MIS1-5 high resolution foraminifera ecostratigraphy in the Adriatic Sea with paleoclimatic inferences for the Late Holocene (EC-EUROSTRATAFORM project) (Comunicazione a convegno)

Type
Label
  • MIS1-5 high resolution foraminifera ecostratigraphy in the Adriatic Sea with paleoclimatic inferences for the Late Holocene (EC-EUROSTRATAFORM project) (Comunicazione a convegno) (literal)
Anno
  • 2006-01-01T00:00:00+01:00 (literal)
Alternative label
  • Piva, A. (1), Asioli, A. (2), Schneider, R. (3), Andersen, N. (4), Langone, L. (1), Vigliotti, L. (1), Trincardi, F. (1) (2006)
    MIS1-5 high resolution foraminifera ecostratigraphy in the Adriatic Sea with paleoclimatic inferences for the Late Holocene (EC-EUROSTRATAFORM project)
    in EGU General Assembly 2006, Vienna (Austria)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Piva, A. (1), Asioli, A. (2), Schneider, R. (3), Andersen, N. (4), Langone, L. (1), Vigliotti, L. (1), Trincardi, F. (1) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
  • Geophysical Research Abstracts, Vol. 8, 04528, 2006 SRef-ID: 1607-7962/gra/EGU06-A-04528 © European Geosciences Union 2006 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#descrizioneSinteticaDelProdotto
  • The EC-EUROSTRATAFORM project allowed obtaining new insights on the Adriatic planktic and benthic foraminifera ecobiostratigraphy for the last 125kyrs. This ecobiostratigraphy has been integrated with O and C stable isotope stratigraphy,tephrochronology, magnetic properties, and 210Pb data. This study is framed in a seismic stratigraphic econstruction of the area and takes into account information from reference cores from previous works. We present a synthesis of the main ecozones detected in the Southern Adriatic for this time interval, with comparisons to the ecozones previously defined in the Central Adriatic. In particular, we present new data for the last 6kyrs from cores collected in Central and Southern Adriatic in complementary shelf (including the modern mud belt) and slope sedimentary settings. The two main planktic foraminifera bioevents for this interval are the well known LO of Globorotalia inflata at ca. 6 kyrs B.P., approximating the maximum flooding surface, and the LCO of Globigerinoides sacculifer at ca. 1200 AD, approximating the beginning of the Little Ice Age (LIA). The planktic foraminifera assemblages revealed, from 6 kyrs to the beginning of the LIA, a paleoclimatic variability much stronger and complex than previously reported in literature for the Adriatic (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • (1) Istituto di Scienze Marine (CNR)–Sezione di Bologna, via Gobetti 101, 40129 Bologna,Italy (2) Istituto di Geoscienze e Georisorse (CNR)- Sezione di Padova, via Giotto, 1, 35137 Padova, Italy, (3) Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel,Ludewig-Meyn-Str. 10, 24118 Kiel, Germany, (4) Leibniz Laboratory for Radiometric Dating and Stable Isotope Research , CAU Kiel, Max-Eyth-Str. 11, D-24118 Kiel, Germany (literal)
Titolo
  • MIS1-5 high resolution foraminifera ecostratigraphy in the Adriatic Sea with paleoclimatic inferences for the Late Holocene (EC-EUROSTRATAFORM project) (literal)
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