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

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            Abstract

            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.

            Content

            Author and article information

            Journal
            UCL Open: Environment Preprint
            UCL Press
            13 August 2019
            Affiliations
            [1 ] : Independent Consultant geologist and Research associate to Lebanon National Council for Scientific Research, Lebanon
            [2 ] Office of the Vice-Provost (Research), University College London, 2 Taviton Street, London WC1H 0BT, UK
            Article
            10.14324/111.444/000018.v1
            e3b3a474-10a7-4590-9bdd-f273eef65a59

            This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY) 4.0 https://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, distribution and reproduction in any medium, provided the original author and source are credited.

            Comments

            Decision date: 13/8/2019

            Handling Editor: Dan Osborn

            This article is a preprint article and has not been peer-reviewed. It is under consideration following submission to UCL Open: Environment Preprint for open peer review.

            2020-09-23 15:12 UTC
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