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(Table 1) Radioisotopic data of bulk sediment from ODP Hole 130-806C
Chronology is taken from Berger et al (1994, doi:10.1130/0091-7613(1994)022<0463:QTSFTO>2.3.CO;2). Mapping of depths between Site 130-806 Holes B and C is taken from Lyle... -
High resolution paleocirculation records from the Bermuda Rise for the past 1...
We present a compilation of paleo-circulation proxies during the Holocene from Bermuda Rise core ODP Site 1063. The data set comprises high resolution 231Pa/230Th (including... -
Age, 232Th, 230Th, 238U, CaCO3, organic carbon, lithogenic fraction, opal, an...
Increased export production (EP) in the Subantarctic Zone (SAZ) of the Southern Ocean due to iron fertilisation has been proposed as a key mechanism for explaining carbon... -
Radionuclides, Nd isotopes and biogenic Opal in Atlanic Ocean sediments
Reconstructing past modes of ocean circulation is an essential task in paleoclimatology and paleoceanography. To this end, we combine two sedimentary proxies, Nd isotopes... -
(Table 1) Radionuclide content in ODP Hole 108-658C
Using a high-resolution 230Th normalized record of sediment flux, we document the deglacial and Holocene history of North African aridity and coastal upwelling at Ocean Drilling... -
Uranium, Thorium and Protactinium isotopes of ODP Site 172-1063
Ocean circulation may have undergone reductions and reinvigorations in the past closely tied to regional climate changes. Measurements of 231Pa/230Th ratios in a sediment core... -
Uranium and strontium concentrations of ODP Hole 117-722B (Appendix B)
High resolution sampling of the upper 10 m of Hole 722B has provided information on the extent of 234U/230Th disequilibrium in Owen Ridge sediments accumulating over the last... -
U and Th concentrations and U-TH ages for bulk carbonate samples from ODP Hol...
Thirty-one new bulk-sediment U–Th dates are presented, together with an improved d18O stratigraphy, for ODP Site 1008A on the slopes of the Bahamas Banks. These ages supplement... -
(Table 1) Th and U concentrations and activity ratios in deep-sea sediments a...
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... -
(Table 1) Radionuclides in the water column at station PS1777-8
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(Table 1) Radionuclides in the water column at station PS1768-2
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(Table 1) Radionuclides in the water column at station PS1759-5
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(Table 1) Radionuclides in the water column at station PS1755-2
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(Table 1) Radionuclides in the water column at station PS1751-8
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(Table 5.3) Contents of calcium carbonate, iron, uranium and thorium isotopes...
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(Table 1) Radionuclides in the water column at station PS18/227
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(Table 1) Radionuclides in the water column at station PS1785-1
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(Table 1) Radionuclides in the water column at station PS1782-7
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(Table 1) Radionuclides in the water column at station PS1772-2
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Radionuclides of sediment core GeoB16202-2
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