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Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry

Abstract

The evolution of the Earth’s atmosphere is marked by a transition from an early atmosphere with very low oxygen content to one with an oxygen content within a few per cent of the present atmospheric level. Placing time constraints on this transition is of interest because it identifies the time when oxidative weathering became efficient, when ocean chemistry was transformed by delivery of oxygen and sulphate, and when a large part of Earth’s ecology changed from anaerobic to aerobic1. The observation of non-mass-dependent sulphur isotope ratios in sedimentary rocks more than 2.45 billion years (2.45 Gyr) old and the disappearance of this signal in younger sediments is taken as one of the strongest lines of evidence for the transition from an anoxic to an oxic atmosphere around 2.45 Gyr ago1,2,3,4,5. Detailed examination of the sulphur isotope record before 2.45 Gyr ago also reveals early and late periods of large amplitude non-mass-dependent signals bracketing an intervening period when the signal was attenuated5,6,7,8,9. Until recently, this record has been too sparse to allow interpretation, but collection of new data has prompted some workers8 to argue that the Mesoarchaean interval (3.2–2.8 Gyr ago) lacks a non-mass-dependent signal, and records the effects of earlier and possibly permanent oxygenation of the Earth’s atmosphere. Here we focus on the Mesoarchaean interval, and demonstrate preservation of a non-mass-dependent signal that differs from that of preceding and following periods in the Archaean. Our findings point to the persistence of an anoxic early atmosphere, and identify variability within the isotope record that suggests changes in pre-2.45-Gyr-ago atmospheric pathways for non-mass-dependent chemistry and in the ultraviolet transparency of an evolving early atmosphere.

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Figure 1: Compilation of Δ 33 S versus age for rock samples.
Figure 2: Plot of Δ 33 S versus δ 34 S that illustrates the fields defined by pre- and post-2.45-Gyr-ago samples.
Figure 3: Plot of Δ 36 S versus Δ 33 S for mass-dependent and mass-independent data.

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Acknowledgements

This study was supported by funds from the NSF EAR, NASA NAI and NASA EXB progammes (to J.F.), and revisions were undertaken while J.F. was supported by a visiting appointment at the IPG of Paris. Other support for this work came from NSF (A.J.K.) and the DFG (H.S.). The manuscript was improved by reviews and comments from P. Knauth and H. Ohmoto. P. Cartigny is thanked for reading and commenting on the manuscript.

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Correspondence to James Farquhar.

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Farquhar, J., Peters, M., Johnston, D. et al. Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry. Nature 449, 706–709 (2007). https://doi.org/10.1038/nature06202

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