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Morphological record of pedogenesis and landscape evolution in the upper quaternary pedosediments within the upper Volga river basin
The morphological record of pedogenesis (mostly at a micromorphological scale) and the features of paleosols developed at the northern geographical extremity of the MIS3 paleopedoshpere (including the Bryansk fossil soils) are described. The profiles of the MIS3 paleosols (dark humic gley and peaty...
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Päätekijät: | , |
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Aineistotyyppi: | Artigo |
Kieli: | Russo |
Julkaistu: |
V.V. Dokuchaev Soil Science Institute
2016-11-01
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Sarja: | Бюллетень Почвенного института им. В.В. Докучаева |
Aiheet: | |
Linkit: | https://bulletin.esoil.ru/jour/article/view/243 |
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