The Inexplicable Thaw: The Younger Dryas Enigma

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A B O U T T H I S E P I S O D E:

By the late 1970s a spectrum of research revealed that over the past 200,000 years, our planet swung violently between full glacial and interglacial climates at least 3 times, during which gigantic masses of glacial ice accumulated on the continental land surfaces while sea levels dropped precipitously, sometimes up to 400 to 500 feet lower than present day sea level. This was followed by equally rapid deglaciation, or disappearance of the ice and correspondingly rapid rise in sea levels, sometimes to many feet higher than the present day. One study from 1977 used 8 cores extracted from the ocean bottom to examine changes in ancient ocean life to correlate temperature changes in the North Atlantic.

Only a year before this study was published a report was published that was based on a collection and analysis of radiocarbon dates around the shores of James Bay and the Hudson Strait in the region of Hudson Bay, which was the geographic center of the great Laurentide Ice Sheet during the last glaciation. What this study revealed was that the deglaciation of the Hudson Bay region was extremely fast, even catastrophic. Scientists continue to try and unravel the accumulating evidence for this inexplicably fast change in global climate. Join us for this edition of Squaring the Circle as we probe the mysteries surrounding the most recent of these extreme upheavals, the Younger Dryas climate catastrophe.

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