Sarnthein, Michael (1997): Composite depth of sediment core GIK16772-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.54383
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, https://doi.org/10.1029/93PA03301
Project(s):
Coverage:
Latitude: -1.350000 * Longitude: -11.961667
Date/Time Start: 1988-01-21T00:00:00 * Date/Time End: 1988-01-21T00:00:00
Minimum DEPTH, sediment/rock: 0.11000 m * Maximum DEPTH, sediment/rock: 14.80000 m
Event(s):
GIK16772-2 * Latitude: -1.350000 * Longitude: -11.961667 * Date/Time: 1988-01-21T00:00:00 * Elevation: -3912.0 m * Recovery: 15.05 m * Location: eastern Romanche Fracture Zone * Campaign: M6/5 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL) * Comment: offset to GIK16772-1 = 27.5 cm
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, composite | Depth comp | mcd | Sarnthein, Michael | Intercore correlation | Reference: GIK16772-1 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
35 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] |
|---|---|
| 0.11000 | 0.385 |
| 0.20000 | 0.475 |
| 0.50000 | 0.775 |
| 0.76600 | 1.041 |
| 1.90000 | 2.175 |
| 2.20000 | 2.475 |
| 2.80000 | 3.075 |
| 3.00000 | 3.275 |
| 3.30000 | 3.575 |
| 3.70000 | 3.975 |
| 3.90000 | 4.175 |
| 4.20000 | 4.475 |
| 4.90000 | 5.175 |
| 5.10000 | 5.375 |
| 5.60000 | 5.875 |
| 6.00000 | 6.275 |
| 6.60000 | 6.875 |
| 6.90000 | 7.175 |
| 7.00000 | 7.275 |
| 7.30000 | 7.575 |
| 7.70000 | 7.975 |
| 8.30000 | 8.575 |
| 9.10000 | 9.375 |
| 9.30000 | 9.575 |
| 9.50000 | 9.775 |
| 10.00000 | 10.275 |
| 10.60000 | 10.875 |
| 11.10000 | 11.375 |
| 11.60000 | 11.875 |
| 12.00000 | 12.275 |
| 12.90000 | 13.175 |
| 13.20000 | 13.475 |
| 13.70000 | 13.975 |
| 14.50000 | 14.775 |
| 14.80000 | 15.075 |