| Literature DB >> 29549601 |
Anne-Lise Mariet1, Anne-Véronique Walter-Simonnet2, Frédéric Gimbert2, Christophe Cloquet3, Carole Bégeot2.
Abstract
Iron mining activities in the Bruche valley (Vosges Mountains, France) date historically from the Roman period to the mid-nineteenth century. The geochemical and palynological study of a core from the peat bog of Le Champ du Feu allows highlighting impacts of these activities over the past millennium. Trace metal contamination is recorded for lead (Pb), arsenic, zinc, and antimony during the Middle Ages, the sixteenth century, and from cal. AD 1750-1900, with several sources distinguished by Pb isotope analyses. Forest exploitation is attested by the palynological analysis of the core, with exploitation of Fagus for smelting processes and cutting of Abies for agro-pastoralism. This approach highlights several patterns of contamination, corresponding to the mixing sources and the contamination intensity, which can be linked to the pollen assemblage zones. Hence, anthropogenic activities such as mining and farming led to long-term modification of the landscape composition in this mountainous area.Entities:
Keywords: Lead isotopes; Mines; Peat bog; Pollen; Vegetation dynamics
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Year: 2018 PMID: 29549601 PMCID: PMC6230328 DOI: 10.1007/s13280-018-1044-9
Source DB: PubMed Journal: Ambio ISSN: 0044-7447 Impact factor: 5.129