Bentaleb I., Freycon V., Gillet J.F., Oslisly Richard, Brémond L., Favier C., Fontugne M., Droissart Vincent, Gourlet-Fleury S., Guillou G., Martin C., Morin-Rivat J., Ngomanda A., Saulieu Geoffroy de, Sebag David, Subitani S., Wonkam C., Ngeutchoua G. (2015). Did the savannah "flourished" 3000 years ago in the so-called Sangha River Interval of the Guineo-Congolian rainforest ? : a retrospective study using stable isotopes and phytoliths : poster. Geophysical Research Abstracts, (17), EGU2015-5483 [1 p.]. European Geosciences Union General Assembly 2015, Vienne (AUT), 2015/04/12-17. ISSN 1607-7962.
Titre du document
Did the savannah "flourished" 3000 years ago in the so-called Sangha River Interval of the Guineo-Congolian rainforest ? : a retrospective study using stable isotopes and phytoliths : poster
Année de publication
2015
Type de document
Colloque
Auteurs
Bentaleb I., Freycon V., Gillet J.F., Oslisly Richard, Brémond L., Favier C., Fontugne M., Droissart Vincent, Gourlet-Fleury S., Guillou G., Martin C., Morin-Rivat J., Ngomanda A., Saulieu Geoffroy de, Sebag David, Subitani S., Wonkam C., Ngeutchoua G.
Source
Geophysical Research Abstracts, 2015,
(17), EGU2015-5483 [1 p.] ISSN 1607-7962
Colloque
European Geosciences Union General Assembly 2015, Vienne (AUT), 2015/04/12-17
We aim to improve our knowledge of the dynamic of the vegetation in Central Africa during the last 5 kyrs and to discuss the main hypothesis described in the literature - humans versus climatic impacts - both suggested as responsible of the Congo basin rainforest decline observed between 3 and 2.5 kyrs. We use the carbon isotopic composition of well-dated Central African soils to reconstruct the dynamic of the vegetation cover. We will discuss the carbon isotopic composition of the soil organic carbon methodology for reconstructing palaeovegetation in the light of Rayleigh distillation model. We showed that numerous sites exhibit a carbon isotopic ratios reflecting the Rayleigh distillation but few sites recorded real vegetation changes. Our study suggests that the vegetation of the Guineo-Congolian Region was disturbed between 3000 and 2000 BP (Before Present) without an extreme savannah expansion. We discussed the two hypotheses human versus climate impacts that may conduct to such new physiography of the vegetation. We suggest that the climate hypothesis is more likely than the human impact to explain the reduction of the Guineo-Congolian rainforest 3000 years ago.
Plan de classement
Evolution [076BOTA02]
;
Formations végétales [082VEGET02]
;
Archéologie [112ARCHEO]
Descripteurs
SAVANE ; FORET DENSE ; DYNAMIQUE DE VEGETATION ; PALEOENVIRONNEMENT ; VARIATION SECULAIRE ; SOL ; CARBONE ORGANIQUE ; ANALYSE ISOTOPIQUE ; FACTEUR ANTHROPIQUE ; FACTEUR CLIMATIQUE
Description Géographique
CONGO ; GUINEE ; AFRIQUE CENTRALE
Localisation
Fonds IRD [F B010064384]
Identifiant IRD
fdi:010064384
