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Dokken, Trond; Jansen, Eystein (1999): IRD, foraminifera abundance, stable isotope ratios of Cassidulina teretis and susceptibility of sediment core MD95-2010. PANGAEA, https://doi.org/10.1594/PANGAEA.61471, In supplement to: Dokken, T; Jansen, E (1999): Rapid changes in the mechanism of ocean convection during the last glacial period. Nature, 401(6752), 458-461, https://doi.org/10.1038/46753

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Project(s):
International Marine Global Change Study (IMAGES)
Coverage:
Latitude: 66.684167 * Longitude: 4.566160
Date/Time Start: 1995-06-07T00:00:00 * Date/Time End: 1995-06-07T00:00:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 11.025 m
Event(s):
MD95-2010 (MD952010) * Latitude: 66.684167 * Longitude: 4.566160 * Date/Time: 1995-06-07T00:00:00 * Elevation: -1226.0 m * Recovery: 33 m * Location: Voring Plateau * Campaign: MD101 (IMAGES I) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO) * Comment: XXI Sections, OK
Comment:
AGE is correlated to Greenland ice-core records (GISP)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2AGEAgeka BPGeocode
3Magnetic susceptibilityMAGS10-6 SIJansen, EysteinGeological High-resolution Magnetic Tool (GHMT)
4Neogloboquadrina pachyderma sinistral, δ18ON. pachyderma s δ18O‰ PDBJansen, EysteinIsotope ratio mass spectrometry
5Neogloboquadrina pachyderma sinistral, δ13CN. pachyderma s δ13C‰ PDBJansen, EysteinIsotope ratio mass spectrometry
6Cassidulina teretis, δ18OC. teretis δ18O‰ PDBJansen, EysteinIsotope ratio mass spectrometry
7Cassidulina teretis, δ13CC. teretis δ13C‰ PDBJansen, EysteinIsotope ratio mass spectrometry
8Foraminifera, per unit sediment massForam/sed#/gJansen, EysteinCounting
9Rock fragments per unit massRock fragm#/gJansen, EysteinCounting >500 µm fraction
10Ice rafted debrisIRD#/gJansen, EysteinCounting >150 µm fraction
Size:
5078 data points

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