A bistable organic-rich atmosphere on the Neoarchaean Earth

Atmospheric Influence of Earth's Earliest Sulfur Cycle

Farquhar, J., Bao, H., & Thiemens, M. (2000) · Science · doi:10.1126/science.289.5480.756 · Cited by 1,805

The oxygenation of the atmosphere and oceans

Holland, H. D. (2006) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2006.1838 · Cited by 1,535

A Whiff of Oxygen Before the Great Oxidation Event?

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Ferruginous conditions: a dominant feature of the ocean through Earth's history

Poulton, S. W., & Canfield, D. E. (2011) · Elements · doi:10.2113/gselements.7.2.107 · Cited by 1,018

Mass-Independent Fractionation of Sulfur Isotopes in Archean Sediments: Strong Evidence for an Anoxic Archean Atmosphere

Pavlov, A. A., & Kasting, J. F. (2002) · Astrobiology · doi:10.1089/153110702753621321 · Cited by 912

Evolution of the Solar Activity over Time and Effects on Planetary Atmospheres. I. High‐Energy Irradiances (1–1700 A)

Ribas, I., Guinan, E. F., Güdel, M., & Audard, M. (2005) · The Astrophysical Journal · doi:10.1086/427977 · Cited by 871

Calibration of Sulfate Levels in the Archean Ocean

Gao, X., Thiemens, M. H., Farquhar, J. D., Jackson, T. L., Savarino, J., Airieau, S., Albarède, F., van der Hilst, R. D., & Kárason, H. (2002) · Cited by 607

The low-temperature geochemical cycle of iron: From continental fluxes to marine sediment deposition

Poulton, S. W. (2002) · American Journal of Science · doi:10.2475/ajs.302.9.774 · Cited by 556

Observation of wavelength‐sensitive mass‐independent sulfur isotope effects during SO2 photolysis: Implications for the early atmosphere

Farquhar, J., Savarino, J., Airieau, S., & Thiemens, M. H. (2001) · Journal of Geophysical Research: Planets · doi:10.1029/2000je001437 · Cited by 518

Biogenic Methane, Hydrogen Escape, and the Irreversible Oxidation of Early Earth

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Mass-independent fractionation processes in the atmosphere

Hemingway, J., & Claire, M. W. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00084-x · Cited by 2

Atmospheric oxygen and methane on the early Earth

Kasting, J. F., & Ji, A. (2025) · Philosophical Transactions of the Royal Society B Biological Sciences · doi:10.1098/rstb.2024.0093 · Cited by 3

Origin of Paleoarchean Sulfate Deposits

Philippot, P., Muller, É., & Rollion‐Bard, C. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00010-1 · Cited by 2

Climate Evolution on the Geological Timescale and the Role of Paleogeographic Changes

Fluteau, F., & Sepulchre, P. (2020) · Frontiers in earth sciences · doi:10.1007/978-3-030-24982-3_22 · Cited by 2

The atmosphere and hydrosphere

Condie, K. C. (2021) · Elsevier eBooks · doi:10.1016/b978-0-12-819914-5.00006-8 · Cited by 2

Origins of Archean organic matter

Alléon, J., & Summons, R. E. (2025) · Elsevier eBooks · doi:10.1016/b978-0-323-95547-8.00033-1 · Cited by 1

Organonitrogen and Organosulfur Compounds in Archean-Analogue Hazes: Impact of CO 2 on Chemical Composition

Christensen, C. M., Reed, N. W., Wing, B. A., McGlynn, S. E., Tolbert, M. A., Browne, E. C., & Surratt, J. D. (2026) · ACS Earth and Space Chemistry · doi:10.1021/acsearthspacechem.5c00366 · Cited by 1

Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments?

Swain, A., Kaufman, A. J., Kalinowski, M., Yarwood, S. A., & Fagan, W. F. (2020) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.118900 · Cited by 1

Archean methane cycling and life's coevolution: intertwining early biogeochemical processes and ancient microbial metabolism

Ebadirad, S., Lyons, T. W., & Fournier, G. P. (2025) · Elsevier eBooks · doi:10.1016/b978-0-323-95547-8.00030-6 · Cited by 3

Photochemistry and haze in chemically reducing terrestrial atmospheres

Gu, L., & Fan, S. (2026) · Fundamental Research · doi:10.1016/j.fmre.2026.04.008 · Cited by 1

Improving the reliability of carbonate-associated sulfate extraction through optimized pre-leaching methods

Tian, Z., Shields, G., & Zhou, Y. (2026) · Applied Geochemistry · doi:10.1016/j.apgeochem.2026.107005 · Cited by 1

Atmospheric Biosignatures

Grenfell, J. L. (2018) · Springer eBooks · doi:10.1007/978-3-319-55333-7_68 · Cited by 1

Phosphorus Cycling under different redox conditions

Xiong, Y. (2018) · White Rose eTheses Online (University of Leeds, The University of Sheffield, University of York) · Cited by 1

Composition des isotopes stables du molybdène dans les carbonates du Précambrien : affinement du proxy et applications paléo-environnementales

Thoby, M. (2018) · theses.fr (ABES) · doi:10.70675/c78aad7dza1d6z46f7z9a74zf411ae3d4b16 · Cited by 1

How low can you go? Maximum constraints on hydrogen concentrations prior to the Great Oxidation Event

Domagal-Goldman, S. D. (2014) · Geological Society of America eBooks · doi:10.1130/2014.2504(02

Volcanic Influence on Atmospheric Sulfur Cycle in 2.7 Ga inferred from Multiple Sulfur Isotope Record of Pyrite Nodules in Black Shales from Nimbus, Western Australia

Zhang, Z. (2018) · ERA: Education and Research Archive (University of Alberta) · doi:10.7939/r3gm82402

Laboratory Studies of Planetary Atmospheres and Organic Hazes

Ugelow, M. S. (2018) · CU Scholar (University of Colorado Boulder)

Interpretación formalista y desproporcionada del agotamiento de la vía administrativa

Bernal, M. T. G. (1994) · Civitas. Revista española de derecho del trabajo/Revista española de derecho del trabajo

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HWO Target Stars and Systems: A Survey of Archival UV and X-Ray Data

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Additional file 1 of Atmospheric oxygenation of the early earth and earth-like planets driven by competition between land and seafloor weathering

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Geobiological significance and identification methods of different types of pyrites

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Aerosols-plasma interaction in Titan’s ionosphere

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Redox State of the Neoarchean Earth Environment

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Multiple oscillations in Neoarchaean atmospheric chemistry

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The Impact of Molecular Oxygen on Anion Composition in a Hazy Archean Earth Atmosphere

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Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments?

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