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PANGAEA.
Data Publisher for Earth & Environmental Science

Sinninghe Damsté, Jaap S; Ossebaar, Jort; Schouten, Stefan; Verschuren, Dirk (2012): TEX86 and BIT in Lake Challa sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.880141, In supplement to: Sinninghe Damsté, JS et al. (2012): Distribution of tetraether lipids in the 25-ka sedimentary record of Lake Challa: extracting reliable TEX86 and MBT/CBT palaeotemperatures from an equatorial African lake. Quaternary Science Reviews, 50, 43-54, https://doi.org/10.1016/j.quascirev.2012.07.001

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Coverage:
Latitude: -3.320000 * Longitude: 37.700000
Minimum Elevation: 880.0 m * Maximum Elevation: 880.0 m
Event(s):
Lake_Challa * Latitude: -3.320000 * Longitude: 37.700000 * Elevation: 880.0 m * Recovery: 21.65 m * Location: Mount Kilimanjaro, Tanzania * Method/Device: Piston corer, UWITEC (PCUWI)
Size:
248 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Age [ka BP]

TEX86

Ratio

BIT

GDGT-2 [%]
12.9440.641.090.640.43
13.1680.630.790.650.41
13.6200.641.130.630.42
13.9770.690.650.580.44
14.1640.640.620.580.41
15.7460.650.480.430.43
16.7590.590.310.310.43
16.9830.560.320.280.41
17.0930.520.440.370.36
17.2030.580.320.270.42
17.3140.590.310.300.44
17.4250.590.330.300.44
17.5360.570.380.330.43
17.6470.570.330.300.43
17.7600.570.290.310.42
17.8730.590.290.300.44
17.9860.550.350.300.40
18.1010.590.360.290.44
18.2160.550.430.320.40
18.3310.570.380.330.43
18.4460.560.390.360.43
18.5590.520.380.280.37
18.6710.520.460.340.38
18.7820.540.460.310.40
18.8890.560.410.350.42
18.9940.540.410.300.40
19.0980.540.490.330.40
19.2050.580.390.290.44
19.3160.480.500.330.33
19.4360.490.450.330.34
19.5660.490.490.370.34
19.7030.490.390.290.34
19.8420.480.510.340.33
19.9800.500.440.320.34
20.1130.490.700.390.32
20.2360.490.480.320.34
20.3460.500.430.330.34
20.4390.500.610.420.33
20.5120.501.650.670.32
20.5700.480.860.430.31
20.6190.481.130.570.31
20.6620.480.870.460.32
20.7050.491.160.550.32
20.7530.490.980.510.32
20.8100.500.950.440.33
20.8830.500.880.490.33
20.9740.490.780.420.33
21.0820.480.720.370.33
21.2070.480.770.420.32
21.3450.491.270.560.32
21.4940.490.800.470.32
21.6520.490.770.490.32
21.8170.500.650.400.33
21.9860.470.660.380.32
22.0710.490.960.570.32
23.2980.471.090.590.31
23.3440.460.750.440.31
23.4350.480.640.390.32
23.7110.490.820.470.32
24.1360.481.690.650.31
24.5860.491.180.600.32
24.8960.491.410.640.31