Geology and Archaeology: Submerged Landscapes of the Continental Shelf

Sea-level change has influenced human population globally since prehistoric times. Even in early phases of cultural development human populations were faced with marine regression and transgression as a result of changing climate and corresponding glacio-isostatic adjustment. Global marine regression during the last glaciation changed the palaeogeography of the continental shelf, converting former marine environments to attractive terrestrial habitats for prehistoric humans. These areas of the shelf were used as hunting and gathering areas, as migration routes between continents, and most probably witnessed the earliest developments in seafaring and marine exploitation, until the postglacial transgression re-submerged these palaeo-landscapes. Based on modern marine research technologies and the integration of large databases, proxy data are increasingly available for the reconstruction of Quaternary submerged landscapes. Also, prehistoric archaeological remains from the recent sea bottom are shedding new light on human prehistoric development driven by rapidly changing climate and environment. This publication contributes to the exchange of ideas and new results in this young and challenging field of underwater palaeoenvironmental investigation.
Late Quaternary beach deposits and archaeological relicts on the coasts of Cyprus, and the possible implications of sea-level changes and tectonics on the early populations
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Published:January 01, 2016
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CiteCitation
E. Galili, M. Şevketoğlu, A. Salamon, D. Zviely, H. K. Mienis, B. Rosen, S. Moshkovitz, 2016. "Late Quaternary beach deposits and archaeological relicts on the coasts of Cyprus, and the possible implications of sea-level changes and tectonics on the early populations", Geology and Archaeology: Submerged Landscapes of the Continental Shelf, J. Harff, G. Bailey, F. Lüth
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Abstract
Late Pleistocene beach deposits in 22 selected sites around Cyprus demonstrate the vertical changes in the Earth’s crust in that island over the last 125 ka. The beach/shallow-marine deposits were observed on the abraded coastal cliffs at 3–22 m above the present sea-level. They overlie Pliocene marls, and some of them contain the Senegalese marine gastropods Persististrombus latus, Bursa granularis and Conus ermineus that no longer live in the Mediterranean. These are index fossils for the Marine Isotope Stage (MIS) 5e in the Mediterranean and, as such, suggest an uplift of up to 15.5 m over about the...
- absolute age
- archaeological sites
- archaeology
- Asia
- beaches
- Cenozoic
- coastal environment
- correlation
- Cyprus
- depositional environment
- event stratigraphy
- field studies
- Holocene
- human ecology
- index fossils
- Invertebrata
- lithostratigraphy
- marine environment
- Mediterranean region
- Mediterranean Sea
- Middle East
- Mollusca
- morphostructures
- Neolithic
- paleoenvironment
- paleogeography
- Pleistocene
- Quaternary
- reconstruction
- resources
- sea-level changes
- sediments
- shells
- shore features
- Stone Age
- tectonics
- Th/U
- uplifts
- upper Pleistocene
- upper Quaternary
- vertical movements
- Cape Greco
- Akanthou
- MIS 5e
- Karpasia Peninsula
- Mylouthkia
- Famagusta Bay