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Se ~= 6 °a hoes <9 ee ee er eres eee ee Sree oon ee eee Coe oe ee eee Pr eee eer ee a a YY EE VG Ee TEU RTE RA TET RPE TRACER G&G) c> === | A AE =F aN = IN mi NANA £3 Ws NW +) i] Z NY \ IVA YN) WW ANEW 77 71S = 7 aN= 7 fe. AN YS } ANG 4 P "= FAN ‘p=! %, *, IW : : 7 7 Weng @ la B = —=s iss! | | fl Ss DSal| | 0 ccc ce ene cr ncn ne rr re nn rn ne creer rrr q a IN | 7] iN en we ee ere ne et te ee ee mew ere ee ee me ee Some me oe —> Ss | DIANA AAA == Ff, =Y SVAN CHRISTMAS !SLAND A Bit of Phosphate Rock from a Dredge’s | Gatherings Revealed Its Secret and Its _ Mines 6f Phosphate [From the New York Sun] | ‘Christmas Island ‘is a® speck of land. Shaped like a dumbbell, rising steeply from the Indian Ocean 190 miles south of Java. _No one is known ever to have landed on ii previous to 1887. It was thought of only as 8 little rock, without good anchorage, not worth examining while large regions were still white on the maps. Bilt today some fifty men are living on _Christmas Island, and now and then we see the increasing quantity of phosphate that it is shipping Last year, for example, as we are told by one of these authorities, the island shipped 71,757 tons of phosphate, and new methods of loading vessels were introduced, something like those by which iron ore is poured into the holds of Lake Superior steamers. The phosphate is tipped from a high pier into the ship. The last vessel to sail loaded in a day with 1800 tons, It was a deep sea research that pointed to Christmas Island as a source of wealth, @ paragraph in the trade journals telling of - 'and the real facts in the case have only | . recently been told. _ About ten years ago a British naval ves- sel started for the Indian Ocean to ex- amine a part of its sea floor. Its main work was a long distance from Christmas | Island, but Sir John Murray, Scottish oceanographer, in mapping out the great the project, ‘happened to think of an area : around Christmas Island where no that the vessel diverge from its course to make soundings and collect samples from Christmas Island. . The work was thoroughly done, and in due time a list of soundings and specimens of the mud and bits of rock dredged from the bottom were delivered at Sir John’s 1a9- oratory near Edinburgh. In the collection was a fragment of rock which he could not identify on casual inspection, and it excited his curiosity. He made an analysis of the fragment and found that it was phosphate. There could be little doubt that it came from some land mass; but where was its place of origin? It was far from any land of important size, and Christmas Island was the only land anywhere near it. Could it have been dropped from a passing vessel; or was it really a part of the rock that built up Christmas Island? ‘The problem was worth investigating. . = ————— ————————— the ocean bed in the neighborhood of: in- | vestigations had been made. He suggested | | | | | | ‘might be loaded easily and cheaply. L PS fs 4 OWLUH OV Lie cg It was not long before another vessel on a scientific mission was sent to the Indian Ocean, and at the request of Sir John Mur- ray she was ordered to stop at Christmas Island and collect specimens illustrating its geology for every twenty feet of altitude from sea level to the summit of the isiard. The specimens were to be sent to him for | his examination. The results fulfilled the most sanguine expectations of the man of science. There was no longer any doubt of the existence of a thick bed of phosphate on the island. But to ascertain all the conditions and the prospects of mining with profit Sir John made a journey to it. He found that the mineral offered a promising, commer- cial possibility; that there was good anch- orage on one side of the island, and that by building a wharf with a second story, on which trucks could be run out, vessels A company was organized, with the necessary capital, Parliament made a con- cession, giving the company the right to work the phosphate for a series of years, and development was begun. \ It has been @ most profitable venture, and the best of it is that it has placed Sir John Murray, who, like most scientific men. had no a ae superfluity of this world’s goods, in very | comfortable circumstances for the rest of his life. = . a. or i. ovis gu Aart A MONOGRAPH OF CHRISTMAS ISLAND. Moll. A MONOGRAPH CHRISTMAS ISLAND (INDIAN OCEAN): PHYSICAL FEATURES AND GEOLOGY BY CHARLES W. ANDREWS, B.A., B.Sc., F.GS. WITH DESCRIPTIONS OF Division ot Mollusks THE FAUNA AND FLORA ceotiono! Librory NUMEROUS CONTRIBUTORS. ILLUSTRATED BY TWENTY-TWO PLATES, A MAP, AND NUMEROUS ILLUSTRATIONS IN THE TEXT. EON EON: PRINTED BY ORDER OF THE TRUSTEES. SOLD BY LONGMANS AND CO., 39, PATERNOSTER ROW. B. QUARITCH, 15, PICCADILLY. DULAU AND ©CO., 37, SOHO SQUARE, W- KEGAN PAUL AND CO., CHARING CROSS ROAD, W.C. AND AT THE BRITISH MUSEUM (NATURAL HISTORY), CROMWELL ROAD, S.W. (All rights reserved.) SMITHSON AS 1900. MAY 0 3 1988 “iBRARIES iy, Pee fa -s tia ‘ iad | ‘ HERTFORD PRINTED BY STEPHEN AUSTIN AND SONS. PREFACE. THe ‘Trustees having been pleased to authorize the preparation of a monograph embracing the scientific results of the exploration of Christmas Island by Mr. C. W. Andrews during a visit extending over ten months in 1897-98, I was requested by the Director to make the necessary arrangements, and obtain the assistance of the several members of the staff of the Natural History Departments in the British Museum and other gentlemen (whose names will be found in this work), without whose kind co-operation Mr. Andrews’ task would have been an impossible one. The valuable help of various special artists had also to be secured to illustrate the work, and within rather over a year from the time of inception the volume has been completed. By Professor Lankester’s desire, this monograph has been restricted to a description of the Physical Features and the Geology, together with the Land Fauna and Flora of the island. ‘ Trustees, by the staff of the Museum, dealing with s r >, geographical units hitherto neglected. K Y HENRY WOODWAR al 3 GEOLOGICAL DEPARTMENT, | British Musrum (Natural History). February, 1900. AUTHORS PREFACE. THE present volume contains an account of the collections and observations made by me during a stay of about ten months in Christmas Island. This period included all the seasonal changes, and it is hoped that the collections of plants and insects are fairly complete. In a few instances specimens obtained by previous collectors are described. The collections of marine animals are discussed elsewhere. I wish especially to express my sincere thanks to the Trustees of the British Museum, who granted me the necessary leave of absence, which, owing to the difficulty of reaching the island and the still greater difficulty of getting away, was prolonged considerably beyond the time that was at first thought necessary ; to Sir John Murray, whose generosity in defraying the necessary expenses rendered the expedition possible; to Mr. George Clunies Ross, of Cocos-Keeling islands, and his brother, Mr. Andrew Ross, for their hospitality, and assistance in numberless ways during my stay; to their nephew, Mr. H. Ross, a resident for some years on the island, whose knowledge of bush- life in general was of the greatest assistance to me; Vill AUTHOR'S PREFACE. and lastly, to Mr. W. A. Wilkinson, the Engineer to the Christmas Island Phosphate Company. I am also greatly indebted to the contributors of the various sections of this book for the trouble and care they have taken in working out the collections I was able to send home. CHAS. W. ANDREWS. GEOLOGICAL DEPARTMENT, British Musrum (Natura. History). February, 1900. INTRODUCTORY NOTE. Curistmas Istanp, in the Indian Ocean, appears to have been known to navigators from about the middle of the seventeenth century. Dampier and other voyagers sent boats ashore, but, until the year 1887, no person appears to have been able to penetrate beyond a few hundred yards from the landing-places, because of the steep and rugged cliffs, covered with dense tropical vegetation, by which the island is everywhere surrounded. In 1887 Captain (now Rear-Admiral) Pelham Aldrich, R.N., visited the island in H.M.S. ‘“ Egeria,’? and with the assistance of a party of blue-jackets cut a way up the cliffs, encamped on the highest point of the island, and made some explorations towards the interior. In consequence of Captain Aldrich’s discoveries during: this expedition, the island was formally annexed to the British Crown in the following year. In the year 1897 a Company acquired the lease of the island, and arrangements were immediately made for its thorough exploitation ;—an agricultural rent is paid to the Government, in addition to royalties on all minerals and timber that may be exported. The total area of the island is about 43 square miles, and in some parts it rises to over 1,000 feet above the level of the sea. Besides being the home of numerous endemic and other species. of animals, it is completely covered by a luxuriant tropical vegetation. Down to a few years ago it was probably the only existing tropical island of any large extent that had never been inhabited by man, savage or civilized. Its interest, from a scientific - point of view, is further increased by the fact that it is at least 190 miles distant from any other land, and is surrounded by an ocean in which the depths exceed three English miles. x INTRODUCTORY NOTE. It seemed highly desirable that this interesting island—which was evidently an upraised coral atoll—should be carefully examined and described by a competent naturalist and geologist, before being opened up by Europeans for agricultural and commercial purposes. Accordingly it was arranged with the Trustees of the British Museum that Mr. C. W. Andrews, B.Sc., F.G.S., of the Geological Department, should be granted leave to carry out this exploration. I undertook to pay all the expenses, and to present a complete set of all specimens procured to the National Collection. During the years 1897 and 1898 Mr. Andrews carried out the exploration with great success, notwithstanding many disappoint- ments, drawbacks, and hardships. He has enriched the British Museum with unique and extensive collections, and it will, I think, be admitted that in the present elaborate report we have the best account of a true oceanic island that has ever been published. It has not hitherto been possible to watch carefully the immediate effects produced by the immigration of civilized man —and the animals and piants which follow in his wake—upon the physical conditions and upon the indigenous fauna and flora of an isolated oceanic island. I hope to arrange that this shall be done in the case of Christmas Island, at the same time that further explorations are undertaken, for Mr. Andrews’. detailed report will enable this to be carried out with every prospect of success, and in a scientific manner. Mr. Andrews, and the other officials of the British Museum who have assisted him in his investigations, are to be congratulated on the production of this excellent monograph of an oceanic island, which forms a most valuable addition to natural knowledge. JOHN MURRAY. CuHatLeNceR Loner, Waxvir, EDINBURGH. february 15, 1900. TABLE OF CONTENTS. Preface, by Dr. H. Woodward, F.R.S., F.G.S. Author’s Preface Introductory Note by Sir John tae K-C:8.. FR:S: Contents List of Figures in the text History and Physical Features, by C. W. Apes B. Se BGS. ZOOLOGY. Mammalia, by C. W. Andrews, B.Sc., F.G.S. Notes on the Osteology of Mus nativitatis and Mus macleart, by Dr. C. I. Forsyth Major, F.Z.8. Aves, by R. Bowdler Sharpe, LL.D., F.L.S. Reptilia, by G. A. Boulenger, F.R.S. Mollusca, by E. A. Smith, F.Z.S. Lepidoptera Rhopalocera, by A. G. Butler, Ph.D., F.L.S., ete. Lepidoptera Phalene, by Sir George F. Hampson, Bart. Micro-Lepidoptera, by the Rt. Hon. Lord Walsingham, M.A., iD:.* EOR.S., ete. Hymenoptera, by W. F. Kirby, F.L.S., F.E.S. Diptera Coleoptera, by C. O. Waterhouse, F.E.S., C. J. Gahan, M.A., F.E.S., and G. J. Arrow, F.E.S. . Xl CONTENTS. Hemiptera, by W. F. Kirby, F.L.S., F.E.S. Homoptera, by W. F. Kirby, F.L.S., F.E.S. Mallophaga, by W. F. Kirby, F.L.S., F.E.S. Neuroptera, by W. F. Kirby, F.L.S., F.E.S. Orthoptera, by W. F. Kirby, F.L.S., F.E.S. Chilopoda, Diplopoda, and Arachnida, by R. I. Pocock Land Crustacea, by C. W. Andrews Vermes (Earth-worms), by Daniel Rosa, D.Sc. BOTANY. Dicotyledons : 3 Polypetale, by E. G. Baker, F.L.S. Gamopetale, by E. G. Baker, F.L.S. Apetale, by A. B. Rendle, M.A., D.Sc. Monocotyledons, by A. B. Rendle, M.A., D.Sc. Gymnosperms, by A. B. Rendle, M.A., D.Sc. Ferns, by A. Gepp, M.A., F.L.S. Mosses, by A. Gepp, M.A., F.L.S. Lichens, by V. H. Blackman, M.A., F.L.S. Fungi, by V. H. Blackman, M.A., F.L.S. Mycetozoa, by A. Lister, F.R.S. . PALZAONTOLOGY AND GEOLOGY. Fossil Mollusca from the Reef Limestones of Christmas Island, by R. B. Newton, F.G.S. Fossil Corals of Christmas Island, be J. We Faas D.Se., PAGS. On the Foraminifera of the Orbitoidal Limestones and Reef Rocks of Christmas Island, by Prof. T. Rupert Jones, F.R.S., ete., and Frederick Chapman, A.L.S., F.R.M.S., etc. PAGE 127 130 138 139 141 153 163 166 200. 201 206 226 CONTENTS. Note on the Composition of some Dolomitic and other Lime- stones from Christmas Island, by E. W. Skeats, B.Sc., F.G.5: 4 Geology, by C. W. Andrews, B.Sc., F.G.S. Note on the Geographical Relations of the Fauna and Flora of Christmas Island, by C. W. Andrews List of Species recorded from Christmas Island List of the Principal Papers relating to Christmas Island Appendix Index . F ; : Plates I-X XI, with explanations and Map, at the end of the volume. Explanation of Plates. ERRATA. p- 61, line 6, for P. sepulchralis read V. sepulchralis. p. 88, line 5 from bottom, for Syrpinde read Syrphide. Xi PAGE 265 269 299 305 318 319 321 p. 142, third genus under ‘Brarrip#,’ for Perrplanata read Periplaneta. mipr OF FIGURES IN THE TEXT. PAGE Outlines of Christmas Island as seen from the sea . . . . 4 Reef-edge at low-water, south side of Flying Fish Cove . . i North coast, looking towards Smith Point. . .... . ri Sections across the edge of the central platean . . . . . 12 Meman-West Point fromthe north .°. . .. =... . # +4165 Seep comtiromthe north . . . .... Meare 5) Skull and mandible of Pteropus natalis, showing dona Waturalisize.: . . 3 a Sav ere eke Go Antebrachium and carpus of Mus slot and Mus nativitatis. 34 Poniodrilus ephippiger ; prostateand sperm-sac . . . . . 166 Pericheta brevis; sperm-sacand spermatheca. . . . . . 168 Leptoria phrygia; part of transverse section, X 5. . . . Qi11 Orbicella herklotsi ry a Sita. ere OLS Orbicella quadrangularis, var. columnata ; any of transverse BeeoOHy SOLE bt ks SRE Aner feat rem R I Prionastrea magnifica; part of ears Be section, 392° o))) BRO Porites, aff. lutea ¥ : SS a aie 2207 Porites belli i - Os th 225 Porites belli; part of transverse section bored by an alga, X 9 223 Montipora dane ; part of transverse section, X 12. . . . 224 Forest on central plateau . . . 270 Sections showing the structure of the lift at Biyine Fish Gave... nie 272 Bed of basalt aan on iT oes Testing es smith ae of Flying Fish Cove .“ . . Lave L204 Mass of Pordtes in sea cliff, south of F eine Fish ales one 24 Sections of cliffin Flying Fish Cove . . . Mae Nes Geological map of the neighbourhood of Flying Fish oe . 280 Mouth of Sidney’s Dale, west coast . . es Fg ee Dyke of basalt, floor of Sidney’s Dale, west coast . . . . 286 Sea-worn basalt in Waterfall (Panchoran) Bay, east coast . 286 ee eo ernie ——————----...ow ial s aor; tf . Cm 7 ua ee os We "en 1 ¥e! ; Caan e tte , ; iy ier 2h ‘ * om Pe nae! . fy " * ha “ ie 7 1 / ' hy | | ' : oe M i . L d \ iv : fi ‘ . i f : a } ¥ r ,. . heels 16 iP ee Pia . de Si ‘ = ba 4” ry m “ € 4 f k 7 nf ll . F 7 ‘ ¢ ‘ . a ¢ 6 , F . . ar Y CHRISTMAS ISLAND (INDIAN OCEAN). HISTORY AND PHYSICAL FEATURES. By C. W. Anprews, B.Sc., F.G.S. Curtstmas Istanp, the subject of the present monograph, lies in the eastern part of the Indian Ocean, in 8. lat. 10° 25’, E. long. 105° 42’. Java, the nearest land, is about 190 miles to the north, while some 900 miles to the south-east is the coast of North-West Australia. A little to the south of west, at a distance of 550 miles, are the two atolls of Cocos and North Keeling, and to the north of these Glendinning Shoal. The submarine slopes of the island are very steep, and soundings of upwards of 1,000 fathoms occur within two or three miles of the coast: at this depth the bottom was found to consist of globigerina ooze. To the north is Maclear Deep, in which 3,200 fathoms were found, and to the south and south-west is the more extensive Wharton Deep, with upwards of 3,000 fathoms. The island, im fact, forms the summit of a submarine peak, the base of which rises from the low saddle which separates these two abysses, and on the western end of which the Cocos-Keeling Islands are situated. The first mention of Christmas Island occurs in a map by Pieter Goos, published in Holland in 1666, in which it is called Moni. In subsequent maps this name and that of Christmas Island are applied to it indifferently, but it is not known by whom the island was discovered and named. The earliest approach to a descriptive account is found in Dampier’s ‘‘ Voyages” [1],* in the following assage :— : ‘“« After leaving New Holland, the ship tried to make Cocos, but was driven to a more easterly course, and met nothing of remark till the twenty-eighth day. Then we fell in with a small woody island in lat. 10° 20’ S. It was deep-water about the island, and there was no anchoring; but we sent two canoes ashore, one of them with the carpenters to cut a tree to make another pump; the other canoe went to search for fresh water, and found a small brook near the south-west point of the island, but there the sea fell on the shore so high that they could not get it off. At noon both the canoes returned on board, and the 1 The numbers in square brackets refer to the list of papers, etc., relating to Christmas Island given at the end of the volume. B 2 Christmas Island. carpenters brought on board a good tree; the other canoe brought aboard as many boobies and man-of-war birds as sufficed all the ship’s company when they were boiled. “They also got a sort of land animal, somewhat resembling a large crawfish without its great claws. The island is a good height, with steep cliffs against the south and south-west, and a sandy bay on the north side, but with very deep water steep to the shore.” The date of Dampier’s visit was March, 1688. The next account of the island is given by Captain Daniel Beekman, in 1718 [2]. He remarks that ‘‘ the island looks exceeding pleasant, being covered with lofty trees, and may be known by the following directions:—Coming from the north-westward, it appears pretty high, with a saddle in the middle; the westernmost land is the highest, trenching away to the northward to a low, flat point; the easternmost point is low, but bluff. I sounded within eight miles of the low point, but had no bottom with the 100-fathom line out. The island is about seven leagues from east to west.” This writer gives a remarkable sketch, in which the heights are ridiculously exaggerated, the hill over the north-western point being made to look like a mountain with three peaks; his estimate of the length of the island also is much in excess of the truth. In 1771 the ‘‘ Pigot,” East Indiaman, attempted to find an anchorage, but failed. The crews of this and other passing vessels reported the occurrence of wild pigs, coconut-palms, and lime-trees, none of which really existed. The first attempt at an exploration of the island was made by the frigate ‘‘ Amethyst’ in 1857, from which a boat’s crew was landed with the object of attempting to reach the summit, but the inland cliffs proved an insuperable obstacle, and the ascent was abandoned. In 1886 the surveying vessel, ‘‘ Flying Fish”’ (Captain Maclear) was ordered to make an examination of the island. The coast was found to consist of limestone cliffs, and it was only after sailing nearly all round the island that an anchorage was found in a bay with a white shingle beach on the north coast. To this the name Flying Fish Cove was given, and it is now the site of a small settlement. Another white beach was seen towards the north- west point, but no anchorage was found near it. A number of men were landed, and collections of the plants and animals were obtained, but, since the island seemed of little value, no serious attempt at exploration was made / 3}. In the following year H.M.S. ‘‘Egeria’’ (Captain Pelham Aldrich) called at the island, and remained about ten days. Captain Aldrich and his men cut a way to the top of the island, and sent home a number of rock specimens obtained on the way, and Mr. J. J. Lister, who accompanied the expedition as naturalist, made extensive col- lections both of the fauna and flora, but had not time to penetrate to the middle of the island [4-6]. The island was formally annexed by H.M.S. “‘ Impérieuse” in June, 1888, and placed under the Straits Settlements Government. History and Physical Features. 3) Tn 1890 H.M.S. ‘‘ Redpole”’ called at the island for a few hours, and Mr. H. N. Ridley, of the Singapore Botanical Gardens, who was on board, collected a number of plants not previously recorded, and has written an interesting account of his visit [8]. Although Messrs. Lister and Ridley had made valuable collections of the fauna and flora of the island, the shortness of the time at their disposal rendered it impossible for them to penetrate far into the interior, or to make any examination of the geological structure. Nevertheless, the rock specimens brought back by the ‘“‘Kgeria”’ showed that the island probably consisted mainly of coral and foraminiferal limestones, resting on a basis of volcanic rocks; and a very interesting paper, in which the results of the expedition were summarized, and the probable structure of the island discussed, was published by Rear-Admiral Sir W. J. L. Wharton in the proceedings of the Royal Geographical Society for 1888 [7]. It seemed desirable, however, that a more complete examination of the island should be undertaken, and, if possible, collections should be made at different seasons of the year, and in 1896 Sir John Murray generously offered to pay the expenses of such an expedition. I was fortunate enough to be able to avail myself of this opportunity, and, the Trustees of the British Museum having granted the necessary leave of absence, I left England at the beginning of May, 1897. At that time the only means of access to the island was by the sailing-vessels belonging to Mr. G. Clunies Ross, of the Cocos-Keeling Islands, which are employed in carrying various supplies from Batavia to those islands, and on their way down usually touch at Christmas Island to land stores for the little colony established in Flying Fish Cove. Unfortunately, one of these vessels had left shortly before I arrived in Java, and I therefore had to wait some weeks before an opportunity of getting to my destination occurred ; but at length, on July 23rd, I sailed from Batavia in the ‘‘J. G. Clunies Ross,”’ a yawl of about 46 tons burden. After a rough passage of five days we sighted the island from the south-west, having run past it im the night. We arrived off Flying Fish Cove soon after sunset, but did not anchor till the following morning (July 29th). Seen from the south-west, the island appears as a long green ridge, nearly level at the top, there being only slight elevations at the north-west and south-east ends. The ridge descends seaward in a succession of terraces, the upper ones bounded by comparatively gentle slopes, the lower by a high and nearly vertical cliff, below which there is a narrow platform sloping gently down to the sea cliff. This is usually about 15 to 30 feet high, and is much undercut by the heavy swell that is continually breaking against its base. On approaching nearer, it can be seen that the whole island is covered by a dense forest, broken only by the grey face of the high inland cliff which runs round the greater part of the island, rising like a wall above the tall trees growing on the shore terrace. gg nas GNV1S! SVWLSIYHS “ysery mot pao Disab 4sqy YINOG WOT] guneg D1toby t+ BSundia FUT TT P20 ‘MINT Christmas Island—Physical Features. 5 The outlines of the land, as seen from the south-west, east, and north, and sections across it at various points, are shown in Figure 1 and in the map. From these it can be gathered that the island consists of a central plateau, highest towards the north and east, and descending to the sea on all sides by a succession of terraces, separated by slopes or cliffs. In most places the arrangement of these, from the edge of the plateau downwards, is—(1) a steep slope strewn with blocks ; (2) a broad terrace, followed by a similar slope (this seems to be wanting on the south); (8) a second terrace, terminating in a cliff 200 or 300 feet high; (4) the shore terrace, sloping gently down to the sea cliff; (5) the present fringing reef. There are, however, many local differences, the more important of which will be noticed below. The greatest length of the island is from North-East Point to Egeria Point, a distance of about 12 miles. The greatest width is from North-East Point to South Point (see Map), about nine miles; the least on a line drawn north and south through Murray Hill, about three and a half miles. ‘The total area of the island may be roughly stated as 43 square miles. - In giving a general account of the physical features of the island, it will be convenient to begin with the fringing reef, and then deal successively with the higher terraces, concluding with the plateau. There are, besides, one or two localities which will need a some- what more detailed description. The Fringing Reef. (Fig. 2.) If the coast be examined in a boat, or from the edge of the sea cliff, it is found that round the greater part of the island there is a submarine terrace or shelf, which varies greatly in width and in its depth beneath the surface. At Flying Fish Cove this terrace consists of two portions—an inner, which is partly dry at low- water, and outside this and about two fathoms below it, a second, which slopes away seaward to about 20-30 fathoms, beyond which the water deepens suddenly. ‘The upper reef is best developed at the northern and southern ends of the cove, and is almost absent in the middle. It exactly resembles the reef flat of an atoll. At low-water it can be seen to be composed of blocks of coral cemented together and forming a smooth, hard surface, like concrete, bored in all directions by marine worms. Some of the individual coral masses are of considerable size, and the section of one spherical mass was about four feet in diameter. On the surface of the reef are numerous loose blocks and large plate-like masses of coral, and towards the beach are a number of enormous masses of white foraminiferal limestone which have fallen from the high cliff above; some of these are 20 feet high and 30 or more long, and several have trees growing on them. In one case a block has rolled a dis- tance of 50 or 60 yards out on to the reef flat. At the lowest tides 6 Christmas Island—The Sea Cliff: the greater part of the surface of the reef is covered with water less than a foot deep, though there are a few holes of greater depth. In some places there are clumps of a small branching madrepore of considerable extent, the tops of which are exposed for nearly a foot for some time at low-water. Except for these there are only a few small corals in the deeper pools, and the chief inhabitants of this part of the reef are holothuria and small echinoids, which live in holes in the rock. The outer rim is raised from a foot to eighteen inches above the surface of the water of the lagoon. It consists mainly of flat blocks of coral overgrown and cemented together by a thick coating of bright red nullipores, and is cleft by numerous deep fissures and channels, through which the water thrown over it escapes; it is on the sides of these fissures that the corals seem to flourish best. The reef flat at the northern end of the cove is of much the same character. Standing on the nullipore-covered edge of this upper reef, the outer lower reef can be seen through the one or two fathoms of clear water that cover it. Its surface is studded with masses of various species of corals, separated by areas of coral sand. As above mentioned, this reef slopes away gently to about 20 fathoms, beyond which the water deepens suddenly. At the southern end of the bay it is interrupted, and at Smith Poimt no bottom was found with 30 fathoms close to the cliffs. A little south of the middle of the cove the reefs are interrupted by a boat-channel forty to fifty yards wide, which runs up to the beach. Its bottom slopes gently down to four or five fathoms, and is composed of coral shingle; beyond this patches of coral appear, and it passes into the general surface of the lower reef. Except at West White Beach and a few small bays with beaches on the east coast, Flying Fish Cove is the only place where any part of the fringing reef is dry at low-water. Round the greater part of the island the foot of the cliff is washed .by the sea at all times of the tide, and the fringing reef, if present at all, is from a yard to three or four fathoms below the surface, even at ebb-tide. Here it seems to consist, on its landward side, of a platform formed by the cutting back of the cliff by the sea, while on the seaward portion coral is luxuriant, and is, no doubt, growing outward on the talus resulting from the denudation of the coast. The Sea Cliff and Beaches. (Fig. 3.) Nearly the whole of the coastline is formed by limestone cliffs, varying in height from about 15 to 150 fect or more. The latter height only occurs at Steep Point, in consequence of certain movements which will be described elsewhere ; in other places the height seldom exceeds 50 feet. The cliffs are nearly everywhere much undercut, and sometimes overhang to the extent of 80 feet or more. There are numerous caves, and occasionally these have openings on the shore terrace at some distance from the sea. ne : See FiG-s 2: Se ¥ SNe ane sors Kaori FIG. 3.—NORTH COAST LOOKING TOWARDS SMITH POINT. 8 Christmas Island. When a heavy sea strikes the cliffs, the air is driven through these ~ passages with great violence, and sometimes accompanied by a column of spray 60 or 70 feet high. These blowholes are most numerous on the south coast, where the cliffs are exposed to the heavy ocean swell caused by the south-east trade-wind, which prevails during the greater part of the year. Along this coast the cliffs are cut up into narrow, finger-like masses, and their summit for some distance inland is bare of vegetation, being continually swept by the spray. Rock-pools containing small living fish some- | times occur on the cliff top. On the north coast, which is more rarely exposed to a heavy sea, the cliffs often form a continuous wall for long distances. The structure of the sea cliff will be described in more detail in the geological part of this memoir. Here it may be mentioned that by far the greater part of it is a section of a recently raised fringing reef; but in some places—e g., on the east coast—the sea has cut back to the older and more central parts of the island, and in such places the cliff may consist largely of vol- canic, mostly basaltic, rocks; even when this is the case, however, the upper portion is usually formed of recent coral limestone. In one or two places the sea cliff is interrupted by beaches of — coral shingle. The most important of these is at Flying Fish Cove, where it forms a crescent some 500 yards long. Towards the southern end it is composed of sand, but to the northward it becomes coarser and coarser, till about the middle it consists of rolled blocks of coral, and on the foreshore masses of yellowish limestone, apparently part of the talus derived from the cliff behind. At the northern end it becomes finer again. In places the shingle has been cemented into hard, compact rock, in sheets several inches thick. The top of the beach is about 15 feet. above low-tide level, and its slope varies much, being very steep after a northerly or north-easterly gale, and gentler during the . prevalence of the trade-wind, when the sea in the cove is quiet. Behind the beach there is a broad, nearly level platform, com- posed mainly of fragments and blocks of coral, but to some extent also of volcanic’ and other rock derived from the cliff above. Formerly the whole of this platform was forest-clad, and even now much of the beach down to high-water mark is fringed with a belt of Ironwoods ( Cordia), Waroo (Hibiscus), and Tournefortia ; but within this much of the forest has been cleared, fruit-trees (custard apples, limes, etc.) and coconut-palms planted, and a number of substantial houses built. At its northern end this platform is shut in by an inland continuation of the sea cliff (10-20 feet), which still shows traces of wave action; and at the back there rises in a semicircle a cliff covered almost entirely with forest, and towards the middle of the cove towering nearly 500 feet above the platform. West White Beach is in some respects similar to Flying Fish Cove, but here the platform is much narrower, and the sea cliff is continued behind it; above this cliff there is a wide terrace, as on The Shore Terrace. 9 other parts of the coast. In many places the beach is covered with slabs of shore cement, but on the whole it consists of finer material than that at the cove. Between it and Smith Point there are three other small beaches, but these are shut in by cliffs and covered at high-water. On the east coast there are several similar beaches of various sizes. At one of these a bed of basalt comes out on the shore, and over it gushes a small stream of excellent fresh water, the volume of which seems to remain constant at all times of the year; this waterfall is called by the Malays ‘‘ Panchoran,”’ and the bay in which it occurs may be named Panchoran Bay. On the west coast, towards North-West Point, I saw a series of small white beaches, which are probably covered at high-tide. The Shore Terrace. By this is meant the terrace extending from the top of the sea cliff to the foot of the first inland cliff. It is the most persistent and best defined of the terraces, being interrupted, so far as I am aware, at Flying Fish Cove and Steep Point only. Its width varies from nearly half a mile to less than a hundred yards. As a rule, it slopes gently upwards to the foot of the first inland cliff, but probably its greatest elevation is less than a hundred feet, and its average height is not more than about fifty. At the outer border there is usually a belt of low, jagged pinnacles, often separated by channels running seaward, precisely like those seen in the present fringing reef; within this is a level area thickly covered with rich soil, and then, towards the foot of the inland cliff, another belt covered with pinnacles and blocks fallen from the heights above. Sometimes, however, the whole width is a chaos of jagged pinnacles and masses of limestone, which, when covered with jungle, is quite impassable. As already mentioned, along the sheltered part of the north coast the forest extends to the very edge of the cliff. Elsewhere there is usually an outer band, where only coarse grass and a few straggling bushes of Pemphis and Scevola will grow. Within this is a zone composed mainly of Pandanus, Cordia, Calophyllum, Hibiscus, Pisonia, and other sea-loving plants; these form a protection to the forest, covering the inner part of the platform. The trees found here are mostly large forest trees, such as occur in the higher parts of the island. ‘The commonest forms are Gyrocarpus, Berria, Erythrina, Ochrosia, Kleinhovia, Celtis, Terminalia, and Arenga, but there are many others. The Gyrocarpus, which is completely bare of leaves during the last six months of the year, gives a very peculiar appearance to the forest during that time. Occasionally the fairly open forest is replaced by dense jungle of pandanus and thorny creepers. In several places on the east coast the shore terrace is composed largely of volcanic rocks, and since these hold up the water which elsewhere sinks through the porous limestone, there are several 10 Christmas Island. small brooks. These are never more than two or three hundred yards long, and rise from springs, welling out at or near the base of the inland cliff. Their banks are very muddy, and are burrowed in all directions by a peculiar grey crab (Cardiosoma), which is provided with a sort of brush on each side of the mouth, apparently for filtering the water which enters the gill chamber. The First Inland Cliff and Terrace. (Fig. 5.) The first inland cliff is the most conspicuous feature in the scenery, and in one form or another it extends round nearly the whole island. In one place it formsa cliff with a nearly vertical face bare of vegetation ; in another it is reduced to a talus slope of blocks of limestone piled up in wild confusion and covered with trailing plants and bushes ; and in others, again, it 1s replaced by a succession of smaller cliffs and terraces of varying height and breadth, rising step-like one behind the other. Whatever form it may take, its summit is between 250 and 3800 feet above the sea-level. On the east coast, about half a mile south of North-East Point, this cliff is absent for a short distance, and on the western coast it is much less distinctly developed than elsewhere. In many places where the cliff face is vertical, or nearly vertical, it shows distinct traces of wave action at two or three levels, the chief evidence of this being lines of small caves, and in places near the foot a very distinct and clearly comparatively recent undercutting of the face. For instance, on the north coast, at about 20 feet above the shore plat- form, the cliff is cut back into a shelf, above which it overhangs considerably, and from 150 to 200 feet higher up there are less distinct traces of a similar structure, the line of wave action being there marked by small caves. Where the single cliff face is replaced by a number of secondary cliffs and terraces, these also indicate that the surface of the sea has stood at successively lower levels with regard to the land, each cliff and terrace apparently marking such a change of level. In places these smaller cliffs and terraces are interrupted by gentler slopes, and one or more may disappear. Although the terraces may be continuous for considerable dis- tances, it is difficult to correlate those occurring in different parts of the island. Both the mode of origin and the composition of the first mland cliff seem to differ considerably in different places, but these poimts will be more fully considered in the geological section. The terrace on the top of the first inland cliff varies much in width and general structure. It is widest opposite the principal headlands, where it is between a quarter and half a mile wide; elsewhere it may be any width from less than 100 to 400 or 500 yards. It usually slopes gently seawards, sometimes becoming steeper towards the cliff edge, which is nearly everywhere bordered with a belt of pinnacles of coral limestone, separated by clefts and channels often parallel to the cliff edge. In one or two places, Inland Cliffs and Terraces. Lt notably near the middle of the north coast, the structure is more complex. Here, on descending the slope of the terrace towards the cliff edge, we come first to a narrow belt of pinnacles, beyond which is a sudden drop of about 50 feet; at the foot of the low cliff thus formed is a perfectly level, soil-clad terrace, some 50 yards broad, which is bounded on the outer side by lines of pinnacles 20-30 feet high, separated by winding channels with level floors ; beyond these is a slope covered with piles of limestone blocks extending to the cliff edge. ‘The channel included between the low cliff and the outer belt of pinnacles extends for half a mile or more roughly parallel to the coast, and may be either the result of a slip downward of the outer part of the cliff, or possibly a channel in a reef formed round the island when the sea was at that level. Whatever its structure, this terrace is always thickly covered with forest. The Upper Cliffs and Terraces. Above the first inland terrace, which, as just mentioned, varies ereatly in width, we meet with a second inland cliff, or rather steep rock-covered slope, for an actual cliff is only found in a few places, as, for instance, west of the southern end of Flying Fish Cove. Usually the limestones composing this cliff show many traces of coral structure. At the summit there is a second terrace sloping gently upwards towards the foot of the third inland cliff, which forms its inland boundary. The width of this terrace, like that of the one below, varies very much, and is greatest opposite the headlands. It is occasionally partly covered with pinnacles and blocks of limestone, but usually is clothed with soil, which supports a luxuriant forest of great trees 150-200 feet high; in some places there is thick undergrowth of Pandanus, Randia, ferns, etc., but as a rule the forest is fairly open. The upper cliff, ike that last described, is usually a steep talus-covered slope, with cliff faces showing in a few places only. Along the east coast, how- ever, the upper 40 or 50 feet may be nearly vertical for long distances, forming a true cliff along the upper rim of the island. For the most part the rocks composing it show few traces of coral, and have been to a great extent dolomitized, as will be described in the geological section. On the south coast one or other of the upper inland cliffs is wanting, or rather the two form a single declivity. The Central Plateau and Hills. Speaking generally, the whole of the upper part of the island consists of a plain, sloping gently to the south and west, and possessing a surface varied with shallow valleys, rounded flat- topped hills, and low ridges and reefs of coral limestone. On the northern and eastern sides the edge forms, in most places, a raised rim, bounded externally by a low cliff, below which comes the 12 Christmas Island. uppermost of the inland cliffs above described. In other places it passes into the inland cliff by a more gentle slope. The actual margin is usually marked by a belt of limestone pinnacles of ereater or less width. Another notable feature is the occurrence on the northern and eastern borders of several peculiar hills, the long axis of which lies parallel to the edge of the plateau. Of these hills Gannet Hill and Phosphate Hill (see Map and Figs. 4A, B) may be taken as typical. If the former be approached from the westward, it will be found that the plateau slopes very gently up to its foot; then there is a steep slope, from 50 to 60 feet high, and above this a level surface from 100 to 200 yards wide. On the outer edge of this, and rising abruptly from it, is a belt of limestone pinnacles, some of which are more than 10 feet high; FIGURE 4. A slope strewn with blocks funnaces of dolomutce Limestone of Phosphate of Lime 183. CONVOLVULACEA. » 65. Ipomeea pes-capree, Roth. This common plant of tropical sea-shores was recorded by Mr. Ridley from the island, but is not in the present collection. 66. Ipomea (Calonyction) grandiflora, Lamk., forma. Climbing on trees, north coast. Flowering in April. This plant approaches very closely to JZ. longifiora, R. Br., ,the type of which is in the British Museum (Natural History) Herbarium. The leaves and sepals are similar, but the peduncles are longer. Robert Brown’s plant came from the Gulf of Carpentaria, and Mr. C. B. Clarke, in FI. Brit. India, iv, p. 198, unites it with J. grandiflora, Lamk. Distrib. (of I. grandiflora, Lamk.).— Widely spread in tropics. | 67. Ipomeea peltata, Choisy. Creeper forming dense masses over low trees, middle of island. | Distrib.— Malaya, Madagascar, Fiji. 68. Ipomea digitata, Linn. Distrib.— Widely spread in tropical countries. 69. Convolvulus parviflorus, Vahl. Trailing herb, White Beach at Settlement No. 33. Distrib. Widely spread in tropics of Old World. SOLANACEA. 70. Solanum biflorum, Loureiro. Middle of island. Native name: Lombok utan. Distrib.—Singapore, Malaya, East Ava. 71. Solanum ferox, Linn. Top of first inland cliff. No. 74. On road above Flying Fish Cove. No. 97. Phosphate Hill Road. No. 99. Native name: Terong glatet. _, Dastrib.— India, Java. 72. Physalis ed ae | _-Phosphate Hill. No. 160. | Distrib.—Tropical Asia, Africa, Australia. 184 Christmas Island. 73. Datura alba, Nees. On all coasts. No. 117. This species in the Flora of British India is considered a variety of D. fastuosa, Linn. Distrib.—India, ACANTHACE A. 74, Ruellia prostrata, Lamk., var. dejecta, C. B. Clarke. Dipteracanthus dejectus, Nees. Common in Flying Fish Cove. No. 96. Distrib.— East Africa, India, Ceylon. 75. Asystasia coromandeliana, Nees, forma. Top of inland cliff, Steep Point. In flower April 5th, 1898. No. 154. Leaves much larger than type, reaching 53ins. long at base, gradually narrowing to petiole. Distrib. (type).—India, Malaya, Africa, Arabia. 76. Dicliptera maclearii, Hemsley. Common on shore platform. Nos. 20 and 22. Distrib.— Endemic. VERBENACEZ. 77. Stachytarpheta indica, Vahl. Settlement, Flying Fish Cove. No. 29. Distrib.—Tropical Asia and America. 78. Callicarpa longifolia, Lamk. Small tree. East coast, shore cliff, and near Flying Fish Cove. No. 39. Native name: Chendana. Distrib.—India, West Malaya to North Australia. 79. Tectona grandis, Linn. fil. This tree is recorded by Mr. Hemsley for the island, but it is not in present collection. The so-called Teak of the island is Berria. [I believe that this record is due to a mistake, and that Tectona grandis does not occur in the island.—C. W. A. ] _ Dicotyledons. | 185 80. Premna lucidula, Miq. Small tree. First inland cliff. No. 108. Native name: Kayu durie. Distrib.—Java. LABIAT&. 81. Anisomeles ovata, R. Br. Common on shore platform. No. 18. Common on shore cliff. No. 34. Distrib.—India, Malaya, China. 82. Leucas javanica, Benth., forma. Shore above the Cove; common. No. 8. Shore cliff, in clearings. No. 124. The calyx is smaller and teeth shorter than in Horsfield’s Java specimens of this plant. Some forms of LZ. mollissima, Benth., seem closely allied to above. Distrib. (type).—Java, Philippine Islands. APETALA. By A. B. Renprz, M.A., D.Sc., F.LS., Of the Botanical Department. NYCTAGINEZ. 83. Boerhaavia diffusa, L., var. pubescens, Choisy. Shore cliff, near Flying Fish Cove. No. 51. Common near the sea; November. No. 101. On shore cliff; January, 1898. No. 123. Distrib.—Tropics generally. 84. Pisonia grandis, R. Br. Large tree near sea; August toSeptember. No. 19. Native name: Ampol. Distrib.— North Australia, Polynesia. 85. P. excelsa, Bl. A tree, common everywhere, especially in middle of plateau. No. 96. Flying Fish Cove; April, 1898. No. 159. Native name: Jamboe. Distrib.— Malay Islands. 186 Christmas Island. AMARANTACEA. 86. Deeringia celosioides, R. Br. Everywhere near cliffs. Flowering in August. Flowers red. No. 22. East coast; first inland cliff. No. 114. Distrib.—India, Malaya, Australia. 87. Celosia argentea, L. Flying Fish Cove; introduced. No. 21. Flying Fish Cove; common; December. No. 77. Native name: Buntoot kuching. Distrib.—Tropical Asia and Africa. 88. Achyranthes aspera, L. Rocky point, shore cliffs; common. Three to four feet high. No: 71. Distvib.—Tropics. PIPERACE. 89. Peperomia levifolia, Miq. Centre of island ; on fallen trees; February, 1898. No. 145. Distrib.—Java. 90. P. rossi, Rendle, sp. nov. Herba parva, carnosula, repens, glabra, foliis oppositis, breviter petiolatis, ellipticis, obtusis, obscure triplinerviis, frequentissime et minute atro-punctulatis; spicis terminalibus, crassis, densifloris, folia duplo excedentibus; bracteolis rotundatis, peltatis; ovario obtrudente, rotunde-obovoideo, stigmate parvo, punctiformi, sub apice lateraliter inserto; fructu brunneo, valde exserto, subgloboso, apiculato, pericarpio punctato. Shoots 3 to 4 ins. long by about 13 line greatest thickness ; leaves 2 to 14 ins. long: by 4 to 7 lines broad, on petioles 2 to 3 lines long. Spikes reaching barely 2 ins. long by. 1 line thick; peduncles less than 4in. Bracteoles- about 4 line in diameter, ’ punctulate like the leaves. Fruit 2 line long, pericarp scarcely fleshy, covered with numerous small roundish warts. The measurements in the above description are taken from a moistened specimen ; the plants shrink considerably on drying. Near the Polynesian P. insularum, Miq., but ceineenes %é its fleshy habit and elliptical leaves. Dicotyledons. 187 _ LAURINEA. 91. Cryptocarya nativitatis, Rendle, sp. nov. Arbor ramulis ferrugine -tomentellis, foliis breviter petiolatis, coriaceis, ovatis vel oblongo-ovatis, interdum lanceolatis vel oblongo -lanceolatis, apice acuminatis, uninerviis, supra glaucis, impresso-costatis, et manifeste reticulatis, subtus glabris cum venis prominentibus et dense prominulo-reticulatis; paniculis floribundis, rhachi ferrugine, ramulis et floribus subfulve-tomentellis, floribus subsessilibus, sesquilineis. Leaves 4 to 6ins. long by 14 to 22ins. broad, with 4 to 6 upwardly curving main lateral veins; ultimate meshes of reticu- lation small, but well marked; petioles + to4in. long. Terminal panicles spreading, reaching 3 ins. long by 33ins. broad, branches 2ins. long or less. Perianth-segments oblong -spathulate, blunt, 1 to 14 line long; fertile stamens 9, anthers bilocular, the 3 inner extrorse, with a pair of shortly-stalked roundly cordate anther-like glands scarcely 2 line long, the 3 staminodes (fourth staminal whorl) subsessile, triangular-ovate, acute, base cordate, apex hairy, 4 line long. Fruit shortly ellipsoidal, about 2 in. long. Approaches the North Australian B. Cunningham, Meissn., but is distinguished by its larger flowers and ovate leaves. Phosphate Hill; April 25, 1898, No. 158. Native name: Jamboo boolut. ~ 92. Hernandia peltata, Meissn. Large tree; common. No. 146. Native name: Commendor. _ Distrib.—India, Malaya, Polynesia. ' Probably the Hernandia ovigera, L., of Hemsley’s list. EUPHORBIACEA. 93. Euphorbia hypericifolia, L. Common on the shore and cliff. Nos. 10, 60. Distrib.—Tropics. 94. E. pilulifera, L. Shore cliff and terrace, Flying Fish Cove; common. No. 54. Coffee garden; common. No. 51. , : Distrib. —Tropics and subtropics. 95. Phyllanthus niruri, L. Distrib.—Tropics. | 188 Christmas Island. 96. Jatropha curcas, L. Distrib.—Tropics generally. 97. Croton caudatus, Geisel. Shore terrace, near North-East Point; December, 1897. No. 107. A single specimen, containing unopened male flowers. Distrib.—India, Malaya. 98. Claoxylon rubescens, Mig. Rocky Point; December, 1897. No. 112. North coast, February; plateau, March, 1898. Small tree, first inland cliff. No. 53. Native names: Chundana, Kayu onjay. Distrib.— Malay Islands to Polynesia. 99. Acalypha wightiana, Muell. Arg. North-East Point; April, 1898. No. 157. Distrib.—India, Java. 100. Cleidion J avanicum, Bl. Small tree, east coast, first inland cliff; August, 1897. No. 37. Distvib.—India, Malaya. 101. Macaranga tanarius, Muell. Arg. Tall tree; common everywhere. No. 64. Flying Fish Cove; February, 1898. Native name: Kayu merah. Distrib. Malayan islands. URTICACEA. 102. Celtis cinnamomea, Lindl. Large tree, common everywhere. In fruit, February, 1898. Stinking wood. No. 63. Native name: Kayu boussouk. Distrib.—India, Malaya. 103. Sponia amboinensis, Decaisn. Small tree, Coffee Garden; October, 1897. No. 32. Distrib.—Tropical Asia, Australia, Polynesia. Dicotyledons. 189 104. Ficus retusa, L. Common everywhere; January, 1898. No. 120. _ Native name: Waringin. Distrib.—India, Malaya to Australia. 105. F. saxophila, Bl., vel aff. Distrib.—Java, Timor. 106. Cudrania javanensis, Trécul. Thorny creeper. Plateau near south-east road; August, 1897. No. 11. Distrib.—Old World tropics. . 107. Fleurya ruderalis, Gaud. No. 134. Native name: Pulus. Distrib.—Malay Archipelago, Polynesia. 108. Laportea crenulata, Gaud. No. 133. Native name: Pulus. Distrib.—India, Malaya. 109. L. murrayana, Rendle, sp. nov. Arbor dioica (?), ramulis crassis, glabris, foliis petiolatis, paulo supra basin rotundatam peltatis, late ovatis, acutis, glabratis, venis subtus sparse stimuloso-pilosis exceptis, marginibus leviter undulatis, siccis atro-viridibus et membranaceis ; inflorescentibus fcemineis axillaribus petiolos subszequantibus, pedunculis compressis vix alatis, cum ramis ramulisque sparse stimuloso-retrorso-hispidis, floribus capitatis; perianthil segmentis 4 inequalibus, plus minus ovyatis vel ellipticis, acuminatis, dorso puberulis; achenio discoideo, glabro, cum stigmate subulato terminato. Leaves 34 to 74.ins. long by 23 to 44 ins. broad, petioles 2 to 3 ins. attached about + in. above the base of the leaf, ee velns about six each side, subprominent below, curving and anastomosing below the margin, united by regular scalariform secondary veins ; reticulations minute, obvious; cystoliths numerous, evident ; stipules bluntly ovate, sparsely hispidulous. Inflorescence to 22 ins. long, lateral branches 14 in. and less; branchlets subterete; florets sessile. Perianth-segments brown, } line or less; stigmas long, ferruginously hairy; achenes = line in diameter. Male flowers absent. 190 Christmas Island. Apparently near the Javanese Z. laxiflora, Wedd. (from the description in DC. Prodr., xv1, i, 81), which, however, has leaves pubescent beneath, and the female inflorescence larger than the petioles. Flying Fish Cove. A tree; leaves stinging severely. February, 1898. No. 147. . Native name: Jelaton. 110. Procris pedunculata, Wedd. A shrub trailing over rocks. First inland cliff, No. 76. Near Flying Fish Cove, No. 91. Distrib,—Malay Islands, Polynesia, Mascarene Islands. 111. Boehmeria platyphylla, Don. Small tree, common everywhere. Stinging leaves; wood very soft; in flower all the year. Nos. 18, 60. Native name: Pulus scrobbo. Distrib.—India, Malaya, to China and Japan; Polynesia. MONOCOTYLEDONS. By A. B. Renpre, M.A.) D.Sc.) ¥.1.8., Of the Botanical Department. (PLATE XVIII.) ORCHIDEA. 1. Dendrobium crumenatum, Sw. Common everywhere on trees. No 110. Distrib.— Malaya. 2. D. macrei, Lindl. The flowers are smaller than usual in the species, but I do not think the Christmas Island plant is specifically distinct. Mstrib.—India, Java. 3. Phreatia listeri, Rolfe. Distrib.—Endemic. 4, P. congesta, Rolfe. Distrib.— Endemic, A small orchid not found in the present collection. Monocotyledons. 191 5. Saccolabium archytas, Ridl. Doritis, sp.n. (?), Rolfe in Hemsley’s list. February, 1898. On trees everywhere. No. 144. This is obviously the plant of which fruiting specimens only were collected, tentatively referred by Mr. Rolfe to Doritis in Mr. Hemsley’s list. Distrib.— Endemic. 6. Sarcochilus carinatifolius, Ridl. On trees everywhere. No. 1438. Flowering and fruiting specimens. Fruit just before dehiscence a little over 2 ins. long, tapering regularly from 14 line diameter at the apex; lobes of dehisced capsule 34 ins. long. Distrib.—Endemic. 7. Corymbis veratrifolia, Reichenb. fil. February, 1898. Common on higher parts of the island. Distrib.—India, Malaya. AMARYLLIDACEA. 8. Crinum asiaticum, L. On cliff, North-East Point; March, 1898. No. 142. Distrib.—Tropical Asia to Japan and North Australia. PALM A. 9. Arenga listeri, Becc. Didymosperma, sp. of Hemsley’s list. Common everywhere; flowering at all times. No. 109. Some- times attains a height of 70 feet and a diameter of 13 inches. Native name: Areng. Distrib.— Endemic. PANDANACEA. 10. Pandanus, sp. Male spikes and leaves only. Apparently allied to the common Indo-Malayan P. odoratissimus, Linn. fil. — Mr. Andrews states that there is another species of Pandanus of which he was unable to procure flowers. It forms trees 40 feet high. 192 Christmas Island. AROIDEA. 11. Remusatia vivipara, Schott. Phosphate Hill Road. No. 115. January, 1898. Distrib.—India, Malaya. CYPERACEA., 12. Fimbristylis cymosa, R. Br. Distrib. — Malaya, Australia, Polynesia. Not found in the present collection. GRAMINE A. 13. Ischemum foliosum, var. leiophyllum, Hack. Flying Fish Cove. Common everywhere round coast. No. 23. Distrib.— Endemic. This is the J. murinum, Forst., of Hemsley’s list; and is probably only a form of the common tropical Asiatic Z. cliare, Retz. I. muticum, L., cited in Mr, Ridley’s list, is perhaps a mistake for I. murinum, Forst. 14. Digitaria sanguinalis, Scop. Common on shore cliffs. No. 25 (in part). Distrib. —Universal. 15, Panicum (Effuse) andrewsi, Rendle, sp. nov. (Plate XVIII.) Planta minor culmis tenuibus, basi repentibus tum ascendentibus, usque paniculam foliatis; foliis lanceolatis, acutis vel acuminatis, basi oblique cordatis, sparse pilosis ; panicula effusa, glabra, ramis solitariis, tenuibus, inferioribus ascendentibus, superioribus patentibus, ramulis filiformibus ;_ spiculis longe - pedicellatis, ellipsoideis, parvis, glabris, gluma i? quam gl. 111 duplo minore, ovata, uninervia, vel obsolete 5-nervia; gl. 11% obovata, obtusa, 5-nervia; gl. ii? vix gl. ii#™ excedente, late elliptica, obtusa, 5-nervia, paleam sterilem includente; gl. fertili coriacea, levi, convexa, elliptica, 5-nervia, marginibus paleam subequalem amplectante. _ | Shoots 6-8 ins. high, internodes short, 6-8 lines long by barely + line or less in diameter, puberulous; sheaths subequal, striate, with pilose margins; ligule very narrow, membranous; blades 1-2 ins. long, 5-7 lines broad, papery, generally seven-nerved ; Gymnosperms. 193 margins pilose below, becoming glabrous above. Panicle not fully developed, 3 ins. long by 12 broad; in Timor specimens 8 ins. long by 4 ins. broad. Spikelets 2 line long; barren glumes membranous, green, gl. i less than 4 line long; gl. ii barely #-line long, very bluntly apiculate, lateral nerves as in gl. iii submarginal; gl. i % line, with an empty pale a little more than half its length; fertile gl. barely 3 line; grain unripe. Resembles P. arborescens, L. (P. ovalifolium, Poir.), in habit, but differs in the much smaller lowest glume, and the shape and size of gls. 11 and iii. . Hab.—Christmas Island, 1897. Also collected in Timor by Wallace and Curtis (in Herb. Kew). 16. Oplismenus compositus, Beauv. Coffee Garden, Flying Fish Cove, and everywhere. Nos. 7, 128. No. 128 is viviparous. Distrib.—Tropics generally. 17. Eleusine indica, L. Common on shore cliffs. No. 25 (in part). Distrib.—Old World tropics. 18. Eragrostis plumosa, Link. Nos. 26, 138. Distrib.—Tropical Asia and Africa. GYMNOSPERMS. By A. B. Renptz, M.A., D.8c., F.LS., Of the Botanical Department. CYCADEZ. Cycas circinalis, L., var. javana, Miq. Flying Fish Cove, beach. Grows all round the island; most plentiful on upper terrace (350 feet) at west end of south coast. Native name: Penawa jambi. Distrib.—Java, Sumatra, Borneo. 194 Christmas Island. FERNS. By A. Gzrp, M.A., F.L.S., of the Botanical Department. FILICIN A. 1. Trichomanes parvulum, Poiret. On trees, plateau; February, 1898. Distrib.—East Asia, Malay Archipelago, Oceania, Madagascar. 2. Davallia solida, Swartz. Common in forest, on trees; November, 1897. No. 82. Distrib.—Malay Peninsula, Java, Polynesia. 3. Davallia dissecta, J. Sm. Common on cliffs. No. 81. Distrib.— Java. 4. Davallia spelunce, Baker. One frond. Distrib.—Tropics and sub-tropics. 5. Asplenium nidus, L. May, 1898. Distrib.—Tropics and sub-tropics of the Old World. 6. Asplenium falcatum, Lam. Common on trees; October, 1897. Nos. 83, 112. Distrib. — Polynesia, Australasia, Malay Archipelago, India, Africa. 7. Asplenium centrifugale, Baker: in Journ. Linn. Soc., xxv, p. 360 (1890). Distrib. —Christmas Island (J. J. Lister). 8. Nephrodium syrmaticum, Baker. Common in forest. No. 87. Distrib.—India, Malay Archipelago. 9. Nephrodium dissectum, Desv. Common in forest. No. 88. Distrib.—India, Malay Archipelago, Oceania, Madagascar. Ferns. 195 10. Nephrodium intermedium, Baker. Distrib.—India, Malay Archipelago, Japan, Christmas Island (J. J. Lister). 11. Nephrodium truncatum, Presl. Panchoran; January, 1898. No. 121. _Distrib.—India, Malaccas, Australia, Polynesia. 12. Nephrodium polymorphum, Baker. North-West Point; not common. No. 94. Distrib.—India, Malay Archipelago. 13. Aspidium membranaceum, Hook. Plateau, common; No. 12. On trees everywhere; No. 131. Distrib.—Ceylon, Java, Philippines, West China, Formosa. 14, Nephrolepis exaltata, Schott. North coast; December, 1897. No. 130. Distrib.—Tropics. 15. Nephrolepis acuta, Presl. Common in forest everywhere. No. 85. Distrib.—T ropics. 16. Nephrolepis ramosa, Moore. Climbing on trees and shrubs, common. No. 92. Distrib.—Tropics of the Old World. 17. Polypodium adnascens, Sw. Distrib.—India and China to Fiji; East and West tropical Africa. 18. Polypodium irioides, Lam. - Common everywhere on trees and rocks. No. 108. Distrib.—India and China to Fiji and New South Wales; East and West tropical Africa. 19. Vittaria elongata, Sw. Sine loc. No. 163. Distrib.—India to Hawaii and New South Wales; East and ‘West tropical Africa. 196 Christmas Island. 20. Acrostichum flagelliferum, Wall. Rare; middle of island; No. 90. Phosphate Hill; January, 1898; No. 126. 4 Distrib.—Himalayas to Java and the Philippines. 21. Acrostichum listeri, Baker: in Journ. Linn. Soc., xxv, p. 361 (1890). Common on higher parts of plateau; No. 19. Phosphate Hill ; January, 1898; No. 125. Sine loc.; No. 129. Distrib.—Christmas Island. LYCOPODIACEA. 22. Lycopodium phlegmaria, L. Middle of island; February, 1897. Distrib.—Tropics of the Old World. MOSSES. By A. Gerr, M.A., F.L.S., of the Botanical Department. 1, Leucobryum chlorophyllosum, C. Muell.: Syn. Musc., ii, p. 585 (1851). Distrib.—Sumbawa, Celebes. 2. Octoblepharum albidum, Hedw.: Muse. frond., iii, p. 15 (1792). Distrib.—Tropical Zone. 3. Thyridium fasciculatum, Mitt.: in Journ. Linn. Soc., x, p. 189 (1869). Distrib.—India, Malay Archipelago, Oceania, Chile, Mauritius. 4, Trachymitrium revolutum, Hampe: in Nuoyv. Giorn. bot. Ital., lv, p. 280 (1872). | : Distrib.—Java, Borneo. 5. Neckera lepiniana, Mont.: in Ann. Sci. Nat., ser. m1, x, p. 107 (1848). Distrib.—Malay Archipelago, Oceania, Mauritius. Lichens. 197 6. Thuidium plumulosum, Doz. et Molk.: Bry. Jav., ii, p. 118, tab. 223 (1865). Distrib.—Ceylon, Malay Archipelago, Oceania. 7. Hypnum montagnei, Lac.: Bry. Jav., ii, p. 181, tab. 279 (1867). Distrib.—Java. | HEPATIC. Ptychanthus squarrosus, Mont. Distrib.—Malay Archipelago. LICHENS. By Vernon H. Bracxmay, M.A., F.L.S., Of the Botanical Department. 1. Parmelia tinctorum, Despr. Distrib.—Wide. Asia, Africa, Australia, New Caledonia. 2. Parmelia appendiculata, Fée ? Very poor specimen. Distrib.—K. Africa. 3. Physcia picta, Nyl. Distrib Very wide. Asia, Africa, America, Oceania (Java, Australia). 4. Pyxine sorediata, Fr. Distrib.—Africa, 8. America, Japan, Tahiti. 5. Pannaria rubiginosa, Del. ? Poor specimen. | | Distrib.—Very wide. Europe, Japan, Africa, America, Australia. 198 Christmas Island. 6. Lecanora varia, Ach. Distrib.—Europe, Siberia, Algeria, Mexico, New Caledonia. 7. Ramalina fraxinea, Ach. Distrib.— Europe, N. and 8. America. 8. Lecidea lutea, Schaer. ? Distrib.—Europe, Africa, Japan, 8. America, Labuan, Sandwich Islands, New Zealand. 9. Leptogium phyllocarpum, Nyl. ? Disirib.— Asia, Africa, S. America, Oceania (Java, Philippines, etc. ). FUNGI. By Vernon H. Buacxmay, M.A., F.L.S., Of the Botanical Department. BASIDIOMYCETES. 1. Schizophyllum commune, Fr. Distrib.—Cosmopolitan. 2. Polyporus confluens, Fr. ? Distrib.— Europe, N. America, Australia. 3. Fomes lucidus, Fr. Distrv1b.—Of almost universal occurrence. 4. Fomes australis, Fr. Distrib.—Europe, Borneo, Venezuela, Ceylon, Australia. 5. Polystictus flabelliformis, K1. Distrib.—S. America, Cuba, India, Ceylon, Malay Peninsula, Borneo. 6. Polystictus xanthopus, Fr. Distrib.-—In tropics generally. Fungi. 199 7. Polystictus luteo-olivaceus, B. & Br. _ Distrib.—Australia (Brisbane). 8 Polystictus sanguineus, Mey. Distrib.—In tropics generally. India, America, Africa, New Zealand, Borneo, Tasmania, Philippines, Java, Pacific Islands. _ 9. Hexagonia polygramma, Mont. Distrib.—Central America, Mexico, Cuba, India, Borneo, Ceylon, Australia. . 10. Daedalea tenuis, Berk. Distrib.—Philippines, Australia (Adelaide). 11. Favolus boucheanus, Klotzsch. Distrib.— Europe, N. America, Australia. 12. Laschia caspitosa, Berk. Distrib.— Australia (Clarence River). 13. Hirneola polytricha, Mont. Distrib.—Mexico, Cuba, India, Ceylon, New Zealand, Java. 14. Hirneola auricula-judz, Berk. Distrvb.— Europe, N. America, Mexico, Cuba, Tasmania, Borneo. 15. Guepinia sparassoides, Kalchbr. Distrib... Africa (Kaffraria). GASTEROMYCETES. 16. Cyathus montagnei, Tul. Distrib.— Cuba, Brazil, Uruguay, Ceylon, Australia. 17. Geaster andrewsi, Blackm., n.sp. Exoperidium in statu humido subcarneum, in statu sicco coriaceum, multifidum, laciniis (circa 7) acutis, basi integra, extus pallidum, siccitate aspero et veniis instructum, intus leve, 200 Christmas Island. cinereum. Endoperidium globoso-depressum, sessile, papyraceum, cinereum; peristomio subconico, minute dentato, in centro areole circularis striate pallidioris posito; columella persistente, e floccis 3-3°5 uw latis, fuscis; sporis globosis, echinulatis, 3°5—4°5 « diam., fuligineis. Exoperidium 20-40mm. latum (expansum), endoperidium 7-12mm. latum. This species is characterized chiefly by the nature of the peri- stomium, but the external veining of the exoperidium and the size of the spores also distinguish it from most of the Geasters. ASCOMYCETES. 18. Trichoscypha tricholoma, Mont. Distrib.—Rio de Janeiro, Guiana, Ceylon, Vera Cruz, S. Domingo. HYPHOMYCETES. 19. Stilbum javanicum, Henn. Distrib.—Sava. MYCETOZOA. By Arruve Lister, F.R.S. 1. Stemonitis splendens, Rost., var. a, genuina. Flying Fish Cove and Phosphate Hill. Distrib.—Kurope, America, Australia, Pacific Islands, Java. 2. Arcyria flava, Pers. © Distrib.— Europe, N. America, Java. 3. Lycogala miniatum, Pers. Distrib.—Europe, N. and 8. America, Guiana, Java. 201 PALAONTOLOGY AND GEOLOGY. FOSSIL MOLLUSCA FROM THE REEF-LIMESTONES OF CHRISTMAS ISLAND. By R. Burren Newron, F.G.S8. Tue reef-limestones of Christmas Island have been referred to in general terms by the few writers who have visited the region, but we are indebted to Mr. C. W. Andrews, through collections made in 1897-98, for our first knowledge of the paleontology of this formation, Among the specimens brought home from these deposits were a small number of shells, which, although of rather bad preserva- tion, and many of them not specifically determinable, are more or less important as a contribution to the Quaternary history of this area. The identifications that have been possible appear to prove conclusively the modern character of these rocks, the species being inhabitants of the surrounding seas at the present day. -MOLLUSCA : GASTEROPODA. Genus TECTUS, De Montfort, 1810. Conchyliologie Systématique, 1810, vol. ii, p. 186. Type.— Tectus pagodalis, De Montfort = Trochus mauritianus, Gmelin. Synonyms.—Pyramis, Schumacher, 1817; Pyramidea, Swainson, 1840. 202 Christmas Island. Tectus pyramis, Born. G. W. Knorr: Vergniigen Sammlung Muscheln, 1757, vol. i, pl. xii, fig. 4. Trochus pyramis, Born: Testacea Musei Ceesarei Vindobonensis, 1780, p. 333 ; Chemnitz, Conchylien- Cabinet, 1781, vol. v, pl. 160, figs. 1510-1512, p. 19. Trochus obeliseus, Gmelin: Systema Nature, 1790, 18th ed., vol.i, pt. 6, p. 3579. Lectus obeliscus, G. W. Tryon: Manual of Conchology, 1889, vol. xi, p. 19, pl. ui, figs. 13, 14. Description.—Born’s original diagnosis of this Trochiform shell expresses very clearly the salient characters of the species. It is as follows: ‘‘ Zesta conica, acuminata, anfractibus imbricatis, servatim granulosis, columella torta, 1mperforata.’’ Ktemarks.— An undoubted specimen of this species has been obtained from the limestone reefs of Christmas Island. It is a tall, conical form, with about twelve or more somewhat flattened whorls, the upper ones being tuberculate or undulating at the suture. The surface of the whorls is ornamented with a regular series of spiral granulations, which on the last whorl are arranged in eight or nine rows; the periphery is obtusely acute. The base of the shell is flat, wide, and sculptured with concentric lirations, which become obsolete near the outer margin. The shell possesses a shallow, subtriangular aperture and a short twisted columella. No internal characters of the mouth are visible, being hidden by matrix. Dimensions.—Length 80, diameter 80 mm. -Tryon’s illustration (fig. 14, see Synonymy) gives an excellent idea of the specimen from Christmas Island. Distribution.—Indian and Pacific Oceans; Samoan, Viti, and Philippine Islands, New Caledonia; North Australia, ete. ; Singapore. (Tryon.) ; fa Locality.—F lying Fish Cove; found in the lowest raised reef. Number on specimen: 609. Examples: 1. Tectus 2 Remarks.—A fragmentary cast, probably of this genus, occurs embedded in a pink-coloured limestone associated with remains of corals, etc. It is not specifically determinable. Locality.—Top of first inland cliff, about 300 feet above sea-level. ' Number on specimen: 951. eS: Examples: 1. Genus TUTUFA, Jousseaume, 1881. Bull. Soc. Zool. France, 1881, vol. vi, pp. 172, 179. Type.—Murex lampas, Linneus. Synonyms.—Lampas, Schumacher, 1817, mec Meuschen, 1787 (Brachiopod), nec De Montfort, 1808 (Foraminiter). Fossil Mollusca. 208: Tutufa granifera, Lamarck. Ranella granifera \ Lamarck: Hist. Nat. Anim. sans Vert., 1822, vol. vii, R. semigranosa } p. 163. Lampas granifera \ GW. Tryon: Manual of Conchology, 1881, vol. ili, p. 41, LI. semigranosa } ‘pl. xxii, figs. 35-37. Description. — This species is represented by a single cast embedded in a cream-coloured limestone. A thin test is sparingly preserved in places, and the typical high spire is well exposed. The characteristic granulations encircling the whorls are also displayed, each row being separated by a nearly obsolete line of granules. The shell has swollen whorls, and terminates with a short recurved canal. On each side of the specimen is a definite rounded or funiculate varix, which agrees with recent forms in not being regularly continuous. . Dimensions.—Length 35, diameter 20 mm. Remarks.—Since the present specimen occurs associated ith coral structures and other organisms, it is interesting to state that according to Tryon this genus is found at less depth than Ranella and invariably frequents coral reefs and rocks. Distribution.—Red Sea, Natal, Paumotus, Philippines, north-east coast of Australia. (Tryon.) Locality.—Top of tirst inland cliff, about 300 feet above sea-level. Number on specimen: 951. Example: 1 (specimen associated with pectinoid and other bivalve shells of doubtful determination). Cyprea, sp. Deseription.—This is a small cast in a cream-coloured compact limestone, of cylindrical shape above but with a depressed base, exhibiting a sub-central, narrow, and longitudinal aperture; the lip bears a regular dentition along its entire length; a short canal is present at each end ; the spiral volutions are well exposed through a small fracture at the base.. Dimensions. — Length 25, width (max.) 15 mm. Remarks.—From a comparison with recent forms this specimen appears to be allied to C. carneola of Linneus, a species living in the Pacific and Indian Oceans. Locality.—¥ lying Fish Cove; about 500 feet above sea-level and above rocks of undoubted Miocene age. ‘Number on specimen: 841. Examples: 1 Turbo 2 Remarks.—Cast of a Gasteropod shell probably referable to Furbo, showing the two last whorls. The absence of sculpture and other 204 Christmas Island. characters renders this specimen of no account for determination purposes. Found in a cream-coloured limestone containing corals and other structures. The front or apertural part of the specimen is embedded in matrix. Locality.—Top of first inland cliff, about 300 me above sea-level. Number on as 951a. Examples : INDETERMINABLE SPECIMENS. First.—A fragment of white limestone weathering a slaty colour, with remains of a Gasteropod cast, probably of Trochoidal affinities, but not identifiable. Locality.—North coast, about 50 feet above the sea-level. Number on specimen: 1048. Examples: 1 Secondly.— A mass of light-coloured limestone contains several small forms of Gasteropod shells whose structures, haying mostly dissolved away, leaving mere casts or impressions, are not capable of accurate determination. Among some of the shells represented in the block appear to be Massa and a number of Cerzthium-like forms with a granular ornamentation, probably belonging to the genus Buttiwm, ete. Locality. —Top of first inland cliff, about 300 feet above sea-level. Number on specomen: 951. Examples: One block; composed entirely of small Gasteropods. MOLLUSCA: LAMELLIBRANCHIATA. Genus VENUS, Linneus, 1758. Systema Nature, 1758, 10th ed., p. 684. Type.— Venus verrucosa, Linneus. Venus verrucosa, Linneus. Venus verrucosa, Linneus: Systema Nature, 1758, 10th ed., p. 685; Philippi, Enum. Moll. Sicilie, 1836, vol. i, p. 48; Romer (E.), Kritische Untersuch. Venus, 1857, p. 26; Fischer (P.), in Tchihatcheff’s ‘¢ Asia Mineure,’’ 1866-69, volume on ‘ Paléontologie,’ p. 360. Deseription.—Shell sub-cordate and thick; sculpture exhibiting nearly equidistant concentric ridges, with a series of intermediate fine and closely-set striations; the ridges are tubercled or verrucose at the sides; a ribbed structure radiating from the beaks lies immediately below the outer coating with the concentric ridges, . Fossil Mollusca. 205 and where the concentric striations cross these a cancellated condition is set up; margins crenulate; ligamental furrow excavated, oblique; characters of lunule obscured by matrix ; no dentition seen. Remarks.—The specimen referred to this species shows extremely well the chief characters of the shell. Both valves are in contact, but not quite cm siti: the left illustrates structural ornamentation ; the right, represented by a cast, shows a posterior oblique ridge and adductor scar, but no sinus or pallial line are decipherable, probably on account of youth, as the specimen is small and apparently a young example. It is in a cream-coloured limestone. Dimensions.—Height 28, length 31, diameter 25 mm. Distribution. —Species of wide distribution occurring in the Post- Pliocene beds of the Clyde Basin, etc.; im the Sicilian strata; and recent examples in the Mediterranean : Canary Islands : America; Indian Ocean (EK. Romer); etc., ete. Locality.—Top of first inland cliff, about 300 feet above sea-level. Number on specimen: 1032. Examples: 1 Venus, sp. A small block of cream-coloured limestone contains casts of a right and left valve of this genus. The position of the muscle marks and sinus, the characters of the posterior oblique area, and the convexity of the valves, appear to show a relationship to Venus puerpera of Linneeus, resembling, in fact, a figure called V. puerpera, var., in Chenu’s ‘‘ Manuel Conchyliologie,” 1862, vol. 1, p. 82, fig. 352, although the absence of dental and sculptural characters renders the specimen of doubtful specific value. Dimensions.—Height 55, length 65, depth of each valve 18mm. Locality.—Top of first inland cliff, about 300 feet above sea-level. Number on specimen: 1082. Examples: Two valves on one slab. INDETERMINABLE SPECIMENS. A small mass of a rather coarse-grained yellowish-white limestone, weathering a drab colour, largely composed of Lamellibranch shells, which occur as casts having little or no characters sufficient for identification. Some of the shells have a trigonal or nuculoid appearance. Locality.—West end of island, about 725 feet above sea-level.’ Number on specimen: 360. Examples: 1 206 Christmas Island. THE FOSSIL CORALS OF CHRISTMAS ISLAND. By Dr. J. W. Grecory, F.G.S., F.Z.S. (PLATE XIX.) Tux collection of fossil Corals made in Christmas Island by Mr. C. W. Andrews includes a little over seventy specimens, which were carefully collected, the exact stratigraphical position of each being recorded. The fauna is of interest, as I understand from Mr. Andrews that no fossils were obtaimed by previous visitors to Christmas Island, and that the only other fossils which he obtained were foraminifera and a few imperfect molluscan shells. Hence the determination of the geological age of the various lime- stones that build up the island must be dependent to a considerable extent on the evidence of the corals. Many of the specimens, however, have been so altered, often by phosphatization, that they are specifically indeterminable ; and the number of corals collected from the oldest limestones in Christmas Island is small, and the specimens fragmentary. But the most serious difficulty in the study of this fauna is that it comes from the borderland between the provinces of the neontologist and paleontologist. The identification of late Cainozoic fossil corals is always a difficult task. For the description of the recent specimens is based on the external form and superficial characters; whereas the description of the fossil corals refers to the essential structure of the corallites, as shown by transverse sections. Hence, consideration of the relations of the living and the latest extinct species of corals involves a comparison of incomparable terms. A further difficulty in the case of the Christmas Island collections is introduced by the fact that the corals are mainly Astreans. And the Astreans in the Zoological Department are not yet arranged, so that I have not always been able to compare the fossil corals with specimens of the species to which they are referred. The fauna includes representatives of nineteen determinable species, of which eight are new. As regards the general character of the fauna, it is typically Indo- Pacific, all the previously known species coming from that region. The corals are all reef-building species, and probably none of them grew at a greater depth than six or eight fathoms. The list of species and their distribution are given in the appended table. The horizons of the fossils have been divided into four 207 Fossil Corals. OGBT Opay *oyloeg -opuy oytoeg-opuy "BACL 2 OTODOIPT d d (5 “ogloB gy -opuy ce “optowg- Opuy -oytoeg-opuy “snoponNy | “Nvsye[ J yerjyue9 "SHIOadg 40 TONVY xX X xX a. Xx x X XK X “BETO [eryuey | pueluy “T1880, Petes, OCP "8BNO BOG "4119003 ‘ANYVIST SYNLISIUHD NO NOILNATULSI(T ‘NOILAGIULISIC UAL GNVY SaIOddS HO LST "HY Pa ‘dst "HP Pa 6¢ *ds'u (-aureyg) "eau ‘vue ‘ds'u ‘oun, *ds*t "eau ‘(HY "PA -ds'u (‘og % ‘TIq) CH ® "pa) WB] "MOHLAY ) ' wunp ye ‘w.odnuoyy . ove eee 1799 66 ee 8s maang "Ye ‘8agt4og " wemaupun DY.10Ur980) eee vaprownt (73 ' tho.und vruas0s1upy poYiUbous DY.AISVU0UNT pyojuapronnd *1eA ‘vynqnd vousnyiuvop eee eee eee eee “ psodoyayoud "s+ asgopyay Pee anes. i nynuunjos *xeA ‘siunjnbuvwponb re" sapprand 017391940 * s1Usofizas DDAISVU0H *** padasinba vurspuvo yy UMNIALPUD 01.4010) ss oss mbhayd 01407407 pe DIDULY IA "The “ossnyT een eee “dg 6 ¢ siuooiaatg "ye ‘v4odopj19007 *"galomag 208 Christmas Island. groups, in accordance with Mr. Andrews’ account’ of the structure of the island. The groups are the limestones of— 1. The sea cliffs. 3. The central plateau. 2. The inland cliffs. 4. The central nucleus. The interpretation of the evidence of the fossil corals as to the ages and relations of the Christmas Island limestones is difficult, as so little is yet known of the coral fauna of Malaysia between early Miocene and recent times. Many Miocene corals from Java have been described by Duncan, von Reuss, and Martin; and the existing Malaysian coral fauna is fairly well known. But from the intervening period no corals have previously been described. © Nevertheless, the evidence of Mr. Andrews’ collection is tolerably clear. The limestones of the sea cliff contain corals many of which are of the same species as those now growing on the fringing reef of Christmas Island; so that the date of those limestones is no doubt Pleistocene. At the other end of the series are the limestones of the central nucleus: they have yielded three determinable species, of which two are new, and the third (Orbicella herklotsc) is found in the older Miocene of Java; of the other two species one belongs to a genus elsewhere known only in the Miocene, and the other is a coral of an ancient aspect, though its genus was founded on a living species from the Red Sea. The limestones of the central nucleus are therefore probably Miocene in age. But the evidence of the corals is insufficient for positive opinion, or for the suggestion of a more precise date. As opportunities for further geological collecting in Christmas Island will probably arise, it may be worth while directing attention to the desirability of obtaining more specimens of corals from the central lmestones. On the central plateau reefs of recent limestone are said to occur; this age is assigned to the rocks on the evidence of the foraminifera. But there are no corals of recent species in the collection from the central plateau. The evidence of the corals renders it probable that outcrops of the central limestones occur on the floor of the plateau. The majority of the specimens were obtained from the limestones of the inland cliffs. Most of the species from this zone are still living, and four of them also occur in the rocks of the sea cliffs. But others are of older aspect, and the occurrence of a weathered specimen of Orbicella herklots: and Anisocenia favoidea shows that the Miocene limestones are exposed in some parts of the inland cliffs. Whether the rest of the cliffs, containing the species 1 C, W. Andrews, ‘‘A Description of Christmas Island (Indian Ocean) ’”’: Geogr. Journ., 1899, vol. xiii, pp. 20-24. Fossil Corals. 209 Mussa aff. echinata, Celoria andrewst, Montipora aff. dane, etc., should be regarded as Pleistocene or Pliocene, the evidence is insufficient to show. It is only certain that these limestones are intermediate in age between the late Pleistocene of the sea cliffs and the Miocene of the central nucleus. Family POCILLOPORIDA. Pocillopora, aff. brevicornis, Lamarck, 1816. Pocillopora is represented among the Christmas Island corals by several fragments included in a limestone from the foot of the first inland cliff on the North Coast (No. 867). One specimen is a cylindrical branch 45 mm. high and 8mm. in diameter. Another is a low, massive, almost hemispherical branch. Mr. Bernard has provisionally identified two recent Poczlopore from Christmas Island as P. favosa and P. brevicornis; the fossil specimens would agree with either in the characters of the corallites. A large number of recent species of this genus have been proposed by neontologists on variations in the shape of the branches. Ortmann,’ however, has suggested that the recent species are mere individual variations. In describing a collection of thirty-three specimens he states that they form a complete transitional series, and fill up the gaps between the previously described species. Ortmann, therefore, did not give a specific name to any of the specimens. Recently Mr. J. 8. Gardiner*® has also questioned whether ‘all these so-called species should not rather be described as varieties of one species,’ though he retains the conventional method of treatment of the group. The most convenient name for the Christmas Island fossil specimens would be P. brevicornis, Lam. Pocillopora, sp. indet. No. 989. From second inland cliff, over Flying Fish Cove ; alt. 500-600 feet. No. 947. Broad reef on middle of the island; alt. 500-600 feet. No. 925. High cliff over south end of Flying Fish Cove; alt. 400 feet. These three specimens are so altered that they are specifically indeterminable. ' Ortmann, Syst. und Verbr. Steinkor.: Zool. Jahrb., vol. ii, Syst. 1888, pp. 162-166. * J. S. Gardiner, ‘‘ Pocilloporide from S.W. Pacific’’: Proc. Zool. Soc., 1897 (1898), p. 942. P 210 Christmas Island. Group ASTRAIDZA. Mussa, aff. echinata (Edwards & Haime), 1849. Lobophyllia echinata, Edwards & Haime, 1849. Mém. Astr., pt. ii: Ann. Sci. nat., Zool., ser. 111, vol. xi, p. 253. Mussa ie Edwards & Haime, 1857. Hist. nat. Cor., vol. ii, -p. 337. This species is represented in the collection by a fragment (No. 203) 70 mm. high, 65 mm. long, and with the calices 28 mm. wide. The specimen includes two confluent calices, and the walls of the corallum are parallel in horizontal sections. As the upper part of the septa is not shown, its absolute specific determination is impossible. But so far as the evidence goes, the specimen agrees with those collected by the ‘‘ Challenger” in the Malay Archipelago, and determined by Quelch as IL. echinata. The only doubtful point is, that in the transverse sections the septa do not appear to be alternately thick and thin; but this arrangement is probably masked by the secondary calcification of the specimen during fossilization. The Christmas Island specimen was collected from the first inland cliff at the Zigzag, at the altitude of 90 feet. Leptoria phrygia (Ell. & Sol.), 1786. Madrepora phrygia, Ellis & Solander, 1786. Hist. Zooph., p. 162, pl. xlviii, hax 2? § : non Leptoria ,, Edwards & Haime, 1849. Mém. Astr., pt. iii: Ann. Sei. nat., Zool., ser. 111, vol. xi, p. 292. nA tenuis (non Dana), Edwards & Haime, 1849. Ibid., p. 292. The name of this species has been the subject of much confusion, owing to an apparent inconsistency between Dana’s figures and description of this species and Z. tenuis (Dana). Milne Edwards and Haime apparently based their diagnoses on Dana’s figures, and thus inverted the main characters of the two species; for they describe LZ. tenuis as having broader gyri and less crowded septa than LL. phrygia, and also as having stouter walls and columella. But Dana does not state the magnification of his enlarged figures, and it therefore appears wiser to base the distinctions between the two species on his diagnoses. He therein states that the gym of L. phrygia are 2-24 lines broad, while those of I. tenws are 13 lines broad. Moreover, in LZ. phrygia there are from 10 to 12 septa to the half-inch, whereas in Z. tenuis there are about 20 septa to the half-inch. Edwards & Haime, however, define L. phrygia as haying the gyri 8mm. broad, against 4mm. in Z. tenuis, and 15 primary septa per centimetre, against 8 in LZ. tenwis. Fossil Corals. 211 Ortmann! appears, therefore, to be perfectly justified in con- cluding that Edwards & Haime reversed the names of these two species. The Christmas Island collection includes three specimens of this species, which have the following dimensions :— No. 53. No. 306. No. 100. Meith of calicinal series 2s, 75.9 9 i3'mm. 2.) 34mm. ... s-— mm. Number of primary septa per cm. 9 Be 7 oe 7-9 They are therefore referable to the Z. tenuis of Edwards & Haime (non Dana) and the LZ. phrygia of Ellis & Solander, with whose figure they agree. | 7 A slide cut from specimen No. 306 affects the generic diagnosis of Leptoria. As generally defined, the walls of adjacent corallites are said to unite directly; but, as shown on Fig. 1, the adjacent series are, in places, united by costee and exotheca, and not by the walls. This fact led me, on first examination of the slide, to feel some doubt whether the coral were a Leptoria. But it appears only necessary to modify the generic diagnosis to this slight extent; for the same mode of union of the series of corallites occurs in L. tenuis (Dana). Thus Dana’s description of that species refers to the corallum as very cellular; and his figure of a transverse section (Dana, op. cit., pl. xii, fig. 7d) shows the compound nature of the walls. _ Mr. Bernard’s manuscript list of the recent corals collected by Mr. Andrews at Christmas Island shows that LZ. phrygia still lives on the neighbouring reefs. 1 Ortmann: op. cit., p. 172. 212 Christmas Island. The distribution of the fossil specimens on Christmas Island. is as follows :— No. 53. From top of sea cliff on the east coast. No. 306. First inland cliff above West White Beach; alt. 260 feet. No. 100. From a limestone breccia on the first inland cliff at the height of 250 feet. Celoria andrewsi, sp.n. Diagnosis.—Corallum, form unknown, but massive; the species is represented by a slab 80mm. high, 55mm. wide, and 20 mm. thick. Corallites in very short series and mostly isolated. The longest series is 7mm. long, and includes three calicinal centres. The single, circumscribed corals occur in regular rows. Walls thick. Columella of stout trabecule, and for the genus fairly well developed. Septa stout; one cycle in young corallites; two incomplete cycles in mature corallites. Distribution.—Represented in the collection by one specimen (No. 175), from the first inland cliff on the north coast ; approximate altitude 90 feet. Figure.—Pl. XIX, Fig. 1. Part of a transverse section, X 2 dia. Affinities.—The nearest ally of this species is the J/eandrina delicatula, Ortm.,! from Samoa, in which the valleys are from 5 to 12mm. in length; the septa occur in three cycles, and the columella is represented only by a trace. Owing to the shortness of the calicinal series the species belongs to the section of Celoria, for which Edwards & Haime once founded the genus ] D 'weysaurz(ev9007¢) 21920640 as =5 Vv roo Ss=5= « esi ar a le Veta ad —— Rape a ee eaas aS es eee on ee ey ee ee ee Sa Se ° AAN_ — 3S AAN A= 383 AASAA — 3N3 ke SO Sist esse ts oi nN So Sa eg bh * RAR rae S é Ba AAS = 3N ALAS ARS Sanne SELES ot Ni z LASS TS ee Se (s2s7euz 02 qnoqo uroy1) ruipyos w aos apounxouddy Geology. 273 commencement of the sea cliff which forms the southern boundary of the bay. It is a very hard compact yellow limestone, showing little or no traces of bedding or jointing. Its upper surface dips at about 40° a little to the. W. of N., and it disappears beneath the beach of coral fragments that has been thrown up at this point on the landward side of the narrow fringing reef. On the land side it can be traced up the cliff for about sixty yards, when it disappears under the talus which entirely conceals its base. This limestone is described above (No. 2, p. 226), and is of Eocene or Oligocene age; it was probably deposited in comparatively shallow water, and before the great accumulations of the Miocene and later limestones of the higher parts of the island could have been formed considerable subsidence must have taken place. In the rocks of corresponding age in Java, several species of Nummulites are said to occur in abundance, but, strangely enough, according to Messrs. Jones & Chapman this genus is entirely wanting in Christmas Island ; its place seems to have been taken by large Heterostegines. Above this limestone is a thick bed of compact black basalt (No. 1; see Fig. 3 and G in Fig. 2, A). The junction is marked by a bed of soft rock some five or six inches thick, in which harder nodules are embedded. These nodules consist of limestone containing foraminifera like those of the rock below, together with fragments of much altered basic glass (No. 3, p. 231). The soft matrix in which these nodules are embedded is a much decomposed rock consisting mainly of fragments of basic glass. The basalt mass measured along the shore is about 40 feet thick; it is roughly jointed into spheroidal masses, and seems to have been exposed on the sea bottom, the joint cracks being filled with a hard yellow rock, consisting of lime and fine detritus, derived from basic volcanic rocks and including numbers of various species of Globigerina. This rock (No. 5) is described on p. 258, and is figured on Pl. X XJ, Big, 17. The basalt’ itself is a compact black rock, very fresh-looking. The ground-mass consists of microliths of plagioclase, many small prisms of purple augite, and much magnetite. ‘There are porphyritic erystals of olivine, more or less altered into serpentine and vinidite. The skeleton crystals of magnetite are often arranged parallel to one another, and at right angles to the axis of the olivines. There are numerous rounded cavities, lined, and in some cases filled, with a strongly pleochroic green mineral, forming radial aggregates which show a black cross between crossed nicols. The upper surface of this basalt flow is covered with thick masses of Miocene Orbitoidal limestone (C in Figs. 2 and 5), which, near the junction, contains numerous fragments of the basalt overgrown 1 In the description of the volcanic rocks I am indebted to Mr. G. T. Prior, of the Department of Mineralogy, for much assistance. T ‘TAOQ HSI’ ONIATY AO HLNOg "IAOD HSIY ONIATY JO FAIS HLAOg nisin ——— IIITQ VIG NI (YSTY 4ooJ OE ynoqu) SaLIMOg AO SSV{—'F “OI T OLSAWI'T AUVILUTT, LAGIO NO ONILSAU LIVSVG JO axgq—'e ‘N1y Geology. 27) with Lithothamnion and Polytrema: this circumstance indicates that this basalt was exposed upon the sea bottom in early Miocene, or perhaps pre-Miocene times. On the right hand of section A on p. 272 this basalt is marked G, and is made to correspond to the upper basalt overlying the limestone B in the rest of the section; this is perhaps a mistake, since it agrees very nearly with tke basalt F underlying that limestone, which, together with the overlying basalt and ash beds, seems to be wanting on this southern end of the cove. It may, however, be remarked that the limestone A is very similar in character to B (No. 522, p. 2381), and if it were not that its fossil contents (see No. 2, p. 226) are said to be rather different and point to a possibly somewhat greater age, I should have regarded it as the southern continuation of B: in that case the basalt would be correctly lettered. Indeed, I believe this last interpretation to be correct. The upper yellow limestone (B) just referred to forms a prominent cliff throughout about the middle two-thirds of the cove. At its southern end it seems to have been cut out by the fault marked Y-Y (Fig. 2, A), but its termination is largely concealed by the talus derived from the lofty cliffs of Miocene limestone (C). A little farther to the north this cliff is again interrupted by another fault, X-X (Fig. 2, A), the downthrow side of which is towards the north ; this causes the limestone to terminate abruptly against basalt and ash, and to reappear at a lower level, where it again forms a nearly continuous cliff, low at first, but increasing in height towards the north, where it sometimes reaches 60 feet. At its northern extremity it becomes broken up into minor cliffs (P, Fig. 2, B) separated by soil-clad slopes, beneath which it finally disappears. The foot of the cliff is from 200 to 250 feet above the sea, but except in one or two places where it rests on volcanic rocks (e.g. at L and F), the base of this limestone is concealed beneath talus which forms a steep rock-strewn slope to the shore platform. This limestone is described on p. 231 as No. 522; it is remarkable for the absence of Orbitozdes, which is found in the rocks both above and below. The beds dip slightly seaward (at from 5° to 10°), and are broken up by joint planes into great cubical masses, many of which strew the platform below, of which, moreover, they probably form the chief foundation; blocks of the same limestone also appear on the foreshore in the middle of the cove. As already mentioned, the base of this limestone is mostly concealed beneath talus, but at a few points it can be seen to rest upon voleanic rocks; in all cases it seems to have been deposited upon these rocks long after their consolidation, and near the junction often contains fragments of them. Of these volcanic rocks there are two series—an older, trachytic, and a later, basaltic. The chief exposure of the former occurs near the middle of the cove (at L on the right-hand side of section B in Fig. 2), where it forms a great boss projecting into the overlying limestone. The extent of the mass cannot be determined, since its borders are mostly concealed 276 Christmas Island. by talus. The surface of this rock in contact with the limestone seems to have been greatly altered before the latter was deposited. In the centre of the mass the rock (No. 929) is light-grey, fine- grained, and made up of a felt of small lath-shaped felspar crystals, giving straight extinctions and showing flow structure round vesicular cavities which themselves show a more or less linear arrangement. There are some traces of a much altered ferro- magnesian mineral between the meshes of the felspars. Professor Judd has kindly had the specific gravity of this rock determined for me; it is 2°45. Figure 56. SECTIONS SHOWING THE STRUCTURE OF THE CuiFF AT Fiy1InG FisH Cove. A. At middle of section B, Fig. 2. B. At right-hand end of section B, Fig. 2. For explanation of lettering see Fig. 2 (p. 272). A few chains farther north trachytic rock again appears, but in this case under peculiar conditions. Here the trachyte forms two or three large masses, apparently completely included in the great bed of basalt which there immediately underlies the yellow limestone. The trachyte is here much altered, and consists of angular nodules separated by a brown powdery substance, apparently produced by the decomposition of the rock along cracks. In one place the basalt sends a finger-like process into the midst of one of the trachytic masses, and in another it appears to have penetrated the trachyte horizontally for some distance, so as to appear to be interbedded with it. The whole structure seems to be the result Geology. 277 of the eruption of a mass of basalt along the same line as that along which an eruption of trachyte had taken place at an earlier date, and the inclusion of portions of the older lava in the newer. The trachyte at this point is made up of a felt of small lath-shaped felspar crystals, giving straight extinctions and sometimes showing traces of a radial arrangement in groups. There are no porphyritic constituents and there are scattered grains of magnetite. The basalt (marked F in section B, Figs. 2 and 5) varies much in character in different parts of the mass. For the most part it is a fine-grained rock, consisting of small lath-shaped crystals of felspar, a little granular augite, and much magnetite. Flow structure is shown in the arrangement of the felspar crystals ; there are no porphyritic crystals. Where this rock forms a narrow tongue penetrating the trachyte it becomes more glassy. In one place the mass of fine-grained basalt is traversed by a vein or dyke of a basalt with large porphyritic crystals of pinkish-brown augite, often showing the characteristic octagonal sections, large fragments of olivine sometimes showing traces of crystal forms and altered into viridite along cracks only, and finally large lath- shaped crystals of felspars with traces of zoning; im one or two instances felspars are included in the augite crystals. The eround-mass consists of felspar microliths, small augites, and much magnetite. This coarser rock was probably injected into a fissure from the deeper portion of the mass. South of the fault X-X the limestone B rests on the upper end of a great mass of basalt (F), which can be traced down nearly to the sea-level. At its upper end it penetrates the limestone, and is repeated twice owing to slight faulting parallel to the main fault X-X. Wherever the talus is wanting it can be seen that the yellow limestone (B) is overlaid by a bed of glassy basalt (G), varying greatly in thickness and attaining its greatest development towards the southern end of the bay (neariy above the letters N.E.-S.W. in section A, Fig. 2). At this poimt it forms the lower portion of a lofty overhanging cliff, which, from the red staining of the lime- stone forming its summit and the colour of the volcanic ash beneath, is called by the people the ‘‘ Katoe merah”’ or the “red rock.” To the north of this point the basalt bed can be seen at intervals only, and to the south it is interrupted (see Fig. 2) by the fault X—X and is finally cut out by the slip Y-Y, the Miocene Orbitoidal limestones (C) resting on its end. The basalt of this bed is a somewhat glassy rock, the ground-mass of which is full of microliths of felspar and granules of magnetite ; there is a considerable quantity of olivine, which except in a few cases is entirely altered into serpentinous material. Numerous rounded vesicles more or less completely filled with a bottle-green substance are present. In the higher part of the bed this rock has undergone further alteration, the whole of the olivine being replaced by serpentine and the green material filling the vesicles 278 Christmas Island. apparently altered into a similar substance, while the glassy base has become palagonitic. The higher parts of the bed also seem to have been more glassy than the lower. The thickness of this basalt 1s, as already noticed, very variable, and the upper surface is nowhere clearly defined. It is covered by beds of palagonite tuffs, which in places attain a thickness of at least 50 feet. The passage from the basalt to the ash beds seems to be marked by an ill-defined band of a peculiar rock consisting of angular fragments of basic glass, some an inch across, embedded in a copious cement of crystalline calcite or, in places, of non-crystalline lime, containing fragments of palagonite (probably merely the smaller fragments of glass completely altered), and occasionally foraminifera; the cementing substance sometimes makes up a great portion of the rock. Seen on a fractured surface the basic glass is black in colour, of a resinoid lustre, and has an irregular splintery fracture. In thin sections it 1s seen to be a yellowish brown, and the fragments are usually altered along their edges to an orange-yellow palagonite ; embedded in the glass are many small nodules and imperfect crystals of olivine and some very small crystals of augite. This rock was not actually seen om sitt, but it invariably occurred in the talus immediately beneath the beds of palagonite tuff, which it almost certainly separated from the basalt below. The palagonite tuffs (H, Figs. 2 and 5), like the underlying basalt, vary considerably in thickness in different parts of the section. Between the faults X-X and Y-Y (see Fig 2) they probably attain a thickness of quite 50 feet. Further towards the middle of Flying Fish Cove they are mostly concealed by talus, but here and there form a low cliff of red or red and green mottled rock, which crumbles beneath the feet. Under the microscope it is seen that the rock consists of small fragments of a highly vesicular basic glass, which has been completely converted into palagonite; the whole is cemented together into a compact mass by crystalline calcite, and here and there the shells of foraminifera occur. The palagonite forms bands of different colours parallel to the outlines -of the fragments or of the vesicles, and there are often zones clouded with immense numbers of small granules, which under a low power appear perfectly opaque. Sometimes these dark zones are numerous, but usually there is one within a narrow band of clear palagonite. In a few instances the whole of the interior of the fragments is clouded with the opaque granules. According to Mr. Chapman the foraminifera which occur scattered through the mass are usually species of Pulvinulina. The glassy basalt, the rock composed of fragments of basic glass, and the thick masses of palagonite tuff above described seem to have been the products of a submarine eruption, the fragments of basic glass being derived from the shattering of the chilled upper surface of the basalt flow, and the palagonite tuffs being composed of the finer fragments of vesicular glass derived from the —— _ Geology. 269 same source and mingled to some extent with sediment containing marine organisms. ‘These rocks are very similar to specimens described by Murray and Renard in the ‘‘ Challenger’? Report on Deep-sea Deposits as forming the nuclei of manganese nodules dredged from depths of more than 2,000 fathoms in the Indian and Pacific Oceans. Thus the more altered portion of the glassy basalt is very similar to that figured in the volume quoted on pl. xix, fig. 4; the palagonite tuff to those shown on pl. xviii, figs. 1, 2, 3; and the basic glass (No. 400) to that figured on pl. xvii, fig. 3; and no doubt they were produced under similar conditions. The degree to which the palagonite tuffs are exposed on the cliff is shown in Fig. 2, where also it will be seen that, like the basalt, these ash beds are cut off by the fault Y-Y and have Miocene Orbitoidal limestones resting on their southern extremity. Inland, about half a mile south of Flying Fish Cove (Fig. 6), we come upon an extensive exposure of this upper basalt. The eastern edge of the exposure runs a little to the west of south, approxi- mately along the 500 feet contour-line; to the westward (that is, the seaward) side the basalt forms a series of steep rounded slopes separated by narrow valleys and running down to about the 300 feet contour-line; here it again disappears beneath limestones, chiefly Miocene and containing Orbitoides, but in some places of more recent origin. This belt of basalt is about a third of a mile wide at its northern end, and can be followed south for about a mile, beyond which it is completely covered with Miocene lme- stones: this is the most extensive exposure of volcanic rock in the island. As already mentioned, the upper surface of the exposure roughly follows the 500 feet contour-line where it disappears beneath the overlying Miocene limestones. The palagonite tuffs found in the cliff section are here almost entirely absent and usually represented only by a bed of impure limestone, often stained and banded red and yellow by water percolating along the surface of the voleanic rock, and containing fragments of palagonite and basalt, sometimes in such quantities as to form a kind of breccia, Towards the southern end of this exposure of basalt there are several patches of Orbitoidal limestone at from 500 to 550 feet above the sea; these rest directly on the basalt, many fragments of which are included in their basal portion, which may present the appearance of a breccia of basalt fragments. Some of these lime- stones (Nos. 835, 827, 581) are described on pp. 254 and 255. Returning to the cliff section, we find that the upper surface of the palagonite tuff bed may be covered directly by Miocene Orbitoidal limestone, or in a few places (e.g. at the points where the sections in Fig. 2 were taken) a thin band of basalt, which is often highly vesicular and contains large crystals of augite; above this may be a thin band of palagonite tuff, or in places a volcanic breccia consisting of fragments of highly altered basic glass and basalt embedded in a ground-mass of yellowish limestone which may contain foraminifera. FLYING FISH COVE Scale Cof fee oN Gardery x 4 x x xX Shore Terrace Muocene Limestone ? Late Pleistocene —— of central nucleus a ee Raised reef and beach re b Limestone older than last Hhasalt xx _* sed le p para i ii Wl Volcanw ash Fic. 6.—GroLtocicaL Map OF THE NEIGHBOURHOOD OF Friyine Fisa Cove. Geology. 281 The Miocene Orbitoidal limestones, which rest upon the upper volcanic series, take a very large part in the formation of the basis upon which the higher and later limestones rest, and extensive exposures of them occur in several localities. Along the summit of the northern half of the Flying Fish Cove cliff they form a vertical face, varying from 10 to 30 feet in height. On the terrace above they are exposed in low pinnacles roughly ranged in rows parallel to the clitf edge, and at the fault X-X (Fig. 2) they form a prominent cliff running inland for about the third of a mile and terminating at its southern end against the basalt mass described above (see Fig. 6). This cliff occurs on the downthrow side of the fault, the limestone on the upthrow side having apparently slipped down the seaward slope; the line marked Y-Y indicates the position of a portion of the slip. South of Y-Y (Fig. 2, A) these limestones thicken out greatly and form cliffs at least 200 feet in height, the mass being split by a series of vertical fissures roughly parallel to the coast south of Smith Point. These fissures mark small slips, which on the terrace above are indicated by a series of small step-like displacements; the high cliff on the south of the cove (Fig. 2, A, between the letters W.S.W. and N.W.) is, in fact, a section across the ends of these terraces. In the extreme south of the cove these limestones have been affected by two or three small faults, which involve the underlying basalt (G) and cause the repetition of the basalt bed in two places in the base of the cliff; the limestones from either side of one of these faults are described above under the numbers 229 (p. 238), 220 (p. 239), 219 (p. 240), 861 (p. 287). The last specimen shows conclusively that these limestones were deposited on a basalt surface exposed beneath the sea and thickly coated with Litho- thamnion and other encrusting organisms. Nos. 229 and 571 (p. 286) are probably from the same bed, both being taken close to the underlying basalt, and both being devoid of Orbitoides ; 571, however, is from a point about 480 feet above the sea, in the middle of the cove, while 229 is from only about 100 feet at the south end, the difference of height being accounted for partly by the slope on which the beds are deposited causing a general dip seaward and partly by the slipping that has occurred. No. 924 (p. 233) closely resembles 220, and is hkewise taken from close to the basalt, but in this Orbztovdes are present, and the same is the case with 968 (p. 252), from a little farther west, at a height of about 60 feet above the sea. Of the rest of the limestones from this locality described above by Messrs. Jones & Chapman, 595 (p. 240) and 845 (p. 241) are from immediately above the line of slip Y-Y; 596 (p. 241) and 844 (p. 242), from above the last; and 841 (p. 248) and 963 (p. 250) are from the summit of the high cliff at this pomt. The two last are stated to be probably of more recent origin than the Miocene rocks below, and may represent a remnant of some much later deposit which formerly covered them. From the north of the fault X-X the specimens 282 Christmas Island. 550 (p. 246) and 562 (p. 243) were taken close to the underlying volcanic rock, and 521 (p. 245), 551 (p. 248), and 646 (p. 246), from pinnacles at the summit of the cliff (about 500 feet). It will be seen that rocks nearly on the same horizon may exhibit considerable diversity in their fossil contents, but since in most cases the fossils were determined from a single section the diversity may be more apparent than real. The whole of these Miocene Orbitoidal limestones were probably deposited in shallow water on the summit and flanks of a sub- marine bank. I never found Orditordes on any rock more than about 600 feet above the sea, although corals of Miocene age are said to occur at much greater elevations (see p. 208). Before these higher rocks could have been formed probably a certain amount of subsidence had taken place. It will be convenient to describe here the northern end of the Flying Fish Cove section (left-hand end of B in Fig. 2), although in so doing it will be necessary to refer to some of the later rocks. It has already been mentioned that at its northern end the cliff of yellow limestone (marked B) becomes broken into minor cliffs (P), which dip somewhat downward and are soon concealed beneath a soil-clad talus slope. At a point slightly to the north of where the main cliff of limestone breaks up, the basalt likewise disappears, being partly concealed by soil, but mostly by a’ consolidated talus composed of blocks of Miocene Orbitoidal limestone, with some pebbles of volcanic rock. This forms a cliff (see N in section) which can be seen to rest upon basaltic and trachytic rocks. At its southern end, which is at a rather higher level than the main face, the talus blocks are angular, but throughout the greater part of its extent they are perfectly rolled and rounded, and there can be no doubt that we have here a section of an old beach which was formed when the sea was 80 or 100 feet higher than now. Still farther north this disappears under a coral-reef rock, probably formed about the same time. Above the point in the section marked N-S traces of beds of Miocene Orbitoidal limestone occur only about 200 feet up the cliff, showing that here also rocks of this age overlap the earlier rocks as in the south. These in turn are concealed beneath a great mass of cemented talus (M in section), which has been cut back into a lofty cliff, M (80-100 feet in places). The rocks comprising this talus include blocks of Orbitoidal limestone, but seem to be mostly of later date. At its northern end this cliff disappears beneath the limestones, forming the first inland cliff at the Zigzag (see note on p. 263), and its foot is concealed by a reef-rock (E) which partly covers the slope below it. In the talus beneath the high cliff are numerous blocks of basalt and palagonite tuffs, showing that the beds of these rocks are continued to the northern end of the cove, where they also pass beneath M and E. The lowest part of the section shows the face of the sea cliff (D), consisting of late Pleistocene or possibly recent limestones. Geology. 283 In this section we appear to have a fair representation of what would be seen in vertical sections through the island at right angles to the coast at any point, the succession being as follows : (1) A central core of older volcanic and Eocene or Oligocene lime- stones; (2) beds of basalt, volcanic ash, and thick masses of Orbitoidal limestones enwrapping 1; (3) masses of talus, derived mainly from the Miocene rocks and covered by (4) a thick detrital limestone, which is derived from the wear of the reefs which cover the higher portions of the island; (5) a raised reef of much later date, which covers the foot of the cliffs and slopes composed of 4; and (6) finally, the late Pleistocene, or even recent, limestones of the sea cliff, which cling to the base of any of the older formations which may be exposed. Rocks of the Central Nucleus in other localities.—As far as I know, the only other locality in the island where there is an exposure of the Eocene or Oligocene limestone containing Discocycline Orbitoides is in Sidney’s Dale (see Map), a deep gorge on the west coast. This valley is one of several which, beginning at a height of between 400 and 500 feet, runs down to the sea in a generally south-west direction. In some cases (e g. Sidney’s Dale) they cut through the sea cliff and terminate at the sea-level (Fig. 7), in others (e.g. Hugh’s Dale) they open out on the top of the lowest terrace. These valleys seem to have been originally formed along lines of cracking and faulting; as a rule, on one side they are shut in by vertical cliffs, on the other by steep slopes. The floor is often formed by basaltic rock, and in one or two instances (e.g. in the lower part of Sidney’s Dale Valley) it appears to form an upper edge of a narrow dyke running along the direction of the valley and showing signs of columnar structure at right angles to it (see Fig. 8). In all cases there are signs that in the rainy season a considerable torrent runs down these valleys, and no doubt has contributed to a considerable extent to their present form. I believe that where the sea cliff has been cut through to the sea-level this is entirely the work of the running water, and that the movements which first gave rise to these gorges did not affect the lowest terrace, which in fact was formed subsequently to them (see Fig. 7). In Sidney’s Dale, at about 250 feet above and 25 chains from the sea, the southern wall of the gorge is formed by cliffs varying from 60 to 100 feet in height; the northern side is very steep and in places cliff-like, while the total width of the floor is not more than 20 or 80 feet, and is mostly occupied by the rounded and water- worn rocks which indicate the existence of a rapid stream at some seasons. When I visited the valley in October it was perfectly dry. The cliffs to the south consist of a basal portion of basalt, about 10 feet high, then a narrow band of soft rock some 18 inches thick, and above this to the summit of the cliff hard yellow Kocene or Oligocene limestone. The basalt has a ground-mass crowded with lath-shaped crystals of plagioclase, some augites, and 284 Christmas Island. numerous skeleton crystals of magnetite; there is some glassy base. — A few porphyritic crystals of pale purple augite and some porphyritic felspars replaced by calcite occur. This basalt is extensively exposed in the neighbourhood and is different from the basalt above referred to as forming a dyke on the floor of the dale. The soft rock (No. 318) forming the thin band separating the basalt from the limestone above, and the massive limestone (No. 347), are described on p. 254. In both, the Lower Tertiary type of Orbitoides is present. Unfortunately the relations of this bed of ancient limestone were not worked out, because in the first Fic. 7.—Movutu or Sipney’s Datz, West Coast. place my stay in the neighbourhood was very brief, and in the second without microscopic examination the age of the beds was not recognizable. It will be noted that, as at Flying Fish Cove, this old limestone occurs at a comparatively low level, not being more than about 250 feet above the sea. The volcanic rocks are exposed over a considerable area on the east coast in the neighbourhood of the fresh-water stream and waterfall marked on the Map. There they do not occur more than about 150 feet at most above the sea-level; but towards the Geology. 285 southern end of this coast, a little north of Ross Hill, I found basalt pebbles up to 400 feet. In the neighbourhood of the fresh-water stream are some rounded knolls, and in a shallow valley between these I found an exposure of a trachytic rock similar to that described from Flying Fish Cove. This exposure was of small extent, and seemed to be completely surrounded by basalt, of which the knolls are composed; the relations of the two could not be made out, the ground being for the most part covered with a dense juiele of screw-pines, very difficult to penetrate. The basalt at this point forms a great part of the shore terrace, and appears on the shore in the waterfall bay and in another bay a little to the south. At the stream it is covered by thick beds of red palagonite tuffs, and it is to the presence of these volcanic rocks that the existence of the two or three small brooks is due. The palagonite tuffs are covered with coral limestones, the age of which is not known. At the waterfall (Panchoran Bay) the basalt forms an extensive sea-worn platform (Fig. 9), and on the beach forms a projecting ledge over which a perennial stream of excellent water flows. The basalt at this point, which is near the centre of the mass, contains porphyritic erystals of felspar, augite, and olivine. There seem to be two kinds of porphyritic felspars, one in well-defined twinned crystals, probably labradorite, the other less well-defined and with distinct zonal banding; this is probably more acid. The olivine is usually altered into a pleochroic fibrous serpentinous mineral. Ground-mass of microliths of felspars, augite, and magnetite. Above the basalt at this point is a bed of volcanic conglomerate, consisting of blocks of basic rock, some vesicular, some compact and glassy, mostly more or less rounded; these are embedded in a ground-mass of red volcanic ash with much lime; in fact, at the top of the bed the pebbles of basaltic rock are embedded in hard limestone. The greatest thickness of this bed measured was about 10 feet. Upon it is a bed of hard yellow limestone, the age of which is doubtful. The absence of Orbitoides (see No. 52, p. 259) is against its Miocene age, but on the other hand Dr. Gregory has doubtfully referred a coral from this bed to a species (Ordicella murrayt, p. 216) found elsewhere in the Orbitoidal limestone. Upon it is a thick mass of limestone breccia, the blocks composing which are of all sizes and cemented by finer material, often filled with phosphatic nodules; probably the whole is a submarine talus of comparatively recent date derived from the cliffs behind. This is capped in turn by a reef-limestone of quite recent date (probably late Pleistocene). The cliff at the north and south of this bay is therefore formed (from below up) by (1) basalt, (2) volcanic agglomerate, (3) yellow limestone (4 or 5 feet), perhaps of Miocenea ge, (4) limestone breccia, an old talus, (5) late reef- limestone with corals like those now living on the coast. A few hundred yards farther south the sea-washed platform is composed of a basalt of a very different character from that t Coast. ES WW; Date, NEY’S F SID , FLoor o E OF BASALT Dyk Fig. 8. East Coast. CHORAN) Bay, = SEA-Worn Basatt in WATERFALL (PA Fic. 9. Geology. 287 just described. This is a much altered glassy basalt with small porphyritic felspars and augites. The base has been for the most part altered into a yellowish and greenish brown palagonite-lke substance which contains many microliths of plagioclase. There are some vesicles filled with concentric layers of a transparent substance showing a black cross between crossed nicols. The lower part of the bed is divided into fairly regular hexagonal vertical’ prisms, the summits of which have been broken into small angular fragments and recemented with crystalline calcite, the resulting rock having a remarkable appearance owing to the sharp contrast between the black basalt and the white lime. This extends up ‘the cliff for about 40 feet, and is in some places capped by a foot or two of a fine-grained brown rock, apparently an ash, and on the top of the cliff there is a thick bed of red palagonite tuff. In a chiff a little to the south a clean section of the basalt shows that it is divided into four or five beds separated by indurated and brecciated limestone. The whole is covered by a conglomerate of blocks of limestone, some of great size, probably a consolidated talus from the inland cliffs. South of Steep Poimt the base of the sea cliff is formed of basalt divided into hexagonal columns, in one case apparently curved. Still farther south there are extensive exposures of basalt, which may be distinguished at a long distance from the summits of the inland cliffs by the great size of the sago-palms (Arenga listert) which grow upon them; in this locality volcanic rocks may occur up to 400 feet above the sea. In some localities on the east coast the Miocene Orbitoidal lime- stones are magnificently developed. The most notable exposure is near North-East Point, where the whole of the first inland cliff for more than half a mile consists of limestones of this age, crowded with the characteristic fossils. This cliff is about 250 feet high, and it appears to have been formed by a slipping away of a portion of the eastern flank of the island. A little farther south a much more extensive slip has taken place, giving rise to a cliff upwards .. of 500 feet in height and consisting apparently almost wholly of Miocene rocks. Towards the summit (about 400 feet) is found the rock which Messrs. Jones & Chapman have described above (No. 955, p. 255) as a breccia of fragments of Orbitoidal limestone cemented by recent reef material, but I am inclined to doubt whether the brecciation and recementing of the rock may not both be of Miocene date. The base of these cliffs is concealed by a talus of great blocks and also in the northern part by comparatively recent reef-lime- stones which once formed a narrow fringing reef along their foot ; it cannot therefore be seen whether here, as at Flying Fish Cove, these Miocene limestones rest on a volcanic basis or not; but since in the immediate neighbourhood pebbles of basaltic rock occur in the shore platform, and since at the same level and only about a mile further south the basalts and tuffs are present and of 288 Christmas Island. considerable thickness, it seems almost certain that this is the case. Cliffs composed of these Orbitoidal limestones are easily dis- tinguishable from those formed of later reef-limestones, by their flat smooth faces and the straightness of all their lines, which is the consequence of the system of jointing which splits the mass up into roughly cubical blocks. The magnificent range of cliffs (first inland) which forms the fine headland, Egeria Point, are no doubt of this age, and so perhaps are those of South Point. On the plateau and higher cliffs no Orbitoidal limestones at all occur, but according to Dr. Gregory some of the corals (eg. Orbicella herklotst) collected from the reefs on the central plateau are of Miocene type. If this is so it indicates that in these - localities the basis of older rocks has been exposed by denudation ; but since no rocks containing Orbitordes were seen and, on the other hand, traces of volcanic rocks were found, it seems probable that the Orbitoidal limestones never completely covered the volcanic basis, for had they done so traces of them should remain on the plateau. Tur Rocks oF THE CENTRAL PLATEAU anD HItts. The general characters of the central plateau and of the hills which occur on its borders are described above in the introductory section (pp. 11-13). As already mentioned, some of the limestones exposed in the interior contain corals of Miocene type (see p. 208), and therefore most probably form part of the central nucleus which has been exposed by the very extensive denudation that the island must have undergone. Other reasons for supposing that this may be the case are, that in the middle of the island occasional pebbles of volcanic rock may be found, and that, as mentioned on p. 18, the great depth of the reddish-brown soil covering much of the central region has certainly been derived from the decomposition of volcanic rock, at least in great part. It is unfortunate that the Miocene age of some of the rocks of the plateau could not be determined by me while on the island, since a careful examination of their relations, and fuller collections of their fossils, might have thrown much light on the age of the highest limestones © and on the date of the first elevation of the island above the sea. This event was no doubt post-Miocene, but that it was not long subsequent to that period seems to be rendered probable by the fact that since it took place a series of negative movements of the shore-line has occurred, a succession of inland cliffs has been cut back, and enormous masses of calcareous rock, both reef-limestones and more especially detrital limestones which cover much of the flanks of the island, have been formed. The latest of the limestones covering the highest parts of the island and forming, in my opinion, an atoll reef and island, have been either to a large extent removed by denudation or have undergone great alteration, which has led to the destruction of the contained organisms. The rocks composing the summit : | Geology. 289 of Murray Hill, Phosphate Hill, and the highest land over Flying Fish Cove are dolomitic limestones, containing 34 to 41 per cent. of carbonate of magnesia. Descriptions and analyses of these rocks (Nos. 378, 514, 800, 811) are given above by Mr. E. W. Skeats (pp. 267-268); and Messrs. Jones & Chapman have described the organisms contained in 378 (p. 257) and 800 (p. 258), and also in No. 143 (p. 256), a similar rock from the summit of Ross Hill. In all cases the fossils aré nearly obliterated, and only imperfect remains of a few foraminifera and fragments of Lithothamnion, which resists destruction to the last, are to be seen: in the rock from Murray Hill there may be traces of coral structure. The rocks forming the rim between the hills are of a similar character both on the seaward side and on the landward slope, or low cliff, which, according to the view expressed above, faced the lagoon. In these, although their general appearance and mode of occurrence point to an origin from a coral reef, yet traces of coral are rarely seen. Insome places, where the limestones contain little carbonate of magnesia, the foraminifera are fairly distinct: an example of such a rock is No. 134 (pp. 256 and 265), which was collected a little below the summit of the upper cliff on the east coast. The rocks of the central plateau have been examined only in part. One of the most interesting is from pinnacles projecting from the soil at about 800 feet above the sea (No. 985, p. 257) : it is a crystalline limestone crowded with fragments of Lthothamnion and Halimeda, together with a few foraminifera, and it seems to be a shallow-water rock, such as might well accumulate in a lagoon. At no great distance from this there is another rock which points more strongly to lagoon conditions. This is a fine white limestone, which for the most part is of a powdery chalk-like consistency, is composed entirely of carbonate of lime, and usually contains no organisms: scattered in it are irregular hardened masses which include numerous foraminifera, which are described above (No. 658, p. 257) as being undersized and thin-shelled, and the nature of the rock as a whole is stated to indicate that it was once the soft mud of a shallow lagoon, an interpretation which the position in which it is found strongly supports. Some of the hard masses closely associated with this rock are dolomitized and the organisms obliterated. (See No. 658, p. 268.) The most important evidence that the higher points on the northern and eastern rim of the plateau once formed islets is the existence upon several of them of thick beds of phosphate of lime, for it is difficult to account for the great accumulation of this substance at these points otherwise than by supposing that. it is derived from thick beds of guano deposited on these elevations under conditions very different from those now prevailing. The necessary conditions would seem to have been fulfilled if these hills formed low treeless islets, whether these consisted merely of accumulations of coral thrown upon the reef by the action of the waves, or were the highest points along the line of reefs which U 290 Christmas Island. had been exposed by a change in the relative levels of the land and sea. Another condition favourable for the accumulation of guano is absence, or at least scantiness, of rainfall, and the low and, as they must at first have been, treeless islets would certainly have a much smaller rainfall than at present occurs. Moreover, at the time when the first upward movement took place, the conditions prevailing in the Malay Archipelago were very different from at present. In Java, for instance, late Miocene or early Pliocene deposits are found at an elevation of 900 metres, so that a smaller land-area was then exposed, and, furthermore, the volcanic mountains were much less elevated than now. ‘These ~ circumstances may have considerably modified the meteorological conditions of Christmas Island, which lies near the southern edge of the region affected by the monsoon (see p. 17). The phosphates, as they now exist, are probably the remains of beds of limestone, which have been altered by the overlying guano, the carbonate of lime being replaced by phosphate. ‘The phosphatization occurred somewhat irregularly, and the removal of the more soluble portions of the beds by the action of perco- lating water has left behind a thick bed of blocks and nodules of phosphate, which covers a large area and extends to a considerable depth (upwards of 10 feet in places). The most important of these deposits is at Phosphate Hill, where a large area is covered by them, but other beds are to be found on some of the hills on the east coast. Moreover, at the present day small nodules of phosphate of lime are scattered widely over the plateau, and particularly on the outer slopes of the island. These nodules also occur embedded in the later limestones, and sometimes may have been formed in sett by segregation, but in most cases are simply derived from the higher beds. In any case the terraces, particularly the shore terrace, are in places thickly strewn with a sort of shingle of nodules of phosphate of lime, which have either weathered out of the limestones or fallen from the beds above. In many places on the plateau the level surface of the soil is thickly strewn with small round black bodies varying in size from that of No. 10 shot to that of small peas. Mr. R. Irvine informs me that these pellets consist of a central nucleus of phosphate of lime, surrounded by a fairly thick coat of manganese dioxide, the whole being again covered with a thin layer of phosphate ; they contain about 18 per cent. of manganese dioxide. This is probably derived from the volcanic tuffs which were extensively exposed on the higher parts of the island, and, as already mentioned, must be to a large extent the parent rock from which the thick soil of the island is derived. Their decomposition may have given rise to mud deposits on the lagoon bottom. The phosphate itself is a very peculiar substance. It is intensely hard (between 6 and 7), and this, combined with the waxy lustre of a newly fractured surface, gives the impression that it is siliceous, though as a matter of fact it contains little or no silica (less than | Geology. 291 1 per cent.). Under the microscope it can be seen that the rock, which has been phosphatized, was a fragmental one; obscure traces of contained organisms (foraminifera) may be observed occasionally, and in some specimens fragments of bone occur. There are numerous irregular cracks and cavities, which are usually lined with nearly transparent phosphate of lime, showing a beautifully banded agate- like structure. The colour of the rock is as a rule a brownish white, but some specimens are of a darker tint. In some cases the rock is found to consist of fragments of dark and light coloured phosphatized rock, embedded in a cement of transparent yellowish phosphate of lime, apparently deposited from solution in concentric layers round the fragments. Under crossed nicols this banded substance is found to be doubly refractive, polarizes feebly in tints of grey and shows traces of the black cross, the banded structure being rendered very prominent. In many respects this phosphatic rock closely resembles in its structure some of the phosphatic nodules from deep water described by Murray & Renard in the ‘‘ Challenger”? Report on Deep-sea Deposits (p. 391 et seq.). These nodules are described as having been formed as segregations of phosphate of lime replacing carbonate in certain marine deposits. This mode of origin may perhaps account for the presence of some of the small nodules found scattered over the island, but cannot be responsible for the formation of the great masses occurring at Phosphate Hill and elsewhere. The average composition of the phosphate is about 39 per cent. phosphoric acid; 51°5 per cent. lime; 3°5 per cent. carbonic acid; 2 per cent. iron and alumina; the remaining 4 per cent. being made of magnesia, water, fluorine, and other substances; there is only about ‘2 per cent. of silica. The brown soil in the neighbourhood of these deposits also contains a considerable amount of phosphoric acid, often amounting to more than 380 per cent. On Murray Hill is a bed of .a remarkable rock which seems to have been produced by the phosphatization of a volcanic rock, probably a bed of tuff. It consists of small brown spherules of phosphatic matter cemented by doubly refractive phosphate of ((?) lime: under the lens it presents somewhat the appearance of an oolite. It contains 39 per cent. of phosphoric acid, only 2°5 per cent. of lime, 32°5 per cent. of iron and alumina, nearly 5 per cent. of silica, the remainder being almost all water, either free or combined. The rock upon which the phosphate beds rest is, in most places, a dolomitic limestone, which, in the specimens examined, curiously enough seems to contain no trace of phosphate of lime. Descriptions and analyses of some of these dolomitic rocks from Phosphate Hill (Nos. 800, 804, 811) are given on p. 267. Tue Uprer Crirrs AND TERRACES. The rocks composing the upper inland cliffs have not been fully examined, but enough has been done to show that in different places rocks of very different characters occur. These upper cliffs 292 Christmas Island. would perhaps be more fitly called talus slopes, since it is rare © or an actual cliff face to be seen, the usual form being a steep: (30°-40°) slope strewn with jagged blocks of limestone sometimes arranged more or less in a succession of small terraces. A general account of them has been given on p. 11. The upper cliff consists entirely of white and cream-coloured limestones, which towards the summit are often more or less dolomitized, and are nearly always more or less cavernous, owing partly to the crystallization which has usually taken place to a greater or less extent. Traces of coral are rare, but in one or two cases I found a rock apparently made up of broken pieces of a branching coral. Some of the beds consist largely of foraminifera, fragments of mollusca, and other organisms. At 725 feet over West White Beach I found a bed composed almost exclusively of a small lamelli- branch, but this was on the south-west side of Murray Hill and perhaps belongs rather to the plateau than the upper cliff. Many of the rocks are clearly of fragmental origin, and consist of angular fragments of older limestones in a later calcareous matrix. No Orbitoides were seen. The rocks on the whole are such as might. have accumulated on the submarine slopes outside a living reef, and, in fact, are probably largely composed of the débris derived from the wear of the rocks described above as forming the rim of the plateau. This upper slope is separated from the one below by a level terrace of varying width, usually soil-clad, but occasionally studded with blocks and pinnacles of limestone. The second inland cliff, like the upper one, is generally reduced to a mere slope covered with talus, but in a few places, e.g. to the north of Steep Point on the east coast, it forms a vertical face. In it coral is found much more often than in the upper cliff, and at the locality just referred to numerous masses of it can be seen embedded in the limestone. Fragmental limestones are again common, and pieces of echinoid spines and molluscan shells are frequently met with ; in some cases foraminifera are very numerous. The limestones are occasionally more or less dolomitic (see 131, p- 257), and in a few cases are partly phosphatized (940, p. 261). In this last case the limestone in question occurs below Phosphate Hill, and the contained phosphate was no doubt derived from that covering the slopes above. No. 131 is from a narrow valley on. the summit of the first inland cliff, between its outer edge and the foot of the second inland eliff. First Intanp Crirr. The general characters of this cliff have been described above on p. 10: both in its mode of origin and composition it is much more complex than the slopes above. It may consist either of (1) limestones of the central nucleus, containing Orbitozdes, as at. North-East Point, or (2) limestones of later date, largely made up of corals, molluscan shells, echinoid fragments, foraminifera, and: —— rl LT Oe Geology. 293 other organisms, which together with other reef débris have accumulated on the flanks of the island; this is the prevailing type. and is found on all sides of the island where this cliff is well developed. The cases where the Miocene rocks are exposed have been noticed above. Rocks forming a cliff of the second type are described by Professor Rupert Jones and Mr. Chapman under the numbers 979 (p. 259), 859, 1002, 1005, 1006 (p. 260), 900, 4034 (p. 261), 937, 864 (p. 262), 200, 202, 208, 209 (p. 263), and 1032 (p. 264). It will be seen that some of these are described as being brecciated or as forming a ‘microconglomerate,’ and as a matter of fact they all seem to me to be mainly of detrital origin. Again, several are described as ‘recent,’ but this can only be regarded as a relative term, since they are probably older than the Pleistocene. It should be noticed, however, that the corals described by Dr. Gregory from this cliff are either recent forms or very closely allied to recent forms (see p. 210 et seqq.), and usually occur also in the sea cliff, but on this point see below (p. 294). Nos. 1002, 1005-6 may be taken as fairly typical of the rocks of the vertical face (200 feet high) of this cliff as developed on the east coast. No. 900 was from the bottom of a cliff forming the western side of the deep cleft by which Steep Point Hill has been cut off from the main mass, and may be taken as typical of deeper parts of this limestone; in this specimen minute fragments of bone are not uncommon. Nos. 200, 202, 208, 209, 211, and 1032 are from the first inland cliff, just north of Flying Fish Cove, and form part of a series of specimens collected every few feet from the bottom to the top. No. 1032 is crowded with organisms, and must have been formed close to a living reef. This series may be taken as giving a fairly good idea of the kind of rocks of which this cliff is, as a rule, composed. The first inland cliff appears to owe its origin to two different causes in different localities. In the first place it may be a fault cliff formed by the foundering of some portion of the outer edge of the island, as described above; this type is as a rule confined to places where the Miocene limestones are exposed, e.g. east coast near North-East Point and probably Egeria Point (south side), where the cliff can be seen to have been formed by one main slip and a number of subsidiary ones, some of which may extend for a short distance only, and form a number of short low cliffs at different levels above the main face. In the second case the cliff is the result of wave action; this is the commonest type, and the cliffs of the north and east coast are excellent examples of it. In many places it is clear that it has been formed by wave action at two or three levels (see p. 10), and that the sea has stood at several horizons along this cliff is abundantly proved by the fact that in places where the cliff is wanting raised reefs occur at different elevations. For instance, south of Smith Point (see Fig. 6, p. 280) there is such a reef terrace on the 180 feet contour-line, and at the foot of 294 Christmas Island. this a still later one at about 100 feet. Again, between Flying Fish Cove and North-East Point, for the greater part of the distance the single high cliff which is found at the Zigzag (see Fig. 6) is replaced by two or three irregular step-like cliffs of reef-limestone, often interrupted by talus slopes, gaps, and channels, and in fact representing the remains of a series of fringing reefs, each of which in turn was raised and cut back by the sea, while at its foot its successor grew up on the talus derived from the cliffs above, Whether a single vertical cliff face or a succession of terraces was formed depended upon the steepness of the submarine slopes. If these were gentle enough to allow talus material to accumulate and afford a foundation for a fringing reef the terraced condition followed, but if on the other hand the slopes were steep and no reef could grow, a vertical cliff was formed. It should be noted that all intermediate conditions occur, the commonest being that in which the upper 150 feet or so form a vertical face, while the foot, from the shore terrace up to about 100 feet above the sea, is formed by a narrow belt of reef. This corresponds to the terrace between the 100 feet and 180 feet contour-lines in Fig. 6, and is the most persistent of these minor terraces. In some places shore conglomerate was observed on its surface, and great limestone blocks fallen upon it from the cliffs above rest on a sort of pedestal of cemented coral fragments like that which is found at the base of the blocks lying on the present fringing reef. Of course these raised fringing reefs are of later date than the rocks in which the first inland cliff has been carved by the sea, and the lower ones may be but little older than the reef forming the present sea cliff and terrace. This probably accounts for the fact that some of the corals labelled as from the first mland cliff are similar to those found in the sea cliff and to recent forms. Tuer Snore Crirr anp TERRACE. The shore terrace and cliff (see pp. 6-10) are formed by the elevated fringing reef that grew round the island before the last negative movement of the shore-line took place. It is the most persistent of the terraces, and, with the exception of about a quarter of a mile in two localities, it runs round the whole island. In some places, as above mentioned, it may be in part formed by the volcanic and other rocks of the central nucleus, but elsewhere it may be described as consisting of a thin capping of coral limestone, resting on a foundation of consolidated talus derived from what are ~ now the inland cliffs, and, of course, varying in characters as the rocks composing those cliffs vary. For instance, on the east coast, in the neighbourhood of the fresh-water stream both the talus foundations and the reef -limestone overlying it are full of blocks of basalt derived from the exposure on the slopes behind. The shore cliff forming the southern boundary of Flying Fish Cove may be taken as fairly typical of the shore cliff in general. It Geology. 295 will be seen (Fig. 2 A, p. 272) that the basalt marked A, which runs down beneath the sea-level, has its upper surface covered with an old talus consisting of blocks derived from the cliffs of Miocene limestone behind, lying in a matrix of smaller limestone fragments mingled with the débris of the basalts and palagonite tuffs which occur in the neighbourhood, and often including the shells of foraminifera. A similar talus forms the foot of the cliff (see Fig. 2A, above the letters S.E.—N.W.), where, being very hard, it forms a projecting ledge which is some 9 or 10 feet high. Upon it is about 50 feet of very fresh-looking coral limestone, in which the individual coral stocks, in the position of growth, may often be distinguished. One mass of Porites is between 20 and 30 feet high and nearly as broad (see Fig. 4, p.274). A fine section of the sea cliff is exposed where it is cut through at the mouth of Sidney’s Dale (Fig. 7, p. 284). Here also it is seen to consist very largely of recent species of corals, some of which, both from this and other localities, have been noticed by Dr. J. W. Gregory (pp. 206-225). If the terrace at the top of the sea cliff be examined it will be found in many places to consist of two parts, an outer broader zone, which is the summit of the raised reef, and wherever the rock is free from soil and vegetation can be seen to consist mainly of fresh-looking corals, and an inner, much narrower zone, running along the foot of the inland cliff and consisting of the same material, being, in fact, the base of the portion which has been cut back by the waves. The present fringing reef forms a narrow shelf round the island, being only interrupted where deep water occurs close to the foot of the sea cliff; and, if a further negative movement of some fifty feet were to take place, it would form a cliff and terrace much like that just described. SuMMARY AND CoNCLUSIONS. From the foregoing account it will be seen that Christmas Island presents some important peculiarities which differentiate it from other oceanic islands, and are difficult to explain. The island is, in fact, the flat summit of a submarine mountain more than 10,000 feet high, the depth of the platform from which it rises being about 14,400 feet, and its height above the sea being upwards of 1,000 feet. The submarine slopes are steep, for depths of 1,100 fathoms occur less than four (in one case less than three) miles, and the foot of the mountain (about 2,400 fathoms) within twenty miles of the coast of the island. As far as the soundings go, they show that the slopes of the upper part of the peak are nearly alike on all sides, being about 2 in 5. Soundings made in the neighbour- hood of the island at depths of more than 1,000 fathoms usually show the bottom to be covered with Globigerina ooze ; off the south-east corner of the island coral-sand was met with in depths 296 Christmas Island. of more than 900 fathoms, and this sand is no doubt derived from the wear of the cliffs of this part of the island, which is exposed to the full force of the swell of the Southern Ocean. Round the rest of the coast fragments of volcanic rocks and pieces of manganese dioxide are recorded from various depths up to 1,100 fathoms: two soundings of 385 and 925 fathoms respectively brought up calcareous alge. Between the island and Java lies a long narrow trough, which is one of the abysses of the Indian Ocean, being upwards of 3,000 fathoms deep in places. Its long axis lies parallel to the south coast of Java, the submarine slopes of which appear to be formed by a great fault and are very steep, the 2,000-fathom line being only a few miles from the land. Forming the flat summit of the Christmas Island peak we meet with a succession of limestones ranging from the Eocene (or Oligocene) up to recent reef deposits, and accompanying the older Tertiary deposits are various volcanic rocks, most important of which are basalts and trachytes lying beneath the Eocene (or Oligocene) limestone, while above it are basalts and basic tuffs separating it from the Miocene Orbitoidal limestone which seems to make up the great mass of the island. The total thickness of these older Tertiary and the interstratified volcanic rocks is, as far as can be ascertained, about 600 feet, but it is probable, as above stated, that some of the rocks exposed on the plateau may be Miocene, in which case the series is considerably thicker. ‘The occurrence of such a series of Tertiary deposits on an oceanic island is, I believe, unknown elsewhere, although ‘Wallace mentions that Upper Miocene deposits occur in the Azores. Another point of importance in the case of these Tertiary rocks is that they, especially the Miocene Orbitoidal limestones, end abruptly on the coast in vertical cliffs sometimes 250 feet high, so that it is clear that the area which they originally covered must have been much larger than the present island, and that it has been cut down to its present dimensions by repeated faulting and slipping down of its peripheral region. All these limestones must have been deposited in shallow water, probably less than 100 fathoms deep. At present the Eocene limestones are found up to about 250-300 feet, the Miocene Orbitoidal limestones up to about 550 feet, while the summit rises 1,200 feet above the sea. Ii we suppose the Eocene limestones to have been deposited in 100 fathoms (and it was probably much less), the range of the oscillation with reference to the sea-level which the island can be proved to have undergone is between 200 and 3800 fathoms, a small proportion of the total depth to the ocean floor. Speaking generally, this oscillation appears to have consisted, first, of a gradual depression, allowing of the accumulation of the Miocene Orbitoidal limestones and those composing the higher land, then a period of rest, followed by a succession of movements of elevation (or better, negative movements of the shore-line), which have given rise to the terraced structure of the island and Geology. 297 continued to the present time. The period of rest between the upward and downward movement of the sea-level must have been a prolonged one, for it was during this time that the atoll condition existed, and the great bulk of the detrital limestone derived from the destruction of the living reefs, and now forming the mass of the first inland cliff, was deposited: the great accumulation of guano that must have taken place would also have required a vast period of time for its formation. In Java the later Eocene deposits include limestones, in which is found the Discocycline Orbitoides dispansa as in Christmas Island, but accompanied by numerous Nummulites, which, curiously enough, according to Messrs. Jones & Chapman, are entirely wanting in the limestones described by them, while on the other hand large Heterostegines occur abundantly. Above these Eocene deposits comes a great mass of volcanic rocks, including andesites, diabases, and other lavas, some derived from submarine eruptions. This volcanic series seems to correspond in time to the basalts and tuffs which overlie the older limestone at Flying Fish Cove. The Miocene rocks consist of three divisions, the lower made up chiefly of volcanic breccias, the middle of soft marls, the upper of calcareous rocks with some dolomites and marls. In Christmas Island these are probably all represented by the massive Orbitoidal limestone, the absence of terrigenous material being only what might be expected. In both areas the calcareous rock is crowded with Lepidocycline Orbitoides, but although some of the Christmas Island forms occur in Sumatra and Borneo none are recorded from Java, and most are described as new; the fact that the Orbitoides of the two areas have been described by different authors may in part account for the discrepancy. It will be seen that the rocks of South Java, if we make allowance for the proximity to land at the time of their deposition, resemble in their general characters and succession those of Christmas Island, and like them they often terminate on the south coast in abrupt faces, or show other indications that they formerly extended farther south, but have been cut back by faulting and slipping. As to the possibility that these rocks in the two localities were deposited in a continuous area, it can only be said that the difficulties in the way of supposing this to have been the case are very great. If it were so it must be imagined that the enormous depth between the two islands has been attained since the Miocene by a general depression of the sea bottom south of the fault line forming the southern margin of the Malayan platform; and further, that during this depression the small area which forms the elevation on which Christmas Island now stands escaped the movement, and in fact forms a ‘horst,’ on all sides of which the sea bottom has been faulted down about 2,400 fathoms. These suppositions, however, appear untenable, and most of the difficulties are avoided by regarding the base of Christmas Island as a volcanic peak which has accumulated in consequence of repeated eruptions. In this case, 298 Christmas Island. since upon its summit shallow-water deposits of Eocene age occur, the depth of the floor of the ocean in the neighbourhood can have undergone little alteration since the Eocene times, unless, indeed, it has been lowered equally round the foot of the mountain by a system of cross faults. This volcano, like those of Java and Sumatra, etc., probably owes its origin to the movements along the line of the great fault forming the south boundary of the Malayan area in pre-Kocene times. Some post-Hocene movements probably caused the eruptions, the products of which form the base of the Miocene both in Christmas Island and Java, and may have resulted in the deepening of the abyss between the two areas. Movements. are still in progress, as the eruptions of the Malayan islands show, and in Christmas Island also two slight earthquakes have been recorded by Mr. A. Clunies Ross within the last few years: the last of these, on October 20th, 1895, was sufficiently severe to. loosen great masses of rock from the cliff. This seems to have been felt in the Cocos-Keeling Islands also, a point of some interest, since these islands almost certainly rest on a volcanic peak which may owe its origin to the same causes as that of Christmas Island. In the foregoing pages I have frequently spoken of the elevation and depression of the island. This is, of course, merely elevation and depression in reference to the sea-level, and it would probably have been better to have employed the terms suggested by Suess, namely, ‘‘ negative and positive movements of the shore-line,”’ since in some cases, at least, particularly in the formation of the later cliffs, it seems very probable that it is the general level of the surface of the sea that has been altered, and not merely a local upheaval of a limited land-area that has taken place. The above description of the geology of Christmas Island must be regarded merely as a first essay, for owing to the fact that the age of many of the limestones could not be recognized by me on the spot, and to other difficulties referred to above, much remains to be done, and in the light of my present knowledge, both of the localities and of the rocks, if it were possible to revisit the island for even a few days, many questions could be definitely settled which during my former visit puzzled me greatly, after repeated examination. One point of special interest may be referred to, namely, the possibility of finding still earlier, perhaps Cretaceous, limestones beneath the Eocene (or Oligocene) limestone in Sidney’s Dale on the west coast. 299 THE GEOGRAPHICAL RELATIONS OF THE FLORA AND FAUNA OF CHRISTMAS ISLAND. By C. W. Anprews, B.Sc., F.G.S. Amone the most interesting subjects of inquiry in connection with an oceanic island are the relations of its flora and fauna to those of the neighbouring lands, the means by which it has been colonized, and the degree to which the changed conditions under which the colonists are placed have led to modifications and have given rise to new species. In the present section these points are briefly discussed, and a list of all the recorded species is appended, together with their approximate distribution or that of their allies. The fauna and flora of Christmas Island are on the whole, as . might be expected, most nearly related to those of the Indo- Malayan islands, but to this there are some exceptions in the case of certain groups. Of the 319 species of animals recorded, 145 or about 45 per cent. are described as endemic: this remarkably high percentage of peculiar forms is, however, no doubt largely due to the fact that in some groups, particularly the insects, the species inhabiting Java and the neighbouring islands are still imperfectly known, and many now described for the first time from Christmas Island will no doubt probably be found to exist also in other localities. Of the mammals all are peculiar species except one, and that is a well-marked variety of a species inhabiting Further India. The nearest allies of the Rats and Fruit-bat are found in the Austro- Malayan islands, a circumstance for which an explanation is offered below. The birds may be divided into four groups. (1) The resident land birds, which are all peculiar species, more nearly allied to Austro-Malayan than to Indo-Malayan forms (Lister, Proc. Zool. Soc., 1888, p. 530). (2) The sea birds, mostly widely spread forms, but in one case, Sula abbotti, previously recorded from Assumption: Island only, and in another, Phaethon fulvus, described from specimens of which the locality is not known. (3) The migrants, which reach the island during the rainy season, corresponding to the northern winter. (4) Accidental visitors, to which division Chalcococcyx basalis and Myristicivorus bicolor may probably be referred. Of the six reptiles four are peculiar, but belong to widely distributed genera, and the other two occur in Java. 300 Christmas Island. Of the fourteen species of land-shells described, six are peculiar, but allied forms are widely distributed in the neighbouring lands. . The same may be said of most of the other species, but two or three are not known from the Indo-Malayan islands, and may have reached the island from the eastward in the same way as some of the mammals. Nine species of butterflies are recorded, of which three are peculiar, while another is a distinct variety of a Javanese species. The others are Indo- Malayan, except two, which may be Australian. Of the larger moths sixty-five species are described, ten of which are peculiar. Of the remainder, most occur in the neighbouring islands, but there is a considerable group of species found in Ceylon, and another from the Austro-Malayan and Pacific islands. Out of nine species of Microlepidoptera six are new, two of the others belong to the Australian region, while the third is recorded from Africa. Of the Hymenoptera nine out of eleven species are said to be peculiar. All belong to widely distributed genera. The Coleoptera are represented by a much greater number of species than any of the other orders of insects, eighty-four in all being described, while ten others have been referred to their genera - only. Fifty-six species are said to be peculiar to the island, but this remarkably high proportion (nearly 67 per cent.) is no doubt due to the fact that the beetles of Java are still incompletely known. The remaining species are mostly either widely dis- tributed forms or are Indo-Malayan. As in the case of the moths, a few are identical with species from Ceylon. All the Homoptera are described as new. Several are related to Austro-Malayan forms. Of the Hemiptera four out of six are new, the remaining two are pelagic. The two new species of Neuroptera belong to widely distributed genera, and the three remaining species are common in the Oriental region. Of the Orthoptera twenty-two species are described, fourteen being endemic, but nearly all belonging to widely distributed genera. The remainder are either cosmopolitan, or at any rate Oriental forms. Of three species of Chilopoda, one is Palearctic (this was not collected by me), the other two Oriental. Two out of three species of Diplopoda are peculiar, the third being a cosmopolitan form. Twelve species of Arachnids have been described, three being new. The remainder, with the exception of one Australian form, are Oriental, mostly occurring in the Indo-Malayan islands. The land Crustacea are all widely distributed on the Indo-Pacific coasts. Finally, of the four species of earth-worms two are peculiar, one having allies in the Aru Islands and Ceylon, the other in Sumatra. The other two species occur both in the Oriental and Australian regions. Distribution of Fauna and Flora. o0L One hundred and eleven species of Dicotyledonous plants are recorded, and of these ten only are referred to as new, but a considerable number, while not specifically distinct, differ markedly from specimens from other localities, and may be regarded as local varieties. In fact, as has been pointed out on the authority of Professor Oliver, we are probably here dealing with species in the making [6, 10]. Most of the other plants either occur in the Indo-Malayan islands or are widely distributed tropical forms. Of the Monocotyledons seven out of eighteen species are endemic, the remainder being either Indo-Malayan or widely distributed. The single Gymnosperm, Cycas circinalis, is found both in the Indo- and Austro-Malayan islands. The ferns are either Indo- Malayan or common tropical forms: only two are described as. endemic. The remaining Cryptogams are all, with the exception of one peculiar species ef fungus, either Indo-Malayan or widely distributed species. The causes which have been instrumental in the introduction of the fauna and flora have been, as usual, the winds and ocean. currents, the work of the former being much the more important. The prevailing wind is the south-east trade, which blows on an average 300 days in the year. The nearest land in the direction from which it comes is the north-west coast of Australia, about 900 miles away, so that, as might be supposed, the number of species possibly introduced by this means is very small; perhaps one or two of the butterflies may have reached the island in this way. In fact, as Wallace ' long ago pointed out in the case of the Azores, the introduction of plants and animals into remote islands is due not so much to ordinary or normal as to extraordinary or exceptional causes. These latter, in the case of Christmas Island, are the storms which, during the rainy season, blow occasionally from the northern quarter, and it is after these, or sometimes even after a few days’ steady breeze from this direction, that birds of passage, dragon-flies, various moths and butterflies, and other insects reach the island. It is no doubt, therefore, to these occasional northern winds and storms, that by far the greater number of the species of plants and animals owe their introduction, and, indeed, considering that new arrivals were observed after nearly every gale, it seems rather remarkable that a greater number of forms have not gained a permanent footing. In the case of the birds most of the newcomers were migrants coming south to avoid the northern winter, and would not, in any case, be likely to remain permanently ; the rails, of which at least two species were seen, would probably find it impossible to breed in the island on account of the rats. Several of the species recorded were only represented i 1 «¢Tgland Life,’’ 2nd ed., p. 261. 302 | Christmas Island. by single individuals, which were picked up in a dying condition ; this was the case with the specimens of Chalcococcyx basalis and of Hirundo gutturalis. Since I left the island several individuals of a black and white fruit-pigeon (Myristicivorus bicolor) have been observed on the island, and I heard reports that similar cases had occurred previously; but it seems unlikely that this species could become a permanent inhabitant, for it would probably come into direct competition with the native fruit-pigeon, which itself sometimes dies in large numbers for want of sufficient food and water. Several other birds, of which I did not obtain specimens, have been observed. Mr. Andrew Ross told me he had shot a small duck and that a fishing hawk had been seen on the coast. I myself saw a number of white-lheaded swifts which remained for some days. Whatever the reason may be, it is certain that for an extremely long period of time no bird has become a permanent denizen of the island, for all the land birds which breed there are peculiar species, whose ancestors must have arrived long ago. It should be noted, moreover, that according to Mr. Lister, who has ably discussed the geographical relations of the Christmas Island birds [5], they are more nearly related to Austro-Malayan than to Javanese types. This circumstance may be accounted for by supposing that when their ancestors reached the island different meteorological conditions prevailed, or that they may owe their introduction to some other cause, e.g. drifting on rafts of floating trees such as not uncommonly occur in these seas. Of the insects the dragon-flies, which arrive in swarms, usually disappear in a few days, most likely because of the absence of standing water. The butterflies and moths were generally much battered during their transit, and it can only rarely happen that the conditions necessary for their establishment as permanent inhabitants are fulfilled. Of the other less conspicuous insects it is impossible to speak, because I was unable to distinguish the new arrivals from the natives, but no doubt many species must from time to time be blown across from Java during these gales. Of the plants, according to Mr. Ridley [8], very few are introduced by the wind, the most important being the various Cryptogams, of which the small spores are easily blown long distances; orchids, of which the seeds are very small; Hoya and Blumea, the seeds of which are plumed; and to these perhaps may be added Berria and Dipterocarpus, the winged fruits of which are sometimes carried high into the air and may be blown long distances. The ocean current which passes the island is the equatorial drift, which comes down from the Timor Sea and receives tributaries through the Straits between the islands of the Archipelago (Bali, Lombok, etc.). It is to the transport of rafts of trees by this current that the rats, the fruit-bat, and possibly some of the land birds, very probably owe their introduction to the island, and this circumstance would account for the similarity of many of them to Distribution of Fauna and Flora. 303 Austro-Malayan forms. Some at least of the Reptilia and Land Mollusca no doubt reached the island by the same means. In the case of the plants this means of transport is perhaps the most important of all, as is shown by the very large number of species which have seeds capable of resisting long immersion in sea-water. To this division belong most of the sea-loving trees (e.g. Calophyllum, Hibiscus, Scevola, Cordia, etc.), as well as many of those found in the forests generally (e.g. Barringtonia, Cryptocarya, Inocarpus, Ochrosia, etc.). Many of the smaller plants also may have been introduced by this means either as seeds or perhaps, in the case of epiphytic plants, attached to floating trees. Several other means by which plants may reach an oceanic island are excellently illustrated in the flora of Christmas Island. Thus a considerable proportion of the trees bear fruits which are eaten by the pigeons and other birds, and may have been brought across the sea by them. It is by no means necessary that the birds themselves should survive in order that the seeds may get a footing,’ so that from time to time plants may have been intro- ‘duced by species of birds which are not now found in the island. Another mode of distribution is by seeds and fruits, which, either by means of a sticky secretion or by hooks, can cling to the plumage of birds. Several species have no doubt been introduced in this manner, the most notable being Pisonia, the fruits of which are extremely sticky, and sometimes clog the feathers of the sea birds to such an extent as to impede their movements. The plants and animals already introduced by man are referred to on p. 20, but considerable additions to these will no doubt quickly follow. In the case of plants especially the reduction in the number of rats near the settlement will render possible the cultivation of many species which hitherto have been destroyed before the fruits could ripen. The following table consists of a list of the species of animals and plants at present recorded from Christmas Island, together with their distribution or, in the case of peculiar species, the distribution of their nearest allies. Species peculiar to the island are marked ‘x’ in the first column, and the regions in which their nearest allies occur are indicated in the succeeding columns by numbers distinguished by an asterisk; in the case of species not peculiar to the island the same numbers are employed without the asterisk. The geographical divisions adopted are those employed 1 See Clement Reid, ‘‘ Origin of the British Flora,’’ p. 30, 1899. 304 Christmas Island. by Wallace in his ‘‘ Distribution of Animals,’ and the numbers refer to his subdivisions of those areas, as follows :— (@) OrrentaL Recion. 1. Hindostan. 2. Ceylon. 3. Indo-China. 4. Indo-Malaya. (6) AustRattan Reeton. 1. Austro-Malaya. 2. Australia. 3. Polynesia. 4. New Zealand. (c) Erutopran Reeion. 1. East Africa. 2. West Africa. 3. South Africa. 4, Madagascar. In the last column the occurrence of species in localities other than those indicated in the preceding columns is noted, and various remarks are appended. ‘The whole of the regions in which a species or its allies occur are not in all cases mentioned, but as far as possible the district nearest to Christmas Island in be they are found is noticed. MAMMALIA. Pteropus natalis ... Pipistrellus murrayr trichura... Mus nativitatis Mus maclearr AVES. | Carpophaga whartoni | Myristicivorus bicolor Chaleophaps natalis Limnobenus fuscus Anous stolidus Glareola orientalis Charadrius dominicus | Ochthodromus geoffroyt Numenius variegatus | Heteractitis brevipes Tringoides hypoleucus - Calidris arenaria ... Limonites ruficollis Gallinago sthenura Demiegretia sacra... Fregata aquila Fregata ariel Sula sula ... Sula abbotti Sula piscatrix : | Phaethon rubricauda | Phaethon fulvus... Astur natalis Ninox natalis Collocaha natalis ... Chalcococcyx basalis Motacilla melanope Motacilla flava \ Crocidura fuliginosa, var. 300 ged = = pee a | eS ca 3 ee |e ls x eae *] x var. x 3 x BP, meat x ¥4 *] | x oe coal Us 3, 4 1 % F1525/3,4| ° *1 19,34 1 I, 3; 4 DZone x *] x ad ae x aah 4 1, 2 Ethiopian gion. Re FAUNA OF CHRISTMAS ISLAND. LIST OF SPECIES. Various localities and remarks. Lombok. Allies widely distributed. Tropical and sub-tropical seas. Migrant wintering in Malay Archipelago and Australia. Ditto. Ditto. Ditto. Ditto. Migrant wintering in 8. Africa, India, and Australia. Nearly cosmopolitan. Migrant wintering in Burmah, Malay Archipelago, and Australia. Migrant wintering in India and Malay Archipelago. Tropical and sub-tropical oceans. Indian and Pacific Oceans. Tropical and sub-tropical oceans. Assumption Island. Tropical and sub-tropical oceans. Tropical regions of Indian and Pacific Oceans. Other localities unknown. Palearctic in summer, going south in winter. Ditto. 306 Zosterops natalis .w.. Merula erythropleura Hirundo gutturalis REPTILIA. Gymnodactylus marmoratus Gecko listert Lygosoma atrocostatum Lygosoma nativitatis Ablepharus egerie Typhlops exocet ... LAND MOLLUSCA. Lamprocystis normani Lamprocystis mabele Lamprocystis mildrede Succinea solidula ... Succinea solitaria ... Succinea listert Opeas subula Pythia scarabeus ... Melampus luteus ... Melampus fasciatus Melampus castaneus Leptopoma mouhoti Truncatella valida Assiminea andrewsiana ... LEPIDOPTERA RHOPALOCERA. Limnas petilia Vadebra macleart... ae Melanitisismene, var. deter - minata ... ace Charaxes andrewst Junonia villida Hypolimnas misippus Hypolimnas nerima, var. listert Nacaduba aluta Terias amplexa LEPIDOPTERA PHALAN A. Euchromia horsfieldi Nola distributa Deiopeia pulchella Argina cribraria ... 5 Peculiar to the Island. 4: bd MMs var. xX Christmas Island. Oriental Region | : 3 a |e¢ . & ep ek = Various localities and remarks. | 5 fan} < es} | al cs Nests in N.E. Asia; migrates as farsouthas Australia in winter. <1 1 ae ... | Allies widely distributed. #1, #2, *3 *1,2,3 *1,2,3 ck Habitat previously unknown. Allies widely distributed. bias EL Ditto. “ns ... | Probably introduced. Us 1,2. 3 198 3 iN 3} ... | Allies Oriental. 2 Mes Wide range. il 2 1 . Allies widely distributed in Asiaj and Africa. 1 4 ... | Old World. 1 4 List of Species. 307 Various localities and remarks. Peculiar to the Island. Oriental Region Australian Region Ethiopian Region i | LEPIDOPTERA, continued. | Mimeusemia econia Ba es *4 | Dipterygia vagivitta oe 3, 4 _ Amyna selenampha ale Wenctemie idea os Jee 3, 4 _ Amyna octo a4 bie oe a ae .... | “Eropies: , | Prodenia littoralis seat’ ices Jn .-. | «| Mediterranean sub-rezion, tropics, sub-tropics. Leocyna tibialis ... Fos aes jes 1, 3 | Armactia columbina Be Ms a3 2 Brana calopasa ... ess ae 2 1 _Patula macrops ... Bae ae 1, 25 | Ophiusa honesta ... oc eee (lela) Or, 14 Ophiusa coronata ... ae ee ea oo, 4 2 Ophiusa serva... ie Ore He 2 Be 4 Bocula limbata ... she x 3 1,2,3,4 _ Acantholipes similis Ses ae 1, 4 Thermesia rubricans ehhh tee | ete, 4 1,3 11,2,3;4 Ophideres salaminia Pa aati eBay ae tol 2; 4 Ophideres ancilia .. me Bee 1 25°38 Ophideres fullonica ie He Le 2s Oy. Ty Ze) a) P28 _ Ophideres materna ¥ 3: i, its .... | Tropical Africa. Cosmophila erosa ... baa I fan Le = ... | Widely distributed. | Cosmophila vitiensis aad 3 | Hutelia delatrix ... a... Sek D2, oy4 2 Stictoptera describens ... aaa 2,4 Hydrillodes vexillifera ... x } Maliattha signifera ee. sos | Leer 2 Rs Hrastria griseomixta Sty x — Tarache olivacea ... Oe ie 2: arias chromataria aes wan 1, 2.3, 4 de 1, 2,3 Porthesia pulverea aae x *4, Orgyia postica i. an sys 1, 2, 3, ; 9 Cherocampa erotus au au 3 herocampa vigil Beet sleds, are heretra lucasi ... ‘ ae ARS 2S T2438 mer bo ee No (Jt) Li) (JN) bo bo & bo Lo Japan. 2,3 | Specimens of a type recorded only from 8. Africa. Pseudosphinx discistriga .. Pephonodes hylas .. Lr PP PRL LP A E yperythra lutea... Le 2, aed, 28 Asplenium centrifugale ... < Nephrodiwn syrmaticum ... 1, 4 Nephrodiwn dissectum eet 1, 4 3 4 Nephrodium intermedium he 1,4 1 ise Japan. Nephrodium truncatum 1, 4 2,3 Nephrodiwn poiymorphwn ed 1,4 1 Aspidium membranaceum... ae 2, 3, 4 Nephrolepis exaltata A Wie i ee .... | Tropics generally. Nephrolepis acuta... ae sf ae fy ae Ditto. Nephrolepis ramosa Bt ae aoe tes oe Ditto. Polypodiwmn adnascens wae Lae 148 ea Polypodium irioides Sap ah 1, 3, 4 Qa touls yee Vittaria elongata .. Ae sie 1, 3, 4 1, 2,.0 21,2 Acrostichum “fagellifer um 56: 1, 4 Acrostichwn listert sixis x Lycopodium phlegmaria ... ee ae _ a Tropics of Old World. Mosszs. Leucobryum chlorophyllosum | ... 4 1 Octoblepharum albidum ... | ... Als ud ios | Lropies. Thyridiwn fasciculatum ... ae 1, 4 3 4 Chile. Trachymitrium revolutum 4 Neckera lepiniana... A sae 4 Thuidium plumulosum ... Her 2, 4 3 Hypnum montagner £ Hepatic. Ptychanthus squarrosus ... wet 4 1 LICHENS. Parmelia tinetorwn om aE dae we vee Widely distributed, Asia, Attion, i Australia, ete. Parmelia appendiculata ... au ash ete 1 Physcia picta sd a we eee en a Very widely distributed. | Pyxine sorediata ... Eee AD cca cu x ... | Africa, S. America, Japan, | Tahiti. | Pannaria rubiginosa seal Py and Se ... | Very widely distributed. Lecamora varia ... ty Lx Be a a Ditto. Ramalina fraxinea SRS tea 2 2s ie ... | Europe, N. and S. America. Lecidea lutea na a oe ee ... | Very widely distributed. Leptogium phyllocar pum .. oe e Be ee: Ditto. List of Species. ol7 CRYPTOGAMS, continucd. Funct. Schizophyllum commune ... Polyporus confluens Fomes lucidus Fomes australis Polystictus flabelliformis y Polystictus xanthopus Polystictus liteo-olivaceus Polystictus sanguineus Hexagonia polygramma Daedalea tenuis ... _ Fawolus boucheanus Laschia cespitosa ... Hirneola polytricha | Hirneola auricula-jude | Guepinia sparassoides Cyathus montagner | Geaster andrewsi ... Trichoscypha tricholoma ... | Stilbum javanicun Mycerozoa. Stemonitis splendens, Rost., var. a, genuina Arcyria flava, Pers. | Lycogala miniatum, Pers. Peculiar to the Island. Oriental Region. i Australian Region. Ethiopian Region. Various localities and remarks. Cosmopolitan. Europe and N. America. Cosmopolitan. Europe, Venezuela. S. America, Cuba. Tropics generally. America. Central America. Europe and N. America. Mexico, Cuba. Widely distributed. Cuba, S. America. S. America, West Indies. Europe, America. Europe, N. America. Europe, N. and S. America. LIST OF THE PRINOIPAL PAPERS RELATING TO 20. 21. CHRISTMAS ISLAND. . Dampier’s Voyages. Edition 1829, vol. i, p. 472. London. . A Voyage to and from the Island of Borneo in the East Indies, ete. By Capt. Daniet Berkman. London, 1718. (See Pinkerton’s Voyages, vol. xi, p. 103.) . Report on a Zoological Collection made by the Officers of H.M.S. ‘‘ Flying Fish’? at Christmas Island, Indian Ocean. Proc. Zool. Soc., 1887, p. 507. (This includes the report of Captain J. P. Maclear, of H.M.S. ‘“ Flying Fish,”’ on the visit to the island, and descriptions of the collections by Dr. A. G. Butler, Dr. R. B. Sharpe, O. Thomas, G. A. Boulenger, HE. A. Smith, R. I. Pocock, C. O. Waterhouse, F. J. Bell, and A. Dendy.) . Report on Christmas Island (Indian Ocean), H.M.S. ‘‘ Egeria,” 1887. By Captain Petuam Aupricu. (With map.) (Admiralty Reports.) . On the Natural History of Christmas Island in the Indian Ocean. By J. J. Lister, M.A., F.R.S. Proc. Zool. Soc., 1888, p. 512. (This is accompanied by reports on the collections by O. Thomas, G. A. Boulenger, E. A. Smith, C. J. Gahan, A. G. Butler, W. F. Kirby, and R. I. Pocock.) . Report on the Botanical Collections from Christmas Island, Indian Ooean, made by Captaim J. P. Maclear, Mr. J. J. Lister, and the Officers of H.M.S. ‘‘Egeria.” By W. Borttnc Hemstey. Journ. Linn. Soc. (Botany), vol. xxv (1890), p. 351. . Account of Christmas Island (Indian Ocean). By Rear-Admiral Sir W. J. L. Wuarton, F.R.S. Proc. Roy. Geogr. Society, vol. x (n.s.), 1888, p. 613. . A Day at Christmas Island. By H. N. Ripiey, F.L.S. Journ. Straits Branch Roy. Asiatic Soc., p. 123, June, 1891. (This paper is accompanied by a list of the plants and animals known from the island at that date.) . Report on Christmas Island. By Rear-Admiral Sir W. J. L. WHarrton, F.R.S., and Captain J. P. Mactzar. Nature, vol. xxxvi (1887), p. 12. . Note on the Flora of Christmas Island. By Sir W. T. Tu1setton-Dyzr, K.C.M.G., F.R.S. Nature, vol. xxxvi (1887), p. 78. . Presidential Address, Section D, Bath Meeting of British Association, 1888, p. 690. By Sir W. T. Tutsetton-Dyer, K.C.M.G., F.R.S. . Letter relating to Christmas Island. J. J. Lister, F.R.S. Nature, vol. xxxvil (1888), p. 203. . Letter relating to Christmas Island. Rear-Admiral Sir W. J. L. WHarron, F.R.S. Nature, vol. xxxvii (1888), p. 204. . Letter relating to Christmas Island. H. B. Guppy. Nature, vol. xxxvii (1888), p. 222. . Die Theorieen iiber Wie Entstehung der Koralleninseln und Korallenriffe. By R. Lancensecr. Leipzig, 1890, p. 136. . Description Géologique de Java et Madoura. By R. D. M. Verseex and R. FennEMA (1896), vol. ii, p. 1031. . Straits Settlements. Papers relating to the Cocos-Keeling and Christmas Islands, 1897. (Parliamentary Papers, C 8367.) . Colonial Reports. Annual, No. 216. Cocos-Keeling and Christmas Islands. Report on the Annual Visit for 1897. (1897, C 8650-14.) . Colonial Reports. Annual, No. 257. Coeos-Keeling and Christmas Islands. Report on the Annual Visit for 1898. (1899, C 9046-25.) A Description of Christmas Island (Indian Oeean). By C. W. AnpReEws. Geogr. Journ., vol. xiii (1899), p. 17. (With map.) Notes on a Collection of Gephyrean Worms found at Christmas Island (Indian Ocean) by Mr. C. W. Andrews. By A. E. Surpiey, M.A., F.R.S. Proc. Zool. Soc., 1899, p. 54. (Papers on the Marine Mollusca, Sponges, Corals, and Foraminifera will appear later in Proc. Zool. Soc. for 1900.) PP PEND x A small collection of birds and insects made by Mr. Hugh Ross since I left the island has recently reached England. The species are nearly all described above, but there are two birds and one beetle new to the island, and also a beetle that is new to science.— eWeai A. ; The birds are :-— AVES. COLUMBIFORMES. Myristicivorus bicolor. Adult male. Flying Fish Cove, February 4, 1899. Several individuals of this species were observed; probably they had been blown to the island during migration. CHARADRIIFORMES. Heteractitis brevipes. Female. Flying Fish Cove, September 22, 1898. INSECTA. The beetles are described below by Messrs. Waterhouse & Arrow. ? Crioceris impressa, Fab., var. A single example sent to Mr. Andrews may provisionally be regarded as a variety of C. impressa, Fab. The body underneath, the head (except at the occiput), legs, and antenne are black, the prothorax and elytra testaceous. The prothorax has a rather distinct transverse impression just a little in front of the base, and this is the only character of importance to suggest the specific distinctness of this new form. 320 APPENDIX. C. impressa is a variable and rather widely distributed species, occurring in most of the Indo-Malayan islands, and in India, Burma, and China. Phileurus convexus, Arrow, sp.n. P. nitidus, angustus, haud depressus; capite rugose punctato, acuminato, fronte cornu parvo conico armata; prothorace sub- quadrato parum transverso, angulis posticis fere rectis, anticis parum approximatis, disco leviter punctato, lateribus paulo crebrius, medio antice et postice carine vestigiis vix apparentibus ; elytris longis, grosse lineato-punctatis, interstitiis minutissime punctatis; abdomine cum pygidio fere polito, propygidio coriaceo. ? Jong. 144 mm. lag Hab.—F¥F lying Fish Cove. This new species is formed for the first representative of the important family Dynastide so far found in the island, a single specimen having been recently discovered by Mr. H. Ross. This species is less flattened, and somewhat longer than usual, but does not differ structurally from the larger described forms of Continental Asia, where all its hitherto known allies are found, for the Ceylon insect described by Walker is evidently wrongly placed. M. Fairmaire has referred to a ‘P. javanus,’ apparently the Heteronychus javanus, Burm., which although allied is hardly congeneric. But the genus Phileurus will probably be eventually restricted to the American insects and new genera formed for the Oriental species. The only other insect new to the island is a large moth: Patula macrops (Linn.), (Syst. Nat., 12th ed., i, p. 225). Africa, Madagascar, Ceylon, India, Burmah. INDEX. abbotti (Sula), 44, 299. abdominalis (Dactylosternum), 90. Abelmoschus, 1738. — (Hibiscus), 173. Ablepharus, 51, 53. abramus (Pipistrellus), 26. Abutilon, 172-3. acaciaria (Boarmia), 70. Acalypha, 188. Acanthacee, 184. Acanthastrea, 207, 218. Acantholipes, 67. Accipitriformes, 46. acervalis (Planorbulina), 241, 249. (Planorbulina), near, 234. Achatina, 57. Achyranthes, 186. Acicnemis, 112. Acidaliane, 71. acidula (Pemphis), 178. ackeringze (Ochrosia), 182. Acronychia, 174. acrophyla (Pericheta), 169. Acrostichum, 198. Aculeata, 81. acuminata (Protetia), 98. acuminatum (Combretum), 178. acuta (Nephrolepis), 195. adjectella (Nigilgia), 77. ————— (Phycodes), 77. adnascens (Polypodium), 195. eenusalis (Epicrocis), 73. Xgocidnus, 124. JKschna, 139. /Eschnidee, 139. /Aschnine, 139. /Ethus, 127. affinis (Hxamfies), 122. (Nogodina), 134, 136. (Ricania), 134. Agaristide, 64. Ageratum, 180. agelutinans (Quinqueloculina), 236. aglaodesma (Cosmoclostis), 76. agrotus (Megapenthes), 101. alba (Datura), 184. albidum (Octoblepharum), 196. alemene (Hypolimnas), 62-3. aldrichii (Hoya), 182. alecto (? Larrada), 84. ? (Notogonia), 84. alienus (Conocephalus), 149. Allophylus, 176. Alphitobius, 106. aluta (Nacaduba), 60, 63. Alveolina, 252, 255. alveoliniformis (Miliolina), 244, 246, 248, 252. Amarantacez, 186. Amarygmus, 107. Amaryllidacez, 191. amboinensis (Sponia), 188. americana (Blatta), 145. (Periplaneta), 142, 145. americanus (Gyrocarpus), 178. ‘¢ Amethyst,’’ Visit of H.M.S., 2. ammonilla (Berria), 173. amooroides (Dysoxylon), 175. Ampelidee, 176. amphibius (Arvicola), 30. Amphistegina, 229, 232, 235, 237, 239-42, 244, 246-7, 249-56, 266, 268. Amphistegine, 253. amplexa (Terias), 60, 63. Amyna, 65. Anax, 139. 240, 242, | Anchastus, 100. ancilla (Ophideres), 67. Andreninz, 81. andrewsi (Acicnemis), 112. ————- (Acronychia), 174. ————_ (Charaxes), 61. (Chrysobothris), 99. (Coeloria), 207, 209, 212. (Coscinarza), 207, 221. (Geaster), 199. (Halictus), 86. (Issus ?), 138. (Megapenthes), 101. (Orychodes), 117. ——— (Panicum), 192. —_——— (Protetia), 98. ——— (Rhyncholobus), 111. -—_——— (Sessinia), 107. andrewsiana (Assiminea), 54, 59. Y 322 andrewsiana (Orbitoides), 256. (Orbitoides, Lepidocyclina), 255-6. Anechura, 142. angustiflora (Ochrosia), 182. Anisoccenia, 207-8, 220-1. Anisolabis, 142-3. Anisomeles, 185. Annexation of Island, 19. anomala (Mantibaria), 82. Anous, 39. Anthophila, 81. Anthribide, 118. antillarum (Heterostegina), 229. antilope (Toxicum), 106. Apatenia, 119. Apetale, 185. Aphanocephalus, sp., 96. Aphodiide, 97. Aphrophoride, 137. apicalis (Apatenia), 119. Apide, 81. Apocynacez, 182. Apomecyna, 128. Appearance of Island from sea, 3. appendiculata (Parmelia), 197. aquila (Fregata), 42. arabica (Cceloria), 213. Arachnida, 1538, 156. Distribution of, 300. Areocerus, 120. Araliacee, 179. Aranez, 158. Araneus, 162. arborescens (Panicum), 193. archytas (Saccolabium), 191. Arctiane, 64. Arcyria, 200. Ardea, 41. Ardeiformes, 41. Ardisia, 181. arenaria (Calidris), 41. Arenga, 50, 191, 287. arenosa (Porites), 224. argentea (Celosia), 186. —__—_——— (Tournefortia), 182. Argina, 64. Argiope, 159. Argiopide, 159. Ariadna, 158. ariel (Fregata), 44. Ariophanta (Microcystis), 55-6. aristella (Bidis), 136. Armactia, 66. armata (Pericheta), 170. armatus (Megascolex), 170. Aroidez, 192. Arvicanthis, 36. Arvicola, 30. Asclepiadacee, 182. INDEX. Ascomycetes, 200. asiatica (Colubrina), 175. asiaticum (Crinum), 191. asiaticus (Gyrocarpus), 178. Asilide, 88. aspera (Achyranthes), 186. asperula (Spiroloculina), 233, 248. Aspidiphorus, 104. Aspidium, 195. Asplenium, 194. assimilis (Dryophthorus), 116. Assiminea, 54-5, 59 Asterocyclina, 253. Astrea, 214-5, 219. Astreide, 210. Astroria, 212-13. Astur, 46. Asystasia, 184. atrocostatum (Lygosoma), 51-2. attenuatus (Nirmus), 138. auberiana (Miliolina), 250, 252. —- (Quinqueloculina), 250. auricula-jude (Hirneola), 199. auritincta (Dichocrocis), 74. auritum (Abutilon), 172. australasice (Hormurus), 156. (Scorpio), 156. australis (Fomes), 198. azedarach (Melia), 174. baculatus (Tinoporus), 229. balder (Polistes), 85. balyi (Psylliodes), 127. banksi (Prosoplus), 123. Barringtonia, 178. basalis (Chalcococcyx), 48, 299, 302. (Olenecamptus), 122. Basalt, 273, 276-7, 279, 283, 285. Basic glass, Breccia of, 278-9. Basidiomycetes, 198. Batavia, 3. Beaches, 6. Beekman, Captain Daniel, Account of Island by, 2. belli (Porites), 207, 223. Berria, 173, 184. beyrichi (Bolivina), 231. bicolor (Myristicivorus), 299, 302, 319. bicornis (Miliolina), 247. (Serpula), 247. Bidis, 136. biflora (Wedelia), 181. biflorum (Solanum), 183. bilobus (Olenecamptus), 122-3. binghami (Halictus), 86. Birgus, 164. Habits of, 165. birmanicus (Chelifer), 157. INDEX. 323 bispinosus (Mecopus), 113. bisulcus (Chelifer), 157. Blatta, 145-6. Blattide, 142, 145. Blowholes, 8 Blumea, 181. Boarmia, 70. Boarmine, 70. Bocula, 66. Boehmeria, 190. Boerhaavia, 185. Bolivina, 231, 266. Bombylide, 88. bonducella ae 177. Booby, 44. Boraginee, 182. Borneo, Orbitoides of, 297. Bostrichide, 105. Bostrichus, 116. Bothrideres, 94. bottai (Ceeloria), 213. boucheanus (Favolus), 199. boueana (Truncatulina), 228. boutonii (Ablepharus), 53. bowringi (Demotina), 126. Brachyrhynchide, 129. Brachyrhynchus, 129. Bradymerus, 106. Brana, 66. Brenthia, 76. Brenthide, 117. brevicornis (Pocillopora), 209. (Pocillopora), aff., brevipes (Heteractitis), 319. brevis (Pericheta), 168. brunnea (Labia), 145. brunnensis (Uvigerina), 234. buccinus (Halictus), 86. budde (Megachile), 88. bufa (Oxypleura), 128. Bulimus, 57. Bull-dog Rat, 30. —_—— (Globigerina), 227, 234, 240, 250, 252-3, 255, 2 Buprestide, 99. buxifolia (Ehretia), 182. Bythoscopus, 138. Ceenognosis, 79. Cerostris, 160. cespitosa (Laschia), 199. Cajanus, 177. Calidris, 41. Callicarpa, 184. Calonyction, 183. calopasa (Brana), 66. Calophyllum, 172. calypso (Oxypleura), 130. —— (Peecilopsaltria), 130. 207, 209. Cambalide, 156. Camponotus, 81, 83. Camptorhinus, 112. Canavalia, 177. Cancer, 165. candida (Deiopeia), 64. capitata (Carpenteria), 246. ————. (Goniastrea), 214. Capparidee, 171. Carabide, 89. Caradrinie, 65. carbonaria (N yctobates), 106. Cardiosoma, 10, 163. caretta (Thalassochelys), 5 carinatifolius (Sar aba 191. carneola (Cyprea), 208. carnifex (Cancer), 164. (Cardiosoma), 164. Carpenteria, 233, 235-41, 244, 246-7, 250, 252, 254-5, 266. Carpophaga, 37. Cassia, 177. castaneiceps (Mecistocephalus), 155. castanella (Doloessa\, 72. castaneus (Lispinus), 90. (Melampus), 54, 58. catappa (Terminalia), 177. caudatus (Croton), 188. Celastrinex, 178. Celastrus, 175. celata (Planispirina), 242. (Sigmoilina), 242. (Spiroloculina), 242. celebensis (Mus), 32. Celosia, 186. celosioides (Deeringia), 186. Celtis, 188. Centipedes, Introduction of, 21. Central plateau, 11. ——— and hills, Geology of, 288. centrifugale (Asplenium), 194. cephalonica (Corcyra), 72. Cephonodes, 70. Cerambycide, 121. ceramensis (Prinobius), 120. ceratophthalmus (Cancer), 164. —— (Ocypoda), 164. Cerbera, 182. Ceresium, 121-2. Ceriopora, 229. Cerithium, 204. cessaria (Boarmia), 71. Cetoniide, 98. Cheerocampa, 69. Cherocampine, 69. Chalcococcyx, 48, 299, 302. Chalcophaps, 39. Chalk-like rock, 13. ‘¢Challenger’’ Report on Deep - sea Deposits, 279, 291. 324 Charadriiformes, 40. Charadrius, 40. charantia (Momordica), 179. Charaxes, 61. Chelifer, 156-7. Cheliferide, 156. Chelisoches, 143. Chelone, 54. Chilopoda, 153-4. ——_—— Distribution of, 300. Chinese coolies, 20. chlorolepis (Tortricomorpha), 78. chlorophyllosum (Leucobryum), 196. Christmas Island, Position of, 1. chromataria (Karias), 69. Chrysobothris, 99. Chrysodema, 99. chrysomelina (Epilachna), 96. Cibicides, 251. Cicadide, 130. cinerosella (Euzophera), 73. cinnamomea (Celtis), 188. Cioide, 105. circinalis (Cyeas), 193. circularis (Miliolina), 252. Cissus, 176. citrifolia (Morinda), 180. Claoxylon, 188. clathrata (Rotalia), 232. clathratus (Bradymerus), 106. claviger (Chelifer), 156. (Trachychernes), 156. Cleidion, 188. Climate, 17. -Clitumnus, 142, 147. Clovia, 137. Clunies Ross, Mr. A., 19. Mr. G., 3, 19. Mr. S., Explorations by, 20. clypeatus (Cancer), 165. — (Ceenobita), 165. coarctata (Orthomorpha), 155. coarctatus (Paradesmus), 155. cobbe (Allophylus), 176. Coccinellide, 95. Coccyges, 48. Cocos- Keeling Islands, 1, 3, 298. — Ceeloria, 207, 209, 212-14. Coenobita, 165. Ceenobitide, 164. coffeze (Arzocerus), 120. Coleoptera, 89. Collocalia, 48. Colubrina, 175. columbina (Armactia), 66. columnata (Orbicella quadrangularis, var.), 207, 216. Colydiide, 94. Combretacez, 177. Combretum, 178. INDEX. commune (Schizophyllum), 198. complanata (Ardisia), 181. Composit, 180. Composition of phosphates, 291. compositus (Oplismenus), 193. compressiuscula (Rotalia papillosa, var.), 238. concimnula (Psammeecus), 95. confinis (Cephnodes), 70. confluens (Polyporus), 198. confluentus (Odynerus), 85. congesta (Phreatia), 190. conglobata (Globigerina), 234, 250.. conglomerata (Porites), 222. Conocephalide, 142, 149. Conocephalus, 149. convexus (Phileurus), 320. Convolvulacee, 183. Convolvulus, 183. conyzoides (Ageratum), 180. Coraciiformes, 48. Corals (fossil), 206. Corcyra, 72. Cordia, 182. cordifolia (Espera), 173. - cornaria (Boarmia), 70. coromandeliana (Asystasia), 184. coronata (Ophiusa), 66. Corymbis, 191. Coscinarza, 207, 221. Cosmoclostis, 75. Cosmophila, 67. Cossonide, 114. Cossonus, 114. coxalis (Prinobius), 120. Crabronide, 81. Craspedia, 71-2. ———_ pp., 72. crassisepta (Anisoccenia), 220. crenulata (Laporta), 189. Cretaceous rocks, 298. eribraria (Argina), 64. crinipes (Camptorhinus), 112. Crinum, 191. Crioceris, 319. Cristellaria, 227. Crocidura, 22, 27. Croton, 188. crumenatum (Dendrobium), 190- Cryptocarya, 187. Cryptophagide, 95. Cryptopide, 154. Cryptops, 154. Cucujidee, 95. Cuculi, 48. Cucurbitacee, 179. Cudrania, 189. Culicide, 88. cunninghamii, 187. curcas (Jatropha), 188. INDEX. 32% Curculionide. 108. Cyanide, 127. cyanops (Sula), 44. Cyathus, 199. Cycadez, 193. Cycas, 193. Cycloclypeinz, 229. Cycloclypeus, 237. Cyclosa, 160-1. cylindricus (Pachyops), 115-16. Cylindrodesmide, 155. Cylindrodesmus, 155. eymosa (Fimbristylis), 192. Cyperacee, 192. Cyprea, 208. Cypseli, 48. Cyrtacanthacris, 142, 151-2. Cyrtophora, 160. Dactylosternum, 90. Daedalea, 199. Dales on west coast, 14, 283. Dampier, Description of Island by, 1. danz (Montipora), aff., 207, 209, 224. Datura, 184. Davallium, 194. decumanus (Mus), 29, 35-6. Deeringia, 186. Deiopeia, 64. dejecta (Ruellia prostrata, var.), 184. dejectus (Dipteracanthus), 184. delatrix (Eutelia), 68. delicata (Paurostauria), 133. delicatula (Mzandrina), 212. Delphacide, 136. Demiegretta, 41. Demotina, 126. Dendrobium, 190. Dendroneura, 80. densiflora (Randia), 179. depressa (Heterostegina), 229, 232, 235, 237, 239-41, 244, 246-9, 252-5. depressus (Palorus), 106. Dermestes, 95. Dermestide, 95. describens (Stictoptera), 68. determinata (Melanitis), 61. (Melanitis ismene, var.), 61. Dicasticus, 111. Dichelia, 78. Dichocrocis, 74. Dicliptera, 184. Dicotyledons, 171. Dictis, 159. diffusa (Boerhaavia), 185. Digitaria, 192. digitata (Ipomeea), 183. dimidiata (Platylabia), 142. ——— (?) (Platylabia), 143. Or diminuta (Lobopelta), 83. (Ponera), 83. Dinoderus, 105. Diplopoda, 1538, 155. —_ Distribution of, 300. Diploptera, 81. Diptera, 88. Dipteracanthus, 184. Dipterygia, 65. discistriga (Pseudosphinx), 70. Discocyclina, 229-30, 253-4, 256. Discocycline Orbitoides, 283. discoidalis (Anchastus), 100. (Piezonotus), 110. ———— (Rhyncholobus), 110. Discorbina, 240, 252. dispansa (Orbitoides), 230, 248, 254. ———— (Orbitoides, Discocyclina), 229-30, 254. (Orbitolites), 230. dispansus (Lycophris), 229-30. dispar (Hierodula), 142, 146. disparilis (Cyrtacanthacris), 142, 151-2. dissecta (Davallium), 194. dissectum (Nephrodium), 194, distinctus (Pholcus), 159. distributa (Nola), 64. Ditoma, 105. doleschallii (Argiope), 149. Dolichopodide, 88. Doloessa, 72. Dolomitic limestones, 265, 289. Dolopius, 100. dolosus (Melanoxanthus), 101. Domestic animals, 20. dominicus (Charadrius), 40. doriz (Camptorhinus), 113. Doritis, 191. Dragon-flies, Arrival of, 17, 302. Dryinine (?), 81. Dryophthorus, 116. dubia (Globigerina), 240. (Prionastrea), 220. dubium (Opatrum), 106. (Phlceophagosoma), 114. duplex (Orbitolites), 252. Dysderide, 158. Dysoxylon, 178. | Farias, 69. Earthquakes in Christmas Island, 298. Earth-worms, 300. echinata (Lobophyllia), 210. ——— (Mussa), aff., 207, 209-10. econia (Mimeusemia), 64. Ectadoderus, 147-8. edulis (Inocarpus), 177. Effuse, 192. «« Hgeria,”’ Visit of H.M.S., 2, 19. - 326 Egeria Point, 4, 14, 16, 293. — Miocene rocks at, 288. egeriz (Ablepharus), 51, 53. Ehretia, 182. elachista (Brenthia), 76. Elateride, 99. elateroides (Zooblax), 121. Eleusine, 193. ellipticum (Heptapleurum), 179. elongata (Vittaria), 196. elongatus (Pholcus), 159. —- (Smeringopus), 159. Elytrogonus, 111. Embrithes, 111. Emoa, 52. Encyocrypta, 162. Endotricha, 73. Endotrichine, 73. enganensis (Xenoceras), 115. ensiformis (Canavalia), 177. ensis (Psyra), 150. Entada, 177. Entomophaga, 81. Entoria, 147. Eocene (? Oligocene) Limestone, 226, OTL, 273.1983. Epacromia, 152. Epagoge, 78. Epalxiphora, 79. Epeira, 159-60. Ephestia, 72. ephippiger (Pontodrilus), 166. ephippioides (Orbitoides), 240, 251-2, 256, 264. ephippium (Orbitoides), 251. Epicrocis, 73. Epilachna, 95-6. Epiplema, 72. Epiplemine, 72. equisepta (Meeandrina), 201, 212. Eragrostris, 193. Erastria, 68. erosa (Cosmophila), 67. erotus (Cherocampa), 69. Erotylide, 96. Erythrina, 176. erythropleura (Merula), 49. erythropleurus (Turdus), 37, 49. Espera, 173. esperi (Astroria), 212 Euchromia, 64. Eucnemide, 99. Kugenia, sp., 178. Eumenide, 81. Eumolpide, 124. Euphorbia, 187. Euphorbiacee, 187. EKupleeine, 60. europzus (Isometrus) = maculatus, 154. Kutelia, 68. INDEX. Euxestus, 96. ; Euzophera, 73. everetti (Mus), 29, 31-2. exaltata (Nephrolepis), 196. Examnes, 122. excelsa (Pisonia), 185. exiguus (Aigocidnus), 124. eximia (Clovia), 137. exocceeti (Iulomorpha), 156. (Spirostreptus, Nodopyge), 156. (Typhlops), 51, 53. fascialis (Zinckenia), 74. fasciatus (Melampus), 58. fasciculatum (Thyridium), 196. Faults, 275. fausti (Rhabdocnemis), 113. Favastrea, 219. Favoidea, 221. favoidea (Anisoceenia), 207-8, 220- Favolus, 199. favosa (Pocillopora), 209. felinus (Dermestes), 99. Ferns, 194. ferox (Solanum), 183. ferussacii (Miliolina), 251. — (Quinqueloculina), 261. Ficus, 189. Figulus, 96. Filicine, 194. filograna (Meandrina), 213. Fimbristylis, 192. First inland cliff, 10. Geology of, 292. flabellatus (Tetrigus), 100. flabelliformis (Polystictus), 198. flagellatus (Xenoceras), 118. flagelliferum (Acrostichum), 196. flava (Arcyria), 200. (Motacilla), 48. flavescens (Libellula), 139. ———— (Pantala), 139. flavicostalis (Ricania), 133. —— (Varcia), 133. flavifrontalis (Ricania), 131. flavipalpis (Ectadoderus), 142, 147. flavirostris (Phaethon), 45. flavocephalus (Ophion), 82. Fleurya, 189. ‘¢ Flying Fish,’’ Visit of H.M.S., 2. Flying Fish Cove, 16, 29%. beach, 8. cliff, Structure of, 271 et seq. foliosum (Ischemum), 192. Fomes, 198. Food plants introduced, 20. Foraminifera, 226. Forcinella, 143. INDEX. Forficulide, 142. Formicaleo, 140. Formicine, 81. Fornax, sp. (?), 99. forskaeli (Cceloria), 213. Fossil Corals, 206. Mollusca, 201. Fossores, 81. fraxinea (Ramalina), 198. Fregata, 42. Fresh-water crabs, 10, 164. —— streams, 9, 10, 283, 285. Frigate-bird, Habits of, 42. Fringing reef, 4, 294. Fruit-bat, Habits of, 25. Fruits eaten by birds, 308. Means of transport of, 302-3. fuliginosa, var. trichura (Crocidura). 22, 27. fuliginosus (Sorex), 27. fullonica (Ophideres), 67. fulva ? (Temnopteryx), 142, 145. fulvus (Phaethon), 45, 299. funebris (Amarygmus), 107. Fungi, 198. Fungida, 221. fuscus (Limnobeenus), 39. fusilinea (Cyrtacanthacris), 151-2. gaimardi (Porites), 224. Galactia, 176. Galleriane, 72. Gallinago, 41. Gamopetale, 179. Gannet Hill, 12. Gasteromycetes, 199. Gaudryina, 236, 266. Geaster, 199. Gecarcinus, 168. Gecko, 51-2. Geckonide, 51. genuina (Stemonitis splendens, var.), 200 Geocarcinide, 163. Geocarcinus, 163. geoffroyi (Ochthodromus), 40. Geology of Island, 269. Geometride, 70. Geometrine, 71. Geophilide, 155. glabra (Pongamia), 177. glareola, 40. Glendinning Shoal, 1. Globigerina, 227, 234, 237, 240, 250, 252-3, 255, 265-6, 273. Globulus (Ceriopora), 229. —— (Gypsina), 229, 231-2, 237-8, 246-7, 250, 252, 254. (Gypsinus), 239. 327 Glyphodes, 74. (Phacellura), 74. Goniastrea, 207, 214. Goodenoviez, 181. Goos, Pieter, Map by, 1. Goshawk, Habits of, 47. gouldi (Pteropus), 24. gracilis (Psylliodes), 127. gramen (‘Textularia), 251. Graminez, 192. grandiflora (Ipomeea, Calonyction), 183. grandis (Nodosaria radicula, var.), 249. (Pisonia), 185. ——-- (Tectona), 184. granifera (Lampas), 203. (Ranella), 203. (Tutufa), 203. Grewia, 87, 174. griseigularis (Astur), 47. griseomixta (Hrastria), 68. grossepunctatum (Pentatoma), 128. Gryllacride, 142, 148. Gryllacris, 142, 148. Gryllide, 142, 147. Guepinia, 199. Guettarda, 180. Guilandina, 177. Guppy, Dr. H. P., 19. guttata (Aischna), 139. guttatus (Anax), 139. Guttifere, 172. gutturalis (Hirundo), 50, 302. Gymnodactylus, 51. Gymnosperms, 193. Gynandropsis, 171. Gypsina, 229, 231-2, 237-9, 241, 246-7, 249-50, 252, 254, 266. Gyrocarpus, 178. Gyrophena, sp., 89. Haddonia, 246, 249. Halictus, 86. Halimeda, 250, 289. halmaheire (Acronychia), 174. Halobates, 129. Halobatide, 129. Halticide, 127. halysideta (Epagoge), 78. hansenii (Chelifer), 157. Haplodesmus, 155. Haplosoma, 155. Harpalus, sp., 89. Hastula, 78. Healthiness of Island, 18. hebreus (Polistes), 85. Heliastrea, 215. heliopora (Orbicella), 217. Hellula, 74. 328 helvetica (Heterostegina), 229. Hemiptera, 136. —— Distribution of, 300. Hepatic, 197. Heptapleurum, 179. Herculia, 73. -: herklotsi (Astrea), 215. (Orbicella), 207-8, 215, 288. Hernandia, 187. Heteractitis, 319. Heterographis, 73. Heterogyna, 81. heterogyra (Mzeandrina), 213. Heteropoda, 154, 161. Heterostegina, 229, 231-2, 235, 237, 939-41, 244, 246-9, 252-5. Hexagonia, 199. Hibiscus, 173. Hierodula, 142, 146-7. Hippoboscide, 88. Hirneola, 199. hirsutus (Cylindrodesmus), 155. hirudinata (Sauris), 71.: Hirundinide, 50. Hirundo, 50, 302. hirsutus (Trichyorhyssemus), 98. Histeride, 90. Hololepta, 90-1. ; holophealis (Glyphodes, Phacellura), (4, Homceosoma, 72. Homoptera, 127. Distribution of, 300. honesta (Ophiusa), 66. Hormurus, 156. horsfieldi (Euchromia), 64. hortensis (Cryptops), 154. hospita (Kleinhovia), 173. Hoya, 182. Hugh’s Dale, 14, 283. hyalina (Nogodina), 134. (Ricania), 134. Hydrillodes, 68. Hydrophilide, 90. Hyleocarcinus, 168. hylas (Cephonodes), 70. Hymenoptera, 81. — Distribution of, 300. hypericifolia (Euphorbia), 187. Hyperythra, 70. Hyphomycetes, 200. Hypnum, 196. ; hypoleucus (Tringoides), 40. Hypolimnas, 60, 62... Hyponomeutide, 76. Ichneumonide, 81. Idiocerus (?),.138... idoneus (Examnes), 122. INDEX. ignarus (Aigocidnus), 124. imbricata (Chelone), 54. imperator (Mus), 29. ‘‘ Impérieuse,’? Annexation by H.M-S.,-2. impressa (Crioceris), 319. inzequalis (Orbitoides, Lepidocycelina, insule-natalis, var.), 254. incerta (Labia), 142, 144. incertus ? (Pachyops), 115. incisa (Czenognosis), 79. indica (Chalcophaps), 39. (Eleusine), 193. (Epilachna), 95. (Erythrina), 176. ———— (Glyphodes), 74. ——— (Hololepta), 91. —_—— (Quisqualis), 178. (Stachytarpheta), 184. indicus (Cajanus), 177. (Pipistrellus), 27. indistincta (Labia), 142, 144. inermipes (Cryptops), 154. infumatus (Anchastus), 101. Inhabitants, 19. inherens (Gypsina), 239, 241, 252. inhians (Epiplema), 72. Inocarpus, 177. inophyllum (Calophyllum), 172. inornatus (Amarygmus), 107. inscitus (Rhyssemus), 97. Insecta, 60. insomnis (Myrmeleon), 140. insule-natalis (Orbitoides, Lepido- cyclina), 242, 248, 251-4, 296. insularis (Pontodrilus), 167-8. insulicola, 160. intermedium (Nephrodium), 195. involva (Polytrema miniaceum, var.), 239, 248-50. iphigenia (Hypolimnas), 62. Ipomeea, 183. iridescens (Myrmeleon), 140. irioides (Polypodium), 196. irregularis (Orbicella), 217. irrorata (Porthesia), 69. Ischemum, 192. ismene (Melanitis), 61. Isometrus, 154. Isoptera, 141. Isside, 138. Issus (?), 138. italica (Cristellaria), 227. (Saracenaria), 227. Iulomorpha, 156. Jasminum, 181. Jasside, 138. Jatropha, 188... INDEX. Java, relations with Christmas Island, 296-7. javana (Cycas circinalis, var.), 193. javanensis (Cudrania), 189. javanica (Colubrina), 175. (Leucas), 185. ———— (Merula), 50. (Panesthia), 142, 146. javanicum (Cleidion), 188. (Stilbum), 200. javanus (Chelifer), 156-7. (Heteronychus), 320. (Mus), 29. (Phileurus), 320. jerdoniana (Mabouya), 52. jordani (Litocerus), 118. jugularis (Ardea), 41. junghuhni (Favoidea), 221. Junonia, 62. jupiter (Charaxes), 61. Kleinhovia, 173. koenigii (Sceevola), 181. Labia, 142-3, 145. Labiz, 144. Labiate, 185. Labidura, 142. Lacertilia, 51. leevitolia (Peperomia), 186. levigata (Grewia), 174. levis (Orbitolina), 229. Lagoon deposits, 289. lagostoma (Gecarcinus), 163. lagostomus (Gecarcinus), 163. Laius, 102. Lamiide, 122. Lampas, 202-3. lampas (Murex), 202. Lamprocystis, 54-6. Land-crabs, 2, 163, 300. Laportea, 189. Larentiane, 71. ? Larrada, 84. Larrine, 81. larvata (Planorbulina), 238, 241, 246, 250, 254. Laschia, 199. Lasioderma, 102. lateralis (Demotina), 126. latro (Birgus), 164. (Cancer), 164. Laurinee, 187. laxiflora (Laportea), 190. laxior (Randia densiflora, var.), 179. Lecanora, 198. Lecidea, 198. leda (Melanitis), 61. Leea, 176. 329 Leguminose, 176, leiophyllum (Ischeemum var.), 192. foliosum, _ lemniscatus (Clovia), 137. Leocyma, 66. Lepidocyclina, 230, 235-6, 240, 242, 244-6, 248, 250-6. Lepidoptera, 60. ——— Phalene, 63. lepiniana (Neckera), 196. Leptaulax, sp., 97. Leptogium, 198. Leptopoma, 55, 58. Leptoria, 207, 210-11. lessonii (Amphistegina), 229, 235, 237, 239-42, 249-56. (Pseudorhynchus), 142, 149. lethifer (Myrmeleon), 141. Leucas, 185. Leucobryum, 196. Leucopheea, 142, 146. lewisi (Tetrigus), 100. Libellula, 139. Libelluline, 139. Lichens, 197. lignarium (Platysoma), 91. lignicolus (Brachyrhynchus), 129. ligniperdus (Camponotus), 83. limbata (Bocula), 66. Limnas, 60. Limnobeenus, 39. Limnocarcinus, 163. Limonites, 41. Linderina, 243. Lindinia, 126. Lispinus, 90. List of species, 305. hasten, J.J, Visit of, 2. listeri (Abutilon), 173. ————- (Acrostichum), 196. (Arenga), 50, 191. (Endotricha), 73. ——— (Gecko), 51. —- (Heteropoda), 161-2. ——— (Hypolimnas), 60, 62-3. ——— (Hypolimnas nerina, var.), 62. (Peederus), 89. (Paregus), 96. (Phisis), 142, 149. (Phreatia), 190. ———- (Sessinia), 108. (Succinea), 56. Listrocelide, 142, 149. Lithocharis, sp., 89. lithothamnica (Carpentaria), 235, 238. Lithothamnion, 227, 231, 236, 238, 240-3, 245-7, 250, 252-4, 256, 265-7, 289. 232, 244, 246-7, Lithyphantes, 162. 330 Litocerus, 118. littida (Sessinia), 108. littoralis (Prodenia), 65. litura (Melanoxanthus), 101-2. lobatula (Truncatulina), 227-8, 231, 234, 241, 249, 255. lobatulus (Nautilus), 229. Lobopelta, 81, 83. Lobophyllia, 210. Locustidee, 142, 150. lombocensis (Pteropus), 24—5. longicornis (Examnes), 122. longifolia (Callicarpa), 184. longiusculus (Lygeeus), 137. Lucanide, 96. lucasi (Theretra), 70. lucidula (Premna), 185. lucidus (Fomes), 198. lunalis (Sylepta), 74. Junatus (Phaseolus), 177. lutea (Hyperythra), 70. (Lecidea), 198. (Porites), aff., 207, 222. -luteo-olivaceus (Polystictus), 199. luteus (Melampus), 58. Lycogala, 200. Lycophris, 229-30. Lycopodium, 196, Lygeide, 128. Lygeus, 128. Lygosoma, 51-2. Lymantriade, 69. lymexyloni (Dryophthorus), 116. Lythracee, 178. mabele (Ariophanta, Microcystis), 5d. (Lamprocystis), 55. Mabouya, 52. Macaranga, 188. Maclear Deep, 1. macleari (Mus), 22, 30, 34-6. ———— (Vadebra), 60-1. maclearii (Dicliptera), 184. macreei (Dendrobium), 190. Macroglossine, 70. macrops (Patula), 320. maculatus (Isometrus), 154. Madrepora, 210. Meeandrina, 207, 212-14. magnifica (Astrea), 219. (Favastrea), 219. (Prionastrea), 207, 219-20. Maliattha, 68. malleata (Hololepta), 90. Mallophaga, 138. Malvacee, 172. Malvastrum, 172. Mammalia, 22. Manganese nodules, 279. INDEX. Manopora, 224. Mantibaria, 82. Mantide, 142, 146. Mantis, 82. Marcorella, 175. Marginal radiale, 35. marginatus (Dolopius), 100. marmorata (Oniscomorpha), 94. marmoratus (Gymnodactylus), 51. materna (Ophideres), 67. matsushimensis (Pontodrilus), 167-8. maura (Xuthia), 94. mauritianus (Trochus), 201. Means by which new forms are intro- duced, 301-3. Measurements of skulls of Mus, 37. Mecistocephalus, 155. Mecopus, 113. mediterranensis (Planorbulina), 227, 237-8, 244, 251, 254. Megachile, 87-8. Megachiline, 81. Megapenthes, 101. Megascolex, 170. Melampus, 54-6, 58. Melanitis, 61. melanoceras (Cyrtacanthacris), 152. melanope (Motacilla), 48. Melanoxanthus, 101. melas (Pteropus), 25. Melia, 174. Meliaces, 174. melichloros (Camponotus), 83. melo (Alveolina), 252, 255. Melothria, 179. Melyride, 102. membranaceum (Aspidium), 195. Menispermacee, 171. Merula, 49, 50. meyeri (Mus), 32. Micracantha, 123. Microcystis, 55-6. Micro-Lepidoptera, 75. —— Distribution of, 300. Micropezide, 88. Migrants, Arrival of, 299. Migratory birds, Arrival of, 17. mildred (Ariophanta, Microcystis), 56. —— (Lamprocystis), 56. Miliolina, 233-4, 236-7, 240, 242-8, 250-2, 254. Milioline, 245. Millepora, 235. Mimeusemia, 64. minahassze (Acronychia), 174. miniacea (Millepora), 235. miniaceum (Polytrema), 241, 246, 248-50, 256. miniatum (Lycogala), 200. minima (Physalis), 183. 235, 239, INDEX. Minthea, 1035. minutus (Dinoderus), 105. Miocene (Orbitoidal) limestones, 16, 271, 273, 281-2. misippus (Hypolimnas), 62. — (Papilio), 62. modesta (Rhyparida), 125. modestus (Dryophthorus), 116. mollissima (Leucas), 188. Mollusca, 54. (fossil), 201. Momordica, 179. Moni, 1. monile (Coscinarea), 221. Monocotyledons, 190. Monohammus, 122. montagnei (Cyathus), 199. (Hypnum), 197. monticola (Ariadna), 158. monticularis (Carpenteria), 235, 238, 247, 250, 252, 254-5. Montipora, 207, 209, 224. Morinda, 180. Morio, 89. morio (Chelisoches), 143. morpheus (Formicaleo), 140. morsicans (Scolopendra), 154. Mosses, 196. Motacilla, 48. Motacillide, 48. mouhoti (Leptopoma), 58. mucronata (Melothria), 179. muelleri (Mus), 32. mulmeinensis (Cyclosa), 160. (Epeira), 160. ——— (Epeira, Cyclosa), 160. Murex, 202. Murray, Sir John, 3, 19. Murray Hill, 4, 289, 292. murrayana (Laportea), 189. (Orbitoides, Lepidocyclina), 252-3. murrayi (Anisoccenia), 207, 220. (Chelifer), 156-7. (Labia), 142-3. (Orbicella), 207, 215, 285. (Pipistrellus), 26. (Tetrigus), 100. Mus, 22, 28, 32. Mus macleari, Allies of, 31-2. Muscide, 88. Mussa, 207, 209-10. Mycetophilide, 88. Mycetozoa, 200. mydas (Chelone), 54. Myristicivorus, 299, 302, 319. Myrmeleon, 140. Myrmeleonide, 140. Myrsinee, 181. Myrtaceze, 178. ook Nacaduba, 60, 63. nannodes (Herculia), 73. Narcisa, 93. Nassa, 204. natalis (Ariadna), 158. (Astur), 46. (Chalcophaps), 39. (Collocalia), 48. (Hyleocarcinus), 163. (Ninox), 47. (Pteropus), 22-3. ——— (Urospizias), 46. (Zosterops), 49. nativitatis (Cryptocarya), 187. — (Kpilachna), 96. -——— (Lygosoma), 51-2. —-— (Monohammus), 122. (Mus), 22, 28, 33-35, 37. (Pittosporum), 171. (Saprosma), 180. (Xenoceras), 118. nauticus (Araneus), 162. Nautilus, 227-8. Neckera, 196. neglecta (Corrocalia), 48. neodispansa (Orbitoides), 240. — (Orbitoides, Lepidocyclina), 235, 245, 252. Neoptinus, 102-3. Nephilia, 160. Nephrodium, 194-6. Nephrolepis, 195. nerina (Hypolimnas), 60, 62. Neuroptera, 139. nicobaricus (Pteropus), 24. nidus (Asplenium), 194. nigerrimalis (Zinckenia), 73. Nigilgia, 77. nigricorne (Cyrtacanthacris), 152. nigricornis (Labidura), 142. nigritarsis (Apomecyna), 123. (Nephilia), 160. nigrum (Ceresium), 121-2. niloticus (Arvicanthus), 36. nimbella, (Homceosoma), 72. Ninox, 47. Nirmus, 138. niruri (Phyllanthus), 187. nitens (Aithus), 127. nitida (Spiroloculina), 233, 252. nitidula (Scelodonta), 126. Nitidulide, 92. nivescens (Megachile), 88. Noctuide, 65. nodiflora (Synedrella), 181. Nodosaria, 249. Nogodina, 134. Nola, 64. normani (Ariophanta, Microcystis), 55. —_——_— (Lamprocystis), 53-6. 332 North-East Point, 4, 14, 16, 293-4. —_— Miocene rocks at, 287. North-West Point, 9, 14. Notogonia, 81, 84. Numenius, 40. Nummulites, 273, 297. Nyctaginew, 185. Nyctobates, 106. Nymphalid, 60. Nymphaline, 61. obeliscus (Tectus), 202. (Trochus), 202. oblonga (Miolina), 234. obscurus (Rhabdocnemis), 113. cean-current, 302. Ochrocarpus, 172. Ochrosia, 182. Ochthiphilide, 88. Ochthodromus, 40. octo (Amyna), 68. ‘Octoblepharum, 196. ‘Ocypoda, 164. Ocypodide, 164. odiosum (Platysoma), 91. odoilam (Cerbera), 182. Odonata, 139. Odynerus, $1, 84. (Kdemeride, 107. Oleacez, 181. Olenecamptus, 122. olivacea (Tarache), 69 Oniscomorpha, 93-4. ‘Oosomides, 111. oparanus (Bulimus), 57. ——— (Opeas), 57. Opatrum, 106. Opeas, 54, 57. Operculina, 229. Ophideres, 67. Ophidia, 53. Ophion, 81-2. Ophionine, 81. Ophiusa, 66. Oplismenus, 193. optivata (Craspedia), 71. Orbicella, 285, 288. orbiculatus (Aspidiphorus), 104. Orbitoides, 229-80, 232-3, 235-6, 238, 240, 242— - 248, 250- 6, 292. —— dispansa i in Java, 297. Orbitolina, 229. Orbitolites, 252. ‘Orbitulites, 230. Orbulina, 240. ‘Orchidex, 190. Orgyia, 69. orientalis (Glareola), 40 207-8, 215-16, 218-19, INDEX. orientalis (Morio), 89. ———_— (Oxyn), Heelan (Primnia ?), 150. —_——— (Stelidota), 92 orites (Chelifer), 157. ornaticornis (Simaethis), 77. Ortalide, 88. Orthomorpha, 159. _ Orthoptera, 141-2. , Distribution of, 300. Orychodes, 1176 Osteology of Mus M. macleari, 34. Otiorrhynchine, 108. ovalifolium (Panicum), 193. ovalifolius (Ochrocarpus), 172. ovata (Anisomeles), 180. ovigera (Hernandia), 187. Owl, Habits of, 47. Oxya, 142, 150. oxyacanthella, 7. Oxychirota, 75. Oxychirotide, 75. Oxyopes, 162. Oxypleura, 128. nativitatis and pachyderma (Globigerina), 237. Pachyops (?), 116. pachypus (Pipistrellus), 27. Peederus, 89. pagodalis (Tectus), 201. Palagonite tuffs, 278-9, 285, 287. Palme, 191. Palorus, 106. Panaretus, 162. Panchlora (Leucopheea), 146. Panchoran, 9, 280. Pandanacee, 191. Pandanus, 50, 191. Panesthia, 142, 146. paniculatus (Celastrus), 175. Panicum, 192. ———— (Effuse), 192. Pannaria, 197. panorpeformis (Ricania), 134-5. Pantala, 139. Papilio, 60, 62. - papillosa (Rotalia), 238. papyracea (Orbitoides), 235, 245, 252. Paradesmus, 108. paradoxa (Oxychirota), 75. Paregus, 96. Paramecosoma, 99. Paranobium, 104. parki (Euxestus) 96. Parmelia, 197. Paromalus, sp., 91. parryi (Tetrigus), 100. parviflorus (Convolvulus), 183. INDEX, parvulum (Trichomanes), 194. parvulus (Xyleborus), 117. parvus (Neoptinus), 103. Passalide, 97. Passeriformes, 48. patellifera (Hierodula), 146. patruelis (Terias), 60, 63. Patula, 320. patula (Acanthastrea), 207, 218. (Orbicella), 218-19. paucidentata (Acanthastrea patula, -var.), 207, 218. Paurostauria, 152-3. pavonacella (Brenthia), 76. pectinata (Meeandrina), 214. — (Phisis), 150. pedata (Cissus), 176. Pedetes, 35-6. Pedicellaria, 171. pedunculata (Colubrina), 179. ——— (Procris), 190. Pelecaniformes, 42. pellucida (Ricania), 136. peltata (Hernandia), 187. (Ipomeea), 183. Pemphis, 88, 178. pentaphylla (Gynandropsis), 171. ———— (Pedicellaria), 171. Pentatoma, 128. Pentatomide, 137. Peperomia, 186. Percentage of peculiar species, 299. perforans (Tomicus), 116. (Xyleborus), 116. Perforata, 222. Pericheta, 168-9. Periplaneta, 142, 146. perplexa (Pterolophia), 123. pes-capre (Ipomea), 183. petilia (Limnas), 60. (Papilio), 60. Phacellura, 74. Phaethon, 45, 299. Phaethontes, 45. Phaneropteride, 142, 150. Phaseolus, 177. Phasmide, 142, 147. Phileurus, 320. philippensis (Examnes), 122. Philonthus, sp., 89. Phisis, 142, 149. phlegmaria (Lycopodium), 196. Phlceophagosoma, 114. pheenicurus (Phaethon), 46. Pholcide, 159. Pholceus, 159. ' Phosphate deposits, Discovery of, 19. — of alumina and iron, 271, 291. | ——— of lime, 271, 289-91. 300: Phosphate Hill, 12, 14, 289. Phreatia, 190. phrygia (Leptoria), 207, 210-11. (Madrepora), 210. | Phycitine, 72. Phycodes, 77. _ Phyllanthus, 187. phyllocarpum (Leptogium), 198. Phyllodromia, 142, 145. Physalis, 183. Physcia, 197. piceus (Alphitobius), 106. picta (Physcia), 197. pictula (Bidis), 137. Piezonotus, 110-11. ‘* Pigot,’’ Visit of the, 2. pilarus (Tinoporus), 229. pilulifera (Euphorbia), 187. Piperaceze, 186. Pipistrellus, 26. piscatrix (Sula), 45. Pisonia, 185. Pittospores, 171. Pittosporum, 171. Placentula, 228. plagiatus (Litocerus), 118-19. Planipennia, 140. Planispirina, 242. Planorbulina, 227, 234, 287-8, 241, 244, 246, 249-51, 254, 265. Plants introduced by man, 303. Platylabia, 142-3. platyphylla (Boehmeria), 190. Platypus, 116. Platysoma, 91. Plecanium, 231. pleiades (Orbicella), 207, 218. plena (Nogodina), 136. plumosa (Eragrostris), 193. plumulosum (Thuidium), 197. Pocillopora, 207, 209. Pocilloporide, 209. Peecilopsaltria, 130. poeyi (Strongylosoma), 159. Polistes, 81, 85. polita (Oxypleura), 128. (Shoguna), 92. polygramma (Hexagonia), 199. polymorphum (Nephrodium), 195. Polypetale, 171. polyphemus (Odynerus), 84. Polypodium, 196. Polyporus, 198. Polystictus, 198-9. Polytrema, 235, 239, 241, 246, 248-80, 256, 266, 268. pomona (Psyra), 142, 150. Ponera, 83. Pongamia, 177. Pontodrilus, 166-8. 334 Porites, 207, 222-4, 295. in sea cliff, 295. Poritide, 222. Porthesia, 69. Possibility of former union with Java, 297. posthuma (Pericheta), 170. postica (Orgyia), 69. posticum (Paranobium), 104. preheliopora (Orbicella), 207, 216-17. Preepollex, 36. Premna, 185. Prevailing winds, 17. Primnia (?), 150. princeps (Halobates), 129. Prinobius, 120. Prionastrea, 207, 219-20. Prionide, 120. proavus (Halobates), 129. Procris, 190. Proctotrypide, 81. Prodenia, 65. Prometopia, 92. proserpina (Hepes) ; 62-3. Prosoplus, 123. prostrata (Ruellia), 184. Protetia, 98. proteus ? (Halictus), 86-7. Psammeecus, 95. Pseudocorylophide, 96. Pseudorhynchus, 142, 149. Pseudoscorpiones, 156. Pseudosphinx, 70. Psylliodes, 127. Psyra, 142, 150. Pterolophia, 123. Pterophoride, 75. Pteropus, 22-3. Ptinide, 102. Ptinides, 103. Ptychanthus, 19% pubescens (Boerhaavia diffusa, var.), 185. puerpera (Venus), 205. pulchella (Deiopeia), 64. Pullenia, 231. pulverea (Porthesia), 69. Pulvinula, 228. Pulvinulina, 228, 231, 238, 254. pumilis (Gecko), 52. punctata (Dendroneura), 80. punctatus (Idiocerus ?), 138. punctifrons (Bidis), 137. pupoides (Gaudryina), 236. pygmea (Bolivina), 231. Pyralide, 72. Pyralidina, 75. Pyraline, 73. Pyramidea, 201. Pyramis, 201. INDEX. pyramis (Tectus), 202. (Trochus), 202. Pyraustine, 73. pyrrhus (Charaxes), 61. Pythia, 55, 58. Pyxine, 197. quadrangularis (Orbicella), aff., 207, 216. quadricorne (Toxicum), 106. quadrimaculata (Prometopia), 92. quadrimaculatum (Ceresium), 121. quadriquadra (Cosmoclostis), 75. ae 236, 240-1. Quisqualis, 178 racemosa (Barringtonia), 178. — (Tiliacora), 171. radicula (Nodosaria), 249. Rainfall, 17, 18. Ramalina, 198. ramosa (Nephrolepis), 195. Randia, 179. Ranella, 203. me Redpole,” Visit of H.M.S., 3. refulgens (Cibicides), 251. ——— (Truncatulina), 231, 251. reinwardti (Argiope), 159. ———- (Epeira), 159. Remusatia, 192. repanda (Placentula), 228. (Pulvinula), 228. ——— (Pulvinulina), 228, 231, 238, 254 (Rotalia), 228. repandus (Nautilus), 228. repens (Cissus), 176. retiformis (Astrea), 214. —— (Goniastrea), 207, 214. retusa (Ficus), 189. ‘ revolutum (Trachymitrium), 196. rex (Mus), 29. Rhabdocnemis, 113: Rhamnacezx, 175. Rhopalocera, 60. Rhyncholobus, 108-9. Rhyneoli, 115. Rhyparida, 124, 126. Rhyssemus, 97. Ricania, 131. Ricaniide, 131. Ridley, H. N., Visit of, 3 Robber-crab, 164. Ross Hill, 289, rossi (Figulus), 96. — (Peperomia), 186. ——. (Rhyncholobus), 109 —— (Rhyparida), 124, Rotalia, 228, 232, 288, 241, 247, 254-6. INDEX. O00 rotulata (Cristellaria), 227. semigranosa (Ranella,) 203. rotundata (Labia), 146. seminitidus (Bradymerus), 106. rotundifolia, 173. sepulchralis (Vadebra), 61. rotundipennis (Megachile), 87. Serpula, 247. ruber (Strongylodon), 176. serrirostris (Orychodes), 118. rubescens (Claoxylon), 188. serva (Ophiusa), 66. Rubiacez, 179. serrata (Paramecosoma), 95. rubiginosa (Pannaria), 197. Sessinia, 107. rubrescens (Brachyrhynchus), 129. rubricans (Thermesia), 67. rubricauda (Phaethon), 45. ruderalis (Fleurya), 189. Ruellia, 184. ruficollis (Limonites), 41. rufostriata (Epacromia), 152. rufotestacea (Shoguna), 93. rufovaria (Gryllacris), 148. rugicollis (Ditoma), 105. (Minthea), 105. rugosa (Textularia), 231, 237-8, 241-38, 249, 251-2. rugosum (Plecanium), 231. Rupertia, 238, 246, 254. Rutacez, 174. Saccolabium, 191. sacra (Demiegretta), 41. Sago-palms, 287. salaminia (Ophideres), 67. sambac (Jasminum), 181. sambucina (Leea), 176. sanguinalis (Digitaria), 192. sanguineus (Polystictus), 199. Sapindacez, 176. Sapotacee, 181. Saprosma, 180. Saracenaria, 227. sarawakensis (Termes), 141. Sarcochilus, 191. Satyrine, 61. Sauris, 71. saxophila (Ficus), 189. Scevola, 88, 181. scandens (Etada), 177. scarabzeus (Pythia), 58. Scelodonta, 126. Schizophyllum, 198. schroeteriana (Rotalia), 228, 232, 237, 241, 247, 254-5. Scincide, 52. Sciurus, 35. Scolopendra, 154. Scolytide, 116. Scorpio, 156. Scorpiones, 156. scotella (Ephestia), 72. scotozonea (Boarmia), 71. Scymnus, sp., 96. Sea cliff, 6, 294-5. selenampha (Amyna), 65. semiasperatus (Bradymerus), 106. Shoguna, 92. Shore cliff and terrace, 294. terrace, 9, siamea (Cassia), 177. Sideroxylon, 181. Sidney’s Dale, 14, 288, 295. Sigmoilina, 242. signifera (Maliattha), 68. Simaethis, 77. similata (Minthea), 105. simplex (Ceresium), 122. (Chrysodema), 99. sinensis (Cceloria), aff., 213. singhalella (Heterographia), 73. Slipping of beds of limestone round Island, 14, 16, 281, 296. Smeringopus, 149. Smith Point, 5, 293. snellemanii (Ariadna), 158. Soil, 19, 291. Solanacee, 183. Solanum, 183. solida (Davallia), 194. solidula (Succinea), 56. solidus (Platypus), 116. solitaria (Succinea), 56. Sorex, 27. South Point, 4, 288. Sparasside, 161. sparassoides (Guepinia), 199. speciosa (Guettarda), 180. spectabilis (Blumea), 181. spelunce (Davallium), 194. Spheroidina, 231. Sphenophorus, 113. Sphingide, 69. Sphingine, 70. Spiroloculina, 233, 242-3, 248, 250, 252 52. Spirostreptus (Nodopyge), 156. splendens (Stemonitis), 104, 200. Sponia, 188. squarrosus (Ptychanthus), 197. stabilis (Rupertia), 254. Stachytarpheta, 184. stali (Anisolabis), 142-3. (Forcinella), 143. Staphylinide, 89. Steep Point, 6, 16, 287. Stelidota, 92. stellata (Orbitoides), 253. Stemonitis, 104, 200. ee ee 336 Stenogyra (Opeas), 57. stenura (Gallinago), 41. Sterculiaceee, 173. Sticky fruits, 303. Stictoptera, 68. Stilbum, 200. stilpnoides (Clitumnus), 142, 147. stilpnus (Clitumnus), 147. stolidus (Anous), 39. Storms, 17, 301. strangulatus (Trochorhopalus), 113. — (Sphenophorus), 113. Stratiomyide, 88. striata (Shoguna), 93. strigatus (Bothrideres), 94. strigosa (Meeandrina), 213. Strongylodon, 176. Strongylosoma, 156. Strongylosomide, 155. strubelli (Haplosoma), 155. Structure of central nucleus of Christ- mas Island, 271. subarmata (Labia ?), 142, 144. subcordata (Cordia), 182. - subcostatus (Dermestes), 95. subrotunda (Miliolina), 233. subrotundum (Vermiculum), 233. subrufescens (Lygzeus), 128. subula (Achatina), 57. (Bulimus), 57. ——— (Opeas), 54, 57. (Stenogyra, Opeas), 57. subviridis (Nogodina), 135. Succinea, 56. suediata (Pyxine), 197. Sula, 44, 299. sula (Sula), 44. sulcicollis (Figulus), 97. Sumatra, Orbitoides of, 297. sumatranus (Chelifer), 157. sumatrensis (Orbitoides), 244, 252, 6 ——— (Orbitoides, Lepidocyclina), 204, 246, 252-3. sundaicum (Sideroxylon), 181. supellectilium (Blatta), 145. — (Phyllodromia), 142. ———— ? (Phyllodromia), 145. suralis (Glyphodes), 74. surinamensis (Leucopheea), 142, 146. (Panchlora, 146. surusalis (Dichocrocis), 74. suturale (Platysoma), 91. suturalis (Cossonus), 114. Syctodes, 159. Syctodide, 159. Sylepta, 74. Synedrella, 181. Syntomide, 64. Leucopheea), INDEX. syrmaticum (Nephrodium), 194. Syrpindz, 88. tabulata (Heliastraea), 215. tanarius (Macaranga), 188. Tarache, 69. Tectona, 184. Tectus, 201-2. Temnopteryx, 142, 145. Temperature, 17. Tenebrionid, 105. tenuepunctata (Psylliodes), 127. tenuiflora (Galactia), 176. tenuis (Daedalea), 199. (Leptoria), 210-11. ——— (Pipistrellus), 27. Terebrantia, 81. Terias, 60, 63. Termes, 141. Terminalia, 177. Termitide, 141. Tertiary limestones in the Azores, 296. tessellata (Gryllacris), 148. testacea (Lasioderma), 102. testaceus (Bostrichus), 116. ———— (Bythoscopus), 138. Tetrigus, 99. Textularia, 231, 287-8, 241-3, 247, 249, 251-2. Thalassochelys, 54. Thalassodes, 71. Theories of atoll formation, 209. Theretra, 70. Thermesia, 67. Thuidium, 197. Thyridium, 196. tibialis (Laius), 102. (Leocyma), 66. Tiliacee, 173. tiliaceus (Hibiscus), 173. Tiliacora, 171. timoriensis (Leptaulax), 97. tinctorum (Parmelia), 197. Tineide, 80. Tineina, 76. Tinoporus, 229. Tipulide, 88. Tomicus, 116. _ torresiensis (Haddonia), 249. Tortricide, 78. Tortricomorpha, 78. Tournefortia, 182. Toxicum, 106. Trachychernes, 156. Trachymitrium, 196.. Trachyte, 275-6, 285. Trade-wind, 301. Trechus (?), 89. Trees of shore terrace, 9. INDEX, ore tricarinata (Miliolina), 245. (Triloculina), 245. tricholoma (Trichoscypha), 290. Trichomanes, 194. Trichoscypha, 200. trichura (Crocidura fuliginosa,var.), 27. Trichyorhyssemus, 98. tricuspidatum (Malvastrum), 172. trifasciata (Epeira), 159. trifoliolata (Acronychia), 174. trigonula (Miliolina), 248, 245, 247, 252 Triloculina, 245. Tringoides, 40. Trithemis, 139. trivialis (Libellula), 139. (Trithemis), 139. Trochammina, 231. Trochorhopalus, 113. Trochus, 201-2. Trogositide, 92. Tropic-bird, 45-6. Truncatella, 55, 59. Truncatulina, 227-8, 231, 234, 241, 249, 251, 255-6, 265-6. truncatum (Nephrodium), 195. ‘ tuberculosa (Manopora), 224. tuberosa (Rotalia), 228. Turbo, 203. Turdide, 49. Turdus, 37, 49. Tutufa, 202-3. Typhlopide, 53. Typhlops, 51, 53. Ugyops, 137. undalis (Hellula), 74. undosa (Miliolina), 236. ungeriana (Truncatulina), 245. unicolor (Bythoscopus), 138. ———— (Cyrtophora), 160. universa (Orbulina), 240. Upper cliffs, 11. —_— and terraces, Geology of, 291. Uraniade, 72. Urospizias, 46. Urticacez, 188. utricularis (Carpenteria), 241, 247, 250, 254-5. Uvigerina, 234. Vadebra, 60-1. vagivitta (Dipterygia), 65. valida (Truncatella), 59. Valleys on west coast, 283. varcia, 131. Qe <1 varia (Lecanora), 198. variabilis (Gryllacris), 148. variegatus (Numenius), 40. variipennis (Cossonus), 114. venatoria (Heteropoda), 154, 161-2. Venus, 204-5. venusta (Dictus), 159. (Syctodes, Dictus), 159. veraria (Thalassodes), 71. veratrifolia (Corymbis), 191. verbeeki (Orbitoides), 235, 252. (Orbitoides, Lepidocyclina), 245, 250, 252-3, 256. Verbenacee, 184. Vermes, 166. Vermiculum, 233. verrucosa (Venus), 204. vesicularis (Gypsina), 229. Vespide, 81. vexillifera (Hydrillodes), 68. vicarius (Paradesmus), 155. vicinus (Halictus), 86. vigil (Cheerocampa), 70. villida (Junonia), 62. (Papilio), 62. villosus (Cylindrodesmus), 155. vitiensis (Cosmophila), 67. vitifolius (Hibiscus), 173. Vittaria, 195. vittatus (Rhyncholobus), 110. vivipara (Remusatia), 192. vriesianus (Hibiscus), 173. vulgaris (Sciurus), 35. Water-borne seeds, 303. Wedelia, 181. West White Beach, 6, 292. Wharton, Rear-Admiral Sir W. J. L., Account of Island by, 3. Wharton Deep, 1. whartoni (Carpophaga), 37. wightiana (Acalypha), 188. Wind-borne seeds, 302. woodmasoniana (Assiminea), 59. xanthopterus (Ectadoderus), 148. xanthopus (Polystictus), 198. xanthurus (Mus), 32. Xenoceras, 118. Xuthia, 94. Xyleborus, 116. Xysticus, 162. Zinckenia, 73. Zooblax, 121. Zosteropide, 49. Zosterops, 49. STEPHEN AUSTIN AND SONS, PRINTERS, HERTFORD. EXPLANATION OF PLATES. PLATE I. Pteropus natalis, Thomas. Adult male. (p. 2 e 2 " s B.M.CHRISTMAS 12 le > K4 PJ.Smit del.et lth. MinternBros.Chromo. Pteropus natalis, Thomas. . - y * ~ ‘ ‘ * ¥ r ytit i “* j ; i r 4 . * . { ‘ \ ' a! ’ . ‘ a ” Ye “, ‘ hi ro 24 ’ { . i : > ‘ fies : 4 we t, fal © : SUULIY / “Sp WPALHDOU sn W . Ouro ry 5 "soa ST ULBPATYT “UYATT qo 2) FUG CP ‘WId al SVNLSTYHO' Wd U) W he os id ATT MA ary #, uP EA Me PP te lee ee 2 ee a " : } +e i hs eo z i) ‘ sii fiat, . i, i oe PLATE II (bis). Mus macleari, Thomas. Figs. 1, 3, 6, 7, 8. } (p. 34.) y Mus nativitatis, Thomas. Figs. 2, 4, 5, 9, 10. cos: wr Figs. 1 and 2, cranium from above; Figs. 3 and 4, from be Figs. 5 and 6, side view with lower jaw; Figs. 7-9, r upper molar series ; Figs. 8 and 10, right lower molar ser Figs. 7-10 x 4; the others natural size. ee he ’ B.M. Christmas Island. Pl. II (dis). ek 10 2. m3. Skulls and Teeth of Wus macleari and Mus nativitates. PLATE III. _ Phaethon fulous, Brandt. (p. 45.) | PAE: Mintern Bros.Chromo. J.GsKeulemamns del.et hth. B.M.CHRISTMAS I? Phaethon fulvus, Brandt. PLATE IV. Ninox natalis, Lister. (p. 47.) B.M.CHRISTMAS P i ive J.GsKeulemans del.et lth. Mintern Bros.Chromo. / 7 2 bs . Ninox natalts. Lister. VW a Ak. Daa PLATE V. Astur natalis (Lister). (p. 46.) B.M. CHRISTMAS Pi J.G. Keulemans del.et lith. Mintern Bros.Chromo. Astur natalis. Lister, sp. Pilea» | Wi ; r 5 Waa’ - “y " . Fi ; ee ‘ i eat 4 A ir, is) Bs Py me, ‘ 4 f ne \ ‘ 2) ee oe : é s sty sees #4 ‘ trae %. , yy J aves Ay rs Arte Been Tey Bs er , Ps a py iciey nu ‘ie Nar br tian ; ‘ta See bie he aee Cine ee ARS vem) Ws ihe so Paar 2: ol re ’ , ; ; I a rr ae i : 4 ee a3 : PLATE VI. Zosterops natalis, Lister. (p. 49.) c fi A BM.CHRISTMAS PlgV1. J.G‘Keulemans delet lth. Mantern Bros.Chromo. Zosterops natalrs, Lister. ; &4 : iv oe a a es i ‘ am he a7 ‘ ae t Tak PRATE VIL REPTILIA. Fic. 1. Gecko listert, Boulenger. (p. 51.) Fies. 2, 2a, 2b. Lygosoma nativitatis, Boulenger. (p. 52. ’ Figs. 3, 3a, 3b. Ablepharus egerie, Boulenger. (p. 53.) a en 4 Pravi: B.M.CHRISTMAS I? pad a la \ } rere ral WON aie A » Mintern Bros amp : Ablepharus eger J.Green del.et kth. LB . 2.lygoesoma nativitatis. 3. U. / Gecko lister. Pb ATE Vert. Lanp SHELLS. Fies. 1-3. Lamprocystis normani (Smith). (p. 55.) Fie. 4. Lamprocystis mabele (Smith). (p. 55.) Fies. 5-7. Lamprocystis mildrede (Smith). (p. 56.) Fies. 8, 9. Succinea solidula, Pfeifier. (p. 56.) Fias. 10, 11. Seecinea solitaria, Smith. (p. 56.) Fies. 12, 13. Succinea listeri, Smith. (p. 57.) — Fig. 14. Opeas subula (Pfeiffer). (p. 57.) Fig. 15. Pythia scarabeus (Linn.). (p. 58.) Fie. 16. Melampus luteus (Quoy & Gaimard). (p. 58.) Fie. 17. Melampus fasciatus (Deshayes). (p. 58.) Fie. 18. Melampus castaneus (Miihlfeldt). (p. 58.) Fias. 19, 20. Leptopoma mouhoti, Pfeiffer, var. (p. 58.) Fies. 21, 22. Truncatella valida, Pfeiffer. (p. 59.) Fig, 23. Assiminea andrewsiana, n.sp. (p. 59.) ovine D B.M.CHRISTMAS I Mintern Bros.amp. J.Green del.et lith. 14 ane 1 y i aes ‘we - i) ¢ * Wine, | ey i sai ah ¥) ar ’ Pn Gn ; ha Wd4, petal’ in ee _ P DA aie X. LEPIDOPTERA. Fires. 1, la. Bocula limbata, Butler. (p. 66.) Fie. 2. Hpiplema inhians, Warr. (p. 72.) Fie. 3. Hndotricha listert, Butler. (p. 73.) x. Fie. 4. Boarmia scotozonea, Hampson, sp.n. (p. 7 Fic. 5. Erastria griseomixta, Hampson, sp.n. (p. 6 Fic. 6. Hydrillodes vexillifera, Hampson, sp.n. Fic. 7. Mimeusemia econia, Hampson, sp.n. (p. 64.) Fie. 8. Charaxes andrewsi, Butler, sp.n. (p. 61.) q Fie. 9. Porthesia pulverea, Hampson, sp.n. (p. 69.) fh Fie. 10. Zinckenia nigerrimalis, Hampson, sp.n. (p. 7a. Me , ? Fic. 11. Glyphodes (Phacellura) holopheatis, Hampson, sp.n. (p. 74.) Fie. 12. Cosmophila vitiensis, Butler. (p. 67.) ce a m Fic. 13. Ephestia scotella, Hampson, sp.n. (p. 72.) “ie oe Fig. 14. Dichocrocis auritincta, Butler, sp.n. (p. 74.) Fia. 15. Boarmia scotozonea, Butler. (p. 71.) ‘ —aen au B.M. CHRISTMAS PF. Plate IX. 4 E.C. Knight ad.nat.ith. West,Newman Chr. Lepidoptera. PAPA, OX. COLEOPTERA. Fic. 1. Pederus listeri, Gahan, sp.n. (p. 89.) Fie. 2. Oniscomorpha marmorata, Arrow, sp.n. (p. 94.) Fig. 3. Bothrideres strigatus, Arrow, sp.n. (p. 94.) Fie. 4. Lavus tibialis, Gahan, sp.n. (p. 102.) Fie. 5. Protetia andrewsi, Gahan, sp.n. (p. 98.) Fie. 6. Hpilachna nativitatis, Arrow, sp.n. (p. 95.) Fie. 7. Megapenthes andrewst, Waterhouse, sp.n. (p. 101.) Fie. 8. Chrysobothris andrewst, Waterhouse, sp.n. (p. 99.) Fie. 9. Paranobium posticum, Gahan, sp.n. (p. 104.) Fie. 10. Neoptinus parvus, Gahan, sp.n. (p. 103.) Fic. 10a. Neoptinus parvus, Gahan, sp.n. Abdomen. (p. 103.) Pink B.M. CHRISTMAS 1°. West,Newman. imp. Coleoptera. MHorman-Fisher del et.lith. (WH Helge ae) Pi Save er a ee aoe. SIT LLL Seen Nese SEANRNN M. Horman-Fisher del.etlth. West, Newman imp. Orthoptera, Neuropterw, and Hymenoptera. a a aa ie ow eee “at a a Wied ty) ral Fie. Fie. Fie. Fic. Fie. Fia. Fic. Fic. Fie. Fic. Fic. Fic. Fig. Fia. Fig. Fic. COI D TP wW pw = ee Do FW HO KK CO PHATE XW. HoMOPTERA AND HEMIPTERA. . Aithus nitens, Kirby, sp.n. (p. 127.) . Pentatoma grossepunctatum, Kirby, sp.n. (p. 128.) . Lygeus subrufescens, Kirby. (p. 128.) . Brachyrhynchus lignicolus, Kirby, sp.n. (p. 129.) . Ricania flavifrontalis, Kirby, sp.n. (p. 131.) Paurostauria delicata, Kirby, sp.n. (p. 133.) . Vareia flaricostalis, Kirby, sp.n. (p. 133.) . Nogodina afinis (Kirby). (p. 134.) . Nogodina hyalina (Kirby). (p. 134.) . Nogodina subviridis, Kirby, sp.n. (p. 135.) . Nogodina subviridis, Kirby, sp.n., var. (p. 136.) . Bidis aristella, Kirby, sp.n. (p. 136.) . Bidis aristella, Kirby, sp.n. (p. 136.) . Clovia eximia, Kirby, sp.n. (p. 137.) . Issus (2) andrews, Kirby, sp.n. (p. 138.) . Idiocerus (?) punctatus, Kirby, sp.n. (p. 138.) Pik B.M.CHRISTMAS FE. ‘West, Newman imp. MHorman-Fisher del.etlith. PLA Xve ARACHNIDA. Fie. 1. Chelifer murray, Pocock, sp.n. Much magnified. (p. 156.) Fie. la. Chelifer murray. Flagellum of movable digit of mandible. (p. 156.) Fia. 2. Argtope remmwardti (Dol.). Enlarged one-fourth. (p. 159.) Fia. 3. Cyrtophora unicolor (Dol.). Enlarged one-fourth. (p. 160.) [This figure and that of Argiope reinwardti are taken from specimens preserved in alcohol. According to Mr. Andrews the abdomen in living examples is more voluminous, and in the case of C. unicolor the anterior prominences project much less than here represented. | Fie. 4. Heteropoda listeri, Pocock, sp.n. Face and mandibles. (p. 161.) [The beard of bristles clothing the front of the upper half of the mandibles stands out more clearly in the actual specimen than in the figure. | Fia. 4a. Heteropoda listerr. Vulva. 9. (p. 161.) Fic. 4b. Heteropoda listerr. Tarsus and distal end of palpus of ¢ from below. (p. 161.) Fie. 4c. Heteropoda listert. Bifid tip of flagellum and its sheath of palpal organ. (p. 161.) Fic. 4d. Heteropodu listert. Tibial spine of palp of ¢ from the side. (p. 161.) *- CHRISTMAS ISLAND. Plate XVI. F.0 Pickard - Cambridge. del.et ith. West, Newman imp. Arachnida. ‘ Se FRETS a Be ee ee oe nn ee ) f oP o. tet gory a yeaa Jal 4 bia eiee ; i AC Pa S nthe f, pare ‘a vi) » Z e ) 5 nv pa. K (7 iy see ; ‘1 Atoms “i See" - ; ; ao ee hh iy & é = 3, PLATE XVII. Pittosporum nativitatis, Baker, fil, spn. (p. 1’ Fig. 1. Branchlet showing inflorescence (natural ; Fig. 2. Flower (x 5). Fic. 3. Sepal (x 5). Fig. 4. Petal (x 5). ig Fig. 5. Stamens and ovary not fully developed (x 5; Fig. 6. Ovary not fully developed (x 5). * Fic. 7. Bract (x 5). | Plate XVII. B.M.CHRISTMAS ‘IP West, Newman imp. RMorgan del.et ith. Pittosporum. nativitatis, Baker fl. f) ee ca ‘s os ; Me , | es Sie § ane -* shit 4 - hs eke y ¥ 2 ‘3 ; Ais é , ‘ L PLATE XV UL — Panicum andrewsi, Rendle, sp.n. (p.192.) | Fic. 1. Barren glume, 1, viewed from inside. Fic. 2. Barren glume, ii, viewed from inside. ; ie Fic. 3. Barren glume, iii, viewed from inside and showing bis . pale. re Fic. 4. Fertile glume. Dorsal view. : Natural size. Figs. 1-4, parts of spikelet, x 18. . Plate XVIII. B.M. CHRISTMAS PF. ‘West, Newman imp - R.Morgan del.et ith. -Pamicum andrewsi, Rendle. A.BRendle anal. Pa AGT aR A Ke Fossin CoRALs. Fig. 1. Celoria andrewsi, Gregory, sp.n. Transverse section. ne ore, Fie. 2. Meandrina equisepta, Gregory, sp.n. Transverse section, Fig. 3. Orbicella murrayi, Gregory, sp.n. Transverse section. Fie. 4. Orbicella preheliopora, Gregory, sp.n. Transverse section. — Fic. 5. Acanthastrea patula, Gregory, var. nov. paucidentata. T verse section. | a Fie. 6. Anisocenia favoides, Gregory, sp.n. Transverse section. _ - . , Fie. 7. Anisocenia murrayt, Gregory, sp.n. Transverse section. Fie. 8. Coscinarea andrewsi, Gregory, sp.n. ‘Transverse mack 1 _ All the figures twice natural size. B.M.CHRISTMAS PF. Awe Plate XIX. UPI ibs SUES CANN, Hi ANS an re AMNLENNB pene “4 SLA SS FART Meee iba E. Drake ad nat.lith. West, Newman Tap : fosstl Corals. AW *2 diam. Fia. Fia. Fic. Fia. PIG: FI«. Fia. Fia. Fia. PLATE XX. FORAMINIFERAL LIMESTONES. No. 2. Oldest Limestone (Eocene or Oligocene) from south end of Flying Fish Cove. x 15. (p. 226.) No. 522. Cove. No. 924. CD: No. 220. x: No. 844. BD No. 562. x 0: No. 521. ? Oligocene Limestone, B of section, Flying Fish x 15. (p. 231.) Miocene Orbitoidal Limestone, Flying Fish Cove. (p. 233.) Miocene Orbitoidal Limestone, Flying Fish Cove. (p. 239.) Miocene Orbitoidal Limestone, ‘Flying Fish Cove. (p. 242.) Miocene Orbitoidal Limestone, Flying Fish Cove. (p. 243.) White Limestone from pinnacles at 500 feet over Flying Fish Cove. x 53. (p. 245.) No. 841. White Limestone from pinnacles at 500 feet over Flying Fish Cove. x 6. (p. 248.) No. 549. a! Os Miocene Orbitoidal Limestone, Flying Fish Cove. (p. 250.) B.M. CuristMAs Ib. PLATE XX. F. CHAPMAN, PHOTO. MORGAN & KIDD, COLLOTYPE. FORAMINIFERAL ROCKS: CHRISTMAS ISLAND. Fia. Fia. Fia. Fig. Fia. Fig. Fia. Fie. 10. De 12. 13. 14. 15. 16. 17. PLATE XXI. FORAMINIFERAL LIMESTONES. Specimen No. 968. Miocene Orbitoidal Limestone, south of Flying Fish Cove. x 6. (p. 252.) Specimen No. 347. Eocene or Oligocene Limestone from high cliff in Sidney’s Dale (see map). x 15. (p. 254.) Specimen No. 835. Miocene Orbitoidal Limestone, south of Flying Fish Cove. x 5. (p. 254.) Specimen No. 827. Miocene Orbitoidal Limestone, south of Flying Fish Cove. x 4$. (p. 255.) Specimen No. 827. Miocene Orbitoidal Limestone, south of Flying Fish Cove. x 6. (p. 255.) Specimen No. 581. Miocene Orbitoidal Limestone. x 5. (p. 255.) Specimen No. 986. Pebble of Orbitoidal Limestone in raised beach, north of Flying Fish Cove. x 2. (p. 253.) Specimen No. 5. From cracks in basalt on south side of Flying Fish Cove. x 15. (p. 258.) B.M. CHRISTMAS Ip. PLATE XXI. *. CHAPMAN, PHOO. MORGAN & KIDD, COLLOTYPE. FORAMINIFERAL RO€KS: CHRISTMAS ISLAND. a ’ an i ¥ . - x °f * : 97,>' ATA , . ae 4 fie ee ar a 4 eo a - é ' 3 P F ‘ ‘ 2 * Pe » “4 ‘ - oy ——— Scale of Miles ooo British Museum (Nat Hist.) Monograp FLYING FISH COVE Obo.cnotes (E% 10°25. 19'S. = (Admiralty Chore) Long. 105°42'57E ) | Pate beach, CHRISTMAS ISLAND : Partly from a sunvey -by 189 C.W.ANDREWS,F.CS. 1897-98. Flying Fish @, Smith Point 4 Seale of Miles OS, f Limestone x Be j 0 : : $ Smith Point Z B ooM 4 y) 7 © Nat. scale 1:100.000 or 1:58 miles - Linch se ° Heights wm feet Depths in. tathores 68 f » ‘a “ys (A o o> Orbitoidal = oes > os lmestone Freshwdter Stream soi S Thick ope and lofty trees Ke Se es lay thick jungla in places Re efs of Coral i \\\ BORNEO I} 4I¢6 / 18 Egeria Point S7 sate A South Point 971 449 Clenidinag » Christmas I —Eeweesws si Cocos ur Keeling I$ ‘ li 570 918 Scale of Miles oa a Reprinted hy permisston of the Royal. Geographical Society - : _-— = j ! et oe ae : : 2 : : : = = é H Horizontal Scale 1-6 inches =1mile. a 1839, = = a ee ‘ J er AREA, @ LIST OF THE CURRENT NATURAL HISTORY PUBLICATIONS OF THE TRUSTEES OF THE BRITISH MUSEUM. The following publications can be purchased through the Agency of Messrs. LONGMANS & Co., 39, Paternoster Row ; Mr. QUARITCH, 15, Piccadilly; Messrs. KEGAN PAUL, TRENCH, TRUBNER & CO., Paternoster House, Charing Cross Road; and Messrs. DULAU & Co., 37, Soho Square ; or at the NATURAL HISTORY MUSEUM, Cromwell Road, London, S.W. Catalogue of the Specimens and Drawings of Mammais, Birds, Reptiles, and Fishes of Nepal and Tibet. Presented by B. H. Hodgson, Esq., to the British Musuem. 2nd edition. By John Edward Gray. Pp. xii., 90. [With an account of the Collection by Mr Hodgson.] 1863, 12mo. 28. od. Catalogue of the Mammalia and Birds of New Guinea in the Collection of the British Museum. 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[With Systematic and Alphabetical Indexes.] 1892, Svo. 1/. 10s. Vol. XVIII. Catalogue of the Picarie in the Collection of the British Museum. Scansores, containing the family Picide. By Edward Hargitt. Pp. xv., 597. Woodcuts and 15 coloured Plates. [With Systematic and Alphabetical Jndexes.] 1890, 8vo. 1/. 6s. Vol. XIX. Catalogue of the Picariz in the Collection of the British Museum. Scansores and Coccyges : con- taining the families Rhainphastide, Galbulide, and Bucconide, by P. L. Sclater; and the families Indi- catoride, Capitonide, Cuculide, and Musophagide, by G. EH. Shelley. Pp. xii., 484: 13 coloured Plates. [ With Systematic and Alphabetical Indexes.] 1891, 8vo. Ll. 5s. Vol. XX. Catalogue of the Psittaci, or Parrots, in the Collection of the British Museum. By T. Salvadori. Pp. xvii., -658: Woodcuts and 18 coloured Plates. [With Systematic and Alphabetical Indexes.] 1891, 8vo. 1/. 10s. Vol. XXI. Catalogue of the Columba, or Pigeons, in the Collection of the British Museum. By T. Saivadori. Pp. xvii., 676 : 15 coloured Plates. [With Systematic and Alphabetical Indexes.] 1893, 8vo. 1/. 10s. Vol. XXII. Catalogue of the Game Birds (Péerocletes, Galline, Opisthocomt, Hemipodit) in the Collection of BRITISH MUSEUM (NATURAL HISTORY). 5 Catalogue of the Birds in the British Museum—continued. the British Museum. By W. R. Ogilvie Grant. Pp. xvi., 585: & coloured Plates. [With Systematic and Alphabetical Indexes.] 1893, 8vo. 17. 6s. 7 Vol. XXIII. Catalogue of the Fulicarie (Rallide and Heliornithide) and Alectorides (Aramide, Eurypy- gidz, Mesitide, Rhinochetide, Gruide, Psophiida, and Otididz) in the Collection of the British Museum. By R. Bowdler Sharpe. Pp. xiii., 353: 9 coloured Plates. [With Systematic and Alphabetical Indexes. | 1894, 8vo. 20s. Vol. XXIV. Catalogue of the Limicolz in the Collection of the British Museum. By R. Bowdler Sharpe. Pp. xii., 794. Woodcutsand 7 coloured Plates. [With eee and Alphabetical Indexes.] 1896, 8vo. l. Os. Vol. XXV. Catalogue of the Gavize and Tubinares in the Collection of the British Museum. Gavie (Terns, Gulls, and Skuas,) by Howard Saunders. Tubinares (Petrels and Albatrosses), by Osbert Salvin. Pp. xv., 475 ; woodcuts and 8 coloured Plates. [With Syste- matic and Alphabetical Indexes.] 1896, 8vo. 1/. 1s. Vol. XXVI. Catalogue of the Platalez, Herodiones, Steganopodes, Pygopodes, Alcz, and Impennes in the Collection of the British Museum. Plataleze (Ibises and Spoonbills) and Herodiones (Herons and Storks), by R. Bowdler Sharpe. Steganopodes (Cormorants, Gannets, Frigate-birds, Tropic-birds, and Pelicans), Pygopodes (Divers and Grebes), Alcz (Auks), and Im- pennes (Penguins), by W. R. Ogilvie-Grant. Pp. xvii., 687: Woodcuts and 14 coloured Plates. [With Sys- tematic and Alphabetical Indexes.] 1898, 8vo. LJ. 5s. Vol. XXVII. Catalogue of the Chenomorphe (Pala- medex, Phoenicopteri, Anseres), Crypturi, and Ratitz in the Collection of the British Museum. By T Salvadori. Pp. xv., 636: 19 coloured Plates. [With Systematic and Alphabetical Indexes.] 1895, 8vo. 17. 12s. A Hand-list of the Genera and Species of Birds. [Nomen- clator Avium tum Fossilium tum Viventium.] By R. Bowdler Sharpe, Lu.D. Vol. I. Pp. xxi., 303. [With Systematic Index.] 1899, 8vo. 10s. List of the Specimens of Birds in the Collection of the British Museum. By George Robert Gray :— Part III., Section I. Ramphastide Pp. 16. [With Index.] 1855, 12mo. 6d. Part III., Section Il. Psittacide. Pp. 110. [With Index.] 1859, 12mo. 2s. Part III., Sections II].and IV. Capitonide and Picide, Pp. 137. [With Index.] 1868, 12mo. 1s. 6d, é ‘LIST OF PUBLICATIONS OF THE List of the Specimens of Birds in the Collectioh of the British Museum—continued. Part IV. Columb. Pp. 73. [With Index.]> fean 12mo. Is. 9d. Part V. Galline. Pp. iv., 120. [With an Alphabetical Index.] 1867, 12mo. 1s. 6d. Catalogue of the Birds of the Tropical Islands of the Pacific Ocean in the Collection of the British Museum. By George Robert Gray, F.L.S., &c. Pp. 72. [With an Alphabetical Index.] 1859, 8vo. 1s. 6d. REPTILES. Catalogue of the Tortoises, Crocodiles, and Amphisbznians in the Collection of the British Museum. By Dr. J. E. Gray, F.R.S., &c. Pp. viii. 80. [With an Alphabetical Index. ] 1844, 12mo. Is. Catalogue of Shield Reptiles in the Collection of the British Museum. By John Edward Gray, F.R.S., &¢.:— Appendix. Pp. 28. 1872, 4to: 2s. 6d. Part II, Emydosaurians, Rhynchocephalia,and Amphis- benians. Pp. vi, 41. 25 Woodcuts. 1872, Ato. as. 6d. | | Hand-List of the Specimens of Shield Reptiles in the British Museum. By Dr. J. HE. Gray, F.R.S., F.LS., &e. _ Pp. iv., 124. [With an Alphabetical Index.] 1873, _-8vo. As. Catalogue of the Chelonians, Rhynchocephalians, and Crocodiles in the British Museum (Natural History). New Edition. By George Albert Boulenger. Pp. x., 311. 73 Woodcuts and 6 Plates. [With Systematic and Alphabetical Indexes.] 1889, 8vo. 15s. Catalogue of the Lizards in the British Museum (Natural His- tory). Second Edition. By George Albert Boulenger :— Vol. I. Geckonide, Kublepharide, Uroplatide, Pygo- podide, Agamide. Pp. xii., 436. 52 Plates. [With Systematic and Alphabetical Indexes.] 1885, 8vo. 20s. Vol. II. IRguanide, Xenosauride, Zonuride, Anguide, Anniellide, Helodermatide, Varanide, Xantusiide, Teiide, Amphisbenide. Pp. xiii, 497. 24 Plates. ei en Sy stematic and Alphabetical Indexes.] 1885, vo. 20s, Vol. III. Lacertide, Gerrhosauride, Scincide, Anelytro- pide, Dibamide, Chameleontide. Pp. xii.,575. 40 Plates. [With a Systematic Index and an Alphabetical Index to the three volumes.] 1887, &vo. 1/. 6s. BRITISH MUSEUM (NATURAL HISTORY). . 7 Catalogue of the Snakes in the British Museum (Natural History). By George Albert Boulenger, F.R.S. :— Vol. I., containing the families Typhlopide, Glauconiide, Boidz, Ilysiide, Uropeltide, Xenopeltide, and Colu- bride aglyphe, part. Pp. xiii., 448: 26 Woodeuts and 28 Plates. [With Systematic and Alphabetical Indexes.] 1893, 8vo. 17. Is. Vol. IL, containing the conclusion of the Colubride aglyphe. Pp. xi., 382: 25 Woodcuts and 20 Plates. | With Systematic and Alphabetical Indexes.] 1894, 8vo. 17s. 6d. Vol. III, containing the Colubride (Opisthoglyphe and Proteroglyphe), Amblycephalide, and Viperide. Pp. xiv., 727: 37 Woodcuts and 25 Plates. [With Systematic Index, and Alphabetical Index to the 3 volumes.] 1896, 8vo. 1/. 6s. Catalogue of Colubrine Snakes in the Collection of the British Museum. By Dr. Albert Giinther. Pp. xvi., 281. | With Geographic, Systematic, and Alphabetical Indexes. ] 1858, 12mo. 4s. | BATRACHIANS. Catalogue of the Batrachia Salientia in the Collection cf the British Museum. By Dr. Albert Giinther. Pp. xvi., 160. 12 Plates. [With Systematic, Geographic, and Alphabetical Indexes.] 1858, 8vo. 6s. | FISHES. Catalogue of the Fishes in the British Museum. Second edition. Vol. I. Catalogue of the Perciform Fishes in the British Museum. Vol. I. Containing the Centrarchide, Percide, and Serranide (part). By George Albert Boulenger, F.R.S. Pp. xix., 394. Woodcuts and 15 Plates. | With Systematic and Alphabetical Indexes.] 1895, 8vo. 15s. List of the Specimens of Fish in the Collection of the British Museum. Part I. Chondropterygii. By J. EH. Gray. Pp. x.,160. 2 Plates. [With Systematic and Alphabetical Indexes.] 1851, 12mo. 3s. Catalogue of Fish collected and described by Laurence Theodore Gronow, now in the British Museum. Pp. Vii., 196. [With a Systematic Index.] 1854, 12mo. 3s. 6d. 8 . LIST OF PUBLICATIONS OF THE Catalogue of Apodal Fish in the Collection of the British Museum. ByDr.Kaup. Pp. viii. 163. 11 Woodcuts and 19 Plates. 1856, 8vo. 10s. Catalogue of Lophobranchiate Fish in the Collection of the British Museum. By J.J. Kaup, Ph.D., &c. Pp. iv., 80. 4 Plates. [With an Alphabetical Index.] 1856, 12mo. 2s. MOLLUSCA. Guide to the Systematic Distribution of Mollusca in the British Museum. Part I. By John Edward Gray, Ph.D., F.R.S., &c. Pp. xii., 230. 121 Woodcuts, 1857, 8vo. 5s. List of the Shells of the Canaries in the Collection of the British Museum, collected by MM. Webb and Berthelot Described and figured by Prof. Alcide D’Orbigny in the “ Histoire Naturelle des Iles Canaries.” Pp. 32. 18954, 12mo. Ls. . List of the Shells of Cuba in the Collection of the British Museum, collected by M. Ramon de la Sagra. Described by Prof. Alcide d’Orbigny in the “ Histoire de ]’Ile de Cuba.” Pp. 48. 1854, 12mo. Ls. List of the Shells of South America in the Collection of the British Museum. Collected and described by M. Alcide D’Orbigny in the “Voyage dans l’Amérique Méridionale.” Pp. 89. 1854, 12mo. 2s. Catalogue of the Collection of Mazatlan Shells in the British Museum, collected by Frederick Reigen. Described by Philip P. Carpenter. Pp. xvi., 552. 1857, 12mo. 8s. List of Mollusca and Shells in the Collection of the British Museum, collected and described by MM. Hydoux and Souleyet in the “Voyage autour du Monde, executé “pendant les annees 1836 et 1837, sur la Corvette ‘La ‘“‘ Bonite,’”’ and in the “ Histoire naturelle des Mollusques “ Pteropodes.” Par MM. P. C. A. L. Rang et Souleyet. Pp. iv., 27. 1855, 12mo. 84d. : _ Catalogue of the Phaneropneumona, or Terrestial Operculated Mollusca, in the Collection of the British Museum. By Dr. L. Pfeiffer. Pp. 324. [With an Alphabetical Index. } 1852, 12mo. 5s. Catalogue of Pulmonata, or Air Breathing Mollusca, in the Collection of the British Museum. Part I. By Dr. Louis Pfeiffer. Pp. iv., 192. Woodcuts. 1855, 12mo. 2s. 6d. Catalogue of the Auriculide, Proserpinide, and Truncatellide in the Collection of the British Museum. By Dr. Louis Pfeiffer. Pp. iv., 150. Woodcuts. 1857, 12mo. Is. 9d. List of the Mollusca in the Collection of the British Museum. By John Edward Gray, Ph.D., F.R.S., &c. Part I. Volutide. Pp. 23. 1855, 12mo. 6d. Part II. Olivide. Pp. 41. 1865, 12mo. 1s. BRITISH MUSEUM (NATURAL HISTORY). 9 Catalogue of the Conchifera, or Bivalve Shells, in the Collection of the British Museum. By M. Deshayes :— Part I. Venerids, Cyprinide, Glauconomide, and Petricolada... Pp. iv., 216. 1853, 12mo. 3s. Part JI. Petricoladee (concluded); Corbiculade. Pp. 217-292. [With an Alphabetical Index to the two parts.| 1854, 12mo. 6d. BRACHIOPODA. Catalogue of Brachiopoda Ancylopoda or Lamp Shells in the Collection of the British Museum. [TJsswed as “ Catalogue of the Mollusca, Part IV.”] Pp. iv., 128. 25 Woodcuts. [ With an Alphabetical Index.] 1853, 12mo. 3s. POLYZOA. Catalogue of Marine Polyzoa in the Collection of the British Museum. Part III. Cyclostomata. By George Busk, F.R.S. Pp. viii., 39. 38 Plates. [With a Systematic Index.] 1875, 8vo. 5s. CRUSTACEA. Catalogue of the Specimens of Amphipodous Crustacea in the Collection of the British Museum. By C. Spence Bate, ER:S., @e.. Pp: iv:, 399.. 58 Plates. [With an’ Alpha- betical Index. | 1862, 8vo. 1/. 5s. ARACHNIDA. Descriptive Catalogue of the Spiders of Burma, based upon the Collection made by Eugene W. Oates and preserved in the British Museum. By TT. Thorell. Pp. xxxvi., 406. [With Systematic List and Alphabetical accel ok 1895, svo. 10s. 6d. MYRIOPODA. Catalogue of the Myriapoda in the Collection of the British Museum. By George Newport, F.R.S., P.E.S., &c. Part I. Chilopoda. Pp. iv., 96. [With an Alphabetical Index. ] 1856, 12mo. 1s. 9d. INSECTS. Coleopterous Insects. Nomenclature of Coleopterous Insects in the Collection of the British Museum :— Part VI. Passalide. By Frederick Smith. Pp. iv., 23. 1 Plate. [With Index.] 1852, 12mo. 8d. Part VII. Longicornia, I. By Adam White. Pp. iv., 174. 4 Plates. 1853, 12mo. 2s. 6d. Part VIII. Longicornia, II. By Adam White. Pp. 237. 6 Plates. 1855, 12mo. 3s. 6d. Part IX. Cassidide. By Charles H. eters Professor of Natural History, Stockholin. 229. | With Index.] 1856, 12mo. 3s. 10 IST OF PUBLICATIONS OF THE Hlustrations of Typical Specimens of Coleoptera in the Collection of the British Museum. Part I. Lycide. By — Charles Owen Waterhouse. Pp. x., 83. 18 Coloured Plates. [With Systematic and Alphabetical n= 1879, 8vo. 16s. Catalogue of the Coleopterous Insects of Madeira in the Collection of the British Museum. By T. Vernon Wollaston, M.A., F.L.S. Pp. xvi., 234 : i Pine [ With a Topographical Catalogue and an Alphabetical. si 1857, 8vo. 3s. Catalogue of the Coleopterous Insects of the Canaries in the Collection of the British Museum. By T. Vernon Wollaston, M.A., F.L.S. Pp. xiii, 648. [With Topo- graphical and Alphabetical Indexes.|] 1864, 8vo. 10s. 6d. Catalogue of Halticidze in the Collection of the British Museum. By the Rev. Hamlet Clark, M.A., F.LS. Physapodes and (Edipodes. Part I. Pp. xii. 301. Frontispiece and 9 Plates. 1860, 8vo. 7s. Catalogue of Hispide in the Collection of the British — Museum. By Joseph 8. Baly, M.E.S.,&¢. Part I. Pp.x., 172. 9 Plates. [With an ‘Alphabetical Index.] 1858, 8vo. 6s. Hymenopterous Insects. List of the Specimens of Hymenopterous Insects in the Collection of the British Museum. By Francis Walker, F.L.S. :-— . Part II. Chalcidites. Additional Species. Appendix. Pp. iv., 99-237. 1848, 12mo. 2s. Catalogue of Hyymenopterous Insects in the Collection of the British Museum. By Frederick Smith. 12mo. :— Part I. Andrenide and Apide. Pp. 197. 6 Plates. ; 1853, 2s. 6d. 7 Part II. Apide. Pp. 199-465. 6 Plates. [With an Alphabetical Index.] 1854, 6s. | Part III. Mutillide and Ppoeiiae Pp. 206. 6 Plates. 1855, 6s. | Part IV. Sphegide, Larride, and Crabronide. Pp. 207- 497. 6 Plates. [With an Alphabetical Index.] 1856, 6s. Part V. Vespide. Pp.147. 6 Plates. [With an Alpha- betical Index.] 1857, 6s. Part VI. Formicide. -Pp. 216. 14 Plates. [With an = Alphabetical Index.] 1858, 6s. Part VII. Dorylide and Thynnide. Pp. 76. 3 Plates. [ With an Alphabetical Index.] 1859, 2s. BRITISH MUSEUM (NATURAL HISTORY). 11 Descriptions of New Species of Hymenoptera in the Collection of the British Museum. By Frederick Smith. Pp. xxi, 240. [With Systematic and Alphabetical Indexes.] 1879, 8vo. 10s. List of Hymenoptera, with descriptions and figures of the Typical Specimens in the British Museum. Vol. L, Tenthredinide and Siricide. By W. F. Kirby. Pp. xxviii., 490. 16 Coloured Plates. [With Systematic and Alphabetical Indexes.] 1882, 8vo. Il. 18s. Dipterous Insects. List of the Specimens of Dipterous Insects in the Collection of the British Museum. By Francis Walker, F.L.S. Part VII. SupplementIII. Asilide. Pp. ii., 507-775. 1855, 12mo. 3s. 6d. Lepidopterous Insects. Catalogue of the Lepidoptera Phalenze in the British Museum. Vol.I. Catalogue of the Syntomide in the Collection of the British Museum. By Sir George F. Hampson, Bart. Pp. xxi., 559. 285 Woodcuts. [With Systematic and Alphabetical Indexes, and Table of the Phylogeny of the Syntomide.] 1898, 8vo., lds. —_———Atlas of 17 Coloured Plates, 8vo., 15s. Illustrations of Typical Specimens of Lepidoptera Heterocera in the Collection of the British Museum :— Part III. By Arthur Gardiner Butler. Pp. xviii., 82. 41-60 Coloured Plates. [With a Systematic Index. ] 1879, 4to. 27. 10s. Part V.' By Arthur Gardiner Butler. Pp. xii., 74. 78-100 Coloured Plates. [With a Systematic Index. ] 1881, 4to. 27. 10s. Part VI. By Arthur Gardiner Butler. Pp. xv., 89. 101-120 Coloured Plates. [Witha Systematic Index. ] 1886, 4to. 27. 4s. : Part VII. By Arthur Gardiner Butler. Pp. iv., 124. 121-138 Coloured Plates. [With a Systematic List. ] 1889, 4to. 27. Part VIII. The Lepidoptera Heterocera of the Nilgiri District. By George Francis Hampson. Pp. iv., 144. 139-156 Coloured Plates. [With a Systematic List.] 1891, 4to. 2. Part IX. The Macrolepidoptera Heterocera of Ceylon. By George Francis Hampson. Pp. v., 182. 157-176. Coloured Plates. [With a General Systematic List of Species collected in, or recorded from, Ceylon.] 1893, 4to. 20. 2s. Catalogue of Diurnal Lepidoptera of the family Satyridze in - the Collection of the British Museum. By Arthur Gardiner Butler, F.L.S., &¢. Pp. vi. 211. 5 Plates. [With an Alphabetical Index.] 1868, 8vo. 5s. bu. 12 LIST OF PUBLICATIONS OF THE Catalogue of Diurnal Lepidoptera described by Fabricius in the Collection of the British Museum. By Arthur Gardiner Butler, F.L.S., &c. Pp. iv., 303. 3 Plates. 1869, 8vo. 7s. 6d. Specimen of a Catalogue of Lycenide in the British Museum. By W. C. Hewitson. Pp. 15. 8 Coloured Plates. 1862, 4to. ll. Ls. List of Lepidopterous Insects in the Collection of the British Museum. Part I. Papilionide. By G. R. Gray, F.L.S. Pp. 106. [With an Alphabetical Index.] 1856, 12mo. 2s. List of the Specimens of Lepidopterous Insects in the Collection of the British Museum. By Francis Walker. 12mo. :— Part XIX. Pyralides. Pp. 799-1036. [With an Alpha- betical Index to Parts XVI.—XIX.] 1859, 3s. éd. Part XX. Geometrites. Pp. 1-276. 1860. 4s. Part XXI. Pp. 277-498. 1860, 3s. Part XXTL. = — Pp. 499-755. 1861, 3s. 6d. Part XXIII. —————— _ Pp. 756-1020. 1861, ds. 6d. Part XXIV. —————— __ Pp. 1021-1280. 1862, 3s. éd. Part XXV. -—————-- Pp. 1281-1477. 1862, 3s. Part XXVI. — — Pp. 1478-1796. [With an Alphabetical Index to Parts XX.-XXVI.] 1862, 4s. 6d. Part XXVII. Crambiies and Tortricites. Pp. 1-286. 1863, 4s. % Part XXVIII. Tortricites and Tineites. Pp. 287-561. 1863, 4s. Part XXIX. Tineites. Pp. 562-835. 1864, 4s. - Part XXX. Pp. 836-1096. [With an Alpha- betical Index to Parts XX VII.-XXX.] 1864, 4s. Part XXXI. Supplement. Pp. 1-821. 1864, 5s. Part XXXII.—- — Part 2. Pp: 322-706. 1865, 5s. Part XXXITI.————_-— Part 3. Pp. 707-12 1865, 6s. Part XXXIV.———--——_ Part 4. Pp. 1121-1533. 1865, 5s. 6d. Part XXXV. — Part 5. Pp. 1534-2040. [With an Alphabetical Index to Parts XXXI- XXXV.] 1866, 7s. Neuropterous Insects. Catalogue of the Specimens of Neuropterous Insects in mile Collection of the British Museum. By Francis Walker. 12mo. :— Part I. Phryganides—Perlides. Py. iv., 192. 1852, 2s. 6d. Part II. Sialide—Nemopterides. Pp. ii. 193-476. 1853, 3s. 6d. Part III. Termitide—Ephemeride. Pp. ii., 477-585. 1853, 1s. 6d. BRITISH MUSEUM (NATURAL HISTORY), 13 Catalogue of the Specimens of Neuropterous Insects in the Collection of the British Museum. By Dr. H. Hagen. Part I. Termitina. Pp. 34. 1858, 12mo. 6d. Orthopterous Insects. Catalogue of Orthopterous Insects in the Collection of the British Museum. Part I. Phasmide. By John Obadiah Westwood, F.L.S., &. Pp. 195. 48 Plates. [With an Alphabetical Index]. 1859, 4to. 37. Catalogue of the Specimens of Blattariz in the Collection of the British Museum. By Francis Walker, F.L.S., &c. Pp. 239. [With an Alphabetical Index.] 1868, 8vo. 5s. 6d. Catalogue of the Specimens of Dermaptera Saltatoria [Part I.] and Supplement to the Blattariz in the Collection of the British Museum. Gryllide. Blattariz. Locustide. By Francis Walker, F.L.S., &e. Pp. 224. [With an Alpha- betical Index.] 1869, 8vo. 5s. Catalogue of the Specimens of Dermaptera Saltatoria in the Collection of the British Museum. By Francis Walker, F.L.S., &c.— Part II. Locustide (continued). Pp. 225-423. [With an Alphabetical Index.] 1869, 8vo. 4s. 6d. Part III. Locustide (continued).—Acridide. Pp. 425- 604. [With an Alphabetical Index.] 1870, 8vo. 4s. Part IV. Acrididz (continued). Pp. 605-809. [With an Alphabetical Index.] 1870, 8vo. 6s. Part V. Tettigide.—Supplement to the Catalogue of Blattarize.—Supplement tothe Catalogue of Dermaptera Saltatoria (with remarks on the Geographical Distri- bution of Dermaptera). Pp. 811-850; 43; 116. [ With Alphabetical Indexes.] 1870, 8vo. 6s. Hemipterous Insects. Catalogue of the Specimens of Heteropterous Hemiptera in the Collection of the British Museum. By Francis Walker, F.L.S., &c. 8vo. :-— Part I. Seutata. Pp. 240. 1867. 5s. Part II. Scutata (continued). Pp. 241-417. 1867. 4s. Part III. Pp.418-599. [With an Alphabetical Index to Parts I., II., III., and a Summary of Geographical Distribution of the Species mentioned.] 1868. 4s. 6d. Part IV. Pp. 211. [Alphabetical Index.] 1871. 6s. Fart Ve< |. Pp. 202. — 1872. 5s. Part VI. Pp. 210. ————- ———-——-_ 1873. 5s. Part Vil. Pp.213. ————--—————___ 1873. 6s. Part VIII. Pp. 220. —__—_—____———— 1873. 6s. éd. 14 LIST OF PUBLICATIONS OF THE Homopterous Insects. List of the Specimens of Homopterous Insects in the Collec- — tion of the British Museum. By Francis Walker. Supple- ment. Pp. ii., 369. [With an Alphabetical Index.] 1858, 12mo., 4s. 6d. VERMES. Catalogue of the Species of Entozoa, or Intestinal Worms, contained in the Collection of the British Museum. by Dr. Baird. Pp. iv., 182. 2 Plates. [With an Index of the Animals in which the Entozoa mentioned in the Catalogue are found, and an Index of Genera and Species.] 1853, 12mo. 2s. ANTHOZOA. Catalogue of Sea-pens or Pennatulariide in the Collection of the British Museum. By J. E. Gray, F.R.S., &c. Pp. iv., 40. 2 Woodcuts. 1870, 8vo. 1s. 6d. Catalogue of Lithophytes or Stony Corals in the Collection — of the British Museum. By J. E. Gray, F.R.S., &e. Pp. iv., 51. 14 Woodcuts. 1870, 8vo. 3s. f Gutaloane of the Madreporarian Corals in the British Museum (Natural History) :— Vol. I. The Genus Madrepora. By George Brook. Pp. xi., 212. 35 Collotype Plates. [With Systematic and Alphabetical Indexes and Explanation of the Plates.] 1893, 4to. 17. 4s. Vol. II. The Genus Turbinaria; the Genus Astreopora. By Henry M. Bernard, M.A. Cantab., F.L.S., F.Z.S. Pp. iv., 106. 30 Collotype and 3 Lithographic Plates. [With Index of Generic and Specific Names, and Explanation of the Plates.] 1896, 4to. 18s. Vol. III. The Genus Montipora; the Genus Anacro- pora. By Henry M. Bernard, M.A. Pp. vii., 192. 30 _ ‘Collotype and 4 Lithographic Plates. [With Syste-_ _ matic Index, Index of Generic and Specific Names, and Explanation of the Plates.] 1897. Ato. 1/. 4s. BRITISH ANIMALS, - Catalogue of British Birds in the Collection of the British Museum. By George Robert Gray, F.L.S., F.Z.8., &c. Pp. xii., 248. [Witha List of Species.] 1863, 8vo. ds. 6d. Catalogue of British Hymenoptera in the Collection of the British Museum. Second edition. Part I. Andrenide and Apide. By Frederick Smith, M.E.S. New Issue. Pp. xi., 236, 11 Plates. [With Systematic and. Alpha- betical Indexes.] 1891, 8vo. 6s. BRITISH MUSEUM (NATURAL HISTORY). 15 Catalogue of British Fossorial Hymenoptera, Formicidae, and Vespidze in the Collection of the British Museum. By Frederick Smith, V.P.E.S. Pp. 236. 6 Plates. [With an Alphabetical Index.] 1858, 12mo. 6s. A Catalogue of the British Non-parasitical Worms in the Coliection of the British Museum. By George Johnston, M.D., Edin., F.R.C.L., Ed., Lu.D., Marischal Coll., Aber- deen, &c. Pp. 365. Woodcutsand 24 Plates. [With an Alphabetical Index.] 1865, 8vo. 7s. Catalogue of the British Echinoderms in the British Museum (Natural History). By F. Jeffrey Bell, M.A. Pp. xvii., 202. Woodcuts and 16 Plates (2 Coloured). [With Table of Contents, Tables of Distribution, Alphabetical Index, - Description of the Plates, &c.] 1892, 8vo. 12s. 6d. List of the Specimens of British Animals in the Collection of the British Museum; with Synonyma and References to figures. 12mo.:— Part IV. Crustacea. By A. White. Pp.iv.,141. (With an Index.) 1850. 2s. 6d. Part V. Lepidoptera. By J. F. Stephens. 2nd Edition. Revised by H. T. Stainton and E. Shepherd. Pp. iv., 224, 1856, 1s. 9d. . Part VI. Hymenoptera. By F.Smith. Pp.134. 1851. 2s. Part VII. Mollusca, Acephala and Brachiopoda. By De JieMeGrayi Pp. iv. Lote) 1854, 3s... 6d. Part VIII. Fish. By Adam White. Pp. xxiii., 164. (With Index and List of Donors.) 1851, 3s. 6d. _- Part IX. Eggs of British Birds. By George Robert Gray. Pp. 143. 1852, 2s. 6d. Part XI. Anoplura, or Parasitic Insects. By H. Denny. Pp. iv., 51. — 1852, 1s. Part XII. Lepidoptera (continued). By James F. Stephens. Pp. iv., 54. 1852, 9d. Part XIII. Nomenclature of Hymenoptera. By _. Frederick Smith. Pp. iv., 74. 1853, 1s.4d. ~ Part XIV. Nomenclature of Neuroptera. By Adam 5» White. Pp. iv., 16. 1853, 6d. Part XV. Nomenclature of Diptera, 1. By Adam oh White.» Pp. iv., 42: 1853, 1s. Part XVI. Lepidoptera (completed). By H.'T. Stainton. Pp. 199. [With an Index.] 1854, 3s. Part XVII. Nomenclature of Anoplura, Kuplexoptera, ‘and Orthoptera. By Adam White. Pp. iv., 17 1855, 6d. , PANES. Catalogue of the African Plants collected by Dr. Friedrich Welwitsch in 1853-61.—Dicotyledons. By William Philip Hiern, M.A., F.L.S., &. :— Part I. [Ranunculacez to Rhizophoracee.| Pp. xxvi., 336.. [ With Portrait of Dr. Welwitsch, Introduction, Bibliography, and Index of Genera.] 1896, 8vo. 7s. 6d. 16 LIST OF PUBLICATIONS OF THE Catalogue of African Plants—continued. Part II. Combretaceze to Rubiacew. Pp. 337-510. [ With Index of Genera.] 1898, 8vo. 4s. Part III. Dipsacez to Scrophulariaceza. Pp. 511-784. [ With Index of Genera.] 1898, 8vo. 5s. Moll Tsieart VL Monocotyledons and Gymnosperms. By Alfred Barton Rendle, M.A., D.Sc. F.L.S., Assistant, Department of Botany. Pp. 260. [With Index of Genera.] 1899, 8vo. 6s. A Monograph of Lichens found in Britain : being a Doudrim tive Catalogue of the Species in the Herbarium of the British Museum. By the Rev. James M. Crombie, M.A., F.L.S., F.G.S., &c. Part I. Pp. viii.,.519:: 74 Woodeuts. [With Glossary, Synopsis, Tabular Conspectus, and Index. ] 1894, 8vo. 16s. ie Monograph of the Mycetozoa: being a Descriptive Catalogue of the Species in the Herbarium of the British Museum. By Arthur Lister, F.L.S. Pp. 224. 78 Plates and 51 Woodcuts. [With Synopsis of Genera and List of Species, and Index.] 1894, 8vo., lds. List of British Diatomacew in the Collection of the British Museum. By the Rev. W. Smith, F.L.S., &c. Pp. iv., 55. 1859, 12mo. Is. FOSSILS. Catalogue of the Fossil’ Mammalia in the British Museum (Natural History). By Richard Lydekker, B.A., F.G.S. :— Part I. Containing the Orders Primates, Chiroptera, Insectivora, Carnivora, and Rodentia. Pp. xxx., 268. 33 Woodcuts. [With Systematic and Alphabetical Indexes.] 1885, 8vo. 5s. Part II. Containing the Order Ungulata, Suborder Artiodactyla. Pp. xxii., 324. 39 Woodcuts. [With Systematic and Alphabetical Indexes.] 1885, 8vo. 6s. Part III. Containing the Order Ungulata, Suborders Perissodactyla, Toxodontia, Condylarthra, and Ambly- poda. Pp. xvi.,186. 30 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.] 1886, 8vo. 4s. Part IV. Containing the Order Ungulata, Suborder Proboscidea. Pp. xxiv., 235. 32 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.] 1886, 8vo. 5s. Part V. Containing the Group Tillodontia, the Orders Sirenia, Cetacea, Edentata, Marsupialia, Monotremata, and Supplement. Pp. xxxv., 345. 55 Woodcuts. [ With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.} 1887, Svo. 6s. Catalogue of the Fossil Birds in the British Museum (Natural History). By Richard Lydekker, B.A. Pp. xxvii., 368. 75 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms. ] bas . 8vo. 10s. 6d. 7) ee BRITISH MUSEUM (NATURAL HISTORY). ae Catalogue of the Fossil Reptilia and Amphibia in the British Jaldins (Natural History). By Richard Lydekker, B.A., PartI. Containing the Orders Ornithosauria, Crocodilia, Dinosauria, Squamata, Rhynchocephalia, and Pro- terosauria. Pp. xxviii., 309. 69 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.] 1888, 8vo. 7s. 6d. Part II. Containing the Orders Ichthyopterygia and Sauropterygia. Pp. xxi., 307. 85 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.] 1889, 8vo. 7s. 6d. Part III. Containing the Order Chelonia. Pp. xviii., 239. 53 Woodcuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms.| 1889, 8vo. 7s. 6d. Part IV. Containing the Orders Anomodontia, Ecaudata, Caudata, and Labyrinthodontia; and Supplement. Pp. xxiii, 295. 66 Woodcuts. [With Systematic Index, Alphabetical Index of Genera and Species, including Synonyms, and Alphabetical Index of Genera and Species to the entire work.] 1890, 8vo. 7s. 6d. Catalogue of the Fossil Fishes in the British Museum (Natural History). By Arthur Smith Woodward, F.G.S., F.Z.8. :— Part I. Containing the Elasmobranchii. Pp. xlvii., A474, 13 Woodcuts and 17 Plates. [With Alphabetical Index, and Systematic Index of Genera and Species. |] 1889, 8vo. 21s. Part Il. Containing the Elasmobranchii (Acanthodii), Holocephali, Ichthyodorulites, Ostracodermi, Dipnoi, and 'Teleostomi (Crossopterygii and Chondrostean Actinopterygii). Pp. xliv., 567. 538 Woodcuts and 16 Plates. [With Alphabetical Index, and Systematic Index of Genera and Species.] 1891, Svo. 21s. Part III. Containing the Actinopterygian Teleostomi of the Orders Chondrostet (concluded), Protospondyli, Aetheospondyli, and Isospondyli (in part). Pp. xlii., 544. 45 Woodcuts and 18 Plates. [With Alphabetical Index, and Systematic Index of Genera and Species. ] 1895, 8vo. 21s. Systematic List of the Edwards Collection of British Oligocene and Eocene Mollusca in the British Museum (Natural History), with references to the type-specimens from similar horizons contained in other collections belonging to the Geological Department of the Museum. By Richard Bullen Newton, F.G.S. Pp. xxviii., 865. [With table of Families and Genera, Bibliography, Correlation-table, Appendix, and Alphabetical Index.] 1891, 8vo. 6s. 43374 . B 18 LIST OF PUBLICATIONS OF THE Catalogue of Tertiary Mollusca in the Department of Geology, British Museum (Natural History). Part I. The Austra- lasian Tertiary Mollusca. By George F. Harris, F.G.S., ete. Pp. xxvi.,407. 8 Plates. [With Table of Families, Genera, and Subgenera, and Index.] 1897, 8vo. 10s. Catalogue of the Fossil Cephalopoda in the British Museum (Natural History) :— Part I. Containing part of the Suborder Nautiloidea, con- sisting of the families Orthoceratide, Endoceratide, Actinoceratide, | Gomphoceratide, Ascoceratide, Poterioceratidz, Cyrtoceratide, and Supplement. By Arthur H. Foord, F.G.S. Pp. xxxi., 344. 51 Woodcuts. [With Systematic Index, and Alphabetical Indéx of Genera and Species, including Synonyms.] 1888, Svo. 10s. 6d. Part II. Containing the remainder of the Suborder Nautiloidea, consisting of the families Lituitide, Trochoceratids, Nautilide, and Supplement. By Arthur H. Foord, F.G.S. Pp. xxviii., 407. 86 Wood- cuts. [With Systematic Index, and Alphabetical Index of Genera and Species, including Synonyms. | 1891, 8vo. 15s. Part III. Containing the Bactritide, and part of the Subarder Ammonoidea. By Arthur H. Foord, Ph.D., ¥.G.S., and George Charles Crick, A.R.S.M., F.G.S. Pp. xxxiii., 303. 146 Woodcuts. [With Systematic Index of Genera and Species, and Alphabetical Index. | L897, Svoriys\od- List of t: heTypes and Figured Specimens of Fossil Cephalopoda in the British Museum (Natural History). By G. C. Crick, ¥.G.8. ,Pp. 103. [With Index.]’ 1898, 8vo. 2s: Ga: A Catalogue "of British Fossil Crustacea, with their Synonyms and the Range in Time of each Genus and Order. By Henry Woodward, F.R.S..-Pp. . xii.,- 155. (nae Alphabetical Index.] 1877, 8vo. 5s. Catalogue of the Fossil Bryozoa in the Department of Geology, British Museum (Natural History):—The Jurassic Bryozoa. By J. W. Gregory, D.Sc., F.G.S., Vga! a [vili.,] 239. 22 Woodcuts and 11 Plates. [With List of Species and Distribution, Bibliography, Index, and Explanatien of Plates. ] 1896, 8vo. 10s. A Catalogue of the Fossil Bryozoa in the Department of Geology, British Museum (Natural History) :—The Creta- ceous Bryozoa. Vol. I. By J. W. Gregory, DSe5 f-aees Pp. viil., 457. 64 Woodcuts and 17 Plates. [With Index and Explanation of Plates.] 1899, 8vo. 16s. Catalogue of the Blastoidea in the Geological Department of the British Museum (Natural History), with an account of the morphology and systematic position of the group, and a revision of the genera and species. By Robert Etheridge, jun., of the Department of Geology, British Museum (Natural History), and P. Herbert Carpenter, D.Sc., F.R.5., F.L.S. (of Eton College). Pp. xv.,322. 20 Plates. [With Preface by Dr. H. Woodward, Table of Contents, General Index, Explanations of the Plates, &c.] 1886, 4to. 25s. | BRITISH MUSEUM (NATURAL HISTORY). 19 The Genera and Species of Blastoidea, with a List of the Specimens in the British Museum (Natural History). By PF. A. Bather, M.A., F.G.S., of the Geological Department. oer Pf pox 70. “L Woodeut: 1899, Svo. 3s. Catalogue of the Fossil Sponges in the Geological Department of the British Museum (Natural History). With descrip- tions of new and little known species. By George Jennings Hinde, Ph.D., F.G.S. Pp. viii., 248. 38 Plates. [With a Tabular List of Species, arranged in Zoological and Stratigraphical sequence, and an Alphabetical Index. | 1883, 4to. 12. 10s. Catalogue of the Fossil Foraminifera in the British Museum (Natural History). By Professor T. Rupert Jones, F.R.S., &c. Pp. xxiv., 100. [With Geographical and Alphabetical Indexes.|] 1882, 8vo. 5s. Catalogue of the Paleozoic Plants in the Department of Geology and Paleontology, British Museum (Natural History). By Robert Kidston, F.G.S. Pp. vili., 288. [With a list of works quoted, and an Index.] 1886, 8vo. ds. Catalogue of the Mesozoic Plants in the Department of Geology, British Museum (Natural History). The Wealden Flora. By A. C. Seward, M.A., F.G.S., University Lecturer in Botany, Cambridge :— Part JI. Thallophyta—Pteridophyta. Pp. xxxviii., 179 : 17 Woodcuts and 11 Plates. [With Preface by Dr. Woodward, Alphabetical Index of Genera, Species, &c. Explanations of the Plates, &c.] 1894, 8vo. 10s. Part II. Gymnosperme. Pp. viii., 259. 9 Woodcuts and 20 Plates. (With Alphabetical Index, Explana- tions of the Plates, &c.] 1895, 8vo. 15s. GUIDE-BOOKS. (To be obtained only at the Museum.) Guide to the Galleries of Mammalia in the Department of Zoology of the British Museum (Natural History). 6th Edition. Pp. 120. 57 Woodcuts and 4 Plans. Index. 1898, 8vo. 6d. Guide to the Galleries of Reptiles and Fishes in the Depart- ment of Zoology of the British Museum (Natural History). Ath Edition. Pp. iv.,119. 101 Woodcuts. Index. 1898. 8vo. 6d. A Guide to the Fossil Mammals and Birds in the Department of Geology and Paleontology in the British Museum (Natural History). 7th Edition. [By Henry Woodward. | Pp. xii., 103. 116 Woodcuts. [With List of Illustrations, Table of Stratified Rocks, and Index.] 1896, 8vo. 6d. A Guide to the Fossil Reptiles and Fishes in the Department of Geology and Palxontology in the British Museum (Natural History). [By Henry Woodward.] Pp. xiVv., 129: 165 Woodcuts. [With List of Illustrations, Table of Stratified Rocks, and Index.] 1896, 8vo. 6d. 20) LIST OF PUBLICATIONS A Guide to the Fossil Invertebrates and Plants in the Department of Geology and Paleontology in the British Museum (Natural History). [By Henry Woodward. ] Pp. xvi., 158. 182 Woodcuts. [With List of Illustrations, Table of Stratified Rocks, Introduction, and Index.] 1897, Svo. ls. The same, in two parts :— Part I. Mollusca to Bryozoa. Pp. xii., 64. 107 Wood- cuts. [With List of Illustrations, Table of Stratified Rocks, and Introduction.] 1897, 8vo. 6d. Part II. Insecta to Plants, &c. Pp. ix., 64*-158. Woodcuts 108-182. [With List of Illustrations and Index to the two parts.] 1897, Svo. 6d. Guide to Sowerby’s Models of British Fungi in the Depart- ment of Botany, British Museum (Natural History). By Worthington G. Smith, F.L.S. Pp. 82. 93 Woodeuts. With Table of Diagnostic Characters, and Index. [2nd Kdition.] 1898, 8vo. 4d. Guide to the British Mycetozoa exhibited in the Department of Botany, British Museum (Natural History). By-Arthur Lister, F.L.S. Pp. 42. 44 Woodcuts. Index. 1895, Svo. 3d. A Guide to the Mineral Gallery of the British Museum (Natural History). [By L. Fletcher, M.A., F.R.S.] Pp.32. Plan. 1898, 8vo. ld. The Student’s Index to the Collection of Minerals, British Museum (Natural History). [By L. Fletcher, M.A., F.R.8.] Pp. 34. With a Plan of the Mineral Gallery. 1899, Svo. 2d. An Introduction to the Study of Minerals, with a Guide te the Mineral Gallery of the British Museum (Natural History). By. L. Fletcher, M.A.,-F.R.S: ~ Pope 41 Woodcuts. With Plan of the Mineral Gallery and — Index. 1897, 8vo. 6d. An Introduction to the Study of Rocks. By L. Fletcher, M.A., F.R.S. Pp. 118. [With plan of the Mineral Gallery, Table of Contents, and Index.] 1898, 8vo. 6d. An Introduction to the Study of Meteorites, with a List of the Meteorites represented in the Collection. By L. Fletcher, M.A., F.R.S. Pp. 95. [With a Plan’ Gite Mineral Gallery, and an Index to the Meteorites repre- sented in the Collection.] 1896, 8vo. 6d. HK. RAY LANKESTER, Director. British Museum (Natural History), Cromwell Road, London, S.W. 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