Abstract
Composite paleotemperature curves (values of average annual temperature and sea surface temperature) for high and low latitudes of Northern Eurasia have been compiled. Based on them, a model of the climatic history of the Northern Hemisphere in the Mesozoic-Cenozoic was compiled. The relationship of climate variations with other significant geological events — cycles of eccentricity of the Earth’s orbit, impact events, inversions of the geomagnetic field is analyzed.
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