[The Malay Archipelago by Alfred Russell Wallace]@TWC D-Link bookThe Malay Archipelago CHAPTER XXV 38/58
We infer this, because encircling reefs are a proof of subsidence; and if the island were again elevated about a hundred feet, what is now the reef and the shallow sea within it would form a wall of coral rock, and an undulating coralline plain, exactly similar to those that still exist at various altitudes up to the summit of the island.
We learn also that these changes have taken place at a comparatively recent epoch, for the surface of the coral has scarcely suffered from the action of the weather, and hundreds of sea-shells, exactly resembling those still found upon the beach, and many of them retaining their gloss and even their colour, are scattered over the surface of the island to near its summit. Whether the Goram group formed originally part of New Guinea or of Ceram it is scarcely possible to determine, and its productions will throw little light upon the question, if, as I suppose, the islands have been entirely submerged within the epoch of existing species of animals, as in that case it must owe its present fauna and flora to recent immigration from surrounding lands; and with this view its poverty in species very well agrees.
It possesses much in common with East Ceram, but at the same time has a good deal of resemblance to the Ke Islands and Banda.
The fine pigeon, Carpophaga concinna, inhabits Ke, Banda, Il-Iatabello, and Goram, and is replaced by a distinct species, C. neglecta, in Ceram.
The insects of these four islands have also a common facies--facts which seem to indicate that some more extensive land has recently disappeared from the area they now occupy, and has supplied them with a few of its peculiar productions. The Goram people (among whom I stayed a month) are a race of traders. Every year they visit the Tenimber, Ke, and Aru Islands, the whole north-west coast of New Guinea from Oetanata to Salwatty, and the island of Waigiou and Mysol.
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