AnimaliaacceptedsuperfamilyAccepted
Colubroidea

Colubroidea

Oppel, 1811

GBIF:229732067

0year

ABOUT

Descriptions(2)

Diagnosis. Vertebral characters used to identify to Colubroidea include: vertebrae longer than wide (length at least 1.2 - 1.3 times as wide at the neural arch) and relatively lightly built (Holman, 2000; Smith, 2013); neural spines thin and long when compared to other groups (Holman, 2000); zygosphenal and zygantral areas less massive than in booids (Holman, 2000); synapophyses distinctly divided into parapophyseal and diapophyseal processes (Holman, 2000); mid- and posterior trunk vertebrae with sharp, relatively thin hemal keels, with hypapophyses often absent in these regions (Rage, 1984; Holman, 2000; Ikeda, 2007; Smith, 2013; Head et al., 2016). When present, trunk vertebral hypapophyses are relatively long and often pointed (Holman, 2000; Ikeda, 2007); both paracotylar and lateral foramina present (Rage, 1984; Ikeda, 2007).
Jacisin Iii, John J., Lawing, A. Michelle (2024): Fossil snakes of the Penny Creek Local Fauna from Webster County, Nebraska, USA, and the first record of snakes from the Early Clarendonian (12.5 - 12 Ma) of North America. Palaeontologia Electronica (a 2) 27 (1): 1-42, DOI: 10.26879/1220, URL: http://dx.doi.org/10.26879/1220
Remarks. There is some disparity in what constitutes the defining characters of colubroid vertebrae because of the vast diversity of the group. As such, we saw it fitting to summarize known characters in this study. Zaher et al. (2009, 2019) point out that no known vertebral synapomorphies currently define Colubroidea, and vertebrae are typically assigned through the combination of the characters listed above. However, Rage (1984) and Ikeda (2007) identified the presence of both paracotylar and lateral foramina together on the vertebrae as consistent throughout the group. Holman (2000) provided a number of additional characters, but some of the proposed characters describe only some groups of colubroids, and as such, are not included in the diagnosis of the group at this time. These disputed characters include the lack of hypapophyses beyond the cervical region in several groups, and possibly the presence of well-developed prezygapophyseal accessory processes, which Ikeda (2007) was unable to find in several Asian viperids. It should be noted that Holman (2000) focused only on North America colubroids, and therefore may have defined the group primarily for North American taxa.
Jacisin Iii, John J., Lawing, A. Michelle (2024): Fossil snakes of the Penny Creek Local Fauna from Webster County, Nebraska, USA, and the first record of snakes from the Early Clarendonian (12.5 - 12 Ma) of North America. Palaeontologia Electronica (a 2) 27 (1): 1-42, DOI: 10.26879/1220, URL: http://dx.doi.org/10.26879/1220

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Source Information

Fossil snakes of the Penny Creek Local Fauna from Webster County, Nebraska, USA, and the first record of snakes from the Early Clarendonian (12.5 - 12 Ma) of North America

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article Jacisin Iii, John J., Lawing, A. Michelle (2024): Fossil snakes of the Penny Creek Local Fauna from Webster County, Nebraska, USA, and the first record of snakes from the Early Clarendonian (12.5 - 12 Ma) of North America. Palaeontologia Electronica (a 2) 27 (1): 1-42, DOI: 10.26879/1220, URL: http://dx.doi.org/10.26879/1220

ABSTRACT

The Penny Creek Local Fauna in southern Webster County, Nebraska, is an early Clarendonian fossil locality within the Ash Hollow Formation. Undescribed fossils from previously collected Penny Creek material represent the first record of snakes from this time interval and confirm the presence of multiple taxa immediately following the Mid-Miocene Climatic Optimum. We identified eight taxa from the locality, including one booid (Charina), three colubrines (Pantherophis, Lampropeltis, and Salvadora), a dipsadid (Heterodon /Paleoheterodon), and several natricids (Neonatrix elongata, Neonatrix magna, and Nerodia). Of these snakes, only Neonatrix is an extinct genus, Charina and Salvadora are presently extirpated from the area, and all other genera are represented in the Central Great Plains today. Habitats occupied by extant members of genera represented in the Penny Creek snake assemblage suggest a relatively open environment with loose substrates and plentiful ground cover near a permanent water source. This further corroborates previous geological and mammalian paleoecological assessments of the Penny Creek area as a somewhat open, woodland-prairie ecotone environment near a permanent, high-energy fluvial water source. Finally, the snakes of Penny Creek help contribute to our understanding of the modernization of North American snake assemblages in the Central Great Plains by providing data for a poorly understood time within the evolution of North American snakes

John J. Jacisin III. Department of Integrative Biology, The University of Texas. Austin, Texas, USA.

john.jacisin@austin.utexas.edu

A. Michelle Lawing. Department of Ecology and Conservation Biology, Texas A&M University. College Station, Texas, USA. alawing@tamu.edu

Jacisin Iii J J, Lawing A M, felipe (2024). Fossil snakes of the Penny Creek Local Fauna from Webster County, Nebraska, USA, and the first record of snakes from the Early Clarendonian (12.5 - 12 Ma) of North America. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.15468/5kavbp accessed via GBIF.org on 2026-06-14.

CC0Published 12/31/2024View dataset
GBIF Usage Key
229732067
Dataset Key
046c2f0d-62aa-4c9e-81a0-98d93b11ca7a
Origin
source
Taxon ID
03B387E8FFA232018786F9FC9DB1FB06.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026