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Multiple Data Sets (multiple + data_set)

Distribution by Scientific Domains

Life Sciences	60%

Selected Abstracts

Radiation of the Spider Genus Dysdera (Araneae, Dysderidae) in the Canary Islands: Cladistic Assessment Based on Multiple Data Sets

CLADISTICS, Issue 4 2001
Miquel A. Arnedo
The volcanic archipelago of the Canary Islands, 100 km off the northwestern coast of Africa, harbors 43 endemic species of the mostly circum-Mediterranean spider genus Dysdera (Araneae, Dysderidae). This amounts to approximately one-fourth of all known Dysdera species in an area that represents 0.1% of the range of the genus. In order to address the origin of this extraordinary number of endemic species, the phylogenetic relationships among all the endemic taxa and a sample of 27 continental species were reconstructed. A simultaneous cladistic analysis was performed on 66 morphological characters, 471 bp of the cytochrome oxidase I and 424 bp of the 16S rRNA mitochondrial genes. The preferred most parsimonious tree supports a single origin for most of the endemic species (84%), although this tree is ambiguous regarding the total number of overseas colonizations (allowing a minimum of two and a maximum of four colonization events). Our data suggest that the Canary Islands have been the source of the colonizers of some of the remaining Macaronesian archipelagoes (certainly for the Selvagem Islands and the Cape Verdes and possibly for Madeira); the Azores have been independently colonized by dysderids from the continent. The present study provides a phylogenetic framework for an exceptional case of insular species radiation, an essential tool for unraveling the factors that have promoted this amazing diversification. Species radiations in oceanic archipelagoes are excellent models for the study of speciation processes. [source]

Determination of directionally dependent structural and microstructural information using high-energy X-ray diffraction

JOURNAL OF APPLIED CRYSTALLOGRAPHY, Issue 6 2008
J. E. Daniels
High-energy synchrotron X-ray diffraction using a monochromatic beam and large area detector offers a unique method for the study of directionally dependent sample information. The very short wavelengths and subsequent low scattering angles mean that scattering vectors at all angles approximately perpendicular to the beam direction are sampled simultaneously. Here a method is proposed and demonstrated in which the magnitude and directions of structural and microstructural changes can be determined with higher resolution than was possible with previously used techniques. The method takes advantage of parametric refinements over multiple data sets using the profile fitting package TOPAS. Examples of the technique applied to the study of strains in multiphase zirconium alloys and microstructural texture in ferroelastic/ferroelectric ceramics are given. The angular precision in lattice strain for a diffraction image with good statistics is found to be below 0.1°. [source]

Historical male-mediated introgression in horseshoe bats revealed by multilocus DNA sequence data

MOLECULAR ECOLOGY, Issue 7 2010
XIUGUANG MAO
Abstract Instances of hybridization between mammalian taxa in the wild are rarely documented. To test for introgression between sibling species of horseshoe bat (Rhinolophus yunanensis and R. pearsoni) and two subspecies of the latter (R. p. pearsoni and R. p. chinensis), we sequenced two mtDNA and two ncDNA markers in individuals sampled from multiple localities within their overlapping ranges. The interspecific mtDNA gene tree corresponded to the expected taxonomic divisions, and coalescent-based analyses suggested divergence occurred around 4 MYA. However, these relationships strongly conflicted with those recovered from two independent nuclear gene trees, in which R. yunanensis clustered with R. p. pearsoni to the exclusion of R. p. chinensis. This geographically widespread discordance is best explained by large-scale historical introgression of ncDNA from R. yunanensis to R. pearsoni by male-mediated exchange in mixed species colonies during Pleistocene glacial periods, when ranges may have contracted and overlapped more than at present. Further species tree,gene tree conflicts were detected between R. p. pearsoni and R. p. chinensis, also indicating past and/or current introgression in their overlapping regions. However, here the patterns point to asymmetric mtDNA introgression without ncDNA introgression. Analyses of coalescence times indicate this exchange has occurred subsequent to the divergence of these subspecies from their common ancestor. Our work highlights the importance of using multiple data sets for reconstructing phylogeographic histories and resolving taxonomic relationships. [source]

Systematics and evolutionary relationships of the mountain lizard Liolaemus monticola (Liolaemini): how morphological and molecular evidence contributes to reveal hidden species diversity

BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY, Issue 3 2009
FERNANDO TORRES-PÉREZ
The delimitation of species is a major issue in systematic biology and has been a re-emerging discipline in the last decade. A number of studies have shown that the use of multiple data sets is critical for the identification of cryptic species, particularly in groups with complex evolutionary histories. Liolaemus monticola is a montane lizard species distributed in central Chile (32°,42°S), with four described subspecies in a latitudinal gradient from north to south: L. m. monticola, L. m. chillanensis, L. monticola ssp. and L. m. villaricensis. In order to test the systematic status and phylogenetic relationships of the taxa included in the L. monticola group, we analysed morphological (morphometric and meristic) and molecular (allozyme and mitochondrial DNA) data sets. The results of the morphological analyses showed that meristic variables correctly assigned individuals with higher accuracy than did morphometric characters. The results of the analyses of allozyme data revealed eight diagnostic loci that are evidence for significant differences among the four L. monticola subspecies. Phylogenetic analyses with mitochondrial DNA data, including additional species, showed that the L. monticola group is polyphyletic. We postulate that the four current subspecies represent independent evolutionary lineages and must be raised to the specific level as L. monticola, L. chillanensis and L. villaricensis. The taxonomic status of the unnamed L. monticola ssp. remains unresolved, although we provide a preliminary proposal. © 2009 The Linnean Society of London, Biological Journal of the Linnean Society, 2009, 96, 635,650. [source]

Palaeo-ice streams and the subglacial landscape mosaic of the North American mid-continental prairies

BOREAS, Issue 3 2009
MARTIN ROSS
The analysis of the glacial landscape of southern Saskatchewan (Canada) through multiple data sets (e.g. digital elevation model, till compositional data) has revealed previously unrecognized subglacial sediment,landform assemblages. A southwest-trending corridor of mega-scale till lineations (Maskwa corridor) bounded on each side by hummocky terrain extends from the Canadian Shield to southwestern Saskatchewan. This landform assemblage is clearly cross-cut by a broad south to southeast trending corridor (Buffalo corridor) consisting of subparallel curvilinear till ridges. The carbonate content of the surface till is spatially consistent within these assemblages, suggesting a strong sediment,landform relationship. The two corridors are interpreted as the product of palaeo-ice streams. The Maskwa palaeo-ice stream flowed up the regional slope and across preglacial valleys, indicating it was thick and stable. Narrow dispersal trains extending across as well as down-glacier from the Athabasca Basin suggest that the Maskwa palaeo-ice stream extended far into the ice sheet across contrasting shield and platform terrains. In comparison, the Buffalo palaeo-ice stream was thinner and largely controlled by subglacial geology and topography. Its catchments were located at the Canadian Shield boundary and the system was oriented along-slope. It experienced lateral shifts and it was fed by a network of tributaries. The glacial dynamics shift from the Maskwa to the Buffalo system occurred at about 13.5 14C kyr BP. The Buffalo system later evolved into thin outlet lobes until final deglaciation of the area. The proposed model has implications for ice-sheet reconstruction and the assessment of till properties in the prairies and in similar terrains. [source]