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...

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Published in:Earth and Planetary Science Letters
Main Authors: Lippold, Jorg, Mulitza, Stefan, Mollenhauer , Gesine, Weyer, Stefan, Heslop, David, Christl, M
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
LGM
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
id ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/72312
record_format openpolar
spelling 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
institution Open Polar
collection 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
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