Insights into the deglacial variability of phytoplankton community structure in the eastern equatorial Pacific Ocean using [(231)Pa/(230)Th]xs and opal-carbonate fluxes

Fully and accurately reconstructing changes in oceanic productivity and carbon export and their controls is critical to determining the efficiency of the biological pump and its role in the global carbon cycle through time, particularly in modern CO(2) source regions like the eastern equatorial Pacific (EEP). Here we present new high-resolution records of sedimentary (230)Th-normalized opal and nannofossil carbonate fluxes and [(231)Pa/(230)Th]xs ratios from site MV1014-02-17JC in the Panama Basin. We find that, across the last deglaciation, phytoplankton community structure is driven by changing patterns of nutrient (nitrate, iron, and silica) availability which, in turn, are caused by variability in the position of the Intertropical Convergence Zone (ITCZ) and associated changes in biogeochemical cycling and circulation in the Southern Ocean. Our multi-proxy work suggests greater scrutiny is required in the interpretation of common geochemical proxies of productivity and carbon export in the EEP.