B. Delesalle et al., DIRECT MEASUREMENTS OF CARBON AND CARBONATE EXPORT FROM A CORAL-REEF ECOSYSTEM (MOOREA ISLAND, FRENCH-POLYNESIA), Coral reefs, 17(2), 1998, pp. 121-132
The export of carbon and carbonate from coral reefs was investigated t
hrough a multidisciplinary investigation of the hydrological, geochemi
cal, sedimentological and biological features of Tiahura reef on the n
orthwestern coast of Moorea Island (French Polynesia). The hydrology o
f the fore-reef is characterised by prevailing longshore western curre
nts and a strong thermocline. As revealed by turbidity structures (ben
thic and intermediate nepheloid layers) and by the amount of particles
collected by near-bottom sediment traps, horizontal and downslope adv
ections of particles dominate over offshore vertical transport. The ex
ported material is rich in carbonate (ca. 80%) and poor in organic mat
ter (ca. 4%). Sedimentation rates at 430 m depth, i.e. definitive expo
rt, reached 209.6 mg m(-2) d(-1) (dry weight). Estimates of carbon and
carbonates export for Tiahura reef also reported here represent respe
ctively 47% and 21% of the organic and inorganic carbon produced withi
n the reef.