Our quantitative MAT record challenges the recent climate model simulations 3 , 58 which yield a decreasing trend in global terrestrial temperature during the past 2 Myr, forced with a modeled gradual lowering of atmospheric CO 2 59 that differs from proxy-based paleo CO 2 reconstructions (Supplementary Fig. 13 ).
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Pleistocene terrestrial warming trend in East Asia linked to Antarctic ice sheets growth.
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