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Geochemical ratio ln(Zr/Rb) from core MD03-2679
The geochemical ratio ln(Zr/Rb) was analyzed in the core MD03-2679 located in the North Atlantic. The geochemical proxy ln(Zr/Rb) is used as grain-size proxy free of ice-rafted... -
Sortable silt data from core MD03-2679
Sortable silt data was obtained from core MD03-2679 located in the North Atlantic. The sediment was analysed with a laser diffractometer at GEOsciences Paris-Sud (GEOPS), in... -
Geochemical ratio ln(Zr/Rb) from core MD03-2673
The geochemical ratio ln(Zr/Rb) was analyzed in the core MD03-2673 located in the North Atlantic. The geochemical proxy ln(Zr/Rb) is used as grain-size proxy free of ice-rafted... -
Sortable silt data from core MD03-2673
Sortable silt data was obtained from core MD03-2673 located in the North Atlantic. The sediment was analysed with a laser diffractometer at Bio-Indicateurs Actuels et Fossiles... -
LegacyPollen2.0: Taxonomically harmonized pollen percentages of South America...
This data set consists of the taxonomically harmonized and temporally standardized fossil pollen data from 3680 records. 1122 records are located in North America, 1446 records... -
LegacyPollen2.0: Taxonomically harmonized pollen counts of South American sam...
This data set consists of the taxonomically harmonized and temporally standardized fossil pollen data from 3680 records. 1122 records are located in North America, 1446 records... -
Annual SST estimates from the late Marine Isotope Stage 6 (140-135 kyr) and c...
This dataset has no description
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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. -
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. -
SST estimates for the Last Interglacial (129-116 ka BP) during the months of ...
Note, that we have assumed a thermal equator of 5 degrees North, where sites above this latitude 'Summer' = JJA, and 'Winter' = DJF. Sites south of this line have 'Summer'... -
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. -
Ba/Ca ratios of N. pachyderma (s) from sediment core MD03-2664
This dataset has no description
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Stable isotope ratios of C. wuellerstorfi from sediment core MD03-2664
This dataset has no description
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CLAM age model and pollen profile of sediment core MD03-2622
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... -
Physical properties of sediment core MD03-2621
This dataset has no description
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Physical properties of sediment core MD03-2622
This dataset has no description
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Physical properties of sediment core MD03-2681
This dataset has no description
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Physical properties of sediment core MD03-2667G
This dataset has no description
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Physical properties of sediment core MD03-2663
This dataset has no description
