FN Archimer Export Format PT J TI Vegetation dynamics in southern France during the last 30 ky BP in the light of marine palynology BT AF BEAUDOUIN, Célia JOUET, Gwenael SUC, Jean-Pierre BERNE, Serge ESCARGUELA, Gilles AS 1:1,2;2:3,4;3:1;4:4;5:1; FF 1:;2:PDG-DOP-DCB-GM-LES;3:;4:PDG-DOP-DCB-GM-LES;5:; C1 Université Claude Bernard Lyon 1? UMR CNRS 5125 Laboratoire PaléoEnvironnements et PaléobioSphère, Campus La Doua, Bâtiment Géode, 2 rue Dubois, 69622 Villeurbanne Cédex, France Department of Earth Sciences, Sun Yat-sen University, 135 Xin Gang Xi Lu, 510275 Guangzhou, China Institut Universitaire Européen de la Mer, UMR CNRS 6538 Domaines océaniques, 1 Place Copernic, 29280 Plouzané, France IFREMER, Laboratoire Environnements Sédimentaires, Géosciences Marines, Centre de Brest, BP 70, 29280 Plouzané, France C2 UNIV LYON, FRANCE UNIV SUN YAT-SEN, CHINA IUEM, FRANCE IFREMER, FRANCE SI BREST SE PDG-DOP-DCB-GM-LES IN WOS Ifremer jusqu'en 2018 copubli-france copubli-univ-france copubli-int-hors-europe copubli-sud IF 4.11 TC 32 TU Centre national de la recherche scientifique Institut français de recherche pour l'exploitation de la mer Service Hydrographique et Océanographique de la Marine Université Claude Bernard - Lyon 1 Université de Bretagne Occidentale Université de Bretagne-Sud École normale supérieure de Lyon UR https://archimer.ifremer.fr/doc/2007/publication-2804.pdf LA English DT Article CR IMAGES V LEG 1-MD114 IMAGES V LEG 4-MD114 PROMESS 1 STRATAFORM 1 BO Marion Dufresne Bavenit Le Suroît DE ;Mediterranean Sea;Pleistocene;Climate;Vegetation AB The composition of the glacial vegetation of southern French plains has been a matter of debate for several decades. Vegetation is considered as steppic according to French and Spanish lacustrine pollen records whereas cave deposits suggest the presence of mesothermophilous trees through the Last Glacial Maximum. In our paper, we display new palynological records from marine sediments of the Gulf of Lions. They indicate the presence of Abies, Picea and deciduous Quercus in the Gulf of Lions, certainly located in the drainage basins of the Pyreneo-Languedocian rivers. These populations that were sensitive to short climatic events during Marine Isotopic Stage 2 could have been linked to northeastern Spanish and southeastern French relicts already evidenced by phylogenetic data. These trees were absent from the Rhone drainage basin during the deglaciation and certainly also disappeared from the Pyreneo-Languedocian drainage basins from ca 17 to 15 ky cal BP. Finally, the Last Glacial Maximum does not appear as stable, cold and dry as previously thought. PY 2007 PD APR SO Quaternary Science Reviews SN 0277-3791 PU Elsevier VL 26 IS 7-8 UT 000248732200014 BP 1037 EP 1054 DI 10.1016/j.quascirev.2006.12.009 ID 2804 ER EF