Karhu, J. A. & Holland, H. D. Carbon isotopes and the rise of atmospheric oxygen. Geology 24, 867–870 (1996).
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-Sci. Rev. 127, 242–261 (2013).
Bekker, A. & Holland, H. D. Oxygen overshoot and recovery during the early Paleoproterozoic. Earth Planet. Sci. Lett. 317–318, 295–304 (2012).
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. Proc. Natl Acad. Sci. USA 109, 18300–18305 (2012).
Scott, C. et al. Pyrite multiple-sulfur isotope evidence for rapid expansion and contraction of the early Paleoproterozoic seawater sulfate reservoir. Earth Planet. Sci. Lett. 389, 95–104 (2014).
Blättler, C. L. et al. Two-billion-year-old evaporites capture Earth’s great oxidation. Science 360, 320–323 (2018).
Konhauser, K. O. et al. Aerobic bacterial pyrite oxidation and acid rock drainage during the Great Oxidation Event. Nature 478, 369–373 (2011).
Partin, C. A. et al. Large-scale fluctuations in Precambrian atmospheric and oceanic oxygen levels from the record of U in shales. Earth Planet. Sci. Lett. 369–370, 284–293 (2013).
Kipp, M. A., Stüeken, E. E., Bekker, A. & Buick, R. Selenium isotopes record extensive marine suboxia during the Great Oxidation Event. Proc. Natl Acad. Sci. USA 114, 875–880 (2017).
Sheen, A. I. et al. A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia. Geochim. Cosmochim. Acta 227, 75–95 (2018).
Canfield, D. E. et al. Oxygen dynamics in the aftermath of the Great Oxidation of Earth’s atmosphere. Proc. Natl Acad. Sci. USA 110, 16736–16741 (2013).
Bachan, A. & Kump, L. R. The rise of oxygen and siderite oxidation during the Lomagundi Event. Proc. Natl Acad. Sci. USA 112, 6562–6567 (2015).
Miyazaki, Y., Planavsky, N., Bolton, E. W. & Reinhard, C. T. Making sense of massive carbon isotope excursions with an inverse carbon cycle model. J. Geophys. Res. Biogeosci. 123, 2485–2496 (2018).
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-Sci. Rev. 48, 71–120 (1999).
Eguchi, J., Seales, J. & Dasgupta, R. Great Oxidation and Lomagundi events linked by deep cycling and enhanced degassing of carbon. Nat. Geosci. 13, 71–76 (2020).
Martin, A. P. et al. Multiple Palaeoproterozoic carbon burial episodes and excursions. Earth Planet. Sci. Lett. 424, 226–236 (2015).
Melezhik, V. A., Fallick, A. E., Brasier, A. T. & Lepland, A. Carbonate deposition in the Palaeoproterozoic Onega basin from Fennoscandia: a spotlight on the transition from the Lomagundi–Jatuli to Shunga events. Earth Sci. Rev. 147, 65–98 (2015).
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 (2019).
Sadler, P. M. The influence of hiatuses on sediment accumulation rates. GeoRes. Forum 5, 15–40 (1999).
Böning, P. et al. Geochemistry of Peruvian near-surface sediments. Geochim. Cosmochim. Acta 68, 4429–4451 (2004).
Reinhard, C. T. et al. Proterozoic ocean redox and biogeochemical stasis. Proc. Natl Acad. Sci. USA 110, 5357–5362 (2013).
Wang, X. et al. A Mesoarchean shift in uranium isotope systematics. Geochim. Cosmochim. Acta 238, 438–452 (2018).
Yang, S., Kendall, B., Lu, X., Zhang, F. & Zheng, W. Uranium isotope compositions of mid-Proterozoic black shales: evidence for an episode of increased ocean oxygenation at 1.36 Ga and evaluation of the effect of post-depositional hydrothermal fluid flow. Precambrian Res. 298, 187–201 (2017).
Dunk, R. M., Mills, R. A. & Jenkins, W. J. A reevaluation of the oceanic uranium budget for the Holocene. Chem. Geol. 190, 45–67 (2002).
Miller, C. A., Peucker-Ehrenbrink, B., Walker, B. D. & Marcantonio, F. Re-assessing the surface cycling of molybdenum and rhenium. Geochim. Cosmochim. Acta 75, 7146–7179 (2011).
Crusius, J., Calvert, S., Pedersen, T. & Sage, D. Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition. Earth Planet. Sci. Lett. 145, 65–78 (1996).
Anderson, R. F., Fleisher, M. Q. & LeHuray, A. P. Concentration, oxidation state, and particulate flux of uranium in the Black Sea. Geochim. Cosmochim. Acta 53, 2215–2224 (1989).
Algeo, T. J. & Lyons, T. W. Mo–total organic carbon covariation in modern anoxic marine environments: implications for analysis of paleoredox and paleohydrographic conditions. Paleoceanography 21, PA1016 (2006).
Helz, G. R. et al. Mechanism of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence. Geochim. Cosmochim. Acta 60, 3631–3642 (1996).
Kendall, B., Dahl, T. W. & Anbar, A. D. The stable isotope geochemistry of molybdenum. Rev. Mineral. Geochem. 82, 683–732 (2017).
Andersen, M. B., Stirling, C. H. & Weyer, S. Uranium isotope fractionation. Rev. Mineral. Geochem. 82, 799–850 (2017).
Dickson, A. J. A molybdenum-isotope perspective on Phanerozoic deoxygenation events. Nat. Geosci. 10, 721–726 (2017).
Tribovillard, N., Algeo, T. J., Lyons, T. & Riboulleau, A. Trace metals as paleoredox and paleoproductivity proxies: an update. Chem. Geol. 232, 12–32 (2006).
Och, L. M. & Shields-Zhou, G. A. The Neoproterozoic oxygenation event: environmental perturbations and biogeochemical cycling. Earth-Sci. Rev. 110, 26–57 (2012).
Föllmi, K. B. et al. Phosphogenesis and organic-carbon preservation in the Miocene Monterey Formation at Naples Beach, California—the Monterey hypothesis revisited. Bull. Geol. Soc. Am. 117, 589–619 (2005).
Andersen, M. B. et al. A modern framework for the interpretation of 238U/235U in studies of ancient ocean redox. Earth Planet. Sci. Lett. 400, 184–194 (2014).
Barnes, C. E. & Cochran, J. K. Uranium geochemistry in estuarine sediments: controls on removal and release processes. Geochim. Cosmochim. Acta 57, 555–569 (1993).
Kump, L. R. et al. Isotopic evidence for massive oxidation of organic matter following the Great Oxidation Event. Science 334, 1694–1696 (2011).
Qu, Y., Črne, A. E., Lepland, A. & van Zuilen, M. A. Methanotrophy in a Paleoproterozoic oil field ecosystem, Zaonega Formation, Karelia, Russia. Geobiology 10, 467–478 (2012).
Paiste, K. et al. Multiple sulphur isotope records tracking basinal and global processes in the 1.98 Ga Zaonega Formation, NW Russia. Chem. Geol. 499, 151–164 (2018).
Asael, D. et al. Coupled molybdenum, iron and uranium stable isotopes as oceanic paleoredox proxies during the Paleoproterozoic Shunga Event. Chem. Geol. 362, 193–210 (2013).
Asael, D., Rouxel, O., Poulton, S. W., Lyons, T. W. & Bekker, A. Molybdenum record from black shales indicates oscillating atmospheric oxygen levels in the early Paleoproterozoic. Am. J. Sci. 318, 275–299 (2018).
Brocks, J. J. et al. The rise of algae in Cryogenian oceans and the emergence of animals. Nature 548, 578–581 (2017).
Lepland, A. et al. Potential influence of sulphur bacteria on Palaeoproterozoic phosphogenesis. Nat. Geosci. 7, 20–24 (2014).
Parfrey, L. W., Lahr, D. J. G., Knoll, A. H. & Katz, L. A. Estimating the timing of early eukaryotic diversification with multigene molecular clocks. Proc. Natl Acad. Sci. USA 108, 13624–13629 (2011).
Betts, H. C. et al. Integrated genomic and fossil evidence illuminates life’s early evolution and eukaryote origin. Nat. Ecol. Evol. 2, 1556 (2018).
Kasting, J. F. & Canfield, D. E. in Fundamentals of Geobiology (eds Knoll, A. H., Canfield, D. E. & Konhauser, K. O.) 93–104 (John Wiley & Sons, 2012).
McLennan, S. M. Relationships between the trace element composition of sedimentary rocks and upper continental crust: trace element composition and upper continental crust. Geochem. Geophys. Geosyst. 2, 1021 (2001).
Karhu, J. A. in Encyclopedia of Geochemistry (eds Marshall, C. P. & Fairbridge, R. W.) 67–73 (Kluwer Academic Publishers, 1999).
Robbins, L. J. et al. Trace elements at the intersection of marine biological and geochemical evolution. Earth-Sci. Rev. 163, 323–348 (2016).
Melezhik, V. A., Fallick, A. E., Filippov, M. M. & Larsen, O. Karelian shungite—an indication of 2.0-Ga-old metamorphosed oil-shale and generation of petroleum: geology, lithology and geochemistry. Earth-Sci. Rev. 47, 1–40 (1999).
Paiste, K. Reconstructing the Paleoproterozoic Sulfur Cycle: Insights from the Multiple Sulfur Isotope Record of the Zaonega Formation, Karelia, Russia. PhD thesis, Univ. Tromsø (2018).
Siebert, C., Nägler, T. F. & Kramers, J. D. Determination of molybdenum isotope fractionation by double-spike multicollector inductively coupled plasma mass spectrometry. Geochem. Geophys. Geosyst. 2, 1032 (2001).
Nägler, T. F. et al. Proposal for an international molybdenum isotope measurement standard and data representation. Geostand. Geoanal. Res. 38, 149–151 (2014).
Mänd, K. et al. Trace Metal Concentrations and Isotope Compositions from Drill Core OnZaP of the Zaonega Formation, NW-Russia (PANGAEA, 2020); https://doi.org/10.1594/PANGAEA.911670
Mänd, K. et al. Trace Metal Concentrations and Isotope Compositions from Drill Core OPH of the Zaonega Formation, NW-Russia (PANGAEA, 2020); https://doi.org/10.1594/PANGAEA.911674
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