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Comparison of Boreal Acid Sulfate Soil Microbial Communities in Oxidative and Reductive Environments
Linnéuniversitetet, Fakulteten för Hälso- och livsvetenskap (FHL), Institutionen för biologi och miljö (BOM). (Ctr Ecol & Evolut Microbial Model Syst EEMiS;Systems Biology of Extreme Microorganisms)ORCID-id: 0000-0003-0021-2452
Linnéuniversitetet, Fakulteten för Hälso- och livsvetenskap (FHL), Institutionen för biologi och miljö (BOM).ORCID-id: 0000-0002-0635-3718
Linnéuniversitetet, Fakulteten för Hälso- och livsvetenskap (FHL), Institutionen för biologi och miljö (BOM). (Ctr Ecol & Evolut Microbial Model Syst EEMiS)
Geological Survey of Sweden, Sweden.
Visa övriga samt affilieringar
2019 (Engelska)Ingår i: Research in Microbiology, ISSN 0923-2508, E-ISSN 1769-7123, Vol. 170, nr 6-7, s. 288-295Artikel i tidskrift, Letter (Refereegranskat) Published
Abstract [en]

Due to land uplift after the last ice age, previously stable Baltic Sea sulfidic sediments are becoming dry land. When these sediments are drained, the sulfide minerals are exposed to air and can release large amounts of metals and acid into the environment. This can cause severe ecological damage such as fish kills in rivers feeding the northern Baltic Sea. In this study, five sites were investigated for the occurrence of acid sulfate soils and their geochemistry and microbiology was identified. The pH and soil chemistry identified three of the areas as having classical acid sulfate soil characteristics and culture independent identification of 16S rRNA genes identified populations related to acidophilic bacteria capable of catalyzing sulfidic mineral dissolution, including species likely adapted to low temperature. These results were compared to an acid sulfate soil area that had been flooded for ten years and showed that the previously oxidized sulfidic materials had an increased pH compared to the unremediated oxidizied layers. In addition, the microbiology of the flooded soil had changed such that alkalinity producing ferric and sulfate reducing reactions had likely occurred. This suggested that flooding of acid sulfate soils mitigates their environmental impact.

Ort, förlag, år, upplaga, sidor
Elsevier, 2019. Vol. 170, nr 6-7, s. 288-295
Nyckelord [en]
sulfide mineral; metal; sulfur; 16S rRNA gene; mitigation; wetland
Nationell ämneskategori
Mikrobiologi Geovetenskap och miljövetenskap
Forskningsämne
Naturvetenskap, Miljövetenskap
Identifikatorer
URN: urn:nbn:se:lnu:diva-77664DOI: 10.1016/j.resmic.2019.06.002ISI: 000491121700006OAI: oai:DiVA.org:lnu-77664DiVA, id: diva2:1246969
Tillgänglig från: 2018-09-10 Skapad: 2018-09-10 Senast uppdaterad: 2019-10-31Bibliografiskt granskad
Ingår i avhandling
1. Function and Adaptation of Acidophiles in Natural and Applied Communities
Öppna denna publikation i ny flik eller fönster >>Function and Adaptation of Acidophiles in Natural and Applied Communities
2018 (Engelska)Doktorsavhandling, sammanläggning (Övrigt vetenskapligt)
Abstract [en]

Acidophiles are organisms that have evolved to grow optimally at high concentrations of protons. Members of this group are found in all three domains of life, although most of them belong to the Archaea and Bacteria. As their energy demand is often met chemolithotrophically by the oxidation of basic ions and molecules such as Fe2+, H2, and sulfur compounds, they are often found in environments marked by the natural or anthropogenic exposure of sulfide minerals. Nonetheless, organoheterotrophic growth is also common, especially at higher temperatures. Beside their remarkable resistance to proton attack, acidophiles are resistant to a multitude of other environmental factors, including toxic heavy metals, high temperatures, and oxidative stress. This allows them to thrive in environments with high metal concentrations and makes them ideal for application in so-called biomining technologies.

The first study of this thesis investigated the iron-oxidizer Acidithiobacillus ferrivorans that is highly relevant for boreal biomining. Several unresolved nodes of its sulfur metabolism were elucidated with the help of RNA transcript sequencing analysis. A model was proposed for the oxidation of the inorganic sulfur compound tetrathionate. In a second paper, this species’ transcriptional response to growth at low temperature was explored and revealed that At. ferrivorans increases expression of only very few known cold-stress genes, underlining its strong adaptation to cold environments.

Another set of studies focused on the environmentally friendly metal winning technology of bioleaching. One of the most important iron-oxidizers in many biomining operations is Leptospirillum ferriphilum. Despite its significance, only a draft genome sequence was available for its type strain.Therefore, in the third paper of this thesis we published a high quality, closed genome sequence of this strain for future use as a reference, revealing a previously unidentified nitrogen fixation system and improving annotation of genes relevant in biomining environments. In addition, RNA transcript and protein patterns during L. ferriphilum’s growth on ferrous iron and in bioleaching culture were used to identify key traits that aid its survival in extremely acidic, metal-rich environments. The biomining of copper from chalcopyrite is plagued by a slow dissolution rate, which can reportedly be circumvented by low redox potentials. As conventional redox control is impossible in heap leaching, paper four explored the possibility of using differentially efficient iron oxidizers to influence this parameter. The facultative heterotrophic Sulfobacillus thermosulfidooxidans was identified as maintaining a redox potential of ~550 mV vs Ag/AgCl, favorable for chalcopyrite dissolution,while L. ferriphilum caused the potential to raise far above this critical value. RNA transcript analysis was used to identify genomic features that may contribute to this behavior.

Lastly, six fields in Northern Sweden were examined for the presence of acid sulfate soils in the fifth paper. The study revealed three acid sulfate soils. The presence of acidophiles that likely catalyze the production of acid in the soil was confirmed by community 16S gene amplicon analysis. One site that was flooded in a remediation attempt and is therefore anoxic still exhibited similar bacteria, however, these now likely grow via ferric iron reduction. This process consumes protons and could explain the observed rise in pH at this site.

This thesis examines acidophiles in pure culture, as well as natural and designed communities. Key metabolic traits involved in the adaptation to their habitats were elucidated, and their application in mining operations was discussed. Special attention was paid to acidophiles in chalcopyrite bioleaching and in cold environments, including environmental acid sulfate soils in Northern Sweden.

Ort, förlag, år, upplaga, sidor
Växjö: Linnaeus University Press, 2018
Serie
Linnaeus University Dissertations ; 328
Nyckelord
Acidophiles, Biomining, Psychrophiles, Adaptation, Acid Sulfate Soil, Redox Control
Nationell ämneskategori
Ekologi
Forskningsämne
Naturvetenskap, Ekologi
Identifikatorer
urn:nbn:se:lnu:diva-77666 (URN)978-91-88761-94-1 (ISBN)978-91-88761-95-8 (ISBN)
Disputation
2018-10-19, Norrgård, Kalmar, 09:30 (Engelska)
Opponent
Handledare
Tillgänglig från: 2018-09-11 Skapad: 2018-09-10 Senast uppdaterad: 2018-11-16Bibliografiskt granskad

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Av författaren/redaktören
Christel, StephanYu, ChangxunWu, XiaofenÅström, Mats E.Dopson, Mark
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Institutionen för biologi och miljö (BOM)
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Research in Microbiology
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