about
A Habitable Fluvio-Lacustrine Environment at Yellowknife Bay, Gale Crater, MarsAstRoMap European Astrobiology RoadmapIsotope ratios of H, C, and O in CO2 and H2O of the martian atmosphereA microbial oasis in the hypersaline Atacama subsurface discovered by a life detector chip: implications for the search for life on MarsA molecular approach to the characterization of the eukaryotic communities of an extreme acidic environment: methods for DNA extraction and denaturing gradient gel electrophoresis analysis.Martian fluvial conglomerates at Gale craterLow upper limit to methane abundance on Mars.Soil diversity and hydration as observed by ChemCam at Gale crater, Mars.Volatile, isotope, and organic analysis of martian fines with the Mars Curiosity rover.The petrochemistry of Jake_M: a martian mugearite.Curiosity at Gale crater, Mars: characterization and analysis of the Rocknest sand shadow.Mineralogy of a mudstone at Yellowknife Bay, Gale crater, Mars.In situ radiometric and exposure age dating of the martian surface.Elemental geochemistry of sedimentary rocks at Yellowknife Bay, Gale crater, Mars.Mars' surface radiation environment measured with the Mars Science Laboratory's Curiosity rover.Volatile and organic compositions of sedimentary rocks in Yellowknife Bay, Gale crater, Mars.Genomic Methods and Microbiological Technologies for Profiling Novel and Extreme Environments for the Extreme Microbiome Project (XMP)Mineralization and Preservation of an extremotolerant Bacterium Isolated from an Early Mars Analog Environment.X-ray diffraction results from Mars Science Laboratory: mineralogy of Rocknest at Gale crater.From Río Tinto to Mars: the terrestrial and extraterrestrial ecology of acidophiles.Underground habitats in the Río Tinto basin: a model for subsurface life habitats on Mars.Some ecological mechanisms to generate habitability in planetary subsurface areas by chemolithotrophic communities: the Río Tinto subsurface ecosystem as a model system.Development and structure of eukaryotic biofilms in an extreme acidic environment, rio tinto (SW, Spain).The responses of an anaerobic microorganism, Yersinia intermedia MASE-LG-1 to individual and combined simulated Martian stresses.Microbiology: eukaryotic diversity in Spain's River of Fire.Coogoon Valles, western Arabia Terra: Hydrological evolution of a complex Martian channel systemIberian Pyrite Belt Subsurface Life (IPBSL), a Drilling Project of Biohydrometallurgical InterestMolecular 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 MarsAstrobiological Field Campaign to a Volcanosedimentary Mars Analogue Methane Producing Subsurface Protected Ecosystem: Imuruk Lake (Alaska)Microbial ecology of Río Tinto, a natural extreme acidic environment of biohydrometallurgical interestExtreme environments as Mars terrestrial analogs: The Rio Tinto caseThe 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 ecosystemREMS: The Environmental Sensor Suite for the Mars Science Laboratory RoverCuriosity's rover environmental monitoring station: Overview of the first 100 solsBioremoval of organic and inorganic sulphur from coal samplesDistribution and seasonal variability in the benthic eukaryotic community of Río Tinto (SW, Spain), an acidic, high metal extreme environment
P50
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P50
description
hulumtues
@sq
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
Felipe Gómez
@ast
Felipe Gómez
@en
Felipe Gómez
@es
Felipe Gómez
@sl
type
label
Felipe Gómez
@ast
Felipe Gómez
@en
Felipe Gómez
@es
Felipe Gómez
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altLabel
MSL team
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prefLabel
Felipe Gómez
@ast
Felipe Gómez
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Felipe Gómez
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Felipe Gómez
@sl
P1053
L-7315-2014
P106
P1153
56817935600
P21
P31
P3829
P496
0000-0001-9977-7060