Global microbial carbonate proliferation after the end-Devonian mass extinction: Mainly controlled by demise of skeletal bioconstructors
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/srep39694.pdf
Reference53 articles.
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2. Kaiser, S. I., Aretz, M. & Becker, R. T. The global Hangenberg Crisis (Devonian-Carboniferous transition): review of a first-order mass extinction. Geol. Soc. London Spec. Publ. 423, 387–437 doi: 10.1144/SP423.9 (2015).
3. Sepkoski, J. J. Patterns of Phanerozoic extinction: a perspective from global data bases in Global Events and Event Stratigraphy in the Phanerozoic (ed. Walliser, O. H. ) 35–51 (Springer-Verlag, Berlin, 1996).
4. Carmichael, S. K. et al. Climate instability and tipping points in the Late Devonian: Detection of the Hangenberg Event in an open oceanic island arc in the Central Asian Orogenic Belt. Gondwana Res. 32, 213–231 (2016).
5. Riding, R. Microbial carbonate abundance compared with fluctuations in metazoan diversity over geological time. Sediment. Geol. 185, 229–238 (2006).
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