Michels, Klaus; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Diekmann, Bernhard; Fütterer, Dieter K; Grobe, Hannes; Uenzelmann-Neben, Gabriele (2002): Ice rafted debris (> 2 mm gravel) distribution in sediment core PS1599-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.53354, In supplement to: Michels, K et al. (2002): The southern Weddell Sea: combined contourite-turbidite sedimentation at the southeastern margin of the Weddell Gyre. In: Stow, D A V; Pudsey, C; Howe, J C; Faugères, J-C & Viana, A R (eds.), Deep-water contourite systems: modern drifts and ancient series, seismic and sedimentary characteristics. Geological Society of London, Memoirs, London, 22, 305-323, hdl:10013/epic.14690.d001
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Project(s):
Coverage:
Latitude: -74.074830 * Longitude: -27.690660
Date/Time Start: 1988-01-22T08:27:00 * Date/Time End: 1988-01-22T08:27:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.46 m
Event(s):
PS1599-1 (PS12/319) * Latitude: -74.074830 * Longitude: -27.690660 * Date/Time: 1988-01-22T08:27:00 * Elevation: -2482.0 m * Penetration: 0.49 m * Recovery: 0.49 m * Location: Halley Bay * Campaign: ANT-VI/3 (PS12) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Ice rafted debris, number of gravel | IRD | #/10 cm3 | Grobe, Hannes | IRD-Counting (Grobe, 1987) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
46 data points
Data
1 Depth sed [m] | 2 IRD [#/10 cm3] |
---|---|
0.01 | 0 |
0.02 | 0 |
0.03 | 1 |
0.04 | 1 |
0.05 | 0 |
0.06 | 2 |
0.07 | 1 |
0.08 | 1 |
0.09 | 0 |
0.10 | 0 |
0.11 | 1 |
0.12 | 0 |
0.13 | 0 |
0.14 | 0 |
0.15 | 2 |
0.16 | 2 |
0.17 | 3 |
0.18 | 1 |
0.19 | 4 |
0.20 | 3 |
0.21 | 3 |
0.22 | 3 |
0.23 | 2 |
0.24 | 2 |
0.25 | 4 |
0.26 | 4 |
0.27 | 2 |
0.28 | 2 |
0.29 | 3 |
0.30 | 2 |
0.31 | 1 |
0.32 | 1 |
0.33 | 0 |
0.34 | 0 |
0.35 | 2 |
0.36 | 0 |
0.37 | 0 |
0.38 | 0 |
0.39 | 1 |
0.40 | 0 |
0.41 | 0 |
0.42 | 2 |
0.43 | 2 |
0.44 | 1 |
0.45 | 2 |
0.46 | 0 |