Seasonality of downward carbon export in the Pacific Southern Ocean revealed by multi-year robotic observations

At high latitudes, the biological carbon pump, which exports organic matter from the surface ocean to the interior, has been attributed to the gravitational sinking of particulate organic carbon. Conspicuous deficits in ocean carbon budgets challenge this as a sole particle export pathway. Recent mo...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Lacour, Léo, Llort, Joan, Briggs, Nathan, Strutton, Peter G., Boyd, Philip W.
Other Authors: Barcelona Supercomputing Center
Format: Article in Journal/Newspaper
Language:English
Published: Nature Research 2023
Subjects:
Online Access:http://hdl.handle.net/2117/385171
https://doi.org/10.1038/s41467-023-36954-7
Description
Summary:At high latitudes, the biological carbon pump, which exports organic matter from the surface ocean to the interior, has been attributed to the gravitational sinking of particulate organic carbon. Conspicuous deficits in ocean carbon budgets challenge this as a sole particle export pathway. Recent model estimates revealed that particle injection pumps have a comparable downward flux of particulate organic carbon to the biological gravitational pump, but with different seasonality. To date, logistical constraints have prevented concomitant and extensive observations of these mechanisms. Here, using year-round robotic observations and recent advances in bio-optical signal analysis, we concurrently investigated the functioning of two particle injection pumps, the mixed layer and eddy subduction pumps, and the gravitational pump in Southern Ocean waters. By comparing three annual cycles in contrasting physical and biogeochemical environments, we show how physical forcing, phytoplankton phenology and particle characteristics influence the magnitude and seasonality of these export pathways, with implications for carbon sequestration efficiency over the annual cycle. L.L. was supported by a European Union’s Horizon 2020 Marie Sklodowska-Curie grant (no. 892653). Visits by L.L. to IMAS/UTas were supported by the Australian Research Council Special Research Initiative for Antarctic Gateway Partnership (Project ID SR140300001), the Australian Research Council Centre of Excellence for Climate System Science (Project ID B0018492), and the UTas visiting scholar program. J.L. was supported by the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 754433. N.B. was supported by a European Research Council Consolidator Grant (GOCART, agreement number 724416). P.S. was supported by the Australian Research Council Centre of Excellence for Climate Extremes (Project ID CE170100023). P.W.B. was funded by the Australian Research Council by Laureate Fellowship ...