Fossil traces of the bone-eating worm Osedax in early Oligocene whale bones

Edited by Robert C. Vrijenhoek, Monterey Bay Aquarium Research Institute, Moss Landing, CA, and accepted by the Editorial Board March 19, 2010 (received for review February 22, 2010)
April 27, 2010
107 (19) 8656-8659

Abstract

Osedax is a recently discovered group of siboglinid annelids that consume bones on the seafloor and whose evolutionary origins have been linked with Cretaceous marine reptiles or to the post-Cretaceous rise of whales. Here we present whale bones from early Oligocene bathyal sediments exposed in Washington State, which show traces similar to those made by Osedax today. The geologic age of these trace fossils (∼30 million years) coincides with the first major radiation of whales, consistent with the hypothesis of an evolutionary link between Osedax and its main food source, although older fossils should certainly be studied. Osedax has been destroying bones for most of the evolutionary history of whales and the possible significance of this “Osedax effect” in relation to the quality and quantity of their fossils is only now recognized.

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Acknowledgments

We thank Eva Vinx (Universität Hamburg) for aid with photography, Bob Vrijenhoek (Monterey Bay Aquarium and Research Institute) for inviting G.W.R. on cruises to collect live Osedax, and Gerardo González-Barba (Universidad Autónoma de Baja California Sur) for identifying fossil shark teeth. We also thank Bob Vrijenhoek and two anonymous reviewers for their efforts to improve the manuscript.

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Information & Authors

Information

Published in

The cover image for PNAS Vol.107; No.19
Proceedings of the National Academy of Sciences
Vol. 107 | No. 19
May 11, 2010
PubMed: 20424110

Classifications

Submission history

Published online: April 27, 2010
Published in issue: May 11, 2010

Keywords

  1. annelids
  2. deep sea
  3. fossil record
  4. symbiosis

Acknowledgments

We thank Eva Vinx (Universität Hamburg) for aid with photography, Bob Vrijenhoek (Monterey Bay Aquarium and Research Institute) for inviting G.W.R. on cruises to collect live Osedax, and Gerardo González-Barba (Universidad Autónoma de Baja California Sur) for identifying fossil shark teeth. We also thank Bob Vrijenhoek and two anonymous reviewers for their efforts to improve the manuscript.

Notes

This article is a PNAS Direct Submission. R.C.V. is a guest editor invited by the Editorial Board.

Authors

Affiliations

Steffen Kiel1 [email protected]
Institut für Geowissenschaften, Christian-Albrechts-Universität, 24118 Kiel, Germany;
James L. Goedert
Burke Museum, University of Washington, Seattle, WA 98195-3010; and
Wolf-Achim Kahl
Institut für Geowissenschaften, Christian-Albrechts-Universität, 24118 Kiel, Germany;
Greg W. Rouse
Scripps Institution of Oceanography, University of California, La Jolla, CA 92093

Notes

1
To whom correspondence should be addressed. E-mail: [email protected].
Author contributions: S.K. designed research; S.K. and J.L.G. performed research; W.-A.K. and G.W.R. analyzed data; and S.K., J.L.G., W.-A.K., and G.W.R. wrote the paper.

Competing Interests

The authors declare no conflict of interest.

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    Fossil traces of the bone-eating worm Osedax in early Oligocene whale bones
    Proceedings of the National Academy of Sciences
    • Vol. 107
    • No. 19
    • pp. 8499-8895

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