Phyto_ and zooplankton paleofluxes during the deposition of sapropel S1 (eastern Mediterranean): Biogenic carbonate preservation and paleoecological implications

The relative and absolute abundances and accumulation rates of foraminifera and calcareous nannofossils were quantified in a box_core containing sapropel S1 from the Florence Rise area (SE of Cyprus; 2302 m water depth). The main objective of this study was to reconstruct in detail variations in paleoecological conditions of water masses during the deposition of this sapropel. In particular, we qualitatively evaluated the importance of carbonate dissolution on planktonic assemblages to better interpret the abundance profiles obtained from the two investigated taxa.Selective carbonate corrosion in the core is shown by 1) the decrease in shell mass weight of selected species of planktonic foraminifera, 2) the decrease in accumulation rate of dissolution_susceptible holococcoliths and coccolith species, and 3) the absence of pteropods. However, the presence of other relatively dissolution_susceptible coccolith species throughout all of the S1 interval suggests moderate dissolution.Florisphaera profunda shows a marked increase in paleofluxes within the sapropel coupled with a decrease in the accumulation rate of the upper_middle photic zone coccoliths, suggesting an ecological depth_separation of the water column, probably characterised by higher nutrient availability at depth and nutrient_depleted surface waters between ∼ 10 and 6.5 kyr BP. In the same interval Turborotalita quinqueloba and Globigerina bulloides, two foraminiferal species frequently occurring during periods of high fertility, increase in relative abundance. The maximum increase in relative abundance of Globigerinoides ruber (var. alba and rosea) marks the climatic optimum phase and the maximum stratification in surface water that occurred at the beginning of sapropel S1 deposition when the bottom waters were anoxic. An important change in foraminiferal assemblages occurs at ∼ 8 kyr BP and corresponds with a negative shift in CaCO3, Ba and Corg contents. This short interval marks the establishment of relatively less anoxic conditions in the bottom water, introducing the last phase of sapropel formation.After ∼ 6.5 kyr BP, a progressive re_establishment of normal oceanographic conditions occurred before the real end of the sapropel S1. This transition is well recorded by the reoccurrence and major accumulation rate of the mixing indicator foraminiferal species Globorotalia inflata and by the gradual decrease in abundance of F. profunda.