Kuznetsov, Yury V; Al'terman, E I; Lisitzin, Alexander P (1981): (Table 2b) Contents of 230Th, Fe2O3, MnO and P2O5 in bottom sediments from Station DM8-576 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755468, In supplement to: Kuznetsov, YV et al. (1981): Possible "normalization" of the experimental curves of the vertical distribution of Th230 in deep-sea sediments. Oceanology, 21(1), 116-121
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: -17.833300 * Longitude: -103.116700
Minimum DEPTH, sediment/rock: 0.060 m * Maximum DEPTH, sediment/rock: 0.640 m
Event(s):
DM8-576 * Latitude: -17.833300 * Longitude: -103.116700 * Elevation: -3980.0 m * Location: Southeast Pacific * Campaign: DM8 * Basis: Dmitry Mendeleev * Method/Device: Grab (GRAB)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, top/min | Depth top | m | Kuznetsov, Yury V | ||
| 3 | Depth, bottom/max | Depth bot | m | Kuznetsov, Yury V | ||
| 4 | Sediment type | Sediment | Kuznetsov, Yury V | for the whole core | ||
| 5 | Thorium-230 | 230Th | ng/kg | Kuznetsov, Yury V | ||
| 6 | Thorium-230, standard deviation | 230Th std dev | ± | Kuznetsov, Yury V | ||
| 7 | Iron oxide, Fe2O3 | Fe2O3 | % | Kuznetsov, Yury V | ||
| 8 | Manganese oxide | MnO | % | Kuznetsov, Yury V | ||
| 9 | Phosphorus pentoxide | P2O5 | % | Kuznetsov, Yury V |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Sediment | 5 230Th [ng/kg] | 6 230Th std dev [±] | 7 Fe2O3 [%] | 8 MnO [%] | 9 P2O5 [%] |
|---|---|---|---|---|---|---|---|---|
| 0.060 | 0.00 | 0.12 | Highly calcareous, foraminiferal-coccolitic, ferruginous-manganic silt | 863 | 12 | 5.610 | 0.76 | 0.92 |
| 0.165 | 0.12 | 0.21 | 572 | 7 | 7.310 | 0.70 | 1.17 | |
| 0.255 | 0.21 | 0.30 | 163 | 1 | 5.180 | 1.08 | 0.63 | |
| 0.350 | 0.30 | 0.40 | 66 | 1 | 3.320 | 1.05 | 0.61 | |
| 0.450 | 0.40 | 0.50 | 27 | 1 | 2.300 | 0.72 | 0.43 | |
| 0.550 | 0.50 | 0.60 | 10 | 1 | 1.620 | 0.54 | 0.38 | |
| 0.640 | 0.60 | 0.68 | 8 | 1 | 1.780 | 0.20 | 0.37 |