Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian Margin (western Tethys): a record of glacioeustatic fluctuations during the greenhouse Cretaceous? (Articolo in rivista)

Type
Label
  • Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian Margin (western Tethys): a record of glacioeustatic fluctuations during the greenhouse Cretaceous? (Articolo in rivista) (literal)
Anno
  • 2009-01-01T00:00:00+01:00 (literal)
Alternative label
  • Galeotti S., Rusciadelli G., Sprovieri M., Lanci L., Pekar S. (2009)
    Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian Margin (western Tethys): a record of glacioeustatic fluctuations during the greenhouse Cretaceous?
    in Palaeogeography, palaeoclimatology, palaeoecology
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Galeotti S., Rusciadelli G., Sprovieri M., Lanci L., Pekar S. (literal)
Pagina inizio
  • 196 (literal)
Pagina fine
  • 205 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 276 (literal)
Rivista
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Istituto di Scienze della Terra, Università degli Studi di Urbino 'Carlo Bo', Campus Scientifico - Località Crocicchia, 61029 Urbino, Italy; Dipartimento di Scienze della Terra Università G. d'Annunzio di Chieti Via dei Vestini, 30, 66013 Chieti Scalo, Italy; Istituto per l'Ambiente Marino Costiero (CNR), Naples, Italy; School of Earth and Environmental Sciences, Queens College, CUNY, 65-30 Kissena Blvd., Flushing, New York 11367, USA; Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA (literal)
Titolo
  • Sea-level control on facies architecture in the Cenomanian-Coniacian Apulian Margin (western Tethys): a record of glacioeustatic fluctuations during the greenhouse Cretaceous? (literal)
Abstract
  • The integrated chemo-, bio- and sequence stratigraphy from the Cenomanian-Coniacian base-of-slope succession of Monte Turno (Abruzzo, central Italy) provides a fine scale calibration of the local sea-level curve inferred from the adjacent platform to records of global sea-level change. Our results indicate that regional marine regressions were coincident with episodes of global cooling and sea-level fall, providing evidences for a causal link between climate changes and sea-level changes. The presence of small polar icecaps during the assumed ice-free Cretaceous is a likely explanation for the observed pattern. (literal)
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