Results 171 to 180 of about 42,133 (278)
Why Are We Here?: Constraining the Milky Way's Galactic Habitable Zone
Moiya McTier
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Chemical gardens are self‐assembled architectures with “life‐like” morphologies that form in the absence of any biological activity. Here we show that such structures can also be obtained by contacting reservoirs of calcium and sulfate ions, under conditions that plausibly emulate those prevailing on early Mars.
Selina Reigl +5 more
wiley +1 more source
Geochemical and Geophysical Controls on Hydrothermal Fluxes on Habitable Worlds
Benjamin M. Tutolo, Nicholas J. Tosca
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Abstract Earth's presently‐active magnetic field is thought to be generated by geodynamo via convection of liquid outer core, primarily composed of Fe alloyed with Ni and light elements, for example, Si. Core thermal conductivity critically controls its thermal evolution, dynamics, and available energy (thermal vs. compositional) powering the geodynamo
Wen‐Pin Hsieh +6 more
wiley +1 more source
Large drainage systems produced half of Mars' ancient river sediment. [PDF]
Zaki AS, Goudge TA, Mohrig D.
europepmc +1 more source
Chance and purpose in the evolution of biospheres. [PDF]
Donoghue PCJ +4 more
europepmc +1 more source
Volcanic emission of reduced sulfur species shaped the climate of early Mars. [PDF]
Bellino LG, Sun C.
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Fundamentals for habitable scenarios for Earth-like planets in the TRAPPIST-1 system
R. C. Payne, Lisa Kaltenegger
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