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来自奥莫组沉积物的化石原始人类的地层背景:肯尼亚和埃塞俄比亚的图尔卡纳湖盆地北部

Stratigraphic context of fossil hominids from the Omo group deposits: northern Turkana Basin, Kenya and Ethiopia.

作者信息

Feibel C S, Brown F H, McDougall I

机构信息

Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112.

出版信息

Am J Phys Anthropol. 1989 Apr;78(4):595-622. doi: 10.1002/ajpa.1330780412.

Abstract

The chronometric framework developed for Plio-Pleistocene deposits of the northern Turkana Basin is reviewed in light of recent advances in lithostratigraphy, geochemical correlation, paleomagnetic stratigraphy, and isotopic dating. The sequence is tightly controlled by 20 precise ages on volcanic materials. These ages are internally consistent but are at variance with estimates for the boundaries of the magnetic polarity time scale by about 0.07 my. This discrepancy can be only partially resolved at present. Based on the established chronometric framework and stratigraphic sequences, depositional ages can be estimated for significant marker beds. These ages can in turn be used to constrain the 449 hominid specimens thus far reported from the basin. Ages for most hominid specimens can be estimated with a precision of +/- 0.05 my. In addition, the chronometric framework will be applicable to other paleontological collections, archeological excavations, and future discoveries in the basin.

摘要

根据岩石地层学、地球化学对比、古地磁地层学和同位素测年等方面的最新进展,对为图尔卡纳湖盆北部上新世-更新世沉积物建立的计时框架进行了综述。该层序由火山物质上的20个精确年龄严格控制。这些年龄在内部是一致的,但与磁极性时间尺度边界的估计值相差约0.07百万年。目前,这种差异只能部分得到解决。基于已建立的计时框架和地层序列,可以估算出重要标志层的沉积年龄。这些年龄反过来又可用于约束该盆地迄今已报道的449件人类化石标本。大多数人类化石标本的年龄可以精确到±0.05百万年。此外,该计时框架将适用于该盆地的其他古生物学藏品、考古发掘以及未来的发现。

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