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 2021-11-01 to 2025-11-01.)
ArticleCitations
Physiology, Not Nutrient Availability, May Have Limited Primary Productivity After the Emergence of Oxygenic Photosynthesis76
A Spatially Restricted Distribution of Thermophilic Endospores in Laptev Sea Shelf Sediments Suggests a Limited Dispersal by Local Geofluids34
Widespread mineralization of soft‐bodied insects in Cretaceous amber33
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process28
Kinetics and mechanisms of cyanobacterially induced precipitation of magnesium silicate23
The role of clay minerals in the preservation of Precambrian organic‐walled microfossils18
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean18
Microbially promoted calcite precipitation in the pelagic redoxcline: Elucidating the formation of the turbid layer17
Dynamics of the osmotic lysis of mineral protocells and its avoidance at the origins of life17
The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time16
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Comprehensive molecular‐isotopic characterization of archaeal lipids in the Black Sea water column and underlying sediments16
Oceanic and Sedimentary Microbial Sulfur Cycling Controlled by Local Organic Matter Flux During the Ediacaran Shuram Excursion in the Three Gorges Area, South China15
Effects of RuBisCO and CO2 concentration on cyanobacterial growth and carbon isotope fractionation12
Branching archaeocyaths as ecosystem engineers during the Cambrian radiation12
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA12
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Divergence time estimates for the hypoxia‐inducible factor‐1 alpha (HIF1α) reveal an ancient emergence of animals in low‐oxygen environments11
Metabarcoding reveals high diversity of benthic foraminifera linked to water masses circulation at coastal Svalbard11
Enameloid‐bound δ15N reveals large trophic separation among Late Cretaceous sharks in the northern Gulf of Mexico11
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Stromatolitic Mounds in Tidal‐Facies Sandstones of the Paleoarchean Moodies Group (Barberton Greenstone Belt, Eswatini)11
Reduction in animal abundance and oxygen availability during and after the end‐Triassic mass extinction11
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New Insights Into Upper Messinian Microbial Carbonates: A Dendrolite‐Thrombolite Build‐Up From the Salento Peninsula, Central Mediterranean10
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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, Argentina9
Protracted oxygenation across the Cambrian–Ordovician transition: A key initiator of the Great Ordovician Biodiversification Event?9
Early‐Branching Cyanobacteria Grow Faster and Upregulate Superoxide Dismutase Activity Under a Simulated Early Earth Anoxic Atmosphere9
Elevated δ15N Linked to Inhibited Nitrification Coupled to Ammonia Volatilization in Sediments of Shallow Alkaline‐Hypersaline Lakes9
Terrestrial surface stabilisation by modern analogues of the earliest land plants: A multi‐dimensional imaging study9
A sedimentary record of the evolution of the global marine phosphorus cycle9
Environmental and temporal patterns in bioturbation in the Cambrian–Ordovician of Western Newfoundland8
The Dziani Dzaha Lake: A long‐awaited modern analogue for superheavy pyrites8
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Exploring the secondary mineral products generated by microbial iron respiration in Archean ocean simulations8
Impact of steroid biosynthesis on the aerobic adaptation of eukaryotes8
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Oxygenation and Alkalinity Drive the Lacustrine Nitrogen Isotope Record Throughout the Past 3.2 Billion Years7
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New keratose sponges after the end‐Permian extinction provide insights into biotic recoveries7
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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A Flourishing Planktonic Microbial Community in an Interglacial Offshore Environment: Silicified Microfossils From the Cryogenian Datangpo Formation, South China7
Morphological and Microbial Diversity of Hydromagnesite Microbialites in Lake Salda: A Mars Analog Alkaline Lake7
Interplay between abiotic and microbial biofilm‐mediated processes for travertine formation: Insights from a thermal spring (Piscine Carletti, Viterbo, Italy)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
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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Endospores associated with deep seabed geofluid features in the eastern Gulf of Mexico6
Biogeochemistry of an Iron‐ and Manganese‐Rich Stratified Lake: Tasik Biru, Malaysia, as a Modern Model Habitat for the Ancient Ocean6
The paleoredox context of early eukaryotic evolution: insights from the Tonian Mackenzie Mountains Supergroup, Canada6
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
Lipid biomarkers recording marine microbial community structure changes through the Frasnian‐Famennian mass extinction event6
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Major contribution of sulfide‐derived sulfur to the benthic food web in a large freshwater lake5
Inferred ancestry of scytonemin biosynthesis proteins in cyanobacteria indicates a response to Paleoproterozoic oxygenation5
Physiological and metabolic responses of chemolithoautotrophic NO3− reducers to high hydrostatic pressure5
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Ediacaran–Cambrianbioturbation did not extensively oxygenate sediments in shallow marine ecosystems5
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Coral calcification and carbonate production in the eastern tropical Pacific: The role of branching and massive corals in the reef maintenance5
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
The role of iron in the formation of Ediacaran ‘death masks’5
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Sulfide Oxidation Products Support Microbial Metabolism at Interface Environments in a Marine‐Like Serpentinizing Spring in Northern California5
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The biogeochemical cycling of chlorine4
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An Anaerobic Microbial Community Mediates Epigenetic Native Sulfur and Carbonate Formation During Replacement of Messinian Gypsum at Monte Palco, Sicily4
Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga4
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Hydrogeological controls on microbial activity and habitability in the Precambrian continental crust4
White and green rust chimneys accumulate RNA in a ferruginous chemical garden4
Microbial biosignatures in ancient deep‐sea hydrothermal sulfides4
Copper mobilisation from Cu sulphide minerals by methanobactin: Effect of pH, oxygen and natural organic matter4
Cyanobacteria Boring Limestones in Freshwater Settings—Their Pioneering Role in Sculpturing Pebbles and Carbonate Dissolution3
Dissolved silica affects the bulk iron redox state and recrystallization of minerals generated by photoferrotrophy in a simulated Archean ocean3
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Ultrastructural Perspectives on the Biology and Taphonomy of Tonian Microfossils From the Draken Formation, Spitsbergen3
Primary to post‐depositional microbial controls on the stable and clumped isotope record of shoreline sediments at Fayetteville Green Lake3
Bioavailability of mineral‐associated trace metals as cofactors for nitrogen fixation by Azotobacter vinelandii3
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Mineralization Controls Informative Biomarker Preservation Associated With Soft Part Fossilization in Deep Time3
Isotopic evidence of environmental changes during the Devonian–Carboniferous transition in South China and its implications for the biotic crisis3
Nubecularia‐coralline algal‐serpulid‐microbial bioherms of the Paratethys Sea—Distribution and paleoecological significance (upper Serravallian, upper Sarmatian, Middle Miocene)3
Microbial Cycling of Sulfur and Other Redox‐Sensitive Elements in Porewaters of San Clemente Basin, California, and Cocos Ridge, Costa Rica3
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
A Biofilm Channel Origin for Vermiform Microstructure in Carbonate Microbialites2
A Reassessment of the Coprostane Biomarker in the Ediacaran With Implications for Dickinsonia2
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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Lateral redox variability in ca. 1.9 Ga marine environments indicated by organic carbon and nitrogen isotope compositions2
Microbial diversity and authigenic siderite mediation in sediments surrounding the Kedr‐1 mud volcano, Lake Baikal2
Bacterial community structure and metabolic potential in microbialite‐forming mats from South Australian saline lakes2
Thallium Isotopes Suggest the Global Deep Ocean Did Not Approach Modern Oxygenation During Cambrian Age 3 Metazoan Radiation2
Contrasting morphology and growth habits of Frutexites in Late Devonian reef complexes of the Canning Basin, northwestern Australia2
Pyritic stromatolites from the Paleoarchean Dresser Formation, Pilbara Craton: Resolving biogenicity and hydrothermally influenced ecosystem dynamics2
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