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Permian continental sequences from North China contain previously unrecognized episodes of plant radiation and elevated extinction. The earliest extinction, in the Lower Shihhotse Formation (Roadian, Guadalupian), records a 45% floral species loss and is tentatively correlated with global extinctions amongst dinocephalian reptiles. Two younger extinctions are dated by correlating the Illawara Reversal and palaeomagnetic polarity sequences from Shanxi Province against global palaeomagnetic history. Missing data from the Shanxi sequence are evaluated using a novel approach estimating likely maximum and minimum sequence changes that provide age estimates for post-Illawara events in North China. The second extinction in the middle Upper Shihhotse Formation is more significant and is dated to the mid-Capitanian, with a loss of 56% of plant species coinciding with two phases of volcanism of the Emeishan Large Igneous Province in South China, previously linked to the mid-Capitanian marine mass extinction. The youngest extinction in the upper Upper Shihhotse Formation (late Capitanian to mid-Wuchapingian) is catastrophic and represents the end of range in the sequence. Changes in sedimentary facies suggest it to be related to global climatic warming and drying. Other viable causal mechanisms for the extinction episodes include plate motion and collision, global climate change, volcanism and biological competition.

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Reinvestigation of Oligocarpia gothanii Halle (Gleicheniaceae) from the Permian Period of China has uncovered a rare demonstration of ontogenetic succession in numerous intact plants and has led to emendation of the diagnosis and typification of the species. Reconstruction of the fern's vegetative life cycle shows a small rosette-shaped juvenile plant with immature fronds of pinnae undifferentiated into pinnules. The second stage is a series of leafy shoots increasing in size and complexity and bearing fronds essentially comparable with those of the adult plants. Mature plants have sphenopteroid-type fronds differentiated into vegetative and fertile fronds. Close association of plants on the same bedding plane and the presence of a connecting root network between shoots, show that juvenile plants spread by vegetative propagation using underground stolons. Sedimentological information and co-occurrence with the bryophyte Thallites hallei Lundblad suggests that O. gothanii occupied a wetland habitat and was preserved in an obrution event consistent with flooding of marginal areas in a fluvio-deltaic setting. Although recent studies on Oligocarpia have focused exclusively on reproductive features, new ontogenetic information suggests that plants growing in rapidly changing environments may have been reliant on vegetative propagation and would not have needed to reach sexual maturity for successful reproduction.