The environment of the Ethiopian highlands at the Mid Pleistocene Transition: Fauna, flora and hominins in the 850-700 ka sequence of Gombore II (Melka Kunture)

Environment, climatic change and human evolution have been debated over the last 50 years giving special attention to the Plio-Pleistocene sites of the Rift Valley. In this paper we discuss the environment and the limits of hominin adaptability based on evidence from Melka Kunture, at 2000 m asl on...

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Veröffentlicht in:Quaternary science reviews 2016-10, Vol.149, p.259-268
Hauptverfasser: Mussi, M., Altamura, F., Bonnefille, R., De Rita, D., Melis, R.T.
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Sprache:eng
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Zusammenfassung:Environment, climatic change and human evolution have been debated over the last 50 years giving special attention to the Plio-Pleistocene sites of the Rift Valley. In this paper we discuss the environment and the limits of hominin adaptability based on evidence from Melka Kunture, at 2000 m asl on the Ethiopian highlands, and specifically on the ∼850 ka to ∼700 ka sequence at sub-site Gombore II. Human fossils and multiple Acheulean occurrences, as well as hippo remains and footprints, combined with palynological analysis, provide a highly detailed chronological resolution of the changing local environmental conditions during the last ∼150 ka of the MPT (Mid Pleistocene Transition), including the sequence of events after a volcanic eruption. Layers containing footprints and fossils are evidence of near-continuous occupation by hippos and their recolonization of the area after a disruptive volcanic eruption. Conversely, Acheulean implements and human fossils suggest that peopling by hominins occurred at a different and discontinuous pace even when the flora and fauna were re-established and the environment was rather stable. Most notably, the assembled evidence points to the limits of Homo erectus s.l. adaptability. Apparently, this hominin could no longer live at 2000 m asl when the climate deteriorated during glacial isotopic stage 20, becoming markedly colder than it is today, but re-colonized the area when the climate turned warmer again during isotopic stage 19. [Display omitted] •First detailed description of the environment at Melka Kunture, Ethiopia, at the MPT.•At 2000 m asl the vegetation always was of Afromontane type and not of savanna type.•Pleistocene hominins and hippos reacted differently to climatic changes at the MPT.•At the MPT hippopotamuses were resilient to climate change and to a volcanic eruption.•We discuss if during MIS20 hominins were able to settle at 2000 m asl at Melka Kunture.
ISSN:0277-3791
1873-457X
DOI:10.1016/j.quascirev.2016.07.033