Henderson, Gideon M (2002): (Table 2) U and Th concentrations and isotope ratios of ODP Site 166-1003 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.710923, In supplement to: Henderson, GM (2002): Seawater (234U/238U) during the last 800 thousand years. Earth and Planetary Science Letters, 199(1-2), 97-110, https://doi.org/10.1016/S0012-821X(02)00556-3
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 24.545967 * Longitude: -79.260750
Date/Time Start: 1996-02-28T00:00:00 * Date/Time End: 1996-02-28T00:00:00
Minimum DEPTH, sediment/rock: 75.65 m * Maximum DEPTH, sediment/rock: 76.87 m
Event(s):
166-1003 * Latitude: 24.545967 * Longitude: -79.260750 * Date/Time: 1996-02-28T00:00:00 * Elevation: -485.6 m * Penetration: 3140 m * Recovery: 694.6 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 172 cores; 1633.1 m cored; 1052.7 m drilled; 42.5% recovery
Comment:
sampled close to the Brunhes/Matuyama reversal
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
126 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 Sample label (DSDP/ODP/IODP sample designation) | 4 U [mg/kg] (conc, Multi-collector inducti...) | 5 U std dev [±] (conc, Multi-collector inducti...) | 6 δ234U [‰] (measured, Multi-collector ind...) | 7 δ234U [‰] (delta 234U(T)) | 8 δ234U std dev [±] (measured, Multi-collector ind...) | 9 δ234U std dev [±] (delta 234U(T)) | 10 (230Th/232Th) (Multi-collector inductively c...) | 11 (230Th/232Th) std dev [±] (Multi-collector inductively c...) | 12 (230Th/234U) (measured, Multi-collector ind...) | 13 (230Th/234U) (corrected) | 14 (230Th/234U) std dev [±] (measured, Multi-collector ind...) | 15 (230Th/234U) std dev [±] (corrected) | 16 U [%] (Det. U) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
75.65 | 780 | 166-1003B-9H-5,15-16 | 8.514 | 0.010 | 7.8 | 71.0 | 1.3 | 2.0 | 242.50 | 0.17 | 0.960 | 0.960 | 0.002 | 0.002 | 0.2 |
75.85 | 780 | 166-1003B-9H-5,35-36 | 7.643 | 0.009 | 10.9 | 99.0 | 1.3 | 2.0 | 218.21 | 0.15 | 0.987 | 0.987 | 0.002 | 0.002 | 0.0 |
76.05 | 780 | 166-1003B-9H-5,55-56 | 7.070 | 0.009 | 11.1 | 101.0 | 1.3 | 2.0 | 203.24 | 0.14 | 0.992 | 0.992 | 0.002 | 0.002 | 0.2 |
76.24 | 780 | 166-1003B-9H-5,74-75 | 7.173 | 0.009 | 8.4 | 76.0 | 1.3 | 2.0 | 200.52 | 0.14 | 0.976 | 0.976 | 0.002 | 0.002 | 0.2 |
76.45 | 780 | 166-1003B-9H-5,95-96 | 7.310 | 0.009 | 30.2 | 32.0 | 1.3 | 1.0 | 353.00 | 0.24 | 1.603 | 1.603 | 0.003 | 0.003 | 0.2 |
76.52 | 780 | 166-1003A-9H-3,10-11 | 8.485 | 0.011 | 9.6 | 87.0 | 1.3 | 2.0 | 245.50 | 0.17 | 0.995 | 0.995 | 0.002 | 0.002 | 0.2 |
76.62 | 780 | 166-1003A-9H-3,20-21 | 7.932 | 0.010 | 8.5 | 77.0 | 1.3 | 2.0 | 262.06 | 0.18 | 0.963 | 0.963 | 0.002 | 0.002 | 0.2 |
76.67 | 780 | 166-1003A-9H-3,25-26 | 8.278 | 0.017 | 7.2 | 65.0 | 1.3 | 2.0 | 240.43 | 0.17 | 1.027 | 1.027 | 0.002 | 0.002 | 0.1 |
76.87 | 780 | 166-1003A-9H-3,45-46 | 9.264 | 0.012 | 13.9 | 126.0 | 1.3 | 2.0 | 258.37 | 0.18 | 0.987 | 0.987 | 0.002 | 0.002 | 0.3 |