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      A novel approach to study the morphology and chemistry of pollen in a phylogenetic context, applied to the halophytic taxon Nitraria L.(Nitrariaceae)

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          Abstract

          Nitraria is a halophytic taxon (i.e., adapted to saline environments) that belongs to the plant family Nitrariaceae and is distributed from the Mediterranean, across Asia into the south-eastern tip of Australia. This taxon is thought to have originated in Asia during the Paleogene (66–23 Ma), alongside the proto-Paratethys epicontinental sea. The evolutionary history of Nitraria might hold important clues on the links between climatic and biotic evolution but limited taxonomic documentation of this taxon has thus far hindered this line of research. Here we investigate if the pollen morphology and the chemical composition of the pollen wall are informative of the evolutionary history of Nitraria and could explain if origination along the proto-Paratethys and dispersal to the Tibetan Plateau was simultaneous or a secondary process. To answer these questions, we applied a novel approach consisting of a combination of Fourier Transform Infrared spectroscopy (FTIR), to determine the chemical composition of the pollen wall, and pollen morphological analyses using Light Microscopy (LM) and Scanning Electron Microscopy (SEM). We analysed our data using ordinations (principal components analysis and non-metric multidimensional scaling), and directly mapped it on the Nitrariaceae phylogeny to produce a phylomorphospace and a phylochemospace. Our LM, SEM and FTIR analyses show clear morphological and chemical differences between the sister groups Peganum and Nitraria. Differences in the morphological and chemical characteristics of highland species ( Nitraria schoberi, N. sphaerocarpa, N. sibirica and N. tangutorum) and lowland species ( Nitraria billardierei and N. retusa) are very subtle, with phylogenetic history appearing to be a more important control on Nitraria pollen than local environmental conditions. Our approach shows a compelling consistency between the chemical and morphological characteristics of the eight studied Nitrariaceae species, and these traits are in agreement with the phylogenetic tree. Taken together, this demonstrates how novel methods for studying fossil pollen can facilitate the evolutionary investigation of living and extinct taxa, and the environments they represent.

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          Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2.

          The sudden, widespread glaciation of Antarctica and the associated shift towards colder temperatures at the Eocene/Oligocene boundary (approximately 34 million years ago) (refs 1-4) is one of the most fundamental reorganizations of global climate known in the geologic record. The glaciation of Antarctica has hitherto been thought to result from the tectonic opening of Southern Ocean gateways, which enabled the formation of the Antarctic Circumpolar Current and the subsequent thermal isolation of the Antarctic continent. Here we simulate the glacial inception and early growth of the East Antarctic Ice Sheet using a general circulation model with coupled components for atmosphere, ocean, ice sheet and sediment, and which incorporates palaeogeography, greenhouse gas, changing orbital parameters, and varying ocean heat transport. In our model, declining Cenozoic CO2 first leads to the formation of small, highly dynamic ice caps on high Antarctic plateaux. At a later time, a CO2 threshold is crossed, initiating ice-sheet height/mass-balance feedbacks that cause the ice caps to expand rapidly with large orbital variations, eventually coalescing into a continental-scale East Antarctic Ice Sheet. According to our simulation the opening of Southern Ocean gateways plays a secondary role in this transition, relative to CO2 concentration.
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            Glossary of pollen and spore terminology

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              Orographic Controls on Climate and Paleoclimate of Asia: Thermal and Mechanical Roles for the Tibetan Plateau

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                Author and article information

                Contributors
                Journal
                PeerJ
                PeerJ
                peerj
                peerj
                PeerJ
                PeerJ Inc. (San Francisco, USA )
                2167-8359
                19 July 2018
                2018
                : 6
                : e5055
                Affiliations
                [1 ]University of Amsterdam, Institute for Biodiversity and Ecosystem Dynamics (IBED) , Amsterdam, The Netherlands
                [2 ]University of Potsdam, Institute of Earth and Environmental Science , Potsdam, Germany
                [3 ]University of Münster, Institute of Geology and Palaeontology , Münster, Germany
                [4 ]Universidad Distrital Francisco José de Caldas, Facultad del Medio Ambiente y Recursos Naturales , Bogotá, Colombia
                [5 ]Key Laboratory of Biogeography and Bioresource in Arid Land, Xinjiang Institute of Ecology and Geography, China Academy of Sciences , Urumqi, China
                [6 ]Gothenburg Global Biodiversity Centre , Göteborg, Sweden
                [7 ]University of Gothenburg, Department of Biological and Environmental Sciences , Göteborg, Sweden
                [8 ]Gothenburg Botanical Garden , Göteborg, Sweden
                [9 ]Harvard University, Department of Organismic and Evolutionary Biology , Cambridge, MA, United States of America
                [10 ]Maastricht University, Maastricht Science Programme , Maastricht, The Netherlands
                [11 ]Université de Rennes, Geosciences Rennes UMR-CNRS , Rennes, France
                Article
                5055
                10.7717/peerj.5055
                6054868
                ef775d1d-4fe8-482d-b447-19e957dfe4b7
                ©2018 Woutersen 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
                : 7 March 2018
                : 1 June 2018
                Funding
                Funded by: ERC consolidator
                Award ID: MAGIC 649081
                Funded by: Swedish Research Council
                Award ID: 2015-04748
                Funded by: Knut and Alice Wallenberg Foundation, the Swedish Research Council
                Award ID: B0569601
                Funded by: The Swedish Foundation for Strategic Research
                Funded by: The Faculty of Sciences at the University of Gothenburg
                Funded by: The David Rockefeller Center for Latin American Studies at Harvard University
                Guillaume Dupont-Nivet received ERC consolidator grant MAGIC 649081, which also provided funding for Phillip E. Jardine. Daniele Silvestro received funding from the Swedish Research Council (2015-04748). Alexandre Antonelli is supported by the Knut and Alice Wallenberg Foundation, the Swedish Research Council (B0569601), the Swedish Foundation for Strategic Research, the Faculty of Sciences at the University of Gothenburg, and the David Rockefeller Center for Latin American Studies at Harvard University. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
                Categories
                Biogeography
                Evolutionary Studies
                Molecular Biology
                Paleontology

                ftir,lm,sem,paratethys,tibet,sporopollenin,mediterranean,steppe-desert,australia,palynology

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