“…The island's subfossil (Late Pleistocene and Holocene) record has contributed greatly to our understanding of Madagascar's recent ecological evolution, and aided interpretations of recent environmental change; this record includes large-bodied lemurs, elephant birds, pygmy hippos, crocodyliforms, turtles, bats, carnivorans, rodents and the aardvark-like Plesiorycteropus Godfrey et al, 1990Godfrey et al, , 1997Gommery et al, 2003;Goodman & Muldoon, 2016;Goodman et al, 2006;Samonds, 2007). The arrival of humans, the timing of which is still under debate (Anderson et al, 2018;Dewar et al, 2013;Godfrey et al, 2019;Hansford et al, 2018;Pierron et al, 2017), nevertheless pre-dated the decline and extinction of many of them, including the island's large (> 10 kg) native animals; the megafaunal crash did not occur until sometime during the past two millennia (Burney et al, 2004;Crowley, 2010;Godfrey et al, 2019). Megafaunal extinction is widely believed to have been induced by humans, either directly (via hunting) or indirectly (via landscape transformation), aided by Late Pleistocene and Holocene climatic change (e.g.…”