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Imbrie, John D; Kellogg, Thomas B; Duplessy, Jean-Claude; Shackleton, Nicholas J; SPECMAP (2005): δ¹⁸O of benthic foraminifera in sediment core K11 (specmap2.019). PANGAEA,

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Related to:
Imbrie, John D; Boyle, Edward A; Clemens, Steven C; Duffy, A; Howard, William R; Kukla, George J; Kutzbach, J; Martinson, Douglas G; McIntyre, Andrew; Mix, Alan C; Molfino, Barbara; Morley, Joseph J; Peterson, Larry S; Pisias, Nicklas G; Prell, Warren L; Raymo, Maureen E; Shackleton, Nicholas J; Toggweiler, J Robbie (1992): On the structure and origin of major glaciation cycles; 1. Linear responses to Milankovitch forcing. Paleoceanography, 7(6), 701-738,
Kellogg, Thomas B; Duplessy, Jean-Claude; Shackleton, Nicholas J (1978): (Table 3) Stable oxygen isotope ratios of Neogloboquadrina pachyderma sinistral from sediment core CH70-K11. PANGAEA,
Kellogg, Thomas B; Duplessy, Jean-Claude; Shackleton, Nicholas J (1978): Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian Sea deep-sea cores. Boreas, 7(1), 61-73,
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Latitude: 71.783333 * Longitude: 1.600000
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 3.200 m
CH70-K11 * Latitude: 71.783333 * Longitude: 1.600000 * Elevation: -2900.0 m * Campaign: CH7X * Basis: Jean Charcot * Method/Device: Gravity corer (GC)
Dataset update 2019-12-19: The isotope values were named erroneously as benthic. Corrected to N. pachyderma sinistral.
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Age modelAge modelkaSPECMAPcalculated ages
3Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBSPECMAP
Change history:
2019-12-19T13:09:35 – d18O von benthisch auf N. pachyderma sinistral umgesetzt, Siehe PGI-2703.
126 data points

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