Kenyanthropus

Kenyanthropus ('man from Kenya') is a genus of extinct hominin identified from the Lomekwi site by Lake Turkana, Kenya, dated to 3.3 to 3.2 million years ago during the Middle Pliocene. It contains one species, K. platyops, but may also include the two-million-year-old Homo rudolfensis, or K. rudolfensis. Before its naming in 2001, Australopithecus afarensis was widely regarded as the only australopithecine to exist during the Middle Pliocene, but Kenyanthropus evinces a greater diversity than once acknowledged. Kenyanthropus is most recognisable by an unusually flat face and small teeth for such an early hominin, with values on the extremes or beyond the range of variation for australopithecines in regard to these features. Multiple australopithecine species may have coexisted by foraging for different food items (niche partitioning), which may be the reason why these apes anatomically differ in features related to chewing.

The Lomekwi site also yielded the earliest stone tool industry, the Lomekwian, characterised by the rudimentary production of simple flakes by pounding a core against an anvil or with a hammerstone. It may have been manufactured by Kenyanthropus, but it is unclear if multiple species were present at the site or not. The knappers were using volcanic rocks collected no more than 100 m (330 ft) from the site. Kenyanthropus seems to have lived on a lakeside or floodplain environment featuring forests and grasslands.

In August 1998, field technician Blasto Onyango discovered a hominin partial left maxilla (upper jaw), specimen KNM-WT 38350, on the Kenyan Lomekwi dig site by Lake Turkana, overseen by prominent paleoanthropologists Louise and Meave Leakey. In August 1999 at the Lomekwi site, research assistant Justus Erus discovered an uncharacteristically flat-faced australopithecine skull, specimen KNM-WT 40000. The 1998–1999 field season subsequently uncovered 34 more craniodental hominin specimens, but the research team was unable to determine if these can be placed into the same species as the former two specimens (that is, if multiple species were present at the site).

The specimens were recovered near the Nabetili tributary of the Lomekwi river in a mudstone layer of the Nachukui Formation. KNM-WT 40000 was recovered from the Kataboi Member, 8 m (26 ft) below the 3.4-million-year-old Tulu Bor Tuff, and 12 m (39 ft) above the 3.57-million-year-old Lokochot Tuff. By linear interpolation, KNM-WT 40000 is approximately 3.5 million years old, dating back to the Middle Pliocene. Only three more specimens were recovered from the Kataboi Member at around the same level, the deepest KNM-WT 38341 probably sitting on 3.53-million-year-old sediments. KNM-WT 38350 was recovered from the Lomekwi Member 17 m (56 ft) above Tulu Bor, and is approximately 3.3 million years old. The other specimens from this member sit 16 to 24 m (52 to 79 ft) above Tulu Bor, roughly 3.3 million years old as well. The highest specimens—KNM-WT 38344, -55 and -56—may be around 3.2 million years old.

In 2001, Meave Leakey and colleagues assigned the Lomekwi remains to a new genus and species, Kenyanthropus platyops, with KNM-WT 40000 the holotype, and KNM-WT 38350 a paratype. The genus name honours Kenya where Lomekwi and a slew of other major human-ancestor sites have been identified. The species name derives from Ancient Greek platus "flat" and opsis "face" in reference to the unusually flat face for such an early hominin.

The classification of early hominins with their widely varying anatomy has been a difficult subject matter. The 20th century generated an overabundance of hominin genera plunging the field into taxonomic turmoil, until German evolutionary biologist Ernst Mayr, surveying a "bewildering diversity of names", decided to recognise only a single genus, Homo, containing a few species. Though other genera and species have since become popular, his more conservative view of hominin diversity has become the mainstay, and the acceptance of further genera is usually met with great resistance. Since Mayr, hominins are classified into Australopithecus which gave rise to Homo (which includes modern humans) and the robust Paranthropus (which is sometimes not recognised as its own genus), which by definition leaves Australopithecus polyphyletic (a non-natural group which does not comprise a common ancestor and all of its descendants). In addition to Kenyanthropus, the 1990s saw the introduction of A. bahrelghazali, Ardipithecus, Orrorin and Sahelanthropus, which has complicated discussions of hominin diversity, though the latter three have not been met with much resistance on account of their greater age (all predating Australopithecus).

At the time Kenyanthropus was discovered, Australopithecus afarensis was the only recognised australopithecine to have existed between 4 and 3 million years ago, aside from its probable ancestor A. anamensis, making A. afarensis the likely progenitor of all other australopithecines as they diversified in the late Pliocene and into the Pleistocene. Leakey and colleagues considered Kenyanthropus to be evidence of a greater diversity of Pliocene australopithecines than previously acknowledged. In 2015, Ethiopian palaeoanthropologist Yohannes Haile-Selassie and colleagues erected a new species, A. deyiremeda, which lived in the same time and region as Kenyanthropus and A. afarensis.

Meave Leakey and colleagues drew attention to namely the flat face and small cheek teeth, in addition to several other traits, to distinguish the genus from earlier Ardipithecus, contemporary and later Australopithecus, and later Paranthropus. Kenyanthropus lacks any of the derived traits seen in Homo. They conceded Kenyanthropus could be subsumed into Australopithecus if the widest definition of the latter is used, but this conservative approach to hominin diversity leaves Australopithecus a grade taxon, a non-natural grouping of similar-looking species whereby it effectively encompasses all hominins not classifiable into Ardipithecus or Homo regardless of how they may be related to each other. Leakey and colleagues further drew parallels with KNM-WT 40000 and the two-million-year-old KNM-ER 1470 assigned to Homo rudolfensis, attributing differences in braincase and nasal anatomy to archaicness. They suggested H. rudolfensis may be better classified as K. rudolfensis.