Malerisaurus , a new eosuchian reptile from the late Triassic of India

Two almost complete skeletons of a new eosuchian reptile, Malerisaurus robinsonae n.sp., were discovered as the presumable gastric contents of ‘twin’ skeletons of Parasuchus hislopi . The specimens are from fluvial flood plain deposits of the late Triassic Maleri Formation of the Gondwana supergroup, India. The osteology of Malerisaurus is described in detail. Malerisaurus was a small, gracile, long-necked eosuchian, facultatively bipedal, and probably able to climb trees or to take to the water when alarmed. It is comparable to modern bipedal lizards in size, proportions and inferred activities. The skull, although showing some carnivorous adaptation, is relatively unspecialized and indicates an insectivorous diet. Because Malerisaurus shows such a combination of primitive and advanced features as a diapsid skull, unossified laterosphenoid, lack of antorbital and mandibular fenestrae, slender limbs, primitive girdles, distinctive elongated cervicals and lack of dermal armour, it is assigned to the suborder Prolacertiformes of the order Eosuchia. A classification of Prolacertiformes indicates four families within this suborder: Petrolacosauridae, Protorosauridae, Prolacertidae and Tanystropheidae. Malerisaurus is tentatively allied to Protorosaurus in the family Protorosauridae; in neither genus is the temporal region of the skull adequately known. Malerisaurus furnishes detailed information about the skeletal morphology of what may be a hitherto undocumented lineage of eosuchian reptiles.

Zootaxa ◽  
2020 ◽  
Vol 4860 (4) ◽  
pp. 503-520
Author(s):  
KEVIN J. LAMBKIN

Ipsvicia Tillyard, 1919, and Ipsviciopsis Tillyard, 1922, in Tillyard’s new family, Ipsviciidae, were two of the most impressive insects from the Denmark Hill locality of the Late Triassic (Norian) Blackstone Formation, Ipswich Coal Measures, south-eastern Queensland. Substantial new material, including several fragmentary body specimens, from the Dinmore locality in the same formation, has enabled a revision of the two genera, with the following results: Ipsvicia jonesi Tillyard, 1919 (= Ipsvicia maculata Tillyard, 1919, syn. nov., = Ipsvicia acutipennis Tillyard, 1919, syn. nov.), Ipsviciopsis elegans Tillyard, 1922 (= Ipsviciopsis magna Tillyard, 1922, syn. nov.). The tegmen of Ipsviciopsis is distinguished from that of Ipsvicia on its narrower shape and less convex costal margin, simpler surface sculpture, longer basal cell, sinuous R, only slightly angulate CuA, and sinuous base of 1A. The tegmina of both I. jonesi and I. elegans are noteworthy for their variability in apical venation and shape of the apex, with no two specimens quite the same. The tegmen of I. jonesi has extraordinary surface sculpture comprising patches of fine tubercles set in a coarser tuberculate/punctate groundmass, the patches extremely variable in shape and pattern, again with no two specimens the same. A new diagnosis of the Ipsviciidae has identified the unique form of the distal portion of Sc (dSc—a long groove running along the costal space and crossed by many costal veinlets), the complex and highly variable apical venation, and the simple CuA, as the most distinctive characters. Analysis of all previous taxa which have been referred to the Ipsviciidae restricts the family to the Middle to Late Triassic, with records from Australia, China, France, Germany, Japan and Kyrgyzstan, and with one Early Jurassic record from Kyrgyzstan. Ipsvicia langenbergensis Barth, Ansorge et Brauckmann, 2011, from the Late Triassic of Germany meets the diagnosis of Ipsviciopsis and is transferred as Ipsviciopsis langenbergensis (Barth, Ansorge et Brauckmann, 2011) comb. nov. All previous Permian records of the family have now been transferred to other families of the Scyctinopteroidea, and there are also numerous additional unconfirmed Triassic records. The new body specimens of both Ipsvicia and Ipsviciopsis show that the ipsviciids where robust hemipterans with tough, coriaceous, fairly flatly-folded tegmina, with a large, shield-like, highly sculptured pronotum covering all but the mesoscutellum, and apparently much of the head. The body form is not dissimilar to ground-dwelling cockroaches, or more especially some ground-dwelling moist environment Heteroptera, such as the nepomorph family Gelastocoridae. This body form, as well as their frequent occurrence among the rich Dicroidium-dominant flood plain and swamp flora of the Dinmore locality, where they represent nearly 20% of the preserved insect fauna (cockroaches represent 25%), suggest that the ipsviciids were ground-dwelling insects of moisture-rich floral environments. 


2011 ◽  
Vol 20 (1) ◽  
pp. 161-173
Author(s):  
A.P. Kassatkina

Resuming published and own data, a revision of classification of Chaetognatha is presented. The family Sagittidae Claus & Grobben, 1905 is given a rank of subclass, Sagittiones, characterised, in particular, by the presence of two pairs of sac-like gelatinous structures or two pairs of fins. Besides the order Aphragmophora Tokioka, 1965, it contains the new order Biphragmosagittiformes ord. nov., which is a unique group of Chaetognatha with an unusual combination of morphological characters: the transverse muscles present in both the trunk and the tail sections of the body; the seminal vesicles simple, without internal complex compartments; the presence of two pairs of lateral fins. The only family assigned to the new order, Biphragmosagittidae fam. nov., contains two genera. Diagnoses of the two new genera, Biphragmosagitta gen. nov. (type species B. tarasovi sp. nov. and B. angusticephala sp. nov.) and Biphragmofastigata gen. nov. (type species B. fastigata sp. nov.), detailed descriptions and pictures of the three new species are presented.


Pathogens ◽  
2021 ◽  
Vol 10 (1) ◽  
pp. 41
Author(s):  
Marcos Godoy ◽  
Daniel A. Medina ◽  
Rudy Suarez ◽  
Sandro Valenzuela ◽  
Jaime Romero ◽  
...  

Piscine orthoreovirus (PRV) belongs to the family Reoviridae and has been described mainly in association with salmonid infections. The genome of PRV consists of about 23,600 bp, with 10 segments of double-stranded RNA, classified as small (S1 to S4), medium (M1, M2 and M3) and large (L1, L2 and L3); these range approximately from 1000 bp (segment S4) to 4000 bp (segment L1). How the genetic variation among PRV strains affects the virulence for salmonids is still poorly understood. The aim of this study was to describe the molecular phylogeny of PRV based on an extensive sequence analysis of the S1 and M2 segments of PRV available in the GenBank database to date (May 2020). The analysis was extended to include new PRV sequences for S1 and M2 segments. In addition, subgenotype classifications were assigned to previously published unclassified sequences. It was concluded that the phylogenetic trees are consistent with the original classification using the PRV genomic segment S1, which differentiates PRV into two major genotypes, I and II, and each of these into two subgenotypes, designated as Ia and Ib, and IIa and IIb, respectively. Moreover, some clusters of country- and host-specific PRV subgenotypes were observed in the subset of sequences used. This work strengthens the subgenotype classification of PRV based on the S1 segment and can be used to enhance research on the virulence of PRV.


2021 ◽  
Vol 20 (7) ◽  
pp. 911-927
Author(s):  
Lucia Muggia ◽  
Yu Quan ◽  
Cécile Gueidan ◽  
Abdullah M. S. Al-Hatmi ◽  
Martin Grube ◽  
...  

AbstractLichen thalli provide a long-lived and stable habitat for colonization by a wide range of microorganisms. Increased interest in these lichen-associated microbial communities has revealed an impressive diversity of fungi, including several novel lineages which still await formal taxonomic recognition. Among these, members of the Eurotiomycetes and Dothideomycetes usually occur asymptomatically in the lichen thalli, even if they share ancestry with fungi that may be parasitic on their host. Mycelia of the isolates are characterized by melanized cell walls and the fungi display exclusively asexual propagation. Their taxonomic placement requires, therefore, the use of DNA sequence data. Here, we consider recently published sequence data from lichen-associated fungi and characterize and formally describe two new, individually monophyletic lineages at family, genus, and species levels. The Pleostigmataceae fam. nov. and Melanina gen. nov. both comprise rock-inhabiting fungi that associate with epilithic, crust-forming lichens in subalpine habitats. The phylogenetic placement and the monophyly of Pleostigmataceae lack statistical support, but the family was resolved as sister to the order Verrucariales. This family comprises the species Pleostigma alpinum sp. nov., P. frigidum sp. nov., P. jungermannicola, and P. lichenophilum sp. nov. The placement of the genus Melanina is supported as a lineage within the Chaetothyriales. To date, this genus comprises the single species M. gunde-cimermaniae sp. nov. and forms a sister group to a large lineage including Herpotrichiellaceae, Chaetothyriaceae, Cyphellophoraceae, and Trichomeriaceae. The new phylogenetic analysis of the subclass Chaetothyiomycetidae provides new insight into genus and family level delimitation and classification of this ecologically diverse group of fungi.


1987 ◽  
Vol 65 (3) ◽  
pp. 691-707 ◽  
Author(s):  
A. F. L. Nemec ◽  
R. O. Brinkhurst

A data matrix of 23 generic or subgeneric taxa versus 24 characters and a shorter matrix of 15 characters were analyzed by means of ordination, cluster analyses, parsimony, and compatibility methods (the last two of which are phylogenetic tree reconstruction methods) and the results were compared inter alia and with traditional methods. Various measures of fit for evaluating the parsimony methods were employed. There were few compatible characters in the data set, and much homoplasy, but most analyses separated a group based on Stylaria from the rest of the family, which could then be separated into four groups, recognized here for the first time as tribes (Naidini, Derini, Pristinini, and Chaetogastrini). There was less consistency of results within these groups. Modern methods produced results that do not conflict with traditional groupings. The Jaccard coefficient minimizes the significance of symplesiomorphy and complete linkage avoids chaining effects and corresponds to actual similarities, unlike single or average linkage methods, respectively. Ordination complements cluster analysis. The Wagner parsimony method was superior to the less flexible Camin–Sokal approach and produced better measure of fit statistics. All of the aforementioned methods contain areas susceptible to subjective decisions but, nevertheless, they lead to a complete disclosure of both the methods used and the assumptions made, and facilitate objective hypothesis testing rather than the presentation of conflicting phylogenies based on the different, undisclosed premises of manual approaches.


Parasitology ◽  
1964 ◽  
Vol 54 (4) ◽  
pp. 601-676 ◽  
Author(s):  
J. C. Pearson

Earlier schemes of classification of the family Heterophyidae have been based in large part on such features as shape of body, presence of oral spines, number and position of testes, and distribution of vitellaria (Witenberg, 1929; Ciurea, 1933; Mueller & Van Cleave, 1932). Price (1940a) was the first to make extensive use of features of the ventrogenital complex (ventral sucker, gonotyl, genital pore, terminal male duct) and excretory bladder, and produced the first reasonable classification of both the family Heterophyidae and the superfamily Opisthorchioidea. In despite of the obvious significance of the rationale of Price's approach, later authors (Morozov, 1952, 1955; Yamaguti, 1958) have largely ignored the ventrogenital complex and recently discovered life-history data, and have used much the same sorts of features as earlier authors.


1895 ◽  
Vol 2 (12) ◽  
pp. 529-539 ◽  
Author(s):  
H. A. Nicholson ◽  
J. E. Marr

Since the remarkable paper by Professor Lapworth “On an Improved Classification of the Rhabdophora” was published in the Geological Magazine for 1873, a great deal of fresh information has been gathered as to these interesting fossils; but the classification given in that paper, though to some extent confessedly artificial, is still generally adhered to. Observations made by the authors in recent years lead them to suppose that that classification will in the future undergo considerable modification; but in the present state of our knowledge it serves a purpose so useful, that it is not our intention to propose any immediate change in it. Our object, on the other hand, is to bring forward certain conclusions which we have independently reached, and which will, we believe, enhance the value of Graptolites to the stratigraphical geologist, and lead to results important to the biologist. Our conclusions are based upon an examination of a large number of forms generally referred to the family Dichograptidæ; but, as we propose very briefly to indicate, they affect the relationships of Graptolites belonging to other families also.


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