scholarly journals “Draculamya” uraniae: A New Small-Sized Bivalve from the Mediterranean Sea (Galeommatida, Lasaeidae)

Taxonomy ◽  
2021 ◽  
Vol 1 (2) ◽  
pp. 142-151
Author(s):  
Luigi Romani ◽  
Stefano Bartolini ◽  
P. Graham Oliver ◽  
Marco Taviani

A new Galeommatid bivalve is described for the Mediterranean Sea, tentatively assigned to the elusive genus Draculamya Oliver and Lützen, 2011. “Draculamya” uraniae n. sp is described upon a number of dead but fresh and articulated specimens, plus many loose valves. Its distribution is almost basin-wide in the Mediterranean, and it possibly occurs in the adjacent Gulf of Cadiz. As for many members in Galeommatida, we hypothesize that “Draculamya” uraniae lives as commensal upon a still-unknown host. The possible co-identity of the extant genus Draculamya with the morphologically similar Pliocene Glibertia Van der Meulen, 1951, is discussed, although the lack of anatomical and genetic support leaves the problem open.

2014 ◽  
Vol 34 (2-3) ◽  
pp. 89-110 ◽  
Author(s):  
Jean Mascle ◽  
Flore Mary ◽  
Daniel Praeg ◽  
Laetitia Brosolo ◽  
Laurent Camera ◽  
...  

2021 ◽  
pp. 103578
Author(s):  
P.M. De Martini ◽  
H.J. Bruins ◽  
L. Feist ◽  
B.N. Goodman-Tchernov ◽  
H. Hadler ◽  
...  

2020 ◽  
Vol 719 ◽  
pp. 134964 ◽  
Author(s):  
I. Laiz ◽  
S. Plecha ◽  
A. Teles-Machado ◽  
E. González-Ortegón ◽  
D. Sánchez-Quiles ◽  
...  

2021 ◽  
Vol 41 (2) ◽  
Author(s):  
Zhi Lin Ng ◽  
F. Javier Hernández-Molina ◽  
Débora Duarte ◽  
Francisco J. Sierro ◽  
Santiago Ledesma ◽  
...  

AbstractThe Mediterranean-Atlantic water mass exchange provides the ideal setting for deciphering the role of gateway evolution in ocean circulation. However, the dynamics of Mediterranean Outflow Water (MOW) during the closure of the Late Miocene Mediterranean-Atlantic gateways are poorly understood. Here, we define the sedimentary evolution of Neogene basins from the Gulf of Cádiz to the West Iberian margin to investigate MOW circulation during the latest Miocene. Seismic interpretation highlights a middle to upper Messinian seismic unit of transparent facies, whose base predates the onset of the Messinian salinity crisis (MSC). Its facies and distribution imply a predominantly hemipelagic environment along the Atlantic margins, suggesting an absence or intermittence of MOW preceding evaporite precipitation in the Mediterranean, simultaneous to progressive gateway restriction. The removal of MOW from the Mediterranean-Atlantic water mass exchange reorganized the Atlantic water masses and is correlated to a severe weakening of the Atlantic Meridional Overturning Circulation (AMOC) and a period of further cooling in the North Atlantic during the latest Miocene.


2008 ◽  
Vol 71 (1-2) ◽  
pp. 195-220 ◽  
Author(s):  
I. Ambar ◽  
N. Serra ◽  
F. Neves ◽  
T. Ferreira

2007 ◽  
Vol 28 (4) ◽  
pp. 379-394 ◽  
Author(s):  
Estefania Llave ◽  
Francisco J. Hernández-Molina ◽  
Dorrik A. V. Stow ◽  
Mari Carmen Fernández-Puga ◽  
Margarita García ◽  
...  

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