Lackschewitz, Klas Sven (2009): (Table A10) Carbonate, total organic carbon and sulphur content of sediment core PS1852-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712778
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Related to:
Lackschewitz, Klas Sven (1991): Sedimentationsprozesse am aktiven mittelozeanischen Kolbeinsey Rücken (nördlich von Island). GEOMAR Report, GEOMAR Research Center for Marine Geosciences, Christian Albrechts University in Kiel, 9, 133 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 70.253000 * Longitude: -15.826200
Date/Time Start: 1990-06-17T04:51:00 * Date/Time End: 1990-06-17T04:51:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 5.70 m
Event(s):
PS1852-2 (GIK21852-2 PS17/018) * Latitude: 70.253000 * Longitude: -15.826200 * Date/Time: 1990-06-17T04:51:00 * Elevation: -1105.0 m * Penetration: 6 m * Recovery: 5.73 m * Location: Kolbeinsey Ridge * Campaign: ARK-VII/1 (PS17) * Basis: Polarstern * Method/Device: Kasten corer (KAL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Calcium carbonate | CaCO3 | % | Lackschewitz, Klas Sven | Element analyser CHN, LECO |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
58 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.05 | 6.80 |
0.10 | 7.20 |
0.20 | 6.40 |
0.30 | 6.80 |
0.40 | 4.90 |
0.50 | 4.50 |
0.60 | 3.40 |
0.70 | 10.60 |
0.80 | 4.90 |
0.90 | 5.70 |
1.00 | 4.90 |
1.10 | 4.50 |
1.20 | 3.80 |
1.30 | 3.00 |
1.40 | 6.80 |
1.50 | 11.40 |
1.60 | 7.20 |
1.70 | 8.00 |
1.80 | 9.10 |
1.90 | 5.70 |
2.00 | 8.70 |
2.10 | 8.70 |
2.20 | 10.20 |
2.30 | 11.40 |
2.40 | 6.10 |
2.50 | 5.30 |
2.60 | 7.20 |
2.70 | 7.60 |
2.80 | 2.30 |
2.90 | 8.30 |
3.00 | 8.30 |
3.10 | 7.20 |
3.20 | 8.30 |
3.30 | 5.70 |
3.40 | 2.30 |
3.50 | 0.00 |
3.60 | 1.50 |
3.70 | 3.00 |
3.80 | 4.90 |
3.90 | 6.40 |
4.00 | 2.30 |
4.10 | 0.80 |
4.20 | 1.50 |
4.30 | 2.30 |
4.40 | 5.30 |
4.50 | 4.90 |
4.60 | 1.90 |
4.70 | 3.40 |
4.80 | 2.70 |
4.90 | 1.90 |
5.00 | 1.50 |
5.10 | 4.20 |
5.20 | 4.90 |
5.30 | 4.90 |
5.40 | 7.20 |
5.50 | 6.40 |
5.60 | 5.70 |
5.70 | 5.30 |