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      Unexpected fish diversity gradients in the Amazon basin

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          Abstract

          Atypical fish diversity gradients suggest a recent formation of the Amazon system such as we know it today.

          Abstract

          Using the most comprehensive fish occurrence database, we evaluated the importance of ecological and historical drivers in diversity patterns of subdrainage basins across the Amazon system. Linear models reveal the influence of climatic conditions, habitat size and sub-basin isolation on species diversity. Unexpectedly, the species richness model also highlighted a negative upriver-downriver gradient, contrary to predictions of increasing richness at more downriver locations along fluvial gradients. This reverse gradient may be linked to the history of the Amazon drainage network, which, after isolation as western and eastern basins throughout the Miocene, only began flowing eastward 1–9 million years (Ma) ago. Our results suggest that the main center of fish diversity was located westward, with fish dispersal progressing eastward after the basins were united and the Amazon River assumed its modern course toward the Atlantic. This dispersal process seems not yet achieved, suggesting a recent formation of the current Amazon system.

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          Most cited references54

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          Chronology of fluctuating sea levels since the triassic.

          Advances in sequence stratigraphy and the development of depositional models have helped explain the origin of genetically related sedimentary packages during sea level cycles. These concepts have provided the basis for the recognition of sea level events in subsurface data and in outcrops of marine sediments around the world. Knowledge of these events has led to a new generation of Mesozoic and Cenozoic global cycle charts that chronicle the history of sea level fluctuations during the past 250 million years in greater detail than was possible from seismic-stratigraphic data alone. An effort has been made to develop a realistic and accurate time scale and widely applicable chronostratigraphy and to integrate depositional sequences documented in public domain outcrop sections from various basins with this chronostratigraphic framework. A description of this approach and an account of the results, illustrated by sea level cycle charts of the Cenozoic, Cretaceous, Jurassic, and Triassic intervals, are presented.
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            The Phanerozoic record of global sea-level change.

            K. Miller (2005)
            We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 +/- 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10(4)- to 10(6)-year scale, but a link between oxygen isotope and sea level on the 10(7)-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present).
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              A comprehensive framework for global patterns in biodiversity

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                Author and article information

                Journal
                Sci Adv
                Sci Adv
                SciAdv
                advances
                Science Advances
                American Association for the Advancement of Science
                2375-2548
                September 2019
                11 September 2019
                : 5
                : 9
                : eaav8681
                Affiliations
                [1 ]UMR EDB (Laboratoire Évolution et Diversité Biologique), CNRS 5174, IRD253, UPS; 118 route de Narbonne, F-31062 Toulouse, France.
                [2 ]Departamento de Ecologia, Universidade de Brasília, Brasilia, DF, Brazil.
                [3 ]University of Louisiana at Lafayette, Lafayette, LA 70504, USA.
                [4 ]Center for Global Change and Earth Observations, Michigan State University, East Lansing, MI 48824, USA.
                [5 ]Museo de Historia Natural Alcide d’Orbigny, Av. Potosí 1458, zona Queru Queru, Cochabamba, Estado Plurinacional de Bolivia.
                [6 ]Department of Freshwater Biology, Royal Belgian Institute of Natural Sciences, Vautierstraat 29, B-1000 Brussels, Belgium.
                [7 ]Department of Biology, University of Ghent, K.L. Ledeganckstraat 35, B-9000 Ghent, Belgium.
                [8 ]Research Institute for Nature and Forrest (INBO), Havenlaan 88 bus 73, 1000 Brussels, Belgium.
                [9 ]Universidade Federal de Minas Gerais (UFMG), Instituto de Ciências Biológicas, Av. Antônio Carlos, 6627 Belo Horizonte, MG, Brazil.
                [10 ]Departamento de Ictiología, Museo de Historia Natural, Universidad Nacional Mayor San Marcos, Lima, Perú.
                [11 ]UMR MARBEC (CNRS, IRD, IFREMER, UM), Université de Montpellier, Montpellier Cedex 5, France.
                [12 ]Unidad de Limnología y Recursos Acuáticos, Universidad Mayor de San Simón, Calle Sucre y Parque La Torre s/n, Cochabamba, Bolivia.
                [13 ]Unidad de Ecología y Sistemática (UNESIS), Laboratorio de Ictiología, Departamento de Biología, Facultad de Ciencias, Pontificia Universidad Javeriana, Bogotá, Colombia.
                [14 ]Departamento de Ictiología, Museo Nacional de Historia Natural, La Paz, Bolivia.
                [15 ]Universidade Federal de São Paulo, Instituto do Mar, Campus Baixada Santista, Rua Doutor Carvalho de Mendonça, 144, Encruzilhada, 11070-100 Santos, SP, Brazil.
                [16 ]Department of Wildlife and Fisheries Sciences, Texas A&M University, College Station, TX 77840, USA.
                [17 ]Instituto Nacional de Pesquisas da Amazônia, Coordenação de Biodiversidade, Avenida André Araújo, 2936, Petrópolis, 69067-375 Manaus, AM, Brazil.
                Author notes
                [* ]Corresponding author. Email: thierry.oberdorff@ 123456ird.fr (T.O.); murilosd@ 123456hotmail.com (M.S.D.)
                [†]

                Deceased.

                Author information
                http://orcid.org/0000-0001-7323-2599
                http://orcid.org/0000-0002-7213-5284
                http://orcid.org/0000-0003-0687-1467
                http://orcid.org/0000-0002-9752-1499
                http://orcid.org/0000-0002-9110-490X
                http://orcid.org/0000-0002-8858-6426
                http://orcid.org/0000-0002-0071-5159
                http://orcid.org/0000-0003-1843-5662
                http://orcid.org/0000-0002-8112-5635
                http://orcid.org/0000-0003-3024-237X
                http://orcid.org/0000-0001-8680-973X
                http://orcid.org/0000-0002-4396-2598
                http://orcid.org/0000-0002-5588-5956
                http://orcid.org/0000-0001-5972-5928
                http://orcid.org/0000-0002-2048-7691
                http://orcid.org/0000-0003-0236-5129
                http://orcid.org/0000-0001-8354-2750
                Article
                aav8681
                10.1126/sciadv.aav8681
                6739107
                31535018
                eca00cc6-36a7-4ab3-b41b-56443a051193
                Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

                This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial license, which permits use, distribution, and reproduction in any medium, so long as the resultant use is not for commercial advantage and provided the original work is properly cited.

                History
                : 27 October 2018
                : 08 August 2019
                Funding
                Funded by: doi http://dx.doi.org/10.13039/100000001, National Science Foundation;
                Award ID: 0614334
                Funded by: doi http://dx.doi.org/10.13039/501100001665, Agence Nationale de la Recherche;
                Award ID: ANR-10-LABX-25-01, ANR-10-LABX-41, ANR-11-IDEX-0002-02
                Funded by: doi http://dx.doi.org/10.13039/501100002322, Coordenação de Aperfeiçoamento de Pessoal de Nível Superior;
                Award ID: 6632/14-9
                Funded by: doi http://dx.doi.org/10.13039/501100003593, Conselho Nacional de Desenvolvimento Científico e Tecnológico;
                Award ID: 313183/2014-7
                Funded by: doi http://dx.doi.org/10.13039/501100003593, Conselho Nacional de Desenvolvimento Científico e Tecnológico;
                Award ID: 150784/2015-5
                Funded by: doi http://dx.doi.org/10.13039/501100004916, Fundação de Amparo à Pesquisa do Estado do Amazonas;
                Award ID: PAREV/FAPEAM 019/2010
                Funded by: Fundação de Amparo à Pesquisa do Estado de São Paulo;
                Award ID: 2016/07910-0
                Funded by: European Union - Latin America and Caribbean;
                Award ID: ELAC2014/ DCC-0210
                Funded by: EU ERA-NET BiodivERsA;
                Award ID: 3-2015-26
                Funded by: Fundação de Amparo à Pesquisa do Estado do Pará;
                Award ID: ICAAF #094/2016
                Categories
                Research Article
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                SciAdv r-articles
                Ecology
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                Judith Urtula

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