http://www.cnr.it/ontology/cnr/individuo/prodotto/ID178152

Deep Marine Record from Sentinelle Valley (Sardinia Channel): Integrated Stratigraphy of A Key Site for Western Mediterranean Paleoceanographic and Geological Reconstruction (Articolo in rivista)

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Label

Deep Marine Record from Sentinelle Valley (Sardinia Channel): Integrated Stratigraphy of A Key Site for Western Mediterranean Paleoceanographic and Geological Reconstruction (Articolo in rivista) (literal)

Anno

Alternative label

F. Budillon; F. Lirer; M. Iorio; P. Macrì; L. Sagnotti; M. Vallefuoco; L. Ferraro; S. Innangi; G. Di Martino; R. Tonielli (2011)
Deep Marine Record from Sentinelle Valley (Sardinia Channel): Integrated Stratigraphy of A Key Site for Western Mediterranean Paleoceanographic and Geological Reconstruction
in DTA; Consiglio Nazionale delle Ricerche - Dipartimento Terra e Ambiente, Roma (Italia)
(literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

F. Budillon; F. Lirer; M. Iorio; P. Macrì; L. Sagnotti; M. Vallefuoco; L. Ferraro; S. Innangi; G. Di Martino; R. Tonielli (literal)

Pagina inizio

Pagina fine

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

Rivista

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

Istituto per l'Ambiente Marino Costiero, IAMC-CNR, Naples, Italy; Istittuto Nazionale di Geofisica e Vulcanologia, INGV, Rome, Italy (literal)

Titolo

Deep Marine Record from Sentinelle Valley (Sardinia Channel): Integrated Stratigraphy of A Key Site for Western Mediterranean Paleoceanographic and Geological Reconstruction (literal)

Abstract

Biotic, petrophysical, paleomagnetic proxies combined with 14C AMS data allowed us to produce, for deep marine record of Sentinelle Valley (Sardinia Channel), a detailed integrated stratigraphic time-framework for the last 80 kyr. Major planktonic foraminiferal changes in quantitative distribution of selected climate sensitive species allowed the identification of 10 eco-biozones and the main climatic global events (Sapropel S1, Younger Dryas, Greenland Isotope Interstadial 1, Greenland Isotope Stadial 2, Heinrich events H1-H6). An accurate age-depth profile has been proposed for the studied record which spans between 2 and 83 kyr cal. BP. The adopted age model was successively confirmed by comparing the colour reflectance data of the studied record with the astronomically tuned deep marine record ODP-Site 964 from the Ionian Sea. Three turbidite event layers were chronologically constrained within the relative low stand and lowering sea level phases associated to the MIS 4 and MIS 3. (literal)

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