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Par Collection Par Auteur- GARDNER, R. (1)
- KIRKBY, M.J., (Editeur scientifique) (1)
- MADRAU, S. (1)
- MCLAREN, S. (1)
- 2004 (2)
- Arid area ; Atlantic Ocean ; Carbonate ; Caribbean Sea ; Coastal environment ; Desert ; Diagenesis ; Electron microscope ; Holocene ; Interglacial ; Libya ; Mediterranean Sea ; Mexico ; Oman ; Palaeoclimatology ; Palaeosol ; Palaeosurface ; Quaternary ; Sand ; Sedimentology ; Subtropical zone (1)
- Atlantique ; Carbonate ; Diagenèse ; Domaine aride ; Désert ; Holocène ; Interglaciaire ; Libye ; Littoral ; Mer des Caraïbes ; Mexique ; Microscope électronique ; Méditerranée ; Oman ; Paléoclimatologie ; Paléosol ; Paléosurface ; Quaternaire ; Sable ; Sédimentologie ; Zone subtropicale (1)
- Cenozoic ; Climatic change ; Italy ; Palaeoclimatology ; Palaeosol ; Pedogenesis ; Sardegna ; Soil properties (1)
- Changement climatique ; Cénozoïque ; Italie ; Paléoclimatologie ; Paléosol ; Propriétés du sol ; Pédogenèse ; Sardegna (1)
- Late Quaternary vadose carbonate diagenesis in coastal and desert dune and beach sands : is there a palaeoclimatic signal ? (1)
- Terrestrial geochemical sediments and geomorphology. Special issue (1)
- The soils as palaeoclimatic indicators. A few sequences of paleosols in the Fiume Santo area (Sassari, Sardinia). Preliminary observations (1)
- Late Quaternary vadose carbonate diagenesis in coastal and desert dune and beach sands : is there a palaeoclimatic signal ?
- A study of the variation in cement amounts in aeolianite and sandy beach calcarenites that range in age from Holocene to Last Interglacial is used to assess whether a palaeoclimatic control on vadose diagenesis can be identified. Examples are taken
- from modern-day arid to subhumid settings and represent a geographical distibution ranging from Libya and Oman, to the Mediterranean, the Caribbean and Mexico. The results indicate that a palaeoclimatic signal can be identified in some deposits. However
- 2004
- The soils as palaeoclimatic indicators. A few sequences of paleosols in the Fiume Santo area (Sassari, Sardinia). Preliminary observations
- 2004