TL;DR: This work focuses on a group of squamate reptiles that share similar ecological requirements and generally occupy the same communities in the western USA, and finds significant congruence between the phylogeographies of E. multicarinata and L. zonata suggests that the succession of vicariance and dispersal events in these species progressed in concert.
Abstract: The ultimate goal of comparative phylogeographical analyses is to infer processes of diversification from contemporary geographical patterns of genetic diversity. When such studies are employed across diverse groups in an array of communities, it may be difficult to discover common evolutionary and ecological processes associated with diversification. In order to identify taxa that have responded in a similar fashion to historical events, we conducted comparative phylogeographical analyses on a phylogenetically and ecologically limited set of taxa. Here, we focus on a group of squamate reptiles (snakes and lizards) that share similar ecological requirements and generally occupy the same communities in the western USA. At a gross level, deep genetic division in Contia tenuis, Diadophis punctatus, Elgaria multicarinata, the Charina bottae complex, and Lampropeltis zonata are often concordant in the Transverse Ranges, the Monterey Bay and Sacramento-San Joaquin Delta region, and the southern Sierra Nevada in California. Molecular clock estimates suggest that major phyletic breaks within many of these taxa roughly coincide temporally, and may correspond to important geological events. Furthermore, significant congruence between the phylogeographies of E. multicarinata and L. zonata suggests that the succession of vicariance and dispersal events in these species progressed in concert. Such congruence suggests that E. multicarinata and L. zonata have occupied the same communities through time. However, across our entire multi-taxon data set, the sequence of branching events rarely match between sympatric taxa, indicating the importance of subtle differences in life history features as well as random processes in creating unique genetic patterns. Lastly, coalescent and noncoalescent estimates of population expansion suggest that populations in the more southerly distributed clades of C. tenuis, D. punctatus, E. multicarinata, and L. zonata have been stable, while populations in more northerly clades appear to have recently expanded. This concerted demographic response is consistent with palaeontological data and previous phylogeographical work that suggests that woodland habitat has become more restricted in southern California, but more widespread in the North during Holocene warming. Future phylogeographical work focusing on allied and ecologically associated taxa may add insight into the ecological and evolutionary processes that yield current patterns of genetic diversity.
TL;DR: Microcomplement fixation immunological data are presented concerning the relationships of several genera of xenodontines to two major clades within that radiation, the previously recognized Central and South American lineages, and it is suggested that an African origin is as likely as an Asian-North American origin for the neotropical lineages.
Abstract: Microcomplement fixation immunological data are presented concerning the relationships of several genera of xenodontines to two major clades within that radiation, the previously recognized Central and South American lineages. Heterodon, Farancia, Carphophis and Conophis probably represent independent lineages. The phylogenetic placements of Diadophis and Contia are ambiguous. Comparisons with representatives of other colubrid lineages do not confirm that the xenodontine lineages discussed are monophyletic. However, no association can be demonstrated between any xenodontine lineage and representatives of the other lineages tested. The albumin divergence among New World colubrines strongly suggests that they are not monophyletic relative to Old World colubrines and that the diversification of New and Old World colubrine genera occurred subsequent to the separation of the major xenodontine lineages. Xenodontines may be older than the fossil record indicates, and an African origin is as likely as an Asian-North American origin for the neotropical lineages.
TL;DR: Contia longicaudae as mentioned in this paper is a colubroid snake from California and Oregon, USA, which is genetically cohesive, possesses a greater number of caudal scales, a proportionately longer tail and tends to be larger overall with more pronounced dorso-lateral stripes and a more muted ventral coloration than C. tenuis.
Abstract: We describe Contia longicaudae, a new colubroid snake from California and Oregon, USA. Because C. longicaudae differs only subtly from the nominate species, C. tenuis, it has long been overlooked. However, genetic and morphological data readily distinguish C. longicaudae as distinct from C. tenuis. Contia longicaudae is genetically cohesive, possesses a greater number of caudal scales, a proportionately longer tail, and tends to be larger overall with more pronounced dorso-lateral stripes and a more muted ventral coloration than C. tenuis. Contia longicaudae also occurs in more mesic and well-shaded habitats than C. tenuis. Both forms appear to be broadly parapatric throughout much of northwestern California, and a few areas of sympatry have already been identified, particularly in southwestern Oregon, but the two species have not yet been found syntopically. Our data also reveal additional structure within C. tenuis; populations from the southern Sierra Nevada Mountains form an incipient lineage...
TL;DR: The existence of a second form of Contia tenuis is disclosed and details of its discovery plus ecological evidence support the hypothesis of its being a new species of sharp-tailed snake.
Abstract: At present, a single species of sharp-tailed snake (Contia tenuis) is recognized. Herein, I disclose the existence of a second form of Contia and provide details of its discovery. Morphological differences in coloration, relative tail length, and ventral and caudal scale counts plus ecological evidence support the hypothesis of its being a new species. A formal description of the new form and re-description of C. tenuis awaits completion of an extensive review of preserved material.