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      Largest Cretaceous lizard track assemblage, new morphotypes and longest trackways comprise diverse components of an exceptional Korean Konservat-Lagerstätten ichnofauna

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          Abstract

          A newly discovered assemblage of lizard tracks from the Lower Cretaceous Jinju Formation (Sindong Group, Gyeongsang Basin) Korea is the largest yet reported from the Cretaceous. It consists of at least 95 tracks comprising five trackways, including a meter-long trackway (T1) with 50 footprints assigned to the new ichnotaxon Neosauroides innovatus ichnosp. nov. Two other trackways (T2 and T3) are designated N. innovatus paratypes characterized by strong heteropody, relatively wide trackways and small narrow manus tracks. These morphological characteristics distinguish Neosauroides innovatus from the previously reported lizard trackways Sauripes hadongensis from the Hasandong Formation and Neosauroides koreaensis from the Haman Formation, both also from the Gyeongsang Basin. These three lizard track assemblages from the Korean Cretaceous constitute the entire global lizard track record for this period. The Mesozoic record of lizard tracksites is more localized than the lizard body fossil record. This limited distribution suggests bias in the track record and the fossil record more generally. However, due to deposition of fine-grained substrates, suitable for high definition track registration, the Jinju Formation is increasingly well known as an ichnological window on small tetrapod activity and based on diversity, abundance and high-quality preservation, is regarded as an exceptional Konservat-Lagerstätten.

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          Konservat-Lagerstätten: cause and classification

          A review of the processes required for exceptional preservation of soft-bodied fossils demonstrates that anoxia does not significantly inhibit decay and emphasizes the importance of early diagenetic mineralization. Early diagenesis is the principal factor amongst the complex processes leading to soft-part preservation. The development of a particular preservational mineral is controlled by rate of burial, amount of organic detritus, and salinity. A new causative classification of soft-bodied fossil biotas is presented based upon fossil mineralogy and mineral paragenesis.
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            At the feet of the dinosaurs: the early history and radiation of lizards

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              TAXONOMIC COMPOSITION AND SYSTEMATICS OF LATE CRETACEOUS LIZARD ASSEMBLAGES FROM UKHAA TOLGOD AND ADJACENT LOCALITIES, MONGOLIAN GOBI DESERT

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                Author and article information

                Contributors
                Martin.Lockley@UCDenver.edu
                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group UK (London )
                2045-2322
                16 September 2019
                16 September 2019
                2019
                : 9
                : 13278
                Affiliations
                [1 ]Department of Science Education, 3 Jinnyangho-ro 369beon-gil, Jinju-si, Gyeongnam, 52673 Korea
                [2 ]ISNI 0000 0001 2109 5369, GRID grid.454168.a, Cultural Heritage Administration, Government Complex-Daejeon, 189, Cheongsa-ro, Seo-gu, ; Daejon, 35208 Korea
                [3 ]ISNI 0000000107903411, GRID grid.241116.1, Dinosaur Trackers Research Group, University of Colorado Denver, ; P.O. Box 173364, Denver, CO 80217-3364 USA
                [4 ]GRID grid.410906.a, National Science Museum, 481 Daedeok-daero, Yuseong-gu, ; Daejeon, 34143 Korea
                [5 ]Museo del Jurásico de Asturias (MUJA), Rasa de San Telmo, s/n, 33328 Colunga, Asturias, Spain
                Author information
                http://orcid.org/0000-0001-8023-3231
                Article
                49442
                10.1038/s41598-019-49442-0
                6746761
                31527673
                4d349987-3022-4d54-9f41-7a56b60b9437
                © The Author(s) 2019

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 27 September 2018
                : 20 August 2019
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                palaeontology
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                palaeontology

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