| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2018JGRE..123.1012M |
| P356 | DOI | 10.1029/2017JE005478 |
| P932 | PMC publication ID | 6049883 |
| P698 | PubMed publication ID | 30034979 |
| P50 | author | Derek Briggs | Q530161 |
| John P. Grotzinger | Q1701289 | ||
| Roger Everett Summons | Q17025799 | ||
| Sean McMahon | Q25662830 | ||
| Abigail A. Fraeman | Q57895473 | ||
| Kenneth H. Williford | Q56424375 | ||
| Ralph Milliken | Q59668352 | ||
| P2093 | author name string | T Bosak | |
| S A Newman | |||
| M Daye | |||
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| Ichnotaxonomy of microbial trace fossils in volcanic glass | Q58012756 | ||
| 3.5 billion years of glass bioalteration: Volcanic rocks as a basis for microbial life? | Q58012759 | ||
| Insights into cyanobacterial fossilization in Ediacaran siliciclastic environments | Q58041229 | ||
| Insights into surface runoff on early Mars from paleolake basin morphology and stratigraphy | Q58041246 | ||
| Experimental evidence that clay inhibits bacterial decomposers: Implications for preservation of organic fossils | Q58041360 | ||
| Biosignatures link microorganisms to iron mineralization in a paleoaquifer | Q58078595 | ||
| Carbon isotope fractionation by circumneutral iron-oxidizing bacteria | Q58078922 | ||
| Sulfate availability and the geological record of cold-seep deposits | Q58080674 | ||
| A hematite-bearing layer in Gale Crater, Mars: Mapping and implications for past aqueous conditions | Q58083192 | ||
| Are the large filamentous microfossils preserved in Messinian gypsum colorless sulfide-oxidizing bacteria? | Q58083291 | ||
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| Microbial membrane lipids in active and inactive sinters from Champagne Pool, New Zealand: Elucidating past geothermal chemistry and microbiology | Q58098112 | ||
| Opaline silica in young deposits on Mars | Q58211436 | ||
| Stratigraphic architectures spotted in southern Melas Chasma, Valles Marineris, Mars | Q58222205 | ||
| Ferric oxides in East Candor Chasma, Valles Marineris (Mars) inferred from analysis of OMEGA/Mars Express data: Identification and geological interpretation | Q58355004 | ||
| Juvenile chemical sediments and the long term persistence of water at the surface of Mars | Q58365456 | ||
| Acid-sulfate weathering of synthetic Martian basalt: The acid fog model revisited | Q58365533 | ||
| Iron-oxidizing microbial ecosystems thrived in late Paleoproterozoic redox-stratified oceans | Q58391458 | ||
| Suboxic deep seawater in the late Paleoproterozoic: Evidence from hematitic chert and iron formation related to seafloor-hydrothermal sulfide deposits, central Arizona, USA | Q58391492 | ||
| Microbiological processes in banded iron formation deposition | Q58417964 | ||
| The potential significance of microbial Fe(III) reduction during deposition of Precambrian banded iron formations | Q58418028 | ||
| Bacterial clay authigenesis: a common biogeochemical process | Q58418039 | ||
| Authigenic mineralization and detrital clay binding by freshwater biofilms: The Brahmani river, India | Q58418040 | ||
| In situ silicification of an Icelandic hot spring microbial mat: implications for microfossil formation | Q58418048 | ||
| Early Jurassic hydrothermal vent community from the Franciscan Complex, San Rafael Mountains, California | Q58457328 | ||
| New evidence for 250 Ma age of halotolerant bacterium from a Permian salt crystal | Q58458056 | ||
| Processes of carbonate precipitation in modern microbial mats | Q58866997 | ||
| A mineralogical signature for Burgess Shale–type fossilization | Q57585282 | ||
| Reply to comment on the paper by Davies et al. “Resolving MISS conceptions and misconceptions: A geological approach to sedimentary surface textures generated by microbial and abiotic processes” (Earth Science Reviews, 154 (2016), 210–246) | Q57660863 | ||
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| Curiosity's Mission of Exploration at Gale Crater, Mars | Q57727553 | ||
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| Fossilization potential of iron-bearing minerals in acidic environments of Rio Tinto, Spain: Implications for Mars exploration | Q57859280 | ||
| Diagenetic silica enrichment and late-stage groundwater activity in Gale crater, Mars | Q57867905 | ||
| Detection of crystalline hematite mineralization on Mars by the Thermal Emission Spectrometer: Evidence for near-surface water | Q57874334 | ||
| Archean (3.33 Ga) microbe-sediment systems were diverse and flourished in a hydrothermal context | Q57884145 | ||
| Defining biominerals and organominerals: Direct and indirect indicators of life | Q57884322 | ||
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| Gypsum-permineralized microfossils and their relevance to the search for life on Mars. | Q34337098 | ||
| Deep fracture fluids isolated in the crust since the Precambrian era. | Q34344887 | ||
| Martian fluvial conglomerates at Gale crater | Q34347765 | ||
| In situ evidence for an ancient aqueous environment at Meridiani Planum, Mars | Q34373014 | ||
| Mineralogy of a mudstone at Yellowknife Bay, Gale crater, Mars | Q34390861 | ||
| In situ radiometric and exposure age dating of the martian surface | Q34390874 | ||
| Mars' surface radiation environment measured with the Mars Science Laboratory's Curiosity rover | Q34390889 | ||
| Volatile and organic compositions of sedimentary rocks in Yellowknife Bay, Gale crater, Mars | Q34390894 | ||
| Sulfates in Martian layered terrains: the OMEGA/Mars Express view | Q34395598 | ||
| Ancient aqueous environments at Endeavour crater, Mars | Q34399846 | ||
| Trajectories of martian habitability | Q34403029 | ||
| The Rhynie cherts: an early Devonian ecosystem preserved by hydrothermal activity | Q34434267 | ||
| Common origins of RNA, protein and lipid precursors in a cyanosulfidic protometabolism | Q34468399 | ||
| Evidence for indigenous nitrogen in sedimentary and aeolian deposits from the Curiosity rover investigations at Gale crater, Mars | Q34469772 | ||
| Bacillus subtilis spores on artificial meteorites survive hypervelocity atmospheric entry: implications for Lithopanspermia | Q34479770 | ||
| Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars | Q34497447 | ||
| Reconstructing the transport history of pebbles on Mars | Q34497799 | ||
| The changing view of eukaryogenesis - fossils, cells, lineages and how they all come together | Q34541216 | ||
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| Iron minerals within specific microfossil morphospecies of the 1.88 Ga Gunflint Formation | Q37733808 | ||
| Subsurface water and clay mineral formation during the early history of Mars | Q37952501 | ||
| Perchlorates on Mars enhance the bacteriocidal effects of UV light | Q38430051 | ||
| Taphonomy of Microbial Biosignatures in Spring Deposits: A Comparison of Modern, Quaternary, and Jurassic Examples | Q38432536 | ||
| Ancient sedimentary structures in the <3.7 Ga Gillespie Lake Member, Mars, that resemble macroscopic morphology, spatial associations, and temporal succession in terrestrial microbialites | Q38446376 | ||
| Morphological biosignatures in gypsum: diverse formation processes of Messinian (∼6.0 Ma) gypsum stromatolites | Q38452813 | ||
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| Fossilization processes in siliceous thermal springs: trends in preservation along thermal gradients | Q41550382 | ||
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| Weighing the deep continental biosphere | Q43777568 | ||
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| Reassessing the evidence for the earliest traces of life | Q44094626 | ||
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| Carbon and sulfur isotopic signatures of ancient life and environment at the microbial scale: Neoarchean shales and carbonates | Q46220673 | ||
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| Habitability on Early Mars and the Search for Biosignatures with the ExoMars Rover. | Q47140722 | ||
| Evidence from fluid inclusions for microbial methanogenesis in the early Archaean era. | Q47297315 | ||
| Archean microfossils and abiomorphs | Q47329606 | ||
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| Microorganisms from the Gunflint Chert | Q47795957 | ||
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| Fungus-like mycelial fossils in 2.4-billion-year-old vesicular basalt | Q55882648 | ||
| Sequence and timing of conditions on early Mars | Q55884346 | ||
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| Evidence for the origin of layered deposits in Candor Chasma, Mars, from mineral composition and hydrologic modeling | Q55919717 | ||
| An abiotic model for stromatolite morphogenesis | Q55922589 | ||
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| The early environment and its evolution on Mars: Implication for life | Q55934496 | ||
| Modelling the surface and subsurface Martian radiation environment: Implications for astrobiology | Q55934497 | ||
| Reanalysis of the Viking results suggests perchlorate and organics at midlatitudes on Mars | Q55934502 | ||
| Exceptional preservation of soft-bodied Ediacara Biota promoted by silica-rich oceans | Q56001443 | ||
| Advanced Oxidation Processes for Organic Contaminant Destruction Based on the Fenton Reaction and Related Chemistry | Q56049490 | ||
| Cambrian Burgess Shale–type deposits share a common mode of fossilization | Q56115275 | ||
| Silica deposits in the Nili Patera caldera on the Syrtis Major volcanic complex on Mars | Q56227225 | ||
| Physical and hydraulic properties of modern sinter deposits: El Tatio, Atacama | Q56270172 | ||
| Simulation of the environmental climate conditions on martian surface and its effect on Deinococcus radiodurans | Q56286419 | ||
| The origins of perchlorate in the Martian soil | Q56385129 | ||
| Unravelling abiogenic and biogenic sources of methane in the Earth's deep subsurface | Q56386952 | ||
| Molecular evidence for life in the 3.5 billion year old Warrawoona chert | Q56431902 | ||
| Secular distribution of Burgess-Shale-type preservation | Q56460317 | ||
| Microbial biofilms and the preservation of the Ediacara biota | Q56460544 | ||
| An assessment of the meteoritic contribution to the Martian soil | Q56475066 | ||
| Geologic setting of serpentine deposits on Mars | Q56552131 | ||
| Carbonaceous and siliceous Neoproterozoic vase-shaped microfossils (Urucum Formation, Brazil) and the question of early protistan biomineralization | Q56553174 | ||
| Rates and mechanisms of chemical weathering of ferromagnesian silicate minerals on Mars | Q56565536 | ||
| Global mapping of Martian hematite mineral deposits: Remnants of water-driven processes on early Mars | Q56568420 | ||
| Gray hematite distribution and formation in Ophir and Candor chasmata | Q56568421 | ||
| HiRISE imaging of impact megabreccia and sub-meter aqueous strata in Holden Crater, Mars | Q56568424 | ||
| Columbus crater and other possible groundwater-fed paleolakes of Terra Sirenum, Mars | Q56568434 | ||
| The Role of Decay and Mineralization in the Preservation of Soft-Bodied Fossils | Q56592815 | ||
| The Weng'an biota and the Ediacaran radiation of multicellular eukaryotes | Q56636716 | ||
| Microfossils of sulphur-metabolizing cells in 3.4-billion-year-old rocks of Western Australia | Q56672579 | ||
| Composition and implications of diverse lipids in New Zealand Geothermal sinters | Q56682505 | ||
| The effect of cyanobacteria on silica precipitation at neutral pH: implications for bacterial silicification in geothermal hot springs | Q56687251 | ||
| The effect of ionizing radiation on the preservation of amino acids on Mars | Q56698040 | ||
| Textured organic surfaces associated with the Ediacara biota in South Australia | Q56766788 | ||
| Remarkable preservation of microbial mats in Neoproterozoic siliciclastic settings: Implications for Ediacaran taphonomic models | Q56766790 | ||
| Sublacustrine depositional fans in southwest Melas Chasma | Q56835279 | ||
| Microbially Induced Sedimentary Structures: A New Category within the Classification of Primary Sedimentary Structures | Q56907925 | ||
| Oxygen-Dependent Morphogenesis of Modern Clumped Photosynthetic Mats and Implications for the Archean Stromatolite Record | Q57541892 | ||
| Carbonates in the Martian meteorite Allan Hills 84001 formed at 18 +/- 4 degrees C in a near-surface aqueous environment | Q35345809 | ||
| Selective stabilization of aliphatic organic carbon by iron oxide | Q35659709 | ||
| Ultrastructural Heterogeneity of Carbonaceous Material in Ancient Cherts: Investigating Biosignature Origin and Preservation. | Q35819140 | ||
| Tracing Biosignature Preservation of Geothermally Silicified Microbial Textures into the Geological Record | Q35819146 | ||
| Evidence for methane in Martian meteorites. | Q35905931 | ||
| The microbial role in hot spring silicification | Q36018155 | ||
| Impact-generated hydrothermal systems on Earth and Mars | Q59153057 | ||
| The igneous oceanic crust – Earth's largest fungal habitat? | Q59267266 | ||
| Identification of hydrated silicate minerals on Mars using MRO-CRISM: Geologic context near Nili Fossae and implications for aqueous alteration | Q59700291 | ||
| Light and variable 37 Cl/ 35 Cl ratios in rocks from Gale Crater, Mars: Possible signature of perchlorate | Q59770459 | ||
| Poor preservation potential of organics in Meridiani Planum hematite-bearing sedimentary rocks | Q59781690 | ||
| Late Archean Calcite-Microbe Interactions: Two Morphologically Distinct Microbial Communities That Affected Calcite Nucleation Differently | Q59781697 | ||
| INFLUENCE OF GAS PRODUCTION AND FILAMENT ORIENTATION ON STROMATOLITE MICROFABRIC | Q59829123 | ||
| Geological context of water-altered minerals in Valles Marineris, Mars | Q59835678 | ||
| Discovery of alunite in Cross crater, Terra Sirenum, Mars: Evidence for acidic, sulfurous waters | Q59835706 | ||
| Evaluating the role of microbial sulfate reduction in the early Archean using quadruple isotope systematics | Q59842425 | ||
| Most Mars minerals in a nutshell: Various alteration phases formed in a single environment in Noctis Labyrinthus | Q59896720 | ||
| Diagenetic haematite and sulfate assemblages in Valles Marineris | Q59896818 | ||
| Stratigraphy of hydrated sulfates in the sedimentary deposits of Aram Chaos, Mars | Q59896877 | ||
| First detection of fluorine on Mars: Implications for Gale Crater's geochemistry | Q59926114 | ||
| Structure and stratigraphy of Home Plate from the Spirit Mars Exploration Rover | Q59935848 | ||
| The origin and occurrence of subaqueous sedimentary cracks | Q59947041 | ||
| The role of experiments in investigating the taphonomy of exceptional preservation | Q59947068 | ||
| Salinity Influences the Response ofHalomonas hydrothermalisto Artificial Fossilization by Evaporative Silicification | Q60038033 | ||
| Light-toned strata and inverted channels adjacent to Juventae and Ganges chasmata, Mars | Q60154056 | ||
| LXXIII.—Oxidation of tartaric acid in presence of iron | Q60304014 | ||
| Feedbacks between flow, sediment motion and microbial growth on sand bars initiate and shape elongated stromatolite mounds | Q60508271 | ||
| Microbial shaping of sedimentary wrinkle structures | Q60508273 | ||
| Microbial biofacies in hot-spring sinters; a model based on Ohaaki Pool, North Island, New Zealand | Q60682930 | ||
| Limitations to a microbial iron cycle on Mars | Q61043906 | ||
| Mineralogy of the Martian Surface | Q66363715 | ||
| Water on Mars and the prospect of Martian life | Q66364390 | ||
| Paleoclimate of Mars as captured by the stratigraphic record in Gale Crater | Q66371318 | ||
| Deep crustal carbonate rocks exposed by meteor impact on Mars | Q68981096 | ||
| The silica cycle in the Precambrian | Q70941452 | ||
| Brazilian Analog for Ancient Marine Environments on Mars | Q70941904 | ||
| Environmental control on diverse stromatolite morphologies in the 3000 Myr Pongola Supergroup, South Africa | Q71066538 | ||
| Examining Archean methanotrophy | Q73892332 | ||
| Spatially-resolved isotopic study of carbon trapped in ∼3.43 Ga Strelley Pool Formation stromatolites | Q73894905 | ||
| The origin and evolution of oxygenic photosynthesis | Q74530080 | ||
| Formation and stability of oxygen-rich bubbles that shape photosynthetic mats | Q82426350 | ||
| Calculated fractionation factors for carbon and hydrogen isotope exchange in the system calcite-carbon dioxide-graphite-methane-hydrogen-water vapor | Q95496895 | ||
| EARLY JURASSIC HYDROTHERMAL VENT COMMUNITY FROM THE FRANCISCAN COMPLEX, CALIFORNIA | Q99659808 | ||
| Distribution, Classification, and Ages of Martian Impact Crater Lakes | Q101248627 | ||
| Wind-blown sandstones cemented by sulfate and clay minerals in Gale Crater, Mars | Q102362276 | ||
| Depth of the Martian cryosphere: Revised estimates and implications for the existence and detection of subpermafrost groundwater | Q105244130 | ||
| Iron oxyhydroxide mineralization on microbial extracellular polysaccharides | Q105726535 | ||
| Distribution and formation of chlorides and phyllosilicates in Terra Sirenum, Mars | Q105737747 | ||
| Extended survival of several organisms and amino acids under simulated martian surface conditions | Q106533516 | ||
| Radiolytic H2in continental crust: Nuclear power for deep subsurface microbial communities | Q106533573 | ||
| Dating ultra-deep mine waters with noble gases and 36Cl, Witwatersrand Basin, South Africa | Q106533579 | ||
| Geochemistry and sedimentology of a facies transition from limestone to iron-formation deposition in the early Proterozoic Transvaal Supergroup, South Africa | Q107369164 | ||
| P433 | issue | 5 | |
| P407 | language of work or name | English | Q1860 |
| P304 | page(s) | 1012-1040 | |
| P577 | publication date | 2018-05-24 | |
| P1433 | published in | Journal of Geophysical Research. Planets | Q27726640 |
| P1476 | title | A Field Guide to Finding Fossils on Mars | |
| P478 | volume | 123 |
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