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Autores principales: Stahl, Wolfgang, Rinow, U
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1973
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Acceso en línea:https://doi.org/10.1594/PANGAEA.548698
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author Stahl, Wolfgang
Rinow, U
author_facet Stahl, Wolfgang
Rinow, U
collection Datos científicos de ciencias marinas y ambientales
contents During the cruises No 17 and 22 of the German research vessel „Meteor“, 45 water samples were taken at 4 stations in the central part of the Mediterranean Sea. Mass spectrometrical analyses showed that systematic, but time variable changes of the oxygen isotope ratios occur. Deep water samples (T> 500 m) have a ± constant isotopic composition of d18O = +1.79‰ (SMOW) and a Chlorinity of 21.399‰. These data are discussed with respect to paleotemperature determinations.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_548698
institution PANGAEA
language en
publishDate 1973
publisher PANGAEA
record_format pangaea
spellingShingle Stable oxygen isotope composition of the sea water in the Mediterranean Sea
Stahl, Wolfgang
Rinow, U
CIM (Cooperative Investigations of the Mediterranean); M17; M17_17A; M17_17B; M22; M22_16; M22_33; Mediterranean Sea; Meteor (1964); OCE; Oceanography
During the cruises No 17 and 22 of the German research vessel „Meteor“, 45 water samples were taken at 4 stations in the central part of the Mediterranean Sea. Mass spectrometrical analyses showed that systematic, but time variable changes of the oxygen isotope ratios occur. Deep water samples (T> 500 m) have a ± constant isotopic composition of d18O = +1.79‰ (SMOW) and a Chlorinity of 21.399‰. These data are discussed with respect to paleotemperature determinations.
title Stable oxygen isotope composition of the sea water in the Mediterranean Sea
topic CIM (Cooperative Investigations of the Mediterranean); M17; M17_17A; M17_17B; M22; M22_16; M22_33; Mediterranean Sea; Meteor (1964); OCE; Oceanography
url https://doi.org/10.1594/PANGAEA.548698