During the last century, Grotta Romanelli (Southern Italy) has been a reference site for the European Late Pleistocene stratigraphy, due to its geomorphological setting and archaeological and palaeontological content. The beginning of the sedimentation inside the cave was attributed to the Last Interglacial (MISs 5e) and the oldest unearthed evidence of human occupation, including remains of hearths, was therefore referred to the Middle Palaeolithic. Recent surveys and excavations produced new U/Th dates, palaeoenvironmental interpretation and a litho-, morpho- and chrono-stratigraphical reassessment, placing the oldest human frequentation of the cave between MIS 9 and MIS 7, therefore 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.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9358667 | PMC |
http://dx.doi.org/10.1038/s41598-022-16906-9 | DOI Listing |
Sci Rep
August 2024
Consiglio Nazionale Delle Ricerche (CNR), Istituto Di Geologia Ambientale E Geoingegneria, Area della Ricerca di Roma 1, 00015, Monterotondo, Rome, Italy.
Sci Rep
August 2022
Consiglio Nazionale Delle Ricerche (CNR), Istituto Di Geologia Ambientale E Geoingegneria, Area della Ricerca di Roma 1, 00015, Monterotondo, Rome, Italy.
During the last century, Grotta Romanelli (Southern Italy) has been a reference site for the European Late Pleistocene stratigraphy, due to its geomorphological setting and archaeological and palaeontological content. The beginning of the sedimentation inside the cave was attributed to the Last Interglacial (MISs 5e) and the oldest unearthed evidence of human occupation, including remains of hearths, was therefore referred to the Middle Palaeolithic. Recent surveys and excavations produced new U/Th dates, palaeoenvironmental interpretation and a litho-, morpho- and chrono-stratigraphical reassessment, placing the oldest human frequentation of the cave between MIS 9 and MIS 7, therefore embracing Glacial and Interglacial cycles.
View Article and Find Full Text PDFSci Rep
August 2020
U.R. Preistoria e Antropologia, Dipartimento di Scienze Fisiche, della Terra e dell'Ambiente, Università degli Studi di Siena, Via Laterina 8, 53100, Siena, Italy.
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