Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent D; Shackleton, Nicholas J (1988): (Appendix 1) Age model of sediment core CH73-139 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52277, In supplement to: Sarnthein, Michael; Winn, Kyaw; Duplessy, Jean-Claude; Fontugne, Michel R (1988): Global variations of surface ocean productivity in low and mid latitudes: influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years. Paleoceanography, 3(3), 361-399, https://doi.org/10.1029/PA003i003p00361
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent D; Shackleton, Nicholas J (1988): Changes in the distribution of d13C of deep water Sigma-CO2 between the last glaciation and the Holocene. Paleoceanography, 3(3), 317-341, https://doi.org/10.1029/PA003i003p00317
Coverage:
Latitude: 54.633300 * Longitude: -16.350000
Date/Time Start: 1973-01-01T00:00:00 * Date/Time End: 1973-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 3.300 m
Event(s):
CH73-139 (CH73-139C) * Latitude: 54.633300 * Longitude: -16.350000 * Date/Time: 1973-01-01T00:00:00 * Elevation: -2209.0 m * Campaign: CH7X * Basis: Jean Charcot * Method/Device: Piston corer (PC)
Comment:
For isotope data of Cibicidoides spp. see Duplessy (1982) dataset: doi:10.1594/PANGAEA.726215
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Curry, William B | Age model, stable isotope stratigraphy |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
36 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.000 | 0.000 |
| 0.150 | 1.200 |
| 0.200 | 1.600 |
| 0.300 | 2.400 |
| 0.400 | 3.200 |
| 0.500 | 4.000 |
| 0.600 | 4.800 |
| 0.700 | 5.600 |
| 0.850 | 6.800 |
| 0.900 | 7.200 |
| 1.000 | 8.000 |
| 1.100 | 8.800 |
| 1.200 | 9.600 |
| 1.300 | 10.400 |
| 1.350 | 10.800 |
| 1.450 | 11.600 |
| 1.500 | 12.300 |
| 1.550 | 13.000 |
| 1.600 | 13.700 |
| 1.700 | 15.100 |
| 1.750 | 15.600 |
| 1.850 | 16.700 |
| 1.900 | 17.300 |
| 2.000 | 18.300 |
| 2.100 | 19.400 |
| 2.250 | 21.000 |
| 2.350 | 22.100 |
| 2.450 | 23.200 |
| 2.550 | 24.200 |
| 2.650 | 25.300 |
| 2.750 | 26.400 |
| 2.850 | 27.500 |
| 3.000 | 29.100 |
| 3.100 | 30.100 |
| 3.200 | 31.200 |
| 3.300 | 32.300 |