Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/12854
Authors: Giaccio, Biagio* 
Leicher, Niklas* 
Mannella, Giorgio* 
Monaco, Lorenzo* 
Regattieri, Eleonora* 
Wagner, Bernd* 
Zanchetta, Giovanni* 
Gaeta, Mario* 
Marra, Fabrizio* 
Nomade, Sebastien* 
Palladino, Danilo Mauro* 
Pereira, Alison* 
Scheidt, Stephanie* 
Sottili, Gianluca* 
Wonik, Thomas* 
Wulf, Sabine* 
Zeeden, Christian* 
Ariztegui, Daniel* 
Cavinato, Gian Paolo* 
Dean, Jonathan R.* 
Florindo, Fabio* 
Leng, Melanie J.* 
Macrì, Patrizia* 
Niespolo, Elizabeth* 
Renne, Paul. R.* 
Rolf, Christian* 
Sadori, Laura* 
Thomas, Camille* 
Tzedakis, Polychronis* 
Title: Extending the tephra and palaeoenvironmental record of the Central Mediterranean back to 430 ka: A new core from Fucino Basin, central Italy
Journal: Quaternary Science Reviews 
Series/Report no.: /225 (2019)
Issue Date: Oct-2019
DOI: 10.1016/j.quascirev.2019.106003
Abstract: Here we present the first tephrostratigraphic, palaeomagnetic, and multiproxy data from a new ~98 m deep sediment core retrieved from the Fucino Basin, central Italy, spanning the last ~430 kyr. Palaeoenvironmental proxy data (Ca-XRF, gamma ray and magnetic susceptibility) show a cyclical variability related to interglacial-glacial cycles since the Marine Isotope Stage (MIS) 12-MIS 11 transition. More than 130 tephra layers are visible to the naked eye, 11 of which were analysed (glass-WDS) and successfully correlated to known eruptions and/or other equivalent tephra. In addition to tephra already recognised in the previously investigated cores spanning the last 190 kyr, we identified for the first time tephra from the eruptions of: Tufo Giallo di Sacrofano, Sabatini (288.0 ± 2.0 ka); Villa Senni, Colli Albani (367.5 ± 1.6 ka); Pozzolane Nere and its precursor, Colli Albani (405.0 ± 2.0 ka, and 407.1 ± 4.2 ka, respectively) and Castel Broco, Vulsini (419e490 ka). The latter occurs at the bottom of the core and has been 40Ar/39Ar dated at 424.3 ± 3.2 ka, thus providing a robust chronological constrain for both the eruption itself and the base of the investigated succession. Direct 40Ar/39Ar dating and tephra geochemical fingerprinting provide a preliminary radioisotopic-based chronological framework for the MIS 11-MIS 7 interval, which represent a foundation for the forthcoming multiproxy studies and for investigating the remaining ~110 tephra layers that are recorded within this interval. Such future developments will contribute towards an improved MIS 11-MIS 7 Mediterranean tephrostratigraphy, which is still poorly explored and exploited.
Appears in Collections:Article published / in press

Files in This Item:
File Description SizeFormat Existing users please Login
Giaccio et al., 2019.pdf8.37 MBAdobe PDF
Giaccio et al_Fucino F4-F5_revised manuscript_text_figs.pdfOpen Access3.69 MBAdobe PDFView/Open
Show full item record

WEB OF SCIENCETM
Citations 20

6
Last Week
0
Last month
checked on Feb 7, 2021

Page view(s)

161
Last Week
0
Last month
6
checked on Sep 27, 2021

Download(s)

15
checked on Sep 27, 2021

Google ScholarTM

Check

Altmetric