A widespread biotic turnover occurred around the time of the Sturtian glaciation. Microfossil analyses show that one regional extinction pre-dates the glacial advance, challenging the more severe models for glacial effects in the Neoproterozoic era.
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References
Nagy, R. M., Porter, S. M., Dehler, C. M. & Shen, Y. Nature Geosci. 2, 415–418 (2009).
Knoll, A. H., Blick, N. & Awramik, S. M. Am. J. Sci. 281, 247–263 (1981).
Moczydłowska, M. Precambrian Res. 167, 1–15 (2008).
Corsetti, F. A., Awramik, S. M. & Pierce, D. Proc. Natl Acad. Sci. USA 100, 4399–4404 (2003).
Olcott, A., Sessions, A., Corsetti, F. A., Kaufman, A. J. & de Oliviera, F. Science 310, 5747–5751 (2005).
Love, G. et al. Nature 457, 718–721 (2009).
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Corsetti, F. Extinction before the snowball. Nature Geosci 2, 386–387 (2009). https://doi.org/10.1038/ngeo533
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DOI: https://doi.org/10.1038/ngeo533