Ocean margins as a significant source of organic matter to the deep open ocean
Continental shelves and slopes comprise less than 20% of the world ocean area, yet they are proposed to be quantitatively important sources of the organic matter that fuels respiration in the open ocean's interior. At least certain regions of the coastal ocean produce more organic carbon than t...
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Language: | English |
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1998
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ftcdlib:qt1mr5v83n 2023-05-15T17:30:55+02:00 Ocean margins as a significant source of organic matter to the deep open ocean Bauer, JE Druffel, ERM 482 - 485 1998-04-02 application/pdf http://www.escholarship.org/uc/item/1mr5v83n english eng eScholarship, University of California qt1mr5v83n http://www.escholarship.org/uc/item/1mr5v83n Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Bauer, JE; & Druffel, ERM. (1998). Ocean margins as a significant source of organic matter to the deep open ocean. Nature, 392(6675), 482 - 485. doi:10.1038/33122. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/1mr5v83n article 1998 ftcdlib https://doi.org/10.1038/33122 2018-06-29T22:51:20Z Continental shelves and slopes comprise less than 20% of the world ocean area, yet they are proposed to be quantitatively important sources of the organic matter that fuels respiration in the open ocean's interior. At least certain regions of the coastal ocean produce more organic carbon than they respire, suggesting that some fraction of this non-respired, unburied organic carbon is available for export from the coastal to the open ocean. Previous studies of carbon fluxes in ocean margins have not considered the potential roles of dissolved organic carbon (DOC) and suspended particulate organic carbon (POC(susp)), even though both pools are quantitatively far larger than sinking POC. Here we report natural radiocarbon (14C) abundance measurements that reveal continental slope and rise waters to contain both DOC and POC(susp) that are concurrently older and in higher concentrations than DOC and POC(susp) from the adjacent North Atlantic and North Pacific central gyres. Mass-balance calculations suggest that DOC and POC(susp) inputs from ocean margins to the open ocean interior may be more than an order of magnitude greater than inputs of recently produced organic carbon derived from the surface ocean. Inputs from ocean margins may thus be one of the factors contributing to the old apparent age of organic carbon observed in the deep North Atlantic and Pacific central gyres. Article in Journal/Newspaper North Atlantic University of California: eScholarship Pacific Nature 392 6675 482 485 |
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Open Polar |
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University of California: eScholarship |
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ftcdlib |
language |
English |
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Continental shelves and slopes comprise less than 20% of the world ocean area, yet they are proposed to be quantitatively important sources of the organic matter that fuels respiration in the open ocean's interior. At least certain regions of the coastal ocean produce more organic carbon than they respire, suggesting that some fraction of this non-respired, unburied organic carbon is available for export from the coastal to the open ocean. Previous studies of carbon fluxes in ocean margins have not considered the potential roles of dissolved organic carbon (DOC) and suspended particulate organic carbon (POC(susp)), even though both pools are quantitatively far larger than sinking POC. Here we report natural radiocarbon (14C) abundance measurements that reveal continental slope and rise waters to contain both DOC and POC(susp) that are concurrently older and in higher concentrations than DOC and POC(susp) from the adjacent North Atlantic and North Pacific central gyres. Mass-balance calculations suggest that DOC and POC(susp) inputs from ocean margins to the open ocean interior may be more than an order of magnitude greater than inputs of recently produced organic carbon derived from the surface ocean. Inputs from ocean margins may thus be one of the factors contributing to the old apparent age of organic carbon observed in the deep North Atlantic and Pacific central gyres. |
format |
Article in Journal/Newspaper |
author |
Bauer, JE Druffel, ERM |
spellingShingle |
Bauer, JE Druffel, ERM Ocean margins as a significant source of organic matter to the deep open ocean |
author_facet |
Bauer, JE Druffel, ERM |
author_sort |
Bauer, JE |
title |
Ocean margins as a significant source of organic matter to the deep open ocean |
title_short |
Ocean margins as a significant source of organic matter to the deep open ocean |
title_full |
Ocean margins as a significant source of organic matter to the deep open ocean |
title_fullStr |
Ocean margins as a significant source of organic matter to the deep open ocean |
title_full_unstemmed |
Ocean margins as a significant source of organic matter to the deep open ocean |
title_sort |
ocean margins as a significant source of organic matter to the deep open ocean |
publisher |
eScholarship, University of California |
publishDate |
1998 |
url |
http://www.escholarship.org/uc/item/1mr5v83n |
op_coverage |
482 - 485 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Bauer, JE; & Druffel, ERM. (1998). Ocean margins as a significant source of organic matter to the deep open ocean. Nature, 392(6675), 482 - 485. doi:10.1038/33122. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/1mr5v83n |
op_relation |
qt1mr5v83n http://www.escholarship.org/uc/item/1mr5v83n |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/33122 |
container_title |
Nature |
container_volume |
392 |
container_issue |
6675 |
container_start_page |
482 |
op_container_end_page |
485 |
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1766128062406066176 |