Seki, Osamu; Kawamura, Kimitaka; Ikehara, Minoru; Nakatsuka, Takeshi; Oba, Tadamichi (2004): Age and sea surface temperature from sediment core KT94-15_PC-9 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.802148, In: Seki, O et al. (2004): Sea surface temperature and age analysis from sediment core KT94-15_PC-9, XP98-PC-4 and XP98-PC-2 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.802171
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Ishiwatari, Ryoshi; Houtatsu, M; Okada, H (2001): Alkenone-sea surface temperatures in the Japan Sea over the past 36 kyr: warm temperatures at the last glacial maximum. Organic Geochemistry, 32(1), 57-67, https://doi.org/10.1016/S0146-6380(00)00151-0
Seki, Osamu; Kawamura, Kimitaka; Ikehara, Minoru; Nakatsuka, Takeshi; Oba, Tadamichi (2004): Variation of alkenone sea surface temperature in the Sea of Okhotsk over the last 85 kyrs. Organic Geochemistry, 35(3), 347-354, https://doi.org/10.1016/j.orggeochem.2003.10.011
Coverage:
Latitude: 39.572700 * Longitude: 139.406800
Minimum Elevation: -807.0 m * Maximum Elevation: -807.0 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | AGE | Age | ka BP | Geocode | ||
| 2 | Sea surface temperature | SST | °C | Seki, Osamu | Calculated from UK37 (Prahl et al., 1988) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
47 data points
Data
| 1 Age [ka BP] | 2 SST [°C] |
|---|---|
| 0.260 | 16.2 |
| 0.790 | 17.0 |
| 1.320 | 15.8 |
| 1.850 | 17.1 |
| 2.370 | 15.5 |
| 2.900 | 17.1 |
| 3.430 | 16.1 |
| 3.960 | 16.5 |
| 4.480 | 16.1 |
| 5.010 | 15.4 |
| 5.540 | 16.4 |
| 6.070 | 17.1 |
| 6.600 | 18.3 |
| 7.120 | 17.6 |
| 7.650 | 18.0 |
| 8.180 | 18.2 |
| 9.060 | 17.3 |
| 9.590 | 17.0 |
| 10.100 | 15.8 |
| 11.000 | 14.0 |
| 11.500 | 13.3 |
| 11.700 | 14.0 |
| 12.100 | 11.8 |
| 12.900 | 12.9 |
| 13.800 | 12.2 |
| 14.700 | 13.3 |
| 15.600 | 13.2 |
| 16.400 | 15.8 |
| 17.200 | 18.9 |
| 17.500 | 19.1 |
| 18.000 | 17.6 |
| 18.800 | 19.0 |
| 19.300 | 19.0 |
| 20.200 | 17.0 |
| 20.600 | 18.0 |
| 22.000 | 18.0 |
| 22.300 | 17.2 |
| 23.100 | 18.3 |
| 23.900 | 18.2 |
| 26.400 | 17.2 |
| 28.100 | 18.4 |
| 29.800 | 18.8 |
| 31.800 | 17.0 |
| 32.500 | 14.5 |
| 34.400 | 15.6 |
| 36.100 | 11.9 |
| 36.900 | 13.6 |