Keigwin, Lloyd D (1986): (Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP Hole 80-548 sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.718959, In supplement to: Keigwin, Lloyd D; Corliss, Bruce H (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: 48.915800 * Longitude: -12.164000
Date/Time Start: 1981-06-10T00:00:00 * Date/Time End: 1981-06-10T00:00:00
Minimum DEPTH, sediment/rock: 112.03 m * Maximum DEPTH, sediment/rock: 148.94 m
Event(s):
80-548 * Latitude: 48.915800 * Longitude: -12.164000 * Date/Time: 1981-06-10T00:00:00 * Elevation: -1251.0 m * Penetration: 211 m * Recovery: 210.2 m * Location: North Atlantic/SPUR * Campaign: Leg80 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 211 m cored; 0 m drilled; 99.6 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | Keigwin, Lloyd D | DSDP/ODP/IODP sample designation | ||
3 | Cibicidoides ungerianus, δ18O | C. ungerianus δ18O | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | |
4 | Cibicidoides ungerianus, δ13C | C. ungerianus δ13C | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | |
5 | Chiloguembelina cubensis, δ18O | C. cubensis δ18O | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | 125-150 µm |
6 | Chiloguembelina cubensis, δ13C | C. cubensis δ13C | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | 125-150 µm |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
51 data points
Data
1 Depth sed [m] | 2 Sample label | 3 C. ungerianus δ18O [‰ PDB] | 4 C. ungerianus δ13C [‰ PDB] | 5 C. cubensis δ18O [‰ PDB] | 6 C. cubensis δ13C [‰ PDB] |
---|---|---|---|---|---|
112.03 | 80-548-16-3,52-54 | 1.09 | 0.61 | ||
112.10 | 80-548-16-3,59-61 | 1.10 | 0.70 | ||
112.16 | 80-548-16-3,65-67 | 0.89 | 0.76 | ||
112.24 | 80-548-16-3,73-75 | 1.02 | 0.84 | ||
112.32 | 80-548-16-3,81-83 | 1.04 | 1.07 | 0.15 | 0.99 |
112.37 | 80-548-16-3,86-88 | 0.90 | -0.96 | 0.30 | 0.98 |
112.44 | 80-548-16-3,93-95 | 0.90 | 1.00 | 0.10 | 1.02 |
148.36 | 80-548-22-5,135-137 | -0.69 | 0.79 | ||
148.42 | 80-548-22-5,141-143 | -0.83 | 0.46 | ||
148.51 | 80-548-22-6,0-2 | -0.72 | 0.21 | ||
148.54 | 80-548-22-6,3-5 | -0.71 | 0.72 | ||
148.59 | 80-548-22-6,8-10 | -0.92 | 0.30 | ||
148.69 | 80-548-22-6,18-20 | -1.54 | -0.11 | ||
148.80 | 80-548-22-6,29-31 | -1.46 | -0.30 | ||
148.94 | 80-548-22-6,43-45 | -1.02 | 0.59 |