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Unveiling microbial preservation under hyperacidic and oxidizing conditions in the Oligocene Rio Tinto deposit

Scientific reports, 2021-11, Vol.11 (1), p.21543-21543, Article 21543

2021

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Coupled C, H, N, S and Fe biogeochemical cycles operating in the continental deep subsurface of the Iberian Pyrite Belt

Environmental microbiology, 2023-02, Vol.25 (2), p.428-453

2023

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Publisher Correction: Unveiling microbial preservation under hyperacidic and oxidizing conditions in the Oligocene Rio Tinto deposit

Scientific reports, 2021-12, Vol.11 (1), p.24460-24460, Article 24460

2021

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Biospeleothems Formed by Fungal Activity During the Early Holocene in the “Salar de Uyuni”

Frontiers in microbiology, 2022-06, Vol.13, p.913452-913452

2022

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The Molecular Profile of Soil Microbial Communities Inhabiting a Cambrian Host Rock

Microorganisms (Basel), 2024-03, Vol.12 (3), p.513

2024

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Preservation of Underground Microbial Diversity in Ancient Subsurface Deposits (>6 Ma) of the Rio Tinto Basement

Microorganisms (Basel), 2021-07, Vol.9 (8), p.1592

2021

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Association between catastrophic paleovegetation changes during Devonian–Carboniferous boundary and the formation of giant massive sulfide deposits

Earth and planetary science letters, 2010-11, Vol.299 (3), p.398-408

2010

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Carbonate precipitation under bulk acidic conditions as a potential biosignature for searching life on Mars

Earth and planetary science letters, 2012-10, Vol.351-352, p.13-26

2012

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Geological record of an acidic environment driven by iron hydrochemistry: The Tinto River system

Journal of Geophysical Research - Planets, 2003-07, Vol.108 (E7), p.5080-n/a

2003

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Productivity Contribution of Paleozoic Woodlands to the Formation of Shale‐Hosted Massive Sulfide Deposits in the Iberian Pyrite Belt (Tharsis, Spain)

Journal of geophysical research. Biogeosciences, 2018-03, Vol.123 (3), p.1017-1040

2018

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Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: Implications for Mars exploration

Icarus (New York, N.Y. 1962), 2008-03, Vol.194 (1), p.72-85

2008

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The environment of early Mars and the missing carbonates

Meteoritics & planetary science, 2011-10, Vol.46 (10), p.1447-1469

2011

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Geobiology of a lower Cambrian carbonate platform, Pedroche Formation, Ossa Morena Zone, Spain

Palaeogeography, palaeoclimatology, palaeoecology, 2013-09, Vol.386, p.459-478

2013

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Aerobic biomineralization of Mg-rich carbonates: Implications for natural environments

Chemical geology, 2011-02, Vol.281 (3), p.143-150

2011

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Formation of iron-rich shelled structures by microbial communities

Journal of geophysical research. Biogeosciences, 2015-01, Vol.120 (1), p.147-168

2015

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Río tinto: a geochemical and mineralogical terrestrial analogue of Mars

Life (Basel, Switzerland), 2014-09, Vol.4 (3), p.511-534

2014

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Molecular biomarkers in the subsurface of the Salar Grande (Atacama, Chile) evaporitic deposits

Biogeochemistry, 2018-08, Vol.140 (1), p.31-52

2018

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The Río Tinto Basin, Spain: Mineralogy, sedimentary geobiology, and implications for interpretation of outcrop rocks at Meridiani Planum, Mars

Earth and planetary science letters, 2005-11, Vol.240 (1), p.149-167

2005

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Microbial mediated formation of Fe-carbonate minerals under extreme acidic conditions

Scientific reports, 2014-04, Vol.4 (1), p.4767-4767, Article 4767

2014

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Stratigraphy of hydrated sulfates in the sedimentary deposits of Aram Chaos, Mars

Journal of Geophysical Research. E. Planets, 2010-06, Vol.115 (E6), p.n/a

2010

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Identification of the subsurface sulfide bodies responsible for acidity in Río Tinto source water, Spain

Earth and planetary science letters, 2014-04, Vol.391, p.36-41

2014

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Hydrogeochemical Variability of the Acidic Springs in the Rio Tinto Headwaters

Water (Basel), 2021-10, Vol.13 (20), p.2861

2021

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Spiders: water-driven erosive structures in the southern hemisphere of Mars

Astrobiology, 2006-08, Vol.6 (4), p.651

2006

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Inhibition of carbonate synthesis in acidic oceans on early Mars

Nature, 2004-09, Vol.431 (7007), p.423-426

2004

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Unveiling microbial preservation under hyperacidic and oxidizing conditions in the Oligocene Rio Tinto deposit

Coupled C, H, N, S and Fe biogeochemical cycles operating in the continental deep subsurface of the Iberian Pyrite Belt

Publisher Correction: Unveiling microbial preservation under hyperacidic and oxidizing conditions in the Oligocene Rio Tinto deposit

Biospeleothems Formed by Fungal Activity During the Early Holocene in the “Salar de Uyuni”

The Molecular Profile of Soil Microbial Communities Inhabiting a Cambrian Host Rock

Preservation of Underground Microbial Diversity in Ancient Subsurface Deposits (>6 Ma) of the Rio Tinto Basement

Association between catastrophic paleovegetation changes during Devonian–Carboniferous boundary and the formation of giant massive sulfide deposits

Carbonate precipitation under bulk acidic conditions as a potential biosignature for searching life on Mars

Geological record of an acidic environment driven by iron hydrochemistry: The Tinto River system

Productivity Contribution of Paleozoic Woodlands to the Formation of Shale‐Hosted Massive Sulfide Deposits in the Iberian Pyrite Belt (Tharsis, Spain)

Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: Implications for Mars exploration

The environment of early Mars and the missing carbonates

Geobiology of a lower Cambrian carbonate platform, Pedroche Formation, Ossa Morena Zone, Spain

Aerobic biomineralization of Mg-rich carbonates: Implications for natural environments

Formation of iron-rich shelled structures by microbial communities

Río tinto: a geochemical and mineralogical terrestrial analogue of Mars

Molecular biomarkers in the subsurface of the Salar Grande (Atacama, Chile) evaporitic deposits

The Río Tinto Basin, Spain: Mineralogy, sedimentary geobiology, and implications for interpretation of outcrop rocks at Meridiani Planum, Mars

Microbial mediated formation of Fe-carbonate minerals under extreme acidic conditions

Stratigraphy of hydrated sulfates in the sedimentary deposits of Aram Chaos, Mars

Identification of the subsurface sulfide bodies responsible for acidity in Río Tinto source water, Spain

Hydrogeochemical Variability of the Acidic Springs in the Rio Tinto Headwaters

Spiders: water-driven erosive structures in the southern hemisphere of Mars

Inhibition of carbonate synthesis in acidic oceans on early Mars

A microbial oasis in the hypersaline Atacama subsurface discovered by a life detector chip: implications for the search for life on Mars

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