
For several years, scientists from Italy, Germany, New Zealand and the United States have been studying a 1300 metre-long rock core recovered by the multinational ANDRILL (ANtarctic geological DRILLing) programme from beneath the Ross Ice Shelf, in McMurdo Sound, Antarctica. The core was recovered in 2006 by a team of drillers and engineers from Antarctica New Zealand, who drilled through the ice to a record-setting depth.
The rock core contains valuable evidence of how Antarctica’s ice sheets and climate have changed over time and scientists use this information to learn what is likely to happen to Antarctica’s ice masses in the future and determine how these changes might affect the world’s climate and sea level.
Professor Tim Naish, Director of Victoria’s Antarctic Research Centre, and Professor Ross Powell from Northern Illinois University in the United States are Co-Chief Scientists of the collaborative research project.…[Nash] says Antarctica’s ice sheets have grown and collapsed at least 40 times over the past five million years. “Much of our research has focused on the time interval from three to five million years ago. This period in Earth’s history is extremely relevant as it represents a global climate analogue to that projected for our very near future.”
“So far results from our studies on this extraordinary archive of Antarctica’s environmental history are providing critical new insights into past changes in Antarctica’s most vulnerable element: the West Antarctic Ice Sheet. If this ice mass were to melt, global sea-level would rise up to 5 metres - our world would be a very different place.”…
An Antarctic glacier visible on the flight to McMurdo Sound, shot by Fred Walton, NOAA
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