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Senior Research Scientist Principal Investigator. Cornell University, Department of Astronomy present: Cornell University, Department of Astronomy: Molecular Biology and Astrobiology.
ALBERTO G. FAIRÉN I. ACADEMIC DEGREES AND PROFESSIONAL EXPERIENCE
Universidad Complutense de Madrid. Astronomy, 41 7 July Nature section Careers, interview. Nature,Harold C.
Refilling the oceans of early Mars. Athena Science Team Member.
ALBERTO G. FAIRÉN I. ACADEMIC DEGREES AND PROFESSIONAL EXPERIENCE – PDF
Proposing and testing a new theory to understand the early Mars environments. December June Oxidation processes and the preservation of aliiro biosignatures in a permafrost dominated environment a martian analogue in the canadian arctic.
April March Stability against freezing of hyperloaded solutions dundamentos Mars. Tracking the weathering of basalts on Mars using lithium isotope fractionation models. Astronomical forcing during the Neogene on the Earth and Mars. Uceda Postdoc Acting Advisor. Life at the dry limit on Earth and the search for life on Mars.
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Exploration of the Red Planet. Master of Science in Exploration Geophysics. Evolution, Geology and Exploration Clntabilidad Science Publishers, Inc. Journal of Geophysical Research-Planets Geophysical Research Letters Icarus, Sedimentary Geology Geochimica et Cosmochimica Acta Beilstein Journal of Nanotechnology Acta AstronauticaPalaios OneWorld Publications, book review Springer, Habitability on other planets and satellites, chapter review Elsevier, Encyclopedia of the Solar System, chapter review Springer, Encyclopedia of planetary landforms, chapter review Summer course Sistemas planetarios en el Universo.
Summer course Vida en el universo. International Astronomical Union approval on November 24, The coupling between reactive surface and diffusion: A way to explain the divergent mineral sequences on Mars.
Tsunami waves extensively resurfaced the shorelines of a receding, early Martian ocean. Geologic history of the Memnonia-Sirenum region, Mars. Journal of Geophysical Research, in review. Geologic expression of earthlike subduction on ancient Mars. Transient phase kinetics of hydrogen peroxide formed during oxidative dissolution of pyrite.
Chemical Geology, in review. Evidence for karst collapse and groundwater discharges in Noctis Labyrinthus, Mars. Geochemistry, Geophysics, Geosystems, 16 4 Stern, J. Evidence for fndamentos martian nitrogen in solid samples from the Curiosity rover investigations at Gale crater.
USA,Rodriguez, J. How did their source aquifers form, and why did they drain so rapidly? Scientific Reports, in press. Journal of Geophysical Research,Rodriguez, J. New insights into the Late Amazonian zonal shrinkage of the Martian south polar plateau.
Icarus,Dohm, J. Geological and hydrological histories of the Argyre province, Mars. Did the Martian outflow channels mostly form during the Amazonian Period? Ocntabilidad cold hydrological system in Gale crater, Mars.
Ancient aqueous environments at Endeavour Crater, Mars. Science,Ming, D. Science,Essefi, E. Assessing the possibility of biological complexity on other worlds, with an estimate of the occurrence of complex life in the Milky Way Galaxy.
Full text of “The Economic Literature Of Latin America A Tentative Bibliography Volume II”
Challenges, 5, Stack, K. Journal of Geophysical Research,doi: Implications for the habitability of Mars.
Life, 4 3; doi: Evidence for Middle Amazonian catastrophic flooding and glaciation on Mars. Icarus,Mahaney, W. Mineralogy, chemistry and biological contingents of an Early-Middle Miocene Antarctic paleosol and its relevance as a Martian analogue.
The overprotection of Mars. Nature Geoscience, 6, Davila A. Evidence for Hesperian glaciation along the Martian dichotomy boundary.
Geology, 41, McKay, C. The Icebreaker Life Mission to Mars: A search for biomolecular evidence for life. Astrobiology, 13, Schulze-Makuch, D. Drastic environmental change and its effects on a planetary biosphere.
Icarus,Battler, M. Icarus,Schulze-Makuch, D. Reduced albedo on early Mars does not solve the climate paradox under a faint young Sun.
Glacial paleoenvironments on Mars revealed by the paucity of hydrated silicates in the Noachian crust of the northern lowlands. Weathering rinds on clasts: Infiltration of Martian outflow channel floodwaters into lowland cavernous systems.
Geophysical Research Letters, 39, L, doi: Cold glacial oceans would have inhibited phyllosilicate sedimentation on early Mars. Nature Geoscience, 4 10Highlighted in Science: Why no clay up North? Contabildad at Meridiani Planum provide evidence for significant amounts of surface and near-surface water on early Mars.
A large sedimentary basin in the Terra Sirenum region of the southern highlands of Mars. Secondary chaotic terrain formation in the higher outflow channels of southern circum-chryse, Mars. An inventory of potentially habitable environments on Mars: Geological and biological perspectives. Geological Society aliroo America Special Paperpdoi: A two-tiered approach to assessing the jesjs of exoplanets.
A cold and wet Mars. Noachian and more recent phyllosilicates contwbilidad impact craters on Mars. Astrobiology through the ages of Mars. Astrobiology, 10 8Lim, D. Scientific field training for human planetary exploration. Evidence for Hesperian impact-induced hydrothermalism on Mars.
Icarus,Davila, A. Hygroscopic salts and the potential for life on Mars.