“…The western North American monsoon was severely depressed by glaciation (Bhattacharya, Tierney, Addison, & Murray, 2018), such that summer temperatures in the continental interior averaged 8-14°C below contemporary levels, while plant communities were depressed 600- with an extensive Holocene drought (Sullivan et al, 2016). These climatic effects were global in nature and greatly impacted aquatic and terrestrial fauna beyond Western North America (Brunner, Douglas, & Bernatchez, 1998;Brunner, Douglas, Osinov, Wilson, & Bernatchez, 2001;Bryson, Murphy, Lathrop, & Lazcano-Villareal, 2011;Migliore et al, 2019;Morales-Barbero, Martinez, Ferrer-Castán, & Olalla-Tárraga, 2018).…”