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Mean morphological measurements of Amphimelissa setosa in plankton, surface s...
BEA: Beaufort Sea; BER: Bering Sea; CHU: Chukchi Sea; ECS: East China Sea; ESS: East Siberian Sea; GOA: Gulf of Alaska; GRE: Greenland Sea; ICE: Iceland Sea; NOR: Norwegian Sea;... -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
Grain-size distribution in surficial seafloor sediments of Eurasian Arctic seas
This dataset has no description
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(Table A2) Geochemistry of sediments of the ash zone from middle substage 5e
This dataset has no description
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(Table A1) Geochemistry of sediments of the ash zone from substage 5d
This dataset has no description
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Clay mineralogy and sedimentology of surface sediments from the Norwegian Sea...
This dataset has no description
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Clay mineral distribution of surface sediments from the Fram Strait, the Arct...
Relative area percentage -
Stable isotope data and calculated sea surface temperature in surface sediment
This dataset has no description
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Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
Geochemistry of sediments of stage 5 of the Nordic seas
Stable isotope, foraminifera and ice rafted detritus (IRD) records covering the last interglacial (the Eemian) from 7 sediment cores in a transect from the Norwegian to the... -
Age models and stable isotopes of sediment cores from the northern seas
Oxygen and carbon isotope measurements were carried out on tests of planktic foraminifers N. pachyderma (sin.) from eight sediment cores taken from the eastern Arctic Ocean, the... -
Clay minerals in the Norwegian Sea and Fram Strait, investigation from sedime...
The grain size distribution and clay mineral composition of lithogenic particles of ice-rafted material, sinking matter, surface sediments, as well as from deep-sea cores are...