Correlation of the KHS Tuff of the Kibish Formation to volcanic ash layers at other sites, and the age of early Homo sapiens (Omo I and Omo II)

• Published in: Journal of human evolution 2012-10, Vol.63 (4), p.577-585
• Main Authors: Brown, Francis H., McDougall, Ian, Fleagle, John G.
• Format: Article
• Language: English
• Subjects: Age; Archaeological sites; Ash layers; Correlation; Crystalline rocks; Early Homo sapiens; Earth sciences; Earth, ocean, space; Ethiopia; Evolutionary anthropology; Exact sciences and technology; Fossils; Geologic Sediments - analysis; Hominids; Human remains; Humans; Igneous and metamorphic rocks petrology, volcanic processes, magmas; Kibish; Marine and continental quaternary; Paleoanthropology; Paleontology; Rift valleys; Sample surveys; sapropels; Surficial geology; Tephra; Vertebrate paleontology; Volcanic Eruptions - analysis; Volcanoes
• ISSN: 0047-2484; 1095-8606
• DOI: 10.1016/j.jhevol.2012.05.014

Hominin specimens Omo I and Omo II from Member I of the Kibish Formation, Ethiopia are attributed to early Homo sapiens, and an age near 196 ka has been suggested for them. The KHS Tuff, within Member II of the Kibish Formation has not been directly dated at the site, but it is believed to have been deposited at or near the time of formation of sapropel S6 in the Mediterranean Sea. Electron microprobe analyses suggest that the KHS Tuff correlates with the WAVT (Waidedo Vitric Tuff) at Herto, Gona, and Konso (sample TA-55), and with Unit D at Kulkuletti in the Ethiopian Rift Valley. Konso sample TA-55 is older than 154 ka, and Unit D at Kulkuletti is dated at 183 ka. These correlations and ages provide strong support for the age originally suggested for the hominin remains Omo I and Omo II, and for correlation of times of deposition in the Kibish region with formation of sapropels in the Mediterranean Sea. The Aliyo Tuff in Member III of the Kibish Formation is dated at 104 ka, and correlates with Gademotta Unit 15 in the Ethiopian Rift Valley.