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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... -
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. -
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... -
(Appendix A3) Trace element and stable isotope measurements of surface sedime...
This dataset has no description
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Alkenone-derived Holocene Sea Surface Temperature database
see dating methoda: Correlation with GISP2 oxygen isotope record (Grootes and Stuiver, 1997).b: The age model of the core AD91-17 is based on AMS 14C, planktonic isotopic record... -
Summary of sea surface temperature trends reconstructed from alkenones for th...
Trend >0 means a warming over the time period, trend <0 means a cooling over the time period. -
Atlantic 231Pa/230Th and biogenic opal compilation of the Holocene and the LGM
The strength and geometry of the Atlantic meridional overturning circulation is tightly coupled to climate on glacial-interglacial and millennial timescales, but has proved... -
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
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... -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
Expanded GHOST database
In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of... -
Radionuclides, Nd isotopes and biogenic Opal in Atlanic Ocean sediments
Reconstructing past modes of ocean circulation is an essential task in paleoclimatology and paleoceanography. To this end, we combine two sedimentary proxies, Nd isotopes... -
Downcore Florisphaera profunda
This dataset has no description
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Multi-sensor global compilation of mid-Holocene (MH) sea surface temperatures...
This dataset has no description
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Occurrence of Globorotalia cavernula in the water column and sediments: globa...
Here, we present a global compilation of previously reported sightings of the rare planktic foraminifer Globorotalia cavernula Bé, 1967 as well as new observations of... -
Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
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'... -
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...