Frank, Martin; Gersonde, Rainer; Rutgers van der Loeff, Michiel M; Kuhn, Gerhard; Mangini, Augusto (1996): Sedimentation rate and radionuclides of sediment core PS2082-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.50868, In supplement to: Frank, M et al. (1996): Late Quaternary sediment dating and quantification of lateral sediment redistribution applying 230Th-excess, a study of the eastern Atlantic sector of the Southern Ocean. Geologische Rundschau, 85(3), 554-566, https://doi.org/10.1007/BF02369010
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Project(s):
Marine Geochemistry @ AWI (AWI_MarGeoChem)
Coverage:
Latitude: -43.218167 * Longitude: 11.759000
Date/Time Start: 1991-04-03T18:40:00 * Date/Time End: 1991-04-03T18:40:00
Minimum DEPTH, sediment/rock: 0.033 m * Maximum DEPTH, sediment/rock: 0.177 m
Event(s):
PS2082-3 (PS18/238) * Latitude: -43.218167 * Longitude: 11.759000 * Date/Time: 1991-04-03T18:40:00 * Elevation: -4611.0 m * Recovery: 0.26 m * Location: Agulhas Basin * Campaign: ANT-IX/4 (PS18) * Basis: Polarstern * Method/Device: MultiCorer (MUC) * Comment: 11 Rohre
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
42 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Age model [ka] (calculated ages, Calculated) | 5 DBD [g/cm3] | 6 230Th xs [dpm/g] (uncorrected, Alpha spectrometry) | 7 230Th xs [dpm/g] (decay corrected, Alpha spectr...) | 8 230Th xs std dev [±] (uncorrected, Alpha spectrometry) | 9 230Th xs std dev [±] (decay corrected, Alpha spectr...) | 10 SR [cm/ka] (Calculated) | 11 SR std dev [±] (Calculated) | 12 MAR [g/cm2/ka] (Calculated) | 13 MAR std dev [±] (Calculated) | 14 Rain rate [g/cm2/ka] | 15 Rain rate std dev [±] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.033 | 0.000 | 0.065 | 1.30 | 0.43 | 31.6 | 32.0 | 0.41 | 0.42 | 2.50 | 0.03 | 1.08 | 0.01 | 0.38 | 0.00 |
0.105 | 0.065 | 0.145 | 4.29 | 0.58 | 24.2 | 25.2 | 0.35 | 0.36 | 2.37 | 0.03 | 1.37 | 0.02 | 0.48 | 0.01 |
0.177 | 0.145 | 0.210 | 6.87 | 0.62 | 14.3 | 15.2 | 0.53 | 0.56 | 3.64 | 0.13 | 2.26 | 0.08 | 0.80 | 0.03 |