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Vertebrate taphonomy, paleontology, sedimentology, and palynology of a fossiliferous Late Devonian fluvial succession, Catskill Formation, north-central Pennsylvania, USA

David R. Broussard, Cayla J. Treaster, Jeffrey M. Trop, Edward B. Daeschler, Pierre A. Zippi, Matthew B. Vrazo and Michael C. Rygel
Vertebrate taphonomy, paleontology, sedimentology, and palynology of a fossiliferous Late Devonian fluvial succession, Catskill Formation, north-central Pennsylvania, USA
Palaios (November 2020) 35 (11): 470-494

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.


ISSN: 0883-1351
Serial Title: Palaios
Serial Volume: 35
Serial Issue: 11
Title: Vertebrate taphonomy, paleontology, sedimentology, and palynology of a fossiliferous Late Devonian fluvial succession, Catskill Formation, north-central Pennsylvania, USA
Affiliation: Lycoming College, Department of Biology, Williamsport, PA, United States
Pages: 470-494
Published: 202011
Text Language: English
Publisher: Society for Sedimentary Geology, Tulsa, OK, United States
References: 114
Accession Number: 2021-006878
Categories: General paleontology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. strat. col., 4 plates, 4 tables, geol. sketch map
N41°40'00" - N41°40'00", W77°00'00" - W77°00'00"
Secondary Affiliation: Bucknell University, USA, United StatesDrexel University, USA, United StatesBiostratigraphy.com, USA, United StatesFood Trust, USA, United StatesState University of New York at Potsdam, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2021, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States. Reference includes data supplied by SEPM (Society for Sedimentary Geology), Tulsa, OK, United States
Update Code: 202105
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