Weber, Michael E; Wiedicke-Hombach, Michael; Riech, Volkher; Erlenkeuser, Helmut (1995): Calcium carbonate content of sediment core SO79-75KL [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351656, In supplement to: Weber, ME et al. (1995): Carbonate preservation history in the Peru Basin: Paleoceanographic implications. Paleoceanography, 10(4), 775-800, https://doi.org/10.1029/95PA01566
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Coverage:
Latitude: -6.531700 * Longitude: -90.470300
Date/Time Start: 1992-05-08T00:00:00 * Date/Time End: 1992-05-08T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.80 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Calcium carbonate | CaCO3 | % | Weber, Michael E | Element analysis (Klosa, 1994) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
82 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 62.9 |
0.08 | 19.1 |
0.18 | 5.2 |
0.20 | 99.3 |
0.28 | 14.3 |
0.30 | 93.9 |
0.33 | 8.8 |
0.40 | 95.3 |
0.40 | 20.7 |
0.47 | 3.2 |
0.50 | 94.0 |
0.54 | 5.7 |
0.60 | 95.7 |
0.62 | 12.2 |
0.70 | 95.7 |
0.80 | 96.0 |
0.90 | 94.8 |
1.00 | 96.9 |
1.10 | 101.9 |
1.20 | 96.5 |
1.30 | 97.6 |
1.40 | 97.8 |
1.50 | 96.8 |
1.60 | 97.5 |
1.70 | 95.4 |
1.80 | 97.9 |
1.90 | 96.4 |
1.95 | 93.3 |
2.00 | 95.9 |
2.10 | 96.0 |
2.20 | 98.1 |
2.30 | 95.2 |
2.40 | 95.7 |
2.50 | 93.8 |
2.60 | 94.8 |
2.70 | 93.9 |
2.70 | 94.9 |
2.80 | 91.8 |
2.90 | 93.8 |
3.00 | 93.8 |
3.10 | 94.1 |
3.20 | 94.3 |
3.30 | 95.2 |
3.40 | 94.2 |
3.50 | 90.1 |
3.60 | 90.6 |
3.70 | 95.4 |
3.80 | 94.6 |
3.90 | 92.6 |
3.95 | 92.3 |
4.00 | 95.7 |
4.10 | 93.6 |
4.20 | 94.7 |
4.30 | 94.8 |
4.40 | 93.8 |
4.50 | 91.2 |
4.60 | 90.8 |
4.70 | 97.3 |
4.80 | 90.6 |
4.80 | 92.0 |
4.90 | 92.1 |
5.00 | 92.8 |
5.10 | 93.6 |
5.20 | 92.9 |
5.30 | 74.1 |
5.40 | 91.0 |
5.50 | 91.5 |
5.60 | 71.4 |
5.70 | 91.5 |
5.80 | 90.2 |
5.90 | 90.4 |
5.95 | 90.4 |
6.00 | 89.8 |
6.10 | 92.4 |
6.20 | 61.6 |
6.30 | 90.8 |
6.40 | 89.4 |
6.50 | 94.2 |
6.60 | 88.1 |
6.70 | 88.7 |
6.70 | 88.6 |
6.80 | 90.9 |