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.
Timing of the emergence of the Europe–Sicily bridge (40–17 cal ka BP) and its implications for the spread of modern humans
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Published:January 01, 2016
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CiteCitation
Fabrizio Antonioli, Valeria Lo Presti, Maurizio Gasparo Morticelli, Laura Bonfiglio, Marcello A. Mannino, Maria Rita Palombo, Gianmaria Sannino, Luigi Ferranti, Stefano Furlani, Kurt Lambeck, Simonepietro Canese, Raimondo Catalano, Francesco Latino Chiocci, Gabriella Mangano, Giovanni Scicchitano, Renato Tonielli, 2016. "Timing of the emergence of the Europe–Sicily bridge (40–17 cal ka BP) and its implications for the spread of modern humans", Geology and Archaeology: Submerged Landscapes of the Continental Shelf, J. Harff, G. Bailey, F. Lüth
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Abstract
The submerged sill in the Strait of Messina, which is located today at a minimum depth of 81 m below sea level (bsl), represents the only land connection between Sicily and mainland Italy (and thus Europe) during the last lowstand when the sea level locally stood at about 126 m bsl. Today, the sea crossing to Sicily, although it is less than 4 km at the narrowest point, faces hazardous sea conditions, made famous by the myth of Scylla and Charybdis. Through a multidisciplinary research project, we document the timing and mode of emergence of this land connection during...
- absolute age
- adaptation
- archaeological sites
- archaeology
- bathymetry
- biogeography
- bottom features
- C-14
- carbon
- Cenozoic
- Chordata
- colonization
- Equidae
- Equus
- erosion
- erosion features
- Europe
- Eutheria
- faults
- faunal studies
- Hippomorpha
- Hominidae
- Homo
- Homo sapiens
- Homo sapiens sapiens
- human activity
- isostasy
- isostatic rebound
- isotopes
- Italy
- land bridges
- landform evolution
- last glacial maximum
- Mammalia
- migration
- multibeam methods
- ocean floors
- paleo-oceanography
- paleocurrents
- paleoecology
- paleogeography
- Paleolithic
- paleorelief
- Perissodactyla
- petrology
- Pleistocene
- populations
- Primates
- Quaternary
- radioactive isotopes
- reconstruction
- sea-level changes
- shorelines
- Sicily Italy
- Southern Europe
- Stone Age
- Strait of Messina
- succession
- tectonics
- Tetrapoda
- Theria
- upper Pleistocene
- Vertebrata
- vicariance
- Equus hydruntinus
- Grotta di San Teodoro