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Laser dust logging of the EPICA Dome C borehole
We deployed a laser dust logger in the EPICA Dome C Ice Core (EDC) borehole in order to obtain a detailed record of dust and ash in order to study the particulate stratigraphy,... -
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... -
Internal reflecting horizons at Little Dome C, Antarctica
This is a dataset of radio-echo sounding internal reflecting horizons (IRH) which were traced across the radar surveys conducted in the 2019/20 Antarctic summer season at Little... -
Stable isotopic methane (dD(CH4)) records of ice core EDC
All data are free of krypton interference during the mass spectrometric analysis. dD(CH4) data are measured using the system described in:Bock, M., J. Schmitt, J. Beck, R.... -
Stable isotopic methane (δ¹³CH4) records of ice core EDC
d13CH4 data are measured using the system described in:Schmitt, J., B. Seth, M. Bock, H. Fischer, "Online technique for isotope and mixing ratios of CH4, N2O, Xe and mixing... -
Internal reflecting horizons in the Dome C region of Antarctica
This dataset consists of radar IRHs (internal reflecting horizons) which were traced across ice-penetrating radar surveys conducted between 2016 and 2018 over the Dome C region... -
Water stable oxygen isotope records from six Antarctic ice core sites for the...
We compare the present and last interglacial periods as recorded in Antarctic water stable isotope records now available at various temporal resolutions from six East Antarctic... -
Dust and calcium record in calculated for ice core EPICA Dome C
Ice core data from Antarctica provide detailed insights into the characteristics of past climate, atmospheric circulation, as well as changes in the aerosol load of the... -
Measurements of stable carbon isotope ratios of CO2 over the last 24000 years...
The stable carbon isotope ratio of atmospheric CO2 (d13Catm) is a key parameter in deciphering past carbon cycle changes. Here we present d13Catm data for the past 24,000 years... -
Chemical measurements from the EPICA Dome C core
Sea ice and dust flux increased greatly in the Southern Ocean during the last glacial period. Palaeorecords provide contradictory evidence about marine productivity in this... -
Data from the EPICA Dome C ice core EDC
The Antarctic Vostok ice core provided compelling evidence of the nature of climate, and of climate feedbacks, over the past 420,000 years. Marine records suggest that the... -
EPICA Dome C carbon dioxide concentrations from 650 to 391 kyr BP
A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2... -
High-resolution carbon dioxide concentration records from the EPICA Dome C ic...
Changes in past atmospheric carbon dioxide concentrations can be determined by measuring the composition of air trapped in ice cores from Antarctica. So far, the Antarctic... -
Rare earth elements determined in Antarctic ice by inductively coupled plasma
Inductively coupled plasma mass spectrometry (ICP-MS) is a suitable tool for multi-element analysis at low concentration levels. Rare earth element (REE) determinations in... -
Dust record from the EPICA Dome C ice core, Antarctica, covering 0 to 800 kyr BP
Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation and it can be a source of micronutrients, such as iron, to the ocean.... -
Aeolian dust and chemistry records from the EDML and EDC ice cores
To improve quantitative interpretation of ice core aeolian dust records a systematic methodical comparison has been made involving methods of water-insoluble particle counting... -
Dome C age scale EDC2 for ice core EDC
EDC2 timescale, adopted by SC December 2003. EDC2 was recommended for all EPICA papers below 800 m until EDC3 was adopted. Matches EDC1 (doi:10.1594/PANGAEA.198748) at 800 m in... -
Dome C age scale EDC1 for ice core EDC99
EDC2 (doi:10.1594/PANGAEA.198749) should be used for all EPICA papers below 800 m until new timescale is adopted. Matches EDC1 at 800 m in ice scale. EDC1 is still recommended... -
Grain radius from selected samples of the EPICA Dome C ice core EDC, 110-3100...
This dataset has no description
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Concentration of insoluble dust in the EPICA Dome C ice core EDC, 100-3138 me...
This dataset has no description
