Geobiology

Papers
(The median citation count of Geobiology is 2. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-03-01 to 2024-03-01.)
ArticleCitations
Groundwater microbial communities reflect geothermal activity on volcanic island875376689
On the co‐evolution of surface oxygen levels and animals81
Radiation of nitrogen‐metabolizing enzymes across the tree of life tracks environmental transitions in Earth history33
Production of diverse brGDGTs by Acidobacterium Solibacter usitatus in response to temperature, pH, and O2 provides a culturing perspective on brGDGT proxies an32
Mineral‐hosted biofilm communities in the continental deep subsurface, Deep Mine Microbial Observatory, SD, USA31
Discovery of the oldest known biomarkers provides evidence for phototrophic bacteria in the 1.73 Ga Wollogorang Formation, Australia25
The Sedimentary Geochemistry and Paleoenvironments Project25
Carbonate facies‐specific stable isotope data record climate, hydrology, and microbial communities in Great Salt Lake, UT25
Chemical signatures of soft tissues distinguish between vertebrates and invertebrates from the Carboniferous Mazon Creek Lagerstätte of Illinois22
Carbon cycle inverse modeling suggests large changes in fractional organic burial are consistent with the carbon isotope record and may have contributed to the rise of oxygen22
A new constraint on the antiquity of ancient haloalkaliphilic green algae that flourished in a ca. 300 Ma Paleozoic lake22
In Situ Fe and S isotope analyses in pyrite from the 3.2 Ga Mendon Formation (Barberton Greenstone Belt, South Africa): Evidence for early microbial iron reduction22
A late Paleoproterozoic (1.74 Ga) deep‐sea, low‐temperature, iron‐oxidizing microbial hydrothermal vent community from Arizona, USA21
The gammaproteobacterium Achromatium forms intracellular amorphous calcium carbonate and not (crystalline) calcite20
The ‘classic stromatolite’ Cryptozoön is a keratose sponge‐microbial consortium20
Stromatolitic digitate sinters form under wide‐ranging physicochemical conditions with diverse hot spring microbial communities18
A new model for silicification of cyanobacteria in Proterozoic tidal flats16
Spherulitic microbialites from modern hypersaline lakes, Rottnest Island, Western Australia16
A micrometer‐scale snapshot on phototroph spatial distributions: mass spectrometry imaging of microbial mats in Octopus Spring, Yellowstone National Park16
Cryptogamic ground covers as analogues for early terrestrial biospheres: Initiation and evolution of biologically mediated proto‐soils15
The occurrence of 2‐methylhopanoids in modern bacteria and the geological record15
Microbial succession and dynamics in meromictic Mono Lake, California13
Formation of micro‐spherulitic barite in association with organic matter within sulfidized stromatolites of the 3.48 billion‐year‐old Dresser Formation, Pilbara Craton13
Unraveling biogeochemical phosphorus dynamics in hyperarid Mars‐analogue soils using stable oxygen isotopes in phosphate12
Understanding the geobiology of the terminal Ediacaran Khatyspyt Lagerstätte (Arctic Siberia, Russia)12
Microbially induced chromium isotope fractionation and trace elements behavior in lower Cambrian microbialites from the Jaíba Member, Bambuí Basin, Brazil11
In situ S‐isotope compositions of sulfate and sulfide from the 3.2 Ga Moodies Group, South Africa: A record of oxidative sulfur cycling11
Inter‐domain horizontal gene transfer of nickel‐binding superoxide dismutase11
Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans10
Infaunal augurs of the Cambrian explosion: An Ediacaran trace fossil assemblage from Nevada, USA10
Inverse hydrogen isotope fractionation indicates heterotrophic microbial production of long‐chain n‐alkyl lipids in desolate Antarctic ponds10
Anoxygenic photosynthesis linked to Neoarchean iron formations in Carajás (Brazil)10
Influence of temperature on the δ13C values and distribution of methanotroph‐related hopanoids in Sphagnum‐dominated peat bogs10
Dubiofossils from a Mars‐analogue subsurface palaeoenvironment: The limits of biogenicity criteria10
Phosphatic scales in vase‐shaped microfossil assemblages from Death Valley, Grand Canyon, Tasmania, and Svalbard10
Effects of seawater Mg2+/Ca2+ ratio and diet on the biomineralization and growth of sea urchins and the relevance of fossil echinoderms to paleoenvironmental reconstructions9
Volcanic controls on the microbial habitability of Mars‐analogue hydrothermal environments9
Biomarker stratigraphy in the Athel Trough of the South Oman Salt Basin at the Ediacaran‐Cambrian Boundary9
Influences of pH and substrate supply on the ratio of iron to sulfate reduction9
A sedimentary record of the evolution of the global marine phosphorus cycle9
Nitrogen‐based symbioses, phosphorus availability, and accounting for a modern world more productive than the Paleozoic9
Detection of the deep biosphere in metamorphic rocks from the Chinese continental scientific drilling8
Messinian bottom‐grown selenitic gypsum: An archive of microbial life8
Metagenomic analysis of microbial communities across a transect from low to highly hydrocarbon‐contaminated soils in King George Island, Maritime Antarctica8
Intense but variable autotrophic activity in a rapidly flushed shallow‐water hydrothermal plume (Kueishantao Islet, Taiwan)8
Electrochemical evidence for in situ microbial activity at the Deep Mine Microbial Observatory (DeMMO), South Dakota, USA7
Marine and terrestrial nitrifying bacteria are sources of diverse bacteriohopanepolyols7
The biogeochemical cycling of chlorine7
Builders, tenants, and squatters: the origins of genetic material in modern stromatolites7
Evaporative silicification in floating microbial mats: patterns of oxygen production and preservation potential in silica‐undersaturated streams, El Tatio, Chile7
Widespread mineralization of soft‐bodied insects in Cretaceous amber7
In search of the RNA world on Mars7
Bacterial and archaeal lipids trace chemo(auto)trophy along the redoxcline in Vancouver Island fjords7
Endospores associated with deep seabed geofluid features in the eastern Gulf of Mexico7
Evidence for local carbon‐cycle perturbations superimposed on the Toarcian carbon isotope excursion7
Subseafloor Archaea reflect 139 kyrs of paleodepositional changes in the northern Red Sea6
Coccolith volume of the Southern Ocean coccolithophore Emiliania huxleyi as a possible indicator for palaeo‐cell volume6
Neoproterozoic syn‐glacial carbonate precipitation and implications for a snowball Earth6
New preparation techniques for molecular and in‐situ analysis of ancient organic micro‐ and nanostructures6
New geochemical tools for investigating resource and energy functions at deep‐sea cold seeps using amino acid δ15N in chemosymbiotic mussels (Bathymodiolus childressi)6
Hematite‐promoted nitrate‐reducing Fe(II) oxidation by Acidovorax sp. strain BoFeN1: Roles of mineral catalysis and cell encrustation6
Carbon reservoir perturbations induced by Deccan volcanism: Stable isotope and biomolecular perspectives from shallow marine environment in Eastern India6
The interplay of environmental constraints and bioturbation on matground development along the marine depositional profile during the Ordovician Radiation6
Structure and function of Shark Bay microbial communities following tropical cyclone Olwyn: A metatranscriptomic and organic geochemical perspective6
Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth5
Molecular dating of the blood pigment hemocyanin provides new insight into the origin of animals5
Widespread seafloor anoxia during generation of the Ediacaran Shuram carbon isotope excursion5
Multiple stages of plant root calcification deciphered by chemical and micromorphological analyses5
The Dziani Dzaha Lake: A long‐awaited modern analogue for superheavy pyrites5
Micro‐ and nano‐scale mineralogical characterization of Fe(II)‐oxidizing bacterial stalks5
Microbially promoted calcite precipitation in the pelagic redoxcline: Elucidating the formation of the turbid layer5
Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile5
The deposition and significance of an Ediacaran non‐glacial iron formation5
Minimum levels of atmospheric oxygen from fossil tree roots imply new plant−oxygen feedback5
Potential role for microbial ureolysis in the rapid formation of carbonate tufa mounds5
Contrasting nutrient availability between marine and brackish waters in the late Mesoproterozoic: Evidence from the Paranoá Group, Brazil5
Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga4
Ediacaran–Cambrian bioturbation did not extensively oxygenate sediments in shallow marine ecosystems4
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean4
Deconstructing Earth’s oldest ichnofossil record from the Pilbara Craton, West Australia: Implications for seeking life in the Archean subseafloor4
The influence of elevated SiO2(aq) on intracellular silica uptake and microbial metabolism4
Microbial chemolithotrophic oxidation of pyrite in a subsurface shale weathering environment: Geologic considerations and potential mechanisms4
Distinguishing cellular from abiotic spheroidal microstructures in the ca. 3.4 Ga Strelley Pool Formation4
Exploring the secondary mineral products generated by microbial iron respiration in Archean ocean simulations4
On the trail of iron uptake in ancestral Cyanobacteria on early Earth4
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter4
Mineralogical characterization of biosilicas versus geological analogs3
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA3
Energetics of Acidianus ambivalens growth in response to oxygen availability3
Low oxygen levels with high redox heterogeneity in the late Ediacaran shallow ocean: Constraints from I/(Ca + Mg) and Ce/Ce* of the Dengying Formation, South China3
Sedimentary pyrite sulfur isotope compositions preserve signatures of the surface microbial mat environment in sediments underlying low‐oxygen cyanobacterial mats3
Microbial helpers allow cyanobacteria to thrive in ferruginous waters3
A 571 million‐year‐old alkaline volcanic lake photosynthesizing microbial community, the Anti‐atlas, Morocco3
Actualistic approaches to interpreting the role of biological decomposition in microbial preservation3
Bioavailability of mineral‐associated trace metals as cofactors for nitrogen fixation by Azotobacter vinelandii3
The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time3
Microbial colonization of metal sulfide minerals at a diffuse‐flow deep‐sea hydrothermal vent at 9°50′N on the East Pacific Rise3
Sulfur isotopes of hydrothermal vent fossils and insights into microbial sulfur cycling within a lower Paleozoic (Ordovician‐early Silurian) vent community3
White and green rust chimneys accumulate RNA in a ferruginous chemical garden3
Comparative soft‐tissue preservation in Holocene‐age capelin concretions3
Using thermodynamics to obtain geochemical information from genomes3
The role of iron in the formation of Ediacaran ‘death masks’3
‘Ten Years After’—a long‐term settlement and bioerosion experiment in an Arctic rhodolith bed (Mosselbukta, Svalbard)3
Effects of RuBisCO and CO2 concentration on cyanobacterial growth and carbon isotope fractionation3
Authigenic anatase within 1 billion‐year‐old cells3
Active and dormant microorganisms on glacier surfaces3
Associations between redox‐sensitive trace metals and microbial communities in a Proterozoic ocean analogue3
Isotopically anomalous organic carbon in the aftermath of the Marinoan snowball Earth3
Influence of aphotic haloclines and euxinia on organic biomarkers and microbial communities in a thalassohaline and alkaline volcanic crater lake3
Bacterial community structure and metabolic potential in microbialite‐forming mats from South Australian saline lakes2
Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi‐dimensional imaging study2
Biogeochemical transformations after the emergence of oxygenic photosynthesis and conditions for the first rise of atmospheric oxygen2
Nanoscale chemical mapping of exometabolites at fungal–mineral interfaces2
Taphonomy of microorganisms and microbial microtextures at sulfidic hydrothermal vents: A case study from the Roman Ruins black smokers, Eastern Manus Basin2
Foraminifera‐derived carbon contribution to sedimentary inorganic carbon pool: A case study from three Norwegian fjords2
Diagenetic nutrient supplies to the Proterozoic biosphere archived in divergent nitrogen isotopic ratios between kerogen and silicate minerals2
Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard2
Carbon cycle dynamics and ecology revealed by the carbon isotopic composition of single organic microfossils during the Late Devonian Biotic Crisis2
Living phosphatic stromatolites in a low‐phosphorus environment: Implications for the use of phosphorus as a proxy for phosphate levels in paleo‐systems2
Absence of canonical trophic levels in a microbial mat2
Sulfur cycling at natural hydrocarbon and sulfur seeps in Santa Paula Creek, CA2
A review of microbial‐environmental interactions recorded in Proterozoic carbonate‐hosted chert2
A re‐examination of the mechanism of whiting events: A new role for diatoms in Fayetteville Green Lake (New York, USA)2
Growth of microaerophilic Fe(II)‐oxidizing bacteria using Fe(II) produced by Fe(III) photoreduction2
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process2
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