“…The oxygen isotopic composition of tooth enamel provides additional paleodietary and paleophysiological information for individual specimens, while an analysis of taxa with a range of thermophysiological adaptations and behaviors may provide additional paleoclimatic information . The recent surge of stable isotopic data from hominins also makes it clear that the middle Pliocene marked significant hominin paleodietary change, when hominins first began to exploit substantial C 4 /CAM-based foods in more open environments (Lee-Thorp et al, 2012;Cerling et al, 2013;Sponheimer et al, 2013;Wynn et al, 2013;Alemseged, 2015;Levin et al, 2015). The timing of this C 4 dietary expansion, combined with other middle Pliocene discoveries, including possible hominin tool use and manufacture (McPherron et al, 2010;Harmand et al, 2015) and potentially increased diversity of hominin taxonomic diversity (Wood and Boyle, 2016), have heightened interest in the ecological, dietary, and behavioral patterns of hominins in the middle Pliocene (~3.8 -3.0 Ma).…”