globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2016.03.018
Scopus记录号: 2-s2.0-84965110368
论文题名:
Sequence stratigraphy and environmental background of the late Pleistocene and Holocene occupation in the Southeast Primor'ye (the Russian Far East)
作者: Chlachula J.; Krupyanko A.A.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2016
卷: 142
起始页码: 120
结束页码: 142
语种: 英语
英文关键词: Late Pleistocene-Holocene ; Prehistoric environmental adaptation ; Primor'ye ; Sequence stratigraphy ; Upper/Final Palaeolithic-Neolithic-Palaeo-metal cultural complexes ; Vegetation succession ; Zerkal'naya river valley
Scopus关键词: Catchments ; Climate change ; Ecology ; Ecosystems ; Employment ; Forestry ; Glacial geology ; Landforms ; Rivers ; Vegetation ; Environmental adaptation ; Late Pleistocene-Holocene ; Primor'ye ; River valley ; Sequence stratigraphy ; Upper/Final Palaeolithic-Neolithic-Palaeo-metal cultural complexes ; Vegetation successions ; Stratigraphy ; archaeology ; aridification ; climate change ; coniferous tree ; cooling ; Holocene ; mountain environment ; paleoclimate ; Pleistocene ; proxy climate record ; river channel ; salmonid culture ; sequence stratigraphy ; vegetation cover ; woodland ; Primorye ; Russian Federation ; Artemisia ; Betula nana ; Filicophyta ; Larix
英文摘要: The paper presents the results of Quaternary palaeoecology and geoarchaeology studies in the Zerkal'naya Basin, with new insights about sequenced natural shifts during the prehistoric occupation of this marginally explored NE Asian maritime territory. The Basin is part of the continental drainage system and the main physiographic and biotic corridor for peopling of the transitive coastal interior SE Primor'ye Region. The Final Pleistocene and Holocene environmental (biotic and abiotic) proxy records from the Upper/Final Palaeolithic to early historical sites document a dynamic climate change with vegetation cover transformations within riverine and mountain valley ecosystems of the Russian Far East. Most of the archaeological sites located on the low terraces and bedrock promontories along the main river channel and its tributary streams suggest traditional hunter gathered lifestyles based on seasonal salmon-fishing supplemented by pastoral economy.Tundra-forests with larch trees, dwarf birch thickets and polypod ferns from the basal stratigraphic units of the late Last Glacial occupation sites associated with the Upper Palaeolithic micro-blade and bifacial stone tool traditions (14C-dated to 19,000-12,000 cal yrs BP) indicate rather pronounced conditions and much lower MAT comparing today. Following a final Pleistocene cooling event, a major climate warming marked the onset of Holocene accompanied by a regional humidity increase promoting the formation of a mixed broadleaved-coniferous oak-dominant taiga, and culminating in the mid-Holocene Climatic Optimum. The appearance of mosaic parklands ca. 5,000-4,000 cal yrs BP. may be partly attributed to the expansion of the Far Eastern Neolithic cultures practicing forest clearance for pastures and dwellings. A progressing landscape opening indicated by the spread of light-demanding thickets and birch-dominated riverine biotopes with Artemisia suggests a further vegetation cover transformation during the late Neolithic and the early Palaeo-Metal (Bronze Age) periods. This trend corroborates the documented climate deterioration between 3,400 and 2,600 cal yrs BP, causing a regional aridification with a parkland-steppe broadening in the main SE Primor'ye river valleys. The late Holocene climate development persisted until the Little Ice Age which led to formation of the present settlement ecosystems with mixed (oak/cedar/fir-dominated) temperate maritime woodlands. © 2016 Elsevier Ltd.
资助项目: The authors thank especially P. Koaczek (Institute of Geoecology and Geoinformation, AMU Poznan) for pollen analyses (2011 fieldwork) and palaeo-vegetation data interpretations ; P. Szymura (IGG AMU) kindly provided the analytical processing of the contextual sedimentary materials ; Dr. Yu. A. Mikishin (Institute of Geology, Far Eastern Branch RAS, Vladivostok) granted access to the unpublished Ustinovka Site geology and palaeoecology data. Prof. N. Rolland (Department of Anthropology, University of Victoria) and Dr. E. Little (Geological Survey of Canada, Devon) contributed valuable comments and formal corrections of the manuscript. Palaeoenvironmental studies in the Zerkal'naya River valley were supported by the Russian Science Foundation grant no. 14-18-01165 Towns of the medieval empires of Far East and by the Far Eastern Federal University Project no. 14-08-05-2
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59583
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作者单位: Institute of Geoecology and Geoinformation, Adam Mickiewicz University, Dziegielowa 27, Poznań, Poland; Laboratory for Palaeoecology, Tomas Bata University in Zlin, nam. TGM 5555, Zlin, Czech Republic; Department of World History, Archaeology and Anthropology, The Far Eastern Federal University, Vladivostok, Russian Federation

Recommended Citation:
Chlachula J.,Krupyanko A.A.. Sequence stratigraphy and environmental background of the late Pleistocene and Holocene occupation in the Southeast Primor'ye (the Russian Far East)[J]. Quaternary Science Reviews,2016-01-01,142
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