Where is mineral ballast important for surface export of particulate organic carbon in the ocean?
Correlations between particulate organic carbon (POC) and mineral fluxes in the deep ocean have inspired the inclusion of ‘ballast effect’ parameterizations in carbon cycle models. A recent study demonstrated regional variability in the effect of ballast minerals on the flux of POC in the deep ocean...
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ftsouthampton:oai:eprints.soton.ac.uk:370462 2023-08-27T04:07:56+02:00 Where is mineral ballast important for surface export of particulate organic carbon in the ocean? Le Moigne, Frédéric A.C. Pabortsava, Katsiaryna Marcinko, Charlotte L.J. Martin, Patrick Sanders, Richard J. 2014-12-16 text https://eprints.soton.ac.uk/370462/ https://eprints.soton.ac.uk/370462/1/Moigne_et_al-2014-Geophysical_Research_Letters.pdf en English eng https://eprints.soton.ac.uk/370462/1/Moigne_et_al-2014-Geophysical_Research_Letters.pdf Le Moigne, Frédéric A.C., Pabortsava, Katsiaryna, Marcinko, Charlotte L.J., Martin, Patrick and Sanders, Richard J. (2014) Where is mineral ballast important for surface export of particulate organic carbon in the ocean? Geophysical Research Letters, 41 (23), 8460-8468. (doi:10.1002/2014GL061678 <http://dx.doi.org/10.1002/2014GL061678>). cc_by_4 Article PeerReviewed 2014 ftsouthampton 2023-08-03T22:20:49Z Correlations between particulate organic carbon (POC) and mineral fluxes in the deep ocean have inspired the inclusion of ‘ballast effect’ parameterizations in carbon cycle models. A recent study demonstrated regional variability in the effect of ballast minerals on the flux of POC in the deep ocean. We have undertaken a similar analysis of shallow export data from the Arctic, Atlantic and Southern Oceans. Mineral ballasting is of greatest importance in the high-latitude North Atlantic, where 60% of the POC flux is associated with ballast minerals. This fraction drops to around 40% in the Southern Ocean. The remainder of the export flux is not associated with minerals, and this unballasted fraction thus often dominates the export flux. The proportion of mineral-associated POC flux often scales with regional variation in export efficiency (the proportion of primary production that is exported). However, local discrepancies suggest that regional differences in ecology also impact the magnitude of surface export. We propose that POC export will not respond equally across all high-latitude regions to possible future changes in ballast availability. Article in Journal/Newspaper Arctic North Atlantic Southern Ocean University of Southampton: e-Prints Soton Arctic Southern Ocean |
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University of Southampton: e-Prints Soton |
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ftsouthampton |
language |
English |
description |
Correlations between particulate organic carbon (POC) and mineral fluxes in the deep ocean have inspired the inclusion of ‘ballast effect’ parameterizations in carbon cycle models. A recent study demonstrated regional variability in the effect of ballast minerals on the flux of POC in the deep ocean. We have undertaken a similar analysis of shallow export data from the Arctic, Atlantic and Southern Oceans. Mineral ballasting is of greatest importance in the high-latitude North Atlantic, where 60% of the POC flux is associated with ballast minerals. This fraction drops to around 40% in the Southern Ocean. The remainder of the export flux is not associated with minerals, and this unballasted fraction thus often dominates the export flux. The proportion of mineral-associated POC flux often scales with regional variation in export efficiency (the proportion of primary production that is exported). However, local discrepancies suggest that regional differences in ecology also impact the magnitude of surface export. We propose that POC export will not respond equally across all high-latitude regions to possible future changes in ballast availability. |
format |
Article in Journal/Newspaper |
author |
Le Moigne, Frédéric A.C. Pabortsava, Katsiaryna Marcinko, Charlotte L.J. Martin, Patrick Sanders, Richard J. |
spellingShingle |
Le Moigne, Frédéric A.C. Pabortsava, Katsiaryna Marcinko, Charlotte L.J. Martin, Patrick Sanders, Richard J. Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
author_facet |
Le Moigne, Frédéric A.C. Pabortsava, Katsiaryna Marcinko, Charlotte L.J. Martin, Patrick Sanders, Richard J. |
author_sort |
Le Moigne, Frédéric A.C. |
title |
Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
title_short |
Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
title_full |
Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
title_fullStr |
Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
title_full_unstemmed |
Where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
title_sort |
where is mineral ballast important for surface export of particulate organic carbon in the ocean? |
publishDate |
2014 |
url |
https://eprints.soton.ac.uk/370462/ https://eprints.soton.ac.uk/370462/1/Moigne_et_al-2014-Geophysical_Research_Letters.pdf |
geographic |
Arctic Southern Ocean |
geographic_facet |
Arctic Southern Ocean |
genre |
Arctic North Atlantic Southern Ocean |
genre_facet |
Arctic North Atlantic Southern Ocean |
op_relation |
https://eprints.soton.ac.uk/370462/1/Moigne_et_al-2014-Geophysical_Research_Letters.pdf Le Moigne, Frédéric A.C., Pabortsava, Katsiaryna, Marcinko, Charlotte L.J., Martin, Patrick and Sanders, Richard J. (2014) Where is mineral ballast important for surface export of particulate organic carbon in the ocean? Geophysical Research Letters, 41 (23), 8460-8468. (doi:10.1002/2014GL061678 <http://dx.doi.org/10.1002/2014GL061678>). |
op_rights |
cc_by_4 |
_version_ |
1775348650204987392 |