The results of a high-resolution multidisciplinary stratigraphic study of a lower Langhian succession, located in theHyblean Plateau (SE Sicily, southern Italy), are here presented.The about 33m thick succession, which belongs to the “Ragusa Fm” (Auct.), has been recovered through a continuous coring surveyand highly-spaced sampled. A total amount of 281 samples has been collected at an average interval of about 12 cm for the followinganalyses: quantitative calcareous nannofossil and planktonic foraminifer biostratigraphy, paleomagnetism, CaCO3 content.The distribution pattern of biostratigraphically significant taxa was reconstructed and paleomagnetostratigraphic data providedtemporal constrains. Cyclostratigraphic reconstruction and astrochronological calibration of the section are proposed, based on theavailable bio- and magnetostratigraphic data, combined with the fluctuations of the Calcium carbonate content.Our results demonstrate that the section entirely falls within the magnetozone C5Br and spans the interval from 15.163 to 15.968Ma. High-resolution stratigraphic data for the early Langhian time interval, including a set of well established calcareous planktonevents, are provided. Thus, the present section plays a strategic role as correlation tool among different coeval successions, in the frameworkof a wider project aiming at the definition of the Global Stratigraphic Section and Point of the Langhian Stage.

High–resolution stratigraphy of the Contrada Pesciarello borehole succession (SE Sicily):a lower Langhian reference section for the Mediterranean region

DI STEFANO, Agata;MANISCALCO, ROSANNA;
2011

Abstract

The results of a high-resolution multidisciplinary stratigraphic study of a lower Langhian succession, located in theHyblean Plateau (SE Sicily, southern Italy), are here presented.The about 33m thick succession, which belongs to the “Ragusa Fm” (Auct.), has been recovered through a continuous coring surveyand highly-spaced sampled. A total amount of 281 samples has been collected at an average interval of about 12 cm for the followinganalyses: quantitative calcareous nannofossil and planktonic foraminifer biostratigraphy, paleomagnetism, CaCO3 content.The distribution pattern of biostratigraphically significant taxa was reconstructed and paleomagnetostratigraphic data providedtemporal constrains. Cyclostratigraphic reconstruction and astrochronological calibration of the section are proposed, based on theavailable bio- and magnetostratigraphic data, combined with the fluctuations of the Calcium carbonate content.Our results demonstrate that the section entirely falls within the magnetozone C5Br and spans the interval from 15.163 to 15.968Ma. High-resolution stratigraphic data for the early Langhian time interval, including a set of well established calcareous planktonevents, are provided. Thus, the present section plays a strategic role as correlation tool among different coeval successions, in the frameworkof a wider project aiming at the definition of the Global Stratigraphic Section and Point of the Langhian Stage.
SE Sicily; Middle Miocene; calcareous plankton biostratigraphy
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/20.500.11769/20865
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