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Eustatic control of late Quaternary sea-level change in the Arabian/Persian Gulf

Published online by Cambridge University Press:  20 January 2017

Thomas Stevens ,
Matthew J. Jestico ,
Graham Evans  and
Anthony Kirkham
Thomas Stevens*
Affiliation:
Centre for Quaternary Research, Department of Geography, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
Matthew J. Jestico
Affiliation:
Centre for Quaternary Research, Department of Geography, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK
Graham Evans
Affiliation:
Ocean and Earth Science, National Oceanographic Centre, Southampton University, Southampton S014 3ZH, UK
Anthony Kirkham
Affiliation:
Sedimentology and Reservoir Development Ltd, Pen-yr-Allt, Village Road, Nannerch, Mold, Flintshire CH7 5RD, UK
*
* Corresponding author.E-mail address: [email protected] (T. Stevens).
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Abstract

Accurate sea-level reconstruction is critical in understanding the drivers of coastal evolution. Inliers of shallow marine limestone and aeolianite are exposed as zeugen (carbonate-capped erosional remnants) on the southern coast of the Arabian/Persian Gulf. These have generally been accepted as evidence of a eustatically driven, last-interglacial relative sea-level highstand preceded by a penultimate glacial-age lowstand. Instead, recent optically stimulated luminescence (OSL) dating suggests a last glacial age for these deposits, requiring >100 m of uplift since the last glacial maximum in order to keep pace with eustatic sea-level rise and implying the need for a wholesale revision of tectonic, stratigraphic and sea-level histories of the Gulf. These two hypotheses have radically different implications for regional neotectonics and land–sea distribution histories. Here we test these hypotheses using OSL dating of the zeugen formations. These new ages are remarkably consistent with earlier interpretations of the formations being last interglacial or older in age, showing that tectonic movements are negligible and eustatic sea-level variations are responsible for local sea-level changes in the Gulf. The cause of the large age differences between recent studies is unclear, although it appears related to large differences in the measured accumulated dose in different OSL samples.

Keywords

Arabian GulfPersian GulfOSLLuminescenceSea levelQuaternary
Type
Articles
Information
Quaternary Research , Volume 82 , Issue 1 , July 2014 , pp. 175 - 184
Copyright
University of Washington

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References

Aitken, M.J. An Introduction to Optical Dating. (1998). Oxford University Press, UK. 267 Google Scholar
Ankjærgaard, C., and Murray, A.S. Total beta and gamma dose rates in trapped charge dating based on beta counting. Radiation Measurements 42, (2007). 352–359.Google Scholar
Armitage, S.J., and Bailey, R.M. The measured dependence of laboratory beta dose rates on sample grain size. Radiation Measurements 39, (2005). 123–127.Google Scholar
Bøtter-Jensen, L., Bulur, E., Duller, G.A.T., and Murray, A.S. Advances in luminescence instrumentation. Radiation Measurements 32, (2000). 523–528.Google Scholar
Bøtter-Jensen, L., McKeever, S., and Wintle, A. Optically Stimulated Luminescence Dosimetry. (2003). Elsevier, Amsterdam. 355 p Google Scholar
Burr, G.S., Edwards, R.L., Donahue, D.J., Druffel, E.R.M., and Taylor, F.W. Mass spectrometric 14C and U–Th measurements in coral. Radiocarbon 34, (1992). 611–618.CrossRefGoogle Scholar
Cunningham, A.C., and Wallinga, J. Selection of integration time intervals for quartz OSL decay curves. Quaternary Geochronology 5, (2010). 657–666.Google Scholar
Duller, G.A.T. Distinguishing quartz and feldspar in single grain luminescence measurements. Radiation Measurements 37, (2003). 161–165.Google Scholar
Duller, G.A.T. Assessing the error on equivalent dose estimates derived from single aliquot regenerative dose measurements. Ancient TL 25, (2007). 15–24.Google Scholar
Duller, G.A.T. Single-grain optical dating of Quaternary sediments: why aliquot size matters in luminescence dating. Boreas 37, (2008). 589–612.Google Scholar
Evans, G. An historical review of the Quaternary sedimentology of the Gulf (Arabian/Persian Gulf) and its geological impact. Kendall, C.G.St.C., and Alsharan, A.S. Quaternary Carbonate and Evaporite Sedimentary Facies and Their Ancient Analogues. A Tribute to Douglas James Shearman. Special Publication No. 43 of the International Association of Sedimentologists (2011). 13–44.Google Scholar
Evans, G., and Kirkham, A. Distribution of Sabkhat within the Arabian peninsula and the adjacent countries. Barth, , Boer, Sabkha Ecosystems. (2002). Kluwer Academic Publishers, 7–20.Google Scholar
Evans, G., and Kirkham, A. The Quaternary deposits. Hellyer, P., and Aspinall, S. The Emirates: A Natural History. (2005). Publ. Trident Press, London. 65–80.Google Scholar
Evans, G., Schmidt, V., Bush, P., and Nelson, H. Stratigraphy and geologic history of the sabkha, Abu Dhabi, Persian Gulf. Sedimentology 121, (1969). 145–159.Google Scholar
Evans, G., Kirkham, A., and Carter, R.A. Quaternary development of the United Emirates coast: new evidence from Marawah Island, Abu Dhabi. GeoArabia 7, (2002). 441–458.CrossRefGoogle Scholar
Farrant, A.R., Ellison, R.A., Thomas, R.J., Pharaoh, T.C., Newell, A.J., Goodenough, K.M., Lee, J.R., and Knox, R. The Geology and Geophysics of the United Arab Emirates. vol. 6 (2012). British Geological Survey, (336 pp. The Geology and Geophysics of the United Arab Emirates, Memoirs, 6) Google Scholar
Glennie, K.W., and Kendall, C.G.St.C. The desert of southeast Arabia: a product of Quaternary climate change. Alsharan, A.S., Glennie, K.W., and Whittle, G.L. Quaternary Deserts and Climatic Change. (1998). Balkema, Rotterdam. 279–291.Google Scholar
Glennie, K.W., and Singhvi, A.K. Event stratigraphy, paleoenvironment and chronology of SE Arabian deserts. Quaternary Science Reviews 21, (2002). 853–869.Google Scholar
Hadley, D.G., Brouwers, E.M., and Brown, T.M. Quaternary palaeodunes, Arabian Gulf coast: age and palaeoenvironmental evolution. Alsharan, A.S., Glennie, K.W., Whittle, G.L., and Kendall, C.G.St.C. Quaternary Deserts and Climatic Change. (1998). Balkema, Rotterdam. 123–141.Google Scholar
Kassler, P. The structural and geomorphological evolution of the Persian Gulf. Purser, B.H. The Persian Gulf, Holocene Carbonate Sedimentation in a Shallow Epicontinental Sea. (1973). Springer, New York. 11–32.Google Scholar
Kirkham, A. Pleistocene carbonate seif dunes and their role in the development of complex past and present coastlines of the U.A.E.. GeoArabia 3, (1998). 19–32.CrossRefGoogle Scholar
Kirkham, A. A Quaternary proximal foreland ramp and its continental fringe, Arabian Gulf, U.A.E.. Wright, V.P., and Burchette, T.P. Carbonate Ramps. Special Publication of the Geological Society of London 149, (1998). 15–41.Google Scholar
Kirkham, A. Halite, sulphates, sabkhat and salinas of the coastal regions and Sabkha Matti of Abu Dhabi, United Arab Emirates. Kendall, C.G.St.C., and Alsharan, A.S. Quaternary Carbonate and Evaporite Sedimentary Facies and Their Ancient Analogues. A Tribute to Douglas James Shearman. Special Publication No. 43 of the International Association of Sedimentologists (2011). 265–276.Google Scholar
Kirkham, A., and Evans, G. Giant burrows in the Quaternary limestones of Futaysi Island and Al Dabb'iya, Abu Dhabi Emirate. Palaeogeography, Palaeoclimatology, Palaeoecology 270, (2008). 324–331.Google Scholar
Lai, Z.P., Mischke, S., and Madsen, D. Paleoenvironmental implications of new OSL dates on the formation of the “Shell Bar” in the Qaidam Basin, northeastern Qinghai–Tibetan Plateau. Journal of Paleolimnology (2013). http://dx.doi.org/10.1007/s10933-013-9710-1 Google Scholar
Lambeck, K. Shoreline reconstructions for the Persian Gulf since the last glacial maximum. Earth and Planetary Science Letters 142, (1996). 43–57.Google Scholar
Mejdahl, V. Thermoluminescence dating: beta-dose attenuation in quartz grains. Archaeometry 21, (1979). 61–72.Google Scholar
Murray, A.S., and Wintle, A.G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose procedure. Radiation Measurements 32, (2000). 57–73.Google Scholar
Murray, A.S., and Wintle, A.G. The single aliquot regeneration dose protocol: potential for improvements in reliability. Radiation Measurements 37, (2003). 377–381.Google Scholar
Nathan, R.P., and Mauz, B. On the dose-rate estimate of carbonate-rich sediments for trapped charge dating. Radiation Measurements 43, (2008). 14–25.Google Scholar
Patterson, R.J., and Kinsman, D.J.J. Marine and continental ground water sources in a Persian Gulf sabkha. Reefs and related carbonates — ecology and sedimentology. American Association of Petroleum Geology Special Publication 4, (1977). 381–397.Google Scholar
Prescott, J.R., and Hutton, J.T. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long term variations. Radiation Measurements 23, (1994). 497–500.Google Scholar
Russell, N.J., and Armitage, S.J. A comparison of single-grain and small aliquot dating of fine sand from Cyrenaica, northern Libya. Quaternary Geochronology 10, (2012). 62–67.CrossRefGoogle Scholar
Scholle, P.A., and Kinsman, D.J.J. Aragonitic and high-Mg calcite caliche from the Persian Gulf — a modern analog for the Permian of Texas and New Mexico. Journal of Sedimentary Petrology 44, (1974). 904–916.Google Scholar
Stevens, T., Kirkham, A., and Evans, G. Quaternary sea levels: recent evidence from Abu Dhabi. Tribulus 19, (2011). 158–159.Google Scholar
Waelbroeck, C., Labeyrie, L., Michel, E., Duplessey, J.C., Lambeck, K., McManus, J.F., Balbon, E., and Labracherie, M. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records. Quaternary Science Reviews 21, (2002). 295–305.CrossRefGoogle Scholar
Whitehouse, P.L., and Bradley, S.L. Eustatic sea-level changes since the last glacial maximum. Elias, S.A. Encyclopaedia of Quaternary Science. Second edition (2013). Elsevier, Amsterdam. 439–451.Google Scholar
Williams, A.H. (1999). Glacioeustatic cyclicity in Quaternary carbonates of the southern Arabian Gulf: sedimentology, sequence stratigraphy, palaeoenvironments and climatic record. Unpublished Ph.D. thesis, Aberdeen University, pp. 535.Google Scholar
Williams, A.H., and Walkden, G.M. Carbonate eolianites from eustatically influenced ramp-like setting: the Quaternary of southern Arabian Gulf. Abegg, F.E., Harris, P.M., and Loope, D.B. Modern and Ancient Carbonate Eolianites: Sedimentology, Sequence Stratigraphy, and Diagenesis. SEPM Special Publication 71, (2001). 77–92.Google Scholar
Williams, A.H., and Walkden, G.M. Late Quaternary highstand deposits of the southern Arabian Gulf: a record of sea-level and climate change. Clift, P.D., Kroon, D., Craig, C., and Craig, J. The Tectonic and Climatic Evolution of the Arabian Sea Region. Special Publication of the Geological Society of London 195, (2002). 371–386.Google Scholar
Wood, W.W., Stokes, S., Brandt, D., Kraemer, T.F., and Imes, J.L. Rapid rise (− 3 mm/yr) of coastal Abu Dhabi. Geological Society of America Annual Meeting and exposition. Abstracts with Programs 38, (2006). 328 Google Scholar
Wood, W.W., Bailey, R.M., Hampton, B.A., Kraemer, T.F., Lu, Z., Clark, D.W., James, R.H.R., and Al Ramadan, K. Rapid late Pleistocene/Holocene uplift and coastal evolution of the southern Arabian (Persian) Gulf. Quaternary Research 77, (2012). 215–220.Google Scholar