THE BEAR GULCH CONGLOMERATE (SERPUKHOVIAN) BEAR GULCH LIMESTONE, CENTRAL MONTANA: INFORMING A STRATIGRAPHIC DEBATE

2017 ◽  
Author(s):  
Amy Singer ◽  
◽  
George D. Stanley ◽  
Nancy W. Hinman
Keyword(s):  
1986 ◽  
Vol 60 (4) ◽  
pp. 952-956 ◽  
Author(s):  
Robt S. Cox

Palynostratigraphic study of the Bear Gulch Member of the Heath Formation, central Montana, indicates an Upper Mississippian age for the deposit corresponding to Carboniferous palynofloral zone TK (ammonoid zone E2b, Namurian A). The palynoflora contains a diverse spore assemblage, including the Mississippian index Tripartites vetustus. In addition, the Bear Gulch Member contains an abundant and diverse acritarch assemblage. The age assignment is consistent with age determinations from studies of the ammonoid, conodont, and bryozoan faunas.


1989 ◽  
Vol 63 (5) ◽  
pp. 578-581 ◽  
Author(s):  
Christopher A. McRoberts ◽  
George D. Stanley

A single limestone slab is described from the Mississippian Bear Gulch Limestone of central Montana containing more than 100 bivalves, including Caneyella sp. and ?Ptychopteria (Actinopteria) sp., attached in original life positions along an 80-cm-long ?brown alga. The assemblage provides clear evidence of life position and choice of substrate for these pterioids. The bivalves increase in size, and appear to be radially disposed in their attachment sites, along the loosely coiled “kelp-like” alga, indicating little postmortem transport and current activity. The bivalve population is interpreted as living on an algal thallus that was either planktonic or attached to the substrate. Observations and comparisons with modern bivalve—seaweed associations support either view. Evidence for local anoxic conditions and stagnant water help explain the superb preservation and confirm past interpretations of the Bear Gulch Limestone.


2006 ◽  
Vol 504 ◽  
pp. 1-8
Author(s):  
Frederick R. Schram ◽  
Arjan C. Boere ◽  
Natalie Thomas
Keyword(s):  

1998 ◽  
Vol 67 (3) ◽  
pp. 155-185 ◽  
Author(s):  
Ronald A. Jenner ◽  
Cees H.J. Hof ◽  
Frederick R. Schram

The palaeostomatopod crustacean Bairdops beargulchensis Schram & Horner, 1978 (Malacostraca, Hoplocarida) from the Mississippian Bear Gulch Limestone is now seen as a taxonomic composite that arose from the confusion of specimens of two distinct hoplocarid species. These species are herein described as the palaeostomatopod Bairdops beargulchensis Schram & Horner, 1978 and a new species of archaeostomatopod, Tyrannophontes acanthocercus. Tyrannophontes acanthocercus is quite distinct from the Pennsylvanian archaeostomatopod T. Theridion from the Essex fauna (Mazon Creek), with which it was originally compared. Bairdops beargulchensis is very similar to the Mississippian palaeostomatopod, B. elegans, from the Scottish Glencartholm fauna. A previously proposed synonymy of B. beargulchensis with T. theridion is therefore rejected. A preliminary restudy of the archaeostomatopods T. Theridion and Gorgonophontes peleron, and the palaeostomatopods Perimecturus Rapax and P. parki, reveals some newly recognized characters of those taxa and suggests some novel interpretations of hoplocarid evolution. A cladistic phylogenetic analysis of the Hoplocarida including the Paleozoic forms resolves the higher level relationships of the hoplocarids (palaeostomatopods, archaeostomatopods, aeschronectids, and unipeltatans).


Stratigraphy ◽  
2017 ◽  
Vol 14 (1-4) ◽  
pp. 97-122 ◽  
Author(s):  
Julie A. Dumoulin ◽  
Craig A. Johnson ◽  
Karen D. Kelley ◽  
Palma Jarboe ◽  
Paul Hackley ◽  
...  
Keyword(s):  

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