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Benthic foraminiferal assamblage in the 125-250 micron fraction of sediment c...
This dataset has no description
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Sedimentation rate and stable isotopes of sediment core GIK17728-1 (Table 1)
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Age model of sediment core GIK17728-2
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Geochemistry of surface sediment from the Norwegian-Greenland Sea
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Morphometry of planktonic foraminifera tests from surface sediment samples at...
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Global data compilation of benthic data sets II
In this study we present a global distribution pattern and budget of the minimum flux of particulate organic carbon to the sea floor (J POC alpha). The estimations are based on... -
Age determination of sediment cores from the Northeast Atlantic
Radiocarbon dating series, bulk sediment, and organic carbon flux from various Atlantic deep-sea regions reveal that the thickness of the bioturbated zone increases by 2 cm if... -
Sea surface temperatures and UK37 of three sediment cores from the Arctic Ocean
Sediment proxy data from the Norwegian, Greenland, and Iceland seas (Nordic seas) are presented to evaluate surface water temperature (SST) differences between Holocene and... -
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... -
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... -
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... -
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. -
Sea surface temperatures calculated for 10 ka BP from planktic foraminifera
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Sea surface temperatures calculated for today from planktic foraminifera
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Planktic foraminiferal assemblage for the 10kyr time slice from different sed...
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Atlantic sea surface temperatures during the last glacial maximum (LGM) time ...
This dataset has no description