The Role of Microbial Sulfur Cycling in the Fate of Metals in Mining-impacted Environments PDF Download
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Author: John William Moreau
Publisher:
ISBN:
Category :
Languages : en
Pages : 528
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Author: John William Moreau
Publisher:
ISBN:
Category :
Languages : en
Pages : 528
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Author: Diana Ayala
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Mining activity accelerates the generation of an extremely toxic fluid known as acid mine drainage (AMD). AMD has low pH and high sulfate, iron, and other metal(loid)s content. Environments impacted by AMD are uninhabitable for most biota. However, acid-tolerant and acidophilic microorganisms thrive under AMD harsh conditions relying on sulfur and iron compounds as main electron donors and acceptors. They are resistant to metal toxicity and can even promote metal precipitation. Many of these microorganisms are now applied in greener technologies for mining and AMD remediation purposes. In the first part of this dissertation, I studied microbial communities responsible for ferrous iron oxidation in lab-scale low-pH reactors. Such reactors constitute a cost-effective alternative for the removal of iron, Fe(II), from AMD. Like many microbial reactors, their overall function can be affected by environmental perturbations such as changes in pH. However, reactors, previously operated by Dr. William Burgos's group at different pH values and Fe(II) concentrations, were shown to be stable with respect to the general rate of microbial Fe(II) oxidation. In chapter 2, I focused on studying biofilms collected at three different times from the reactors when operated under the same chemical conditions (e.g., pH = 2.7 and influent [Fe(II)] = 300 mg.L-1). The microbial communities had differential growth of multiple autotrophic Fe(II) oxidizers affiliated with Acidithiobacillus, Ferrovum, and Leptospirillum genera. Metagenomic analyses of these communities revealed differences in the metabolic potential of the dominant taxa for key metabolic functions such as Fe(II) oxidation, carbon fixation, oxygen reduction, nitrogen acquisition, and biofilm formation. The distinct metabolic potential of the autotrophic Fe(II) oxidizers allowed their access to different resources over time and coexistence in the biofilm. The distribution of key metabolic functions across the multiple coexisting taxa supported functional redundancy and imparted stability to the reactors with respect to Fe(II) oxidation at low pH. In the second part of this dissertation, I focused on microbial communities living in the acidic pit lake Cueva de la Mora (CM) located in the Iberian Pyrite Belt in Spain. CM is a stratified lake with dramatic physico-chemical gradients and increasing metal concentrations with depth. It is one of the most extensively characterized acidic pit lakes in the world. However, knowledge gaps existed with respect to active microbial activity shaping the unique geochemistry of CM and potentially contributing to the lake's natural attenuation. By using a combination of metagenomics and metatranscriptomics, I studied the in situ microbiology of this acidic pit lake from three perspectives: metal resistance (Chapter 3), element cycling (Chapter 4), and contributions to biosulfidogenesis (Chapter 5). CM has three distinct microbial communities characterizing the upper layer, chemocline, and deep layer of the lake. Chapter 3 described the microbial composition of each layer by shotgun metagenomics only. Chapter 4 included results from amplicon sequencing. The upper layer was dominated by the green algae Coccomyxa onubensis from the phylum Chlorophyta. Surprisingly, despite having very limited available light, C. onubensis was also present in the chemocline along with bacteria mainly from the phylum Proteobacteria. Desulfomonile spp. were the most abundant bacteria in the chemocline followed by taxa affiliated with the order Ca. Acidulodesulfobacterales (non-described previously). Until now, the deep layer was largely uncharacterized. Currently, the metagenomic analysis revealed abundance of the archaea Euryarchaeota along with bacteria from the superphylum Patescibacteria. Other abundant bacteria were part of the phyla Actinobacteria, Chloroflexi, and Nitrospirae. Findings with respect to microbial metal resistance in CM were described in Chapter 3. A database of 222 metal resistant genes (MRGs) was constructed and used to compare MRGs across the three communities representing each layer of the lake. Genes (from metagenomes) and transcripts (from metatranscriptomes) annotated as MRGs were quantified per layer and classified by mechanisms of resistance and metal(loid). Eukaryotes, bacteria, and archaea expressed different metal resistance strategies. Expression of genes involved in resistance to the most toxic metals was not correlated to dissolved metal concentrations, especially for As and Cu. Finally, MRG expression patterns were studied among in silico populations (represented by metagenome assembled genomes - MAGs) from the same depth, and differences in metal resistance mechanisms among members of the same community were found. Chapter 4 focused on the active roles of predominant phyla in carbon, sulfur, iron, and nitrogen cycling in CM. The green algae Coccomyxa onubensis were active in the upper layer and chemocline and provided organic carbon to the less abundant heterotrophic bacteria in the upper layer and chemocline. Organic carbon associated with settling ferric iron minerals dissolved in the deep layer might fuel the heterotrophic activity of the most abundant taxa in the deep layer: Thermoplasmatales (Euryarchaeota). Autotrophic activity was observed in the chemocline and deep layer mainly associated with bacteria from the phylum Proteobacteria, Actinobacteria, Chloroflexi, and/or Nitrospirae. As expected, microbial sulfide/sulfur oxidation was active in the chemocline associated with Desulfomonile and Ca. Acidulodesulfobacterium populations which were also involved in sulfate reduction. Sulfide/sulfur oxidation was surprisingly active in the deep layer associated with the most abundant taxa (Euryarchaeota) and other less abundant bacteria such as Actinobacteria populations. The abundance of transcripts involved in oxygen respiration in the deep layer was also unexpected and related to potential sulfur-oxidizing populations. Activity for microbial sulfate reduction in the deep layer was associated with uncultured taxa from Actinobacteria, Chloroflexi, Nitrospirae, Firmicutes, and Proteobacteria. Fe(II) oxidation was mainly observed in the chemocline contributed by Ferrovum, Leptospirillum, and Ca. Acidulodesulfobacterium taxa. Although expected in the chemocline, no genomic information was gathered to support activity for Fe(III) reduction. The deep layer had Fe(III) reduction activity associated with low abundant Geobacter bacteria. Nitrogen fixation, nitrate reduction, and ammonia oxidation were active in the chemocline with Ca. Acidulodesulfobacterium populations as main contributors. In contrast the upper layer presented active assimilatory nitrogen metabolisms associated with Coccomyxa, and the deep layer presented dissimilatory nitrate reduction associated with uncultured Actinobacteria and Proteobacteria. Chapter 5 described novel acidophilic populations involved in active biosulfidogenesis in the deep layer of CM. Biosulfidogenesis is the generation of sulfide by microbial reduction of oxidized sulfur compounds. Sulfide precipitates dissolved metals as metal-sulfides that can be removed from the system. Despite the high sulfate and metal concentrations of the deep layer of CM, biosulfidogenic taxa had not been reported before. In Chapter 5, I reconstructed eighteen high quality MAGs from the deep layer that represented abundant phyla such as Euryarchaeota, Parcubacteria, Actinobacteria, Chloroflexi, and Nitrospirae. A phylogenetic analysis of the MAGs revealed their novelty as no similar culture or uncultured genomes to the MAGs were found. Thirteen of these MAGs had at least one gene, and three MAGs presented most genes and transcripts involved in sulfate reduction. The three MAGs belonged to the Actinobacteria, Chloroflexi, and Nitrospirae phyla, with no previous representatives of acidophilic and mesophilic sulfate reducers. These populations were predicted to be actively contributing to biosulfidogenesis in the deep layer. In accordance with Chapter 4 findings, MAGs representing some of the abundant populations in the deep layer had predicted activity for oxidation of sulfur compounds. These results suggest that CM has the potential of natural attenuation of metals by biosulfidogenesis, but such potential is diminished by cryptic sulfur cycling.
Author: Pamela J. Edwards
Publisher:
ISBN:
Category : Forest soils
Languages : en
Pages : 48
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Author:
Publisher:
ISBN:
Category : Dissertations, Academic
Languages : en
Pages : 886
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Author: Alexandra V. Turchyn
Publisher: Frontiers Media SA
ISBN: 2889456528
Category :
Languages : en
Pages : 213
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Sulfur has many redox states and is a major metabolite in suboxic and anaerobic environments including, but not restricted to, marine and marginal marine sediments, the water column of oxygen minimum zones, salt marshes and oil wells. Microbially mediated redox cycling of sulfur typically comprises dissimilatory sulfate reduction (MSR), sulfide reoxidation, disproportionation and the oxidation and reduction of sulfur redox intermediates. These processes contribute to the degradation of organic matter, link the cycles of sulfur and carbon, control the production and consumption of methane and are critical for the long term budget of O2 in the atmosphere. Microbial and abiotic processes at redox interfaces also connect the sulfur cycle to the redox cycles of nitrogen, iron and other elements, producing distinctive geochemical and molecular signatures. Studies that couple microbiology with stable isotope geochemistry have informed interpretations of microbial sulfur cycling in modern and past environments. Laboratory-based studies and models of MSR have sought to understand the physiological and environmental controls of the magnitude of sulfur isotope fractionation. The fractionations of stable sulfur and oxygen isotopes during MSR are also used to track enzymatic activity during MSR and processes that oxidize sulfide in the presence of environmental oxidants. Outstanding questions in the field concern the importance of oxidative processes within the natural environment, the delivery of oxidants and carbon sources to the zones of sulfate reduction and the ability to detect or reconstruct oxidative processes from the chemical, isotopic, metagenomic, transcriptomic, proteomic and metabolomics profiles in the environment. Recent studies have emphasized the complex connections between sulfur and methane, iron, nitrogen and other elements. These links may involve the redox cycling of species that occur at concentrations difficult to detect by standard geochemical techniques or that are cycled at very rapid rates (cryptic cycles). Of particular interest is the use of isotope geochemistry to quantify links among various electron acceptors, including sulfate, ferric iron, and nitrate, during the anaerobic methane oxidation. For example, recent geochemical measurements have hinted that microbial sulfate reduction coupled to organic matter oxidation is mechanistically different to when sulfate reduction is coupled to methane oxidation. Recent studies have also suggested a possible contribution of a number of previously uncultured microbial groups in sulfur cycling in sulfidic environments, inspiring further studies of these organisms and their partnerships in anaerobic environments. This Research Topic highlights studies of microbial interactions, processes and communities that couple the sulfur cycle to the cycles of other elements in aphotic environments.
Author: Maynard
Publisher: CRC Press
ISBN: 9780824789923
Category : Technology & Engineering
Languages : en
Pages : 388
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Presents the latest research on sulfur in temperate agricultural and forest ecosystems-integrating experimental findings with models of spatial scales from the cellular to the landscape level. Provides a general overview of sulfur in terrestrial ecosystems.
Author: Martin G. Klotz
Publisher: Frontiers E-books
ISBN: 2889190099
Category :
Languages : en
Pages : 258
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Sulfur is the tenth most abundant element in the universe and the sixth most abundant element in microbial biomass. By virtue of its chemical properties, particularly the wide range of stable redox states, sulfur plays a critical role in central biochemistry as a structural element, redox center, and carbon carrier. In addition, redox reactions involving reduced and oxidized inorganic sulfur compounds can be utilized by microbes for the generation and conservation of biochemical energy. Microbial transformation of both inorganic and organic sulfur compounds has had a profound effect on the properties of the biosphere and continues to affect geochemistry today. For these reasons, we present here a collection of articles from the leading edge of the field of sulfur microbiology, focusing on reactions and compounds of geochemical significance.
Author: Emily J. Fleming
Publisher:
ISBN:
Category :
Languages : en
Pages : 284
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Author:
Publisher: ScholarlyEditions
ISBN: 1464963630
Category : Technology & Engineering
Languages : en
Pages : 3062
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Issues in Environmental Research and Application: 2011 Edition is a ScholarlyEditions™ eBook that delivers timely, authoritative, and comprehensive information about Environmental Research and Application. The editors have built Issues in Environmental Research and Application: 2011 Edition on the vast information databases of ScholarlyNews.™ You can expect the information about Environmental Research and Application in this eBook to be deeper than what you can access anywhere else, as well as consistently reliable, authoritative, informed, and relevant. The content of Issues in Environmental Research and Application: 2011 Edition has been produced by the world’s leading scientists, engineers, analysts, research institutions, and companies. All of the content is from peer-reviewed sources, and all of it is written, assembled, and edited by the editors at ScholarlyEditions™ and available exclusively from us. You now have a source you can cite with authority, confidence, and credibility. More information is available at http://www.ScholarlyEditions.com/.
Author: Jerome O. Nriagu
Publisher: John Wiley & Sons
ISBN: 9780471042556
Category : Medical
Languages : en
Pages : 504
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Book Description
Collection of articles dealing with the chemical behavior and biological effects of sulfur as a pollutant.
