208 D11. Recent Advances in Geoarchaeology: Studies from Asia, Europe and the Americas
Wednesday, 18 October 2023
8:00 AM - 12:00 PM
330
MIDDLE PLEISTOCENE-HOLOCENE CAVE SEDIMENT RECORD OF GROTTA ROMANELLI, ITALY
Paper number: 208-10
Program: Technical Sessions
Time: 10:05 AM – 10:20 AM
Authors
-
Pierluigi PierucciniUniversity of Turin, Turin
-
Raffaele SardellaSapienza University of Roma, Rome
-
Guido S. MarianiUniversity of Turin, Turin
-
Luca FortiUniversity of Milan La Statale, Milano
Abstract
European Late Pleistocene stratigraphy, due to its geomorphological setting and its rich archaeological and
palaeontological content. The beginning of the sedimentation inside the cave has been attributed so far to
MISs 5e, and the oldest unearthed evidence of human occupation, including evidence of use of fire, was
therefore referred to the Middle Palaeolithic. Broad range geoarchaeological investigations were recently
carried out in the site: geological/geomorphological surveys and analysis, micromorphology,
micropalaeontology, palynology, palaeomagnetism, U/Th, radiocarbon and OSL dating are among the main
methods already applied or in progress. The results led to the re-assessment of the litho-, morpho- and
chrono-stratigraphical setting, highlighting an earlier human frequentation of the cave (Middle Pleistocene,
between MIS 9 and MIS 7), embracing Glacial and Interglacial cycles. These new data provide evidence that
the sea reached the cave during the Middle Pleistocene and human occupation occurred long before MISs
5e and persisted beyond the Pleistocene- Holocene boundary providing a new insight within the
chronology and characteristics of the human occupation and the terrestrial ecosystem evolution in the
Mediterranean area.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-396187
© Copyright 2023 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.