Dataset - B2FIND

Sea surface temperatures reconstructed from sediment core GIK17050-1

This dataset has no description

Radiogenic Nd isotope signatures of marine sediments (bulk and detrital) and ...

This dataset includes the results of the analysis of a set of surface sediment samples recovered from the Labrador Sea. Analysis includes measurement of the radiogenic Nd...

(Table 1) Age determination and sedimentation rates of surface sediments of t...

This dataset has no description

Age control of sediment core GIK17049-6

dry bulk density measurements (K. Winn, unpubl.); d18O values of G. bulloides have been corrected by 0.4 per mill because of a systematic measurement deviation (K. Winn,...

Age control of sediment core GIK17050-2

Abudant ice rafted debris between 345-392 cm; d18O/d13C minimum at 465 cm is expected to correlete with laminated layers at 226-270 cm in 17049-6

Age control of sediment core GIK17051-3

This dataset has no description

Age control of sediment core GIK17050-1

Abudant ice rafted debris between 345-392 cm; d18O/d13C minimum at 465cm is expected to correlete with laminated layers at 226-270 cm in 17049-6

Age control of sediment core GIK17045-3

Corg + DBD data (Sarnthein et al., 1989; K. Winn, unpubl.); volc. glass shards (colorless, rhyolite variety: Vedde ash) sporadic at 48 cm, decreasing towards 40 cm (rare); black...

Age control of sediment core GIK17045-2

Corg and DBD data (Sarnthein et al., 1989; K. Winn, unpubl.); Volc. glass shards (colorless, rhyolite variety: Vedde ash) sporadic at 48 cm; decreasing towards 40 cm (rare)....

Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean

We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle...

Last Glacial Maximum seawater temperature estimates based on planktonic foram...

Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS...