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Article dans une revue
Geochronological arguments for a close relationship between surficial formation profiles and environmental crisis (c. 3000-2000 BP) in Gabon (Central Africa).
Abstract : We present new 14C data on charcoal fragments recovered from the lower (coarse-grained Stone Line) and upper (fine-grained Cover Horizon) portions of surficial formation profiles in Gabon. These data and others compiled from the literature enable a reconstruction of the Upper Holocene geological regional history of Gabon. The connection between the geological events recorded in the surficial formations and the upper Holocene environmental crisis is discussed and a scenario connecting geological events with climatic and environmental changes is proposed. Such a scenario suggests that following the climatic crisis, the reconstitution of soils by aeolian sedimentation could have been an important factor of Bantu expansion.
https://hal-brgm.archives-ouvertes.fr/hal-00904029
Contributeur : Denis Thiéblemont Connectez-vous pour contacter le contributeur
Soumis le : mercredi 13 novembre 2013 - 15:41:08
Dernière modification le : lundi 28 mars 2022 - 09:38:09
Contributeur : Denis Thiéblemont Connectez-vous pour contacter le contributeur
Soumis le : mercredi 13 novembre 2013 - 15:41:08
Dernière modification le : lundi 28 mars 2022 - 09:38:09