Meyer, Vera D; Hefter, Jens; Köhler, Peter; Tiedemann, Ralf; Gersonde, Rainer; Wacker, Lukas; Mollenhauer, Gesine (2019): Contents and fractional abundances of homohopane isomers in sediment core SO201-2-114KL [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.901959, In supplement to: Meyer, VD et al. (2019): Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming. Environmental Research Letters, 14(8), 085003, https://doi.org/10.1088/1748-9326/ab2653
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Coverage:
Latitude: 59.230660 * Longitude: 166.988830
Date/Time Start: 2009-09-25T02:21:00 * Date/Time End: 2009-09-25T03:17:00
Minimum DEPTH, sediment/rock: 0.250 m * Maximum DEPTH, sediment/rock: 2.450 m
Event(s):
Comment:
Missing values indicate where compounds were below detection limit.
Parameter(s):
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
81 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 C31bbR homohopane | 4 C31bbR homohopane/TOC [µg/g] | 5 C31bbR homohopane/sed [ng/g] | 6 C31baS + baR homohopanes/TOC [µg/g] | 7 C31baS + baR homohopanes/sed [ng/g] | 8 C31abS homohopane/TOC [µg/g] | 9 C31abS homohopane/sed [ng/g] | 10 C31abR homohopane/TOC [µg/g] | 11 C31abR homohopane/sed [ng/g] |
---|---|---|---|---|---|---|---|---|---|---|
0.250 | 10.01 | 0.75 | 49.160 | 675.930 | 6.397 | 87.960 | 5.713 | 78.550 | 9.990 | 137.350 |
0.750 | 11.38 | 0.72 | 40.140 | 529.080 | 5.611 | 73.960 | 6.105 | 80.460 | 9.900 | 130.440 |
1.000 | 12.60 | 0.61 | 53.000 | 496.610 | 11.991 | 112.350 | 16.035 | 150.250 | 21.920 | 205.420 |
1.140 | 13.21 | 0.67 | 45.410 | 499.010 | 7.628 | 83.830 | 10.104 | 111.040 | 14.780 | 162.390 |
1.500 | 14.58 | 0.52 | 28.750 | 344.980 | 7.638 | 91.660 | 15.826 | 189.910 | 18.630 | 223.500 |
1.750 | 15.32 | 0.38 | 26.240 | 314.850 | 11.552 | 138.620 | 30.315 | 363.770 | 30.930 | 371.140 |
1.910 | 15.74 | 0.46 | 25.800 | 286.630 | 8.220 | 91.330 | 20.000 | 222.200 | 22.550 | 250.500 |
2.000 | 16.02 | 0.67 | 36.070 | 278.830 | 6.267 | 48.450 | 7.734 | 59.790 | 11.830 | 91.480 |
2.450 | 17.14 | 0.70 | 20.770 | 155.380 | 3.161 | 23.640 | 3.638 | 27.210 | 5.650 | 42.230 |