Evolution of the Permian and Triassic foraminifera in South China*
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Cited by (26)
Migration controls extinction and survival patterns of foraminifers during the Permian-Triassic crisis in South China
2020, Earth-Science ReviewsCitation Excerpt :The behaviours of foraminifera during the PTME exhibit high selectivity in both taxonomy and ecology, and they are, therefore, an informative group for evaluating different drivers of extinction. The Order Fusulinida experienced a severe extinction during the late Guadalupian (Capitanian, Middle Permian) mass extinction, and never re-established their Middle Permian levels of diversity (Stanley and Yang, 1994; Tong and Shi, 2000; Yang et al., 2004; Bond and Wignall, 2009). In the aftermath of that crisis, non-fusulinacean fusulinids rapidly came to dominate Lopingian assemblages in low palaeolatitudinal tropical shallow carbonate platform settings (Tong and Shi, 2000; Mohtat-Aghaï and Vachard, 2005; Kobayashi, 2006; Gaillot and Vachard, 2007).
Permian–Triassic extinction pattern revealed by foraminifers and geochemical records in the central Persian Gulf, southern Iran
2020, Palaeogeography, Palaeoclimatology, PalaeoecologyA newly discovered earliest Triassic chert at Gaimao section, Guizhou, southwestern China
2012, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :The end-Permian saw the largest mass extinction in life's history with 80–96% of species disappearing (Sepkoski, 1981; Raup and Sepkoski, 1982; Jin et al., 2000; Erwin et al., 2002; Erwin, 2006; Kozur, 2007) with major groups such as rugose corals that were totally wiped out (Stanley, 2003) and others, such as the radiolarian and foraminifera nearly, so (Racki, 1999; Tong and Shi, 2000).
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This research is sponsored by support of the National Natural Science Foundation of China (No. 49502022, 49632070) (to JNT) and the Australian Research Council (to GRS).