Sarnthein, Michael (1997): Stable isotope analysis on sediment core GIK16773-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.54390
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, https://doi.org/10.1029/93PA03301
Project(s):
Coverage:
Latitude: -0.971667 * Longitude: -9.443333
Date/Time Start: 1988-01-22T00:00:00 * Date/Time End: 1988-01-22T00:00:00
Minimum DEPTH, sediment/rock: 0.01000 m * Maximum DEPTH, sediment/rock: 0.57000 m
Event(s):
GIK16773-1 * Latitude: -0.971667 * Longitude: -9.443333 * Date/Time: 1988-01-22T00:00:00 * Elevation: -4662.0 m * Recovery: 15.53 m * Location: Sierra Leone Basin/Guinea Basin * Campaign: M6/5 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Age model | Age model | ka | Sarnthein, Michael | Age, calculated calendar years | calculated ages |
4 | Globigerinoides ruber white, δ18O | G. ruber w δ18O | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 | |
5 | Globigerinoides ruber white, δ13C | G. ruber w δ13C | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 | |
6 | Cibicidoides wuellerstorfi, δ18O | C. wuellerstorfi δ18O | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 | |
7 | Cibicidoides wuellerstorfi, δ13C | C. wuellerstorfi δ13C | ‰ PDB | Sarnthein, Michael | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
145 data points
Data
1 Event | 2 Depth sed [m] | 3 Age model [ka] | 4 G. ruber w δ18O [‰ PDB] | 5 G. ruber w δ13C [‰ PDB] | 6 C. wuellerstorfi δ18O [‰ PDB] | 7 C. wuellerstorfi δ13C [‰ PDB] |
---|---|---|---|---|---|---|
GIK16773-1 | 0.01000 | 0.39000 | -1.310 | 2.260 | 2.540 | 0.940 |
GIK16773-1 | 0.03000 | 1.18000 | -1.340 | 2.090 | 2.510 | 0.670 |
GIK16773-1 | 0.05000 | 1.96000 | -1.060 | 1.610 | 2.820 | 0.420 |
GIK16773-1 | 0.07000 | 2.74000 | -1.180 | 2.190 | 2.460 | 0.880 |
GIK16773-1 | 0.09000 | 3.53000 | -1.610 | 2.010 | 2.490 | 0.880 |
GIK16773-1 | 0.11000 | 4.31000 | -1.270 | 2.210 | 2.950 | 0.570 |
GIK16773-1 | 0.13000 | 5.10000 | -1.280 | 2.100 | 2.470 | 0.640 |
GIK16773-1 | 0.15000 | 5.88000 | -1.230 | 2.280 | 2.530 | 0.980 |
GIK16773-1 | 0.17000 | 6.66000 | -1.200 | 2.140 | 2.460 | 0.590 |
GIK16773-1 | 0.19000 | 7.45000 | -1.210 | 2.060 | 2.390 | 0.750 |
GIK16773-1 | 0.21000 | 8.23000 | -1.290 | 2.160 | 2.690 | 0.690 |
GIK16773-1 | 0.23000 | 9.02000 | -1.390 | 2.060 | 2.750 | 0.700 |
GIK16773-1 | 0.25000 | 9.80000 | -1.540 | 2.020 | 2.430 | 0.840 |
GIK16773-1 | 0.27000 | 10.23000 | -1.390 | 2.130 | 2.640 | 0.610 |
GIK16773-1 | 0.29000 | 10.67000 | -1.610 | 2.140 | 2.920 | 0.700 |
GIK16773-1 | 0.31000 | 11.10000 | -1.440 | 2.150 | 3.070 | 0.620 |
GIK16773-1 | 0.33000 | 11.53000 | -1.300 | 1.750 | 2.950 | 0.850 |
GIK16773-1 | 0.35000 | 11.97000 | -1.280 | 2.200 | 2.980 | 0.680 |
GIK16773-1 | 0.37000 | 12.40000 | -1.240 | 1.720 | 3.800 | 0.250 |
GIK16773-1 | 0.39000 | 12.87000 | -1.090 | 1.890 | 3.500 | 0.520 |
GIK16773-1 | 0.41000 | 13.34000 | -0.700 | 1.680 | 3.600 | 0.660 |
GIK16773-1 | 0.43000 | 13.81000 | -0.930 | 1.630 | 3.350 | 0.550 |
GIK16773-1 | 0.45000 | 14.28000 | -0.770 | 1.650 | 3.160 | 0.690 |
GIK16773-1 | 0.47000 | 14.75000 | -1.040 | 1.630 | 3.340 | 0.580 |
GIK16773-1 | 0.49000 | 15.22000 | -0.650 | 1.360 | 3.720 | 0.220 |
GIK16773-1 | 0.51000 | 15.69000 | -0.620 | 1.360 | 3.960 | 0.190 |
GIK16773-1 | 0.53000 | 16.16000 | -0.720 | 1.570 | 3.840 | 0.240 |
GIK16773-1 | 0.55000 | 16.63000 | -0.610 | 1.290 | 3.780 | 0.280 |
GIK16773-1 | 0.57000 | 17.10000 | -0.540 | 1.610 | 3.740 | 0.320 |