Conclusion : Evolution pédo-géochimique et interprétation paléobioclimatique de piémont quaternaire garonnais

Conclusions concerning chiefly the soils and geochemical weathering studies in the Garonne Pyrenean piemont. Very developed soils and strong weathered - even with neoformation of kaolinits and gibbsite - pebble alluvions, do not mean the reality of hot ancient - especially pre-Riss - paleoclimatic periods. Soils and weathered formations mean at first their "self-development" during very long interphases, between relatively short alluvial periods, interphases probably characterized by wet moderate climates.Hubschman Jacques. Conclusion : Evolution pédo-géochimique et interprétation paléobioclimatique de piémont quaternaire garonnais. In: Bulletin de l'Association française pour l'étude du quaternaire, vol. 12, n°3-4, 1975. pp. 211-216