Oceanic efflux of ancient marine dissolved organic carbon in primary marine aerosol

Breaking waves produce bubble plumes that burst at the sea surface, injecting primary marine aerosol (PMA) highly enriched with marine organic carbon (OC) into the atmosphere. It is widely assumed that this OC is modern, produced by present-day biological activity, even though nearly all marine OC i...

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Detalles Bibliográficos
Autores principales: Beaupré, Steven R., Kieber, David J., Keene, William C., Long, Michael S., Maben, John R., Lu, Xi, Zhu, Yuting, Frossard, Amanda A., Kinsey, Joanna D., Duplessis, Patrick, Chang, Rachel Y.-W., Bisgrove, John
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6810255/
https://www.ncbi.nlm.nih.gov/pubmed/31681848
http://dx.doi.org/10.1126/sciadv.aax6535
Descripción
Sumario:Breaking waves produce bubble plumes that burst at the sea surface, injecting primary marine aerosol (PMA) highly enriched with marine organic carbon (OC) into the atmosphere. It is widely assumed that this OC is modern, produced by present-day biological activity, even though nearly all marine OC is thousands of years old, produced by biological activity long ago. We used natural abundance radiocarbon ((14)C) measurements to show that 19 to 40% of the OC associated with freshly produced PMA was refractory dissolved OC (RDOC). Globally, this process removes 2 to 20 Tg of RDOC from the oceans annually, comparable to other RDOC losses. This process represents a major removal pathway for old OC from the sea, with important implications for oceanic and atmospheric biogeochemistry, the global carbon cycle, and climate.

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