Keigwin, Lloyd D; Corliss, Bruce H (1986): (Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP Hole 41-366 sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.718957, In supplement to: Keigwin, LD; Corliss, BH (1986): Stable isotopes in late middle Eocene to Oligocene foraminifera. Geological Society of America Bulletin, 97(3), 335-345, https://doi.org/10.1130/0016-7606(1986)97%3C335:SIILME%3E2.0.CO;2
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 5.678000 * Longitude: -19.851300
Date/Time Start: 1975-02-22T00:00:00 * Date/Time End: 1975-02-22T00:00:00
Minimum DEPTH, sediment/rock: 399.54 m * Maximum DEPTH, sediment/rock: 417.18 m
Event(s):
41-366 * Latitude: 5.678000 * Longitude: -19.851300 * Date/Time: 1975-02-22T00:00:00 * Elevation: -2853.0 m * Penetration: 850.5 m * Recovery: 302.8 m * Location: North Atlantic/CONT RISE * Campaign: Leg41 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 53 cores; 499 m cored; 19 m drilled; 60.7 % recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
44 data points
Data
1 Depth sed [m] | 2 Sample label | 3 O. tener δ18O [‰ PDB] | 4 O. tener δ13C [‰ PDB] | 5 C. ungerianus δ18O [‰ PDB] | 6 C. ungerianus δ13C [‰ PDB] | 7 Bulimina sp. δ18O [‰ PDB] | 8 Bulimina sp. δ13C [‰ PDB] | 9 Uvigerina spp. δ18O [‰ PDB] | 10 Uvigerina spp. δ13C [‰ PDB] | 11 Hantkenina δ18O [‰ PDB] | 12 Hantkenina δ13C [‰ PDB] | 13 C. cubensis δ18O [‰ PDB] | 14 C. cubensis δ13C [‰ PDB] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
399.54 | 41-366-8-4,54 | -1.07 | 1.55 | ||||||||||
404.51 | 41-366-9-1,51 | 1.87 | 0.10 | 1.46 | 1.08 | 1.82 | 0.49 | -1.05 | 1.58 | ||||
406.00 | 41-366-9-2,50 | 1.95 | 0.18 | 1.55 | 1.43 | -1.27 | 1.76 | ||||||
414.02 | 41-366-10-1,52 | 1.01 | -0.36 | 0.70 | 0.49 | -1.49 | 1.83 | ||||||
415.72 | 41-366-10-2,72 | 0.89 | -0.25 | 0.49 | 0.70 | 0.93 | 0.09 | 0.97 | 0.31 | -0.71 | 0.60 | ||
417.18 | 41-366-10-3,68 | 1.10 | -0.36 | 0.88 | 0.38 | 1.01 | 0.40 |