The stratigraphic succession of the "Mar Piccolo" basin (Taranto, Southern Italy) is well known in the scientific literature dealing with last interglacial (Belluomini et alii, 2002; Amorosi et alii, 2014; Negri et alii, 2014) and its morphological evolution is influenced by sea level changes during Late Pleistocene-Holocene (e.g.: Mastronuzzi and Sansò, 1998). In order to reconstruct the evolutionary model of the Mar Piccolo, as connected to the sea level rise, an Accelerator Mass Spectrometry (AMS) 14C dating campaign was carried out on Cerastoderma glaucum (Poiret,1789).
Estimation of the reservoir age in the Mar Piccolo basin in Taranto (Southern Italy) by AMS 14 C dating on Cerastoderma glaucum (Poiret, 1789)
Cipriano G.;Scardino G.;Valenzano E.;Mastronuzzi G.
2018-01-01
Abstract
The stratigraphic succession of the "Mar Piccolo" basin (Taranto, Southern Italy) is well known in the scientific literature dealing with last interglacial (Belluomini et alii, 2002; Amorosi et alii, 2014; Negri et alii, 2014) and its morphological evolution is influenced by sea level changes during Late Pleistocene-Holocene (e.g.: Mastronuzzi and Sansò, 1998). In order to reconstruct the evolutionary model of the Mar Piccolo, as connected to the sea level rise, an Accelerator Mass Spectrometry (AMS) 14C dating campaign was carried out on Cerastoderma glaucum (Poiret,1789).File in questo prodotto:
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2018_Fago et al_ Cerastoderma glaucum Mar Piccolo_IGCP639.pdf
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