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Large carbon export, but short residence times, of transparent exopolymer particles in the global ocean

Authors :
Reche, Isabel
Peralta-Maraver, Ignacio
Ortega-Retuerta, E.
Mazuecos, Ignacio P.
Catalá, Teresa S.
Forn, Irene
Picazo, Félix
Marañón, Emilio
Cermeño, Pedro
González, Natalia
Sobrino, Cristina
Fernández, Ana
Huete-Ortega, María
López-Sandoval, Daffne
Vidal, Montserrat
Morán, Xosé Anxelu G.
Álvarez-Salgado, Xosé Antón
Agustí, Susana
Duarte, Carlos M.
Gasol, Josep M.
Arístegui, Javier
Reche, Isabel
Peralta-Maraver, Ignacio
Ortega-Retuerta, E.
Mazuecos, Ignacio P.
Catalá, Teresa S.
Forn, Irene
Picazo, Félix
Marañón, Emilio
Cermeño, Pedro
González, Natalia
Sobrino, Cristina
Fernández, Ana
Huete-Ortega, María
López-Sandoval, Daffne
Vidal, Montserrat
Morán, Xosé Anxelu G.
Álvarez-Salgado, Xosé Antón
Agustí, Susana
Duarte, Carlos M.
Gasol, Josep M.
Arístegui, Javier
Publication Year :
2023

Abstract

Acidic polysaccharides released by phytoplankton and prokaryotic heterotrophs promote the formation of gel-like transparent exopolymer particles (TEPs). TEPs can have a relevant contribution to the biological carbon pump due to their carbon-rich composition and their ability to coagulate and sink towards the deep ocean. However, little is known about TEPs distribution, carbon export, and residence times below the export (200 m) and sequestration (1000 m) depths. We provide the first comprehensive inventory of TEP from the ocean surface to a depth of 4000 meters in the tropical and subtropical Atlantic, Indian, and Pacific Oceans, evaluating its contribution to carbon export and sequestration into the deep ocean. Results indicate that TEP concentration is primarily determined by primary production, with higher concentrations located above the deep chlorophyll maxima. In the deep ocean, TEP concentrations are lower yet mirror the concentrations in the surface, demonstrating the significance of TEP sinking below both the export compartment (2.8 Pg C yr-1; 27% of total POC flux at 200 m) and the sequestration compartment (0.8 Pg C yr-1; 36% of total POC flux at 1000 m). In situ incubation experiments conducted across ocean basins indicate short TEP residence times, averaging 27 and 333 days in the export and sequestration compartments, respectively. These findings reveal that the export and subsequent sequestration of carbon by TEP sinking into the deep ocean diverts it from the long times observed for the dissolved carbon fraction (i.e. centuries) in the global carbon cycle

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1431959541
Document Type :
Electronic Resource