Geneviève C Littot

TL;DR: The recovery of a deep ice core from Dome C, Antarctica, that provides a climate record for the past 740,000 years is reported, suggesting that without human intervention, a climate similar to the present one would extend well into the future.

TL;DR: In this paper, a glacial climate record derived from an ice core from Dronning Maud Land, Antarctica, which represents South Atlantic climate at a resolution comparable with the Greenland ice core records was presented.

TL;DR: Continuous chemical proxy data spanning the last eight glacial cycles from the Dome C Antarctic ice core constrain winter sea-ice extent in the Indian Ocean, Southern Ocean biogenic productivity and Patagonian climatic conditions and observe large glacial–interglacial contrasts in iron deposition, which is infer reflects strongly changing Patagonia conditions.

TL;DR: In this paper, the authors used a simple conceptual transport model to estimate that transport can explain only 40% of the atmospheric dust concentration changes in Antarctica, while factor 5-10 changes occurred.

TL;DR: The EPICA ice core from Dome C extends 3259 m in depth, and encompasses 800 ka of datable and sequential ice as discussed by the authors, and the results suggest a possible correction to accumulation rates in one early interglacial.