Middle Permian Ostracods from Tak Fa Limestone, Phetchabun Province, Central Thailand

This paper presents the first Permian ostracod fauna discovered in Thailand. The ostracods are recovered from the Tak Fa Limestone (Middle Permian) in Phetchabun province, central Thailand. The ostracods belong to eight genera and 15 species. Four species are newly described: Sargentina phetchabunensis nov. sp., Geffenina bungsamphanensis nov. sp., Reviya subsompongensis nov. sp. and Bairdia takfaensis nov. sp. The ostracod assemblages characterize a shallow marine, near shore environment at the time of deposition. Except for one species, which shows palaeobiogeographical links between Central Thailand and South China, all the other species are endemic.     

Taxonomy, biostratigraphy and paleoecology of Cenomanian and Turonian ostracodes from the Western Interior Basin, Southwest Utah, USA

Cenomanian-Turonian ostracodes are reported from the western Colorado Plateau (Western Interior Basin) in the United States. Fifteen genera and twenty species are illustrated, six of which are new: Cytheromorphaperornata nov. sp., Looneyellaleckiei nov. sp., Asciocythereposterangulata nov. sp., Asciocytherearizonensis nov. sp., Cytheropteronclavifragilis nov. sp. and Hourcqiadakotaensis nov. sp. Three ostracode interval zones are proposed that broadly correspond to the existing late Cenomanian through to Middle Turonian Ammonite-zones of Kauffman et al. (1993). Paleoenvironments range from estuarine to coastal plain.     

On the Cyprideis species flock (Crustacea, Ostracoda) in Lake Tanganyika, with the description of four new species

Four new species, belonging to three genera, of ostracods from Lake Tanganyika are described: Mesocyprideis nitida sp.nov., Romecytheridea belone sp.nov., R. plegma sp. nov. and Cyprideis loricata sp. nov. The Cyprideis species flock of Lake Tanganyika now consists of 17 formally described species (16 endemic) in 6 genera (4 endemic). The geographical and ecological distribution of the four species is briefly discussed and some supplementary remarks on the radiation of the Cyprideis species flock in Lake Tanganyika are offered.     

Cyprididae (Ostracoda) du Miocène supérieur du Bassin de Turiec (Slovaquie) : Taxonomie et Paléoécologie

Twelve species of the family Cyprididae were found in the Upper Miocene of the Turiec Basin, of which three are new - Herpetocypris denticulata nov. sp., H. pusilla nov. sp. et Psychrodromus janzi nov. sp. The occurrence of Mediocypris suggests that ostracods occupied the Turiec Basin since the Middle Miocene. The psychrophilic genera (Psychrodromus and Cavernocypris) provide evidence of cold springs around the lake. In the sediments studied, the Cyprididae are associated with other ostracods that characterise shallow aquatic habitats and a diverse community of both aquatic and terrestrial plants. The sexual paleo-populations of Heterocypris salina (Brady, 1868), Herpetocypris pusilla nov. sp. and Psychrodromus janzi nov. sp. are observed.     

Late Cretaceous Arman Flora of the Magadan District: Composition, age, and new plant species

The Arman Flora comes from volcanic-sedimentary deposits of the Arman Formation in the Arman River basin and from volcanic and volcanic-sedimentary rocks of the Nel??kandzha-Khasyn Interfluve. It comprises about 80 fossil plant species. The Arman Flora is dated as Turonian and Coniacian because of its similarity to the reliably dated Penzhina and Kaivayam floras of the northwestern Kamchatka Peninsula and Tylpegyrgynai Flora of the Pekul??nei Ridge. This is corroborated by isotopic (U-Pb and ⁴⁰Ar/³⁹Ar) age determination for the plant-bearing layers. New conifer and angiosperm species of the Arman Flora are described: Pagiophyllum parvum sp. nov., Araliaephyllum armanensis sp. nov., Terechovia philippovae sp. nov., and Parvileguminophyllum samylinae sp. nov.     

Miocene ostracods from the Tremiti Islands and Hyblean Plateau: biostratigraphy and description of new and poorly known species

The main taxonomic and stratigraphical results of a study of ostracods from the middle-late Miocene of the Tremiti Islands and the Hyblean Plateau are presented. The faunas are mostly typical of deep thermospheric or psychrospheric bathyal environments. Excluding a few, mostly juvenile shallow water contaminants, a total of 127 species were recorded. Twenty-four taxa are discussed herein; of these, 13 species (Cytherella dissimilis nov. sp., Cytherella parvula nov. sp., Cytherella subtilis nov. sp., Argilloecia triangularis nov. sp., Retibythere (Retibythere)? claudii nov. sp., Retibythere (Retibythere)? gibba nov. sp., Cytheropteron (Cytheropteron) joachinoi nov. sp., Cytheropteron (Aversovalva) consuetum nov. sp., Cytheropteron (Aversovalva) trimerumense nov. sp., Cytheropteron (Aversovalva) turgidum nov. sp., Loxoconcha julianii nov. sp., Buntonia whatleyi nov. sp., Pterygocythere nuda nov. sp.) and a subspecies (Costa tricostata dorsoarcuata nov. subsp.) are described as new, while six are left in open nomenclature. The stratigraphical distribution of ostracods is expressed in terms of planktonic foraminiferal zones. Information obtained from this study enriches biostratigraphical data on Mediterranean Miocene deep-sea ostracods, especially with respect to the Langhian.     

Ostracodes de la Formation de Bhanness,Kimméridgien (Jurassique supérieur) du Liban central : taxonomie,paléoécologie et paléobiogéographie

A microfauna composed of 11 species of ostracodes belonging to 11 genera have been recovered from the Bhanness Formation of Kimmeridgian age, in Central Lebanon. Four species are new and are described herein: Ektyphocythere dahressawanensis nov. sp., Dicrorygma (Orthorygma) libanensis nov. sp., Citrella? elongata nov. sp. and Procytherura inflata nov. sp. From a palaeobiogeographical standpoint, this fauna characterizes the North Gondwana province which differs from the South Gondwana province, particularly by the presence of the genus Schuleridea and the absence of the genus Majungaella.     

Diversity and paleoenvironmental significance of Middle Triassic ostracods (Crustacea) from northern Thailand: Pha Kan Formation (Anisian,Lampang Group)

The Pha Kan Formation that crops out at the Phra That Muang Kham section, south of Lampang city, was measured and sampled for ostracod analysis. We here report the occurrence of 29 species distributed among 14 genera. Four new species are described: Triassocypris phakanella Forel nov. sp., Leviella lampangensis Forel nov. sp., Bektasia yawella Forel nov. sp. and Hungarella poli Chitnarin nov. sp. The present data represent the first detailed report of Middle Triassic (Anisian) ostracods from the Sukhothai terrane and the first insight into diversity dynamics following the end-Permian extinction in this area. The ostracod assemblages of the Phra That Muang Kham section are discussed and document an important shift from siliciclastic to carbonate conditions, from a protected to an open marine environment, followed by a slight regressive trend up-section associated with repeated salinity fluctuations. This fauna illustrates the post-crisis recovery during the Middle Triassic and some hypothesis are issued on the distribution pathways of several taxa.     

Tremadoc (earliest Ordovician) brachiopods from Purmamarca and the Sierra de Mojotoro, Cordillera Oriental of northwestern Argentina

The Late Tremadoc storm-dominated shoreface to inner platform deposits exposed west of the Purmamarca village (Coquena Formation) contain a considerably more diverse brachiopod fauna than previously reported. Coquinite horizons from the lower heterolitic succession have yielded monospecific associations of Nanorthis purmamarcaensis nov. sp. (formerly assigned to N. christianiae KJERULF), which is also reported from the Late Tremadoc rocks of the Cerro San Bernardo area. The fine-grained Upper Member of the Coquena Formation contains a more diverse fauna composed by Nanorthis brachymyaria nov. sp., Astraborthis quebradensis nov. sp. and the new plectorthid genus Lipanorthis (type species L. andinus nov. sp.). A different species of Lipanorthis (L. santalaurae nov. sp.) from the Mid Tremadoc Floresta Formation of the Sierra de Mojotoro is also described.     

Nouvelles données sur les macro-invertébrés du Turonien de la région de Libreville (bassin côtier nord-gabonais)

Thirteen species of macroinvertabrates have been identified for the first time from the Turonian deposits of the Libreville region. Seven ones correspond to bivalves: Lima (Plagiostoma) subsimplex Thomas and Péron, 1890, ?Osteomya sp., Plicatula ferryi Coquand, 1862, P. fourneli Coquand, 1862, P. ventilabrum var. suffetulensis Pervinquière, 1912, Plicatula sp., Pleuromya sp.; three other ones are echinoid species: Mecaster batnensis (Coquand, 1862), Mecaster nicaisei (Coquand, 1862), Mecaster sp.; and the last three are gastropods: Cylichna sp. ? Pterocerella poinsettiformis Stephenson, 1941, Columbellina sp. Excepted Plicatula ferryi Coquand and P. ventilabrum var. suffetulensis Pervinquière which are identified in the Senonian of Gabon, all species are found for the first time in Gabonese coastal basin. Their paleobiogeographic distribution is extended to Gabon. In Gabonese coastal basin, the stratigraphic and geographic ranges of the Plicatula genus are extended in Turonian and Libreville region respectively. The macrofaunal assemblage found in the Libreville region is cosmopolitan. Its shows paleogeographical affinities with Tethys and south of South Atlantic.     

Three new species ofPenicillium isolated from soil

Three new species ofPenicillium Linkex Gray nom. cons. prop. are described and illustrated. These species have been recovered from samples of sandy soil under pine trees. They differ from all species of theGenus described so far and are, therefore, considered and proposed as new taxa:Penicillium rubefaciens sp. nov.,Penicillium vaccaeorum sp. nov. andPenicillium michaelis sp. nov.     

New click beetles (Coleoptera: Elateridae) from the cretaceous of Russia and Kazakhstan

A new tribe, two new genera, and seven new species of click beetles are described: Pollostelaterini, trib. nov., Pollostelater baissensis, gen. et sp. nov. from the Lower Cretaceous of Transbaikalia (Baisa locality), five new species in the genus Cryptocoelus Dolin et Nel C. sinitshenkovae, sp. nov. (Romanovka locality), C. shcherbakovi, sp. nov., C. baissensis, sp. nov., C. lukashevichae, sp. nov., C. dolini, sp. nov. (all from Baisa locality), and Turonelater giganteus, gen. et sp. nov. from the Turonian of Southern Kazakhstan (Kzyl-Dzhar locality).     

Contribution a l'étude des ostracodes du crétacé supérieur de Dordogne

Sixteen species of ostracods are described from upper Cenomanien, Turonian and Campanian of Dordogne (region of Saint-Cyprien). Thirteen of them are new and belong to genera Cytherella, Dolocythere, Hazelina?, Cythereis, Platycythereis, Quasihermanites, Kikliocythere, Netrocytheridea, Annosacythere, Neocythere (Physocythere), Amphicytherura. The three others belong to the genera Platella?, Paracypris and Hemicytherura? are left in open nomenclature.     

A NEW PALAEOCTOPUS (CEPHALOPODA: COLEOIDEA) FROM THE LATE CRETACEOUS OF VALLECILLO,NORTH‐EASTERN MEXICO,AND IMPLICATIONS FOR THE EVOLUTION OF OCTOPODA

Abstract: Palaeoctopus pelagicus sp. nov. is described from the early Turonian Vallecillo Limestone in north‐eastern Mexico. The species represents the first record of a fossil octopod from the Americas and the second species of the genus Palaeoctopus. The holotype and only known specimen preserves one half of an originally bipartite gladius vestige. Soft parts are not preserved. The gladius vestige is distinguished from P. newboldi from the Santonian Limestone of Lebanon by the arrangement of fields, striation and reinforcements. The new material supports previous ideas suggesting that the paired stylets of modern Octopoda evolved through gradual reduction of a Teudopsis‐like gladius via a transitional stage similar to Palaeoctopus. The origin of Octopoda and Cirroctopoda likely dates back to a period between the Toarcian (180 Ma) and the early Turonian (93 Ma). Palaeoecological conditions in the Vallecillo ocean suggest that P. pelagicus sp. nov. inhabited the pelagic shelf. Hostile low oxygen conditions on the sea floor exclude a benthic mode of life for P. pelagicus sp. nov.     

Intraspecific variation in Triassic Ophthalmidiid Foraminifera from Timor

Four ophthalmidiid species are described as free specimens extracted from mudstones and wackestones of Triassic age: Atsabella bandeiraensis nov. gen. nov. sp., Karaburunia atsabensis nov. sp., Ophthalmidium sp. cf. O. primitivum Ho and Spirophthalmidium grunaui nov. sp. Analysis of morphological variation found in large suites of specimens suggests that, as in modern miliolids, apertural characteristics, chamber shape and adult test size are features that vary within narrow limits and may be used to define species. In genera with milioline coiling in the post-embryonic stage, chamber arrangement may be highly variable. Post-embryonic coiling in K. atsabensis varies from quinqueloculine to almost spiroloculine and encompasses morphotypes that, in thin-section studies, have been attributed to a number of other genera. In Timor Leste, A. bandeiraensis, K. atsabensis and S. grunaui have been found with conodonts indicative of the Carnian, but the full local stratigraphic range of these species is uncertain. K. atsabensis occurs at another locality with conodonts suggestive of the Middle Triassic or less likely Carnian. Ophthalmidium sp. cf. O. primitivum has been found at one locality associated with A. bandeiraensis and K. atsabensis in a stratigraphic succession that suggests a correlation to the Carnian or Norian. The ophthalmidiids are found commonly associated with organic-cemented agglutinated and hyaline foraminifera and at some localities common to abundant ostracods and mollusc debris. They were most common in organic-rich carbonate mud of shallow-marine environments.     

On some eurypterids (Eurypterida, Chelicerata) from the Devonian of South Siberia

Fossil eurypterids from the Lake Shunet area (Lower Devonian of the Republic of Khakassia) and the Torgashino locality (Devonian of Krasnoyarsk Region) have been reexamined. New species of eurypterids are described: Stylonuroides orientalis sp. nov., Parahughmilleria longa sp. nov., and Nanahughmilleria notosibirica sp. nov.     

Aspects of permian palaeobotany and palynology,VII. the majonicaceae,a new family of late permian conifers

On the basis of rich vegetative and fertile material from the Val Gardena Formation in the Dolomites and the Vicentinian Alps, coniferous remains have been studied in detail with the aid of cuticle analysis. Except the genus Ortiseia Florin, three other natural genera can be distinguished: Majonica nov. gen, Dolomitia nov. gen. and Pseudovoltzia Florin. Within both Majonica and Dolomitia a single species is recognized, Majonica alpina nov. sp. and Dolomitia cittertiae nov. sp., respectively. Within Pseudovoltzia two species can be recognized: P. liebeana (Geinitz) Florin and P. sjerpii nov. sp.The genera Majonica, Dolomitia and Pseudovoltzia are associated with ovuliferous fructifications and Majonica even with polliniferous cones and bisaccoid bitaeniate pollen grains.A new family—the Majonicaceae—is proposed to include the genera Majonica, Dolomitia and Pseudovoltzia. The family is characterized by a peculiar organization of the ovuliferous dwarf-shoots, i.e. the places of ovule-attachment on the lateral fertile scales varying from explicitly laterally situated to more or less shifted to the adaxial side of the dwarf-shoot.     

Palynology of the Dockum group (Upper Triassic), Texas,U.S.A.

A palynofloral assemblage is described from the Upper Triassic Dockum Group of Texas. Forty palynomorph species are recorded and these are correlated with European Upper Triassic assemblages. The Dockum Group assemblage is considered to be of late Karnian age.Two new genera, Tulesporites gen. nov., type species T. briscoensis sp. nov., and Daughertyspora gen. nov., type species D. chinleanus (Daugherty) comb. nov. have been erected; new species are Converrucosisporites matsenii sp. nov., Pyramidosporites traversei sp. nov., Callialasporites triassicus sp. nov., Plicatipollenites minutotriletus sp. nov., Triadispora dockumensis sp. nov., Bhardwajispora jansonii sp. nov., Protodiploxypinus americus sp. nov., P. ujhelyi sp. nov., Klausipollenites gouldii sp. nov., Pityosporites old-hamensis sp. nov., Abietineaepollenites bujakii sp. nov., Falcisporites oviformis sp. nov. and F. tecovasensis sp. nov.