Luca Giusberti
University of Padua
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Publication
Featured researches published by Luca Giusberti.
Geological Society of America Bulletin | 2007
Luca Giusberti; Domenico Rio; Claudia Agnini; Jan Backman; Eliana Fornaciari; Fabio Tateo; Massimo Oddone
Mode and tempo of an expanded Paleocene Eocene Thermal Maximum section in the Venetian Pre-Alps
Paleoceanography | 2009
Claudia Agnini; Patrizia Macrì; Jan Backman; Henk Brinkhuis; Eliana Fornaciari; Luca Giusberti; Valeria Luciani; Domenico Rio; Appy Sluijs; Fabio Speranza
An early Eocene carbon cycle perturbation at ~52.5 Ma from the southern Alps: Chronology and biotic response
Geological Society of America Bulletin | 2011
Claudia Agnini; Eliana Fornaciari; Luca Giusberti; Paolo Grandesso; Luca Lanci; Valeria Luciani; Giovanni Muttoni; Heiko Pälike; Domenico Rio; David J. A. Spofforth; Cristina Stefani
The Alano section has been presented at the International Subcommission on Paleogene Stratigraphy (ISPS) as a potential candidate for defi ning the global boundary stratotype section and point (GSSP) of the late Eocene Priabonian Stage. The section is located in the Venetian Southern Alps of the Veneto region (NE Italy), which is the type area of the Priabonian, being exposed along the banks of the Calcino torrent, near the village of Alano di Piave. It consists of ~120–130 m of bathyal gray marls interrupted in the lower part by an 8-m-thick package of laminated dark to black marlstones. Intercalated in the section, there are eight prominent marker beds, six of which are crystal tuff layers, whereas the other two are bioclastic rudites. These distinctive layers are useful for regional correlation and for an easy recognition of the various intervals of the section. The section is easily accessible, crops out continuously, is unaffected by any structural deformation, is rich in calcareous plankton, and contains an expanded record of the critical interval for defi ning the GSSP of the Priabonian. In order to further check the stratigraphic completeness of the section and constrain in time the critical interval for defi ning the Priabonian Stage, we performed a high-resolution study of integrated calcareous plankton biostratigraphy and a detailed magnetostratigraphic analysis. Here, we present the results of these studies to open a discussion on the criteria for driving the “golden spike” that should define the middle Eocene–late Eocene boundary.
Paleoceanography | 2010
David J. A. Spofforth; Claudia Agnini; Heiko Pälike; Domenico Rio; Eliana Fornaciari; Luca Giusberti; Valeria Luciani; Luca Lanci; Giovanni Muttoni
We present trace metal geochemistry and stable isotope records for the middle Eocene Alano di Piave section, NE Italy, deposited during magnetochron C18n in the marginal Tethys Ocean. We identify a
Paleoceanography | 2014
F. Boscolo Galazzo; Ellen Thomas; Mark Pagani; C. Warren; Valeria Luciani; Luca Giusberti
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Rivista Italiana Di Paleontologia E Stratigrafia | 2005
Luca Giusberti; Marco Fantin; John Buckeridge
500 kyr long carbon isotope perturbation event we infer to be the middle Eocene Climatic Optimum (MECO) confirming the northern hemisphere expression and global occurrence of MECO. Interpreted peak climatic conditions are followed by the rapid deposition of two organic rich intervals (
Paleoceanography | 2016
Roberta D'Onofrio; Valeria Luciani; Eliana Fornaciari; Luca Giusberti; Flavia Boscolo Galazzo; Edoardo Dallanave; Thomas Westerhold; Mario Sprovieri; Sonia Telch
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Facies | 2016
Alessandro Vescogni; Francesca R. Bosellini; Cesare Andrea Papazzoni; Luca Giusberti; Guido Roghi; Eliana Fornaciari; Stefano Dominici; Roberto Zorzin
3\% TOC) and contemporaneous positive
PALAIOS | 2017
Cesare Andrea Papazzoni; Eliana Fornaciari; Luca Giusberti; Alessandro Vescogni; Beatrice Fornaciari
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Rivista Italiana Di Paleontologia E Stratigrafia | 2016
Elena Ghezzo; Luca Giusberti
C excursions. These two intervals are associated with increases in the concentration of sulphur and redox-sensitive trace metals, and low concentrations of Mn, as well as coupled with the occurrence of pyrite. Together these changes imply low, possibly dysoxic, bottom water O