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Hillaire-Marcel, Claude; Aksu, Ali E; Causse, Christiane; de Vernal, Anne; Ghaleb, Bassam (1990): (Table 1) Th and U concentrations and activity ratios in deep-sea sediments at ODP Hole 105-646B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711768

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Abstract:
The Labrador Sea is a particularly suitable high-latitude basin for investigating U and Th behavior in deep-sea sediments. During the late Quaternary, the cyclic development and decay of huge ice sheets on adjacent land masses resulted in large-amplitude changes in sedimentation rates and organic paleoproductivities. The resulting magnification of U and Th response is well illustrated by high-resolution studies on piston-cored sediments from the Greenland continental rise at Ocean Drilling Program Leg 105 Site 646 spanning isotopic stages 8 to 1. Our results show a clear positive correlation of 238U/232Th ratios with organic paleoproductivity indicators (e.g., dinocyst) due to U uptake in the water column and/or during the early early diagenesis of organic matter responding to carbon fluxes and to their climate forcing. 230Th excesses over 234U exceed the theoretical value of the 230Th rain from the overlying water column, indicating lateral input possibly from the Greenland slope and shelf. Because these horizontal fluxes of 230Th may be partly controlled by physical parameters, 230Th excesses cannot be unequivocally correlated with sedimentation rates and/or productivity as reported elsewhere. In this subarctic basin characterized by low overall organic carbon burial, the 238U/232Th ratio appears to be a sensible geochemical indicator of organic activity and paleoproductivity.
Related to:
Hillaire-Marcel, Claude; Aksu, Ali E; Causse, Christiane; de Vernal, Anne; Ghaleb, Bassam (1990): Response of Th/U in deep Labrador Sea sediments (ODP Site 646) to changes in sedimentation rates and paleoproductivities. Geology, 18(2), 162-165, https://doi.org/10.1130/0091-7613(1990)018%3C0162:ROTUID%3E2.3.CO;2
Project(s):
Coverage:
Latitude: 58.209300 * Longitude: -48.369100
Date/Time Start: 1985-10-04T08:45:00 * Date/Time End: 1985-10-13T21:01:00
Minimum Elevation: -3459.0 m * Maximum Elevation: -3459.0 m
Event(s):
105-646B * Latitude: 58.209300 * Longitude: -48.369100 * Date/Time Start: 1985-10-04T08:45:00 * Date/Time End: 1985-10-13T21:01:00 * Elevation: -3459.0 m * Penetration: 766.7 m * Recovery: 404.25 m * Location: Labrador Sea * Campaign: Leg105 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 80 cores; 766.2 m cored; 0 m drilled; 52.8 % recovery
Comment:
Age data have been obtained by interpolation between 18O stage boundaries.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1AGEAgeka BPGeocode
2Sample code/labelSample labelHillaire-Marcel, ClaudeDSDP/ODP/IODP sample designation
3Sample, optional label/labor noLab noHillaire-Marcel, Claude
4Thorium-232232Thmg/kgHillaire-Marcel, ClaudeAlpha spectrometry
5Thorium-232, standard deviation232Th std dev±Hillaire-Marcel, ClaudeCalculated
6Uranium-238238Umg/kgHillaire-Marcel, ClaudeAlpha spectrometry
7Uranium-238, standard deviation238U std dev±Hillaire-Marcel, ClaudeCalculated
8Uranium-234/Uranium-238 activity ratio(234U/238U)Hillaire-Marcel, ClaudeAlpha spectrometry
9Uranium-234/Uranium-238 activity ratio, standard deviation(234U/238U) std dev±Hillaire-Marcel, ClaudeCalculated
10Uranium-238/Thorium-232 ratio238U/232ThHillaire-Marcel, ClaudeAlpha spectrometry
11Uranium-238/Thorium-232 ratio error238U/232Th e±Hillaire-Marcel, ClaudeCalculated
12Thorium-230/Thorium-232 ratio230Th/232ThHillaire-Marcel, ClaudeAlpha spectrometry
13Thorium-230/Thorium-232 ratio error230Th/232Th e±Hillaire-Marcel, ClaudeCalculated
14Thorium-230/Uranium-234 activity ratio(230Th/234U)Hillaire-Marcel, ClaudeAlpha spectrometry
15Thorium-230/Uranium-234 activity ratio, standard deviation(230Th/234U) std dev±Hillaire-Marcel, ClaudeCalculated
16Age, errorAge e±Hillaire-Marcel, ClaudeCalculated
17Thorium-230230Thdpm/gHillaire-Marcel, ClaudeAlpha spectrometryexcess at the origin
Size:
352 data points

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