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As reviewed in Trauth et al. (2021), the Onset of Northern Hemispheric Glaciation (ONHG) and glacial intensifications were originally credited as primary drivers of Plio-Pleistocene human evolutionary events (e.g., deMenocal, 1995, 2004; Vrba et al., 1995; Potts and Faith, 2015; Faith et al., 2019), but mounting evidence points to insolation-dominated climatic forcing as the main control on fluctuations in hydroclimate and vegetation structure relevant to biotic evolution in the EARS (e.g.,
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