Geobiology

Papers
(The H4-Index of Geobiology is 13. 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 2021-05-01 to 2025-05-01.)
ArticleCitations
An experimental study on post‐mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process62
Widespread mineralization of soft‐bodied insects in Cretaceous amber35
Physiology, Not Nutrient Availability, May Have Limited Primary Productivity After the Emergence of Oxygenic Photosynthesis25
A Spatially Restricted Distribution of Thermophilic Endospores in Laptev Sea Shelf Sediments Suggests a Limited Dispersal by Local Geofluids24
The role of clay minerals in the preservation of Precambrian organic‐walled microfossils21
Kinetics and mechanisms of cyanobacterially induced precipitation of magnesium silicate21
Influences of pH and substrate supply on the ratio of iron to sulfate reduction20
Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile19
Iron‐mediated anaerobic ammonium oxidation recorded in the early Archean ferruginous ocean19
Organic preservation of vase‐shaped microfossils from the late Tonian Chuar Group, Grand Canyon, Arizona, USA15
14
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
Oceanic and Sedimentary Microbial Sulfur Cycling Controlled by Local Organic Matter Flux During the Ediacaran Shuram Excursion in the Three Gorges Area, South China13
Structural and chemical heterogeneity of Proterozoic organic microfossils of the ca. 1 Ga old Angmaat Formation, Baffin Island, Canada13
Dynamics of the osmotic lysis of mineral protocells and its avoidance at the origins of life13
Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans13
The diagenetic fate of collagen as revealed by analytical pyrolysis of fossil fish scales from deep time13
0.036324977874756