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Endemic Fauna of Andaman and Nicobar Islands Bay of Bengal

Endemic Fauna of Andaman and Nicobar Islands Bay of Bengal

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level. Quite a few lists <strong>of</strong> endemic species <strong>of</strong> the isl<strong>and</strong>s on various groups are made available (Tikader<br />

<strong>and</strong> Das, 1985; Chakraborty, 1997; Agarwal, 1998; M<strong>and</strong>al <strong>and</strong> Chakraborthy, 1999; Alfred <strong>and</strong><br />

Chakraborty, 2002 <strong>and</strong> Jayaraj <strong>and</strong> Andrews, 2005). Subsequently many species <strong>and</strong> subspecies<br />

considered as endemics have been shifted to non-endemics <strong>and</strong> many new species have been added.<br />

By summing up <strong>of</strong> all the available literature records, an updated list <strong>of</strong> endemics <strong>of</strong> the isl<strong>and</strong>s has<br />

been prepared. About 1117 species <strong>and</strong> subspecies <strong>of</strong> animals <strong>of</strong> major groups, both vertebrate <strong>and</strong><br />

invertebrates, inhabiting terrestrial, freshwater <strong>and</strong> marine habitats considered endemic to the<br />

<strong>Andaman</strong> <strong>and</strong> <strong>Nicobar</strong> Isl<strong>and</strong>s is presented here. For the higher vertebrate groups viz. mammals,<br />

birds, reptiles, amphibians <strong>and</strong> fish common name, diagnostic features, habitat, distribution <strong>and</strong><br />

current status is given. Where as for other groups like molluscs, crustaceans, mei<strong>of</strong>aunal elements,<br />

insects, etc. only their habitat, distribution <strong>and</strong> current staus is given as these small organisms can not<br />

be identified to species level by the common man or an amature in the field. The literature cited in<br />

the text is given at the end.<br />

Physiography <strong>of</strong> the isl<strong>and</strong>s<br />

The <strong>Andaman</strong> <strong>and</strong> <strong>Nicobar</strong> Archipelago comprises several hundred isl<strong>and</strong>s were once part <strong>of</strong><br />

the Asian main l<strong>and</strong> but got separated over 100 million years ago during the Upper Mesozoic Period.<br />

The archipelago can be broadly divided into two groups, namely the <strong>Andaman</strong>s <strong>and</strong> the <strong>Nicobar</strong>s<br />

separated by the Ten-degree Channel which is about 150 km wide <strong>and</strong> 400 fathoms deep. The main<br />

part <strong>of</strong> <strong>Andaman</strong> Group is collectively called as the Great <strong>Andaman</strong>s comprising five adjoining isl<strong>and</strong>s,<br />

viz. North <strong>Andaman</strong>, Middle <strong>Andaman</strong>, South <strong>Andaman</strong>, Baratang <strong>and</strong> Rutl<strong>and</strong> isl<strong>and</strong>s. All these isl<strong>and</strong><br />

masses are separated by narrow channels. The southern most <strong>of</strong> the isl<strong>and</strong> group is Little <strong>Andaman</strong><br />

which is separated by a straight called Ducnan Passage. The <strong>Nicobar</strong> group comprises <strong>of</strong> about 24<br />

isl<strong>and</strong>s with a total l<strong>and</strong> mass <strong>of</strong> about 1,841 sq km. The northern most point <strong>of</strong> the group is Car<br />

<strong>Nicobar</strong> Isl<strong>and</strong> <strong>and</strong> the southern most is Indira Point or Pigmilion Point <strong>of</strong> the Great <strong>Nicobar</strong> Isl<strong>and</strong>. Of<br />

all the isl<strong>and</strong>s <strong>of</strong> <strong>Nicobar</strong> Group, Great <strong>Nicobar</strong> isl<strong>and</strong> is the largest having an area <strong>of</strong> 1,045 sq.km. The<br />

other major isl<strong>and</strong>s <strong>of</strong> the group are Car <strong>Nicobar</strong>, Chowra, Tillanchong, Teressa, Bompoka, Camorta,<br />

Trinket, Nancowry, Katchal, Pulomilo, Kondul <strong>and</strong> Little <strong>Nicobar</strong>. All the isl<strong>and</strong>s <strong>of</strong> the archipelago are<br />

fertile <strong>and</strong> support evergreen vegetation. The present configuration achieved by these isl<strong>and</strong>s only<br />

about 26 million years ago. The two isl<strong>and</strong>s, Narcondam <strong>and</strong> Barren are <strong>of</strong> volcanic origin. The<br />

Narcondam was totally dormant <strong>and</strong> extinct for quite long period, shown the signs <strong>of</strong> eruption during<br />

the mega earth quake took place on 26 th December 2004 <strong>and</strong> the Brren Isl<strong>and</strong> is highly active <strong>and</strong><br />

frequently erupting. The soil cover is more or less thin varying between two to five meters in the hill<br />

tracts. The coastal flats are admixture <strong>of</strong> silty clay, s<strong>and</strong> <strong>and</strong> fragments <strong>of</strong> coral lime. The soil is<br />

moderately acidic with high humus on top layer. The climate is <strong>of</strong> tropical nature. Due to proximity <strong>of</strong><br />

2

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