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Last Glacial Maximum (LGM) paleo-dust record
This dataset has no description
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Pre-industrial Holocene (pi-HOL) paleo-dust record
This dataset has no description
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Deglacial diatom silicon isotope record from the sediment core MD88-773
This dataset has no description
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Deglacial diatom silicon isotope record from the sediment core MD88-772
This dataset has no description
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Relative abundance of organic-walled dinoflagellate cysts in surface sediments
This dataset has no description
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Sedimentology and susceptibility of core MD88-791
This dataset has no description
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Sedimentology and susceptibility of core MD88-787
This dataset has no description
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Sedimentology and susceptibility of core MD88-772
This dataset has no description
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Sedimentology and susceptibility of core MD88-770
This dataset has no description
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Sedimentology and susceptibility of core MD88-769
This dataset has no description
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Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
Detriral flux of sediment cores in the southeast Indian Ocean
Because of a close relationship between detrital flux variations and magnetic susceptibility (MS) flux (MS cm**3 of bulk sediment multiplied by the linear sedimentation rate)... -
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... -
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. -
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... -
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... -
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...
