Lower Cambrian tubular micro-to macrofossils from the Paseky Shale of the Barrandian area (Czech Republic)

The carbonaceous megafossil (mega-alga)Marpolia spissa Walcott 1919 is described from the Early Cambrian of the Barrandian area for the first time. Macroscopic remains of colonies ofM. spissa are compared with tubular microfossils of the same rocks. Different areas in colonies ofM. spissa are assignable to several (part-based) genera and species of microfossils. Therefore, the microfossil taxaSiphonophycus robustum (Schopf 1968)Knoll et al. 1991,S. typicum (Hermann 1974)Butterfield 1994,S. kestron Schopf 1968,S. capitaneum Nyberg &Schopf 1984,Polytrichoides lineatus Hermann 1974, emend.Knoll et al. 1991,Tortunema angusta (Kolosov 1984)Butterfield 1994 andTortunema wernadskii (Schepeleva 1960)Butterfield 1994 should only be used as form-species in the sense of an artificial taxonomy. The palaeoenvironment of the Paseky Shale and the biological assignment ofMarpolia spissa are discussed.     

Chemical composition,protein digestibility and heat of combustion of filamentous green algae

The filamentous green algae investigated (Hormidium sp. strainHindák 1963/21,Ulothrix sp. strainHindák 1964/2,Uronema gigas Visch. strainVischer/Bloom. 174,Uronema sp. strainHindák 1963/25 andStigeoclonium sp. strainHindák 1964/1), contain similar amounts of proteins, lipids, cellulose and ash as the hitherto used production strains of the generaChlorella andScenedesmus. The digestibility of proteins in vitro is about one-third higher in the filamentous algae than in the employed referenceScenedesmus quadricauda strainGreifswald/15, used in Czechoslovakia as a model production strain. The heats of combustion of the filamentous algae are relatively lower (5519–5923 cal/g dry weight) than in the reference strain (6145 cal/g dry weight). From the point of view of application of filamentous green algae to mass cultivation their advantages over the presently employed chlorococcal algae (Chlorella, Scenedesmus) consist in a pronouncedly greater digestibility of their proteins without special technological treatment of the material obtained and a greater production of biomass.     

A revision of the genusOlpitrichum Atk

A revision of the genusOlpitrichum Atk. was undertaken, revealing three species:O. macrosporum (Farlow exSacc.)Sumstine,O. patulum (Sacc etBerl.)Hol.-Jech. andO. tenellum (Berk. etCurt)Hol.-Jech.O. macrosporum andO. tenellum occur on decayed cotton bolls,O. patulum on dead rotten wood and bark. Aspergilliform phialosporous state has been found inO. macrosporum andO. patulum.     

Foraminifera from the Silberberg Formation («Lower Oligocene») at Silberberg,near Helmstedt (Germany)

From the Silberberg Quarry, type locality of the Silberberg Formation (Martini &Ritzkowski 1968), some planktonic foraminifera are described:Globigerina officinalis Subbotina, Globigerina ouachitaensisHowe &Wallace,G. praebulloides leroyi Blow &Banner, G.praebulloides occlusa Blow &Banner which taxa are here suggested to form intergrading morphotypes within the range of variation of a population dominated byG. officinalis. In addition,G. cf.danvillensis Howe &Wallace is found. The planktonic fauna, together with some elements in the benthonic fauna, suggests a possible correlation with the Danville Landing Member of the Jackson Formation, Louisiana, traditionally ascribed to the Upper Eocene. There is some similarity with European Uppermost Eocene — Lower Oligocene faunas described by various authors. The Silberberg Formation was suggested to be a Neostratotype for the Latdorfian Stage of the Lower Oligocene byMartini &Ritzkowski (1968). It is suggested that the Silberberg Formation may well be coeval with the Upper Priabonian as proposed byCita 1969.     

Notes on some African hepatic genera 6–9

The present study deals with African species ofSyzygiella Spruce,Allisoniella Hodgs. andGymnomitriaceae Klinggr. Three species ofSyzygiella Spruce,S. geminifolia (Mitt.) Steph.,S. concreta (Gott.) Spruce and one indeterminable species with orbicular leaves (known only in sterile condition) occur in Africa.Allisoniella nigra (Rodw.) Schust. represents a genus hitherto unreported for the African flora. The present knowledge ofGymnomitriaceae Klinggr. in subsaharan Africa is summarised; five species ofMarsupella Dum., one ofGymnomitrion Corda and five ofHerzogobryum Grolle are reported. Finally, some additions to the generaIsotachis Mitt.,Anastrophyllum (Spruce) Steph. andLophozia (Dum.) Dum. are presented.     

The trilobiteProtostygina and the composition of the Styginidae, with two new genera

The Styginidae is regarded as an exclusively Ordovician family of trilobites, separate from the Scutelluidae. The hitherto poorly known genusProtostygina Prantl &P?ibyl, 1949 is revised. It is recorded with certainty only from the Llanvirn of the Czech Republic, and the type species is a senior synonym of“Raymondaspis” rubensi rubensi P?ibyl &VANěK, 1968 and“R.” rubensi lybar ?najdr, 1976. Two new styginid genera are proposed:Cyrtocybe, with type species“Raymondaspis” turgida Whittington, 1965, is known from the upper Arenig and lower Llanvirn of Newfoundland, Maine and Norway; andPromargo, with type speciesP.forteyi n. sp., occurs in the Arenig of Newfoundland and Spitsbergen.Turgicephalus Fortey, 1980 is regarded as a junior synonym ofRaymondaspis P?ibyl inPrantl &P?ibyl, 1949. Three genera are excluded from the Styginidae:Kirkdomina Tripp, 1962,Pseudostygina Zhou inZhou et al., 1982 andStyginella P?ibyl &Vaněk, 1971.     

Taxonomic and biochronological significance of specimens of the Triassic dicynodontDinodontosaurus Romer 1943 in the Tübingen collection

Two species of the dicynodontDinodontosaurus from the Middle Triassic interval of the Santa Maria Formation in Rio Grande do Sul, southern Brazil,D. tener (von Huene 1935) andD. turpior (von Huene 1935), are based on undiagnostic lectotypes and thus arenomina dubia. The oldest valid, available name for a species ofDinodontosaurus isD. oliveirai Romer 1943, the type species of the genus. (The unused senior subjective synonymDiodontosaurus pedroanum Caldas, 1936 has been suppressed by the International Commission on Zoological Nomenclature).Chanaria platyceps Cox 1968 andDinodontosaurus brevirostris Cox 1968 are junior subjective synonyms ofD. oliveirai Romer 1943.Dinodontosaurus thus is a monospecific genus known from the Santa Maria Formation and the Ischichuca (= Chañares) Formation of northwestern Argentina. This dicynodont and associated tetrapods characterize the Chanarian land-vertebrate faunachron, which is of Middle Triassic age, probably Ladinian.     

New internally structured decapod microcoprolites from Germany (Late Triassic/Early Miocene), Southern Spain (Early/Middle Jurassic) and Portugal (Late Jurassic): Taxonomy, palaeoecology and evolutionary implications

Fossil faecal pellets with internal structures are described from non-marine environments for the first time. In the Late Triassic Lehrberg Beds (Middle Keuper, Carnian) of Germany, the oldest stratigraphic record of the form genusHelicerina Brönnimann &Masse,Helicerina keuperina Seegis n. sp., occurs.Favreina kalankyra Ebli from the Norian Hauptdolomit Formation is also attributed to this genus. Another new speciesof Helicerina, H. ruttei Schweigert n. sp., is described from the Early Miocene calcareous freshwater tufas of Southern Germany. It is attributed to the brachyuran freshwater crabProballaya quenstedti (Zittel) which occurs abundantly at the same locality. Hence, the coprolite genusHelicerina is the product of brachyuran decapods or their Triassic ancestors, and not of anomuran decapods as thought before. From younger Early to Middle Jurassic pelagic ferrugineous limestones of the Subbetic area (Southern Spain), the new speciesFavreina belandoi Fels n. sp. is described besidesHelicerina siciliana Senowbari-Daryan, Schäfer &Catalano, and the better known speciesPalaxius salataensis Brönnimann, Cros &Zaninetti. The number of canals withinFavreina belandoi varies but is clearly correlated with different ontogenetic stages of the same producer. From the Late Jurassic of Portugal, the new speciesPetalina hexalunulata Leinfelder n. gen. n. sp. is reported. It co-occurs withFavreina prusensis (Paréjas). The new genusPetalina is distinct fromFavreina by its hemispherical cross sections of the canals. In Portugal, both species are restricted to intrajurassic marine karstic fissures of the reefal Ota Limestone.     

Phytosociological nomenclature and typification of names of heathland syntaxa from W Europe (classCalluno-Ulicetea)

The correct names, author citations and nomenclatural types of the syntaxa names are established for the principal ranks above the association. These syntaxa areUlicion minoris Malcuit 1929,Ericion umbellatae Br.-Bl., P. Silva, Rozeira etFontes 1952,Genisto-Vaccinion Br.-Bl. 1926,Ulicetalia minoris Quantin 1935 andCalluno-Ulicetea Br.-Bl. etR. Tx. 1943     

LignicolousHyphomycetes from Czechoslovakia 8.Endophragmiella andPhragmocephala

Thirteen species and one variety ofEndophragmiella Sutton and three species ofPhragmocephala Mason etHughes collected by the author in Czechoslovakia, and occasionally in other regions of Europe are described and illustrated. Four new species and one new variety are described inEndophragmiella—E. aseptata Hol.-Jech.,E. fatrensis Holt.-Jech.,E. ramificata Hol.-Jech.,E. similis Hol.-Jech. andE. uniseptata (Ellis) Hughes var.pusilla Hol.-Jech..     

Evolutionsmodelle für den Ursprung der Echinodermen: Zusammenfassung und Kritik

The origin of echinoderms is one of the most crucial questions within the evolutionary history of deuterostomes. An ancestral position was suggested byGarstang, Romer andNichols. They also assumed that hemichordates and chordates are sistergroups. In all other hypotheses the echinoderms took a more derived position.Gislén, Jefferies andHolland viewed the hemichordates as basal to the deuterostomes and postulated that echinoderms and chordates are sistergroups. According toJollie, Peterson et al. andMooi &; David echinoderms and hemichordates are sistergroups.Gudo andGutmann adopted the view ofMetschnikoff who combined the hemichordates and echinoderms in the Ambulacraria; they supposed that echinoderms were derived from pterobranchs. This variety of views is linked with different approaches to phylogenetic reconstruction utilized by each of the authors.Garstang, Romer, Jefferies andGislén compared morphological features, in the case ofGislén andJefferies with some attention to fossil evidence, whereasJollie, Holland andGislén also considerd embryological aspects.Mooi &;David as well asPeterson et al. used modern embryological (epigenetical) approaches.Nichols combined functional morphology and comparative anatomy. Evolutionary scenarios were reconstructed only by a few authors.Holland associated the development of echinoderms from pterobranch-like ancestors with repeated changes in feeding modes.Nichols envisioned that echinoderms had evolved from sipunculids that gained protection from predators through skeletal armor. In our own investigations based on constructional morphology echinoderms are interpreted as highly derived chordates.     

Redescription of the largest trigonotarbid arachnid —Kreischeria wiedei Geinitz 1882 from the Upper Carboniferous of Zwickau, Germany

Kreischeria wiedei Geinitz 1882 (Arachnida: Trigonotarbida) from the Upper Carboniferous (Westphalian D) of Zwickau, Germany is redescribed. The family KreischeriidaeHaase 1890 is reinstated and rediagnosed to accomodate this species. We provisionally refer the speciesAnzinia thevenini (Pruvost 1919),Gondwanarachne argentinensis Pinto &Hünicken 1980,Hemikreischeria geinitzi (Thévenin 1902),Pseudokreischeria pococki Gill 1924 andPseudokreischeria varia Petrunkevitch 1949 to Kreischeriidae too.     

Polyploidy and variation in theCampanula rotundifolia complex. Part II. (Taxonomic) I. Revision of the groupsSaxicolae,Lanceolatae andAlpicolae in Czechoslovakia and adjacent regions

A survey is given of three natural groups of the subsectionHeterophylla (Witas.)Fed. of the genusCampanula L. Within theSaxicolae four taxa of higher rank have been revealed:c. xylocarpa Kovanda (2n=34),C. gentilis Kovanda (2n=34),C. moravica (Spitzner)Kovanda subsp.moravica (2n=68), andC. moravica subsp.xylorrhiza (O. Schwarz)Kovanda (2n=102). BothAlpicolae andLanceolatae are represented by a single species: the first byC. cochleariifolia Lam. (2n=34), the latter byC. serrata (Kit. ap.Schult.)Hendrych (2n=34). Cytology, ecology and geographical distribution of all these taxa have been reviewed, and relationships to the other members of the complex discussed. Infraspecific variation within each species has also been examined.     

Petrodavisia,a new genus inCentaureinae (Asteraceae)

A new monotypic genus based onPtosimopappus bracteatus Boiss. =Centaurea ptosimopappa Hayek is described. The history of its classification and relationships toCheirolophus Cass. andMicrolophus Cass. are discussed.     

New and critical species ofVicia in Iran and neighbouring countries 1. TheVicia variegata group

In Iran and the neighbouring regions of Turkey, Iraq, U.S.S.R. and Afghanistan, eight already known species belonging to the subsectionVariegatae Radzhi, occur:V. persica Boiss.,V. armena Boiss.,V. variegata Willd.,V. akhmaganica Kazar.,V. gregaria Boiss. etHeldr.,V. aucheri Jaub. etSpach and the two new species described here,V. rechingeri Chrtková-?ertová andV. afghanica Chrtková-?ertová. The occurrence of most species is restricted to a limited area which may be one of the evolutionary centres of this subsection.     

Hybridization studies inSilene subgen.Petrocoptis (Caryophyllaceae)

Silene subgenusPetrocoptis comprises sexual diploid taxa and it is restricted to calcareous cliffs in the Iberian peninsula. Artificial crosses involvingSilene pyrenaica (Bergeret)Mayol etRosselló (≡Petrocoptis pyrenaica (Bergeret)Walp.),Silene laxipruinosa Mayol etRosselló andS. montserratii subsp.crassifolia (Rouy)Mayol etRosselló (≡P. crassifolia Rouy) were attempted to assess the extent of barriers developed within the subgenusPetrocoptis. Usually, intraspecific crosses involving allopatric populations were successful, suggesting that geographically isolated populations are not genetically isolated. Cross-compatibility was noted among the polymorphicS. pyrenaica, which developed fertile F₁ hybrids. All other interspecific crosses failed due to cross- or seed-incompatibility. Crossing results agree with available evidence supporting the merging of segregates ofS. pyrenaica within a single taxon.     

Notes on some African hepatic genera 1–5

The present study deals with five genera of hepatics in Africa, Isotachis Mitt., Anastrophyllum (Spruce) Steph., Tritomaria Schiffn. ex Loeske, Gymnocoleopsis (Schust.) Schust. and Lophozia (Dum.) Dum. All African populations of the genus Isotachis Mitt. are considered to be one species, I. aubertii (Schwaegr.) Mitt. Four species of Anastrophyllum (Spruce) Steph. (s.l.), A. auritum (Lehm.) Steph., A. piligerum (Nees) Spruce, A. subcomplicatum (Lehm. et Lindenb.) Steph. and A. minutum (Schreb.) Schust., and two species of Tritomaria Schiffn. et Loeske, T. camerunensis S. Arnell and T. exsecta (Schrad.) Schiffn. ex Loeske occur in Africa. Gymmocoleopsis multiflora (Steph.) Schust. represents a genus and species hitherto unreported for the African flora. Finally, five Lophozia (Dum.) Dum. species, L. argentina (Steph.) Schust., L. capensis S. Arnell, L. decolorans (Limpr.) Steph., L. hedbergii S. Arnell and L. tristaniana (S. Arnell) Váňa, are reported from central and southern Africa; two of these (L. argentina (Steph.) Schust. and L. decolorans (Limpr.) Steph.) represent the first reports from Africa.     

Two new setae-lessPhellinus species with large coloured spores (Fungi,Hymenochaetaceae)

Two new species ofPhellinus rimosus complex are described, viz.Phellinus coffeatoporus Kotl. etPouz. from Florida (U.S.A.) characterized by globose spores andPhellinus resinaceus Kotl. etPouz. from Papua-New Guinea and Australia which is distinguished by a very thick and faintly yellowish tinted spore wall.