Decoupling of Δar and particulate organic carbon dynamics in nearshore surface ocean waters

Abstract

We report results from two Lagrangian drifter surveys off the Oregon coast, using continuous shipboard sensors to estimate mixed-layer gross primary productivity (GPP), community respiration (CR), and net community production (NCP) from variations in biological oxygen saturation (ΔO2=Ar) and optically derived particulate organic carbon (POC). At the first drifter survey, conducted in a nearshore upwelling zone during the development of a microplankton bloom, net changes in ΔO2=Ar and [POC] were significantly decoupled. Differences in GPP and NCP derived from ΔO2=Ar (NCPO2=Ar) and POC (NCPPOC/time series suggest the presence of large POC losses from the mixed layer. At this site, we utilized the discrepancy between NCPO2=Ar and NCPPOC, and additional constraints derived from surface water excess nitrous oxide (N2O), to evaluate POC loss through particle export, DOC production, and vertical mixing fluxes. At the second drifter survey, conducted in lower-productivity, density-stratified offshore waters, we also observed offsets between ΔO2=Ar and POCderived GPP and CR rates. At this site, however, net [POC] and ΔO2=Ar changes yielded closer agreement in NCP estimates, suggesting a tighter relationship between production and community respiration, as well as lower POC loss rates. These results provide insight into the possibilities and limitations of estimating productivity from continuous underway POC and ΔO2=Ar data in contrasting oceanic waters. Our observations support the use of diel POC measurements to estimate NCP in lower-productivity waters with limited vertical carbon export and the potential utility of coupled O2 and optical measurements to estimate the fate of POC in highproductivity regions with significant POC export.