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首页> 外文期刊>Quaternary International >Palaeoenvironment of the Late Pleistocene - Holocene interval in the Tanalyk river valley of the Southern Trans-Ural region (Russia)
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Palaeoenvironment of the Late Pleistocene - Holocene interval in the Tanalyk river valley of the Southern Trans-Ural region (Russia)

机译:南部跨乌拉尔地区(俄罗斯)的塔纳里克河谷晚更新世-全新世间隔的古环境

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摘要

Palaeoenvironmental reconstruction of the Tanalyk River valley (Trans-Uralian area, Bashkortostan Republic, Russia) between the Late Pleistocene and the Late Holocene has been established through biostratigraphic investigations. The Tanalyk Bronze Age settlement is located on the first overflood terrace of the Tanalyk River. From the base to the top, this terrace consists of fluvial and lacustrine deposits of the Tabulda horizon, water-slope deposits of the Kudashevo horizon (Late Pleistocene), and subaerial deposits of the Middle and Upper Holocene. During the Late Pleistocene, open landscapes covered by herbs-Artemisia-Chenopodiaceae meadow-steppe associations with Ephedra sp. admixture dominated. Betula and Pinus forests grew in small areas. Picea with Polypodiaceae understory grew in humid valleys. The climate was warm and dry during the Tabulda and cold during the Kudashevo. The subaerial Holocene deposits (soil and cultural layer) were correlated with the Boreal and Subboreal periods of the Blytt-Sernander scale. The late Subboreal climate was cold and dry. The vegetation of this period was represented by Artemisia-Chenopodiaceae steppe and by small Pinus forests with Betula, Tilia and Alnus. The climate of the Subatlantic was wet at the beginning and drier at the end. The vegetation of this period was represented mainly by the Artemisia steppe associations. Small mammals, and land and freshwater mollusc remains have been discovered in the same deposits and complete the palae-oecological characteristic of these periods. A cultural layer has been dated at 2830 ± 110 BP LU-3713 on bones of Equus sp. Numerous Holocene large mammal remains have been found in the cultural layer deposits, dated to Subboreal-3. The large Holocene mammal fauna is constituted of eurybiotic species and species of semi-open landscapes. Bone remains of domestic animals dominate in the collection. Pastoral farming constituted the base of the economy of this ancient people, and the role of hunting was small. The investigated area is now covered by the waters of the Tanalyk water reservoir.
机译:通过生物地层学调查,已经确定了晚更新世和晚全新世之间的塔纳利克河谷(俄罗斯,巴什科尔托斯坦共和国,跨乌拉里地区)的古环境重建。 Tanalyk青铜时代的定居点位于Tanalyk河的第一个溢洪阶地上。从底部到顶部,该阶地包括塔布达河层的河流和湖相沉积物,库达谢沃层位的水坡沉积物(晚更新世)以及中新世和上新世的陆上沉积物。在晚更新世期间,开阔的地貌被药草-蒿-藜科草甸-草原协会与麻黄(Ephedra sp。)外加剂为主。桦树和松树森林生长在小区域。云杉和木Poly科植物在潮湿的山谷中生长。在塔布达(Tabulda),气候温暖干燥。地下全新世沉积物(土壤和文化层)与Blytt-Sernander规模的北方和次北方时代相关。 Subboreal晚期气候干燥阴冷。这一时期的植被以艾蒿-藜科草原和带桦木,T树和Al木的小松林为代表。次大西洋的气候开始时是湿润的,而结束时是较干燥的。这一时期的植被主要以蒿蒿草原协会为代表。在相同的矿床中发现了小型哺乳动物以及陆地和淡水软体动物的遗体,并完成了这些时期的古生态特征。在Equus sp。的骨骼上已形成了2830±110 BP LU-3713的培养层。在文化层沉积物中发现了许多全新世的大型哺乳动物遗骸,其历史可追溯到Subboreal-3。全新世的大型哺乳动物动物群由尤利希生物物种和半开放景观物种组成。家畜的骨骸在该集合中占主导地位。牧业是这个古代人的经济基础,狩猎的作用很小。现在,被调查的地区被塔纳利克水库的水所覆盖。

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  • 来源
    《Quaternary International》 |2013年第23期|74-84|共11页
  • 作者单位

    Institute of Ecology of Plants and Animals, Ural Branch, Russian Academy of Sciences, 8th March St., 202, 620008, Ekaterinburg, Russia;

    Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences K. Marx St., 16/2, 450000, Ufa-centre, Bashkortostan, Russia;

    Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences K. Marx St., 16/2, 450000, Ufa-centre, Bashkortostan, Russia;

    Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences K. Marx St., 16/2, 450000, Ufa-centre, Bashkortostan, Russia;

    Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences K. Marx St., 16/2, 450000, Ufa-centre, Bashkortostan, Russia;

    Institute of Geology, Ufa Scientific Centre, Russian Academy of Sciences K. Marx St., 16/2, 450000, Ufa-centre, Bashkortostan, Russia;

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