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Sponges of the New Caledonian lagoon - IRD

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30<br />

<strong>Sponges</strong><br />

<strong>of</strong> <strong>the</strong> <strong>New</strong><br />

<strong>Caledonian</strong><br />

Lagoon<br />

water slows down thus enabling <strong>the</strong> choanocytes to absorb available nutrients and<br />

oxygen. Similarly, waste products are expelled into excurrent canals which have a<br />

larger diameter, and finally jettisoned into <strong>the</strong> surrounding seawater through <strong>the</strong><br />

oscules which are larger than inhalant pores. The water flow in <strong>the</strong> inhalant and<br />

exhalant canals varies from place to place, being fastest in <strong>the</strong> area <strong>of</strong> pores and<br />

oscules and slowest in <strong>the</strong> areas <strong>of</strong> absorption (choanocyte region). Water circula­<br />

tion can be fur<strong>the</strong>r controlled by <strong>the</strong> sponge by diverting <strong>the</strong> flow into additional,<br />

non-choanocytic chambers and sphincter-like sieves or filters, to slow down or<br />

increase flow rates as required. Water flow can also be halted completely or redirected<br />

to o<strong>the</strong>r parts <strong>of</strong> <strong>the</strong> body, if <strong>the</strong>re is a particle overflow in <strong>the</strong> network, for<br />

example. It is easy to observe this water flow using fluorescein injected into <strong>the</strong><br />

water system and subsequently ejected by <strong>the</strong> sponge. The generation <strong>of</strong> a strong<br />

exhaled current through <strong>the</strong> oscule is important as it minimises contamination<br />

between inhaled and exhaled water, <strong>the</strong> latter containing no food and molecular<br />

waste <strong>of</strong> no fur<strong>the</strong>r use to <strong>the</strong> sponge.<br />

There is a great diversity <strong>of</strong> aquiferous systems in Porifera. Some are relatively<br />

simple with short inhalant canals, a single choanocyte chamber and a single<br />

oscule, but most are much more complex reflecting particular ecophysiological<br />

adaptations. A hierarchy <strong>of</strong> complexity <strong>of</strong> <strong>the</strong> aquiferous system has its own terminology<br />

asconoid, syconoid, leuconoid, from simple to complex. These various<br />

modes <strong>of</strong> water canal systems were at one time considered to be <strong>the</strong> most important<br />

criteria in <strong>the</strong> taxonomy and evolution <strong>of</strong> <strong>the</strong> class Calcarea, whereas it is now<br />

recognised that <strong>the</strong>se different grades <strong>of</strong> body organisation have developed independently<br />

in several lines <strong>of</strong> calcareous sponges, now haVing little importance to<br />

<strong>the</strong>ir taxonomy. In <strong>the</strong> oemospongiae all known species are <strong>of</strong> <strong>the</strong> complex (Ieuconoid)<br />

construction, although recent discoveries indicate that some deep sea species<br />

lack choanocytes and associated water canal systems completely, being<br />

instead carnivorous.<br />

The distribution and size <strong>of</strong> pores and oscules, and <strong>the</strong> drainage canals associated<br />

with <strong>the</strong>se are frequently related to <strong>the</strong> general shape <strong>of</strong> <strong>the</strong> sponge. The morphology<br />

and organisation <strong>of</strong> <strong>the</strong> aquiferous system <strong>of</strong>ten clearly reflect adaptation <strong>of</strong> <strong>the</strong><br />

species to environmental hydrodynamic conditions. For example, in foliose<br />

sponges <strong>the</strong> pores are <strong>of</strong>ten on one side and <strong>the</strong> oscules on <strong>the</strong> o<strong>the</strong>r. In cup or<br />

vase-shaped sponges <strong>the</strong> pores are on <strong>the</strong> external surface and <strong>the</strong> oscules are

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