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Archive · collection · 1973

Stable oxygen isotope composition of the sea water in the Mediterranean Sea

Listed in PANGAEA and DataCite — shown once because both records carry DOI 10.1594/pangaea.548698

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.

Description

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.

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Provenance · 2 source records, 9 field assertions
SourceKeyLast seenRaw
PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.54869812 d agoJSON v1
DataCite10.1594/pangaea.54869812 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · PANGAEAconnector:pangaea@1.0.0
concepts[field].fos:earth-and-related-environmental-sciencessource · DataCiteconnector:datacite@1.0.0
concepts[field].local:field:earth-environmentalmapping · PANGAEAconnector:pangaea@1.0.0
concepts[field].local:field:ocean-atmosphericmapping · DataCitevocabulary-mapper@1.0.0keywords['Oceanography']
descriptionsource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/description
licensesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/rights
publication_datesource · PANGAEAconnector:pangaea@1.0.0
spatialsource · PANGAEAconnector:pangaea@1.0.0
titlesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/title