Contribution of fossil Lagomorpha (Mammalia) to the refinement of the late Miocene–Quaternary palaeobiogeographical setting of Italy

Fossil lagomorphs are very useful palaeogeographical indicators. In the last 15 years, several papers centered on fossil lagomorphs contributed to improve the Italian late Miocene–Quaternary palaeogeographical setting, solving palaeobiogeographical enigmas debated for decades, and providing new, challenging palaeogeographic data. The high number of endemic fossil lagomorphs of Italy is due in part to its complex tectonic history (insular endemisms), and in part to the semi-isolation and the physiography of the Peninsula (continental endemisms). In Italian lagomorphs, a direct causal relationship between dispersal and turnovers is not observed, except for the Toringian. Actually, species replacements are customarily due to archipelago effect (late Miocene), phyletic speciation (Pliocene of Sardinia and Italian mainland) or occur after the extinction of older congeneric species (early Pleistocene).     

金龙胆草提取液体外抑菌活性分析

金龙胆草是传统道地中药材,但目前受到材料来源不足的限制,其应用和研究均受到很大限制,为更好地开发和应用该道地中药材,本研究以实验室野生金龙胆草和组培金龙胆草出发,分别采用热水浴和索式提取法对金龙胆草有效成份进行了提取和体外抑菌活性研究。结果表明,热水浴浸提法的抑菌效果优于索式提取法,均表现出对金黄色葡萄球菌和枯草芽孢杆菌这类革兰氏阳性菌有很好的抑制效果,最小抑菌浓度分别达到12.5 mg/mL和50 mg/mL。野生型提取液和组培型的提取液体外抑菌比较实验显示,野生型金龙胆草的抑菌效果要显著优于组培型金龙胆草提取液。这将为金龙胆草作为中药抗菌药的合理利用提供一定的指导作用,同时为减少抗生素的滥用造成的环境污染作出一定的贡献。     

Revised radiolarian zonation of the Upper Cretaceous Izumi inter-arc basin (SW Japan)

The radiolarian zonation of the Izumi Group is revised for an integrated biostratigraphy across the Campanian/Maastrichtian boundary, together with the ammonite occurrence, fission track and magnetostratigraphic calibration of the acidic tuff key beds. The significance of direct correlation in the same sections, between macro- and micro-fossils (i.e. between relatively near-shore nektonic and turbiditic planktonic-fauna) is discussed in relation to the litho- and bio-facies of the Izumi group. Late Cretaceous paleoceanographic changes inferred from the studied radiolarian fauna represent a regional marker event for the chronostratigraphic correlation of continental shelf to turbidite deep-sea sequences, which accumulated on a mid latitudinal margin facing towards the NW paleo-Pacific. The proposed Campanian/Maastrichtian boundary is at the limit between Pachydiscus awajiensis and Nostoceras hetonaiense ammonite zones. This boundary corresponds to the radiolarian last occurrence of Amphipyndax pseudoconulus (= A. enesseffi), Archaeodictyomitra sliteri, Dictyomitra formosa, D. koslovae and Rhopalosyringium magnificum at the top of the Myllocercion acineton Assemblage Zone (uppermost Campanian), and the first occurrence of Clathrocyclas gravis and Dorcadospyris sp. A, at the base of the Maastrichtian C. gravis Assemblage Zone. The new data settle partly a chronostratigraphic discrepancy between radiolarian and ammonite zonations in the Izumi Group, which was pointed out previously by Ishida et al. (2010).     

Paleobiogeographic implications of Paleocene ostracods from Senegal and related West and North Africa basins

This work summarizes biostratigraphic and paleogeographic data on Paleocene ostracods from the Senegalese-Mauritanian, West African and North African basins. In the Senegalese-Mauritanian basin, late Paleocene ostracods of high diversity suffered a mass extinction in the early Eocene. Comparison between Senegalese faunas and others of the Gulf of Guinea, Sahara and North African basins shows great similarities, with 10 common species identified: Bairdia ilaroensis Reyment and Reyment, Buntonia apatayeriyerii Reyment, B. fortunata Apostolescu, B. tichittensis Apostolescu, Cytherella sylvesterbradleyi Reyment, Dahomeya alata Apostolescu, Isohabrocythere teiskotensis Apostolescu, Phalcocythere vesiculosa (Apostolescu) Quadracythere lagaghiroboensis (Apostolescu) and Trachyleberis teiskotensis (Apostolescu). I. teiskotensis and P. vesiculosa are restricted to the upper Paleocene and are good stratigraphic markers for these basins. Faunal exchanges between West African, trans-Saharan and North African basins are highlighted. The directions of migration of some species are specified. Many West African species migrated to North Africa at the end of the Paleocene-Early Eocene. Migrations are related to climatic and paleobathymetric changes of the Paleocene-Eocene Thermal Maximum (PETM) that occurred during the Paleocene-Eocene transition.     

A newly recognized Mesozoic–Recent interspecific association: calcifying bacteria on decapod crustaceans

Using microscopy and spectroscopy tools, we succeeded in identifying undescribed diminutive epibionts (as epibiotic bacterial colonies) both on exceptionally well‐preserved fossil shrimps and on extant taxa (N. Robin, S. Bernard, J. Miot, M.‐M. Blanc‐Valleron, S. Charbonnier & G. Petit, submitted). This study outlines the ecological parameters of this totally newly recognized interspecific association. To this aim, the systematics and environmental setting of fossil and modern decapod hosts are described; count of bacterial colonies is made to assess prevalence and intensity; scanning electron microscopy is used to illustrate colonial growth patterns; and histological sections of the extant colonies nested in cuticle are stained to determine their incidence on the carapace of their decapod hosts. Thus, the prevalent and intense association is found on decapods of the superfamily Penaeoidea Rafinesque‐Schmaltz 1815 occupying up to 2 cm² of the entire carapace. The association is here observed in deep environments such as that of the Jurassic La Voulte‐sur‐Rhône Lagerstätte. A non‐random distribution of colonial growth patterns is determined; it illustrates a favourite access site along the ventral margin of the shrimp carapace. SEM images and stained sections reveal strong colony embedment within the cuticle, but also damage such as erasing of the cuticular layers. This bioeroding effect, possibly linked to a feeding benefit to the bacteria, brings this interspecific association that has existed, for at least 160 myr, near to parasitism. In addition to illustrating a rare case of interaction in Recent forms that could be described due to previous recognition in fossils, it constitutes a textbook example of the preservation of intimate interactions through geological time.     

Les grands mammifères du Villafranchien supérieur des travertins du Bassin de Denizli (Sud-Ouest Anatolie,Turquie)

The large mammals from travertine deposits in the Denizli basin include the following species: Archidiskodon meridionalis meridionalis, Equus cf. altidens s. l., E. cf. apolloniensis, Stephanorhinus cf. etruscus, Metacervoceros rhenanus, Cervalces (Libralces) ex gr. minor-gallicus, Palaeotragus sp., Bovinae gen. and sp. indet. This association resembles those from the late Villafranchian of Southern and Eastern Europe, and, to some extent, fromWestern Asia, and could be older than 1.2 Ma.     

Associations de kystes de dinoflagellés des séries du Jurassique supérieur (Oxfordien–Tithonien) du Rif externe (Prérif interne et Mésorif,Maroc) et comparaisons régionales

A biostratigraphic study of dinoflagellate cysts of the Upper Jurassic series from the eastern External Rif Chain, has been achieved for the first time on four outcrop sections : the DM section (Douar Marticha), the TB section (the Tarhchenna “Sof”), the KSD section (the Kef Mallou “Sof”) and the Y section (Douar Lamriene) among which three sections (TB, KSD and Y) are well-dated by ammonites and calpionellids fauna. The DM and TB sections are complementary in terms of stratigraphy and correspond respectively to the upper part of the “Ferrysch” Formation, a thick shaly–silty and sandy sequence assigned to the Callovian-Oxfordian stages and to the El Gouzat limestones Formation (Kimmeridgian - Lower Tithonian age) and to the Tarhchenna marly limestones Formation (Upper Tithonian age) from the EL Gouzat area (Mesorif). The KSD and Y sections are also complementary and correspond to the Kimmeridgian-Lower Tithonian Msila limestones Formation and to the overlying marly limestones Massif Formation of Upper Tithonian age, outcropping in the Msila region (Internal Prerif). These four sections have shown many dinocysts rich levels, which had allowed characterizing the Middle? and Upper Oxfordian substages in the DM section. In the other sections, the dinoflagellate cyst assemblages are nearly similar to those of the Kimmeridgian–Tithonian of many sections from the Boreal, Sub-boreal and North tethyan realms, particularily from England, Russia and South-East France basin. The results of the present work confirm once again, the important value of dinoflagellate cysts, for age dating of ammonites-lacking Mesozoic sedimentary sequences and for biostratigraphic correlations.     

Phosphorylation mediated structural and functional changes in pentameric ligand-gated ion channels: Implications for drug discovery

Pentameric ligand-gated ion channels (pLGICs) mediate numerous physiological processes, including fast neurotransmission in the brain. They are targeted by a large number of clinically-important drugs and disruptions to their function are associated with many neurological disorders. The phosphorylation of pLGICs can result in a wide range of functional consequences. Indeed, many neurological disorders result from pLGIC phosphorylation. For example, chronic pain is caused by the protein kinase A-mediated phosphorylation of α3 glycine receptors and nicotine addiction is mediated by the phosphorylation of α4- or α7-containing nicotinic receptors. A recent study demonstrated that phosphorylation can induce a global conformational change in a pLGIC that propagates to the neurotransmitter-binding site. Here we present evidence that phosphorylation-induced global conformational changes may be a universal phenomenon in pLGICs. This raises the possibility of designing drugs to specifically treat disease-modified pLGICs. This review summarizes some of the opportunities available in this area.     

Der Beitrag der Grünen Gentechnik

Yield increase: the contribution of plant biotechnology Modern plant breeding is facing increasing challenges to meet future needs caused by global climate changes, decreasing reserves of fossil fuels, an increasing world population as well as an aging society. Therefore, besides input traits, breeding aims focus on renewable resources and to ensure production of sufficient high quality food and feed. In particular, the world‐wide rising in energy demand harbors the risk that more and more agricultural land will be used for industrial purposes instead for food production. Therefore, breeding of highly productive crop plants for the production of valuable biological materials is of great importance. To optimize the production of valuable compounds a profound molecular and biochemical knowledge of the underlying metabolic pathways and the availability of technologies for the transfer of these findings into crop plants are needed. Plant biotechnology can be a key technology being important for deciphering molecular relationships as well as being required for the implementation of these findings into breeding programs.     

Les pistes dinosauroïdes du Trias moyen français : interprétation et réévaluation de la nomenclature

Numerous dinosauroid footprints which showing sometimes manus imprint mark were gathered, since 1960, from the lower sandstones Triassic formations of the eastern border of the Massif Central (France). Tracks bearing levels are dated from palynological, micropalaeontological and palichnological data. They belong to the period upper Anisian-lower Ladinian. The paleontological results show bipedal digitigrade reptiles with erected, long hind limbs, having also pentadactyl mani and (II-IV) tridactyl feet. The osteological feet inferred structure is like that of Ceratosauria of Late Triassic age. The skeletons of first Dinosauria, diversified already well, are known in summit Ladinian and lower Carnien and those of their ancestors, Dinosauriformes, in Ladinian. And, for this reason, the aniso-ladinian dinosauroid footprints are ascribed to these last animals which thus appeared earlier, to Anisan even to late Olenekian. The chirotheroid hands show a “pseudosuchian” origin which possibly took place during the late Olenekian; feet modifications of these Crurotarsi being characterized by I and V digits reduction and a meso-tarsal joint. The Anisian-Ladinian dinosauroid footprints are ascribed to the ichnospecies Coelurosaurichnus perriauxi and Anchisauripus bibractensis. The discriminant analysis computed from these latter ichnospecies, and others from the German Triassic, French and USA Hettangian indicate that C. perriauxi and A. bibractensis can not be included into Grallator sensu Lull, 1953 or Coelurosaurichnus of Franconie. By this way, these taxa are well original and till now, there was no reason to change their nomenclature. Nevertheless because the numerous changes of Grallator which gathers now, most of dinosauroid footprints, it could be possible to include them into Grallator for the feet and into Atreipus when the manus trace is connected with the foot.