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Keigwin, Lloyd D; Lehmann, Scott J (1994): (Table 1) Stable isotope ratios of foraminifera in sediment core CH82-20. PANGAEA, https://doi.org/10.1594/PANGAEA.52678, In supplement to: Keigwin, LD; Lehmann, SJ (1994): Deep circulation change linked to Heinrich event 1 and Younger Dryas in a middepth North Atlantic core. Paleoceanography, 9(2), 185-194, https://doi.org/10.1029/94PA00032

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Event(s):
CH82-20pc * Elevation Start: -3020.0 m * Elevation End: 0.0 m * Campaign: CH8X * Basis: Jean Charcot * Method/Device: Piston corer (PC) * Comment: Position not given
CH82-20pg * Elevation Start: -3020.0 m * Elevation End: 0.0 m * Campaign: CH8X * Basis: Jean Charcot * Method/Device: Trigger corer (TC) * Comment: Position not given
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2DEPTH, sediment/rockDepthmGeocode
3Depth, compositeDepth compmcdKeigwin, Lloyd DIntercore correlation
4AGEAgeka BPGeocode
5Neogloboquadrina pachyderma sinistralN. pachyderma s%Keigwin, Lloyd DCounting >150 µm fraction
6Ice rafted debrisIRD#/gKeigwin, Lloyd DCounting >150 µm fraction
7Planulina wuellerstorfiP. wuellerstorfi#/gKeigwin, Lloyd DCounting >150 µm fraction
8Foraminifera, per unit sediment massForam/sed#/gKeigwin, Lloyd DCounting >150 µm fraction
9Globigerina bulloides, δ18OG. bulloides δ18O‰ PDBKeigwin, Lloyd DIsotope ratio mass spectrometry150-250 µm
10Globigerina bulloides, δ13CG. bulloides δ13C‰ PDBKeigwin, Lloyd DIsotope ratio mass spectrometry150-250 µm
11Planulina wuellerstorfi, δ18OP. wuellerstorfi δ18O‰ PDBKeigwin, Lloyd DIsotope ratio mass spectrometry>150 µm
12Planulina wuellerstorfi, δ13CP. wuellerstorfi δ13C‰ PDBKeigwin, Lloyd DIsotope ratio mass spectrometry>150 µm
Size:
630 data points

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