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Download (3398Kb) - ePrints Soton - University of Southampton

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al., 1997). In a review (Vrijenhoek, 1997) citing hydrothermal vent-endemic<br />

molluscs, two species <strong>of</strong> bivalves and two species <strong>of</strong> limpets showed evidence <strong>of</strong> high<br />

rates <strong>of</strong> gene flow that were not restricted by the topology <strong>of</strong> the ridge system or by<br />

geographical distance.<br />

In the deep sea, species with planktotrophic larval development may be<br />

restricted to regions where there is sufficiently high surface production in order to<br />

produce an important amount <strong>of</strong> fine detrital food at bathypelagic and abyssopelagic<br />

depths. Therefore planktotrophic larvae could be limited by food in oligotrophic areas,<br />

whereas lecithotrophic larvae may survive even if advected to areas <strong>of</strong> low<br />

productivity using energy stored internally (Young et al., 1997). A very important<br />

case to mention regarding planktotrophy and widespread distribution is the deep-sea<br />

synaptid holothurian Protankyra brychia Verrill, which essentially has a cosmopolitan<br />

distribution. The oocyte diameters <strong>of</strong> P. brychia indicate planktotrophic larval<br />

development or lecithotrophic larval development followed by planktotrophy (Billet,<br />

1991; Pearse, 1994). Pawson et al. (2003) presented evidence that this species has a<br />

near surface planktotrophic larval stage which had been reported in the literature as<br />

the Giant Auricularia larva Auricularia nudibranchiata Chun (Chun, 1896; Oshima,<br />

1911; MacBride, 1920; Inaba, 1934; Garstang, 1939).<br />

1.3- Deep-water formation and species dispersal<br />

Developmental mode is not the only factor that might determine dispersal<br />

distance. Scheltema (1986b) established that “the maximum potential distance that a<br />

larva can be dispersed and the likelihood that it survives to settlement is related to (a)<br />

the length <strong>of</strong> its planktonic life and (b) to the rate and direction <strong>of</strong> the currents that<br />

transport it”.<br />

20

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