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New marine reptile fossils from the Oxfordian (Late Jurassic) of Greenland

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    Resumé

    Knowledge about marine reptile diversity and disparity during the Late Jurassic is increasing. This contribution describes marine reptile skeletal elements (ichthyosaur and plesiosaur) from Kingofjeld mountain in NE Greenland. The assemblage is early Late Oxfordian (Late Jurassic) in age, and consists of c. 100 disarticulated skeletal elements. The location is of biogeographic importance as it was at the time situated between the Boreal realm and the Tethys Sea and is promising in terms of future prospecting.

    OriginalsprogEngelsk
    Sider (fra-til)1612-1621
    Antal sider10
    TidsskriftGeological Magazine
    Vol/bind157
    Udgave nummer10
    DOI
    StatusUdgivet - 1 okt. 2020

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