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Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
FRONTISPIECE
TO
SIR JOSEPH DALTON HOOKER,
K.C.S.I., C.B., F.R.S., ETC., ETC
WHO, MORE THAN ANY OTHER WRITER,
HAS ADVANCED OUR KNOWLEDGE OF THE GEOGRAPHICAL
DISTRIBUTION OF PLANTS, AND ESPECIALLY
OF INSULAR FLORAS,
I Dedicate this Volume;
ON A KINDRED SUBJECT,
AS A TOKEN OF ADMIRATION AND REGARD
PREFACE TO THE SECOND EDITION
This edition has been carefully revised throughout, and owing to the great increase to our knowledge of the Natural History of some of the islands during the last twelve years considerable additions or alterations have been required. The more important of these changes are the following:—
Chapter VII. The account of the migrations of animals and plants during and since the Glacial Epoch, has been modified to accord with newer information.
Chapters VIII and IX. The discussion of the causes of Glacial Epochs and Mild Arctic Climates has been somewhat modified in view of the late Dr. Croll's remarks, and the argument rendered clearer.
Chapter XIII. Several additions to the Fauna of the Galapagos have been noted.
Chapter XV. Considerable additions have been made to this chapter embodying the recent discoveries of birds and insects new to the Sandwich Islands, while a much fuller account has been given of its highly peculiar and very interesting flora.
Chapter XVI. Important additions and corrections have been made in the lists of peculiar British animals and plants embodying the most recent information.
Chapter XVII. Very large additions have been made to the mammalia and birds of Borneo, and full lists of the peculiar species are given.
Chapter XVIII. A more accurate account is given of the birds of Japan.
Chapter XIX. The recent additions to the mammals and birds of Madagascar are embodied in this chapter, and a fuller sketch is given of the rich and peculiar flora of the island.
Chapter XXI. and XXII. Some important additions have been made to these chapters owing to more accurate information as to the depth of the sea around New Zealand, and to the discovery of abundant remains of fossil plants of the tertiary and cretaceous periods both in New Zealand and Australia.