Abstract
Globally, the Paleogene period experienced several events marking the Paleocene-Eocene transition which is especially to one of the hottest periods that the Earth has ever known (Paleocene-Eocene Thermal Maximum, PETM), followed by the biological crisis that affected benthic foraminifera. The Bekrit Syncline, subject of this study, shows three Formations of range from the Cretaceous to the Eocene ages (the El Koubbat, Irbzer and Bekrit-Timahdite Formations). Sedimentological, palynological and geochemical analyses of collected samples, in the Bekrit syncline, were studied to determine the paleogeographic and paleoenvironmental conditions of the Middle Atlas. The carbonate rocks were analyzed by microscopic study and geochemical analysis by X-ray Fluorescence (XF) and Inductively Coupled Plasma Spectrometry (ICP). The results obtained highlight the sedimentary events that took place during the Paleogene. Thus, the Maastrichtian is characterized by a closed euxinic marine environment shared by a more open and oxidizing environment. On the other hand, the Paleocene was a restricted marine environment with evaporitic sedimentation, while the Eocene sees the installation of a carbonate platform with a bioclastic Shoal.
Highlights
The Meso-cenozoic deposits of the Moroccan Middle Atlas correspond to a shallow shelf marine environment [1] [2]
The carbonate rocks were analyzed by microscopic study and geochemical analysis by X-ray Fluorescence (XF) and Inductively Coupled Plasma Spectrometry (ICP)
This period shelters the KT (Cretaceous-Tertiary) crisis and the climatic crisis of the Paleocene-Eocene transition. The latter is responsible for global warming of the Earth (≈+5 ̊C), global change in the ocean circulation pattern and for the quick extinction of benthic Foraminifera [13]. This crisis is known among scientists by the name “Paleocene-Eocene Thermal Maximum (PETM)” (Paleocene Eocene Thermal Maximum)
Summary
The Meso-cenozoic deposits of the Moroccan Middle Atlas correspond to a shallow shelf marine environment [1] [2]. The Paleogene, the subject of this study, represented an important period of geological history on the scale of the Earth This period shelters the KT (Cretaceous-Tertiary) crisis and the climatic crisis of the Paleocene-Eocene transition. The latter is responsible for global warming of the Earth (≈+5 ̊C), global change in the ocean circulation pattern and for the quick extinction of benthic Foraminifera [13]. This crisis is known among scientists by the name “PETM” (Paleocene Eocene Thermal Maximum)
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