Age determination of sediment cores close to the Strait of Gibralta

Fuente: PANGAEA
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Autores principales: Zahn, Rainer, Sarnthein, Michael, Erlenkeuser, Helmut
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1987
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author Zahn, Rainer
Sarnthein, Michael
Erlenkeuser, Helmut
author_facet Zahn, Rainer
Sarnthein, Michael
Erlenkeuser, Helmut
collection Datos científicos de ciencias marinas y ambientales
contents A suit of sediment cores close to and south of the Strait of Gibraltar (12°-36°N, 500-2800 m water depth) were analyzed for stable isotopes in epibenthic foraminifers Cibicidoides wuellerstorfi and Planulina ariminensis. During peak glacial times, the data exhibit higher delta13C values of up to 1.6 per mil at intermediate depths near the Strait of Gibraltar (36°N). The values decrease to the south as evidenced by our data, but also to the north as revealed by data of intermediate depth cores north of 38°N (in Duplessy et al. (1987)). Thus, the distribution pattern of delta13C provides crucial evidence for an increased influence of nutrient depleted Mediterranean Outflow Water (MOW) on the glacial northeast Atlantic hydrography. During oxygen isotope Terminations I and II, the meridional carbon isotope gradient indicates a significantly decreased but still active MOW. As deduced from the delta18O fluctuations, the temperatures of the MOW in the Atlantic were lower during glacial times by as much as 5°C. During glacial times and during Termination I the maximum delta13C values of the MOW correlate with minimum values of the North Atlantic Deep Water (NADW) and vice versa. This inverse response to climatic change of the carbon isotope signals of both water masses indicates, that the supply of saline MOW to the north Atlantic may be less important for the formation of NADW than previously assumed.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_725956
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Age determination of sediment cores close to the Strait of Gibralta
Zahn, Rainer
Sarnthein, Michael
Erlenkeuser, Helmut
Atlantic Ocean; GIK15666-6; GIK15669-1; GIK15670-5; GIK16004-1; GIK16006-1; GIK16017-2; Gravity corer (Kiel type); KOL; M53; M53_166; M53_169; M53_170; M60; Meteor (1964); off West Africa; Piston corer (Kiel type); SL; SUBTROPEX 82
A suit of sediment cores close to and south of the Strait of Gibraltar (12°-36°N, 500-2800 m water depth) were analyzed for stable isotopes in epibenthic foraminifers Cibicidoides wuellerstorfi and Planulina ariminensis. During peak glacial times, the data exhibit higher delta13C values of up to 1.6 per mil at intermediate depths near the Strait of Gibraltar (36°N). The values decrease to the south as evidenced by our data, but also to the north as revealed by data of intermediate depth cores north of 38°N (in Duplessy et al. (1987)). Thus, the distribution pattern of delta13C provides crucial evidence for an increased influence of nutrient depleted Mediterranean Outflow Water (MOW) on the glacial northeast Atlantic hydrography. During oxygen isotope Terminations I and II, the meridional carbon isotope gradient indicates a significantly decreased but still active MOW. As deduced from the delta18O fluctuations, the temperatures of the MOW in the Atlantic were lower during glacial times by as much as 5°C. During glacial times and during Termination I the maximum delta13C values of the MOW correlate with minimum values of the North Atlantic Deep Water (NADW) and vice versa. This inverse response to climatic change of the carbon isotope signals of both water masses indicates, that the supply of saline MOW to the north Atlantic may be less important for the formation of NADW than previously assumed.
title Age determination of sediment cores close to the Strait of Gibralta
topic Atlantic Ocean; GIK15666-6; GIK15669-1; GIK15670-5; GIK16004-1; GIK16006-1; GIK16017-2; Gravity corer (Kiel type); KOL; M53; M53_166; M53_169; M53_170; M60; Meteor (1964); off West Africa; Piston corer (Kiel type); SL; SUBTROPEX 82
url https://doi.org/10.1594/PANGAEA.725956