Net Community Production, Dissolved Organic Carbon Accumulation, and Vertical Export in the Western North Atlantic

The annual North Atlantic phytoplankton bloom represents a hot spot of biological activity during which a significant fraction of net community production (NCP) can be partitioned into dissolved organic carbon (DOC). The fraction of seasonal NCP that is not respired by the heterotrophic bacterial community and accumulates as seasonal surplus DOC (Delta DOC) in the surface layer represents DOC export potential to the upper mesopelagic zone, and in the North Atlantic this is facilitated by winter convective mixing that can extend to depths > 400 m. However, estimates of Delta DOC and vertical DOC export for the western North Atlantic remain ill-constrained and the influence of phytoplankton community structure on the partitioning of seasonal NCP as Delta DOC is unresolved. Here, we couple hydrographic properties from autonomous in situ sensors (ARGO floats) with biogeochemical data from two meridional transects in the late spring (similar to 44-56 degrees N along similar to -41 degrees VV) and early autumn (similar to 42-53 degrees N along similar to -41 degrees W) as part of the North Atlantic Aerosols and Marine Ecosystems Study (NAAMES). We estimate that 4-35% of seasonal NCP is partitioned as Delta DOC and that annual vertical DOC export ranges between 0.34 and 1.15 mol C m(-2) in the temperate and subpolar western North Atlantic. Two lines of evidence reveal that non-siliceous picophytoplankton, like Prochiorococcus, are indicator species of the conditions that control the accumulation of DOC and the partitioning of NCP as Delta DOC.