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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. -
Total organic carbon content in surface sediments, a compilation from differe...
This dataset has no description
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Compilation of planktonic foraminiferal census counts from the Southern Hemis...
We present an improved database of planktonic foraminiferal census counts from the Southern Hemisphere Oceans (SHO) from 15°S to 64°S. The SHO database combines 3 existing... -
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. -
Grain size analysis of surface sediments from the South Pacific Ocean
This dataset has no description
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Granulometry of surface sediments in 0.05 µm classes from the South Pacific O...
This dataset has no description
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Grain size fractions of surface sediments from the South Pacific Ocean
Silt and clay (%) represent the respective terrigenous weight fractions of dried bulk sediment. -
Clay mineralogy of surface sediments from the South Pacific Ocean
The relative clay-mineral contents (rel%) of illite, smectite, chlorite and kaolinite were determined semi-quantitatively by calculating the integrated peak areas of the... -
Sea surface temperature reconstructed from foraminifera in surface sediments ...
This dataset has no description
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(Table S1) Diatom abundance in coastal upwelling systems
Coastal upwelling systems account for approximately half of global ocean primary production and contribute disproportionately to biologically driven carbon sequestration.... -
Stable isotopes measured on foraminifera from the 120 kyr time slice reconstr...
This dataset has no description
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Clay mineraology and grain size composition of surface sediments from South P...
The reconstruction of low-latitude ocean-atmosphere interactions is one of the major issues of (paleo-)environmental studies. The trade winds, extending over 20° to 30° of... -
Foraminiferal faunal estimates of paleotemperature: Circumventing the no-anal...
The sensitivity of the tropics to climate change, particularly the amplitude of glacial-to-interglacial changes in sea surface temperature (SST), is one of the great... -
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'... -
120 kyr time slice reconstruction of sea surface temperature
This dataset has no description
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Stable isotope data of the 120 k time slice
This dataset has no description
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Paleotemperature calclulated for the 120 k time slice
This dataset has no description
