AnimaliaNot EvaluatedacceptedspeciesAccepted
Charina prebottae

Charina prebottae

Brattstrom, 1958

GBIF:229732085

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Descriptions(4)

Description. The vertebra appears near square in shape from dorsal view, but is slightly wider at the prezygapophyses than the postzygapophyses. The postzygapophyses are rounded, while the prezygapophyses are moderately pointed with reduced accessory processes, and are raised antero-laterally. The neural spine is low, broad, and is longer than it is tall or wide. The top of the neural spine is weathered, but this does not appear to affect the overall shape of the neural spine in dorsal view. The neural spine tapers in width anteriorly and is incised posteriorly. The zygosphene is dorsally flat and v-shaped overall, with somewhat rounded lateral edges that extend slightly forward on the anterior face. In anterior view, the zygosphene is concave. The neural arch is somewhat flattened and deeply incised posteriorly. The cotyle is round and mildly angled ventrally, with the dorsal edge extending more anteriorly and the ventral edge extending more posteriorly. Paracotylar foramina are absent. The hemal keel is wide, flat, and smooth ending just before reaching the condylar head. It is bordered laterally by a flat indentation, primarily on the anterior end.
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
Figure 5
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. The fossil described here is similar in size and morphology to known species of Charina (see above for description and comparisons with Lichanura). It is most similar to Charina prebottae specimens from other Nebraska localities, as it possesses a more strongly developed hemal keel when compared to the same vertebral region in extant species of Charina (Holman, 1987) and no break in the slope of the anterior neural spine in lateral view as it descends to the zygosphene (Bell and Mead, 1996). Other characters described by Brattstrom (1958) for C. prebottae may represent individual and intracolumnar variation as well as differences between his fossils from California and the fossils from Nebraska. Holman (2000) noted that Charina prebottae also exhibits notable variation across a wide geographic area throughout the Miocene. Previous literature suggests that C. prebottae may be a catch-all taxon for multiple species, as Brattstrom’s (1958) un-illustrated account and subsequent illustrated accounts do not completely match, warranting further in-depth study (Bell and Mead, 1996; Holman, 2000). Although this vertebra is weathered and missing the extreme parts of several of its structures, it exhibits features of the neural spine (Brattstrom, 1958; Bell and Mead, 1996) and hemal keel (Holman, 2000) matching those of C. prebottae. As such, we confer this vertebra to C. prebottae until the taxon is more comprehensively assessed and re-diagnosed.
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
Material. UNSM 139981 (posterior middle trunk vertebra).
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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FIGURE 5. Trunk vertebra of Charina cf. Charina prebottae from the Penny Creek local fauna. From top left: dorsal, ventral, anterior, posterior, and lateral views (anterior to the left). Scale bar equals 1 mm.

Imageimage/png© Jacisin Iii, John J.;Lawing, A. MichelleJacisin Iii, John J.;Lawing, A. Michelle

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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
229732085
Dataset Key
046c2f0d-62aa-4c9e-81a0-98d93b11ca7a
Origin
source
Backbone Key
5935973
Taxon ID
03B387E8FFA0320387A1FE299C03FD86.taxon
Last Crawled
6/9/2026
Last Interpreted
6/9/2026