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The Aganane Formation is a Pliensbachian (Early Jurassic) geologic formation in the Azilal Province, central Morocco, known mostly for its rich tracksites (up to 1350 tracks) including footprints of thyreophoran, sauropod and theropod dinosaurs. This formation has been dated to the Pliensbachian stage of the Lower Jurassic, thanks to the find of the ammonite Arieticeras cf. algovianum, indicator of Middle Domerian=Uppermost Pliensbachian) in the upper zone, and lower delimitation by the foraminifers termieri and praecursor (indicators of Carixian=Lower Pliensbachian age). The dinosaur tracksites are all located a few metres below the Pliensbachian-Toarcian limit, being coeval and connected with the lowermost layers of the continental Azilal Formation. The Aganane Formation was also coeva

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  • Aganane Formation (en)
  • تشكل أكنان (ar)
  • Formation d'Aganane (fr)
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  • تشكّل أكنان وقد يردُ في بعض المصادر باسمِ تكوين أكانان أو تشكّل أكانان هو تكوين جيولوجي لبيلينسباشي في المغرب. أُبلغَ عن آثار وحشيات الأرجل و‌ستيغوصوريات من التكوين. (ar)
  • The Aganane Formation is a Pliensbachian (Early Jurassic) geologic formation in the Azilal Province, central Morocco, known mostly for its rich tracksites (up to 1350 tracks) including footprints of thyreophoran, sauropod and theropod dinosaurs. This formation has been dated to the Pliensbachian stage of the Lower Jurassic, thanks to the find of the ammonite Arieticeras cf. algovianum, indicator of Middle Domerian=Uppermost Pliensbachian) in the upper zone, and lower delimitation by the foraminifers termieri and praecursor (indicators of Carixian=Lower Pliensbachian age). The dinosaur tracksites are all located a few metres below the Pliensbachian-Toarcian limit, being coeval and connected with the lowermost layers of the continental Azilal Formation. The Aganane Formation was also coeva (en)
  • La Formation d'Aganane est une formation géologique du Pliensbachien (Jurassique inférieur) dans la Province d'Azilal, centre du Maroc, connue surtout pour sa richesse en pistes (Jusqu'à 1350 pistes) dont des empreintes de Dinosaures Thyréophores, Sauropodes et Théropodes. Cette Formation a été contrainte en âge au stade Pliensbachien du Jurassique inférieur, grâce à la découverte de l'ammonite cf. algovianum Indicateur du Domérien moyen=Pliensbachien supérieur) dans la zone supérieure, et la délimitation inférieure par les foraminifères termieri & praecursor (Indicateurs d'âge Carixien=Pliensbachien inférieur). Les sites à traces de dinosaures sont tous situés à quelques mètres sous la limite Pliensbachien-Toarcien, étant coévalents et connectés avec les couches les plus basses de la F (fr)
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  • Aganane Formation (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/Cast_of_Eubrontes_Gigantis_track_by_Paul_Olsen.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Otozoum_tracks_cropped.jpg
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