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    Review of 'Insights on the Cenozoic Geology of North Beirut (Harbour Area): Biostratigraphy; Sedimentology and Structural history'

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    Insights on the Cenozoic Geology of North Beirut (Harbour Area): Biostratigraphy; Sedimentology and Structural historyCrossref
    A timely new paper on the geology of North Beirut
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        Rated 4.5 of 5.
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        Rated 4 of 5.
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        Rated 4 of 5.
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        Rated 4 of 5.
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        Rated 5 of 5.
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    Insights on the Cenozoic Geology of North Beirut (Harbour Area): Biostratigraphy; Sedimentology and Structural history

    The biostratigraphy and sedimentology of the outcrops and bedrock exposed in archaeological excavations around the harbour area of Beirut (~5 km 2 ) unlock the geological and structural history of that area, which in turn are key to understanding the hydrocarbon and hydrogeological potential of the region. A key location (Site 2) of a studied outcrop section and newly uncovered bedrock is on the northern foothill cliff of East Beirut (Achrafieh). The outcrop section of carbonates is of Eocene beds overlain by conformable Miocene beds. The excavation of the slope bordering the outcrop uncovers a bedrock section of an early Pliocene shoreline of carbonate/siliciclastic sands at its base and a beach-rock structure at top. The age of the shoreline section is dated by an assemblage of planktonic foraminifera including Sphaeroidinellopsis subdehiscens , Sphaeroidinella dehiscens , and Orbulina universa. The Eocene carbonates of Site 2 extend the coverage of the previously reported Eocene outcrops in the harbour area. They form a parasequence of thin bedded chalky white limestones that includes the youngest fossil fish deposits in Lebanon ( Bregmaceros filamentosus ). The deposits are dated as early Priabonian by their association with the planktonic foraminiferal assemblage of Porticulasphaera tropicalis , Globigerinatheka barri , Dentoglobigerina venezuelana, Globigerina praebulloides , Turborotalia centralis and Borelis sp. The Middle Miocene carbonates that conformably overlie the early Priabonian parasequence, include a planktonic foraminiferal assemblage of Globigerinoides trilobus, Orbulina universa and Borelis melo. Elsewhere, in the harbour area, the preserved Eocene limestones are equally directly overlain by conformable Miocene carbonate parasequences of the Langhian - Serravallian age. Younger argillaceous limestone beds of the Mio/Pliocene age occur in the eastern central part of the harbour area and enclose an assemblage of Truncorotalia crassaformis , Globorotalia inflata , and Orbulina universa . The three markers of old and recently raised structural blocks in the harbour area are a Lutetian/Bartonian marine terrace in the south west corner, a lower Pliocene shoreline carbonate section in the north east side and a Holocene raised beach of marine conglomerates in the north east corner of the area. The locations of these paleo-shorelines, less than 2 kms apart, indicate a progressive platform narrowing of North Beirut since the Paleogene. This study underpins the geological complexity of the region and contributes to understanding the underlying geology which will be needed for future archaeological, hydrocarbon and hydrogeological exploration.
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      Review information

      10.14293/S2199-1006.1.SOR-EARTH.AW89XA.v1.RRAJFF

      This work has been published open access under Creative Commons Attribution License CC BY 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Conditions, terms of use and publishing policy can be found at www.scienceopen.com.

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      Review text

      Insights on the Cenozoic Geology of North Beirut (Harbour Area): Biostratigraphy; Sedimentology and Structural history

       

      I have now completed my review of the above paper by Germaine Noujaim Clark and Marcelle Boudagher-Fadel. The manuscript presents new geological data from the ancient harbour area of Beirut. The authors describe, for the first time, unreported Eocene carbonates, Eocene fish deposits, old and young Cenozoic shorelines by the eastern foothill of Beirut West, and northern foothill of Beirut East. The sequences are dated using fossil assemblages, with a particular focus on the micropalaeontology.  The paper is well structured and nicely illustrated, and the arguments set forward by the authors are both convincing and pertinent. In sum, I fully support the publication of the paper in UCL Open: Environment.

       

      Missing references

      Marriner, N., Morhange, C. & Beydoun, M. (2008) Geoarchaeology of Beirut’s ancient harbour, Phoenicia. Journal of Archaeological Science, 35, 2495-2516.

       

      Throughout the paper, it would be interesting to place some percentage estimates on the different fossil assemblages described.

       

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