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Proxies for paleo-oxygenation: a downcore comparison between benthic foramini...
Benthic foraminiferal surface porosity (the mean percentage of surface area covered by pores; higher porosity: lower oxygenation) and iodine to calcium ratio (I/Ca, higher I/Ca:... -
NGRIP ice-core volcanic sulfate concentration and deposition from 79.14 to 80...
We present continuous records of 1 cm resolved sulfate concentrations, insoluble particle number and mass concentration, and liquid conductivity using a Continuous Flow Analysis... -
Carbon stable isotopes of Globigerina bulloides from 19 sediment cores in the...
This dataset has no description
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Carbon stable isotopes of Globigerina bulloides from 68 core tops in the sout...
This dataset has no description
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Micro-inclusions identified with Raman spectroscopy in thirteen samples (1360...
Micro-inclusions in thirteen samples (1360-2115 m) from the Last Glacial of the East Greenland Ice Core Project ice core in North-East Greenland were located with microstructure... -
Modern, pre-industrial and past (last 25 ka) carbon isotopic (δ13C) variabili...
Carbon stable isotopes of Globigerina bulloides from 68 core tops and 19 cores (published and unpublished) were compiled for the SW Pacific to determine latitudinal changes in... -
Boron isotope data on uranium-thorium dated Desmophyllum dianthus deep sea co...
The cause of changes in atmospheric carbon dioxide (CO₂) during the recent ice ages is yet to be fully explained. Most mechanisms for glacial–interglacial CO₂ change have... -
Benthic isotope records in three sediment cores
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Pollen counts of sediment core Colonia_CO14
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Pollen counts of sediment core Colonia_CO3
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Carbon and oxygen stable isotopes measured on benthic foraminifera from IODP ...
High latitude deep water upwelling has the potential to control global climate over glacial timescales through the biological pump and ocean-atmosphere CO2 exchange. However,... -
Upwelling index from IODP Site 323-U1343
High latitude deep water upwelling has the potential to control global climate over glacial timescales through the biological pump and ocean-atmosphere CO2 exchange. However,... -
MAAT reconstruction of sediment core Colonia_CO14
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Element analysis of peat core Colonia_CO14
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Microcharcoal of sediment core Colonia_CO14
This dataset has no description
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Chironomid abundances for a Mid Weichselian record from Reichwalde (Germany)
This dataset provides chironomid abundance data for a Mid Weichselian sediment sequence retrieved from the Reichwalde mine situated in the Niederlausitz area (Germany) in 1999.... -
Chironomid percent-abundances for an Early Weichselian record from Nochten (G...
This dataset provides chironomid percent-abundance data for an Early Weichselian sediment sequence retrieved from the Nochten mine (Niederlausitz area, Germany) in 2004.... -
Pollen, XRF, microcharcoal and mean air annual temperature of the CO3 and CO1...
We analysed changes in mean air annual temperature (MAAT), vegetation and biomass burning on a long and continuous lake-peat sediment record from the Colônia basin, southeastern... -
Reconstructing the oxygen depth profile in the Arabian Sea during the last gl...
A total of six core sites of western Arabian Sea were selected to form a depth transect with water depths ranging from 600 to 3650 m, in order to reconstruct the oxygen depth... -
A database of cosmogenic nuclide dates from glaciated mountain landscapes acr...
This database is a compilation of cosmogenic nuclide dates obtained from glaciated mountain landscapes across the Mediterranean. The dates have been sourced from the published...
