Biogenic carbon pool production maintains the Southern Ocean carbon sink

Through biological activity, marine dissolved inorganic carbon (DIC) is transformed into different types of biogenic carbon available for export to the ocean interior, including particulate organic carbon (POC), dissolved organic carbon (DOC), and particulate inorganic carbon (PIC). Each biogenic ca...

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Bibliographic Details
Published in:Proceedings of the National Academy of Sciences
Main Authors: Huang, Yibin, Fassbender, Andrea J., Bushinsky, Seth M.
Format: Text
Language:English
Published: National Academy of Sciences 2023
Subjects:
Physical Sciences
Antarc*
Antarctic
Sea ice
Southern Ocean
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10160987/
http://www.ncbi.nlm.nih.gov/pubmed/37099629
https://doi.org/10.1073/pnas.2217909120
Description
Summary:Through biological activity, marine dissolved inorganic carbon (DIC) is transformed into different types of biogenic carbon available for export to the ocean interior, including particulate organic carbon (POC), dissolved organic carbon (DOC), and particulate inorganic carbon (PIC). Each biogenic carbon pool has a different export efficiency that impacts the vertical ocean carbon gradient and drives natural air–sea carbon dioxide gas (CO(2)) exchange. In the Southern Ocean (SO), which presently accounts for ~40% of the anthropogenic ocean carbon sink, it is unclear how the production of each biogenic carbon pool contributes to the contemporary air–sea CO(2) exchange. Based on 107 independent observations of the seasonal cycle from 63 biogeochemical profiling floats, we provide the basin-scale estimate of distinct biogenic carbon pool production. We find significant meridional variability with enhanced POC production in the subantarctic and polar Antarctic sectors and enhanced DOC production in the subtropical and sea-ice-dominated sectors. PIC production peaks between 47°S and 57°S near the “great calcite belt.” Relative to an abiotic SO, organic carbon production enhances CO(2) uptake by 2.80 ± 0.28 Pg C y(−)(1), while PIC production diminishes CO(2) uptake by 0.27 ± 0.21 Pg C y(−)(1). Without organic carbon production, the SO would be a CO(2) source to the atmosphere. Our findings emphasize the importance of DOC and PIC production, in addition to the well-recognized role of POC production, in shaping the influence of carbon export on air–sea CO(2) exchange.

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