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 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
A new model for silicification of cyanobacteria in Proterozoic tidal flats20
The gammaproteobacterium Achromatium forms intracellular amorphous calcium carbonate and not (crystalline) calcite20
The occurrence of 2‐methylhopanoids in modern bacteria and the geological record17
Cryptogamic ground covers as analogues for early terrestrial biospheres: Initiation and evolution of biologically mediated proto‐soils16
A sedimentary record of the evolution of the global marine phosphorus cycle16
Microbial succession and dynamics in meromictic Mono Lake, California15
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
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
0.025015115737915