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<document id="921099E5DECDF2138233FC4367672110" ID-CLB-Dataset="305606" ID-DOI="10.5852/cr-palevol2023v22a35" ID-GBIF-Dataset="dc3e7628-5a2c-4555-b7c7-44c8eb16335d" ID-ISSN="1777-571X" ID-Zenodo-Dep="14232601" ID-ZooBank="urn:lsid:zoobank.org:pub:E41471F9-7425-482F-9A32-118346B7FC66" IM.bibliography_approvedBy="julia" IM.illustrations_approvedBy="julia" IM.materialsCitations_approvedBy="julia" IM.metadata_approvedBy="julia" IM.tables_approvedBy="julia" IM.taxonomicNames_approvedBy="julia" IM.treatmentCitations_approvedBy="felipe" IM.treatments_approvedBy="julia" checkinTime="1732634920582" checkinUser="felipe" docAuthor="Métais, Grégoire, Coster, Pauline, Licht, Alexis, Ocakoğlu, Faruk &amp; Beard, K. Christopher" docDate="2023" docId="03B687A8FFBCDF43FC37FE6B611622E5" docLanguage="en" docName="CRPalevol.22.35.711-727.pdf" docOrigin="Comptes Rendus Palevol 22 (35)" docSource="http://dx.doi.org/10.5852/cr-palevol2023v22a35" docStyle="DocumentStyle:DACF86F01658A8850E13A63D98C287FD.1:CRPalevol.2020-.journal_article" docStyleId="DACF86F01658A8850E13A63D98C287FD" docStyleName="CRPalevol.2020-.journal_article" docStyleVersion="1" docTitle="Iberomeryx Gabunia 1964" docType="treatment" docVersion="4" lastPageNumber="714" masterDocId="FF8FFFD0FFB9DF46FF8EFFDC643C2612" masterDocTitle="Additions to the late Eocene Süngülü mammal fauna in Easternmost Anatolia and the Eocene-Oligocene transition at the periphery of Balkanatolia" masterLastPageNumber="727" masterPageNumber="711" pageNumber="714" updateTime="1732826742167" updateUser="ExternalLinkService" zenodo-license-document="CC-BY-4.0">
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<mods:title id="0181D1DC47B8B3705F35D214ADA6987C">Additions to the late Eocene Süngülü mammal fauna in Easternmost Anatolia and the Eocene-Oligocene transition at the periphery of Balkanatolia</mods:title>
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<mods:namePart id="21EBA2C95C3A1E49A7DB46124B14493B">Métais, Grégoire</mods:namePart>
<mods:affiliation id="4AEF11B4A1915D2F8055A351D65FF5D9">Centre de Recherche en Paléontologie - Paris (CR 2 P), CNRS, Sorbonne Université, Muséum national dHistoire naturelle, case postale 38, 57 rue Cuvier, F- 75231 Paris, cedex 05 (France) gregoire. metais @ mnhn. fr (corresponding author)</mods:affiliation>
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<mods:namePart id="DD122A2C089D4181E18F3B8DB05B4E66">Coster, Pauline</mods:namePart>
<mods:affiliation id="5B2FCD6AFCAFB3A35B0BA47043997918">Réserve Naturelle Nationale Géologique du Luberon, Parc naturel régional du Luberon, Luberon UNESCO Global Geopark, 60 Place Jean Jaurès, F- 84400 Apt (France) pauline. coster @ parcduluberon. fr</mods:affiliation>
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<mods:namePart id="BECB87F5C1638F34177A5B94DC623C6A">Licht, Alexis</mods:namePart>
<mods:affiliation id="1298EA9F16566D9EBF7A96405F10B339">CEREGE, Technopole Environnement Arbois-Méditerranée, Aix Marseille University, CNRS, IRD, INRAE, CEREGE, BP 80, 13545 Aix-en-Provence, cedex 04 (France) licht @ cerege. fr</mods:affiliation>
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<mods:namePart id="59D60DA3BF6871618215F46DC9682104">Ocakoğlu, Faruk</mods:namePart>
<mods:affiliation id="C2507CEE681AA012763666B8E37F35A0">Department of Geological Engineering, Eskişehir Osmangazi University, Meşelik Yerleşkesi, 26040, Odunpazarı, Eskişehir (Turkey) focakoglu @ gmail. com</mods:affiliation>
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Genus
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<emphasis id="B96BEAACFFBCDF43FB88FE6B604527C3" box="[1030,1145,439,465]" italics="true" pageId="5" pageNumber="714">Iberomeryx</emphasis>
<bibRefCitation id="EF8E4B4FFFBCDF43FBF1FE6B611F27C3" author="GABUNIA L. K." box="[1151,1315,439,465]" pageId="5" pageNumber="714" pagination="1 - 267" refId="ref12937" refString="GABUNIA L. K. 1964. - Benara fauna of Oligocene vertebrates. &quot; Metsniereba &quot; Press: 1 - 267." type="book chapter" year="1964">Gabunia, 1964</bibRefCitation>
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<emphasis id="B96BEAACFFBCDF43FCA3FE2C67A9241A" box="[813,917,496,520]" italics="true" pageId="5" pageNumber="714">Iberomeryx</emphasis>
<bibRefCitation id="EF8E4B4FFFBCDF43FC15FE2C6058241A" author="GABUNIA L. K." box="[923,1124,496,520]" pageId="5" pageNumber="714" pagination="1 - 267" refId="ref12937" refString="GABUNIA L. K. 1964. - Benara fauna of Oligocene vertebrates. &quot; Metsniereba &quot; Press: 1 - 267." type="book chapter" year="1964">Gabunia, 1964: 179</bibRefCitation>
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.
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. —
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<emphasis id="B96BEAACFFBCDF43FC59FDFC60BF2425" box="[983,1155,544,568]" italics="true" pageId="5" pageNumber="714">Iberomeryx parvus</emphasis>
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.
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(from
<bibRefCitation id="EF8E4B4FFFBCDF43FC6AFD8C60FA2475" author="MENNECART B. &amp; AIGLSTORFER M. &amp; LI Y. &amp; WANG S. - Q." box="[996,1222,591,615]" pageId="5" pageNumber="714" refId="ref14773" refString="MENNECART B., AIGLSTORFER M., LI Y. &amp; WANG S. - Q. 2021. - Ruminants reveal Eocene Asiatic palaeobiogeographical provinces as the origin of diachronous mammalian Oligocene dispersals into Europe. Scientific Report 11: 17710. https: // doi. org / 10.1038 / s 41598 - 021 - 96221 - x" type="journal volume" year="2021">
Mennecart
<emphasis id="B96BEAACFFBCDF43FBD6FD8C60B52475" box="[1112,1161,591,615]" italics="true" pageId="5" pageNumber="714">et al.</emphasis>
2021
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). — Small-sized ruminant with upper molars possessing the following combination of characters: well-marked parastyle and mesostyle in small-column shape; strong paracone rib; metacone rib absent; metastyle absent; unaligned external walls of metacone and paracone; strong postprotocrista stopping against the anterior side of the premetaconulecrista; continuous lingual cingulum, stronger under the protocone. Lower dental formula is primitive (3-1-4-3) with non-molarized premolars. Tooth c is adjacent to i3. Tooth p1 is single-rooted, reduced and separated from c and p2 by short diastemata. The premolars have a well-developed anterior conid. Teeth p2-p3 display a distally bifurcated mesolabial conid. Tooth p3 is the largest premolar. Tooth p4 displays no mesolingual conid and a large posterior valley. Regarding the lower molars, the trigonid and talonid are lingually open with a trigonid more tapered than the talonid. The anterior fossa is open, due to a forward orientation of the preprotocristid and the presence of a paraconid. The internal postprotocristid is oblique and the external postprotocristid reaches the prehypocristid. The internal postprotocristid, postmetacristid and preentocristid are fused and Yshaped. Protoconid and metaconid display a weak
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<emphasis id="B96BEAACFFBCDF43FA85FB9A6167224C" box="[1291,1371,1094,1118]" italics="true" pageId="5" pageNumber="714">Tragulus</emphasis>
Brisson, 1762
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fold and a well-developed
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<emphasis id="B96BEAACFFBCDF43FBD7FBBC60E7226A" box="[1113,1243,1120,1144]" italics="true" pageId="5" pageNumber="714">Dorcatherium</emphasis>
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fold, respectively. The mandible displays a regularly concave ventral profile in lateral view, a marked incisura vasorum, a strong mandibular angular process, a vertical ramus, and a stout condylar process.
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. — Benara,
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, late Oligocene.
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