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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. -
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. -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
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'... -
Global compilation of benthic data sets I, supplement to: Seiter, Katherina; ...
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Bulk sedimentological parameters of surface sediment samples from the Mid-Atl...
This dataset has no description
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Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean, s...
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle... -
Bulk sedimentological parameters of sediment core GeoB2215-10, representing t...
The time interval of the LGM was fixed at 19-23 ka B.P. (calendar years). -
Bulk sedimentological parameters of surface samples, representing the Holocene
All surface samples are assumed to be of Holocene age. -
Downcore Florisphaera profunda
This dataset has no description
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(Table S1, Figure 2) Sedimentation rates for 108 sediment core sites during t...
The SR errors in Fig.2 are given by the averaged values of 'Error [+, 97.5%]' and 'Error [-, 2.5%]'.The calculation focused on 19-21 ka since the age model did not cover the... -
Peak flux time (day of year) for all species for each sediment trap time series
NA means no significant periodic component in the flux. -
Peak prominence for all species at all time series
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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Carbon and silica particle flux data compiled from different sources
This dataset has no description
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Global temperature calibration of the Long chain Diol Index in marine surface...
0 = coel.; *0 = not available.Note 1: If there was no salinity data (WOA13) available for a certain core-top location, and there was also no LDI or C32 1,15-diol fractional... -
Environmental controls on the Emiliania huxleyi calcite mass, supplement to: ...
Although ocean acidification is expected to impact (bio)calcification by decreasing the seawater carbonate ion concentration, [CO3]2-, there exists evidence of non-uniform... -
Compilation of downward flux observations from sediment trap deployments in t...
We provide a compilation of downward fluxes (total mass, POC, PON, BSiO2, CaCO3, PIC and lithogenic/terrigenous fluxes) from over 6000 sediment trap measurements distributed in... -
Particle fluxes for the sampling interval, various ratios and major nutrients...
This dataset has no description