http://www.cnr.it/ontology/cnr/individuo/prodotto/ID49541
Preboreal climatic oscillations recorded by pollen and foraminifera in the southern Adriatic Sea (Articolo in rivista)
- Type
- Label
- Preboreal climatic oscillations recorded by pollen and foraminifera in the southern Adriatic Sea (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Alternative label
Favaretto S. (a), Asioli A. (b), Miola A. (c), Piva A. (d) (2008)
Preboreal climatic oscillations recorded by pollen and foraminifera in the southern Adriatic Sea
in Quaternary international
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Favaretto S. (a), Asioli A. (b), Miola A. (c), Piva A. (d) (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- doi:10.1016/j.quaint.2008.04.005 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (a) Department of Geography, Università di Padova, via del Santo 26, Padova, Italy
(b) Istituto Geoscienze e Georisorse, CNR, Sede di Padova, via Giotto, 1, Padova, Italy
(c) Department of Biology, Università di Padova, via U. Bassi 58/B, 35100 Padova, Italy
(d) Istituto Scienze Marine, CNR, Sede di Bologna, via Gobetti, 101, Bologna, Italy (literal)
- Titolo
- Preboreal climatic oscillations recorded by pollen and foraminifera in the southern Adriatic Sea (literal)
- Abstract
- Core SA03-1 from the southern Adriatic Sea (EC-Eurostrataform project) provides new information about climate changes and palaeocirculation in the Adriatic region during the last deglaciation. The results of an integrated study based on pollen and foraminifera records of the part of the core spanning the late Pleistoceneearly Holocene transition (including the late Younger Dryas, the Preboreal and the beginning of the Boreal) are presented. The major vegetation changes and the short-term oscillations occurred during the early Holocene warming in the southern Adriatic basin on the basis of a high-resolution pollen record are documented. Vegetation changes are correlated to short-term oscillations detected in the foraminifera record during the same interval. The two independent terrestrial and marine proxies indicate at least three short-term cold and dry oscillations occurring at 11.211, 10.810.4 and 10 cal ka BP, according to the agedepth model adopted in this study. Finally, adopting an event-stratigraphy approach, the comparison of these results with two western Mediterranean records of Preboreal short-term oscillations suggest the occurrence of synchronous bio-events in the Mediterranean basin. (literal)
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