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Results 79<br />

Figure 4.5 Perspective view of the pycnocline for the four rotations (interpolated<br />

by cubic splines). While the cline is globally always around 70 m, local holes<br />

and bumps largely differ from one rotation to another<br />

“pump” water up or push it down). Cyclonic eddies may locally enrich<br />

the water in nutrients through upwelling, while anticyclonic ones may<br />

trap terrigenous products. In both cases, they are good candidates to<br />

test for correlations with the abundance of larval fish.<br />

4.3.2 Patchy distribution of fish larvae<br />

Of the 576 MOCNESS samples, 572 could be used. The mean volume<br />

filtered per sample was 1056 m 3 (Standard Deviation = 302 m 3 ). They<br />

contained an estimate of 47,800 fish larvae, comprised of at least 94 families<br />

(pelagic or deep specimen were not all sorted). Epi- and mesopelagic<br />

species dominated the samples with more than twice as many pelagic<br />

larvae than coral reef fish larvae. The two most abundant orders were<br />

the Clupeiformes (mostly Engraulidae) and the Myctophiformes. 10,794<br />

coral reef fish larvae were identified and the most common, by far, were<br />

Acanthuridae (Table 4.1). The relative abundances of coastal vs. oceanic<br />

taxa are comparable to those observed around another isolated atoll in<br />

the tropical North-Pacific 74 or in the Florida Keys 184 . Compared to the<br />

Keys, Bregmacerotidae were notably less prominent and Acanthuridae<br />

were particularly abundant. Among these > 10,000 coral reef fish larvae,<br />

Over 10,000 coral<br />

reef fish larvae,<br />

mostly pre-flexion

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