Geobiology

Papers
(The median citation count of Geobiology is 3. 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 2022-06-01 to 2026-06-01.)
ArticleCitations
A Spatially Restricted Distribution of Thermophilic Endospores in Laptev Sea Shelf Sediments Suggests a Limited Dispersal by Local Geofluids91
Physiology, Not Nutrient Availability, May Have Limited Primary Productivity After the Emergence of Oxygenic Photosynthesis47
Kinetics and mechanisms of cyanobacterially induced precipitation of magnesium silicate39
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean29
The role of clay minerals in the preservation of Precambrian organic‐walled microfossils28
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process25
Paleoenvironmental Stasis for the Bioturbating Community During the Paleocene‐Eocene Thermal Maximum at the Southern Iberian Margin24
Comprehensive molecular‐isotopic characterization of archaeal lipids in the Black Sea water column and underlying sediments23
Localized and Transient Oxygenation of Shallow Oceans of Southwestern Laurentia at the Ediacaran–Cambrian Boundary23
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The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time19
Dynamics of the osmotic lysis of mineral protocells and its avoidance at the origins of life18
Effects of RuBisCO and CO 2 concentration on cyanobacterial growth and carbon isotope fractionation18
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Oceanic and Sedimentary Microbial Sulfur Cycling Controlled by Local Organic Matter Flux During the Ediacaran Shuram Excursion in the Three Gorges Area, South China15
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA14
Membrane Vesicle Formation Removes Iron Sulfide Mineral Crusts From the Cell Surface of Growing Sulfate‐Reducing Bacteria14
Branching archaeocyaths as ecosystem engineers during the Cambrian radiation14
Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard13
Stromatolitic Mounds in Tidal‐Facies Sandstones of the Paleoarchean Moodies Group (Barberton Greenstone Belt, Eswatini)13
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Enameloid‐bound δ15N reveals large trophic separation among Late Cretaceous sharks in the northern Gulf of Mexico13
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Early‐Branching Cyanobacteria Grow Faster and Upregulate Superoxide Dismutase Activity Under a Simulated Early Earth Anoxic Atmosphere13
Divergence time estimates for the hypoxia‐inducible factor‐1 alpha (HIF1α) reveal an ancient emergence of animals in low‐oxygen environments13
New Insights Into Upper Messinian Microbial Carbonates: A Dendrolite‐Thrombolite Build‐Up From the Salento Peninsula, Central Mediterranean12
Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi‐dimensional imaging study12
A sedimentary record of the evolution of the global marine phosphorus cycle12
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Elevated δ15N Linked to Inhibited Nitrification Coupled to Ammonia Volatilization in Sediments of Shallow Alkaline‐Hypersaline Lakes11
Reduction in animal abundance and oxygen availability during and after the end‐Triassic mass extinction11
Exploring the secondary mineral products generated by microbial iron respiration in Archean ocean simulations11
Impact of steroid biosynthesis on the aerobic adaptation of eukaryotes11
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, Argentina11
Protracted oxygenation across the Cambrian–Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?11
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A 1 Ma sedimentary ancient DNA (sedaDNA) record of catchment vegetation changes and the developmental history of tropical Lake Towuti (Sulawesi, Indonesia)9
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Interplay between abiotic and microbial biofilm‐mediated processes for travertine formation: Insights from a thermal spring (Piscine Carletti, Viterbo, Italy)9
Environmental and temporal patterns in bioturbation in the Cambrian–Ordovician of Western Newfoundland9
A Flourishing Planktonic Microbial Community in an Interglacial Offshore Environment: Silicified Microfossils From the Cryogenian Datangpo Formation, South China8
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Oxygenation and Alkalinity Drive the Lacustrine Nitrogen Isotope Record Throughout the Past 3.2 Billion Years8
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 China8
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New keratose sponges after the end‐Permian extinction provide insights into biotic recoveries7
Tricks of Nature From the Ancient Earth and Early Mars: Chemical Gardens Generate Biomorphs With High Preservation Potential7
Endospores associated with deep seabed geofluid features in the eastern Gulf of Mexico7
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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
Biogeochemistry of an Iron‐ and Manganese‐Rich Stratified Lake: Tasik Biru, Malaysia, as a Modern Model Habitat for the Ancient Ocean7
The illusion of balance in the history of the biosphere7
Issue Information7
The paleoredox context of early eukaryotic evolution: insights from the Tonian Mackenzie Mountains Supergroup, Canada7
Lipid biomarkers recording marine microbial community structure changes through the Frasnian‐Famennian mass extinction event7
Morphological and Microbial Diversity of Hydromagnesite Microbialites in Lake Salda: A Mars Analog Alkaline Lake7
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Carbonate chimneys at the highly productive point Dume methane seep: Fine‐scale mineralogical, geochemical, and microbiological heterogeneity reflects dynamic and long‐lived methane‐metabolizing habit6
Major contribution of sulfide‐derived sulfur to the benthic food web in a large freshwater lake6
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Two Worlds on a Stone: Arctic Desert Hypoliths and Epiliths Show Spatial Niche Differentiation6
The role of iron in the formation of Ediacaran ‘death masks’6
Ediacaran–Cambrianbioturbation did not extensively oxygenate sediments in shallow marine ecosystems6
Biogeochemical transformations after the emergence of oxygenic photosynthesis and conditions for the first rise of atmospheric oxygen6
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Inferred ancestry of scytonemin biosynthesis proteins in cyanobacteria indicates a response to Paleoproterozoic oxygenation6
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An Anaerobic Microbial Community Mediates Epigenetic Native Sulfur and Carbonate Formation During Replacement of Messinian Gypsum at Monte Palco, Sicily5
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Sulfide Oxidation Products Support Microbial Metabolism at Interface Environments in a Marine‐Like Serpentinizing Spring in Northern California5
Hydrogeological controls on microbial activity and habitability in the Precambrian continental crust5
Physiological and metabolic responses of chemolithoautotrophic NO3− reducers to high hydrostatic pressure5
Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga5
White and green rust chimneys accumulate RNA in a ferruginous chemical garden5
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter4
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Microbial Cycling of Sulfur and Other Redox‐Sensitive Elements in Porewaters of San Clemente Basin, California, and Cocos Ridge, Costa Rica4
Redox Gradient Shapes the Chemical Composition of Peatland Microbial Communities4
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Mineralization Controls Informative Biomarker Preservation Associated With Soft Part Fossilization in Deep Time4
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Isotopic evidence of environmental changes during the Devonian–Carboniferous transition in South China and its implications for the biotic crisis4
The biogeochemical cycling of chlorine4
Microbial biosignatures in ancient deep‐sea hydrothermal sulfides4
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Cyanobacteria Boring Limestones in Freshwater Settings—Their Pioneering Role in Sculpturing Pebbles and Carbonate Dissolution3
Primary to post‐depositional microbial controls on the stable and clumped isotope record of shoreline sediments at Fayetteville Green Lake3
Thallium Isotopes Suggest the Global Deep Ocean Did Not Approach Modern Oxygenation During Cambrian Age 3 Metazoan Radiation3
Nubecularia‐coralline algal‐serpulid‐microbial bioherms of the Paratethys Sea—Distribution and paleoecological significance (upper Serravallian, upper Sarmatian, Middle Miocene)3
Dissolved silica affects the bulk iron redox state and recrystallization of minerals generated by photoferrotrophy in a simulated Archean ocean3
A Biofilm Channel Origin for Vermiform Microstructure in Carbonate Microbialites3
Lateral redox variability in ca. 1.9 Ga marine environments indicated by organic carbon and nitrogen isotope compositions3
A Reassessment of the Coprostane Biomarker in the Ediacaran With Implications for Dickinsonia3
Ultrastructural Perspectives on the Biology and Taphonomy of Tonian Microfossils From the Draken Formation, Spitsbergen3
Bioavailability of mineral‐associated trace metals as cofactors for nitrogen fixation by Azotobacter vinelandii3
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Pyritic stromatolites from the Paleoarchean Dresser Formation, Pilbara Craton: Resolving biogenicity and hydrothermally influenced ecosystem dynamics3
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