Sarnthein, Michael (2004): Sedimentology on core V29-135 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134732
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: -19.700000 * Longitude: 8.883000
Date/Time Start: 1972-05-12T00:00:00 * Date/Time End: 1972-05-12T00:00:00
Minimum DEPTH, sediment/rock: 0.0050 m * Maximum DEPTH, sediment/rock: 3.2000 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sedimentation rate | SR | cm/ka | Sarnthein, Michael | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
57 data points
Data
1 Depth sed [m] | 2 SR [cm/ka] |
---|---|
0.0050 | 5.10 |
0.0375 | 5.10 |
0.0375 | 5.10 |
0.0375 | 5.10 |
0.1000 | 5.10 |
0.2000 | 5.10 |
0.2000 | 5.10 |
0.2000 | 5.10 |
0.3000 | 5.10 |
0.4000 | 5.10 |
0.4500 | 5.10 |
0.5000 | 5.10 |
0.5500 | 3.85 |
0.6000 | 3.85 |
0.6500 | 5.08 |
0.7000 | 5.08 |
0.7500 | 5.08 |
0.8000 | 5.08 |
0.8500 | 5.08 |
0.9000 | 5.08 |
0.9500 | 4.46 |
1.0000 | 4.46 |
1.0000 | 4.46 |
1.0000 | 4.46 |
1.1000 | 4.46 |
1.2000 | 4.46 |
1.3000 | 4.46 |
1.3500 | 4.46 |
1.4000 | 4.46 |
1.4500 | 6.41 |
1.5000 | 6.41 |
1.5500 | 6.41 |
1.6000 | 6.41 |
1.6500 | 6.41 |
1.7000 | 6.41 |
1.7500 | 6.41 |
1.8000 | 6.41 |
1.9000 | 6.41 |
2.0000 | 6.41 |
2.0000 | 6.41 |
2.0000 | 6.41 |
2.1000 | 6.41 |
2.2000 | 6.41 |
2.3000 | 6.41 |
2.4000 | 6.41 |
2.5000 | 6.41 |
2.6000 | 6.41 |
2.6000 | 6.41 |
2.6000 | 6.41 |
2.7000 | 6.41 |
2.8000 | 6.41 |
2.9000 | 6.41 |
3.0000 | 6.41 |
3.1000 | 6.41 |
3.2000 | 6.41 |
3.2000 | 6.41 |
3.2000 | 6.41 |