All Stories

  1. Enhanced Immobilization of Arsenic from Acid Mine Drainage by Detrital Clay Minerals
  2. Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32
  3. Salinity, microbe, and carbonate mineral relationships in brackish and hypersaline lake sediments: a case study from the tropical Pacific coral atoll of Kiritimati
  4. Seasonal microbial variation accounts for arsenic dynamics in shallow alluvial aquifer systems
  5. Influence of pH on the balance between methanogenesis and iron reduction
  6. Dissolved carbon dynamics in meltwaters from the Russell Glacier, Greenland Ice Sheet
  7. Microbial diversity and biomarker analysis of modern freshwater microbialites from Laguna Bacalar, Mexico
  8. Parallelized, Aerobic, Single Carbon-Source Enrichments from Different Natural Environments Contain Divergent Microbial Communities
  9. Natural polyreactive IgA antibodies coat the intestinal microbiota
  10. Orenia metallireducens sp. nov. Strain Z6, a Novel Metal-Reducing Member of the Phylum Firmicutes from the Deep Subsurface
  11. Tepidibacillus decaturensis sp. nov.: a microaerophilic, moderately thermophilic iron-reducing bacterium isolated from a depth of 1.7 km in the Illinois Basin, USA
  12. Transhydrogenase and Growth Substrate Influence Lipid Hydrogen Isotope Ratios in Desulfovibrio alaskensis G20
  13. Thiosulfate oxidation byThiomicrospira thermophila: metabolic flexibility in response to ambient geochemistry
  14. Solute Concentrations Influence Microbial Methanogenesis in Coal-bearing Strata of the Cherokee Basin, USA
  15. Innate and Adaptive Humoral Responses Coat Distinct Commensal Bacteria with Immunoglobulin A
  16. Sulfur-mediated electron shuttling during bacterial iron reduction
  17. H alomonas sulfidaeris ‐dominated microbial community inhabits a 1.8 km‐deep subsurface C ambrian S andstone reservoir
  18. Effects of Bound Phosphate on the Bioreduction of Lepidocrocite (γ-FeOOH) and Maghemite (γ-Fe 2 O 3 ) and Formation of Secondary Minerals
  19. Functional microbial diversity explains groundwater chemistry in a pristine aquifer
  20. The active bacterial community in a pristine confined aquifer
  21. The thermodynamic ladder in geomicrobiology
  22. Attached and suspended microbial communities in a pristine confined aquifer
  23. STRUCTURES OF STRONTIUM- AND BARIUM-DOMINANT COMPOUNDS THAT CONTAIN THE AUTUNITE-TYPE SHEET
  24. The role of water in the structures of synthetic hallimondite, Pb2[(UO2)(AsO4)2](H2O)nand synthetic parsonsite, Pb2[(UO2)(PO4)2](H2O)n, 0 ≤n≤ 0.5
  25. DIVALENT TRANSITION METALS AND MAGNESIUM IN STRUCTURES THAT CONTAIN THE AUTUNITE-TYPE SHEET
  26. MONOVALENT CATIONS IN STRUCTURES OF THE META-AUTUNITE GROUP