Multiple drivers of production and particle export in the western tropical North Atlantic : Particle export in western Atlantic Ocean

• Published in: Limnology and Oceanography
• Main Authors: Korte, Laura F., Brummer, Geert-Jan A., van der Does, Michèlle, Guerreiro, Catarina V., Mienis, Furu, Munday, Chris I., Ponsoni, Leandro, Schouten, Stefan, Stuut, Jan-Berend W.
• Other Authors: UCL - SST/ELI/ELIC - Earth & Climate
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Society of Limnology and Oceanography, Inc. 2020
• Subjects: Aquatic Science; Oceanography; North Atlantic
• Online Access: http://hdl.handle.net/2078.1/229116; https://doi.org/10.1002/lno.11442

To assess the impacts of Amazon River discharge, Saharan dust deposition, N2â€fixation and mixedâ€layer deepening on the biological carbon pump, sediment traps were moored from October 2012 to November 2013 at two sites in the western tropical North Atlantic (49°W,12°N/57°W,12°N). Particle exports interpreted along with satellite†and Argoâ€float data show peak fluxes in biogenic silica (31 mg m−2 d−1) and organic carbon (25 mg m−2 d−1) during the fall of 2013 that were ten to five times higher than any time earlier during the year. These high export fluxes occurred in tandem with high surface chlorophyll a concentrations associated with the dispersal of the Amazon River plume, following retroflection into the Northâ€Atlanticâ€Counterâ€Current. High fucoxanthin fluxes (> 80 μg m−2 d−1) and low δ15Nâ€values (−0.6‰) suggest a large contribution by marine diatomâ€diazotrophicâ€associations, possibly enhanced by wet Saharan dust deposition. During summer, the Amazon River plume resulted in high mass fluxes at 57°W that were enriched in biogenic silica but weakly influenced by diazotrophicâ€associations compared to the fall event at 49°W. High carbonateâ€carbon fluxes (17 mg m−2 d−1) dominated a second single event at 49°W during spring that was likely triggered by mixedâ€layer deepening. Rainâ€ratios of BSi/Ccarb amounted to 1.7 when associated with high export fluxes linked to the Amazon River plume. Compared to an annual average of 0.3, this indicates a more efficient uptake of CO2 via the biological pump compared to when the plume was absent, hence supporting earlier observations that the Amazon River plume is important for ocean CO2 sequestration.