Category Archives: Priabonian

Priabonian stratotype

GSSP for Priabonian Stage (Eocene) Definition: The GSSP for the Base of the Priabonian Stage (Paleogene System, Eocene Series) is defined at meter level 63.57 in the Alano section (Alano di Piave, NE Italy: 45°54’51.10″N – 11°55’4.87″E). This level coincides with the base of a prominent crystal tuff layer, the Tiziano bed for which absolute […]

Priabonian of the Urtsadzor section (Armenia)

Upcoming paper in Newsletter on Stratigraphy: Integrated stratigraphy of the Priabonian (upper Eocene) Urtsadzor section, by Laura J. Cotton, Elena Y. Zakrevskaya, Annique van der Boon, Gayane Asatryan, Flora  Hayrapetyan, Arsen Israyelyan, Wout Krijgsman, György Less, Simonetta Monechi, Cesare  A. Papazzoni, Paul N. Pearson, Anatoly Razumovskiy, Willem Renema, Ekaterina Shcherbinina and Bridget S. Wade, presented […]

Annual Report Priabonian – 2004

Annual Report 2004 of the Bartonian/Priabonian Boundary Stratotype Working Group The Veneto region in the Southern Alps (NE Italy) is a classical area for the Paleogene Stratigraphy. In particular, the historical stratotype and the parastratotype of the Priabonian (Munier-Chalmas & De Lapparent, 1893) stage are located close to the Priabona and Possagno villages, respectively. However, […]

Annual Report Priabonian – 2005

Annual Report 2005 of the Bartonian/Priabonian Boundary Stratotype Working Group A great wealth of data have been collected on the well-exposed Alano section (Veneto region, NE Italy), a potential candidate for the Upper Eocene GSSP. In particular, the >120 m-thick section is now completely sampled in high resolution for multiple biostratigraphies. The surveyed section spans […]

Annual Report Priabonian – 2006

Annual Report 2006 of the Bartonian/Priabonian Boundary Stratotype Working Group Studies in 2006 focused on the Alano di Piave section (Veneto region, NE Italy), the potential candidate for defining the GSSP of Middle/Upper Eocene, equated to the base of the Priabonian Stage. The Alano section, continuously exposed along the banks of the Calcino Creek, consists […]

Annual Report Priabonian – 2007

Annual Report 2007 of the Bartonian/Priabonian Boundary Stratotype Working Group Tasks of the Italian scientific community were to search for GSSPs of the Middle-Upper Eocene Transition. Investigations on both transitions have been undertaken by a number of researchers from several Italian Universities (i.e. Padua, Ferrara, Urbino, Milan) and CNR Institutes as well as from some […]

Annual Report Priabonian – 2008

Annual Report 2008 of the Bartonian/Priabonian Boundary Stratotype Working Group Tasks of the Italian scientific community were to search for GSSPs of the Middle-Upper Eocene and Lower-Upper Oligocene Transitions. Investigations on both transitions have been undertaken by a number of researchers from several Italian Universities (i.e. Padua, Ferrara, Florence, Urbino, Milan) and CNR Institutes as […]

Annual Report Priabonian – 2009

Annual Report 2009 of the Bartonian/Priabonian Boundary Stratotype Working Group Tasks of the Italian scientific community were to search for GSSPs of the Middle-Upper Eocene and Lower-Upper Oligocene Transitions. Investigations on both transitions have been undertaken by a number of researchers from several Italian Universities (i.e. Padua, Ferrara, Florence, Urbino, Milan) and CNR Institutes as […]

Annual Report Priabonian – 2010

Annual Report 2010 of the Bartonian/Priabonian Boundary Stratotype Working Group The Italian scientific community was very active in 2010. Investigations on GSSPs of the Middle-Upper Eocene transition have been completed by a number of researchers from several Italian Universities (i.e. Padua, Ferrara, Florence, Urbino, Milan) and CNR Institutes as well as from some European and […]

Annual Report Priabonian – 2011

Annual Report 2011 of the Bartonian/Priabonian Boundary Stratotype Working Group The multidisciplinary studies on the Alano di Piave section (Veneto region, NE Italy), the potential candidate for defining the GSSP of the Middle/Upper Eocene, equated to the base of the Priabonian Stage, have been presented in an article entitled “Integrated bio-magnetostratigraphy of the Alano section […]