Zabel, Matthias (2002): Phosphate of sediment core GeoB1712-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87921
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: -23.255000 * Longitude: 12.805000
Date/Time Start: 1992-01-12T00:00:00 * Date/Time End: 1992-01-12T00:00:00
Minimum DEPTH, sediment/rock: 0.100 m * Maximum DEPTH, sediment/rock: 10.300 m
Event(s):
GeoB1712-3 * Latitude: -23.255000 * Longitude: 12.805000 * Date/Time: 1992-01-12T00:00:00 * Elevation: -1003.0 m * Recovery: 10.57 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geochemie
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:
42 data points
Data
1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
---|---|
0.100 | 9.07 |
0.350 | 6.73 |
0.600 | 6.73 |
0.850 | 6.29 |
1.100 | 6.73 |
1.350 | 6.73 |
1.600 | 6.99 |
1.850 | 6.32 |
2.100 | 6.51 |
2.350 | 5.81 |
2.600 | 6.73 |
2.850 | 6.97 |
3.100 | 6.51 |
3.350 | 6.73 |
3.600 | 6.85 |
3.850 | 7.20 |
4.100 | 6.98 |
4.350 | 6.73 |
4.600 | 9.27 |
4.850 | 10.53 |
5.100 | 10.21 |
5.350 | 9.79 |
5.600 | 9.79 |
5.850 | 12.42 |
6.100 | 10.74 |
6.350 | 12.11 |
6.600 | 12.42 |
6.850 | 13.58 |
7.100 | 14.32 |
7.350 | 11.90 |
7.600 | 13.61 |
7.850 | 12.71 |
8.100 | 13.90 |
8.350 | 13.37 |
8.600 | 13.90 |
8.850 | 15.37 |
9.100 | 17.90 |
9.350 | 19.90 |
9.550 | 19.59 |
9.800 | 19.37 |
10.050 | 20.85 |
10.300 | 20.85 |