Add to ORKGThe ratification by IUGS of the recently defined base of the Zanclean Stage and of the Pliocene Series brings years of controversy to an end. The boundary-stratotype of the stage is located in the Eraclea Minoa section on the southern coast of Sicily (Italy), at the base of the Trubi Formation. The age of the Zanclean and Pliocene GSSP at the base of the stage is 5.33 Ma in the orbitally calibrated time scale, and lies within the lowermost reversed episode of the Gilbert Chron (C3n.4r), below the Thvera normal subchron
The data on Tuscan Pliocene basins (which were acquired during recent years) are revised and re-eval...
In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) forma...
A high-resolution magnetostratigraphy (planktonic foraminiferal) biostratigraphy and cyclostratigrap...
The base of the Piacenzian Stage, representing the Lower Pliocene-Middle Pliocene boundary, has been...
TheMiocene-Pliocene boundary in the Northern Apennine was the object of several studies prior to the...
TheMiocene-Pliocene boundary in the Northern Apennine was the object of several studies prior to the...
The concept of a geologically instantaneous earliest Zanclean reflooding of the Mediterranean Basin ...
The data on Tuscan Pliocene basins (which were acquired during recent years) are revised and re-eval...
In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) forma...
Detailed correlations of magnetostratigraphy, biostratigraphy and lithostratigraphy reveal that the ...
The Gelasian has been formally accepted as third (and uppermost) subdivision of the Pliocene Series,...
Over recent decades, with extended exploration of all the oceans, with the study of ice cores from G...
The Calabrian Stage is now formally defined by the Global Boundary Stratotype Section and Point (GSS...
The base of the Priabonian Stage is one of two stage boundaries in the Paleogene that remains to be ...
The base of the Priabonian Stage is one of two stage boundaries in the Paleogene that remains to be ...
The data on Tuscan Pliocene basins (which were acquired during recent years) are revised and re-eval...
In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) forma...
A high-resolution magnetostratigraphy (planktonic foraminiferal) biostratigraphy and cyclostratigrap...
The base of the Piacenzian Stage, representing the Lower Pliocene-Middle Pliocene boundary, has been...
TheMiocene-Pliocene boundary in the Northern Apennine was the object of several studies prior to the...
TheMiocene-Pliocene boundary in the Northern Apennine was the object of several studies prior to the...
The concept of a geologically instantaneous earliest Zanclean reflooding of the Mediterranean Basin ...
The data on Tuscan Pliocene basins (which were acquired during recent years) are revised and re-eval...
In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) forma...
Detailed correlations of magnetostratigraphy, biostratigraphy and lithostratigraphy reveal that the ...
The Gelasian has been formally accepted as third (and uppermost) subdivision of the Pliocene Series,...
Over recent decades, with extended exploration of all the oceans, with the study of ice cores from G...
The Calabrian Stage is now formally defined by the Global Boundary Stratotype Section and Point (GSS...
The base of the Priabonian Stage is one of two stage boundaries in the Paleogene that remains to be ...
The base of the Priabonian Stage is one of two stage boundaries in the Paleogene that remains to be ...
The data on Tuscan Pliocene basins (which were acquired during recent years) are revised and re-eval...
In June 2009, the Executive Committee of the International Union of Geological Sciences (IUGS) forma...
A high-resolution magnetostratigraphy (planktonic foraminiferal) biostratigraphy and cyclostratigrap...