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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. -
(Table S1) Planktonic foraminifera abundances for the 1223 surface sediment s...
Our training set (SH0911C2, available from http://www.ncdc.noaa.gov/paleo/paleo.html) augments that used by Crundwell el al . [2008, Figure 2] with additional data from Mohtadi... -
Distribution of planktic foraminifera in surface sediments of the Atlantic Oc...
This dataset has no description
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Time slice 2 of planktic foraminifera of the last glacial maximum
This dataset has no description
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Sea surface temperatures of the last glacial maximum, GLAMAP
This dataset has no description
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Distribution of planktic foraminifera at the last glacial maximum
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... -
Database of the GLAMAP project
A uniform chronology for foraminifera-based sea surface temperature records has been established in more than 120 sediment cores obtained from the equatorial and eastern... -
Glacial North Atlantic: Sea surface conditions reconstructed by GLAMAP 2000
The response of the tropical ocean to global climate change and the extent of sea ice in the glacial nordic seas belong to the great controversies in paleoclimatology. Our new... -
Oxygen isotopic ratio of Globigerinoides ruber (white variety) in the surface...
The application of stable oxygen isotopic ratio of surface dwelling Globigerinoides ruber (white variety) (δ¹⁸Oruber) to reconstruct past hydrological changes requires precise... -
Sea surface temperatures in Drake Passage throughflow
This dataset has no description
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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... -
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'... -
(Table 4) Percentages of planktonic foraminiferal taxa from the 214 surface-s...
This dataset has no description
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Sea surface temperatures reconstructed from sediment core RC12-294
This dataset has no description
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Sea surface temperatures reconstructed from sediment core RC12-267
This dataset has no description
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Total organic carbon content in surface sediments, a compilation from differe...
This dataset has no description
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Sea surface temperatures calculated for 10 ka BP from planktic foraminifera
This dataset has no description