Pattern of marine mass extinction near the Permian-Triassic boundary in South China.

By In South China Y. G. Jin, Yan Wang, Wen I. Wang, Q. Shang, Changqun Cao, Douglas H. Erwin. Science, 2000

644 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/00b7e4f39b68ba7dbc790230d7b1af8bcd40dc5f

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Citations in the corpus

A macroevolutionary mosaic: episodic host‐switching, geographical colonization and diversification in complex host–parasite systems (2008, background): “…(like free-living organisms) can exhibit independent trajectories in which biogeographical context, palaeoenvironmental parameters, and ecological settings are critical in determining faunal structure and patterns of diversity over time (Hoberg, 1997a, 2005a; Erwin, 1998; Hoberg & Klassen, 2002).”
Rapid demise and recovery of plant ecosystems across the end-Permian extinction event (2010, neutral): “In the Meishan (GSSP) section (Jin et al., 2000) the corresponding isotopic shifts take place within an interval of about 30.”
Land-plant diversity and the end-Permian mass extinction (2002, background): “This two-step decline is compatible with observations of the marine faunal record (e.g., Erwin, 1994; Knoll et al., 1996; Hallam and Wignall, 1999; Jin et al., 2000), but reveals nothing about possible causes.”
Birth and early evolution of metazoans (2014, background): “…possibly correspond in magnitude to the biggest mass extinction of the Phanerozoic across the Paleozoic/Mesozoic (or Permo-Triassic) boundary (e.g., Jin et al., 2000; Erwin, 2006), because the extinctions during the Ediacaran– Cambrian time involved the terminations of various animal phyla, and…”
The recovery of terrestrial vertebrate diversity in the South African Karoo Basin after the end-Permian extinction (2005, background): “Numerous marine PTB sections have provided a broad indication of the devastation of marine life [22,24,25,36,60].”
Origination and Extinction through the Phanerozoic: A New Approach (2003, result): “To determine whether there was a true extinction peak in the Tatarian, for example, we need to know not only whether extinction follows the pulsed model in the Late Permian but also whether it does so in the Early Triassic.”
A case for a comet impact trigger for the Paleocene/Eocene thermal maximum and carbon isotope excursion (2003, background): “If supported by further evidence of tracers of extraterrestrial material in CIE deposits, the P/E impact may have implications for the cause of other catastrophic events accompanied by sudden negative carbon isotope excursions, such as at the Permo^Triassic boundary [77].”
Fungal abundance spike and the Permian^Triassic boundary in the Karoo Supergroup (South Africa) (2003, background): “The end-Permian mass extinction eliminated more than 90% of marine species (Raup, 1979; Jin et al., 2000).”
The evolution of modern corals and their early history (2003, background): “Detailed studies of latest Permian strata in South China and strata at other key sites suggest that the global end-Permian catastrophe was more abrupt than previously thought (Bowring et al., 1998; Jin et al., 2000).”
How to kill (almost) all life: the end-Permian extinction event (2003, background): “Siberian Trap eruptions have moved from having been allotted a relatively minor role in the PTr crisis as part of a complex web of interacting processes [20], to being the most probable trigger for the catastrophe [2, 4 ,21].”