4.2 Article

40Ar/39Ar temporal framework for the Alleret maar lacustrine sequence (French Massif-Central): Volcanological and paleoclimatic implications

Journal

QUATERNARY GEOCHRONOLOGY
Volume 5, Issue 1, Pages 20-27

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.quageo.2009.07.001

Keywords

Early Middle Pleistocene; 40Ar/39Ar; Lacustrine sediments; Ash-beds; Sancy volcano; Massif Central

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The Alleret maar (Massif Central, France) is part of the few Western European early middle Pleistocene lacustrine sequences. In the AD core several new ash layers were recovered in the 10 first meters of the sedimentary filling. We obtained three 40Ar/39Ar ages, which range from 683 +/- 5 ka (MSWD: 1.2, n = 17) to 722 6 ka (MSWD: 3.2, n = 18). All the studied ash layers belong to the Super-Besse eruptive cycle of the Sancy volcano. Based on the chronostratigraphy that we have derived we estimate that the age of the main eruption could correspond to the Sancy volcano caldera formation at 725 ka close to the end of MIS 18 and that the Super-Besse explosive episode duration lasted only about 40 ka. The time framework we build evidences that the Alleret lacustrine sequence represents a time interval of probably 180 ka spanning from MIS 18 to MIS 14. This sequence offers the first well constrained comparison between terrestrial environmental history and that preserved in marine sediments during the Mid-Pleistocene Revolution. (C) 2009 Elsevier B.V. All rights reserved.

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