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Berriasella is a discoidal evolute perisphinctacean ammonite, and type genus for the neocomitid subfamily Berriasellinae. Its ribbing is distinct, consisting of both simple and bifurcated ribs that extend from the umbilical seam across the venter; its whorl section generally compressed, the venter more or less narrowly rounded. The species Berriasella jacobi traditionally has been regarded an index fossil defining the base of the Cretaceous, however since 2016 this had been replaced by the first occurrence of Calpionella alpina. Some authors regard B. jacobi as instead belonging to the genus .

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rdf:type
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  • Berriasella (en)
  • Berriasella (eu)
  • Berriasella (pl)
  • 貝利亞斯菊石 (zh)
rdfs:comment
  • Berriasella ongi ezagunak diren ammonite izeneko zefalopodoen artean genero fosil bat da. Jurasiko eta Kretazeoan bizi ziren, Tithoniar eta Berriasiarrean , hau da, orain dela 145 milioi urte inguru. (eu)
  • Berriasella – rodzaj głowonogów z wymarłej podgromady amonitów. Żył na przełomie jury i kredy (tyton - berrias). (pl)
  • 貝利亞斯菊石(學名:Berriasella),又名貝里阿斯菊石,是生存在侏羅紀末提通期至白堊紀初貝里亞期海洋中的一屬菊石,在該段時期的地層中有廣泛的分布,為此兩紀間過渡階段的代表物種之一,其名稱即源自於貝里亞期。牠們是繁盛於侏羅紀的旋菊石類之後裔。其化石被發現於歐洲、中南美和西南亞等地。 (zh)
  • Berriasella is a discoidal evolute perisphinctacean ammonite, and type genus for the neocomitid subfamily Berriasellinae. Its ribbing is distinct, consisting of both simple and bifurcated ribs that extend from the umbilical seam across the venter; its whorl section generally compressed, the venter more or less narrowly rounded. The species Berriasella jacobi traditionally has been regarded an index fossil defining the base of the Cretaceous, however since 2016 this had been replaced by the first occurrence of Calpionella alpina. Some authors regard B. jacobi as instead belonging to the genus . (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Neocomitidae_-_Berriasella_jabronensis.jpg
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