Historical mining and smelting in the Vosges Mountains (France) recorded in two ombrotrophic peat bogs

被引:32
作者
Forel, B. [1 ]
Monna, F. [1 ]
Petit, C. [1 ]
Bruguier, O. [2 ,3 ]
Losno, R.
Fluck, P. [4 ]
Begeot, C. [5 ]
Richard, H. [5 ]
Bichet, V. [5 ]
Chateau, C. [6 ]
机构
[1] Culture Univ Bourgogne, Lab ARTeHIS, UFR SVTE, CNRS,UMR 5594, F-21000 Dijon, France
[2] Univ Montpellier 2, Geosci Montpellier, CNRS, UMR 5243, F-34095 Montpellier 5, France
[3] Univ Paris 07, LISA, Fac Sci, CNRS, F-94010 Creteil, France
[4] UHA, CRESAT, F-68093 Mulhouse, France
[5] Univ Franche Comte, Lab Chronoenvironm, UFR Sci & Tech, CNRS,UMR 6249, F-25030 Besancon, France
[6] Univ Bourgogne, UFR SVTE, F-21000 Dijon, France
关键词
Environment; Pollution; Geochemistry; Archaeology; Lead isotopes; Peat; Mining; Metal; Vosges; Medieval; ATMOSPHERIC LEAD-DEPOSITION; ENVIRONMENTAL-IMPACT; ISOTOPIC COMPOSITION; JURA MOUNTAINS; ENRICHMENT FACTORS; PB DEPOSITION; POLLUTION; SWITZERLAND; PROFILES; GREENLAND;
D O I
10.1016/j.gexplo.2010.05.004
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Two peat sequences were sampled in the vicinity of the main mining districts of the Vosges Mountains: Sainte-Marie-aux-Mines and Plancher-les-Mines. Lead isotopic compositions and excess lead fluxes were calculated for each of these radiocarbon-dated sequences. Geochemical records are in very good agreement with the mining history of the area, well known over the last millennium. Except for an anomaly corresponding to the Middle Bronze Age which has not yet been resolved, there is no clear geochemical evidence of local metal production in the Vosges before the 10th century as excess lead deposition archived between 500 BC and 500 AD is attributed to long-range transport of polluted particulate matter. The approach described here can be applied to other mining districts where archaeological evidence is scarce or even lacking, but where past exploitation is suspected. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:9 / 20
页数:12
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