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 2020-11-01 to 2024-11-01.)
ArticleCitations
Production of diverse brGDGTs by Acidobacterium Solibacter usitatus in response to temperature, pH, and O2 provides a culturing perspective on brGDGT proxies an50
The Sedimentary Geochemistry and Paleoenvironments Project31
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 oxygen28
A new constraint on the antiquity of ancient haloalkaliphilic green algae that flourished in a ca. 300 Ma Paleozoic lake27
A late Paleoproterozoic (1.74 Ga) deep‐sea, low‐temperature, iron‐oxidizing microbial hydrothermal vent community from Arizona, USA26
The ‘classic stromatolite’ Cryptozoön is a keratose sponge‐microbial consortium22
The gammaproteobacterium Achromatium forms intracellular amorphous calcium carbonate and not (crystalline) calcite20
A new model for silicification of cyanobacteria in Proterozoic tidal flats20
The occurrence of 2‐methylhopanoids in modern bacteria and the geological record17
A sedimentary record of the evolution of the global marine phosphorus cycle16
Cryptogamic ground covers as analogues for early terrestrial biospheres: Initiation and evolution of biologically mediated proto‐soils16
Microbial succession and dynamics in meromictic Mono Lake, California15
Ediacaran–Cambrianbioturbation did not extensively oxygenate sediments in shallow marine ecosystems13
Volcanic controls on the microbial habitability of Mars‐analogue hydrothermal environments13
Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans13
Metagenomic analysis of microbial communities across a transect from low to highly hydrocarbon‐contaminated soils in King George Island, Maritime Antarctica13
Neoproterozoic syn‐glacial carbonate precipitation and implications for a snowball Earth13
Inter‐domain horizontal gene transfer of nickel‐binding superoxide dismutase12
Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile12
Microbially induced chromium isotope fractionation and trace elements behavior in lower Cambrian microbialites from the Jaíba Member, Bambuí Basin, Brazil12
Anoxygenic photosynthesis linked to Neoarchean iron formations in Carajás (Brazil)11
Hematite‐promoted nitrate‐reducing Fe(II) oxidation by Acidovorax sp. strain BoFeN1: Roles of mineral catalysis and cell encrustation11
Evaporative silicification in floating microbial mats: patterns of oxygen production and preservation potential in silica‐undersaturated streams, El Tatio, Chile11
The biogeochemical cycling of chlorine11
Phosphatic scales in vase‐shaped microfossil assemblages from Death Valley, Grand Canyon, Tasmania, and Svalbard11
Inverse hydrogen isotope fractionation indicates heterotrophic microbial production of long‐chain n‐alkyl lipids in desolate Antarctic ponds11
Dubiofossils from a Mars‐analogue subsurface palaeoenvironment: The limits of biogenicity criteria10
Widespread mineralization of soft‐bodied insects in Cretaceous amber10
Nitrogen‐based symbioses, phosphorus availability, and accounting for a modern world more productive than the Paleozoic10
Active and dormant microorganisms on glacier surfaces10
Widespread seafloor anoxia during generation of the Ediacaran Shuram carbon isotope excursion10
Messinian bottom‐grown selenitic gypsum: An archive of microbial life10
Influences of pH and substrate supply on the ratio of iron to sulfate reduction10
Electrochemical evidence for in situ microbial activity at the Deep Mine Microbial Observatory (DeMMO), South Dakota, USA10
Marine and terrestrial nitrifying bacteria are sources of diverse bacteriohopanepolyols9
In search of the RNA world on Mars9
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean9
Detection of the deep biosphere in metamorphic rocks from the Chinese continental scientific drilling9
The Dziani Dzaha Lake: A long‐awaited modern analogue for superheavy pyrites8
Builders, tenants, and squatters: the origins of genetic material in modern stromatolites8
The influence of elevated SiO2(aq) on intracellular silica uptake and microbial metabolism8
Carbon reservoir perturbations induced by Deccan volcanism: Stable isotope and biomolecular perspectives from shallow marine environment in Eastern India8
Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga8
Silicate minerals as a direct source of limiting nutrients: Siderophore synthesis and uptake promote ferric iron bioavailability from olivine and microbial growth8
Subseafloor Archaea reflect 139 kyrs of paleodepositional changes in the northern Red Sea7
Endospores associated with deep seabed geofluid features in the eastern Gulf of Mexico7
Contrasting nutrient availability between marine and brackish waters in the late Mesoproterozoic: Evidence from the Paranoá Group, Brazil7
Minimum levels of atmospheric oxygen from fossil tree roots imply new plant−oxygen feedback7
The interplay of environmental constraints and bioturbation on matground development along the marine depositional profile during the Ordovician Radiation7
Exploring the secondary mineral products generated by microbial iron respiration in Archean ocean simulations7
Bacterial and archaeal lipids trace chemo(auto)trophy along the redoxcline in Vancouver Island fjords7
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter7
Influence of aphotic haloclines and euxinia on organic biomarkers and microbial communities in a thalassohaline and alkaline volcanic crater lake6
Biogeochemical transformations after the emergence of oxygenic photosynthesis and conditions for the first rise of atmospheric oxygen6
New geochemical tools for investigating resource and energy functions at deep‐sea cold seeps using amino acid δ15N in chemosymbiotic mussels (Bathymodiolus childressi)6
The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time6
Using thermodynamics to obtain geochemical information from genomes6
A re‐examination of the mechanism of whiting events: A new role for diatoms in Fayetteville Green Lake (New York, USA)6
Structure and function of Shark Bay microbial communities following tropical cyclone Olwyn: A metatranscriptomic and organic geochemical perspective6
Sedimentary pyrite sulfur isotope compositions preserve signatures of the surface microbial mat environment in sediments underlying low‐oxygen cyanobacterial mats6
The deposition and significance of an Ediacaran non‐glacial iron formation6
A review of microbial‐environmental interactions recorded in Proterozoic carbonate‐hosted chert6
Potential role for microbial ureolysis in the rapid formation of carbonate tufa mounds6
Diagenetic nutrient supplies to the Proterozoic biosphere archived in divergent nitrogen isotopic ratios between kerogen and silicate minerals5
Bioavailability of mineral‐associated trace metals as cofactors for nitrogen fixation by Azotobacter vinelandii5
Microbially promoted calcite precipitation in the pelagic redoxcline: Elucidating the formation of the turbid layer5
White and green rust chimneys accumulate RNA in a ferruginous chemical garden5
Mineralogical characterization of biosilicas versus geological analogs5
Evolution of iron and oxygen biogeochemical cycles during the Precambrian5
Microbial chemolithotrophic oxidation of pyrite in a subsurface shale weathering environment: Geologic considerations and potential mechanisms5
Distinguishing cellular from abiotic spheroidal microstructures in the ca. 3.4 Ga Strelley Pool Formation5
‘Ten Years After’—a long‐term settlement and bioerosion experiment in an Arctic rhodolith bed (Mosselbukta, Svalbard)5
Growth of microaerophilic Fe(II)‐oxidizing bacteria using Fe(II) produced by Fe(III) photoreduction5
Molecular dating of the blood pigment hemocyanin provides new insight into the origin of animals5
The role of iron in the formation of Ediacaran ‘death masks’4
Nickel and zinc micronutrient availability in Phanerozoic oceans4
On the trail of iron uptake in ancestral Cyanobacteria on early Earth4
The role of clay minerals in the preservation of Precambrian organic‐walled microfossils4
Coral calcification and carbonate production in the eastern tropical Pacific: The role of branching and massive corals in the reef maintenance4
Inferred ancestry of scytonemin biosynthesis proteins in cyanobacteria indicates a response to Paleoproterozoic oxygenation4
Microbial helpers allow cyanobacteria to thrive in ferruginous waters4
Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi‐dimensional imaging study4
Nanoscale chemical mapping of exometabolites at fungal–mineral interfaces4
Microbial biosignatures in ancient deep‐sea hydrothermal sulfides4
Comparative soft‐tissue preservation in Holocene‐age capelin concretions4
Protracted oxygenation across the Cambrian–Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?4
Taphonomy of microorganisms and microbial microtextures at sulfidic hydrothermal vents: A case study from the Roman Ruins black smokers, Eastern Manus Basin4
Stable carbon isotope values of syndepositional carbonate spherules and micrite record spatial and temporal changes in photosynthesis intensity4
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 China4
Bacterial community structure and metabolic potential in microbialite‐forming mats from South Australian saline lakes3
Coccolith Sr/Ca is a robust temperature and growth rate indicator that withstands dynamic microbial interactions3
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA3
Sulfur isotopes of hydrothermal vent fossils and insights into microbial sulfur cycling within a lower Paleozoic (Ordovician‐early Silurian) vent community3
A 571 million‐year‐old alkaline volcanic lake photosynthesizing microbial community, the Anti‐atlas, Morocco3
Revisiting marine redox conditions during the Ediacaran Shuram carbon isotope excursion3
Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard3
Effects of RuBisCO and CO2 concentration on cyanobacterial growth and carbon isotope fractionation3
Absence of canonical trophic levels in a microbial mat3
Actualistic approaches to interpreting the role of biological decomposition in microbial preservation3
Structural and chemical heterogeneity of Proterozoic organic microfossils of the ca. 1 Ga old Angmaat Formation, Baffin Island, Canada3
Deep water cuspate stromatolites of the Cryogenian Trezona Formation3
Environmental and temporal patterns in bioturbation in the Cambrian–Ordovician of Western Newfoundland3
Distinctive microfossil supports early Paleoproterozoic rise in complex cellular organisation2
Deep‐water first occurrences of Ediacara biota prior to the Shuram carbon isotope excursion in the Wernecke Mountains, Yukon, Canada2
A carbonate corrosion experiment at a marine methane seep: The role of aerobic methanotrophic bacteria2
Carbon cycle dynamics and ecology revealed by the carbon isotopic composition of single organic microfossils during the Late Devonian Biotic Crisis2
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process2
Carbon pump dynamics and limited organic carbon burial during OAE1a2
Foraminifera‐derived carbon contribution to sedimentary inorganic carbon pool: A case study from three Norwegian fjords2
Lipid biomarkers recording marine microbial community structure changes through the Frasnian‐Famennian mass extinction event2
Fire activity across Cretaceous/Paleogene transition: Evidence from pyrogenic biomarkers preserved in the Mahadeo‐Cherrapunji section, Meghalaya, India2
New keratose sponges after the end‐Permian extinction provide insights into biotic recoveries2
Contrasting morphology and growth habits of Frutexites in Late Devonian reef complexes of the Canning Basin, northwestern Australia2
Interplay between abiotic and microbial biofilm‐mediated processes for travertine formation: Insights from a thermal spring (Piscine Carletti, Viterbo, Italy)2
Sulfur cycling at natural hydrocarbon and sulfur seeps in Santa Paula Creek, CA2
Microbial influence on dolomite and authigenic clay mineralisation in dolocrete profiles of NW Australia2
Sulfur disproportionating microbial communities in a dynamic, microoxic‐sulfidic karst system2
Hydrogeological controls on microbial activity and habitability in the Precambrian continental crust2
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