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首页> 外文期刊>Journal of Human Evolution >Tephrostratigraphy of the Waki-Mille area of the Woranso-Mille paleoanthropological research project, Afar, Ethiopia
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Tephrostratigraphy of the Waki-Mille area of the Woranso-Mille paleoanthropological research project, Afar, Ethiopia

机译:埃塞俄比亚阿法尔Woranso-Mille古人类学研究项目的Waki-Mille地区的地层

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Tephra geochemistry and Ar-40/Ar-39 geochronology are reported for the Waki-Mille area in the northwestern part of the Woranso-Mille paleoanthropological project area in the west central Afar region of Ethiopia. Previous studies documented dentognathic fossils that are morphologically intermediate between Australopithecus anamensis and Australopithecus afarensis and some that are attributed to Australopithecus afarensis. Additional dentognathic remains from the study area were assigned to the newly identified species Australopithecus deyiremeda. These fossil hominin taxa were recovered from volcanic and sedimentary strata containing tuffs ranging in age from more than 3.77 million years ago (Ma) to less than 3.469 Ma. One of the tuffs was correlated based on geochemistry, feldspar mineralogy, and age to the Lokochot Tuff of the Omo-Turkana Basin of southern Ethiopia and Kenya. Variations in major and minor element abundances in volcanic glass demarcate ten geochemically distinct tuffs and tuff sequences, including three that are geochemically similar to widespread regional tuffs, specifically the Lomogol, Lokochot, and beta- Tulu Bor/Sidi Hakoma tuffs. A new Ar-40/Ar-39 age for the Waki Tuff, which is geochemically similar to the Lomogol Tuff, is 3.664 +/- 0.016 Ma. Other tuffs in the Waki-Mille area are geochemically dissimilar to regional tuffs documented to date. Identification of tuffs based on character, stratigraphic position, and geochemistry refines local stratigraphic correlations and delineates the geographic distributions of precisely dated fossiliferous levels within the Waki-Mille area. (C) 2016 Elsevier Ltd. All rights reserved.
机译:据报道,埃塞俄比亚中西部阿法尔地区Woranso-Mille古人类学项目区西北部的Waki-Mille地区有Tephra地球化学和Ar-40 / Ar-39年代学。以前的研究记录了牙颌类化石,它们在形态学上介于南美古猿和阿法古猿之间,而其中一些归因于阿法古猿。来自研究区域的其他牙颌遗骸被分配给新近鉴定的物种澳大利亚古猿。这些人类化石化石群是从含凝灰岩的火山和沉积地层中回收的,其年龄从377万年前(Ma)到3.469 Ma以下。根据地球化学,长石矿物学和年龄,其中一种凝灰岩与埃塞俄比亚南部和肯尼亚的Omo-Turkana盆地的Lokochot凝灰岩相关。火山玻璃中主要和次要元素丰度的变化划分了十个地球化学上不同的凝灰岩和凝灰岩序列,包括三个在地球化学上与广泛的区域凝灰岩相似的凝灰岩,特别是Lomogol,Lokochot和β-TuluBor / Sidi Hakoma凝灰岩。 Waki Tuff的新Ar-40 / Ar-39年龄在地球化学上类似于Lomogol Tuff,为3.664 +/- 0.016 Ma。 Waki-Mille地区的其他凝灰岩在地球化学上与迄今记录的区域凝灰岩不同。根据特征,地层位置和地球化学对凝灰岩的识别可以改善局部地层的相关性,并勾勒出Waki-Mille地区精确标有日期的化石层的地理分布。 (C)2016 Elsevier Ltd.保留所有权利。

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