Limited carbon sources prevent sulfate remediation in circumneutral abandoned mine drainage

Distribution and abundance of iron-sulfur cycle bacteria in acid mine drainage-impacted sediments of the Shandi river basin

Iron-sulfur cycle bacteria are considered the principal participants in the regulation of iron and sulfur cycles, ubiquitously found in diverse natural ecosystems. This study concentrated on the spatial distribution patterns of iron-sulfur bacteria in the acid mine drainage (AMD) sediments, compared with AMD-impacted river sediments, and evaluated the potential influences of iron-sulfur bacteria on the metals in the Shandi River basin. The results showed that the water and sediments near the mine from the Shandi River basin had been seriously polluted by heavy metals and sulfate. Specifically, the Nemerow index (P) exceeded 5, and the comprehensive potential ecological risk factor (RI) surpassed 600. The sediment samples collected exhibited a profusion of iron-sulfur cycle bacteria, with the abundance of these organisms being higher within river sediments compared to AMD sediments, particularly for iron-sulfur reducing bacteria. The results of correlation and redundancy analysis showed that most metals had an impact on the abundance of iron-sulfur cycle microorganisms in different degrees. Meanwhile, SEM-EDS analysis revealed the presence of sulfate minerals in diverse forms in sediments, which might be biogenic. All of findings indicated that iron-sulfur cycle bacteria might regulate the forms of metal and sulphur, fixed most metals and sulfate, and further influencing the synthesis and phase transition of sulfate minerals in the sediments. This study confirmed the ecological values of iron-sulfur bacteria, which will be help for bioremediation of AMD contaminants in Shandi River basin.

Bacterial nitrite production oxidizes Fe(II) bioremediating acidic abandoned coal mine drainage

Passive remediation systems (PRSs) treating either acidic or neutral abandoned coal mine drainage (AMD) are colonized by bacteria that can bioremediate iron (Fe) through chemical cycling. Due to the low pH in acidic AMD, iron oxidation from soluble Fe(II) to precipitated Fe(III) is mainly directed by microbial oxidation. Less well described are biotic reactions that lead to iron remediation through abiotic secondary reactions. We describe here iron oxidation in acidic AMD that is mediated by the bacterial reduction of nitrate to nitrite followed by the geochemical oxidation of Fe(II). Within an acidic PRS, 4,560 bacteria cultured from the microbial community were screened for their ability to oxidize iron and to perform nitrate-dependent iron oxidation (NDFO). Iron oxidation in the culturable community was observed in every pond of the system, ranging from 2.1% to 11.4%, and NDFO was observed in every pond, ranging from 1.4% to 6.0% of the culturable bacteria. Five NDFO isolates were purified and identified as Paraburkholderia spp. One of our isolates, Paraburkholderia sp. AV18 was shown to drive NDFO through the bacterial production of nitrite that in turn chemically oxidizes Fe(II) (nitrate reduction-iron oxidation; NRIO). AV18 expressed nitrate reductase, napA, concurrent to nitrite production. Burkholderiales are found by 16S rRNA gene sequencing in every pond of the PRS. The frequency of NDFO metabolism in the culturable microbial community and abundance of Burkholderiales in the PRS suggest nitrite producers contribute to the bioremediation of iron in acidic AMD and may be an unharnessed opportunity to increase iron bioremediation in acidic conditions.

IMPORTANCE

Our study sheds light on a poorly defined biogeochemical interaction, nitrate-dependent iron oxidation (NDFO), that has been described in several environments. We show that bacterial nitrate reduction produces nitrite, which can chemically oxidize ferrous iron, leading to insoluble ferric iron. We show that bacteria capable of the nitrate reduction-iron oxidation (NRIO) reactions are prevalent throughout multiple passive remediation systems that treat acidic coal mine drainage, indicating this may be a widespread mechanism for iron removal under acidic conditions. In acidic coal mine remediation, iron precipitation has been shown to be solely bacterially mediated, and NRIO provides a simple mechanism for aerobic oxidation of iron in these conditions.

Decreasing lactate input for cost-effective sulfidogenic metal removal in sulfate-rich effluents: Mechanistic insights from (bio)chemical kinetics to microbiome response

High material cost is the biggest barrier for the industrial use of low-molecular-weight organics (i.e. lactate) as external carbon and electron source for sulfidogenic metal removal in sulfate-rich effluents. This study aims to provide mechanistic evidence from kinetics to microbiome analysis by batch modeling to support the possibility of decreasing the lactate input to achieve cost-effective application. The results showed that gradient COD/SO42- ratios at a low level had promising treatment performance, reaching neutralized pH with nearly total elimination of COD (91%-99%), SO42- (85%-99%), metals (80%-99%) including Cu, Zn, and Mn. First-order kinetics exhibited the best fit (R2 = 0.81-0.98) to (bio)chemical reactions, and the simulation results revealed that higher COD/SO42- accelerated the reaction rate of SO42- and COD but not suitable to that of metals. On the other hand, we found that the decreasing COD/SO42- ratio increased average path distance but decreased clustering coefficient and heterogeneity in microbial interaction network. Genetic prediction found that the sulfate-reduction-related functions were significantly correlated with the reaction kinetics changed with COD/SO42- ratios. Our study, combining reaction kinetics with microbiome analysis, demonstrates that the use of lactate as a carbon source under low COD/SO42- ratios entails significant efficiency of metal removal in sulfate-rich effluent using SRB-based technology. However, further studies should be carried out, including parameter-driven optimization and life cycle assessments are necessary, for its practical application.

Isolation and Genome Analysis of an Amoeba-Associated Bacterium Dyella terrae Strain Ely Copper Mine From Acid Rock Drainage in Vermont, United States

Protozoa play important roles in microbial communities, regulating populations via predation and contributing to nutrient cycling. While amoebae have been identified in acid rock drainage (ARD) systems, our understanding of their symbioses in these extreme environments is limited. Here, we report the first isolation of the amoeba Stemonitis from an ARD environment as well as the genome sequence and annotation of an associated bacterium, Dyella terrae strain Ely Copper Mine, from Ely Brook at the Ely Copper Mine Superfund site in Vershire, Vermont, United States. Fluorescent in situ hybridization analysis showed this bacterium colonizing cells of Stemonitis sp. in addition to being outside of amoebal cells. This amoeba-resistant bacterium is Gram-negative with a genome size of 5.36 Mbp and GC content of 62.5%. The genome of the D. terrae strain Ely Copper Mine encodes de novo biosynthetic pathways for amino acids, carbohydrates, nucleic acids, and lipids. Genes involved in nitrate (1) and sulfate (7) reduction, metal (229) and antibiotic resistance (37), and secondary metabolite production (6) were identified. Notably, 26 hydrolases were identified by RAST as well as other biomass degradation genes, suggesting roles in carbon and energy cycling within the microbial community. The genome also contains type IV secretion system genes involved in amoebae resistance, revealing how this bacterium likely survives predation from Stemonitis sp. This genome analysis and the association of D. terrae strain Ely Copper Mine with Stemonitis sp. provide insight into the functional roles of amoebae and bacteria within ARD environments.