Grotta Romanelli, located in southern Italy, is a natural coastal cave renowned for its exceptional stratigraphical record and its critical role in understanding the Middle Pleistocene‐Holocene geomorphological and paleoenvironmental evolution of the Mediterranean region. Its importance has long been recognized with numerous studies focusing on dating its deposits using radiocarbon analyses and biological proxies. In this study, we introduce the use of the Paleosecular Variation (PSV) of the geomagnetic field to compute a depth‐age model for the uppermost stratigraphic unit of Grotta Romanelli (Unit IUS5), traditionally referred to as “Terre Brune.” This Unit, previously associated with the Late Pleistocene‐Holocene transition, lacked a precise chronological framework. Using stepwise alternating field demagnetization, we obtained well‐defined paleomagnetic directions which were compared with the reference …
Late Pleistocene‐Holocene paleosecular variation dating of cave sediments: Insights from Grotta Romanelli (Apulia, Italy) / Tema, E., Lanci, L., Mariani, G.S., Pieruccini, P., Mazzini, I., &, , ., Sardella, R.. - In: GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS. - ISSN 1525-2027. - (2025).
Late Pleistocene‐Holocene paleosecular variation dating of cave sediments: Insights from Grotta Romanelli (Apulia, Italy)
Mazzini I.;Sardella, R
2025
Abstract
Grotta Romanelli, located in southern Italy, is a natural coastal cave renowned for its exceptional stratigraphical record and its critical role in understanding the Middle Pleistocene‐Holocene geomorphological and paleoenvironmental evolution of the Mediterranean region. Its importance has long been recognized with numerous studies focusing on dating its deposits using radiocarbon analyses and biological proxies. In this study, we introduce the use of the Paleosecular Variation (PSV) of the geomagnetic field to compute a depth‐age model for the uppermost stratigraphic unit of Grotta Romanelli (Unit IUS5), traditionally referred to as “Terre Brune.” This Unit, previously associated with the Late Pleistocene‐Holocene transition, lacked a precise chronological framework. Using stepwise alternating field demagnetization, we obtained well‐defined paleomagnetic directions which were compared with the reference …I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.


