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挑战人类摇篮——南非的古老性:地质年代学证据将欧洲鼹形鼠和副狒狒在博尔特农场160号航路点的年代限制在230万年以内。

Challenging the antiquity of the Cradle of Humankind, South Africa: Geochronological evidence restricts the age of Eurotomys bolti and Parapapio to less than 2.3 Ma at Waypoint 160, Bolt's Farm.

作者信息

Edwards Tara R, Pickering Robyn, Mallett Tom L, Herries Andy I R

机构信息

Department of Geological Sciences, Human Evolution Research Institute, University of Cape Town, Rondebosch, 7700, South Africa; Human Evolution Research Institute, University of Cape Town, Rondebosch, 7700, South Africa.

Department of Geological Sciences, Human Evolution Research Institute, University of Cape Town, Rondebosch, 7700, South Africa; Human Evolution Research Institute, University of Cape Town, Rondebosch, 7700, South Africa.

出版信息

J Hum Evol. 2023 May;178:103334. doi: 10.1016/j.jhevol.2023.103334. Epub 2023 Mar 15.

Abstract

Waypoint 160 is a paleocave at Bolt's Farm in the 'Cradle of Humankind,' South Africa. It is known for the novel murid taxa Eurotomys bolti, argued to be morphologically intermediate between Eurotomys pelomyoides from Langebaanweg (∼5.1 Ma) and the earliest Otomyinae from Makapansgat Limeworks (∼3.0-2.6 Ma). Based on the presence of this specimen, an age of ∼4.5 Ma was inferred for Waypoint 160, making it far older than other Cradle sites. This biochronological age was used to argue that Parapapio and Cercopithecoides fossils from Waypoint 160 were the oldest in the region. Here, we provide a detailed sedimentological context for the in-situ deposits at Waypoint 160. We have identified interior cave deposits, in contrast to other sites at Bolt's Farm. Petrography confirms that one unit (facies D) contains in-situ microfaunal fossils, indicating the likely provenience of the E. bolti specimen. Palaeomagnetic analysis shows four periods of magnetic polarity in the sequence. Using U-Pb ages as chronological pins, we argue that the upper part of the sequence records a polarity change at the end of the Olduvai subChron (1.78 Ma). The lower part of the sequence records a polarity shift from normal to reversed that likely relates to the Feni subChron (2.16-2.12 Ma), based on a basal flowstone U-Pb age of 2.269 ± 0.075 Ma. Together this points to a depositional window of ∼500 ka, with the Parapapio and E. bolti tentatively attributed to the micromammal fossil-bearing layers dating to ∼2.27-2.07 Ma. This has significant implications for other biochronological dates in South Africa, as E. bolti is now less than ∼2.27 Ma, younger than the oldest Otomyinae at Makapansgat Limeworks and thus not ancestral to them. This chronology for Waypoint 160 challenges the presence of older, early to mid-Pliocene deposits >3.20 Ma in the Gauteng portion of the Cradle.

摘要

160号地点是位于南非“人类摇篮”博尔特农场的一个古洞穴。它以新的鼠科类群欧洲鼹形鼠(Eurotomys bolti)而闻名,该类群在形态上被认为介于来自兰格班维格(约510万年前)的欧洲鼹形鼠(Eurotomys pelomyoides)和来自马卡潘斯盖特石灰厂(约300 - 260万年前)的最早的鼹形鼠亚科之间。基于该标本的存在,推断160号地点的年代约为450万年前,这使其比“人类摇篮”的其他地点古老得多。这个生物年代学年龄被用来论证来自160号地点的副狒狒(Parapapio)和非洲古猿(Cercopithecoides)化石是该地区最古老的。在这里,我们为160号地点的原地沉积物提供了详细的沉积学背景。与博尔特农场的其他地点不同,我们识别出了洞穴内部沉积物。岩石学证实一个单元(相D)含有原地微动物化石,这表明了欧洲鼹形鼠标本的可能来源。古地磁分析显示该序列中有四个磁极性时期。使用铀铅年龄作为年代学标记,我们认为该序列的上部记录了奥杜威亚时(Olduvai subChron,178万年前)末期的极性变化。基于底部流石的铀铅年龄为226.9 ± 7.5万年,该序列的下部记录了从正向到反向的极性转变,这可能与费尼亚时(Feni subChron,216 - 212万年前)有关。综合起来,这表明有一个约50万年的沉积窗口,副狒狒和欧洲鼹形鼠暂时被归为年代约为227 - 207万年前的含微型哺乳动物化石层。这对南非的其他生物年代学日期有重大影响,因为欧洲鼹形鼠现在不到227万年前,比马卡潘斯盖特石灰厂最古老的鼹形鼠亚科更年轻,因此不是它们的祖先。160号地点的这个年代学对“人类摇篮”豪登省部分地区存在年龄大于320万年前的上新世早期到中期更古老沉积物的观点提出了挑战。

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