Abstract
The early Tertiary southern Arctic was an important biogeographic exchange route between the Old and New Worlds. A variant of the nearest living relative method of paleoclimatic estimation suggests that the mean temperature of the coldest month of the Eocene southern Arctic was about 10 °C, with the possibility of limited frost. The mean annual range of temperature was probably low, and moisture availability may have been limited in the cool season.
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Tiffney, B.H. (1994). An Estimate of the Early Tertiary Paleoclimate of the Southern Arctic. In: Boulter, M.C., Fisher, H.C. (eds) Cenozoic Plants and Climates of the Arctic. NATO ASI Series, vol 27. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79378-3_19
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