavy June rains there were 17,954 million gallons in storage and the dam was filled within three days. The overflow at the time of the June flood is estimated at 4,421,324,500 gallons. The rainfall for that month was 13:95 inches and the run-off was 74:7%. The total amount of water stored in the Cataract dam in May and June was 15,273,000,000 gallons. On the Cordeaux catchment area records from three stations only are known and their readings give a mean rainfall of 23:19 inches for May. The increase in storage of the dam was 6,848,000,000 gallons and the run-off was 58-4% of the rainfall. The June rains averaged.15:29 inches but the run-off was higher, 70:3%, and increased the storage by 5,439,000,000 gallons, making a total increase of 12,287,000,000 gallons in the Cordeaux storage for May and June. The dam did not reach its full capacity. Records from the Avon catchment area are also very approximate, being based on observations from three stations only. For May a mean precipitation of 20-1 inches is recorded, 25% less than that of Cataract, while the run-off was 66% and gave an increase in the storage of 10,625 million gallons. In June the rainfall of 13:47 inches with a high run-off of 85:8% gave an increase in storage of 9,193,000,000 gallons. The total increase in the Avon storage was 19,816,000,000 gallons, but as the dam was almost empty at the begin- ning of the rains it did not then reach its full capacity. Storage was commenced on the Avon River at the end of May, 1924, and by the end of June, 1925, 22,308 million gallons had been impounded; practically the whole yield at the catchment, as only a trifling amount was sent to Sydney. Another 71 inches were then required to fill the storage. It is calculated that the mean precipitation over the whole catchment area of 354 square miles for May and June was 18-54 inches, giving a run-off of 105,372 million gallons, of which 48,233,000,000 gallons, or nearly 50% was caught and held in the Cataract, Avon and Cordeaux reservoirs. Some of the excess water not held by the dams was probably discharged down BY LESLEY D. HALL. 145 the canal to Prospect, but in quantity so small as not to affect the calculations, since at the height of the flood the gates are closed to prevent the blocking of the canal by debris. Details as to the rainfall and discharge from the Warragamba and Grose catchment areas are supplied by the following letter from the Water Conservation and Irrigation Commission: “The most notable falls on the Warragamba River catchment area during the months of May and June were: Robertson LAT Mit Mndties, pe 44°20) inches Goulburn SP ARERR A. te celOs38 Py Katoomba Se See ae ye aad MAAS e Wiha Wiiewore, oo co oc ao IbupmHy) h Bowral te Sse ee i sscaes eeepc £9 ki Taralga mabe. Tey a Ys ote Ss LOOP 6 The rainfall stations are not evenly distributed over the catchment area; on the sparsely settled districts the records are scanty, but by giving each station its proper ‘zone of influence’ the mean depth of precipitation over the catchment area is estimated at 17 inches. The amount of water discharged by the Warra- gamba at a point a litttle up stream from its junction with the Nepean, during May and June is estimated at 297,715,000,000 gallons or enough to supply Sydney for 14 years at the present annual consumption rate. About 35:5% of the rainfall was discharged by the Warragamba, the rest being lost by percolation and evaporation. There are no reliable measurements of the amount of water contributed by the Grose River to the floods of May and June. The catchment area of the stream at its affluence with the Hawkesbury above Richmond is 250 square miles. A con- servative estimate of the discharge, basing it on the relation of its area to that of the Warragamba, would be 22,000 million gallons of water, which is little more than the capacity of Cataract Dam. Rainfall stations on the Grose catchment area are Springwood, Lawson and Blackheath.”’ From a combination of the figures for the three catchment areas the following table is derived: Area in Run-off, Storage, Catchment. square million million Storage %. miles. gallons. gallons. Wiarracambayiesy wee fhe hee os 3,383 297,715 — “= i Nepean Seot eich eT Pete OR, ao Ont 354 105,372 48,233 45-7 Grose aigiyett ato o. Mesoraes Ghee Ie RRSnOaeteT 250 22,000 — — PIN OVATE ee RP a ai | oie iat otal Bic 3,987 425,087 | 48,233 11:3 This gives approximately the total run-off from a catchment area of 3,987 square miles, figures for the other 853 square miles of the Windsor catchment area not being recorded. Yet considering that the dams caught and held almost half the 7 146 FLOODING OF HAWKESBURY RIVER AT WINDSOR. water discharged from the Nepean catchment area and practically 10% of the total water discharged at Windsor, it is obvious that if these dams had not been in existence the magnitude of the floods at Penrith and Windsor would have been greatly increased. The dams on the Nepean cannot prevent floods at Windsor, nor decrease the number experienced there, but their existence is felt in a tendency towards modification during a flood period, although their effect is a variable factor depending on a number of conditions. The Nepean drainage is only about 10% of the Warragamba, but its area is nearer the coast and consequently receives more rainfall, so that in the June, 1925 flood its run-off was equal to 35% of the Warragamba run-off. It is possible for coastal rains to cause floods of the Nepean without additional water from the Warragamba and in such cases there is no doubt that the effect of the dams is very great. The actual amount of water which is held back by the dams depends on the number of gallons already stored at the beginning of the rains. The heavy rains of May were preceded by a dry period and the water in Cataract Dam was low. Also dams at Cordeaux and Avon were only on the verge of completion and almost empty, so that a considerable quantity of water was capable of being stored. A flood of any magnitude at Windsor is due to a cyclonic disturbance, which causes sudden heavy rain of only short duration over the whole catchment area. As a result a great deal of excess water is discharged in a few days, causing an abrupt rise and fall in the river level. The dams, therefore, by holding back water at the-.time of general discharge decrease the height to which the flood would have risen and the consequent damage which would have been done. HEven if the dams are full and cannot hold back the water from the flood they decrease its peak discharge, because the whole surface of still water must be raised above the level of the dam before the overflow takes place and the drainage from such a surface is necessarily slower. It is not the actual amount of water but the rate of discharge which causes the river to rise and flood the lowlands and an arrange- ment whereby the water is delayed and caused to pass more slowly down the river does much to lessen its evil effects. DECREASE IN RAINFALL. The decrease in the number of floods experienced at Windsor of late years seems rather to be a factor of the decreasing rainfall than to be due to dam building on the Nepean. At Grove Farm the river rose to 67 feet 10 inches on the present gauge in 1867 and only 35 feet 4 inches in 1925. This difference could not be accounted for by the building of the dams. It must be associated with a diminution in rainfall, a factor not due to deforestation as this area, being rugged inhospitable country, is still uncleared to a large extent. The difficulty in this connection is the absence of long time rainfall records by which a decline in precipitation might be verified. Goulburn is the oldest established rainfall station on the Warragamba catchment area. The records commenced in 1858 and the average for 67 years was 25-41 inches, while for the last 30 years the average has been 22-83 inches, a falling off of about 10%. Rainfall records at Cordeaux gauging weir were started in 1872, the average rainfall for 53 years being 53:58 inches, while the average since 1900 shows a decrease of about 20% and is only 44-45 inches. The following table shows how the ten yearly averages compare with the total averages since the formation of the station at various places on the catchment area (figures obtained from Hunt, 1916, and from the Weather Bureau). ILALL. BY LESLEY D. (hOO0 '3oc shva2ny SS eee Lithgow- Me Viectorva Actual Raunfall. Average Ratnrall. Nn —_ ba [? /; uv > fe) Ho) < La Kapeoey 300 200 100 3 8 8 ‘qqeduivy do sayouy 1200 1100 1000 Joo 300 700 6 4ebI 6b! trbl Itbh orb bibt 8161 Ltbl VItbt Gibt W161 1b Tibet 11bt orbl bobl Bobr Lobi 1061 Sobt 4obl G06! Sa See ae a SS MoT iobt 9994 Pees oS SS? Gusany se? u oe eA figure 8.—Summation hydrographs showing the variation in the rainfall above and below the average for a number of years, of six stations on the Windsor catchment Text- area. The summation hydrograph is made by adding together the averages of the rainfall at a certain place over a number of years and then plotting the result as a rising graph. The final point on the graph is joined to the first point by a straight line which is the general average rainfall over the total number of years. When the graph line is parallel Where it inclines away from to the average line the years were ones of normal rainfall. the average the rainfall during those years was above normal and where it inclines in to the average the rainfall was less than normal. 148 FLOODING OF HAWKESBURY RIVER AT WINDSOR. Average Rainfall. Total IRIS: 1871— | gsteen) tsg1— || loots | tones ||) onsale eas 1880. | 1890. 1900. 1910. | 1920. 1924. Cordeaux seer 60-0 | 57-42 69-66 46-34 47-91 39-58 53-48 | ipictonuasee eee = 27-45 35-26 24-74 34-94 28-38 30-15 Maralleala eee = 30-87 30-35 24-49 28-69 27-05 28-28 Goulburn ...... 28-51 22-53 27-21 20-39 23-58 26-038 27-06 | 1871-1880 are years of good rainfall, 1881-1890 are not so good. From 1891-1900 the stations all record rainfall above the average, then from 1901-1910 the rainfall is uniformly low. 1911-1920 shows an increase with two stations above and two below, but 1921 to 1924 are years of low rainfall again. The rainfall at these stations is also depicted on the graph (Text-figure 8), where summation hydro- graphs show the variation above and below the average from year to year. These graphs show that since 1900 the yearly rainfall has mostly been below the average with a marked decrease in the number of inches precipitated. For six years, 1904- 1910, there was a low water condition in the upper Sydney water supply canal from the Nepean, unparalleled in 80 years, and though the average rainfall discharge has increased since then, it is still lower than it was before the dry period. The graph (Text-figure 9) shows the 11 year cycle of maximum and minimum sun spots with a decrease in the maximum number from 1870 onwards. 1870 was a year of good rainfall everywhere and a time when the greatest number of sun Text-figure 9—Major and minor sun spot cycles (Huntington, 1915). spots have been recorded. From 1881 to 1890 the rainfall was not so good, but at that time the sun spot maximum was not nearly so large as the one preceding. Between 1891 and 1900 the maximum was greater and the rainfall recorded is better, but from that time onwards there has been a steady deciine both in sun spots and precipitation. Thus rainfall does seem to vary, not only with the eleven years’ cycle but possibly also in accordance with a superimposed major cycle as shown by Huntington, 1915. If this is the case the recent floods of 1925 might be taken to indicate the beginning of a new cycle in which the seasons would gradually improve. Such conclusions are necessarily very tentative as it is difficult to arrive at any definite principle. BY LESLEY D. HALL. 149 FrLoop SILTS OF THE HAWKESBURY RIVER. The silts brought down by the Hawkesbury when in flood are of two varieties, the rich black mud and the useless sand. The Warragamba, Grose and Nepean flow through sandstone country which is easily weathered, supplying these rivers with large quantities of sandy sediment of no fertilizing value. The mud which is so important to the farmer is derived by the Cox and Wollondilly from the older palaeozoic rocks through which they flow before entering the sandstone region. By the time the waters reach Windsor the sand and the muds have been mixed together giving a light sandy loam which is very fertile. Pure mud is also deposited, enriching the land, but sometimes the flood currents leave behind them patches of sand which ruin the area on which they are placed. The Grose River carries only sandy sediments yet after the flood of June, 1925, black mud inches deep was deposited along the banks of this stream for seven miles above its junction with the Nepean, thus showing the distance to which the flood water must have backed up the Grose against the normal flow of the river. The depth of silt left behind by the flood is a variable factor depending largely on the topography of the district, but also on the height of the waters and their velocity. As the river spreads over the flats it meets resistance and the velocity is checked causing a great deal of the silt load to be immediately dropped. In this way levees or mounds of silt are formed along the banks of the river which prevent the overflow water from drain- ing away from the flats again. In the Windsor district, therefore, large areas of still water result, the silts of which are deposited in a fine layer over the entire surface. Farther down the river where the flats are smaller and more isolated the silt deposit is greater and was from 4 to 6 inches in the June flood. As seen in the river bank at Windsor the flood silts form a series of fine laminations of varying colour according to the proportion of mud and sand (Plate viii, fig. 1). As the surface layer dries it hardens and contracts, breaking into small pieces by a number of small and irregular cracks (Plate viii, fig. 2). When dry it is very soft and friable and soon becomes worn down into the soil. David and Guthrie (1904) give an analysis of flood silt from the Hawkesbury water during the flood of 1904 which shows that the lime, potash, phosphoric acid and nitrogen content of the soil is renewed by flood waters. This is undoubtedly very good, especially in a place such as the Hawkesbury flats where constant tilling is wearing out the good of the soil and artificial manures must be used. Provided the flood comes at the right season it is more beneficial than other- wise in the more northerly reaches of the river where it is only the orchard flats which are covered by the waters. Here the houses are built on the higher sand- stone terraces and so escape damage. The fruit trees are grown in the long flat gullies at the base of the sandstone hills where the flood forms quiet backwaters in which silt is deposited inches deep over the farms. However, floods are very uncertain in their coming and on the low flats between Wilberforce and Windsor often large areas of growing crops are destroyed in addition to other extensive damage which tends to outweigh any good effect. After the flood of June, 1925, the water remained on the surface for days which, although impeding the work of reconstruction, enabled the subsoil to become thoroughly wet. As a result it was possible for the farmer to grow valuable areas of lucerne, a crop which cannot be grown there under ordinary rainfall conditions as rain does not penetrate deeply enough into the soil. Moreover, throughout the dry summer which followed the crops flourished on water stored beneath the surface of the ground. Therefore, although the general opinion is one of censure against the floods, there is always 150 FLOODING OF HAWKESBURY RIVER AT WINDSOR. some benefit to be derived from them. In the Windsor district another difficulty at flood times is the shifting of the land as the river increases the scope of its meanders. The velocity of the flood waters gives them great erosive power and as they swing round a meander the river bank is washed away on one side while sand and debris are deposited on the other. During the June flood a land slide occurred in which 200 yards of the road along the bank was completely washed away. With every flood the channel of the river is altered, the meanders becoming more and more curved and unless they are prevented by artificial means the meanders will become cut off with resulting ox-bow lake formation. This action of the river is a source of great difficulty in a region where the land is divided into private farms whose owners lose large blocks of land with every flood. FLoop PREDICTION AND CONTROL. As floods in the Windsor district are due to irregular cyclonic disturbances on the coast, to forecast their occurrence would be a matter of some difficulty. At one time the people were caught by the water when quite unprepared, but they are now warned by telephone communication which gives them about 24 hours in which to evacuate. The warnings, however, are never very accurate and the people do not know how high the water may be expected to come, nor will they leave their homes till they are quite sure that it will be necessary. The best way of controlling flood waters is to build levees along the river banks high enough to prevent the water from coming over. in the Windsor district this would be an enormous task owing to the great extent of flat land through which the river flows in that locality. Moreover the expense of such an undertaking would not be justified by the value of the land. It is doubtful whether any farmer round Windsor would be willing to go to the expense of erecting a bank to protect his property against the ravages of the river even if it did not do good as well as harm. The risk of life does not even cause them to take precautions, for many still live in houses well within the danger zone and do not even keep a boat when their only means of escape at flood times is by water. The rescue work is carried on by special boats which have to be sent to the afflicted areas from Sydney. To control floods in the Windsor district it has been suggested to build a dam in the Warragamba gorge to collect all the run-off from the Wollondilly water- shed and permit of it being released in more or less regulated volumes. A wall 300 feet high in this gorge would impound the water for 25 miles up the Wollondilly and 20 miles up the Cox. Such a dam might not actually prevent floods for the Burrenjuck Dam, which captures nearly all the headwaters of the Murrumbidgee, was unable to prevent flooding of that river in 1925. However, besides lessening the discharge by an amount proportional to the number of gallons already in the dam at the beginning of the rains, it would offer a very large surface of still water over which the excess would have to pass and would thus make the floods less intense and therefore lower in height. If the overflow water were to be discharged down the river more slowly it might possibly be contained within the river banks. The dam would give a continual flow of 200 million gallons per day to Sydney. It is calculated by water supply experts that up to 1967 Sydney, with the 80 million gallons from the Nepean, will only require 160 million gallons from the Warragamba, and if the surplus is not used it will bank up and overflow. This will decrease its usefulness in the prevention of floods and in order to use the excess water schemes for the generation of electric power and for the irriga- tion of the lowlands have been suggested. The water from the dam on the BY LESLEY D. HALL. 151 Murrumbidgee is used to irrigate land which is naturally fertile and only requires water to make it good for agriculture. It is well drained with uniform surface levels which make redistribution easy, while the low rainfall insures a constant demand for water. Conditions are different in the county of Cumberland. Here there are 26,390 acres of good river land, 14,300 acres of second class river land and the rest is Wianamatta shale, poor soil almost worthless for cultivation with unequal levels which would make the application of water a costly process. 'The area supports 778 persons per square mile, including the city of Sydney and only 98 per square mile if that town is excluded. Also the rainfall is a very variable factor and the demand for irrigation water would fluctuate. Yet on the river flats the dam would greatly decrease the possibility of floods and irrigation, though costly, would increase the productivity of the land which is the closest agricultural region to the city of Sydney. Nevertheless the proposal to dam the Warragamba is not much favoured by people of the Windsor district, who depend on the river for their water supply. The towns of Richmond and Windsor both obtain water from the river by electric pumps and anything which would check or interfere with the flow of the river or any of its tributaries upstream must seriously jeopardize the supply from the Hawkesbury, especially in dry seasons when the salt water works its way towards Windsor rendering the river water unfit for use. SUMMARY AND CONCLUSIONS. Floods in the Windsor district are due to the presence of a river with wide- spread upland drainage, discharging its waters from the mountains on to the flat lands of this locality. They are caused mainly by heavy coastal storms of short duration and result from the sudden and simultaneous discharge of excess water from the large number of tributary streams. This gives a typical high peaked flood wave which passes very quickly so that the rise and fall of the waters is only a matter of days. A high flood is very destructive covering the crops and often entering the homes of the farmers, who are forced to seek shelter on higher ground. The black mud left behind by the waters is fertile and the ground is improved by the moisture yet the damage of the flood outweighs its good effects. Prevention, however, is a difficult matter. The flats are far too extensive and not Tich enough to pay for the building of levees. Aliso floods are not nearly so numerous or so high as they used to be. The best method of controlling floods is by water storage. There are at present three dams on the Nepean which hold back some of the water at time of flood and, by thus knocking off the peak of the flood wave, do much good by making the rise of the waters less abrupt. The river is the one nearest to Sydney and therefore its natural source of water supply, while the inhospitable character of the rugged mountainous area through which it flows prevents settlement and keeps the water fairly pure. It is suggested to build a large dam on the Warragamba River which will assure an ample supply of water to Sydney and at a time of heavy rain will help to smooth down the flood wave so considerably that the water may possibly be contained within the river banks. Dams, however, cannot actually prevent floods and those built on the Nepean have not been the cause of the decrease in the number of floods experienced at Windsor of late years. This decrease is rather a factor of declining rainfall for precipitation on the catchment area has been steadily less ever since the heavy rainfall of 1870. References. Davin, T. W. E., and GuTHRIE, F. B., 1904: ‘The flood silts of the Hunter and Hawkesbury Rivers.” Proc. Roy. Soc. N.S.W., xxxviii, pp. 191-202. 152 FLOODING OF HAWKESBURY RIVER AT’ WINDSOR. DE BurcH, 1908: “Warragamba River and Water Supply of the County of Cumberland.” Report to the Water Conservation and Irrigation Commission, Sydney, N.S.W. HUNTINGTON, E., 1915: “Civilization and Climate.’’ University Press, London. HUNTINGTON, E., and VisHmr, S. S., 1922: “‘Climatic Changes, their Nature and Causes.’ Yale University Press. Hunt, 1916: “Results of Rainfall Observations made in N.S.W. during 1909-1914.” Krom the Commonwealth Bureau of Meteorology. METROPOLITAN BOARD OF WATER SUPPLY AND SEWERAGE: Thirty-sixth Annual Report for year ended 20th June, 1924. Taytor, T. G., 1923a: “The Warped Littoral Round Sydney.’’ Proc. Roy. Soc. N.S.W., lvii, pp. 58-79. : Taytor, T. G., 19238b: “Geography and Australian National Problems.” Report Aus- tralasian Association Advancement of Science, Wellington, Vol. 16, pp. 4383-487, 1924. TEBBUTT, 1908: ‘““Windsor Rainfall. A Retrospect for 45 Years.” Windsor and Richmond Gazette, January, 1908. WATER CONSERVATION AND IRRIGATION COMMISSION: Annual Report for Year ended June, 1925. DESCRIPTION OF PLATE VIII. Figure 1.—Flood silts on a grassy bank at Windsor showing the laminated character of the deposits. Figure 2.—Irregular cracks due to drying in the flood silts at Windsor. NEW GALL-FORMING THYSANOPTERA OF AUSTRALIA. By Dupitry Movurron. (Communicated by W. W. Froggatt.) (Plate ix and fourteen Text-figures. ) [Read 25th May, 1927.] The gall-making thrips of Australia include some of the most interesting forms of all the Thysanoptera, and I am greatly indebted to Mr. W. W. Froggatt who has supplied me with abundant material of many species, several of which are new. Iam offering this brief paper as a preliminary one and hope it will help to stimulate other entomologists to collect and study these thrips whenever they are observed. I wish here to express my appreciation to Dr. H. Priesner for examining many of these specimens. KLADOTHRIPS AUGONSAXXOS, n. Sp. (Plate ix, No. 1347.) This species of Kladothrips can be distinguished from K. rugosus, the one other known species of this genus, also found by Mr. Froggatt, by the following characters: K. rugosus Froggatt. K. augonsaxrxos n. sp. All antennal segments except the first, more or less uniformly light yellow to yellowish brown. Pterothorax and first two or _ three abdominal segments yellow, or yellowish orange. Middle and hind legs uniformly dark brown. Third antennal segment, also sometimes tip of two, yellow, all others dark brown. Pterothorax and abdominal segments quite uniformly dark brown. Tips of middle and hind tibia and tarsi often yellowish. The most striking difference is the enlargement of the egg sac in the abdomen of K. augonsaxxos which I have never before observed among the Thysanoptera. The abdomen is normal in one specimen before me, apparently before the develop- ment of the egg sac. Its sides are almost parallel, being reduced gradually from the sixth to ninth segments and there is no apparent distention of the connecting tissue between the segments. In other specimens the egg sac is variously enlarged, although the chitinous walls of the segments do not appear to lose their original shape. In one specimen which is typical, the connecting tissue between segments three and four is distended and forms a small, transparent ring extending entirely around the body. The connecting tissue between segments four and five is distended into a larger transparent ring which could possibly contain a single row of eggs, placed end to end. The great spherical egg sac formed between segments five and six is three or four times the width of the body in diameter, tough and strong, whitish, almost transparent in colour, and is seen to contain a great mass of eggs. Segments six to nine and the tube appear to retain their normal shape and size. U 154 NEW GALL-FORMING THYSANOPTERA OF AUSTRALIA. Female holotype—Measurements: Total body length in normal condition about 2:60 mm., with distended egg sac about 2:75 mm. Head length 0:33 mm., width 0-165 mm.; prothorax length 0:33 mm., width 0-36 mm., including prominent fore coxae, 0°45 mm.; width of pterothorax 0-45 mm.; tube length 0:20 mm., width at base 0°08 mm. Antennae, length (width) segment i, 30 microns (39 microns) ; ii, 60 (38); iii, 75 (33); iv, 69 (36); v, 63 (32); vi, 48 (30); vii and viii, 72 (27); total 435 microns. Length (width) of femora, fore femora 416 yu (133 »), middle femora 135 w (63 «); hind femora 225 uw (90 uw). Colour dark brown. Extreme tips of fore femora, fore tibia and tarsi including tarsal claws, also third segment of antenna and extreme tip of two orange yellow. Fore coxae, pterothorax except outer borders, extreme bases and tips of middle and hind tibia, and middle and hind tarsi light brown. Connecting tissue between abdominal segments light brownish yellow, especially conspicuous after the egg sac begins to form. Head about as long as prothorax and half as wide, with straight, almost parallel sides (Text-fig. 1). Postocular spines short and stumpy with dilated tips, Kladothrips augonsaxxvos, n. sp. Fig. 1. 9 Head and prothorax, dorsal view. Fig. 2. @ Right antenna, dorsal view. situated well back from the eyes. Eyes comparatively small, neither prominent nor protruding, with small facets, not pilose. Anterior ocellus on apex of head, posterior ocelli contiguous with inner margins of eyes. Mouth cone _ short, triangular, reaching hardly one-third the length of the prosternum, with bluntly rounded tip. Antenna apparently 7-sezgmented. The terminal segment has a distinct transverse, oblique suture indicating clearly that it is formed by the fusion of the two terminal segments. (This is also true of the antennae of K. rugosus Froggatt, specimens of which are before me.) Antennae about one and one-third times as long as head; segment three club-shaped, segments four, BY DUDLEY MOULTON. 155 five and six abruptly constricted, each at about one-fourth its length from the base, these narrowed portions cylindrical, the rest of the segments subglobose. Segment three with one simple sense cone near tip on ventral side, segments four and five each with two, and segment seven with one. All sense cones short and transparent (Text-fig. 2). Prothorax, not including prominent coxae, somewhat wider than long, shield- shaped, with a distinct median longitudinal thickening. Prominent spines on anterior and posterior angles, also on prominent coxae. All spines stout and trans- parent, with blunt tips, those on posterior angles 75 microns long. Pterothorax as wide as prothorax and fore coxae combined, sides almost parallel with a small angular indentation in the middle on either side. Anterior legs much enlarged, fore femora about one-fourth longer than head and three-fourths as wide as width of head. Armature of fore tibia reduced to blunt inconspicuous knobs at end on inner side. Claws of fore tarsi are long, straight and pointed, as long or longer than length of tarsi, and project at right angles. Middle legs much reduced, the median femora smaller than the fore tibia; posterior legs somewhat larger. Wings well developed, entirely clear, not narrowed in the middle, with ten double fringe hairs along posterior margin near tip. Abdomen of normal shape before the formation of egg sac. Tube almost two-thirds as long as head. This thrips is a true gall maker and produces a spherical gall from one-half to three-quarters of an inch in diameter, hollow, with an outer shell wall of about one-sixteenth of an inch in thickness. The gall is a deformity growing out of the leaf. One female inhabits each gall; she scatters her eggs, hundreds of them, on the inner surface where the larvae hatch, and apparently feed as I have found larvae within the parent gall in all stages. No males have been observed. Female holotype in author’s collection; paratypes in the Froggatt Collection, Canberra, Australia. , Hostplant: Gallmaker on Acacia doratoxylon. Habitat: Gilgandra, New South Wales. CHOLEOTHRIPS, new genus (No. 518). (Sub-family Kladothripinae. ) Head one and one-third times as long as wide and slightly shorter than prothorax, broadest across at the eyes, constricted uniformly toward the base. Cheeks with several thorn-like bristles, a single pair about one-third the length of the head from posterior margin, long and conspicuous and almost one-half as long as prominent postoculars. Eyes large. Ocelli present. Mouth cone short, reaching about two-fifths the length of the prosternum, bluntly rounded, labrum blunt. Prothorax shield-shaped. Fore coxae enlarged, prominent, and together with the prothorax wider than the pterothorax. Fore femora greatly thickened. Fore tibia stout and armed at the end within with a strong tooth. Each fore tarsus with two teeth. Wings not constricted sole-shaped, but still a little smaller in the middle. Tube almost as long as head. Type: Choleothrips geijerae n. sp. CHOLEOTHRIPS GEIJERAE, n. sp. (Plate ix, No. 518). Female holotype-—Measurements: Total body length 2.42 mm. Head length 0-33 mm., width 0:25 mm.; prothorax length 0-36 mm.; width 0-416 mm.; including 156 NEW GALL-FORMING THYSANOPTERA OF AUSTRALIA. coxae 0:55 mm.; mesothorax width 0-52 mm.; abdomen width 0-416 mm. Antennae: Segment i 27 microns, segment ii 54 microns, other segments broken off. Legs, fore femora length 0-41 mm., width 0:20 mm.; middle femora length 0:23 mm., width 0:10 mm.; hind femora length 0:33 mm., width 0:12 mm. Tube length 0-315 mm., width near base 0:09 mm. Colour: Prothorax and fore legs quite uniformly yellowish brown; head, first antennal segments, pterothorax, abdomen, middle and hind legs dark brown, with joints and tarsi of middle and hind legs lighter. Wings uniformly smoky coloured. All prominent spines yellow. (Two paratype specimens have the prothorax and fore legs dark brown like the rest of the body.) Head one-third longer than greatest width across at the eyes, constricted posteriorly (Text-fig. 3). Postocular spines pointed, 90 uw long. Longest cheek Fig. 5 Fig. 6, Choleothrips geijerae, n. sp. Fig. 3. 2 Head and prothorax, dorsal view. Fig. 4. 92 Tip of abdomen, dorsal view. Fig. 5. 92 Right fore leg, ventral view. Fig. 6. 9? First segment of abdomen, dorsal view. spines 39 w long. Eyes large, occupying four-fifths the width and about four- ninths the length of the head. Facets very small, not pilose. Ocelli present, placed well forward on head, anterior one on apex, posterior ocelli contiguous with anterior inner margins of eyes; mouth cone short, rounded, labrum blunt. There are two distinct swellings ventrally, one on either side of the head, just anterior to the base of the mouth cone. Antennae 8-segmented. Unfortunately the antennal segments beyond the second joint have been broken from all of the specimens before me. BY DUDLEY MOULTON. 157 Prothorax distinctly shield-shaped, one-eighth wider than long but about one-third wider than long when the fore coxae are included. A prominent spine on each fore angle, 90 u long and one on each posterior angle 180 uw. Long spines on angle of fore coxae 135 yw. All spines pointed. The median dorsal suture terminates in front in a triangular enlargement with distinct sculpturing. Mesothorax widest, excluding protruding fore coxae of prothorax, with sides almost parallel. Metathorax with sides tapering gradually to meet the more slender abdomen. Fore femora greatly enlarged, about four-fifths as wide as head and nearly one-third longer (Text-fig. 5). Fore tibia enlarged and armed with a strong curved tooth at the end on the inner margin. Fore tarsi each armed with two teeth, the larger inner one almost as long as the width of the tarsus and with a curved tip, the outer smaller one on the ventral or outer side. The middle and hind legs are much smaller with clearly enlarged femora but small in comparison with the fore pair. Wings fully developed, reaching nearly to tip of abdomen with sides almost parallel; twenty-eight accessory hairs on posterior margin of fore pair. Abdominal segments three to seven inclusive, are almost equal in length and width, and have parallel sides. Segment two is subequal in width but longer. The tergum of segment one is broad in the centre but compressed to curved points on either side, each bearing a long spine 0:93 mm., with distinet sculpturing (Text-fig. 6). The tube is almost as long as the head with straight sides tapering only slightly toward the tip. The long spines of the ninth segment reach approximately four-fifths the length of the tube, spines on the end of the tube are somewhat shorter (Text-fig. 4). Described from twelve females, including holotype, with prothorax and fore legs distinctly yellowish, and two paratypes with prothorax and fore legs con- colorous with the rest of the body. Holotype in author’s collection. Several paratypes in Froggatt Collection, Canberra, Australia. Hostplant: Geijera parviflora (Wilga), forming rolled leaf galls. Habitat: Gunnedah, New South Wales (W. W. Froggatt). DOLEROTHRIPS (?) GEIJERAE, n. Sp. (Plate ix, No. 518.) Female holotype——Measurements: Total body length 2-48 mm. Head length 0:30 mm., width 0:20 mm.; prothorax length 0°30 mm., width 0:30 mm., and 0°36 mm., including fore coxae; mesothorax width 0°55 mm. Antennae: Segment i, 36 microns, segment ii 54 microns, other segments broken off. Legs, fore femora length 0-31 mm., greatest width 0-12 mm.; middle femora length 0:21 mm.; greatest width 0:09 mm.; hind femora length 0:25 mm., greatest width 0-12 mm. Tube length 0°33 mm., width 0:10 mm. across swollen part near base and 0:06 mm. just before tip. Colour quite uniformly deep brown, wings transparent to slightly smoky. Head almost one-half longer than width across at eyes. Cheeks swollen in the middle and clearly constricted toward the base, with several short sharp spines. Postocular spines not conspicuous, set back from eyes about one-third the distance between posterior margin of eyes and posterior margin of head. Eyes large occupying two-thirds the width and one-third the length of the head. Outer border of eyes clear light yellow, facets very small; not pilose. Ocelli present, placed well forward on head, anterior one on apex but not protruding over basal segments of antennae, posterior ocelli contiguous with inner anterior margins of 158 NEW GALL-FORMING THYSANOPTERA OF AUSTRALIA. eyes (Text-fig. 7). Mouth cone short, rounded labrum _ blunt. Antennae 8-segmented. Prothorax shield-shaped, as wide as long but about one-fifth wider with the prominent fore coxa included. Spines on fore angles weak, spines on posterior angles pointed, 60 m. long, several short stout spines on angles of fore coxa, longest 40 m. Median dorsal thickening fades in front a short distance before the anterior margin but extends almost to the posterior margin of the prothorax. Mesothorax with rounded anterior angles, sides of both mesa- and meta-thorax constricted gradually toward the posterior margins. Fore femora enlarged, as long as head. Fore tibia unarmed; fore tarsi each with two [ S™ Fig./] & Dolerothrips (7?) geijerae, n. sp. Fig. 7. @ Head and prothorax, dorsal view. Fig. 8. 9? Tip of abdomen, dorsal view. Fig. 9. @ First segment of abdomen, dorsal view. Fig. 10. @ Tip of right fore tibia and tarsus, ventral view. Fig. 11. co Tip of right fore tibia and tarsus, ventral view. teeth, the larger more conspicuous one extends outward at right angles and is nearly straight, the terminal smaller ventral one is distinctly curved (Text-fig. 10). The middle and hind legs are strong, with femora enlarged, but small in com- parison with the fore femora. Wings fully developed, reaching to middle of seventh segment, sides almost parallel, 21 double fringe hairs on posterior margin of fore wing. Abdomen elongate, first segment broad in the centre and narrowed to a point on either side, it displays distinct sculpturing and bears a single long yellow spine at each outer angle (Text-fig. 9); segments two to six increase in width gradually, and seventh, eighth and ninth with sides rounded and clearly BY DUDLEY MOULTON. 159 narrowed posteriorly; tergites of segments two to nine more or less distinctly reticulated; tube slightly longer than head, swollen at the base, narrowed gradually to a rounded tip (Text-fig. 8). Male: The male is somewhat smaller, about 1:88 mm. in length, similar in colour and shape. The fore tarsus is smaller and tarsal tooth is about one-half as large as in female (Text-fig. 11). Described from nine females and three males. Holotype in author’s collection. .Paratypes in the Froggatt Collection, Canberra, Australia. Hostplant: Geijera parviflora (Wilga), found in company with Choleothrips geijerae forming rolled leaf galls. Habitat: Gunnedah, New South Wales. EOTHRIPS BURSARTAE, n. sp. (No. 516.) Female holotype.—Measurements: Total body length 1:66 mm. Head length 0-21 mm., width 0-20 mm.; prothorax length 0-166 mm., width 0°33 mm.; meso- thorax width 0:38 mm. Tube length 0:183 mm., width 0:08 mm. Antenna length (width) segment i, 30 microns (33 microns); ii, 48 (36); iii, 54 (36); iv, 48 (39); v, 48 (36); vi, 42 (33); vii, 48 (27); viii, 24 (18); total length 345 microns. Hothrips bursariae, n. sp. Fig. 12. 9 Head and prothorax, dorsal view. Fig. 13. 9 Left fore tibia and tarsus, ventral view. Fig. 14. 92 Right antenna, dorsal view. Colour brown to dark brown with tips of fore tibia, all tarsi and segments three to five and sometimes six lighter. Wings uniformly light smoky grey. Prominent spines yellow to yellowish brown. Body with numerous orange pigment spots or blotches visible in light coloured specimens. 160 NEW GALL-FORMING THYSANOPTERA OF AUSTRALIA. Head broadly rounded with cheeks slightly arched, broadest across middle line, dorsum with numerous confluent cross striations; postocular spines rather short, stump with dilated tips; cheeks with several short spines. Eyes occupying three-eights the length of the head, with small facets, indistinctly pilose. Ocelli placed far forward, posterior ocelli contiguous with anterior inner margins of eyes, with dark orange red crescents (Text-fig. 12). Mouth cone reaching posterior third of prosternum, bluntly rounded labium but with pointed labrum. Antennae 8-segmented, approximately one and two-thirds times longer than head, all seg- ments comparatively stout, fourth segment almost five-sixths as wide as long. Two sense cones on segments three, four, five and six, one on segment seven, all are short, blunt and transparent (Text-fig. 14). Prothorax almost as long as head but noticeably wider, with sides diverging posteriorly. Spines on anterior angles short, mid-laterals a little longer, those on posterior angles longest, all, however, are short, stocky and with dilated tips; each prominent angle of fore coxa also has a similar blunt tipped spine and two or three short pointed ones. Pterothorax broadest, sides almost parallel, converging only slightly near posterior line. Legs rather short, fore femora thickened, fore tibia unarmed, fore tarsi armed each with a spur-like tooth on inner margin and a smaller horn-shaped tooth near tip on ventral side (Text-fig. 13). Wings fully developed, broad, with parallel sides, not constricted in the middle, with ten or twelve double fringe hairs. Abdomen almost as wide as pterothorax, first seven segments of equal width, eight and nine conspicuously narrowed. Tube slightly shorter than head. Two prominent spines on each posterior angle of segments two to nine, the outer shorter ones (38 microns on segment two) gradually become longer until they reach a maximum length of 111 microns on segment nine; the inner ones, 60 microns on segment two, increase to a maximum length of 135 microns on segment nine, both pairs have blunt or dilated tips. Segments two to seven also have two additional pairs of curved spines on either side, the posterior pair on each segment much stronger than the anterior pair. The longest spines on the end of the tube are two-thirds as long as the tube, 135 microns. The male is very similar to the female, although somewhat smaller, the abdomen decreases in width gradually from the fourth segment to the tube. Described from numerous females and males taken from galls on leaves of Bursaria spinosa (Native blackthorn) at Warrah and Sydney, New South Wales, Australia, by W. W. Froggatt. Holotype in author’s collection. Paratypes in the Froggatt Collection, Canberra, Australia. EXPLANATION OF PLATE IX. No. 518. Rolled leaf galls on Geijera parviflora (Wilga) made by Choleothrips geijerac and Dolerothrips geijerae. Natural size. ; No. 1347. Galls on Acacia doratoxylon made by Kladothrips augonsaxxos Moulton Slightly enlarged. AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON. Part iv. HasitTat FACTORS AND PLANT RESPONSE. By Joun McLucnis, M.A., D.Sc., Assistant-Professor of Botany, the University of Sydney; AND ArtHuR H. K. Perrizt, M.Se., Senior Demonstrator in Botany, the University of Melbourne. (Twenty Text-figures.) [Read 25th May, 1927.] Contents. 1. Introduction. 2. The Habitat Factors. Climate of the Region. Humidity and Evaporative Power of the Air. The Moisture-Content of the Soil. The Physical Structure of the Soil. The Hydrogen-Ion Concentration of the Soil Solution. 3. Plant Response. Leaf Structure of the Chief Constituents of the Ceratopetalum-Doryphora Association. Leaf Structure of the Chief Components of the Hucalyptus piperita- E. haemastoma Association. Root-systems. The Ultimate Conception of the Vegetation of Mount Wilson. 5. Summary. 1. Introduction. The previous studies (Part i, 1924, Brough, McLuckie and Petrie; part ii, 1925, Petrie; Part iii, 1926, McLuckie and Petrie) of the vegetation of Mount Wilson have brought to light many interesting problems, the solution of which demands intensive study. The most outstanding feature of the vegetation of this region is the great contrast between different associations occurring in close juxta- position: sclerophyllous Hucalyptus Forest alternating with Sub-tropical Rain Forest frequently and sharply in a comparatively small area. This condition has led us to make a more detailed enquiry into the habitat factors which are probably responsible for these remarkable distributional features, and the results of the investigation form the subject of the present communication. Owing to the absence of a properly equipped permanent field laboratory, the scope of quantitative investigations was somewhat limited. From what has been done, however, it is possible to deduce, in a general manner, what are the basic factors controlling the distribution of the plant communities in this region, and to give an explanation of some of the remarkable features which were recorded in the previous papers. A number of more detailed observations are also recorded upon the ecological structure of the vegetation and upon the nature of its responses to the environment. Vv 162 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. We have to record our indebtedness to Mr. D. J. Mares, Commonwealth Divisional Meteorologist, for rainfall and temperature data which have been utilized in this paper. 2. THE HapitatT FACTORS. It is evident that in a small region like that under consideration, certain factors, e.g. climate, will be practically uniform throughout, and, although stamping their impress on the nature of the vegetation, are not directly the cause of the diversity of habitats within the region. Neither rainfall nor the general regional features of climate and season are variable to any marked extent at Mount Wilson, although it must not be thought that they are without their effect on the vegetation; but it is in other directions that one has to seek for the explanation of xerophytic and mesophytic associations existing side by side, and for the occurrence of Rain-Forest in a region with a rainfall rather below that of the typical habitat of that association-type. From what has already been written it will be clear that the edaphic factors, rather than the climatic, are of fundamental importance in producing the great differences in habitat which result in the presence of these two types; and it appears that we have here an example of compensating factors; in a region in which the climax association-type is sclerophyllous Forest, a local high edaphic favourableness apparently produces the same resultant as would a much higher rainfall with a poorer type of soil; so that a “post-climax’’, to use Clements’s term (Clements, 1916), is here possible in the form of mesophytic Forest. It has also been made evident, however, that it is only in places where exposure is favourable that this effect is produced, so that exposure becomes a second factor of outstanding importance. It is therefore the edaphic factors, and the atmos- pheric humidity, which depends largely on exposure, that have claimed the greatest consideration in the present enquiry. Among the general problems of distribution which it was hoped to elucidate are the following: (1) The comparatively small amount of invasion of the basalt by types from the Eucalyptus Forests of the sandstone. (2) The reason why the Rain-Forest grows equally well in the sandstone gullies and on the basalt caps. | (3) The absence from the basalt of certain Rain-Forest components in the sandstone gullies, such as Callicoma, Todea, Blechnum capense and Histiopteris incisa (see Part iii). CLIMATE OF THE REGION. Temperature. No regular records have been taken at Mount Wilson, but the accompanying averages (Table i) of an eight years’ record at Mount Victoria, which is only a few miles distant and is of approximately the same altitude, will give a sufficiently accurate conception of the nature of this factor in the region under study. From these figures it is seen that the extremes are moderate; and although the summer months are fairly hot, the comparatively low minimum values in winter, and the occasional occurrence of snow, are undoubtedly of great significance in controlling the development of the Rain-Forest. We have described it as a luxuriant forest; yet it has not the tropical luxuriance of the more northern Rain- Forests. The floristic composition is comparatively limited, and there are only two dominants; whereas a tropical forest is characterized by great floristic variation. The structure is not excessively complex. The common features of a BY J. MCLUCKIE AND A. H. K. PETRIE. ° 163 TABLE i. Monthly Temperature Averages at Mount Victoria. | | Mean Maximum. Mean Minimum. Month. Degrees Fahrenheit. Degrees Fahrenheit. January Reacts: Sey pL ieee 74-7 53:6 TRAUEIRY ca ou Go oe | 73:3 54-3 March .. : | 68:6 51-0 April 5) or. oe oe er eee ee 61:7 46-3 May Akush nical onary et CS MECC | 53:8 41:6 INCOME Ee! pre ys 6 a 48-4 | 37-3 July 5 Sia EApruee Es acne 41-6 | 35-2 August Set UN as ie RIO le 51-6 | 37-0 Sepiemalaee o5 boa G0 oc | 58-8 | 39-6 October JSS eee a an A 65-4 | 44-3 INIOWENM NS oo oo po <6 | 71:5 | 48-0 IDYXOEIIN GVO 56 bo oa los 74-9 50:6 | Average for year .. =. | 62-4 44-9 | tropical Rain-Forest, e.g. very large leaves, plank buttresses, cauliflory, or epiphylly, such as are found even in the coastal forests of the same latitude in New South Wales, are practically absent. While epiphytic mosses and lichens are abundant, epiphytes of Pteridophytic and Angiospermic affinity are not profuse. Indeed, we are driven to realize that the luxuriant physiognomy of the Rain-Forest at Mount Wilson is imparted not by tropical structure and adaptation, but by its wealth of Pteridophytes and by its closeness of structure arising from high edaphic favourableness. Features such as these are in accordance with what one would expect in a montane sub-tropical or temperate Rain-Forest; and although the moderate rainfall is an important factor in causing them, there is no doubt that low temperatures in winter are also effective to a considerable degree. Rainfall. While the Blue Mountains as a whole have an average annual rainfall of 30 to 40 inches, Mount Wilson is exceptional in having the higher value of 46 inches. In Text-fig. 1 is given the monthly variation at Mount Wilson and also that at Mount Victoria, a more typical Blue Mountain area. It will be seen that not only is the rainfall at Mount Wilson higher than that at Mount Victoria throughout the whole year, but during the summer it is much higher: the maximum precipitation takes place during the hottest months, December to March. This state of affairs is of considerable importance in connection with the occurrence of the Rain-Forest at Mount Wilson. While the basalt soil is the main factor leading to the development of this community on the plateau, there is no doubt that were it not for the high summer precipitation it would be a much less favourable habitat for the Malayan Rain-Forest types which at present characterize it. During the winter when desiccation is less, the smaller rainfall is not deleterious. At Mount Victoria, although the maximum rainfall is also in the summer, it is not by any means so high; and this fact probably explains in part the 164 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. MAR. | APR. | MAY. |JUNE.|JULY.] AUS. | SEP | OCT.] NOV, [DEC | JAN. | be v A pyanlt |e Text-figure 1. Annual rainfall graphs for Mount Wilson and Mount Victoria. occurrence of Rain-Forest in shallow sandstone gullies at Mount Wilson which at Mount Victoria would probably be occupied merely by sclerophyllous Hucalyptus Forest. The basaltic soil and the comparatively high summer rainfall then, are respon- sible for the maintenance of the luxuriant vegetation of the Mount Wilson area. HUMIDITY AND EVAPORATIVE POWER OF THE AIR. Methods. At the beginning of September, 1924, measurements were made of the evaporative power of the air in different habitats in order to obtain some knowledge of the requirements of the vegetation with regard to this factor. As standard Livingston atmometer cups were unobtainable at the time, evyaporimeters were made from Chamberland filter-candles attached to burettes by a piece of rubber-tubing, the whole being carefully filled with water so as to avoid the inclusion of air-bubbles. As it was desired to compare daily with nightly readings in the Rain-Forest to ascertain whether conditions bordering on satura- tion obtained there, burettes were used in place of the jars more commonly associated with the Livingston atmometer. This apparatus gave a rapid and accurate record of the water evaporated; it was found, however, during preliminary tests in the laboratory, that in a very humid atmosphere the presence of a column of water in the burette above the level of the filter candle resulted in a tendency towards exudation of water through the pores of the porcelain. To avoid this in all the evaporimeters used, the filter was raised above the level of the water in the burette by the insertion of a vertical piece of glass tubing between the filter and the burette. After this was done, and so long as the water in the burette was not above the level of the filter, trials in the laboratory showed that in an atmos- BY J. MCLUCKIE AND A. H. K. PETRIE. | 165 phere of constant humidity the rate of evaporation was constant, and was not measurably affected by the level of water in the burette. Shreve (1914, p. 43) has pointed out that atmometer readings taken in very dry and very moist climates are not strictly comparable, owing to a difference in the character of the evaporating water-film; and this objection would probably apply to our comparisons of readings taken in the Hucalyptus Forests with those in the Rain-Forests. The error, however, is not likely to be large enough to influence the general conclusions to be drawn from the results cbtained. The evaporimeters, although having approximately the same rate of evapora- tion, were standardized in the laboratory by comparison with the evaporation from an open water surface, whereby a factor was obtained for each evaporimeter. By this means the readings were standardized to the evaporation in cubic centimetres from an open water surface one square metre in area in which form they are expressed in the results given in Text-fig. 2. Readings were taken early in the morning and at sundown for five successive days, the total evaporation for the twelve hours representing day or night being calculated therefrom. The total daily and nightly evaporation for the whole period is given for each station in Text-fig. 2. Discussion of Results. This comparative study of the evaporative power of the air in different habitats gives an interesting confirmation of our observations upon the effect of the exposure on the distribution of the various communities. The Rain-Forest, as we have previously stressed, is limited to the most sheltered habitats; and it is seen that the evaporative power of the air within it is very much less than in any other habitat. Water vapour appears to arise in considerable amount from the damp soil, forming a humid layer among the ferns on the floor of the forest. Owing to the deep shade and the extreme absence of wind in the forest, the moisture-content at the ground-level is high, and must border on, and no doubt at times attain saturation during the night. The greatly increased insolation at high levels in the Forest lowers the relative humidity and causes a striking difference between the values for the two strata expressed in the diagram. No such dissimilarity is noticeable in the more open communities, where there is little difference in the insolation of the various strata. The Alsophila society of the Hucalyptus goniocalyx-E. Blazxlandi association has been described as much more tolerant of exposure, avoiding only the full brunt of the westerly winds on the open summits of the basalt caps, which are occupied by the Pteridium society in the H. Blaxzlandi consociation (Part ii, p. 149). The results from stations 4, 5, and 6 show that the Alsophila society can withstand very high atmospheric dryness. The values in stations 5 and 6 are even higher than that in station 8 in the H. piperita Forest; and, although it is to be expected that more exposed westerly regions in the latter community would give higher values still, it is nevertheless evident that the series of increasingly mesophilous communities is not distributed in a series of habitats characterized by a corres- pondingly increasing atmospheric humidity. We are therefore led to suppose that the distribution of the Alsophila society is governed mainly by soil-moisture, and that it is very largely indifferent to exposure, except perhaps where it reaches an extreme on the open summits of the basalt caps. The low values of the evaporation during the night periods are sUsleningant since the westerly wind prevalent during the day ceases in the evening. COLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. Oj AN I 166 ay} JUoseIdel SUI] Youlq Iu ey} jo uorT}eUT}se jo synsea.t 008 OT ‘VYUSIU BY} JOJ SAIOIII}UL 9JIYM YY} YIM VSO} ‘potsed AVp oy} JOJ UOTVeIOdevAD 009°6 JO UOorl}e]UEeSIIdeI ‘S}VUIGVY SNOLIVA UI JIB 94} JO JAaMOd SATVIOdvAD OIVUIWIBISBIG “% IINSY-}x9 7, ‘AOVAIUNS YUALVAA NGdO AO ‘W ‘OS Ud “SOO NI NOWVYOdVATT 00F'8 008'L 0009 008°F 009°¢ 00F 008‘T 0 =F — ——— ‘CWs) wmjenNs qniys ‘‘0q “IoOyY ! neaze[d Jo oa}Uea !uOoTJeIOOSUOD DYIIadI = SsnidAhjpaonW, ‘USI V9 {0d “USI “IIE :ado[s “A-"N jo }tuunsS { AJaTOOS win}eBINs D)ydos] PY :UOI}VIOOSUOD LALYIOIWOH snzdfhjpvong “TUINRIYS Udey-801) 2 "Od “IOOY '4SeA WoTy pelszays ‘6gp “‘d ‘t WAV ‘eg ‘“By-}xey Jo WSII uo sdo[s A[JeJsaM !AJOIOOS uM} BNS oprydos;Y !uoIyeIOOSUOD wApYI0IMWOH snjdfhjpong WIM} BIIS UIeJ-99.9 | 0d “IOOY. YSaaoy S}LVSseVeq !UOT}PVIOOSSY DLOYAMRLOd-wnNjY,ad0ID4LaD wn” cr) Er) BY J. MCLUCKIE AND A. H. K. PETRIE. — 167 THE MOISTURE-CONTENT OF THE SOIL. A large number of samples of soil were collected at various times at Mount Wilson, in each case after a moderate spell of dry weather. These samples were passed through a 3 mm. sieve and the moisture content was then estimated by drying at 100° C. Ceratopetalum-Doryphora association (basalt). Ceratopetalum-Doryphora association (sandstone). Eucalyptus goniocalyx consociation; Alsophila stratum-society; Blech- num discolor fern society. Eucalyptus goniocalyx consociation; Ptcridium society. Eucalyptus piperita consociation. ° 10 20 30 40 50 PERCENTAGE MOISTURE IN FRESH SOIL. Text-figure 38. Graphical representation of the soil-moisture ranges of the main associations. The ranges for the values obtained for the soil-moisture of each association are given in Text-fig. 3. It must be understood that these ranges might possibly be found to be somewhat greater if samples were taken continuously throughout the year; they are nevertheless indicative of the striking features of difference between the habitats of the various communities. From an examination of Text-fig. 3 it is seen how the range of soil moisture- content for the Rain-Forests, whether on sandstone or basalt soil, does not vary beyond 13%. Thus, although a lower minimum may perhaps sometimes be reached, comparison with the ranges of the other communities at once suggests that the distribution of the Ceratopetalum-Doryphora association is determined by water- content of the soil: the association as a whole is apparently independent of soil- type, so long as it finds the necessary high moisture-content. This view is supported by the occurrence of the Rain-Forest on other soils, e.g. shales, in other parts of the State. The Alsophila society of the Eucalyptus goniocalyx consociation is not limited to the same extent by moisture-content, the values ranging from 45-2% near the Rain-Forest to 23-5% at the outer boundary; it is probable, however, that there is a minimum value for the lower extremity of the range (in the neigh- bourhood of 20%) for the habitat of this community, beyond which it is replaced by the Pteridium society. It may be asked why the high value of 45-2% is attained in this open community: the answer appears to be that the dense fern stratum may protect the soil from evaporation just as much as the Rain-Forest tree canopy. If then the soil is capable of holding this high percentage of moisture it would be expected that the Ceratopetalum-Doryphora Forest would be occupying the habitat; but, as we have seen, the exposure and the prevailing atmospheric humidity are not suited to the requirements of the Rain-Forest here, and in a strong westerly wind this high moisture-content no doubt decreases rapidly. The Pteridium society appears to be one step further in the succession of the mesophilous to xerophilous communities; it is also noticeable that the Hucalyptus goniocalyx consociation is evidently confined to soils of a minimum soil-moisture 168 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. range, which, although low, is much higher than that of the #. piperita consociation. The HE. piperita Forest has the lowest values, and there is no doubt, more- over, that after periods of drought the minimum value would be even lower than that given. It is thus clear that the sandstone plateau is a highly xerophytic habitat. It is probable nevertheless that, since water drains rapidly downwards to the lower levels in sandstone soil, it does not have time to dry out between falls of rain, more especially as we have seen that the rainfall is fairly evenly distributed throughout the year. The comparison of the soil-moisture values of this series of communities indicates clearly how the zonation of vegetation tends to coincide with a zonation of soil-moisture. There is no doubt that the falling gradient is increased by the progressive decrease in the capacity of the vegetation to conserve soil-moisture by shade and humus production. It appears then that the Ceratopetalum-Doryphora, Hucalyptus goniocalyz-H. Blaxlandi, and EH. piperita-E. haemastoma var. micrantha associations are adapted to habitats of decreasing soil-moisture content: each will occupy the habitat where it finds its range, provided the other controlling factor of exposure permits; if this does not, one of the following associations in the series will occupy the habitat. The more xerophytic communities are no doubt excluded from the more mesophytic habitats by competition. THE PHYSICAL STRUCTURE OF THE SOIL. Samples of soil were taken at a depth of six inches from a number of typical habitats, and on arrival at the laboratory they were passed through a 3 mm. sieve. Two portions were then removed, the one being dried at 100° C. and ignited for the estimation of humus, the other being analysed mechanically by the method adopted by the British Agricultural Education Association (see appendix to Russell, 1921). The smaller separations, such as coarse and fine sand, were not made, as only the salient features of difference between the various soils were required. The results of these determinations are given in Table ii. Discussion of Results. Obviously the great difference in the physical structure between the basalt and sandstone soils will be a key to a number of other factors, since it will affect the aeration, moisture-retaining capacity, colloidal properties, etc., and will also be likely to have a marked influence on the root-systems. Aeration is one of the chief concomitants of the physical structure of a soil; and it is well known that sandstone, open and porous in nature, is abundantly ventilated and well drained, while clays, on account of the smallness of the component particles are poorly aerated and poorly drained, and tend to be infertile through lack of calcium carbonate. ! | i 7 170 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. content, which appears to counteract the effect of other components, the soils are perhaps not so fundamentally different in their influence on vegetation. Conse- quently it is not suprising that the actual number of plants with soil preferences were found to be very few (Part iii). Such preferences as appear to exist are probably in most cases the results of differences in properties of the soil solution. Although the humus will have this striking effect near the surface, at depths of some feet its content in soils decreases rapidly, as is indicated in the present instance in samples 5 and 6, and eventually becomes quite low. At the same time the basalt soil is deep, since the rainfall is such as to cause rapid and penetrative weathering, and water and organic acids from the humus percolate through the soil and decompose the underlying rock. It is clear then that at greater depths the soil will not receive the beneficial effects of a high humus content; so that the vegetation would be expected to root in the upper regions if it is a type adapted to a well aerated soil. This point will arise again for discussion in a later portion of the paper. The large percentage of clay and humus in sample 1 is plainly the key to the high moisture-retaining capacity, and consequent mesophilous vegetation, of the basalt soil. Probably, however, in the surface layers the humus is more important in this respect than the clay; for, as is usually the case, the moisture- content closely follows the humus-content. Text-fig. 4 shows that the ranges of I Ceratopetalum-Doryphora association H ae CREO | t Ceratopetalum-Doryphora association igtiiiet eres (sandstone). Eucalyptus goniocalyx consociation; Alsophila stratum-society; 3lech- riggs dale num discolor fern society. | Eucalyptus goniocalyx consociation; Pteridium society. Eucalyptus piperita consociationu, Ee i re) 10 20 30 40 PERCENTAGE OF HUMUS. Text-figure 4. Graphical representation of the humus-content-ranges of the soils of the main associations. these two properties correspond in a striking manner. It is thus the water- retaining capacity of the humus which makes it possible for the soil-moisture of the sandstone habitats clothed by Rain-Forest to be as high as those of the basalt, despite the absence of clay from the sandstone soil. It must be added, however, that the stations in the sandstone Rain-Forest from which samples were taken for moisture estimations were more particularly in the erosion channels occupied by Dicksonia and Todea, no samples unfortunately being taken from the apparently drier slopes devoid of tree-ferns; and, moreover, the Rain-Forest on the sandstone occurs only in valleys, where water is continually draining down from the high- lands. In this connection it is interesting to note that, as was mentioned previously, the Rain-Forest at Mount Wilson occurs in gullies which on the other parts of the Blue Mountains would probably be occupied by a much more xerophytic community, since the water supply would not be sufficiently constant. In such habitats the gravitational water drains away rapidly and during a dry period disappears from the heights and so causes the gullies to become dried BY J. MCLUCKIE AND A. H. K. PETRIE. Abra up. Hence the suggestion is offered that the water supply for the gullies at Mount Wilson is to some extent kept uniform and continuous by slow drainage from the basalt caps; owing to the low capillary power of such heavy clay soils the water would be conserved after rain and would be allowed to drain away slowly and uniformly, thus maintaining a constant supply for the gullies below. This does not depreciate the previous statement that the humus is the main factor controlling the moisture-content of the soil, since these two factors are reciprocal: the formation of a water-retaining Humus depends on the nature of the aspect and the vegetation allowing an accumulation of moisture in the soil: and were it not for this humus the water would probably dry out from the sandstone soil. The relationship between moisture-content and humus is probably responsible also for differences in the properties of the organic portion of the various soils. The moist volcanic soil and the moist and well-aerated and well-drained soil of the sandstone gullies must favour the production of a “mild humus”, as in such habitats earthworms, fungi, and bacteria flourish; in particular the effect of earthworms is important since large species are abundant on the basalt and prove an important factor in ventilating the soil. On the other hand the dry sandstone soil forms a very different medium for the existence of these organisms, so that little humification goes on; in this case, therefore, although 7% to 8% of organic matter was found it is improbable that it would have the same moisture- retaining capacity as that of the more humid habitats, and therefore is contributing to the xerophytic nature of the sandstone soil. This absence of humification in the habitat of the Hucalyptus piperita-E. haemastoma var. micrantha association adds point to its facies, as the bare patches between the individual plants are usually occupied by fallen leaves, twigs and branches, which in a more humid forest would soon rot away, but which here dry and accumulate until they provide material for the next forest fire. A consideration of the analytical results shows that apart from the basalt there is no fundamental difference in the physical structure of the other soils. There is no evidence of mixing of the two main types except in the case of the basalt which contains a fairly high extraneous sand fraction, probably blown in by winds. The clay and silt fractions of the sandstone soils are largely composed of ferric oxide, a common mineral in the Hawkesbury sandstone, and which comes down with these fractions in the analysis. Samples such as 9 and 20 show that even on steep slopes there is no evidence of basalt soil being carried down very far and mixed with the sandstone, although there is no doubt that a mixture occurs in the ecotone region of the Rain-Forest referred to in Part iii (p. 98); the main erosion of the basalt, however, takes place in definite drainage channels, and has been described already (Part iii, p. 105). In Part iii (p. 108) a description was given of the extension of the Hucalyptus piperita consociation to the basalt on a westerly slope. This spread is apparently only a small one, since the analysis of sample 14 shows that the Lomatia society is actually on the sandstone side of the junction, although from field observations we concluded that the soil was basalt. The salient feature of this part of the investigation is the striking corres- pondence between the ranges of the moisture- and humus-contents of the soil. The clay fraction of the basalt soil holds sufficient moisture to provide a suitable substratum for the development of a rich humus, and is aided by shade and humidity in the Rain-Forest. This explains the mesophytic structure of the vegetation of the basalt soil, a vegetation which extends on to the sandstone only 172 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. on slopes or in valley floors which are damp through drainage. The predominant 5; effect of the basalt soil on the distribution of the various associations depends almost solely upon its capacity for retaining water. Up to this stage then we seem to have found two outstanding factors controlling the distribution of the plant associations. The first of these is aspect, which has both a direct effect on the vegetation through the atmospheric humidity, and also an indirect effect by influencing the evaporation of water from the soil. The second factor is the moisture-content of the soil, dependent on the humus, which in turn is dependent on the clay fraction of the basalt soil, upon drainage and upon shade. THE HYDROGEN-ION CONCENTRATION OF THE SOIL SOLUTION. On account of the high base-content of basalt soils, and the continuous filtering of water through it, it was thought probable that leaching would have an influence on the soil acidity; in any case the latter was likely to be a factor of interest in a region so marked as Mount Wilson in edaphic variation. Clark and Lubbs’ indicators were used for the estimations of the hydrogen- ion concentration of the soil. The procedure was based on Wherry’s field-method (Wherry, 1920), with certain modifications: thus it was found necessary in the case of soils which remained turbid for a long period to filter them through ashless filter-papers, having carefully leached these until the washings gave a neutral reaction with brom-thymol blue; it was also found advisable to use the same quantity of water for each extract in order to obtain comparative results, a conclusion arrived at also by other workers (Wherry, 1924). In Table iii are given the P, values for samples taken at a depth of 6 inches from the various habitats. Each represents the results of a number of deter- minations from different parts of the community. The acidity was found to be practically uniform in these habitats at depths from 2 to 8 inches. TABLE iii. Hydrogen-Ion Concentration of the Soil Solution from the Habitats of the Main Communities. me Ceratopetalum-Doryphora association; basalt .. .. doa) PE 7/O10) Eucalyptus Blaxlandi consociation; summit of basalt cap. oa, Web) E. goniocalyx consociation; Alsophila society .. .. .. .. 6:5 E. goniocalyx consociation; Pteridiwm society BOS Tea rel. ORS eb) EH. piperita consociation we Pchiec MMLUCCGT NERS AALL | Asay a ent” cud) Ceratopetalum-Doryphora arneseniten 2 sandstone ad) bay gree] Pee ROLD The lack of variation in these results is a prominent feature. Despite the high content of bases, such as calcium, characteristic of basalt soil, the buffer action apparently prevents any fluctuation in the hydrogen-ion concentration of the soil solution. In all the soils except the dry sandstone the high content of colloidal material in the form of humus and also of clay in the case of the basalt, readily explains this buffer action; in the case of the sandstone it is to be presumed that the absence of an appreciable quantity of basic material on the one hand, and the absence of much humification or abundance of respiring root-systems on the other, mitigate any tendencies towards departure from neutrality in the soil-moisture. From this it is clear that the hydrogen-ion concentration of the soil solution is not a factor of significance in the study of the distribution of the vegetation at Mount Wilson. BY J. MCLUCKIE AND A. H. K. PETRIE. 173 3. PLANT RESPONSE. In preceding communications on the ecology of the Mount Wilson area, we have described the main features of the physiognomy and distribution of the flora and have endeavoured to interpret these as responses to certain factors or factor complexes of the environment. In the present paper we have endeavoured to analyse the environmental factors and to deduce the relative significance to the flora of each of the more important. We have indicated the outstanding differences in the various plant associations which occur throughout this area, and now furnish an account of the chief anatomical characters of the most important types of these associations. As Cannon (1924, p. 103) points out, two different and important groups of factors must be considered in the attempt to interpret the anatomical peculiarities of plants from the physiological point of view, namely heredity and immediate environment. The fact that different genera of the same family and even different species of the same genus attain to harmony with the environment by the most varied anatomical characters, seems to us to indicate that another set of influences of an hereditary nature is acting simultaneously with the present environment, and that the structure of the living types is, generally speaking, the result of the impress of two different categories of forces. On the other hand the physiologist knows on experimental grounds that certain characters are definitely plastic and modifiable by changing environment; hairiness may be replaced by glabrousness by cultivation in a more humid atmosphere; sclerophylly may be replaced by more mesophytic characters under similar conditions; nanism may give way to a taller habit; in short most of the characters of a highly xerophytic plant are changeable under a changed environment, provided it acts for a sufficiently long period during the develop- ment of the individual. The different “adaptations” of plants to the more xerophytic or mesophytic conditions appear to us to support the view that the present structure is the resultant of factors now operating but modified in certain respects by the cumulative influence of hereditary forces. This is all the more reasonable when we consider that members of the same family growing under precisely the same conditions in the same locality, show, amidst a general similarity of response certain individual differences. Speaking generally the types from the Ceratopetalum-Doryphora Rain-Forest (as the following descriptions will show) have thin unwettable cuticles, little or no sclerenchyma, stomata flush with the epidermis and without the outer vestibule characteristic of xerophytic types, poorly developed palisade and a great development of spongy mesophyll with large air spaces. The types from the Eucalyptus piperita-H. haemastoma association on the dry exposed sandstone habitat have stomata sunken in grooves or pits, hairiness, considerable sclerenchyma as hypoderma or as girders associated with the veins, strongly developed palisade and proportionately poorly developed spongy mesophyll, tannin deposits, enormously thick cuticles and outer epidermal walls, and frequently oil sacs. In these xerophytic types the outer epidermal wall is generally heavily thickened owing to the deposition of anhydrides under the influence of the desiccating conditions. Strong cuticularization is a prevailing feature as the deposition of cutin is intimately associated with the transpiratory activity of the leaf. In the species of Banksia mentioned the stomata occur in pits, the cuticle of which is poorly developed. The stomata are usually sunk below the general surface of the leaf, and the cuticle forms, in many types, a prominent ridge overarching the guard cells, thus constricting the approach to them. 174 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. Between these two extreme groups of structures are those displayed by components of the Eucalyptus goniocalyx-E. Blaxlandi association which develops on a much less xerophytic habitat than the HL. piperita-E. haemastoma association. The anatomical characters common to these components of the associations at Mount Wilson may be seen more readily from the following descriptions and figures. LEAF STRUCTURE OF THE CHIEF CONSTITUENTS OF THE Ceratopetalum-Doryphora ASSOCIATION. Fieldia australis. The chief characteristics are (a) the very thin cuticle for facilitating cuticular transpiration, (0b) the poor development of palisade tissue owing to growth in a shaded environment, (c) the extensive intercellular space system of the leaf facilitating aeration and transpiration (the air channels being internal evaporating surfaces), (d) the poorly developed vascular tissue, (e) the numerous short hydathodes for secretion of excess water, and (f) the numerous stomata on the lower surface for aeration and passage of water vapour. These are structural features which characterize a type growing in a shaded moist environment, where aeration and transpiration require to be stimulated as far as possible by anatomical deviations from the normal type (Text-fig. 5, 5a). It has been shown earlier in the paper that in the lower strata of the Rain-Forest, which form the habitat of Fieldia, the atmospheric humidity is often in the neighbour- hood of saturation. Text-figure 5. Section of leaf of Fieldia australis. x 115. Text-figure 5a. Hydathode of Pieldia australis. x 300. Text-figure 6. Section of leaf of Atherosperma moschatuwm. x 115. Atherosperma moschatum. In this type the cuticle and outer epidermal cells are thin; the stomata are numerous and on the lower surface only. A hypodermal layer of relatively large clear cells is present on the upper surface, suggesting an aqueous tissue in structure; a narrow palisade layer is developed, while a loose spongy mesophyll occupies more than half the cross section of the leaf. BY J. MCLUCKIE AND A. H. K. PETRIE. 175 The palisade layer contains relatively more chromatophores than the cells of the spongy mesophyll (Text-fig. 6). Doryphora sassafras also has a hypodermal layer of clear thin-walled cells devoid of chlorophyll and suggesting an aqueous tissue. This may be correlated with the fact that Doryphora frequently grows in more illuminated and drier situations than prevail in true Rain-Forest areas. The palisade layer is narrow with considerable spaces between certain cells, and large lysigenous oil-glands. The spongy mesophyll occupies more than half of the cross section of the leaf as in Atherosperma. The stomata are numerous and occur on the lower surface. The cuticle on both surfaces is thin (Text-fig. 7). Text-figure 7. Section of leaf of Doryphora sassafras. x 115. Text-figure 8. Section of leaf of Ceratopetalum apetalum. 5 Lala, Ceratopetalum apetalum. There is no hypodermal layer below the upper epidermis as in Atherosperma and Doryphora, while the palisade layer is slightly more elongated in comparison with those types. The spongy tissue is extensively developed, while a few isolated tannin cells are distributed through it. A few comparatively thick-walled cells surround the vascular bundles. The cuticle on the upper surface is more strongly developed than in the previous types (Text-fig. 8). Quintinia Sieberi. This is also a typical mesophyte which frequently starts development from seeds deposited on the trunks of treeferns etc. Compared OS a oe eareherare bpe@ae aT Text-figure 9. Section of leaf of Quintinia Sieberi. x 115. Text-figure 10. Section of leaf of Callicoma serratifolia. x 115. 176 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. with Atherosperma, Doryphora, and Fieldia, the palisade is more strongly developed, although the proportion of palisade to spongy mesophyll is only very slightly different. Thick walled cells are absent from the smaller veins, while stomata are both numerous and flush with the other epidermal cells (Text-fig. 9). Callicoma serratifolia occurs in water courses and drainage channels through- out the sandstone and consequently shows an anatomical structure intermediate between the mesophytes of the Rain-Forest and the xerophytes of the Hucalyptus piperita forest. The upper cuticle is much thicker than in Ceratopetalum. 'The hypodermal layer contains a tannin-like deposit, the palisade layer is better developed and occupies more than half of the cross section of the leaf. Air channels are extensive, stomata are numérous, and hairs are developed from the lower epidermis. Numerous thick-walled cells occur on the adaxial and abaxial surfaces of the vascular bundles. These are characteristics which stamp Callicoma as a form somewhat intermediate between the Rain-Forest Flora and the highly xerophytic individuals of the exposed sandstone habitat. (Text-fig. 10). LEAF STRUCTURE OF THE CHIEF COMPONENTS OF THE Hucalyptus piperita- E. haemastoma ASSOCIATION. Telopea speciosissima. The upper cuticle is very thick and laminated, the outer epidermal wall is also thick, and the palisade tissue is composed of elongated cells occupying about half the cross section of the leaf; stereids occur Text-figure 11. Section of leaf of Telopea speciosissima. x 115. Text-figure 12. Section of leaf of Persoonia salicina. x 115. as strengthening cells both in the palisade and spongy mesophyll. The latter is composed of small cells in the centre and more elongated cells within the lower epidermis somewhat suggesting a palisade layer. The cuticle of the lower epidermis is very papillate and forms a cuticular ridge over the stomata which are sunk slightly beneath the other epidermal cells. A small outer and large inner vestibule occur in association with the guard cells—a character to be expected in a xerophytic sandstone type (Text-fig. 11). BY J. MCLUCKIE AND A. H. K. PETRIE. ° 177 Persoonia salicina is an isobilateral type in which palisade tissue is developed on both surfaces, with larger air channels than might be expected in a xerophytic type. The leaf is thick and slightly succulent, and intensely green owing to the enormous chlorophyll content of the cells. The centre of the leaf is occupied by large colourless cells with mucilaginous sap, and cells with thick stratified mucilaginous walls. Isolated stone cells also occur. The guard cells are not so sunk as in Telopea, possibly owing to the vertical position assumed by the lamina through the twisting of the petiole through an angle of 90°. The cuticle is not nearly so thick as in Jelopea, and forms a smooth layer on the surface (Text- iiez, 1074) . Banksia serrata is one of the most extreme xerophytic types in this associa- tion. The upper epidermis is covered by a very thick smooth cuticle; a hypo- dermis of two or three layers of clear cells probably represents an aqueous tissue. The palisade tissue is developed in relation to the cavities on the lower surface, and is composed of long narrow cells with large air spaces between them. The cavities occur at frequent intervals and are lined by epidermal cells, interrupted by raised stomata, and producing twisted hairs. Directly beneath the cavities there is developed a very loose network of mesophyll cells containing few chloro- plasts compared with the palisade cells. The vascular bundles are strengthened by means of sclerenchyma extending as girders from one epidermis to another. The lower epidermis, excepting that of the cavities, is strongly cuticularized while a hypodermal layer of colourless cells is situated beneath the epidermis (Text- fig. 13) (compare Hamilton, A. G., Aust. Ass. Adv. Sci., 1907, Adelaide, p. 484, 1908). ai es stnepet Soe eek 6 =. sale re 5 pou J wi | Text-figure 13. Section of leaf of Banksia serrata. x 115. Text-figure 14. Section of leaf of Persoonia acerosa. x 115. Persoonia acerosa. The cuticle of this pinoid type is fairly thick, and the guard cells are depressed at the base of the outer vestibule formed by the cuticular ridges. The palisade tissue is arranged concentrically within the epidermis. The centre of the leaf is occupied by the vascular bundle and by colourless cells, some of which contain starch, and others probably represent aqueous tissue. Isolated groups of sclerenchyma cells occur in the mesophyll, and in relation to the vascular bundles. The air space system is more elaborate than might be expected in a xerophytic type (Text-fig. 14). Ww 178 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. Banksia spinulosa. In this type the leaf margin is recurved, and numerous slightly raised stomata occur in the cavity so formed. Hairs arise from the epidermal cells in the vicinity of the guard cells, which open into fairly large sub-epidermal chambers or cavities. Very little tissue of a spongy nature is developed, while about three-fourths of the cross section of the leaf is composed of elongated palisade cells with very narrow intercellular spaces. The cuticle is strongly developed on both surfaces, while the outer epidermal wall is thickened; the hypodermis is composed of deeply staining tannin cells and sclerenchyma. All the anatomical characters of this type confirm the xerophytic structure of the leaf to be expected from the habitat of the plant (Text-fig. 15). Hakea dactyloides is an isobilateral type with strongly developed palisade on both surfaces. The main bundles are surrounded by sclerenchyma developed as girders connecting the surfaces of the leaf. The centre of the leaf is occupied by colourless loosely arranged cells, while the stomata are deeply depressed and the ridges of the thick cuticle form comparatively large cavities above the guard cells. Many of the epidermal cells contain a deepiy staining substance like tannin (Text-figs. 16, 16a) (compare Hamilton, A. G., Proc. Linn. Soc. N.S.W., 1914, p. 152). Text-figure 16. Section of leaf of Hakea dactyloides. x 115. Text-figure 16a. Surface view of cuticular ridges overarching the guard Céellss xX eLs: BY J. MCLUCKIE AND A. H. K. PETRIE. ' n9 Eucalyptus piperita has an isobilateral type of leaf, with compact palisade tissue and narrow air spaces. Stomata are found on both surfaces, while aqueous tissue occupies the centre of the leaf on each side of the main vascular bundles. Sclerenchyma is formed in association with the chief vascular bundles and forms a girder across the leaf. A layer of water-jacket cells is frequently present on each side of the vascular bundles. The cuticle is very thick, but the outer epidermal wall is exceptionally thin (Text-fig. 17). : ——— oo \ Hl Mh) iat a Hh Me ! a iA : mn He un a Sy ae aii \ i Text-figure 17. Section of leaf of Hucalyptus piperita. x 115. Text-figure 18. Section of leaf of Hucalyptus haemastoma. x 115. Eucalyptus haemastoma resembles #. piperita in its isobilateral structure. The chief differences are in the greater development of the cuticle, and the definite central aqueous zone between the palisade of the lower and upper surface. The guard cells of this type like those of H. Blaxlandi are distinctly elevated, but protected by a well-developed outer vestibule formed by the enormously thick cuticle. The very narrow intercellular spaces and the consequent compactness of the palisade cells of this species are definite indications of the necessity of rigid control of the transpiring surface, both internal and external. The large proportion of oil glands in these two species may be regarded as an indication of their habitat being more xerophytic than that occupied by the species H. goniocalyx and H. Blaxlandi in which the glands are less numerous in the leaf (Text-fig. 18). The components of the H. piperita-E. haemastoma association have adopted sclerophylly instead of succulence as their adaptation to the environment. The majority of the species are glabrous and strongly cutinized epidermal cells take the place of trichomes. Several of the species are isobilateral, and develop palisade tissue on both surfaces. The intercellular space system of the mesophyll is exceedingly variable; but generally speaking, types with strongly developed palisade tissue have relatively small and narrow intercellular spaces. In ‘he spongy parenchyma of dorsiventral leaves the spaces are comparatively larger. Perhaps these features of the photosynthetic tissue may be correlated with the aridity of the habitat. 180 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. The structure of the foliage of the species of Hucalyptus from the various associations characterized generally by differences of environment, indicates some degree of correlation between the anatomical structure and the more important environmental factors, almost amounting to direct cause and effect. In #. goniocalyx the palisade tissue is loosely arranged with numerous inter- vening spaces for aeration, while central aqueous tissue like that in E. haemastoma is generally absent, except in association with the vascular bundles. The cuticle and outer epidermal wall are not so extremely developed aes NU \ iy LG \ ) Text-figure 19. Section of leaf of Hucalyptus goniocalyx. x 115. Text-figure 20. Section of leaf of Hucalyptus Blaxlandi. x 115. as in EH. haemastoma, but nevertheless they indicate a xerophytic type, despite the fact that it grows in a soil with a high water content. Owing to the height attained by the individual and the consequent high rate of transpiration due to exposure and the general evaporating effect of the atmosphere water control is very necessary (Text-fig. 19). In Eucalyptus Blazlandi the same structural features are revealed. As in E. goniocalyx, the guard cells of the stomata are practically flush with the other epidermal cells, or slightly raised and situated at the base of a cavity formed by the overarching cuticle (Text-fig. 20). In these two species of Hucalyptus the stomata are much more numerous than in the sandstone species, and taken as a whole the anatomical characters of their foliage stamps them as being types growing under much more favourable conditions of water-supply than E. piperita and E. haemastoma. As compared with H. haemastoma and E. piperita the number of oil glands per unit area is less—a fact which might be interpreted as having some relation with the difference in the aridity of the habitat. In E£. haemastoma the colourless aqueous tissue forms a definite zone in the centre of the leaf between the abaxial and adaxial palisade. -BY J. MCLUCKIE AND A. H. K. PETRIE. 181 Table iv gives the relative number of stomata in some of the chief components of the various associations: TABLE iv. Stomata per sq. mm. Ceratopetalum- E. goniocalyxz- E. piperita- Plant. Doryphora EF. Blazxlandi EE, haemastoma Association. Association. Association. Upper Lower Upper Lower Upper _ Lower Surface. Surface. |Surface. Surface.| Surface. Surface. Eucalyptus goniocalyx .. (Isobilateral) 33 109 E. Blaxlandi (Isobilateral) 184 188 Alsophila australis 0 99 Acacia melanoxylon (1sobilateral) 236 246 Lomatia longifolia .. 0 205 Drimys dipetala 0 280 Pittosporum undulatum 0 184 Blechnum discolor .. 0 60 Dicksonia antarctica 0 113 Eucalyptus piperita (Isobilateral) 60 107 EH. haemastoma (Isobilateral) 81 Bi Persoonia salicina .. : (Isobilateral) 24 28 Telopea speciosissima .. .. 0 184 Hakea dactyloides .. (Isobilateral) 134 140 THE ROOT-SYSTEMS. The relation of root-reaction and root-type to species distribution is a most important feature of ecological study, and yet, on account of the difficulty of investigation, it has been too much neglected. In the present instance, although no detailed drawings have been made, we are able to place on record some qualitative observations which have proved of interest. ‘The Rain-Forest of the basalt soil is characterized by the superficial root- systems of all its components. The root development of the tree-ferns is meagre and shallow; that of the trees, although spreading broadly and considerably branched, is confined to a great extent to the first feet of the soil. This is clearly a reflex of the conditions of aeration as previously described: the lower layers are probably quite unfavourable for root-growth; at all events no types at Mount Wilson appear specially adapted to deep penetration in this soil. In the sandstone Rain-Forests the root-systems of the trees may be some- what deeper: upon this point our observations are incomplete. It is worthy of note, however, that Callicoma serrdtifolia, in exception to the other types, has a deeply penetrating root-system.. This gives some insight into the absence of this type from the basalt Rain-Forests: if a deep root development is a rigid character, it is obvious that Callicoma could not grow on the heavy basalt soil without being suffocated. Although this suggestion presents itself in the case of Callicoma, it has nevertheless, still to be explained why TJodea barbara, T. Fraseri, Biechnum capense, and Histiopteris incisa occur in the Rain-Forest of the sandstone but not on the basalt; and it must be confessed that no satisfactory interpretation of 182 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. this has been found. The following observations, however, are placed on record in the hope that they may be of use in subsequently arriving at the solution. Todea barbara and Histiopteris in the Rain-Forest are mainly confined to rivulets; such rivulets have not been observed in the basalt Rain-Forests; but one specimen of Todea barbara was seen in a creek running over basalt soil in a Eucalyptus-Alsophila community on the south-eastern side of the plateau. Todea barbara will occur in creeks outside the Rain-Forest in highly isolated habitats on the sandstone; it has also been found, however, in deep shade under damp rocks where there was no trace of running water. It may be that the chemical composition of the soil solution has some influence on the distribution of these types, but this is a fact which still awaits intensive study. The Hucalyptus piperita-E. haemastoma var. micrantha association of the sandstone is characterized by the extremely deep root-systems of most of the components. It has already been explained that there is probably a higher moisture-content in the lower strata of the sandstone soil, and it is now evident that the plants growing thereon penetrate deeply for the apparent purpose of obtaining this; the open texture of the soil permits them to do so without suffocation. By this means not only are the roots enabled to obtain sufficient moisture, but they escape from what is likely to be a high soil temperature in the upper strata during the summer season. This character is a common feature of sclerophyllous plants, as has been shown by Cannon (1924). The absence of these sandstone plants from the basalt, as in the case of Callicoma, is perhaps due to the character of the root-system: it may be that a deep root-system is a rigid character here, which, as Cannon (1915) has suggested, is often the case. Observations on the components of the Hucalyptus goniocalyz-H. Blaxlandi association have not been made, but it has been found that H. Blaxlandi growing on basalt soil has a shallow root-system, a fact perhaps correlated with its preclusion from the dry sandstone. On the whole, then, it appears that the character of the root-system is a significant factor in the distribution of the vegetation of Mount Wilson. In the physiological reaction to their environment the roots of the sclerophyllous sand- stone types have had to penetrate deeply and this character seems to have eventually become rigid: the Rain-Forest types have found it better to exploit the superficial strata where they could obtain all the moisture and nutritive substances required. The different plants appear to be confined to those habitats to which their particular type of root-system is adapted. 4, THE ULTIMATE CONCEPTION OF THE VEGETATION OF MouNT WILSON. Few montane forest regions offer such a unique field as Mount Wilson for ecological study, provided as it is with two such widely different floras and with two such widely different habitats. The main basis for our study has, indeed, centred round the way in which these two fleras have competed for the occupa- tion of these two habitats, and the way in which they have reacted to the environmental conditions. Superficial survey would suggest that in a. region such as this with alternating basalt and sandstone, the geological formation must be the habitat factor of most outstanding significance; yet observations have disclosed the striking fact that distribution of the communities is not to be correlated with this but rather with the edaphic water supply. Apart from the role of humus in the determination of soil moisture-content, neither chemical nor physico-chemical properties of the soil BY J. MCLUCKIE AND A. H. K. PETRIE. ' 183 appear to have any fundamental distributional significance, except in the case of several minor subordinate species. Given the climate and the moderately favour- able summer rainfall such as they are, wherever the aspect is sheltered, and conditions, whether they be due to drainage or to the physical structure of the soil, permit the establishment of a permanent high edaphic moisture-content, Rain- Forest holds its own; wherever, on the contrary, the true climatic climax habitat conditions establish themselves on the dry and bleak sandstone plateau, the sclerophyllous Hucalyptus Forest has unchallenged sway; and wherever conditions are of an intermediate nature, transitional types of community are to be found. As progression or retrogression appears to be the fundamental feature in the development of plant communities we regard the Rain-Forest as a vestigial remnant of a former vegetation of widespread range in eastern Australia, which, now faced in most parts with xerophytie conditions inimical to its survival, has retreated to such habitats as we have shown still to furnish it with optimum conditions. The xerophytic habitats provided by the elevation of the Blue Mountain Plateau of sandstone, favoured the advance of the xerophilous endemic Flora which now occupies the greater part of this formerly Rain-Forest-clad terrain. Yet, though the old Malayan Flora is securely entrenched in the most favourable mesophytic habitat at Mount Wilson, and though it can even displace the autochthonous element in changing habitats, still wherever the conditions become a little more extreme, Hucalyptus secures a footing; and, as through future ages the basalt hills are slowly carried away by the unceasing agents of geological denudation, the area of the Malayan Forest will shrink before the dominance of the autochthonous Flora. Summary. 1. This paper is a study of the habitat factors, and an attempt to correlate these with the interesting distributional features of the vegetation of Mount Wilson. 2. An explanation of the small amount of invasion of the basalt by types from the Hucalyptus forests of the sandstone, and why the Rain-Forest grows as well in many sandstone gullies as on the basalt caps is given in this paper. 3. An analysis of the data of rainfall, temperature, humidity and evaporative powers of the atmosphere in the different habitats, of the hydrogen-ion concen- tration of the soil solution, of the moisture-content of the soil is made, and the relative significance of these factors upon the distribution and organization of the various plant communities is discussed. 4. The Py value of the soil solution is proved to be an insignificant factor in the distribution of the vegetation at Mount Wilson. 5. The moisture content of the soil—affected by its humus content, by the component clay fraction, by drainage, exposure ete, is of the greatest significance as a controlling factor of the distribution throughout this area. The significance of aspect and moisture-content of the soil outweigh the effect of all other factors. 6. The response of the more important components to the habitat factors is discussed; the general development of the root system in the various habitats, and the structure of the photosynthetic organs are investigated and correlated with the environment. 7. The distribution of the communities throughout the Mount Wilson area is controlled by the edaphic water supply rather than by the nature of the geological formation. 184 AN ECOLOGICAL STUDY OF THE FLORA OF MOUNT WILSON, iv. 8. The Ceratopetalum-Doryphora association is the dominant community in the most favoured habitats, e.g. on the basalt slopes, and in the sandstone gullies. The sclerophyllous Eucalyptus forests, represented by the FHucalyptus goniocalyz-E. Blaxlandi and the Eucalyptus piperita-Eucalyptus haemastoma asso- ciations, are the climax communities wherever the environmental factors fall below the optimum required for the Ceratopetalum-Doryphora association, e.g. on the sandstone slopes and more exposed habitats of the area. 9. The Malayan exotic flora represented by the Ceratopetalum-Doryphora association is a mesophytic community which formerly had a very extensive distribution in New South Wales but is now preserved in sheltered valleys and on basalt residuals. Its present area will become smaller as the agents of denudation carry away the basalt caps of the sandstone. Addendum. Note on the occurrence of Fucalyptus amygdalina var. nitida. Since the publication of the previous parts of this work Hucalyptus amygdalina Labill. var. nitida Benth. has been observed at Mount Wilson. It was found as an almost pure consociation of the Hucalyptus goniocalyx-H. Blaxlandi association on a south-westerly slope. H. Blaxlandi was occasional, and the usual stratum-societies of Alsophila and Pteridium were present. References. BroucH, P., McLuckisz£, J., and PrEtTrig, A. H. K., 1924.—An Ecological Study of the Flora of Mount Wilson. Part i. The Vegetation of the Basalt. Proc. LINN. Soc. IN-SIW)., xtix, p. 475. CANNON, W. A., 1915.—The Relation of Root Growth and Development to the Temperature and Aeration of the Soil Amer. Jour. Bot. 2. , 1924.—General and Physiological Features of the Vegetation of the more Arid Portions of Southern Africa, with Notes on the Climatic Environment. Carneg. Inst. Wash. Publ. 354. \ CLEMENTS, F. E., 1916.—Plant Succession. Carneg. Inst. Wash. Publ. 242. McLuckKIE, J., and PETRIE, A. H. K., 1926.—An Ecological Study of the Flora of Mount Wilson. Part iii. The Vegetation of the Valleys. Proc. Linn. Soc. N.S.W., li, p. 94. PETRIE, A. H. K., 1925.—Id. Part ii. The Eucalyptus Forests. Proc. LINN. Soc. N.S.W., horas ales. RUSSELL, E. J., 1921.—Soil Conditions and Plant Growth. SHREVE, F., 1914.—A Montane Rain-Forest. Carneg. Inst. Wash. Publ. 199. WHERRY, E. T., 1920.—Soil Acidity and a Field Method for its Measurement. Ecology, i. , 1924.—How much Water should be added in making Determinations of the Soil Reaction?’ Ecology, v, p. 310. TWO NEW SPECIES OF SETARIA FROM WESTERN AUSTRALIA. By Dr. A. S. HircHcock, Systematic Agrostologist of the United States Department of Agriculture. (Communicated by W. M. Carne.) [Read 27th April, 1927.] Recently I received from Mr. W. M. Carne, Botanist and Plant Pathologist of Western Australia, two species of Setaria which appear to be undescribed. At the request of Mr. Carne I am submitting technical descriptions. It is unfortunate that there is not more material at hand, but it will aid in the study of this critical genus if these tentative descriptions are placed on record. SETARIA BUCHANANI, Nn. SD. Planta annua; culmis glabris, ad 70 cm. altis; laminis planis, scabris, 15-25 cm. longis, 2-6 mm. latis; panicula densa, spiciformis, basi interrupta, 7-12 cm. longa; axi scabro; ramulis 1-1-5 cm. longis, suberectis; setis antrorsum scabris; spiculis ellipticis, 24 mm. longis; gluma prima spiculam 4 aequante, acuta; gluma secunda ' longitudine spiculae; lemmate sterile longitudine spiculae: lemmate fertile rugulose. | Annual; culms branching at base, glabrous (scabrous below panicle), about 70 em. tall; sheaths glabrous; ligule 1 to 1-5 mm. long, membranaceous at base, Dilose above; blades flat, scabrous, 15 to 25 cm. long, 2 to 6 mm. wide; panicle dense, spikelike, pale green, interrupted, 7 to 12 cm. long, the axis scabrous, angled, the branches 1 to 1:5 cm. long; bristles solitary below a part of the spikelet, antrorsely scabrous, 2 to 3 times as long as the spikelets; spikelets elliptic, glabrous, about 2-4 mm. long; first glume about half as long as the spikelet, acute; second glume as long as spikelet, 5-nerved; sterile lemma as long as the spikelet, 5-nerved, with an additional pair of nerves above; fertile lemma about as long as the sterile lemma, rather faintly transversely rugulose, pale. Type specimen: Murchison District, Western Australia, G. Buchanan, H. 201, April, 1925. This species differs from Setaria viridis (L.) Beauv. in the elongate blades, the interrupted panicle, the fewer bristles, and the longer acute first glume. SETARIA CARNEI, DN. Sp. Planta perennis; culmis glabris, 40-50 cm. altis; laminis planis, scabris,, 10-20 em. longis, 2-5 mm. latis; panicula densa, spiciformis, interrupta, 7-12 cm. longa; axi scabro; setis retrorsum scabris; spiculis ellipticis, glabris, 2 mm. latis. Perennial; culms glabrous (roughish below panicle), 40 to 50 cm. tall; sheaths smooth, compressed; ligule about 1 mm. long, pilose; blades flat, glabrous beneath, scabrous on the upper surface, 10 to 20 cm. long, 2 to 5 mm. wide; panicle dense, spikelike, interrupted, pale, 7 to 12 cm. long, the axis scabrous, angled, the X 186 NEW SETARIA FROM WESTERN AUSTRALIA. branches 3 to 5 mm. long; bristles solitary below each spikelet, retrorsely scabrous, 2 to 4 times as long as the spikelet; spikelets elliptic, glabrous, 2 mm. long; first glume about half as long as the spikelet, acutish; second glume as long as the spikelet, distinctly 7-nerved; sterile lemma as long as the spikelet, 5-nerved, with an additional pair of nerves above; fertile lemma rather faintly transversely rugulose, pale. Type specimen: Broome, Western Australia, collected by the North West Department, H. 197, April, 1925. In the U.S. National Herbarium there is a specimen of this species from West Australia, collected by Drummond. This species resembles S. buchanani in aspect but differs in being apparently perennial, in the retrorsely scabrous bristles, and in the smaller spikelets. aoe a A heer ce OR aia eke Fad) ek Pie BURL AY vey Proc. Linn. Soc. N.S.W., 1927. PLATE I. ; Li hy. 4 “cl i =“ To DUNGOG N = 205° | 4} v t\ONBLAaTEAUASe ON l atl" ak f “, rg 1 a iz " 5 us lt el |] v v v op My iy 3 3 10400 . “8 PATERSON S i rom as y im ays. Westar 2 - een [ lis 2= q Vv miner. BY To Y SEAHAM GEOLOGICAL MAP OF” ThE LAMB’S VALLEY-PATERSON DISTRICT * To STANHOPE SCALE To DALWOOD SALES, id i Wigee sot _ a | ys , op oF A AoA Bs Pe a * Pa a4 j a a Shh t 5 oy Proc. Linn. Soc. N.S.W., 1927. PLATE Il. 1,2. Deltopecten rienitsi, n. sp. 3-5. Estheria coghlani Cox. 6. E. glenleensis, n. sp. 7, 8. H. wianamattensis, n. sp. Proc. Linn. Soc. N.S.W., 1927. PLATE Itt. 1-4. Estheria ipsviciensis, n. sp. 5, 6. EH. novocastrensis, N. Sp. 7. E. lenticularis, n. sp. 8, 9. H. lata, n. sp. Proc. Linn. Sou. N.S.W., 1927. PLATE IV. 1. EHstheria obliqua, n. sp. 2, 3. E. glabra, n. sp. 4. H. linguiformis, n. sp. 5. E. belmontensis, n. sp. 6. EH. trigonellaris, n. sp. 7, 8. E. (?) bellambiensis, n. sp. Proc. Linn. Soc. N.S.W., 1927. PLATE V. oe ee ci Photomicrographs of fossil wood from Ulladulla, N.S.W. Proc. Linn. Soc. N.S.W., 1927. M PLATE VI. Photomicrographs of fossil wood from Ulladulla, N.S.W. Proc. Linn. Soc. N.S.W., 1927. PLATE VII. 1. Grevillea laurifolia. 2-5. Forms of G. Gaudichaudii. 6. G. acanthifolia. ‘ ay a Ny 4 Proc. Linn. Soc. N.S.W., 1927. PLATE VIII. 1. Character of deposits of fiood silts. 2. Cracks due to drying in flood silts. a. ' ‘ m 7 Ley A ics 0 Newer iw lyes . ou rans 2 Le ; ; aa > * Proc. Linn. Sou. N.S.W., 1927. PLATE [X. 1347. Galls of Kladothrips augonusaxxos, n. sp. on Acacia doratoxylon. 518. Galls of Choleothrips geijerae, n. sp. and Dolerothrhips geijerae, n. sp. on Geijera parviflora. THE VEGETATION OF THE KOSCIUSKO PLATEAU. Part i. THE PLANT COMMUNITIES. By JoHn McLucxigr, M.A., D.Sc., Assistant-Professor of Botany and Lecturer in Plant Physiology and Ecology, the University of Sydney; AND - ArtHuUR H. K. Petrig, M.Se., Senior Demonstrator in Botany, the University of Melbourne. (From the Botanical Laboratory, University of Sydney.) (Plates x-xix and eight Text-figures. ) [Read 27th July, 1927.] Contents. Introduction. Meteorological Data. The Hucalyptus Forests. The Eucalyptus coriacea Consociation. The Eucalyptus Gunnii Consociation. The Hucalyptus coriacea-E. Gunnii Ecotone and the EH. stellulata Consociation. The Leptospermum Shrub Society. Regeneration of the Hucalyptus Forests after Fire. Factors causing or modifying the Timber-line. The Marsh Vegetation. The Poa-Hypolaena Ecotone. The Hypolaena Associes. The Restio Associes. The Richea Associes. The Epacris Associes. The Baeckea-Callistemon Association. The Luzula-Carex Associes. The Alpine Vegetation. The Poa-Celmisia Association. The Epacris petrophila Consociation Summary. Introduction. The Kosciusko Plateau, the plant ecology of which forms the subject of this paper, lies in the Snowy Range in the southern portion of New South Wales, and is the highest land surface on the Continent.’ It is an elevated block about 20 miles long by 6 miles broad, rising gradually from east to west. At the junction of the Thredbo and Snowy Rivers, it is 3,000 feet above the sea. Mount Kosciusko at the other extreme (its westerly limit) is about 7,328 feet high. Only a few isolated points rise above 7,000 feet. A horse shoe-shaped area surrounding the Snowy head-waters exceeds 6,500 feet (contour map Plate x? and block diagram Text-fig. 1). 1The following description of the topography of the Kosciusko Plateau is taken from the paper “The Kosciusko Plateau,” by G. Taylor, W. R. Browne and F. Jardine, published in the Proc. Roy. Soc. N.S.W., 1925, pp. 200-205. 2The block, from which this map has been printed, has been kindly lent by the Royal Society of New South Wales, it having appeared in the Proceedings of that Society for 1925 as Plate i. A N OF THE KOSCIUSKO PLATEAU, i, EGETATIO THE V 188 ‘\svo 0] SOM WoaJ SoTL NE SI Jopowm oy, “T eansy-7xey, [942] eas sA0ge y 008'Z st osed ss@q aopieyd ' SW, iw ZB —— Willi Ga \ eZ | 2 WA Ss WWE SN MIME Hanes cwe : gl LZ SS), St WM! == NWS | 2427 210 oye] gay APT AMID 33 » -YPAAD) saystuay ! orci ' 2 4aaty Amoug REO ashe aun a WAY AMouG roysuag) WW ME - Eira tinil| a JRANY auaquinony Yy S10'S Jo adojs sayy, Y 0972 euiqiy/ a4e7] PussumMoT IW CGzZ6L ‘Aoupsg ‘10[ABT ‘q pue ‘y Aq AOVeIOGeT [VOIYdeIs094 9Y} WOT) ‘OVHLVId OMSOIOSOM HO WVYUOVIG MOOTH VY Or09 JaAlyy AMOUG JO peat] ' oysnvosoy Yop7ed W BY J. MCLUCKIE AND A. H.’K. PETRIE. 189 “There is a very marked drop in the Plateau east of Perisher Creek, for practically all the high land (over 6,000 feet) lies to the west”. . . “The 5,000 feet contour bounds the Plateau uplands around the lower Snowy River, which flows through a gorge which is largely below that level’. “The drainage is arranged according to a very interesting plan. The main stream of the district is really the broad Eucumbene Valley in the extreme east. This is longer and ‘older’ than the Snowy Valley. The latter has cut back as a gorge into the uplifted plateau—probably along fault planes—as far back as Charlotte’s Pass. Above this the valley is fairly wide and approaches maturity. Further west, the head-waters, above the road-ford, flow and meander through a flat senile valley. The Crackenback-Thredbo Valley is a profound gorge for most of its extent. 5 Besides these two parallel gorges of the Snowy and Crackenback, there is a third more or less continuous valley running between: them. . . . It consists of a series of shallow basins linked by cols or gaps. . . . Hach of these basins drains to the north by a creek leading into the Snowy River: This ‘Road Valley’ is about 1,000 feet above the two parallel river valleys. Its topography is probably in part due to bygone giacial erosion”. This region is the coldest portion of Australia, and for six months in the year the higher elevations are covered in snow. It thus offers features of special interest so far as the vegetation of Australia is concerned. The Plateau is an elevated land surface composed of gneissic granite, which ascends abruptly from the surrounding plains at about 3,000 feet above sea-level, to an altitude of 5,000 to 6,000 feet, from which level it rises more gradually until it culminates in various peaks ranging up to 7,328 feet. The lower slopes are steep and well drained, and are dissected by various defiles formed by erosion; the higher portion of the Plateau, however, above 5,000 feet, is traversed by long shallow valleys, whose flat bottoms form marshes by the slow draining away of the water from the melting snow of the higher peaks. A consideration of the plant communities has led us to recognize three unit- areas in the region under discussion: (1) The montane zone, from 3,000 to approximately 5,000 feet, comprising the lower slopes of the Plateau. (2) The sub-alpine zone, from approximately 5,000 feet to the tree-line at 6,000 to 6,500 feet. (3) The alpine zone, from the tree-line to the highest elevations. The montane zone is entirely clad with sclerophyllous Eucalyptus forest, as is characteristically the case with the mountain regions of Eastern Australia. Eucalyptus forest also clothes the ridges and slopes in the sub-alpine zone; the boundary between the montane and sub-alpine zones, however, is also the position of the junction of the two main consociations of the forest. The lower portions of the slopes of the sub-alpine region, below the forest, are occupied by low- tussock grassland, which, admixed with mat herbage, is also the main formation of the alpine zone. A marsh vegetation occupies the shallow valley-bottoms throughout the sub-alpine and alpine regions. These three types of vegetation will be discussed in detail in the subsequent portion of the paper. The lists of plants from this area, published by Maiden (1898-99) and Helms (1896-97) proved of great value to the writers in their identification work, but did not furnish an analysis of the communities of the plateau, which is attempted in this paper. 190 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, Meteorological Data. The following information dealing with the distribution of snow falls throughout the season, the mean monthly humidity and the absolute maximum and minimum temperatures, has been kindly supplied to us by Mr. D. J. Mares, Divisional Meteorologist of the Commonwealth of Australia. The greatest mean monthly humidity occurs during tne winter months from about May to September, during which period considerable snow or rain falls, and heavy frosts are frequent. The absolute maximum temperature so far recorded is 88° on the 9th November, 1919. The. mean monthly humidity is lowest during the summer months. The lowest absolute minimum temperature for any month occurred on the 15th August, 1920, and other very low temperatures during 1919 in the months July to September of the same and the following years, that is just subsequent to the devastating fires which. swept over the plateau and destroyed great areas of the Poa-Celmisia and Eucalyptus coriacea-E. Gunnii associations, and the #H. stellulata consociation. Perhaps the severity of the climate during such periods has been responsible for the tardy renaissance of the Zucalyptus forests and for the killing of areas near the highest portion of the tree-line. Low temperatures and severe frosts during certain winters if followed by droughty conditions during the summers, retard the development of buds, and flowering and fruiting, and may temporarily destroy the more exposed parts of the Poa and Eucalyptus associations. ' Commonwealth Meteorology. Mt. Kosctusko.—-TABLE I. Mean Monthly Humidity 9 a.m. (14 years). Jan. Feb. | Mar.| April} May | June| July |. Aug.| Sept.| Oct. Nov. | Dec. 56% | 60% | 62% | 65% 69% | 79% | 84% | 79% | 70% | 60% | 55% | 58% Absolute Maximum Temperature, 1911-24 (Fahrenheit). Jan. | Feb. | Mar.| April| May | June | July | Aug.} Sept. | Oct. Nov. | Dec. 84-0 85-0 77-0 71-0 67-0 56-0 52-2 57-1 78-0 78-0 88-0 | 78-0 30th | 15th 5th 4th 2nd 7th 25th | 27th |} 26th} 10th 9th 9th 10th 1912 | 1919 | 1924 | 1911 | 1922 | 1919 | 1916 | 1914 | 1922 | 1922 | 1919 | 1918 ‘ 4th 29th 1st 1923 1924 1924 Absolute Minimum Temperature, 1911-24. | | | Jan. | Feb. Mar. April | May June | July een Sept. Oct. Nov. | Dec. i lentes ace aes A 21-0 | 24-9 | 19-8 | 15-0 |) 12:00) Wao 70 6-3 | 14:0 | 16:0 | 13-0 | 20-0 27th 5th) 24th | 27th | 28th | 22nd | 16th 15th 8th 22nd 4th 3rd POLS LST LOL, Hat | 1913 | 1917 | 1919 | 1920 | 1919 1918 | 1911 | 1924 191 | | BY J. MCLUCKIE AND A. H. K. PETRIE: 191 Mt. Kosciusko.—TABLE II. Days of Snow. Jan. Feb. | Mar.} April| May | June | July | Aug.| Sept. |} Oct Nov. | Dec. 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 | 1924 —t | 1 — 2 2 37 4 3t 7 — — — * Snow still abundant round summit of Mt. Kosciusko. + Frosts more severe and sustained than for several years. t Rarity remarkable. Frosts severe. Jan. | Feb. | Mar.| April| May | June July | Aug.| Sept. | Oct. Nov.| Dec. 1923 | 1923 | 1928 | 1923 | 1923 | 1923 | 1923 | 1923 | 1923 | 1923 | 1923 | 1923 iL — — — | 4 5 §* 2 5 1 — — * So much snow over such an extended area not seen since 1914. Jan. Feb. | Mar.| April| May | June July | Aug.| Sept. | Oct. Nov Dec. 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 | 1922 —_— oe 1 1 2 11 6 aba ook 6 4 — — Jan. Feb. | Mar.| April| May | June | July | Aug.| Sept. Oct. Nov. | Dec. 1921 | 7921 | W921 | L92T | L921 | 1921) L921 7 1921 | W921 | 1921 | 1927 |) 1921 ae poe — = 2 ons 5T 9 1 2 — — * Season mild. Very little snow below 6,000 feet level. + More rain than snow. THE EUCALYPTUS FORESTS. In the region under study there is only one association of Hucalyptus forest, namely, the Hucalyptus coriacea-E. Gunnii association, which extends from the foot of the Snowy Mountains on the edge of the Monaro Plains up to the tree-line. It occurs also on the exposed wind-swept Monaro Plains themselves, from” which the Snowy Mountains rise. The following three consociations occur: 1. The Eucalyptus coriacea consociation, which is typical of the sub-alpine zone, and is found chiefly from about 4,500 feet to the tree-line between 6,100 and 6,500 feet, although it occurs also at lower altitudes. 2. The Eucalyptus Gunnii consociation which is found chiefly between 3,500 and 5,000 feet, and generally prefers the more sheltered slopes characteristic of the montane region. 3. The Eucalyptus stellulata consociation which occupies small areas between the altitudes of 4,000 and 5,000 feet. THE EUCALYPTUS CORIACEA CONSOCIATION. Habitat. While the main adaptive feature of Hucalyptus forest is xerophily, the Eucalyptus coriacea consociation has fitted itself also for existence amid the 192 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, severities of a sub-alpine climate, and is the only forest which has ascended above > an altitude of 5,000 feet in Australia. The same community occurs on the Monaro Plains, at an altitude of 2,700 to 4,000 feet, where it-is exposed to bleak and desiccating winds from the west. Hucalyptus coriacea has also been recorded from other mountain tops in New South Wales, where it is found in similar habitats: aura So. far as the Snowy Mountains are concerned, the Eucalyptus coriacea ‘consociation is found chiefly from about 4,500 to 5,000 feet up to 6,500 feet, which is the absolute limit of tree vegetation. It probably occurs, however, at a much lower altitude than 4,500 feet on the western slopes of the mountains owing to exposure to west and north-west winds. Above 5,000 feet the forest is confined to the upper and middle portions of the slopes of the hills, giving place below to grassland (Plate xi, figs. 1 and 2; Plate xii, fig. 3). All flat and gently sloping ground above this altitude is extremely damp, or even water-logged, owing to the drainage from the melting snow on the upper slopes, combined with the impervious nature of the granite substratum. The restricted distribution of the Hucalyptus forest which avoids all swampy areas is probably the result of the water-logging and consequent lack of aeration of the lower strata of the soil. Near the tree- line the forest is still further limited on account of the greater amount of snow, and the trees are confined to the drier ridges (Plate xvi, fig. 4). Structure and Physiognomy. Eucalyptus coriacea is not only dominant, but is the only tree in the consociation at the higher altitudes; it has a distinctive appearance imparted by its smooth white bark, gnarled branches, excessively glaucous twigs, and thick coriaceous leaves. At an altitude of about 5,000 feet, in less exposed areas, Hucalyptus coriacea attains a height of about fifty feet and forms an extensive and fairly close forest (Plate xi, fig. 1); at higher altitudes, however, and on the hill-tops above 5,000 feet, the trees become stunted and the forest is more open (Plate xii, fig. 3); while near the tree-line they are rarely taller than twelve to fifteen feet, and often their gnarled branches and trunks are almost prostrate (Plate xvi, fig. 4). This condition is no doubt the result of the heavy snow-falls and frosts during several months of the year and the stimulation of excessive transpiration by strong winds, which are frequent at these altitudes. While Eucalyptus coriacea forms a pure consociation at the higher altitudes, £. stellulata becomes frequent at 5,000 feet, as will be described subsequently. E. Gunnii is occasional at 5,000 feet, and also becomes abundant in Digger’s Creek valley, where an extensive ecotone region exists between the £. coriacea and E. Gunnii consociations. EH. viminalis is also occasional in this ecotone region; since, however, the lower strata are highly typical of the H. Gunnii consociation, neither this species nor EH. viminalis can be considered typical of the HH. coriacea forest. Shrubs form a conspicuous element in the Hucalyptus forests of certain slopes, occurring in dense societies composed chiefly of a dominant species, or else scattered and mixed in composition. In more exposed areas, e.g., on the top of the ridges, shrubs are absent, and the ground is occupied by Poa caespitosa, forming low tussocks, and by other grasses and herbaceous types, which also occupy the ground between the shrubs when they are so scattered as to permit of the development of lower strata. Between 5,000 and 5,500 feet societies of Oxylobium ellipticum var. alpinum are common, containing as subordinates Pimelea ligustrina, Drimys aromatica var. pedunculata, Cassinia aculeata, Olearia myrsinoides, Pimelea axiflora and Veronica Derwentia, 40 Feet UPPER # SS 5 *ue sss s Ss Sis BY J. MCLUCKIE AND A. H. K. 17 Feet PETRIE. 193 Text-figure 2, Chart of an area in an. open Hucalyptus coriacea forest (5,500 ft.). This chart illustrates the vegetation on a typical slope. The lower end of this chart is within a few feet of a small creek traversing the hill-side. As_ the water is approached certain types such as Oreomyr- rhis andicola and Veronica disappear, while species. of Helichrysum become more abundant. Veronica is always abundant on the slopes of the water courses, while Oxylobium ellipticum prefers the drier hill- sides more remote from the streams. @ ~ Veronica Derwentia (0%- Oxylobium ellipticum. S @=Stellarium pungens. H = Helichrysum bracteatum. G@ — Geranium dissectum.. T = Tarazacum sp. Or- Oreomyrrhis andicola. Hs = Helichrysum scorpioides. Ep ~ Epilobium glabellum. Se - Senecio pectinatus. Ol - Olearia myrsinoides. &9)- Eucalyptus coriacea, seedlings. Ca - Cassinia aculeata. All space between symbols is occupied by Poa _ caespitosa forming a close grassy cover- ing with occasional tussocks and withered patches. An attempt has been made to convey an impression of the relative pro- portion of the area that is occupied by each component. Scale: 1 cm. = 2 feet. 194 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, The Oxylobium society is replaced by one dominated by Callistemon Sieberi in the little watercourses which frequently run down the slopes to the creeks and swampy areas invariably occupying the flat bottoms of the shallow valleys. This society is closely related to the Callistemon Sieberi consociation of the marsh vegetation, and contains a number of swamp-loving types not found elsewhere in the Eucalyptus forests. Floristic Composition. Shrub Stratum Callistemon Sieberi D.C. d* Cassinia aculeata R.Br. f Oxzylobium ellipticum R.Br., var. alpinum Maiden and Betche o-f Drimys aromatica F.v.M., var. pedunculata Maiden co) Panax sambucifolius Sieb. r Leptospermum lanigerum Sm. If Ground Stratum Richea Gunnii For. Acaena sanguisorba Vahl. Anagallis arvensis Linn. Epilobium glabellum Forst. Rumeax acetosella Linn. Taraxacum dens-leonis Desf. Stylidium graminifolium Swartz. Linum marginale Cunn. Blechnum penna-marina (Poir.) Kuhn Galium umbrosum Sol. Sphagnum societies Prostanthera cuneata Benth. Epacris paludosa R.Br. ii ©) ©) ©C) 6) © ©) ©. ©) fs eo !n0 = e} Veronica Derwentia also forms dense societies (Text-fig. 2), especially in more open areas, with Olearia megalophylla (f{), Drimys (f), and Ozylobium ellipticum var. alpinum (o) (Plate xiii, fig. 2). Above 5,500 feet these societies are not so frequent, their place being taken by Prostanthera cuneata, which forms abundant societies up to and beyond the tree-line (Plate xvi, fig. 4; Plate xix, fig. 2). Phebalium ovatifolium is a frequent subordinate in this society. Elsewhere the shrubs are mixed or absent, Helichrysum baccharoides and H. rosmarinifolium being conspicuous. On the tops of the ridges, and between the shrubs where they are less dense, Poa caespitosa, with its many herbaceous subordinates, forms a close covering. At the foot of the slopes and at the tree-line this stratum-society passes out unchanged beyond the trees, and assumes the rank of an association, a feature which will be referred to again subsequently (Plate xii, fig. 3). Floristic Composition. Tree Stratum. Bucalyptus coriacea Cunn. d E. stellulata Sieb. f (up to 5,000 ft.)—o (to 5,500 ft.) E. Gunnii Hook. o (to 5,000 ft.) Tall-Shrub Stratum. Helichrysum rosmarinifolium Less. f-c (above 5,500 ft.) Drimys aromatica F.v.M. var. pedunculata Maiden f-la Cassinia aculeata R.Br. f-la Veronica Derwentia Littlej. f-la *In these lists, a = abundant, ec = common, d = dominant, f = frequent, 1 = locally, o = occasional, r = rare, sd = subdominant, vr = very rare. Tall-Shrub Stratum. Hovea longifolia R.Br. Oxylobium ellipticum BY J. MCLUCKIE AND A. H. K. PETRIE. R.Br. var. alpinum Maiden o-a (5,200-6,000 ft.) and Betche Bossiaea foliosa Cunn. o-la Olearia myrsinoides F.v.M. o-le Helichrysum baccharoides F.v.M. o-le Olearia megalophylla F.v.M. o-lf-le Pimetlea ligustrina Labill. var. hypericina Benth. o-f Phebalium ovatifolium F.v.M. Pimelea axviflora F.v.M. Rubus rosifolius Sm. Orites lancifolia F.v.M. Grevillea australis R. Hakea Macreana F.v. Lissanthe montana R.Br. Acacia alpina F.v.M. Panax sambucifolius Prostanthera cuneata Benth. fo) ro) {o) Br. Oo M. Ts r Tt Sieb. vr (below 5,100 ft.) Leptospermum lanigerum Sm. if Callistemon Sieberi D.C. Low-Shrub Stratum. Hibbertia linearis R. Ground Stratum. Poa caespitosa Forst. a-lo Taraxacum dens-leonis Desf. f-a Trifolium sp. f-a Rumex acetosella Linn. ; f-la Helichrysum scorpioides Labill. f-¢ Geranium dissectum Linn. fy Ranunculus lappaceus Sm. ifs Plantago varia R.Br. f Senecio lautus Sol. f Wahlenbergia gracilis D.C. if Acaena sanguisorbae Vahl. o-a Stellaria pungens Brongn. o-a Brachycome scapiformis D.C. , o-a Craspedia Richea Cass. o-a Podolepis longipedata Cunn. o-la Stylidium graminifolium Swartz. o-f Epilobium glabellum Forst. {o) Viola betonicifolia Sm. fo) Scaevola Hookeri F.v.M. societies. ° Comesperma retusum Labill. Oo (5,000 ft.) Brachycome decipiens Hook. Oo Poranthera microphylla Brongn. ra) FPolystichum aculeatum (l.) Schott. o (under rocks) Kunzea Muelleri Benth. fo} Celmisia longifolia Cass. o-f Stellaria flaccida Hook. {o) Oreomyrrhis andicola Endl. ro) Euphrasia Brownii F.v.M. fo) Helichrysum bracteatum Willd. (0) Blechnum penna-marina (Poir.) Kuhn. r Galium umbrosum Sol. r Linum marginale Cunn. ie Dianella tasmanica Hook. r Podocarpus alpina R.Br. societies r (above 5,600 ft.) Asplenium flabellifolium Cav. Chiloglottis Gunnii Lindl. Ic Pterostylis mutica R.Br. lf Richea Gunnii For. lo Sphagnum societies lo Anagallis arvensis Linn. lo (5,000 ft.) Br. var. obtusifolia Benth. 0 (below 5,000 ft.) Epacris paludosa R.Br. lo f (5,500 ft. upwards) o-f (above 5,600 ft.) (near tree-line) (at tree-line) vr (5,300 ft.)—a (6,000 ft.) lf (5,000 ft.) (above 5,200 ft.) vr (5,000 ft. downwards) 195 196 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, THE EUCALYPTUS GUNNII CONSOCIATION. Passing into the sheltered gullies just below 5,000 feet, the Eucalyptus coriacea consociation gives place to the H. Gunnii consociation, very gradually in Digger’s Creek valley, comparatively abruptly in other areas. H. Gunnii grows taller than E. coriacea, the trees averaging about seventy feet in height. For some distance into this consociation a number of shrubs characteristic of the H. coriacea forest persist, but a distinct and continuous change is noticeable as one descends the Plateau, new types appearing and former ones disappearing. Poa caespitosa tussocks are much less abundant; although they still form a carpet in certain areas where the soil is damper, a considerable amount of the ground is quite bare of grass or only sparsely covered (Plate xvi, fig. 3). In general this forest has a more xerophilous impress since many of the herbaceous types of the H. coriacea consociation are absent, the rich carpet of grass is less evident, and the shrubs have a more scraggy, sclerophyllous appearance; indeed the general physiognomy of the community resembles that of the H. piperita forest characteristic of the sandstone plateau at Mount Wilson. The smaller rainfall which characterizes the lower altitudes of the mountains probably contributes to this feature of the ZH. Gunnii consociation, as also does a change in the topography. We are here below the level of the marshy flats and the continual streams of water from the melting snow; the water is concentrated in the deep gorges of the Snowy River and its tributaries, by means of which the gravitational water passes rapidly away, resulting in a general lowering of the soil moisture-content. Moreover this consociation dominates an area from which the snow disappears early on the approach of summer; there is therefore less soil moisture as compared with the higher zones, and the plant life is dependent directly upon the rainfall for its moisture requirements throughout the summer months. The extremely xerophilous structure of the plants inhabiting this zone indicates an approximation t6 the conditions which have stimulated the development of the highly xerophytic sclerophyllous forest on the Hawkesbury Sandstone habitat around Sydney. Floristic Composition.~ Tree Stratum. Eucalyptus Guninii Hook. d E£. viminalis Labill. o-c E. coriacea Cunn. o-f E. stellulata Sieb. fo) E. amygdalina Labill. var. nitida Benth. Ts Low-Tree Stratum. Acacia rubida Cunn. Shrub Stratum. Ozylobium ellipticum R.Br. var. alpinum Maiden and Betche Bossiaea foliosa Cunn. Daviesia ulicina Sm. Leptospermum stellatum Cay. Cassinia aculeata R.Br. Baeckea Gunniana Schau. Grevillea lanigera Cunn. Lomatia longifolia R.Br. Acacia penninervis Sieb. Rubus parvifolivs Linn. Panag sambucifolius Sieb. Daviesia corymbosa Sm. o} ieee ei © ® = OL OTOUO FOL OROTO ES mh ho BY J. MCLUCKIE AND A. H. K. PETRIE: 197 Low-Shrub Stratum. Discaria australis Hook. (0) Grass Stratum. Poa caespitosa Forst. c-O Wahlenbergia gracilis D.C. f-c Stellaria pungens Brongn. f-c Taraxacum dens-leonis Desf. f-c Hibbertia linearis R.Br. var. obtusifolia Benth. f-c Helichrysum semipapposum D.C. Geranium dissectum Linn. Rumex acetosella Linn. Brachycome scapiformis D.C. Plantago varia R.Br. Epilobium glabellum Forst. Trifolium sp. Velleya paradoxa R.Br. Acaena sanguisorbae Vahl. Prunella vulgaris D.C. Xerotes longifolia R.Br. Pimelea glauca R.Br. Arthropodium paniculatum R.Br. Persoonia chamaepeuce Lhotsky Stylidium graminifolium Swartz. Galium umbrosum Sol. Lotus australis Andr. Lotus corniculatus Linn. Helichrysum scorpioides Labill. Pterostylis coccinea Fitzg. vr Bulbine bulbosa Haw. vr Erythraea australis R.Br. pala} fini LS (a) i) ' fear) Lar) ta © OOO © OO © OOO [ay trp Inoilnd [nd tnd 1d THE EUCALYPTUS CORIACEA—E. GUNNII ECOTONE AND THE E. STELLULATA CONSOCIATION. As has been mentioned earlier, the slopes of Digger’s Creek valley (4,000-5,000 feet) are clothed by a forest which represents an ecotone between the Z. coriacea and EH. Gunnii consociations. The continuity of this ecotone is interrupted by the occasional presence of a pure consociation of H. stellulata. Where Digger’s Creek valley joins the main gorge of the Snowy River (at about 4,000 feet) the ecotone gives place gradually to the #. Gunnii consociation. One may suppose that in this region the conditions are intermediate between the exposed habitat yet damp soil occupied by the E. coriacea forest on the one hand, and the drier, yet more sheltered environment normally occupied by H. Gunnii. The valley is sheltered, and the sides are steep; yet the soil in many parts has still much of the dampness characteristic of the higher altitudes. We have not up to the present been able to discover definitely the factors leading to the interruption of the ecotone by occasional consociations of #H. stellulata, but it is possible that a slightly greater degree of exposure may be the key to its presence; nor did we observe any difference in the floristic composition of the two communities. Floristic Composition. Tree Stratum. Ecotone. EF. stellulata. Eucalyptus coriacea Cunn. d fo) H. Gunnii Hook. a-f —_ EH. viminalis Labill. fo) —_— EH. stellulata Sieb. to) d Small-Tree Stratum. Acacia neriifolia Cunn. o in societies 198 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, Shrub Stratum. Veronica Derwentia Littlej. f-a Epacris sp. f Pimelea axiflora F.v.M. f Oxylobium ellipticum R.Br. var. alpinum Maiden and Betche Bossiaea foliosa Cunn. Hymenanthera dentata R.Br. Olearia megalophylla F.v.M. Hovea longifolia R.Br. Olearia myrsinoides F.v.M. Drimys aromatica F.v.M. var. pedunculata Maiden Pimelea ligustrina Labill. var. hypericina Benth: Panax sambucifolius Sieb. Daviesia ulicina Sm. Acacia decurrens Willd. Lomatia longifolia R.Br. Acacia penninervis Sieb. Persoonia chamaepeuce Lhotsky Hibbertia linearis R.Br. var. obtusifolia Benth. Acacia siculiformis Cunn. Leptospermum stellatum Cav. Leptospermum lanigerwm Sm. Callistemon Sieberi D.C. Hakea Macreana F.v.M. Rubus parvifoliws Linn. Low-Shrub Stratum. Helichrysum semipapposum D.C. Cassinia aculeata R.Br. Ground Stratum. Stellaria pungens Brongn. Poa caespitosa Forst. Acaena sanguisorbae Vahl. Geranium dissectum Linn. Trifolium sp. Wahlenbergia gracilis D.C. Taraxacum dens-leonis Desf. Galium umbrosum Sol. Rumex acetosella Linn. Brachycome scapiformis D.C. Blantago varia R.Br. Viola betonicifolia Sm. Velleya paradoza R.Br. Velleya montana Hook. Helichrysum bracteatum Willd Prunella vulgaris D.C. Podolepis longipedata Cunn. Oreomyrrhis andicola Endl. Linum marginale Cunn. Craspedia Richea Cass. Stylidium graminifolium Swartz. Hypericum japonicum Thunb. Lotus australis Andr. Goodenia hederacea Sm. Poranthera microphylla Brongn. Xerotes longifolia R.Br. Helichrysum scorpioides Labill. Asplenium flabellifolium Cay. Exzocarpus nana Hook. Arthropodium paniculatum R.Br, Pterostylis acuminata R.Br. Dianella sp. Gastrodia sesamoides R.Br. 1 Hh @uOMOMOMmO) C/O} OF OMONOMOMOC Om Gi (in drainage channels) oy tooo 0 oo moan0oa0nD ' ie) -O (below 4,650 ft.) CO) fry tno tnd Ina ind tna) tnd Id (below 4,400 ft.) (below 4,100 ft.) (under rocks) gpod SE UOT) @)@) © G0) GY QO) -C ©) BY J. MCLUCKIE AND A. H. K. PETRIE. 199 Ground Stratum. ‘ Stackhousia monogyna Lindl. ? If Lotus corniculatus Linn. lf-la a Reson Epilobium glabellum Forst. 1f-le SiEVeae) Juncus pallidus R.Br. lo J Lotus australis Andr. ra) THE LEPTOSPERMUM SHRUB SOCIETY. Along the banks of the rivers occupying the beds of the valleys whose slopes are clad by the Eucalyptus Gunnii consociation or by the ZH. coriacea-E. Gunnii ecotone, occurs a society of shrubs about five to seven feet in height. In the upper part of the ecotone at about 4,600 feet Leptospermum lanigerum is the dominant, while, as the beginning of the HE. Gunnii consociation is approached, Leptospermum stellatum becomes co-dominant. (Plate xiv, fig. 2). The majority of the components of this society appear to be species requiring a moderate degree of shelter and soil-moisture. It is interesting to note also that Kunzea Muelleri and Hakea microcarpa here attain a height of four to five feet, whereas above the 5,000 feet altitude Kunzea is only about six inches high, and Hakea one foot. In many cases this society is so dense as to be almost impenetrable and, during periods of flooding of the river, is practically submerged. Floristic Composition. Shrub Stratum, 4,650 ft. Leptospermum lanigerum Sm. Callistemon Sieberi D.C. Daviesia corymbosa Sm. Leptospermum stellatum Cav. Cassinia aculeata R.Br. Hakea Macreana F.v.M. Kunzea Muelleri Benth. Hakea microcarpa R.Br. Correa Lawrenciana Hook. Lomatia longifolia R.Br. Ground Stratum. Juncus pusillus Buch. c Hypolaena lateriflora Benth. f Epilobium glabellum Forst. 9) Lotus australis Andr. (e) Lotus corniculatus Linn. 6) Drosera peltata Sm. . Oreomyrrhis andicola Endl. Stylidium graminifolium Swartz. Hypericum Japonicum Thunb. Utricularia dichotoma Labill. var. wniflora Benth. Juncus pallidus R.Br. Creeper. Glycine clandestina Wendl. emg Q a AO oO Oo: 0 Oo oo000 ae rt fo} REGENERATION OF THE EUCALYPTUS FORESTS AFTER FIRE. On account of the high rainfall and general dampness of the ground, bush fires are by no means so prevalent on the Kosciusko Plateau above an altitude of 5,000 feet as in other more arid regions of the State; and at the time of study (1924 and 1925) none had occurred since 1919 in the area under review. The fire which took place in the latter year, however, swept over large areas of the Eucalyptus coriacea consociation between 5,000 and 5,500 feet, as well as through a small consociation of EZ. stellulata. 200 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, It appears that the Hucalyptus coriacea consociation by no means possesses the power of speedy renascence which characterizes Eucalyptus forests in other regions. Whereas most Hucalyptus forests would have recovered from the fire before the lapse of six years, here we found renascence to be tardy, and sometimes not even to have started. Neither H. coriacea nor E. stellulata appear readily to produce adventitious shoots from the stem, renascence taking place rather from the root-stock; thus most of the regenerating H. coriacea forest showed young shoots rising from the ground surrounding the old dead trunk, and only a few feet high (Plate xviii, fig. 1). In the more exposed areas no renascence was evident, and it seems that here the severity of the climatic conditions has prevented it. In these areas the dead trees are standing while the normal lower strata of the forest and especially the Poa stratum have re-developed. It is likely that regeneration of the forest will be slow, as it will now be chiefly dependent upon migration, followed by a precarious ecesis (Plate xi, fig. 2). The Eucalyptus stellulata consociation regenerates more rapidly, perhaps because of the lower altitude and the consequently greater shelter of its environ- ment; in this case a mass of shrub-like growth surrounded the base of the old trunks, so dense as to cover the ground almost completely. The regeneration of the lower strata was more advanced, and the burnt areas did not appear to differ appreciably in these strata from those which were unburnt, except that very dense shrub-societies had arisen in places. Where renascence of the trees is slow dense societies of Veronica Derwentia, accompanied by Olearia — megalophylla (f), Drimys (f), and Oxylobium ellipticum var. alpinum (0), are generally characteristic features (Plate xiii, fig. 2). The rapid recovery of these types is no doubt due to their resistant subterranean root-stocks or rhizomes. The Eucalyptus Gunnii consociation is subject to more frequent burns and is more akin in its reaction, to the Hucalyptus piperita Forest at Mount Wilson. FACTORS CAUSING OR MODIFYING THE TIMBER-LINE. In certain more exposed areas on the summits of the hills and on the higher slopes, the tree-trunks in the Hucalyptus coriacea consociation appear to have been killed by severe climatic conditions rather than by fire; for although regeneration is taking place as usual from the base of the stem, there is no indication of fire on the trunks, and moreover, these conditions are found only in exposed areas. An analogous phenomenon is seen at altitudes of 6,500 feet, where the stunted Eucalyptus forest has migrated during favourable seasons above the normal level of the timber-line, and subsequently, possibly as the result of an unusually severe season, has been entirely destroyed (Plate xvi, fig. 1). These observations lead us to consider the factors which are effective in controlling the tree-line in this region. Rhydberg (1914) has enumerated some of those which he considered to be important in the case of the Rocky Mountains, and it is of interest to note their significance in the case of the vegetation of the Kosciusko Plateau. The chief of these factors described by Rhydberg are as follows: (1) low temperature during the growing season; (2) shortness of the growing season; (3) late frosts; (4) strong winds; (5) deep snow; (6) form of precipitation; (7) large mountain masses; (8) physiographical barriers. The timber-line on the Kosciusko Plateau varies from 6,100 feet in exposed habitats to 6,500 feet in sheltered habitats. At these altitudes the forest thins out and the trees are represented by low gnarled and stunted shrubby individuals; the zone, however, between the absolute tree-line (where arboreal species disappear BY J. MCLUCKIE AND A. H. K. PETRIE. 201 entirely) and the relative tree-line (where the arboreal species just cease to form forest) is comparatively narrow. Exposure to desiccating westerly and north- westerly winds, very cold in winter and hot in summer, determines the points where the forest suddenly merges into isolated stunted individuals. In other | alpine regions of the earth coniferous forests frequently exist above the angio- spermic forest, but at Kosciusko the highest arboreal community is that composed of Hucalyptus coriacea. : Competition is of considerable importance in connection with the effect of the various climatic factors on the tree-line; the transition zone is undoubtedly a scene of constant struggle between the grassland and the scanty forest. In good seasons seeds of Eucalyptus coriacea germinate and develop in the true grassland areas, and if they survive, the grassland community becomes reduced to the status of a subordinate stratum. No doubt this tree after difficult ecesis tends to carry the forest upwards in this manner, but unfavourable seasons, when snow lies late in summer as it occasionally does, and late frosts followed by a dry summer, cause many of the trees to die down, perhaps for good, or perhaps till renascence sets in; the grassland types then for the time resume their dominance, probably to be subordinated again and again during long periods of slow oscillation. Throughout the whole of this district, the higher forest tracts show abundant evidence of the struggle against the grassland types. 3 The lowering of the temperature during the growing season (from November to March), the first of Rhydberg’s factors, has an intermittent effect which probably influences ecesis of the forest trees in their own or the grassland zone. The shortness of the season, however, is more important in the Kosciusko district; but both factors are closely related, for the prevalence of a low temperature during the growing season as the result of late snow-falls or frosts, must inevitably curtail the season for growth. Late snows are common in this area; in some years very heavy falls take place in September, and lie long, water-logging the soil in certain places and delaying the germination and growth not only of herbaceous but also of arboreal types. In such seasons the small alpine and sub-alpine herbs are several weeks later in flowering as compared with other seasons which have no late snow-falls. Strong wind in winter, especially during frosty periods, appears to be the most important factor affecting the higher forest on the Snowy Mountains. Along the upper limit of the forest, and where it passes into isolated groves or individuals, the trees show the effect of wind by their gnarled, stunted, irregular, often prostrate habit, and their frequently unilateral growth (Plate xix, fig. 2). This peculiar and characteristic growth-form is probably due as much to the desiccating effect of wind, by increasing transpiration from the youngest parts, as to its mechanical action. This wind action prohibits the forest development above 6,100 feet on exposed slopes and peaks, while on the leeward slopes, as has previously been mentioned, the forest ascends to approximately 6,500 feet. The valley-heads and erosion channels on the leeward side, however, are devoid of the forest which occurs on the slopes, as has been described; this is no doubt due to the persistence of the deep snow drifts in such positions, and the smothering of the root-systems while the aerial organs are exposed to strong insolation and high transpiration. This feature has been observed also by Rhydberg in the Rocky Mountains. The significance of the amount of rainfall during the growing season is by no means certain. On account of the high rainfall and low temperatures generally associated with montane zones—to which the Snowy Mountains are no exception— trees normally occurring in such habitats are usually found to have relatively high 202 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, moisture requirements and low temperature requirements (Pearson, 1920); and it is noteworthy that the Hucalyptus coriacea forest maintains its optimum develop- ment between about 4,500 and 5,600 feet, which is the zone of greatest rainfall. Yet at the same time, although it may be that #H. coriacea has low temperature requirements, and that this factor causes it to replace the H. Gunnii forest at Baeckia Corsociation Callisemor Consociation Epacris paludosa Consocies ~—____Epacris serpyllifolia Congocies Richea Associes. Sphagnum Stratum-Society inthe Associes Restio Associes WA | Hy polaena eee Poa-Hypolaena Ecotone Carex Consocies) Luzula Consocies Poa Consociation Text-figure 3. Illustrating the succession in the shallow valleys above 5,000 feet. Baeckia should be spelt Baeckea. BY J. MCLUCKIE AND A. H. K. PETRIE, 203 4,500 feet, its occurrence in exposed habitats near Goulburn, near Clarence, and on the Monaro Plains, regions with a rainfall probably often bordering on 20 inches per annum during some months of the year, suggests that it is an extreme xerophyte, more especially as the soil in these regions is dry and generally of low moisture-retaining power. It is improbable that #. Gunnii or EH. stellulata have lower moisture requirements, while our observations on H#. viminalis in other localities seem to indicate that this has a moisture requirement somewhat higher than most species of Eucalyptus. So far as the upper limit of the distribution of Eucalyptus coriacea is concerned, however, it may be that the rainfall is of importance, since it is to be expected that in the alpine region the effective rainfall is low during the summer, the precipitation being mainly of the nature of light showers which, while sufficing for the grassland vegetation, do not penetrate deep enough to reach the roots of trees. . THE MARSH VEGETATION. In the flat, water-logged floors of the shallow valleys above an altitude of 5,000 feet, the Poa association, which occupies the lower portions of the slopes, gives place to reed- and bush-swamp. This vegetation is exceedingly complex in structure, comprising a large number of communities, all of which seem to be in successional relation. The causes of this succession appear to be somewhat obscure, and require detailed investigation. We have endeavoured in the present paper, however, to characterize the communities and to indicate, to the extent of our observations, the main lines along which succession seems to take place. No doubt the amount, nature and distribution of the precipitation from year to year and factors which modify the drainage system temporarily or permanently, influence this vegetation materially. The accompanying diagram (Text-fig. 3) will help to elucidate the remarks which are made upon succession in the following detailed consideration of the communities of this habitat. Our present investigations indicate that there is little material physiognomic or floristic variation in the communities of*the marsh vegetation throughout the extent of their range, from 5,000 to about 6,500 feet, with the exception of the Richea and Restio associes, which extend in a modified form to 7,000 feet. THE POA-HYPOLAENA ECOTONE. Where the Poa association of the lower parts of the slopes encroaches upon the damp soil of the valley bottom it forms an ecotone in which it is mixed with Hypolaena lateriflora, the dominant of the community which seems to be one of the early stages in the development of the swamp flora. Hypolaena is a reed-like plant about six inches in height, and grows densely between the tussocks of Poa. Reference to the accompanying statement of the floristic composition shows that a large number of the subordinates of the Poa consociation are absent from the ecotone; these are apparently more suited to the drier soil, although in the case of Stellaria pungens, which favours the damp erosion channels higher up the slopes, it is possible that lack of drainage is an inhibiting factor. It will also be observed that, in the case of a number of the components of the Poa consociation, the frequency decreases on passing into the ecotone, which represents the limit of their range; and in the same manner in this region first appear a number of the subordinates of the Hypolaena associes, such as Oreomyrrhis andicola. Certain types occurring in the Poa consociation, e.g. Prasophyllum fuscum, appear to find a more favourable habitat in the ecotone, and their frequency increases. The B 204 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, ny, | 1 Pox \thy 0 Pe «j= Poa caespitosa tussocks. H Cry Comesperma retusum. / ey H = ypolaecia laterifiora. €>- Epacris serpyllifolia. Text-figure 4. Quadrat Vo =" Lotss australis. ER- Craspedia Richet. 4 sq. metres of the Poa- Hypolaena ecotone, near- is est the marsh commun- Lee Luzule campestris. 0 Olearia sp. ities. The spaces. be- tween the tussocks of T= nicnca Gunilt Q- Restio australis. Poa caespitosa are either : bare, or occupied by typically moisture-loving D — Drosera peltata. Br- Brachycome sp. types, e.g. Hypolaena, Drosera, Polytrichum, ep LS paeh On a0. wat a eave, Richea and Liuzula. Correct spelling should Heo- Hemarthria compressa. S — _ S8tylidium lineare. be Craspedia Richea and Baeckea. Cs- Callistemon Sicberi. Wyk Sphagnum sp. Eu- Buphrasia Brownii. BY J. MCLUCKIE AND A. H. K. PETRIE. 205 tussocks of Poa are less continuous in the ecotone than in the Poa consociation, the drainage channels between them which are occupied by Hypolaena and the subordinates, being much wider (Text-figs. 4, 5). 2) ae & = Poa caespitosa tussocks. Gg) Beccrie Gunviana, seedlings. H = Ilypolaena laterifiora. Eh) eruori paludosa, seedlings. Ss = Stylidium lineare. ++ HE Polytrichune sp. Mii Sphagnum sp. iit i hn q R HM + He - Welichrysum sp. Br - Brachycome Eu - Huphrasia Brownii. fic)- Ilemarthria compressa, Text-figure 5. Quadrat of the Poa ecotone 1 m. square. The spaces between the Poa tussocks are drainage channels. The presence of Restio, Hypolaena, Epacris and Baeckea suggests the developmental nature of the community, while in addition the mosses represent types not present in the Poa consociation. The Restio associes (R) is developing somewhat precociously on the right at the bottom. Generally speaking this ecotone occupies the transitional habitat between that of the Poa and that of the Hypolaena community. It may arise also, however, as a result of a definite succession; local alterations in the drainage frequently lead to increase in the soil-moisture-content of areas occupied by Poa, leading to invasion by Hypolaena; as a consequence the same mixed community is found as occurs in the ecotone, although here it possesses rather the character of a mictium (Clements, 1916, p. 140). THE HYPOLAENA ASsocIES. (Text-fig. 6.) As the water-table reaches the surface of the soil, on passing from the Poa-Hypolaena ecotone towards the centre of the marsh, the Poa disappears, yielding the dominance to Hypolaena. This species forms a kind of uniform basal 206 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, stratum throughout all the communities of the marsh; and where it is not inter- mingled with taller types it constitutes a distinct community. All stages of abundance of these taller types may be found, especially in the case of Restio australis; sometimes their distribution is so open that they rank merely as subordinates in the Hypolaena‘associes although taller than the dominant, from which condition they pass to being dominants themselves when in more close formation. Epacris serpyllifolia. OO Epacris serpyllifolia, seedlings. 4+4t Callistemon Sieberi. + e+, Callistemon Sieberi, seedlings. ed es Epacris paludosa, @#@ « +* + be } Epacris paludosa, seedlings. Ae a Baeckia Gwiuniana. er + tp “4 + + ¥4 * Baeckia Gwuviana, seedlings. Sphagnum sp. S+@ Restio australis. Poa caespitosa:; o @&) » | Stylidium lineare. Polytrichum Sp. $f t O — Oreomyrrhis andicola. Text-figure 6. Quadrat 1 m. square of the Hypolaena associes, showing development of the Restio in the centre. A typical Sphagnum patch is seen on the right, while the numerous Hpacris seedlings indicate that further development is taking place. Observations seem to indicate that Restio appears in flat areas where the content of gravitational water is higher than it is normally in the Hypolaena associes, and becomes more prolific with increased water supply. We suggest, therefore, that the accumulation of water in parts, owing to the defective drainage from the great quantities of melting snow on flat ground such as the valley bottoms, causes Restio to spring up among the Hypolaena and to form a new community. Isolated societies of Sphagnum occur in the Hypolaena associes; in these the normal subordinates of the associes, except Oreomyrrhis andicola, are often less abundant, and occasionally Hypolaena alone remains. In some of the larger BY J. MCLUCKIE AND A: H. K. PETRIE. 207 Sphagnum societies numerous seedlings of the epacrid Richea Gunnii appear, and, since this type when found mature is usually growing in a dense cushion on old Sphagnum beds, it is thought probable that the establishment of Sphagnum in the Hypolaena associes paves the way for the development of a new community dominated by Richea. In somewhat drier areas than that in which the above succession takes place, the Hypolaena associes contains numbers of seedlings, often exceedingly small, of Epacris serpyllifolia or of HE. paludosa. There is no doubt but that this is evidence of another succession taking place from Hypolaena to the Epacris associes; and it is this evidence in particular, which clearly establishes the seral nature of the Hypolaena associes. In the earlier stages of the developing Hpacris associes, E. serpyllifolia seems often more abundant, with only occasional seedlings of E. paludosa, although more rarely a pure developing consocies of the latter is found; in the older stages, however, only the H#. paludosa consocies was seen, although there is every reason to believe that the Hypolaena associes must be capable of giving rise to both the Hpacris communities. It must be added at the same time that there is undoubted evidence in places that the Epacris serpyllifolia consocies gives place to the EH. paludosa consocies, the dominant of the later community being a larger shrub; and it certainly seems in many cases that a telescoping of this succession takes place in the developing Epacris associes, so that the originally abundant seedlings of E. serpyllifolia subsequently give place to an invasion of seedlings of H. paludosa, which is perhaps a more vigorous type. A more probable explanation is that EH. serpyllifolia is better adapted to establish itself first in the Hypolaena and that #. paludosa has to await further changes in the conditions before it can colonize the habitat, after which it readily assumes dominance on account of its larger size. / It thus appears that the Hypolaena associes is a synthetic seral community, which, collaterally with habitat changes in different directions, develops along various lines. THE RESTIO ASSOCIES. Restio australis, which we have already referred to as dominating a community developing in all probability from the Hypolaena associes, is a restiaceous plant from one foot to eighteen inches high, growing densely and often occupying large areas (Plate xii, fig. 2). The subordinates of the Restio associes will be seen from the accompanying table to be much the same as in the Hypolaena associes, and Hypolaena itself forms an almost constantly present lower stratum. FRestio, however, occurs often with no subordinates as a pure society in little flat water- holes so characteristic of the sub-alpine and montane marshy areas. Sphagnum societies are occasional, in which communities most subordinates except Hypolaena are absent; and judging by analogy with the previously recorded observations in the Hypolaena associes, it is possible that these societies may lead to the development of the Richea associes. Seedlings of Epacris serpyllifolia and E. paludosa are abundant in places, so that there appears reason to believe that when these have attained maturity the Restio associes will have developed to a further stage in the sere dominated by Epacris. A large area of the Restio associes was observed where dead white gnarled stems of Epacris indicated that this plant had previously made fair headway and subsequently died out. Apparently its disappearance was followed by the estab- 208 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, lishment of the previous stage of the sere, viz., the Restio associes, suggesting that a reversal of the changes in the habitat was the factor leading to the destruction of the Epacris. THE RICHEA ASSOCIES. Richea Gunnii is a megaphyllous, unbranched or sparsely branched epacrid, growing in dense clumps, usually on old Sphagnum beds (Plate xiii, fig. 1). The habit of Sphagnum of forming mounds is well known, and Richea appears to find its most favourable environment on these, sending long shoots upwards through the Sphagnum; by this means the clumps of Richea reach a height of two or three feet, although the normal height of the plant under ordinary conditions is usually only about one foot. : Richea grows so densely and in such a sodden substratum, that it ordinarily has few subordinates. It seems, however, to consolidate the Sphagnum beds, and, as the water in the soil gradually finds drainage channels by which to pass away, other types are able to come in. The first to appear is Restio, after which comes Hypolaena, suggestive of reversion of the sere owing to reversion of the habitat changes. Hypolaena grows up through the Richea on long attenuated stalks, in order to reach air and light, so that, although the plant is normally only about six inches high this ecad attains a length of two or three feet. Where the drainage and consolidation has proceeded further, Baeckea Gunniana gains entrance, as also less frequently does Callistemon Sieberi. This seems to suggest a possibility of Richea giving place to the Baeckea-Callistemon association, which is the climax stage in the succession taking place in the swamp flora. Probably one may explain in the same way the rather curious local presence among the Richea of Ozylobium ellipticum var. alpinum, a type which usually inhabits much drier places in the Hucalyptus forests. Epacris paludosa also is present in some of the dying clumps of Richea, which suggests succession from Richea to the Hpacris associes; this is rendered more probable by the fact that Hpacris is usually an intermediate stage in the develop- ment of the Baeckea-Callistemon association. The distribution of Richea between 5,000 and 5,500 feet is much more restricted than that ef the communities previously described, nor do the clumps often occupy very extensive areas. From 5,500 to near 7,000 feet (the upward limit of its range), however, the Richea associes gradually becomes more frequent and wide- spread, until it eventually occupies extensive areas of the valley floors where the habitat is sufficiently wet. Its structure in the alpine regions will be referred to again subsequently. THE EPACRIS ASSOCIES. (Text-fig. 7). Reference has already been made to the presence of Hpacris seedlings in the Poa-Hypolaena ecotone and in the Restio, Hypolaena and Richea associes, which appear to develop into a community having Hpacris as dominant. So far, the communities we have been considering have been distributed in zones of increasing content of gravitational water in the soil; Hpacris, however, occurs in drier soils more akin to that of the habitat of the Poa-Hypolaena ecotone and the Hypolaena associes. The Hpacris associes may be a natural development of these two communities in an unchanging habitat; and, indeed, every stage may be observed between these two communities with only a few plants of Hpacris scattered here and there (Plate xvii, fig. 1), to where it is abundant with only a BY J. MCLUCKIE AND A. H. K. PETRIE. 209 subordinate stratum of either Poa with a little Hypolaena or Hypolaena with a little Poa (Plate xv, fig. 2; Plate xvi, fig. 2). Consequently the transitional area between the Poa consociation and the marsh may be occupied in places by a Poa-Epacris ecotone rather than by a Poa-Hypolaena ecotone. The Epacris associes also appears to follow the Restio and Richea associes coincident with the drainage of the excess of gravitational water from the soil which takes place eventually as the result of the gradual formation of erosion channels. In this case Poa is not present, but later it is possible that Poa enters the habitat and becomes as abundant as if the Hpacris had directly succeeded the Poa-Hypolaena ecotone. (Ba) - Baeckia Gwiniana. Be- Bacckia Guuniana, seedlings. &5- Epacris serpyllifolia. &- Epacris serpyllifolia, seedlings. (Eh)- Epacris heteronema. “EX Epacris heteronema, seedlings. DI 4 (i) Wypolaena laterifiora. R - Restiad australis. Br- Brachycome sp. C ~ Craspedia Richei. D — Droscra peltatu. Cs- Callistemon Sieber. Ss — Stylidium lineare. 0 ~ Olearia sp. Cr = Comesnerma rvetuswm, Pou ccaespitosa, Text-figure 7. Quadrat, 1 m. square of the Hpacris serpyllifolia consocies in process of developing into the Baeckea consocies. In certain drier parts of the swamp the Poa consociation was observed merging into the ecotone, which in parts had apparently developed directly to Restio with the omission of the pure Hypolaena stage, Poa still being present in the Restio associes. In places the latter was developing into the Hpacris serpyllifolia consocies, with scattered plants of the dominant between which Poa was abundant. This seems to be a telescoping of the sere owing to drier edaphic conditions. Destruction of the Epacris paludosa consocies and its replacement by the Poa- Hypolaena mictium was observed in several places, where the habitat was littered with the dead gnarled and knotted stems (Plate xv, fig. 1). This destruction may 210 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, have been caused by snow lying long on the ground and killing out the Epacris. The latter would then naturally be replaced by the Poa-Hypolaena community which, as has been mentioned above, is akin in its habitat requirements. As has already been mentioned, two consocies occur, dominated respectively by HE. serpyllifolia and E. paludosa. The former seems to appear first and often subsequently to give place to the latter, but in large areas EZ. paludosa is absent and the EH. serpyllifolia consocies develops directly to the Baeckea-Callistemon association, which usually follows the Epacris associes as the next and final stage of the sere. Evidence of this interrelationship between these communities is seen in the presence among the Epacris of locally abundant seedlings of both Baeckea and Callistemon. Occasionally in the Epacris associes occur single mature plants + \ ha \ \ SNC Sh: Gm MEAL: \ , \ -\ Pe Ng ¢ ee BS LY eatt fe + ++ t ( } ( ! aN 4 W . OGG 2 Fao on, (a 0 2 g Peo ss + iN ie} (4 + 27 40 208 Q o o acs LE. + o a0 + . 4 2O) --\ 50% 5 oo eee ++ a Epacris serpyllifolia consociation. 4 - .Poa caespitosa consociation. Op Poa-Hypolaena ecotone. whe, Aan. <~ Hypolaena and Restio associes. C)- Richea associes. 632. Luzula consociation. oo ome 4 ‘ é ome, ‘ contour line. -o® Text-figure 8. Diagrammatic Chart (not to scale) of a portion of the marsh vegetation. BY J. MCLUCKIE AND A. H. K. PETRIE. 211 of Callistemon Sieberi and Hakea microcarpa, shrubs about three feet high which stand conspicuously above the dwarf EHpacris (Plate xvi, fig. 2). The Epacris associes is one of the most widespread communities in the marsh between 5,000 and 5,500 feet, and in many cases, indeed, may possibly be a sub-climax. Above 5,500 feet, however, it gradually gives place to the extensive Richea associes which apparently is more suited to the sub-alpine environment. Text-figure 8 shows the interrelationship of the communities described in detail in the preceding pages. THE BAECKEA-CALLISTEMON ASSOCIATION. This association appears to be the climax stage in the development of the marsh vegetation, but rather curiously it is very restricted in its distribution, and it is only here and there that conditions appear to permit the existence of the dominants. The association is present sometimes as a zone round the edge of the marsh in a manner suggesting the occurrence of the Epacris associes, but only where the ground has a well-marked slope; at other times it colonizes the margins of channels of water running rapidly through the marsh. These facts of distribution suggest that the association requires a more aerated soil than normally constitutes the marsh; and this conclusion is supported by the similarity between the Callistemon consociation of the association under discussion and the Callistemon society which inhabits water-courses in the Hucalyptus forest higher up the slope (Plate xii, fig. 1). The dominants occur separately as consociations, the Baeckea consociation being the more abundant and containing Callistemon Sieberi and Hakea microcarpa as subordinates. The number of species in this association is small, since the closeness of the shrubs prevents the occurrence of lower strata and necessitates the display of all foliage at one level; Richea, Hypolaena and Restio are present in the Baeckea consociation growing up on long attenuated stalks through the mass of knotty branches of the Baeckea, in the manner described for Hypolaena in the Richea associes. The light ecad of Hypolaena in this community attains a height of three feet, six times the normal height of the plant. The destruction of Hpacris by severe conditions with consequent return to the Poa-Hypolaena stage of the sere has already been described. A similar case was observed of the destruction of the aerial shoots of Callistemon in a consociation of that type, leaving the characteristic white stems standing erect throughout the _ area. After the ground had been so bared, the Hypolaena associes had appeared, and in parts had developed to the Restio associes, although not so far as. the Epacris associes, H. serpyllifolia being only occasional. In the meantime a fundamental difference between the epacrid and the myrtaceous type had asserted itself. All our observations indicate that members of the Epacridaceae have generally no means of renascence after destruction of the aerial shoots as is characteristic of the Myrtaceae and many other families represented in Eucalyptus forests; therefore, while regeneration of the Epacris associes has to await the comparatively slow process of migration and ecesis, Callistemon, before even the Restio stage had fully asserted itself, had commenced active renascence everywhere by the production of adventitious shoots from the base of the stem, which no doubt would rapidly grow up and restore the original structure of the community, while the Restio and Hypolaena would be stamped out (Plate xiv, fig. 1). It is interesting to note that Baeckea which was apparently occasional in the original 212 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, community, had survived destruction, suggesting that Baeckea is a more vigorous type; a conclusion supported by its greater abundance at higher altitudes in the Poa-Celmisia association. THE LUZULA-CAREX ASSOCIES. In flat shallow pools of water occur two closely related consocies dominated respectively by the sedge-like Luzula campestris and Carex Gaudichaudiana. The Luzula consocies occurs not only in the marsh vegetation, but also in little flat hollows or natural drains in the Poa consociation or in flat areas of the Callistemon Sieberi society in the Hucalyptus coriacea consociation. The Luzula-Carex association does not appear to form a stage in the complex sere already described, although it passes into it in several ways, as is about to be mentioned. The floristic composition is also considerably different from that of the various stages in that sere, since there are present a number of amphibious or semi-aquatic types such as three species of Ranunculus, Utricularia, and even the definitely hygrophytic Chara or Nitella. In one example of the Luzula consocies Oreomyrrhis andicola was observed to be equally abundant with Luzula. Since the leaves of that rosette-type form a lower stratum than the Luzula we have termed it arbitrarily a sub-dominant; at the same time when Oreomyrrhis is in flower or fruit, its pedicel is equally as tall as the haulm of Luzula, so that during a large period of its existence it is co- dominant. The community in which this observation was made was a less wet habitat than is normally occupied by the Luzula consocies; and it is possible that Oreomyrrhis has gained entrance to the community on this account. Increasing drainage of the habitat in one part has resulted in the establishment of numerous seedlings of Epacris serpyllifolia, indicating that the community is able to develop into the #. serpyllifolia consocies and so link up with the main sere of the marsh vegetation. Another instance of this is exemplified by the presence of Restio in parts of both the Carex and Luzula consocies, which of course on account of its larger size soon becomes dominant, forming the typical Restio associes. Occasionally Hypolaena is also locally abundant in the Carex consocies so that development to the Hypolaena associes may possibly take place concomitant with consolidation of the substratum and ablation of the surface water. These various lines of possible succession are illustrated in Text-fig. 3. Floristic Composition. Reed Stratum. L. Gs Restio australis R.Br. If Epilobium glabellum Forst. Grass Stratum. ir} Luzula campestris D.C. d f-e Carez Gaudichaudiana Kunth. lf d Hypolaena lateriflora Benth. — la Rumex acetosella Linn. r — Poa caespitosa Forst. If —_— Plantago varia R.Br. ; If — Brachycome sp. If —_ Oreomyrrhis andicola Endl. lsd — Ground Stratum. Ranunculus Millani_-F.v.M. a o-a Utricularia dichotoma Labill. var. wniflora Benth. — la Chara sp. or Nitella sp. — la Velleya montana Hook. lf oo Epacris serpyllifolia Labill. (seedlings) Ic — Moss societies (chiefly Sphagnum and Polytrichum) ° — 213 Kk. PETRIE. H. BY J. 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MCLUCKIE AND A. H. K. PETRIE. 215 THE ALPINE VEGETATION. THE POA-CELMISIA ASSOCIATION. Above the tree-line in the neighbourhood of 6,000 to 6,500 feet, the open. stunted Eucalyptus forest gives place to a vegetation composed mainly of low- tussock grassland and herbs. This vegetation has a characteristically alpine physiognomy, and forms a low dense covering over the treeless peaks which reach an altitude of over 7,000 feet. Two consociations are found, the one being dominated by Poa caespitosa, and forming a typical low-tussock grassland community. This is in reality the same community as occurs below the Hucalyptus forest on the slopes of the sub-alpine region, and as forms the ground stratum of the forest itself. The composition of the subordinates, however, differs somewhat, as will be seen by comparing the statement of the floristic composition at the end of this section of the paper, with that of the ground stratum of the Hucalyptus coriacea consociation and with that of the Poa consociation of the sub-alpine region given with that of the marsh vegetation. The other consociation is dominated by a creeping rosette composite, Celmisia longifolia, which forms a dense felt-like growth. The Poa gives a rich olive-green to the hills in the distance; Celmisia, however, with its glaucous leaves, thick white tomentum and numerous inflorescences, appears in the distance as large bluish-white patches scattered over the hillsides; this feature is illustrated in Plate xviii, figs. 2 and 3. The subordinates of these two communities, as will be seen from the accompanying statement of the floristic composition, are largely composed of the same species, although it appears that the more delicate mesophytic types favour rather the Celmisia consociation. The majority of the species conform to characteristic alpine life-forms, as will also be seen from the statement of the floristic composition. Apart from the tussock grass represented by Poa and the mat grass represented by Hemarthria compressa, the dominant life-form is the rosette herb, intermixed with a smaller proportion of cushion herbs. Shrubs are only occasional and tend to be confined to the shelter of granite boulders; they exhibit a marked degree of nanism, being either prostrate or in the form of low cushions, usually occurring flattened close against the rock surfaces, in order to avoid the effects of the strong winds (Plate xix, fig. 1). Among these shrubs may be mentioned Grevillea australis, Podocarpus alpina, and the fern Polystichum aculeatum. The extreme shortness of the vegetative season at these high altitudes results in every species flowering at the same period; consequently there is a wealth of floral production unmatched in other regions of the State, more especially as the flowers are mostly large and brightly coloured (Plate xix, fig. 3). A certain amount of competition and overlapping takes place between the Poa and Celmisia consociations, and often the two types are co-dominant. In damper parts of the slopes and valley-bottoms in both consociations occurs the dwarfed and prostrate HEpacris petrophila, which in parts becomes dominant, thus forming a new consociation retaining the typical subordinates of the Poa and Celmisia communities. The Richea Gunnii associes occurs also in the swampy areas, where it is the main community, as has been mentioned earlier; this species is also sometimes locally abundant in the Celmisia consociation. The Epacris associes of the marsh vegetation, however, does not occur, and it appears that the Richea associes forms the climax at these high altitudes. The Hypolaena associes its found pure in one or two marshes, and this develops directly into the Richea associes, which then contains Hypolaena in abundance. The EHpacris 216 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, petrophila consociation occurs associated with the Richea consociation in these marshes but does not appear to be developmentally related. In water-courses below the melting snow-drifts a Ranunculus rivularis society occurs with a number of semi-aquatic subordinates, including Caltha introloba which is confined to altitudes bordering on 7,000 feet. On many drier areas Celmisia and Poa occur practically alone, since it appears that the subordinates are the less hardy and more mesophytic types. During nine months of the year the alpine region is covered in snow which in places frequently lies as drifts throughout the summer. The effect of this on the vegetation is naturally very pronounced. All the herbaceous types die down when the snow comes, but perennate from season to season by subterranean organs of propagation. Thus an area from which the snow has just been melted is seen to be covered with the withered remains of vegetation; and later appear the young shoots of Poa, etc. In some areas where snow has remained continuously for several years these withered remains have very largely disappeared, and no doubt the perennating organs are here entirely killed out, so that a new migration will have to take place. These occasional patches are the only areas of granite soil which, in summer-time, are not clothed with a dense carpet of vegetation. Contrary to this feature of the lifehistory of the herbaceous plants, the shrubs are able to withstand the effects of the snow covering, without even losing their leaves, since no periodically deciduous species occur in the New South Wales flora: At the same time the shrubs are often killed during severe seasons, as is evinced by the bleached, gnarled and thick woody stems which are often to be seen. The Poa and Celmisia consociations occur also on a large area of slate in the alpine region, where they possess practically the same features. A number of smaller differences in floristic composition appear to exist, as will be seen from the accompanying lists; but we have no definite record of any plant being confined to the consociation on the slate, nor have we definite record of any species not occurring on the slate. It is probable, however, that further work may modify this statement, since our observations on the composition of the slate flora are incomplete. In the alpine region numerous very typical structural and growth features are exhibited by the herbaceous and shrubby plants. The habit of the shrubs varies with exposure to wind. In the most exposed situations where the desiccating effect of wind is predominant and retards normal elongation of the aerial shoots, nanism, or stunted, dwarfed and distorted growth results. The larger shrubs such as Phebalium ovatifolium, Orites lancifolia, Prostanthera cuneata, Podocarpus alpina and Grevillea australis assume a close, dense, caespitose habit, which favours reduction of transpiration and natural protection from wind-action. Forms like Pimelea alpina, Lissanthe montana, and Kunzea Muelleri frequently assume a typical espalier habit, prostrate and straggling, and raising their growing tips only a few inches above the level of the soil or protective rock. Several mat-forming herbs occur in the alpine zone, being generally very dwarfed forms which cling closely to the surface of the soil. The most important of the plants in this category are Stackhousia pulvinaris, Raoulia catipes, and Epilobium confertifolium. The rosette leaf habit is represented in a number of types, as will be seen from the accompanying statement of the floristic composition. The majority of these plants are characterized by deep tap roots. Sclerophylly is a characteristic feature of the shrubs, while many types, both shrubby and herbaceous, have extensive and dense coverings of silky or woolly Species. Acaena sangwisorbae Vahl. Aciphylla glacialis F.v.M. Astelia alpina R.Br. ...... Brachycome cardiocarpa F.v.M. var. alpina Brachycome scapiformis D.C. Barbarea vulgaris R.Br. Carex breviculmis R.Br. ... Celmisia longifolia Cass. Claytonia australasica Hook. Craspedia Richea Cass. Craspedia Richea Cass. var. alpina Benth. Drapetes Tasmanica Hook. Epacris petrophila Hook. .. Huphrasia Brownii, F.v.M.° Galium wumbrosum Sol. Grevillea australis R.Br. Helipterum incanum D.C... Hemarthria compressa R.Br. Hymenanthera dentata R.Br. Kunzea Muelleri Benth. Lissanthe montana R.Br. .. Lycoperdon sp. Lycopodium clavatum R.Br. Myosotis australis R.Br. ... Olearia floribunda Benth. .. Oreomyrrhis andicola Endl. Oreomyrrhis pulvinifica F.v.M. Orites lancifolia F.v.M. Pimelea alpina F.v.M. Pimelea axiflora F.v.M. var. alpina F.v.M. Phebalium ovatifolium F.v.M. Poa caespitosa Forst. Podocarpus alpina R.Br. Polystichum aculeatum (L.) Schott. Polytrichum sp. Pentachondra pumila R.Br. Prostanthera cuneata Benth. Ranunculus anemoneus F.v.M. Ranunculus dissectifolius F.v.M. Ranunculus Gurnnianus Hook. Ranunculus Muelleri Benth. Azorella dichopetala Benth. Ranunculus sp. Raoulia catipes Hook. Richea Gunnii Hook. Senecio pectinatus D.C. Stackhousia pulvinaris F.v.M. Taraxacum dens-leonis Desf. Viola betonicifolia Sm. Danthonia robusta F.v.M... Epilobium confertifolium Coprosma Nertera F.v.M... Lycopodium Selago, Linn... —_—_—————————————— BY J. MCLUCKIE AND A. H. K. PETRIE. Floristic Composition. Poa-Celmisia Association. Life-form. Creeping mat herb Rosette herb Rosette herb Rosette herb Rosette herb ..... Low erect herb Sedeere io cee Creeping rosette herb Mat herb se ee ee Rosette herb ...... Prostrate shrub Prostrate shrub Low erect herb .... Low herb ......... Caespitose or pros- trate shrub ..... Creeping rosette herb IOWA LASS eee Espalier shrub Hspalier shrub Hspalier shrub italy wary eicueencee: Decumbent herb Herb Espalier shrub Rosette herb Rosette herb Caespitose shrub Espalier shrub Espalier shrub Caespitose shrub Low-tussock grass Caespitose shrub ee ew ew we ey Hspalier shrub Caespitose shrub Rosette herb ...... Rosette herb Creeping rosette herb Rosette herb Rosette herb Rosette herb Mat herb Low caespitose shrub Erect herb Mat herb Rosette herb Creeping rosette herb Tufted grass Mat herb 5.250... Espalier shrub see eee | | | | | Granite. Poa | Celmisia consociation.| consociation. la — f f — fo) -O Co) f fs — Oo (0) fo) lf d —_— o-Ice f (e) (6) f fo} fo) la lo-la la fs o up to — 6,700 ft. (e) — — o-c c lf vr vr — fo} ro) = (8) We vr EST r r ae ray sett r poke vr — oO o-le Co) fo) o-le d o-a oO Bee r aoe — la oO pte B: r ae — (e) — o-lf fo) fo) — o-lf f f ra) f — la r rae lo lo o-c fo) vr — o-le — —- (o) oO a r — Poa consociation.| consociation. la 217 Slate. Celmisia 218 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, hairs on their inflorescences, leaves and young shoots. Examples of this class are Celmisia longifolia, Helipterum incanum, Podolepis longipedata, Craspedia Richea var. alpina, Raoulia catipes, Oreomyrrhis andicola and Ranunculus Muelleri. The relation of hairiness of alpine and sub-alpine plants to protection against intense insolation, and consequent excessive transpiration and inhibition of growth, is so well known that it needs no discussion here. Epacris petrophila Consociation. Epacris petrophila Hook. d Celmisia longifolia Cass. f-e Richea Gunnii Hook. la Craspedia Richea Cass. o-f Richea Associes. Richea Gunnii Hook. d Restio australis R.Br. la Sphagnum sp. (9) Ranunculus rivularis Society. Herb Stratum. Ranunculus Gunirianus Hook. Brachycome cardiocarpa F.v.M. var. alpina f Ground Stratum. Ranunculus rivularis Banks and Sol. Caltha introloba F.v.M. Drosera Arcturi Hook. Sphagnum sp. oov em THE EPACRIS PETROPHILA CONSOCIATION. The summits of certain of the peaks in the slate region of the Plateau represent an extremely barren habitat: the ground is composed of the upturned edges of the strata of slate, and there is practically no soil. The conditions seem too severe for the grassland which tends to accumulate the raw humus of a moisture retaining soil, and a few of the hardy species form an open community which has the characteristic physiognomy of fell-field or alpine rocky desert (Plate xvii, fig. 2). None of the individuals are more than three or four inches in height, and they are scattered intermittently over the rocky ground. The available moisture is less than elsewhere, hence the plants are mostly xerophytes, especially the dominant, Epacris petrophila. It is curious in this connection that this species should have been characteristic of the damper slopes in the Poa- Celmisia association. Although the majority of the components of the community were found in the Poa-Celmisia association, the great difference in physiognomy marks it out as a distinct association, distinct even from the consociation of the Poa-Celmisia association having the same dominant. A remarkable feature is the sudden replacement of the Hpacris petrophila association by the Poa consociation on passing to a more sheltered habitat over the brow of the hill, the ecotone region being only a few yards in breadth. Floristic Composition. Epacris petrophila Hook. Colobanthus subulatus Hook. Carez breviculmis R.Br. Azorella dichopetala Benth. Azorella cuneifolia F.v.M. Poa caespitosa Forst. Brachycome sp. Buphrasia Brownii F.v.M. very small form Lichens lay bei (a) (a) (co) (o) Ley ia-y jen BY J. MCLUCKIE AND A. H. K. PETRIE. 219 Summary. The paper comprises an account of the plant communities of the Kosciusko Plateau. ; Three regions are recognized on the plateau, viz., the alpine, sub-alpine and montane zones. The montane zone and the slopes of the ridges in the sub-alpine zone are occupied by Eucalyptus forests, the former mainly by a Hucalyptus Gunnii consociation, the latter by a Hucalyptus coriacea consociation. Accounts are given of the structure and adaptations of these forests, including certain features of regeneration, and of the factors controlling the timber-line at the upper limit of the sub-alpine zone. The flat bottoms of the shallow valleys of the alpine and sub-alpine regions are occupied by a: marsh vegetation comprising reed-swamp and dwarf-shrub heath. The interrelationships of a number of seral communities in this habitat are discussed at some length. The alpine zone, extending from the upper limit of arboreal vegetation to the summit of the plateau, is occupied mainly by a Poa-Celmisia association. The ‘Poa consociation forms a low-tussock grassland community, and occurs also in the sub-alpine zone between the Hucalyptus forest on the slopes and the marsh vegetation in the valley bottoms; the Celmisia consociation forms a mat-herb community and is confined to the alpine region. Acknowledgements. The authors desire to record their thanks to Professor Griffith Taylor and his associates for the privilege of reproducing their reconnaissance map and the block diagram of the Kosciusko Plateau, and to Mr. EK. Cheel of the National Herbarium for kindly identifying a few of the specimens. References. CLEMENTS, F. E., 1916.—Plant Succession. Carneg. Inst. Wash. Publ. 242. HeumMs, R., 1896 and 1897.—The Australian Alps or Snowy Mountains. Jour. Roy. Geog. Soc. N.S.W., Vol. VI, 4, 1896, and 5, 1897. MAIDEN, J. H., 1898-99.—The Flora of Mt. Kosciusko. Agric. Gaz., N.S.W., 1898 and 1899. PEARSON, 1920.—Factors controlling the Distribution of Forest Types. Hcology, 1. RHYDBHRG, 1914.—Review of two papers in Journ. Ecol., II, p. 140. TAYLOR, G., BROWNE, W. R., and JARDINE, F., 1925.—The Kosciusko Plateau, a topographic reconnaissance. Proc. Roy. Soc. N.S.W., 59, p. 200. EXPLANATION OF PLATES X-XIX. Plate x. Map of Kosciusko Plateau (20 miles by 6 miles), where the elevations are represented by form-lines or approximate contours. Plate xi. 1. Slope of a shallow valley at about 5,100 feet. The Hucalyptus coriacea consociation, with its characteristic shrubs, is seen in the rear. The typical life-form of the dominant is well illustrated in the comparatively large tree on the left. The Poa consociation is present on the slopes on the right and left, while the marsh vegetation occupies the level ground where water collects. The low dark heath-like portion is the Hpacris association, while the Hypolaena associes and such communities constitute the remaining portion of the marsh vegetation. 2. A shallow valley at about 5,500 feet, showing destruction of Hucalyptus coriacea by severe climatic conditions. The lower stature of the trees at this altitude compared with those of the previous photograph is evident. The replacement of the forest by the Poa consociation on the lower parts of the slopes is shown; the marsh vegetation is Cc 220 THE VEGETATION OF THE KOSCIUSKO PLATEAU, i, sparingly developed, as the drainage is comparatively good in this instance, but darker patches of it are seen in the middle distance. The occurrence of isolated trees on small raised drier hummocks in the Poa consociation is a conspicuous feature. Plate xii. 1. View at 5,200 feet, showing the Eucalyptus coriaecea consociation in the back- ground, and the Callistemon consociation in the foreground. 2. The Restio associes in gently undulating country at 5,500 feet. The Poa and Eucalyptus coriacea consociations are seen on the higher ground in the distance. 8. A shallow valley at 5,600 feet showing the Hucalyptus coriacea forest on the ridge and the Poa consociation in the foreground. The lower stature of the trees than in Plate xi, fig. 1, is again evident. The tussock-like nature of Poa caespitosa is more noticeable at this higher altitude on account of the greater abundance of drainage water. This is particularly seen in the foreground. Plate xiii. 1. A granite boulder in a marsh at 6,000 feet, showing Baeckea Gunniana flattened against it, in order to obtain protection from wind. Richea Gunnii is seen in the right foreground. 2. A society of Veronica Derwentia in a portion of the Hucalyptus coriacea consociation at 5,500 feet, which has been killed by fire. Poa is seen to occupy the ground between the plants of Veronica. Plate xiv. 1. A regenerating plant of Callistemon Sieberi, whose aerial portion has previously been killed by severe climatic conditions. 2. The Snowy River at 4,000 feet, showing the Hucalyptus Gunnii consociation clothing the slope in the background, and the Leptospermum society lining the river bank. The difference in the topography from the higher altitude, as well as the denser forest is evident. The bare nature of the forest floor in the H. Gunnii consociation is seen on the right. Plate xv. 1. In the middle distance is seen the Epacris paludosa consocies in flower. The foreground was originally occupied by this type, which has, however, died out, as is evident by the dead branches, and has been replaced by the Poa-Hypolaena mictium. The Eucalyptus coriacea is well developed in the background. Altitude 5,100 feet. 2. Another view of the Hpacris paludosa consocies in flower, passing through the Poa-Hypolaena mictium which reaches as far as the foot of the white tree on the right and then merges into the Poa stratum society of the forest. Plate xvi. 1. A view in the alpine region at 6,700 feet. The white patches on the steep slope on the left are dead trunks of a low forest of Hucalyptus coriacea, which has migrated upwards and subsequently been killed by severe seasons. In the foreground is seen the Celmisia consociation, the dominant being admixed with Poa. The distant ranges are in Victoria. 2. The Epacris paludosa consocies, 5,100 feet. A bush of Hakea microcarpa is seen in the background. a 3. A view in the Hucalyptus Gunnii consociation, 4,000 feet, showing the tall trees and the ground almost devoid of vegetation. 4. A shallow valley at 5,800 feet. The Hucalyptus coriacea consociation is seen to be here very stunted and confined to the ridges between the erosion-channels running down the slope. Between the patches of forest are dense societies of Prostanthera cuneata which extend down over the Poa consociation on the lower part of the slope, On the floor of the valley in the creek bed occur the Restio and Hypolaena associes. Plate xvii. 1. The Poa-Hypolaena ecotone developing into the Hpacris associes. Plants of Epacris paludosa are scattered through the Poa. \ Text-fig. 53. Longitudinal section of apex of style. The young stigma, s., is growing up from the base of the pollen cup, and forcing out the microspores through the apical pore, p. x 73. Text-fig. 54. Another view of same showing conducting tissue of style. The portion of the cup r. has been slightly displaced in cutting the section. x 73. Text-fig. 55. Part of stigma of previous figure shown under a higher power of magnification in order to illustrate nature of component cells. x 133. : Text-fig. 56. Longitudinal section of an older stage of style showing stigma occupying centre of pollen cup. The bi-lobed nature of stigma, and the central papillate cells, p., are evident. x 33. BY P. BROUGH. 493 investigations on record in the case of certain species of Goodenia. The conclusions arrived at are so varied, however, that a careful study of the method of pollination in other genera of the family seems advisable. In the case of Dampiera stricta the method of dehiscence of the anthers, and the depositing of the pollen grains within the hollow indusium have already been described. The cup is filled to overflowing, the spores forming a pyramidal mass. Thereafter the indusium closes owing to the contraction of the margins. At the time when the style finally elongates, and the flower bud is on the point of opening, the indusium is forcibly thrust into a chamber formed by the auricles in the line of junction between the two posterior petals. The two flap-like appendages aid in the complete enclosing of the indusium, which is orientated so as to face the anterior side of the flower. At no period then, has the pollen been exposed, although part of the bent style is visible, outside the corolla between the two posterior petals. By this time the anthers have withered, and are of no further significance. The rudimentary stigma at the base of the closed indusium now commences to grow rapidly (Text-figs. 53 and 54) and gradually pushes the pollen in front of it, and out through the narrow aperture now present at the top of the fringed pollen cup (Plate xxxvii, figs. 3, 4 and 5). The pollen thus ejected either lodges on the outer sloping sides of the indusium, as indicated in the photographs just referred to, or is deposited in the chamber in which the indusium is imprisoned. Obviously such pollen grains cannot regain their former position resting on the apex of the stigma. Eventually the steadily expanding and rounded stigma protrudes above the rim of the inner cup of the indusium (Text-fig. 56) and occupies the cavity formerly filled by pollen grains. A few microspores may remain lodged between the lower portion of the stigma and the inner wall of the indusium, but such are ineffective from the point of view of pollination. The stigma finally becomes slightly two-lobed, and the cells within and around the depression so formed become papillate, and eventually receptive in relation to the pollen grains (Text-figs. 56, 57 and 22). Furthermore, the sub-epidermal cells immediately within this cleft, and also the tissue leading therefrom, and down through the centre of the style are of a loose, thin-walled nature. Such cells have all the characters of a typical conducting tissue for the nutrition of the advancing pollen tube. Pollen tubes in considerable number were found when the central tissue of the style was dissected out, and examined under a microscope. In no case were microspores seen to germinate while still within the indusium, although at this stage they are in the binucleate condition, and in many cases show the slight protrusion of the intine through the four weak areas in the exine characteristic of the mature microspore. Judging from the various stigmas examined, at different stages of growth up to and including the emergence of the stigma from the indusium, it seems clear that the pollen grains do not germinate within their own indusium. Evidently, then, the stigma does not become receptive until the pollen grains from the same flower have been ejected from the pollen cup. Now, five well developed nectaries are found at the base of and within the whorl of stamens. These are obviously related to insect visitation, and it is well known that bees are frequent visitors to the flower in question. That insects are instrumental in the transference of pollen is proved by the fact that in one case foreign pollen was actually found on a stigma examined. The contrast which this pollen (which was round and spiny) made with the characteristic microspores of Dampiera, rendered this point peculiarly easy of elucidation. The foreign 494 STUDIES IN TILE GOODENIACEAE, i, pollen had not germinated. From what has already been demonstrated in regard . to the rate of growth of the pollen-tube (Text-fig. 23), it follows that fertilization may occur within a few hours of the pollen being deposited on the ripe stigma. An insect entering the flower pushes the two adaxial perianth segments apart, and, at the same time releases the pollen cup from its chamber. Pollen thus falls on the visitor, and such action will continue until all the pollen has been removed, Text-fig. 57. Papillate cells of stigma under higher power of magnification. x 266. Text-fig. 58. Longitudinal section of nectary, n., situated at base of style, s., 2nd within filament of stamen, f. x 150. a consummation which may well be effected before the stigma becomes receptive. Pollen from the pouch is also removed at this stage. It was also observed that a considerable proportion (about 20% or more) of the pollen grains never reach maturity. Thus when the stigma becomes receptive the pollen grains have either been removed by insects or have been pushed aside, and so subsequent insects will deposit pollen from their backs or heads on the surface of the receptive stigma. It must be conceded then, that pollen is actually transferred by insects from one flower of Dampiera stricta to another flower on the same or on another plant, and so cross pollination is effected. It is not impossible, however, that self pollination may occur in the event of the flower not being visited by the insects, although the writer is of the opinion that the available evidence is against the view that self-fertilization does actually occur. The point. can be settled only by taking means to prevent the access of foreign pollen, and then determining whether embryos have formed in the ovaries concerned. The writer hopes to elucidate this point in the near future. An experiment of this nature has already been carried out in the case of BY P. BROUGH. 495 Goodenia cycloptera by Haviland, F. E. (1914), who found that embryos were not formed. A survey of the facts laid bare by this investigation of various phases in the life-history of Dampiera stricta reveals few features differing markedly from those characteristic of the various forms comprising the higher Sympetalae. The details of organogeny, microsporogenesis, megasporogenesis and embryogeny conform to type, and indicate that the Goodeniaceae find their natural position in the order Campanales. The genus Dampiera despite its being endemic to Australia does not show any signal aberrant features, such as was laid bare by an examination of another great Australian family, namely the Epacridaceae, a member of which, Styphelia longifolia (Brough, 1923, 1924), showed unique characters more especially in megasporogenesis. Reverting to Dampiera it is interesting to observe the syngenesious anthers— a feature so characteristic of the Campanales. The piston-like action of the style is also typical, but Dampiera with its protandry, pollen cup, delicate anther dehiscence, method of dispersing the pollen, and the very late exposure of receptive stigmatic cells is perhaps the most outstanding in an Order noted for its highly developed pollinating mechanisms. The genus would seem to present an epitome of the many peculiarities portrayed by the various members of the most recent and specialized of all the Orders of flowering plants. On looking for genetic relationships between the Goodeniaceae and the other members of the Order Campanales certain striking features already noted in Dampiera are seen to be reflected in the tribe Lobelioideae of the Campanulaceae. In this tribe one finds the herbaceous habit, the zygomorphic flowers, the blue corolla often split to the base, the syngenesious anthers, the piston-action of the style, and the nutritive jacket around the embryo sac. The genus Lobelia is represented by eighteen species in Australia (Bentham and Hooker), and the writer has come to the conclusion that all the available evidence goes to show that the genus Dampiera—if not the Goodeniaceae as a whole—has been derived from the Lobelioideae. Summary. Organogeny. The primordia of the various sets of floral organs arise separately and in acropetal succession. The five young sepals eventually fuse, and form a gamosepalous calyx joined to the ovary. The five petal primordia maintain their identity until an advanced stage of bud development has been attained, when the three abaxial segments fuse to form the lower lip, while the two remaining adaxial segments form the upper lip which is split almost to the base. The two lips are separate throughout. The stamens retain their identity until about the microspore mother cell stage, when the syngenesious condition arises by fusion of contiguous cuticles of the anthers. The two young carpels fuse to form a common style and inferior ovary. The characteristic pollen cup arises during late bud development by the relatively slow rate of growth at the organic apex of the style, and the increased merismatic activity in the marginal region. Microsporangium. The archesporial cells divide by periclinal walls giving rise to a primary parietal layer and a primary sporogenous layer. The cells of the former divide once thereby producing a wall layer and the tapetum. The cells of the primary sporogenous layer divide two or three times before attaining the spore mother cell stage. K 496 STUDIES IN THE GOODENIACEAE, 1, The spore mother cells undergo reduction division and then ordinary somatic - division, whereby simultaneous pollen tetrads are produced. The great rapidity in growth is attested by the wide range in development depicted in the longitudinal section of a single sporangium. In the mature pollen sac the spores are binucleate, each spore wall bears four equidistant thin areas, the hypodermal cells constitute the fibrous layer, and dehiscence is effected by longitudinal splitting along two median vertical contingent rows of unthickened cells of the hypodermal layer. The mature stamens are short, and are never exposed outside the flower. The male gametophyte. The mature tetrahedral pollen grain contains a generative and a vegetative nucleus. During germination a single pollen tube grows out through one of the four unthickened areas of the mature microspore. Evidence testifying to the rapidity in growth of the pollen tube was obtained by careful observation of its development in a five per cent. sugar solution. Pollen tubes were traced from the receptive cells of the stigma, throughout the style, and in the ovary from the base of the style to the micropyle. The tube grows through the micropyle, and enters the embryo sac in the region of the egg apparatus. The megasporangium. A solitary nucellus arises within the ovary. A single thick integument gradually encloses the young megasporangium, which consists of an axial row of cells surrounded by a jacket one cell thick. The anatropous nature of the ovule is early foreshadowed. The megaspore mother cell is formed at the micropylar end of the axial row of the megasporangium. The mother cell gives rise to a linear tetrad of megaspores, the innermost of which is the functional megaspore; this develops rapidly and absorbs the other three megaspores. The wall cells of the megasporangium are also absorbed. Meantime the cells of the integument lining the micropyle enlarge, become densely cyto- plasmic, and eventually form a very definite and noteworthy nutritive jacket around the embryo sac. The female gametophyte. The functional megaspore increases in size, and steadily invades the micropyle. During this development, the bi-nucleate, four- nucleate, and eight-nucleate stages of the female gametophyte are attained. The egg apparatus, polar nuclei, and antipodal cells are normal in structure and polarity. These are described in detail. Fertilization. The pollen tube enters the embryo sac. One male nucleus fertilizes the oosphere, while the other joins the partially fused polar nuclei. Endosperm formation. The endosperm nucleus divides before that of the oospore—free endosperm nuciei being formed. Wall formation, accompanied by rapid growth of the embryo sac then supervenes. A massive endosperm is formed. Embryogeny. The oospore commences development soon after wall formation in the endosperm has been initiated. A long suspensor is formed which pushes the terminal cell well down into the soft endosperm tissue. The embryonal cell attains the quadrant and octant stages respectively. Later periclinal walls cut off the dermatogen, and in the final stages examined, the periblem and plerome had been differentiated. Pollination. Many investigators, for example R. Brown, H. Mueller, E. Haviland, F. E. Haviland, and A. G. Hamilton, have carried out investigations regarding the methods of pollination in members of the Goodeniaceae. Conflicting views have been expressed. In the case of Dampiera stricta the elongating style carries the pollen cup up through the syngenesious mature anthers causing BY P. BROUGH. 497 introrse dehiscence of the microsporangia, and the filling of the cup with pollen grains. The style further elongates and thrusts the cup into a pouch in the line of junction of the two adaxial segments of the corolla. The cup is orientated so as to face the centre of the corolla. The stigma then arises from the base of the pollen cup, and very gradually forces the microspores out through the pore at the apex. Such microspores are then in a suitable position for removal on the backs of visiting insects. Eventually the fully developed and slightly bi-lobed stigma occupies the whole of the interior of the cup. Then, and not till then, do receptive cells appear in the apical region of the stigma, which is now ready to receive pollen from insect visitors coming from less mature flowers. A very exact mechanism to ensure cross pollination is thus demonstrated. It would seem, however, that self pollination is possible in the absence of insect visitors. The evidence derived from this investigation strongly supports the view that the genus Dampiera is derived from the Lobelioideae. List of References. BALIKA-IWANOWSKA, G. P., 1899.—Contribution & l’étude du sac embryonnaire chez certaines Gamopetals. Flora, 86, pp. 47-71, pls. 3-10. BarRNEs, C. R., 1885.—The Process of Fertilization in Campanula americana. Bot. Gazette 10, pp. 349-354, pl. 10. BENTHAM AND HooKeEr, 1869.—Flora Australiensis. Biuuines, F. H., 1901.—Beitr’ige zur Kenntniss der Sammenentwicklung. Flora 88, pp. 253-318. BrouGH, P., 1923.—Preliminary note on the Embryo Sac of Styphelia longifolia. Proc. Linn. Soc. N.S.W., xlviii, pp. 674-680. , 1924.—Studies in the Epacridaceae. i. The Life-history of Styphelia longifolia. Proc. Linn. Soc. N.S.W., xlix, pp. 162-178. Brown, R., 1818.—Queries respecting the Indusium of Brunonia and Goodeniaceae. Trans. Linn. Soc., xii, p. 134. , 1866.—Miscellaneous botanical notes, Vol. i, p. 31. CHAMBERLAIN, C. J., 1895.—The Embryo-sac of Aster novae-anglicae. Bot. Gazette 20, pp. 205-212, pls. 15-16. CHODAT, R., AND BERNARD, C., 1900.—Sur le sac embryonnaire de lVHelosis guayanensis. Jour. Botanique 14, pp. 72-79, pls. 1-2. CouLTerR, J. M., AND CHAMBERLAIN, C. J., 1915.—Morphology of Angiosperms, p. 1038. ENGLER AND PRANTL, 1889.—Die Naturlichen Pflanzenfamilien. HAMILTON, A. G., 1885.—On the Fertilization of Goodenia hederacea. Proc. LINN. Soc. N.S.W., x, pp. 157-160. , 1894.—Notes on the Methods of Fertilization of the Goodeniaceae. Proc. LINN. Soc. N.S.W., xix, p. 201-212. HAVILAND, E., 1884.—Occasional notes on Plants indigenous in the immediate Neighbour- hood of Sydney. Proc. LINN. Soc. N.S.W., ix, pp. 449-452. , 1885.—Some remarks on the Fertilization of the Genus Goodenia. Proc, LINN. Soc. N.S.W., xX, pp. 237-240. HAVILAND, F. E., 1914.—The Pollination of Goodenia cycloptera. Proc. LINN. Soc. N.S.W., xxxix, pp. 851-854. Luoyrp, F. E., 1902.—The Comparative Embryology of the Rubiaceae. Mem. Torr. Bot. Club, 8, pp. 27-112. MUELLER, H., 1883.—The Fertilization of Flowers. Wiis, J. C., 1919.—Flowering Plants and Ferns. Index Kewensis. EXPLANATION OF PLATES XXXVI-XXXVII. Plate xxxvi. 1. General habit of Dampiera stricta; about one-third natural size 2. Flowers of D. stricta; about one and a half times natural size. 498 STUDIES IN THE GOODENIACEAE, 1. Plate xxxvii. Style supporting pollen cup with narrow orifice through which microspores are being gradually ejected. 4. A style slightly more advanced than that of previous figure. The pollen cup is now at right angles to main style. The gradual ejection of microspores from the pollen cup is illustrated. 5. View showing the short stamens arranged around the style. The anthers have separated, and dehiscence has occurred. (Je) 6. Microspores germinating. x 100 (approx.). PLACENTATION AND OTHER PHENOMENA IN THE SCINCID LIZARD LYGOSOMA (HINULIA) QUOYI. By H. CriarreE WEEKES, B.Sc., Linnean Macleay Fellow of the Society in Zoology. (From the Department of Zoology, University of Sydney.) (Plates’ xxxviii-xl and twenty-three Text-figures. ) [Read 26th October, 1927.] Contents. IT. Introduction. II. Material and Methods. III. Description of Material. 1. Period of ‘‘pro-oestrus”’. 2. Period of ovulation and fertilization. 3. Period of placental activity. Stage A. Early development of the placentae. Stage B. The stage of placental maturity. Stage C. The placentae immediately prior to the birth of the foetus. 4. Period after birth. IV. Comparison with the lizards, Chalcides tridactylus, Lygosoma (Liolepisma), entrecasteauaxi and Tiliqua scincoides and with the marsupial, Perameles. V. Theoretical Considerations. VI. Summary and Conelusions. I. INTRODUCTION. In a “Note on Reproductive Phenomena in some Lizards’ communicated to this Society in May, 1927, the placentation of the Scincid lizard Lygosoma (Hinulia) quoyi was described briefly and compared and contrasted with that of the Scincid lizards Chalcides tridactylus, Lygosoma (Liolepisma) entrecasteauxi and Tiliqua scincoides and with that of the marsupial Perameles. It is proposed to describe the placentation of L. quoyi and to discuss its relationship with that of the three above-mentioned Scincid lizards and of the marsupial Perameles in more detail in this communication. In a previous paper (Harrison and Weekes, 1925) in which the occurrence of the placentation of the Scincid lizard L. entrecasteauxri was described, L. quoyi was mentioned, specimens of both having been collected at Barrington Tops during January and February, 1925, by the members of a party from the University of Sydney, under the leadership of Professor Harrison. In this paper (p. 471) it was stated that examination of pregnant females of Trachysaurus rugosus, T. scincoides, L. quoyi, Egernia striolata and EH. whitei revealed “highly vascularized external allantoic and uterine walls with their respective circulations in close apposition but no marked placental area such as is described below” (for L. entrecasteauw-ri). A study of the condition in L. quoyi has shown that there is a very definite type of allantoplacenta present, although there is not the same degree of external differentiation of the uterine placental area. A further study has shown that a L 500 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, somewhat similar placental condition occurs in #. striolata and H. whitei and probably also in 7. rugosus. Definite placentation among lizards has now been recorded in Chalcides tridactylus and C. ocellatus by Giacomini (1898) and (1906) respectively; in Tiliqua scincoides by Flynn (1923); in Lygosoma (Liolepisma) entrecasteauxi by Harrison and Weekes (1925); in Lygosoma (Hinulia) quoyi, Egernia striolata and E. whitei by Weekes (1927); and omphaloplacentation in 7’. scincoides by Weekes (1927). In addition Haacke (1885) mentions certain relations between the wall of the uterus and that of the yolk-sac in Trachysaurus rugosus. It is probable that a further investigation of the viviparous reptiles will reveal BEY interesting phenomena with regard to placentation. I wish to thank Professor L. Harrison, in whose department this investization was carried out, for the personal interest he has taken in the work and for the help he has given; Dr. I. M. Mackerras for specimens of L. quoyi collected at Barrington Tops; Mr. J. Hopson for collecting and forwarding material; Miss L. Wood, Mr. W. Graham, Mr. G. Vance and Miss B. White for help in collecting material; the Department of Zoology, University of Sydney, for grants covering the cost of collecting. This investigation was begun under a Science Research Scholarship of the University of Sydney, and continued after my appointment as a Linnean Macleay Fellow of this Society. II. MATERIAL AND METHODS. Specimens of L. quoyi containing young were collected from Barrington Tops, 150 miles north of Sydney, at a height of 4,500-5,000 feet, during January, February and December, 1925; from Mount Kosciusko, 300 miles south of Sydney, at a height of approximately 5,000 feet, during November and December, 1925; from the Biue Mountains, 70 miles west of Sydney, at a height of approximately 3,000 feet, during January and February, 1927; from Sydney, at sea level, during November and December, 1925, and September, October, November, December, 1926, and January, 1927; from Kiama, on the Coast, 70 miles south of Sydney, ayes January, October and November, 1926. The study of L. quoyi is interesting apart from the factor of plaventations The specimens collected from Barrington Tops and Mount Kosciusko, at a height of approximately 5,000 feet, differ from those collected at sea level, although each type has been identified as Lygosoma (Hinulia) quoyi. Those collected at Barrington Tops and Mount Kosciusko have an average length of five inches and the pregnant females contain from three to five young; those from the coast are much larger measuring from ten to thirteen inches and the pregnant females contain from five to nine young. The difference in scale marking between the two types of lizard is slight, since members of the same type vary among them- selves, and the placentae in both are identical. The difference in the number of young carried during the gestation period seems to depend on the size of the parent lizard, although this conclusion may not be correct, since the increase in the size of the adult is naturally followed by a corresponding increase in the size of the embryo, those of the mountain type measuring approximately 3 cm. at the time of birth, and those of the coastal type measuring approximately 5 cm. Those females collected at the Blue Mountains, at 3,000 feet, were intermediate in size between the two above described types measuring on an average eight inches in length and containing frqm three to five young. BY H. CLAIRE WEEKES. 501 The reason for the difference in the size of the mountain and coastal types of lizard is not apparent, but in January, 1927, an intermediate type was collected at a height of 3,000 feet indicating that altitude may be the determining factor, and that the change from the small to the large type of lizard may be gradual as the altitude decreases. L. quoyi is essentially a water loving animal and always lives near a creek or water hole. The flat marshy land at Barrington Tops and Mount Kosciusko with its network of small watercourses is infested with them. They live in holes in the banks of the watercourses, and at the coast they live in similar holes in the banks of coastal streams. As mentioned, pregnant females were collected from Mount Kosciusko during November and December, 1925, and from Barrington Tops during January and February, 1925. They were first collected from Mount Kosciusko on the !4th November and the contained embryos are estimated to be one week old, hence fertilization occurred during the first week in November. The females collected from Barrington Tops during the first week in February contained embryos which were within a few days of hatching, but since it is at present unknown to the writer whether the times of the fertilization of the ova of the lizards at Mount Kosciusko and Barrington Tops correspond, the exact length of the gestation period of the mountain type is unknown. Females of the coastal type collected at Sydney on 10th September and 7th October, 1926, had the ova still within the ovaries. On the 18th October females were collected which had the ova in early stages of segmentation within the oviducts, so that fertilization in these lizards occurred in the middle of October, which is two weeks earlier than at Mount Kosciusko. Lizards were collected from the same locality at Sydney, from the time of the fertilization of their ova until the time of the birth of the young, which was the second week in January. Hence the development of L. quoyi at sea level covers a period of approximately three months. Females were kept alive until the young were born and thus post partum stages were obtained. Summarizing the above, specimens of L. quoyi were collected at a height of 4,500-5,000 feet which contained embryos in stages of development ranging from the first week after fertilization until the time of hatching; specimens were collected at sea level at all stages ranging from the condition of non-pregnancy to the condition after birth. All material was fixed in Bles’ Solution (90 parts of 70% alcohol, 7 parts of 5% formol, and 3 parts glacial acetic acid). The ventral body wall of each female was cut longitudinally to expose the oviducts, the female with young in situ then being immersed in the fixative. It is not advisable to leave the material in ‘the fixative indefinitely as Bles’ Solution hardens yolk. As most of the material contained much yolk it was found difficult at first to get satisfactory results when infiltrating without using the method of double embedding in celloidin and paraffin, a method which has many disadvantages when dealing with yolky material. Embedding in paraffin alone was successful when the following precautions were taken: (a) to secure a thorough dehydration of the material, the latter, if bulky, being passed through many changes of absolute alcohol over a period of at least two days; (b) to use pure clearing agents, preferably xylol or cedar wood oil. As an inferior quality of xylol is usually sold which gives a white precipitate when mixed with alcohol, it is advisable to use cedar wood oil. However, if the xylol will mix with 70% alcohol without 502 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, giving a permanent precipitate, it will give better results than the cedar wood oil. Cedar wood oil which is sold as pure often contains water, but it was found that by mixing the oil with a fair quantity of anhydrous copper sulphate, shaking well and allowing to stand for twenty-four hours and then filtering, the water and other impurities were removed and the oil made perfect for use; (c) to infiltrate gradually, leaving the cleared material at room temperature in a solution of the clearing agent saturated with paraffin for about twenty-four hours, then leaving it another twenty-four hours at about 30° C., more paraffin having been added, and finally passing it through several changes of pure wax inside the paratiin bath for a few hours before embedding. If the material became brittle a shorter time in the solution of clearing agent and wax was allowed. I have successfully cut lizards’ ova § mm. in diameter when these precautions were taken. When staining,’if the yolky sections washed off the slides this was usually due to imperfect floating out of the wax ribbons on the slides, and imperfect drying of the ribbons after floating out. The floating out was most successful when done gradually and at a moderate temperature. Floating out on the top of a paraffin bath is not a perfect method as the copper bath is usually much too hot and the floating out dangerously rapid. I use a large piece of thick plate glass arranged at a suitable distance above an electric light bulb, so that the glass is just warm and the slides may be left on it for hours without damage, until they are thoroughly dry. This method of dry heating eliminates the danger of imperfect fixation due to a moist atmosphere. It was found more important to take these precautions than to use a greater quantity of egg albumen, since ribbons that are well floated out and thoroughly dried should not leave the slides even when passed into 0:5% acid alcohol. For an examination of anatomy the material was stained in bulk in carmalum. For histological work, sections were stained in Delafield’s haematoxylin and counterstained in eosin. III. DESCRIPTION OF MATERIAL. The material is described in four parts. The first part covers the period of “pro-oestrus’’, the second the period of ovulation and fertilization, the third the period of placental activity and the fourth the period after birth. The period of placental activity is divided into three stages, Stage A presenting the early develop- ment of the placentae and covering the first two weeks of the gestation period; Stage B presenting the mature placentae, and covering the following eight weeks of the gestation period; and Stage C presenting the placentae immediately prior to the birth of the foetus and covering the last two weeks of the gestation period. The description of the periods of ‘‘pro-oestrus” and of ovulation and fertiliza- tion are based on examinations of lizards collected at sea level. However it is more than probable that during these periods the condition of the reproductive organs of females inhabiting the mountain regions is the same. The descriptions of the period of placental activity and of the period after birth are based upon an examination of both types of lizard, and as the placentae of both are identical no distinction is made between them. 1. Period of “pro-oestrus’’. As mentioned above, females, which presumably had not copulated, were collected at Sydney on 10th September, 1926. The reasons for assuming that copulation had not taken place are: when collected the ova were still within BY H. CLAIRE WEEKES. 503 the ovaries and had not reached maturity, the largest ovum measuring 6 mm. in diameter, the measurement at maturity being approximately 13 mm.; also, during the beginning of September the weather is not warm enough to bring the lizards out in any number, only three being caught on 10th September after searching for two days; again, fertilization does not take place until the middle of October and one would expect copulation to occur nearer the time of fertilization than 10th September, which is five weeks earlier, and although actual copulation was not observed during the middle of October, it is extremely probable that it occurred: then, since the lizards were observed living in pairs, a male with a female, the females being easily distinguished by their greater girth due to the presence of the enlarged ovaries. The female reproductive organs consist of a right and a left ovary each equally well developed, and two oviducts which open separately into the cloaca. Each ovary is situated at the middle of the length of the corresponding oviduct. In each of the two females collected on 10th September, the right ovary was more anteriorly situated than the left, and the stomach was on the left side above the left ovary and closely pressed against it. In one female there were four large ova in each ovary, in the other there were four large ova in the right ovary and three in the left. This species of lizard has only one breeding season each year and the development of the ova is regulated accordingly, so that there is little gradation in the size of the ova at this stage, but a marked contrast between a number of small ova, all at approximately the same stage of development, to a number of larger ova, also at approximately uniform stages in development. At this stage these large ova have the same structure as that described for the developing ova of Lacerta agilis (Hett, 1924), where the follicle cells are of two varieties, some being enormously enlarged and the others comparatively small. The oviducts are pleated, twisted and flattened against the dorsal body wall of the lizard, the average length of an extended oviduct being 5 cm. The width varies considerably, from 5 mm. to 2-5 mm. owing to an indication of division into “incubatory chambers’’, which is due to the failure of the oviducts to regain completely their natural shape after the preceding year’s gestation period. Giacomini (1891) wrote that these chambers are evident in the oviducts of C. tridactylus three months after birth. In ZL. quoyi it seems that they never completely disappear. The structure of the oviducts in these females is regarded as normal and only variations from it, found in the oviducts during the period of placental activity, are considered placental modifications. In section the wall of the oviduct at this stage is more or less uniform in structure throughout its length with the exception of the extreme anterior end which is modified for the reception of the ova. The arrangement of the tissues of the oviductal wall seems uniform for lizards in general, as it occurs in every species examined by the writer as well as in C. tridactylus. The wall at the anterior end is thrown into folds, is comparatively thin and the epithelium lining the lumen of the oviduct in this region is glandular and ciliated, consisting of deep columnar cells which are much larger than those lining the rest of the lumen. The wall of the remaining part of the oviduct (Text-fig. 1) consists of the following layers: an external layer of peritoneum; a thick muscular coat consisting of an outer coat of longitudinal muscle and an inner coat of circular muscle; a thick mucous membrane in which glands are embedded and which is lined by ciliated epithelium. The glands embedded in the mucosa are simple or branched and open into the lumen by short narrow mouths. M 504 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, EY They are saccular, the cells being composed of vacuolated cytoplasm with small . oval nuclei arranged round the periphery, and the cell walls being usually indistinct. Many of the nuclei are undergoing mitosis, indicating the growth of the glands. The epithelium lining the lumen of the oviduct is composed of narrow ciliated cells, closely crowded together, with many of their nuclei also dividing. li Ve — =) FF <2 =a [-® z a ef | CIR. MUS. | LONG. MUS. Text-fig. 1. Section of the wall of the oviduct of a non-pregnant female. CAP., capillary ; CIL. UT: EPI., ciliated uterine epithelium; CIR. MUS., circular muscle; GL, gland; LONG. MUS., longitudinal muscle. x 706. The active cell division in the epithelium and glands indicates a “pro-oestrus”’ condition. The ordinary stimulus is certainly not copulation, since the ova in the females under discussion are at a stage about five weeks prior to ovulation, and it is extremely unlikely, as indicated above, that copulation has taken place. It is more likely that the stimulus is an external periodical one in which temperature is the main factor. That the breeding season of L. quoyi is influenced by climatic conditions is evident from the fact that the lizards inhabiting the warmer regions at sea level, Sydney, are at least two weeks earlier in their sexual season than those inhabiting the colder regions at Mount Kosciusko, 300 miles south of Sydney and with later seasonal changes. 2. Period of ovulation and fertilization. On the 7th October, females containing ova at a stage prior to ovulation were collected from the same locality as on the 10th September. The ova had reached their maximum size and were packed with yolk. The membranes correspond with those described by Hett (1924) for Lacerta agilis at this stage, the cells of the BY H. CLAIRE WEEKES. 505 follicular epithelium being uniform in size and much smaller and flatter than those surrounding the younger ovum described above. There is a thicker band of thecal connective tissue in which numerous large blood vessels are present. The oviducts have reached the final stage of preparation for the entrance of the ova. Each is roughly divided into three regions, namely, the anterior end described above, the more extensive middle region containing the majority of the glands, and the extreme basal region leading to the cloaca containing no glands and having its wall deeply convoluted. In section these regions differ somewhat from the corresponding regions of the oviducts of females collected four weeks earlier (10th September). At the anterior end the epithelial cells lining the lumen of the oviduct are markedly glandular and their free surfaces are covered by a thick secretion obviously derived from them and serving to facilitate the entrance of the ova. In the middle region the glands are most numerous and their cells are full of secretion and are distended until the central cavity is obliterated, thus indicating a period of glandular activity. The nature of the secretion from these glands is not apparent. At first, from the abundance of the glands and their position in the middle region of the oviduct, it was naturally supposed that they were for the secretion of albumen, but an examination showed that there is no sign of albumen surrounding the ovum after its passage into the oviduct or at any stage in its development. With the stretching of the “uterus” upon the entrance of the ova and the consequent squeezing of the glands, their secretion is forced out into the surrounding tissues of the uterus and some of it passes between the muscle layers and in stained material is identical in appearance with the substance of the shell membrane. The shell membrane is occasionally found adhering to the mouth of one of the glands when it has been torn away from the rest of the uterine wall, and a substance similar to it is present in the mouth of the gland. The cells of the epithelium lining the lumen of the oviduct in this region are also full of secretion, their cilia being matted together by the exuded secretion which is thought to be for the general purpose of lubrication. It is not definitely known to the writer whether the process of ovulation in L. quoyi depends on some physiological stimulus such as the act of copulation, or whether it is independent of such stimulus; also, whether the liberated ova pass into the body cavity and thence into the oviduct with the aid of ciliary action, or whether they pass directly into the oviduct as a result of the latter actively clasping the ovum while still in the ovary. As in other animals it is usual for the ova in each ovary to pass into the oviduct on the corresponding side, but a female was collected which had received an injury on the left side, damaging the left oviduct, so that, when ovulation took place, the mature ova, five in number, passed into the right oviduct. The liberation of ova from both ovaries was indicated by the presence of two burst follicles in the left ovary and three in the right. The five ova in the right oviduct were so tightly squeezed as to bend the oviduct completely out of position. The passage of ova across the body cavity is not uncommon among mammals, having been recorded for mammals ‘‘with a bicornuate uterus becoming pregnant in the uterine horn on the side opposite to that on which the ovary had discharged’”’ (Marshall, 1910, p. 136). When the ovum enters the oviduct and is fertilized, it becomes surrounded by a thin shell membrane which is divided into three layers composed of matted fibres. The uterus surrounds each egg as an expanded chamber called by Giacomini the “incubatory chamber”. The wall of each incubatory chamber is uniform in 506 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, thickness measuring approximately 0-025 mm. and hence being much thinner than - the wall of the uterus of a non-pregnant female. This decrease in thickness is due to the stretching of the uterus on the entrance of the eggs. Owing to this stretching, the coats of longitudinal and circular muscle are compressed into a thin band of tissue and the glands, which are swollen and saccular in the uterus of a non-pregnant female, are greatly compressed at this stage. The epithelial cells lining the mucosa are much larger and not as crowded as in the non-pregnant condition, and are of uniform size over the entire area of the incubatory chamber. There is a curious substance surrounding the ovaries after ovulation, which, in prepared sections, has the appearance of a deep blue coagulum mixed with blood clot containing corpuscles and numerous small round cells. Immediately after ovulation the ruptured follicles are visible as large white flat oval sacs, each with the cicatrix present as a median longitudinal groove. However, a few days after ovulation they become smaller, spherical, yellow and richly vascular, the alteration in the appearance of the follicles being due to the presence of a corpus luteum in each, the growth of which is rapid, each follicle being completely filled with luteal cells a few days after ovulation. It is not probable that the corpora lutea have any influence on the retention of the ova of reptiles comparable with their supposed function in mammals, since they occur in ovaries of the oviparous lizard Lacerta agilis, which lays its eggs immediately after their passage down the oviducts (Hett, 1924). 3. Period of placental activity. Stage A. Early development of the placentae. Twenty females were collected containing young embryos with placentae at early stages in development, nine at Mount Kosciusko, eight at Sydney and three at Kiama. Of the nine from Mount Kosciusko, seven contained three young, one five and the remaining one six; of the eight from,Sydney, four contained six, two seven and two eight; of the three from Kiama, one contained six, one seven and one eight. In every case where a female contained an even number of young, half were in each oviduct, and where a female contained an odd number of young the right oviduct held one more than the left. This arrangement of embryos was found to be the same in all lizards collected during the rest of the gestation period. In the paper on the placentation in L. entrecasteauxi (Harrison and Weekes, 1925, p. 472) the authors wrote that “it seems remarkable that the number should be odd in every one of nine examples, and we cannot find any explanation for this condition”, also, “of the six females examined, four had more embryos in the right oviduct than in the left’. Taking into consideration the conditions in both L. entrecasteauxi and L. quoyi, it seems that there is a tendency for the female to contain an odd number of embryos, and for the right oviduct to contain more than the left. This may be due to the fact that the stomach of the non-pregnant female is almost invariably on the left side and closely pressed against the left ovary thus possibly interfering with the number of ova developing in this ovary. The developing embryo is dorsal in position with regard to the parent and lies with its head directed mesially whether the embryo be in the right or left oviduct. The embryos in the one female are not all at identical stages of develop- ment, but the range of difference is negligible, L. quoyi resembling L. entrecasteausi and not @. tridactylus in this respect. The uterus surrounds each egg as a thick BY H. CLAIRE WEEKES. 507 white envelope which persists as the expanded incubatory chamber on the extraction of the egg. These chambers are connected each to each by a short, narrow, strap-like portion of the uterus which is deeply folded. Occasionally the uterus is pigmented, the pigment being sometimes scattered over the surface of each incubatory chamber, but usually restricted to the dorsal body wall of the parent. The uterine wall shows as a smooth, semi-transparent membrane whose uniformity is broken only by its thick opaque blood vessels, since there are no villous foldings such as occur in C. tridactylus and L. entrecasteauzi. However, when viewed through the binocular microscope the uterine wall is seen to be covered by numerous branched glands (Text-fig. 2, A and B), which are homologous with the saccular glands in the uterine wall of the non-pregnant female (described above). They are present throughout the development of the embryo and are outstanding and characteristic. The vascularization of the wall of the incubatory chamber of L. quoyi is on the same plan as that of L. entrecasteauzi. A single large artery and vein run longitudinally along the dorsal wall of each uterus, the artery giving off branches which pass transversely round the uterus to the base of the yolk-sac of the contained blastocyst, where they break up into a rich network of capillaries, and the vein receiving branches which also pass round the incubatory chamber from the base of the yolk-sac, parallel to and roughly alternating with the arteries (Text-fig. 2B). The villous folds in the wall of the uterus of L. entrecasteauzi are fed by short branches from the main artery and vein and by branches from the branch arteries and veins. In L. quoyi the allantoplacental region is similarly vascularized. In the early stages of development the uterus fits closely round the contained embryos and keeps them in a fairly steady position, but with the preparation for allantoplacentation a more perfect state of fixation results when the cells of the chorion attach themselves to the epithelium of the uterus. However, before this occurs the intervening shell membrane must disappear and in early stages of development the chorionic cells appear to attack and absorb it. When the allanto- placenta is mature there are often areas where a thin remnant of membrane can be detected between the uterus and the modified chorion. The expansion of the growing embryo aids the chorionic cells in their destruction of the shell membrane by causing it to break and gradually fall away from the sides of the embryo taking up a position at the base of the yolk-sac in the form of a flat fibrous pad. This may be the “nodule” which occurs at the base of the yolk-sac of the embryos of C. tridactylus, and which Giacomini (1891) terms the vitelline membrane. In L. quoyi the vitelline membrane is delicate and almost imperceptible and could not possibly be confused with the shell membrane. Of the two placentae the omphaloplacenta is the first formed, since its requisites from the embryo, namely the chorionic ectoderm and a vascularized yolk-sac, are formed early in development, whereas the allantoplacenta, depending as it does on the presence of an allantois of sufficient extent to lie immediately under the chorion, is comparatively late in its development. The Omphaloplacenta. The embryos which show the earliest signs of omphaloplacental modification are approximately one week old (Text-fig. 3, A), their average length being 5 mm. Each has turned on to its left side, its head being flexed and its body slightly curved. The amnion is completed and the allantois present as a small swelling at the posterior end of the embryo. There 508 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, are three gill slits and approximately thirty somites. The chorionic ectoderm completely surrounds the blastocyst and the extra-embryonic mesoderm extends over a small area at the surface of the yolk-sac, which is entirely lined by endoderm. Although there are indications of foetal omphaloplacentation at this stage, the uterine wall is as yet unmodified. In all earlier stages the development of the extra-embryonic tissues is normal, the chorionic ectoderm cells being small and in all respects resembling those in the chorion of oviparous lizards, but at this stage the chorionic ectoderm at the base of the yolk-sac is slightly modified with the beginning of omphaloplacentation and the further growth of the extra- Text-fig. 2A. Incubatory chamber cut in half horizontally. Dorsal view of ventral half showing the termination of the uterine arteries and veins in the region of the base of the yolk-sac of the contained blastocyst, x 7:5; GL., gland; UT. ART., uterine artery; UT. V., uterine vein. embryonic mesoderm is abnormal. In the former case, a few of the cells of the chorionic ectoderm at the lower pole multiply and become enlarged until a small area of enlarged cells is formed (Text-fig. 3B and 4). Occasionally there is more than one centre of modification, but each is small and they gradually join together to form a single area. As the development of the embryo proceeds and the omphaloplacenta approaches maturity, the modification BY H. CLAIRE WEEKES. 509 of the chorionic ectoderm spreads over the entire under surface of the yolk-sac, until a continuous sheet of moderately large columnar cells is formed. In the embryos selected for description the area of modified ectoderm measures approximately 0-8 mm. in diameter by 0-1 mm. in height, being thickest at the centre (Text-fig. 4). It consists of a mass of deeply staining cytoplasm containing irregularly arranged nuclei, there being no definite cell boundaries present, even at the edge of the area where it merges into the unmodified chorionic ectoderm which covers the rest of the yolk-sac. The yolk-sac endoderm immediately overlies and mingles with the modified ectoderm and consists of a similarly staining cytoplasm with scattered nuclei. The cytoplasm of the ectoderm is denser than that of the Text-fig. 2B. Ventral view of dorsal half showing the main uterine artery and vein, x 7:5. BR. GL., branched gland; M. UT. ART., main uterine artery; M. UT. V., main uterine vein. endoderm, which is vacuolated and has the appearance of having been mixed with a fluid which coagulated during the process of fixation (Text-fig. 4), and hence the line of junction between the two cytoplasmic regions is evident. The nuclei embedded in the ectodermal cytoplasm are large and irregular in shape, with no outstanding characteristics, and are easily distinguished from the endodermal nuclei, which are larger when healthy but which are mostly degenerating, many PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, VIT.VES. VS.END, BS AR.MOD OMP== Text-fig. 3. A, embryo approximately one week old, x 21:5; B, transverse section of blastocyst containing an embryo about one week old, showing the position of the area first modified for omphaloplacentation, x 11; AR. MOD. OMP., area modified for omphaloplacentation; CH., chorion; EX. COEL., extra- embryonic coelome; VIT. VES., vitelline vessel; Y.S., yolk-sac; Y. S. END., yolk-sac endoderm. BY H. CLAIRE WEEKES. 511 having been reduced to scattered groups of granules. The shell membrane under- lies the chorionic ectoderm and between them is a gap which is partly filled with a coagulum stained deeply by haematoxylin, and thought to be maternal secretion passed through the shell membrane. It is possibly the presence of this secretion in the protoplasm of the yolk-sac endoderm which gives the latter its peculiar appearance. The uterine wall is pressed closely against the shell membrane and, as stated, shows no indication of placental modification. In embryos taken from a female collected during the second week of pregnancy, the chorionic ectoderm cells are modified over a considerable area of the yolk-sac, but the original centre of modification is evident at the middle of the base of the yolk-sac where the cells are especially large and where the plug of endodermal cytoplasm is still present (Text-fig. 5, A; Pl. xxxviii, fig. 1). Some of the chorionic ectoderm cells are enlarged more than others, but are only about one- third the height they eventually attain. They are narrow but definite, with their free surfaces rounded and often bulging into peculiar shapes (Text-fig. 5, A, CH. ECT.; Pl. xxxviii, fig. 1). The nuclei vary in size sometimes almost filling the cell and they are arranged at the cell bases, staining deeply and standing out from the rest of the cell cytoplasm. The cells are closely attached to an underlying layer of yolk-sac endoderm, the cells of which are smaller than the ectoderm cells and lie at the bases of the latter with the appearance of dovetailing. They are so closely attached to the ectoderm cells that, when the layer of ectoderm is torn away SH.MEMB CH.ECT. COAG UT.EPI- ¥S.END. DEG.NUC. Text-fig. 4. Section of the omphaloplacental region, Stage A, showing the area of modified tissue, x 511. CH. ECT., chorionic ectoderm; COAG., coagulum ; DEG. NUC., degenerating nucleus; SH. MEMB., shell membrane; UT. EPI., uterine epithelium; Y. S. END., yolk-sac endoderm. N 512 PLACENTATION IN LYGOSOMA (HINULIA) QUOYI, from the overlying yolk-sac in the preparation of material for sectioning, the endoderm cells come away with it. The structure of the mass of endodermal cytoplasm at the approximate middle of the base of the yolk-sac is unchanged. DEG. NUG. = a =e eee Et ke —— Sa en SS ( EE CPUC SS GD o7 >»? ASH eee) Ce WEE. SMa TAs Nelbnes ~ CI yyy Text-fig. 5.