Abstract

• Hydrozincite exhibits significant control on heavy metal mobility in other abandoned mining sites. • No morphological similarity between biomineralized hydrozincite and hydrozincite in Victoria Mine. • Microbiological effects on metal attenuation and aqueous geochemistry are negligible. • Microbial growth patterns and community structure represent oligotrophic conditions. 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 (Zn 5 (CO 3 ) 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. Graphical Abstract. .

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