A climate scientist who has suggested how mountain building can lower Earth’s thermostat and why ice ages sometimes wax and wane at different speeds has been awarded one of geology’s oldest and most coveted prizes: the British Wollaston Medal. The first woman to win a Wollaston in the prize's183-year history, Maureen Raymo, a researcher at Columbia University’s Lamont-Doherty Earth Observatory, joins the company of Victorian giants Charles Darwin and Louis Agassiz, and major 20th-century figures including climatologist Sir Nicholas Shackleton and James Lovelock, originator of the Gaia hypothesis. Raymo, 54, will receive the medal, cast in the platinum-like metal palladium discovered by Henry Wollaston in 1803, at the Geological Society of London’s annual meeting in June.
|Name||Title||Fields of interest|
|Athanasios Koutavas||Adjunct Associate Research Scientist||Paleoclimatology|
March 04, 2014
September 08, 2010
As the last ice age was ending, about 13,000 years ago, a final blast of cold hit Europe, and for a thousand years or more, it felt like the ice age had returned. But oddly, despite bitter cold winters in the north, Antarctica was heating up. For the two decades since ice core records revealed that Europe was cooling at the same time Antarctica was warming over this thousand-year period, scientists have looked for an explanation.
June 18, 2009
Researchers have reconstructed atmospheric carbon dioxide levels over the past 2.1 million years in the sharpest detail yet, shedding new light on its role in the earth’s cycles of cooling and warming.