Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112-0102, USA.
J Hum Evol. 2012 Oct;63(4):577-85. doi: 10.1016/j.jhevol.2012.05.014. Epub 2012 Jul 17.
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.
来自埃塞俄比亚基比什组 I 成员的人属标本奥莫 I 和奥莫 II 被归因于早期智人,有人提出它们的年龄接近 19.6 万年。基比什组 II 成员中的 KHS 凝灰岩在该地点没有直接定年,但据信它是在形成地中海 S6 腐泥岩的时期或附近沉积的。电子探针分析表明,KHS 凝灰岩与赫托、贡纳和孔索的 WAVT(Waidedo 玻璃质凝灰岩)(样品 TA-55)以及埃塞俄比亚裂谷谷 Kulkuletti 的 D 单元相关,孔索的 TA-55 样品年龄大于 15.4 万年,Kulkuletti 的 D 单元的年龄为 18.3 万年。这些相关性和年龄为奥莫 I 和奥莫 II 人类遗骸的原始年代以及基比什地区的沉积时间与地中海腐泥岩的形成时间的相关性提供了强有力的支持。基比什组 III 成员中的 Aliyo 凝灰岩定年为 10.4 万年,与埃塞俄比亚裂谷谷的 Gademotta 单元 15 相关。