Microbiology of an abandoned Pb–Zn mine: Impact on environmental metal contamination

Large-scale Zn, Pb, Cu, Fe and Ag mining ceased over 70 years ago in the Aran Valley (Catalonia, Spain). Some of the abandoned mining relics (e.g. tunnels, processing facilities and tailings dumps) exhibit elevated concentrations of metals in the associated water systems, thus posing a health risk i...

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Detalles Bibliográficos
Autores: Giannetta, Max G., Benaiges-Fernández, Robert, Cama, Jordi, Queralt Mitjans, Ignacio, Soler, Josep M.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2022
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/285006
Acceso en línea:http://hdl.handle.net/10261/285006
https://api.elsevier.com/content/abstract/scopus_id/85143147599
Access Level:acceso abierto
Palabra clave:Water contamination
Abandoned mine
Biomineralization
Hydrozincite
Microbiology
Descripción
Sumario:Large-scale Zn, Pb, Cu, Fe and Ag mining ceased over 70 years ago in the Aran Valley (Catalonia, Spain). Some of the abandoned mining relics (e.g. tunnels, processing facilities and tailings dumps) exhibit elevated concentrations of metals in the associated water systems, thus posing a health risk in the neighboring ecosystem. In this study, the largest underground zinc mine in the area was chosen as a field site to showcase the processes affecting metal mobility in the environment. The precipitation of hydrozincite (Zn5(CO3)2(OH)6) that occurs along the walls and ground of galleries where water flows serves as a metal (e.g. Zn, Ni, Cd) polishing mechanism. We focus on the microbiology at the site and its potential impact on metal mobility. Microbial DNA was sampled from several locations inside and outside of the mine and subsequently sequenced. This is used to further determine the relative diversity of each community to make comparisons between indoor and outdoor locations. By way of DNA sequencing of local communities, microbial batch experiments, and morphological comparisons to samples known to be a product of biomineralization, it is confirmed that the mineral forms abiotically at the mine.