Format

Send to

Choose Destination
Sci Rep. 2018 Dec 13;8(1):17837. doi: 10.1038/s41598-018-36111-x.

The archaeological ensemble from Campoverde (Agro Pontino, central Italy): new constraints on the Last Interglacial sea level markers.

Author information

1
Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143, Rome, Italy. fabrizio.marra@ingv.it.
2
Università di Roma "Sapienza", Dipartimento di Scienze della Terra, P.le Aldo Moro 5, 00185, Rome, Italy.
3
Freelance, Tivoli, (Rome), Italy.
4
Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143, Rome, Italy.
5
Università di Roma "Tor Vergata", Department of History, Humanities and Society, Via Columbia 1, 00133, Rome, Italy.
6
University of York, Department of Archaeology, The King's Manor, York, UK.
7
Ecomuseo dell'Agro Pontino, Via G.B. Vico 15, Latina, Italy.

Abstract

We present a combined geomorphological and biochronological study aimed at providing age constraints to the deposits forming a wide paleo-surface in the coastal area of the Tyrrhenian Sea, south of Anzio promontory (central Italy). We review the faunal assemblage recovered in Campoverde, evidencing the occurrence of the modern fallow deer subspecies Dama dama dama, which in peninsular Italy is not present before MIS 5e, providing a post-quem terminus of 125 ka for the deposit hosting the fossil remains. The geomorphological reconstruction shows that Campoverde is located within the highest of three paleosurfaces progressively declining towards the present coast, at average elevations of 36, 26 and 15 m a.s.l. The two lowest paleosurfaces match the elevation of the previously recognized marine terraces in this area; we define a new, upper marine terrace corresponding to the 36 m paleosurface, which we name Campoverde complex. Based on the provided evidence of an age as young as MIS 5e for this terrace, we discuss the possibility that previous identification of a tectonically stable MIS 5e coastline ranging 10-8 m a.s.l. in this area should be revised, with significant implications on assessment of the amplitude of sea-level oscillations during the Last Interglacial in the Mediterranean Sea.

Supplemental Content

Full text links

Icon for Nature Publishing Group Icon for PubMed Central
Loading ...
Support Center