Zabel, Matthias (2002): Phosphate of sediment core GeoB1721-6 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87926
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Zabel, Matthias; Dahmke, Andreas; Schulz, Horst D (1998): Regional distribution of diffusive phosphate and silicate fluxes through the sediment–water interface: the eastern South Atlantic. Deep Sea Research Part I: Oceanographic Research Papers, 45(2-3), 277-300, https://doi.org/10.1016/S0967-0637(97)00073-3
Project(s):
Coverage:
Latitude: -29.171667 * Longitude: 13.085000
Date/Time Start: 1992-01-17T00:00:00 * Date/Time End: 1992-01-17T00:00:00
Minimum DEPTH, sediment/rock: 0.100 m * Maximum DEPTH, sediment/rock: 9.500 m
Event(s):
GeoB1721-6 * Latitude: -29.171667 * Longitude: 13.085000 * Date/Time: 1992-01-17T00:00:00 * Elevation: -3051.0 m * Recovery: 9.73 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geochemie, Karbonatschl.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Phosphate | [PO4]3- | µmol/l | Zabel, Matthias | Continuous Flow Analysis (CFA) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
38 data points
Data
1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
---|---|
0.100 | 2.72 |
0.350 | 12.93 |
0.600 | 17.74 |
0.850 | 18.92 |
1.100 | 17.05 |
1.350 | 16.47 |
1.600 | 15.64 |
1.850 | 14.10 |
2.100 | 14.87 |
2.350 | 14.10 |
2.600 | 13.58 |
2.850 | 14.10 |
3.100 | 13.07 |
3.350 | 12.81 |
3.600 | 12.30 |
3.850 | 12.81 |
4.100 | 12.81 |
4.300 | 13.46 |
4.550 | 12.05 |
4.800 | 12.30 |
5.300 | 11.79 |
5.550 | 11.79 |
5.800 | 11.79 |
6.050 | 11.79 |
6.300 | 11.28 |
6.550 | 12.17 |
6.800 | 11.20 |
7.050 | 10.85 |
7.300 | 10.85 |
7.550 | 10.73 |
7.800 | 10.61 |
8.050 | 10.32 |
8.300 | 10.02 |
8.550 | 10.02 |
8.800 | 10.32 |
9.000 | 10.61 |
9.250 | 10.61 |
9.500 | 11.20 |