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S Temperate Marine Phylogeography, with New Evidence from High‐ Journal of Biogeography (J. Biogeogr.) (2017) 44, 217–229 ORIGINAL An overview of Australia’s temperate ARTICLE marine phylogeography, with new evidence from high-dispersal gastropods Peter R. Teske1,2, Jonathan Sandoval-Castillo1, Jonathan Waters3 and Luciano B. Beheregaray1* 1Molecular Ecology Lab, School of Biological ABSTRACT Sciences, Flinders University, Adelaide, SA Aim We provide an overview of the location and ages of coastal phylogeographi- 5001, Australia, 2Molecular Zoology Lab, cal breaks in southern Australian planktonic dispersers, and test the hypothesis Department of Zoology, University of Johannesburg, Auckland Park 2006, South that the absence of such breaks in some species is an artefact of insufficient reso- Africa, 3Department of Zoology, Allan Wilson lution of genetic markers when such breaks evolved comparatively recently. Centre for Molecular Ecology and Evolution, Location Temperate coastal Australia. University of Otago, Dunedin, New Zealand Methods We generated a large (> 1500 individuals) data set from rapidly evolving microsatellite markers for two codistributed Australian coastal gas- tropods, and compared it with mitochondrial DNA data. Both study species, the snail Nerita atramentosa and the limpet Siphonaria diemenensis, have long planktonic dispersal phases, and neither taxon exhibits substantial regional genetic structure on the basis of mitochondrial DNA. We tested for the pres- ence of genetic structure by means of AMOVA, Bayesian clustering (struc- ture) and iterated realloction (flock). Results There was no compelling evidence for the existence of more than one evolutionary lineage in either species. Main conclusions Discrepancies in the phylogeographical structuring of co-distributed intertidal taxa cannot be attributed to insufficient marker resolu- tion for the two species considered here, and likely reflect a combination of abiotic and biotic factors that include porous dispersal barriers, life history and species age/history. It appears that contemporary oceanography does not explain the presence of phylogeographical breaks, but may serve to maintain breaks that evolved earlier. Deep genetic divergence in some of the previously studied coastal invertebrates suggests that these could be cryptic species, in which case competitive exclusion may play a role in constraining species biogeography. *Correspondence: Luciano Beheregaray, School Keywords of Biological Sciences, Flinders University, biogeography, dispersal, microsatellites, mitochondrial DNA, molluscs, Adelaide, SA 5001, Australia. E-mail: luciano.beheregaray@flinders.edu.au planktonic larvae, population connectivity (e.g. Waters et al., 2005; Doubleday et al., 2009; Teske INTRODUCTION et al., 2011). Genetic studies on marine organisms conducted in recent Molecular dating indicates that phylogeographical breaks decades have rejected the idea (e.g. Caley et al., 1996; shared by co-distributed species did not all evolve contempo- Eckman, 1996) that there are few barriers to connectivity raneously, but instead have multiple independent origins, with in the sea. Genetic discontinuities between regional clusters most of the spatially congruent breaks identified originating within species (phylogeographical breaks, which may be throughout the Pliocene and Pleistocene (Ayre et al., 2009; evident on the basis of either phylogenetic monophyly or Teske et al., 2013; Mmonwa et al., 2015; Table 1). These differences in allele frequencies) are very common, even epochs were characterized by climate oscillations (alternating in species with theoretically high dispersal capabilities glacial and interglacial phases) during which changes in global ª 2016 John Wiley & Sons Ltd http://wileyonlinelibrary.com/journal/jbi 217 doi:10.1111/jbi.12783 P. R. Teske et al. sea levels (Fisher et al., 2010), and the associated alterations in 2003; Ayre et al., 2009). Physical factors, such as oceanogra- hydrography (Bostock et al., 2006; Lu€er et al., 2009) and habi- phy or habitat continuity, may thus be insufficient to tat availability (Toms et al., 2014), may have repeatedly explain coastal phylogeographical breaks, and a greater focus resulted in the formation of similar dispersal barriers. would need to be placed on the role of biological factors, Given the ubiquity of phylogeographical breaks in coastal such as larval behaviour, competition, predation or species- habitats, and the considerable amount of time available for specific tolerance ranges to environmental variables. Study- these to evolve, it is puzzling that some species that disperse ing these factors is considerably more challenging, and their by means of planktonic larvae have phylogeographical roles would have to be assessed individually for each breaks, whereas co-distributed species with similar and often species. potentially lower dispersal potential exhibit apparent pan- However, before a definite conclusion concerning the role mixia (e.g. Ayre et al., 2009; Teske et al., 2014a). Moreover, of abiotic factors in driving and maintaining genetic struc- many high-dispersal species have phylogeographical breaks ture can be reached, it is necessary to thoroughly assess the across environmental features that are assumed to present possibility that numerous phylogeographical breaks are in only modest barriers to gene flow, such as areas of occa- fact present, but could not be detected because previously sional cold-water upwelling (Teske et al., 2011), weak river generated molecular data sets that were mostly based on sin- discharge (Ridgway et al., 1998) and coastal dunefields gle-locus data from the mitochondrial genome (mtDNA) (Teske et al., 2006; Hidas et al., 2007). These phenomena (Colgan, 2015), were not sufficiently informative. are usually attributed to unexpected discrepancies between Despite the global escalation of phylogeographical surveys expected and realized dispersal (e.g. Taylor & Hellberg, using multilocus DNA data (Beheregaray, 2008; Garrick Table 1 Phylogeographical breaks identified in temperate Australian marine organisms with a planktonic dispersal phase, and their approximate ages. Barrier codes correspond to those in Fig. 1. Barrier Species Marker N Time of split (Ma) References B Aplodactylus spp. mtDNA CytbP & COIP 1,1 7.8–11.2 Burridge (2000) B1 Lasaea australis mtDNA COIIIP 4,8 13.1–13.4 Li et al. (2013) mtDNA 16SP 41,66 (not dated) nuDNA ITS2P 19,27 (not dated) C, E, F Catomerus polymerus mtDNA COIP 23,11 1.1–1.9 York et al. (2008) mtDNA CRP 20,12 (not dated) nuDNA MicrosatellitesA 3995 (not dated) C Meridiastra spp.2 mtDNA COIP 17,11 2.1–2.4 Waters et al. (2004) C Scutus spp. mtDNA COIP, A 6,45 (not dated) Waters et al. (2006) DorE Nemadactylus spp. mtDNA CytbP & COIP 1,1 2.7–3.8 Burridge (2000) E Austrolittorina unifasciata mtDNA COIP, A 50,50 (not dated) Waters et al. (2006) E Catomerus polymerus mtDNA COIP, A 23,21 0.2–0.5 Ayre et al. (2009) E Catostylus mosaicus mtDNA COI 6,6 c. 1.4 Dawson (2005) nuDNA ITS1 7,5 (not dated) E Cellana tramoserica mtDNA COIP, A 23,25 0.2–0.6 Ayre et al. (2009) E Coscinasterias muricata mtDNA COIP 4,2 0.2–0.3 Waters & Roy (2003) E Donax deltoides nuDNA MicrosatellitesA 1115,6 (not dated) Miller et al. (2013) E Meridiastra calcar mtDNA COIP, A 25,19 0.2–0.3 Ayre et al. (2009) E Meridiastra spp.3 mtDNA COIP 19,11 2.1–2.4 Waters et al. (2004) E Scutus spp. mtDNA COIP, A 21,30 (not dated) Waters et al. (2006) E Plaxiphora albida mtDNA COIP, A 16,12 0.4–11.6 Ayre et al. (2009) F4,G Durvillea potatorum4 mtDNA COIP 1075 (not dated) Fraser et al. (2009) cpDNA rbcLP 775 (not dated) F Pyura spp. mtDNA COIP 245,44 (not dated) Rius & Teske (2013) nuDNA ANT intronP 142,76 (not dated) G Lasaea australis mtDNA COIIIP 2,6 11.7–12.0 Li et al. (2013) mtDNA 16SP 39,27 (not dated) nuDNA ITS2P 13,14 (not dated) G Nerita spp. mtDNA COIP, A 38,49 5.0–6.0 Waters et al. (2005) G Octopus maorum nuDNA MicrosatellitesA 93,35 (not dated) Doubleday et al. (2009) 1Geographical position differed for different markers; 2western versus central lineages; 3central versus eastern lineages; 4eastern portion of the range only; 5only total sample size provided (lineages do not have strict geographical divisions); 6corresponding mtDNA data were not genetically structured; Ma = million years ago; mtDNA = mitochondrial DNA; nuDNA = nuclear DNA; cpDNA = chloroplast DNA. Presence of genetic breaks was identified on the basis of P = Phylogenetic monophyly (based trees or haplotype networks) or A = Allele frequency differences using F-statistics (FST, ΦST, AMOVA etc.); N = number of samples included per regional lineage. 218 Journal of Biogeography 44, 217–229 ª 2016 John Wiley & Sons Ltd Temperate Australian marine phylogeography et al., 2015), research on marine phylogeographical breaks effect can be reduced by increasing sample sizes (Kalinowski, continues to be dominated by single-locus studies based on 2005). mtDNA (e.g. Haye et al., 2014; Teske et al., 2015a; Wright Here, we present an overview of the ages and locations of et al., 2015; Table 1). The application of multi-locus genetic phylogeographical breaks on the temperate Australian coast, data sets has revealed discrepancies in the levels of introgres- and explore why such breaks are absent in some coastal species. sion and lineage sorting between mtDNA and nuclear DNA Specifically, we tested the hypothesis that species that show no (nuDNA) that has resulted in conflicting phylogeographical broad phylogeographical differentiation on the basis of patterns in the same species (Toews & Brelsford, 2012). In mtDNA data sets of
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