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南非斯泰克方丹含南方古猿沉积物的修订年代估计。

Revised age estimates of Australopithecus-bearing deposits at Sterkfontein, South Africa.

作者信息

Berger Lee R, Lacruz Rodrigo, De Ruiter Darryl J

机构信息

Palaeoanthropology Unit for Research and Exploration, Bernard Price Institute for Palaeontology, University of the Witwatersrand, Johannesburg 2050, South Africa.

出版信息

Am J Phys Anthropol. 2002 Oct;119(2):192-7. doi: 10.1002/ajpa.10156.

Abstract

The Sterkfontein fossil site in South Africa has produced the largest concentration of early hominin fossils from a single locality. Recent reports suggest that Australopithecus from this site is found within a broad paleontological age of between 2.5-3.5 Ma (Partridge [2000] The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 100-125; Partridge et al. [2000a], The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 129-130; Kuman and Clarke [2000] J Hum Evol 38:827-847). Specifically, the hominin fossil commonly referred to as the "Little Foot" skeleton from Member 2, which is arguably the most complete early hominin skeleton yet discovered, has been magnetostratigraphically dated to 3.30-3.33 Ma (Partridge [2000] The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 100-125; Partridge et al. [2000a], The Cenozoic of Southern Africa, Oxford: Oxford Monographs, p. 129-130). More recent claims suggest that hominin fossils from the Jacovec Cavern are even older, being dated to approximately 3.5 Ma. Our interpretation of the fauna, the archeometric results, and the magnetostratigraphy of Sterkfontein indicate that it is unlikely that any Members yet described from Sterkfontein are in excess of 3.04 Ma in age. We estimate that Member 2, including the Little Foot skeleton, is younger than 3.0 Ma, and that Member 4, previously dated to between 2.4-2.8 Ma, is more likely to fall between 1.5-2.5 Ma. Our results suggest that Australopithecus africanus should not be considered as a temporal contemporary of Australopithecus afarensis, Australopithecus bahrelghazali, and Kenyanthropus platyops.

摘要

南非的斯泰克方丹化石遗址出土了来自单一地点的最密集的早期人类化石。最近的报告表明,该遗址的南方古猿处于250万至350万年前的一个广泛古生物学年代范围内(帕特里奇[2000年]《南部非洲的新生代》,牛津:牛津专论,第100 - 125页;帕特里奇等人[2000a],《南部非洲的新生代》,牛津:牛津专论,第129 - 130页;库曼和克拉克[2000年]《人类进化杂志》38:827 - 847)。具体而言,通常被称为“小脚”骨架的人类化石来自第2层,这可以说是迄今发现的最完整的早期人类骨架,其磁性地层年代测定为330万至333万年前(帕特里奇[2000年]《南部非洲的新生代》,牛津:牛津专论,第100 - 125页;帕特里奇等人[2000a],《南部非洲的新生代》,牛津:牛津专论,第129 - 130页)。最近的说法表明,来自雅科韦克洞穴的人类化石甚至更古老,年代测定约为350万年前。我们对斯泰克方丹动物群、考古测年结果和磁性地层学的解释表明,斯泰克方丹迄今描述的任何层位的年龄都不太可能超过304万年前。我们估计,包括“小脚”骨架在内的第2层的年龄小于300万年前,而之前测定为240万至280万年前的第4层更有可能处于150万至250万年前之间。我们的结果表明,非洲南方古猿不应被视为阿法南方古猿、巴赫尔加扎勒南方古猿和扁脸肯尼亚人的同时代物种。

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