Sarnthein, Michael (2003): Age model of sediment core GIK13519-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134241
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: 5.670000 * Longitude: -19.851667
Date/Time Start: 1979-03-01T00:00:00 * Date/Time End: 1979-03-01T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 10.500 m
Event(s):
GIK13519-1 * Latitude: 5.670000 * Longitude: -19.851667 * Date/Time: 1979-03-01T00:00:00 * Elevation: -2862.0 m * Recovery: 10.7 m * Location: Atlantic Ocean * Campaign: M51 (FGGE-Equator 79 - First GARP Global Experiment) * Basis: Meteor (1964) * Method/Device: Gravity corer (Kiel type) (SL)
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 | Sarnthein, Michael | ||
3 | Age, comment | Comm | Sarnthein, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
---|---|---|
0.000 | 0.00 | assumption of no sediment loss |
0.135 | 9.80 | deduced from C14 analog age of 9.1 ka; after Bard et al. (1990) |
0.248 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
0.535 | 29.50 | deduced from C14 analog age of 26 ka; after Bard et al. (1990) |
0.835 | 55.45 | d18O;event 3.31; after Martinson et al. (1987) |
0.945 | 71.12 | d18O;event 4.24; after Martinson et al. (1987) |
1.125 | 79.25 | d18O;event 5.1; after Martinson et al. (1987) |
1.240 | 90.95 | d18O;event 5.2; after Martinson et al. (1987) |
1.475 | 110.79 | d18O;event 5.4; after Martinson et al. (1987) |
1.665 | 122.19 | d18O;event 5.5; after Martinson et al. (1987) |
1.812 | 129.84 | d18O;event 6.0; after Martinson et al. (1987) |
1.915 | 135.34 | d18O;event 6.2; after Martinson et al. (1987) |
2.770 | 189.61 | d18O event 7; after Martinson et al. (1987) |
3.700 | 244.18 | d18Oevent 8; after Martinson et al. (1987) |
4.160 | 303.00 | d18O event 9; after Imbrie et al. (1984) |
5.060 | 339.00 | d18O event 10; after Imbrie et al. (1984) |
5.580 | 362.00 | d18O event 11; after Imbrie et al. (1984) |
6.220 | 423.00 | d18O event 12; after Imbrie et al. (1984) |
6.850 | 478.00 | d18Oevent 13; after Imbrie et al. (1984) |
7.440 | 524.00 | d18O event 14; after Imbrie et al. (1984) |
7.580 | 565.00 | d18Oevent 15; after Imbrie et al. (1984) |
8.290 | 620.00 | d18O event 16; after Imbrie et al. (1984) |
8.840 | 659.00 | d18O event 17; after Imbrie et al. (1984) |
9.160 | 689.00 | d18O event 18; after Imbrie et al. (1984) |
9.680 | 726.00 | d18O event 19; after Imbrie et al. (1984) |
9.870 | 730.00 | Brunhes;Matuyama |
9.960 | 736.00 | d18O event 20; after Imbrie et al. (1984) |
10.500 | 774.00 | d18O event 20; after Imbrie et al. (1984) |