Leduc, Guillaume; Schneider, Ralph R; Kim, Jung-Hyun; Lohmann, Gerrit (2010): Sea surface temperature reconstruction from sediment core MD97-2141 using Mg/Ca-ratios [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.736998, In supplement to: Leduc, G et al. (2010): Holocene and Eemian Sea surface temperature trends as revealed by alkenone and Mg/Ca paleothermometry. Quaternary Science Reviews, 29(7-8), 989-1004, https://doi.org/10.1016/j.quascirev.2010.01.004
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Coverage:
Latitude: 8.786000 * Longitude: 141.295000
Event(s):
MD97-2141 (MD972141) * Latitude: 8.786000 * Longitude: 141.295000 * Recovery: 36.3 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 | AGE | Age | ka BP | Geocode | ||
2 | Sea surface temperature | SST | °C | References, proxy Mg/Ca | SST from Mg/Ca ratios |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
76 data points
Data
1 Age [ka BP] | 2 SST [°C] |
---|---|
4.330 | 28.92 |
4.530 | 29.20 |
4.580 | 29.15 |
4.720 | 28.55 |
4.910 | 28.33 |
4.990 | 29.44 |
5.090 | 28.36 |
5.160 | 29.06 |
5.250 | 28.11 |
5.320 | 29.14 |
5.420 | 28.32 |
5.480 | 29.75 |
5.580 | 28.67 |
5.640 | 28.52 |
5.740 | 28.24 |
5.800 | 29.59 |
5.900 | 28.63 |
5.970 | 28.96 |
6.030 | 29.54 |
6.060 | 28.25 |
6.130 | 30.03 |
6.190 | 29.32 |
6.260 | 28.88 |
6.290 | 29.30 |
6.360 | 29.19 |
6.390 | 28.86 |
6.480 | 29.62 |
6.600 | 29.03 |
6.660 | 28.78 |
6.790 | 29.55 |
6.970 | 29.28 |
7.030 | 28.20 |
7.090 | 28.47 |
7.150 | 28.83 |
7.330 | 28.63 |
7.390 | 28.75 |
7.450 | 28.65 |
7.680 | 28.58 |
7.740 | 28.74 |
7.910 | 28.90 |
7.970 | 29.09 |
8.090 | 28.99 |
8.260 | 29.06 |
8.550 | 28.99 |
8.670 | 28.48 |
8.720 | 29.12 |
8.840 | 29.53 |
8.960 | 29.72 |
9.010 | 29.07 |
9.070 | 29.26 |
9.130 | 29.23 |
9.190 | 29.33 |
9.250 | 30.07 |
9.360 | 29.83 |
9.420 | 29.42 |
9.480 | 29.19 |
9.540 | 28.61 |
9.650 | 28.86 |
9.710 | 29.61 |
9.770 | 28.76 |
9.830 | 29.30 |
9.880 | 29.10 |
9.940 | 28.72 |
10.040 | 29.04 |
10.070 | 29.80 |
10.110 | 28.65 |
10.180 | 29.20 |
10.210 | 28.70 |
10.240 | 29.37 |
10.280 | 28.89 |
10.310 | 28.49 |
10.350 | 28.78 |
10.380 | 29.30 |
10.420 | 29.36 |
10.450 | 29.41 |
10.490 | 28.99 |