机构地区:[1]Yunnan Institute of Cultural Relics and Archaeology [2]School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia [3]Mengzi Institute of Cultural Relics [4]Archaeomagnetism Laboratory, Archaeology Program, School of Historical and European Studies, La Trobe University, Melbourne 3086, Australia [5]Institute for Environmental Research, Australian Nuclear Science and Technology Organisation, Sydney 2001, Australia [6]Honghe Prefectural Institute of Cultural Relics [7]School of Earth Sciences, University of Melbourne, Melbourne 3010, Australia [8]Place, Evolution and Rock Art Heritage Unit, School of Humanities, Gold Coast Campus, Griffith University, Gold Coast 4222, Australia
出 处:《Chinese Science Bulletin》2013年第35期4472-4485,共14页
基 金:the Australian Research Council (DP0877603), the Yunnan Institute of Cultural Relics and Archaeology, the University of New South Wales and Griffith University for funding this research
摘 要:Three-dimensional mapping and section work undertaken by us in 2008 have identified 11 stratigraphic units at Maludong site.AMS radiocarbon dating of charcoal established an accurate and internally consistent age profile for the sequence of 17.8±0.2 ka to 13.2±0.1 ka.Archaeomagnetic analysis showed changes in externally derived pedogenically enhanced material consistent with a warming in climate between the cold period of Henrich Event 1 and the B lling-Aller d interstadial.Human remains recovered during the 1989 excavation were derived from a deposit dating to this interstadial,or between 14.3±0.3 ka and 13.5±0.1 ka.Anthropogenic features,including burnt rocks,baked sediment and thick charcoal and ash layers,were identified and examined through archaeomagnetic analysis.Two monkey fossils are described here,one of them being reassigned from Macaca robustus to M.aff.M.assamensis.They confirm the young age of the site and also show signs of anthropogenic alteration in the form of burning.Additional human cranial remains are reported for the first time and new data are provided for some specimens described previously.A range of new features is identified that strengthen the affinities of the Maludong remains to archaic humans.The presence of this globally unique mosaic of archaic and modern features raises important questions about human evolutionary history in East Asia during the Late Upper Pleistocene.Three-dimensional mapping and section work undertaken by us in 2008 have identified 11 stratigraphic units at Maludong site. AMS radiocarbon dating of charcoal established an accurate and internally consistent age profile for the sequence of 17.8±0.2 ka to 13.2±0.1 ka. Archaeomagnetic analysis showed changes in externally derived pedogenically enhanced material consistent with a warming in climate between the cold period of Henrich Event 1 and the Blling-AllerCd interstadial. Human remains recovered during the 1989 excavation were derived from a deposit dating to this interstadial, or between 14.3±0.3 ka and 13.5±0.1 ka. An- thropogenic features, including burnt rocks, baked sediment and thick charcoal and ash layers, were identified and examined through archaeomagnetic analysis. Two monkey fossils are described here, one of them being reassigned from Macaca robustus to M. aft'. M. assamensis. They confirm the young age of the site and also show signs of anthropogenic alteration in the form of burning. Additional human cranial remains are reported for the first time and new data are provided for some specimens described previously. A range of new features is identified that strengthen the affinities of the Maludong remains to archaic humans. The presence of this globally unique mosaic of archaic and modern features raises important questions about human evolutionary his- tory in East Asia during the Late Upper Pleistocene.
关 键 词:古人类遗址 中国西南地区 古人类学 云南省 地质 地层单位 三维制图 年龄分布
分 类 号:Q981[天文地球—古生物学与地层学] P618.130.2[生物学—人类学]
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