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The Astyanax genus represents an extraordinary example of phenotypic evolution, being their most extreme examples the blind and depigmented morphs, which have evolved from independent surface-dwelling lineages. Among cave organisms, Astyanax cavefish is a prominent model system to study regressive evolution. Before this study, 34 cave populations were known for the Astyanax genus to be inhabited by the cave morph. The majority of those cave populations are distributed in Northeast México, at the Sierra Madre Oriental (32 cavefish), in three main areas: Sierra de Guatemala, Sierra de El Abra, and Micos, and two in the Balsas basin in the state of Guerrero, Mexico. In the present study, we describe a new cave population found 4.5 km Southward of Pachón cave, the most northern cave population known for the Sierra de El Abra limestone. El Refugio cave is a resurgence with a mixed population of fish with different levels of troglomorphism, and surface fish, resembling other hybrid populations within the Sierra de El Abra. Based on a mitochondrial DNA characterization of the 16S ribosomal DNA sequence, we could identify the mitochondrial lineage of this population, which was placed closely related to the “New Lineage”, sharing haplotypes with the surface (i.e. Arroyo Lagartos) and Pachón populations, instead of with the cave populations from Central Sierra de El Abra (e.g. Tinaja cave). El Refugio cave population gives additional evidence of the intricate history of this system, where migration, drift, and selection have shaped the evolution of the cave morphs through the independent episodes of the Astyanax mexicanus history.

The genus Texoreddellia (Zygentoma; Nicoletiidae) is an important component of the cave-adapted fauna of Texas and northern Mexico. Specimens are often found in caves in central Texas. They are less common in western Texas and Coahuila, Mexico. We describe a new species, Texoreddellia chihuahuensis n. sp., from Chihuahua, Mexico, greatly expanding the range for the genus. The new species is found in an isolated karstic zone, far removed from the other cave forming areas inhabited by Texoreddellia spp. Phyletic analyses show the species to be the most basal and earliest to diverge within the genus. When compared to a calibrated molecular clock of the 16S rRNA for nicoleiids, its sequence supports a divergence of roughly 20 mya. Such a date is congruent with the geological origins of the Rio Grande and the Pecos River. Structural deformations coupled with long term erosion and downcutting through major river basins may have contributed in forming biological barriers that influenced speciation and isolation, especially between the western and eastern species of Texoreddellia.

The characiform fish Astyanaxmexicanus comes in two forms, a surface-dwelling morph which lives in the rivers of North and Central America and a blind, depigmented cave-dwelling morph which inhabits caves in Mexico. In recent years, this species has arguably become among the most influential model system for the study of evolutionary development and genomics in cave biology. While recent articles have analysed in great detail Astyanax genetics, development, physiology, phylogeny and behaviour, there have been comparatively few recent studies concerning its ecology and in particular its biogeography. Mitchell et al. (1977) reported the species inhabiting 29 caves in the Sierra de El Abra region. Despite the elapsing of over 40 years and the latest surge of interest in the model, not a single new cave locality had been described for the species. We describe here a new and 30th cave locality, Chiquitita Cave, inhabited by troglomorphic A.mexicanus. Their morphology, eye histology, 16S rRNA DNA sequence, and smelling capabilities are analysed. This cave represents the southernmost extension for the cave morph’s habitat within the Sierra de El Abra. Its name, Chiquitita Cave (Tiny Cave), was chosen in reference to a potential hydrologic connection to “Chica Cave” (small cave), which is among the most studied populations of Astyanax.

The "thysanuran" (Zygentoma: Nicoletiidae) Speleonycta ozarkensis is the only troglobiotic nicoletiid from the Ozark Highlands. It was originally described with only four specimens from four different cave systems in Arkansas and Oklahoma. The scarcity of available specimens has made it difficult to determine whether morphological variation among populations represents intraspecific or interspecific variation. We examined molecular (16S rRNA) variation among populations and found no evidence that they represent a species complex. Because of its limited distribution and lack of ecological and life history data, S. ozarkensis may be a species of conservation concern. We therefore conducted a conservation status assessment. We bioinventoried 44 caves in Arkansas and Oklahoma to determine the distribution of S. ozarkensis. A new locality in Adair Co., Oklahoma, was discovered and new specimens were collected to better assess morphological variation among populations. Data on ecology and life history was gathered. We determined the conservation status of the species and identified potential threats to existing populations. Despite being known from a few localities, S. ozarkensis has a broad distribution approaching 10,000 km2. Molecular data suggest S. ozarkensis is capable of considerable dispersal and is primarily an epikarstic species, perhaps explaining why it has been infrequently collected from caves. Conservation assessments revealed that S. ozarkensis is at a slight risk of extinction. We identified seven threats impacting populations that vary in scope and severity, but only recreational caving (three caves) and development associated with urbanization (one cave) have the greatest potential to immediately impact populations.