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      A Late Cretaceous mammal from Brazil and the first radioisotopic age for the Bauru Group

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          Abstract

          In the last three decades, records of tribosphenidan mammals from India, continental Africa, Madagascar and South America have challenged the notion of a strictly Laurasian distribution of the group during the Cretaceous. Here, we describe a lower premolar from the Late Cretaceous Adamantina Formation, São Paulo State, Brazil. It differs from all known fossil mammals, except for a putative eutherian from the same geologic unity and Deccanolestes hislopi, from the Maastrichtian of India. The incompleteness of the material precludes narrowing down its taxonomic attribution further than Tribosphenida, but it is larger than most coeval mammals and shows a thin layer of parallel crystallite enamel. The new taxon helps filling two major gaps in the fossil record: the paucity of Mesozoic mammals in more northern parts of South America and of tribosphenidans in the Cretaceous of that continent. In addition, high-precision U-Pb geochronology provided a post-Turonian maximal age (≤87.8 Ma) for the type stratum, which is overlain by the dinosaur-bearing Marília Formation, constraining the age of the Adamantina Formation at the site to late Coniacian–late Maastrichtian. This represents the first radioisotopic age for the Bauru Group, a key stratigraphic unit for the study of Cretaceous tetrapods in Gondwana.

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          Resolution of the early placental mammal radiation using Bayesian phylogenetics.

          Molecular phylogenetic studies have resolved placental mammals into four major groups, but have not established the full hierarchy of interordinal relationships, including the position of the root. The latter is critical for understanding the early biogeographic history of placentals. We investigated placental phylogeny using Bayesian and maximum-likelihood methods and a 16.4-kilobase molecular data set. Interordinal relationships are almost entirely resolved. The basal split is between Afrotheria and other placentals, at about 103 million years, and may be accounted for by the separation of South America and Africa in the Cretaceous. Crown-group Eutheria may have their most recent common ancestry in the Southern Hemisphere (Gondwana).
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            Zircon U–Pb chemical abrasion (“CA-TIMS”) method: Combined annealing and multi-step partial dissolution analysis for improved precision and accuracy of zircon ages

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              Phylogenomic datasets provide both precision and accuracy in estimating the timescale of placental mammal phylogeny.

              The fossil record suggests a rapid radiation of placental mammals following the Cretaceous-Paleogene (K-Pg) mass extinction 65 million years ago (Ma); nevertheless, molecular time estimates, while highly variable, are generally much older. Early molecular studies suffer from inadequate dating methods, reliance on the molecular clock, and simplistic and over-confident interpretations of the fossil record. More recent studies have used Bayesian dating methods that circumvent those issues, but the use of limited data has led to large estimation uncertainties, precluding a decisive conclusion on the timing of mammalian diversifications. Here we use a powerful Bayesian method to analyse 36 nuclear genomes and 274 mitochondrial genomes (20.6 million base pairs), combined with robust but flexible fossil calibrations. Our posterior time estimates suggest that marsupials diverged from eutherians 168-178 Ma, and crown Marsupialia diverged 64-84 Ma. Placentalia diverged 88-90 Ma, and present-day placental orders (except Primates and Xenarthra) originated in a ∼20 Myr window (45-65 Ma) after the K-Pg extinction. Therefore we reject a pre K-Pg model of placental ordinal diversification. We suggest other infamous instances of mismatch between molecular and palaeontological divergence time estimates will be resolved with this same approach.
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                Author and article information

                Journal
                R Soc Open Sci
                R Soc Open Sci
                RSOS
                royopensci
                Royal Society Open Science
                The Royal Society Publishing
                2054-5703
                May 2018
                30 May 2018
                30 May 2018
                : 5
                : 5
                : 180482
                Affiliations
                [1 ]Laboratório de Paleontologia, FFCLRP, Universidade de São Paulo , Ribeirão Preto-SP 14040-901, Brazil
                [2 ]División Paleontología Vertebrados, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata , Paseo del Bosque S/N°, B1900FWA La Plata, Argentina
                [3 ]LASBE, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata , Paseo del Bosque S/N°, B1900FWA La Plata, Argentina
                [4 ]División Zoología Vertebrados, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata , Paseo del Bosque S/N°, B1900FWA La Plata, Argentina
                [5 ]CONICET , Buenos Aires, Argentina
                [6 ]Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology , Cambridge, MA 02139, USA
                [7 ]Department of Geology and Natural Resources, IG, Universidade Estadual de Campinas , Campinas-SP, Brazil
                Author notes
                Author for correspondence: Mariela C. Castro e-mail: marielaccastro@ 123456yahoo.com.br
                [†]

                Present address: Departamento de Ciências Biológicas, IBiotec, Universidade Federal de Goiás, Regional Catalão, Catalão-GO, Brazil.

                Electronic supplementary material is available online at https://dx.doi.org/10.6084/m9.figshare.c.4097852.

                Author information
                http://orcid.org/0000-0002-5734-9639
                Article
                rsos180482
                10.1098/rsos.180482
                5990825
                bb25702c-b796-4ffd-9c58-1ba888e6e11c
                © 2018 The Authors.

                Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

                History
                : 23 March 2018
                : 23 April 2018
                Funding
                Funded by: Fundação de Amparo à Pesquisa do Estado de São Paulo, http://dx.doi.org/10.13039/501100001807;
                Award ID: 2013/23114-1
                Award ID: 2014/03825-3
                Award ID: 2014/23815-2
                Award ID: 2015/17632-5
                Award ID: 2016/02473-1
                Categories
                1001
                144
                183
                Biology (Whole Organism)
                Research Article
                Custom metadata
                May, 2018

                tribosphenida,enamel reduction,bauru basin,south america,u-pb geochronology,mesozoic

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