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Geological Setting, Palaeoenvironment and Archaeology of the Red Sea pp 341–365Cite as

Pleistocene Coral Reef Terraces on the Saudi Arabian Side of the Gulf of Aqaba, Red Sea

Abstract

A major geomorphic feature of the coastal Red Sea region is represented by Pleistocene raised marine terraces that occur on both sides of the Gulf of Aqaba. Those bordering the Saudi Arabian sector have received little attention thus far, and are comparatively less known than their counterparts in the Sinai sector of the Gulf and in the Red Sea. As is the rule in the Red Sea region, the best developed marine terrace system is reefal and pertains to the last interglacial (Marine Isotope Stage 5e = MIS5e, ~125 ka BP), although older Pleistocene terraces also occur. All such deposits are very fossiliferous and most carbonates are relatively unaltered, providing suitable material for geochronological purposes. Syndepositional marine botryoidal aragonite cements have been identified infilling vugs in the host bedrock at some sites. In some respect, the MIS5e deposits are unique, reflecting the structurally-controlled bedrock geology and the Gulf’s topography. The Gulf of Aqaba is rather narrow and characterized by steep and precipitous topography along its flanks. Coastal marine deposits commonly plaster the crystalline Arabian basement which faces the present seashore, extending from the Jordan border to almost two thirds of the coastal strip. Terraces sitting on this basement have been tectonically uplifted to considerable altitudes (up to 26 m) over the present mean sea level (m.s.l.). The bulk of the marine deposits represent upper fore-reef to beach settings, with better developed back-reef to lagoonal facies only preserved in those favourable conditions (wadi valleys) where sufficient accommodation space was available during the MIS5e to allow inland marine expansion. This is observed in the north at Al Wasel, and ~14 km south of Ra’s Suwayhil as Saghir. The terraces further to the south lie instead over a more recent bedrock, including Miocene sedimentary strata. Here MIS5e deposits are found close to standard altitudes between ~4–8 m above present m.s.l., and preserve shallow reefal habitats, as seen at Ash Shaykh Humayd. A rare example of a putative MIS5e salina-mangal complex has been identified in the area of Ra’s Suwayhil as Saghir at ~23 m above m.s.l.

Keywords

  • Pleistocene Coral
  • Coral Terraces
  • Marine Isotope Stage 5e (MIS5e)
  • Botryoidal Aragonite
  • Saghir

These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Acknowledgements

We thank the Saudi Geological Survey for the invitation to present this study at the ‘2nd Red Sea Book Workshop’ held in Jeddah on February 2016. The expedition in the Gulf of Aqaba has been promoted and funded by the Saudi Geological Survey in Jeddah. We acknowledge all participants to the Winter 2013 Field Party SGS personnel for field work (Ali Saeedi, Abdulnasser Al-Qutub, Salem Al-Nomani, Nawaf Widinly, Mostafa Khorshid, Thamer Bakarman) and post-expedition sample processing (Adel Jarees, Ali Al-Tharowi, Mohamed M. Bin Himd, Hassan Khamis Ali). Abdulnasser Al-Qutub was also part of the diving team and responsible for underwater photography. We thank Francesca Bosellini for helping with coral identification. Michele Morsilli and two anonymous referees provided valuable critical comments. This paper is part of PRIN2012 Programme (Project 20125JKANY_002, Principal Investigator Marco Ligi) and is Ismar-CNR, Bologna, scientific contribution no. 1905.

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Authors and Affiliations

  1. Istituto di Scienze Marine (ISMAR-CNR), Via Gobetti 101, 40129, Bologna, Italy

    Marco Taviani, Paolo Montagna & Lorenzo Angeletti

  2. Biology Department, Woods Hole Oceanographic Institution, 266 Woods Hole Road, Woods Hole, MA, 02543, USA

    Marco Taviani

  3. Stazione Zoologica Anton Dohrn, Villa Comunale, 80121, Naples, Italy

    Marco Taviani

  4. Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, NY, 10964, USA

    Paolo Montagna

  5. Center for Marine Geology, Saudi Geological Survey, Jeddah, Saudi Arabia

    Najeeb M. A. Rasul

  6. Apache Egypt Companies, 11 Street 281, New Maadi, Cairo, Egypt

    William Bosworth

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  1. Marco Taviani
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  4. Lorenzo Angeletti
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Correspondence to Lorenzo Angeletti .

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  1. Center for Marine Geology, Saudi Geological Survey, Jeddah, Saudi Arabia

    Dr. Najeeb M.A. Rasul

  2. Stewart Geophysical Consultants Pty. Ltd., College Park, SA, Australia

    Dr. Ian C.F. Stewart

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Taviani, M., Montagna, P., Rasul, N.M.A., Angeletti, L., Bosworth, W. (2019). Pleistocene Coral Reef Terraces on the Saudi Arabian Side of the Gulf of Aqaba, Red Sea. In: Rasul, N., Stewart, I. (eds) Geological Setting, Palaeoenvironment and Archaeology of the Red Sea. Springer, Cham. https://doi.org/10.1007/978-3-319-99408-6_16

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