Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Effect of nutrient availability on marine origination rates throughout the Phanerozoic eon

Abstract

Throughout the Phanerozoic eon (542 Myr ago to the present), the diversity of marine organisms has varied. These changes are fairly well resolved1, but the controls on origination and diversification are less well understood. Changes in origination rates are thought to arise from a complex interplay between biological forces such as competition and predation2, phytoplankton stoichiometry3 and bioturbation3 and abiotic controls such as environmental setting4, temperature5,6, sea level7 and nutrient availability8. Here we statistically assess relationships between records of environmental conditions9,10,11,12,13,14 and global marine origination rates2 during the Phanerozoic. We find significant positive correlations between changes in origination rates and variations in indicators of continental weathering (87Sr/86Sr) and phosphorus recycling (δ34S), as well as a significant negative correlation between variability in origination rates and eustatic sea level. We suggest that continental weathering, phosphorus recycling and sea level—through the exposure of the continental shelf area to erosion—are all controls on the availability of marine nutrients. We therefore propose that over secular timescales, nutrient availability, as controlled by continental weathering and phosphorus recycling, is an important regulator of genus-level origination in the marine realm, with periods of increased nutrient availability associated with higher origination rates.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Figure 1: Time series used in the analyses.
Figure 2: Relationships obtained between changes in both Phanerozoic marine invertebrate origination dynamics and environmental constraints.

Similar content being viewed by others

References

  1. Alroy, J. et al. Phanerozoic trends in the global diversity of marine invertebrates. Science 321, 97–100 (2008).

    Article  Google Scholar 

  2. Alroy, J. Dynamics of origination and extinction in the marine fossil record. Proc. Natl Acad. Sci. USA 105, 11536–11542 (2008).

    Article  Google Scholar 

  3. Martin, R. E., Quigg, A. & Podkovyrov, V. Marine biodiversification in response to evolving phytoplankton stoichiometry. Palaeogeogr. Palaeoclimatol. Palaeoecol. 258, 277–291 (2008).

    Article  Google Scholar 

  4. Kiessling, W., Simpson, C. & Foote, M. Reefs as cradles of evolution and sources of biodiversity in the Phanerozoic. Science 327, 196–198 (2010).

    Article  Google Scholar 

  5. Valentine, J. W. Climatic regulation of species diversification and extinction. Geol. Soc. Am. Bull. 79, 273–276 (1968).

    Article  Google Scholar 

  6. Mayhew, P. J., Jenkins, G. B. & Benton, T. G. A long-term association between global temperature and biodiversity, origination and extinction in the fossil record. Proc. R. Soc. B 275, 47–53 (2008).

    Article  Google Scholar 

  7. Erwin, D. H. Early introduction of major morphological innovations. Acta Palaeontol. Pol. 38, 281–294 (1994).

    Google Scholar 

  8. Martin, R. E. Secular increase nutrient levels through the Phanerozoic: Implications for productivity, biomass, and diversity of the marine biosphere. Palaios 11, 209–219 (1996).

    Article  Google Scholar 

  9. Veizer, J. et al. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater. Chem. Geol. 161, 59–88 (1999).

    Article  Google Scholar 

  10. McArthur, J. M., Howarth, R. J. & Bailey, T. R. Strontium isotope stratigraphy: LOWESS version 3: Best fit to the marine Sr-isotope curve for 0-509 Ma and accompanying look-up table for deriving numerical age. J. Geol. 109, 155–170 (2001).

    Article  Google Scholar 

  11. Kampschulte, A. & Strauss, H. The sulfur isotopic evolution of Phanerozoic seawater based on the analysis of structurally substituted sulfate in carbonates. Chem. Geol. 204, 255–286 (2004).

    Article  Google Scholar 

  12. Haq, B. U. & Schutter, S. R. A chronology of Paleozoic sea-level changes. Science 322, 64–68 (2008).

    Article  Google Scholar 

  13. Haq, B. U., Hardenbol, J. & Vail, P. R. Chronology of fluctuating sea levels since the Triassic. Science 235, 1156–1167 (1987).

    Article  Google Scholar 

  14. Miller, K. G. et al. The Phanerozoic record of global sea-level change. Science 310, 1293–1298 (2005).

    Article  Google Scholar 

  15. Benton, M. J. The Red Queen and the Court Jester: Species diversity and the role of biotic and abiotic factors through time. Science 323, 728–732 (2009).

    Article  Google Scholar 

  16. Foote, M. & Raup, D. M. Fossil preservation and the stratigraphic ranges of taxa. Paleobiology 22, 121–140 (1996).

    Article  Google Scholar 

  17. Shields, G. A. A normalized seawater strontium isotope curve: Possible implications for Neoproterozoic-Cambrian weathering rates and the further oxygenation of the Earth. Electron. Earth 2, 35–42 (2007).

    Google Scholar 

  18. Wheat, C. G., McManus, J., Mottl, M. J. & Giambalvo, E. Oceanic phosphorus imbalance: Magnitude of the mid-ocean ridge flank hydrothermal sink. Geophys. Res. Lett. 30, 1895 (2003).

    Article  Google Scholar 

  19. Follmi, K. B. 160 m.y. record of sedimentary phosphorus burial: Coupling of climate and continental weathering under greenhouse and icehouse conditions. Geology 23, 859–862 (1995).

    Article  Google Scholar 

  20. Van Cappellen, P. V. & Ingall, E. D. Redox stabilization of the atmosphere and oceans by phosphorus-limited marine productivity. Science 271, 493–496 (1996).

    Article  Google Scholar 

  21. Wortmann, U. G. & Chernyavsky, B. M. Effect of evaporite deposition on early Cretaceous carbon and sulphur cycling. Nature 446, 654–656 (2007).

    Article  Google Scholar 

  22. Arthur, M. A. & Sageman, B. B. Marine black shales: Depositional mechanisms ad environments of ancient deposits. Annu. Rev. Earth Planet. Sci. 22, 499–551 (1994).

    Article  Google Scholar 

  23. Vermeij, G. J. Economics, volcanoes, and Phanerozoic revolutions. Paleobiology. 21, 125–152 (1995).

    Article  Google Scholar 

  24. Allmon, W. D. in Evolutionary Paleoecology (eds Allmon, W. D. & Botjer, D. J.) 9–26 (Columbia Univ. Press, 2001).

    Book  Google Scholar 

  25. Gradstein, F. M., Ogg, J. G. & Smith, A. G. A Geologic Time Scale 2004 (Cambridge Univ. Press, 2004).

    Book  Google Scholar 

  26. Wei, W. & Peleo-Alampay, A. Updated Cenozoic nannofossil magnetobiochronology. INA Newslet. 15, 15–21 (1993).

    Google Scholar 

  27. Vermeij, G. in Evolution on Planet Earth: The Impact of the Physical Environment (eds Rothschild, L. J. & Lister, A. M.) 209–232 (Academic, 2003).

    Book  Google Scholar 

  28. Sharp, Z. Stable Isotope Geochemistry (Pearson Prentice Hall, 2007).

    Google Scholar 

  29. Raymo, M. E. & Ruddiman, W. F. Tectonic forcing of late Cenozoic climate. Nature 359, 117–122 (1992).

    Article  Google Scholar 

Download references

Acknowledgements

We thank J. Alroy and K.G. Miller for sharing their databases on Phanerozoic marine origination rates and sea level, respectively. J.S. Crampton and G.S. Herbert provided insightful comments on an earlier draft. D.C. Roman and G. Fox as well as C.H. Cuartas gave helpful advice on the various statistical questions and on R programming, respectively. We are also very grateful to W. Kiessling and R.E. Martin for constructive comments, which helped improve the manuscript. This is Paleobiology Database publication no. 116.

Author information

Authors and Affiliations

Authors

Contributions

Both authors contributed to the research, data interpretation and manuscript preparation.

Corresponding authors

Correspondence to Andrés L. Cárdenas or Peter J. Harries.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Supplementary Information

Supplementary Information (PDF 560 kb)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Cárdenas, A., Harries, P. Effect of nutrient availability on marine origination rates throughout the Phanerozoic eon. Nature Geosci 3, 430–434 (2010). https://doi.org/10.1038/ngeo869

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo869

This article is cited by

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing