Pregled bibliografske jedinice broj: 702876
Post-Roman sea-level changes on Pag Island (Adriatic Sea): Dating Croatia's “enigmatic” coastal notch?
Post-Roman sea-level changes on Pag Island (Adriatic Sea): Dating Croatia's “enigmatic” coastal notch? // Geomorphology, 221 (2014), 83-94 doi:10.1016/j.geomorph.2014.06.002 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 702876 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Post-Roman sea-level changes on Pag Island (Adriatic Sea): Dating Croatia's “enigmatic” coastal notch?
Autori
Marriner, Nick ; Morhange, Christophe ; Faivre, Sanja ; Flaux, Clément ; Vacchi, Matteo ; Miko, Slobodan ; Dumas, Vincent ; Boetto, Giulia ; Radić Rossi, Irena
Izvornik
Geomorphology (0169-555X) 221
(2014);
83-94
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Notch ; Holocene sea level ; Salt-marsh stratigraphy ; Subsidence ; Croatia ; Adriatic
Sažetak
The presence of a regional-wide notch (45 to 115 cm below present biological mean sea level [BMSL]) along the Adriatic coast of Croatia, at a string of sites between Zadar and Rijeka, provides evidence for a rapid but poorly constrained subsidence event(s) after Roman times. For more than a century, this geomorphological tidal level indicator has attracted rich scientific debate but many unresolved questions remain. In this paper, we present new results from Caska Bay (Pag Island) looking at notch morphology and Holocene salt- marsh stratigraphy to constrain the chronology of this crustal deformation on Pag Island. The typical salt-marsh stratigraphy comprises low to high salt-marsh muds interjected by an unconformable marine layer (which lies between −50 and −100 cm BMSL) consistent with an abrupt transgression. The palaeoecological record shows an abrupt shift in assemblages across the salt- marsh mud–sand sediment contact translating abrupt coastal changes. Geochronological data constrain this event to around 1000 to 1200 cal. AD. The altitude of the layer is coeval with the submerged notch attested on limestone cliffs around the bay. The U-shape of the notch profile, coupled with the sharp palaecological contacts and submerged Roman pier, implies that sea-level rise was episodic and not gradual as suggested by regional numerical models. Together, our findings shed new light on the chronology of the “enigmatic” Croatian notch on the island of Pag, and highlight the need to couple geomorphological studies of rocky coasts with high-resolution sediment records.
Izvorni jezik
Engleski
Znanstvena područja
Arheologija, Geografija
POVEZANOST RADA
Projekti:
119-1191306-1305 - Geomorfološka i geoekološka istraživanja krša RH (Faivre, Sanja, MZOS ) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Matematički odjel, Zagreb,
Hrvatski geološki institut,
Sveučilište u Zadru
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus