Dataset - B2FIND

(Table 3) Age determination of sediment core GeoB6729-1

Analyses of Lophelia pertusa

(Table 3) Age determination of sediment core GeoB6728-1

Analyses of Lophelia pertusa

(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1009

U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in...

(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1008

U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in...

Protactinium, thorium, uranium and opal of sediment core GeoB1515

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(Table 1) U and Th isotopic composition and 230Th ages of samples from the A1...

The 14C reservoir age of the surface ocean was determined for two Holocene periods (4908-4955 and 3008-3066 calendar (cal) B.P.) using U/Th-dated corals from Biscayne National...

(Appendix) Th, U and Pa chemistry of North Atlantic deep-sea sediments

The Atlantic Meridional Overturning Circulation (AMOC) is a key feature of the climate system. However, its role during climate change is still poorly constrained particularly...

Dissolved Pa-231, Th-230, and Th-232 in the Western N-Atlantic during the exp...

Five water column profiles were sampled under trace metal clean conditions during the expedition of RV Pelagia (GEOTRACES Cruise A02) on a transect following the North Atlantic...

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...

(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...