Temperatures of sea water fringing South Pole were tropical 50 million years ago
The conclusions are based on analyses on sediments retrieved from the ocean floor east of Tasmania. This area bordered to Antarctica during the early Paleogene (60-35 milion years ago). Much global warming research is focused on polar areas, because these are particularly sensitive to climate change.
Previously, scientists from Utrecht University and the Royal NIOZ presented in a suite of Nature and Science articles the manifestation of Greenhouse climates in the Arctic regions, with the invasion of tropical algae and sea surface temperatures of up to 24ºC. Meanwhile, temperatures of waters fringing the Antarctic continent during the Greenhouse climates were a great unknown to climate scientists. The multidisciplinary research, published in Nature, now reached a breakthrough.
What emerges from these results is that the Greenhouse pole-to-equator sea surface temperature gradient was close to non-existent. After the warmest phase (about 50 million years ago), the world gradually cooled down to an ‘Icehouse’ state, like today. Along with this cooling, the temperature gradient turned more and more into its present day shape.
The interest to society is evident: the fossil Greenhouse world is generally considered to be a potential analogue for future climates. “The fossil Greenhouse world of 50 Million years ago is generally considered analogous to future climates”, says Peter Bijl, paleo-climatologist at Utrecht University. “These field data imply that polar temperatures can be much higher than the IPCC computer models predict for a high-CO2 world. In turn, climate change can be even more severe than the worst case scenario’s of the IPCC.”
More information: Letter in Nature: Early Palaeogene Temperature evolution of the Southwest Pacific Ocean, by Peter K. Bijl, Stefan Schouten, Appy Sluijs, Gert-Jan Reichart, James C. Zachos and Henk Brinkhuis.