Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning
The231Pa/230Th method is a promising tool to reconstruct Ocean circulation over the past Glacial-Interglacial cycle. However, marine particle flux may constrain the applicability of this ratio as a direct quantitative proxy for the strength of Atlantic Meridional Overturning Circulation (AMOC) by in...
Published in: | Earth and Planetary Science Letters |
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Online Access: | http://hdl.handle.net/1885/72312 https://doi.org/10.1016/j.epsl.2012.04.005 https://openresearch-repository.anu.edu.au/bitstream/1885/72312/5/EarthScavenging.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/72312/7/01_Lippold_Boundary_scavenging_at_the_2012.pdf.jpg |
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ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/72312 2024-01-14T10:08:49+01:00 Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning Lippold, Jorg Mulitza, Stefan Mollenhauer , Gesine Weyer, Stefan Heslop, David Christl, M http://hdl.handle.net/1885/72312 https://doi.org/10.1016/j.epsl.2012.04.005 https://openresearch-repository.anu.edu.au/bitstream/1885/72312/5/EarthScavenging.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/72312/7/01_Lippold_Boundary_scavenging_at_the_2012.pdf.jpg unknown Elsevier 0012-821X http://hdl.handle.net/1885/72312 doi:10.1016/j.epsl.2012.04.005 https://openresearch-repository.anu.edu.au/bitstream/1885/72312/5/EarthScavenging.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/72312/7/01_Lippold_Boundary_scavenging_at_the_2012.pdf.jpg Earth and Planetary Science Letters Keywords: African margin AMOC Boundary scavenging LGM North Atlantic Deep Water Geology Mathematical models Oceanography core analysis glacial-interglacial cycle in situ measurement isotopic composition Last Glacial Maximum meridional circulation ocea 231Pa/ 230Th African margin Journal article ftanucanberra https://doi.org/10.1016/j.epsl.2012.04.005 2023-12-15T09:34:26Z The231Pa/230Th method is a promising tool to reconstruct Ocean circulation over the past Glacial-Interglacial cycle. However, marine particle flux may constrain the applicability of this ratio as a direct quantitative proxy for the strength of Atlantic Meridional Overturning Circulation (AMOC) by influencing the fractionation between the in situ produced231Pa and230Th in ocean water. Here we present231Pa/230Th down-core profiles from high particle flux areas off Namibia and Senegal covering the past ~35ka. The231Pa/230Th profiles at these sites show very different responses to temporal variations of particle fluxes and to changes in water masses. Our results show that sedimentary231Pa/230Th in the Eastern Atlantic margin is linked to particle flux, but controlled primarily by the mode of the AMOC. Our data suggest that during the past ~30ka the high productivity Eastern margin was not capable of importing and storing significant amounts of231Pa from the open Ocean. Consequently, the applicability of the231Pa/230Th proxy to reconstruct past ocean circulation is not hampered by this potentially additional231Pa sink. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Australian National University: ANU Digital Collections Earth and Planetary Science Letters 333-334 317 331 |
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Open Polar |
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Australian National University: ANU Digital Collections |
op_collection_id |
ftanucanberra |
language |
unknown |
topic |
Keywords: African margin AMOC Boundary scavenging LGM North Atlantic Deep Water Geology Mathematical models Oceanography core analysis glacial-interglacial cycle in situ measurement isotopic composition Last Glacial Maximum meridional circulation ocea 231Pa/ 230Th African margin |
spellingShingle |
Keywords: African margin AMOC Boundary scavenging LGM North Atlantic Deep Water Geology Mathematical models Oceanography core analysis glacial-interglacial cycle in situ measurement isotopic composition Last Glacial Maximum meridional circulation ocea 231Pa/ 230Th African margin Lippold, Jorg Mulitza, Stefan Mollenhauer , Gesine Weyer, Stefan Heslop, David Christl, M Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
topic_facet |
Keywords: African margin AMOC Boundary scavenging LGM North Atlantic Deep Water Geology Mathematical models Oceanography core analysis glacial-interglacial cycle in situ measurement isotopic composition Last Glacial Maximum meridional circulation ocea 231Pa/ 230Th African margin |
description |
The231Pa/230Th method is a promising tool to reconstruct Ocean circulation over the past Glacial-Interglacial cycle. However, marine particle flux may constrain the applicability of this ratio as a direct quantitative proxy for the strength of Atlantic Meridional Overturning Circulation (AMOC) by influencing the fractionation between the in situ produced231Pa and230Th in ocean water. Here we present231Pa/230Th down-core profiles from high particle flux areas off Namibia and Senegal covering the past ~35ka. The231Pa/230Th profiles at these sites show very different responses to temporal variations of particle fluxes and to changes in water masses. Our results show that sedimentary231Pa/230Th in the Eastern Atlantic margin is linked to particle flux, but controlled primarily by the mode of the AMOC. Our data suggest that during the past ~30ka the high productivity Eastern margin was not capable of importing and storing significant amounts of231Pa from the open Ocean. Consequently, the applicability of the231Pa/230Th proxy to reconstruct past ocean circulation is not hampered by this potentially additional231Pa sink. |
format |
Article in Journal/Newspaper |
author |
Lippold, Jorg Mulitza, Stefan Mollenhauer , Gesine Weyer, Stefan Heslop, David Christl, M |
author_facet |
Lippold, Jorg Mulitza, Stefan Mollenhauer , Gesine Weyer, Stefan Heslop, David Christl, M |
author_sort |
Lippold, Jorg |
title |
Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
title_short |
Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
title_full |
Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
title_fullStr |
Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
title_full_unstemmed |
Boundary scavenging at the East Atlantic margin does not negate use of Pa-231/Th-230 to trace Atlantic overturning |
title_sort |
boundary scavenging at the east atlantic margin does not negate use of pa-231/th-230 to trace atlantic overturning |
publisher |
Elsevier |
url |
http://hdl.handle.net/1885/72312 https://doi.org/10.1016/j.epsl.2012.04.005 https://openresearch-repository.anu.edu.au/bitstream/1885/72312/5/EarthScavenging.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/72312/7/01_Lippold_Boundary_scavenging_at_the_2012.pdf.jpg |
genre |
North Atlantic Deep Water North Atlantic |
genre_facet |
North Atlantic Deep Water North Atlantic |
op_source |
Earth and Planetary Science Letters |
op_relation |
0012-821X http://hdl.handle.net/1885/72312 doi:10.1016/j.epsl.2012.04.005 https://openresearch-repository.anu.edu.au/bitstream/1885/72312/5/EarthScavenging.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/72312/7/01_Lippold_Boundary_scavenging_at_the_2012.pdf.jpg |
op_doi |
https://doi.org/10.1016/j.epsl.2012.04.005 |
container_title |
Earth and Planetary Science Letters |
container_volume |
333-334 |
container_start_page |
317 |
op_container_end_page |
331 |
_version_ |
1788063222822076416 |