Titlebook: Brachiopods around the Permian-Triassic Boundary of South China; Wei-Hong He,G. R. Shi,Yang Zhang Book 2019 Springer Nature Singapore Pte

灯泡

Introduction,012). The event has inspired (and would inspire) generations of palaeontologists to interrogate this great dying, with no sign of abating. South China, as an isolated block, was located in the eastern Palaeotethyan gape during the Late Permian.earliest Triassic (Blakey 2008) and contains some of the

幻想

爱花花儿愤怒

Depositional Sequences, Biotic Assemblages and Review on Changhsingian (or Late Changhsingian) Pala The upper Talung Formation is dominated by dark grey thin-bedded cherts and siliceous mudstones, intercalated with medium-bedded grey argillaceous limestones, thin-bedded calcareous mudstones and volcanic ash. The siliceous mudstones abundantly yield horizontal beddings. The upper Talung Formation

Anthropoid

拱形面包

提名

Lacunar-Stroke

Discussion on Changes of Brachiopod Diversity and Morphologic Features and Their Implications for triassic transition. This phenomenon lets us recall the scenario that the upward migration of anoxic deep waters in a stratified ocean caused the radiolarian extinction in a Japanese pelagic environment (Isozaki 2009; Takahashi et al. 2013). Therefore, elsewhere we have proposed that the formation of

古董

albuminuria

印第安人

Introduction,entred around the Permian.Triassic mass extinction (e.g., Jin et al. 2000; Xie et al. 2005; Shen et al. 2001; Joachimski et al. 2012; Algeo et al. 2013; Song et al. 2013; He et al. 2015). Based on the research, an episodic mass-extinction pattern (e.g., single- or two-episode) has been proposed (Yan