The Biological Carbon Pump in the North Atlantic

Mediated principally by the sinking of organic rich particles from the upper ocean, the Biological Carbon Pump (BCP) is a significant component of the global carbon cycle. It transfers roughly 11 Gt C yr?1 into the ocean’s interior and maintains atmospheric carbon dioxide at significantly lower leve...

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Published in:Progress in Oceanography
Main Authors: Sanders, Richard, Henson, Stephanie A., Koski, Marja, De la Rocha, Christina L., Painter, Stuart C., Poulton, Alex J., Riley, Jennifer, Salihoglu, Baris, Visser, Andre, Yool, Andrew, Bellerby, Richard, Martin, Adrian
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://eprints.soton.ac.uk/364390/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:364390 2023-07-30T04:05:09+02:00 The Biological Carbon Pump in the North Atlantic Sanders, Richard Henson, Stephanie A. Koski, Marja De la Rocha, Christina L. Painter, Stuart C. Poulton, Alex J. Riley, Jennifer Salihoglu, Baris Visser, Andre Yool, Andrew Bellerby, Richard Martin, Adrian 2014-12 https://eprints.soton.ac.uk/364390/ English eng Sanders, Richard, Henson, Stephanie A., Koski, Marja, De la Rocha, Christina L., Painter, Stuart C., Poulton, Alex J., Riley, Jennifer, Salihoglu, Baris, Visser, Andre, Yool, Andrew, Bellerby, Richard and Martin, Adrian (2014) The Biological Carbon Pump in the North Atlantic. Progress in Oceanography, 129 (B), 200-218. (doi:10.1016/j.pocean.2014.05.005 <http://dx.doi.org/10.1016/j.pocean.2014.05.005>). Article PeerReviewed 2014 ftsouthampton https://doi.org/10.1016/j.pocean.2014.05.005 2023-07-09T21:52:36Z Mediated principally by the sinking of organic rich particles from the upper ocean, the Biological Carbon Pump (BCP) is a significant component of the global carbon cycle. It transfers roughly 11 Gt C yr?1 into the ocean’s interior and maintains atmospheric carbon dioxide at significantly lower levels than would be the case if it did not exist. More specifically, export by the BCP in the North Atlantic is ?0.55–1.94 Gt C yr?1. A rich set of observations suggests that a complex set of processes drives this export. However, significant uncertainties exist regarding the BCP in the North Atlantic, including both the magnitude of the downward flux and the ecological, chemical and physical processes by which it is sustained and controlled. Our lack of detailed mechanistic understanding has also hindered modelling attempts to quantify and predict changes to the BCP. In this paper, we assess current knowledge concerning the BCP in the North Atlantic in order to identify priorities for future research, as well as suggesting how they might be addressed. Article in Journal/Newspaper North Atlantic University of Southampton: e-Prints Soton Progress in Oceanography 129 200 218
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Mediated principally by the sinking of organic rich particles from the upper ocean, the Biological Carbon Pump (BCP) is a significant component of the global carbon cycle. It transfers roughly 11 Gt C yr?1 into the ocean’s interior and maintains atmospheric carbon dioxide at significantly lower levels than would be the case if it did not exist. More specifically, export by the BCP in the North Atlantic is ?0.55–1.94 Gt C yr?1. A rich set of observations suggests that a complex set of processes drives this export. However, significant uncertainties exist regarding the BCP in the North Atlantic, including both the magnitude of the downward flux and the ecological, chemical and physical processes by which it is sustained and controlled. Our lack of detailed mechanistic understanding has also hindered modelling attempts to quantify and predict changes to the BCP. In this paper, we assess current knowledge concerning the BCP in the North Atlantic in order to identify priorities for future research, as well as suggesting how they might be addressed.
format Article in Journal/Newspaper
author Sanders, Richard
Henson, Stephanie A.
Koski, Marja
De la Rocha, Christina L.
Painter, Stuart C.
Poulton, Alex J.
Riley, Jennifer
Salihoglu, Baris
Visser, Andre
Yool, Andrew
Bellerby, Richard
Martin, Adrian
spellingShingle Sanders, Richard
Henson, Stephanie A.
Koski, Marja
De la Rocha, Christina L.
Painter, Stuart C.
Poulton, Alex J.
Riley, Jennifer
Salihoglu, Baris
Visser, Andre
Yool, Andrew
Bellerby, Richard
Martin, Adrian
The Biological Carbon Pump in the North Atlantic
author_facet Sanders, Richard
Henson, Stephanie A.
Koski, Marja
De la Rocha, Christina L.
Painter, Stuart C.
Poulton, Alex J.
Riley, Jennifer
Salihoglu, Baris
Visser, Andre
Yool, Andrew
Bellerby, Richard
Martin, Adrian
author_sort Sanders, Richard
title The Biological Carbon Pump in the North Atlantic
title_short The Biological Carbon Pump in the North Atlantic
title_full The Biological Carbon Pump in the North Atlantic
title_fullStr The Biological Carbon Pump in the North Atlantic
title_full_unstemmed The Biological Carbon Pump in the North Atlantic
title_sort biological carbon pump in the north atlantic
publishDate 2014
url https://eprints.soton.ac.uk/364390/
genre North Atlantic
genre_facet North Atlantic
op_relation Sanders, Richard, Henson, Stephanie A., Koski, Marja, De la Rocha, Christina L., Painter, Stuart C., Poulton, Alex J., Riley, Jennifer, Salihoglu, Baris, Visser, Andre, Yool, Andrew, Bellerby, Richard and Martin, Adrian (2014) The Biological Carbon Pump in the North Atlantic. Progress in Oceanography, 129 (B), 200-218. (doi:10.1016/j.pocean.2014.05.005 <http://dx.doi.org/10.1016/j.pocean.2014.05.005>).
op_doi https://doi.org/10.1016/j.pocean.2014.05.005
container_title Progress in Oceanography
container_volume 129
container_start_page 200
op_container_end_page 218
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