Table 1. All hominids described for Africa during the Late Miocene (11.6–5.3 Ma).
Age (Ma) | Fossil site(s) | Taxon | Reference(s) | |
---|---|---|---|---|
ca. 5.4 | ESC2;3;8, Gona, Ethiopia | Ardipithecus kadabba | (Simpson et al., 2015) | |
5.6–5.2* | Amba East, Ethiopia | Ardipithecus cf. kadabba | (Haile-Selassie, 2001; Haile-Selassie, Suwa & White, 2004) | |
5.77–5.54 | ALA; ASK; DID; STD† | Ardipithecus kadabba | ||
5.8–5.7 | Tugen Hills, Kenya | Kapcheberek | Orrorin tugenensis | (Senut et al., 2001; Sawada et al., 2002; Pickford & Senut, 2005; Senut, 2010, 2015; Senut, Pickford & Gommery, 2018) |
5.9–5.8 | Kapsomin | Orrorin tugenensis | ||
Incertae sedis (early Gorilla?) | ||||
ca. 6.1 | Cheboit | Orrorin tugenensis | ||
Incertae sedis (early Pan?) | ||||
Aragai | Orrorin tugenensis | |||
6–5 | Nkondo, Uganda | cf. Gorillini | (Pickford et al., 1988) | |
6.3 | ABD1, Gona, Ethiopia | cf. Ardipithecus kadabba | (Simpson et al., 2015) | |
6.5–5‡ | Lothagam, Kenya | Homininae indet. | (Leakey & Walker, 2003) | |
7.34-7.1§ | Toros-Menalla, Chad | Sahelanthropus tchadensis | (Brunet et al., 2002, 2005) | |
8.0 | Ch’orora, Ethiopia | Chororapithecus abyssinicus | (Suwa et al., 2007) | |
9.5 | Samburu Hills, Kenya | Samburupithecus kiptalami | (Ishida & Pickford, 1997) | |
9.9–9.8 | NA39, Nakali, Kenya | Nakalipithecus nakayamai | (Kunimatsu et al., 2007) | |
Hominidea indet. | (Kunimatsu et al., 2016) | |||
11–8¶ | N 885, Niger | Incertae sedis (early Pan?) | (Pickford et al., 2008, 2009) |
Notes:
Probably closer to 5.2 Ma than 5.6, but the Kuserale Mb of the Sagantole Fm is bracketed as in Renne et al. (1999).
Fossiliferous localities in the Asa Koma Mb of the Adu Asa Fm (Middle Awash, Ethiopia). ALA = Alayla (ALA-VP-2), ASK = Asa Koma (ASK-VP-3), DID = Digiba Dora (DID-VP-1); STD = Saitune Dora (STD-VP-2).
Not the KNM-LT 329 mandible, but two teeth (KNM-LT 22930 M3; KNM-LT 25935 I1) from older deposits (Upper Nawata).
Cosmogenic nuclide dating (Lebatard et al., 2010).
Only biostratigraphic dating available, a more conservative range would be 11.6–5.3 Ma (Late Miocene).