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综合地质年代学校准了埃塞俄比亚阿法尔裂谷的中石器时代和晚石器时代。

Integrative geochronology calibrates the Middle and Late Stone Ages of Ethiopia's Afar Rift.

机构信息

Department of Earth & Planetary Science, University of California, Berkeley, CA 94720;

Berkeley Geochronology Center, Berkeley, CA 94709.

出版信息

Proc Natl Acad Sci U S A. 2021 Dec 14;118(50). doi: 10.1073/pnas.2116329118.

DOI:10.1073/pnas.2116329118
PMID:34873047
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8685921/
Abstract

The Halibee member of the Upper Dawaitoli Formation of Ethiopia's Middle Awash study area features a wealth of Middle and Later Stone Age (MSA and LSA) paleoanthropological resources in a succession of Pleistocene sediments. We introduce these artifacts and fossils, and determine their chronostratigraphic placement via a combination of established radioisotopic methods and a recently developed dating method applied to ostrich eggshell (OES). We apply the recently developed Th/U burial dating of OES to bridge the temporal gap between radiocarbon (C) and Ar/Ar ages for the MSA and provide C ages to constrain the younger LSA archaeology and fauna to ∼24 to 21.4 ka. Paired C and Th/U burial ages of OES agree at ∼31 ka for an older LSA locality, validating the newer method, and in turn supporting its application to stratigraphically underlying MSA occurrences previously constrained only by a maximum Ar/Ar age. Associated fauna, flora, and fossils are thereby now fixed between 106 ± 20 ka and 96.4 ± 1.6 ka (all errors 2σ). Additional Ar/ results on an underlying tuff refine its age to 158.1 ± 11.0 ka, providing a more precise minimum age for MSA lithic artifacts, fauna, and fossils recovered ∼9 m below it. These results demonstrate how chronological control can be obtained in tectonically active and stratigraphically complex settings to precisely calibrate crucial evidence of technological, environmental, and evolutionary changes during the African Middle and Late Pleistocene.

摘要

Halibee 成员来自埃塞俄比亚中阿瓦什研究区的上达沃特利组,在更新世沉积物的连续地层中拥有丰富的中石器时代和晚期石器时代(MSA 和 LSA)古人类学资源。我们介绍了这些人工制品和化石,并通过结合已建立的放射性同位素方法和最近开发的应用于鸵鸟蛋壳(OES)的测年方法来确定它们的年代地层位置。我们应用最近开发的 OES 的 Th/U 埋藏测年来弥合 MSA 的放射性碳 (C) 和 Ar/Ar 年龄之间的时间差距,并提供 C 年龄来限制年轻的 LSA 考古学和动物群到约 24 到 21.4 ka。对于较老的 LSA 地点,OES 的配对 C 和 Th/U 埋藏年龄在约 31 ka 处一致,验证了较新的方法,并反过来支持其应用于以前仅由最大 Ar/Ar 年龄约束的地层下的 MSA 出现。因此,相关的动物群、植物群和化石现在被固定在 106 ± 20 ka 和 96.4 ± 1.6 ka 之间(所有误差均为 2σ)。对下伏凝灰岩的额外 Ar/结果将其年龄细化为 158.1 ± 11.0 ka,为在其下方约 9 m 处回收的 MSA 石器、动物群和化石提供了更精确的最小年龄。这些结果表明,在构造活跃且地层复杂的环境中如何获得年代控制,以精确校准非洲中更新世和晚更新世期间技术、环境和进化变化的关键证据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/bd34de39c955/pnas.202116329fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/16ad169fe4d6/pnas.202116329fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/790a58bcc670/pnas.202116329fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/bd34de39c955/pnas.202116329fig03.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/16ad169fe4d6/pnas.202116329fig01.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/790a58bcc670/pnas.202116329fig02.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e1af/8685921/bd34de39c955/pnas.202116329fig03.jpg

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