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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 />

I. Major Rivers and Associated Lakes<br />

Description<br />

Photo courtesy <strong>of</strong> Donald Bason<br />

Rivers<br />

Borneo is an island <strong>of</strong> great rivers, <strong>in</strong>clud<strong>in</strong>g the Mahakam and Kayan <strong>in</strong> <strong>East</strong> <strong>Kalimantan</strong>,<br />

which orig<strong>in</strong>ate <strong>in</strong> the western Iban Mounta<strong>in</strong>s. The Mahakam River, at around 650 km <strong>in</strong><br />

length, is one <strong>of</strong> the longest rivers <strong>in</strong> Indonesia; its catchment area encompasses<br />

approximately 77,700 sq.km (Suryadiptra et al. 2000). The chemical, physical and biological<br />

conditions <strong>in</strong> these large rivers change from the headwaters to their large term<strong>in</strong>al deltas at<br />

the sea. In the headwaters, rivers are narrow, turbulent, clear water and covered by a canopy<br />

<strong>of</strong> trees - whereas <strong>in</strong> the lower pla<strong>in</strong> country, they are broad meander<strong>in</strong>g ribbons, full <strong>of</strong><br />

sediment, which colors them a muddy brown. Heavy ra<strong>in</strong>s produce dramatic changes <strong>in</strong><br />

water levels, and flash floods are frequent.<br />

Current velocity and concentration <strong>of</strong> dissolved salts is greater <strong>in</strong> the lower reaches <strong>of</strong> rivers<br />

than the headwaters, but temperatures are higher and consequently the concentration <strong>of</strong><br />

dissolved oxygen tends to be less <strong>in</strong> the lower reaches (MacK<strong>in</strong>non et al. (1996). Fish species<br />

as well as the Mahakam River Dolph<strong>in</strong> (Pesut), respond to these changes <strong>in</strong> flood<strong>in</strong>g and<br />

water velocity. Pesut move from their core range area upstream <strong>in</strong>to the tributaries follow<strong>in</strong>g<br />

the first important ra<strong>in</strong>s where they appear to feed <strong>in</strong>tensively <strong>in</strong> areas that harbor good<br />

populations <strong>of</strong> fish. The flood<strong>in</strong>g cycle also greatly changes the fisheries catch <strong>in</strong> the area.<br />

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