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- > Loess-paleosol and paleoclimatic investigations. Principles, methods and criteria (supprimer)
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Par Collection Par Auteur- PÉCSI, M., (Editeur scientifique) (2)
- GREKHOVA, L.V. (1)
- GRIBCHENKO, Y.N. (1)
- PÉCSI, M., (Editeur scientifique) (1)
- VELICHKO, A.A., (Editeur scientifique) (1)
- CHICHAGOVA, O.A. (1)
- KURENKOVA, E. (1)
- PÉCSI, M. (1)
- 1995 (3)
- Archaeology ; Archeological site ; European part of Russia ; Loess ; Palaeo-environment ; Palaeolithic ; Palaeosol ; Quaternary ; Russia (1)
- Archéologie ; Loess ; Paléo-environnement ; Paléolithique ; Paléosol ; Quaternaire ; Russie ; Russie d'Europe ; Site archéologique (1)
- C 14 dating ; Humus ; Organic materials ; Palaeo-environment ; Palaeosol ; Quaternary ; Russia ; Soil properties ; West Siberia (1)
- Concept ; Corrélation stratigraphique ; Lithostratigraphie ; Loess ; Paléo-environnement ; Paléosol ; Quaternaire ; Stratigraphie (1)
- Concept ; Lithostratigraphy ; Loess ; Palaeo-environment ; Palaeosol ; Quaternary ; Stratigraphic correlation ; Stratigraphy (1)
- Datation C 14 ; Humus ; Matière organique ; Paléo-environnement ; Paléosol ; Propriétés du sol ; Quaternaire ; Russie ; Sibir' Zapadnaâ (1)
- Loess-paleosol and paleoclimatic investigations. Principles, methods and criteria (3)
- Composition, properties and radiocarbon age of humus in paleosols (1)
- Paleolithic archeology and the paleogeographical study of loess-paleosol sequences in Eastern Europe (1)
- The roles of principles and methods in loess-paleosol investigations (1)
Paleolithic archeology and the paleogeographical study of loess-paleosol sequences in Eastern Europe
- Paleolithic archeology and the paleogeographical study of loess-paleosol sequences in Eastern Europe
- Paleosols of various age from the Russian Plain and Western Siberia were studied for their humus composition and physico-chemical properties. The permanent features of humus in paleosols useful for paleogeographical reconstruction and geoecological
- and reflect different climatic and paleogeographical conditions. The A. emphasizes that the erosion gaps common in loess profiles exclude the reconstruction of some paleoclimatic events.