Island Life; Or, The Phenomena and Causes of Insular Faunas and FlorasWallace, Alfred Russel
Science
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Wallace, Alfred Russel
Biogeography; Glacial epoch; Island ecology
_Special Relations of the Javan Fauna to that of the Asiatic
Continent._--These relations are indicated by comparatively few examples,
but they are very clear and of great importance. Among mammalia, the genus
Helictis is found in Java but in no other Malay country, though it inhabits
also North India; while two species, _Rhinoceros javanicus_ and _Lepus
kurgosa_, are natives of Indo-Chinese countries and Java, but not of
typical Malaya. In birds there are five genera or sub-genera--Zoothera,
Notodela, Crypsirhina, Allotrius, and Cochoa, which inhabit Java, the
Himalayas, and Indo-China, all but the last extending south to Tenasserim,
but none of them occurring in Malacca, Sumatra, or Borneo. There are also
two species of birds--a trogon (_Harpactes oreskios_), and the Javanese
peacock (_Pavo muticus_), which inhabit only Java and the Indo-Chinese
countries, the former reaching Tenasserim and the latter Perak in the Malay
Peninsula.
Here, then, we find a series of remarkable similarities between Java and
the Asiatic continent, quite independent of the typical Malay
countries--Borneo, Sumatra, and the Malay Peninsula, which latter have
evidently formed one connected land, and thus appear to preclude any
independent union of Java and Siam.
The great difficulty in explaining these facts is, that all the required
changes of sea and land must have occurred within the period of existing
species of mammalia. Sumatra, Borneo, and Malacca have, as we have seen, a
great similarity as regards their species of mammals and birds, while Java,
though it differs from them in so curious a manner, has no greater degree
of speciality, since its species, when not Malayan, are almost all North
Indian or Siamese.
There is, however, one consideration which may help us over this
difficulty. It seems highly probable that in the equatorial regions species
have changed less rapidly than in the north temperate zone, on account of
the equality and stability of the equatorial climate. We have seen, in
Chapter X., how important an agent in producing extinction and modification
of species must have been the repeated changes from cold to warm, and from
warm to cold {385} conditions, with the migrations and crowding together
that must have been their necessary consequence. But in the lowlands, near
the equator, these changes would be very little if at all felt, and thus
one great cause of specific modification would be wanting. Let us now see
whether we can sketch out a series of not improbable changes which may have
brought about the existing relations of Java and Borneo to the continent.
Public-domain text, read in full here on John Shaqi.
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