Number of the records: 1  

Miocene bristlemouths (Teleostei: Stomiiformes: Gonostomatidae) from the Makrilia Formation, Ierapetra, Crete

  1. 1.
    SYSNO ASEP0473704
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleMiocene bristlemouths (Teleostei: Stomiiformes: Gonostomatidae) from the Makrilia Formation, Ierapetra, Crete
    Author(s) Přikryl, Tomáš (GLU-S) RID, SAI, ORCID
    Carnevale, G. (IT)
    Source TitleAcademie des Sciences. Comptes Rendus. Palevol. - : Elsevier Masson - ISSN 1631-0683
    Roč. 16, č. 3 (2017), s. 266-277
    Number of pages12 s.
    Publication formOnline - E
    Languageeng - English
    CountryFR - France
    KeywordsTeleostei ; Gonostomatidae ; Crete ; Neogene ; Tortonian ; Cyclothone gaudanti sp. nov.
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryPaleontology
    Institutional supportGLU-S - RVO:67985831
    UT WOS000398065300006
    EID SCOPUS85009787099
    DOI10.1016/j.crpv.2016.11.004
    AnnotationBristlemouths of the genus Cyclothone are currently regarded as the most abundant vertebrates on Earth. The fossil record seems to suggest that these fishes diversified during the Miocene in the Pacific Ocean, but there is no evidence of their presence in the Miocene of the Atlantic Ocean and Mediterranean basin. A new bristlemouth, Cyclothone gaudanti sp. nov. (Teleostei, Stomiiformes, Gonostomatidae), is described herein based on 16 specimens from the Upper Miocene Makrilia Formation (late Tortonian of Crete, Greece). The small sized species is characterized by light pigmentation, 30–31 (14–15 and 15–16) vertebrae, dorsal fin with 10–13 rays, anal fin with 10–14 rays, premaxilla bearing seven closely spaced teeth, maxilla with 42–55 teeth, epipleurals, and autogenous parhypural. The presence of epipleurals appears to be unique of this Miocene species, and the re-establishment of this ancestral character state may be possibly interpreted as related to a phylogenetic character reversal. Morphological and paleoecological considerations suggest that this species possibly inhabited the upper mesopelagic layer, at depths ranging from 2–300 and 500 meters.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2018
Number of the records: 1  

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