nieuwe zoekopdracht
[ meld een fout in dit record ]mandje (1): toevoegen | toon Print deze pagina

one publication added to basket [347175]
New evidence of MIS 3 relative sea level changes from the Messina Strait, Calabria (Italy)
Antonioli, F.; Calcagnile, L.; Ferranti, L.; Mastronuzzi, G.; Monaco, C.; Orrù, P.; Quarta, G.; Pepe, F.; Scardino, G.; Scicchitano, G.; Stocchi, P.; Taviani, M. (2021). New evidence of MIS 3 relative sea level changes from the Messina Strait, Calabria (Italy). Water 13(19): 2647. https://dx.doi.org/10.3390/w13192647
In: Water. MDPI AG: Basel. ISSN 2073-4441, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Author keywords
    Marine Isotope Stage 3; relative sea level; tectonics; GIA; Calabria

Auteurs  Top 
  • Antonioli, F.
  • Calcagnile, L.
  • Ferranti, L.
  • Mastronuzzi, G.
  • Monaco, C.
  • Orrù, P.
  • Quarta, G.
  • Pepe, F.
  • Scardino, G.
  • Scicchitano, G.
  • Stocchi, P., meer
  • Taviani, M.

Abstract
    Investigation of sea-level positions during the highly-dynamic Marine Isotope Stage 3 (MIS 3: 29–61 kyrs BP) proves difficult because: (i) in stable and subsiding areas, coeval coastal sediments are currently submerged at depths of few to several tens of meters below the present sea level; (ii) in uplifting areas, the preservation of geomorphic features and sedimentary records is limited due to the erosion occurred during the Last Glacial Maximum (LGM) with sea level at a depth of −130 m, followed by marine transgression that determined the development of ravinement surfaces. This study discusses previous research in the Mediterranean and elsewhere, and describes new fossiliferous marine deposits overlaying the metamorphic bedrock at Cannitello (Calabria, Italy). Radiocarbon ages of marine shells (about 43 kyrs cal BP) indicate that these deposits, presently between 28 and 30 m above sea level, formed during MIS 3.1. Elevation correction of the Cannitello outcrops (considered in an intermediate-to-far-field position with respect to the ice sheet) with the local vertical tectonic rate and Glacial Isostatic Adjustment (GIA) rate allows the proposal of a revision of the eustatic depth for this highstand. Our results are consistent with recently proposed estimates based on a novel ice sheet modelling technique.

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid Top | Auteurs 
IMIS is ontwikkeld en wordt gehost door het VLIZ, voor meer informatie contacteer .