Wang, Luejiang; Sarnthein, Michael; Erlenkeuser, Helmut; Grimalt, Joan O; Grootes, Pieter Meiert; Heilig, S; Ivanova, Elena V; Kienast, Markus; Pelejero, Carles; Pflaumann, Uwe (1999): Globigerinoides ruber (white) isotopes of sediment core GIK17964-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.55612, In supplement to: Wang, L et al. (1999): East-Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Marine Geology, 156(1-4), 245-284, https://doi.org/10.1016/S0025-3227(98)00182-0
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Project(s):
Coverage:
Latitude: 6.158333 * Longitude: 112.213333
Date/Time Start: 1994-06-01T00:00:00 * Date/Time End: 1994-06-01T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 12.60 m
Event(s):
GIK17964-2 * Latitude: 6.158333 * Longitude: 112.213333 * Date/Time: 1994-06-01T00:00:00 * Elevation: -1556.0 m * Penetration: 22 m * Location: South China Sea * Campaign: SO95 (MONITOR MONSUN) * Basis: Sonne * Method/Device: Piston corer (Kiel type) (KOL) * Comment: TWC 115 cm
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Globigerinoides ruber white, δ18O | G. ruber w δ18O | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 | |
| 3 | Globigerinoides ruber white, δ13C | G. ruber w δ13C | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
34 data points
Data
| 1 Depth sed [m] | 2 G. ruber w δ18O [‰ PDB] | 3 G. ruber w δ13C [‰ PDB] |
|---|---|---|
| 0.00 | -3.180 | 1.150 |
| 0.20 | -3.180 | 1.130 |
| 0.40 | -3.280 | 1.100 |
| 0.60 | -3.230 | 1.110 |
| 0.80 | -3.510 | 1.000 |
| 1.00 | -3.370 | 1.030 |
| 1.20 | -3.350 | 0.850 |
| 1.40 | -3.310 | 0.750 |
| 1.60 | -3.420 | 0.700 |
| 1.80 | -2.680 | 0.830 |
| 2.00 | -2.210 | 0.880 |
| 2.20 | -2.530 | 0.580 |
| 2.40 | -2.460 | 0.410 |
| 2.80 | -1.710 | 0.820 |
| 3.00 | -1.710 | 0.860 |
| 11.80 | -2.170 | 0.710 |
| 12.60 | -2.240 | 0.710 |