GENETIC PORE TYPES AND A DIAGENESIS LOG FOR CARBONATES AND MICROBIALITE RESERVOIRS (UPPER CAMBRIAN MICROBIAL REEFS, MASON COUNTY, CENTRAL TEXAS)

2017 ◽  
Author(s):  
Jacob Michael Proctor ◽  
◽  
Heath Hilton Hopson ◽  
André W. Droxler ◽  
Naum Derzhi ◽  
...  
Author(s):  
Pulkit Singh ◽  
◽  
André W. Droxler ◽  
Heath H. Hopson ◽  
Pankaj Khanna ◽  
...  

2017 ◽  
Author(s):  
Heath Hilton Hopson ◽  
◽  
Andre W. Droxler ◽  
Pankaj Khanna ◽  
Dan Lehrmann ◽  
...  

2020 ◽  
Vol 121 ◽  
pp. 104590
Author(s):  
Pankaj Khanna ◽  
Michael Pyrcz ◽  
André W. Droxler ◽  
Heath H. Hopson ◽  
Paul M. (Mitch) Harris ◽  
...  

1997 ◽  
Vol 71 (1) ◽  
pp. 86-102 ◽  
Author(s):  
James H. Stitt ◽  
Wendy Metcalf Straatmann

Trilobites assigned to 29 genera and 39 species are reported from the Deadwood Formation in the Black Hills of South Dakota. Two new species, Prosaukia lochmani and Arcifimbria pahasapaensis, are described. Brachiopods are reported from the Taenicephalus Zone.A biostratigraphic zonation is established for the upper part of the Deadwood Formation. The Taenicephalus Zone in the lower part of the study interval is succeeded upsection by the Ellipsocephaloides Zone, both of which are assigned to the Franconian Stage. These two zones are overlain in turn by the Illaenurus and Saukia Zones of the Trempealeauan Stage. These zones are used to correlate this part of the Deadwood with coeval strata in Montana and Wyoming, central Texas, Oklahoma, and Alberta, Canada. The lowstand of sea level that occurred in the Great Basin at the time of the deposition of the Saukiella junia Subzone of the Saukia Zone probably extended eastward into the Black Hills, resulting in the absence of this fauna in the Black Hills.


1998 ◽  
Vol 72 (3) ◽  
pp. 577-584 ◽  
Author(s):  
Ben R. Spincer

The origin and affinity of the problematic Nuia Maslov is reappraised from exceptionally preserved specimens in Upper Cambrian (Sunwaptan) rocks of the Llano Uplift, central Texas. Nuia is suggested to be a radial calcitic ooid that has nucleated on fragments of reworked filamentous calcimicrobes rather than a separate microorganism as has been assumed previously. Nuia is found predominantly in intrareef grainstone accumulations, as well as in interreef grainstones, invariably accompanied by other bioclastic debris showing similar radial calcite ooid overgrowths.


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