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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... -
CLAM age model and pollen profile of sediment core MD03-2622
This dataset has no description
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Low field magnetic susceptibility in Holocene sediment cores MD99-2251 and MD...
Low field magnetic susceptibility normalized by the volume and measured on u-channels with a Bartington MS2C 45-mm diameter susceptibility bridge at 2 cm intervals with a... -
Low field magnetic susceptibility in Holocene sediment core MD03-2678Cq from ...
Low field magnetic susceptibility normalized by the volume and measured on u-channels with a Bartington MS2C 45-mm diameter susceptibility bridge at 2 cm intervals with a... -
LegacyPollen2.0: Overview of taxonomically harmonized pollen records
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... -
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... -
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. -
ACER pollen and charcoal database, links to single data sets
This dataset has no description
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(Table S3) Geochemical analyses of sediments from different Holes of ODP Site...
This dataset has no description
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Correlations between the proxy SST anomalies (annual, boreal summer and borea...
This dataset has no description
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Mg/Ca and Sr/Ca ratios of planktonic foraminifera from North Atlantic surface...
Reliable temperature estimates from both surface and subsurface ocean waters are needed to reconstruct past upper water column temperature gradients and past oceanic heat... -
Mean annual SST reconstruction by the UK'37 proxy for the Younger Dryas-Holoc...
The UK'37 sea surface temperature (SST) proxy, based on the distribution of long-chain akenones, was measured via mass spectrometry imaging (MSI) at 100-µm resolution in a 60-cm... -
Seasonal SST reconstruction by the UK'37 proxy for the Younger Dryas-Holocene...
The UK'37 sea surface temperature (SST) proxy, based on the distribution of long-chain akenones, was measured via mass spectrometry imaging (MSI) at 100-µm resolution in a 60-cm... -
Elemental geochemistry of sediment core MD03-2685
All elemental data were obtained with a X-Ray Fluorescence (XRF) core-scanner Avaatech 4th generation at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), and... -
Elemental geochemistry of sediment core MD03-2679
All elemental data were obtained with a X-Ray Fluorescence (XRF) core-scanner Avaatech 4th generation at the Laboratoire des Sciences du Climat et de l'Environnement (LSCE), and...
