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Significant Increase of Continental Freeboard During the Early Paleoproterozoic: Insights From Metasediment‐Derived Granites

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Dated gene duplications elucidate the evolutionary assembly of eukaryotes

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The end of the isotopic evolution of atmospheric xenon

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Testing the early Paleoproterozoic connection of the Superior and Wyoming cratons with geochronology and geochemistry

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Global continental volcanism controlled the evolution of the oceanic nickel reservoir

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A battle against arsenic toxicity by Earth’s earliest complex life forms

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Marine sulphate captures a Paleozoic transition to a modern terrestrial weathering environment

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The Black Angel deposit, Greenland: a Paleoproterozoic evaporite-related Mississippi Valley-type Zn–Pb deposit

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Transient marine bottom water oxygenation on continental shelves by 2.65 billion years ago

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Climate shapes the oxygenation of Earth's atmosphere across the Great Oxidation Event

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Isotopic Constraints on the Nature of Primary Precipitates in Archean–Early Paleoproterozoic Iron Formations from Determinations of the Iron Phonon Density of States of Greenalite and 2L- and 6L-Ferrihydrite

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Earth’s oldest terrestrial red beds as direct evidence for the Great Oxidation Event ca. 2.3 Ga

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Evolution of iron and oxygen biogeochemical cycles during the Precambrian

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Geochemical behavior of iron-sulfur coupling in coastal wetland sediments and its impact on heavy metal speciation and migration

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Evolution of continental crust and sedimentary rock chemistry through time

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Bioavailable phosphite in the surface ocean during the Great Oxidation Event

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Insights from modern diffuse-flow hydrothermal systems into the origin of post-GOE deep-water Fe-Si precipitates

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Archaean oxygen oases driven by pulses of enhanced phosphorus recycling in the ocean

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Geochemical behavior of redox sensitive trace metals in marine environment and their applications as paleoredox proxies

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A diverse Palaeoproterozoic microbial ecosystem implies early eukaryogenesis

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Origin of the Neoarchean VMS-BIF Metallogenic Association in the Qingyuan Greenstone Belt, North China Craton: Constraints from Geology, Geochemistry, and Iron and Multiple Sulfur (δ33S, δ34S, and δ36S) Isotopes

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A seawater oxygen oscillation recorded by iron formations prior to the Great Oxidation Event

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Commensal resilience: ancient ecological lessons for the modern microbiota

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Limited expression of the Paleoproterozoic Oklo natural nuclear reactor phenomenon in the aftermath of a widespread deoxygenation event ~2.11–2.06 billion years ago

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Towards a holistic sulfate-water-O2 triple oxygen isotope systematics

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Precessional pacing of early Proterozoic redox cycles

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Evidence for contemporaneous deposition of the Duitschland and Rooihoogte formations (Transvaal Supergroup): Implications for tempo and mode of Earth’s Great Oxidation

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Oolitic ironstones, continental iron flux and reverse weathering in the Proterozoic Eon: Insights from the Tonian Katherine Group, Yukon

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Mo isotope composition of the 0.85 Ga ocean from coupled carbonate and shale archives: Some implications for pre-Cryogenian oxygenation

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A craton-wide geochemical survey of late Archean banded iron formations in China

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Dynamic redox conditions in Mesoproterozoic shallow seawater: Constraints from carbonate fabrics and geochemistry

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A reassessment of the “hard-steps” model for the evolution of intelligent life

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Marine phosphorus and atmospheric oxygen were coupled during the Great Oxidation Event

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Ecological constraints and evolutionary trade-offs shape nitrogen fixation across habitats

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Sulfur mass-independent fractionation during SO2 photolysis in low-temperature/pressure atmospheres

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Lethal Surface Ozone Concentrations Are Possible on Habitable Zone Exoplanets

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Paleoproterozoic manganese oxide precipitation in oxic seawater surface and reductive enrichment in anoxic seafloor

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The nitrate-limited freshwater environment of the late Paleoproterozoic Embury Lake Formation, Flin Flon belt, Canada

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Timing of Earth’s Oxygenation May Need a 100-Million-Year Revision

Lee, J. K. (2021) · Eos · doi:10.1029/2021eo158543

Earth’s atmosphere took two billion years to become fully oxygenated

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Onset of coupled atmosphere–ocean oxygenation 2.3 billion years ago

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Large-scale fluctuations in Precambrian atmospheric and oceanic oxygen levels from the record of U in shales

Partin, C. A., Bekker, A., Planavsky, N. J., Scott, C. T., Gill, B. C., Li, C., Podkovyrov, V., Maslov, A., Konhauser, K. O., Lalonde, S. V., et al. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.03.031 · Cited by 404 · see citing works

Evidence that the GOE was a prolonged event with a peak around 1900 Ma

Large, R. R., Hazen, R. M., Morrison, S. M., Gregory, D., Steadman, J. A., & Mukherjee, I. (2022) · Geosystems and Geoenvironment · doi:10.1016/j.geogeo.2022.100036 · Cited by 23 · see citing works