Abstract
Borehole studies indicate three stratigraphical units in the Holocene sediments on the Aegean coastal plains of Anatolia. These are early Holocene shallow marine- estuarine muds at the bottom, fine sandy-silty flood-plain sediments at the top, and a transition layer between them. The transition layer, a few meters thick and a few meters below the present sea-level, generally consists of the coarse sandy sediments of shallow coastal environments. C14 datings show that the change in sedimentation occurred during the third millennium BC In addition, relative sea-level fell a few meters during the same period, which accelerated deltaic progression. The transition layer has similar characteristics all along the coastal plains investigated, indicating that the change in sedimentation is a result of normal geomorphological development dependent on sea-level changes; local or regional tectonic movements and sediment compactions are not important here. Climatic-ecstatic sea-level changes may be considered the best explanation for the sedimentation change.
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References
De La Geniére, J. (1990) Le sanctuaire d’Apollon á Claros; Nouvelles découvertes. Revue des Etudes Grecques. CIII, 490–491: 95–110. Paris.
Kayan, I. (1988a) Datça yarimadasinda Eski Knidos yerleŞmesini etkileyen dogal çevre özellikleri.Cografya Arastirmalari Dergisi. 11: 51–70. Ankara Universitesi Dil ve Tarih Cografya Faköltesi. Ankara.
Kayan, I. (1988b) Late Holocene sea-level changes on the Western Anatolian coast. Palaeogeography, Palaeoclimatology, Palaeoecology. 68, 2–4: 205–218. Special issue: Quaternary Coastal Changes. Ed. by P. A. Pirazzoli - D. B. Scott. (A selection of papers presented at the IGCP-200 meetings). Elsevier Science Publishers B.V. Amsterdam
Kayan, I. (1991) Holocene geomorphic evolution of the BeŞik plain and changing environment of ancient man. Studia Troica. Band 1: 79–92. Verlag Philipp von Zabern. Mainz am Rhein.
Kayan, I. (1994) Tuzla ovasinin (Ayvacik-Çanakkale) alüvyal jeomorfolojisi ve Holosen’deki kiyi çizgisi degismeleri (Summary: Alluvial geomorphology of the Tuzla plain and Holocene coastal changes). Ege Üniversitesi Rektörlügü Arastirma Fonu Proje No: Edf 1988–027. 74 pp. Izmir. (Unpublished report)
Kayan, I. (1995a) The Troia bay and potential harbor sites in the Bronze Age. Studia Troica. Band 5. Philipp von Zabern, Mainz am Rhein. Germany. (In print).
Kayan, I. (1995b) Klaros kazi alaninda jeomorfolojik-jeoarkeolojik arastirmalar (Summary: Geomorphological-geoarchaeological investigations on the Klaros excavation area). Aegean Geographical Journal. 8: 1–26. Ege University. Izmir. (In print).
Kraft J. C., Kayan İ. and Erol O. (1980) Geomorphic reconstructions in the environs of ancient Troy. Science. American Association for the Advancement of Science. Vol. 209, No. 4458: 776 – 782
Kraft, J. C., Kayan I., and Erol, O. (1982) Geology and Paleogeographic Reconstructions of the Vicinity of Troy, in: Rapp, G. Jr. and Gifford, J. A. (eds.), Troy: The Archaeological Geology, Supplementary Monograph 4, 11–40. Cincinnati.
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© 1997 Springer-Verlag Berlin Heidelberg
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Kayan, İ. (1997). Bronze Age Regression and Change of Sedimentation on the Aegean Coastal Plains of Anatolia (Turkey). In: Dalfes, H.N., Kukla, G., Weiss, H. (eds) Third Millennium BC Climate Change and Old World Collapse. NATO ASI Series, vol 49. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60616-8_17
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DOI: https://doi.org/10.1007/978-3-642-60616-8_17
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