Late Pliocene variations of the Mediterranean outflow ...

Late Pliocene changes in the advection of Mediterranean Outflow Water (MOW) derivates were reconstructed at northeast Atlantic DSDP/ODP sites 548 and 982 and compared to records of WMDW at West Mediterranean Site 978. Neodymium isotope (epsilon-Nd) values more positive than ~10.5/~ 11 reflect dilute...

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Main Authors: Khélifi, Nabil, Sarnthein, Michael, Frank, Martin, Andersen, Nils, Garbe-Schönberg, Dieter
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.863957
https://doi.pangaea.de/10.1594/PANGAEA.863957
id ftdatacite:10.1594/pangaea.863957
record_format openpolar
spelling ftdatacite:10.1594/pangaea.863957 2024-09-15T18:25:19+00:00 Late Pliocene variations of the Mediterranean outflow ... Khélifi, Nabil Sarnthein, Michael Frank, Martin Andersen, Nils Garbe-Schönberg, Dieter 2014 application/zip https://dx.doi.org/10.1594/pangaea.863957 https://doi.pangaea.de/10.1594/PANGAEA.863957 en eng PANGAEA https://dx.doi.org/10.1016/j.margeo.2014.07.006 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Deep Sea Drilling Project DSDP Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2014 ftdatacite https://doi.org/10.1594/pangaea.86395710.1016/j.margeo.2014.07.006 2024-08-01T11:01:20Z Late Pliocene changes in the advection of Mediterranean Outflow Water (MOW) derivates were reconstructed at northeast Atlantic DSDP/ODP sites 548 and 982 and compared to records of WMDW at West Mediterranean Site 978. Neodymium isotope (epsilon-Nd) values more positive than ~10.5/~ 11 reflect diluted MOW derivates that spread almost continuously into the northeast Atlantic from 3.7 to 2.55 Ma, reaching Rockall Plateau Site 982 from 3.63 to 2.75 Ma. From 3.4 to 3.3 Ma average MOW temperature and salinity increased by 2°-4 °C and ~1 psu both at proximal Site 548 and distal Site 982. The rise implies a rise in flow strength, coeval with a long-term rise in both west Mediterranean Sea surface salinity by almost 2 psu and average bottom water salinity (BWS) by ~1 psu, despite inherent uncertainties in BWS estimates. The changes were linked with major Mediterranean aridification and a drop in African monsoon humidity. In contrast to model expectations, the rise in MOW salt discharge after 3.4 Ma did not translate ... : Supplement to: Khélifi, Nabil; Sarnthein, Michael; Frank, Martin; Andersen, Nils; Garbe-Schönberg, Dieter (2014): Late Pliocene variations of the Mediterranean outflow. Marine Geology, 357, 182-194 ... Article in Journal/Newspaper Northeast Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
spellingShingle Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
Khélifi, Nabil
Sarnthein, Michael
Frank, Martin
Andersen, Nils
Garbe-Schönberg, Dieter
Late Pliocene variations of the Mediterranean outflow ...
topic_facet Deep Sea Drilling Project DSDP
Ocean Drilling Program ODP
description Late Pliocene changes in the advection of Mediterranean Outflow Water (MOW) derivates were reconstructed at northeast Atlantic DSDP/ODP sites 548 and 982 and compared to records of WMDW at West Mediterranean Site 978. Neodymium isotope (epsilon-Nd) values more positive than ~10.5/~ 11 reflect diluted MOW derivates that spread almost continuously into the northeast Atlantic from 3.7 to 2.55 Ma, reaching Rockall Plateau Site 982 from 3.63 to 2.75 Ma. From 3.4 to 3.3 Ma average MOW temperature and salinity increased by 2°-4 °C and ~1 psu both at proximal Site 548 and distal Site 982. The rise implies a rise in flow strength, coeval with a long-term rise in both west Mediterranean Sea surface salinity by almost 2 psu and average bottom water salinity (BWS) by ~1 psu, despite inherent uncertainties in BWS estimates. The changes were linked with major Mediterranean aridification and a drop in African monsoon humidity. In contrast to model expectations, the rise in MOW salt discharge after 3.4 Ma did not translate ... : Supplement to: Khélifi, Nabil; Sarnthein, Michael; Frank, Martin; Andersen, Nils; Garbe-Schönberg, Dieter (2014): Late Pliocene variations of the Mediterranean outflow. Marine Geology, 357, 182-194 ...
format Article in Journal/Newspaper
author Khélifi, Nabil
Sarnthein, Michael
Frank, Martin
Andersen, Nils
Garbe-Schönberg, Dieter
author_facet Khélifi, Nabil
Sarnthein, Michael
Frank, Martin
Andersen, Nils
Garbe-Schönberg, Dieter
author_sort Khélifi, Nabil
title Late Pliocene variations of the Mediterranean outflow ...
title_short Late Pliocene variations of the Mediterranean outflow ...
title_full Late Pliocene variations of the Mediterranean outflow ...
title_fullStr Late Pliocene variations of the Mediterranean outflow ...
title_full_unstemmed Late Pliocene variations of the Mediterranean outflow ...
title_sort late pliocene variations of the mediterranean outflow ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.863957
https://doi.pangaea.de/10.1594/PANGAEA.863957
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_relation https://dx.doi.org/10.1016/j.margeo.2014.07.006
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.86395710.1016/j.margeo.2014.07.006
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