Age determination of sediment core SO75-26KL, Portuguese margin ...

A benthic isotope record has been measured for core SO75-26KL from the upper Portuguese margin (1099 m water depth) to monitor the response of thermohaline overturn in the North Atlantic during Heinrich events. Evaluating benthic delta18O in TS diagrams in conjunction with equilibrium deltac fractio...

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Main Authors: Zahn, Rainer, Schönfeld, Joachim, Kudrass, Hermann-Rudolph, Park, M-H, Erlenkeuser, Helmut, Grootes, Pieter Meiert
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1997
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.734077
https://doi.pangaea.de/10.1594/PANGAEA.734077
id ftdatacite:10.1594/pangaea.734077
record_format openpolar
spelling ftdatacite:10.1594/pangaea.734077 2024-09-15T18:21:33+00:00 Age determination of sediment core SO75-26KL, Portuguese margin ... Zahn, Rainer Schönfeld, Joachim Kudrass, Hermann-Rudolph Park, M-H Erlenkeuser, Helmut Grootes, Pieter Meiert 1997 application/zip https://dx.doi.org/10.1594/pangaea.734077 https://doi.pangaea.de/10.1594/PANGAEA.734077 en eng PANGAEA https://dx.doi.org/10.1029/97pa00581 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Piston corer BGR type SO75/3 Sonne article Collection Supplementary Publication Series of Datasets 1997 ftdatacite https://doi.org/10.1594/pangaea.73407710.1029/97pa00581 2024-07-03T13:16:23Z A benthic isotope record has been measured for core SO75-26KL from the upper Portuguese margin (1099 m water depth) to monitor the response of thermohaline overturn in the North Atlantic during Heinrich events. Evaluating benthic delta18O in TS diagrams in conjunction with equilibrium deltac fractionation implies that advection of Mediterranean outflow water (MOW) to the upper Portuguese margin was significantly reduced during the last glacial (< 15% compared to 30% today). The benthic isotope record along core SO75-26KL therefore primarily monitors variability of glacial North Atlantic conveyor circulation. The 14C-accelerator mass spectrometry ages of 13.54±.07 and 20.46±.12 ka for two ice-rafted detritus (IRD) layers in the upper core section and an interpolated age of 36.1 ka for a third IRD layer deeper in the core are in the range of published 14C ages for Heinrich events H1, H2, and H4. Marked depletion of benthic delta13C by 0.7-1.1 per mil during the Heinrich events suggests reduced thermohaline ... : Supplement to: Zahn, Rainer; Schönfeld, Joachim; Kudrass, Hermann-Rudolph; Park, M-H; Erlenkeuser, Helmut; Grootes, Pieter Meiert (1997): Thermohaline instability in the North Atlantic during meltwater events: Stable isotope and ice-rafted detritus records from core SO75-26KL, Portuguese margin. Paleoceanography, 12(5), 696-710 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Piston corer BGR type
SO75/3
Sonne
spellingShingle Piston corer BGR type
SO75/3
Sonne
Zahn, Rainer
Schönfeld, Joachim
Kudrass, Hermann-Rudolph
Park, M-H
Erlenkeuser, Helmut
Grootes, Pieter Meiert
Age determination of sediment core SO75-26KL, Portuguese margin ...
topic_facet Piston corer BGR type
SO75/3
Sonne
description A benthic isotope record has been measured for core SO75-26KL from the upper Portuguese margin (1099 m water depth) to monitor the response of thermohaline overturn in the North Atlantic during Heinrich events. Evaluating benthic delta18O in TS diagrams in conjunction with equilibrium deltac fractionation implies that advection of Mediterranean outflow water (MOW) to the upper Portuguese margin was significantly reduced during the last glacial (< 15% compared to 30% today). The benthic isotope record along core SO75-26KL therefore primarily monitors variability of glacial North Atlantic conveyor circulation. The 14C-accelerator mass spectrometry ages of 13.54±.07 and 20.46±.12 ka for two ice-rafted detritus (IRD) layers in the upper core section and an interpolated age of 36.1 ka for a third IRD layer deeper in the core are in the range of published 14C ages for Heinrich events H1, H2, and H4. Marked depletion of benthic delta13C by 0.7-1.1 per mil during the Heinrich events suggests reduced thermohaline ... : Supplement to: Zahn, Rainer; Schönfeld, Joachim; Kudrass, Hermann-Rudolph; Park, M-H; Erlenkeuser, Helmut; Grootes, Pieter Meiert (1997): Thermohaline instability in the North Atlantic during meltwater events: Stable isotope and ice-rafted detritus records from core SO75-26KL, Portuguese margin. Paleoceanography, 12(5), 696-710 ...
format Article in Journal/Newspaper
author Zahn, Rainer
Schönfeld, Joachim
Kudrass, Hermann-Rudolph
Park, M-H
Erlenkeuser, Helmut
Grootes, Pieter Meiert
author_facet Zahn, Rainer
Schönfeld, Joachim
Kudrass, Hermann-Rudolph
Park, M-H
Erlenkeuser, Helmut
Grootes, Pieter Meiert
author_sort Zahn, Rainer
title Age determination of sediment core SO75-26KL, Portuguese margin ...
title_short Age determination of sediment core SO75-26KL, Portuguese margin ...
title_full Age determination of sediment core SO75-26KL, Portuguese margin ...
title_fullStr Age determination of sediment core SO75-26KL, Portuguese margin ...
title_full_unstemmed Age determination of sediment core SO75-26KL, Portuguese margin ...
title_sort age determination of sediment core so75-26kl, portuguese margin ...
publisher PANGAEA
publishDate 1997
url https://dx.doi.org/10.1594/pangaea.734077
https://doi.pangaea.de/10.1594/PANGAEA.734077
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1029/97pa00581
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.73407710.1029/97pa00581
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