Speleothems turned out to be a great stroke of luck: dripstones from two caves in the Swiss Alps provide for the first time a continuous reconstruction of temperatures during the Last Interglacial period. A new study shows that high alpine regions were affected by stronger temperature increases than lower altitudes.
source https://www.sciencedaily.com/releases/2020/12/201211100620.htm
Monday, 14 December 2020
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