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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 1 – Background & Analysis Process<br />

Identification <strong>of</strong> annual precipitation zones<br />

In the portfolio assembly process, target ecological system occurrences were also selected to<br />

represent three major precipitation zones with<strong>in</strong> each stratigraphic unit ∗ (Figure J). In<br />

stratigraphic units 1 to 3 there are generally gradients that show <strong>in</strong>creas<strong>in</strong>g aridity from the<br />

western upper elevation areas eastward to the coast. The exception is the area <strong>in</strong> stratigraphic<br />

unit 1 between the Kayan and the Sesayap rivers. These trends <strong>in</strong> aridity also occur along the<br />

ma<strong>in</strong> gradients <strong>of</strong> the water catchment areas; they are more compressed <strong>in</strong> the 2,000 mm -<br />

3,000 mm zone <strong>of</strong> the Mahakam River catchment compared to the Kayan River, for example.<br />

From a biological<br />

standpo<strong>in</strong>t, ra<strong>in</strong>fall gradients<br />

with<strong>in</strong> these catchments<br />

typically translate to trends<br />

<strong>in</strong> phenology <strong>of</strong> flower<strong>in</strong>g<br />

and fruit<strong>in</strong>g along the<br />

catchments. Such trends can<br />

be seen <strong>in</strong> the flower<strong>in</strong>g<br />

occurrences (mast<br />

flower<strong>in</strong>g) <strong>of</strong> dipterocarp<br />

species and Ficus species <strong>in</strong><br />

<strong>East</strong> <strong>Kalimantan</strong> (Kade<br />

Sidiyasa pers. com.). It can<br />

be reasoned that <strong>in</strong> the past,<br />

many <strong>of</strong> the more vagile<br />

species, such as bats, birds,<br />

and pigs followed these<br />

trends <strong>in</strong> flower<strong>in</strong>g and<br />

fruit<strong>in</strong>g and exhibited local<br />

movement patterns along<br />

these river systems and<br />

associated catchment areas.<br />

Such is also the case with<br />

some <strong>of</strong> the more<br />

charismatic fauna like the<br />

Bornean gibbon and<br />

orangutan.<br />

Figure J – Precipitation Zones across <strong>East</strong> <strong>Kalimantan</strong><br />

∗ The gradients for these precipitation zones were generated us<strong>in</strong>g mean annual ra<strong>in</strong>fall data from 35 stations distributed throughout <strong>East</strong><br />

<strong>Kalimantan</strong> from the period 1890-1970. Additionally, 6 <strong>of</strong> the 35 stations distributed north to south <strong>in</strong> the Prov<strong>in</strong>ce cont<strong>in</strong>ued to generate<br />

data from 1990-2000. These gauges <strong>in</strong>dicated a general dry<strong>in</strong>g trend by an average <strong>of</strong> 200 mm from the values reflected for those same<br />

stations <strong>in</strong> the first 80-year period.<br />

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