1 Melezhik, V. A., Huhma, H., Condon, D. J., Fallick, A. E. & Whitehouse, M. J. Temporal constraints on the Paleoproterozoic Lomagundi-Jatuli carbon isotopic event. Geology 35, 655-658, doi:10.1130/g23764a.1 (2007).
2 Martin, A. P., Condon, D. J., Prave, A. R. & Lepland, A. A review of temporal constraints for the Palaeoproterozoic large, positive carbonate carbon isotope excursion (the Lomagundi–Jatuli Event). Earth-Science Reviews 127, 242-261, doi:https://doi.org/10.1016/j.earscirev.2013.10.006 (2013).
3 Gumsley, A. P. et al. Timing and tempo of the Great Oxidation Event. Proceedings of the National Academy of Sciences 114, 1811, doi:10.1073/pnas.1608824114 (2017).
4 Karhu, J. A. & Holland, H. D. Carbon isotopes and the rise of atmospheric oxygen. Geology 24, 867-870, doi:10.1130/0091-7613(1996)024<0867:ciatro>2.3.co;2 (1996).
5 Holland, H. D. Volcanic gases, black smokers, and the Great Oxidation Event. Geochim Cosmochim Ac 66, 3811-3826, doi:https://doi.org/10.1016/S0016-7037(02)00950-X (2002).
6 Aharon, P. Redox stratification and anoxia of the early Precambrian oceans: Implications for carbon isotope excursions and oxidation events. Precambrian Res 137, 207-222, doi:https://doi.org/10.1016/j.precamres.2005.03.008 (2005).
7 Bekker, A. & Holland, H. D. Oxygen overshoot and recovery during the early Paleoproterozoic. Earth Planet Sc Lett 317-318, 295-304, doi:https://doi.org/10.1016/j.epsl.2011.12.012 (2012).
8 Hayes, J. M. & Waldbauer, J. R. The carbon cycle and associated redox processes through time. Philosophical Transactions of the Royal Society B: Biological Sciences 361, 931-950, doi:doi:10.1098/rstb.2006.1840 (2006).
9 Planavsky, N. J., Bekker, A., Hofmann, A., Owens, J. D. & Lyons, T. W. Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event. Proceedings of the National Academy of Sciences 109, 18300, doi:10.1073/pnas.1120387109 (2012).
10 Pufahl, P. K. & Hiatt, E. E. Oxygenation of the Earth's atmosphere–ocean system: A review of physical and chemical sedimentologic responses. Mar Petrol Geol 32, 1-20, doi:https://doi.org/10.1016/j.marpetgeo.2011.12.002 (2012).
11 Lyons, T. W., Reinhard, C. T. & Planavsky, N. J. The rise of oxygen in Earth’s early ocean and atmosphere. Nature 506, 307-315, doi:10.1038/nature13068 (2014).
12 Canfield, D. E. et al. Oxygen dynamics in the aftermath of the Great Oxidation of Earth’s atmosphere. Proceedings of the National Academy of Sciences 110, 16736, doi:10.1073/pnas.1315570110 (2013).
13 Shields, G. A. & Mills, B. J. W. Tectonic controls on the long-term carbon isotope mass balance. Proceedings of the National Academy of Sciences 114, 4318, doi:10.1073/pnas.1614506114 (2017).
14 Daines, S. J., Mills, B. J. W. & Lenton, T. M. Atmospheric oxygen regulation at low Proterozoic levels by incomplete oxidative weathering of sedimentary organic carbon. Nat Commun 8, 14379, doi:10.1038/ncomms14379 (2017).
15 Bellefroid, E. J. et al. Constraints on Paleoproterozoic atmospheric oxygen levels. Proceedings of the National Academy of Sciences 115, 8104, doi:10.1073/pnas.1806216115 (2018).
16 Miyazaki, Y., Planavsky, N. J., Bolton, E. W. & Reinhard, C. T. Making sense of massive carbon isotope excursions with an inverse carbon cycle model. Journal of Geophysical Res.: Biogeoscience 123, 2485-2496, doi:10.1029/2018jg004416 (2018).
17 Hodgskiss, M. S. W., Crockford, P. W., Peng, Y., Wing, B. A. & Horner, T. J. A productivity collapse to end Earth’s Great Oxidation. Proceedings of the National Academy of Sciences 116, 17207, doi:10.1073/pnas.1900325116 (2019).
18 Préat, A. et al. Paleoproterozoic high δ13C dolomites from the Lastoursville and Franceville basins (SE Gabon): Stratigraphic and synsedimentary subsidence implications. Precambrian Res 189, 212-228, doi:https://doi.org/10.1016/j.precamres.2011.05.013 (2011).
19 Ossa Ossa, F. et al. Two-step deoxygenation at the end of the Paleoproterozoic Lomagundi Event. Earth Planet Sc Lett 486, 70-83, doi:https://doi.org/10.1016/j.epsl.2018.01.009 (2018).
20 Bakakas Mayika, K. et al. The Paleoproterozoic Francevillian succession of Gabon and the Lomagundi-Jatuli event. Geology, doi:10.1130/g47651.1 (2020).
21 Galimov, E. M., Kuznetsova, N. G. & Prokhorov, V. S. On the problem of the Earth’s ancient atmosphere composition in connection with results of isotope analysis of carbon from the Precambrian carbonates. Geokhimiya 11, 1376-1381 (1968).
22 Yudovich, Y. E., Makarikhin, V. V., Medvedev, P. V. & Sukhanov, N. V. Carbon isotope anomalies in carbonates of Karelian Complex. Geokhimiya 7, 792-798 (1980).
23 Karhu, J. A. Paleoproterozoic evolution of the carbon isotope ratios of sedimentary carbonates in the Fennoscandian Shield. Geol. Surv. Finland Bull. 371, 1-87 (1993).
24 Tikhomirova, M. & Makarikhin, V. V. Possible reasons for the δ13C anomaly of Lower Proterozoic sedimentary carbonates. Terra Nova 5, 244-248, doi:10.1111/j.1365-3121.1993.tb00255.x (1993).
25 Melezhik, V. A., Fallick, A. E., Medvedev, P. V. & Makarikhin, V. V. Extreme 13Ccarb enrichment in ca. 2.0 Ga magnesite–stromatolite–dolomite–`red beds' association in a global context: a case for the world-wide signal enhanced by a local environment. Earth-Science Reviews 48, 71-120, doi:https://doi.org/10.1016/S0012-8252(99)00044-6 (1999).
26 Brasier, A. T., Fallick, A. E., Prave, A. R., Melezhik, V. A. & Lepland, A. Coastal sabkha dolomites and calcitised sulphates preserving the Lomagundi-Jatuli carbon isotope signal. Precambrian Res 189, 193-211, doi:https://doi.org/10.1016/j.precamres.2011.05.011 (2011).
27 Melezhik, V. et al. Reading the Archive of Earth’s Oxygenation, Volume 2: The Core Archive of the Fennoscandian Arctic Russia - Drilling Early Earth Project. (Springer, 2013).
28 Scott, C. et al. Pyrite multiple-sulfur isotope evidence for rapid expansion and contraction of the early Paleoproterozoic seawater sulfate reservoir. Earth Planet Sc Lett 389, 95-104, doi:https://doi.org/10.1016/j.epsl.2013.12.010 (2014).
29 Swart, P. K. Global synchronous changes in the carbon isotopic composition of carbonate sediments unrelated to changes in the global carbon cycle. Proceedings of the National Academy of Sciences 105, 13741, doi:10.1073/pnas.0802841105 (2008).
30 Geyman, E. C. & Maloof, A. C. A diurnal carbon engine explains 13C-enriched carbonates without increasing the global production of oxygen. Proceedings of the National Academy of Sciences 116, 24433, doi:10.1073/pnas.1908783116 (2019).
31 Stiller, M., Rounick, J. S. & Shasha, S. Extreme carbon-isotope enrichments in evaporating brines. Nature 316, 434-435, doi:10.1038/316434a0 (1985).
32 Shields, G. & Veizer, J. Precambrian marine carbonate isotope database: Version 1.1. Geochemistry, Geophysics, Geosystems 3, 1 of 12-12 of 12, doi:10.1029/2001gc000266 (2002).
33 Črne, A. E. et al. Petrography and geochemistry of carbonate rocks of the Paleoproterozoic Zaonega Formation, Russia: Documentation of 13C-depleted non-primary calcite. Precambrian Res 240, 79-93, doi:https://doi.org/10.1016/j.precamres.2013.10.005 (2014).
34 Kreitsmann, T. et al. Hydrothermal dedolomitisation of carbonate rocks of the Paleoproterozoic Zaonega Formation, NW Russia - Implications for the preservation of primary C isotope signals. Chem Geol 512, 43-57, doi:10.1016/j.chemgeo.2019.03.002 (2019).