Stable oxygen isotope composition of the sea water in the Mediterranean Sea
| Cobertura |
MEDIAN LATITUDE: 35.952083 * MEDIAN LONGITUDE: 17.315417 * SOUTH-BOUND LATITUDE: 35.550000 * WEST-BOUND LONGITUDE: 15.000000 * NORTH-BOUND LATITUDE: 36.308333 * EAST-BOUND LONGITUDE: 19.895000 * DATE/TIME START: 1969-06-18T00:00:00 * DATE/TIME END: 1971-03-10T00:00:00 |
|---|---|
| Data(s) |
21/11/1973
|
| Resumo |
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. |
| Formato |
application/zip, 4 datasets |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.548698 doi:10.1594/PANGAEA.548698 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Stahl, Wolfgang; Rinow, U (1973): Sauerstoffisotopenanalysen an Mittelmeerwässern. Ein Beitrag zur Problematik von Paläotemperaturbestimmungen. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C14, 55-59 |
| Palavras-Chave | #CIM (Cooperative Investigations of the Mediterranean); d18O H2O; delta 18O, water; DEPTH, water; Depth water; M17; M17_17A; M17_17B; M22; M22_16; M22_33; Mediterranean Sea; Meteor (1964); OCE; Oceanography; Sal; Salinity; Temperature, water, potential; Tpot |
| Tipo |
Dataset |
