Dataset - B2FIND

SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...

Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES.

Multi-sensor global compilation of mid-Holocene (MH) sea surface temperatures...

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List of cores with links to documentation datasets

This dataset has no description

Magnetic susceptibility and ice-rafted debris in surface sediments of the Nor...

Magnetic susceptibility and ice-rafted debris of surface sediments in the Nordic Seas were investigated to reconstruct source areas and recent transport pathways of magnetic...

Geochemistry on surface sediments from the Northern Atlantic and Arctic Ocean

Longitude of POS146/1 Events were corrected on 2023-11-14

Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...

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Susceptibility of surface sediments of the Nordic Seas

Please note: Lat/Long of POS137 Events was slightly corrected on 2020-07-30. Longitude of POS146/1 Events were corrected on 2023-11-14

Geochemical analysis of surface sediments from the ocean floor and from sea i...

Barium in marine terrigenous surface sediments of the European Nordic Seas is analysed to evaluate its potential as palaeoproductivity proxy. Biogenic Ba is calculated from Ba...

Mixed layer depth reconstructions based on dinocyst assemblage data of sedime...

Winter mixed layer depth (MLD) was reconstructed from the dinocyst assemblage data of sediment core GIK23323-1 using two different approaches: modern analogue technique (MAT)...

New size-normalised weight (SNW) data

This table includes the new SNW data produced for this manuscript. The foraminiferal weight data is normalized using the measurement-based weight (MBW) method of Barker (2002)....

Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)

Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES.

Annual SST estimates for the Last Interglacial (129-116 ka BP)

Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES.