Boyle, Edward A; Keigwin, Lloyd D (2003): Stable isotope analysis on sediment core CHN82-24 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.106531
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Related to:
Boyle, Edward A; Keigwin, Lloyd D (1985): Comparison of Atlantic and Pacific paleochemical records for the last 215.000 years: changes in deep ocean circulation and chemical inventories. Earth and Planetary Science Letters, 76(1-2), 135-150, https://doi.org/10.1016/0012-821X(85)90154-2
Project(s):
Glacial Atlantic Ocean Mapping (GLAMAP2000)
Coverage:
Latitude: 43.465000 * Longitude: -32.850000
Minimum DEPTH, sediment/rock: 0.025 m * Maximum DEPTH, sediment/rock: 2.910 m
Event(s):
CHN82-24 * Latitude: 43.465000 * Longitude: -32.850000 * Elevation Start: -3427.0 m * Elevation End: 0.0 m * Campaign: CH8X * Basis: Jean Charcot * 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 | Cibicidoides wuellerstorfi, δ18O | C. wuellerstorfi δ18O | ‰ PDB | Boyle, Edward A | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
53 data points
Data
1 Depth sed [m] | 2 C. wuellerstorfi δ18O [‰ PDB] |
---|---|
0.025 | 2.69 |
0.085 | 2.61 |
0.115 | 2.59 |
0.160 | 2.69 |
0.235 | 2.84 |
0.320 | 3.13 |
0.535 | 4.16 |
0.575 | 4.37 |
0.605 | 4.40 |
0.635 | 4.41 |
0.720 | 4.08 |
0.740 | 4.09 |
0.815 | 4.08 |
0.895 | 3.96 |
0.955 | 3.77 |
1.085 | 3.93 |
1.152 | 3.81 |
1.178 | 4.02 |
1.245 | 3.78 |
1.280 | 3.69 |
1.315 | 3.93 |
1.372 | 3.42 |
1.398 | 3.72 |
1.448 | 3.63 |
1.470 | 3.91 |
1.540 | 3.76 |
1.632 | 3.80 |
1.738 | 3.74 |
1.782 | 3.69 |
1.828 | 3.52 |
1.858 | 3.54 |
1.885 | 3.35 |
1.915 | 3.81 |
1.965 | 3.72 |
1.995 | 3.57 |
2.020 | 3.86 |
2.030 | 3.81 |
2.075 | 3.74 |
2.120 | 3.79 |
2.170 | 4.13 |
2.210 | 3.61 |
2.298 | 4.24 |
2.345 | 3.68 |
2.408 | 3.75 |
2.428 | 3.49 |
2.490 | 3.35 |
2.550 | 3.48 |
2.590 | 3.44 |
2.640 | 3.38 |
2.692 | 3.33 |
2.770 | 3.26 |
2.870 | 3.25 |
2.910 | 3.17 |