Aim
We analysed data from an insect host (Cryptocercus punctulatus) and its maternallyâinherited obligate bacterial endosymbiont (Blattabacterium cuenoti str. punctulatus) to address the following: (1) to what extent do these species exhibit cophylogenetic structure, (2) do the spatialâgenetic structures of these species differ, and (3) what is the relative importance of codivergence versus other events in explaining congruence, or instances of incongruence, between their molecular phylogenies?
Location
The southern Appalachian Mountains, USA.
Methods
We conducted fineâscale populationâlevel sampling and screening of DNA sequence variation in two mitochondrial genes from the host, and four genic or intergenic regions from the endosymbiont. Inferences were made using analyses that have the potential to identify isolated instances of cophylogenetic discord, uncover subtle differences in geographic locations of genetic discontinuities, and disentangle different evolutionary processes that contributed to observed patterns.
Results
The host and its endosymbiont showed similar phylogenetic and geographic patterns. Cophylogenetic analyses revealed that while topological discord is rare (and restricted within major clades), some instances are potentially nonânegligible. Assessments of spatialâgenetic structure showed that most abrupt breaks occur in the same locations, but they differ in strength, again underscoring some subtle discordance. The main process generating observed patterns was inferred to be codivergence due to hostâtracking; however, incomplete lineage sorting seems likely to have also played a minor role.
Main conclusions
Our overarching finding of strong congruence is reflected by broaderâscale cophylogenetic studies of related Cryptocercus and Blattabacterium taxa. Accordingly, we suggest that members of this symbiosis may provide an excellent opportunity for investigating geographic scaling of processes that affect biogeographic patterns. However, fineâscale sampling coupled with geospatial analyses detected rare and/or minor discordances that appeared to be localized within the most deeply dissected topographic regions of the southern Appalachian Mountains, and these warrant further exploration.