Land-plant diversity and the end-Permian mass extinction

By P. Rees. 2002

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A Bayesian approach for detecting the impact of mass‐extinction events on molecular phylogenies when rates of lineage diversification may vary (2016, background): “Each event is estimated to have caused the loss of 70–75%of contemporaneous terrestrial species (e.g. Raup & Sepkoski 1982; Labandeira & Sepkoski 1993; Rees 2002; McElwain & Punyasena 2007; Cascales-Mi~nana & Cleal 2014).”
Paleophysiology and End-Permian Mass Extinction (2007, background): “Plants show evidence of rapid boundary-level extinction and floral reorganization in both Gondwana [97] and the peri-North Atlantic region [15]; however, data compiled by Rees [98] show an increase of floral diversity in the northern temperate regions of Angara (see also [99]), suggesting that plant”
Late Permian (Lopingian) terrestrial ecosystems: A global comparison with new data from the low-latitude Bletterbach Biota (2017, background): “, 2005) was probably driven by the development of climate regimes (Rees, 2002; Sidor et al., 2005; Roscher et al., 2008), although latitudinal distribution was a strong predictor of ecosystem compositional affinity.”
Evolution of leafy liverworts (Jungermanniidae, Marchantiophyta) : estimating divergence times from chloroplast DNA sequences using penalized likelihood with integrated fossil evidence (2007, unknown): “60% of plant genera (Anderson & al., 1999; Rees, 2002; Wing, 2004).”