Wei, Kuo-Yen; Chiu, Tzu-Chien; Chen, Yue-Gau (2003): (Table 1) Age determination in sediment core MD97-2142 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.740011, Supplement to: Wei, K-Y et al. (2003): Toward establishing a maritime proxy record of the East Asian summer monsoons for the late Quaternary. Marine Geology, 201(1-3), 67-79, https://doi.org/10.1016/S0025-3227(03)00209-3
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Published: 2003 (exact date unknown) • DOI registered: 2010-07-08
Abstract:
An astronomically tuned late Quaternary planktic foraminiferal delta18O record of Site MD972142 (12°41.33'N, 119°27.90'E; 1557 m water depth) in the southeastern South China Sea was established. The difference in delta18O between MD972142 and ODP792 of the Sulu Sea is regarded as a maritime proxy of the summer monsoon intensity over the South China Sea and Southeast Asia. The profile of this maritime proxy matches well with the summer monsoon index obtained from the terrestrial record of Louchuan, central Chinese Loess Plateau. The amplified planktic delta18O signals of the South China Sea relative to the Sulu Sea record are partly caused by the changing intensities of the East Asian Monsoons at the glacial-interglacial time-scale throughout the late Quaternary.
Project(s):
Coverage:
Latitude: 12.685000 * Longitude: 119.465000
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 35.61 m
Event(s):
MD97-2142 (MD972142) * Latitude: 12.685000 * Longitude: 119.465000 * Recovery: 35.91 m * Campaign: MD106 (IMAGES III - IPHIS) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Wei, Kuo-Yen | ||
| 3 | Age, comment | Comm | Wei, Kuo-Yen |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
110 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.01 | 1 | AMS14C |
| 0.69 | 5 | AMS14C |
| 1.45 | 6 | |
| 2.01 | 12 | AMS14C |
| 2.25 | 14 | AMS14C |
| 2.41 | 16 | |
| 2.97 | 21 | AMS14C |
| 4.25 | 34 | |
| 6.01 | 52 | MIS3.1 |
| 6.75 | 64 | |
| 7.47 | 80 | MIS5.1 |
| 8.13 | 94 | |
| 8.65 | 106 | MIS5.4 |
| 8.93 | 122 | MIS5.5 |
| 9.29 | 128 | MIS6.0 |
| 9.95 | 136 | |
| 10.34 | 148 | |
| 10.56 | 156 | |
| 11.04 | 166 | |
| 11.40 | 176 | |
| 11.72 | 194 | MIS7.1 |
| 13.47 | 214 | MIS7.3 |
| 13.79 | 224 | MIS7.4 |
| 14.19 | 234 | |
| 14.93 | 250 | |
| 15.89 | 266 | MIS8.4 |
| 16.63 | 288 | MIS8.5 |
| 17.05 | 296 | MIS8.6 |
| 17.78 | 316 | MIS9.2 |
| 18.38 | 328 | MIS9.3 |
| 18.96 | 342 | |
| 19.24 | 348 | MIS10.3 |
| 19.74 | 358 | |
| 20.42 | 370 | MIS11.1 |
| 20.90 | 384 | MIS11.23 |
| 21.26 | 392 | |
| 22.21 | 420 | |
| 22.56 | 434 | MIS12.2 |
| 22.84 | 452 | |
| 24.25 | 482 | MIS13.11 |
| 24.41 | 492 | MIS13.12 |
| 24.57 | 500 | MIS13.13 |
| 24.89 | 510 | MIS13.2 |
| 25.29 | 524 | MIS13.3 |
| 25.89 | 536 | MIS14.2 |
| 27.13 | 574 | MIS15.1 |
| 27.77 | 596 | |
| 28.09 | 604 | MIS15.4 |
| 28.57 | 616 | MIS15.5 |
| 28.81 | 624 | |
| 29.21 | 630 | |
| 29.29 | 644 | |
| 29.61 | 662 | |
| 30.33 | 690 | |
| 30.73 | 702 | |
| 31.21 | 710 | |
| 31.53 | 718 | MIS18.2 |
| 31.93 | 730 | MIS18.3 |
| 32.65 | 754 | MIS18.4 |
| 33.29 | 766 | MIS19.1 |
| 33.85 | 780 | |
| 34.17 | 792 | MIS20.2 |
| 34.49 | 796 | |
| 34.65 | 808 | |
| 34.73 | 820 | MIS21.1 |
| 34.89 | 828 | MIS21.2 |
| 35.05 | 838 | MIS21.3 |
| 35.37 | 848 | MIS21.4 |
| 35.61 | 858 | MIS21.5 |