广西南垌早石炭世巴平组下段牙形刺新材料

本文系统研究了广西南垌早石炭世巴平组下段丰富的牙形刺,识别出Siphonodella duplicata,S.cooperi,S.obosoleta,S.quadruplicata,S.lobata,S.crenulata,S.sandbergi,S.eurylobata,S.isosticha,Gnathodus delicatus等重要的带化石。首次报道和描述了产自Siphonodella crenulata带下部牙形刺新材料,其中确立一新种:Siphonodella nandongensis sp.nov.Li;一新未定种:Siphonodellasp.nov.A;且修订了Siphonodella trirostrata Druce(1969)的含义。依据上述牙形刺:Siphonodella nandongensis sp.nov.Li;Siphonodellasp.nov.A和Siphonodella trirostrata Druce(1969)发育特征,认为Siphonodella nandongensis sp.nov.Li与Siphonodella sexplicata;Siphonodella sp.nov.A与Siphonodella quadruplicata(Branson et Mehl);Siphonodella trirostrata Druce(1969)与Siphonodella sandbergi Klapper演化关系密切,并确定所描述的化石新材料的层位是Siphonodella crenulata带下部,地质时代为早石炭世早期,为进一步精细地层划分提供了翔实资料。     

Nomenclatural changes in the tribe Empoascini of the subfamily Typhlocybinae (Hemiptera,Cicadellidae)

One genus and species are synonymized in the tribe Empoascini of the subfamily Typhlocybinae. Bhatasca Dworakowska, 1995is a junior synonym of Alebrasca Hayashi & Okada, 1994, Bhatasca rectangulata Qin & Zhang, 2011is a junior synonym of Alebrasca actinidiae Hayashi & Okada, 1994. Furthermore, Bhatasca expansa is (necessarily) transferred to the genus Alebrasca.     

New data on the systematics of leaf-beetle genus Chrysolina (Coleoptera, Chrysomelinae) from the Palaearctic region

Chrysolina przewalskii (Jacobson, 1895) and Ch. lucidula Chen, 1934 are redescribed based on the type specimens. Neotype of Ch. przewalskii is designated. Ch. daccordii Lopatin, 2000 is a new junior synonym of Ch. juldusana (Lopatin, 1962); Ch. daosana Lopatin, 2007 is a new junior synonym of Ch. tani Lopatin, 1998; Ch. burchana Lopatin, 1998 is a new junior synonym of Ch. przewalskii (Jacobson, 1895). Ch. lucidula Chen, 1934 described from a mislabeled specimen is a new junior synonym of the South European Ch. lucida (Olivier, 1807). Ch. hyrcana var. cyanescens (Jacobson, 1894) is synonymized with Ch. circumducta (Ménétriés, 1848) and is merely a color form of the latter species.     

The heteromorph ammonite genus Ammonitoceras Dumas, 1876 (Ancyloceratidae) in the lower Aptian (Lower Cretaceous) of the Les Ferres Aptian Basin (southeastern France)

Ammonitoceras Dumas, 1876 is a genus of heteromorph ammonites characterized by the presence of a peculiar ontogenetic stage in its inner whorls: the Ammonitoceras stage. But in spite of its wide paleogeographic and biostratigraphic extension throughout the Aptian (Lower Cretaceous), this genus remains poorly known. In the present work we study specimens of Ammonitoceras from the lower Aptian Deshayesites multicostatus (Deshayesites deshayesi Zone) to Dufrenoyia furcata (Dufrenoyia furcata Zone) subzones of the Les Ferres Aptian Basin (southeastern France). The results are as follows: (1) representatives of Ammonitoceras from this area are regarded dimorphic with criocone macroconchs and ancylocone microconchs, (2) their ontogenetic sequence is described, (3) their intraspecific variability is significant and concerns the adult size and the duration of the ontogenetic stages, especially the Ammonitoceras stage, (4) two species are recognized: the earlier Ammonitoceras ucetiae Dumas, 1876, characterized by a brief Ammonitoceras stage on average, and the latter Ammonitoceras lahuseni (Sinzow, 1906), characterized by a longer Ammonitoceras stage on average. The sample of the Deshayesites grandis Subzone (Deshayesites deshayesi Zone) is composed of specimens too fragmentary to be identified at species level.     

Updated hypothesis on the evolution of oligotrichid ciliates (Ciliophora, Spirotricha, Oligotrichida) based on somatic ciliary patterns and ontogenetic data

The two recently established genera ApostrombidiumXu et al., 2009 and VaristrombidiumXu et al., 2009 and the analysis of ontogenetic data in Strombidium constrictum, S. montagnesi, S. wilberti, Omegastrombidium elegans, and Paratontonia gracillima necessitated a revision of the hypothesis about the somatic ciliary pattern evolution in oligotrichid ciliates. As a consequence, the species-rich genus Strombidium was split, establishing two genera for species with a horizontal girdle kinety posterior to the oral primordium: Opisthostrombidium nov. gen. with the extrusome attachment sites along the anterior margin of the girdle kinety and posterior to the oral primordium and Foissneridium nov. gen. with the extrusome attachment sites distinctly apart from the girdle kinety and anterior to the oral primordium. The ontogenetic data revealed that the Ω-shaped girdle kinety pattern evolved convergently from the Pseudotontonia pattern with its horizontal girdle kinety in the tailed genus Paratontonia and from the Novistrombidium pattern with its dextrally spiralled girdle kinety in the tailless genus Omegastrombidium. The somatic ciliary pattern of the latter genus probably gave rise to the patterns of Apostrombidium and Varistrombidium.     

Systematics and evolution of the genus Clathrobaculus Cossmann, 1912 (Gastropoda, Mathildidae)

The morphology and ontogeny of Jurassic gastropods those have been included in the genera Clathrobaculus Cossmann, 1912 and Gordenella Gründel, 1990 are discussed. Based on the ontogenetic research of their shells, several types of ontogeny are established in the species of these genera. The suggestion is made that the genus Gordenella should be considered as a junior synonym of Clathrobaculus within the family Mathildidae. The protoconchs of Clathrobaculus species are studied to reveal their morphological variability and a number of distinguishing characters in which they differ from the protoconchs of other mathildid genera. Four species of Clathrobaculus, of which two are new (C. medidilatatus and C. inconstantiplicatus), are described from the Jurassic deposits of the European part of Russia. The composition of C. fahrenkohli (Rouillier, 1846) and C. krantzi (Rouillier, 1849) is emended, and the protoconchs of these species and of the species C. inconstantiplicatus are described for the first time.     

Validity of <Emphasis Type="Italic">Scorpaena jacksoniensis</Emphasis> and a redescription of <Emphasis Type="Italic">S. cardinalis</Emphasis>, a senior synonym of <Emphasis Type="Italic">S. cookii</Emphasis> (Scorpaeniformes: Scorpaenidae)

The Scorpaena cardinalis complex, including S. cardinalis, S. jacksoniensis and S. orgila, is defined. The genus Ruboralga (type species: S. jacksoniensis) is regarded as a junior synonym of Scorpaena. Scorpaena jacksoniensis Steindachner 1866, previously treated as a junior synonym of Scorpaena cardinalis Solander and Richardson 1842, is regarded here as a valid species. Scorpaena cookii Günther 1874, previously treated as a valid species, is regarded here as a junior synonym of S. cardinalis. Thus, recent recognition of the two Australasian scorpionfishes, i.e., S. cardinalis and S. cookii, are re-identified in this study as S. jacksoniensis and S. cardinalis, respectively. Scorpaena plebeia Solander 1842 is regarded as a junior synonym of S. cardinalis. Scorpaena jacksoniensis is distributed along the east coast of Australia from southern Queensland to eastern Victoria, whereas S. cardinalis occurs around northern New Zealand, the Kermadec Islands and offshore islands of the Tasman Sea. A neotype is designated for S. cardinalis. Morphological changes with growth in the two species are described in detail.     

A review of Semigenetta (Viverridae,Carnivora) from the Miocene of Eurasia based on material from the hominid locality of Hammerschmiede (Germany)

The present article offers a detailed review of the taxonomy, distribution and palaeoecology of the genus Semigenetta. The study is based on new craniodental and postcranial remains of the genus from the early late Miocene (Tortonian) locality of Hammerschmiede (Bavaria, Germany). Most of the new specimens are attributed to the medium-sized species Semigenetta sansaniensis, whereas one lower carnassial is assigned to the large-sized Semigenetta grandis, making Hammerschmiede 4 the first known locality with two species of the genus. The variability of the material of S. sansaniensis from Europe allows us to revise the taxonomic weight of some previously used characters, and to identify the smaller-sized late Miocene form Semigenetta ripolli as a junior synonym of the former. Such an evolutionary transition of S. sansaniensis towards smaller forms is explained by niche partitioning with larger carnivorans of similar ecology, such as the herein reported S. grandis. Additionally, the species Semigenetta huaiheensis is here considered as a junior synonym of Semigenetta elegans.     

Late Middle to Late Frasnian Atrypida, Pentamerida, and Terebratulida (Brachiopoda) from the Namur-Dinant Basin (Belgium)

In the Namur-Dinant Basin (Belgium), the last Atrypida and Pentamerida originate from the top of the Upper Palmatolepis rhenana Zone (Late Frasnian). Within this biozone, their representatives belong to the genera Costatrypa, Desquamatia (Desquamatia), Radiatrypa, Spinatrypa (Spinatrypa), Spinatrypina (Spinatrypina?), Spinatrypina (Exatrypa), Waiotrypa, Iowatrypa and Metabolipa. No representative of these orders occurs within the Palmatolepis linguiformis Zone. The disappearance of the last pentamerids, mostly confined to reefal ecosystems, is clearly related to the end of the edification of the carbonate mounds; it precedes shortly the atrypid one. This event, resulting from a transgressive episode, which induces a progressive and dramatic deterioration of the oxygenation conditions, takes place firstly in the most distal zones of the Namur-Dinant Basin (southern border of the Dinant Synclinorium; Lower P. rhenana Zone). It is only recorded within the Upper P. rhenana Zone in the Philippeville Anticlinorium, the Vesdre area, and the northern flank of the Dinant Synclinorium. It would seem that the terebratulids were absent during the Famennian in this basin, probably due to inappropriate facies. Among the 13 species described or briefly discussed (Palmatolepis hassi to Upper P. rhenana zones), Pseudoatrypa godefroidi nov. sp. and Spinatrypina (Exatrypa) marmoris nov. sp. are proposed as new.     

A review of the threadfin breams of the genusNemipterus (Nemipteridae) from Japan and Taiwan,with description of a new species

Species of the fish genusNemipterus (Nemipteridae) from Japan and Taiwan are reviewed. A key, diagnoses and synonymies are provided for 9 species, including a new species:N. aurora sp. nov. (previously misidentified asN. delagoae Smith);N. bathybius Snyder;N. furcosus (Valenciennes) [mistakenly referred to asN. peronii (Valenciennes)];N. hexodon (Quoy et Gaimard);N. japonicus (Bloch);N. peronii (Valenciennes) [previously referred to asN. tolu (Valenciennes), a junior synonym];N. thosaporni Russell [previously misidentified asN. marginatus (Valenciennes)];N. virgatus (Houttuyn); andN. zysron (Bleeker) [previously referred to asN. metopias (Bleeker), a junior synonym].N. aurora is described from specimens from Taiwan, the Gulf of Thailand, East Malaysia and Indonesia. It appears to be closely allied toN. bipunctatus (Ehrenberg) (N. delagoae is a junior synonym), an Indian Ocean species, but the two species are readily distinguished on the basis of colour pattern of the dorsal and anal fins:N. aurora has a broad orange-yellow submedial stripe along the dorsal fin, and a lemon submedial stripe on the anal fin; whereas inN. bipunctatus the dorsal fin is uniformly rosy, and the anal fin has 2–4 wavy yellow stripes.     

Dujardinascaris mormyropsis n. sp. (Nematoda: Anisakidae) from the osteoglossiform fish Mormyrops anguilloides (Linnaeus) (Mormyridae) in Central Africa

A new nematode species, Dujardinascaris mormyropsis n. sp. (Anisakidae), is described from specimens found in the stomach and intestine of the cornish jack Mormyrops anguilloides (Linnaeus) (Osteoglossiformes; Mormyridae) in the Sangha River (Congo River basin) in Dzanga-Sangha Protected Areas, Central African Republic. Based on light and scanning electron microscopical examination, the new species differs from the only other congeneric species parasitising fishes in Africa, D. malapteruri (Baylis, 1923), mainly in the presence of dentigerous ridges on lips, absence of lateral caudal alae in the cloacal region, in the anteriorly curved, non-bifid distal tip of the gubernaculum and larger eggs (60–90 × 52–78 vs 45 × 30 μm); males of D. mormyropsis are characterised by the presence of a ventral precloacal cuticular ornamentation not observed in other Dujardinascaris spp. Dujardinascaris mormyropsis and D. malapteruri also differ in the order of their fish hosts (Osteoglossiformes vs Siluriformes). Specimens previously reported as Dujardinascaris graberi Troncy, 1969, a junior synonym of D. malapteruri, from Mormyrops engystoma Boulenger in Chad belong to the new species D. mormyropsis.     

<Emphasis Type="Italic">Goniatites sphaericus</Emphasis> (Sowerby, 1814), the archetype of Palaeozoic ammonoids: a case of decreasing phenotypic variation through ontogeny

The Late Viséan (Early Carboniferous) ammonoid species Goniatites sphaericus (Sowerby, 1814) is revised with the use of the type material. With respect to conch morphology, suture line and particularly shell ornament, it is regarded as a senior synonym of the species Goniatites fimbriatus (Foord and Crick, 1897) and must therefore be re-established as an important index fossil for the ammonoid stratigraphy of the Rhenohercynian and Subvariscan shelves. The Goniatites fimbriatus Zone has been re-named Goniatites sphaericus Zone on this basis. The study of ontogenetic changes in the conch parameters shows that intraspecific variation occurs within a wide range. In the whorl profile, variation is very high in small juveniles, while in the coiling rate, intermediate growth stages are more strongly affected.     

Neoaplectana Steiner, 1929 a junior synonym of Steinernema Travassos, 1927 (Nematoda; Rhabditida)

Summary A type specimen of Steinernema kraussei and a population of this nematode from the type host were compared with three species of Neoaplectana. No characters were found to separate the two genera and so Neoplectana Steiner, 1929 is considered to be a junior synonym of Steinernema Travassos, 1927. Valid species now included within the genus Steinernema are: S. kraussei (Steiner, 1923) Travassos, 1927 (type species); S. glaseri (Steiner, 1929) n.comb.; S. feltiae (Filipjev, 1934) n.comb. and S. bibionis (Bovien, 1937) n.comb. A key is given to these four species and their junior synonyms are listed.     

Identity of the lectotype of the East Asian flatfish Pleuronichthys cornutus (Temminck and Schlegel 1846) and reinstatement of Pleuronichthys lighti Wu 1929

The taxonomy of two species of Pleuronichthys from East Asia was re-examined on the basis of scale characteristics. The lectotype of Pleuronichthys cornutus (Temminck and Schlegel 1846) was shown to be conspecific with Pleuronichthys japonicus Suzuki, Kawashima and Nakabo 2009, being characterized by oval scales, a greater exposed scale area and lower scale counts than a second species, formerly recognized as P. cornutus, but to which Pleuronichthys lighti Wu 1929, formerly considered a junior synonym of P. cornutus, should now be applied. Accordingly, P. japonicus is now considered a junior synonym of P. cornutus.     

The taxonomic status of Western Pacific mysid species of Neomysis awatschensis (Brandt, 1851) group

The discussion of the taxonomic status of West Pacific mysid species Neomysis awatschensis (Brandt, 1851), N. intermedia (Czerniavsky, 1882) and N. nigra Nakazawa, 1910 has continued over the last century. Examination of a large taxonomic collection of the Zoological Institute of the Russian Academy of Sciences, including syntypes of N. awatschensis and N. intermedia, revealed that N. intermedia is a junior synonym of N. awatschensis and N. nigra is a valid species, not a synonym of N. awatschensis. N. nigra was first recorded in Russian waters in the Possyet Bay (Sea of Japan).     

A new Devonian species of the enigmatic Carboniferous conodont Dollymae

Arrow-shaped P₁ elements of Dollymae are characteristic for the Tournaisian conodont faunas worldwide but the phylogeny of this conodont remains obscure and its origin is cryptic. Dollymae peregrina n. sp., from the upper Famennian (upper expansa Zone) strata in the Holy Cross Mountains (central Poland), is the oldest representative of the Dollymae lineage. The morphology of the new species’ P₁ element shows primitive features in comparison to other members of this genus and is transitional in the number of element processes. Thus D. peregrina n. sp. is most probably ancestral to the remaining species. The genus appears to be monophyletic, probably rooted in Pelekysgnathus within the Icriodontidae.     

Ammonite biostratigraphy of the uppermost Hauterivian in the Betic Cordillera (SE Spain)

A detailed analysis of the stratigraphic distribution of ammonites from fourteen sections in the External Zones of the Betic Cordillera has enabled us to identify accurately the sequence of bioevents that take place throughout the uppermost Hauterivian and to propose a more precise biostratigraphic scheme for this interval. Thus, we have divided the two currently admitted zones (the Crioceratites balearis Zone and the Pseudothurmannia angulicostata auct. Zone) into several subzones. Four subzones can be recognised within the Cr. balearis Zone. The base of each subzone is defined by the first occurrence of one of four successive species belonging to the same Crioceratites lineage. These species are: Cr. balearis, Cr. binelli, Cr. krenkeli and Cr. angulicostatus. The Ps. ohmi Zone (which replaces the classical Ps. angulicostata Zone) can be divided into three subzones characterised by three successive species of the genus Pseudothurmannia: Ps. ohmi, Ps mortilleti (here considered as a senior synonym of Ps. catulloi) and Ps. picteti. According to the current definition, the first occurrence of Taveraidiscus hugii (OOSTER) marks the lower boundary of the Barremian stage. This event fits into a major faunal-renewal episode that begins in the upper part of the Ps. picteti Subzone.     

A brief history and revision of the systematics of the cladid crinoid Sinocrinus

The erisocrinid Sinocrinus differs from other erisocrinid genera (Erisocrinus and Exaetocrinus) by possessing a rounded, bowl-shaped cup, bearing tumid cup plates with impressed sutures. Sinocrinus Tien, 1926 is refined using Principal Component Analysis and neighborhood cluster analysis. The genotype of Sinocrinus, S. microgranulosus Tien, 1926, is a junior subjective synonym of S. granulatus (Wanner, 1924). Sinocrinus [Erisocrinus] stefaninii (Yakovlev, 1934) is a junior synonym of Sinocrinus lichengensis Tien, 1926 and S. asymmetricus Strimple and Watkins, 1969 is the junior synonym of S. sheareri Strimple and Watkins, 1969. Other valid species include: S. [Erisocrinus] cernuus (Trautschold, 1867); S. [Erisocrinus] obliquus (Wanner, 1916); S. houkouensis Tien, 1926; S. nodosus Tien, 1926; S. [Erisocrinus] stefaninii (Yakovlev, 1934). Because of its refined inclusiveness, the temporal span of the genus now extends from the Late Carboniferous (Moscovian) through the early Permian (Sakmarion). This study also widens the current geographic range of Sinocrinus, with specimens collected across a wider span of Eurasia.     

Uppermost Devonian–Lower Carboniferous conodonts from the Indert Formation in the Shine Jinst area,South Mongolia

In southwestern Mongolia, conodonts from the Indert Formation at its type locality in Shine Jinst were investigated to improve regional and global correlation of the uppermost Devonian–lowermost Carboniferous. The abundance and diversity of the conodont fauna is quite low in general, whereas representatives of Siphonodella, Protognathodus, Pseudopolygnathus, Polygnathus and Bispathodus have been collected from the Indert-Uul section. Five conodont biointervals, from the Bi. costatus-Pr. kockeli Interregnum (ckI) to the Siphonodella sandbergi Zone, could be recognized from the top Heermorit Member and the lower part of the Shombon Member, while the middle and upper parts of the Shombon Member cannot be zoned based on the conodonts. Absence of index fossils Si. sulcata, Pr. kuehni and Pr. kockeli hampered precise recognition of the Devonian–Carboniferous boundary (DCB) at Indert-Uul, but this transition is well delineated by typical uppermost Famennian and Tournaisian conodont assemblages. The DCB is tentatively placed at the base of the Shombon Member, consistent with the lithological boundary and the resuming of carbonate production during the DCB transitional interval.