[The Malay Archipelago Volume I. (of II.) by Alfred Russell Wallace]@TWC D-Link bookThe Malay Archipelago Volume I. (of II.) CHAPTER I 12/24
I term these respectively the Indo-Malayan and the Austro-Malayan divisions of the Archipelago. On referring to pages 12, 13, and 36 of Mr.Earl's pamphlet, it will be seen that he maintains the former connection of Asia and Australia as an important part of his view; whereas, I dwell mainly on their long continued separation.
Notwithstanding this and other important differences between us, to him undoubtedly belongs the merit of first indicating the division of the Archipelago into an Australian and an Asiatic region, which it has been my good fortune to establish by more detailed observations. Contrasts in Natural Productions .-- To understand the importance of this class of facts, and its bearing upon the former distribution of land and sea, it is necessary to consider the results arrived at by geologists and naturalists in other parts of the world. It is now generally admitted that the present distribution of living things on the surface of the earth is mainly the result of the last series of changes that it has undergone.
Geology teaches us that the surface of the land, and the distribution of land and water, is everywhere slowly changing.
It further teaches us that the forms of life which inhabit that surface have, during every period of which we possess any record, been also slowly changing. It is not now necessary to say anything about how either of those changes took place; as to that, opinions may differ; but as to the fact that the changes themselves have occurred, from the earliest geological ages down to the present day, and are still going on, there is no difference of opinion.
Every successive stratum of sedimentary rock, sand, or gravel, is a proof that changes of level have taken place; and the different species of animals and plants, whose remains are found in these deposits, prove that corresponding changes did occur in the organic world. Taking, therefore, these two series of changes for granted, most of the present peculiarities and anomalies in the distribution of species may be directly traced to them.
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