Hommers, Harald; Sarnthein, Michael (2003): Stable isotope analysis on sediment core GIK13291-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.106208
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Project(s):
Coverage:
Latitude: 18.053000 * Longitude: -18.067300
Date/Time Start: 1975-08-06T00:00:00 * Date/Time End: 1975-08-06T00:00:00
Minimum DEPTH, sediment/rock: 0.035 m * Maximum DEPTH, sediment/rock: 4.450 m
Event(s):
GIK13291-1 * Latitude: 18.053000 * Longitude: -18.067300 * Date/Time: 1975-08-06T00:00:00 * Elevation: -2696.0 m * Recovery: 5.92 m * Location: Atlantic Ocean * Campaign: VA-10/3 * Basis: Valdivia (1961) * Method/Device: Kasten corer (KAL)
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 | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
59 data points
Data
1 Depth sed [m] | 2 G. ruber w δ18O [‰ PDB] |
---|---|
0.035 | -1.64 |
0.080 | -1.34 |
0.120 | -0.94 |
0.150 | -1.54 |
0.200 | -0.99 |
0.250 | -1.17 |
0.310 | -1.32 |
0.350 | -1.29 |
0.410 | 0.13 |
0.450 | -1.09 |
0.510 | -1.10 |
0.560 | -0.27 |
0.590 | 0.10 |
0.640 | -0.44 |
0.710 | -0.50 |
0.750 | -0.26 |
0.810 | 0.93 |
0.850 | 0.28 |
0.910 | 1.10 |
0.950 | 0.60 |
1.010 | 0.95 |
1.050 | 1.04 |
1.085 | 1.02 |
1.150 | 0.88 |
1.210 | 1.28 |
1.250 | 0.90 |
1.310 | 0.76 |
1.350 | 0.78 |
1.410 | 1.02 |
1.450 | 0.76 |
1.510 | 0.93 |
1.550 | 0.79 |
1.640 | 0.45 |
1.750 | 0.71 |
1.850 | 0.65 |
1.960 | 0.87 |
2.050 | 0.44 |
2.150 | 0.29 |
2.250 | 0.45 |
2.350 | -0.39 |
2.450 | 0.05 |
2.650 | -0.26 |
2.750 | -0.02 |
2.850 | 0.54 |
2.950 | 0.54 |
3.060 | 0.03 |
3.250 | -0.02 |
3.350 | -0.55 |
3.450 | -0.22 |
3.550 | -0.50 |
3.650 | -0.07 |
3.730 | 0.21 |
3.850 | 0.38 |
3.950 | -0.20 |
4.050 | 0.53 |
4.130 | 0.61 |
4.250 | 0.29 |
4.350 | -0.24 |
4.450 | -0.28 |