PALEOENVIRONMENTAL ANALYSIS OF LATE DEVONIAN TETRAPOD AND FISH ASSEMBLAGES FROM CATSKILL FORMATION SITES IN NORTH-CENTRAL PENNSYLVANIA

2016 ◽  
Author(s):  
Jeffrey M. Trop ◽  
◽  
David Broussard ◽  
Rae Donofrio ◽  
Michael C. Rygel ◽  
...  
Palaios ◽  
2020 ◽  
Vol 35 (11) ◽  
pp. 470-494
Author(s):  
DAVID R. BROUSSARD ◽  
CAYLA J. TREASTER ◽  
JEFFREY M. TROP ◽  
EDWARD B. DAESCHLER ◽  
PIERRE A. ZIPPI ◽  
...  

ABSTRACT The fluvial facies of the Catskill Formation record important ecological events that occurred during Late Devonian time. A well-exposed section between the towns of Blossburg and Covington, in north-central Pennsylvania, contains abundant macrofossils and sedimentary features, making it well-suited for linking Upper Devonian fossil occurrences with depositional environments and sedimentary processes. Strata consist of two distinct fluvial facies: floodplain lithofacies consist of mudrocks, with evidence of pedogenic overprinting and sharp-based sandstones interpreted as crevasse splays; channel-bar lithofacies consist of single- and multi-storied cross-stratified lenticular sandstone bodies interpreted as fluvial channel-bar complexes. Macrofossils occur in 22 discrete horizons spanning > 240 m of stratigraphic succession that include Archanodon bivalve shell impressions, two genera of “placoderms” (Bothriolepis, Phyllolepis), an unidentified acanthodian, and several taxa of sarcopterygian fishes, including lungfish (Dipnoi indet.), Holoptychius, Langlieria, and Sauripterus. Most vertebrate macrofossils are preserved as disarticulated, abraded plates, scales, and bone fragments in sandstone channel-bar deposits. Articulated, unabraded remains are preserved in proximal floodplain deposits. Miospores recovered from Catskill Formation fossil sites in the Blossburg-Covington section belong to the COR subzone of the VCo (Diducites versabilis-Grandispora cornuta) palynological zone, indicating deposition ca. 362 to 361.8 Ma during the late Famennian stage of the Late Devonian. Catskill Formation fluvial strata exposed tens of kilometers to the south and west yield latest Famennian palynomorphs. These broadly contemporaneous continental depositional environments supported Late Devonian vertebrate evolution, including the fin-to-limb transition in tetrapodomorphs, and the possible euryhalinity of vertebrates occupying marine-to-nonmarine transitional habitats.


2010 ◽  
Vol 83 (2-3) ◽  
pp. 91-102 ◽  
Author(s):  
Walter L. Cressler ◽  
Cyrille Prestianni ◽  
Ben A. LePage

2014 ◽  
Vol 88 (6) ◽  
pp. 1251-1256 ◽  
Author(s):  
Wade T. Jones ◽  
Rodney M. Feldmann ◽  
Carrie E. Schweitzer ◽  
Frederick R. Schram ◽  
Rose-Anna Behr ◽  
...  

A single specimen of a shrimp-like crustacean,Devonostenopus pennsylvaniensis, new genus and species is described from the Huntley Mountain Formation, which is Devonian–Carboniferous (Mississippian) in age. The specimen was collected in north-central Pennsylvania.Devonostenopus pennsylvaniensisis attributed to Stenopodidae. Co-occurrence of the specimen with pinnules ofArchaeopteris hallianaGoeppert, 1852, suggests that it is Devonian in age. Occurrence of a stenopodidean in the Devonian of North America is significant, as only three definitive decapods have been previously described from the Paleozoic and only two have been described from the Devonian. The earliest stenopodideans described to date are Cretaceous (Cenomanian and Santonian) in age. As such,Devonostenopus pennsylvaniensisextends the geologic range of Stenopodidea from Cretaceous to Late Devonian. Occurrence of a stenopodidean in the Devonian of North America, as well as the occurrence of the only two other known Devonian decapods in North America, suggests that Laurentia might have been a major area of endemism for Devonian decapods.


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