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  2. Ammonoidea - Wikipedia

    en.wikipedia.org/wiki/Ammonoidea

    Iridescent ancient ammonite fossil on display at the American Museum of Natural History, New York City, around 2 feet in diameter. The Ammonoidea can be divided into six orders, listed here starting with the most primitive and going to the more derived: Agoniatitida, Lower Devonian – Middle Devonian; Clymeniida, Upper Devonian

  3. Ammolite - Wikipedia

    en.wikipedia.org/wiki/Ammolite

    An iridescent ammonite from Madagascar Map of North America highlighting the shallow inland sea present during the mid-Cretaceous period. Ammolite comes from the fossil shells of the Upper Cretaceous disk-shaped ammonites Placenticeras meeki and Placenticeras intercalare, and (to a lesser degree) the cylindrical baculite, Baculites compressus.

  4. List of ammonite genera - Wikipedia

    en.wikipedia.org/wiki/List_of_ammonite_genera

    This list of ammonites is a comprehensive listing of genera that are included in the subclass †Ammonoidea, excluding purely vernacular terms. The list includes genera that are commonly accepted as valid, as well as those that may be invalid or doubtful ( nomina dubia ), or were not formally published ( nomina nuda ), as well as junior ...

  5. Douvilleiceras - Wikipedia

    en.wikipedia.org/wiki/Douvilleiceras

    Douvilleiceras is a genus of ammonites from the Middle to Late Cretaceous. Its fossils have been found worldwide, in Africa, Asia, Europe, and North and South America.

  6. Parapuzosia seppenradensis - Wikipedia

    en.wikipedia.org/wiki/Parapuzosia_seppenradensis

    Parapuzosia seppenradensis is the largest known species of ammonite. [1] It lived during the Lower Campanian Epoch of the Late Cretaceous period, in marine environments in what is now Westphalia, Germany. A specimen, found in Seppenrade near Lüdinghausen, Germany in 1895 measures 1.8 m (5.9 ft) in diameter, although the living chamber is ...

  7. Sphenodiscus - Wikipedia

    en.wikipedia.org/wiki/Sphenodiscus

    The ventral edge of the shell tends to be sharply angled. The outer surface is generally smooth in fossil specimens, although certain species at different stages of ontogenic development may possess many small tubercles along their surfaces. [11] Sphenodiscus had a complex suture pattern with many small branching lobes and saddles.