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 2021-08-01 to 2025-08-01.)
ArticleCitations
Widespread mineralization of soft‐bodied insects in Cretaceous amber67
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process29
The role of clay minerals in the preservation of Precambrian organic‐walled microfossils27
Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile24
A Spatially Restricted Distribution of Thermophilic Endospores in Laptev Sea Shelf Sediments Suggests a Limited Dispersal by Local Geofluids19
Physiology, Not Nutrient Availability, May Have Limited Primary Productivity After the Emergence of Oxygenic Photosynthesis18
Kinetics and mechanisms of cyanobacterially induced precipitation of magnesium silicate16
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean16
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Effects of RuBisCO and CO2 concentration on cyanobacterial growth and carbon isotope fractionation14
Microbially promoted calcite precipitation in the pelagic redoxcline: Elucidating the formation of the turbid layer14
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA14
The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time14
Dynamics of the osmotic lysis of mineral protocells and its avoidance at the origins of life13
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Comprehensive molecular‐isotopic characterization of archaeal lipids in the Black Sea water column and underlying sediments12
Branching archaeocyaths as ecosystem engineers during the Cambrian radiation12
Oceanic and Sedimentary Microbial Sulfur Cycling Controlled by Local Organic Matter Flux During the Ediacaran Shuram Excursion in the Three Gorges Area, South China12
The interplay of environmental constraints and bioturbation on matground development along the marine depositional profile during the Ordovician Radiation11
Divergence time estimates for the hypoxia‐inducible factor‐1 alpha (HIF1α) reveal an ancient emergence of animals in low‐oxygen environments11
Enameloid‐bound δ15N reveals large trophic separation among Late Cretaceous sharks in the northern Gulf of Mexico10
Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi‐dimensional imaging study10
Microbial mats and their palaeoenvironmental analysis in offshore – shelf facies of the Los Molles Formation (Toarcian – Lower Callovian) in the Chacay Melehue area, Neuquén Basin, Argentina10
Stromatolitic Mounds in Tidal‐Facies Sandstones of the Paleoarchean Moodies Group (Barberton Greenstone Belt, Eswatini)10
Reduction in animal abundance and oxygen availability during and after the end‐Triassic mass extinction10
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Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard10
A sedimentary record of the evolution of the global marine phosphorus cycle10
Protracted oxygenation across the Cambrian–Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?9
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Exploring the secondary mineral products generated by microbial iron respiration in Archean ocean simulations9
New Insights Into Upper Messinian Microbial Carbonates: A Dendrolite‐Thrombolite Build‐Up From the Salento Peninsula, Central Mediterranean9
Carbon reservoir perturbations induced by Deccan volcanism: Stable isotope and biomolecular perspectives from shallow marine environment in Eastern India9
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Early‐Branching Cyanobacteria Grow Faster and Upregulate Superoxide Dismutase Activity Under a Simulated Early Earth Anoxic Atmosphere9
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Interplay between abiotic and microbial biofilm‐mediated processes for travertine formation: Insights from a thermal spring (Piscine Carletti, Viterbo, Italy)8
Impact of steroid biosynthesis on the aerobic adaptation of eukaryotes8
The Dziani Dzaha Lake: A long‐awaited modern analogue for superheavy pyrites8
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Elevated δ15N Linked to Inhibited Nitrification Coupled to Ammonia Volatilization in Sediments of Shallow Alkaline‐Hypersaline Lakes8
Environmental and temporal patterns in bioturbation in the Cambrian–Ordovician of Western Newfoundland8
A 1 Ma sedimentary ancient DNA (sedaDNA) record of catchment vegetation changes and the developmental history of tropical Lake Towuti (Sulawesi, Indonesia)7
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Production of diverse brGDGTs by Acidobacterium Solibacter usitatus in response to temperature, pH, and O2 provides a culturing perspective on brGDGT proxies an7
New keratose sponges after the end‐Permian extinction provide insights into biotic recoveries7
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Contrasting nutrient availability between marine and brackish waters in the late Mesoproterozoic: Evidence from the Paranoá Group, Brazil7
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The paleoredox context of early eukaryotic evolution: insights from the Tonian Mackenzie Mountains Supergroup, Canada7
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 China7
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Morphological and Microbial Diversity of Hydromagnesite Microbialites in Lake Salda: A Mars Analog Alkaline Lake6
The illusion of balance in the history of the biosphere6
Biogeochemical transformations after the emergence of oxygenic photosynthesis and conditions for the first rise of atmospheric oxygen6
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Evaporative silicification in floating microbial mats: patterns of oxygen production and preservation potential in silica‐undersaturated streams, El Tatio, Chile6
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Lipid biomarkers recording marine microbial community structure changes through the Frasnian‐Famennian mass extinction event6
Endospores associated with deep seabed geofluid features in the eastern Gulf of Mexico6
Major contribution of sulfide‐derived sulfur to the benthic food web in a large freshwater lake6
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Ediacaran–Cambrianbioturbation did not extensively oxygenate sediments in shallow marine ecosystems5
The role of iron in the formation of Ediacaran ‘death masks’5
Carbonate chimneys at the highly productive point Dume methane seep: Fine‐scale mineralogical, geochemical, and microbiological heterogeneity reflects dynamic and long‐lived methane‐metabolizing habit5
Two Worlds on a Stone: Arctic Desert Hypoliths and Epiliths Show Spatial Niche Differentiation5
Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga5
Inferred ancestry of scytonemin biosynthesis proteins in cyanobacteria indicates a response to Paleoproterozoic oxygenation5
Sulfide Oxidation Products Support Microbial Metabolism at Interface Environments in a Marine‐Like Serpentinizing Spring in Northern California4
Neoproterozoic syn‐glacial carbonate precipitation and implications for a snowball Earth4
Hydrogeological controls on microbial activity and habitability in the Precambrian continental crust4
The biogeochemical cycling of chlorine4
Influence of aphotic haloclines and euxinia on organic biomarkers and microbial communities in a thalassohaline and alkaline volcanic crater lake4
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Coral calcification and carbonate production in the eastern tropical Pacific: The role of branching and massive corals in the reef maintenance4
An Anaerobic Microbial Community Mediates Epigenetic Native Sulfur and Carbonate Formation During Replacement of Messinian Gypsum at Monte Palco, Sicily4
Physiological and metabolic responses of chemolithoautotrophic NO3− reducers to high hydrostatic pressure4
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter4
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White and green rust chimneys accumulate RNA in a ferruginous chemical garden4
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Growth of microaerophilic Fe(II)‐oxidizing bacteria using Fe(II) produced by Fe(III) photoreduction3
Redox Gradient Shapes the Chemical Composition of Peatland Microbial Communities3
Microbial Cycling of Sulfur and Other Redox‐Sensitive Elements in Porewaters of San Clemente Basin, California, and Cocos Ridge, Costa Rica3
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Isotopic evidence of environmental changes during the Devonian–Carboniferous transition in South China and its implications for the biotic crisis3
Microbial chemolithotrophic oxidation of pyrite in a subsurface shale weathering environment: Geologic considerations and potential mechanisms3
Bioavailability of mineral‐associated trace metals as cofactors for nitrogen fixation by Azotobacter vinelandii3
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Microbial biosignatures in ancient deep‐sea hydrothermal sulfides3
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Ultrastructural Perspectives on the Biology and Taphonomy of Tonian Microfossils From the Draken Formation, Spitsbergen3
Potential role for microbial ureolysis in the rapid formation of carbonate tufa mounds3
Metagenomic analysis of microbial communities across a transect from low to highly hydrocarbon‐contaminated soils in King George Island, Maritime Antarctica3
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Dissolved silica affects the bulk iron redox state and recrystallization of minerals generated by photoferrotrophy in a simulated Archean ocean2
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Bacterial community structure and metabolic potential in microbialite‐forming mats from South Australian saline lakes2
Pyritic stromatolites from the Paleoarchean Dresser Formation, Pilbara Craton: Resolving biogenicity and hydrothermally influenced ecosystem dynamics2
Cyanobacteria Boring Limestones in Freshwater Settings—Their Pioneering Role in Sculpturing Pebbles and Carbonate Dissolution2
A Biofilm Channel Origin for Vermiform Microstructure in Carbonate Microbialites2
Absence of canonical trophic levels in a microbial mat2
Multiple sulphur isotope record of Paleoarchean sedimentary rocks across the Onverwacht Group, Barberton Greenstone Belt, South Africa2
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Primary to post‐depositional microbial controls on the stable and clumped isotope record of shoreline sediments at Fayetteville Green Lake2
Nubecularia‐coralline algal‐serpulid‐microbial bioherms of the Paratethys Sea—Distribution and paleoecological significance (upper Serravallian, upper Sarmatian, Middle Miocene)2
Microbial diversity and authigenic siderite mediation in sediments surrounding the Kedr‐1 mud volcano, Lake Baikal2
Lateral redox variability in ca. 1.9 Ga marine environments indicated by organic carbon and nitrogen isotope compositions2
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