globalchange  > 过去全球变化的重建
DOI: 10.1007/s12520-018-0664-0
WOS记录号: WOS:000466856100037
论文题名:
Environmental context and adaptations of prehistoric and early historical occupation in the Southern Altai (SW Siberia-East Kazakhstan)
作者: Chlachula, Jiri1,2
通讯作者: Chlachula, Jiri
刊名: ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES
ISSN: 1866-9557
EISSN: 1866-9565
出版年: 2019
卷: 11, 期:5, 页码:2215-2236
语种: 英语
英文关键词: Altai ; Glacial landforms ; Human occupation ; Geoarchaeology ; Permafrost
WOS关键词: LATE PLEISTOCENE ; HOLOCENE CLIMATE ; MONGOLIAN ALTAI ; DAMMED LAKES ; CENTRAL-ASIA ; BRONZE-AGE ; MOUNTAINS ; DYNAMICS ; STEPPE ; REGION
WOS学科分类: Anthropology ; Archaeology ; Geosciences, Multidisciplinary
WOS研究方向: Anthropology ; Archaeology ; Geology
英文摘要:

The Altai Mountains are well-known for their unique archaeological records, with rich, chronologically sequenced Palaeolithic, Neolithic and the Bronze Age (late fourth-early first millennium BC) sites and, in particular, the Iron Age Scytho-Siberian and early historical monuments represented by burial sites, ritual structures, and rock-art. The Altai prehistoric archaeological localities are distributed across a broad range of topographic and ecological settings, encompassing altitudinal zones from 800m asl in the lower reaches of glacial river valleys up to 2500/3000m asl on the high mountain plateaus. The partial spatial overlap of these (often multi-component) geoarchaeological loci over time suggests that similar adaptive strategies were employed by countless generations of hunter and later nomadic communitiestheir actions constrained by the locally specific forms of (palaeo-)relief and the associated ecosystems. The dynamics of the initial occupation of the boreal and alpine Altai landscapes and subsequent processes of (re-)colonisation during the Final Pleistocene-Holocene transition are directly linked to transformations in the regional hydrological systems after the LGM. The principal settings for early pastoral settlements were the xerothermic grasslands that formed on the flat glacio-lacustrine terraces which rise above the modern fluvial floodplainsthe remains of ice-dammed wastage lake basins drained at the end of the Pleistocene (15,000-13,000year BP). Marked climatic changes, evidenced by regional variations in temperature and humidity across the territory, are well attested in the geological, biotic and archaeological records. The initial Sub-Boreal aridification correlated with the beginnings of the Altai Bronze Age traditions continued until the early Iron Agecausing an expansion of parkland-steppe in the main valleys and a forest retreat in the foothills. Mountain steppes constituted the most essential food-procurement habitat for the Holocene prehistoric and historical settlements of Southern Altai. The current degradation of insular alpine permafrost poses an imminent threat to preservation of the region's most precious archaeological monumentsthe frozen burial mounds of the Pazyryk culture (sixth-third century BC) belonging to the UNESCO World cultural heritage.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/137744
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作者单位: 1.Adam Mickiewicz Univ, Inst Geoecol & Geoinformat, B Krygowskiego 10, PL-61618 Poznan, Poland
2.Tomas Bata Univ Zlin, Lab Palaeoecol, TGM 5555, Zlin 76201, Czech Republic

Recommended Citation:
Chlachula, Jiri. Environmental context and adaptations of prehistoric and early historical occupation in the Southern Altai (SW Siberia-East Kazakhstan)[J]. ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES,2019-01-01,11(5):2215-2236
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