Keigwin, Lloyd D; Corliss, Bruce H (1986): (Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP Hole 3-19 sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.718944, 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: -28.534700 * Longitude: -23.677200
Date/Time Start: 1969-01-07T00:00:00 * Date/Time End: 1969-01-07T00:00:00
Minimum DEPTH, sediment/rock: 63.90 m * Maximum DEPTH, sediment/rock: 130.40 m
Event(s):
3-19 * Latitude: -28.534700 * Longitude: -23.677200 * Date/Time: 1969-01-07T00:00:00 * Elevation: -4677.0 m * Penetration: 145.2 m * Recovery: 96.5 m * Location: South Atlantic/RIDGE * Campaign: Leg3 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 12 cores; 103.8 m cored; 0 m drilled; 93 % 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 | Oridorsalis tener, δ18O | O. tener δ18O | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | |
| 4 | Oridorsalis tener, δ13C | O. tener δ13C | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | |
| 5 | Globocassidulina subglobosa, δ18O | G. subglobosa δ18O | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry | |
| 6 | Globocassidulina subglobosa, δ13C | G. subglobosa δ13C | ‰ PDB | Keigwin, Lloyd D | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
86 data points
Data
| 1 Depth sed [m] | 2 Sample label | 3 O. tener δ18O [‰ PDB] | 4 O. tener δ13C [‰ PDB] | 5 G. subglobosa δ18O [‰ PDB] | 6 G. subglobosa δ13C [‰ PDB] |
|---|---|---|---|---|---|
| 63.90 | 3-19-4-5,120 | 1.59 | -0.12 | ||
| 65.40 | 3-19-4-6,120 | 1.70 | 0.15 | ||
| 76.20 | 3-19-5-1,60 | 1.78 | -0.02 | 1.64 | -0.43 |
| 76.80 | 3-19-5-1,120 | 1.79 | 0.59 | ||
| 77.73 | 3-19-5-2,63 | 1.30 | 0.49 | ||
| 80.74 | 3-19-5-4,64 | 1.09 | 0.19 | ||
| 81.30 | 3-19-5-4,121 | 1.36 | 0.35 | ||
| 82.20 | 3-19-5-5,60 | 1.12 | 0.14 | 1.22 | 0.47 |
| 82.80 | 3-19-5-5,120 | 1.16 | 0.58 | 1.27 | 0.88 |
| 83.70 | 3-19-5-6,60 | 1.36 | |||
| 84.30 | 3-19-5-6,120 | 0.99 | 0.79 | ||
| 86.61 | 3-19-6-1,61 | 0.86 | 0.17 | ||
| 88.10 | 3-19-6-2,60 | 1.15 | 0.55 | ||
| 89.62 | 3-19-6-3,62 | 1.08 | 0.77 | ||
| 92.60 | 3-19-6-5,60 | 1.25 | 0.84 | ||
| 94.10 | 3-19-6-6,60 | 1.41 | 0.39 | ||
| 98.60 | 3-19-7-3,60 | 0.84 | 0.17 | ||
| 101.60 | 3-19-7-5,50 | 0.50 | -0.14 | 0.50 | 0.27 |
| 104.90 | 3-19-8-1,60 | 0.85 | 0.55 | ||
| 107.90 | 3-19-8-3,60 | 0.18 | 0.27 | 0.34 | 0.79 |
| 110.90 | 3-19-8-5,60 | 0.68 | -0.16 | 0.85 | 0.20 |
| 114.00 | 3-19-9-1,60 | 0.47 | 0.11 | ||
| 117.05 | 3-19-9-3,65 | 0.63 | 0.16 | ||
| 120.00 | 3-19-9-5,60 | 0.60 | 0.21 | ||
| 130.40 | 3-19-10-5,60 | 0.47 | 0.19 |