- Research article
- Open Access
Strong genetic structure corresponds to small-scale geographic breaks in the Australian alpine grasshopper Kosciuscola tristis
BMC Evolutionary Biology volume 14, Article number: 204 (2014)
Mountain landscapes are topographically complex, creating discontinuous `islands’ of alpine and sub-alpine habitat with a dynamic history. Changing climatic conditions drive their expansion and contraction, leaving signatures on the genetic structure of their flora and fauna. Australia’s high country covers a small, highly fragmented area. Although the area is thought to have experienced periods of relative continuity during Pleistocene glacial periods, small-scale studies suggest deep lineage divergence across low-elevation gaps. Using both DNA sequence data and microsatellite markers, we tested the hypothesis that genetic partitioning reflects observable geographic structuring across Australia’s mainland high country, in the widespread alpine grasshopper Kosciuscola tristis (Sjösted).
We found broadly congruent patterns of regional structure between the DNA sequence and microsatellite datasets, corresponding to strong divergence among isolated mountain regions. Small and isolated mountains in the south of the range were particularly distinct, with well-supported divergence corresponding to climate cycles during the late Pliocene and Pleistocene. We found mixed support, however, for divergence among other mountain regions. Interestingly, within areas of largely contiguous alpine and sub-alpine habitat around Mt Kosciuszko, microsatellite data suggested significant population structure, accompanied by a strong signature of isolation-by-distance.
Consistent patterns of strong lineage divergence among different molecular datasets indicate genetic breaks between populations inhabiting geographically distinct mountain regions. Three primary phylogeographic groups were evident in the highly fragmented Victorian high country, while within-region structure detected with microsatellites may reflect more recent population isolation. Despite the small area of Australia’s alpine and sub-alpine habitats, their low topographic relief and lack of extensive glaciation, divergence among populations was on the same scale as that detected in much more extensive Northern hemisphere mountain systems. The processes driving divergence in the Australian mountains might therefore differ from their Northern hemisphere counterparts.
Mountain landscapes form a matrix of mountain-top `sky islands’ , high-elevation ridges and intervening low-elevation habitat. This creates a discontinuous and fragmented landscape with features such as valleys and river drainages forming potential barriers to gene flow for species restricted to high elevations ,. The scope of these barriers has changed over time. For example, recent warming and consequent upslope distribution shifts have driven fragmentation of previously continuous alpine populations . In contrast, widespread cooling during the Pleistocene glacial periods (0.7-0.01 Ma) is thought to have created corridors of suitable habitat between currently isolated mountain ranges ,. Such large-scale climatic fluctuations have left signatures in the genetic structure of high-elevation taxa worldwide ,,–.
During Pleistocene climate cycles, the creation of habitat corridors and tracking of cooler climates to low elevations would have reduced the effective distance between populations and enabled migration of alpine species between previously-isolated mountains ,. Alternatively, glaciation might have driven population contraction to lowland refugia, driving deep lineage divergence across different mountain ranges ,–. Different patterns are evident across mountain systems that vary in their continuity, extent and ecological characteristics (e.g. dispersal ability) of the focal species. These patterns have most frequently been explored in mountain systems of North America and Europe, which extend across hundreds of kilometres. In Australia, high-elevation areas are highly fragmented but distances between distinct mountain regions are much smaller – usually less than 50 km (Figure1). Alpine and sub-alpine habitats are confined to a relatively small (5200 km2) area of southeastern Australia, with most of this area within the States of Victoria and New South Wales (`Kosciuszko region’) (Figure1a) . During the Pleistocene, alpine/sub-alpine conditions would have extended to lower elevations, connecting some, if not all, of these regions ,. At the same time, lack of large-scale glacial activity may have allowed persistence of populations in high-elevation areas . In Victoria (see Figure1), high endemism and strong divergence among arthropod populations across mountains points to a stable system in which populations have persisted on mountain summits through past climate cycles . Nevertheless, the limited geographic scope of genetic studies in the Australian alps area to-date (see , for a recent exception) – a consequence of the highly restricted distributions of most Australian alpine taxa – means that patterns of genetic structure across the remainder of the high country remain poorly understood.
Several features of the Victorian and Kosciuszko mountain regions suggest that patterns of historic and contemporary population structure are likely to differ between them. First, while alpine and sub-alpine habitat in Victoria is highly fragmented, currently separated into four main areas by low-elevation agricultural land, the Kosciuszko region comprises largely contiguous alpine/sub-alpine habitat contained within reserved land. Although the Kosciuszko region has few isolated peaks, Mt Jagungal (Figure1d), which marks the northernmost point of the this region, is separated from the main range by approximately 25 km of sub-alpine plains (~1500 m elevation). Second, the highest areas of the Kosciuszko region experienced some glaciation during Pleistocene climate cycles – the only area of the Australian mainland to do so ,. A recent study of wind-dispersing Poa grasses found no genetic structure within the Kosciuszko region, with significant divergence only apparent among isolated mountains in southern Victoria . However, species with low dispersal ability are likely to show greater structure (e.g. ,).
The most extensive areas of alpine and sub-alpine habitat in Australia, lying within the Kosciuszko region in New South Wales and the Bogong High Plains in Victoria, are separated by approximately 100 km of lowland across the Murray River valley, which also marks the State border (Figure1a). This geographic discontinuity represents a significant divergence point for several alpine reptile and mammalian species –. For example, the skink Egernia guthega, an alpine endemic, shows an average 2.2% mitochondrial (ND4) sequence divergence between a population from Kosciuszko and three populations from the Bogong High Plains. However, no genetic structure across this valley was detected among alpine Poa. Thus, with the exception of Poa, the restricted distributions of species studied to-date provides no means to assess the context of the Kosciuszko-Bogong High Plains break within the broader alps area.
In this study, we examine the importance of broad-scale geographic discontinuities in shaping patterns of genetic structure in the Australian high country. In particular, we explore the following questions: (1) at the relatively small spatial scale of Australia’s high country, what is the extent of lineage divergence among and within regions and does the timing of divergence relate to Pleistocene glacial cycles? (2) Are differences in geographic structure and historic climate between the Victorian and Kosciuszko mountains regions reflected in lower historic and contemporary genetic structure in the latter? (3) To what extent does the gap between Kosciuszko and the Bogong High Plains represent a primary divergence point? We investigate these questions using phylogenetic and population genetic frameworks, with markers of different temporal resolutions to capture signatures of both current range fragmentation and potential distribution shifts in the past.
The grasshopper Kosciuscola tristis (Sjösted) was identified as an ideal species in which to explore these genetic patterns. Although restricted to Australia’s alpine and sub-alpine habitat, primarily above 1500 m, it is abundant and its distribution stretches from Mt Baw Baw in the south to Mt Jagungal in the north (~300 km). This gives it one of the largest ranges of any mountain-endemic animal in Australia and makes it an ideal model for testing broad-scale phylogeographic patterns in this system. Like many alpine insects, K. tristis is flightless and, consequently, is likely to have limited dispersal abilities over the distances separating major mountain regions. Two subspecies are described , with K. tristis tristis occurring in the Kosciuszko region and K. tristis restrictus on the Mt Buffalo plateau (Figure1). Rehn  also describes Victorian populations from Mt Hotham and the Bogong High Plains as morphologically intermediate between the two proposed subspecific forms. We thus predicted (a) genetic divergence across the Murray River valley, and (b) that K. tristis from Mt Buffalo would be genetically distinct from other populations of K. tristis. Some study has been made of the genetic structure of this species ,, providing a basis from which to extend the research to cover a greater geographic extent.
Phylogeographic structure and genetic diversity
In total, 75 individuals were sequenced, representing 35 unique CO1 haplotypes and 12 unique ITS1 haplotypes. Of these, 12 CO1 and 3 ITS1 haplotypes were represented in the Kosciuszko region, with the remainder from populations in Victoria. Mean CO1 sequence divergence between haplotypes in Victoria was five times that of the Kosciuszko region (Victoria: mean = 2.4 ± 1.1%; Kosciuszko: 0.4 ± 0.2%), and nucleotide diversity was also greater in Victoria (Victoria: = 0.006 ± 0.013; Kosciuszko: = 0.001 ± 0.001).
The maximum likelihood CO1 phylogeny indicates strong statistical support for a southern Victorian clade incorporating populations from Mt Baw Baw, Mt Buller and Mt Stirling. Within this group, further geographic structure was apparent with good support for the monophyly of haplotypes from Mt Baw Baw and from Mt Buller (Figure2). We found no statistical support for phylogeographic structure across the remaining mountains, although Mt Buffalo (representing the subspecies K. tristis restrictus) did cluster. Mt Hotham showed a particularly interesting pattern, with haplotypes falling out in several places on the phylogeny and two individuals – potentially hybrids – showing strong divergence from the other haplotypes. The ITS1 data, however, placed Mt Hotham with the southern Victorian mountains (Mts Stirling, Buller and Baw Baw). In contrast to the CO1 phylogeny, ITS1 sequences showed divergence between the Kosciuszko region and the Bogong High Plains (separated by the Murray River valley), with populations from each region represented by one primary haplotype (Figure3).
There was an average 2.9% (range 1.9 – 4.1%) sequence divergence between CO1 haplotypes from the southern Victorian mountains and those from the Bogong High Plains and Kosciuszko. This corresponds to divergence 0.8 to 1.3 Ma (range 0.5 – 1.8 Ma) using a divergence rate of 2.3% or 3.5% Myr-1 respectively. Within these southern mountains, divergence of the Mt Baw Baw clade was estimated at 0.4 to 0.7 Ma (range 0.21 – 0.8 Ma) based on a 1.5% (range 0.8 – 1.9%) mean sequence divergence, and the Mt Buller clade at 0.1 Ma (range 0.1 – 0.2 Ma) with 0.3% (range 0.3 – 0.4%) sequence divergence. We were unable to give an estimated divergence time between populations from the Bogong High Plains and Kosciuszko as there was no phylogenetic split based on CO1 data.
Microsatellite data: null alleles and diversity
Due to poor amplification of some loci in Victoria (see Methods) we split the data into two. The first dataset consisted of all 13 populations sampled (388 individuals) with five microsatellite loci (five-locus dataset) and the second included the six populations from the Kosciuszko region (177 individuals) and eight loci (Kosciuszko dataset).
The two datasets contained 20% and 14% missing data, respectively. After correcting for multiple comparisons, only one pair of loci at one site showed significant linkage disequilibrium. All loci deviated from Hardy-Weinberg Equilibrium (HWE) in at least one of the sampled sites, with locus Ktr88 showing the highest level of deviation, departing from HWE at all sites. The other loci that deviated from HWE did so in 4–7 of the seven Victorian populations and in 1–6 of the six Kosciuszko populations. Microchecker [ indicated the presence of null alleles at four loci: Ktr30, Ktr58, Ktr60 and Ktr88, with estimated null allele frequencies for these loci between 0.12 (Ktr58) and 0.3 (Ktr88) (Additional file 2: Table S2-S3).
The five-locus dataset of 13 populations harboured 136 alleles across the five loci (range 21 to 38 per locus), while 147 alleles were detected across the eight loci in the Kosciuszko dataset (6–38 alleles/locus). Although observed heterozygosity was generally low (all HO < 0.6), likely due to the presence of null alleles, genetic diversity measured by expected heterozygosity was high (mean H E = 0.82) and varied little across sites (with the exception of the Baw Baw population, with H E = 0.59) (Table 1).
Population genetic structure
Deviations from HWE and the presence of null alleles means that estimates of F-statistics are problematic and should be treated cautiously. Nevertheless, we present F ST values, corrected for null alleles, and F’ ST values as measures of divergence for comparability. The patterns of structure presented below, detected using FST, principal components analysis and Bayesian clustering analyses are concordant.
There was significant pairwise differentiation between 73 of 78 site pairs in the five-locus dataset, and between 13 of 14 pairs in the Kosciuszko dataset, after a correction for null alleles using the ENA method (see Methods for details), although F ST values were generally low (Additional file 3: Tables S4-S5). The exceptions were Falls Creek-Mt Cope (F ST = 0.002, F’ ST = 0), Mt Buller-Mt Stirling (F ST = 0.010, F’ ST = 0.112), Thredbo 2 – Mt Tate (F ST = 0.014, F’ST = 0.189), Thredbo 1-Thredbo 2 (F ST = 0.002, F’ ST = 0.017) and Thredbo 2-Thredbo 3 (F ST = 0.013, F’ ST = 0.057). The greatest differentiation was observed between populations from the Kosciuszko region and those from Victoria (mean F ST = 0.100).
These broad-scale patterns were supported by the discriminant analysis of principal components, which indicated clear differentiation of geographic groups (Figure4). In particular, the Kosciuszko region represented a robust cluster with 93% of individuals correctly assigned to the region, compared to 83% and 84% for the southern Victorian and Bogong High Plains clusters, respectively.
Population structure was also assessed with the Bayesian assignment method implemented in TESS, which supported five clusters in the five-locus dataset (all populations) and six clusters in the Kosciuszko dataset (Figure5). Strong regional divergence was again evident: three clusters were almost exclusively assigned to individuals from Victoria (<4% in the Kosciuszko region), while the remaining clusters were largely exclusive to the Kosciuszko region. The Bogong High Plains region showed equivalent admixture proportions from clusters associated with southern Victoria and the Kosciuszko region (10 – 18% admixture), in addition to a distinct local cluster representing an average 57% of individual admixture proportions. In Victoria, Mt Buffalo and Mt Baw Baw were characterised by very high single-cluster assignment (97% and 89% respectively). Similarly, in the Kosciuszko region, the isolated peak of Mt Jagungal showed high single-cluster assignment (average 93%).
Spatial patterns of genetic divergence
We tested for isolation-by-distance (IBD) in both the microsatellite and CO1 datasets, and examined this pattern in the Victorian and Kosciuszko regions alone, as well across all populations. There was significant isolation-by-distance in both the microsatellite (all populations (Five-locus): r2 = 0.640, p = 0.001; Victoria (Five-locus): r2 = 0.395, p = 0.020; Kosciuszko: r2 = 0.666, p = 0.001) and CO1 (all populations: r2 = 0.213, p = 0.003; Victoria: r2 = 0.304, p = 0.005), datasets. Within the Kosciuszko region, however, CO1 sequence divergence showed no relationship with geographic distance (r2 = 0.009, p = 0.367).
The topographic complexity of mountain landscapes, coupled with large-scale climatic fluctuations, has shaped the evolution and population structure of high-elevation species worldwide ,,–,. In the comparatively small (both in area and altitudinal range) and geologically stable Australian high country, we found genetic divergence associated with discontinuities in alpine and sub-alpine habitats. Four primary genetic groups were identified across the Kosciuszko region of New South Wales and mountain areas of Victoria, with the greatest structure evident in the latter. Here we discuss population structure within Kosciuszko and Victoria, genetic structure across major geographic breaks and the extent to which patterns in Australia parallel (and differ from) those in larger mountain systems.
The Kosciuszko alpine region contains Australia’s highest mountains and the most extensive area of alpine and sub-alpine habitat. Despite this, previous work in a variety of taxa [grasses: 18, skinks: 22, mammals: 23, insects: 25] has shown low genetic structure within this region. Likewise, we found no phylogeographic structure in K. tristis. An absence of isolation-by-distance suggests either very high gene flow over a long period of time or incomplete lineage sorting following relatively recent (re)colonisation ,. We suggest the latter is more likely. The slopes on and near Mt Kosciuszko are the only areas of mainland Australia where glacial formations during the Pleistocene are known to have occurred . In addition to concurrent changes in the distribution and structure of vegetation , K. tristis has poor cold tolerance (R Slatyer, unpublished data) and may thus have retreated to refugia during glacial periods. Subsequent recolonization during interglacial periods could lead to low diversity and low regional structure – a pattern which is seen among many alpine taxa in the Northern Hemisphere ,,.
In contrast to the lack of phylogenetic structure, microsatellite data suggested significant population differentiation across small spatial scales (<20 km) coupled with a strong signature of isolation-by-distance. This could reflect more recent differentiation. In particular, we report a new genetic break, with unambiguous clustering of individuals from Mt Jagungal, which is separated from Kosciuszko proper by 25 km of sub-alpine plains at around ~ 1500 m elevation – also the lower-elevation limit of K. tristis in the area. Patterns of recent, fine-scale population differentiation (over distances < 50 km) are common across high-elevation taxa – even among species with high dispersal ability (e.g. –). Habitat features such as forest fragments within high-elevation meadows, topographic relief and water availability have been identified as putative dispersal barriers ,–. Although sub-alpine and alpine habitats are largely contiguous within the Kosciuszko region, as far north as Mt Jagungal, grasshoppers are patchily distributed throughout the landscape (R Slatyer & K Umbers, unpublished observations). This is likely to reflect microhabitat variation which, in turn, could be driving the genetic differentiation across small geographic distances within the Kosciuszko region.
Victoria’s high country is highly fragmented, with disjunct mountain regions separated by 50 to 100 km. In line with our predictions that populations from this region would thus show stronger genetic structure than those from Kosciuszko, divergence and diversity were both higher within Victoria. Despite this pattern of generally high regional divergence, however, the Bogong High Plains and Mt Buffalo showed low differentiation. Mt Buffalo contains several endemic flora and fauna species ,, showed strong phylogeographic isolation in four other alpine invertebrates  and emerged as one of few distinct genetic clusters in wind-dispersed alpine Poa grasses . It was therefore surprising to find no support for a distinct Mt Buffalo clade in our phylogenetic analyses, particularly as this would correspond to the subspecies described from morphological data . As for populations within the Kosciuszko region, however, assignment analyses based on microsatellite data suggest that this population is genetically distinct from those of the adjacent Bogong High Plains. Mutations arise rapidly in microsatellites , and this differentiation could suggest recent population isolation.
Evolutionary history of the Australian alps
Rapid cooling and drying in southeastern Australia during the late Miocene to Pliocene (5–2.5 Ma) is thought to have promoted the evolution of the cold-adapted sub-alpine and alpine biota, with this species assemblage persisting through subsequent climatic shifts –. This corresponds to estimated dates of divergence among the four mainland Kosciuscola species . Divergence time estimates for the southern Victorian (0.5 – 1.8 Ma), and subsequently, Mt Baw Baw and Mt Buller clades (0.1 – 0.8 Ma), are consistent with the intense climate cycling of the Pleistocene ,,. A lack of current gene flow is indicated by an absence of widespread haplotypes and haplotype sharing only between proximate populations .
Depression of the snowline during glacial periods is thought to have resulted in continuous alpine/sub-alpine conditions from Mt Jagungal into southern Victoria ,. While this depression might have facilitated range expansion and, consequently, low differentiation across the alpine area as a whole ,, previous studies on geographic subsets of Australia’s high country have found high endemism among mountain suggesting relatively stable population histories and isolation among mountains ,,. In particular, considering both the sequence and microsatellite datasets, we identify four primary genetic groups: two southern Victorian groups comprising Mt Baw Baw and Mt Buller/Mt Stirling; a Bogong High Plains cluster comprising the Bogong High Plains proper and Mt Buffalo; and a Kosciuszko cluster.
One of the most surprising results to emerge in this study was the inconsistent support for the (relatively) well-studied phylogeographic break between the Kosciuszko and Bogong High Plains regions, across the Murray River valley. Approximately 100 km separates alpine/sub-alpine habitats on either side of the valley but two of five previous studies , have not found significant genetic structure. From both sequences and microsatellite data, we suggest that there is significant divergence between K. tristis populations from Mt Kosciuszko and the Bogong High Plains. Perhaps more importantly, however, our data suggest that the Murray River valley (which also forms a State border) may not be the greatest point of divergence among alpine taxa (see also ).
The Australian alps in a global perspective
For high-elevation taxa in North America and Europe, phylogeographic patterns reflect contrasting population histories of glacial and interglacial expansion and contraction (e.g. ,,,,). In many respects, our phylogenetic results mirror those from mountains in the Northern hemisphere – phylogeographic breaks among widespread mountain regions contrast with shallow historical divergence within ranges ,,. However, mountain regions in Australia are of a different scale to those most often studied – peaks are separated by tens of kilometres, rather than by hundreds of kilometres, and alpine/sub-alpine habitat is confined to just 700 vertical metres. Further, all current high-mountain regions on mainland Australia are thought to have been connected by alpine/sub-alpine conditions during glacial periods. Given that the processes typically invoked to explain distribution shifts and demographic change - such as ice sheet formation – are not applicable to much of the Australian high country, and that distances among mountain regions are relatively small, it is remarkable that strong lineage divergence (such as for the southern Victorian mountains) is clearly evident. Indeed, sequence divergence was akin to estimates of inter-specific divergence among alpine grasshoppers in the North American Rocky Mountains , and across the mountains of Europe .
Despite the small spatial scale and past intermittent connectivity of Australian alpine and sub-alpine habitats, consistent patterns of divergence among the two molecular datasets indicate differentiation, associated with geographic breaks in alpine/sub-alpine habitat, that has persisted through glacial cycles and into the present. Populations from peaks within the highly fragmented Victorian high country showed much greater population structure than those from the more continuous Kosciuszko region and structure patterns indicate that the former is comprised of at least three distinct genetic groups. The microsatellite data, although problematic, suggests more fine-scale and possibly more recent structure than either CO1 or ITS1, and genetically distinct populations corresponding to the northern- and southern-most parts of the species’ range and to the described sub-species K. tristis restrictus. The evolutionary histories of these peaks, particularly the under-studied Mt Jagungal, need to be assessed further. The wide alpine/sub-alpine distribution and ecological characteristics of K. tristis make it a good model for exploring associations between genetic markers and adaptive processes across the Australian high country.
Study species and sampling
Kosciuscola tristis Sjösted (1933) (Orthoptera: Acrididae) is a small (15–30 mm) grasshopper, endemic to Australia’s alpine region . The species has a patchy distribution across small geographic scales, but population density can be very high during the peak adult activity period between February and April. The species is univoltine with discrete generations, all adults dying by late-May and eggs hatching in early summer. Of the four grasshopper species endemic to the sub-alpine and alpine regions of the Australian mainland, K. tristis has the narrowest altitudinal range. It is found between 1500 m and 2200 m with a known distribution spanning five distinct mountain areas across two States: New South Wales (Kosciuszko alpine region) and Victoria (Bogong High Plains, Mt Buffalo plateau, Mt Buller/Mt Stirling and the Baw Baw plateau) (Figure1).
Between January and May of 2012 and 2013, a total of 396 adult K. tristis were collected by hand from 15 mountains spanning K. tristis’ full known geographic distribution (Figure1, Additional file 1: Table S1). Some mountains were separated by low-elevation, while others represent peaks within continuous alpine/sub-alpine habitat. The geographic distance between sampled locations ranged from 1.7 km to 284 km, but adjacent mountains were always less than 100 km apart. One hind leg was removed from each individual in the field and stored in 100% ethanol until DNA extraction.
Phylogeny reconstruction: DNA extraction, amplification and sequencing
Total genomic DNA was extracted from muscle tissue from the femur. Tissue was placed in a microcentrifuge tube and crushed with a glass bead and mixer mill at 20,000 Hz for 2 min. Samples were centrifuged (30 sec at 13,000 rpm) after which 150 μL of 5% Chelex-100 resin® (BioRad, Hercules, USA) and 3 μL proteinase K (10mg/mL) (Roche, Basel, Switzerland) were added. Samples were incubated at 56°C for 3 hours, followed by 95°C for 10 min .
Phylogenetic analyses were performed using DNA sequence data from fragments of the mitochondrial cytochrome oxidase subunit I (CO1) gene and the nuclear internal transcribed spacer 1 (ITS1) region for five individuals per collection site (total 75 individuals). Polymerase Chain Reactions (PCRs) were used to amplify a 801 base-pair (bp) fragment of the CO1 gene using primer pairs C1-J-2183 and TL2-N-3014 , and a 573 bp fragment of the ITS1 gene using primer pairs CAS18sF1 and CAS5p8sB1d . PCR was carried out under the following reaction conditions: CO1: 94°C for 4 min, 35 cycles of 94°C for 30 sec, 45°C for 30 sec, 72°C for 30 sec, then 72°C for 5 min; ITS1: 94°C for 4 min, 35 cycles of 94°C for 30 sec, 64°C for 40 sec, 72°C for 30 sec, then 72°C for 5 min. PCRs were performed in 25 μL (see Additional file 4: Table S6 for reaction concentrations) and products were sequenced on an ABI 3730 DNA analyser (Macrogen Inc, Korea). Kosciuscola cognatus, a congener occupying the sub-alpine zone, was sequenced as an outgroup taxon, using identical PCR conditions.
Phylogeny reconstruction: sequence analysis and divergence time estimation
DNA sequences were aligned using muscle with default settings and refined manually in geneious 6.1.7 . CO1 sequences were translated into amino acid sequences and checked for internal stop codons to determine product authenticity and the correct reading frame. Unique haplotypes in each dataset were identified and used for subsequent phylogenetic analyses [Genbank: KJ870103-KJ870137 & KJ870139-KJ870149] (Additional file 5: Table S7). We used two approaches to test phylogeographic structure.
First, we used maximum likelihood (ML) to estimate phylogenetic relationships of CO1 haplotypes. The data were partitioned by codon position and RAxML 7.4.2  was used to estimate a maximum likelihood tree using the gtrgamma model and a rapid bootstrapping analysis  with 1000 iterations. RAxML was implemented in raxmlGUI 1.3 . Two sequences from the congener K. cognatus were used to root the tree [Genbank: KJ870138, KM407143].
Second, as there was low variation in the ITS1 sequences (12 haplotypes), we generated a phylogenetic network using a median-joining approach  implemented in network 18.104.22.168 ,, with standard settings. Kosciuscola cognatus was again included as an outgroup [Genbank: KJ870150].
We used the mitochondrial CO1 sequences to estimate divergence time among clades. In particular, we were interested in the timing of divergence among Victorian and Kosciuszko populations. No fossil of geological evidence was available for node calibration. Instead, we estimated divergence times using two divergence rates: 3.5% Myr-1, based on a recent insect molecular clock estimate  and 2.3% Myr-1, which has been used for grasshoppers in the past . Although it is unrealistic to assume a fixed substitution rate across taxa and lineages , we proceeded with this method to allow comparisons with other studies and to place population divergence in a rough time period. Sequence divergence was measured as uncorrected p-distance, calculated with the ape package  in R 3.1.0 .
Finally, we calculated average nucleotide diversity (π) for each collection site using DnaSP v5.10.1 , and mean p-distance between haplotypes in Victoria and in the Kosciuszko region, to compare levels of diversity among these areas. Diversity statistics were calculated only for the CO1 data, as ITS1 sequences showed extremely low diversity.
Population genetic structure: DNA extraction, amplification and genotyping
Genomic DNA was extracted from femur tissue, which was placed in a 96-well plate with 3 μL proteinase K and 150 μL of 5% Chelex. The plate was then incubated at 56°C for 16 h . Population genetic analyses were performed using 29–31 individuals from 13 collection sites (Table 1), three of which were from a single elevation gradient (at elevations of 1901, 1781, and 1681 m a.s.l) near Thredbo, NSW (Thredbo 1, 2, and 3 respectively). Eight microsatellite loci were amplified across two multiplexes, using primers developed by Umbers, et al. for K. tristis (Multiplex 1: loci Ktr29, Ktr73, Ktr76 and Ktr82; Multiplex 2: loci Ktr30, Ktr58, Ktr60 and Ktr88). Microsatellites were designed and tested with K. tristis from the Thredbo 2 population and details of the design methodology are given in . PCRs were performed in 11 μL volumes containing 5 μL QIAGEN Multiplex PCR Master Mix (QIAGEN Inc., Valencia, CA, U.S.A), 0.1 μM forward primer, 0.2 μM reverse primer, 0.1 μM fluorescent tags (FAM, VIC, NED, PET), and approximately 7 ng of genomic DNA . PCR cycling was performed under the following conditions: 95°C for 15 minutes, 40 cycles of 94°C for 30 s, 59°C for 90 s, and 72°C for 60 s; followed by 30 min at 60°C. PCR products were size-separated on an AB3730 DNA analyser, standardised against a GeneScan™ Liz®500 size standard (Life Technologies, CA, USA) at the Australian Genome Research Facility, Melbourne. Fragment sizes were scored manually using Geneious v6.1.7 . The loci Ktr73, Ktr82 and Ktr60 had high failure rates (>60 %) for all Victorian populations. Subsequent analyses were therefore run with two datasets (unless indicated otherwise): (1) all populations with the five remaining loci (five-locus dataset), and (2) the six populations from the Kosciuszko region (Kosciuszko dataset).
Population genetic structure: diversity and differentiation
Prior to analysis, individual microsatellite loci were checked for linkage disequilibrium, departure from Hardy-Weinberg equilibrium (HWE) and null alleles. The data were initially screened for anomalies using microchecker. Genepop 4.2.2  was used to test for linkage disequilibrium (LD) among loci in each population, using default parameters, and to estimate deviations from HWE. Significance values were adjusted for multiple comparisons with False Discovery Rates , implemented in R 3.1.0 . The frequency of null alleles at each locus was estimated using FreeNA and diversity statistics, including allelic richness and estimates of observed (H O ) and expected (H E ) heterozygosity, were calculated with GenAlEx 6.5b3 ,.
We used three methods to examine population structure. First, we used FreeNA to calculate global and pairwise F ST values, correcting for the presence of null alleles with the ENA method . We also computed the standardised statistic F’ ST in Genodive 2.0b23 . F ST values are influenced by the amount of genetic variation within populations, with the maximum attainable value of F ST decreasing as heterozygosity increases . Thus, differentiation among populations is often underestimated, particularly for highly variable molecular markers such as microsatellites, and several authors have recommended calculation of standardised statistics, such as F’ ST , as a more appropriate measure of genetic differentiation –. Both statistics were calculated for consistency and comparability with other studies.
Second, we used a discriminant analysis of principal components (DAPC; ) to investigate the relationship among geographic regions. This approach does not have underlying assumptions of HWE and was thus appropriate for our dataset (see Results). The method attempts to optimise between-cluster variation whilst minimising variation within clusters, thus producing a clearer distinction of clusters . As populations were spatially discrete, DAPC was run using a priori clusters : (a) the southern Victorian mountains (Mt Baw Baw, Mt Buller, Mt Stirling), (b) the Bogong High Plains and Mt Buffalo, and (c) Kosciuszko populations. DAPC was run in the adegenet package (v1.4-1)  in R, with the first 50 principal components retained (capturing 80% of variation), along with all the discriminant functions. As we were interested in genetic relationships among regions, this analysis was only run using the five-locus dataset.
Third, we examined population structure within the Kosciuszko region and across the study area using a Bayesian clustering approach, implemented in tess 2.3 ,. TESS incorporates individual geographic coordinates as a priori information and can thus incorporate spatial trends and spatial autocorrelation in estimates of individual ancestry . As tess only accepts individual coordinates, population coordinates were permuted with a standard deviation of 0.005°. We used the conditional autoregressive (CAR) admixture model, with a burn-in of 50,000 steps followed by 100,000 MCMC steps. The admixture parameter (α) and interaction parameter (ρ) were initially set to α = 1 and ρ = 0.6, then automatically updated. We searched for the optimal number of clusters (K) using 10 runs at K = 2 to K = 10. The most likely number of clusters was selected from the lowest Deviance Information Criterion (DIC), averaged over these 10 runs. We then did 100 additional runs at the optimal value of K and the 20 runs with the lowest DIC were averaged using clumpp 1.1.2  with the `greedy’ algorithm and default settings. The level of admixture in each population was displayed graphically with distruct 1.1 .
Spatial patterns of genetic divergence
We examined spatial patterns of divergence using both the CO1 and microsatellite data. First, we tested for a relationship between genetic distance (p-distances for CO1 data and F’ ST for microsatellites) and log-transformed geographic distance (isolation-by-distance) . For both mtDNA and microsatellites, we tested for IBD across all populations, populations from Victorian only, and populations from NSW only. Mantel tests were run using the vegan package  in R, with 999 permutations to test statistical significance.
RAS conducted the fieldwork, laboratory work, genetic analysis and wrote the manuscript. MAN assisted with field collections. YE conducted laboratory work and assisted with genetic analyses. ADM assisted with genetic analyses. YE, MAN, ADM, AAH and KU provided critical comments on the analysis and drafting of the manuscript. All authors helped design the study, and read and approved the final manuscript.
Magri D, Vendramin GG, Comps B, Dupanloup I, Geburek T, Gomory D, Latalowa M, Litt T, Paule L, Roure JM, Tantau I, Van der Knaap WO, Petit RJ, De Beaulieu JL: A new scenario for the Quaternary history of European beech populations: palaeobotanical evidence and genetic consequences. New Phytol. 2006, 171: 199-221. 10.1111/j.1469-8137.2006.01740.x.
Schoville SD, Roderick GK, Kavanaugh KD: Testing the `Pleistocene species pump’ in alpine habitats: lineage diversification of flightless ground beetles (Coleoptera: Carabidae: Nebria) in relation to altitudinal zonation. Biol J Linn Soc. 2012, 107: 95-111. 10.1111/j.1095-8312.2012.01911.x.
Rubridge EM, Patton JL, Lim M, Burton AC, Brashares JS, Moritz C: Climate-induced range contraction drives genetic erosion in an alpine mammal. Nature Clim Change. 2012, 2 (4): 285-288. 10.1038/nclimate1415.
DeChaine EG, Martin AP: Historic cycles of fragmentation and expansion in Parnassius smintheus (Papilionidae) inferred using mitochondrial DNA. Evolution. 2004, 58 (1): 113-127. 10.1111/j.0014-3820.2004.tb01578.x.
Galbreath KE, Hafner DJ, Zamudio KR: When cold is better: climate-driven elevation shifts yield complex patterns of diversification and demography in an alpine specialist (American pika, Ochotona princeps). Evolution. 2009, 63 (11): 2848-2863. 10.1111/j.1558-5646.2009.00803.x.
DeChaine EG, Martin AP: Historical biogeography of two alpine butterflies in the Rocky Mountains: broad-scale concordance and local-scale discordance. J Biogeogr. 2005, 32: 1943-1956. 10.1111/j.1365-2699.2005.01356.x.
Knowles LL: Tests of Pleistocene speciation in montane grasshoppers (genus Melanoplus) from the sky islands of western North America. Evolution. 2000, 54 (4): 1337-1348. 10.1111/j.0014-3820.2000.tb00566.x.
Schönswetter P, Stehlik I, Holderegger R, Tribsch A: Molecular evidence for glacial refugia of mountain plants in the European Alps. Mol Ecol. 2005, 14 (11): 3547-3555. 10.1111/j.1365-294X.2005.02683.x.
VanDyke KA, Kazmer DJ, Lockwood JA: Genetic structure of the alpine grasshopper, Melanoplus alpinus (Orthoptera: Acrididae). Ann Entomol Soc Am. 2004, 97 (2): 276-285. 10.1603/0013-8746(2004)097[0276:GSOTAG]2.0.CO;2.
Knowles LL: Did the Pleistocene glaciations promote divergence? Tests of explicit refugial models in montane grasshoppers. Mol Ecol. 2001, 10 (3): 691-701. 10.1046/j.1365-294x.2001.01206.x.
Schoville SD, Roderick GK: Alpine biogeography of Parnassian butterflies during Quaternary climate cycles in Northern America. Mol Ecol. 2009, 18 (16): 3471-3485. 10.1111/j.1365-294X.2009.04287.x.
Schoville SD, Roderick GK: Evolutionary diversification of cryophilic Grylloblatta species (Grylloblattodea: Grylloblattidae) in alpine habitats of California. BMC Evol Biol. 2010, 10: 163-10.1186/1471-2148-10-163.
Schmitt T: Molecular biogeography of Europe: Pleistocene cycles and postglacial trends. Front Zool. 2007, 4: 11-10.1186/1742-9994-4-11.
Costin AB: The Alps in a global perspective. The Scientific Significance of the Australian Alps. Edited by: Good R. 1989, Australian Alps National Parks Liaison Committee, Canberra, ACT, 7-19.
Frakes LA, McGowran B, Bowler JM: Evolution of Australian environments. Fauna of Australia V1A. Edited by: Walton DW, Dyne GR. 1987, Australian Government Public Service, Bureau of Flora and Fauna, Canberra, Australia
Mark BG, Harrison SP, Spessa A, New M, Evans DJA, Helmens KF: Tropical snowline changes at the last glacial maximum: A global assessment. Quatern Int. 2005, 138–139: 168-201. 10.1016/j.quaint.2005.02.012.
Endo Y, Nash MA, Hoffmann AA, Slatyer RA, Miller AD: Comparative phylogeography of alpine invertebrates indicates deep lineage diversification and historical refugia in the Australian Alps.J Biogeogr 2014, in press.,
Griffin PC, Hoffmann AA: Limited genetic divergence among Australian alpine Poa tussock grasses coupled with regional structuring points to ongoing gene flow and taxonomic challenges. Ann Bot. 2014, 113 (6): 953-965. 10.1093/aob/mcu017.
Barrows TT, Stone JO, Fifield LK, Cresswell RG: Late Pleistocene glaciation of the Kosciuszko Massif, Snowy Mountains, Australia. Quaternary Res. 2001, 55: 179-189. 10.1006/qres.2001.2216.
Barrows TT, Stone JO, Fifield LK, Cresswell RG: The timing of the Last Glacial Maximum in Australia. Quaternary Sci Rev. 2002, 21 (1–3): 159-173. 10.1016/S0277-3791(01)00109-3.
Koumoundouros T, Sumner J, Clemann N, Stuart-Fox D: Current genetic isolation and fragmentation contrasts with historical connectivity in an alpine lizard (Cyclodomorphus praealtus) threatened by climate change. Biol Conserv. 2009, 142 (5): 992-1002. 10.1016/j.biocon.2008.12.026.
Chapple DG, Keogh JS, Hutchinson MN: Substantial genetic substructuring in southeastern and alpine Australia revealed by molecular phylogeography of the Egernia whitii (Lacertilia: Scincidae) species group. Mol Ecol. 2005, 14 (5): 1279-1292. 10.1111/j.1365-294X.2005.02463.x.
Mitrovski P, Heinze DA, Broome L, Hoffmann AA, Weeks AR: High levels of variation despite genetic fragmentation in populations of the endangered mountain pygmy-possum, Burramys parvus, in alpine Australia. Mol Ecol. 2007, 16 (1): 75-87. 10.1111/j.1365-294X.2006.03125.x.
Rehn JAG: The grasshoppers and locusts (Acridoidea) of Australia. Volume III: Family Acrididae: Subfamily Cyrtacanthacridinae, Tribe Oxyini, Spathosternini, and Praxibulini. 1957, CSIRO, Melbourne, Australia
Tatarnic NJ, Umbers KDL, Song H: Molecular phylogeny of the Kosciuscola grasshoppers endemic to the Australian alpine and montane regions. Invertebr Syst. 2013, 27 (3): 307-316.
Van Oosterhout C, Hutchinson WF, Wills DPM, Shipley P: micro-checker: software for identifying and correcting genotyping errors in microsatellite data. Mol Ecol Notes. 2004, 4: 535-538. 10.1111/j.1471-8286.2004.00684.x.
Hewitt G: Post-glacial re-colonization of European biota. Biol J Linn Soc. 1999, 68 (1–2): 87-112. 10.1111/j.1095-8312.1999.tb01160.x.
Crandall ED, Taffel JF, Barber PH: High gene flow due to pelagic larval dispersal among South Pacific archipelagos in two amphidromous gastropods (Neritomorpha: Neritidae). Heredity. 2010, 104: 563-572. 10.1038/hdy.2009.138.
Nielson R, Wakeley J: Distinguishing migration from isolation. A Markov Chain Monte Carlo approach. Genetics. 2001, 158: 885-896.
Hope GS: Quaternary vegetation. History of the Australian Vegetation. Edited by: Hill RS. 1994, Press Syndicate of the University of Cambridge, Cambridge, 368-389.
Taberlet P, Fumagalli L, Wust-Saucy AG, Cosson JF: Comparative phylogeography and postglacial colonization routes in Europe. Mol Ecol. 1998, 7 (4): 453-464. 10.1046/j.1365-294x.1998.00289.x.
Church SA, Kraus JM, Mitchell JC, Church DR, Taylor DR: Evidence for multiple pleistocene refugia in the postglacial expansion of the eastern tiger salamander, Ambystoma tigrinum tigrinum. Evolution. 2003, 57 (2): 372-383. 10.1111/j.0014-3820.2003.tb00271.x.
Keyghobadi N, Roland J, Strobeck C: Influence of landscape on the population genetic structure of the alpine butterfly Parnassius smintheus (Palilionidae). Mol Ecol. 1999, 8 (9): 1481-1495. 10.1046/j.1365-294x.1999.00726.x.
Keyghobadi N, Roland J, Strobeck C: Genetic differentiation and gene flow among populations of the alpine butterfly, Parnassius smintheus, vary with landscape connectivity. Mol Ecol. 2005, 14 (7): 1897-1909. 10.1111/j.1365-294X.2005.02563.x.
Britten HB, Brussard PF, Murphy DD, Ehrlich P: A test for isolation-by-distance in central Rocky Mountain and Great Basin populations of Edith’s checkerspot butterfly (Euphydryas editha). J Hered. 1995, 86 (3): 204-210.
Garnier S, Alibert P, Audiot P, Prieur B, Rasplus J-Y: Isolation by distance and sharp discontinuities in gene frequences: implications for the phylogeography of an alpine insect species, Carabus solieri. Mol Ecol. 2004, 13: 1883-1897. 10.1111/j.1365-294X.2004.02212.x.
Henry P, Sim Z, Russello MA: Genetic evidence for restricted dispersal along continuous altitudinal gradients in a climate change-sensitive mammal: the American pika. Plos One. 2012, 7 (6): e39077-10.1371/journal.pone.0039077.
Castillo JA, Epps CW, Davis AR, Cushman SA: Landscape effects on gene flow for a climate-sensitive montane species, the American pika. Mol Ecol. 2014, 23 (4): 843-856. 10.1111/mec.12650.
Gerber AS, Templeton AR: Population sizes and within-deme movement of Trimerotropis saxatilis (Acrididae), a grasshopper with a fragmented distribution. Oecologia. 1996, 105 (3): 343-350. 10.1007/BF00328737.
Mount Buffalo National Park management plan. 1996, Department of Natural Resources and Environment, Victoria, East Melbourne, Victoria
Field R: Butterflies: identification and life history. 2013, Museum Victoria Publishing, Melbourne, Victoria
Whittaker JC, Harbord RM, Boxall N, Mackay I, Dawson G, Sibly RM: Likelihood-based estimation of microsatellite mutation rates. Genetics. 2003, 164: 781-787.
Gallagher SJ, Greenwood DR, Taylor DR, Smith AJ, Wallace MW, Holdgate GR: The Pliocene climatic and environmental evolution of southeastern Australia: evidence from the marine and terrestrial realm. Palaeogeogr, Palaeoclimatol, Palaeoecol. 2003, 193 (3–4): 349-382. 10.1016/S0031-0182(03)00231-1.
Galloway RW, Kemp E: Late Cainozoic environments in Australia. Vertebrate Zoogeography and Evolution in Australia. Edited by: Archer M, Clayton G. 1984, Hesperian Press, Sydney, Australia, 83-108.
Green K, Osborne W: Wildlife of the Australian Snow Country. 1994, Sydney, NSW, Reed
Barrows TT, Stone JO, Fifield LK: Exposure ages for Pleistocene periglacial deposits in Australia. Quaternary Sci Rev. 2004, 23 (5–6): 697-708. 10.1016/j.quascirev.2003.10.011.
Beavis FC: Pleistocene glaciation on the Bogong High Plains. Aust J Sci. 1959, 21: 182-
Berger D, Chobanov DP, Mayer F: Interglacial refugia and range shifts of the alpine grasshopper Stenobothrus cotticus (Orthoptera: Acrididae: Gomphocerinae). Org Divers Evol. 2010, 10 (2): 123-133. 10.1007/s13127-010-0004-4.
Hafner DJ, Sullivan RM: Historical and ecological biogeography of nearctic pikas (Lagomorpha, Ochotonidae). J Mammal. 1995, 76 (2): 302-321. 10.2307/1382343.
Cooper SJB, Ibrahim KM, Hewitt GM: Postglacial expansion and genome subdivision in the European grasshopper Chorthippus parallelus. Mol Ecol. 1995, 4: 49-60. 10.1111/j.1365-294X.1995.tb00191.x.
The native alpine and subalpine fauna of the Snowy Mountains. Biodiversity in the Snowy Mountains. Edited by: Green K. 2002, Institute of Alpine Studies, Jindabyne, NSW, 134-148.
Walsh PS, Metzger DA, Higuchi R: Chelex-100 as a medium for simple extraction of DNA for PCR-based typing from forensic material. Biotechniques. 1991, 10 (4): 506-513.
Simon C, Frati F, Beckenbach A, Crespi B, Liu H, Flook P: Evolution, weighting, and phylogenetic utility of mitochondrial gene sequences and a compilation of conserved polymerase chain reaction primers. Ann Entomol Soc Am. 1994, 87 (6): 651-701.
Ji YJ, Zhang DX, He LJ: Evolutionary conservation and versatility of a new set of primers for amplifying the ribosomal internal transcribed spacer regions in insects and other invertebrates. Mol Ecol Notes. 2003, 3 (4): 581-585. 10.1046/j.1471-8286.2003.00519.x.
Edgar RC: MUSCLE: multiple sequence alignment with high accuracy and high throughput. Nucleic Acids Research. 2004, 32 (5): 1792-97. 10.1093/nar/gkh340.
Biomatters: Geneious version 6.1.7 created by Biomatters. 2012, Available at ., [http://geneious.com]
Stamatakis A: RAxML-VI-HPC: maximum likelihood-based phylogenetic analyses with thousands of taxa and mixed models. Bioinformatics. 2006, 22 (21): 2688-2890. 10.1093/bioinformatics/btl446.
Stamatakis A, Hoover P, Rougemont J: A rapid bootstrap algorithm for the raxml web servers. Systematic Biology. 2008, 57: 758-771. 10.1080/10635150802429642.
Silvestro D, Michalak I: raxmlGUI: a graphical front-end for RAxML. Org Divers Evol. 2012, 12 (4): 335-337. 10.1007/s13127-011-0056-0.
Bandelt H-J, Forster P, Röhl A: Median-joining networks for inferring intraspecific phylogenies. Mol Biol Evol. 1999, 16: 37-48. 10.1093/oxfordjournals.molbev.a026036.
Fluxus Engineering.., [www.fluxus-engineering.com]
Papadopoulou A, Anastasiou I, Vogler AP: Revisiting the insect mitochondrial molecular clock: the mid-Aegean Trench calibration. Mol Biol Evol. 2010, 27 (7): 1659-1672. 10.1093/molbev/msq051.
Thomas JA, Welch JJ, Woolfit M, Bromham L: There is no universal molecular clock for invertebrates, but rate variation does not scale with body size. Proc Nat Acad Sci. 2006, 103 (19): 7366-7371. 10.1073/pnas.0510251103.
Paradis E, Claude J, Strimmer K: APE: analyses of phylogenetics and evolution in R language. Bioinformatics. 2004, 20: 289-290. 10.1093/bioinformatics/btg412.
R Core Team: R: A Language and Environment for Statistical Computing. Vienna, Austria: 2014. Available at : R Foundation for Statistical Computing., [http://www.R-project.org]
Librado P, Rozas J: DnaSP v5: a software for comprehensive analysis of DNA polymorphism data. Bioinformatics. 2009, 25: 1451-1452. 10.1093/bioinformatics/btp187.
Casquet J, Thebaud C, Gillespie RG: Chelex without boiling, a rapid and easy technique to obtain stable amplifiable DNA from small amounts of ethanol-stored spiders. Mol Ecol Resour. 2012, 12 (1): 136-141. 10.1111/j.1755-0998.2011.03073.x.
Umbers KDL, Dennison S, Manahan CA, Blondin L, Pagés C, Risterucci AM, Chapuis MP: Microsatellite markers for the chameleon grasshopper (Kosciuscola tristis) (Orthoptera: acrididae), an Australian alpine specialist. Int J Mol Sci. 2012, 13 (9): 12094-12099. 10.3390/ijms130912094.
Blacket MJ, Robin C, Good RT, Lee SF, Miller AD: Universal primers for fluorescent labelling of PCR fragments - an efficient and cost-effective approach to genotyping by fluorescence. Mol Ecol Resour. 2012, 12 (3): 456-463. 10.1111/j.1755-0998.2011.03104.x.
Rousset F: Genepop’007: a complete reimplementation of the Genepop software for Windows and Linux. Mol Ecol Resour. 2008, 8: 103-106. 10.1111/j.1471-8286.2007.01931.x.
Benjamini T, Hochberg Y: Controlling the false discovery rate: a practical and powerful approach to multiple testing. J Roy Stat Soc B. 1995, 57: 289-300.
Chapuis MP, Estoup A: Microsatellite null alleles and estimation of population differentiation. Mol Biol Evol. 2007, 24 (3): 621-631. 10.1093/molbev/msl191.
Peakall R, Smouse PE: GenAlEx 6: genetic analysis in Excel. Population genetic software for teaching and research. Mol Ecol Notes. 2006, 6: 288-295. 10.1111/j.1471-8286.2005.01155.x.
Peakall R, Smouse PE: GenAlEx 6.5: genetic analysis in Excel. Population genetic software for teaching and research - an update. Bioinformatics. 2012, 28: 2537-2539. 10.1093/bioinformatics/bts460.
Meirmans PG, Van Tienderen PH: GENOTYPE and GENODIVE: two programs for the analysis of genetic diversity of asexual organisms. Mol Ecol Notes. 2004, 4: 792-794. 10.1111/j.1471-8286.2004.00770.x.
Hedrick PW: A standardized genetic differentiation measure. Evolution. 2005, 59: 1633-1638. 10.1111/j.0014-3820.2005.tb01814.x.
Heller R, Siegismund HR: Relationship between three measures of genetic differentiation GST, DEST and G’ST: how wrong have we been?. Mol Ecol. 2009, 18 (10): 2080-2083. 10.1111/j.1365-294X.2009.04185.x.
Jost L: GST and its relatives do not measure differentiation. Mol Ecol. 2008, 17: 4015-4026. 10.1111/j.1365-294X.2008.03887.x.
Meirmans PG, Hedrick PW: Assessing population structure: FST and related measures. Mol Ecol Resour. 2011, 11 (1): 5-18. 10.1111/j.1755-0998.2010.02927.x.
Jombart T, Devillard S, Balloux F: Discriminant analysis of principal components: a new method for the analysis of genetically structured populations. BMC Genet. 2010, 11: 94-10.1186/1471-2156-11-94.
Chen C, Durand E, Forbes F, François O: Bayesian clustering algorithms ascertaining spatial population structure: A new computer program and a comparison study. Mol Ecol Notes. 2007, 7: 747-756. 10.1111/j.1471-8286.2007.01769.x.
Durand E, Jay F, Gaggiotti OE, François O: Spatial inference of admixture proportions and secondary contact zones. Mol Biol Evol. 2009, 26: 1963-1973. 10.1093/molbev/msp106.
Jakobsson M, Rosenberg NA: CLUMPP: a cluster matching and permutation program for dealing with label switching and multimodality in analysis of population structure. Bioinformatics. 2007, 23 (14): 1801-1806. 10.1093/bioinformatics/btm233.
Rosenberg NA: DISTRUCT: a program for the graphical display of population structure. Mol Ecol Notes. 2004, 4: 137-138. 10.1046/j.1471-8286.2003.00566.x.
Wright S: Isolation by distance. Genetics. 1943, 28: 114-138.
Oksanen J, Blanchet FG, Kindt R, Legendre R, Legendre P, Minchin PR, O’Hara RB, Simpson GL, Solymos P, Henry M, Stevens H, Wagner H: vegan: Community Ecology Package. R package version 2.0-10. 2013, ., [http://CRAN.R-project.org/package=vegan]
Slatyer, Rachel, Nash, Michael, Endo, Yoshinori, Miller, Adam, Umbers, Kate, Hoffmann, Ary: Microsatellite data forKosciuscola tristis.Figshare 2014, ., [http://dx.doi.org/10.6084/m9.figshare.1165613]
We would like to thank Philippa Griffin, Rebecca Jordan, Rob Lanfear and Joel Huey, for advice on data analysis and interpretation. Three anonymous reviewers and editor Steven Cooper also provided insightful comments and suggestions that greatly improved the manuscript and for which we are most grateful. Thanks also to Harry, Tony and Robyn Slatyer, Mira Wawn, Nick and Leo Barnard, Nik Tatarnic, and Martina Hoffmann for help catching grasshoppers. This work was funded by the Australian Research Council, the Long Term Terrestrial Research Network, the Holsworth Wildlife Research Endowment (grants to RAS and YE) and a Victorian Environmental Assessment Council Bill Borthwick Scholarship to RS. Grasshoppers were collected under permit numbers SL101032 (NSW Department of Environment) and 10006742 (Victorian Department of Environment and Primary Industry).
The authors declare that they have no competing interests.