Actinocamax primus arkhangelsky (belemnitellidae; upper cretaceous) biometry,comparison and biostratigraphy

A sample ofActinocamax primus Arkhangelsky, 1912 from the Lower Middle Cenomanian limestones of the Wunstorf quarry west of Hannover (NW Germany) is studied by univariate and bivariate biometric methods in order to analyse the variation of critical characters.A. primus is closely related toA. plenus (Blainville, 1825) but differs from that species by being smaller and more slender.A. primus appears in the Lower Cenomanian and continues into the Lower Middle Cenomanian. It is mainly distributed in the northern part of the North European Palaeobiogeographic Province.A. plenus is recorded from the Middle Cenomanian-lower Lower Turonian of the Russian Platform, but only from the Middle Upper Cenomanian in NW Europe. It is widespread in the North European Province.The primus event in the Lower Middle Cenomanian and theplenus event in the Middle Upper Cenomanian are briefly discussed.     

Die Wirbeltierfährtenfundstelle Borgholzhausen (Teutoburger Wald, NW-Deutschland) aus der Oolith-Zone (Unterer Muschelkalk, Mitteltrias)

At a new Middle Triassic vertebrate track site, Borgholzhausen sports field in the central Teutoburger Wald (NW Germany), 36 superimposed track horizons were discovered in the Graue Zwischenmittel beds of the Oolith Member (Lower Muschelkalk Formation, Bithynian substage, Middle Triassic). The track-bearings beds consist of micritic laminites with a variety of sediment surface marks. They document extensive tidal flat facies along the northern margin of the Rhenish Massif. The track inventory consists ofRhynchosauroides peabodyi (Faber) andProcolophonichnium haarmuehlensis (Holst, Smit &; Veenstra), as well as scratch marks, drag marks, and an unidentified tetrapod track. TheR. peabodyi ichnofacies is associated with the moist carbonates of intertidal ponds. The tracks in this facies show a variety of preservational types and were left by reptiles such as prolacertilians.P. haarmuehlensis, on the other hand, was produced by small terrestrial reptiles, and theP. haarmuehlensis ichnofacies originated in the partially dry intertidal to supratidal carbonates. Borgholzhausen sports field and other new localities indicate that tracks of both ichnotaxa are widespread in several stratigraphic units of the Lower and Middle Muschelkalk along the northern margin of the Rhenish Massif and represent megatracksites.     

The Upper Cretaceous belemnite <Emphasis Type="Italic">Praeactinocamax plenus</Emphasis> (Blainville, 1827) from Lower Saxony (Upper Cenomanian,northwest Germany) and its distribution pattern in Europe

Occurrences of the Upper Cenomanian (Upper Cretaceous) belemnite Praeactinocamax plenus from the plenus Bed of northwest Germany (Söhlde-Loges working quarry near Salzgitter, Lower Saxony) are documented and described for the first time on the basis of two in situ finds. The find horizon and its surrounding beds are re-evaluated in a sequence stratigraphical context. In contrast to the interpretations of other authors, the plenus Bed is seen as a pelagization event in a parasequence of transgressively stacked beds, delimited by two significant erosion surfaces below and above. The exclusive occurrence of P. plenus in the top part of the plenus Bed and its absence from the post-plenus Bed succession, in the equivalent of which (higher part of the Plenus Marls Member) it is very common in southern England (Anglo-Paris Basin), is explained by ecological factors in stratigraphically complete sections (intra-shelf depressions) and by gaps in the stratigraphic records in swell settings. The distribution pattern of P. plenus suggests a preference for nearshore settings and a demersal mode of life.     

Soft–part preservation in heteromorph ammonites from the Cenomanian–Turonian Boundary Event (OAE 2) in north–west Germany

Abstract: From thinly laminated marlstones of the Hesseltal Formation, representing the Late Cenomanian Oceanic Anoxic Event (OAE) 2, at Lengerich in the Teutoburger Wald (Westfalen, north‐west Germany), 17 sediment‐compacted baculitid ammonites with carbonised and partially phosphatised soft parts are recorded. Some preserve remains of the buccal mass, including jaws (occasionally articulated) and radulae, as well as of the cephalic cartilage, such as eye capsules. Such have not yet been recorded previously for the order Ammonoidea. In addition, originally unmineralised parts found preserved in these specimens include extensive portions of the digestive tract, the siphonal tube, false colour patterns (megastriae), as well as traces of what would appear to be the oviduct. At the same levels, patches with numerous isolated horny upper and rarer lower jaws as well as radulae occur; these may represent regurgitates or faeces of larger predators. The cephalopod remains described were deposited in an epicontinental setting, possibly at palaeodepths between 200 and 600 m. In this particular Late Cretaceous fossil Lagerstätte, upper jaws and anaptychi of ammonites rank among the commonest fossils.     

Ammoniten des Cenomans vom Südrand der westfälischen Kreide zwischen Unna und Möhnesee

Systematically collected ammonites from the different levels of the transgressive Cenomanian of the Haarstrang Mountains between Unna and Möhnesee (southern border of the westfalian Cretaceous, NW Germany) have been investigated. Twenty-one taxa (genera and species), partly previously unknown from this region, have been found and described. The fauna from the immediate transgression level is preserved as phosphoritic internal moulds (steinkerns). Fragmentary preservation and fossil condensation levels indicate reworking processes in these basal Cretaceous deposits. The age of the Cretaceous transgression in the area investigated can be precisely established as Lower Cenomanian (=carcitanensis subzone). The Cenomanian sequence, which is lithofacially very variable, can be, on the basis of the ammonite fauna, subdivided according to the modern Cretaceous stratigraphy for the boreal realm.     

Vegetation on anthropogenic metalliferous soils in the Eastern Alps

A syntaxonomic revision of vegetation of anthropogenic metalliferous habitats (mine spoils of lead, zinc and copper mining) in the Eastern Alps (Austria, Germany, Italy and Slovenia) was made. The communities studied belong to theThlaspietea rotundifolii (Linaria alpina-Cerastium uniflorum comm.,Papaveri kerneri-Thlaspietum kerneri, Violetum dubyanae, Thlaspietum cepaeifolii, Thlaspietum rotundifolii, Scrophulario juratensis-Erysimetum sylvestris, Minuartia gerardii-Silene glareosa comm.,Epipactido atrorubentis-Silenetum glareosae andSileno alpestris-Moehringietum muscosae) and to theAsplenietea trichomanis (Sileno rupestris-Asplenietum). There is neither floristic support nor syntaxonomic justification for the concepts of theGalio anisophylli-Minuartion vernae, theVioletalia calaminariae and theVioletea calaminariae in the Eastern Alps. These units should be included within theThlaspion rotundifolii, Thlaspietalia rotundifolii andThlaspietea rotundifolii, respectively.     

The genusPlatythyris (Brachiopoda) and its relationship to the Pygopidae

Platythyris is included in the Pygopidae because of the resemblance of its internal structures to that family, despite the great difference in external form. The genus occurs in strata of Barremian to Senonian age in Europe north and west of the Alpine line and probably originated in the Caucasian-Crimean region. Three new species are described:P. vendeensis (Cenomanian),P. cristobali (Turonian) andP. viaudi (Senonian).Terebratula squamosa Mantell (Cenomanian) is assigned toPlatythyris and redescribed.Terebratula disparilis D’Orbigny (Cenomanian) is described as a subspeciesP. squamosa disparilis.     

Die Korallenfauna des Korallenooliths (Oxfordium, Oberjura, NW-Deutschland): Zusammensetzung, Stratigraphie und regionale Verbreitung

The stratigraphie and regional distribution of Oxfordian scleractinian reef corals in the Korallenoolith Formation (NW German Malm Group) is described from the Süntel, Deister, Kleiner Deisler and Osterwald Mountains. In the study area four horizons with (par-) autochthonous corals are developed two of which can be traced region-wide (Untere Korallenbank Member andflorigemma-Bank Member / Obere Korallenbank Member). The coral fauna of the biostromes, forming the Untere Korallenbank Member, is impoverished and dominated by ubiquitous r-strategists. In contrast, the reefal bioconstruetions of theflorigemma-Bank Member show a high variability in their regional appearances, partly forming highly diverse coral associations. The highest diversity is developed in the patch reefs from the Obere Korallenbank Member of the Osterwald Mountains (about 40 species). Corals are an important part of the Korallenoolith fauna. Altogether, 20 species belonging to 15 genera have been identified which were formerly unknown from NW German Oxfordian successions.     

Palaeobiogeography of late cretaceous belemnites of Europe

A North Temperate Realm, characterized by Belemnitellidae Pavlov, and a South Temperate Realm, characterized by Dimitobelidae WHITEHOUSE, existed throughout the Late Cretaceous, while Tethyan belemnites belonging to Belemnopseidae Naef existed only in the Cenomanian and disappeared afterwards. The North Temperate Realm may be subdivided into North European and North American Provinces. The latter province includes Greenland, Canada, the Western Interior Region of North America, and the Atlantic and Gulf coasts of North America. The belemnites from the North American Province, consisting of populations of the generaActinocamax Miller andBelemnitella d’Orbigny, are closely related to the belemnites of the North European Province and appear to have migrated from this province to North America via Greenland and Arctic Canada. The North European Province extends from Ireland to the Ural Mountains. Belemnites from this province belong to the following genera:Neohibolites Stolley,Parahibolites Stolley,Belemnocamax Crick,Actinocamax Miller,Belemnellocamax Naidin,Gonioteuthis Bayle,Belemnitella d’Orbigny,Belemnella Nowak, andFusiteuthis Kongiel. Two subprovinces within the North European Province have been recognized: the Central European and Central Russian Subprovinces. These subprovinces are well-defined in the late Coniacian-Early Campanian and are characterized by theGonioteuthis stock andBelemnitella stock, respectively. The two subprovinces are less distinct in other periods of the Late Cretaceous and may disappear completely.     

Cenomanian Cephalopods of Bellezma-Aures mountains,NE Algeria: Taxonomy and biostratigraphy

The Cenomanian Smail Marl Formation in the Bellezma and Aures mountains of northeastern Algeria is well exposed and rich in macroinvertebrates, including cephalopods. Twenty-five ammonite species and two nautiloid species from the Thénièt El Manchar, Djebel Metrassi and Djebel Bouarif sections are described and seven assemblage zones proposed as provisional working units: Mantelliceras mantelli–Sharpeiceras laticlavium Assemblage Zone (lower Cenomanian), Mantelliceras dixoni Assemblage Zone (uppermost lower Cenomanian), Cunningtoniceras inerme Assemblage Zone (lower middle Cenomanian), Acanthoceras rhotomagense and Acanthoceras cf. rhotomagense Assemblage Zone (middle middle Cenomanian), Acanthoceras amphibolum Assemblage Zone (upper middle Cenomanian), Acanthoceras jukesbrownei Assemblage Zone (uppermost middle Cenomanian), and Neolobites vibrayeanus Assemblage Zone (lower upper Cenomanian). The lower Cenomanian Mantelliceras mantelli–Sharpeiceras laticlavium Zone is subdivided into the Submantelliceras aumalense, Sharpeiceras schlueteri and Mantelliceras saxbii subzones. The base of the middle Cenomanian is marked by the disappearance of species of Mantelliceras and the appearance of the scleractinian coral Aspidiscus cristatus (Lamarck, 1801), associated with Cunningtoniceras inerme (Pervinquière, 1907). The middle Cenomanian contains abundant A. cristatus and species of Acanthoceras, i.e., A. cf. rhotomagense (Defrance in Brongniart, 1822), A. jukesbrownei (Spath, 1926) and A. amphibolum Morrow, 1935. An ammonite zonal scheme is then applied to the Cenomanian exposed in the Bellezma-Aures mountains located on the southern Tethys margin in Algeria.     

TheCBP2 gene fromSaccharomyces douglasii is a functional homologue of theSaccharomyces cerevisiae gene and is essential for respiratory growth in the presence of a wild-type (intron-containing) mitochondrial genome

InSaccharomyces cerevisiae the only known role of theCBP2 gene is the excision of the fifth intron of the mitochondrialcyt b gene (bI5). We have cloned theCBP2 gene fromSaccharomyces douglasii (a close relative ofS. cerevisiae). A comparison of theS. douglasii andS. cerevisiae sequences shows that there are 14% nucleotide substitutions in the coding region, with transitions being three times more frequent than transversions. At the protein level sequence identity is 87%. We have demonstrated that theS. douglasii CBP2 gene is essential for respiratory growth in the presence of a wild-typeS. douglasii mitochondrial genome, but not in the presence of an intronlessS. cerevisiae mitochondrial genome. Also theS. douglasii andS. cerevisiae CBP2 genes are completely interchangeable, even though the intron bI5 is absent from theS. douglasii mitochondrial genome.     

The late Cenomanian event in eastern England

The Cenomanian/Turonian boundary event has been fully documented from a series of localities between Flamborough Head in Humberside and Marham in Norfolk. The carbon isotope excursion can be identified and extrapolated to all the studied sections using bed‐by‐bed correlation. Evidence from studies of the isotope data, trace element geochemistry, and the micropalaeontology are presented. The famous “Black Band” is seen to change laterally into a “red” horizon and then a “green” horizon when traced southwards. This appears to represent the “feather‐edge” of the anoxic event when traced towards a palaeo‐high which is located in the region of the Wash. All the events, so‐identified, can be correlated with the A. plenus Marl succession in southern England.     

Cis-trans isomerization of proline in the peptide (his 105-Val 124) of ribonuclease a containing the primary nucleation site

Conformational energy calculations have been carried out to determine the relative stabilities of the C-terminal sequence 105–124 of ribonuclease A, withcis andtrans forms, respectively, of Asn 113-Pro 114. Thecis form of Pro 114 is the one that occurs in the native protein. This peptide contains the sequence 106–118, which, on the basis of both theoretical and experimental studies, is thought to constitute the primary nucleation site for the folding of ribonuclease A. It is shown that both conformations of the isolated peptide (with Pro 114 in thecis andtrans forms, respectively) are of approximately equal stability. Both forms have similar conformations from residues 105–110 and 118–124, while they differ in the bend region involving residues 111–117. Calculations have also been carried out to deduce the possible low-energy paths for the interconversion between thecis andtrans forms of both Pro 114 and Pro 117. It is shown that there are two low-energy paths (with a minimum activation energy of 16.5 kcal/mole) for the interconversion of Pro 114. Attractive nonbonded interaction energies stabilize the transition state on these paths. Only one relatively low-energy path (with an activation energy of 18 kcal/mole) could be found for the isomerization of Pro 117, which occur in thetrans form in the native protein; in this case, allcis forms have significantly higher energy than thetrans form. These calculations thus show that native-like forms for the isolated peptide can exist with Pro 114 in either thecis or thetrans form and that these forms are readily interconvertible.     

Paleobotanical evidence on the early radiation of nonmagnoliid dicotyledons

Paleobotanical studies indicate that several isolated and systematically depauperate groups of extant woody dicotyledons originated in the Mid Cretaceous. TheChloranthaceae had probably differentiated into insect-pollinated (Chloranthus andSarcandra) and wind-pollinated (Ascarina andHedyosmum) forms by the end of the Albian, and leaves referable to theTrochodendrales are known from the Albian and Cenomanian. In the latest Cretaceous and Early Tertiary, extinct representatives of theTrochodendrales includedNordenskioldia and theJoffrea-Nyssidium complex. ThePlatanaceae also differentiated before the end of the Albian and initially had insect-pollinated, unisexual flowers with five carpels or stamens. Some of these features persisted in the platanoid lineage until the Early Tertiary, and during the Paleocene and Eocene thePlatanaceae included forms with elliptical, palmate and pinnate foliage. The history of thePlatanaceae suggests that several features of the reproductive morphology of extant taxa may have arisen in association with a trend toward wind pollination. In the Mid Cretaceous, platanoid foliage partially intergrades with pinnateSapindopsis and pedateDebeya-Dewalquea leaves suggesting a close relationship betweenPlatanaceae andRosidae andFagaceae respectively. TheChloranthaceae, Trochodendrales, andPlatanaceae all occupy a somewhat intermediate position between theMagnoliidae andHamamelidae and are of considerable interest with respect to their role in the initial radiation of nonmagnoliid (higher) dicotyledons.     

Pollen analysis of dust preserved in four medieval books

Pollen spectra of three samples of dust taken from four medieval books are reported. The books, printed A.D. 1500–1530, were preserved in the Franciscan monastery of Kadaň (NW Bohemia) up to c. 30 years ago, and thereafter in Prague. Sample 1 contains rather few pollen grains, most of which are derived from cereals, probably from pastries or bread. Sample 2 is rich in pollen, containing abundant tree pollen, mainlyQuercus andFagus, indicating that the dust indeed comes from NW Bohemia rather than from Prague. Its overall pollen spectrum also corresponds well to published data from medieval forests and the cultural landscape of the region. The spectrum of sample 3 (two books) is rather rich in pollen, mainly of synanthropic plants. The remarkably high pollen numbers of cultivated plants (Sambucus nigra, Lathyrus type andSymphytum) are still unexplained.