Location: Pest Management Research Unit
Title: Genetic Structure of the Alpine Grasshopper, Melanoplus Alpinus (Orthoptera: Acrididae) Authors
|Vandyke, K - UNIVERSITY OF WYOMING|
|Lockwood, J - UNIVERSITY OF WYOMING|
Submitted to: Annals of the Entomological Society of America
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: September 20, 2003
Publication Date: January 1, 2004
Citation: Vandyke, K.A., Kazmer, D.J., Lockwood, J.A. 2004. Genetic structure of the alpine grasshopper, melanoplus alpinus (Orthoptera: Acrididae). Annals of the Entomological Society of America. 97(2):276-285. Interpretive Summary: Understanding the mechanisms influencing spatial variation in the genetic diversity of a species is important to conserving genetic diversity in that species and to predicting how genetic diversity in species with similar life histories and ecological requirements varies. In this study, we examined the spatial genetic variability of a grasshopper that currently occupies alpine meadows in the northern Rocky Mountains. Alpine areas in the Rocky Mountains are sometimes referred to as “sky islands” because the small alpine areas are spatially separated from one another by subalpine and lower elevation areas. However, during the last Pleistocene glaciation approximately 18,000 years ago, many of today’s sky islands were glaciated and the plant and animal species characteristic of today’s sky islands may have occupied much broader areas in the valleys that were not spatially separated. We examined DNA variation in this alpine grasshopper species based on collections from 43 meadows in 10 drainages of 4 mountain ranges in Montana and Wyoming. Spatial patterns in the DNA variability are consistent with the idea that grasshopper was widely-distributed and interbreeding at the end of the Pleistocene but has since retreated to today’s sky islands.
Technical Abstract: Understanding the population dynamics of a montane/alpine grasshopper species with a disjunct distribution may help to clarify the evolutionary mechanisms of the genus Melanoplus during the Pleistocene era. A total of 215 individuals of one such species, Melanoplus alpinus Scudder, was collected from 43 meadows (5 individuals per meadow) in 10 drainages of four mountain ranges in Wyoming and Montana. This sample structure allows for genetic analysis at four spatial scales: among mountain ranges, among drainages within ranges, among meadows within drainages, and within meadows. We examined whether genetic structuring differed among the sampling scales analyzed and whether present isolation between populations of M. alpinus reflects similar historical isolation. Polymerase chain reaction restriction fragment-length polymorphism analyses were conducted on two mtDNA regions (COI and COII), revealing nine haplotypes amongthe 215 individuals. DNA sequence analysis of 496 bp of the COI region for 23 individuals representing the various restriction fragment length polymorphism haplotypes and ranges revealed three major lineages, with divergence rates that have been typically observed between species of Melanoplus. The three lineages may represent three cryptic species or a relatively ancient paraphyly in a single species. Regardless of which of these scenarios is true, analysis of molecular variance suggested that “M. alpinus” was a widely distributed, panmictic species at the end of the last Pleistocene glaciation that has since retreated to montane/alpine meadows of the central and northern Rocky Mountains. The presently fragmented distribution of the species is not indicative of historically similar isolation. The degree of genetic differentiation varied among geographical scales, being greatest among drainages and meadows within mountain ranges. Very little genetic differentiation existed among mountain ranges.