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Global marine radiocarbon data compilation for the last deglaciation, spline ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, global ...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation, zonal a...
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
Global marine radiocarbon data compilation for the last deglaciation
Compiled marine radiocarbon data from the global ocean, derived from planktonic/benthic foraminifera and corals, spanning the last deglaciation, with associated calendar ages... -
δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
List of cores with links to documentation datasets
This dataset has no description
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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. -
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 ...
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. -
Age-depth model of sediment core GIK23415-9 and associated dating uncertainty
Undatable run on 2019-01-09 15:31:26. nsim=10000 bootpc=10 xfactor=0.1 combine=Yes -
A summary of consistently dated Atlantic sediment cores over the last 40 thou...
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear... -
Metadata for a compilation of 127 benthic δ¹³C time series (20-6 ka)
Abbreviations for ocean and sea regionsINA: intermediate North Atlantic OceanUDNA: upper deep North Atlantic OceanLDNA: lower deep North Atlantic OceanISA: intermediate South... -
Sea surface temperature estimates from several sediment cores in the North At...
Here, we have calculated new sea-surface temperature estimates over Dansgaard-Oeschger (DO) events 5-8 (c. 30-40 ka) from 14 sites in the North Atlantic, based on previously... -
(Table A4) Stable isotope and Cd/Ca ratios of benthic foraminifera of sedimen...
Isotope analyses from Jung (1996) and 14C age model from Sarnthein et al. (1994). -
Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 fo...
Compilation of planktonic foraminiferal census data for Heinrich Stadial 1 of those five species modeled by PLAFOM, i.e., N. pachyderma, N. incompta, G. bulloides, G. ruber... -
Correlations between the proxy SST anomalies (annual, boreal summer and borea...
This dataset has no description
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Sea surface temperatures reconstructed from sediment core GIK23419-8
This dataset has no description
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Sea surface temperatures reconstructed from sediment core GIK23415-9
This dataset has no description
