http://www.cnr.it/ontology/cnr/individuo/prodotto/ID49317
Reply to the comment by C. Ravazzi on \"Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology\" [Quaternary International 140&141, 37-52] (Articolo in rivista)
- Type
- Label
- Reply to the comment by C. Ravazzi on \"Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology\" [Quaternary International 140&141, 37-52] (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.quaint.2006.04.001 (literal)
- Alternative label
Bertoldi R; Canali G; Serandrei Barbero R (*); Donnici S. (*); Lezziero A (2007)
Reply to the comment by C. Ravazzi on "Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology" [Quaternary International 140&141, 37-52]
in Quaternary international
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bertoldi R; Canali G; Serandrei Barbero R (*); Donnici S. (*); Lezziero A (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Note
- Scopu (literal)
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (*) CNR-ISMAR, Sede di Venezia, Castello 1364/a, 30122 Venezia
Dipartimento Biologia Evolutiva e Funzionale, Universita` di Parma, Viale delle Scienze, 43100 Parma, Italy (literal)
- Titolo
- Reply to the comment by C. Ravazzi on \"Paleoclimatic record of the past 22,000 yr in Venice (Northern Italy): Biostratigraphic evidence and chronology\" [Quaternary International 140&141, 37-52] (literal)
- Abstract
- Four new 20-m cores drilled (2000-2001) in the historical city centre of Venice, provided new data on Late Pleistocene and
Holocene deposits from pollen biostratigraphy, foraminiferal associations and 10 new 14C dates.
About 22,000 years ago, alluvial deposits were laid down in an environment characterized by intense flooding with episodes of
swamp conditions between 22,4107130 and 20,8307130 years BP. This full glacial phase was followed by one of prevailing fine
materials between 19,7907120 and 19,2807120 years BP. The Flandrian marine invasion occurred 5520750 years BP, and gave
rise to a layer about 5m thick, in which the foraminiferal associations show ancient channels and buried salt marshes.
Palynological analysis indicates two different pollen zones: one is full glacial, with two phases of climatic warming going back to
the Tursac and Laugerie interstages; the second corresponds to Holocene lagoonal deposits. The main peat layers represent episodes
of stagnation in stadial conditions. The two warm interstages lasted a few centuries. Above the Laugerie interstage, peaty remains in
continental sands underlying the Holocene lagoonal deposits of Atlantic age date back to 9173780-7165760 years BP, showing the
presence of the Early Holocene. (literal)
- Prodotto di
- Autore CNR
- Insieme di parole chiave
Incoming links:
- Prodotto
- Autore CNR di
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi
- Insieme di parole chiave di