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Ecoregional Assessment of Biological Diversity in East Kalimantan

Ecoregional Assessment of Biological Diversity in East Kalimantan

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<strong>East</strong> <strong>Kalimantan</strong> <strong>Ecoregional</strong> <strong>Assessment</strong>: Chapter 2 – Target Ecological Systems<br />

These <strong>in</strong>clude the Dulit Frogmouth, Batrachostomus harterti; Hose’s Broadbill,<br />

Calyptomena hosei and Pygmy Darkeye, Oculoc<strong>in</strong>cta squamifrons (Sujatnika et al. 1995).<br />

Mammal species are also usually moderately high <strong>in</strong> Lower Montane/ Cloud Forest <strong>in</strong> Lore<br />

L<strong>in</strong>du National Park, and do not decl<strong>in</strong>e substantially from their diversity <strong>in</strong> lowland forests,<br />

except for bats, which decl<strong>in</strong>e dramatically above 1500m a.s.l. Evidence from Pen<strong>in</strong>sular<br />

Malaysia suggests that biomass <strong>of</strong> primates (Caldecott 1980) and some groups <strong>of</strong> soil<br />

macr<strong>of</strong>auna (Coll<strong>in</strong>s et al. <strong>in</strong> MacK<strong>in</strong>non et al. 1996) may <strong>of</strong>ten be highest <strong>in</strong> these lower<br />

montane ra<strong>in</strong>forests, especially oligochaetes. This does not appear to be the case with the<br />

higher order primate Orangutan, which tend to favor vegetation below 1000m a.s.l. Nijman<br />

& Meijaard <strong>in</strong> Nijman (2001) stated that <strong>in</strong> <strong>East</strong> <strong>Kalimantan</strong>, the Bornean Gibbon was<br />

“conf<strong>in</strong>ed to closed canopy forest <strong>in</strong> the lowlands and hills up to c.1500m a.s.l.” Suzuki et al.<br />

(1997) noted that <strong>in</strong> the Berau and Kutai District <strong>of</strong> <strong>East</strong> <strong>Kalimantan</strong>, Bornean gibbon is<br />

more common on hills and uplands.<br />

MacK<strong>in</strong>non et al. (1996: Table 7.4) reported that there was no clear trend for gibbon to<br />

decl<strong>in</strong>e <strong>in</strong> density between altitudes <strong>of</strong> 0-900m. Numbers <strong>of</strong> groups <strong>of</strong> gibbon <strong>in</strong> Sabah (H.<br />

muelleri) also did not decl<strong>in</strong>e up to 1500m above sea level – although they did <strong>in</strong> the<br />

altitud<strong>in</strong>al range <strong>of</strong> 1500 – 3000m. However, it is possible that this decl<strong>in</strong>e at very high<br />

altitudes was strongly <strong>in</strong>fluenced by their typical low density <strong>in</strong> cloud forests. This would be<br />

expected given the low, stunted nature <strong>of</strong> the trees and the low abundance <strong>of</strong> fruit <strong>in</strong> cloud<br />

forests. It is reasonable to assume that gibbon group size would also decl<strong>in</strong>e markedly <strong>in</strong><br />

upper montane ra<strong>in</strong>forests (1800-2000m).<br />

Evidence from Mt. K<strong>in</strong>abalu, <strong>in</strong> the Malaysian State <strong>of</strong> Sabah, <strong>in</strong>dicates that species richness<br />

<strong>of</strong> butterflies <strong>in</strong> these Lower Montane Ra<strong>in</strong>forests is less than <strong>in</strong> Lowland Ra<strong>in</strong>forests, but is<br />

higher than <strong>in</strong> the Upper Montane Ra<strong>in</strong>forest /Cloud Forest system type.<br />

Conservation issues and threats<br />

• Logg<strong>in</strong>g<br />

Logg<strong>in</strong>g <strong>of</strong> Lower Montane Ra<strong>in</strong>forest is much less than what occurs below 1000m a.s.l.<br />

because <strong>of</strong> the costs <strong>of</strong> operat<strong>in</strong>g on high slopes. However, there is some logg<strong>in</strong>g above<br />

1000m. The contribution <strong>of</strong> such logg<strong>in</strong>g to <strong>in</strong>creased suspended sediments <strong>in</strong> streams<br />

and rivers caused by erosion on these steep slopes is out <strong>of</strong> proportion to the relatively<br />

small areas that are logged. Also, the removal <strong>of</strong> forest from the lowland areas<br />

surround<strong>in</strong>g these Montane forests will be critically dependent upon the seed production<br />

from these protected forests to replenish and restore the lowland forests – provided <strong>of</strong><br />

course that they are left alone for decades to naturally revegetate. This seems unlikely<br />

given current population and <strong>in</strong>dustrial development trends <strong>in</strong> the region.<br />

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