Carbon sequestration in the deep Atlantic enhanced by Saharan dust

Enhanced atmospheric input of dust-borne nutrients and minerals to the remote surface ocean can potentially increase carbon uptake and sequestration at depth. Nutrients can enhance primary productivity, and mineral particles act as ballast, increasing sinking rates of particulate organic matter. Her...

Full description

Bibliographic Details
Published in:Nature Geoscience
Main Authors: Pabortsava, Katsiaryna, Lampitt, Richard S., Benson, Jeff, Crowe, Christian, McLachlan, Robert, Le Moigne, Frederic A. C., Mark Moore, C., Pebody, Corinne, Provost, Paul, Rees, Andrew P., Tilstone, Gavin H., Woodward, E. Malcolm S.
Format: Article in Journal/Newspaper
Language:English
Published: Nature Research 2017
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/37380/
https://oceanrep.geomar.de/id/eprint/37380/1/ngeo2899.pdf
https://oceanrep.geomar.de/id/eprint/37380/2/ngeo2899-s1.pdf
https://doi.org/10.1038/NGEO2899
id ftoceanrep:oai:oceanrep.geomar.de:37380
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:37380 2023-05-15T17:28:33+02:00 Carbon sequestration in the deep Atlantic enhanced by Saharan dust Pabortsava, Katsiaryna Lampitt, Richard S. Benson, Jeff Crowe, Christian McLachlan, Robert Le Moigne, Frederic A. C. Mark Moore, C. Pebody, Corinne Provost, Paul Rees, Andrew P. Tilstone, Gavin H. Woodward, E. Malcolm S. 2017-02-27 text https://oceanrep.geomar.de/id/eprint/37380/ https://oceanrep.geomar.de/id/eprint/37380/1/ngeo2899.pdf https://oceanrep.geomar.de/id/eprint/37380/2/ngeo2899-s1.pdf https://doi.org/10.1038/NGEO2899 en eng Nature Research https://oceanrep.geomar.de/id/eprint/37380/1/ngeo2899.pdf https://oceanrep.geomar.de/id/eprint/37380/2/ngeo2899-s1.pdf Pabortsava, K., Lampitt, R. S., Benson, J., Crowe, C., McLachlan, R., Le Moigne, F. A. C. , Mark Moore, C., Pebody, C., Provost, P., Rees, A. P., Tilstone, G. H. and Woodward, E. M. S. (2017) Carbon sequestration in the deep Atlantic enhanced by Saharan dust. Nature Geoscience, 10 (3). pp. 189-194. DOI 10.1038/NGEO2899 <https://doi.org/10.1038/NGEO2899>. doi:10.1038/NGEO2899 info:eu-repo/semantics/restrictedAccess Article PeerReviewed info:eu-repo/semantics/article 2017 ftoceanrep https://doi.org/10.1038/NGEO2899 2023-04-07T15:32:19Z Enhanced atmospheric input of dust-borne nutrients and minerals to the remote surface ocean can potentially increase carbon uptake and sequestration at depth. Nutrients can enhance primary productivity, and mineral particles act as ballast, increasing sinking rates of particulate organic matter. Here we present a two-year time series of sediment trap observations of particulate organic carbon flux to 3,000 m depth, measured directly in two locations: the dust-rich central North Atlantic gyre and the dust-poor South Atlantic gyre. We find that carbon fluxes are twice as high and a higher proportion of primary production is exported to depth in the dust-rich North Atlantic gyre. Low stable nitrogen isotope ratios suggest that high fluxes result from the stimulation of nitrogen fixation and productivity following the deposition of dust-borne nutrients. Sediment traps in the northern gyre also collected intact colonies of nitrogen-fixing Trichodesmium species. Whereas ballast in the southern gyre is predominantly biogenic, dust-derived mineral particles constitute the dominant ballast element during the enhanced carbon fluxes in the northern gyre. We conclude that dust deposition increases carbon sequestration in the North Atlantic gyre through the fertilization of the nitrogen-fixing community in surface waters and mineral ballasting of sinking particles Article in Journal/Newspaper North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Nature Geoscience 10 3 189 194
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description Enhanced atmospheric input of dust-borne nutrients and minerals to the remote surface ocean can potentially increase carbon uptake and sequestration at depth. Nutrients can enhance primary productivity, and mineral particles act as ballast, increasing sinking rates of particulate organic matter. Here we present a two-year time series of sediment trap observations of particulate organic carbon flux to 3,000 m depth, measured directly in two locations: the dust-rich central North Atlantic gyre and the dust-poor South Atlantic gyre. We find that carbon fluxes are twice as high and a higher proportion of primary production is exported to depth in the dust-rich North Atlantic gyre. Low stable nitrogen isotope ratios suggest that high fluxes result from the stimulation of nitrogen fixation and productivity following the deposition of dust-borne nutrients. Sediment traps in the northern gyre also collected intact colonies of nitrogen-fixing Trichodesmium species. Whereas ballast in the southern gyre is predominantly biogenic, dust-derived mineral particles constitute the dominant ballast element during the enhanced carbon fluxes in the northern gyre. We conclude that dust deposition increases carbon sequestration in the North Atlantic gyre through the fertilization of the nitrogen-fixing community in surface waters and mineral ballasting of sinking particles
format Article in Journal/Newspaper
author Pabortsava, Katsiaryna
Lampitt, Richard S.
Benson, Jeff
Crowe, Christian
McLachlan, Robert
Le Moigne, Frederic A. C.
Mark Moore, C.
Pebody, Corinne
Provost, Paul
Rees, Andrew P.
Tilstone, Gavin H.
Woodward, E. Malcolm S.
spellingShingle Pabortsava, Katsiaryna
Lampitt, Richard S.
Benson, Jeff
Crowe, Christian
McLachlan, Robert
Le Moigne, Frederic A. C.
Mark Moore, C.
Pebody, Corinne
Provost, Paul
Rees, Andrew P.
Tilstone, Gavin H.
Woodward, E. Malcolm S.
Carbon sequestration in the deep Atlantic enhanced by Saharan dust
author_facet Pabortsava, Katsiaryna
Lampitt, Richard S.
Benson, Jeff
Crowe, Christian
McLachlan, Robert
Le Moigne, Frederic A. C.
Mark Moore, C.
Pebody, Corinne
Provost, Paul
Rees, Andrew P.
Tilstone, Gavin H.
Woodward, E. Malcolm S.
author_sort Pabortsava, Katsiaryna
title Carbon sequestration in the deep Atlantic enhanced by Saharan dust
title_short Carbon sequestration in the deep Atlantic enhanced by Saharan dust
title_full Carbon sequestration in the deep Atlantic enhanced by Saharan dust
title_fullStr Carbon sequestration in the deep Atlantic enhanced by Saharan dust
title_full_unstemmed Carbon sequestration in the deep Atlantic enhanced by Saharan dust
title_sort carbon sequestration in the deep atlantic enhanced by saharan dust
publisher Nature Research
publishDate 2017
url https://oceanrep.geomar.de/id/eprint/37380/
https://oceanrep.geomar.de/id/eprint/37380/1/ngeo2899.pdf
https://oceanrep.geomar.de/id/eprint/37380/2/ngeo2899-s1.pdf
https://doi.org/10.1038/NGEO2899
genre North Atlantic
genre_facet North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/37380/1/ngeo2899.pdf
https://oceanrep.geomar.de/id/eprint/37380/2/ngeo2899-s1.pdf
Pabortsava, K., Lampitt, R. S., Benson, J., Crowe, C., McLachlan, R., Le Moigne, F. A. C. , Mark Moore, C., Pebody, C., Provost, P., Rees, A. P., Tilstone, G. H. and Woodward, E. M. S. (2017) Carbon sequestration in the deep Atlantic enhanced by Saharan dust. Nature Geoscience, 10 (3). pp. 189-194. DOI 10.1038/NGEO2899 <https://doi.org/10.1038/NGEO2899>.
doi:10.1038/NGEO2899
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1038/NGEO2899
container_title Nature Geoscience
container_volume 10
container_issue 3
container_start_page 189
op_container_end_page 194
_version_ 1766121277050847232