Coccolithophore carbonate during the last 450 ka in the NW Pacific Ocean (ODP site 1209B, Shatsky Rise)

This study focuses on Pleistocene–Holocene sediments from the Shatsky Rise (Ocean Drilling ProgramSite 1209B, NW Pacific Ocean). We quantify the contribution of calcite made by coccoliths in oceanic sediments,investigating the role of calcareous nannoplankton during the last 450 ka. Coccolith carbonate constitutes 60–90% ofbulk carbonate. Coccolith carbonate accumulation rates (CARs) and CaCO3 fine fraction confirm that coccolithophoresare major contributors to the carbonate export and accumulation. Primary productivity shows highest values frommarine isotope stage (MIS) 12 to 8. Thereafter, although coccolith calcite content remains high, other sedimentcomponents, such as as foraminifera and biogenic opal, seem to be favored, perhaps related to an increase infertilization by eolian dust. Our results demonstrate the important role of coccolithophore production and sedimentationon the regulation of ocean carbonate chemistry on time scales >1000–100 000 years. On glacial–interglacial scales,coccolithophore productivity could have affected deep-water saturation by buffering deep-sea CO2 through increasedcarbonate dissolution episodes. Spectral and wavelet analyses are consistent with CARs primarily driven by glacial–interglacial variability and obliquity-controlled changes. Coccolith-based paleoceanographic reconstructions allow us toestablish that during the last 450 ka the mid-latitudes of the NW Pacific are controlled by the dynamics of the El Nino Southern Oscillation perturbations and Boreal Monsoon system.