Huang, Chen-Yue; Wu, Sheu-Feng; Zhao, Meixun; Chen, Min-Te; Wang, Chung-Ho; Tu, Xia; Yuan, Peter B (1997): (Table 4) SST, UK`37 alkenone index and C37 ketones concentration of sediment core SCS90-36 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.441529, In supplement to: Huang, C-Y et al. (1997): Surface ocean and monsoon climate variability in the south China Sea since last glaciation. Marine Micropaleontology, 32(1-2), 71-94, https://doi.org/10.1016/S0377-8398(97)00014-5
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Coverage:
Latitude: 17.995000 * Longitude: 111.494000
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 1.01 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Alkenone, unsaturation index UK'37 | UK'37 | Calculated, see reference(s) | |||
| 3 | Sea surface temperature, annual mean | SST (1-12) | °C | Calculated from UK'37 (Prahl et al., 1988) | ||
| 4 | Alkenone, C37:3+C37:2 | K37 | ng/g | see reference(s) | C37 ketones concentration |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
96 data points
Data
| 1 Depth sed [m] | 2 UK'37 | 3 SST (1-12) [°C] | 4 K37 [ng/g] |
|---|---|---|---|
| 0.01 | 0.937 | 26.4 | 700 |
| 0.05 | 0.915 | 25.8 | 620 |
| 0.08 | 0.919 | 25.8 | 461 |
| 0.11 | 0.920 | 25.9 | 527 |
| 0.14 | 0.885 | 24.8 | 396 |
| 0.19 | 0.851 | 23.9 | 612 |
| 0.20 | 0.921 | 25.9 | 543 |
| 0.23 | 0.928 | 26.1 | 571 |
| 0.26 | 0.917 | 25.8 | 479 |
| 0.29 | 0.917 | 25.8 | 495 |
| 0.32 | 0.917 | 25.8 | 541 |
| 0.35 | 0.899 | 25.2 | 592 |
| 0.38 | 0.887 | 24.9 | 600 |
| 0.41 | 0.888 | 24.9 | 635 |
| 0.44 | 0.863 | 24.2 | 575 |
| 0.47 | 0.853 | 23.9 | 1039 |
| 0.50 | 0.846 | 23.7 | 1225 |
| 0.53 | 0.838 | 23.4 | 1214 |
| 0.56 | 0.852 | 23.9 | 1082 |
| 0.59 | 0.845 | 23.7 | 949 |
| 0.62 | 0.826 | 23.1 | 973 |
| 0.65 | 0.823 | 23.0 | 1163 |
| 0.68 | 0.841 | 23.5 | 987 |
| 0.71 | 0.833 | 23.3 | 1442 |
| 0.74 | 0.818 | 22.9 | 909 |
| 0.77 | 0.819 | 22.9 | 869 |
| 0.80 | 0.825 | 23.1 | 889 |
| 0.86 | 0.803 | 22.4 | 1181 |
| 0.89 | 0.804 | 22.5 | 1220 |
| 0.92 | 0.833 | 23.3 | 1058 |
| 0.98 | 0.848 | 23.7 | 955 |
| 1.01 | 0.850 | 23.1 | 1126 |