The family Phryganeidae (Insecta,Trichoptera) from the Mesozoic and Cenozoic of Asia (with a brief worldwide overview of the fossil caddisfly fauna)

The following new taxa of the family Phryganeidae are described: Proagrypnia sinitsae gen. et sp. nov. from the Upper Jurassic or Lower Cretaceous of Russia (Chernovskie Kopi locality) and Baissophryganoides popovi sp. nov. from the Lower Cretaceous of Mongolia (Anda-Khuduk locality). A larval case of Folindusia (Acrindusia) phryganoides sp. nov. from the Paleocene of Russia (Arkhara–Boguchan brown coal field) is described. A worldwide overview of the records of fossil adult insects and larval cases of Phryganeidae is presented.     

Echinocampidae fam. nov., a new family of Late Jurassic-Early Cretaceous radiolarians of Arctic Siberia

When studying Late Jurassic-Early Cretaceous radiolarians from the Nordvik section (Arctic Siberia), unique morphotypes of multicyrtoid nassellarians with many horns in the apical part of the shell, which continue the rays A, V, 2l, D, and 2L of the cephalic spicule, were recorded. These morphotypes are assigned to a new family, Echinocampidae fam. nov., including three new genera (Echinocampe gen. nov., Nordvikella gen. nov., and Arctocapsula gen. nov.) and eight new species. The family Echinocampidae was probably restricted to high latitudes and belonged to the boreal fauna of the terminal Jurassic and the basal Cretaceous.     

Heterochrony and heterotopy in the phylogeny of sea urchins

The role of heterochrony is evident in ontogeny and phylogeny of irregular (exocyclic) sea urchins. After metamorphosis, a juvenile passes the stage of regular (endocyclic) sea urchin, in which the periproct is surrounded by plates of the apical system. A shift of the periproct in the area of the fifth interambulacrum occurs in extant taxa at early stages of postlarval development and is accompanied by the reduction of genital plate 5. In some ancient (Jurassic) adult irregular sea urchins, the endocyclic state of the apical system is retained for a long time and the derivative of the fifth genital plate is sometimes observed even in Early Cretaceous species. Considerable transformations in the structure of the lower test surface in members of the order Spatangoida are manifested in changes in the relative positions of plastron plates and ambulacral areas I and V, separation of sternal plates from the labrum, etc. The mechanism of these changes is connected with translocation or “sliding” of sutures of particular plates as a result of nonuniform growth and partial resorption. The study of evolutionary lineages of Cretaceous and Cenozoic sea urchins has shown that the evolution was connected with the directional changes in some morphological characters at late ontogenetic stages. The process was accompanied by either extension, peramorphosis (lineages of the genera Micraster, Infulaster–Hagenowia in the European Province), or the loss of these stages, paedomorphosis (Hemiaster (Bolbaster) lineage, Late Eocene–Middle Miocene of Australia). The phenomena of heterochrony and heterotopy in the development of peripetal, marginal, and lateroanal fascioles in the Late Cretaceous and Paleocene families Hemiasteridae, Schizasteridae, and Paleopneustidae are described. The heterotopy is also illustrated by the example of the development of additional genital pores on ocular plates II and IV of the Middle Jurassic species Pygomalus analis (Disasteroida); its apical system has five pores instead of four. In the Late Cretaceous species Guettaria roccardi (Holasteroida), ocular plates II and IV have two pores each; in the apical system, there are eight genital pores instead of four. In some members of the order Holectypoida, the place of lost genital plate 5 is occupied by a new plate sometimes pierced by a pore, but judging from crystallographic data, it is not homologous to other genital plates. The order Clypeasteroida is characterized by the development of very small pores in both ambulacral and interambulacral fields; they provide passage for numerous accessory tube feet.     

New and little-known grylloblattids of the family Geinitziidae (Insecta: Grylloblattida) from the Triassic and Jurassic of Europe,Asia, and South Africa

The fossil history of the family Geinitziidae is reviewed. New taxa are described in the family: Shurabia hissarica, sp. nov. (Lower Jurassic of Tajikistan), Sh. shartegica, sp. nov. (Upper Jurassic of Mongolia), Sh. serrata, sp. nov. and Ginitzia sagulensis, sp. nov. (both Lower Jurassic of Kyrgyzstan). The subfamily Stegopterinae Sharov, 1961 is synonymized under Geinitziinae Handlirsch, 1906. The genera Minesedes Fujiyama, 1973 and Ominea Fujiyama, 1973 (Upper Triassic of Japan) are synonymized under Shurabia Martynov, 1937 and Geinitzia Handlirsch, 1906, respectively. Geinitzia varia Bode, 1953 (Lower Jurassic of Germany) and Fletchizia picturata Riek, 1976 (Upper Triassic of South Africa) are redescribed from their holotypes. F. kapokraalensis Wappler, 2001 and F. aleda Wappler, 2001 (both Upper Triassic of South Africa) are transferred to the genus Shurabia.     

Revision of <Emphasis Type="Italic">Scoliocystis</Emphasis> (Rhombifera: Echinoencrinitidae) and related cystoid genera

Species attributed to Scoliocystis Jaekel, 1899, including the type species S. pumila (Eichwald, 1860) and S. thersites Jaekel, 1899 from the Ordovician of the Leningrad Region, are reviewed. Scoliocystis sp. from the Upper Ordovician of Estonia, figured by Hecker (1964), is redescribed as Maennilocystis heckeri gen. et sp. nov. and it is attributed to the family Callocystitidae Bernard, 1895. The genus Scoliocystis is intermediate between the families Cheirocrinidae and Echinoencrinitidae in having five periproct border plates (as in cheirocrinids), but lacking plate R5 and having a reduced oral area, as in echinoencrinitids, but is retained in the Echinoencrinitidae. The similarity of Scoliocystis to the unusual North American cheirocrinid genus Sprinkleocystis is convergent. The genus Gonocrinites Eichwald, 1840, with two species, is restored among echinoencrinitids, as having four periproct border plates, whereas Echinoencrinites sensu stricto has three. The families Echinoencrinitidae and Callocystitidae arose from cheirocrinids with closed plate circlets by the loss of plate R5 and substitution of radial:lateral for radial:radial pectinirhombs. In addition, echinoencrinitids are characterized by a reduced oral area, whereas in callocystitids, the recumbent ambulacra are extensive. Scoliocystis is a stem-group genus to Echinoencrinitidae plus Callocystitidae. Several glyptocystitoid genera independently developed advanced pectinirhombs.     

New bryozoans (Stenolaemata) from the Middle Jurassic of Moscow City and the Moscow Region

Five new species of stenolaematous bryozoans are described from the Middle Callovian of Moscow City (Krasnopresnenskii Region) and the Moscow Region (Gzhel’ Railroad Station and the quarry between the small towns of Rechitsy and Troshkovo): Entalophora alexeevi sp. nov., Cellulipora retshitsiensis sp. nov., Diplosolen pravus sp. nov., Siphodictyum primarium sp. nov., and Ceata kamushkiensis sp. nov. The last four species belong to the genera that have never been recorded from deposits older than the Lower Cretaceous. The presence of different types of heterozooecia in these bryozoans shows that the functional polymorphism of zooids developed considerably in the class Stenolaemata as early as the Middle Jurassic.     

Earliest Divergence of Stagodontid (Mammalia: Marsupialiformes) Feeding Strategies from the Late Cretaceous (Turonian) of North America

Two new unequivocal stagodontids, Fumodelphodon pulveris, gen. et. sp. nov., and Hoodootherium praeceps, gen. et. sp. nov., are described from the Turonian (~92 Ma) Smoky Hollow Member of the Straight Cliffs Formation, of southern Utah, USA. Mammals from this time period are poorly represented; the recovery of these two large stagodontids demonstrates the early emergence of faunal elements mostly associated with the later Cretaceous. These taxa represent the earliest stagodontids with crushing premolars (Fumodelphodon) and sectorial premolars (Hoodootherium), morphologically similar to the well-known stagodontids Didelphodon and Eodelphis, respectively. The similar morphologies suggest that these two new genera may be early members of later Cretaceous stagodontid clades, implying a ~ 7 Ma ghost lineage leading to Eodelphis and a ~ 15 Ma ghost lineage to Didelphodon. A reexamination of stagodontid characters suggests a basal placement of Pariadens within Stagodontidae, contrary to some recent studies. The discovery of two new stagodontids bearing lower molars morphologically similar to, but premolars distinct from, Eodelphis highlights the importance of the specialized premolar morphology for resolving the relationships between genera within Stagodontidae.     

Mesozoic rissoid gastropods: History of the study,systematics, and diversity

The history of the study and review of generic and species diversity of Mesozoic rissoid gastropods are provided. The generic composition of Jurassic rissoid gastropods is revised, so that it is proposed to regard them as the family Rissoidae, comprising the genera Bralitzia, Buvignieria, Palaeoceratia, and Palaeorissoina. It is tentatively proposed to assign the genus Hudlestoniella to Rissoidae; this is caused by insufficient morphological knowledge of this genus. The family Palaeorissoidae is regarded as a synonym of Rissoidae. Stratigraphical and geographical distribution of Rissoidae genera is reviewed. From the Jurassic of European Russia, the following species of the genus Buvignieria are described: B. calloviana Gründel, B. imminuera Gründel, B. paucicostata Gründel, B. eichwaldiana (Rouillier), B. choroshovensis Gerasimov, and B. gruendeli sp. nov. The morphological characteristics and stratigraphical distribution of these species are provided. Based on extensive material, the taxonomic significance of particular conchological characters for the establishment of species is discussed.     

New Insects (Insecta: Trichoptera,Reculida, Eoblattida) from the Mesozoic of Asia

New caddisflies, reculid and eoblattid insects from the Mesozoic of Asia are described. Caddisflies of the families Philopotamidae (Mesoviatrix paradoxa gen. et sp. nov. and Kempia piotri gen. et sp. nov.) and Polycentropodidae (Polylongevus eskovi gen. et sp. nov.) from the Upper Jurassic–Lower Cretaceous of the Kempendyai locality in Yakutia are described. A short review and comparison of fossil members in these families are provided. New Gryllones insects, Shurabia tanga sp. nov., Sauk batkenicus gen. et sp. nov. from the Sauk Tan’ga locality (Lower Jurassic of Kyrgyzstan), Say kirgizicus gen. et sp. nov. from the Shurab III locality (Reculida: Geinitziidae; Lower or Middle Jurassic of Kyrgyzstan) Griphopteron iya sp. nov. (Eoblattida: Blattogryllidae) from Iya locality (Middle Jurassic of Russia) are described.     

On Late Jurassic–Early Cretaceous oysters of the genus <Emphasis Type="Italic">Deltoideum</Emphasis> Rollier (Bivalvia,Ostreoidea) from Siberia

Morphology, palaeoecology, and phylogeny of oysters of the genus Deltoideum Rollier from the Upper Jurassic and Lower Cretaceous deposits of Siberia are discussed. The diagnosis and composition of the genus are revised. A new endemic subgenus, Boreiodeltoideum subgen. nov., of the genus Deltoideum is described. This subgenus includes two species, D. (B.) praeanabarensis (Zakharov) and D. (B.) anabarensis (Bodylevsky).     

Comparative Flower and Inflorescence Organogenesis among Genera of Betulaceae: Implications for Phylogenetic Relationships

Betulaceae have simple flowers but complex inflorescences. Recent phylogenetic analyses using molecular data have produced robust phylogenetic trees of Betulaceae. In this study, we evaluated the phylogenetic value of comparative organogenetic data of reproductive organs in the context of molecular phylogenies. Flower and inflorescence developmental processes of 21 species from all six genera in Betulaceae were documented with scanning electron microscopy. In each pistillate cyme, there are one primary bract, two secondary bracts, and two or three flowers in the six genera; only in Alnus are there two tertiary bracts on the abaxial side. The pistillate flower of all genera but Alnus has tepal primordia. Two tepals stop developing early on, resulting in the lack of tepals in mature flowers of Betula; while the tepals are initiated from a common circular primordium at the base of pistil in Corylus, Ostryopsis, Carpinus, and Ostrya, and the developed tepals with irregular shape and unstable number of lobes are adnate to the top of the pistil. In staminate organogenesis, each cyme has one primary bract and three flowers in all genera; two secondary bracts are only present in Alnus, Betula, and Corylus. Staminate flowers have no tepals except in Alnus and Betula, and exhibit high variation in number of stamens among genera. The number of secondary and tertiary bracts in each pistillate and staminate cyme, as well as the presence of tepals in pistillate and staminate flowers was clarified in all genera. Micro-morphological characters were used to infer the phylogenetic relationships of genera and sections of Betulaceae. Our analyses support the division of two subfamilies: Betuloideae (Alnus and Betula) and Coryloideae (Corylus, Carpinus, Ostrya, and Ostryopsis), and three tribes: Betuleae (Alnus and Betula), Coryleae (Corylus), and Carpineae (Carpinus, Ostrya, and Ostryopsis). The results agree with those from molecular phylogenetic studies, and suggest that micro-morphological characters are phylogenetically informative in Betulaceae, and reproductive organs of Betulaceae have evolved in the direction of reduction in bracts and tepals.     

Two new species of poecilostomatoid copepods symbiotic on the venomous echinoid <Emphasis Type="Italic">Toxopneustes pileolus</Emphasis> (Lamarck) (Echinodermata) from Vietnam

Two new coexisting species of crustacean copepods (Poecilostomatoida) belonging to the echinoid-specific genera Mecomerinx Humes, 1977 (Pseudanthessiidae) and Clavisodalis Humes, 1970 (Taeniacanthidae) found associated with the venomous flower urchin Toxopneustes pileolus (Lamarck) (Echinodermata: Echinoidea: Toxopneustidae) in the South China Sea (Vietnam) are described. The diagnostic features of Mecomerinx ohtsukai n. sp. are: (i) three setae and one aesthetasc on the first segment of antennules; (ii) relatively long caudal ramus; (iii) elongated terminal segment of the antenna; and (iv) two claws on the terminal segment of antenna slightly unequal in length. The taeniacanthid copepod Clavisodalis toxopneusti n. sp. is distinguished from all seven known congeners by having two-segmented endopod of the legs 2–4 and four setae on the distal endopodal segment of the leg 1. This is the first report on copepods associated with echinoids of the genus Toxopneustes Agassiz and the first finding of Mecomerinx as well as taeniacanthid copepods in the South China Sea associated with echinoids.     

New Angarosphecidae (Insecta: Hymenoptera: Apoidea) from the Lower Cretaceous of Northeastern China

Two new species of the family Angarosphecidae, Angarosphex saxosus sp. nov. and Vitimosphex vividus sp. nov., from the Lower Cretaceous Yixian Formation of northeastern China are described and illustrated. Generic diagnoses are revised. The genera Palaeapis Hong, 1984, Mataeosphex: Zhang, 1985, and Calobaissodes Zhang, 1992 are synonymized under Angarosphex Rasnitsyn, 1975, and new combinations Angarosphex beiboziensis (Hong, 1984), comb. nov., Angarosphex venulosus (Zhang, 1985), comb. nov., and Angarosphex strigosus Zhang, 1992, comb. nov. are proposed. The genus Vitimosphex Rasnitsyn, 1975 is found reaching northeastern China in its distribution. New morphological data are presented to complete characteristics of the genera concerned.     

A revision of <Emphasis Type="Italic">Sphaeria pilosa</Emphasis> Pers. and re-evaluation of the Trichosphaeriales

Sphaeria pilosa, the basionym of the type of Trichosphaeria, T. pilosa, was insufficiently described by Persoon. The current interpretation of T. pilosa comes from Fuckel and is based on his own material published in the exsiccatal series Fungi Rhen. Exs. no. 946. The examination of the type and other authentic material of S. pilosa and T. pilosa revealed several different fungi. Fresh material of T. pilosa is not available and Fuckel’s historical specimens have never been sampled for DNA. In order to reconcile Persoon’s concept of S. pilosa with Fuckel’s concept of T. pilosa, we designate a neotype in our study. The species is a unitunicate ascomycete characterized by perithecial ascomata, persistent paraphyses, and cylindrical short-stipitate asci without visible apical annulus containing eight hyaline, ellipsoidal ascospores. The genus Trichosphaeria includes 87 described species and the Trichosphaeriales with the single family Trichosphaeriaceae recently accommodate 17 genera of apparently diverse phylogenetic affinity. Although the relationship of Trichosphaeria with other members of the Sordariomycetes is unknown, the family and order based on it are widely used to label incertae sedis clades inferred in phylogenetic analyses. Based on these findings, the Trichosphaeriales are re-evaluated and their use in phylogenetic studies is recommended to be abandoned until recognition of T. pilosa by molecular data.     

Two new lineages of aquatic ascomycetes: <Emphasis Type="Italic">Atractospora</Emphasis> gen. nov. and <Emphasis Type="Italic">Rubellisphaeria</Emphasis> gen. et sp. nov., and a sexual morph of <Emphasis Type="Italic">Myrmecridium montsegurinum</Emphasis> sp. nov.

Two new genera, Atractospora and Rubellisphaeria, are described for perithecial ascomycetes occurring on decaying wood submerged in freshwater habitats. Their relationships with other morphologically similar fungi were investigated utilising four nuclear ribosomal and protein-coding loci. They are nested together with members of five orders and families and numerous genera incertae sedis in the Sordariomycetidae in a clade supported by Maximum Likelihood and Bayesian inference methods. Their closest relative is Lentomitella. Atractospora includes species characterised by dark, immersed to semi-immersed beaked ascomata lying horizontally to the host, stipitate asci with a pronounced non-amyloid apical annulus and hyaline, fusiform, septate, thick-walled ascospores with smooth or ornamented wall. Three novel species are introduced (A. decumbens, A. reticulata and A. verruculosa). A new combination for Aquaticola ellipsoidea is proposed in Atractospora based on molecular data and morphological characters. Rubellisphaeria, with a new species R. abscondita, is distinct by subhyaline to reddish brown, immersed ascomata with a lateral neck, short-stipitate asci and ellipsoidal smooth ascospores with a delayed formation of a middle septum. The sexual morph of the dematiaceous hyphomycete genus Myrmecridium was encountered for the first time on decaying wood submerged in a stream. It is nested in a strongly supported monophyletic clade of the Myrmecridiales. The novel species M. montsegurinum is described; it possesses papillate ascomata immersed beneath a clypeus with subhyaline to weakly pigmented ascomatal wall, long-stipitate asci with a non-amyloid apical annulus and three-septate, hyaline, ellipsoidal, delicately verruculose ascospores. A morphology-based key is provided to facilitate identification of species of Atractospora.     

Fossil Mesozoic and Cenozoic weevils (Coleoptera,Obrienioidea, Curculionoidea)

All known extinct species of Mesozoic and Cenozoic weevils are listed. Ten species of Obrienioidea and 895 Curculionoidea species are recognized, including 88 Nemonychidae, 43 Anthribidae, 44 Ithyceridae, 65 Scolytidae, 12 Belidae, 67 Brentidae, 508 Curcuionidae, 45 Rhynchitidae, six Attelabidae, and 16 Platypodidae. The Triassic beds have yielded six fossil species; Jurassic, 64; Jurassic–Cretaceous boundary, 2; Cretaceous, 105; Paleogene, 510; Neogene, 190; and Pleistocene–Holocene, 22 (5 are synonyms). A new subfamily, Montsecbelinae Legalov, subfam. nov. (with the type genus Montsecbelus Zherikhin et Gratshev, 1997); the new tribes Cretochoragini Legalov, trib. nov. (with the type genus Cretochoragus Soriano et al., 2006), Montsecanomalini Legalov, trib. nov. (with the type genus Montsecanomalus Soriano et al., 2006), Montsecbelini Legalov, trib. nov. (with the type genus Montsecbelus Zherikhin et Gratshev, 1997), Gratshevibelini Legalov, trib. nov. (with the type genus Gratshevibelus Soriano, 2009), Davidibelini Legalov, trib. nov. (with the type genus Davidibelus Zherikhin et Gratshev, 2004); the new genera Allandroides Legalov, gen. nov. (with the type species Allandroides vossi Legalov, sp. nov.), Baissabrenthorhinus Legalov, gen. nov. (with the type species Baissabrenthorhinus mirabilis Legalov, sp. nov.), Ithyceroides Legalov, gen. nov. (with the type species Ithyceroides klondikensis Legalov, sp. nov.), Furhylobius Legalov, gen. nov. (with the type species Furhylobius troesteri Legalov, sp. nov.), Electrauletes Legalov, gen. nov. (with the type species Electrauletes unicus Legalov, sp. nov.); new species Allandroides vossi Legalov, sp. nov. (Baltic amber), Glaesotropis gusakovi Legalov, sp. nov. (Baltic amber), G. succiniferus Legalov, sp. nov. (Baltic amber), G. alleni Legalov, sp. nov. (Baltic amber), G. gratshevi Legalov, sp. nov. (Baltic amber), Baissabrenthorhinus mirabilis Legalov, sp. nov. (Baissa locality), Ithyceroides klondikensis Legalov, sp. nov. (Republic Graben locality), Melanapion poinari Legalov, sp. nov. (Baltic amber), M. gusakovi Legalov, sp. nov. (Baltic amber), Furhylobius troesteri Legalov, sp. nov. (Mors locality), Baltocar convexus Legalov, sp. nov. (Baltic amber), and Electrauletes unicus Legalov, sp. nov. (Baltic amber) are newly described.     

<Emphasis Type="Italic">Perturbatacrusta</Emphasis><Emphasis Type="Italic">leini</Emphasis> n. gen., n. sp. a new microencruster incertae sedis (? sponge) from Late Jurassic to earliest Cretaceous platform margin carbonates of the Northern Calcareous Alps of Austria

A new microencruster of unknown systematic position is described as Perturbatacrusta leini n. gen., n. sp. from the Late Jurassic Plassen Carbonate Platform of the Northern Calcareous Alps and its resediments (p.p. Barmstein Limestone). The labyrinthic interior canal system and marginal openings reveal a possible sponge origin. Differences and affinities to allied taxa such as Radiomura cautica Senowbari-Daryan and Schäfer are discussed. The biostratigraphic range of Perturbatacrusta leini n. gen., n. sp. known so far is Kimmeridgian to Tithonian (?Early Berriasian) so far reported from Austria, Bulgaria, Romania, and Greece. Perturbatacrusta leini was detected in boundstones with a diverse association of microencrusters and mainly encrusting sponges occurring together with microbial crusts. Together with the other encrusting organisms and reef builders, Perturbatacrusta leini played an important role for the carbonate production and stabilization of the reefal and slope carbonates in the Late Jurassic to earliest Cretaceous of the western Neotethys realm.     

Molecular phylogeny,morphology and pathogenicity of <Emphasis Type="Italic">Pseudopestalotiopsis</Emphasis> species on <Emphasis Type="Italic">Ixora</Emphasis> in Taiwan

Pestalotiopsis-like species are phytopathogenic, causing numerous diseases on different hosts, and are widely distributed in tropical and temperate ecosystems. These taxa were recently segregated into several genera and species having brown to dark brown or olivaceous median cells, with or without knobbed apical appendages, were classified under the new genus Pseudopestalotiopsis. Pseudopestalotiopsis species are well known for their capability to produce novel medicinal compounds that may have medicinal, agricultural and industrial applications. Ixora is among the largest genera in the family Rubiaceae and is cultivated throughout Taiwan, as a garden plant. During a survey of fungal diseases associated with Ixora species in Taiwan, several Pestalotiopsis-like species causing leaf spot were isolated. Based on morphology coupled with single- and multi-gene (ITS, TUB, TEF) phylogenies, these taxa belong to two novel species of Pseudopestalotiopsis and are introduced herein as Ps. ixorae and Ps. taiwanensis. These two new taxa fit well with Pseudopestalotiopsis in having dark concolourous median cells with knobbed apical appendages, but differ from the known species in the size of conidiomata, size of the conidia, the number of apical appendages, the length of basal appendages plus ecology and distribution. Pathogenicity testing showed that Ps. ixorae and Ps. taiwanensis are capable of causing leaf disease on Ixora and to the best of our knowledge, this is the first record of Pseudopestalotiopsis species associated with leaf spots of Ixora in Taiwan.     

New Ichneumonids (Hymenoptera: Ichneumonidae) from the Lower Cretaceous Khasurty Locality

A new species of Ichneumonidae, Amplicella minor sp. nov., is described from the Lower Cretaceous of Transbaikalia (Khasurty locality). The diagnosis of Amplicella mininae Kopylov, 2011 is amended. Ichneumonids from Khasurty are only represented by two genera, Amplicella and Khasurtella, both belonging to the subfamily Tanychorinae. This assemblage seems to be the most basal ichneumonid assemblage ever known.