Schimanski, Alexander; Stattegger, Karl (2005): Coarse fraction analysis of core GIK18417-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.96983, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: 14.746000 * Longitude: 109.293000
Date/Time Start: 1999-04-17T00:00:00 * Date/Time End: 1999-04-17T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 7.90 m
Event(s):
GIK18417-3 * Latitude: 14.746000 * Longitude: 109.293000 * Date/Time: 1999-04-17T00:00:00 * Elevation: -96.0 m * Recovery: 7.98 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:
48 data points
Data
| 1 Depth sed [m] | 2 Foram plankt [%] | 3 Foram benth [%] | 4 Shells [%] | 5 Rock fragm [%] | 6 Plants [%] | 7 Glt [%] |
|---|---|---|---|---|---|---|
| 0.10 | 5.7 | 11.3 | 69.7 | 13.4 | 0.0 | 0.0 |
| 1.10 | 3.7 | 14.0 | 73.8 | 1.0 | 7.5 | 0.0 |
| 2.10 | 4.1 | 7.9 | 75.4 | 0.0 | 12.6 | 0.0 |
| 3.50 | 3.0 | 3.4 | 55.0 | 0.0 | 38.7 | 0.0 |
| 4.50 | 2.8 | 5.0 | 41.4 | 0.0 | 50.8 | 0.0 |
| 5.70 | 1.3 | 2.6 | 39.7 | 0.0 | 56.4 | 0.0 |
| 7.00 | 0.4 | 4.4 | 52.2 | 0.0 | 43.0 | 0.0 |
| 7.90 | 0.0 | 5.4 | 28.3 | 0.0 | 66.4 | 0.0 |