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| Formato: | Artículo científico |
| Lenguaje: | en |
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Universidad Nacional Autónoma de México
2004
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| Acceso en línea: | https://www.redalyc.org/articulo.oa?id=57221111 |
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- The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain Alexey V. Rusakov Mariya A. Korkka Ciencias de la Tierra East paleosol Bryansk Soil European Plain moraine deposits The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soilformed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciationare described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene andcorresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation.The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shownthat the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in thecenter of the Russian Plain. 2004 artículo científico 1026-8774 https://www.redalyc.org/articulo.oa?id=57221111 en http://www.redalyc.org/revista.oa?id=572 Revista Mexicana de Ciencias Geológicas application/pdf Universidad Nacional Autónoma de México Revista Mexicana de Ciencias Geológicas (México) Num.1 Vol.21