Simultaneous ice melt in Antarctic and Arctic

"The decline in the Antarctic ice sheets thus commenced almost 5,000 years earlier than assumed to date, though our investigations show great regional differences and demonstrate how important deepwater archives are," says the lead author of the study, Dr. Michael Weber from the Geological Institute of the University of Cologne.

"Our results suggest that Antarctica was not as climatically isolated as previously assumed," adds Dr. Gerhard Kuhn from the Alfred Wegener Institute for Polar and Marine Research in the Helmholtz Association. "Now we have to presume that the reaction of the large ice sheets in the Arctic and Antarctic to climate change is more closely linked in time than thought. At least that's the way it was during the last ice age."

This simultaneous melting was presumably caused by changes in the global sea level and deepwater circulation in the Atlantic Ocean. As a result, warm water reached the Antarctic continental margin. This early ice retreat is evidence of an instability in the East Antarctic ice sheet unsuspected to date. "Forecasts of the future rise in the sea level caused by climate change will also have to be adjusted accordingly," explains Dr. Weber.

"However, our study also clearly points out how important access to long data series, good archives and high-quality scientific databases is," Gerhard Kuhn specifies key prerequisites for reconstruction of climate history. "It's only because we at the Alfred Wegener Institute can fall back on sediment cores archived on a long-term basis and a data archive that has been built up over decades that such comparative studies are possible at all. Some of the now investigated sediment cores, for instance, were taken back in the years 1987 and 1990."

Scientists from the Geological Institute of the University of Cologne (Dr. Michael Weber, lead author), the Alfred Wegener Institute for Polar and Marine Research in the Helmholtz Association (Dr. Gerhard Kuhn, coordinator), Oregon State University and Harvard University were involved in the research work. The investigations were funded by the German Research Foundation (DFG), among others.