| Literature DB >> 22427830 |
Ylenia Chiari1, Arie van der Meijden, Mauro Mucedda, João M Lourenço, Axel Hochkirch, Michael Veith.
Abstract
Detecting the factors that determine the interruption of gene flow between populations is key to understanding how speciation occurs. In this context, caves are an excellent system for studying processes of colonization, differentiation and speciation, since they represent discrete geographical units often with known geological histories. Here, we asked whether discontinuous calcareous areas and cave systems represent major barriers to gene flow within and among the five species of Sardinian cave salamanders (genus Hydromantes) and whether intraspecific genetic structure parallels geographic distance within and among caves. We generated mitochondrial cytochrome b gene sequences from 184 individuals representing 48 populations, and used a Bayesian phylogeographic approach to infer possible areas of cladogenesis for these species and reconstruct historical and current dispersal routes among distinct populations. Our results show deep genetic divergence within and among all Sardinian cave salamander species, which can mostly be attributed to the effects of mountains and discontinuities in major calcareous areas and cave systems acting as barriers to gene flow. While these salamander species can also occur outside caves, our results indicate that there is a very poor dispersal of these species between separate cave systems.Entities:
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Year: 2012 PMID: 22427830 PMCID: PMC3299655 DOI: 10.1371/journal.pone.0032332
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Figure 1Map of sampling sites in Sardinia.
Sampling localities are indicated with numbers corresponding to populations described in Table 1. The smaller insert, top right, indicates the geographic location of Sardinia Island. Populations: 1–9, H. flavus; 10–28, H. imperialis; 29–37, H. supramontis; 38–39, H. sarrabusensis; 40–48, H. genei. Localities 18–19, 22–23, 40–41, and 46–47 are indicated together due to the small size of the map, but they are separated from each other by several km. Major calcareous areas of the island are indicated in grey.
Sampling localities, sample sizes, and summary of genetic data.
| Species | Population (pop #) |
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| Total | 32 | 496 | 10 | 26 | 26 | 0.879±0.03 | 0.017±0.01 | 8.532±4.05 |
| Lula, Monte Albo- Grotta Conca 'e Crapa (1) | 3 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Lula, Monte Albo- Grotta di Nurai (2) | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Lula, Monte Albo- Voragine su Saccu (3) | 2 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Lula, Monte Albo- Grotta Pupa Niedda (4) | 2 | 2 | 3 | 3 | 1.000±0.50 | 0.006±0.01 | 3.000±2.44 | ||
| Lula, Monte Albo- Badde Viola (5) * | 5 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Siniscola, Monte Albo- Locoli (6) * | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Siniscola, Monte Albo- Grotta dell'Inghiottitoio di Locoli (7) | 4 | 3 | 3 | 3 | 0.833±0.22 | 0.003±0.00 | 1.667±1.22 | ||
| Siniscola, Monte Albo- Nurra di Fruncu 'e Oche (8) | 4 | 2 | 1 | 1 | 0.500±0.27 | 0.001±0.00 | 0.500±0.52 | ||
| Siniscola, Badde Ghiramonte (9) * | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
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| Total | 42 | 572 | 11 | 51 | 50 | 0.877±0.02 | 0.032±0.02 | 18.433±8.34 |
| Dorgali, Monte Coazza- Grotta Gurennoro (29) | 5 | 3 | 2 | 2 | 0.700±0.22 | 0.002±0.00 | 1.000±0.80 | ||
| Oliena, Lanaitto- Grotta su Bentu (30) | 8 | 2 | 1 | 1 | 0.250±0.18 | 0.000±0.00 | 0.250±0.31 | ||
| Oliena, Punta sos Nidos- Nurra de sas Palumbas (31) | 2 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Oliena, Scala 'e Pradu- Pozzetto di Scala 'e Pradu (32) | 5 | 2 | 1 | 1 | 0.400±0.24 | 0.001±0.00 | 0.400±0.44 | ||
| Galtelli, Monte Tuttavista- Pozzo 1 di Tres Puntas (33) | 5 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Urzulei, Tuvoddoli- Grotta Nurra Tuvodduli (34) | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Urzulei- Punta Cuccuttos (35) | 3 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Baunei- Grotta ‘Nurra su Sirbone (36) and * | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Baunei, Tentinole’- Inghiottitoio di Su Canale (37) | 6 | 2 | 1 | 1 | 0.333±0.22 | 0.001±0.00 | 0.333±0.38 | ||
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| Total | 10 | 508 | 3 | 3 | 3 | 0.644±0.10 | 0.003±0.00 | 1.622±1.04 |
| Castadias, Monte Minniminni (38) * | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Burcei, Monte Settefratelli- Sorgente 3 Tulinu (39) | 6 | 2 | 1 | 1 | 0.333±0.22 | 0.001±0.00 | 0.333±0.38 | ||
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| Total | 76 | 477 | 28 | 61 | 58 | 0.963±0.01 | 0.030±0.02 | 14.445±6.54 |
| Sedilo- Funtana Zia Rega (10) | 4 | 2 | 2 | 2 | 0.500±0.27 | 0.002±0.00 | 1.000±0.83 | ||
| Ardauli- Ponte Canale (11) * | 2 | 2 | 1 | 1 | 1.000±0.50 | 0.002±0.003 | 1.000±1.00 | ||
| Ula Tirso- Lago Omodeo (12) * | 7 | 2 | 3 | 3 | 0.476±0.17 | 0.003±0.002 | 1.429±0.99 | ||
| Samugheo, Castello di Medusa- Grotta degli Spelerpes (13) | 5 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Asuni, Abba Suergiu- Grotta Stampu de Muscione (14) | 4 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Seui, Monte Tonneri- Grotta Sa Muragessa (15) | 4 | 2 | 1 | 1 | 0.500±0.27 | 0.001±0.001 | 0.500±0.52 | ||
| Seui, Funtana 'e Pauli- Grutta 'e Pauli (16) | 5 | 2 | 1 | 1 | 0.400±0.24 | 0.001±0.00 | 0.400±0.44 | ||
| Gairo, Taquisara- Grotta di Taquisara (17) | 5 | 2 | 1 | 1 | 0.400±0.24 | 0.001±0.00 | 0.400±0.44 | ||
| Osini, Serra di Orroli- Grotta di Orroli (18) | 6 | 3 | 3 | 3 | 0.733±0.16 | 0.004±0.00 | 1.733±1.17 | ||
| Ulassai, Truculu- Grotta de Is Lianas and along the road before and after the Grotta de Is Lianas (19) and * | 6 | 3 | 4 | 4 | 0.600±0.22 | 0.004±0.00 | 1.933±1.27 | ||
| Sadali, Foresta di Addoli- Near Grotta Margiani Ghiani (20) * | 2 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Nurri, Crabarida- Grotta Asuta 'e Scracca (21) | 1 | - | - | - | - | - | - | ||
| Tertenia- Bosco di San Pietro (22) * | 2 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Tertenia- Aqueduct S'ena e Gabudu (23) | 2 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Perdasdefugu, Su Sarmentargiu- Grotta Sa Rutta e' Linus (24) | 5 | 2 | 1 | 1 | 0.600±0.18 | 0.001±0.00 | 0.600±0.56 | ||
| Perdasdefugu, Se Tomeu- Near Grotta 6 Se Tomeu (25) * | 3 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Villaputzu, Suergiu- Fossa de Suergiu (26) | 3 | 1 | 0 | 0 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| San Nicolo Gerrei, Monte Taccu- Grotta Risorgenza Sa Turru (27) | 5 | 2 | 1 | 1 | 0.600±0.18 | 0.001±0.00 | 0.600±0.56 | ||
| Villasalto, Pardu- Grotta Sa Rutta 'e Scusi (28) | 5 | 2 | 2 | 2 | 0.400±0.24 | 0.002±0.00 | 0.800±0.68 | ||
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| Total | 24 | 490 | 13 | 64 | 61 | 0.924±0.03 | 0.037± 0.02 | 18.159±8.35 |
| Fluminimaggiore - Mine di Terras Nieddas (40) | 5 | 2 | 1 | 1 | 0.400±0.24 | 0.001±0.00 | 0.400±0.44 | ||
| Fluminimaggiore - Grotta su Mannau (41) | 1 | - | - | - | - | - | - | ||
| Domusnovas - Mine Su Corovau (42) | 4 | 3 | 2 | 2 | 0.833±0.22 | 0.002±0.00 | 1.000±0.83 | ||
| Iglesias - Near Grotta Cuccuru Tiria (43) * | 1 | - | - | - | - | - | - | ||
| Iglesias - Grotta Gutturu 'e Sattu (44) | 2 | 2 | 1 | 1 | 0.000±0.00 | 0.000±0.00 | 0.000±0.00 | ||
| Carbonia- Monte Tasua (45) * | 5 | 2 | 2 | 2 | 0.600±0.18 | 0.002±0.00 | 1.200±0.91 | ||
| Nuxis, Tattinu - Grotta dei geotritoni (46) | 4 | 2 | 2 | 2 | 0.500±0.27 | 0.002±0.00 | 1.000±0.83 | ||
| Nuxis, Tattinu - La Cava Romana (47) | 1 | - | - | - | - | - | - | ||
| Domus de Maria, Orbai - Galleria Mazzini (48) | 1 | - | - | - | - | - | - | ||
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| 184 | 65 |
Pop # refers to population number as indicated in Figure 1; N indicates the sample size for each species and population, bp the number of base pairs used after removal of sites with missing or ambiguous characters in at least one of the sequences (see Materials and Methods), h the number of haplotypes, #Mut the number of mutations, S the number of polymorphic sites, Hd the haplotype diversity, π the nucleotide diversity, k the mean number of pairwise differences between sequences. Hd, π, and k has been calculated only for populations with two or more individuals. Populations are indicated with the municipality name first followed by the population name. “*” next to the population names indicates that animals were sampled in old quarries, outside caves or deeply buried under stones. No “*” indicates that populations were sampled in caves.
Figure 2Phylogenetic reconstruction.
Phylogenetic Maximum Likelihood tree with bootstrap support and Bayesian posterior probabilities indicated at the nodes. Divergent clades within each species further investigated for genetic distances are indicated with the species name and the clade number next to the tree. Network correspondence (as in Figures 5 and 6) is indicated next to each clade. Differently colored bars next to the haplotype names indicate distinct calcareous areas as shown in the maps next to the tree. Numbers on the maps refer to sampling localities (Table 1). Bootstrap values and posterior probabilities below 50 and 0.7, respectively and outgroups are not shown.
Figure 5Haplotype networks for Sardinian Hydromantes species.
A) Haplotype networks of H. flavus; B) Haplotype networks of H. supramontis; C) Haplotype network of H. sarrabusensis. The length of the respective fragment and the number of individuals used for each species are given in Table 1. Numbers in parentheses after the locality name correspond to population numbers as in Figure 1. Small white circles indicate missing haplotypes. Rectangles indicate possible ancestral haplotypes. The size of the rectangles and ellipses is proportional to the number of individuals sharing the same haplotypes as indicated. Colors correspond to distinct localities as indicated in each legend. Small insets next to each species network indicate calcareous massifs groups (circles in grey) according to current geological knowledge for the sampled localities. Localities which are not encircled by grey shadows do not occur in a calcareous area. H. sarrabusensis does not occur in a calcareous area.
Figure 6Haplotype networks for Sardinian Hydromantes species.
A) Haplotype networks of H. imperialis, and B) Haplotype networks of H. genei. See Figure 5 for details.
Figure 3Bayesian phylogeography results.
Maximum clade credibility tree from Bayesian phylogeography analysis showing posterior probabilities >0.6 on branch nodes. Color coding and thickness of branches indicate different dispersal rates: thicker and red colored branches correspond to higher dispersal rates, while blue and thinner branches correspond to slower dispersal rates. Numbers at the bottom of the figure indicate relative time scale in percentage from the last common ancestor. “0” indicates that no time has passed and “1” that 100% time has passed since the last common ancestor.
Figure 4Cladogenesis and dispersal patterns of Sardinian cave salamanders.
Origin and dispersal patterns of the species Hydromantes flavus, H. supramontis, H. imperialis, and H. sarrabusensis. The progressive origin and dispersal patterns - from step 1 (ancestral species, “start” point) to the final/current situation- obtained by Bayesian phylogeographic analysis is indicated from left to right on the map of Sardinia with the localities sampled for the four species (as in Figure 1). Numbers correspond to the same localities coded as in Figure 1. The red-yellow-grey color gradient corresponds to different dispersal rates (from a more rapid to a slower dispersion, respectively).
Figure 7Optimal intraspecific grouping that maximizes genetic divergence.
Plot of the number of groupings (K, on the x-axes) versus the F values obtained for each K grouping (y-axes) according to the SAMOVA results. See text for details.