Schimanski, Alexander; Stattegger, Karl (2005): Coarse fraction analysis of core GIK18408-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.96978, In supplement to: Schimanski, A; Stattegger, K (2005): Deglacial and Holocene evolution of the Vietnam shelf: stratigraphy, sediments and sea-level change. Marine Geology, 214(4), 365-387, https://doi.org/10.1016/j.margeo.2004.11.001
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Project(s):
Coverage:
Latitude: 14.239000 * Longitude: 109.317000
Date/Time Start: 1999-04-15T00:00:00 * Date/Time End: 1999-04-15T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 7.40 m
Event(s):
GIK18408-3 * Latitude: 14.239000 * Longitude: 109.317000 * Date/Time: 1999-04-15T00:00:00 * Elevation: -107.0 m * Recovery: 7.54 m * Location: South China Sea * Campaign: SO140A (SÜDMEER III) * Basis: Sonne * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Foraminifera, planktic | Foram plankt | % | Schimanski, Alexander | Counting 250-500 µm fraction | |
| 3 | Foraminifera, benthic | Foram benth | % | Schimanski, Alexander | Counting 250-500 µm fraction | |
| 4 | Shell debris | Shells | % | Schimanski, Alexander | Counting 250-500 µm fraction | |
| 5 | Rock fragments | Rock fragm | % | Schimanski, Alexander | Counting 250-500 µm fraction | |
| 6 | Plant fragments | Plants | % | Schimanski, Alexander | Counting 250-500 µm fraction | |
| 7 | Glauconite | Glt | % | Schimanski, Alexander | Counting 250-500 µm fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
60 data points
Data
| 1 Depth sed [m] | 2 Foram plankt [%] | 3 Foram benth [%] | 4 Shells [%] | 5 Rock fragm [%] | 6 Plants [%] | 7 Glt [%] |
|---|---|---|---|---|---|---|
| 0.10 | 10.2 | 6.0 | 73.6 | 0.0 | 10.2 | 0.0 |
| 0.60 | 7.2 | 12.9 | 76.4 | 0.0 | 3.4 | 0.0 |
| 1.10 | 12.0 | 13.0 | 67.9 | 0.0 | 7.0 | 0.0 |
| 1.60 | 10.8 | 11.7 | 70.3 | 0.6 | 2.5 | 4.1 |
| 2.40 | 8.4 | 11.1 | 72.8 | 0.0 | 3.1 | 4.6 |
| 3.40 | 2.8 | 11.1 | 25.0 | 26.9 | 34.3 | 0.0 |
| 4.40 | 8.7 | 12.0 | 9.8 | 49.7 | 19.7 | 0.0 |
| 5.40 | 1.2 | 23.5 | 18.5 | 29.6 | 27.2 | 0.0 |
| 6.40 | 8.0 | 18.0 | 58.0 | 8.0 | 8.0 | 0.0 |
| 7.40 | 0.7 | 8.6 | 12.9 | 52.9 | 25.0 | 0.0 |