No abstract

No abstract

The Marmoucha syncline is located in the eastern part of the Middle Atlas. In this syncline, the “Gypsum marls” (Bathonian-? Callovian) are covered by red detrital deposits which outcrop in Aït Bazza locality. The upper limit of these detrital deposits is below the transgressional unconformity of the Albian? - Cenomanian marine series. The present work introduces a synthesis of stratigraphical, sedimentological and micropalaeontological studies, which has led to new dating and to the identification of different depositional environments. These results have allowed us to define a new chrono-lithostratigraphic unit, the "Aït Bazza Formation", which comprises three superimposed members (AB1, 2 and 3 Mbs) separated by two sedimentary discontinuities. This formation, exceeding 300m in thickness, is formed by conglomerate, sandstone, sand and varicolored marls. Micropalaeontological bulk sampling in marly horizons revealed associations of charophytes and ostracods, particularly in member 2 (AB2 Mb). The charophytes are represented by oogonia of small Porocharaceae, Clavatoraceae such as Globator rectispirale, Dictyoclavator ramalhoi, and Nodosoclavator bradleyi that characterize the Tithonian. The ostracod microfauna is diverse, consisting of non-marine and lagoonal- shallow marine species at several horizons, associated with sea urchin spines and rare foraminifera, which indicating fluvio-deltaic sedimentary environments subjected to marine influences. This new age contraints of AB2 Mb to the Late Jurassic, and the discovery of marine influences in this eastern part of the folded Middle Atlas, consequently indicates the existence of palaeogeographical connections with the Tethyan domain located to the NE in the Rif foreland.