The DOI matches its Crossref record; 75 of the 77 references it cites were found in a registry or an index.
Why the atmosphere became oxygenated: A proposal
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“Hypotheses for a slowly decreasing O2 sink to the GOE tipping point rely on a decline in the ratio of reduced-to-oxidized species from volcanic, metamorphic, and hydrothermal sources (9, 123, 124, 133, 134).”
From The Archean atmosphere (2020) · cites this paper as [123]
In the citing paper
“These O2 levels would have only been attained when the O2 flux from the burial of organic carbon exceeded the kinetically efficient sink from O2-consuming gases (CO, H2, H2S, and SO2) from volcanism and metamorphism plus fluxes of reducing cations such as Fe2+ from seafloor vents (9, 120, 121, 123, 124).”
From The Archean atmosphere (2020) · cites this paper as [123]
In the citing paper
“Higher inputs of reductant relative to today—either due to higher mantle fluxes52, ongoing crustal oxidation during metamorphism hence more reduced metamorphic fluxes40 or greater submarine volcanism resulting in more reduced volatiles53—would affect the stability of an oxygen-sink-controlled feedback regime.”
From Atmospheric oxygen regulation at low Proterozoic levels by incomplete oxidative weathering of sedimentary organic carbon (2017) · cites this paper as [52]
Citations
Cites
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The Chemical Evolution of the Atmosphere and Oceans
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Self-citationAtmospheric Influence of Earth's Earliest Sulfur Cycle
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The snowball Earth hypothesis: testing the limits of global change
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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
Self-citationThe chemistry of the atmosphere and oceans
Sibley, D. F. (1979) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(79)90059-0 · Cited by 1,141
(1978) · Medical Entomology and Zoology · Cited by 1,073
Self-citationTHE EARLY HISTORY OF ATMOSPHERIC OXYGEN: Homage to Robert M. Garrels
Canfield, D. E. (2005) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.33.092203.122711 · Cited by 1,032
Volcanic gases, black smokers, and the great oxidation event
Holland, H. D. (2002) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(02)00950-x · Cited by 920
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2 of the 77 references couldn’t be matched to a known paper.
Research works printed but not linked: 7
- Bekker, 2003, Fe2O3/FeO ratio in average shale through time: a reflection on the stepwise oxidation of the atmosphere, Geol. Soc. Am., 34, 83
- Holland, 1990, A paleoweathering profile from Griqualand, South Africa: evidence for a dramatic rise in atmospheric oxygen between 2.2 and 1.9 BYBP, Am. J. Sci., 290A, 1
- Porcelli D., Turekian K. K. (2004) The history of planetary degassing as recorded by noble gases, chapter 4.11. In The Treatise on Geochemistry, vol. 4 (eds. R. F. Keeling (Volume), H. D. Holland and K. K. Turekian (Exec.)). Elsevier Pergamon, Amsterdam, pp. 281–318.
- Rye, 2000, Life associated with a 2.76 Ga ephemeral pond?, Geology, 28, 483, 10.1130/0091-7613(2000)28<483:LAWAGE>2.0.CO;2 · DOI
- Seiler, 1974, Dissolved nonconservative gases in seawater, chapter 7, 219
- Shields, 2007, The marine carbonate and chert isotope records and their implications for tectonics, life, and climate on the early Earth, chapter 7.6, 971
- Veizer J., Mackenzie F. T. (2004) Evolution of sedimentary rocks, chapter 7.15. In Treatise on Geochemistry, vol. 7 (eds. F. T. Mackenzie (volume), H. D. Holland and K. K. Turekian (Exec.)). Elsevier, Amsterdam, pp. 369–407.
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Items 101–191 of 191
Crustal carbonate build-up as a driver for Earth’s oxygenation
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“This mechanism has been hypothesized to promote oxygenation 22,37 , and previous modelling implied a trend towards oxygenation before the model breaks down 8 , but it has not been included in a coupled model including carbon, nutrients and climate or been tested against combined geological data.”
Eriksson, P. G., Lenhardt, N., Wright, D. T., Mazumder, R., & Bumby, A. J. (2011) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2011.05.007 · Cited by 19
“Late Neoarchaean-Palaeoproterozoic supracrustal basin-fills of the Kaapvaal craton: relevance of the supercontinent cycle, the "Great Oxidation Event" and "Snowball Earth"?”
BackgroundInfluentialWeathering during the Great Oxidation Event: Fennoscandia, arctic Russia 2.06 Ga ago
Rybacki, K. S., Kump, L. R., Hanski, E., & Melezhik, V. A. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.01.010 · Cited by 18
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Modeling the Archean Atmosphere and Climate
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Rosa, D., Leach, D., Guarnieri, P., & Bekker, A. (2022) · Mineralium Deposita · doi:10.1007/s00126-022-01125-z · Cited by 15
“2004, 2020; Holland 2006, 2009; Poulton et al.”
Robinson, T. D. (2005) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816540068-ch015 · Cited by 21
“A number of potential drivers have been suggested for the GOE, including secular tectonic processes (Kump & Barley 2007; Holland 2009; Gaillard et al. 2011), changes in global biological fluxes (Kopp et al. 2005; Konhauser et al. 2009), and time-integrated hydrogen escape from the atmosphere…”
BackgroundHavig, J. R., & Hamilton, T. L. (2019) · Frontiers in Earth Science · doi:10.3389/feart.2019.00015 · Cited by 15
“…oxygen driving oxidative weathering as far back as 3.0 Ga (e.g., Anbar et al., 2007; Kump and Barley, 2007; Wille et al., 2007; Frei et al., 2009; Holland, 2009; Reinhard et al., 2009; FIGURE 1 | Zoom in highlighting pigmented phototrophic microbial community exposed following disturbance of a…”
BackgroundInfluentialEvolution of continental crust and sedimentary rock chemistry through time
Kamber, B. S., & Ossa, F. O. (2023) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00007-3 · Cited by 12
The Evolution of Photosynthesis and Its Environmental Impact
Björn, L. O., & Jee, G. (2007) · Springer eBooks · doi:10.1007/978-0-387-72655-7_12 · Cited by 12
Conditions of subaerial weathering of basalts in the Neoarchean and Paleoproterozoic
Alfimova, N. A., Novoselov, A. A., Matrenichev, V. A., & Filho, C. R. D. S. (2013) · Precambrian Research · doi:10.1016/j.precamres.2013.09.013 · Cited by 12
Early Paleoproterozoic Metallogenic Explosion in North China Craton
Tang, H., Chen, Y., Li, K., Chen, W., Zhu, X., Ling, K., & Sun, X. (2016) · Springer geology · doi:10.1007/978-981-10-1064-4_12 · Cited by 11
Kanzaki, Y., & Murakami, T. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.08.020 · Cited by 10
Formation mechanism and geochemical process of porphyry molybdenum deposits
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Ethics and aims of cosmetic surgery: a contribution from an analysis of claims after minor damage.
Meningaud, J., Servant, J. M., Hervé, C., & Bertrand, J.-C. (2000) · PubMed · Cited by 10
Lajoinie, M. F., Arnol, J. A., Lanfranchini, M. E., Uriz, N. J., Basei, M. Â. S., & Cingolani, C. A. (2024) · Precambrian Research · doi:10.1016/j.precamres.2024.107330 · Cited by 9
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Microbial helpers allow cyanobacteria to thrive in ferruginous waters
Szeinbaum, N., Toporek, Y. J., Reinhard, C. T., & Glass, J. B. (2021) · Geobiology · doi:10.1111/gbi.12443 · Cited by 9
“…of cyanobacterial O2 production and O2 accumulation in the atmosphere may have been modulated by geophysical drivers (Catling et al., 2001; Holland, 2009; Lee et al., 2016), but may also reflect the time required for metabolic innovations to appear in early cyanobacteria or for the…”
BackgroundMantle cooling causes more reducing volcanic gases and gradual reduction of the atmosphere
Kadoya, S., Catling, D. C., Nicklas, R. W., Puchtel, I. S., & Anbar, A. D. (2020) · Geochemical Perspectives Letters · doi:10.7185/geochemlet.2009 · Cited by 10
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Mechanistic Links Between the Sedimentary Redox Cycle and Marine Acid‐Base Chemistry
Reinhard, C. T., & Fischer, W. W. (2019) · Geochemistry Geophysics Geosystems · doi:10.1029/2019gc008621 · Cited by 7
“In a similar fashion, the oxygen (O2) abundance in Earth's atmosphere and the overall redox state of the ocean‐atmosphere system are largely controlled by the flow of electrons through the crust and between the exogenic system (crust‐ocean‐atmosphere) and Earth's interior (Berner & Canfield, 1989; Garrels & Perry, 197…”
Bekker, A. (2014) · Encyclopedia of Astrobiology · doi:10.1007/978-3-642-27833-4_1752-4 · Cited by 8
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Strachan, R. A., Murphy, J. B., Darling, J. R., Storey, C. D., & Shields, G. (2020) · Elsevier eBooks · doi:10.1016/b978-0-12-824360-2.00016-4 · Cited by 7
Discovering the History of Atmospheric Oxygen
Holland, H. D. (2011) · Frontiers in Geochemistry · doi:10.1002/9781444329957.ch3 · Cited by 7
Self-citationShan, E., Xiao, Y., Wang, Y., Tan, D., & Sun, H. (2024) · Precambrian Research · doi:10.1016/j.precamres.2024.107527 · Cited by 6
Zhang, Y., Lai, G., Gong, E., Wilson, M. A., Huang, W., Guan, C., & Yuan, D.-C. (2022) · Palaeoworld · doi:10.1016/j.palwor.2022.06.003 · Cited by 6
Zhang, S., Wang, H., Tang, H., Cai, Y., Kong, L., Pei, J., Zhang, Q., Hu, G., & Zhao, Y. J. (2023) · Terra Nova · doi:10.1111/ter.12687 · Cited by 6
“…2.33– 2.32 Ga (Bekker et al., 2004; Luo et al., 2016; Poulton et al., 2021) is a profound turning point in Earth's history and represents the first significant buildup in Earth's atmospheric oxygen (Canfield, 2005; Holland, 1999, 2002, 2009; Konhauser et al., 2009; Kump, 2008; Lyons et al., 2014).”
BackgroundInfluentialDong, R., Chen, A., Feng, J., Zhang, S., Jiang, W., Hu, X., Wu, Y., Wang, J., Wang, X., & Jiang, Y. (2024) · Physical Review A · doi:10.1103/physreva.110.053110 · Cited by 5
The Atmosphere and Hydrosphere
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Савко, К. А., Кузнецов, А. Б., Ovchinnikova, M. Y., & Kramchaninov, A. Y. (2021) · Doklady Earth Sciences · doi:10.1134/s1028334x21040140 · Cited by 5
Gaillard, F., Scaillet, B., & Arndt, N. (2012) · Nature · doi:10.1038/nature11275 · Cited by 4
Mohanty, S. (2018) · Society of Earth Scientists series · doi:10.1007/978-3-319-89698-4_4 · Cited by 4
Rybacki, K. S., Kump, L. R., Hanski, E., & Melezhik, V. A. (2012) · Frontiers in earth sciences · doi:10.1007/978-3-642-29670-3_4 · Cited by 4
“Today, it is not clear what caused the GOE (Canfield 2005; Catling and Claire 2005; Farquhar et al. 2010; Holland 2009).”
BackgroundRamsay, B., Fralick, P. W., Homann, M., Lalonde, S. V., & Riding, R. (2025) · Precambrian Research · doi:10.1016/j.precamres.2025.107886 · Cited by 3
Goswami, A., Mohanty, S., Sarangi, S., Das, S., Mohanty, D., & Barik, A. (2025) · International Journal of Earth Sciences · doi:10.1007/s00531-025-02538-7 · Cited by 3
“…around 2450 Ma, tracked in multiple phases (Lyons et al. 2014), was followed by a second step of oxygenated atmosphere, towards the beginning of the Neoproterozoic (Durrheim and Mooney 1994; Pavlov and Kasting 2002; Holland 2002, 2004, 2006, 2009; Can-field 2005; Narbonne 2010; Doyle et al. 2018).”
Time Between 3 and 2 Ga: Transitional Events in the Earth’s History
Yarmolyuk, V. V., Kuzmin, M. I., Donskaya, Т. V., Gladkochub, D. P., & Kotov, A. B. (2021) · Russian Geology and Geophysics · doi:10.2113/rgg20204226 · Cited by 3
Section 2. Classification of Natural Resources
Sverdrup, H. U., & Ragnarsdottir, K. V. (2014) · Geochemical Perspectives · Cited by 3
Varentsov, I. M., & Kuleshov, V. N. (2019) · Lithology and Mineral Resources · doi:10.1134/s0024490219050067 · Cited by 3
“Contents of manganese and iron oxides in the studied samples ref lect the intensity of supergene alterations of the primary Mn-carbonates and testify to changes of the oxygen content in the Proterozoic atmosphere (Holland, 1984, 2002, 2006, 2009).”
BackgroundWhite, W. M. (2017) · Kirk-Othmer Encyclopedia of Chemical Technology · doi:10.1002/0471238961.koe00029 · Cited by 3
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“Such an increase in oxygen levels during the Neoproterozoic is well documented in the chemostrati-graphic record (Logan et al., 1995; Canfield, 2005; Fike et al., 2006; Holland, 2006, 2009; Canfield et al., 2008; Scott et al., 2008; Och & Shields-Zhou, 2012; Partin et al., 2013).”
A New Progress of the Proterozoic Chronostratigraphical Division
Ming-xiang, M., & Khaing, K. K. (2016) · Acta Geologica Sinica - English Edition · doi:10.1111/1755-6724.12764 · Cited by 2
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Dong, R., Chen, A., Zhang, Y., Feng, J., Ma, H., Liu, T., Shen, Y., Jiang, J., Shen, Z., Hu, X., et al. (2026) · The Journal of Chemical Physics · doi:10.1063/5.0322986 · Cited by 1
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Metadata
- Authors
- Holland, H. D.
- Affiliations
- University of Pennsylvania (US)
- Corresponding author
- Holland, Heinrich D.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 2009-09
- Volume
- 73
- Issue
- 18
- Pages
- 5241-5255
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2081154678
- Cited by
- 191
- References
- 77
- Citations by year
- 2026: 8 · 2025: 5 · 2024: 10 · 2023: 6 · 2022: 6 · 2021: 14 · 2020: 10 · 2019: 12 · 2018: 9 · 2017: 12 · 2016: 11 · 2015: 15 · 2014: 14 · 2013: 22 · 2012: 17
- FWCI
- 8.88
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Funders
- Hebrew University of Jerusalem
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Environmental Science › Global and Planetary Change › Earth Systems and Cosmic Evolution
- Keywords
- atmospheric oxygenation, atmospheric evolution, volcanic gases, CO2/H2O ratio, degassing, CO2 recycling, sulfur dioxide, photosynthesis, Earth history
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Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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