Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...

The shoaling and final closure of the Central American Seaway (CAS) resulted in a major change of the global ocean circulation and has been suggested as an essential driver for strengthening of Atlantic Meridional Overturning Circulation (AMOC). The exact timing of CAS closure is key to interpreting...

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Main Authors: Osborne, Anne H, Newkirk, Derrick R, Groeneveld, Jeroen, Martin, Ellen E, Tiedemann, Ralf, Frank, Martin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.834759
https://doi.pangaea.de/10.1594/PANGAEA.834759
id ftdatacite:10.1594/pangaea.834759
record_format openpolar
spelling ftdatacite:10.1594/pangaea.834759 2024-04-28T08:29:18+00:00 Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ... Osborne, Anne H Newkirk, Derrick R Groeneveld, Jeroen Martin, Ellen E Tiedemann, Ralf Frank, Martin 2014 application/zip https://dx.doi.org/10.1594/pangaea.834759 https://doi.pangaea.de/10.1594/PANGAEA.834759 en eng PANGAEA https://dx.doi.org/10.1002/2014pa002676 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ocean Drilling Program ODP article Supplementary Publication Series of Datasets Collection 2014 ftdatacite https://doi.org/10.1594/pangaea.83475910.1002/2014pa002676 2024-04-02T10:00:39Z The shoaling and final closure of the Central American Seaway (CAS) resulted in a major change of the global ocean circulation and has been suggested as an essential driver for strengthening of Atlantic Meridional Overturning Circulation (AMOC). The exact timing of CAS closure is key to interpreting its importance. Here we present a reconstruction of deep and intermediate water Nd and Pb isotope compositions obtained from fossil fish teeth and the authigenic coatings of planktonic foraminifera in the eastern equatorial Pacific (Ocean Drilling Program (ODP) Site 1241) and the Caribbean (ODP Sites 998, 999, and 1000) covering the final stages of CAS closure between 5.6 and 2.2 Ma. The data for the Pacific site indicate no significant Atlantic/Caribbean influence over this entire period. The Caribbean sites show a continuous trend to less radiogenic Nd isotope compositions during the Pliocene, consistent with an enhancement of Upper North Atlantic Deep Water (UNADW) inflow and a strengthening of the AMOC. ... : Supplement to: Osborne, Anne H; Newkirk, Derrick R; Groeneveld, Jeroen; Martin, Ellen E; Tiedemann, Ralf; Frank, Martin (2014): The seawater neodymium and lead isotope record of the final stages of Central American Seaway closure. Paleoceanography, 29 ... Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Ocean Drilling Program ODP
spellingShingle Ocean Drilling Program ODP
Osborne, Anne H
Newkirk, Derrick R
Groeneveld, Jeroen
Martin, Ellen E
Tiedemann, Ralf
Frank, Martin
Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
topic_facet Ocean Drilling Program ODP
description The shoaling and final closure of the Central American Seaway (CAS) resulted in a major change of the global ocean circulation and has been suggested as an essential driver for strengthening of Atlantic Meridional Overturning Circulation (AMOC). The exact timing of CAS closure is key to interpreting its importance. Here we present a reconstruction of deep and intermediate water Nd and Pb isotope compositions obtained from fossil fish teeth and the authigenic coatings of planktonic foraminifera in the eastern equatorial Pacific (Ocean Drilling Program (ODP) Site 1241) and the Caribbean (ODP Sites 998, 999, and 1000) covering the final stages of CAS closure between 5.6 and 2.2 Ma. The data for the Pacific site indicate no significant Atlantic/Caribbean influence over this entire period. The Caribbean sites show a continuous trend to less radiogenic Nd isotope compositions during the Pliocene, consistent with an enhancement of Upper North Atlantic Deep Water (UNADW) inflow and a strengthening of the AMOC. ... : Supplement to: Osborne, Anne H; Newkirk, Derrick R; Groeneveld, Jeroen; Martin, Ellen E; Tiedemann, Ralf; Frank, Martin (2014): The seawater neodymium and lead isotope record of the final stages of Central American Seaway closure. Paleoceanography, 29 ...
format Article in Journal/Newspaper
author Osborne, Anne H
Newkirk, Derrick R
Groeneveld, Jeroen
Martin, Ellen E
Tiedemann, Ralf
Frank, Martin
author_facet Osborne, Anne H
Newkirk, Derrick R
Groeneveld, Jeroen
Martin, Ellen E
Tiedemann, Ralf
Frank, Martin
author_sort Osborne, Anne H
title Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
title_short Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
title_full Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
title_fullStr Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
title_full_unstemmed Seawater Nd and Pb isotopic record in central Pacific and Caribbean sediments ...
title_sort seawater nd and pb isotopic record in central pacific and caribbean sediments ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.834759
https://doi.pangaea.de/10.1594/PANGAEA.834759
genre North Atlantic Deep Water
North Atlantic
Planktonic foraminifera
genre_facet North Atlantic Deep Water
North Atlantic
Planktonic foraminifera
op_relation https://dx.doi.org/10.1002/2014pa002676
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83475910.1002/2014pa002676
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