The Malay archipelago : the land of the orang-utan ... - Wallace Online

The Malay archipelago : the land of the orang-utan ... - Wallace Online The Malay archipelago : the land of the orang-utan ... - Wallace Online

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12 THE MALAY ARCHIPELAGO. [chap.thrushes, and leaf-thi'ushes : they are seen daily, and form the^reat ornithological features of the country. In tlie EasternIslands tliese are absolutely unknown, honeysuckers and smalllories being the most common birds ; so that the naturalist feelshimself in a new world, and can hardly realize that he has passedfrom the one region to the other in a few days, witliout everbeing out of sight of land.The inference that we must draw from these facts is undoubtedly,that the whole of the islands eastwards beyondJava and Borneo, with the exception, perhaps, of Celebes, doessentially form a part of a former Australian or Pacific continent,although some of tliem may never have been actuallyjoined to it. This continent must have been broken np notonly before the Western Islands wei'e separated from Asia,but probablj^ before the extreme south-eastern portion of Asiawas raised above the waters of the ocean ; for a great partof the land of Borneo and Java isknown to be geologically ofquite recent formation, while the very great difference of species,and in many cases of genera also, between the productions of theEastern Malay Islands and Australia, as well as the great depthof the sea now separating them, all jDoint to a comparativelylong period of isolation.It is interesting to observe among the islands themselves,liow a shallow sea always intimates a recent land-connexion.The Aru Islands, Mysol, and Waigiou, as well as Jobie, agreewith New Guinea in their species of mammalia and birds muchmore closely than they do with the Moluccas, and we find thatthey are all united to Xew Guinea by a shallow sea. In fact,the 100-fathom line round New Guinea marks out accuratelythe range of tlie true Paradise birds.It is further to be noted—and this is a very interesting pointin connexion with theories of the dependence of special formsof life on external conditions—that tliis division of the Archipelagointo two regions characterized by a striking diversity intheir natural pi'oductions, does not in any way correspond tothe main physical or climatal divisions of the surface. Thegreat volcanic chain runs througli both parts, and appears toproduce no effect in assimilating their productions. Borneoclosely I'esembles New Guinea, not only in its vast size and itsfreedom fi"om volcanoes, but in its variety of geological structure,its uniformity of climate, and the general aspect of the forestvegetation that clotlies its surface. The Moluccas ai-e the counterpartof the Philijipines in their A'olcanic structure, theirextreme fertility, their luxuriant forests, and their frequentearthquakes ;and Bali with the east end of Java has a climatealmost as dry and a soil almost as arid as that of Timor. Yetbetween tliese corresj^onding groups of islands, constructed asit were after the same pattern, subjected to the same climate,and bathed by the same oceans, there exists the greatest possiblecontrasts when we compare their animal productions. Nowhere

I.] PHYSICAL GEOGRAPHY. 13does the ancient docti'ine—tliat difierences or similarities inthe various forms of life that inhabit different countries aredue to corresponding physical difierences or similarities in thecountries themselves—meet with so direct and palpable a contradiction.Borneo and Xew Guinea, as alike physically as twodistinct countries can be, are zoologically wide as the polesasunder ; while Australia, Avith its dry winds, its open plains,its stony deserts, and its temperate climate, yet produces birdsand quadrupeds which ai-e closely related to those inhabitingthe hot, damp, luxuriant forests which everywhere clothe theplains and mountains of New Guinea.In order to illustrate more clearly the means by which Isuppose this great contrast has been brought about, let usconsider what would occur if two strongly contrasted di\dsionsof the earth were, by natural means brought into proximity.No two parts of the world ditter so radically in their productionsas Asia and Australia, but the difference between Africa andSouth America is also very great, and these two regions willwell serve to illustrate the question we are considering. Onthe one side we have baboons, lions, elephants, buftaloes, andgiraffes ; on the other spider-monkeys, pumas, tapirs, ant-eaters,and sloths ;while among birds, the hornbills, tui'acos, orioles,and honeysuckers of Africa contrast strongly with the toucans,macaws, chatterers, and humming-birds of America.Now let us endeavour to imagine that a slow upheaval of thebed of the Altantic should take place, while at the same timeearthquake-shocks and volcanic action on the land should causeincreased volumes of sediment to be poured down by the river.s, sothat the two continents should gradually spread out by the additionof newlj^-formed lands, and thus reduce the Atlantic Avliichnow separates them to an arm of the sea a few hundred milesAt the same time we may suppose islands to be upheaved inwide.mid-channel ; and, as the subterranean forces varied in intensity,and shifted their points of greatest action, these islands Avouldsometimes become connected with the land on one side or otherof the strait, and at other times again be separated from it.Several islands would at one time be joined together, at anotherwould be broken up again, till at last, after many long ages ofsuch intermittent action, we might have an irregular archipelagoof islands tilling up the ocean channel of the Atlantic, in whoseappearance and arrangement we could discover nothing to tellus which had been connected with Africa and which withAmerica. The animals and plants inhabiting these islandswould, however, certainly reveal this portion of their formerhistory. On those islands which had ever formed a part of theSouth American continent we should be sure to tind such commonbirds as chatterers and toucans and humming-birds, andsome of the peculiar American quadrupeds ; while on thosewhich had been separated from Africa, hornbills, orioles, andhoneysuckers would as certainly be found. Some portion of

I.] PHYSICAL GEOGRAPHY. 13does <strong>the</strong> ancient docti'ine—tliat difierences or similarities in<strong>the</strong> various forms <strong>of</strong> life that inhabit different countries aredue to corresponding physical difierences or similarities in <strong>the</strong>countries <strong>the</strong>mselves—meet with so direct and palpable a contradiction.Borneo and Xew Guinea, as alike physically as twodistinct countries can be, are zoologically wide as <strong>the</strong> polesasunder ; while Australia, Avith its dry winds, its open plains,its stony deserts, and its temperate climate, yet produces birdsand quadrupeds which ai-e closely related to those inhabiting<strong>the</strong> hot, damp, luxuriant forests which everywhere clo<strong>the</strong> <strong>the</strong>plains and mountains <strong>of</strong> New Guinea.In order to illustrate more clearly <strong>the</strong> means by which Isuppose this great contrast has been brought about, let usconsider what would occur if two strongly contrasted di\dsions<strong>of</strong> <strong>the</strong> earth were, by natural means brought into proximity.No two parts <strong>of</strong> <strong>the</strong> world ditter so radically in <strong>the</strong>ir productionsas Asia and Australia, but <strong>the</strong> difference between Africa andSouth America is also very great, and <strong>the</strong>se two regions willwell serve to illustrate <strong>the</strong> question we are considering. On<strong>the</strong> one side we have baboons, lions, elephants, buftaloes, andgiraffes ; on <strong>the</strong> o<strong>the</strong>r spider-monkeys, pumas, tapirs, ant-eaters,and sloths ;while among birds, <strong>the</strong> hornbills, tui'acos, orioles,and honeysuckers <strong>of</strong> Africa contrast strongly with <strong>the</strong> toucans,macaws, chatterers, and humming-birds <strong>of</strong> America.Now let us endeavour to imagine that a slow upheaval <strong>of</strong> <strong>the</strong>bed <strong>of</strong> <strong>the</strong> Altantic should take place, while at <strong>the</strong> same timeearthquake-shocks and volcanic action on <strong>the</strong> <strong>land</strong> should causeincreased volumes <strong>of</strong> sediment to be poured down by <strong>the</strong> river.s, sothat <strong>the</strong> two continents should gradually spread out by <strong>the</strong> addition<strong>of</strong> newlj^-formed <strong>land</strong>s, and thus reduce <strong>the</strong> Atlantic Avliichnow separates <strong>the</strong>m to an arm <strong>of</strong> <strong>the</strong> sea a few hundred milesAt <strong>the</strong> same time we may suppose is<strong>land</strong>s to be upheaved inwide.mid-channel ; and, as <strong>the</strong> subterranean forces varied in intensity,and shifted <strong>the</strong>ir points <strong>of</strong> greatest action, <strong>the</strong>se is<strong>land</strong>s Avouldsometimes become connected with <strong>the</strong> <strong>land</strong> on one side or o<strong>the</strong>r<strong>of</strong> <strong>the</strong> strait, and at o<strong>the</strong>r times again be separated from it.Several is<strong>land</strong>s would at one time be joined toge<strong>the</strong>r, at ano<strong>the</strong>rwould be broken up again, till at last, after many long ages <strong>of</strong>such intermittent action, we might have an irregular <strong>archipelago</strong><strong>of</strong> is<strong>land</strong>s tilling up <strong>the</strong> ocean channel <strong>of</strong> <strong>the</strong> Atlantic, in whoseappearance and arrangement we could discover nothing to tellus which had been connected with Africa and which withAmerica. <strong>The</strong> animals and plants inhabiting <strong>the</strong>se is<strong>land</strong>swould, however, certainly reveal this portion <strong>of</strong> <strong>the</strong>ir formerhistory. On those is<strong>land</strong>s which had ever formed a part <strong>of</strong> <strong>the</strong>South American continent we should be sure to tind such commonbirds as chatterers and toucans and humming-birds, andsome <strong>of</strong> <strong>the</strong> peculiar American quadrupeds ; while on thosewhich had been separated from Africa, hornbills, orioles, andhoneysuckers would as certainly be found. Some portion <strong>of</strong>

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