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Winn, Kyaw; Sarnthein, Michael (2003): Stable isotope analysis on sediment core GIK16415-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.107064

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Keyword(s):
GLAMAP
Related to:
Brassell, Simon C; Brereton, R G; Eglinton, Geoffrey; Grimalt, G; Liebezeit, Gerd; Marlowe, I T; Pflaumann, Uwe; Sarnthein, Michael (1985): Paleoclimatic signals recognised by chemometric treatment of molecular stratigraphic data. Organic Geochemistry, 19(4-6), 649-660, https://doi.org/10.1016/S0146-6380(86)80001-8
Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, https://doi.org/10.1029/93PA03301
Winn, Kyaw; Sarnthein, Michael; Erlenkeuser, Helmut (1991): d18O stratigraphy and chronology of Kiel sediment cores from the East Atlantic. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 45, 99 pp, https://doi.org/10.2312/reports-gpi.1991.45
Coverage:
Latitude: 9.566667 * Longitude: -19.095000
Date/Time Start: 1983-07-25T00:00:00 * Date/Time End: 1983-07-25T00:00:00
Minimum Elevation: -3845.0 m * Maximum Elevation: -3845.0 m
Event(s):
GIK16415-2 * Latitude: 9.566667 * Longitude: -19.095000 * Date/Time: 1983-07-25T00:00:00 * Elevation: -3845.0 m * Recovery: 13.35 m * Location: Atlantic Ocean * Campaign: M65 (GEOTROPEX 83, NOAMP I) * Basis: Meteor (1964) * Method/Device: Gravity corer (Kiel type) (SL)
Comment:
compiled data of core GIK16415-1 and core GIK16415-2 versus composite depth, no original depth available
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Depth, compositeDepth compmcdSarnthein, MichaelIntercore correlation
2Cibicidoides wuellerstorfi, δ18OC. wuellerstorfi δ18O‰ PDBSarnthein, MichaelIsotope ratio mass spectrometry
3Globigerinoides ruber white, δ18OG. ruber w δ18O‰ PDBSarnthein, MichaelIsotope ratio mass spectrometry
Size:
106 data points

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