Many species of nannoplankton with carbonate shells vanished during the mass extinction 65 million years ago. An analysis of extinction rates from the world's oceans reveals a geographic bias in the demise and recovery of nannoplankton species.
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References
Jiang, S.-J., Bralower, T. J., Patzkowsky, M. E., Kump, L. R. & Schueth, J. D. Nature Geosci. 3, 280–285 (2010).
Hollis, C. J. in Cretaceous-Tertiary Mass Extinctions: Biotic and Environmental Changes. (eds Macleod, N. & Keller, G.) 173–204 (W. W. Norton, 1996).
Coxall, H. K., D'Hondt, S. & Zachos, J. C. Geology 34, 297–300 (2006).
Raup, D. M. & Jablonski, D. Science 260, 971–973 (1993).
Zachos, J. C., Arthur, M. A. & Dean, W. E. Nature 337, 61–64 (1989).
Antia, N. J. & Cheng, J. Y. Phycologia 9, 179–183 (1970).
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Wignall, P. Safer in the south. Nature Geosci 3, 228–229 (2010). https://doi.org/10.1038/ngeo827
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DOI: https://doi.org/10.1038/ngeo827