Academic Journal

Palaeogeographical evolution of the Egadi Islands (western Sicily, Italy). Implications for late Pleistocene and early Holocene sea crossings by humans and other mammals in the western Mediterranean

التفاصيل البيبلوغرافية
العنوان: Palaeogeographical evolution of the Egadi Islands (western Sicily, Italy). Implications for late Pleistocene and early Holocene sea crossings by humans and other mammals in the western Mediterranean
المؤلفون: Lo Presti V., Antonioli F., Palombo M. R., Agnesi V., Biolchi S., Calcagnile L., Di Patti C., Donati S., Furlani S., Merizzi J., Pepe F., Quarta G., Renda P., Sulli A., Tusa S.
المساهمون: Lo Presti, V., Antonioli, F., Palombo, M. R., Agnesi, V., Biolchi, S., Calcagnile, L., Di Patti, C., Donati, S., Furlani, S., Merizzi, J., Pepe, F., Quarta, G., Renda, P., Sulli, A., Tusa, S.
سنة النشر: 2019
المجموعة: Università degli studi di Trieste: ArTS (Archivio della ricerca di Trieste)
مصطلحات موضوعية: Dwarf elephant, Egadi archipelago, Food remain, Mammal, Marine geological data, Mediterranean voyaging, Palaeogeographical reconstruction, Palaeoshoreline, Vertical tectonic movements
الوصف: The continental shelf morphology offshore of western Sicily suggests that during the Last Glacial Maximum (LGM, 20 ka cal BP), two of the Egadi Islands, Favignana and Levanzo, were connected to Sicily by a wide emerged plain, while Marettimo was only separated from the other islands by a narrow channel. We studied the relative sea-level variation from the LGM until today, focussing on two important time slices: the Mesolithic (9.5–13 ka cal BP)and the Neolithic (6.5–7.5 ka cal BP). In this research, we discuss a sea-level rise model by means of geomorphological, archaeological and geophysical observations and new radiocarbon dating of marine and terrestrial fossil fauna. The results enabled us to provide a detailed palaeogeographical reconstruction of the focal area from the LGM until they became isolated. The evidence that has emerged from this research, in particular the radiometric data, supports the hypothesis that seafaring in the western Mediterranean area may have started between the early Mesolithic and late Epigravettian (between 8.4 and 13.5 ka cal BP), although it probably became a well-established practice only during the Neolithic.
نوع الوثيقة: article in journal/newspaper
وصف الملف: ELETTRONICO
اللغة: English
Relation: info:eu-repo/semantics/altIdentifier/wos/WOS:000472687000008; volume:194; firstpage:160; lastpage:181; numberofpages:22; journal:EARTH-SCIENCE REVIEWS; http://hdl.handle.net/11368/2952231; info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85065675870; http://www.sciencedirect.com/science/journal/00128252
DOI: 10.1016/j.earscirev.2019.04.027
الاتاحة: http://hdl.handle.net/11368/2952231
https://doi.org/10.1016/j.earscirev.2019.04.027
http://www.sciencedirect.com/science/journal/00128252
Rights: info:eu-repo/semantics/openAccess
رقم الانضمام: edsbas.C367FA36
قاعدة البيانات: BASE
الوصف
DOI:10.1016/j.earscirev.2019.04.027