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Pedostratigraphy of glaciated and non-glaciated areas in western Europe in Glaciations quaternaires dans l'Hémisphère Nord.
  • Europe ; Europe de l'Ouest ; Géographie de l'Europe ; Paléosol ; Quaternaire ; Stratigraphie
  • A correlation is given between paleosols of glaciated and non-glaciated areas. From the glaciated areas are shown paleosols in Schleswig-Holstein, especially at Sylt, and from the non-glaciated area amongst others the paleosols of Normandy at St
Is typical loess older than one million years? in Lithology and stratigraphy of loess and paleosols.
  • Is typical loess older than one million years? in Lithology and stratigraphy of loess and paleosols.
  • Datation ; Datation paléomagnétique ; Formation superficielle ; Géochronologie ; Géographie physique ; Hongrie ; Lithologie ; Loess ; Paléosol ; Sédimentologie
  • information serves to date paleosols, red and mottled clays and silts. (DLO).
Corrélation entre la présence de charbon de bois au sommet de paléosols et les dégradations climatiques
  • Corrélation entre la présence de charbon de bois au sommet de paléosols et les dégradations climatiques
  • Belgique ; Géographie de l'Europe ; Méthode ; Paléoclimatologie ; Paléosol
Pliocene and Pleistocene soil formation in the Ukraine in Lithology and stratigraphy of loess and paleosols.
  • Pliocene and Pleistocene soil formation in the Ukraine in Lithology and stratigraphy of loess and paleosols.
  • Cénozoïque ; Géographie de l'Europe ; Paléopédologie ; Paléosol ; Pliocène ; Pléistocène ; Pédogenèse ; Pédologie ; Quaternaire ; Sédimentation ; URSS d'Europe ; Ukrainskaja SSR
On the development of Pleistocene soils in Czechoslavakia in Lithology and stratigraphy of loess and paleosols.
  • On the development of Pleistocene soils in Czechoslavakia in Lithology and stratigraphy of loess and paleosols.
  • Géographie de l'Europe ; Loess ; Paléopédologie ; Paléosol ; Pleistocène ; Pédogenèse ; Quaternaire ; Roche carbonatée ; Stratigraphie ; Sédiment lacustre ; Sédiment volcanique ; Tchécoslovaquie
Pédologie, sols, paléosols et climats
  • Pédologie, sols, paléosols et climats
  • Congrès ; Domaine méditerranéen ; Géographie physique ; Holocène ; Paléoclimatologie ; Paléosol ; Quaternaire zones moyennes ; Zone subtropicale
Nachweis und Vorkommen von Paläoboden in SW-Deutschland. (Mise en évidence et présence de paléosols dans le SO de l'Allemagne)
  • Nachweis und Vorkommen von Paläoboden in SW-Deutschland. (Mise en évidence et présence de paléosols dans le SO de l'Allemagne)
  • Allemagne de l'Ouest ; Géographie physique ; Paléoclimatologie ; Paléosol ; Pédologie ; Sol ; Terra fusca
Micromorphology of a Mousterian paleosol in aeolianites at the site Habonim, Israel
  • Micromorphology of a Mousterian paleosol in aeolianites at the site Habonim, Israel
  • Argile minéral ; Datation ; Domaine méditerranéen ; Géochimie ; Israël ; Micromorphologie ; Paléo-environnement ; Paléosol ; Propriétés du sol ; Pédogenèse ; Thermoluminescence
  • A paleosol with Mousterian tools in aeolianites at the Habonim site (Carmel Coastal plain, Israel) is a complex pedosedimentary sequence which records a succession of soil-forming episodes and stages of coastal dune instability. In order to better
  • understand the nature of the Mousterian paleosol, an integrated micromorphological approach has been employed.
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
  • Loess-paleosol and paleoclimatic investigations. Principles, methods and criteria
  • Archéologie ; Loess ; Paléo-environnement ; Paléolithique ; Paléosol ; Quaternaire ; Russie ; Russie d'Europe ; Site archéologique
  • Analyse des problèmes rencontrés lors de l'étude des sites paléolithiques dans les régions de loess de la Plaine Russe. La corrélation des habitats préhistoriques avec les cycles loess-paléosols du Pléistocène supérieur apporte des résultats très
Determination of total carbonate content in some representative loess-paleosol profiles
  • Determination of total carbonate content in some representative loess-paleosol profiles
  • Loess-paleosol and paleoclimatic investigations. Principles, methods and criteria
  • Carbonate ; Concrétion ; Géochimie ; Loess ; Microstructure ; Paléosol ; Propriétés du sol ; Sol
  • Samples taken from loess and paleosols were examined for carbonate content. The main results were: 1) the carbonate content measured differed significantly when the samples were analysed jointly with the concretions occuring in them or separately
The roles of principles and methods in loess-paleosol investigations
  • The roles of principles and methods in loess-paleosol investigations
  • Loess-paleosol and paleoclimatic investigations. Principles, methods and criteria
  • Concept ; Corrélation stratigraphique ; Lithostratigraphie ; Loess ; Paléo-environnement ; Paléosol ; Quaternaire ; Stratigraphie
  • In the process of loessification, the development of loess fabric, the role of zonal, regional and partly of local environmental factors is regarded decisive. In the loess sequences various genetic types of loess pockets and paleosols occur
Paleosols and their environmental significance during Holocene in Daqingshan Mountain region of inner Mongolia, North China
  • Paleosols and their environmental significance during Holocene in Daqingshan Mountain region of inner Mongolia, North China
  • Chine ; Datation C 14 ; Microstructure ; Neimenggu ; Paléo-environnement ; Paléosol ; Variation climatique
  • Studies on the paleosol and the environmental changes during the Holocene in the Daquingshan Mountain were carried out based on the analyses of strata section structure, morphological properties, 14C data, physico-chemical characteristics and soil
  • micromorphology. The paleosol developed in five periods and it is believed that there probably experienced five climatic changes with cold-arid and warm-humid climate alternating during the Holocene.
The role of loess-paleosols formation in the study of the regularities of pedogenesis in Loess and environment - selected papers.
  • The role of loess-paleosols formation in the study of the regularities of pedogenesis in Loess and environment - selected papers.
  • Cycle climatique ; Formation superficielle ; Glaciation ; Géographie de l'Europe ; Holocène ; Loess ; Paléo-environnement ; Paléosol ; Pléistocène ; Pédogenèse ; Quaternaire ; Russkaja ravnina ; Sol ; URSS d'Europe ; Variation climatique
  • The paleosols have inherited features which correspond to previous natural climatic conditions as well as indications of the subsequent changes. That is why AA. suggest to distinguish synevent , postevent and protoevent processes revealed in loess
  • -paleosols formations. The most studied macrocycle is the late Pleistocene macrocycle comprising the Mikulino Interglacial (warm semi-cycle) and the Valdai Ice Age (cold semi-cycle).
The paleosol complex S5 in the China loess plateau. A record of climatic optimum during the last 1,2 M.A. in Loess (INQUA).
  • The paleosol complex S5 in the China loess plateau. A record of climatic optimum during the last 1,2 M.A. in Loess (INQUA).
  • Chine ; Granulométrie ; Géographie de l'Asie ; Loess ; Micromorphologie ; Palynologie ; Paléoclimat ; Paléosol ; Pléistocène ; Quaternaire
  • The A. have found that the paleosol complex S5 is of special significance in terms of Pleistocene paleoclimate. Paleopedological, micromorphological, palynological and paleomagnetic evidences indicate that this paleosol complex formed
The loess-paleosol and related subaereal sequence in Hungary in Loess (INQUA).
  • The loess-paleosol and related subaereal sequence in Hungary in Loess (INQUA).
  • Formation superficielle ; Granulométrie ; Géographie de l'Europe ; Hongrie ; Lithostratigraphie ; Loess ; Paléoclimatologie ; Paléosol ; Pliocène ; Pléistocène ; Quaternaire
  • The loess of type localities is subdivided into 3 subseries on the basis of the paleosols allowing even an Eurasian comparison for their lithostratigraphy. It can be concluded that the reddish paleosol developed under climatic, and in general
Paleorainfall reconstructions from pedogenic magnetic susceptibility variations in the Chinese loess and paleosols
  • Paleorainfall reconstructions from pedogenic magnetic susceptibility variations in the Chinese loess and paleosols
  • Chine ; Loess ; Mousson ; Paléoclimatologie ; Paléosol ; Plateau ; Propriétés du sol ; Précipitation ; Quaternaire ; Susceptibilité magnétique ; Variation climatique
  • In order to use the specific soil property, pedogenic susceptibility, as a paleoclimate recorder for the Chinese loess and paleosols, it is essential to establish that it is a property reaching near-steady state within a few thousand years
  • , and hence one providing a snapshot of soil-forming conditions for every paleosol that has had this minimum exposure time to weathering. Here, the AA. present evidence that suggests rapid development of pedogenic susceptibility, especially on loess parent
Use of rubidium to date loess and paleosols of the Louchan sequence, Central China
  • Use of rubidium to date loess and paleosols of the Louchan sequence, Central China
  • Beijing ; Chine ; Datation ; Géochimie ; Loess ; Mousson ; Paléoclimat ; Paléomagnétisme ; Paléosol ; Quaternaire ; Rubidium
  • Rb concentrations, analyzed at 20-cm intervals from the Luochuan sequence of loess and paleosols, are sensitive to the loess-paleosol alternation controlled by monsoon climate. A curvilinear relation has been developed between the measured Rb
Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols
  • Paleoclimatic significance of the mineral magnetic record of the Chinese loess and paleosols
  • Chine ; Loess ; Oxygène 18 ; Paléoclimatologie ; Paléosol ; Quaternaire ; Stratigraphie ; Susceptibilité magnétique ; Variation climatique
  • China ; Climatic variation ; Loess ; Magnetic susceptibility ; Oxygen 18 ; Paleoclimatology ; Paleosols ; Quaternary ; Stratigraphy
  • The origins of the magnetic susceptibility variations of the Chinese loess and paleosols are explored by scanning and transmission electron microscopy of magnetic extracts, and by magnetic modeling of magnetic hysteresis data, to provide quantified
Loess paleosol-sequences along climatic gradient in Northern Iran
  • Loess paleosol-sequences along climatic gradient in Northern Iran
  • Iran ; Loess ; Paléoclimat ; Paléogéographie ; Paléosol
  • In Northern Iran, loess is found in different geomorphological settings along a climatic gradient ranging from subhumid to semiarid conditions. Loess-paleosol sequences were investigated in detail in three key sections located on the northern
  • foothills of Alborz mountains and in the less hills north of Gonbad-e Kavus. The loess-paleosol sequences indicate pronounced climate changes from dry and cool to moist and warm conditions with loess deposition and soil formation, respectively
Paleoclimatic implications of micromorphic features of Quaternary paleosols of NW Himalayas
  • Paleoclimatic implications of micromorphic features of Quaternary paleosols of NW Himalayas
  • Ganga ; Inde ; Micromorphologie ; Paléoclimatologie ; Paléosol ; Plaine alluviale ; Propriétés du sol ; Pédogenèse ; Quaternaire
  • Micromorphological examination of the paleosols developed in alluvial fan deposits of the NW Himalayas and the bordering polygenetic soils (mainly Holocene) of the Gangetic Plains has been used to differenciate the pedosedimentary features
  • indicating climatic changes during late Quaternary time. This study suggests that formation of the paleosols in NW Himalayas was mainly controlled by warmer intervals during the last glaciation and the movement along the adjacent thrusts.