The Acerno lacustrine basin is a tectonic palaeolake formed during the Middle Pleistocene. Pollen analysis and tephrostratigraphy performed on the lacustrine succession (about 100 m thick) allowed the vegetation history to be reconstructed and correlated with OIS 9 and 8 on the basis of the presence of the Lower WTT (297 ka) marker level.
A late Middle Pleistocene climatic cycle in southern Italy inferred from pollen analysis and tephrostratigraphy of the Acerno lacustrine succession / Munno, Rosalba; Petrosino, Paola; Romano, Paola; RUSSO ERMOLLI, Elda; Juvigne, E.. - In: GEOGRAPHIE PHYSIQUE ET QUATERNAIRE. - ISSN 0705-7199. - STAMPA. - 55:(2001), pp. 87-99.
A late Middle Pleistocene climatic cycle in southern Italy inferred from pollen analysis and tephrostratigraphy of the Acerno lacustrine succession.
MUNNO, ROSALBA;PETROSINO, PAOLA;ROMANO, PAOLA;RUSSO ERMOLLI, ELDA;
2001
Abstract
The Acerno lacustrine basin is a tectonic palaeolake formed during the Middle Pleistocene. Pollen analysis and tephrostratigraphy performed on the lacustrine succession (about 100 m thick) allowed the vegetation history to be reconstructed and correlated with OIS 9 and 8 on the basis of the presence of the Lower WTT (297 ka) marker level.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
