New Famennian bryozoans (Upper Devonian) from Azerbaijan and Armenia

New bryozoans are described from the Famennian of Southern Transcaucasia: Petalotrypa myunkhbalaensis sp. nov. and Eridotrypella danzikensis sp. nov. (order Trepostomata) and Rectifenestella kadrluiensis sp. nov. and R. famenniensis sp. nov. (order Fenestrata). The paleobiogeographic relations that existed between Nakhichevan (Azerbaijan) and Armenia and other regions of Eurasia and the United States at the end of the Devonian are investigated.     

Predatory boreholes in Tournaisian (Lower Carboniferous) spiriferid brachiopods

A brachiopod fauna from the uppermost part of the Tournaisian Tournai Formation (Belgium) contains an undetermined species of Crurithyris (Spiriferida, Ambocoeliidae), which displays numerous bored shells. About 8% of the 432 specimens with conjoined valves display single, small (≤ 1 mm) boreholes, which are smooth-sided, cylindrical or weakly conical, circular to slightly elliptical in plan view, perpendicular to the shell surface and generally complete. Of the 35 bored articulated specimens, 27 were drilled on the ventral valve. Most of the boreholes are located in the posterior half of the shell, and no case of edge-drilling has been observed. The boreholes were drilled by a predator, or possibly a parasite, which selected individuals greater than 2.5 mm long. Crurithyris sp. may have represented an attractive (in terms of energy cost) and easy target for a small-sized predator because of its thin shell and ornament of minute spines.     

Two unusual trepostome bryozoans from the Lower Carboniferous of the Karatau (south Kazakhstan)

Two bryozoan species from the Lower Carboniferous of south Kazakhstan are described. Both species are placed in the genusNipponostenopora Sakagami 1960. InNipponostenopora karatauensis n. sp., colonies have a pseudobifoliate form resembling true bifoliate colonies but lacking a mesotheca. Peculiarities of the internal structure of this species and ofN. bifoliata (Nikiforova) are discussed.     

Stenolaemate bryozoans from the Geirud Formation (Upper Devonian/Lower Carboniferous) of Central Alborz (Iran)

Two bryozoan species are described from the Geirud Formation (Upper Devonian/Lower Carboniferous) of Central Alborz (Iran). Trepostome Schulgina mutabilis Troizkaya, 1975 is known from the Upper Devonian (Famennian) of Central Kazakhstan. The new species Ascopora geirudensis n. sp. is the earliest known representative of the rhabdomesine genus Ascopora Trautschold, 1876.     

New Devonian and Carboniferous bryozoans of the Holy Cross Mountains (central Poland)

New bryozoans from the Middle-Upper Devonian (Eifelian-Frasnian) and the Lower Carboniferous (Tournaisian) of the Holy Cross Mountains in central Poland are described: Bigeyella sparsa gen. et sp. nov., B. separata gen. et sp. nov., Eridopora singula sp. nov., Leptotrypa pulchra sp. nov., Kysylschinipora klarae sp. nov., Coelotubulipora rara sp. nov., Alternifenestella genuina sp. nov., Exfenestella polonica sp. nov., and Rectifenestella localis sp. nov. Some paleogeographic and stratigraphic aspects of the Paleozoic deposits of this region are discussed and main bryozoan localities are described.     

New bryozoans from the Devonian of Afghanistan and the Carboniferous of Iran

A new family, Vidronovellidae, with a new genus, Vidronovella, and its type species V. fastigata sp. nov., and a new species, Europora gerirudensis, are described from the Famennian of Afghanistan, and the new species Primorella iranica, Heloclema magnificum, and Worthenopora elbursensis are described from the Viséan of Iran.     

New bryozoans (Bryozoa) from the Upper Devonian (Lower Famennian) of the Kuznetsk Basin

New bryozoans from the Upper Devonian (Famennian) of the borderlands of the Kuznetsk Coal Basin are described: Orthopora tomensis sp. nov. and Minussina incrustata sp. nov.     

Kulm trilobites (Lower Carboniferous) from S-China

Some trilobite remains are described from the Lower Carboniferous/Mississippian (Tournaisian/Viséan boundary) of S-China, representing two species:Liobole (Liobole) devuysti n. sp. andLiobole (Sulcubole) xiangzhouensis n. sp.Liobole is a typical member of the central European Kulm Facies and index fossil for the Erdbachian. For the first time, twoLiobole species are recorded from outside of Europe. They demonstrate that a passage existed between Europe and East Asia across the Palaeotethys through which Kulm trilobites have occupied new geographical regions.      

New data on the genus Chrysotoxum Meigen (Diptera: Syrphidae) from North-East Turkey,Armenia, Azerbaijan and Iran including descriptions of three new species

New data and records of the genus Chrysotoxum Meigen, 1803 are reported, arising from taxonomic and faunistic examination of adult specimens collected from 1920 to 2011 from four northeastern provinces of Turkey (Erzurum, Bayburt, Kars, and Artvin), and from the neighboring countries of Armenia, Azerbaijan and Iran. Three new species are described: Chrysotoxum antennalis Vuji?, Nedeljkovi? &; Hayat sp. n., C. clausseni Vuji?, Nedeljkovi? &; Hayat sp. n. and C. persicum Vuji?, Nedeljkovi? &; Hayat sp. n. The first two are known only from northeastern Turkey, and the third also occurs in Armenia, Azerbaijan and Iran. These new species have in common an antenna with the basoflagellomere being shorter than the scape and pedicel together.

http://www.zoobank.org/urn:lsid:zoobank.org:pub:4C264678-8E47-4DE0-AC7D-91DABC597BCD     

New data on the phylogeny of Choristitidae (Carboniferous brachiopods)

A new species and genus of Choristitinae, Adventochoristites abavus gen. et sp. nov., is described from the Upper Serpukhovian of the Donets Basin and is considered as an ancestor of the Middle-Late Carboniferous Choristites linage. The characteristic features differing Alphachoristites from Choristites and Trautscholdia are specified. New species Alphachoristites berestovensis sp. nov. and Quizhouspirifer tshaikensis sp. nov. are established.     

New bryozoans from the Devonian of Gorny Altai (Russia)

New bryozoans Saffordotaxis altaicus sp. nov. from the Givetian Stage (Middle Devonian) and Cyphotrypa olgae sp. nov. and Crustopora aliena sp. nov. from the Famennian Stage (Upper Devonian) are described from the Devonian of Gorny Altai.     

Revision of some spiriferide and spiriferinide brachiopods from the historical type area of the Tournaisian stage (Carboniferous,southern Belgium)

Spiriferides, and to a lesser extent the spiriferinides, rank among the major elements of the Tournaisian brachiopod fauna from the mixed argillaceous–carbonate succession of the Tournai area (Hainaut sedimentation area, southern Belgium), along with productides (chonetidines and productidines) and athyridides. Based on well-preserved and silicified material from the Tournai Formation (Ivorian), representatives of the families Ambocoeliidae (Crurithyris goldfussiana), Strophopleuridae (Voiseyella roemeriana), Mucrospiriferidae (Tylothyris laminosa), and Cyrtinidae (Cyrtina koninckiana, C. sp. indet.) are described. Cyrtina hibernica is reported for the first time in the Visean of Visé (Visé Formation, Belgium). Biotic interactions between spiriferides and diverse organisms are illustrated, notably the diverse epizoans fixed on brachiopods (e.g., microconchids, cornulitids, crinoid holdfasts), single and multiple drill holes, and regeneration traces after predator attacks.     

New data on osteostracans (Agnatha) from the Lower Devonian of the Severnaya Zemlya Archipelago

The osteostracans Reticulaspis menneri gen. et sp. nov. and Nucleaspis unica gen. et sp. nov. from the Lower Devonian Severnaya Zemlya Formation of October Revolution Island of the Severnaya Zemlya Archipelago are described. The perfect preservation of the exoskeleton structure of Reticulaspis menneri allows the design and growth mode of the exoskeleton, with a continuous reticular dental surface of the cephalothoracic shield to be characterized. Nucleaspis unica is represented by a juvenile stage, which is extremely scarce in this vertebrate group. The preoccupied generic name Ungulaspis Afanassieva et Karatajūt?-Talimaa, 1998 is replaced by Paraungulaspis.     

The genus Laxifenestella (Bryozoa) from the Lower Carboniferous of the East European platform

Twelve species of the genus Fenestella from the Lower Carboniferous of the East European platform are placed in the genus Laxifenestella Morozova, 1974 based on the analysis of its species composition. These species and their stratigraphical range are described in more detail. Two species are shown to be synonymous. The stratigraphical distribution of these species over the horizons of the Viséan and Serpukhovian stages of the East European platform suggests a high degree of endemism of these bryozoans.     

New data on the distribution of the Upper Carboniferous (Pennsylvanian) flexible crinoid Cibolocrinus (Crinoidea,Flexibilia)

Two new species of flexible crinoids of the genus Cibolocrinus (Crinoidea, Flexibilia) from the Upper Carboniferous of the Moscow Region are described: C. kutasovi (Moscovian Stage, Podolskian Regional Substage) and C. gerassimovi (Gzhelian Stage, Dobryatinian Regional Substage). The first species, C. kutasovi, belongs to a group with low cone shaped cups that first appeared in the Moscow Basin and then spread to the Midcontinent of North America. In one specimen of C. gerassimovi the smallest infrabasal plate is situated in the A ray, which is not typical for flexible crinoids. A poorly preserved crown of Cibolocrinus sp. from the Upper Carboniferous (Gzhelian Stage) of the Darvaz Ridge (western Pamir, central Tajikistan) is also described. The described specimens of Cibolocrinus from the Moscow Region and the Darvaz Ridge are the first reliable specimens of this genus described from Europe and Asia.     

Mississippian (Lower Carboniferous) microfossils from the Chios Mélange (Chios Island, Greece)

The Chios Mélange is a thick Paleozoic wildflysch sequence that crops out on the Greek island Chios. It is composed of chert, limestone and volcanic blocks floating in a siliciclastic turbiditic matrix. New data suggest that the youngest blocks within the Chios Mélange are clasts of a breccia from the Kouramia-Nenitouria area that contain conodonts of late Visean or early Serpukovian age. The conodont fauna from the breccias is characterized by the genera Gnathodus and Lochriea, which favored deeper-water, open-marine facies. Elsewhere on the island, in the Papalia-Nagos area, calcareous microfossils of middle to late Visean age have been recovered from lime grainstone beds within the Chios Mélange. Allochems making up the grainstones are interpreted to have been transported into deeper-water turbiditic facies, but there is no evidence of stratigraphic reworking. Age-diagnostic calcareous microfossils include the alga Koninckopora inflata and foraminifers in the genus Paraarchaediscus. In situ Mississippian microfossils indicate that the Chios Mélange is older than Pennsylvanian (Upper Carboniferous) - Permian, as previously thought. The revised age suggests that the origin of the Chios Mélange may be related to the development of an accretionary prism during the Hercynian Orogeny.© 2003 Éditions scientifiques et médicales Elsevier SAS. All rights reserved.     

New observations on the skeletons of the earliest bryozoans from the Fenhsiang Formation (Tremadocian,Lower Ordovician), Yichang,China

The earliest unequivocal bryozoans occurred in the Fenhsiang Formation (upper Tremadocian, Lower Ordovician) of Yichang, South China, providing important clues about the early evolution of primitive bryozoans. In this study, SEM and EDAX were used to analyze the microstructure of the walls of two bryozoan genera, Nekhorosheviella and Orbiramus, from the Fenhsiang Formation. All walls of Nekhorosheviella and endozonal walls of Orbiramus show poor preservation in thin sections, with a granular appearance reflecting extensive neomorphism, whereas exozonal walls of Orbiramus are distinctly laminated. These preservational differences may reflect skeletal chemistry, particularly the magnesium content of the calcite. Phosphatic skeletal linings were found to be distributed unevenly in the autozooecia of Nekhorosheviella, but were absent in Orbiramus.     

New data on eurypterids (Eurypterida,Chelicerata) of the upper Carboniferous of the Donets Basin

Eurypterid finds are described from the Carboniferous (Kasimovian) localities Lomuvatka (Luhansk Region, Ukraine) and Kakichev (Rostov Region, Russia). These eurypterids are supposedly juveniles of Adelophthalmus carbonarius Chernyshev, 1933, the only eurypterid previously described from the Donets Basin.