Late Miocene Desiccation of the Mediterranean

Nature ◽  
1973 ◽  
Vol 242 (5395) ◽  
pp. 240-244 ◽  
Author(s):  
K. J. HSÜ ◽  
W. B. F. RYAN ◽  
M. B. CITA
2017 ◽  
Vol 472 ◽  
pp. 25-37 ◽  
Author(s):  
Dirk Simon ◽  
Alice Marzocchi ◽  
Rachel Flecker ◽  
Daniel J. Lunt ◽  
Frits J. Hilgen ◽  
...  

1998 ◽  
Vol 17 (2) ◽  
pp. 125-130 ◽  
Author(s):  
J. Szczechura

Abstract. Late Middle Miocene (Upper Badenian) strata of the Fore-Carpathian Depression of Poland yield a shallow-water ostracod fauna which contains the species Triebelina raripila (G. W. Müller, 1894) and Carinocythereis carinata (Roemer, 1838). The palaeobiogeographic distribution of the two main species suggests, that in the late Middle Miocene, Central Paratethys was still connected to the Mediterranean, although still separated from the Eastern Paratethys and from southeastern Eurasia. The continuous occurrence of Triebelina raripila and Carinocythereis carinata in the Mediterranean basins, from the Early Miocene to Recent, indicates that marine conditions existed throughout, thereby allowing them to survive the Late Miocene salinity crisis.


2004 ◽  
Vol 19 (1) ◽  
pp. n/a-n/a ◽  
Author(s):  
P. Th. Meijer ◽  
R. Slingerland ◽  
M. J. R. Wortel

2019 ◽  
Vol 6 (1) ◽  
pp. 27-32 ◽  
Author(s):  
Giovanni Pasini ◽  
Alessandro Garassino ◽  
Marco Sami

An assemblage of axiidean and brachyuran decapods is reported from the late Miocene pre-evaporitic (early-middle Messinian) limestone of Cò di Sasso, nearby Brisighella (Ravenna, Emilia- Romagna), located in Romagna Apennines (NE Italy). Except Monodaeus bortolottii Delle Cave, 1988 (Xanthidae MacLeay, 1838), which is reported here for the first time in Miocene, all the other specimens have been assigned to species previously known in the Italian Miocene (Messinian s.l.), but never reported in this area. The report of Galathea cf. G. weinfurteri Bachmayer, 1950 (Galatheidae Samouelle, 1819) and Medorippe ampla Garassino, De Angeli, Gallo and Pasini, 2004 (Dorippidae MacLeay, 1838) enlarges the stratigraphic range of these Miocene species. This report enlarges our limited knowledge on the composition and distribution of the axiidean, anomuran, and brachyuran decapods during the early-middle Messinian before the evaporitic event in the Mediterranean Basin.


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