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. 2020 Apr 21;928:1–216. doi: 10.3897/zookeys.928.47517

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Nizar Ibrahim, Paul C. Sereno, David M. Varrricchio, David M. Martill, Didier B. Dutheil, David M. Unwin, Lahssen Baidder, Hans C. E. Larsson, Samir Zouhri, Abdelhadi Kaoukaya

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Figure 34. — Geology and paleontology at the boundary between the Douira Formation and the Gara Sbaa Member of the Cenomanian-Turonian limestone at Gara Sbaa. A Marly limestone separating the Kem Kem Group from the Cenomanian-Turonian limestone B Close-up of a basal limestone unit in the Gara Sbaa Member C Oyster fossil in situ in the basal limestone D Deep-bodied teleost (Diplomystus sp.) from the Gara Sbaa Member of the Cenomanian-Turonian limestone E Long-bodied teleost (Agoultichthys chattertoni) showing preservation of soft fin structures from the Gara Sbaa Member (Murray and Wilson 2009) D and E from Martill et al. (2011). Scale bars equal 1 cm in D and 2 cm in E.