Mediterranean Outflow Water variability during the Early Pleistocene ...

Gaining insights into the evolution of Mediterranean Outflow Water (MOW) during the Early Pleistocene climate transition has been so far hampered by the lack of available paleoclimatic archives. Here we present the first benthic foraminifera stable oxygen and carbon isotope records and grain-size da...

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Main Authors: Kaboth, Stefanie, Grunert, Patrick, Lourens, Lucas Joost
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2017
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.871499
https://doi.pangaea.de/10.1594/PANGAEA.871499
id ftdatacite:10.1594/pangaea.871499
record_format openpolar
spelling ftdatacite:10.1594/pangaea.871499 2024-09-15T18:22:25+00:00 Mediterranean Outflow Water variability during the Early Pleistocene ... Kaboth, Stefanie Grunert, Patrick Lourens, Lucas Joost 2017 application/zip https://dx.doi.org/10.1594/pangaea.871499 https://doi.pangaea.de/10.1594/PANGAEA.871499 en eng PANGAEA https://dx.doi.org/10.5194/cp-13-1023-2017 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Exp339 Joides Resolution Integrated Ocean Drilling Program / International Ocean Discovery Program IODP article Collection Supplementary Publication Series of Datasets 2017 ftdatacite https://doi.org/10.1594/pangaea.87149910.5194/cp-13-1023-2017 2024-08-01T10:51:31Z Gaining insights into the evolution of Mediterranean Outflow Water (MOW) during the Early Pleistocene climate transition has been so far hampered by the lack of available paleoclimatic archives. Here we present the first benthic foraminifera stable oxygen and carbon isotope records and grain-size data from IODP Expedition 339 Site U1389 presently located within the upper core of the MOW in the Gulf of Cadiz for the time interval between 2.6 and 1.8 Ma. A comparison with an intermediate water mass record from the Mediterranean Sea strongly suggest an active MOW supplying Site U1389 on glacial-interglacial timescales during the Early Pleistocene. We also find indication that the increasing presence of MOW in the Gulf of Cadiz during the investigated time interval aligns with the progressive northward protrusion of Mediterranean sourced intermediate water masses into the North Atlantic, possibly modulating the intensification of the North Atlantic Meridional Overturning Circulation at the same time. ... : Supplement to: Kaboth, Stefanie; Grunert, Patrick; Lourens, Lucas Joost (2017): Mediterranean Outflow Water variability during the Early Pleistocene. Climate of the Past, 13(8), 1023-1035 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Exp339
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
spellingShingle Composite Core
Exp339
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
Kaboth, Stefanie
Grunert, Patrick
Lourens, Lucas Joost
Mediterranean Outflow Water variability during the Early Pleistocene ...
topic_facet Composite Core
Exp339
Joides Resolution
Integrated Ocean Drilling Program / International Ocean Discovery Program IODP
description Gaining insights into the evolution of Mediterranean Outflow Water (MOW) during the Early Pleistocene climate transition has been so far hampered by the lack of available paleoclimatic archives. Here we present the first benthic foraminifera stable oxygen and carbon isotope records and grain-size data from IODP Expedition 339 Site U1389 presently located within the upper core of the MOW in the Gulf of Cadiz for the time interval between 2.6 and 1.8 Ma. A comparison with an intermediate water mass record from the Mediterranean Sea strongly suggest an active MOW supplying Site U1389 on glacial-interglacial timescales during the Early Pleistocene. We also find indication that the increasing presence of MOW in the Gulf of Cadiz during the investigated time interval aligns with the progressive northward protrusion of Mediterranean sourced intermediate water masses into the North Atlantic, possibly modulating the intensification of the North Atlantic Meridional Overturning Circulation at the same time. ... : Supplement to: Kaboth, Stefanie; Grunert, Patrick; Lourens, Lucas Joost (2017): Mediterranean Outflow Water variability during the Early Pleistocene. Climate of the Past, 13(8), 1023-1035 ...
format Article in Journal/Newspaper
author Kaboth, Stefanie
Grunert, Patrick
Lourens, Lucas Joost
author_facet Kaboth, Stefanie
Grunert, Patrick
Lourens, Lucas Joost
author_sort Kaboth, Stefanie
title Mediterranean Outflow Water variability during the Early Pleistocene ...
title_short Mediterranean Outflow Water variability during the Early Pleistocene ...
title_full Mediterranean Outflow Water variability during the Early Pleistocene ...
title_fullStr Mediterranean Outflow Water variability during the Early Pleistocene ...
title_full_unstemmed Mediterranean Outflow Water variability during the Early Pleistocene ...
title_sort mediterranean outflow water variability during the early pleistocene ...
publisher PANGAEA
publishDate 2017
url https://dx.doi.org/10.1594/pangaea.871499
https://doi.pangaea.de/10.1594/PANGAEA.871499
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.5194/cp-13-1023-2017
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.87149910.5194/cp-13-1023-2017
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