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Springer Science and Business Media LLC
Reference59 articles.
1. Bambach, R. K., Knoll, A. J. & Wang, S. C. Origination, extinction, and mass depletions of marine diversity. Paleobiology 30, 522–542 (2004).
2. Brenchley, P. J. Late Ordovician extinctions and their relationship to the Gondwana glaciations. In Brenchley, P.J. (ed.), Fossils and Climate. (JohnWiley & Sons, Chichester, pp. 291–316, 1984).
3. Harper, D. A. T., Hammarlund, E. U. & Rasmussen, C. M. Ø. End Ordovician extinctions: a coincidence of causes. Gondwana Res. 25, 1294–1307 (2014).
4. Melchin, M. M., Mitchell, C. E., Holmden, C. & Štorch, P. Environmental changes in the Late Ordovician–early Silurian: review and new insights from black shales and nitrogen isotopes. Geol. Soc. Am. Bull. 125, 1635–1670 (2013).
5. Zhou, L. et al. Changes in marine productivity and redox conditions during the Late Ordovician Hirnantian glaciation. Palaeogeogr. Palaeoclimatol. Palaeoecol. 420, 223–234 (2015).
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