C. Riauxgobin et al., UNDAMAGED SEDIMENTED COCCOLITHOPHORIDS IN A DEEP ENVIRONMENT (CONTINENTAL-SLOPE OF THE GULF OF LIONS), Marine geology, 123(3-4), 1995, pp. 239-252
At different periods of the year, undisturbed sediment samples from th
e continental slope of the Gulf of Lions were collected with a multipl
e gravity corer. The overlying water (0-20 cm above the sediment) and
the surface water masses were also collected. The following stations w
ere sampled: R(4), an interfluve (a platform between two canyons), 760
m deep; R(5), at the junction of two canyon floors, 1540 m and R(6),
at the top of the wall, 1280 m. At all stations, the top sediment laye
r and the overlying water were enriched with coccoliths. During a late
spring cruise (March 22-April 5, 1991) a thin microphyte-enriched lay
er at the water-sediment interface of station R, contained encysted di
atoms, dinophytes and coccolithophorids. Several of the coccolithophor
id species were in good preservation, among which Emiliania: huxleyi w
as dominant and showed a considerable range of morphological variation
s in coccolith length and degree of calcification. The presence of tin
tinnids that use coccoliths to build their loricae reflects the specie
s composition in the water masses from which this biodeposit originate
d. Homogeneous hydrological conditions favoured the accumulation of th
is deep biodeposit.