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      Reappraisal of the extinct seal “ Phocavitulinoides from the Neogene of the North Sea Basin, with bearing on its geological age, phylogenetic affinities, and locomotion

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          Abstract

          Background

          Discovered on the southern margin of the North Sea Basin, “ Phocavitulinoides represents one of the best-known extinct species of Phocidae. However, little attention has been given to the species ever since its original 19th century description. Newly discovered material, including the most complete specimen of fossil Phocidae from the North Sea Basin, prompted the redescription of the species. Also, the type material of “ Phocavitulinoides is lost.

          Methods

          Phocavitulinoides is redescribed. Its phylogenetic position among Phocinae is assessed through phylogenetic analysis. Dinoflagellate cyst biostratigraphy is used to determine and reassess the geological age of the species. Myological descriptions of extant taxa are used to infer muscle attachments, and basic comparative anatomy of the gross morphology and biomechanics are applied to reconstruct locomotion.

          Results

          Detailed redescription of “ Phocavitulinoides indicates relatively little affinities with the genus Phoca, but rather asks for the establishment of a new genus: Nanophoca gen. nov. Hence, “ Phocavitulinoides is recombined into Nanophoca vitulinoides. This reassignment is confirmed by the phylogenetic analysis, grouping the genus Nanophoca and other extinct phocine taxa as stem phocines. Biostratigraphy and lithostratigraphy expand the known stratigraphic range of N. vitulinoides from the late Langhian to the late Serravallian. The osteological anatomy of N. vitulinoides indicates a relatively strong development of muscles used for fore flipper propulsion and increased flexibility for the hind flipper.

          Discussion

          The extended stratigraphic range of N. vitulinoides into the middle Miocene confirms relatively early diversification of Phocinae in the North Atlantic. Morphological features on the fore- and hindlimb of the species point toward an increased use of the fore flipper and greater flexibility of the hind flipper as compared to extant Phocinae, clearly indicating less derived locomotor strategies in this Miocene phocine species. Estimations of the overall body size indicate that N. vitulinoides is much smaller than Pusa, the smallest extant genus of Phocinae (and Phocidae), and than most extinct phocines.

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          Bioenergetics and the Determination of Home Range Size

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            Home Range, Time, and Body Size in Mammals

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              Pinniped phylogeny and a new hypothesis for their origin and dispersal.

              The relationships and the zoogeography of the three extant pinniped families, Otariidae (sea lions and fur seals), Odobenidae (one extant species, the walrus), and Phocidae (true seals), have been contentious. Here, we address these topics in a molecular study that includes all extant species of true seals and sea lions, four fur seals and the walrus. Contrary to prevailing morphological views the analyses conclusively showed monophyletic Pinnipedia with a basal split between Otarioidea (Otariidae+Odobenidae) and Phocidae. The northern fur seal was the sister to all remaining otariids and neither sea lions nor arctocephaline fur seals were recognized as monophyletic entities. The basal Phocidae split between Monachinae (monk seals and southern true seals) and Phocinae (northern true seals) was strongly supported. The phylogeny of the Phocinae suggests that the ancestors of Cystophora (hooded seal) and the Phocini (e.g. harp seal, ringed seal) adapted to Arctic conditions and ice-breeding before 12 MYA (million years ago) as supported by the white natal coat of these lineages. The origin of the endemic Caspian and Baikal seals was dated well before the onset of major Pleistocene glaciations. The current findings, together with recent advances in pinniped paleontology, allow the proposal of a new hypothesis for pinniped origin and early dispersal. The hypothesis posits that pinnipeds originated on the North American continent with early otarioid and otariid divergences taking place in the northeast Pacific and those of the phocids in coastal areas of southeast N America for later dispersal to colder environments in the N Atlantic and the Arctic Basin, and in Antarctic waters.
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                Author and article information

                Contributors
                Journal
                PeerJ
                PeerJ
                PeerJ
                PeerJ
                PeerJ
                PeerJ Inc. (San Francisco, USA )
                2167-8359
                16 May 2017
                2017
                : 5
                : e3316
                Affiliations
                [1 ]Department of Geology, Ghent University , Ghent, Belgium
                [2 ]O.D. Earth and History of Life, Royal Belgian Institute of Natural Sciences , Brussels, Belgium
                [3 ]Arbeitsgruppe Morphologie und Formengeschichte, Humboldt Universität Berlin , Berlin, Germany
                [4 ]Paläontologisches Institut und Museum, University of Zürich , Zürich, Switzerland
                Author information
                http://orcid.org/0000-0003-1474-9613
                http://orcid.org/0000-0003-0740-5791
                Article
                3316
                10.7717/peerj.3316
                5436577
                28533965
                4a68fc7a-fd55-444d-8af8-0be5b6d32241
                © 2017 Dewaele 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
                : 3 December 2016
                : 14 April 2017
                Funding
                Funded by: FWO Ph.D. Fellowship program
                Funded by: Swiss National Fund SNF
                Award ID: 31003A_149605
                Funded by: Alexander von Humboldt Foundation
                DL was financially supported through the FWO Ph.D. Fellowship program. EA was supported by the Swiss National Fund SNF 31003A_149605 granted to MR Sánchez-Villagra and subsequently by the Alexander von Humboldt Foundation. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
                Categories
                Evolutionary Studies
                Paleontology
                Taxonomy
                Zoology

                phocidae,neogene,north sea basin,belgium,redescription,taxonomy,locomotion

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