The osteology of a Lower Permian eosuchian from Texas and a review of diapsid phytogeny

Apsisaurus witteri (gen. et sp. nov. . from the Lower Permian of Texas is identified as a diapsid, based on the presence of both a lateral temporal fenestra and a suborbital fenestra. Derived characters shared with neodiapsids but not with araeoscelidians suggest that Apsisaurus is more closely related to modern diapsids than to araeoscelidians. A phylogenetic analysis suggests that younginiforms are not part of the crown group of diapsids.     

Classification and phylogeny of the diapsid reptiles

Reptiles with two temporal openings in the skull are generally divided into two groups–the Lepidosauria (lizards, snakes, Sphenodon , 'eosuchians') and the Archosauria (crocodiles, thecodontians, dinosaurs, pterosaurs). Recent suggestions that these two are not sister-groups are shown to be unproven, whereas there is strong evidence that they form a monophyletic group, the Diapsida, on the basis of several synapomorphies of living and fossil forms. A cladistic analysis of skull and skeletal characters of all described Permo-Triassic diapsid reptiles suggests some significant rearrangements to commonly held views. The genus Petrolacosaurus is the sister-group of all later diapsids which fall into two large groups–the Archosauromorpha (Pterosauria, Rhynchosauria, Prolacertiformes, Archosauria) and the Lepidosauromorpha (Younginiformes, Sphenodontia, Squamata). The pterosaurs are not archosaurs, but they are the sister-group of all other archosauromorphs. There is no close relationship between rhynchosaurs and sphenodontids, nor between Prolacerta or Tanystropheus and lizards. The terms 'Eosuchia', 'Rhynchocephalia' and 'Protorosauria' have become too wide in application and they are not used. A cladistic classification of the Diapsida is given, as well as a phylogenetic tree which uses cladistic and stratigraphic data.     

Osteoderm microstructure indicates the presence of a crocodylian‐like trunk bracing system in a group of armoured basal tetrapods

Buchwitz, M., Witzmann, F., Voigt, S. and Golubev, V. 2012. Osteoderm microstructure indicates the presence of a crocodylian‐like trunk bracing system in a group of armoured basal tetrapods. —Acta Zoologica (Stockholm) 93 : 260–280. The microstructure of dorsal osteoderms referred to the chroniosuchid taxa Chroniosuchus, Chroniosaurus, Madygenerpeton and cf. Uralerpeton is compared to existing data on the bystrowianid chroniosuchian Bystrowiella and further tetrapods. Chroniosuchid osteoderms are marked by thin internal and relatively thick external cortices that consist of lowly vascularised parallel‐fibred bone. They are structured by growth marks and, in case of Madygenerpeton, by lines of arrested growth. The cancellous middle region is marked by a high degree of remodelling and a primary bone matrix of parallel‐fibred bone that may include domains of interwoven structural fibres. Whereas the convergence of Bystrowiella and chroniosuchid osteoderms is not confirmed by our observations, the internal cortex of the latter displays a significant peculiarity: It contains distinct bundles of shallowly dipping Sharpey’s fibres with a cranio‐ or caudoventral orientation. We interpret this feature as indicative for the attachment of epaxial muscles which spanned several vertebral segments between the medioventral surface of the osteoderms and the transversal processes of the thoracic vertebrae. This finding endorses the hypothesis that the chroniosuchid osteoderm series was part of a crocodylian‐like trunk bracing system that supported terrestrial locomotion. According to the measured range of osteoderm bone compactness, some chroniosuchian species may have had a more aquatic lifestyle than others.     

中国Waagenophyllum（Waagenophyllum）种的分支分析

在对材料产自我国的Waagenophyllum (Waagenophyllum)的种进行系统分类厘定的基础上,以Waagenophyllum (Liangshanophyllum)wengchengense作为外类群,对22个种的10个性状进行分支分析,探讨各种之间的系统发育关系。分支分析结果表明,Waagenophyllum (Liangshanophyllum)与Waagenophyllum(Waagenophyllum)关系很近,一些研究者提出的Liangshanophyllum作为一个独立属的分类意见值得商榷。     

Bone microstructures and mode of skeletogenesis in osteoderms of three pareiasaur taxa from the Permian of South Africa

The extinct parareptilian clade of pareiasaurs was in the past often presented to constitute a morphocline from larger, less armoured forms to smaller, well armoured forms, indicating that the osteoderm cover became an increasingly prominent aspect in the post‐cranial skeleton of these animals. Here, we describe microanatomical and microstructural aspects of osteoderms of the three pareiasaur taxa Bradysaurus, Pareiasaurus and Anthodon from the Permian of South Africa. A generalized mode of osteoderm formation, consistent with intramembraneous skeletogenesis, is hypothesized to be present in all pareiasaurs. Few characters are shared between pareiasaur dermal armour and turtle shell bones and osteoderms. Otherwise, there is strong evidence from microanatomy and histology (i.e. absence of structures that formed via metaplasia of dermal tissue) that indicates nonhomology between pareiasaur dermal armour and the armour of living eureptiles. Analysis with bone profiler revealed no clear connection between bone compactness and lifestyle in the amniote osteoderm sample.     

Phylogeny of the Neotropical moth tribe Josiini (Notodontidae: Dioptinae): a hidden case of Miillerian mimicry

The Neotropical moth tribe Josiini (Notodontidae: Dioptinae) contains over 100 described species in 11 genera. All are diurnal, with brightly-coloured, presumably aposematic wing patterns. Larval hostplants are exclusively in the genus Passiflora (Passifloraceae) except for two new records, reported here, from Tumera (Turneraceae). A comparative morphological study of 26 representative josiine species yielded 86 characters from adults, larvae and pupae, all of which are figured and discussed. Phylogenetic analysis of these data produced a single most-parsimonious cladogram. According to the phylogenetic results: (1) monophyly of the Josiini is strongly supported; (2) the currently accepted generic classification is in disarray; (3) morphological character variation is extensive, and adult traits reflect phylogeny more effectively than do those of immature stages; (4) wing pattern types have undergone convergent evolution. A rare phenotype, longitudinal wing stripes, appears in two widely divergent clades, suggesting the evolution of Miillerian mimicry within the Josiini.     

Phylogeny reconstruction in the neogene bryozoan metrarabdotos: A paleontologic evaluation of methodology

An adequate stratigraphic record can not only aid in both cladistic and stratophenetic reconstruction of phytogenies, but can also serve in estimating the temporal consistency of the resulting phylogenetic trees. For hypothetical data sets, cladistically constructed trees can be as consistent with the temporal distribution of sampled populations or species as those constructed stratophenetically. Empirical testing in taxonomic groups with sufficiently dense fossil records is needed to show whether, and under what conditions, this potential can be realized. A stratophenetic tree and cladistic trees based on several approaches to character weighting were constructed for Caribbean Neogene species of the bryozoan Metrarabdotos with multiple‐character data from closely spaced sequential populations. The modular morphology and highly punctuated evolutionary pattern of these species blur the distinction between continuous and discrete characters, so that all available characters are potentially of equal significance in establishing phytogenies, rather than just those with discrete states conventionally used in cladistic analysis. However, only the cladistic trees generated with all characters weighted to emphasize contribution to species discrimination have temporal consistencies that are clearly significant statistically and approach that of the stratophenetic tree in magnitude. These results provide a start toward establishing general guidelines for cladistic analysis of taxa with stratigraphie records too sparse for stratophenetic reconstruction.     

The population biology of Gehyra (Gekkonidae). III. Patterns of microgeographic variation

The distribution of allozymic and chromosomal polymorphisms was examined among central Australian populations of the chromosomally variable genus Gehyra to assess whether they typically have the small deme size and low gene flow levels required by some models of chromosomal speciation. Particular attention was given to comparisons between rock-specialists (Gehyra nana) and habitat-generalists (Gehyra variegata) to investigate whether the former have more restricted gene flow. Both allozyme and chromosome data sets showed greater among population differentiation in the rock-specialists than the habitat-generalists, consistent with predictions from a previous ecological study (Moritz, 1987), although this pattern could also be due to historical effects. This was evident from the relationships between genetic and geographic distance, the conditional frequency of alleles, and F-statistics. However, both taxa appear to have substantial levels of gene flow. This indicates that Gehyra populations typically do not meet the stringent conditions for the fixation of strongly underdominant chromosome rearrangements through strong genetic drift. A consistent deficiency of heterozygotes does, however, suggest the possibility of inbreeding which would increase the likelihood of the establishment of underdominant rearrangements.     

Caractères et évolution des enzymes chitinolytiques chez les vertébrés infèrieurs

The activity of chitinases extracted from various organs of different fish, amphibians and reptiles was estimated as a function of pH by using “native” chitin as substrate. Three types of chitinase activity were recorded, suggesting the existence of three different chitinase types: Type 1: (optimum pH; 4.5, no activity at pH 1.0) was found in various organs, such as intestine, pyloric caeca, pancreas, liver, spleen, etc.); Type IIa: (optimum pH; 3.0, weak activity at pH 1.0) was obtained from the gastric mucosa of fish and one species of urodele; Type IIb: (optimum pH; 3.0, strong activity at pH 1.0) was found in the gastric mucosa of reptiles and batrachian anura. Chitinase activity appears to be adapted to the pH of the digestive fluids. A tentative scheme is presented of chitinase evolution among lower vertebrates.