Cortijo, Elsa (2003): Stable isotope analysis on sediment core SU90-39 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.106761
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Related to:
Cortijo, Elsa (1995): La variabilité climatique rapide dans lAtlantique Nord depuis 128 000 ans: relations entre les calottes de glace et locéan de surface. PhD Thesis, Université de Paris-Sud, UFR Scientifique dOrsay, Paris, 235 pp
Project(s):
Glacial Atlantic Ocean Mapping (GLAMAP2000)
Coverage:
Latitude: 52.566667 * Longitude: -21.940000
Date/Time Start: 1990-01-01T00:00:00 * Date/Time End: 1990-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.440 m * Maximum DEPTH, sediment/rock: 2.580 m
Event(s):
SU90-39 * Latitude: 52.566667 * Longitude: -21.940000 * Date/Time: 1990-01-01T00:00:00 * Elevation: -3955.0 m * Recovery: 12.95 m * Location: North Atlantic * Campaign: PALEOCINAT * Basis: Le Suroît * Method/Device: Piston corer (PC)
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 | Cortijo, Elsa | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
42 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] |
|---|---|
| 0.440 | 3.00 |
| 0.460 | 3.34 |
| 0.480 | 2.93 |
| 0.520 | 3.17 |
| 0.560 | 3.32 |
| 0.580 | 2.80 |
| 0.600 | 2.99 |
| 0.610 | 3.07 |
| 0.620 | 3.30 |
| 0.630 | 2.98 |
| 0.690 | 3.97 |
| 0.700 | 3.60 |
| 0.710 | 4.25 |
| 0.720 | 4.13 |
| 0.730 | 4.24 |
| 0.740 | 4.00 |
| 0.750 | 4.18 |
| 0.760 | 4.18 |
| 0.770 | 4.30 |
| 0.780 | 4.11 |
| 0.790 | 4.26 |
| 0.800 | 4.16 |
| 0.810 | 4.20 |
| 0.900 | 4.20 |
| 0.990 | 3.82 |
| 1.080 | 3.86 |
| 1.190 | 4.07 |
| 1.280 | 3.95 |
| 1.350 | 3.38 |
| 1.420 | 3.64 |
| 1.500 | 3.39 |
| 1.590 | 3.79 |
| 1.680 | 3.55 |
| 1.790 | 3.50 |
| 1.880 | 3.60 |
| 1.990 | 3.19 |
| 2.090 | 2.89 |
| 2.200 | 2.99 |
| 2.290 | 3.47 |
| 2.380 | 3.72 |
| 2.490 | 3.59 |
| 2.580 | 3.42 |