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      A new basal ichthyosauromorph from the Lower Triassic (Olenekian) of Zhebao, Guangxi Autonomous Region, South China

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          Abstract

          Here we describe a newly discovered basal ichthyosauromorph from the Lower Triassic of South China, Baisesaurus robustus gen. et sp. nov. The only known specimen of this new species was collected from the Lower Triassic (Olenekian) Luolou Formation in the Zhebao region of Baise City, on the northwest margin of the Nanpanjiang Basin, and comprises a partial skeleton including the ribs, the gastralia, a limb element, 12 centra, and seven neural arches. Comparisons to a wide variety of Early Triassic marine reptiles show Baisesaurus robustus to be a basal ichthyosauromorph based on the following features: neural arches lack transverse processes; dorsal ribs are slender, and not pachyostotic even proximally; and median gastral elements have long, sharp anterior processes. The limb element is long and robust, and is most likely to be a radius. Baisesaurus robustus is large (estimated length more than 3 m) relative to early ichthyosauromorphs previously discovered in China, and shares noteworthy morphological similarities with Utatsusaurus hataii, particularly with regard to body size and the morphology of the probable radius. Baisesaurus robustus also represents the first record of an Early Triassic ichthyosauromorph from Guangxi Autonomous Region, extending the known geographic distribution of ichthyosauromorphs in South China.

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          Phylogeny of the Ichthyopterygia

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            Early Triassic Marine Biotic Recovery: The Predators' Perspective

            Examining the geological past of our planet allows us to study periods of severe climatic and biological crises and recoveries, biotic and abiotic ecosystem fluctuations, and faunal and floral turnovers through time. Furthermore, the recovery dynamics of large predators provide a key for evaluation of the pattern and tempo of ecosystem recovery because predators are interpreted to react most sensitively to environmental turbulences. The end-Permian mass extinction was the most severe crisis experienced by life on Earth, and the common paradigm persists that the biotic recovery from the extinction event was unusually slow and occurred in a step-wise manner, lasting up to eight to nine million years well into the early Middle Triassic (Anisian) in the oceans, and even longer in the terrestrial realm. Here we survey the global distribution and size spectra of Early Triassic and Anisian marine predatory vertebrates (fishes, amphibians and reptiles) to elucidate the height of trophic pyramids in the aftermath of the end-Permian event. The survey of body size was done by compiling maximum standard lengths for the bony fishes and some cartilaginous fishes, and total size (estimates) for the tetrapods. The distribution and size spectra of the latter are difficult to assess because of preservation artifacts and are thus mostly discussed qualitatively. The data nevertheless demonstrate that no significant size increase of predators is observable from the Early Triassic to the Anisian, as would be expected from the prolonged and stepwise trophic recovery model. The data further indicate that marine ecosystems characterized by multiple trophic levels existed from the earliest Early Triassic onwards. However, a major change in the taxonomic composition of predatory guilds occurred less than two million years after the end-Permian extinction event, in which a transition from fish/amphibian to fish/reptile-dominated higher trophic levels within ecosystems became apparent.
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              Ichthyosauria: their diversity, distribution, and phylogeny

              P. Sander (2000)
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                Author and article information

                Contributors
                Journal
                PeerJ
                PeerJ
                PeerJ
                PeerJ
                PeerJ Inc. (San Diego, USA )
                2167-8359
                7 April 2022
                2022
                : 10
                : e13209
                Affiliations
                [1 ]School of Li Siguang, China University of Geosciences (Wuhan) , Wuhan, Hubei Province, China
                [2 ]School of Earth Sciences, China University of Geosciences (Wuhan) , Wuhan, Hubei Province, China
                [3 ]Guizhou Geological Survey , Guiyang, Guizhou Province, China
                [4 ]Department of Biological Sciences, University of Alberta , Edmonton, Canada
                [5 ]Philip J. Currie Dinosaur Museum , Wembley, Canada
                [6 ]Wuhan Centre of China Geological Survey , Wuhan, China
                Author information
                http://orcid.org/0000-0001-9636-0307
                http://orcid.org/0000-0002-5488-6797
                Article
                13209
                10.7717/peerj.13209
                8995025
                7c1ac171-82e4-41e2-b6d1-28f9dc4febd6
                © 2022 Ren et al.

                This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited.

                History
                : 20 May 2021
                : 10 March 2022
                Funding
                Funded by: National Natural Science Foundation of China
                Award ID: 41830320; 41688103; 41972014
                Funded by: Guizhou Scientific and Technology Planning Project
                Award ID: QKHPTRC [2018]5626
                Funded by: Guizhou Bureau of Geology and Mineral Exploration and Development
                Award ID: QDKKH [2020]29
                Funded by: Natural Sciences and Engineering Research Council of Canada
                Award ID: RGPIN-2017-06246
                This project was supported by the National Natural Science Foundation of China (grant no. 41830320; 41688103; 41972014), the Guizhou Scientific and Technology Planning Project (QKHPTRC [2018]5626), the Scientific Research Project of the Guizhou Bureau of Geology and Mineral Exploration and Development (QDKKH [2020]29), and the Natural Sciences and Engineering Research Council of Canada (Discovery Grant RGPIN-2017-06246). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
                Categories
                Evolutionary Studies
                Paleontology
                Zoology

                early triassic,china,morphology,ichthyosauromorpha
                early triassic, china, morphology, ichthyosauromorpha

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