Imbrie, John D; Boyle, Edward A (1997): Age model of sediment core CH82-24 (specmap2.026) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52210
Always quote citation above when using data! You can download the citation in several formats below.
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
Imbrie, John D; Boyle, Edward A; Clemens, Steven C; Duffy, A; Howard, William R; Kukla, George J; Kutzbach, J; Martinson, Douglas G; McIntyre, Andrew; Mix, Alan C; Molfino, Barbara; Morley, Joseph J; Peterson, Larry S; Pisias, Nicklas G; Prell, Warren L; Raymo, Maureen E; Shackleton, Nicholas J; Toggweiler, J Robbie (1992): On the structure and origin of major glaciation cycles; 1. Linear responses to Milankovitch forcing. Paleoceanography, 7(6), 701-738, https://doi.org/10.1029/92PA02253
Project(s):
Coverage:
Latitude: 43.470000 * Longitude: -30.660000
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 6.325 m
Event(s):
CH82-24 * Latitude: 43.470000 * Longitude: -30.660000 * Elevation Start: -3070.0 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 | Age model | Age model | ka | Boyle, Edward A | calculated ages |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
24 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.000 | 0.00 |
| 0.160 | 4.40 |
| 0.535 | 14.80 |
| 0.635 | 22.30 |
| 0.955 | 28.00 |
| 1.372 | 43.60 |
| 1.885 | 57.50 |
| 2.490 | 71.60 |
| 2.910 | 81.50 |
| 3.025 | 88.80 |
| 3.237 | 95.90 |
| 3.267 | 97.10 |
| 3.562 | 100.50 |
| 3.847 | 109.00 |
| 4.305 | 122.50 |
| 4.452 | 127.30 |
| 4.730 | 139.90 |
| 5.135 | 159.29 |
| 5.670 | 183.79 |
| 5.827 | 190.62 |
| 6.097 | 197.67 |
| 6.132 | 202.83 |
| 6.210 | 210.49 |
| 6.325 | 220.77 |