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Islands Between the Realms: A Revised Checklist of the ...

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108 André KOCH et al.: A <strong>Revised</strong> <strong>Checklist</strong> <strong>of</strong> <strong>the</strong> Herpet<strong>of</strong>auna <strong>of</strong> <strong>the</strong> Talaud Archipelago, Indonesia<br />

1. INTRODUCTION<br />

The Talaud Archipelago represents <strong>the</strong> nor<strong>the</strong>rn most area<br />

within <strong>the</strong> Wallacea transition zone between <strong>the</strong> Oriental<br />

and Australian faunal regions. The remote island group lies<br />

in <strong>the</strong> nor<strong>the</strong>rn Molucca Sea between North Sulawesi,<br />

Mindanao in <strong>the</strong> sou<strong>the</strong>rn Philippines, and Halmahera in<br />

<strong>the</strong> nor<strong>the</strong>rn Moluccas. The Talaud Archipelago comprises<br />

three main islands: Karakelong, Salibabu and Kaburuang<br />

(Fig. 1). Geologically, <strong>the</strong> Molucca Sea Plate with its<br />

inverted U-shape dips east under Halmahera and west under<br />

<strong>the</strong> Sangihe Arc (MCCAFFREY et al. 1980). The Talaud<br />

<strong>Islands</strong> are situated on <strong>the</strong> Sangihe forearc separated by<br />

a deep ocean trench from <strong>the</strong> largely submarine Sangihe<br />

Arc with its few emergent volcanic islands like Sangihe<br />

and Siau (HALL 2002). The Talaud Island group consists<br />

<strong>of</strong> a sedimentary sequence <strong>of</strong> Middle Miocene to Pleistocene<br />

age and includes probable mid-Miocene volcanic<br />

rocks and volcaniclustic turbidites (MOORE et al. 1981).<br />

Pleistocene coral limestone, <strong>the</strong> youngest rocks on Talaud,<br />

are exposed mostly along <strong>the</strong> coast lines (Fig. 2), but also<br />

at 400–500 m elevation on Kaburuang, showing <strong>the</strong> significant<br />

amount <strong>of</strong> recent uplift (MOORE et al. 1981). The<br />

highest elevation <strong>of</strong> only 650 m above sea level is found<br />

on Karakelong Island.<br />

The Talaud <strong>Islands</strong> toge<strong>the</strong>r with Sulawesi and o<strong>the</strong>r islands<br />

<strong>of</strong> present day central Indonesia belong to a biogeographic<br />

transition region called Wallacea (see summaries<br />

by MAYR [1944] and SIMPSON [1977]). Australopapuan and<br />

Asian animals meet at <strong>the</strong> respective outer limits <strong>of</strong> <strong>the</strong>ir<br />

distribution. Consequently, in <strong>the</strong> light <strong>of</strong> biogeography,<br />

<strong>the</strong> Talaud <strong>Islands</strong> form <strong>the</strong> nor<strong>the</strong>rnmost submerged area<br />

<strong>of</strong> this region. Traditionally, <strong>the</strong> Talaud Archipelago has<br />

been dealt with scientifically with Sulawesi to which it is<br />

indirectly connected via <strong>the</strong> Sangihe Island arch. However,<br />

<strong>the</strong> direct over-water distance to North Sulawesi <strong>of</strong><br />

about 300 km is significantly more distant than Halmahera<br />

in <strong>the</strong> Moluccas (ca. 210 km) or Mindanao in <strong>the</strong><br />

Philippines (ca. 170 km).<br />

Fig. 1.<br />

Map <strong>of</strong> <strong>the</strong> Talaud <strong>Islands</strong> located between Sulawesi, Halmahera (Moluccas) and Mindanao (Philippines).

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