Schulz, Hartmut (1995): Stable isotope analysis on planktic foraminifera in sediment core SU90-I02 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.107750, In supplement to: Schulz, H (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp, https://doi.org/10.2312/reports-gpi.1995.73
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Project(s):
Coverage:
Latitude: 45.090000 * Longitude: -39.438333
Date/Time Start: 1990-01-01T00:00:00 * Date/Time End: 1990-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.425 m
Event(s):
SU90-I02 * Latitude: 45.090000 * Longitude: -39.438333 * Date/Time: 1990-01-01T00:00:00 * Elevation: -1965.0 m * Recovery: 0.45 m * Location: North Atlantic Ocean * Campaign: PALEOCINAT * Basis: Le Suroît * Method/Device: MultiCorer (MUC)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Schulz, Hartmut | Mass spectrometer Finnigan MAT 250 | |
3 | Neogloboquadrina pachyderma sinistral, δ13C | N. pachyderma s δ13C | ‰ PDB | Schulz, Hartmut | Mass spectrometer Finnigan MAT 250 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] | 3 N. pachyderma s δ13C [‰ PDB] |
---|---|---|
0.010 | 2.66 | 0.32 |
0.030 | 2.52 | 0.24 |
0.050 | 2.64 | 0.11 |
0.070 | 2.58 | 0.19 |
0.090 | 2.76 | 0.16 |
0.110 | 2.70 | 0.24 |
0.130 | 2.68 | -0.03 |
0.150 | 2.53 | 0.00 |
0.170 | 2.75 | 0.09 |
0.190 | 2.64 | 0.05 |
0.210 | 2.80 | -0.04 |
0.230 | 2.63 | -0.03 |
0.230 | 2.63 | -0.12 |
0.250 | 3.49 | -0.02 |
0.270 | 3.66 | -0.04 |
0.290 | 3.69 | -0.01 |
0.310 | 3.64 | -0.14 |
0.330 | 3.59 | -0.18 |
0.350 | 3.63 | -0.08 |
0.370 | 3.13 | 0.07 |
0.390 | 3.13 | -0.25 |
0.410 | 3.22 | 0.01 |
0.410 | 3.01 | -0.01 |
0.425 | 3.47 | -0.03 |