about
Inhibition of carbonate synthesis in acidic oceans on early MarsMicrobial mediated formation of Fe-carbonate minerals under extreme acidic conditionsA microbial oasis in the hypersaline Atacama subsurface discovered by a life detector chip: implications for the search for life on MarsRío tinto: a geochemical and mineralogical terrestrial analogue of Mars.Spiders: water-driven erosive structures in the southern hemisphere of Mars.Deep subsurface sulfate reduction and methanogenesis in the Iberian Pyrite Belt revealed through geochemistry and molecular biomarkers.Detection of peptidic sequences in the ancient acidic sediments of Río Tinto, Spain.From Río Tinto to Mars: the terrestrial and extraterrestrial ecology of acidophiles.The preservation and degradation of filamentous bacteria and biomolecules within iron oxide deposits at Rio Tinto, Spain.Classification of modern and old Río Tinto sedimentary deposits through the biomolecular record using a life marker biochip: implications for detecting life on Mars.Underground habitats in the Río Tinto basin: a model for subsurface life habitats on Mars.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.Some ecological mechanisms to generate habitability in planetary subsurface areas by chemolithotrophic communities: the Río Tinto subsurface ecosystem as a model system.Quantitative Raman spectroscopy as a tool to study the kinetics and formation mechanism of carbonates.Molecular biomarkers in the subsurface of the Salar Grande (Atacama, Chile) evaporitic depositsCoogoon Valles, western Arabia Terra: Hydrological evolution of a complex Martian channel systemOrbital evidence for clay and acidic sulfate assemblages on Mars based on mineralogical analogs from Rio Tinto, SpainAcidophiles and AstrobiologyIberian Pyrite Belt Subsurface Life (IPBSL), a Drilling Project of Biohydrometallurgical InterestGeobiology of a lower Cambrian carbonate platform, Pedroche Formation, Ossa Morena Zone, SpainAstrobiological Field Campaign to a Volcanosedimentary Mars Analogue Methane Producing Subsurface Protected Ecosystem: Imuruk Lake (Alaska)Association between catastrophic paleovegetation changes during Devonian–Carboniferous boundary and the formation of giant massive sulfide depositsMicrobial ecology of Río Tinto, a natural extreme acidic environment of biohydrometallurgical interestThe Case of the Lacking Carbonates and the Emergence of Early Life on MarsMicrobial Ecology of a Natural Extreme Acidic Environment: Lessons from Río TintoSubsurface Geomicrobiology of the Iberian Pyritic BeltExtreme environments as Mars terrestrial analogs: The Rio Tinto caseFinding mineralogically interesting targets for exploration from spatially coarse visible and near IR spectraInstrument development to search for biomarkers on mars: Terrestrial acidophile, iron-powered chemolithoautotrophic communities as model systemsPrime candidate sites for astrobiological exploration through the hydrogeological history of MarsThe Tinto River, an Extreme Gaian EnvironmentThe Tinto River, an extreme acidic environment under control of iron, as an analog of the Terra Meridiani hematite site of MarsInteraction of the sulfur and iron cycles in the Tinto River ecosystemImportance of Chemolithotrophy for Early Life on Earth: The Tinto River (Iberian Pyritic Belt) Case
P50
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P50
description
hulumtues
@sq
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
David C Fernández-Remolar
@ast
David C Fernández-Remolar
@en
David C Fernández-Remolar
@es
David C Fernández-Remolar
@sl
type
label
David C Fernández-Remolar
@ast
David C Fernández-Remolar
@en
David C Fernández-Remolar
@es
David C Fernández-Remolar
@sl
prefLabel
David C Fernández-Remolar
@ast
David C Fernández-Remolar
@en
David C Fernández-Remolar
@es
David C Fernández-Remolar
@sl
P1053
E-5534-2013
P106
P1153
6603201886
P21
P2798
P31
P3829
P496
0000-0003-2409-7444