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The impacts of intensive mining on terrestrial and aquatic ecosystems: A case of sediment pollution and calcium decline in cool temperate Tasmania, Australia.
Beck, K K; Mariani, M; Fletcher, M-S; Schneider, L; Aquino-López, M A; Gadd, P S; Heijnis, H; Saunders, K M; Zawadzki, A.
Afiliação
  • Beck KK; Lincoln Centre for Water and Planetary Health, School of Geography, University of Lincoln, Lincoln, UK; School of Geography, University of Melbourne, Melbourne, Australia. Electronic address: kbeck@lincoln.ac.uk.
  • Mariani M; School of Geography, University of Melbourne, Melbourne, Australia; School of Geography, University of Nottingham, Nottingham, UK; ANU College of Asia and the Pacific, Australian National University, Canberra, Australia.
  • Fletcher MS; School of Geography, University of Melbourne, Melbourne, Australia.
  • Schneider L; ANU College of Asia and the Pacific, Australian National University, Canberra, Australia.
  • Aquino-López MA; Maynooth University, Arts and Humanities Institute, Maynooth, Co. Kildare, Ireland.
  • Gadd PS; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia.
  • Heijnis H; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia.
  • Saunders KM; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia.
  • Zawadzki A; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia.
Environ Pollut ; 265(Pt A): 114695, 2020 Oct.
Article em En | MEDLINE | ID: mdl-32806416
Mining causes extensive damage to aquatic ecosystems via acidification, heavy metal pollution, sediment loading, and Ca decline. Yet little is known about the effects of mining on freshwater systems in the Southern Hemisphere. A case in point is the region of western Tasmania, Australia, an area extensively mined in the 19th century, resulting in severe environmental contamination. In order to assess the impacts of mining on aquatic ecosystems in this region, we present a multiproxy investigation of the lacustrine sediments from Owen Tarn, Tasmania. This study includes a combination of radiometric dating (14C and 210Pb), sediment geochemistry (XRF and ICP-MS), pollen, charcoal and diatoms. Generalised additive mixed models were used to test if changes in the aquatic ecosystem can be explained by other covariates. Results from this record found four key impact phases: (1) Pre-mining, (2) Early mining, (3) Intense mining, and (4) Post-mining. Before mining, low heavy metal concentrations, slow sedimentation, low fire activity, and high biomass indicate pre-impact conditions. The aquatic environment at this time was oligotrophic and dystrophic with sufficient light availability, typical of western Tasmanian lakes during the Holocene. Prosperous mining resulted in increased burning, a decrease in landscape biomass and an increase in sedimentation resulting in decreased light availability of the aquatic environment. Extensive mining at Mount Lyell in the 1930s resulted in peak heavy metal pollutants (Pb, Cu and Co) and a further increase in inorganic inputs resulted in a disturbed low light lake environment (dominated by Hantzschia amphioxys and Pinnularia divergentissima). Following the closure of the Mount Lyell Co. in 1994 CE, Ca declined to below pre-mining levels resulting in a new diatom assemblage and deformed diatom valves. Therefore, the Owen Tarn record demonstrates severe sediment pollution and continued impacts of mining long after mining has stopped at Mt. Lyell Mining Co.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Poluentes Químicos da Água / Ecossistema Idioma: En Ano de publicação: 2020 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Poluentes Químicos da Água / Ecossistema Idioma: En Ano de publicação: 2020 Tipo de documento: Article