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Age determination of Vostock Ice Core
The object of the present study is to introduce a means of comparing the Vostok and marine chronologies. Our strategy has been to use the delta18O of atmospheric O2 (denoted... -
Stable isotope ratios of foraminifera from last glacial-interglacial sediment...
A set of numerical equations is developed to estimate past sea surface temperatures (SST) from fossil Antarctic diatoms. These equations take into account both the biogeographic... -
Age determination and sea surface temperature reconstruction for the Southern...
The isotopic and micropaleontological deglacial records of three deep-sea cores from 44°S to 55°S have been dated by accelerator mass spectrometry. The available records did not... -
Stable oxygen isotope composition of planktonic foraminifera from the Adriati...
Under modern conditions, the reoxygenation of eastern Mediterranean deep water is the result of the formation of dense bottom water in the southern Adriatic Sea. Oxygen isotopic... -
Stable carbon and oxygen isotope ratios of foraminifera from North Atlantic s...
Oxygen-18 records of benthic foraminifera from the Atlantic Ocean are significantly different from those of the Pacific and Indian Oceans indicating that the Glacial North... -
Stable carbon and oxygen isotope ratios of benthic foraminifera
Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean delta13C values were 0.46 per mil lower during the last glacial... -
Stable carbon and oxygen isotope analyses of Neogloboquadrina pachyderma
Detailed records of the carbon and oxygen isotopic ratios of Neogloboquadrina pachyderma are compared between nine high-latitude sediment cores, from the Northern and Southern... -
A low-latitude Upper Pleistocene oxygen isotope stack
Below oxygen isotope stage 16, the orbitally derived time-scale developed by Shackleton et al. (1990) from ODP site 677 in the equatorial Pacific differs significantly from... -
Compositional and isotopic data on core MD84641
The organic carbon isotopic record of the sapropels(S1 and S3-S10) and intercalated marl oozes has been determined in a 12-m piston core from the eastern Mediterranean. The... -
Relative abundance of dinoflagellate cysts in surface sediments and dinoflage...
In this study we investigate the potential of organic-walled dinoflagellate cysts (dinocysts) as tools for quantifying past sea-surface temperatures (SST) in the Southern Ocean.... -
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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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 deglacial Southern Ocean planktic foraminiferal d18O data
This dataset contains a compilation of planktic foraminiferal d18O from sediment cores spanning the last deglaciation in the Southern Ocean. The compilation includes 4610 data... -
Primary data sets of the hydrographic atlas of the Southern Ocean
The general knowledge of the hydrographic structure of the Southern Ocean is still rather incomplete since observations particularly in the ice covered regions are cumbersome to... -
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... -
Nd isotope composition obtained on mixed planktonic foraminifera samples from...
Neodymium isotopes were measured on mixed planktonic foraminifera from the washed >150 µm size fraction of the samples. The foraminifera tests were crushed between two glass... -
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.