Publication:
Paleochannel and beach-bar palimpsest topography as initial substrate for coralligenous buildups offshore Venice, Italy

dc.creatorTosi, Luigi
dc.creatorZecchin, Massimo
dc.creatorFranchi, Fulvio
dc.creatorBergamasco, Andrea
dc.creatorDa Lio, Cristina
dc.creatorBaradello, Luca
dc.creatorMazzoli, Claudio
dc.creatorMontagna, Paolo
dc.creatorTaviani, Marco
dc.creatorTagliapietra, Davide
dc.creatorCarol, Eleonora Silvina
dc.creatorFranceschini, Gianluca
dc.creatorGiovanardi, Otello
dc.creatorDonnici, Sandra
dc.date.issued2017-12
dc.description.abstractWe provide a model for the genesis of Holocene coralligenous buildups occurring in the northwestern Adriatic Sea offshore Venice at 17-24 m depth. High-resolution geophysical surveys and underwater SCUBA diving reconnaissance revealed meandering shaped morphologies underneath bio-concretionned rocky buildups. These morphologies are inferred to have been inherited from Pleistocene fluvial systems reactivated as tidal channels during the post-Last Glacial Maximum transgression, when the study area was a lagoon protected by a sandy barrier. The lithification of the sandy fossil channel-levee systems is estimated to have occurred at ca. 7 cal. ka BP, likely due to the interaction between marine and less saline fluids related to onshore freshwater discharge at sea through a sealed water-table. The carbonate-cemented sandy layers served as nucleus for subsequent coralligenous buildups growth.
dc.identifierTosi, Luigi; Zecchin, Massimo; Franchi, Fulvio; Bergamasco, Andrea; Da Lio, Cristina; et al.; Paleochannel and beach-bar palimpsest topography as initial substrate for coralligenous buildups offshore Venice, Italy; Nature Publishing Group; Scientific Reports; 7; 1; 12-2017; 1-10
dc.identifier2045-2322
dc.identifierhttp://hdl.handle.net/11336/49363
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/57710
dc.languageeng
dc.publisherNature Publishing Group
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://dx.doi.org/10.1038/s41598-017-01483-z
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/s41598-017-01483-z
dc.subjectQUATERNARY EVOLUTION
dc.subjectADRIATIC SEA
dc.subjectBIO-CONCRETIONNED
dc.titlePaleochannel and beach-bar palimpsest topography as initial substrate for coralligenous buildups offshore Venice, Italy
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion
dspace.entity.typePublication

Files

Collections