THE STRUCTURE OF MICROBIAL COMMUNITY IN THE BOTTOM WATERLAYER OF LAKE BAIKAL AND POSSIBLE ROLE OF EUBACTERIAIN DESTRUCTION OF DIATOMSPP‐41Zakharova Yu.P. 1 , Kurilkina M.I. 1 , Likhoshvay Al.V. 1 , Shishlyannikov S.M. 1 , Petrova D.P. 1 ,Kalyuzhnaya Ok.V. 1 , Ravin N.V. 2 , Mardanov A.V. 2 , Beletsky A.V. 2 , Galachyants Yu.P. 1 ,Zemskaya T.I. 1 , Likhoshway Ye.V. 11 Limnological Institute SB RAS, 3, Ulan‐Batorskaya, Irkutsk 664033, Russia,zakharova@lin.irk.ru2 Centre “Bioengineering” RAS, 7, Av. 60‐letiya Octyabrya, Moscow, RussiaIt is important to determine the possible role of bacteria in degradation of diatoms, aswell as the role of factors and participants in the silicon cycle in aquatic ecosystems. The aimof this work was to study associations of bacteria and diatoms in natural objects before theirburial in the sediments and under experimental conditions. The preservation of diatoms inthe surface sediment layer and the amount of bacteria associated with diatom cellsdecreased with depth. The maximal abundance of bacteria associated with diatoms (112thousand bacterial sequences of the 16S rRNA gene fragments) was recorded by means ofpirosequencing in the bottom water layer. The microbial community was represented by thefollowing dominant phylogenetic groups: Proteobacteria, Acidobacteria, Actinobacteria,Cyanobacteria, Bacteroidetes, Verrucomicrobia, Firmicutes, and Nitrospira. However, 32% ofthe sequences appeared to be non‐classified because of the absence of analogues in thedatabase. Seven strains of eubacteria were isolated during cultivation on a medium withdiatom extract. According to the data of microbiological analysis and sequencing of 16SrRNA gene, these strains were identified as Mycoplana bullata, Sphingomonas rhizogenes,Agrobacterium tumefaciens, Bacillus simplex, Acinetobacter johnsonii, Methylobacteriumadhaesivum, and Deinococcus aquaticus. Joint cultivation of these strains with a diatomSynedra acus subsp. radians (Kütz.) Skabitsch. caused inhibition of the diatom growthfollowed by cell destruction. Isolated strains revealed activity of hydrolytic enzymes:protease (B.simplex, M. bullata, and D. aquaticus) of β‐xylosidase, β‐glucosidase, β‐galactosidase, chitobiase (M. bullata, S. rhizogenes, A. tumefaciens, and B. simplex), andamylase (D. aquaticus). The data obtained demonstrate that potential participants in siliconcycle that degrade siliceous valves of diatoms may be present among a great variety ofmicroorganisms in the bottom layer of Lake Baikal.This work was supported by the RAS Presidium Programme “Biosphere Origin andEvolution”, project No. 18.4 and RFBR Gran No. 09‐04‐12231‐ofi‐m.207
PP‐42HOLLOW SPINES IN RADIOLARIAN SKELETONS AND SPONGE SPICULESAfanasieva M.S.*, Amon E.O.***Borissiak Paleontological Institute RAS, Moscow, Russia**Zavaritsky Institute of Geology and Geochemistry, Uralian Branch of RAS,Ekaterinburg, RussiaThe shape of main spines in radiolarian skeletons is very diversiform. In overwhelmingmajority the main spines are solid: rodlike, conical or faceted; rarer meet hollow spines.Spines frequently serve as a simple prop for axopodia; but in the inner channel of hollowspines or inside various microtubes can stretch axopodial filaments or bunches of axopods.The texture of hollow main spines and other hollow skeletal structures is variant. Certainhollow spines and internal spicules represent the simple tubes (pl. 1, figs. 1‐4, 6, 7, 8, 9).Other hollow spines and crossbeams are sectioned by horizontal lamellar septum (pl. 1, figs.14, 15). Several hollow spines are complicated with development of special inner capsules(pl. 1, figs. 10, 13) which are supported precisely on the center of spine by radial lamellarseptum (pl. 1, figs. 5, 10‐13, 16, 17), quite often dual (pl. 1, figs. 5, 10). Capsules are hollow(pl. 1, figs. 10). If they are solid (pl. 1, figs. 13), it is most likely a secondary phenomenon.Wall thickness of capsule is comparable to wall thickness of hollow spine, or somewhat less(pl. 1, figs. 10). Internal surface of hollow spine smooth, but internal and external surfaces ofcapsules rough, with small tubercles and ledges (pl. 1, figs. 10, 13). Functional purpose ofsuch capsules not clearly. Probably, they could be as a part of the hydrostatic apparatus.The morphology of initial spicules and spiny radiolarians resemble sponge spicules.However, main difference between radiolarian skeleton and Porifera spicules consists is inpeculiarities of skeleton formation: radiolarians spines grow spirally (pl. 1, figs. 18, 19),whereas spicules of sponges grow away from the center (pl. 1, figs. 20, 21).Radiolarian hollow spines and other hollow skeletal structures, especially spines withhollow capsules, meet extremely rare in fossil state. Only twenty species with various hollowskeletal elements of all classes of radiolarians from Ordovician, Devonian, Carboniferous,Cretaceous and Paleogene are presented in our collection. Probably, subcylindrical spineswith hollow internal channel are the initial, most ancient and primitive structures, whichhave originated in Cambrian. However, the further development of skeletons went on a wayof formation of faceted solid spines. This was the optimal form, provides the greateststrength of spines in the least amount of a mineral material. Nevertheless, themorphogenesis of subcylindrical hollow spines repeated many times during all Phanerozoicup to the present.The study was supported by the Program of Presidium of RAS "Origin of Biosphere and Evolution of Geo‐Biological Systems" and the Russian Foundation for Basic Research, project no. 10‐04‐00143.208
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Boreskov Institute of Catalysis of
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INTERNATIONAL SCIENTIFIC COMMITTEEA
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PLENARY LECTURES
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PL‐1first planetesimals (embryos
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PL‐5ON THE COMPLEXITY OF PRIMORDI
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PL‐8MOLECULAR COLONIES AS A PRE
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PROTOBIOLOGICAL STRUCTURES, PREBIOL
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OP‐1developed a theory of the gre
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OP‐3HOT ABIOGENESIS AND EARLY BIO
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OP‐4acetic acid [5,6], acetonitri
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OP‐11threshold is reached the sel
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OP‐12nanoparticles of polysilicic
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OP‐15of photochemical transformat
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OP‐30EVOLUTION OF TRANSLATION TER
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WHY WE NEED NEW EVIDENCES FOR DEEP
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OP‐33Taxonomic structure (alpha d
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“BUTTERFLY EFFECT” IN PLANETESI
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FRAMEWORKS OF LIFE ORIGIN RESEARCH
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to run the analysis. Lifeless conde
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the pairs of the “very first” (
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aromatic hydrocarbons (PAHs) and th
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GROWTH OF MICROORGANISMS IN MARTIAN
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Under methodical mistakes I mean fi
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A FRACTAL SPATIOTEMPORAL STRUCTURE
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[13]. Gusev, V.A., Arithmetic and a
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PP‐10that are much darker (probab
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GENERATION OF MODERN MINERAL‐BIOL
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Lomakina AnnaLimnological institute
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Rogov Vladimir IgorevichTrofimuk In
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Zamulina Tatiana VladimirovnaBoresk
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PL‐9Kolchanov N.A., Afonnikov D.A
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OP‐15Gontareva N.B., Kuzicheva E.
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Nagovitsin K.COMPLEX HETEROTROPHIC
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PP‐17.PP‐18.PP‐19.PP‐20.PP
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PP‐35.Polishchuk Y.M., Yashchenko
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PP‐54.PP‐55.Kuznetsova S.A.PROD
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III INTERNATIONAL CONFERENCEBIOSPHE