Abstract:Background: Models of the maintenance of sex predict that one reproductive strategy, sexual or parthenogenetic, should outcompete the other. Distribution patterns may reflect the outcome of this competition as well as the effect of chance and historical events. We review the distribution data of sexual and parthenogenetic biotypes of the planarian Schmidtea polychroa.
“…Sequences of the mitochondrial gene Cox1 and the 28S ribosomal RNA gene (28S) of the different Schmidtea species were downloaded from GenBank. In the case of S. mediterranea and S. polychroa, those sequences were selected that capture the maximum genetic variability of the species, based on previous studies (L azaro et al, 2011;Pongratz et al, 2003), while for S. lugubris and S. nova, all available…”
Section: Taxon Samplingmentioning
confidence: 99%
“…The first Cox1 sequences of S. mediterranea and S. polychroa were obtained by Baguñ a, Carranza, Paps, Ruiz-Trillo, and Riutort (2001). Two years later, Cox1 of many populations of S. polychroa was sequenced for a phylogeographic study and two sequences of S. lugubris and S. nova were used as Translocation from one chromosome of the first pair to one chromosome of the third pair (Baguñ a et al, 1999) outgroup (Pongratz et al, 2003). Some years later, a Cox1 sequence of each Schmidtea species was included in a study on the molecular phylogeny of the triclads ( Alvarez-Presas, Baguñ a, & Riutort, 2008).…”
The freshwater flatworm genus Schmidtea is endemic in the Western Palearctic region, where it is represented by only four species, thus contrasting with the high species diversity of the closely related genus Dugesia within Europe. Although containing an important model species in developmental and regeneration research, viz. Schmidtea mediterranea, no evolutionary studies on the genus Schmidtea have been undertaken. For the first time, we present a well‐resolved molecular phylogenetic tree of the four species of the genus, inferred on the basis of two molecular markers, and provide also the first detailed morphological account of Schmidtea nova. The phylogenetic tree generated corroborates an earlier speciation hypothesis based on karyological data and points to chromosomal rearrangements as the main drivers of speciation in this genus. The high genetic divergence between the four species, in combination with previous dating studies and their current geographic distribution, suggests that Schmidtea could have originated in Laurasia but lost most of its diversity during the Oligocene. Thus, its present distribution pattern may be the result of the expansion of three of its four relictual species over Europe, probably after the Pleistocene glaciations. Our detailed morphological study of S. nova revealed that it shows a number of remarkable features: interconnected testis follicles, parovaria, an ejaculatory duct exiting into the primary as well as the secondary seminal vesicle by means of a nipple, and the wall of the distal section of the ejaculatory duct being sclerotic or chitinized.
“…Sequences of the mitochondrial gene Cox1 and the 28S ribosomal RNA gene (28S) of the different Schmidtea species were downloaded from GenBank. In the case of S. mediterranea and S. polychroa, those sequences were selected that capture the maximum genetic variability of the species, based on previous studies (L azaro et al, 2011;Pongratz et al, 2003), while for S. lugubris and S. nova, all available…”
Section: Taxon Samplingmentioning
confidence: 99%
“…The first Cox1 sequences of S. mediterranea and S. polychroa were obtained by Baguñ a, Carranza, Paps, Ruiz-Trillo, and Riutort (2001). Two years later, Cox1 of many populations of S. polychroa was sequenced for a phylogeographic study and two sequences of S. lugubris and S. nova were used as Translocation from one chromosome of the first pair to one chromosome of the third pair (Baguñ a et al, 1999) outgroup (Pongratz et al, 2003). Some years later, a Cox1 sequence of each Schmidtea species was included in a study on the molecular phylogeny of the triclads ( Alvarez-Presas, Baguñ a, & Riutort, 2008).…”
The freshwater flatworm genus Schmidtea is endemic in the Western Palearctic region, where it is represented by only four species, thus contrasting with the high species diversity of the closely related genus Dugesia within Europe. Although containing an important model species in developmental and regeneration research, viz. Schmidtea mediterranea, no evolutionary studies on the genus Schmidtea have been undertaken. For the first time, we present a well‐resolved molecular phylogenetic tree of the four species of the genus, inferred on the basis of two molecular markers, and provide also the first detailed morphological account of Schmidtea nova. The phylogenetic tree generated corroborates an earlier speciation hypothesis based on karyological data and points to chromosomal rearrangements as the main drivers of speciation in this genus. The high genetic divergence between the four species, in combination with previous dating studies and their current geographic distribution, suggests that Schmidtea could have originated in Laurasia but lost most of its diversity during the Oligocene. Thus, its present distribution pattern may be the result of the expansion of three of its four relictual species over Europe, probably after the Pleistocene glaciations. Our detailed morphological study of S. nova revealed that it shows a number of remarkable features: interconnected testis follicles, parovaria, an ejaculatory duct exiting into the primary as well as the secondary seminal vesicle by means of a nipple, and the wall of the distal section of the ejaculatory duct being sclerotic or chitinized.
“…This can allow the identification of parental taxa [13] as well as provide information on the number of clonal origins [14], the ages of clonal lineages [15], and the proportion of genetic variation in parthenogens due to post-formation mutation [16]. Recently developed molecular markers and analytical techniques have allowed for more detailed and informative genetic and phylogeographic comparisons between sexual and asexual taxa [7], [17]–[19]. In addition, combination of phylogeographic approaches with analyses of ecological tolerances and interactions can permit cross-validation of phylogeographic inferences [20] and lead to considerably more insight into the underlying processes that generate the observed patterns of geographic distributions, amounts and distributions of genetic variation, and ecological and climatic correlates [e.g.…”
Phylogenetic and geographic evidence suggest that many parthenogenetic organisms have evolved recently and have spread rapidly. These patterns play a critical role in our understanding of the relative merits of sexual versus asexual reproductive modes, yet their interpretation is often hampered by a lack of detail. Here we present a detailed phylogeographic study of a vertebrate parthenogen, the Australian gecko Heteronotia binoei, in combination with statistical and biophysical modeling of its distribution during the last glacial maximum. Parthenogenetic H. binoei occur in the Australian arid zone and have the widest range of any known vertebrate parthenogen. They are broadly sympatric with their sexual counterparts, from which they arose via hybridization. We have applied nested clade phylogeographic, effective migration, and mismatch distribution analyses to mitochondrial DNA (mtDNA) sequences obtained for 319 individuals sampled throughout the known geographic ranges of two parthenogenetic mitochondrial lineages. These analyses provide strong evidence for past range expansion events from west to east across the arid zone, and for continuing eastward range expansion. Parthenogen formation and range expansion events date to the late Pleistocene, with one lineage expanding from the northwest of its present range around 240,000 years ago and the second lineage expanding from the far west around 70,000 years ago. Statistical and biophysical distribution models support these inferences of recent range expansion, with suitable climatic conditions during the last glacial maximum most likely limited to parts of the arid zone north and west of much of the current ranges of these lineages. Combination of phylogeographic analyses and distribution modeling allowed considerably stronger inferences of the history of this complex than either would in isolation, illustrating the power of combining complementary analytical approaches.
“…Often, these patterns differ from those observed in similarly distributed terrestrial taxa. For example, many aquatic species have occupied numerous microrefugia (e.g., Weiss et al 2002, Pongratz et al 2003, Verovnik et al 2005. The high numbers of refugia observed in the Iberian (e.g., Gomez and Lunt 2007) and Balkan Peninsulas (e.g., Krystufek et al 2007) and in the Carpathian Mountains and basin (Botosaneanu 1973, 1975, Malicky 2006 indicate the importance of these regions as Pleistocene refugia and diversification centers.…”
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