High particle export over the continental shelf of the west Antarctic Peninsula

[1] Drifting cylindrical traps and the flux proxy 234 Th indicate more than an order of magnitude higher sinking fluxes of particulate carbon and 234 Th in January 2009 than measured by a time-series conical trap used regularly on the shelf of the west Antarctic Peninsula (WAP). The higher fluxes me...

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Main Authors: Ken O Buesseler, Andrew M P Mcdonnell, Oscar M E Schofield, Deborah K Steinberg, Hugh W Ducklow, K O Buesseler, A M P Mcdonnell, O M E Schofield, D K Steinberg, H W Ducklow
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2010
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.391
http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1046.391 2023-05-15T13:46:19+02:00 High particle export over the continental shelf of the west Antarctic Peninsula Ken O Buesseler Andrew M P Mcdonnell Oscar M E Schofield Deborah K Steinberg Hugh W Ducklow K O Buesseler A M P Mcdonnell O M E Schofield D K Steinberg H W Ducklow The Pennsylvania State University CiteSeerX Archives 2010 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.391 http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.391 http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf text 2010 ftciteseerx 2020-04-05T00:19:26Z [1] Drifting cylindrical traps and the flux proxy 234 Th indicate more than an order of magnitude higher sinking fluxes of particulate carbon and 234 Th in January 2009 than measured by a time-series conical trap used regularly on the shelf of the west Antarctic Peninsula (WAP). The higher fluxes measured in this study have several implications for our understanding of the WAP ecosystem. Larger sinking fluxes result in a revised export efficiency of at least 10% (C flux/net primary production) and a requisite lower regeneration efficiency in surface waters. High fluxes also result in a large supply of sinking organic matter to support subsurface and benthic food webs on the continental shelf. These new findings call into question the magnitude of seasonal and interannual variability in particle flux and reaffirm the difficulty of using moored conical traps as a quantitative flux collector in shallow waters. Citation: Text Antarc* Antarctic Antarctic Peninsula Unknown Antarctic Antarctic Peninsula
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description [1] Drifting cylindrical traps and the flux proxy 234 Th indicate more than an order of magnitude higher sinking fluxes of particulate carbon and 234 Th in January 2009 than measured by a time-series conical trap used regularly on the shelf of the west Antarctic Peninsula (WAP). The higher fluxes measured in this study have several implications for our understanding of the WAP ecosystem. Larger sinking fluxes result in a revised export efficiency of at least 10% (C flux/net primary production) and a requisite lower regeneration efficiency in surface waters. High fluxes also result in a large supply of sinking organic matter to support subsurface and benthic food webs on the continental shelf. These new findings call into question the magnitude of seasonal and interannual variability in particle flux and reaffirm the difficulty of using moored conical traps as a quantitative flux collector in shallow waters. Citation:
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ken O Buesseler
Andrew M P Mcdonnell
Oscar M E Schofield
Deborah K Steinberg
Hugh W Ducklow
K O Buesseler
A M P Mcdonnell
O M E Schofield
D K Steinberg
H W Ducklow
spellingShingle Ken O Buesseler
Andrew M P Mcdonnell
Oscar M E Schofield
Deborah K Steinberg
Hugh W Ducklow
K O Buesseler
A M P Mcdonnell
O M E Schofield
D K Steinberg
H W Ducklow
High particle export over the continental shelf of the west Antarctic Peninsula
author_facet Ken O Buesseler
Andrew M P Mcdonnell
Oscar M E Schofield
Deborah K Steinberg
Hugh W Ducklow
K O Buesseler
A M P Mcdonnell
O M E Schofield
D K Steinberg
H W Ducklow
author_sort Ken O Buesseler
title High particle export over the continental shelf of the west Antarctic Peninsula
title_short High particle export over the continental shelf of the west Antarctic Peninsula
title_full High particle export over the continental shelf of the west Antarctic Peninsula
title_fullStr High particle export over the continental shelf of the west Antarctic Peninsula
title_full_unstemmed High particle export over the continental shelf of the west Antarctic Peninsula
title_sort high particle export over the continental shelf of the west antarctic peninsula
publishDate 2010
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.391
http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf
geographic Antarctic
Antarctic Peninsula
geographic_facet Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
genre_facet Antarc*
Antarctic
Antarctic Peninsula
op_source http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1046.391
http://cafethorium.whoi.edu/website/publications/Buesseler%20et%20al%20High%20particle%20export%20over%20WAP%20GRL%20v37%20L22606%202010.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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