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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... -
Magnetic properties and sortable silt data from marine sedimentsfrom the Gard...
Magnetic properties coupled with sortable silt are investigated for Holocene marine sedimentary sequences located in the subpolar North Altantic, in the Charlie– Gibbs fracture... -
Sequence of seasonally to annually laminated diatomaceous sediment from sedim...
Diatoms account for a large proportion of primary productivity in Antarctic coastal and continental shelf zones. Diatoms, which have been used for a long time to infer past sea... -
Stable isotopes, radionuclides, and calculated sea surface temperature of two...
The Eastern Mediterranean Transient (EMT) occurred in the Aegean Sea from 1988 to 1995 and is the most significant intermediate-to-deep Mediterranean overturning perturbation... -
Model - data comparison of western African rainfall evolutions during the Las...
This dataset characterizes the evolution of western African precipitation indicated by marine sediment geochemical records in comparison to transient simulations using CCSM3... -
Diatoms and biomarkers in sediments from the Antarctic Peninsula
The Antarctic Peninsula (AP) has been identified as one of the most rapidly warming region on Earth. Satellite monitoring currently allows for a detailed understanding of the... -
Diatom assemblages, HBIs and TEXL86 in sediment core NBP99-03_10
The West Antarctic ice sheet is particularly sensitive to global warming and its evolution and impact on global climate over the next few decades remains difficult to predict.... -
Paleotemperatures and paleosalinities from the Celtic Margin (Bay of Biscay)
During the late Quaternary, both external and internal forcings have driven major climatic shifts from glacial to interglacial conditions. Nonlinear climatic steps characterized... -
Diatom biostratigraphy and sea ice concentration reconstruction from core DA0...
A diatom-based sea-ice concentration (SIC) transfer function is developed using 72 surface samples from west of Greenland and around Iceland, and through comparison with the... -
Number of laminae in sediment core MD95-2002, Celtic Margin
This dataset has no description
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Paleotemperatures and paleosalinities (10-35 ka BP) from sediment core MD95-2...
This dataset has no description
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Low field magnetic susceptibility in Holocene sediment core MD08-3182Cq 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... -
Low field magnetic susceptibility in Holocene sediment core CH77-02 from the ...
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... -
The mean sortable silt size in Holocene sediment core MD08-3182Cq from the Ga...
For measurements of the mean sortable silt size of the detrital faction, biogenic carbonates were dissolved using acetic acid (20 %) and the organic matter was removed using... -
20. Last Interglacial benthic foraminiferal stable isotopes from sediment cor...
AGE [ka BP] = Age [ka]; Benthic isotopic alignment to core MD95-2042 on AICC2012 time scale. -
17. Last Interglacial benthic foraminiferal stable isotopes from sediment cor...
AGE [ka BP] = Age [ka]; Benthic isotopic alignment to core MD95-2042 on AICC2012 time scale. -
14. Last Interglacial benthic foraminiferal stable isotopes from sediment cor...
AGE [ka BP] = Age [ka]; Benthic isotopic alignment to core MD95-2042 on AICC2012 time scale. -
5. Last Interglacial benthic foraminiferal stable isotopes from sediment core...
AGE [ka BP] = Age [ka], Benthic isotopic alignment to core MD95-2042 on AICC2012 time scale. -
10. Last Interglacial Al/Si log-ratio data from sediment core GeoB9528-3
Geocode AGE [ka BP] = Age [ka]; Median ages obtained from the Monte-Carlo analysis (to include dating uncertainties). -
8. Last Interglacial Al/Si log-ratio data from sediment core GeoB9516-5
Geocode AGE [ka BP] = Age [ka]; Median ages obtained from the Monte-Carlo analysis (to include dating uncertainties).
