Schimanski, Alexander; Stattegger, Karl (2005): Coarse fraction analysis of core GIK18376-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.96968, 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: 7.087000 * Longitude: 108.107000
Date/Time Start: 1999-04-09T00:00:00 * Date/Time End: 1999-04-09T00:00:00
Minimum DEPTH, sediment/rock: 0.30 m * Maximum DEPTH, sediment/rock: 4.50 m
Event(s):
GIK18376-2 * Latitude: 7.087000 * Longitude: 108.107000 * Date/Time: 1999-04-09T00:00:00 * Elevation: -89.0 m * Recovery: 4.77 m * Location: South China Sea * Campaign: SO140A (SÜDMEER III) * Basis: Sonne * Method/Device: Vibro corer (VC)
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 [%] |
|---|---|---|---|---|---|---|
| 0.30 | 16.4 | 5.5 | 31.3 | 46.1 | 0.8 | 0.0 |
| 0.75 | 7.6 | 7.0 | 22.1 | 60.8 | 2.5 | 0.0 |
| 1.30 | 1.1 | 0.5 | 5.4 | 74.1 | 18.9 | 0.0 |
| 1.80 | 0.0 | 0.0 | 0.2 | 60.4 | 39.4 | 0.0 |
| 2.30 | 0.0 | 0.0 | 0.7 | 76.0 | 23.3 | 0.0 |
| 2.60 | 0.0 | 0.0 | 1.7 | 69.4 | 28.9 | 0.0 |
| 3.40 | 0.0 | 0.3 | 6.2 | 87.9 | 5.6 | 0.0 |
| 3.75 | 0.0 | 0.0 | 0.8 | 98.5 | 0.7 | 0.0 |
| 4.25 | 0.8 | 0.8 | 5.7 | 59.5 | 33.3 | 0.0 |
| 4.50 | 2.3 | 4.6 | 53.9 | 38.3 | 0.9 | 0.0 |