Table_1_Net Community Production, Dissolved Organic Carbon Accumulation, and Vertical Export in the Western North Atlantic.DOCX

• Main Authors: Nicholas Baetge, Jason R. Graff, Michael J. Behrenfeld, Craig A. Carlson
• Format: Dataset
• Language: unknown
• Published: 2020
• Subjects: Oceanography; Marine Biology; Marine Geoscience; Biological Oceanography; Chemical Oceanography; Physical Oceanography; Marine Engineering; North Atlantic Aerosols and Marine Ecosystems Study; net community production; dissolved organic carbon; ARGO; convective overturn; vertical export; phytoplankton community composition; North Atlantic
• Online Access: https://doi.org/10.3389/fmars.2020.00227.s001; https://figshare.com/articles/Table_1_Net_Community_Production_Dissolved_Organic_Carbon_Accumulation_and_Vertical_Export_in_the_Western_North_Atlantic_DOCX/12219551

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 (ΔDOC) 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 ΔDOC 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 ΔDOC 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 (∼44–56°N along ∼−41°W) and early autumn (∼42–53°N along ∼−41°W) as part of the North Atlantic Aerosols and Marine Ecosystems Study (NAAMES). We estimate that 4–35% of seasonal NCP is partitioned as ΔDOC 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 Prochlorococcus, are indicator species of the conditions that control the accumulation of DOC and the partitioning of NCP as ΔDOC.