“…On Kilimanjaro, high-elevation paleoenvironmental studies have characterized late Pleistocene and Holocene vegetation and climate change derived from soils (Zech, 2006; Zech et al, 2011; Montade et al, 2018), sediments (Coetzee, 1967; Schüler et al, 2012; Schüler, 2012), and glacial ice (Thompson et al, 2002; Gabrielli et al, 2014), and are also informed by records from nearby Lake Challa (Table 1) (Verschuren et al, 2009; Barker et al, 2011; Nelson et al, 2012; Martin-Jones et al, 2020). Archaeological evidence and oral tradition summaries show a long and varied history of land use on and around Kilimanjaro (Fosbrooke and Sassoon, 1965; Odner, 1971; Mturi, 1986; Clack, 2007, 2009), though as yet, there are no published archaeological sites above 2000 m asl.…”