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RESEARCH PRODUCT
Continental late Pliocene paleoclimatic history recorded in the Bresse Basin (France)
Henriette MéonNadine Bachiri TaoufiqGenevieve FarjanelJean-jacques PuisségurDenis-didier RousseauChristophe Petitsubject
010506 paleontology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryBoreholePaleontologyMagnitude (mathematics)myrStructural basin010502 geochemistry & geophysicsOceanographymedicine.disease_causeNeogene01 natural sciences[SHS]Humanities and Social SciencesPaleontology13. Climate actionPollenPaleoclimatologymedicine[SHS] Humanities and Social SciencesQuaternaryEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processesdescription
International audience; We present results to show that the Beaune P & C borehole, cored in the Bresse Basin (France), records late Pliocene climatic variations. Pollen analysis allows precise correlations with northern and southern European stratigraphies. Using Kukla et al.'s (1981) climate index, we show that cold climate phases occur during the Brunssumian, at around 3.2, 3.6 and 5.2 Myr B.P., respectively, in agreement with Atlantic core results. The onset of a general cooling trend is felt early in the Reuverian, at about 3 Myr B.P. which corresponds to the end of a warm event characterized by high percentages of oak. This is followed by minor climatic pulses of increasing magnitude since about 2.7 Myr B.P., that are also recorded in marine sediments. Finally a major cooling occurs at about 2.4 Myr B.P., corresponding to the beginning of the Praetiglian.
year | journal | country | edition | language |
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1992-09-01 |