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印度尼西亚中爪哇巴庞组古人类的早更新世40Ar/39Ar年龄

Early Pleistocene 40Ar/39Ar ages for Bapang Formation hominins, Central Jawa, Indonesia.

作者信息

Larick R, Ciochon R L, Zaim Y, Rizal Y, Aziz F, Reagan M, Heizler M

机构信息

URS Corporation, 100 California Street, Suite 500, San Francisco, CA 94111-4529, USA.

出版信息

Proc Natl Acad Sci U S A. 2001 Apr 24;98(9):4866-71. doi: 10.1073/pnas.081077298. Epub 2001 Apr 17.

Abstract

The Sangiran dome is the primary stratigraphic window for the Plio-Pleistocene deposits of the Solo basin of Central Jawa. The dome has yielded nearly 80 Homo erectus fossils, around 50 of which have known findspots. With a hornblende (40)Ar/(39)Ar plateau age of 1.66 +/- 0.04 mega-annum (Ma) reportedly associated with two fossils [Swisher, C.C., III, Curtis, G. H., Jacob, T., Getty, A. G., Suprijo, A. & Widiasmoro (1994) Science 263, 1118-1121), the dome offers evidence that early Homo dispersed to East Asia during the earliest Pleistocene. Unfortunately, the hornblende pumice was sampled at Jokotingkir Hill, a central locality with complex lithostratigraphic deformation and dubious specimen provenance. To address the antiquity of Sangiran H. erectus more systematically, we investigate the sedimentary framework and hornblende (40)Ar/(39)Ar age for volcanic deposits in the southeast quadrant of the dome. In this sector, Bapang (Kabuh) sediments have their largest exposure, least deformation, and most complete tephrostratigraphy. At five locations, we identify a sequence of sedimentary cycles in which H. erectus fossils are associated with epiclastic pumice. From sampled pumice, eight hornblende separates produced (40)Ar/(39)Ar plateau ages ranging from 1.51 +/- 0.08 Ma at the Bapang/Sangiran Formation contact, to 1.02 +/- 0.06 Ma, at a point above the hominin-bearing sequence. The chronological sequence of (40)Ar/(39)Ar ages follows stratigraphic order across the southeast quadrant. An intermediate level yielding four nearly complete crania has an age of about 1.25 Ma.

摘要

桑吉兰穹窿是中爪哇梭罗盆地更新世-上新世沉积物的主要地层窗口。该穹窿已出土了近80具直立人化石,其中约50具已知出土地点。据报道,与两块化石相关的角闪石(40)Ar/(39)Ar坪年龄为1.66±0.04百万年(Ma)[斯威舍,C.C.三世、柯蒂斯,G.H.、雅各布,T.、格蒂,A.G.、苏普里乔,A.和维迪亚斯莫罗(1994年)《科学》263卷,第1118 - 1121页],该穹窿提供了证据表明早期直立人在更新世最早期就扩散到了东亚。不幸的是,角闪石浮石是在乔科廷基尔山采集的,该中心地点存在复杂的岩石地层变形且标本来源存疑。为了更系统地研究桑吉兰直立人的年代,我们调查了穹窿东南象限火山沉积物的沉积框架和角闪石(40)Ar/(39)Ar年龄。在这个区域,巴庞(卡布)沉积物的暴露面积最大、变形最小且火山灰层序最完整。在五个地点,我们识别出了一系列沉积旋回,其中直立人化石与碎屑浮石相关。从采集的浮石中,八个角闪石分离物产生的(40)Ar/(39)Ar坪年龄范围从巴庞/桑吉兰组接触处的1.51±0.08 Ma到含人亚科化石层序上方某点的1.02±0.06 Ma。(40)Ar/(39)Ar年龄的时间顺序与东南象限的地层顺序一致。产出四个近乎完整颅骨的中间层年龄约为1.25 Ma。

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