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The Paleocene-Lower Eocene series of the Gafsa basin (South-Central Tunisia): integrated stratigraphy and paleoenvironments

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Abstract

In the Gafsa basin, the Paleocene-Eocene interval is represented by the evaporite deposits of Thelja Formation, the phosphatic series of Chouabine Formation, and the carbonate bed of Kef Eddour Formation. The Thanetian-Ypresian transition lies within the lower unit (C1) of the Chouabine Formation. These different facies characterize circalittoral to margino-littoral paleoenvironments. Sedimentological analyzes of this interval allowed to define eleven genetic sequences. The comparison of these sequences with the global chart of Sneeden and Liu (2010) shows a good correlation with the third-order cycles. In the eastern part of the Gafsa basin (Jebel Chemsi), the Paleocene-Ypresian transition is characterized by a marly-carbonate series deposited in an isolated open marine environment not recording minor relative sea-level changes. The Selandian Pg10 major maximum flooding is detected within the S2 sequence of the Oued Thelja section. The Thanetian-Ypresian transition (55.8 Ma), identified in the S7 sequence of this section, coincides with a major sea-level rise at the origin of phosphate sedimentation onset in the Gafsa basin and around the Kasserine Island.

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Correspondence to Mohamed Slim El Ayachi.

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El Ayachi, M.S., Zagrarni, M.F., Snoussi, A. et al. The Paleocene-Lower Eocene series of the Gafsa basin (South-Central Tunisia): integrated stratigraphy and paleoenvironments. Arab J Geosci 9, 395 (2016). https://doi.org/10.1007/s12517-016-2403-0

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  • DOI: https://doi.org/10.1007/s12517-016-2403-0

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