Persististrombus latus (GMELIN, 1791) (=Strombus bubonius LAMARCK, 1822), is the most iconic representative of the “Senegalese fauna”, a fossil assemblage of tropical water organisms thought to have colonized the Mediterranean Sea during the last interglacial. As such, P. latus has become an important stratigraphic marker of Marine Isotope Stage (MIS) 5.5, allowing the correlation of raised coastal deposits used in studies of sea level variations and tectonic uplift. P. latus is found in shallow marine sediments of Tyrrhenian age (~124 ka) in several localities of the Italian peninsula. However, despite intensive surveying through the years, the late Pleistocene marine terraces of the Crotone peninsula, which preserve an extensive volume of fossiliferous deposits attributed to MIS 5, have yielded very few specimens of P. latus. This paper reports the finding of several new specimens of P. latus near Isola di Capo Rizzuto, in deposits that had been independently assigned to MIS 5.5, and two specimens from the Capo Colonna terrace, which is thought to correlate with MIS 5.3 or 5.1. The Crotone peninsula, therefore, represents one of the few localities in Italy where multiple stratigraphically distinct P. latus-bearing units can be observed.

Nalin, R., Bracchi, V., Basso, D., Massari, F. (2012). Persististrombus latus (GMELIN) in the upper Pleistocene deposits of the marine terraces of the Crotone peninsula (southern Italy). ITALIAN JOURNAL OF GEOSCIENCES, 131(1), 95-101 [10.3301/IJG.2011.25].

Persististrombus latus (GMELIN) in the upper Pleistocene deposits of the marine terraces of the Crotone peninsula (southern Italy)

BRACCHI, VALENTINA ALICE;BASSO, DANIELA MARIA;
2012

Abstract

Persististrombus latus (GMELIN, 1791) (=Strombus bubonius LAMARCK, 1822), is the most iconic representative of the “Senegalese fauna”, a fossil assemblage of tropical water organisms thought to have colonized the Mediterranean Sea during the last interglacial. As such, P. latus has become an important stratigraphic marker of Marine Isotope Stage (MIS) 5.5, allowing the correlation of raised coastal deposits used in studies of sea level variations and tectonic uplift. P. latus is found in shallow marine sediments of Tyrrhenian age (~124 ka) in several localities of the Italian peninsula. However, despite intensive surveying through the years, the late Pleistocene marine terraces of the Crotone peninsula, which preserve an extensive volume of fossiliferous deposits attributed to MIS 5, have yielded very few specimens of P. latus. This paper reports the finding of several new specimens of P. latus near Isola di Capo Rizzuto, in deposits that had been independently assigned to MIS 5.5, and two specimens from the Capo Colonna terrace, which is thought to correlate with MIS 5.3 or 5.1. The Crotone peninsula, therefore, represents one of the few localities in Italy where multiple stratigraphically distinct P. latus-bearing units can be observed.
Articolo in rivista - Articolo scientifico
Strombus bubonius, Persististrombus latus, Tyrrhenian, Crotone Peninsula, marine terraces, MIS 5
English
feb-2012
2012
131
1
95
101
none
Nalin, R., Bracchi, V., Basso, D., Massari, F. (2012). Persististrombus latus (GMELIN) in the upper Pleistocene deposits of the marine terraces of the Crotone peninsula (southern Italy). ITALIAN JOURNAL OF GEOSCIENCES, 131(1), 95-101 [10.3301/IJG.2011.25].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10281/49466
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