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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 />

C. Peat Swamp Forest<br />

Description<br />

In <strong>East</strong> <strong>Kalimantan</strong>, Peat Swamp Forests are most abundant <strong>in</strong> the lakes area <strong>of</strong> the middle<br />

Mahakam Bas<strong>in</strong> and around the mar<strong>in</strong>e alluvial pla<strong>in</strong>s <strong>of</strong> the Kayan River. MacK<strong>in</strong>non et al.<br />

(1996; Table 3.1) reports that the extent <strong>of</strong> this forest type <strong>in</strong> <strong>East</strong> <strong>Kalimantan</strong> has shrunk<br />

from an orig<strong>in</strong>al area <strong>of</strong> 749,000 ha. to 594,000 ha. <strong>in</strong> 1996. Our LandSat analysis shows an<br />

areal extent <strong>of</strong> just over 303,000 hectares as <strong>of</strong> 2001 – <strong>in</strong>dicat<strong>in</strong>g perhaps an even swifter<br />

decl<strong>in</strong>e <strong>of</strong> this endangered habitat type.<br />

Peat Swamps are typically large ra<strong>in</strong>-fed swamps throughout <strong>Kalimantan</strong> that occur beh<strong>in</strong>d<br />

the coastal mangrove swamps along the coast and <strong>in</strong> poorly-dra<strong>in</strong>ed depressions at higher<br />

altitudes. The soil <strong>of</strong> these swamps has more than 65% organic matter content, which is<br />

commonly around 50cm deep but can be as much as 20 meters deep. The surface is a solid<br />

fibrous material form<strong>in</strong>g a crust over the semi-liquid <strong>in</strong>terior. It is extremely deficient <strong>in</strong><br />

nutrients and has a high acidity (pH ≤ 4).<br />

Peat Swamps are dra<strong>in</strong>ed by ‘blackwater rivers’, as is the case with the Heath Forests. Most<br />

peat swamps are zonal <strong>in</strong> nature with several concentric r<strong>in</strong>gs, start<strong>in</strong>g with tall forest with an<br />

outer uneven canopy (See Figure2.C.1 – adapted from MacK<strong>in</strong>non, 1996), then <strong>in</strong>ner zones<br />

<strong>of</strong> trees <strong>of</strong> dim<strong>in</strong>ish<strong>in</strong>g height- with a reduction <strong>in</strong> species richness <strong>of</strong> plants towards the<br />

center <strong>of</strong> the swamp. These forests share many <strong>of</strong> the tree species found <strong>in</strong> adjacent lowland<br />

evergreen dipterocarp forests. There are conspicuous parallels <strong>in</strong> structure and physiognomy<br />

between the more central parts <strong>of</strong> the Peat Swamp Forests and the Heath Forests (Whitmore<br />

1984).<br />

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