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高强度采矿对陆地和水生生态系统的影响:以澳大利亚塔斯马尼亚凉爽温带地区的沉积物污染和钙含量下降为例。

The impacts of intensive mining on terrestrial and aquatic ecosystems: A case of sediment pollution and calcium decline in cool temperate Tasmania, Australia.

机构信息

Lincoln Centre for Water and Planetary Health, School of Geography, University of Lincoln, Lincoln, UK; School of Geography, University of Melbourne, Melbourne, Australia.

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.

出版信息

Environ Pollut. 2020 Oct;265(Pt A):114695. doi: 10.1016/j.envpol.2020.114695. Epub 2020 May 1.

Abstract

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 (C and Pb), 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.

摘要

采矿通过酸化、重金属污染、泥沙负荷和钙下降对水生生态系统造成广泛破坏。然而,人们对南半球淡水系统采矿的影响知之甚少。澳大利亚塔斯马尼亚州西部就是一个很好的例子,该地区在 19 世纪广泛开采,导致严重的环境污染。为了评估采矿对该地区水生生态系统的影响,我们对来自塔斯马尼亚州欧文湖的湖泊沉积物进行了多指标研究。这项研究包括放射性测年(C 和 Pb)、沉积物地球化学(XRF 和 ICP-MS)、花粉、木炭和硅藻的组合。广义加性混合模型用于检验水生生态系统的变化是否可以用其他协变量来解释。该记录的结果发现了四个关键的影响阶段:(1)采矿前,(2)早期采矿,(3)密集采矿,和(4)采矿后。在采矿前,重金属浓度低、沉降缓慢、火灾活动低、生物量高,表明存在未受影响的条件。此时的水生环境贫营养、营养不良,光照充足,是全新世塔斯马尼亚西部湖泊的典型特征。繁荣的采矿业导致燃烧增加,景观生物量减少,沉降增加,导致水生环境的光照减少。20 世纪 30 年代在莱尔山的大规模采矿导致重金属污染物(Pb、Cu 和 Co)达到峰值,无机输入的进一步增加导致低光照的湖泊环境受到干扰(以 Hantzschia amphioxys 和 Pinnularia divergentissima 为主)。1994 年莱尔山铜矿公司关闭后,Ca 下降到低于采矿前的水平,导致新的硅藻组合和变形的硅藻阀。因此,欧文湖的记录表明,在莱尔山矿业公司停止采矿很久之后,这里的沉积物仍受到严重污染,而且仍在继续受到采矿的影响。

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