Large Perturbations of the Carbon Cycle During Recovery from the End-Permian Extinction

By Jonathan L. Payne, D. Lehrmann, Jiayong Wei, M. Orchard, D. Schrag, Andrew H. Knoll. Science, 2004

840 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Geology, Paleontology

View Paper: https://www.semanticscholar.org/paper/a5c4239e8a201f79caf12f0f8009d1532d27333b

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In Geochemistry and Petrology

Andrew H. Knoll

In Geology

In Paleontology

Citations in the corpus

ENVIRONMENTAL AND BIOLOGICAL CONTROLS ON THE INITIATION AND GROWTH OF A MIDDLE TRIASSIC (ANISIAN) REEF COMPLEX ON THE GREAT BANK OF GUIZHOU, GUIZHOU PROVINCE, CHINA (2006, background): “Figure 6 illustrates the stratigraphic position of samples containing Tubiphytes grains relative to both co-occurring conodonts and fossil grains, and the positive carbon-isotopic excursion across the Spathian-Anisian boundary (see Payne et al., 2004).”
Evolution and Geological Significance of Larger Benthic Foraminifera (2018, background): “Explanations for this vary from invoking the sheer scale of the Permian extinction to the prolonged stresses of the environment post end- Permian extinction (Hallam, 1991; Payne et al., 2004; Chen and Benton, 2012), or the effects of further extinction crises in the Early Triassic (Orchard, 2007; St”
The first half of tetrapod evolution, sampling proxies, and fossil record quality (2013, background): “Following a late Olenekian peak of 90 tetrapod genera, diversity fell to 76 in the lower Anisian, rose again to 96 in the late Anisian, and then plummeted to 39 in the lower Ladinian (Fig.”
Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the Permo-Triassic mass extinction (2013, background): “These identify a complete Anisian succession, from Bithynian at the base to Illyrian at the top of the sequence, but the fossil vertebrates come from the middle of the Pelsonian succession (Member II of the Guanling Formation), just slightly younger than the Luoping biota.”
Rapid demise and recovery of plant ecosystems across the end-Permian extinction event (2010, positive): “However, new paleontological and chemostratigraphic data from Early Triassic reveal reiterated crises throughout this epoch, including major disturbances in the C-cycle, which affected not only marine but also terrestrial ecosystems (Brühwiler, 2010; Galfetti et al., 2007a; Hermann et al., 2010; Hoc”
Non-commercial Research and Educational Use including without Limitation Use in Instruction at Your Institution, Sending It to Specific Colleagues That You Know, and Providing a Copy to Your Institution's Administrator. All Other Uses, Reproduction and Distribution, including without Limitation Comm (2005, neutral): “In a similar spirit Stephenson and Binsch developed a basic algorithm which relies on a matrix method derived from a general formulation of the least-squares problem [6].”
Paleophysiology and End-Permian Mass Extinction (2007, background): “Recent observations show that the boundary excursion was just the first of a series of strong C-isotope fluctuations that continued throughout the Early Triassic [47].”
A review of the evolution, biostratigraphy, provincialism and diversity of Middle and early Late Triassic conodonts (2016, background): “One possible explanation is episodic harsh environmental conditions during the Early Triassic (Payne et al. 2004; Richoz 2006; Sun et al. 2012; Romano et al. 2013; Chen et al. 2015b) with multiple small-scaled extinctions and following elevated origination rates (Stanley 2009; Hofmann et al.”
The palaeoclimatology, palaeoecology and palaeoenvironmental analysis of mass extinction events (2006, background): “Very large d(13)C excursions in the aftermath of the end-Permian event are almost certainly not the result of methane venting (Payne et al., 2004).”