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Early Pleistocene 40Ar/39Ar ages for Bapang Formation hominins, Central Jawa, Indonesia
Journal article   Open access   Peer reviewed

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

Roy Larick, Russell L Ciochon, Yahdi Zaim, Sudijono, Suminto, Yan Rizal, Fachroel Aziz, Mark Reagan and Matthew Heizler
Proceedings of the National Academy of Sciences - PNAS, Vol.98(9), pp.4866-4871
04/17/2001
DOI: 10.1073/pnas.081077298
PMCID: PMC33129
PMID: 11309488
url
https://doi.org/10.1073/pnas.081077298View
Published (Version of record) Open Access

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.
Biological Sciences geochronology Homo erectus human evolution Southeast Asia tephrostratigraphy

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