Skip to main content
Log in

Sedimentology

Digging deeper

  • News & Views
  • Published:

From Nature Geoscience

View current issue Submit your manuscript

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.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1: Burrows and oxygen.

MURRAY GINGRAS

References

  1. Tarhan, L., Droser, M. L., Planavsky, N. J. & Johnston, D. T. Nature Geosci. 8, 865–869 (2015).

    Article  Google Scholar 

  2. Canfield, D. & Farquhar, J. Proc. Natl Acad. Sci. USA 106, 8123–8127 (2009).

    Article  Google Scholar 

  3. Boyle, R. et al. Nature Geosci. 7, 671–676 (2014).

    Article  Google Scholar 

  4. Seilacher, A. Palaios 14, 86–93 (1999).

    Article  Google Scholar 

  5. Harazim, D., Callow, R. & McIlroy, D. Sedimentology 60, 1621–1638 (2013).

    Article  Google Scholar 

  6. Mangano, M. G. & Buatois, L. A. Proc. R. Soc. B 281, 20140038 (2014).

    Article  Google Scholar 

  7. Bottjer, D., Hagadorn, J. & Dornbos, S. GSA Today 10, 1–7 (2000).

    Google Scholar 

  8. Gingras, M. et al. Nature Geosci. 4, 372–375 (2011).

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Murray Gingras.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Gingras, M., Konhauser, K. Digging deeper. Nature Geosci 8, 825–826 (2015). https://doi.org/10.1038/ngeo2548

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo2548

  • Springer Nature Limited

Navigation