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