OSL and ESR studies of Aeolian quartz from the Upper Pleistocene loess sequence of Nussloch (Germany)

被引:30
作者
Tissoux, H. [1 ,2 ]
Valladas, H. [2 ]
Voinchet, P. [1 ]
Reyss, J. L. [2 ]
Mercier, N. [3 ]
Falgueres, C. [1 ]
Bahain, J. -J. [1 ]
Zoeller, L. [4 ]
Antoine, P. [5 ]
机构
[1] Museum Natl Hist Nat, Dept Prehist, UMR 7194, F-75013 Paris, France
[2] UVSQ, CEA, CNRS, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France
[3] Univ Bordeaux, CNRS, UMR5060, Ctr Rech Phys Appl Archeol, F-33607 Pessac, France
[4] Univ Bayreuth, Chair Geomorphol, D-95440 Bayreuth, Germany
[5] UMR8591, Lab Geog Phys, F-92195 Meudon, France
关键词
Nussloch; Upper Pleistocene; Quartz; Loess; ESR; OSL; REGENERATIVE-DOSE PROTOCOL; UPPER RHINE AREA; PALEOSOL SEQUENCES; CLIMATIC CHANGES; VALLEY; CHRONOLOGIES; DEPOSITS; RECORDS; IMPACT; C-14;
D O I
10.1016/j.quageo.2009.03.009
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
As part of a chronological study of the famous Upper Pleistocene Nussloch (Germany) loess sequence, three samples were collected to check the applicability of palaeodosimetric dating methods (OSL and ESR) to quartz grains. The ESR-multicentre method showed a partial bleaching of the ESR centers in aeolian sands. This partial bleaching was also observed by OSL. Laminated loess seemed to be sufficiently bleached but showed a large scatter of the doses, which we ascribed to heterogeneous responses of the luminescent grains to the SAR protocol. Ages could nevertheless be calculated for the three samples and were found to be somewhat older than the IRSL and (14)C ages obtained for the same layers of the laminated loess. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:131 / 136
页数:6
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