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June 1 - 3 , 1978 - University of Hawaii at Manoa

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HAWAII IBP SYNTHESIS:<br />

8. ISLAND ECOSYSTEMS: WHAT IS UNIQUE ABOUT THEIR ECOLOGY?<br />

Dieter Mueller-Dombois<br />

Department <strong>of</strong> Botany<br />

<strong>University</strong> <strong>of</strong> <strong>Hawaii</strong> <strong>at</strong> <strong>Manoa</strong><br />

Honolulu, <strong>Hawaii</strong> 96822<br />

We may now ask the question whether we have found anything<br />

unique or different in the ecology <strong>of</strong> island ecosystems from our<br />

studies. This is not an easy question.<br />

It is clear th<strong>at</strong> the biological evolution <strong>of</strong> our island ecosystems<br />

has been r<strong>at</strong>her unique. Four factors stand out which<br />

contribute to the unique biological evolution <strong>of</strong> ecosystems here.<br />

These are the extreme isol<strong>at</strong>ion <strong>of</strong> the island group, the small<br />

- size <strong>of</strong> the island habit<strong>at</strong>s, the recenc <strong>of</strong> the oceanic islands<br />

as a group, and their perturb<strong>at</strong>ion dy in connection with<br />

volcanism.<br />

The extreme isol<strong>at</strong>ion had a significant "screening effect"<br />

on wh<strong>at</strong> organism groups could get here and establish themselves<br />

successfully. This screening effect excluded any plants with<br />

large seeds or small seeds <strong>of</strong> short longevity. It also excluded<br />

among animals, all terrestrial mammals (except the hoary b<strong>at</strong>),<br />

large reptiles, and prim<strong>at</strong>es, except man.<br />

The small size <strong>of</strong> the island habit<strong>at</strong>s is the result <strong>of</strong> small<br />

isiand land masses jutting h-i-gh ou~f-o~f the-ocean. Thus, we have<br />

distinct altitudinal segreg<strong>at</strong>ions <strong>of</strong> habit<strong>at</strong>s with their own<br />

temper<strong>at</strong>ure regimes. Furthermore, these small land masses are<br />

segreg<strong>at</strong>ed into windward (pluvio tropical) and leeward (xerotropical)<br />

habit<strong>at</strong>s with their own rainfall regimes. The habit<strong>at</strong>s<br />

are further fractioned by gre<strong>at</strong> vari<strong>at</strong>ions in substr<strong>at</strong>e, ranging<br />

from recent volcanic flows to old, sceletized, and nutrientdepauper<strong>at</strong>ed<br />

l<strong>at</strong>osols. This island habit<strong>at</strong> mosaic brings about<br />

another factor <strong>of</strong> important ecological consequences, and th<strong>at</strong> is<br />

the very limited recurrence <strong>of</strong> similar habit<strong>at</strong>s across the island<br />

chain. These narrow habit<strong>at</strong> dimensions strongly l i m i t the<br />

popul<strong>at</strong>ion sizes <strong>of</strong> the island biota.<br />

The recency <strong>of</strong> oceanic islands as a group is undoubtedly <strong>of</strong><br />

evolutionary significance also. They origin<strong>at</strong>ed in the Tertiary,<br />

when the modern angiosperm flora had already evolved. In con-<br />

trast, some <strong>of</strong> the continental tropical ecosystems evolved with-<br />

out major geological disturbances forming a primary succession<br />

from seed fern forests to primitive gymnosperm and angiosperm<br />

forests to modern angiosperm forests. These continental eco-<br />

systems developed during a much gre<strong>at</strong>er evolutionary time span.

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