Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic
This work aims to reconstruct the evolution of deep ocean circulation patterns in the North Atlantic during the last 10-100 kyr using abiotic proxies. Nd and Pb isotopic ratios have been measured on the clay-sized fraction of two sediment cores drilled in the Labrador Sea off southern Greenland (MD9...
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ftvliz:oai:oma.vliz.be:239361 2023-05-15T14:24:19+02:00 Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic Fagel, N. 2009 http://www.vliz.be/nl/open-marien-archief?module=ref&refid=239361 en eng info:eu-repo/semantics/altIdentifier/wos/000264132700009 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1007/978-1-4020-9460-6_9 http://www.vliz.be/nl/open-marien-archief?module=ref&refid=239361 info:eu-repo/semantics/restrictedAccess ,+%3Cb%3E%3Ci%3Ein%3C%2Fi%3E%3C%2Fb%3E%3A+Nihoul,+J.C.J.+%3Ci%3Eet+al.%3C%2Fi%3E+%3Ci%3EInfluence+of+climate+change+on+the+changing+Arctic+and+Sub-Arctic+conditions.+Proceedings+of+the+NATO+Advanced+Research+Workshop+on+Influence+of+Climate+Change+on+the+Changing+Arctic,+Li%C3%A8ge,+Belgium,+8-10+May+2008.+NATO+Science+for+Peace+and+Security+Series%3A+C.+Environmental+Security,%3C%2Fi%3E+%3A+pp.+109-123.+%3Ca+href%3D%22https%3A%2F%2Fdx.doi.org%2F10.1007%2F978-1-4020-9460-6_9%22+target%3D%22_blank%22%3Ehttps%3A%2F%2Fdx.doi.org%2F10.1007%2F978-1-4020-9460-6_9%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2009 ftvliz https://doi.org/10.1007/978-1-4020-9460-6_9 2022-05-01T10:17:52Z This work aims to reconstruct the evolution of deep ocean circulation patterns in the North Atlantic during the last 10-100 kyr using abiotic proxies. Nd and Pb isotopic ratios have been measured on the clay-sized fraction of two sediment cores drilled in the Labrador Sea off southern Greenland (MD99-2227, ODP646). At present this site is under the influence of the Western Boundary Undercurrent that drives the water masses involved in the fort-nation of the North Atlantic Deep Water. Based on an identification of regional sources areas sedimentary isotopic signatures allow to determine the origin of the particles driven by the North Atlantic deep Currents: any change in the sediment supplies reflects a relative change in the contribution of the deep water masses. Our isotopic dataset emphasizes several main changes in the relative contribution of the two major components of North Atlantic Deep Water, i.e. the North East Atlantic Deep water (NEADW) and the Denmark Strait Overflow Water (DSOW) throughout the last 12 kyr, and especially during the Late Holocene. The inception of the modem deep circulation seems to be quite recent, occurring during the last 3 kyr. Over glacial/interglacial time-scale deep current variability is less pronounced and/or partly masked by variable proximal supplies. Labrador Sea results emphasize that the application of mineralogical and isotopical tools on sediments allow to monitor variability in sedimentary supplies driven by deep currents. This indirect approach is further promising to identify deep currents pathways and reconstruct past circulation. Article in Journal/Newspaper Arctic Arctic Denmark Strait Greenland Labrador Sea North Atlantic Deep Water North Atlantic North East Atlantic Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) Arctic Greenland 109 123 Dordrecht |
institution |
Open Polar |
collection |
Flanders Marine Institute (VLIZ): Open Marine Archive (OMA) |
op_collection_id |
ftvliz |
language |
English |
description |
This work aims to reconstruct the evolution of deep ocean circulation patterns in the North Atlantic during the last 10-100 kyr using abiotic proxies. Nd and Pb isotopic ratios have been measured on the clay-sized fraction of two sediment cores drilled in the Labrador Sea off southern Greenland (MD99-2227, ODP646). At present this site is under the influence of the Western Boundary Undercurrent that drives the water masses involved in the fort-nation of the North Atlantic Deep Water. Based on an identification of regional sources areas sedimentary isotopic signatures allow to determine the origin of the particles driven by the North Atlantic deep Currents: any change in the sediment supplies reflects a relative change in the contribution of the deep water masses. Our isotopic dataset emphasizes several main changes in the relative contribution of the two major components of North Atlantic Deep Water, i.e. the North East Atlantic Deep water (NEADW) and the Denmark Strait Overflow Water (DSOW) throughout the last 12 kyr, and especially during the Late Holocene. The inception of the modem deep circulation seems to be quite recent, occurring during the last 3 kyr. Over glacial/interglacial time-scale deep current variability is less pronounced and/or partly masked by variable proximal supplies. Labrador Sea results emphasize that the application of mineralogical and isotopical tools on sediments allow to monitor variability in sedimentary supplies driven by deep currents. This indirect approach is further promising to identify deep currents pathways and reconstruct past circulation. |
format |
Article in Journal/Newspaper |
author |
Fagel, N. |
spellingShingle |
Fagel, N. Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
author_facet |
Fagel, N. |
author_sort |
Fagel, N. |
title |
Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
title_short |
Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
title_full |
Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
title_fullStr |
Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
title_full_unstemmed |
Reconstruction of oceanic circulation using mineralogical and isotopical (Nd/Pb) signatures of deep sea sediments: the case study of the northern North Atlantic and some perspectives for the Arctic |
title_sort |
reconstruction of oceanic circulation using mineralogical and isotopical (nd/pb) signatures of deep sea sediments: the case study of the northern north atlantic and some perspectives for the arctic |
publishDate |
2009 |
url |
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=239361 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Arctic Denmark Strait Greenland Labrador Sea North Atlantic Deep Water North Atlantic North East Atlantic |
genre_facet |
Arctic Arctic Denmark Strait Greenland Labrador Sea North Atlantic Deep Water North Atlantic North East Atlantic |
op_source |
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op_relation |
info:eu-repo/semantics/altIdentifier/wos/000264132700009 info:eu-repo/semantics/altIdentifier/doi/doi.org/10.1007/978-1-4020-9460-6_9 http://www.vliz.be/nl/open-marien-archief?module=ref&refid=239361 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1007/978-1-4020-9460-6_9 |
container_start_page |
109 |
op_container_end_page |
123 |
op_publisher_place |
Dordrecht |
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1766296748076040192 |