Review of Irish Lower Carboniferous (Mississippian) Mud Mounds

Author(s):  
Ian D. Somerville
Author(s):  
Pedro Cózar ◽  
Marta Rodríguez-Martínez ◽  
Santiago Falces ◽  
Ramón Mas ◽  
Sergio Rodríguez

2009 ◽  
pp. 273-287 ◽  
Author(s):  
D. L. Meyer ◽  
W. I. Ausich ◽  
D. T. Bohl ◽  
W. A. Norris ◽  
P. E. Potter

2017 ◽  
Vol 120 (3) ◽  
pp. 421-432 ◽  
Author(s):  
C. Browning ◽  
M. Reid

AbstractThe Lower Carboniferous, probably Tournaisian, Kweekvlei Formation is part of the Witteberg Group (Cape Supergroup) of South Africa. Together with the overlying Floriskraal Formation, it forms an upward-coarsening succession within the Lake Mentz Subgroup. Sedimentary features of the Kweekvlei Formation suggest deposition in a storm-wave dominated marine setting, within the storm-influenced, distal part of an offshore transition zone environment. This predominantly argillaceous formation preserves a low diversity trace fossil assemblage. Reworked vascular plant debris (including the problematic genus Praeramunculus sp.) and a shark spine have been reported for the Kweekvlei Formation. There are no known stratigraphic equivalents in South Africa.


Author(s):  
Christian Scheibner ◽  
Christoph Hartkopf-Fröder ◽  
Dierk Blomeier ◽  
Holger Forke
Keyword(s):  

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