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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
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. . 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.
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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.
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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 Op. cit., 0, p. 16 (E879).
Mammalia. 383
This species is by far the commonest of the mammals found
in the island; in every part I visited, it occurred in swarms.
During the day nothing is to be seen of it, but soon after sunset
numbers may be seen running about in all directions, and the
whole forest is filled with its peculiar querulous squeaking and
the noise of frequent fights. These animals, like most of those
found in the island, are almost completely devoid of fear, and
in the bush if a lantern be held out they will approach to examine
the new phenomenon. As may be imagined, they are a great
nuisance, entering the tents or shelters, running over the sleepers,
and upsetting everything in their search for food. They seem to
eat anything, and destroy any boots or skins incautiously left
within their reach. Their natural food appears to be mainly fruits
and young shoots, and to obtain the former they ascend trees to
a great height. I have often seen them run up the trailing stems
of the lianas, and, in fact, they can climb as well as a squirrel.
In the settlement they utterly destroy all the fruit they can get at,
and frequently come into conflict with the fruit-bats on the tops
of the papaia-trees. A number of dogs is kept to keep them
in check, and near the settlement they are certainly already less
numerous than elsewhere.
In the daytime these rats live in holes among the roots of trees,
in decaying logs, and shallow burrows. They seem to breed all
the year round.
In the bush beaten tracks a few inches broad may often be seen,
and Mr. Ross informs me that these are made by rats travelling
in great numbers in search of food. I never had an opportunity
of observing this, and am not sure whether it is this species or
Mus nativitatis which makes the paths.
The measurements of the specimens of this species in the pr ere at
collection are given below :—
Head and Body. Tail. Ear. Hind-foot.
3 : 238 mm. ey a0 mit) i. 24 mm. ae 49 mm.
ze yey ate "iS Gin os ae 2. ns ee. 50M,
g 238 4,, Ese Nee af Pane? | eee
En 210 1,5 Ae ee DAD Ros es 7) Doe ADs ss
é 210. t;, SO ee AS 2B A oy 50 ,,
gd 208 ,, SO gees oe) OR te Soe eye,
3 200) \;, ce DASE bee O3} fs ane au. 43
é ESf 3, Bag. mee 4. Bins: Bae 4G>s;,
é ieee ie oe ADC 3, sad 93\,; Gs AD 55
a 152 ,, Sig Ge a tee ee 40s,
8 200 55 pak ee ee oS ee a AD. 55
2 een ee OOM ag hae Te ant: GO "5
9 240 ,, eet Soar ee pare.) ae st Sa AG
: 7 om dal? 4 DOL 5s Aa pe ae B- 47 55
D
34 Christmas Island.
NOTES ON THE OSTEOLOGY OF WYUS NATIVITATIS
AND MUS MACLEARL.
By Dr. C. I. Forsyra Masor, F.Z.S.
(PLATE II, Jis.)
Even if it were not known that Jus nativitatis is terrestrial and
burrowing, while us macleart is arboreal, the examination of the
manus of both species would reveal this fact at once. The bones of
the antebrachium, the carpals, metacarpals, and proximal phalanges
Fig. 1.—Antebrachium and carpus of Mus macleari.
Fig. 2.—Antebrachium and carpus of Mus nativitatis.
R, radius; U, ulna; +r, radiale; «, ulnare; 2m, radiale marginale ;
p, pisiforme; c, centrale; 1-4, first to fourth carpale; a, dorsal
phalange of first digit ; i-v, first to fifth digit.
are all slenderer and more elongate in the latter species, stouter
and broader in the former, the longitudinal dimensions of the
fore-limb as a whole being about the same in both.
Mammalia. 35
The above remark does not, however, apply to the ungual
phalanges, which in Jf nativitatis are longer, stronger, and less
curved than in the other species; the difference in length is the
more striking, as with regard to the proximal phalanges and
metapodials the proportions are reversed, these being more elongate
in M. macleart, as already pointed out.
The ungual phalange of the first digit of IL nativitatis is
not different in character from those of the other digits. In
M. macleart the whole of the thumb, including the Metac. i, is
more reduced than in the former species; and its ungual phalange
has a rounded, nail-like form, absolutely different from the claw-
like, curved ungual phalanges in the other fingers, and resembling
somewhat the same element in Primates. A still more appropriate
comparison of the digits of the arboreal JL macleari is with that
of Sevurus (e.g. S. rulgaris), where we find the same curved, claw-
like, ungual phalanges of digits ii-v, and the same rounded,
nail-like, ungual phalange of the first digit. The reduction of the
thumb has, however, in the squirrel, proceeded further than in
M. macleari; whilst the third and fourth digits have further
proceeded in the opposite sense, being disproportionately long.
In both JL nativitatis and I. macleart, an ossicle overlies,
dorsally, the interphalangeal articulation of the thumb. I have,
on a recent occasion, P.Z.S. London, 1899, p. 430, suggested that
this ossicle, which, although never mentioned before, is of quite
common occurrence in Rodentia and Insectivora, may be the second
phalange of the thumb, having been thrust out on the dorsal surface.
In the same place, quoted before, I have treated at length of
the distal pisiform of Muride, ete.; this bone forms, so to say,
a ‘pendant’ to the distal ‘prepollex’ (see below); it occurs in
both the species. See Text-fig. 5, op. cit.
The ossicle, which in the figures given in the above quoted
paper is marked wz, is equally present in both species from
Christmas Island, situated on the volar side, between the latero-
distal angle of the radius and the pisiform; in old specimens
it becomes fused with the former, but it is quite possible that it
often vanishes.
In I. nativitatis it is much smaller than in the other species.
Marginal radiale—The only writer, to my knowledge, who has
_ made mention of the ‘prepollex’ in the genus Jus, is Emery,
who describes it in Jf decumanus. In this species there is in
connection with the distal extremity of the bone in question
a lamina of tendinous connective tissue haying cartilaginous con-
sistence (‘‘eine knorpelharte Platte von schnigem Bindegewebe as
and acting as a support to the very prominent and compact radial
pad. The single bone of Mus decumanus is considered to be the
homologue of the proximal of the two bones occurring 1n Pedetes ;
to the distal bone of the latter would correspond the ‘ tendinous
lamina’ of Mus decumanus. ‘the character of a cartilage being
denied to the latter structure, the inference drawn from this is that
36 Christmas Island.
its homologue in Pedetes is a dermal bone of secondary origin.
In the latter genus the radial pad of other Rodents has been
transformed into the volar prominence sheathed with a horny cap;
in other words, the structure which in most Rodents is an organ of
touch has been adapted to fossorial functions in Pedetes.*
It is not clear to me on what grounds Emery here denies
a cartilaginous condition to the distal element of Mus decumanus.
In a subsequent memoir? he seems disposed to adopt a different
view. After having shown that in Marsupialia the ‘ prepollex ’
is ‘typically’ composed of two elements, he adds: ‘‘It will be of
particular interest to investigate whether in other mammals,
provided with a compound prepollex, the distal element has
a cartilaginous Anlage (‘knorpelig angelegt wird’), and is the
homologue of the distal portion of the marsupial prepollex.”
Like all Muride which have come under my observation,
both Mus natiwitatis and Ifus macleart have a large-sized marginal
radiale, articulating with the ‘scapholunar’ and the Metac. i on
their median and volar side,. and thence extending obliquely across
the vola in the direction of the distal pisiform bone. In both the
species there is attached to the distal and ulnar margin of the
marginal radiale, what appears to be a laminar cartilaginous
appendix, incompletely ossified on the ulnar side. Neither of the
two specimens—one from each species—is adult. I expect that in
adult specimens the ossification will be found to extend over the
whole of the distal part also. This condition I find to be the case
in an individual of a genus closely allied with Jus, viz. in
Arvicanthis (A. niloticus), although the specimen is not perfectly
adult.
The principal differences in the skulls of the two specimens have
been pointed out by O. Thomas (P.Z.S., 1888, pp. 5383, 534), and
are borne out by the figures of Plate II (67s), The skull of
M. nativitatis is weaker, more slender, and narrower than that
of the other species; the outer wall of the infraorbital foramen
is shorter and projects less forward; the incisive foramina extend
farther backwards. The molars of this species likewise are weaker
and less complicated with secondary cusps. In JM. macleari, the
outer cusps of the upper and the inner cusps of the lower molars
are much stronger than the corresponding parts in JL. nativitatis.
In several specimens of the latter the teeth present a diseased
appearance, which is not the case in any of the specimens of
M. macleart. I append the measurements in millimetres of some
of the skulls collected by Mr. Andrews, three of J. macleari and
two of I. nativitatis.
1 C. Emery, ‘‘ Zur Morphologie des Hand- und Fuss-skelets’?: Anat. Anz.,
Vv, pp- 288-291 (1890).
2 C. Emery, ‘‘ Beitrage z. Entwicklungsgesch. und Morphologie des Hand- und
Fuss-skelets der Marsupialier ’’ : Semon’s Forschungsreisen, li, p. 394 (1897).
Manmalia—A ves. 37
| 2 ne
| § S g = 33
: s&s Conn | > 10 > ~ 2 S = a:
. . . fl
Seal wsh He Neetu Gee
Basilar length (Henselion) . 47-4 40°5 42 42°5 | 425
Greatest breadth of skull ee o26rk 22°5 23°5 23°5 | 23°5
Length of nasals ............... 19°6 18 | 18-5 19°5 1y
Greatest breadth of nasals ... 5°8 OO: the ae anObes| 5 5°
Least breadth ininterorbital : : : wy ee
COWSEICHON :.........<. ae oe li 13 pater
Least length of outer wall ) | ‘ te Ln fet ;
of infraorb. foramen . | et ue ae me | ay
Length of palate ............... | 80°1 24:0 24:0 2275.7 |» 28
Breadth outside m.! ......... fa elit) sD 9-0 8° 9 —
Back of incisor to m.1 ... re Bit 14-5 | 214 16 15°5
Length of upper molar series. 8-0 8-0 8-0 7 | G50
Length of lower molar series. 8°2 | 8-0 8:0 GPS slo) Grd
AES.
By R. Bowptzr SHarrz, LL.D., F.L.S., F.Z.S.
(PLATES II-VI.)
Wuen the ‘Flying Fish” under Captain Maclear first visited
Christmas Island in January, 1887, two new species of birds were
discovered by the expedition, viz., Carpophaga whartoni and
Lurdus erythropleurus. The ‘ Egeria” shortly afterwards paid
a visit to the island, and Mr. J. J. Lister, who was naturalist
to the expedition, made a good collection of birds and discovered
several new species. His notes on his collection were also of great
interest.
Mr. Andrews obtained series of all the species found on Christmas
Island by Mr. Lister, and he was able to add several migratory
species which the other expeditions had not met with, while the
number of birds and eggs which he has obtained evince great
energy on his part. In the following pages his field notes are
accompanied by his initials ‘C. W. A.’
Order COLUMBIFORMES.
1. Carpophaga whartoni.
Carpophaga whartoni, Sharpe, P.Z.S., 1887, p. 514, pl. xiii; Lister, Pi ZiS.,
1888, p. 520; Salvad., Cat. B. Brit, Mus., xxi, p. 184 (1893) ;
Sharpe, Handl. B., i, p. 64 (1899).
No. 6, g ad. Flying Fish Cove, August 8, 1897.
No. 57, Q ad. Flying Fish Cove, October 21, 1897.
38 Christmas Island.
No. 61, g ad. Flying Fish Cove, October 22, 1897.
a, 6, Q juv. Phosphate Hill, October 24, 1897.
c,d,e, 6 ad. etimm. Flying Fish Cove, November 29, 1897.
No. 72, d imm. Flying Fish Cove, November 21, 1897.
d ad. Phosphate Hill, November 3, 1897.
gad. Flying Fish Cove, November 28, 1897.
No. 71, Qimm. Flying Fish Cove, November 24, 1897.
6 imm. Flying Fish Cove, November 16, 1897.
Of this fine and peculiar Fruit-Pigeon Mr. Andrews procured
a good series. There does not seem to be any appreciable
difference in the colour of the sexes, but the young birds are more
reddish underneath, and the first feathers of the throat and breast
are of a dull grey, without any purplish or vinous tint whatever.
[The large Fruit-Pigeon, called by the Malays ‘ Pergam,’ is very
common over the whole island, but is much more often heard than
seen, since it lives among the thick foliage of the tops of the lofty
forest trees, where to the unpractised eye it is extremely difficult to
discover. In addition to the ordinary cooing note, the male utters
a deep booming cry which is the most striking of the forest sounds
during the daytime. This note is said to resemble closely the
noise made by tigers, and Mr. Ross told me that an old Bantamese
wood-cutter who came to the island was at first afraid to enter
the forest, and was with much difficulty persuaded that a bird
was responsible for the sound. These birds are very tame, and
when a number were feeding in a tree it was generally possible
to shoot several, one after the other, without disturbing the rest.
The boys in the island used to catch them with a noose of string at
the end of a long stick, and the birds would sit quietly while the
instrument of their destruction was prepared, and the boy climbed
into a convenient position for using it. On one occasion I caught
one with my hands while it was drinking at a puddle on a tree
trunk.
The food is the fruit and leaf-buds of the various forest trees,
and the birds gather in great numbers in trees of which the fruit
is just ripening. The feet are very powerful, prehensile organs,
and, while feeding, this Pigeon clambers about among the branches
like a Parrot. The nest is a very scanty structure of sticks placed
high up in a tree. The eggs are two in number, white, and
elongated, with both ends alike. I saw a pai building on
December 24th, and obtained an egg on January 6th; many young
birds were shot in April. There seem to be two broods a year, for
in the middle of November there were also great numbers of young
birds, characterized by their looser, duller plumage and grey legs ;
in the adult the legs are a bright red. I have counted between
fifty and sixty on the bushes round the small waterfall on the east
coast. The year before I visited the island was a very dry one,
and Mr. Ross informed me that great numbers of these Pigeons had
died of thirst.—C. W. A. ]
Aves. 39
2. Chalcophaps natalis.
Chalcophaps natalis, Lister, P.Z.S., 1888, p. 522; Salvad., Cat. B. Brit. Mus.,
XXi, p. 520 (1893); Sharpe, Handl. B., i, p. 84 (1899).
Nos. 24, 26, g ad.; No. 25, 9 ad. Flying Fish Cove, August 6,
1897.
6 Qad. Flying Fish Cove, October 21, 1897.
No. 54, Q ad. Flying Fish Cove, October 21, 1897.
No. 55, ¢ juv. Flying Fish Cove, October 21, 1897.
Q ad. Flying Fish Cove, November 15, 1897.
Young birds have the greater wing-coverts for the most part
rufous, and the under parts irregularly mottled with dusky bars.
As Count Salvadori points out, the male is not to be distinguished
from some of the males of C. indica, but the female differs con-
siderably from the female of that species.
_ [The Ground-Pigeon is by far the most brightly coloured of the
birds of Christmas Island. It usually feeds on the ground, and
can run rapidly. ‘Though generally seen in pairs, small flocks
sometimes occur, particularly near water. The food consists of
small fruits. ‘The nest is said to be placed in thickets of screw-pine
(Pandanus), but I never saw either it or the eggs. At pairing-
time the males fight fiercely, and are said to kill one another
occasionally. Young birds are seen in April. In spite of the
brightness of its colouring, this bird is difficult to see, the green
of the back and chestnut brown of the breast matching very closely
the colours of the leaves and soil.—C. W. A. |
Order RALLIFORMES.
3. Limnobzenus fuscus.
Limnobenus fuscus (Linn.), Sharpe, Cat. Brit. Mus., xxiii, p. 146 (1894).
No. 40, Q ad. Flying Fish Cove, August 29, 1897.
Iris brownish red, lightest round the pupil; legs reddish brown.
This is an interesting addition to the list. The species may
visit the island regularly on migration, but Mr. Andrews only
obtained one specimen.
Order LARIFORMES.
4, Anous stolidus.
Anous stolidus (Linn.), Saunders, Cat. B. Brit. Mus., xx, p. 136 (1896).
a, 6 ad. Rocky Point, November 15, 1897.
6, Qad. Flying Fish Cove, November 16, 1897.
40 Christmas Island.
This species has not been obtained on Christmas Island before,
but it was met with by Dr. H. O. Forbes on the Cocos-Keeling
Islands in February.
[Breeds round the coast, the eggs being deposited on small
shelves of the sea cliff.—C. W. A. |
Order CHARADRIIFURMES.
5. Glareola orientalis.
Glareola orientalis, Leach: Sharpe, Cat. B. Brit. Mus., xxiv, p. 58 (1896).
No. 48, Qimm. Flying Fish Cove, October 3, 1897.
Not previously noted from the island, but certain to be a regular
visitor on migration.
6. Charadrius dominicus,
Charadrius dominicus, P. L. S. Miill.: Sharpe, Cat. B. Brit. Mus., xxiv, p. 195
(1896) ; id., Handl. B., i, p. 152 (1599).
Simm. Flying Fish Cove, November 14, 1897.
Not met with by Mr. Lister, but certainly a regular visitor on
migration.
7. Ochthodromus geoffroyi.
Charadrius geoffroyi, Wagl.: Lister, P.Z.S., 1888, p. 528.
Ochthodromus geoffroyi, Sharpe, Cat. B. Brit. Mus., xxiv, p. 217 (1896); id.,
Handl. B., i, p. 153 (1899).
Q ad. Flying Fish Cove, November 14, 1897.
An adult female in full winter plumage. It is evidently a
regular visitor to Christmas Island on migration.
8. Numenius variegatus.
Numenius variegatus (Scop.), Sharpe, Cat. B. Brit. Mus., xxiv, p. 361 (1896).
a,b, 8 Qad. Flying Fish Cove, November 17, 1897.
e,Qad. Flying Fish Cove, December 26, 1897.
New to the Avifauna of Christmas Island, but doubtless a more
or less regular visitor on migration. Mr. Andrews only saw one
small flock of four, out of which three specimens were killed.
9. Tringoides hypoleucus.
Tringoides hypoleucus (Linn.), Lister, P.Z.S., 1888, p. 528; Sharpe, Cat. B.
Brit. Mus., xxiv, p. 456 (1896); id., Handl. B., i, p. 161 (1899).
No. 62, 9 imm. Flying Fish Cove, October 22, 1897.
This is also apparently a regular visitor on migration, as it was
likewise obtained by Mr. Lister.
Aves. 41
10. Calidris arenaria.
Calidvis arenaria (L.), Sharpe, Cat. B. Brit. Mus., xxiv, p. 526 (1896).
An adult bird in moult, still retaining a few of the feathers of
the summer plumage on the back. This is an interesting addition
to the Avifauna of Christmas Island, and increases our knowledge
of the line of migration pursued by the Sanderling, which has in
recent years been discovered in North Australia and in the Malay
Archipelago.
11. Limonites ruficollis.
Limonites ruficollis (Pall.), Sharpe, Cat. B. Brit. Mus., xxiv, p. 545 (1896) ;
id., Handl. B., i, p. 163 (1899).
a,b, 8 juv., Q juv. Flying Fish Cove, September 20, 1897.
Both these specimens are immature birds in their first winter
plumage. The male has the wing 4°15 inches and the female 4:0.
The species has not been met with before on Christmas Island, but
is doubtless a regular visitor on migration.
12. Gallinago stenura.
Gallinago stenwra, Bp.: Sharpe, Cat. B. Brit. Mus., xxiv, p. 619 (1896) ; id.,
Handl. B., i, p. 166 (1899).
a 6 ad. Flying Fish Cove, December 1, 1897.
Not previously recorded from Christmas Island.
Order ARDEIFORMES.
13. Demiegretta sacra.
Ardea jugularis, Wagl.: Sharpe, P.Z.S., 1889, p. 516; Lister, P.Z.S., 1888,
. 138
Pp :
Demiegretta sacra (Gm.), Sharpe, Cat. B. Brit. Mus., xxvi, p. 138 (1898) ; id.,
Handl. B., i, p. 198 (1899).
No. 5 ad. Flying Fish Cove, July, 1897.
ad. [ white phase ].
Nos. 2,4, dimm. Flying Fish Cove, August, 1897.
No. 3, ad. [ white phase }.
a, dg ad. Flying Fish Uove. November 18, 1897.
The bird in the white phase of plumage has very little crest,
but the long ornamental breast-plumes are fully developed. Two
of the outer scapulars are grey externally, and another grey plume
is concealed by the long ornamental feathers of the lower back.
42 Christmas Island.
Order PELECANIFORMES.
Sub-Order FREGATI.
14. Fregata aquila.
Fregata aquila (Linn.), Sharpe, P.Z.8., 1887, p. 516; Lister, P.Z.S., 1888,
. 629; Ogilvie Grant, Cat. B. Brit. Mus. -» XXvi, p. 443 (1898);
Sharpe, Handl. B. yp Apezar (1899).
a,b, 6 Q. Flying Fish Cove, November 18, 1897.
e, d, 6 Q juv. Flying Fish Cove, November 4, 18, 1897.
According to Mr. Andrews, who shot some breeding birds, the
male of the large Frigate Bird is almost entirely black, being
white only from the lower breast down to the vent, including the
lower flanks and upper part of the thighs. The female is black
above, and has the throat black, but is white from the lower throat
downwards; the sides of the body black, with a large white patch
on the flanks. The young birds have a rusty-coloured head and
throat.
[Perhaps the most interesting of the birds of Christmas Island
are the Frigate-birds, two species of which occur. Numbers of
these birds could nearly always be seen sailing and circling in the
air at all heights; in calm weather they often soar till scarcely
visible. The flight is wonderfully graceful, and it is a pleasure
to watch a group moving along the coast in a succession of
sweeping circles, rising against the wind, or descending with it.
In flight the head is carried close to the body, so that the bird
seems to have no neck, and the tip of the beak is about on a level
with the anterior angle of the outstretched wings. The feathers
are often cleaned during flight, and occasionally the bird shakes
itself like a dog that has just left the water, dropping through
the air meanwhile. The young birds seem to be able to fly
perfectly well as soon as they leave the nest, and groups of them
could often be seen near the coast stooping to the water, one after
the other, to pick up leaves and other floating objects, and then
dropping them, apparently practising the method by which their
parents obtain their food, which consists of surface fish and
cephalopods. I never saw a Frigate-bird dive.
The old birds by no means depend for food on the fish they catch
themselves, but systematically rob the Gannets, which breed in
great numbers on the island. Towards sunset many Frigate-birds
may be seen sailing along the coast, watching for the return of the
Gannets, full-fed from the fishing grounds. The birds being well
aware of what is in store for them, and knowing that if they can
reach the shelter of the trees they are safe, approach the island at
a great speed, flying as low down as possible. Usually, while they
are still at some distance, two or three Frigate-birds give chase, and
——
Aves. 43
hunt the Gannet backwards and forwards, continually trying to get
beneath it and to cut off its retreat to the trees. ‘The chase may
last several minutes, but at length the exhausted bird disgorges
some of the fish it had swallowed, and this is immediately caught
in mid-air by one of the pursuers. Mr. Ross told me that
occasionally two Frigate-birds would come into collision and break
their wings, but this I never saw. The twigs for building the
nests are obtained on the same system of robbery, and although
these birds will pick up twigs floating in the sea and lying on
the beach, I never saw one attempt to break them off the dead
branches as the Gannets do. If, when a nest is partly built,
the bird in charge of it is killed, dozens of its neighbours come
round and steal the material thus conveniently collected for them.
The nest consists merely of a few handfuls of twigs placed on the
fork of a small branch, and it seems wonderful how the egg
remains on it. When the young has been hatched a few days the
nest becomes converted into a hard, nearly flat cake of twigs and
excrement. Old nests, and those of Gannets, are often utilized.
About the beginning of January the adult males begin to acquire
the remarkable pouch of scarlet skin beneath their throat. This
they can inflate till it is nearly as large as the rest of the body,
and a dozen or more of these birds sitting in a tree with out-
stretched drooping wings and this great scarlet bladder under their
heads are a most remarkable sight. When a hen bird approaches
the tree the males utter a peculiar cry, a sort of ‘ wow-wow-wow-
wow,’ and clatter their beaks like castanets, at the same time
shaking the wings. When they take to flight the air is allowed
to escape from the pouch, but occasionally they might be seen
flying with it partly inflated.
The pairing season extended from January till April; eggs were
found in February, and in August there were still many young
birds in white down, but by October all had flown. The young
continue to get a certain amount of food from their parents even
after the latter have begun to build again.
In the neighbourhood of Flying Fish Cove the large species
builds near the sea, the small one on the higher part of the island
farther inland. The cry of the male in the small species is quite
different from, and much more musical than that of the large one.
At present Frigate-birds are one of the chief articles of food
of the inhabitants of Christmas Island, and they are very good
indeed. The usual way of obtaining them is for a man to climb
into the topmost branches of a high tree near the coast, armed
with a pole eight or ten feet long and a red handkerchief. The
latter he wayes about, at the same time yelling as loudly as possible.
The birds attracted by the noise and the red colour swoop round
in large numbers, when they are knocked down with the long pole.
In this way sufficient birds to supply the small colony with food
can usually be obtained in an hour or two; occasionally, however,
in unfayourable states of the wind, they are difficult to procure.
44 Christmas Island.
Young. Brownish on back, head fawn brown, whiter on back
and upper part of neck. The brown of the front of the neck passes
on breast into a band of brownish-black feathers. Breast and
belly white. Beak greyish pinkish- white; throat and eyelid
ereyish white. Feet ditto. Some white feathers on sides of
breast. Secondary-coverts blackish brown, axillaries white, edged
with white. Rectrices slightly tipped with brownish white.—
Ch ae a
15. Fregata ariel.
Fregata ariel (Gould), Ogilvie Grant, Cat. B. Brit. Mus., xxvi, p. 447 (1898).
No. 18, g. Flying Fish Cove, August, 1897.
No. 45, Q. Flying Fish Cove, August, 1897.
According to Mr. Andrews, the male is entirely black below, but
the female is white on the throat, breast, and sides of body. The
centre of the lower breast, abdomen, and lower flanks are black.
Sub-Order SUL.
16. Sula sula.
Sula sula (Linn.), Ogilvie Grant, Cat. B. Brit. Mus., xxvi, p. 4386 (1898) ;
Sharpe, Handl. B., i, p. 236 (1899).
Nos. 7, 9, Q ad. Flying Fish Cove, August 4, 5, 1897.
No. 10, Q pull. Flying Fish Cove, August 4, 1897.
No. 94, Qimm. Flying Fish Cove, November 16, 1897.
The young bird was obtained by Mr. Andrews on the 4th of
August, with its mother (No. 9). It is still covered with white
down, though more than half-grown.
{ Sula sula (Booby) breeds near the coast. Nest of sticks on
ground, usually near edge of sea cliff, but sometimes on the high
inland cliffs at some distance from the sea. One or two eggs.—
C. W. A.J
17. Sula abbotti.
Sula abbotti, Ridgw., Proc. U.S. Nat. Mus., xvi, p. 599 (1893) ; Sharpe, Handl.
B., i, p. 237 (1899).
a, dg ad. East coast, October, 1897..
This species was hitherto known only from Assumption Island
in the Indian Ocean. Mr. Ogilvie Grant united it to Sula cyanops,
but it is certainly quite distinct.
[ Builds nests of sticks near the tops of the highest trees, usually
on the high land round the plateau. Shot young in September.
This bird is rarely seen on the north coast of the island, but
on the south it seems largely to take the place of S. piscatriz.—
C. Woo Ae]
Aves, 45
18. Sula piscatrix.
Sula piscatriz (Linn.), Sharpe, P.Z.S., 1887, p. 516; Ogilvie Grant, Cat. B.
Brit. Mus. xxvi, p. 432 (1898) ; Sharpe, Handl. B., i, p. 237.
No. 94, Qimm. Flying Fish Cove.
[ Suda piscatriz is very common all round the coast. Builds nest
of sticks in high trees. Begins to breed about January, and there
are great numbers of young birds in grey plumage in October.—
C. W. A.]
Sub-Order PHAETHONTES.
19. Phaethon rubricauda.
Phaethon phenicurus, Gm.: Lister, P.Z.S., 1888, p. 529.
Phacthon rubricauda, Bodd.: Ogilvie Grant, Cat. B. Brit. Mus., xxvi, p. 451
(1898); Sharpe, Handl. B., i, p. 238 (1899).
No. 14, g ad. Flying Fish Cove, August, 1897.
a,b, 8 Qad. Flying Fish Cove.
No. 15, Q juv. Flying Fish Cove, August, 1897.
e, 9 ad. Flying Fish Cove, August, 1897. ‘‘ Taken on nest
with No. 15.”
d, 6 ad. Flying Fish Cove, March 21, 1898. Taken from nest
in hole of cliff.
[The habits of the white Tropic Bird are much like those of
the yellow one, but it seems to nest almost exclusively in holes
in the cliffs, and I never saw it flying among the trees. The
colour of the young bird is exactly lke that of the other species.—
C.W. A.]
20. Phaethon fulvus. (Plate III.)
Phaethon flavirostris (nec Brandt), Lister, P.Z.S., 1888, p. 528.
Phaethon fulvus, Brandt: Grant, Cat. B. Brit. Mus., xxvi, p. 455 (1898).
No. 38, g ad. Flying Fish Cove, August 28, 1897.
No. 41, Q ad. Flying Fish Cove, August 30, 1897.
No. 47, Q juv. Flying Fish Cove, September 20,1897. ‘‘ Just
beginning to fly.”
Nos. 67, 69, Q ad. Flying Fish Cove, November 19, 1897.
No. 68, g ad. Flying Fish Cove, November 19, 1897.
a,b, @ Qad. Flying Fish Cove. December 26, 1897.
There appears to be no difference in the colour of the sexes, and
the orange tint is equally well developed in both the male and
female. The young bird, however, shows no orange in the
plumage, but is white, spotted on the head and barred on the back
with black; the inner secondaries with black longitudinal markings
of irregular shape on the outer web; the primaries and a few of
46 Christmas Island.
the secondaries black-shafted, the outer primaries with more or
less black along the outer web; tail-feathers white, with a sub-
terminal black spot; a circular spot of black im front of the eye,
extending below backwards in a line under the latter, and with
a black line above the ear-coverts; flanks with a tuft of chequered
black feathers with white notches and spots. These latter
feathers, and also many on the back and secondaries, seem to
indicate by the variation of their pattern that the latter changes
a great deal, so that the aspect of the feather becomes gradually
whiter and whiter.
[The most beautiful of the sea birds is the yellow Tropic Bird,
which, though much less numerous than the Frigate-birds, is still
fairly common. The flight of these birds is swift, though, owing
to the rapidity of the strokes of the wing, it often seems as if they
were labouring. I never saw them sail except for a short distance
when wheeling round. On hot days they may be seen in twos
and threes, flying rapidly up and down above and among the tree
tops, continually uttering their peculiar crackling cry, and pausing
now and then to hover before holes in the trees which seem to
offer an eligible position for a nest. It can hardly be said, however,
that they make a nest, for the single dark-brown mottled egg
is merely placed in a slight hollow on the floor of a hole in a tree
or in the sea cliff. The young bird, when nearly full-grown, is
white, barred with black, and since I never saw one in this
plumage out of the nest, it seems that the yellow colour is
acquired before it flies. The only distinguishing mark of the
youngest bird I ever saw flying was the presence of a few black
bars on the back just above the root of the tail. Eggs and
young were obtained in August and September; the breeding
season seems to be less definite than in the case of the other
birds.—C. W. A. ]
Order ACCIPITRIFORMES.
21. Astur natalis. (Plate V.)
Urospizias natalis, Lister, P.Z.S., 1888, p. 523.
Astur natalis, Sharpe, Handl. B., i, p. 241 (1899).
¢ juv. Flying Fish Cove, August 14, 1897.
Nos. 30-33, ¢ Q juv. Flying Fish Cove, August 13, 1897.
No. 86, Q ad. Flying Fish Cove, August 20, 1897.
Vg
ieee pom Flying Fish Cove, August 22, 1897.
@ juv. Flying Fish Cove, September, 1897.
¢ juv. Flying Fish Cove, October, 1897.
Q juv. Phosphate Hill, November 28, 1897.
No. 35, g < ad. South-east coast, August 20, 1897.
3 juv.
Aves. 47
Mr. Lister has given a very good description of this species,
and has pointed out its similarity to A. grisecgularis. It differs
from the latter species, however, in its much darker slaty-grey
head, slaty-grey bars on the chest, and in the lhghter underwing-
and tail-coverts, which are barred with white and vinous rufous,
and are not so uniform vinous as in A. grisergularis.
[The Goshawk is common all over the island, and is very
destructive to young poultry in Flying Fish Cove. Its food
consists of the White-eyes, Ground-Thrushes, and Ground-Pigeons,
and it is said to kill the large Fruit-Pigeon also, but this I never
saw. In the crop of one there were remains of numerous locusts.
The nest is made of twigs and pieces of creepers, and is placed
near the top of a high tree. A nest with one young was found
on January 24th. The cry is a sharp ‘tweet-tweet-tweet,’ and
when shooting Fruit-Pigeons in the high trees a rough imitation
of this call was often employed to cause them to thrust out their
head, so that they could be more easily seen, and would present
a better mark.—C. W. A. ]
22. Ninox natalis. (Plate IV.)
Ninox natalis, Lister, P.Z.S., 1888, p. 525.
No. 37, g ad. Flying Fish Cove, August 8, 1897.
No. 65, Q ad. Flying Fish Cove, October 24, 1897.
No. 66, g ad. Flying Fish Cove, November 9, 1897.
No. 70, g ad. Flying Fish Cove, November 24, 1897.
Q ad. Flying Fish Cove, December 24, 1897. Iris and feet
bright lemon-yellow.
The sexes do not differ in colour, and there is scarcely any
variation in size, as the males have the wing 7°6—7°8 inches and
the females 7:4—7°8.
[The Owl is most often seen in thickets of screw-pine and in the
denser parts of the forest. Its food consists of lizards, locusts,
white-eyes, and perhaps rats. The nest I never found, but
Mr. Hugh Ross told me it is usually placed in a screw-pine and
made of twigs. The peculiar cry, resembling very closely the bark
of a small dog, has been described by Mr. Lister. In the forest
after sun-down several of these birds could be heard barking in
answer to one another. They usually begin with a scarcely
audible ‘chuk-chuk,’ which is repeated crescendo till they break
out into a regular bark, which may be repeated a considerable
number of times; this may stop suddenly or die away gradually
as it began.—C. W. A. ]
48 Christmas Island.
Order CORACIIFORMES.
Sub-Order CYPSELI.
23. Collocalia natalis.
Collocalia natalis, Lister, P.Z.S., 1888, p. 520; Hartert, Cat. B. Brit. Mus., xvi,
p- 511 (1892) ; id., Tierreich, Lief. i, Aves, Macropt., p. 70 (1897).
No. 28, ad. Flying Fish Cove, August, 1897.
Q ad. Flying Fish Cove, November 24, 1897.
6 6 Gad. Flying Fish Cove, November 25, 1897.
Q ad. Flying Fish Cove, December 28, 1897.
ad: Flying Fish Cove, February 15, 1898.
$6 9 Qad. Flying Fish Cove, March 4, 1898.
66 OQ Qad. Flying Fish Cove, March 7, 1898.
The series brought home by Mr. Andrews confirmed the
characters of the species, but the differences between C. natalis
and C. neglecta are not very strongly pronounced.
Order COCCYGES.
Sub-Order CUCULI.
24, Chalcococcyx basalis.
Chalcococcyx basalis (Horsf.), Shelley, Cat. B. Brit. Mus., xix, p. 294 (1891).
A single immature female in full moult. This species has not
before been obtained on Christmas Island.
Order PASSERIFORMES.
Family MOTACILLIDA.
25. Motacilla melanope.
Motacilla melanope, Pall.: Sharpe, Cat. B. Brit. Mus., x, p. 497 (1885).
@ ad. Flying Fish Cove, October 7, 1897.
Tris blue-black. On the shore. Stomach contained small marine
Worms.
Also not recorded from Christmas Island previously.
26. Motacilla flava.
Motacilla flava, Linn.: Sharpe, Cat. B. Brit. Mus., x, p. 516, pl. vi, figs. 3-5
(1885).
No. 49, gd imm. Flying Fish Cove, October, 1897.
a, 6,imm. Flying Fish Cove.
Three young birds, evidently procured‘on migration.
Aves. 49
Family ZOSTEROPIDA.
27. Zosterops natalis. (Plate VI.)
Zosterops natalis, Lister, P.Z.S., 1888, p. 518, pl. xxvii.
No. 21, g ad. Flying Fish Cove, August 5, 1897.
a, dg ad. Flying Fish Cove, August 10, 1897.
b,c, d ad. Flying Fish Cove, November 29, 1897.
d, g6 ad. Flying Fish Cove, November 24, 1897.
e, G ad. Flying Fish Cove, December 3, 1897.
i,9,6 Qad. Flying Fish Cove, March 4, 1898.
The White-eye of Christmas Island is a large species, and easily
recognized by its colour. I can see no difference in the plumage
of specimens killed in various months, and the young resemble
the adults. The yellow at the base of the bill scarcely amounts
to more than a small loral patch and does not form a frontal band.
N.B.—In Mr. Lister’s diagnosis of the species (p. 519) the first
character, viz., that the crown becomes paler ‘‘ towards the base
of the ¢a/,”’ must be a misprint for ‘ bill.’
The nest is a pretty little structure —a shallow cup suspended
between the forks of a twig, to which it is attached. The nest
consists of vegetable fibre, with wool as a basis, and it is lined
with the same black fibre of the sago-palm as that used by the
Thrush for its nest. A second nest is deeper in the cup, contains
more cotton, and has a few white feathers interlaced in the
outside. The two eggs, obtained by Mr. Andrews in November,
are uniform bluish white. Axis 0°7; diam. 0°5.
[The little Zosterops (Burung Waringin) swarm everywhere,
even in the middle of the forest. They seem to form small flocks,
and behave much like Titmice, climbing about among the foliage
and often hanging head downwards under a leaf or branch in their
search for insects. They also eat a good deal of fruit, and destroy
many papaias, custard-apples, and bananas, of which they are so
fond that they often come on to the dinner-table to get them.
They have only a twittermg note, but when a Hawk is im the
neighbourhood the noise made by a flock of them is considerable.
The nest is usually placed between two twigs or in the fork of
small branches of bushes, and is made of fibres of the sago-palm,
or any other vegetable fibre they can get. They seem to breed
nearly all the year round.—C. W. A. }
Family TURDIDZ.
28. Merula erythropleura.
Turdus erythropleurus, Sharpe, P.Z.S., 1887, p. 515.
Merula erythropleura, Lister, P.Z.8., 1888, p. 517.
No. 28, ad. Flying Fish Cove, August, 1897.
Nos. 52, 58, @ Q ad. Flying Fish Cove, October 20, 1897.
E
50 Christmas Island.
No. 60, g ad. Flying Fish Cove, October 22, 1897.
6 Qad. Flying Fish Cove, November 4, 1897.
¢ ad. Flying Fish Cove, November 12, 1897.
gad, Flying Fish Cove, November 21, 1897.
6 Qad. Flying Fish Cone December 29, 1897.
Go juv. Flying Fish Cove, February 14, 1898.
Qad. Flying Fish Cove, February 20, 1898.
Q ad. Flying Fish Cove, March 7, 1898.
juv. North Coast, March 17, 1898.
ad. Phosphate Hill, November 3, 1897.
This species is of the group of Merula javanica, but is especially
remarkable for the size of its bill, which is very large in proportion
to the bird. The sexes are alike in colour, and the young birds
are more dusky brown, with pale shaft-lines to the feathers of the
upper surface. In the young the bill is horn brown, not yellow,
and the under surface of the body is mottled with dusky-brown
edges to the feathers.
[The Ground-Thrush is common everywhere, but is most numerous
near the coast. Like the other birds of the island, it is very tame,
and when I was breaking up rotten wood searching for beetles,
several of them would stand quite close by in readiness to pick
up any grubs that were uncovered. Its food consists of msects,
seeds, and any carrion it can find, and I have seen one kill a small
brown lizard, though it seemed to have some difficulty in doing so.
When hunting for insects among the dead leaves, the colours of the
plumage harmonize so exactly with the surroundings that, were
it not for the bright yellow beak and eye-lids the bird would be
almost inyisible. The alarm cry is much lke that of the European
Blackbird, and in the pairing season (December-January) the male
has a song something like that of the English Thrush, but harsher
and less varied. The nest is made of fibres of the wild sago-palm
(Arenga listeri), skeleton leaves, and other vegetable fibre; it is
not mud-lined. One nest was taken from the crown of a screw-
pine (Pandanus), another from the hollow top of a broken tree
trunk, some fifteen feet from the ground. Eggs were found in
December, and in the following month young birds just able to
fly were numerous, and continued to be so till April.—C. W. A. ]
Family HIRUNDINIDA.
29. Hirundo gutturalis.
Hirundo gutturalis, Scop. : Sharpe, Cat. B. Brit. Mus., x, p. 184 (1885).
Q juv. Flying Fish Cove, October 16, 1897.
A young female of the Eastern Chimney Swallow, in moult
from the first plumage to the glossy dress of the adult. |
Reptilia. 51
REPTILIA.
By G. A. Boutencer, F.R.S.
(PLATE VIL.)
‘Tae first collection made on Christmas Island by the officers of
H.M.S. ‘Flying Fish” yielded examples of three species —
Gymnodactylus marmoratus, Kuhl, Lygosoma nativitatis (n.sp.), and
Typhlops exoceti (n.sp.). Mr. Lister’s visit to the island in 1888
resulted in the discovery of two further new species— Gecko listeri
and Ablepharus egerie. To these five species Mr. Andrews has
added a sixth, the widely distributed Lygosoma atrocostatum.
LACERTILIA.
Family GECKONIDA.
1. Gymnodactylus marmoratus, Kuhl.
Gymnodactylus marmoratus, Boulenger, Cat. Liz., 1, p. 44 (1885).
Known from Java, Sumatra, and Borneo; also from the mountains
-of Perak, in the Malay Peninsula, whence I have recently received
-Q specimen.
2. Gecko listeri. (Pl. VII, Fig. 1.)
-Gecko listeri, Boulenger, P.Z.S., 1888, p. 536.
Head moderate, snout once and one-third the diameter of the
orbit, which equals its distance from the very small round ear-
opening; forehead scarcely concave. Head covered with small
-granules, which are considerably larger on the snout; rostral
quadrangular, more than twice as broad as deep, without cleft;
nostril pierced between the rostral, the first labial, and three
nasals; twelve upper and ten lower labials; three transverse rows
of small hexagonal chin-shields. Dorsal scales uniform, minutely
granular; ventrals much larger, roundish hexagonal, subimbricate.
Digits with a very slight rudiment of web; seven or eight
angularly curved lamelle under the median toes. A short angular
‘series of twelve preanal pores. Tail cylindrical, covered with
uniform small flat scales, which are largest inferiorly. Pale grey-.
‘brown above, with a few rather indistinct brown spots and
scattered white dots; a brown streak from the nostril to the eye;
lower parts white, with small brown spots.
Total length ... ... 79 mm. Bore WetBy .. cen «ss 12
Head 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.
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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
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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
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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. [With list of Species
of New Guinea Birds, and those of the neighbouring
Localities.] By John Edward Gray, Ph.D., F.R.S., and
George Robert Gray, F.L.S., &c. Pp. 63. Woodcuts.
1859, 8vo. Is. 6d.
Report on the Zoological Collections made in the Indo-
Pacific Ocean during the voyage of H.M.S., “ Alert,” 1381-2,
Pp. xxv., 684. 54 Plates. 1884, 8vo.
Summary of the Precis ... By.Dr. R. W. Coppinger.
Mammalia ae ee 55 O. Thomas.
AVES ©. «.. aoe it, LE. Bepharpe:
Reptilia, Batrachia, Pisces ... 5, A. Giinther.
Mollusca as soe UCAS Smith,
Echinodermata ida os) ell
Crustacea ws - ie), WediMiersi
Coleoptera ste vc .. 5, C. O. Waterhouse.
Lepidoptera... 3) ig ASG Botler,
Alcyonaria and Spongiida saci Cig, toe Os Midley.
TZ. 10s.
4337r—1500—12/99 Wt 20849 D&S 9 A
a)
LIST OF PUBLICATIONS OF THE
MAMMALS. -
List of the Specimens of Mammalia in the Collection of the
British Museum. By Dr. J. E. Gray, F.R.S. Pp. xxviii.
216. [With Systematic List of the Genera of Mammalia,
Index of Donations, and Alphabetical Index.] 1843, 12mo.
2s. 6d.
Catalogue of ne Bones of Mammalia in the Collection of the
British Museum. By Edward Gerrard. Pp. iv., 296.
1862, 8vo. 5s.
Catalogue of Monkeys, Lemurs, and Fruit-eating Bata § in the
Collection of the British Museum. By Dr. J. E. Gray,
F.R.S., &c. Pp. viti 137: 21 Woodcuts, 1870 ouom eae
Catalogue of cnr enae Pachydermatous, and HEdentate
‘Mammalia in the British Museum. By John Edward
Gray, F.R.S., &c. Pp. vii., 398. 47 Woodcuts. 1869,
8vo. 6s. 6d. ;
Catalogue of Seals and Whales in the British Museum. By
John Edward Gray, F.R.S., &c. 2nd edition. nhs Vile os
402. 101 Woodcuts. 1866, Bv0. 8s.
——— Supplement. | By John Edward Gray, F,B.S., &c.
Pp. vi; 103. 11 Woodeuts: 187i; 8vo. 2s. Gd.
List of the Specimens of Cetacea in the Zoological Depart-
ment of the British Museum. By William Henry Flower,
LL.D., F.R.S., &c. [With Systematic and Alphabetical
Indexes. ] Pp. iv.,.36. 1885, 8vo. Is. 6d.
Catalogue of Reinsinearis Mammalia (Pecora, Linnzus) in the
British Museum. By John Edward Gray, F.R.S., &e.
Pp. viil,, 102... 4.Plates. ..1872, Sve. -_3s. hd. 7
Catalogue of the Marsupialia and Monotremata in the
Collection of the British Museum. By Oldfield Thomas.
Pp. xiii, 401. 4 coloured and 24 plain Plates. [With
Systematic and Alphabetical Indexes.] 1888, 8vo. L/. 8s.
~
BIRDS.
big of the Birds in the British Museum :—
Vol. VI. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum. |
Cichlomorphe : Part III., containing the first portion
of the family Timeliides (Babbling Thrushes). By
R. Bowdler Sharpe. Pp. xiii., 420. Woodeuts and
18 coloured Plates. [With Systematic and Alpha-
betical Indexes.] | 1881, 8vo..1/.
Vol. VII. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Cichlomorphe : Part IV., containing the concluding ~
_ portion of the family Timeliide (Babbling Thrushes).
BRITISH MUSEUM (NATURAL HISTORY). 3
Catalogue of the Birds in the British Museum—continued.
By R. Bowdler Sharpe. Pp. xvi.,698. Woodeuts and
15 coloured Plates. [With Systematic and Alpha-
betical Indexes.] 188%, 8vo. 17. 6s.
Vol. VIII. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Cichlomorphe: Part V., containing the families
Paride and Laniide (Titmice and “Shrikes) ; and
Certhiomorphe (Creepers and Nuthatches). By Hans
Gadow, M.A., Ph.D. Pp. xiii., 386. Woodcuts and
9 coloured Plates. [ With Systematic and Alpha-
betica] Indexes.] 1883, 8vo. 17s.
Vol. 1X. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Cinnyrimorphe, containing the families Nectariniide
and Meliphagide (Sun Birds and Honey-eaters). By
- Hans Gadow, M.A., Ph.D. Pp. xii., 310. Woodcuts
and 7 coloured Plates. [With Systematic and Alpha-
betical Indexes.] 1884, 8vo. 14s.
Vol. X. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Fringilliformes : Part I., containing the families
Diceide, Hirundinide, Ampelide, Mniotiltide, and
Motacillide. By R. Bowdler Sharpe. Pp. xiii., 682.
Woodcuis and 12 coloured Plates. [With Systematic
and Alphabetical Indexes.] 1885, 8vo. 1/. 2s.
Vol. XI. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Fringilliformes: Part II., containing the families
Cerebide, Tanagride, and Icteride. By Philip Lutley
Sclater, M.A., F.R.S. Pp. xvii. 431. [With Syste-
matic and Alphabetical Indexes.] Woodcuts and 18
coloured Plates. 1886, 8vo. 17.
Vol. XII. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Fringilliformes: Part IIIJ., containing the family
Fringillide. By R. Bowdler Sharpe. Pp. xv., 871.
Woodeuts and 16 coloured Plates. [With Systematic
and Alphabetical Indexes.] 1888, Svo. 1/. 8s.
Vol. XIII. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Sturniformes, containing the families Artamide,
Sturnide, Ploceide,and Alaudidz. Also the families
Atrichiide and Menuride. By R. Bowdler Sharpe.
: Pp. xvi., 701. Woodcuts and 15 coloured Plates.
[ With Systematic and Alphabetical Indexes.] 1890,
8vo., 17. 8s.
Vol. XIV. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Oligomyode, or the families Tyrannide, Oxyrham-
_ phide, Pipride, Cotingide, Phytotomida, Philepittida,
4337r AZ
4
LIST OF PUBLICATIONS OF THE
Catalogue of the Birds in the British Museum—continued.
Pittide, Xenicide, and Eurylemide. By Philip
Lutley Sclater, M.A., F.R.S. Pp. xix.,494. Woodcuts
and 26 coloured Plates. [With Systematic and Alpha-
betical Indexes.] 1888, 8vo. Ld. 4s.
Vol. XV. Catalogue of the Passeriformes, or Perching
Birds, in the Collection of the British Museum.
Tracheophone, or the families Dendrocolaptide,
Formicariide, Conopophagide, and Pteroptochide.
By Philip Lutley Sclater, M.A., F.R.S. Pp. xvii., 371.
Woodcuts and 20 coloured Plates. [With Systematic
and Alphabetical Indexes.] 1890, 8vo. 11.
Vol. XVI. Catalogue of the Picariz in the Collection of
the British Museum. Upupe ana Trochili, by Osbert
Salvin. Coracie, of the families Cypselide, Capri-
mulgide, Podargide, and Steatornithide, by Ernst
Hartert. Pp. xvi., 703. Woodcuts and 14 coloured
Plates. [With Systematic and Alphabetical Indexes. |
1892, 8vo. 10. 16s. '
Vol. XVII. Catalogue of the Picarie in the Collection
of the British Museum. OCoracie (contin.) and
Halcyones, with the families Leptosomatide, Coraciide,
Meropide, Alcedinide, Momotide, Totide and Coliide,
by R. Bowdler Sharpe. Bucerotes and Trogones by
W. R. Ogilvie Grant. Pp. xi., 522. Woodecuts and 17
coloured Plates. [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.
January Ist, 1900.
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