Improved efficiency of the biological pump as a trigger for the Late Ordovician glaciation

Author:

Shen Jiaheng,Pearson Ann,Henkes Gregory A.,Zhang Yi Ge,Chen Kefan,Li Dandan,Wankel Scott D.ORCID,Finney Stanley C.,Shen YananORCID

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference56 articles.

1. Sepkoski, J. J. in Global Events and Event Stratigraphy in the Phanerozoic: Results of the International Interdisciplinary Cooperation in the IGCP-Project 216 ‘ Global Biological Events in Earth History’ (ed. Walliser, O. H.) 35–51 (Springer, Berlin Heidelberg, 1996).

2. Finnegan, S. et al. The magnitude and duration of Late Ordovician–Early Silurian glaciation. Science 331, 903–906 (2011).

3. Brenchley, P. et al. High-resolution stable isotope stratigraphy of Upper Ordovician sequences: constraints on the timing of bioevents and environmental changes associated with mass extinction and glaciation. Geol. Soc. Am. Bull. 115, 89–104 (2003).

4. Sheehan, P. M. The Late Ordovician mass extinction. Annu. Rev. Earth Planet. Sci. Lett. 29, 331–364 (2001).

5. Yapp, C. J. & Poths, H. Ancient atmospheric CO2 pressures inferred from natural goethites. Nature 355, 342 (1992).

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