Integrated stratigraphy and 40Ar/39Ar chronology of early Middle Miocene sediments from DSDP Leg 42A, Site 372 (Western Mediterranean)

2008 ◽  
Vol 257 (1-2) ◽  
pp. 123-138 ◽  
Author(s):  
H. Abdul Aziz ◽  
A. Di Stefano ◽  
L.M. Foresi ◽  
F.J. Hilgen ◽  
S.M. Iaccarino ◽  
...  
1962 ◽  
Vol S7-IV (5) ◽  
pp. 760-773 ◽  
Author(s):  
Claude Grandjacquet

Abstract A large view of the evolution and structural history of the Tyrrhenian sea and bordering areas suggests that towards the end of the Permian distensions occurring in the western Mediterranean resulted in the opening of a passage to the Atlantic. Lower Eocene deformations along the Sicilian-Tunisian front were either due to local marginal disequilibrium or to the northern drift of the African continent. Oligocene emergence is evident in the Apennines and in Calabria through the existence of widespread hiatuses and by bauxitic and ferruginous beds. Large scale Oligocene movements brought the African continent to its maximum proximity with Europe. It was in the same period that the clay scaglia and flysch nappes began sliding in Tuscany although the movement of Calabrian nappes in southern Italy did not occur until the lower and middle Miocene.


2009 ◽  
Vol 99 (8) ◽  
pp. 1859-1886 ◽  
Author(s):  
Hayfaa Abdul Aziz ◽  
Madelaine Böhme ◽  
Alexander Rocholl ◽  
Jerome Prieto ◽  
Jan R. Wijbrans ◽  
...  

2017 ◽  
Vol 68 (2) ◽  
pp. 109-118 ◽  
Author(s):  
Nicoletta Mancin ◽  
Michael A. Kaminski

Abstract The occurrence of agglutinated foraminiferal specimens belonging to the Badenian (middle Miocene) genus Colominella Popescu, 1998 was recently documented for the first time in a lower Pliocene succession of the western Mediterranean area. Direct comparisons with topotype specimens of Colominella paalzowi (Cushman 1936), sampled in the Badenian type section of Lăpugiu de Sus (Transylvania), show that the Pliocene individuals from the western Mediterranean morphologically resemble the type species C. paalzowi, but they also differ in possessing a longer biserial chamber arrangement with a higher number of internal chamber partitions, in lacking a clear early triserial stage and in having a more complex microstructure of the agglutinated wall, thereby supporting the idea that the Pliocene Mediterranean specimens represent a new, more highly evolved species. The fact that the Pliocene individuals from the Mediterranean appear to be more evolved with respect to the Badenian specimens from Paratethys represents an interesting evolutionary development of the genus Colominella that also permits the known stratigraphical and geographical range of the genus, previously limited to the middle Miocene (Badenian) of the Paratethys, to be extended.


2018 ◽  
Vol 48 (2) ◽  
pp. 172-180 ◽  
Author(s):  
Nicoletta Mancin ◽  
Michael A. Kaminski

AbstractWe formally describe a new agglutinated foraminiferal species belonging to the genus Colominella Popescu, 1998 (Textulariida) recovered in two Pliocene successions of the western Mediterranean region. The formal description of Colominella piriniae n. sp. reported here permits the known stratigraphical and geographical range of the genus, previously limited to the Badenian (middle Miocene) of the Paratethys, to be extended into the Pliocene of the Mediterranean. The present work demonstrates the importance of microstructural studies performed on sectioned specimens in taxonomic assignments and reviews.


2020 ◽  
Vol 35 (1) ◽  
pp. 89
Author(s):  
Ignacio García-Sanz ◽  
Juan Usera ◽  
Jordi Guillem ◽  
Carmen Alberola

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