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  • The palaeoclimatic significance of paleosols in Southern Fezzan (Libyan Sahara) : morphological and micromorphological aspects
  • , and discusses their palaeoclimatic significance in relation to Late Tertiary and Quaternary palaeoenvironmental changes in North Africa.
  • 1998
  • which was created by a rock collapse that dammed the paleovalley of the Doubs River about 12 000 years ago. Since this event, the sediment trap provides a continuous palaeoclimatic record for the Postglacial period. In conclusion, the story
  • 1998