| Literature DB >> 28793855 |
Anja Palandačić1, Alexander Naseka2,3, David Ramler4, Harald Ahnelt2,5.
Abstract
BACKGROUND: Molecular taxonomy studies and barcoding projects can provide rapid means of detecting cryptic diversity. Nevertheless, the use of molecular data for species delimitation should be undertaken with caution. Especially the single-gene approaches are linked with certain pitfalls for taxonomical inference. In the present study, recent and historical species descriptions based upon morphology were used as primary species hypotheses, which were then evaluated with molecular data (including in type and historical museum material) to form secondary species hypotheses. As an example of cryptic diversity and taxonomic controversy, the European Phoxinus phoxinus species complex was used.Entities:
Keywords: Cryptic diversity; Molecular taxonomy; Phoxinus (Cyprinidae); Species delimitation
Mesh:
Substances:
Year: 2017 PMID: 28793855 PMCID: PMC5549366 DOI: 10.1186/s12862-017-1032-x
Source DB: PubMed Journal: BMC Evol Biol ISSN: 1471-2148 Impact factor: 3.260
Primary species vs. secondary species hypotheses
| Primary species hypothesis | Secondary species hypothesis | ||||||
|---|---|---|---|---|---|---|---|
| From the literature | Result of this study | ||||||
| Species ( | Species range | Remarks | Clade | mtDNA | ntDNA | Adjusted range | Remarks |
|
| River Morača and its tributary Zeta, belonging to the Skadar Lake basin | 7 | synonym of | ||||
|
| Adour drainage, Ebro drainage, streams of Cantabric range, introduced in Douro drainage | 13 | confirmed | confirmed | Ugarna drainage, Bay of Biscay | Indication of two species, other species with distribution ranges Adour and Ebro drainages | |
|
| According to Kottelat [ | Elevated to species level Bogutskaya & Naseka [ | 18 | confirmed | confirmed | Natanebi drainage, Black Sea | Indication of two species confirmed; other species Mchishta drainage, Black Sea |
|
| Probably endemic to the karstic Popovo Polje–Trebinje endorheic river system | 7 | confirmed | confirmed | Skadar Lake drainage and some sinking streams, Adriatic Sea | ||
|
| Krk Island, Zrmanja River, probably other rivers of the Dalmatian district (Krka, Neretva) | 1 | synonym of | Krka and Neretva belong to other clades (see below) | |||
|
| Probably endemic to the endorheic river system of Lika region | 1 | synonym of | ||||
|
| Po River, Italy, according to Kottelat [ | Originally | 1 | confirmed | confirmed sensu stricto | North Adriatic Sea basin and middle Danube drainage, Black Sea | |
|
| According to Kottelat [ | Originally | 10 | confirmed | limited support | Rhine drainage, North Sea | According to molecular data very restricted range |
|
| According to Kottelat [ | 14 | uncertain | limited support | Unchanged | Denser sampling and further analysis needed | |
|
| Struma, possibly Loudias and Filiouris drainages | 15 | uncertain | no data available | Unchanged | Denser sampling and further analysis needed | |
|
| Mediterranean coastal streams from Gardon to Tech | 12 | confirmed | limited support | Unchanged | ||
|
| Only the type locality given in the description—Korita, Bijelo Polje | According to Kottelat [ | 5 | confirmed | confirmed sensu stricto | Mostly right tributaries of Danube drainage, Black Sea | |
|
| Small streams in the surroundings of Vienna and beyond | According to Kottelat [ | 9 | confirmed | limited support | Middle and lower Danube drainage, mostly the left tributaries, Black Sea | |
|
| Only the type locality given in the description: Bode Creek near Rübeland, Germany, Elbe drainage, North Sea | Originally | 11 | uncertain | no data available | Elbe and Weser drainages, North Sea, but also Danube | Specimens from the type locality needed |
|
| 2 | uncertain | confirmed | Neretva drainage and sinking streams mouthing to middle Adriatic Sea; but also Danube drainage, Black Sea basin | Denser sampling and further analysis needed | ||
|
| 3 | uncertain | limited support | Danube drainage, Black Sea | Denser sampling and further analysis needed | ||
|
| 4 | uncertain | limited support | Danube drainage, Black Sea | Denser sampling and further analysis needed | ||
|
| 6 | confirmed | confirmed | Krka River, Adriatic Sea basin | Well separated from other clades | ||
|
| 8 | confirmed | limited support | Ohrid Lake basin, Adriatic Sea | Well separated from other clades | ||
|
| 16 | uncertain | no data available | Rhone drainage, Mediterranean Sea | Only one specimen with this haplotype found | ||
|
| 17 | confirmed | confirmed | Baltic, North Sea basins (excluding southern coast of the North Sea) | Indication of two species confirmed with ntDNA. | ||
Fig. 1Sampling sites used in this study. Data set comprise a combination of new material and data downloaded from Genbank. For details see Additional file 2: Tables S2. Target symbols denote type localities of Phoxinus csikii, P. marsilii and P. morella. We do not have genetic data from the type localities of P. csikii and P. morella (points marked in pale red and pale violet, respectively). The arrows on the figure mark areas, where hybrids were detected. They correspond to arrows in Fig. 3b
Fig. 3Haplotype networks constructed with nuclear DNA. The colours represent lineages detected by mitochondrial DNA analysis. For both genes, the gametic phase of heterozygous individuals was determined using Phase 2.1 [38, 39], then an unrooted minimum-spanning networks were constructed with median-joining algorithm [32] implemented in Network 5.1 (www.fluxus-engineering.com) with default settings. Figure 3a Rhodopsin haplotype network was constructed from 782 base pair long phased alignment. Figure 3b Recombination activating gene 1 (RAG1) haplotype network was constructed using 1413 base pair long phased alignment. The arrows denote areas, where hybrids were detected and correspond to Fig. 1
An overview of the material, genes and analysis used is this study
Versions of programs used: BEAST 1.8.0 [26]; PhyML [29], GARLI 2.01 [30, 31], NETWORK 5.0 (www.fluxus-engineering.com), MEGA 5.0 [24]; species delimitation programs: ABGD Automatic Barcode Gap Discovery [33], GMYC General Mixed Yule Coalescent model [34], PTP Poisson Tree Processes [35]; ISOLATION-BY-DISTANCE calculated in IBD web service (http://ibdws.sdsu.edu/~ibdws/); genes: COI cytochrome oxidase I, cytb cytochrome b; RH rhodopsin, RAG1 recombination activating gene 1
Fig. 2Phylogenetic reconstruction and haplotype network for revision of the genus Phoxinus. Figure 2a Phylogenetic tree constructed from the barcoding region of mitochondrial gene cytochrome oxidase I (COI). Collapsed alignment includes 139 unique haplotypes. The tree was created using Bayesian inference (BI) with BEAST 1.8.0 [26]. Branches carry posterior probabilities (PP) and bootstraps (BS) from the tree constructed with the Maximum-Likelihood (ML) method (PhyML; [29]). Weakly supported nodes are grey and only PP above 0.9 are shown for the main clades (no subclades). -, denotes lack of bootstraps originating from the difference between the BEAST and ML trees. Figure 2b Phylogenetic tree constructed with two partitions: COI and cytochrome b. Collapsed alignment includes 162 unique haplotypes. As in Fig. 2a, BI and ML were used. Because PhyML does not support partitions, GARLI v.2.01 [30, 31] was used for ML. Figure 2c An unrooted minimum-spanning network was constructed with COI using the median joining algorithm [32] implemented in Network 5.0 (www.fluxus-engineering.com) with default settings. The position of the type material in the network is denoted with TYPE PM for Phoxinus marsilii and TYPE PC for P. csikii