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      Land Snail with Periostracal Hairs Preserved in Burmese Amber

      research-article
      1 , 2 , 8 , 9 , , 3 , 4 , 8 , ∗∗ , 5 , 6 , 7
      iScience
      Elsevier
      Mollusca, Paleontology, Paleobiology

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          Summary

          Excellently preserved fossils often provide important insights into evolutionary histories and adaptations to environmental change in Earth's biogeologic record. Mid-Cretaceous Burmese amber, for example, is a proven reservoir for spectacular findings. Here we document the first record of a fossil land snail with periostracal hairs preserved in amber. We interpret the development of hairs as an adaptation to the tropical forest environment, serving as a mechanism to increase adhesion of the snail to plants during foraging while collecting and transporting seeds in the process. The present record coincides with a major global radiation of angiosperms, a main food resource for terrestrial snails. As such, the expansion of flowering plants likely triggered this evolutionary adaptation and, thus, the diversification of land snails in the Cretaceous.

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          Highlights

          • We document the oldest fossil record of a hairy land snail

          • The hairs are interpreted as adaptation to a tropical forest environment

          • Hairs are suggested to increase adhesion to plants during foraging

          • The adaptation was potentially caused by the coeval radiation of flowering plants

          Abstract

          Molluscum; Paleontology; Paleobiology

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          Most cited references31

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          Fossiliferous Cretaceous Amber from Myanmar (Burma): Its Rediscovery, Biotic Diversity, and Paleontological Significance

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            Revised Classification, Nomenclator and Typification of Gastropod and Monoplacophoran Families

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              Seed Size, Fruit Size, and Dispersal Systems in Angiosperms from the Early Cretaceous to the Late Tertiary.

              Fossil data from 25 angiosperm floras from the Early Cretaceous ( approximately 124 million years ago) to the Pliocene ( approximately 2 million years ago) were compiled to estimate sizes of seeds and fruits and the relative proportion of two different seed-dispersal systems by animals and by wind. The results suggest that, first, seed and fruit sizes were generally small during most of the Cretaceous, in agreement with previous suggestions, but the trend of increasing sizes started before the Cretaceous-Tertiary boundary; second, there was a decrease in both seed and fruit sizes during late Eocene and Oligocene, reaching a level that has continued to the Late Tertiary; third, the fraction of animal dispersal was, in contrast to previous suggestions, rather high also during the Cretaceous but increased drastically in the Early Tertiary and declined congruently with the declining seed and fruit sizes from the late Eocene; and fourth, the fraction of wind dispersal showed a bimodal pattern, being high in the Late Cretaceous and in the Oligocene-Miocene but with a drop in between. We find that the observed trends are only weakly related to the availability of animal fruit dispersers. Instead, the trends are congruent with a climate-driven change in environmental conditions for recruitment, where larger seeds are favored by closed forest vegetation. The prevalence of semiopen, dry, and probably herbivore-disturbed vegetation during the Cretaceous, the development of closed multistratal forests in the Eocene, and the later development of a more open vegetation and grasslands starting in the Oligocene-Miocene, are reflected in the distribution of angiosperm seed and fruit sizes and in the dispersal systems.
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                Author and article information

                Contributors
                Journal
                iScience
                iScience
                iScience
                Elsevier
                2589-0042
                12 October 2019
                25 October 2019
                12 October 2019
                : 20
                : 567-574
                Affiliations
                [1 ]Department of Animal Ecology & Systematics, Justus Liebig University, 35392 Giessen, Germany
                [2 ]Naturalis Biodiversity Center, 2300 RA Leiden, the Netherlands
                [3 ]State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
                [4 ]School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
                [5 ]Naturhistorisches Museum der Burgergemeinde Bern, 3005 Bern, Switzerland
                [6 ]Institute of Ecology and Evolution, University of Bern, 3012 Bern, Switzerland
                [7 ]Senckenberg Forschungsinstitut und Naturmuseum, 60325 Frankfurt am Main, Germany
                Author notes
                []Corresponding author tneub@ 123456zo.jlug.de
                [∗∗ ]Corresponding author xinglida@ 123456gmail.com
                [8]

                These authors contributed equally

                [9]

                Lead Contact

                Article
                S2589-0042(19)30373-6
                10.1016/j.isci.2019.09.034
                6834951
                31611056
                0934d1b0-be06-4c5f-869b-57059ab613af
                © 2019 The Author(s)

                This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

                History
                : 2 July 2019
                : 3 September 2019
                : 23 September 2019
                Categories
                Article

                mollusca,paleontology,paleobiology
                mollusca, paleontology, paleobiology

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