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The maximum likelihood (ML) phylogram of 26 unique M. nichollsi ND2 haplotypes shows three major lineages with Arenophryne rotunda and Myobatrachus gouldii as outgroups. Clade support is provided by maximum parsimony bootstrap/ML bootstrap/Bayesian posterior probabilities. The TIM+I+G model of DNA evolution was enforced in ML analyses selected by Akaike information criterion tests in modeltest ver. 3.7. A map of the south-western Australian coastline is shown inset with shaded areas representing the distribution of the main range, south coastal and Stirling Ranges lineages. Tissue collection locations [•] for the Metacrinia nichollsi phylogeographic study cover the entire known distribution of the species. Site names and abbreviations are as follows: Naturaliste Ridge Nth (NRN, n = 3); Naturaliste Ridge Mid (NRM, n = 4); Naturaliste Ridge Sth (NRS, n = 4); Sabina (SAB, n = 3); Blackwood Nth (BN, n = 4); Blackwood Sth (BS, n = 4); Donnelly-Warren Nth (DWN, n = 4); Donnelly-Warren Sth (DWS, n = 4); Shannon-Gardner Nth (SGN, n = 2); Shannon-Gardner Sth (SGS, n = 3); Deep-Frankland Nth (DFN, n = 5); Deep-Frankland Sth (DFS, n = 5), Kent-Hay Nth (KHN, n = 3); Kent-Hay Sth (KHS, n = 5); Kalgan Nth (KALN, n = 10); Kalgan Sth (KALS, n = 5).

The maximum likelihood (ML) phylogram of 26 unique M. nichollsi ND2 haplotypes shows three major lineages with Arenophryne rotunda and Myobatrachus gouldii as outgroups. Clade support is provided by maximum parsimony bootstrap/ML bootstrap/Bayesian posterior probabilities. The TIM+I+G model of DNA evolution was enforced in ML analyses selected by Akaike information criterion tests in modeltest ver. 3.7. A map of the south-western Australian coastline is shown inset with shaded areas representing the distribution of the main range, south coastal and Stirling Ranges lineages. Tissue collection locations [•] for the Metacrinia nichollsi phylogeographic study cover the entire known distribution of the species. Site names and abbreviations are as follows: Naturaliste Ridge Nth (NRN, n = 3); Naturaliste Ridge Mid (NRM, n = 4); Naturaliste Ridge Sth (NRS, n = 4); Sabina (SAB, n = 3); Blackwood Nth (BN, n = 4); Blackwood Sth (BS, n = 4); Donnelly-Warren Nth (DWN, n = 4); Donnelly-Warren Sth (DWS, n = 4); Shannon-Gardner Nth (SGN, n = 2); Shannon-Gardner Sth (SGS, n = 3); Deep-Frankland Nth (DFN, n = 5); Deep-Frankland Sth (DFS, n = 5), Kent-Hay Nth (KHN, n = 3); Kent-Hay Sth (KHS, n = 5); Kalgan Nth (KALN, n = 10); Kalgan Sth (KALS, n = 5).

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Aim To assess phylogeographic pattern throughout the range of Metacrinia nichollsi in order to develop specific biogeographical hypotheses for the wet forests of south‐western Australia. This was carried out by contrasting a direct‐developing frog species, M. nichollsi , that breeds independently of free surface water with conventional, aquatic bre...

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... individuals were sampled (toe-clips) from 16 sites across the entire species distribution, with two to five animals sampled per site (Fig. 1). The gap that exists between the Stirling Ranges population and the main range of the species is real: both current and historical surveys have failed to find the species in intervening areas. Past and present surveys in the Porongurup Mountains (34°40¢46¢¢, 117°52¢23¢¢) have recovered no records of the species (B.Y. Main has ...
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... Base = (0.2825; 0.3564; 0.1272), Nst = 6, Rmat = (1.0000; 23.0322; 0.3433; 0.3433; 5.8514), Rates = gamma, Shape = 0.7316 and Pinvar = 0.6805 were enforced in a likelihood analysis with 100 bootstrap replicates to assess branch support. Parallel Bayesian runs were identical, and major lineages were all well supported. The phylogram presented in Fig. 1 shows three main lineages. The first lineage has a disjunct distribution across some south coastal catchments (SCL), a second is endemic to the Stirling Ranges (SRL), and a third covers the remainder of the species main range (MRL). The SRL had no genetic diversity, despite the fact that samples came from two sites across the range of ...
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... are two major phylogenetic divergence events within the M. nichollsi lineage that account for the majority of the genetic diversity observed. The first is the separation of the relictual Stirling Ranges populations (SRL) from the populations in the remainder of the species range during the late Miocene-early Pliocene (Figs 1 and 3). The second splits the remainder of the species distribution into a lineage with a disjunct distribution across the south coast (SCL) and another covering the majority of the species range (MRL), with divergence estimates dating this split during the mid-to late Pliocene (Figs 1 and 3). ...
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... first is the separation of the relictual Stirling Ranges populations (SRL) from the populations in the remainder of the species range during the late Miocene-early Pliocene (Figs 1 and 3). The second splits the remainder of the species distribution into a lineage with a disjunct distribution across the south coast (SCL) and another covering the majority of the species range (MRL), with divergence estimates dating this split during the mid-to late Pliocene (Figs 1 and 3). The biogeographical patterns observed in each of these clades appear to be vastly different. ...
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... is likely to have contracted towards the coast, where rainfall remained high, albeit reduced, during arid cycles, as indicated by the large number of relictual animals and plants ( Hopper et al., 1996). In the north (MRL), individuals may have persisted in a number of sites, for example Lake Muir or parts of the upper Blackwood catchment (see Fig. 1), which may have remained wet enough during severe arid pulses in the Pliocene. The individual phylogeographic histories of the two lineages, SCL and MRL, give some indication of the possible historic scenarios that might explain the current distribution of these divergent ...

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... Interestingly, the spatial structuring found in W. carteri is similar to that observed in other taxa including flora and fauna for which intraspecific genetic diversity is not uniformly distributed (Hopper & Gioia, 2004;Davies & Stewart, 2013;Rix et al., 2015). Many species within the region also comprise highly divergent western and southern lineages as a result of contraction to separate mesic refugia during early-mid Pleistocene arid cycling (Edwards, Roberts & Keogh, 2007;Edwards, Roberts & Keogh, 2008;Nistelberger et al., 2014). Within these primary lineages, a secondary pattern of highly localized haplotypes is also common, indicating more recent isolation of populations as a result of increasing aridification (Byrne, 2008;Byrne et al., 2011). ...
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... Genetic structure has been identified in the native range of P. lophantha as part of studies focusing on the population structure outside Australia [37] and adaptive responses to novel ranges [38]. Phylogeographic patterns within Australia have not been explored in detail in P. lophantha, but phylogeographic structure identified in SW WA in both plants (e.g., [5,[54][55][56]) and animals (e.g., [57][58][59][60][61]) has contributed to conservation in the region by enabling genetically informed management. ...
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... In the same broad region as G. leai, Crinia georgiana and Metacrinia nichollsi have marked, genetic subdivisions (Edwards et al., , 2008, and the range of Heleioporus inornatus is split into west coast and southeast coast occurrences with no obvious landscape feature separating these sets of populations (Lee, 1967). Intraspecific variation of frog lineages in southwestern Australia may reflect the impact of broad drying and cooling trends since the Miocene Rix et al., 2015), recent climate variations, or complex but subtle physiographic properties of the landscapes (Pain et al., 2011). ...
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... The reliance of Onychophora on moist habitats has possibly confined them to the high-rainfall area along the coast of south-western Australia and also to the upland areas such as the Stirling and Porongurups Ranges. This substantiates the hypotheses supported by the biogeographic distributions of other fauna such as Bertmainius mygalomorph spiders (Cooper et al. 2011;Harvey et al. 2015;Rix et al. 2017), assassin spiders (Rix and Harvey 2012), millipedes (Moir et al. 2009) and frogs (Edwards et al. , 2008; see Rix et al. (2015) for further discussion. ...
... This study supports the growing body of evidence that suggests that the climatic history of Australia, paired with the topographical conditions of south-western Australia, have caused an explosion of speciation in the region (e.g . Hopper 1979;Hopper and Gioia 2004;Edwards et al. , 2008Moir et al. 2009;Cooper et al. 2011), arguing for increased protection of forests in the area, especially those in upland regions (e.g. Porongurups, Stirling Range). ...
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... We also quantified morphology for a much larger group of animals (see below and S1 Fig for the distribution of morphotyped individuals). Metacrinia nicholsii, Arenophryne rotunda and A. xiphorhyncha were included due to their close relationship with M. gouldii and as a comparison of intra-specific genetic distances [36,37]. ...
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... Within the SMB, major climatic gradients and physical features across the landscape are thought to have been important in shaping phylogeographic patterns (Kay and Keogh 2012). For example, strong rainfall and temperature gradients between the High Rainfall Zone of the southwest coast and the inland Transitional Rainfall Zone (Hopper 1979) appear to have been significant barriers to frogs (Wardell-Johnson and Roberts 1993;Edwards et al. 2007Edwards et al. , 2008 and skinks (Kay and Keogh 2012). In addition, physical barriers such as the Darling Scarp (Kay and Keogh 2012) and the waterlogged Pingerup Plains (Wardell-Johnson and Roberts 1993;Edwards et al. 2008) as well as sea-level fluctuations in coastal areas (Edwards et al. 2008;Kay and Keogh 2012) also appear to have been important in the regional diversification of herpetofauna in the SMB. ...
... For example, strong rainfall and temperature gradients between the High Rainfall Zone of the southwest coast and the inland Transitional Rainfall Zone (Hopper 1979) appear to have been significant barriers to frogs (Wardell-Johnson and Roberts 1993;Edwards et al. 2007Edwards et al. , 2008 and skinks (Kay and Keogh 2012). In addition, physical barriers such as the Darling Scarp (Kay and Keogh 2012) and the waterlogged Pingerup Plains (Wardell-Johnson and Roberts 1993;Edwards et al. 2008) as well as sea-level fluctuations in coastal areas (Edwards et al. 2008;Kay and Keogh 2012) also appear to have been important in the regional diversification of herpetofauna in the SMB. ...
... For example, strong rainfall and temperature gradients between the High Rainfall Zone of the southwest coast and the inland Transitional Rainfall Zone (Hopper 1979) appear to have been significant barriers to frogs (Wardell-Johnson and Roberts 1993;Edwards et al. 2007Edwards et al. , 2008 and skinks (Kay and Keogh 2012). In addition, physical barriers such as the Darling Scarp (Kay and Keogh 2012) and the waterlogged Pingerup Plains (Wardell-Johnson and Roberts 1993;Edwards et al. 2008) as well as sea-level fluctuations in coastal areas (Edwards et al. 2008;Kay and Keogh 2012) also appear to have been important in the regional diversification of herpetofauna in the SMB. ...
... However, the location of the south-eastern nuclear genetic cluster in K. coccinea was notable, given its apparent demarcation by the Blackwood River system, south of which the broad geomorphological zone of the region also changes (Schoknecht et al., 2004). The Blackwood River has been identified as a boundary between lineages within two small animal species (Gouws et al., 2006;Edwards et al., 2008), although chloroplast lineage structure in jarrah did not follow the same pattern (Wheeler & Byrne, 2006). The river may therefore act as a stronger barrier to gene flow for understorey species and small animals than it does for large, dominant forest trees. ...
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Aim Terrestrial plant ecology and evolution is significantly influenced by the phenomenon of fire, but studies of its potential impact on intraspecific genetic variation and phylogeography are rare. This understanding will be important for predicting the biogeographical consequences of changing fire regimes under global climate change. Here, we asked whether changing historical fire regimes, together with climatic and geological history, have influenced phylogeographical patterns in a fire‐ephemeral vine. We also asked whether demographic stochasticity associated with a fire‐ephemeral life history results in nuclear genetic drift as expected from spatio‐temporal patchiness, or if this effect is buffered by the connectivity and diversity afforded by a persistent soil seed bank. Location The fire‐prone, mediterranean‐type climate region of south‐western Australia. Methods We used Bayesian phylogeny reconstruction and statistical tests of demographic expansion based on variation at three non‐coding chloroplast sequence regions ( atpF, ndhF–rpl32, psbD–trnT ) to reconstruct phylogeographical history. Nuclear diversity and population structure at 11 microsatellite loci were investigated for evidence of genetic drift. Results Evidence for prolonged persistence and a lack of vicariance within the species range was found, together with strong evidence of historical demographic expansion. Contrary to expectations, there was little evidence of nuclear genetic drift despite strong, above‐ground spatio‐temporal population patchiness. Main conclusions Our findings suggest that a late Pleistocene increase in fire frequency may have led to demographic expansion in this fire‐ephemeral species; alternatively, the expansion signal may be an inherent feature of fire ephemerals with a persistent soil seed bank. Prolonged climatic stability has likely fostered persistence within the species range in contrast to contraction and vicariance. The notable lack of genetic drift implies a role for ample pollen dispersal and a long‐lived soil seed bank in the maintenance of diversity and connectivity in an otherwise stochastic, fire‐driven system.