FN Archimer Export Format
PT J
TI Onshore and offshore evidences for four abrupt “warming” episodes during MIS 6 at the westernmost tip of continental Europe: did they control the migrations of Neanderthals?
BT 
AF Lefort, J.P.
   Danukalova, G.A.
   Eynaud, F.
   Monnier, J.L.
AS 1:1;2:2,3;3:4;4:1;
FF 1:;2:;3:;4:;
C1 CNRS UMR 6566 CReAAH, Université de Rennes 1, Campus de Beaulieu, Laboratoire Archéosciences (bât. 24-25), CS 74205, 35042, Rennes Cedex, France
   Institute of Geology, Ufimian Federal Research Centre, Russian Academy of Sciences, 450077, Ufa, K. Marx, Str. 16/2, Russia
   Kazan Federal University, 18, Kremlevskaya St., 420008, Kazan, Russia
   UMR 5805 EPOC, Université de Bordeaux, Allée Goeffroy Saint-Hilaire, F-33615, Pessac, France
C2 CNRS, FRANCE
   RUSSIAN ACAD SCI, RUSSIA
   UNIV FED KAZAN, RUSSIA
   UNIV BORDEAUX, FRANCE
IF 2.003
TC 2
UR https://archimer.ifremer.fr/doc/00483/59445/85210.pdf
LA English
DT Article
CR MD 133 / SEDICAR
BO Marion Dufresne
DE ;MIS 6 climatic changes;Westernmost Europe;Malacology;"Warming" episodes;Palaeolithic migrations
AB The total shell production typical of the Pupilla association in the onshore site of Nantois (Brittany, France) evidenced for the first time four brief, abrupt, warm and humid episodes during the Upper Saalian (MIS 6) loess deposition. These “warming” events were also found in the marine deposits of the Celtic Sea (MD03-2692 core). Comparison with the variations of the sea-level, show that the “warming” episodes were not only of regional interest but corresponded to global events ruled by precession and insolation cycles. Other comparisons with biomarker records (mollusсs, charcoal and rodents) of the Paris Basin (Villiers-Adam) and Jersey Island (La Cotte de Saint Brolade) confirm the existence of these warmer events. Tentative correlations with the discontinuous Neanderthal dwelling phases recorded in Brittany suggest that these populations were mainly (only?) present in Westernmost Europe during the warmer episodes. 
PY 2019
PD DEC
SO Quaternary International
SN 1040-6182
PU Elsevier BV
VL 534
UT 000503173900009
BP 103
EP 115
DI 10.1016/j.quaint.2019.02.024
ID 59445
ER

EF