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Post-Saalian transformation of dry valleys in eastern Europe: An example from NE Poland

机译:萨利期后东欧干旱谷地的转型:以波兰东北地区为例

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摘要

The studies were conducted in a dry valley in NE Poland. They were aimed at determining the origin of this structure and tracing the processes that have shaped the dry valley in a time span of about 130 ka. The research included detailed geological mapping, including piercing of a number of boreholes and electrical resistivity tomography (ERT) surveys. The obtained material was pollen analysed, OSL dated, and the grain size distribution and the morphoscopy of sand quartz grains were investigated; additionally the organic matter (OM) content was determined. Based on the obtained results it was concluded that the structure currently occupied by sediments of the dry valley was formed during the Warta Stadial of the Odranian Glaciation (Saalian; MIS 6) as a glacial tunnel valley. Small, probably isolated depressions functioned in the dry valley bottom after the ice sheet retreat. The sediments record a full succession of climate oscillations from the Eemian Interglacial (MIS 5e) (pollen zones E1 to E7) through the Early Vistulian (MIS 5a-5d) to MIS 4. In the Early Vistulian, the depressions functioned as lakes, or got shallower and were replaced by peat-bogs, depending on the climate conditions. During MIS 4, the bottom of the dry valley was subjected to erosion as a result of concentrated water flow. This caused draining of the existing depressions and their incorporation within the flow. Probably during MIS 3, solifluction was activated on the slopes of the dry valley. During LGM, permafrost aggradation occurred in the study area, recorded by two generations of epigenetic sand wedges and development of aeolian processes. In contrast to analogous processes within the European Sand Belt, the latter processes acted for a short time and only locally. The final record are Holocene soils. It seems that the analysed valley is a good example of palaeoenvironmental conditions in Eastern Europe. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:这些研究是在波兰东北部的一个干燥山谷中进行的。他们的目的是确定这种结构的起源,并追踪在约130 ka的时间范围内形成干旱谷的过程。该研究包括详细的地质测绘,包括许多钻孔的穿刺和电阻率层析成像(ERT)调查。对得到的材料进行花粉分析,OSL测年,研究了砂石英晶粒的粒度分布和形貌。此外,测定了有机物(OM)含量。根据获得的结果,可以得出结论,干谷沉积物目前所占据的结构是在奥德兰冰川的瓦尔塔体育场(Saalian; MIS 6)期间形成的,是一个冰川隧道谷。冰盖退缩后,干燥的山谷底部开始出现可能很小的凹陷。沉积物记录了从艾米斯冰间期(MIS 5e)(花粉区E1至E7)到早期Vistulian(MIS 5a-5d)到MIS 4的全部气候振荡。在Vistulian早期,,陷起着湖泊作用,或变浅,取而代之的是泥炭沼泽,具体取决于气候条件。在MIS 4期间,由于集中的水流,干谷的底部受到了侵蚀。这造成了现有凹陷的排空,并将它们合并到流中。可能是在MIS 3期间,干旱谷的斜坡上发生了固溶作用。在LGM期间,研究区发生了多年冻土的凝结,这是由两代后生砂楔和风成过程的发展所记录的。与欧洲沙带内部的类似过程相反,后者的过程仅在短时间内且仅在本地起作用。最终记录是全新世土壤。经过分析的山谷似乎是东欧古环境状况的一个很好的例子。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2018年第ptaa期|161-177|共17页
  • 作者单位

    Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland;

    Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland;

    Nicolaus Copernicus Univ, Fac Earth Sci, Lwowska Str 1, PL-87100 Torun, Poland;

    Univ Bialystok, Fac Biol & Chem, Ciolkowskiego Str 1J, PL-15245 Bialystok, Poland;

    Nicolaus Copernicus Univ, Fac Earth Sci, Lwowska Str 1, PL-87100 Torun, Poland;

    Univ Bialystok, Fac Biol & Chem, Ciolkowskiego Str 1J, PL-15245 Bialystok, Poland;

    Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland;

    Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland;

    Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dry valley; Eemian interglaciale; Early Vistulian; Lake fluctuation; Pollen analysis; Periglacial;

    机译:干旱谷;Eemian冰川间;Vistulian早期;湖面涨落;花粉分析;边缘冰川;
  • 入库时间 2022-08-18 03:35:06

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