scholarly article | Q13442814 |
P356 | DOI | 10.1038/S41561-017-0015-2 |
P50 | author | Tullis Onstott | Q91285867 |
John F. Mustard | Q106513527 | ||
Joseph R. Michalski | Q106533287 | ||
Stephen J. Mojzsis | Q56457588 | ||
Paul B. Niles | Q68980470 | ||
Queenie H. S. Chan | Q87675416 | ||
P2093 | author name string | Sarah Stewart Johnson | |
P2860 | cites work | Prokaryotes: the unseen majority | Q22066200 |
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Extraterrestrial amino acids in Orgueil and Ivuna: tracing the parent body of CI type carbonaceous chondrites | Q24620582 | ||
Ionizing radiation: how fungi cope, adapt, and exploit with the help of melanin | Q24650544 | ||
Cell proliferation at 122 degrees C and isotopically heavy CH4 production by a hyperthermophilic methanogen under high-pressure cultivation | Q24653236 | ||
Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures | Q28005492 | ||
Synthesis of purines under possible primitive earth conditions. I. Adenine from hydrogen cyanide | Q28186376 | ||
Synthesizing life | Q28201137 | ||
Experimental models of primitive cellular compartments: encapsulation, growth, and division | Q28212244 | ||
Amino acid racemization on Mars: implications for the preservation of biomolecules from an extinct martian biota | Q28215374 | ||
Borate minerals stabilize ribose | Q28238098 | ||
Active formation of 'chaos terrain' over shallow subsurface water on Europa | Q28253142 | ||
Long-term sustainability of a high-energy, low-diversity crustal biome | Q28269593 | ||
Detection of silica-rich deposits on Mars | Q28280943 | ||
Evidence for life on Earth before 3,800 million years ago | Q28295460 | ||
Fluid mixing and the deep biosphere of a fossil Lost City-type hydrothermal system at the Iberia Margin | Q28606895 | ||
The drive to life on wet and icy worlds | Q28658605 | ||
Manganese-oxidizing photosynthesis before the rise of cyanobacteria | Q28678436 | ||
Martian surface mineralogy from Observatoire pour la Minéralogie, l'Eau, les Glaces et l'Activité on board the Mars Express spacecraft (OMEGA/MEx): Global mineral maps | Q29543492 | ||
Geochemistry of Carbonates on Mars: Implications for Climate History and Nature of Aqueous Environments | Q29543622 | ||
Methylotrophic methanogenesis discovered in the archaeal phylum Verstraetearchaeota | Q31134331 | ||
A serpentinite-hosted ecosystem: the Lost City hydrothermal field | Q31151154 | ||
Atmospheric influence of Earth's earliest sulfur cycle | Q33912369 | ||
Origin and evolution of prebiotic organic matter as inferred from the Tagish Lake meteorite | Q34191425 | ||
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Ancient hydrothermal seafloor deposits in Eridania basin on Mars | Q38369389 | ||
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Geologic setting of serpentine deposits on Mars | Q56552131 | ||
The effect of ionizing radiation on the preservation of amino acids on Mars | Q56698040 | ||
Outgassing History and Escape of the Martian Atmosphere and Water Inventory | Q57662423 | ||
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A fracture history on Enceladus provides evidence for a global ocean | Q60307944 | ||
Comparison of “warm and wet” and “cold and icy” scenarios for early Mars in a 3-D climate model | Q60369829 | ||
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Probing for evidence of plumes on Europa with HST/STIS | Q69125201 | ||
A sawtooth-like timeline for the first billion years of lunar bombardment | Q73892248 | ||
P433 | issue | 1 | |
P304 | page(s) | 21-26 | |
P577 | publication date | 2017-12-18 | |
P1433 | published in | Nature Geoscience | Q1337483 |
P1476 | title | The Martian subsurface as a potential window into the origin of life | |
P478 | volume | 11 |
Q106533457 | The biomass and biodiversity of the continental subsurface |
Q106414430 | The next frontier for planetary and human exploration |
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