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230Th dating results of Schrattenkarst speleothem
U decay constants: l238 = 1.55125x10-10 (Jaffey et al., 1971) and l234 = 2.82206x10-6 (Cheng et al., 2013). Th decay constant: l230 = 9.1705x10-6 (Cheng et al., 2013).o account... -
Stable carbon and oxygen isotope ratios of Speleothem M37-1-23A
This dataset has no description
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Stable carbon and oxygen isotope ratios of Speleothem M37-1-16C
This dataset has no description
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Stable carbon and oxygen isotope ratios of Speleothem M37-1-16A
This dataset has no description
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Stable carbon and oxygen isotope ratios of Speleothem M6-73-3
This dataset has no description
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Sea ice-related diatoms of sediment core PS67/219-1
This dataset has no description
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Sea ice-related diatoms of sediment core PS118_63-1
This dataset has no description
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Organic geochemistry and biomarkers of sediment core PS118_63-1
This dataset has no description
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MIS 5e Southern Ocean September sea-ice concentrations and summer sea-surface...
Marine Isotope Stage (MIS) 5e is the latest period when global atmospheric temperatures were warmer than present and global sea levels were higher than present. Environmental... -
Sea-ice distribution and ocean temperature variation in the Powell Basin and ...
Presently, there is a scarcity of coastal (paleo) sea-ice reconstructions for periods prior to the Last Glacial Maximum. In this study, we investigated sea ice and ocean... -
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. -
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'... -
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. -
IODP 353-U1448 bulk sediment elemental variations across Marine Isotope Stage 5
IODP 353-U1448 bulk sediment elemental variations (Ti, Ca, K, Al, Si, Rb, Sr, Zr, Mn, Fe) measured using portable-XRF across ~70-140 thousand years ago. Elemental variations... -
IODP Site 353-U1446 Mg/Ca, Mn/Ca, Nd/Ca, U/Ca, δ18O and δ13C records of Neogl...
IODP 353-U1448 trace element (Mg/Ca, Mn/Ca, Nd/Ca and U/Ca) and isotope (δ18O and δ13C) of planktic foraminifera Neogloboquadrina dutertrei across ~70-140 thousand years ago.... -
IODP Site 353-U1448 Mg/Ca, Mn/Ca, Nd/Ca, U/Ca, and δ13C records of Globigerin...
IODP 353-U1448 trace element (Mg/Ca, Mn/Ca, Nd/Ca and U/Ca) and isotope (δ13C) of planktic foraminifera Globigerinoides ruber (sensu-stricto) across ~70-140 thousand years ago.... -
IODP 353-U1446 bulk sediment elemental variations across Marine Isotope Stage 5
IODP 353-U1446 bulk sediment elemental variations (Ti, Ca, K, Al, Si, Rb, Sr, Zr, Mn, Fe) measured using portable-XRF across ~70-140 thousand years ago. Elemental variations... -
IODP Site 353-U1446 Mg/Ca, Mn/Ca, Nd/Ca, U/Ca, δ18O and δ13C records of Neogl...
IODP 353-U1446 trace element (Mg/Ca, Mn/Ca, Nd/Ca and U/Ca) and isotope (δ18O and δ13C) of planktic foraminifera Neogloboquadrina dutertrei across ~70-140 thousand years ago....