The Campania Plain is a wide coastal plain characterized by a huge quaternary sedimentary record more than two thousand meters thick. In order to analyze the most superficial portion of theinfilling succession an 80 m-long core was drilled in the northernsector of the plain. The upper part of the core is entirely made upof an ignimbrite formation (Campania Ignimbrite, 39 ka), lyingunconformably above marine sediments alternating with volcanic products. Macro- and micro-paleontological analysis together with tephrostratigraphy and 39Ar/40Ar dating allowed the paleoenvironmental evolution of the studied area to be reconstructed. The paleogeography during OIS 7 and 5 was characterized by the presence of lagoon systems. These are now located 28 km inland from the present coastline and buried at –40 and –18 m with respect to the present sea level, as a consequence of tectonic subsidence. Two major periods of volcanic activity were recorded in the core prior to Campania Ignimbrite emplacement, confirming the existence of important phases of volcanic activity in the plain during the end of the Middle Pleistocene. The SME multiproxy record represents the first continuous record of volcanic products emplaced in the last 200 ka north of the Campania volcanic sources.

Late Quaternary buried lagoons in the northern Campania plain (southern Italy): evolution of a coastal system under the influence of volcano-tectonics and eustatism / Santangelo, Nicoletta; Ciampo, Giuliano; DI DONATO, Valentino; P., Esposito; Petrosino, Paola; Romano, Paola; RUSSO ERMOLLI, Elda; Santo, Antonio; F., Toscano; I. M., Villa. - In: ITALIAN JOURNAL OF GEOSCIENCES. - ISSN 2038-1719. - 129:1(2010), pp. 156-175. [10.3301/IJG.2009.12]

Late Quaternary buried lagoons in the northern Campania plain (southern Italy): evolution of a coastal system under the influence of volcano-tectonics and eustatism.

SANTANGELO, NICOLETTA;CIAMPO, GIULIANO;DI DONATO, VALENTINO;PETROSINO, PAOLA;ROMANO, PAOLA;RUSSO ERMOLLI, ELDA;SANTO, ANTONIO;
2010

Abstract

The Campania Plain is a wide coastal plain characterized by a huge quaternary sedimentary record more than two thousand meters thick. In order to analyze the most superficial portion of theinfilling succession an 80 m-long core was drilled in the northernsector of the plain. The upper part of the core is entirely made upof an ignimbrite formation (Campania Ignimbrite, 39 ka), lyingunconformably above marine sediments alternating with volcanic products. Macro- and micro-paleontological analysis together with tephrostratigraphy and 39Ar/40Ar dating allowed the paleoenvironmental evolution of the studied area to be reconstructed. The paleogeography during OIS 7 and 5 was characterized by the presence of lagoon systems. These are now located 28 km inland from the present coastline and buried at –40 and –18 m with respect to the present sea level, as a consequence of tectonic subsidence. Two major periods of volcanic activity were recorded in the core prior to Campania Ignimbrite emplacement, confirming the existence of important phases of volcanic activity in the plain during the end of the Middle Pleistocene. The SME multiproxy record represents the first continuous record of volcanic products emplaced in the last 200 ka north of the Campania volcanic sources.
2010
Late Quaternary buried lagoons in the northern Campania plain (southern Italy): evolution of a coastal system under the influence of volcano-tectonics and eustatism / Santangelo, Nicoletta; Ciampo, Giuliano; DI DONATO, Valentino; P., Esposito; Petrosino, Paola; Romano, Paola; RUSSO ERMOLLI, Elda; Santo, Antonio; F., Toscano; I. M., Villa. - In: ITALIAN JOURNAL OF GEOSCIENCES. - ISSN 2038-1719. - 129:1(2010), pp. 156-175. [10.3301/IJG.2009.12]
File in questo prodotto:
File Dimensione Formato  
SANTANGELO et al 2010 carota SME.pdf

non disponibili

Tipologia: Documento in Post-print
Licenza: Accesso privato/ristretto
Dimensione 1.14 MB
Formato Adobe PDF
1.14 MB Adobe PDF   Visualizza/Apri   Richiedi una copia

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11588/362012
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 42
  • ???jsp.display-item.citation.isi??? 33
social impact