Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...

Weddell Sea-derived Antarctic Bottom Water (AABW) is one of the most important deep water masses in the Southern Hemisphere occupying large portions of the deep Southern Ocean (SO) today. While substantial changes in SO-overturning circulation were previously suggested, the state of Weddell Sea AABW...

Full description

Bibliographic Details
Main Authors: Huang, Huang, Gutjahr, Marcus, Eisenhauer, Anton, Kuhn, Gerhard
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.909084
https://doi.pangaea.de/10.1594/PANGAEA.909084
id ftdatacite:10.1594/pangaea.909084
record_format openpolar
spelling ftdatacite:10.1594/pangaea.909084 2024-09-15T17:41:27+00:00 Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ... Huang, Huang Gutjahr, Marcus Eisenhauer, Anton Kuhn, Gerhard 2019 application/zip https://dx.doi.org/10.1594/pangaea.909084 https://doi.pangaea.de/10.1594/PANGAEA.909084 en eng PANGAEA https://dx.doi.org/10.1038/s41467-020-14302-3 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Helmholtz Centre for Ocean Research Kiel GEOMAR Ocean Drilling Program ODP Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Publication Series of Datasets Collection article 2019 ftdatacite https://doi.org/10.1594/pangaea.90908410.1038/s41467-020-14302-3 2024-08-01T10:54:44Z Weddell Sea-derived Antarctic Bottom Water (AABW) is one of the most important deep water masses in the Southern Hemisphere occupying large portions of the deep Southern Ocean (SO) today. While substantial changes in SO-overturning circulation were previously suggested, the state of Weddell Sea AABW export during glacial climates remains poorly understood. Here we report seawater-derived Nd and Pb isotope records that provide evidence for the absence of Weddell Sea-derived AABW in the Atlantic sector of the SO during the last two glacial maxima. Increasing delivery of Antarctic Pb to regions outside the Weddell Sea traced SO frontal displacements during both glacial terminations. The export of Weddell Sea-derived AABW resumed late during glacial terminations, coinciding with the last major atmospheric CO~2~ rise in the transition to the Holocene and the Eemian. Our new records lend strong support for a previously inferred AABW overturning stagnation event during the peak Eemian interglacial. ... Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Weddell Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Helmholtz Centre for Ocean Research Kiel GEOMAR
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Helmholtz Centre for Ocean Research Kiel GEOMAR
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Huang, Huang
Gutjahr, Marcus
Eisenhauer, Anton
Kuhn, Gerhard
Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
topic_facet Helmholtz Centre for Ocean Research Kiel GEOMAR
Ocean Drilling Program ODP
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Weddell Sea-derived Antarctic Bottom Water (AABW) is one of the most important deep water masses in the Southern Hemisphere occupying large portions of the deep Southern Ocean (SO) today. While substantial changes in SO-overturning circulation were previously suggested, the state of Weddell Sea AABW export during glacial climates remains poorly understood. Here we report seawater-derived Nd and Pb isotope records that provide evidence for the absence of Weddell Sea-derived AABW in the Atlantic sector of the SO during the last two glacial maxima. Increasing delivery of Antarctic Pb to regions outside the Weddell Sea traced SO frontal displacements during both glacial terminations. The export of Weddell Sea-derived AABW resumed late during glacial terminations, coinciding with the last major atmospheric CO~2~ rise in the transition to the Holocene and the Eemian. Our new records lend strong support for a previously inferred AABW overturning stagnation event during the peak Eemian interglacial. ...
format Article in Journal/Newspaper
author Huang, Huang
Gutjahr, Marcus
Eisenhauer, Anton
Kuhn, Gerhard
author_facet Huang, Huang
Gutjahr, Marcus
Eisenhauer, Anton
Kuhn, Gerhard
author_sort Huang, Huang
title Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
title_short Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
title_full Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
title_fullStr Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
title_full_unstemmed Authigenic Pb and Nd isotope composition of sediments from the Southern Ocean ...
title_sort authigenic pb and nd isotope composition of sediments from the southern ocean ...
publisher PANGAEA
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.909084
https://doi.pangaea.de/10.1594/PANGAEA.909084
genre Antarc*
Antarctic
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Southern Ocean
Weddell Sea
op_relation https://dx.doi.org/10.1038/s41467-020-14302-3
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.90908410.1038/s41467-020-14302-3
_version_ 1810487626739744768