scholarly journals Karstified and fractured Lower Carboniferous (Mississippian) limestones of the UK ‒ A cryptic geothermal reservoir

Author(s):  
Nadia S. Narayan ◽  
Charlotte A. Adams ◽  
Jon G. Gluyas
2013 ◽  
Vol 151 (2) ◽  
pp. 244-253 ◽  
Author(s):  
GEORGE D. SEVASTOPULO ◽  
MILO BARHAM

AbstractThe Task Group charged with proposing the GSSP for the base of the Serpukhovian Stage (Mississippian, Lower Carboniferous) is likely to use the global First Appearance Datum (FAD) of the conodontLochriea ziegleriin the lineageLochriea nodosa–L.zieglerifor the definition and correlation of the base of the stage. It is important to establish that the FAD ofL.ziegleriin different basins is penecontemporaneous. Ammonoids provide high-resolution biostratigraphy in the Late Mississippian but their use in international correlation is limited by provincialism. However, it is possible to assess the levels of diachronism of the First Occurrence Datum (FOD) ofL.ziegleriin sections in NW Europe using ammonoid zones. Published conodont distribution in the Rhenish Slate Mountains of Germany show the FOD ofL.ziegleriin theEmstites novalisBiozone (upper part of the P2czone of the UK and Ireland) butL.zieglerihas also been reported as occurring in theNeoglyphioceras spiraleBiozone (P1dzone). In the Yoredale Group of northern England, the FOD ofL.ziegleriis in either the P1cor P1dzone. In NW Ireland, the oldest records of bothL.nodosaandL.ziegleriare from theLusitanoceras granosumBiozone (P2a). Although there is some discrepancy in the recorded levels of the FOD ofL.ziegleriin NW Europe, this may be as a result of collection failure. The base of the Serpukhovian based on the FAD ofLochriea ziegleriwill be in the middle of the Brigantian regional Substage.


2019 ◽  
Vol 177 (2) ◽  
pp. 276-282
Author(s):  
Hannah C. Bird ◽  
Angela C. Milner ◽  
Anthony P. Shillito ◽  
Richard J. Butler
Keyword(s):  

2002 ◽  
Vol 21 (2) ◽  
pp. 97-104
Author(s):  
Mark A. Purnell ◽  
Peter H. Von Bitter ◽  
Eric Groessens

Abstract. Lower Carboniferous conodont faunas from shallow shelf and more offshore settings have few taxa in common and correlation is difficult. Consequently, reports of shallow shelf taphrognathid conodonts and indications that the Taphrognathus transatlanticus Range Zone may be recognizable in Lower Carboniferous sequences in Belgium (Conil et al., 1991) are potentially significant for international correlation using conodonts. Here we present a review of the usefulness of taphrognathid conodonts in international correlation and a brief summary of the current state of their taxonomy. Taphrognathus transatlanticus von Bitter & Austin, 1984 cannot be accommodated within Taphrognathus Branson & Mehl, 1941 and, until a new genus is erected, it is best referred to as aff. Taphrognathus transatlanticus. The status of T. rhodesi as a distinct species is uncertain. The affinities of T. alaskensis are currently obscure, but we strongly doubt that it is a species of Taphrognathus. Regarding Belgian taphrognathids, examination of specimens from the collection reported by Conil et al. (1991) reveals that Taphrognathus carinatus (Higgins & Varker, 1982) is present. This extends the geographical range of T. carinatus beyond the UK, but we are unable to confirm the presence of aff T. transatlanticus in Belgium.


2000 ◽  
Vol 111 (1) ◽  
pp. 78-90 ◽  
Author(s):  
C. R. M. Hay ◽  
T. P. Baglin ◽  
P. W. Collins ◽  
F. G. H. Hill ◽  
D. M. Keeling

2006 ◽  
Vol 175 (4S) ◽  
pp. 476-477
Author(s):  
Freddie C. Hamdy ◽  
Joanne Howson ◽  
Athene Lane ◽  
Jenny L. Donovan ◽  
David E. Neal

2006 ◽  
Vol 175 (4S) ◽  
pp. 210-210
Author(s):  
◽  
Freddie C. Hamdy ◽  
Athene Lane ◽  
David E. Neal ◽  
Malcolm Mason ◽  
...  
Keyword(s):  

2003 ◽  
Vol 2 (1) ◽  
pp. 131
Author(s):  
A ZAPHIRIOU ◽  
S ROBB ◽  
G MENDEZ ◽  
T MURRAYTHOMAS ◽  
S HARDMAN ◽  
...  

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