Serpentes
Lineage (NCBI):
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» Serpentes
node name Serpentes Look for this name in NCBI Wikipedia Animal Diversity Web | ||
recommended citations http://palaeo-electronica.org/content/fc-6 Head, 2015 |
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node minimum age 98.32 Ma OMNH 33520 and 33520 were both collected in the uppermost Cedar Mountain Formation (Mussentuchit Member), Emery County, Utah. The Cedar Mountain Formation spans the Early Cretaceous and Early-Late Cretaceous transition (Cifelli et al., 1997). 40Ar/39Ar dating of Sanidine phenocrysts from smetitic ash horizons directly overlying snake-bearing fossil localities produced a weighted mean age of 98.39 ± 0.07 Ma, which is used as the hard minimum age for Serpentes. | ||
node maximum age 113 Ma The soft maximum age is based on uncertainty in age estimates for late Albian snakes from Algeria. | ||
primary fossil used to date this node | ||
OMNH 33520 | ||
phylogenetic justification
These specimens possess unambiguous apomorphies of all known total clade Serpentes, including a well-developed zygosphene-zygantral articulation consisting of a transversely wide zygosphene with dorsolaterally angled articular facets and a medially convex anterior margin, and a deep zygantrum with distinct ventromedially angled articular facets. Additional characters include synapophyses with distinct para- and diapophyseal articular surfaces, and well-developed intergyapophyseal ridges. These characters do not differentiate between crown and stem taxa, and there are no diagnostic characters present, or defined, for Coniophis. |
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phylogenetic reference(s)
Gardner, J.D. and Cifelli, R.L. 1999. A primitive snake from the Cretaceous of Utah. Special Papers in Palaeontology, 60:87-100
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tree image (click image for full size) | ||
Figure 1 from Head (2015).
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