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Data Publisher for Earth & Environmental Science

Griffiths, James D; Barker, Stephen; Hendry, Katharine R; Thornalley, David J R; van de Flierdt, Tina; Hall, Ian R; Anderson, Robert F (2013): (Table S3) Radionuclides of sediment core RC24-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.822025, In supplement to: Griffiths, JD et al. (2013): Evidence of silicic acid leakage to the tropical Atlantic via Antarctic Intermediate Water during Marine Isotope Stage 4. Paleoceanography, 28(2), 307-318, https://doi.org/10.1002/palo.20030

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Coverage:
Latitude: 0.563000 * Longitude: -13.650000
Date/Time Start: 1983-03-19T00:00:00 * Date/Time End: 1983-03-19T00:00:00
Minimum DEPTH, sediment/rock: 2.845 m * Maximum DEPTH, sediment/rock: 3.735 m
Event(s):
RC24-1 * Latitude: 0.563000 * Longitude: -13.650000 * Date/Time: 1983-03-19T00:00:00 * Elevation: -3850.0 m * Recovery: 7.68 m * Campaign: RC24 * Basis: Robert Conrad * Method/Device: Piston corer (PC) * Comment: depth uncertain
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
AGEAgeka BPGeocode
Opal, biogenic silicabSiO2%Griffiths, James D
Accumulation rate, massMARg/cm2/kaGriffiths, James D230Th norm
Accumulation rate, standard deviationAcc rate std dev±Griffiths, James D230Th norm
Uranium, authigenicU authdpm/gGriffiths, James D
Uranium, standard deviationU std dev±Griffiths, James D
Size:
60 data points

Data

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


Depth sed [m]

Age [ka BP]

bSiO2 [%]

MAR [g/cm2/ka]

Acc rate std dev [±]

U auth [dpm/g]

U std dev [±]
2.84560.926.651.2590.0230.8800.012
2.93562.888.401.2200.0291.2570.017
3.02564.847.781.2700.0351.7810.026
3.10566.5810.591.0620.0382.6440.034
3.18568.3210.381.2050.0402.8180.039
3.25569.848.941.2390.0472.0460.027
3.33571.597.091.3210.0501.4860.020
3.44574.974.621.3320.0531.2980.018
3.51578.045.321.2990.0451.0970.017
3.53578.924.951.3310.0370.7780.013
3.65584.183.671.4030.0430.3040.005
3.73587.163.731.5380.0410.1330.002