[1] Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome, Antarctica

[2] A study of the decontamination procedures used for chemical analysis of polar deep ice cores

[3] Age of the Mt. Ortles ice cores, the Tyrolean Iceman and glaciation of the highest summit of South Tyrol since the Northern Hemisphere Climatic Optimum

[4] new constraints on the gas age-ice age difference along the epica ice cores, 0–50 kyr

[5] direct linking of greenland and antarctic ice cores at the toba eruption (74 ka bp)

[6] high-resolution continuous-flow analysis setup for water isotopic measurement from ice cores using laser spectroscopy