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High-resolution record of the Matuyama–Brunhes transition constrains the age of Javanese Homo erectus in the Sangiran dome, Indonesia
Abstract
A detailed paleomagnetic study conducted in the Sangiran area, Java, has provided a reliable age constraint on hominid fossil-bearing formations. A reverse-to-normal polarity transition marks a 7-m thick section across the Upper Tuff in the Bapang Formation. The transition has three short reversal episodes and is overlain by a thick normal polarity magnetozone that was fission-track dated to the Brunhes chron. This pattern closely resembles another high-resolution Matuyama–Brunhes (MB) transition record in an Osaka Bay marine core. In the Sangiran sediments, four successive transitional polarity fields lie just below the presumed main MB boundary. Their virtual geomagnetic poles cluster in the western South Pacific, partly overlapping the transitional virtual geomagnetic poles from Hawaiian and Canary Islands’ lavas, which have a mean 40 Ar/ 39 Ar age of 776 ± 2 ka. Thus, the polarity transition is unambiguously the MB boundary. A revised correlation of tuff layers in the Bapang Formation reveals that the hominid last occurrence and the tektite level in the Sangiran area are nearly coincident, just below the Upper Middle Tuff, which underlies the MB transition. The stratigraphic relationship of the tektite level to the MB transition in the Sangiran area is consistent with deep-sea core data that show that the meteorite impact preceded the MB reversal by about 12 ka. The MB boundary currently defines the uppermost horizon yielding Homo erectus fossils in the Sangiran area.
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“Conversely during the deposition of the more lacustrine and fluviatile Bapang fm., which may span up to 1 Ma until the last appearance of H. erectus in Sangiran ca. 0.78 Ma35, sedimentation rates are much lower.”
From Javanese homo erectus on the move in SE asia circa 1.8 ma (2022) · cites this paper as [35]
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“The dated unit is bracketed by layers of compatible ages, from the base of the Sangiran fm. (⁴⁰Ar/³⁹Ar and paleomagnetic ages of ∼1.914 and ∼1.7 Ma12,13) and from its core (U-Pb ages of ∼1.7 Ma15), to the Upper Tuff unit in the upper part of the Bapang fm. (paleomagnetic ages, ∼0.8 Ma35).”
From Javanese homo erectus on the move in SE asia circa 1.8 ma (2022) · cites this paper as [35]
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Metadata
- Authors
- Hyodo, M., Matsu'ura, S., Kamishima, Y., Kondo, M., Takeshita, Y., Kitaba, I., Danhara, T., Aziz, F., Kurniawan, I., & Kumai, H.
- Affiliations
- Research Center for Inland Seas, and
- Laboratory of Physical Anthropology, Ochanomizu University, Tokyo 112-8610, Japan;
- Department of Earth and Planetary Sciences, Kobe University, Kobe 657-8501, Japan;
- Faculty of Education, Shinshu University, Nagano 380-8544, Japan;
- Kyoto Fission-Track Corporation, Kyoto 603-8832, Japan;
- Centre for Geological Survey, Geological Agency, Bandung 40122, Indonesia; and
- Department of Geoscience, Osaka City University, Osaka 558-8585, Japan
- Venue
- Proceedings of the National Academy of Sciences
- Publisher
- National Academy of Sciences
- Published
- 2011-11-21
- Volume
- 108
- Issue
- 49
- Pages
- 19563-19568
- ISSN
- 0027-8424
- 1091-6490
- Cited by
- 62
- References
- 0
- Language
- en
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- Hyodo, M., Matsu'ura, S., Kamishima, Y., Kondo, M., Takeshita, Y., Kitaba, I., Danhara, T., Aziz, F., Kurniawan, I., & Kumai, H. (2011). High-resolution record of the Matuyama–Brunhes transition constrains the age of Javanese Homo erectus in the Sangiran dome, Indonesia. Proceedings of the National Academy of Sciences. https://doi.org/10.1073/pnas.1113106108