The Cambrian evolution of burrowing species is thought to have facilitated sediment mixing. However, sediment fabrics suggest that bioturbation remained insignificant until the appearance of more efficient sediment mixers in the Silurian.
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References
Tarhan, L., Droser, M. L., Planavsky, N. J. & Johnston, D. T. Nature Geosci. 8, 865–869 (2015).
Canfield, D. & Farquhar, J. Proc. Natl Acad. Sci. USA 106, 8123–8127 (2009).
Boyle, R. et al. Nature Geosci. 7, 671–676 (2014).
Seilacher, A. Palaios 14, 86–93 (1999).
Harazim, D., Callow, R. & McIlroy, D. Sedimentology 60, 1621–1638 (2013).
Mangano, M. G. & Buatois, L. A. Proc. R. Soc. B 281, 20140038 (2014).
Bottjer, D., Hagadorn, J. & Dornbos, S. GSA Today 10, 1–7 (2000).
Gingras, M. et al. Nature Geosci. 4, 372–375 (2011).
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Gingras, M., Konhauser, K. Digging deeper. Nature Geosci 8, 825–826 (2015). https://doi.org/10.1038/ngeo2548
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DOI: https://doi.org/10.1038/ngeo2548