All Stories

  1. The Molecular Profile of Soil Microbial Communities Inhabiting a Cambrian Host Rock
  2. Coupled C, H, N, S and Fe biogeochemical cycles operating in the continental deep subsurface of the Iberian Pyrite Belt
  3. Formation of chloride deposits on Early Mars under acidic and reducing crustal conditions
  4. Unveiling microbial preservation under hyperacidic and oxidizing conditions in the Oligocene Rio Tinto deposit
  5. The Molecular Record of Metabolic Activity in the Subsurface of the Río Tinto Mars Analog
  6. Preservation of Underground Microbial Diversity in Ancient Subsurface Deposits (>6 Ma) of the Rio Tinto Basement
  7. The potential science and engineering value of samples delivered to Earth by Mars sample return
  8. Molecular biomarkers in the subsurface of the Salar Grande (Atacama, Chile) evaporitic deposits
  9. A mineralogical archive of the biogeochemical sulfur cycle preserved in the subsurface of the Río Tinto system
  10. Productivity Contribution of Paleozoic Woodlands to the Formation of Shale‐Hosted Massive Sulfide Deposits in the Iberian Pyrite Belt (Tharsis, Spain)
  11. Coogoon Valles, western Arabia Terra: Hydrological evolution of a complex Martian channel system
  12. Orbital evidence for clay and acidic sulfate assemblages on Mars based on mineralogical analogs from Rio Tinto, Spain
  13. Oxalate formation under the hyperarid conditions of the Atacama desert as a mineral marker to provide clues to the source of organic carbon on Mars
  14. Acidophiles and Astrobiology
  15. Formation of iron-rich shelled structures by microbial communities
  16. Iron Oxides, Hydroxides and Oxy-hydroxides
  17. Rio Tinto
  18. Reply to the Comment on “Identification of the subsurface sulfide bodies responsible for acidity in Río Tinto source water, Spain” (Earth Planet. Sci. Lett. 391 (2014) 36–41)
  19. Río Tinto: A Geochemical and Mineralogical Terrestrial Analogue of Mars
  20. Report of the workshop for life detection in samples from Mars
  21. Microbial mediated formation of Fe-carbonate minerals under extreme acidic conditions
  22. Identification of the subsurface sulfide bodies responsible for acidity in Río Tinto source water, Spain
  23. Geology of the Ariadnes Basin, NE Eridania quadrangle, Mars – 1:1Million
  24. Biogeochemical Cycles
  25. Biosphere
  26. Abiotic
  27. Rio Tinto
  28. Iron Oxides, Hydroxides and Oxy-hydroxides
  29. Quantitative Raman spectroscopy as a tool to study the kinetics and formation mechanism of carbonates
  30. Deep subsurface sulfate reduction and methanogenesis in the Iberian Pyrite Belt revealed through geochemistry and molecular biomarkers
  31. Iberian Pyrite Belt Subsurface Life (IPBSL), a Drilling Project of Biohydrometallurgical Interest
  32. Geobiology of a lower Cambrian carbonate platform, Pedroche Formation, Ossa Morena Zone, Spain
  33. Molecular preservation in halite‐ and perchlorate‐rich hypersaline subsurface deposits in the Salar Grande basin (Atacama Desert, Chile): Implications for the search for molecular biomarkers on Mars
  34. Carbonate precipitation under bulk acidic conditions as a potential biosignature for searching life on Mars
  35. Planning for Mars Returned Sample Science: Final Report of the MSR End-to-End International Science Analysis Group (E2E-iSAG)
  36. A Microbial Oasis in the Hypersaline Atacama Subsurface Discovered by a Life Detector Chip: Implications for the Search for Life on Mars
  37. Detection of Peptidic Sequences in the Ancient Acidic Sediments of Río Tinto, Spain
  38. The environment of early Mars and the missing carbonates
  39. The preservation and degradation of filamentous bacteria and biomolecules within iron oxide deposits at Rio Tinto, Spain
  40. Aerobic biomineralization of Mg-rich carbonates: Implications for natural environments
  41. Rio Tinto
  42. Iron Oxyhydroxides
  43. Biogeochemical Cycles
  44. Biosphere
  45. Abiotic
  46. Astrobiological Field Campaign to a Volcanosedimentary Mars Analogue Methane Producing Subsurface Protected Ecosystem: Imuruk Lake (Alaska)
  47. Classification of Modern and Old Río Tinto Sedimentary Deposits Through the Biomolecular Record Using a Life Marker Biochip: Implications for Detecting Life on Mars
  48. From Río Tinto to Mars
  49. Río Tinto sedimentary mineral assemblages: A terrestrial perspective that suggests some formation pathways of phyllosilicates on Mars
  50. Association between catastrophic paleovegetation changes during Devonian–Carboniferous boundary and the formation of giant massive sulfide deposits
  51. Microbial ecology of Río Tinto, a natural extreme acidic environment of biohydrometallurgical interest
  52. The Case of the Lacking Carbonates and the Emergence of Early Life on Mars
  53. Fluvial Bedform Generation by Biofilm Activity in the Berrocal Segment of Río Tinto: Acidic Biofilms and Sedimentation
  54. Microbial Ecology of a Natural Extreme Acidic Environment: Lessons from Río Tinto
  55. The 2005 MARTE Robotic Drilling Experiment in Río Tinto, Spain: Objectives, Approach, and Results of a Simulated Mission to Search for Life in the Martian Subsurface
  56. Underground Habitats in the Río Tinto Basin: A Model for Subsurface Life Habitats on Mars
  57. Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: Implications for Mars exploration
  58. Some Ecological Mechanisms to Generate Habitability in Planetary Subsurface Areas by Chemolithotrophic Communities: The Río Tinto Subsurface Ecosystem as a Model System
  59. Subsurface Geomicrobiology of the Iberian Pyritic Belt
  60. Extreme environments as Mars terrestrial analogs: The Rio Tinto case
  61. Finding mineralogically interesting targets for exploration from spatially coarse visible and near IR spectra
  62. Spiders: Water-Driven Erosive Structures in the Southern Hemisphere of Mars
  63. The subsurface and surface acidic system of Río Tinto: Sulfur and iron transfer from underground weathering to subaerial precipitation
  64. Thermal evolution of several sulfate-rich brines and hydrated sulfate minerals at the environmental conditions of the martian surface
  65. Interglacial clathrate destabilization on Mars: Possible contributing source of its atmospheric methane
  66. Prime candidate sites for astrobiological exploration through the hydrogeological history of Mars
  67. The Río Tinto Basin, Spain: Mineralogy, sedimentary geobiology, and implications for interpretation of outcrop rocks at Meridiani Planum, Mars
  68. Instrument development to search for biomarkers on mars: Terrestrial acidophile, iron-powered chemolithoautotrophic communities as model systems
  69. Efficiently using connectivity information between triangles in a mesh for real-time rendering
  70. Inhibition of carbonate synthesis in acidic oceans on early Mars
  71. The Tinto River, an Extreme Gaian Environment
  72. Early Cambrian molluscs from Sierra de Córdoba (Spain)
  73. The Tinto River, an extreme acidic environment under control of iron, as an analog of the Terra Meridiani hematite site of Mars
  74. Importance of Chemolithotrophy for Early Life on Earth: The Tinto River (Iberian Pyritic Belt) Case
  75. Tírez Lake as a Terrestrial Analog of Europa
  76. Geomicrobiology of the Tinto River, a model of interest for biohydrometallurgy
  77. Geological record of an acidic environment driven by iron hydrochemistry: The Tinto River system
  78. Interaction of the sulfur and iron cycles in the Tinto River ecosystem
  79. Latest Neoproterozoic to Middle Cambrian body fossil record in Spain (exclusive of trilobites and archaeocyaths) and their stratigraphic significance
  80. Preservation Windows for Paleobiological Traces in the Mars Geological Record