The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals.
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References
Langer, G., Nehrke, G., Probert, I., Ly, J. & Ziveri, P. Biogeosciences 6, 2637–2646 (2009).
Lohbeck, K. T., Riebesell, U. & Reusch, T. B. H. Nature Geosci. 5, 346–351 (2012).
Caldeira, K. & Wickett, M. E. Nature 425, 365 (2003).
Gibbs, S. J. et al. Nature Geosci. 6, 218–222 (2013).
Zachos, J. C. et al. Science 302, 1551–1554 (2003).
Zachos, J. C. et al. Science 308, 1611–1615 (2005).
Gibbs, S. J., Bralower, T. J., Bown, P. R., Zachos, J. C. & Bybell L. Geology 34, 233–236 (2006).
Gibbs, S. J., Bown, P. R., Sessa, J., Bralower, T. J. & Wilson, P. A. Science 314, 1770–1773 (2006).
Stoll, H. M., Shimizu, N., Archer, D. & Ziveri, P. Earth Planet. Sci. Lett. 258, 192–206 (2007).
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Langer, G. Plankton in a greenhouse world. Nature Geosci 6, 164–165 (2013). https://doi.org/10.1038/ngeo1750
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DOI: https://doi.org/10.1038/ngeo1750
