M. Knappertsbusch, GEOGRAPHIC-DISTRIBUTION OF LIVING AND HOLOCENE COCCOLITHOPHORES IN THE MEDITERRANEAN-SEA, Marine micropaleontology, 21(1-3), 1993, pp. 219-247
The distribution patterns of living coccolithophores in the Mediterran
ean Sea during September-October, 1986 and February-March, 1988 were i
nvestigated and compared with the coccolith assemblages in the underly
ing surface sediments. The highest coccolithophore production was obse
rved during late winter, when maximum cell densities in the upper wate
r column reached 2.3 X 10(5) individuals per liter, which is more than
5 to 10 times the average concentration in summer. During February to
March 1988 E. huxleyi dominated the community and probably was close
to bloom conditions in the Eastern Mediterranean Sea. Although these f
luctuations in the living flora between September-October and February
-March represent snapshots during the seasonal succession-cycle of the
coccolithophore flora in the Mediterranean Sea, they are interpreted
to be related to seasonal, wind-induced hydrological changes from a hi
ghly stratified upper water mass during summer to a homogenized waterc
olumn during winter. The enrichment of E. huxleyi in the surface sedim
ents suggests, that this species probably produces regular blooms in s
urface waters during late winter or spring in that area. The rather co
nsistent abundance of the deep dwelling species Florisphaera profunda
in the surface sediments may be related to the less pronounced seasona
lity in the lower photic zone. Although most of the observed geographi
c change in the taxonomic composition in either of the two plankton da
ta sets are due to seasonal and daily to weekly fluctuations of the co
ccolithophorid populations, at least in one species, Gephyrocapsa ocea
nica, a relationship to surface currents was found. This species proba
bly enters the Mediterranean Sea through the Strait of Gibraltar and i
s a tracer for Atlantic surface waters. Other species that preferencia
lly occurred in the Western Mediterranean Sea are Gephyrocapsa ericson
ii and Gephyrocapsa protohuxleyi, but relationships to surface cur-ren
ts were less clear.