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PP‐9Acknowledgement. This work was supported by the Program of presidium RAS No. 15(09‐П‐5‐1009) and Russian Foundation of Basic Research (Nos. 08‐05‐00993, 11‐03‐00870).References[1]. Ostrovskii V. E., Kadyshevich E. A. Russ. J. Phys. Chem. 2000, 74, 1114–1124.[2]. Jorgensen W. L., et al. J. Chem. Phys. 1983, 79, 926–935.[3]. Dzyabchenko A.V. Russ. J. Phys. Chem. A. 2008, 82, 1663–1671.[4]. Bernal J.D., Fowler R.H. J. Chem. Phys. 1933, 1, 515‐548.[5]. Kirov M.V. Crystallography reports 2010, 55, 353‐361.147
PP‐10FUNGAL‐LIKE ELEMENTS IN THE CONSTRUCTION OF THE RIPHEANUNICELLULAR MICROFOSSILSGerman T.E., Podkovyrov V.N.Institute of Precambrian Geology and Geochronology RAS,Makarova emb., 2, St.‐Petersburg 199034, Russia, e‐mail: vpodk@mail.ruPrecambrian microfossils are useful in comparative studies of such fundamental aspectsas the transition from unicellular to multicellular organization. The specific population of theRiphean unicellular organisms has been described from ~1Gyr sediments (Lakhanda Group,Uchur‐Maya region, SE Siberia). They have been recorded in shales and consistentlyassociated with water‐deposited sediments. Unicells having a hollow shell of highly variedshape (spherical, ellipsoidal, elongate or sometimes polygonal) are composed of an organicsubstance and show net‐like distribution.A considerable number of Precambrian genera remained of undetermined affinity andgenera defined on morphology only, without implication as to relationships, it is undesirablethat they should be classed into the Linnaean hierarchy of orders and families. It is clearlypreferable that any classification, adopted should give no false impression of any naturalrelationship and should facilitate the easy transfer away of genera when their affinities cameto be determined. The lakhandinian microfossils were interpreted as probable yeasts thathave evidence in growth habit, general morphology, mode of reproduction commonly canbe discerned features that provide a basis for comparison of extant and fossil taxa. Ripheanunicells display the coincidence of their morphology, the mode of typical multilateralbudding of Saccharomyces and give additional evidence of the very early existence of suchbiological organization. These organic‐walled fossils have been described asEosaccharomyces ramosus Herm. (Hermann, 1979). Precambrian unicellular organismsextremely numerous and show innovations in biologic organization involved in theevolutionary transition from a single cell to multicellular pseudo tissue‐like microcolonies.Adjacent or loosely connected cells in these colonies tend to be similar texture andcolor, but differ in their diameter and shape. The connection between adjacent cells incolonies is usually with indication of cytoplasmic connection. Within an array fossils areequidimensional, but more often with one of the cells two to three times longer than itsneighbor and resemble sack‐like body called an ascus. There are some spheroidal structures148
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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‐2case the primary Earth substa
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PL‐310. If the high‐carbon rock
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PL‐5ON THE COMPLEXITY OF PRIMORDI
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MICROFOSSILS, BIOMOLECULES AND BIOM
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PL‐8MOLECULAR COLONIES AS A PRE
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PL‐9GENE NETWORKS AND THE EVOLUTI
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EMERGENT LIFE DRINKS ORDERLINESS FR
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PROTOBIOLOGICAL STRUCTURES, PREBIOL
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ORAL PRESENTATIONS
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OP‐1developed a theory of the gre
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OP‐2field of the Sun and the fiel
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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‐6processes. Mentioned above as
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OP‐7polymerization of simple mole
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OP‐9SYNTHESIS OF BIOLOGICALLY IMP
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OP‐11threshold is reached the sel
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OP‐12nanoparticles of polysilicic
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OP‐13We aimed to relate entropy m
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OP‐14gene sequence as about 100 M
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OP‐15of photochemical transformat
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OP‐16modeled by the varying of in
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OP‐17[2]. Mulkidjanian, A. Y., Ko
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OP‐19LIFE ORIGINATION HYDRATE HYP
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OP‐20PREBIOLOGICAL EVOLUTION OF M
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OP‐21The manifestation of this ge
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OP‐22dominated by ostracodes, fir
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OP‐23present as Fe 0 , Fe +2 , an
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PROCARYOTIC ASSEMBLAGES OF EARLY PR
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OP‐26OPTIMIZATION OF STRESS RESPO
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OP‐27LICHENS COULD BE RESPONSIBLE
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OP‐28ROLE OF CYANOBACTERIA FROM D
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OP‐29COMPUTER TOOL FOR MODELING T
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OP‐30EVOLUTION OF TRANSLATION TER
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WHY WE NEED NEW EVIDENCES FOR DEEP
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ENDEMIC GENERA IN LATITUDINAL FAUNI
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OP‐33Taxonomic structure (alpha d
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OP‐34populations of different gas
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OP‐36in the reef frame, thus incr
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OP‐37extracorporeal digestion. Pl
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Page 102 and 103: OP‐40geological history was favor
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Page 106 and 107: OP‐44COEVOLUTION OF MAMMALIAN FAU
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Page 110 and 111: OP‐45[8]. Lincoln T.A., Joyce G.F
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Page 116 and 117: aromatic hydrocarbons (PAHs) and th
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Page 120 and 121: PP‐67ADAPTATION OF THE PYROCOCCUS
Page 122 and 123: GROWTH OF MICROORGANISMS IN MARTIAN
Page 124 and 125: 2.3. Cellular thalli (or colonies?)
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Page 128 and 129: A FRACTAL SPATIOTEMPORAL STRUCTURE
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Page 132 and 133: ABIOGENIC SELF‐ASSEMBLAGE OF THE
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Page 136 and 137: PP‐3PALEOZOIC APOCALYPSE: WHAT CA
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Page 140 and 141: PP‐5EDIACARAN SOFT‐BODIED ORGAN
Page 142 and 143: PP‐6SOFTWARE MODELLER OF EVOLUTIO
Page 144 and 145: PP‐8THE EARLIEST STEPS OF ORGANIS
Page 146 and 147: PP‐9MODELING THE CONFIGURATIONS O
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Page 152 and 153: PP‐12GTF2I DOMAIN: STRUCTURE, EVO
Page 154 and 155: PP‐13DEEP INSIDE INTO VERTEBRATES
Page 156 and 157: GENERATION OF MODERN MINERAL‐BIOL
Page 158 and 159: ADSORPTION OF RIBOSE NUCLEOTIDES ON
Page 160 and 161: PP‐16cells. Thus, in addition to
Page 162 and 163: PP‐17organizing photosynthetic pi
Page 164 and 165: PP‐19YOUNGEST OIL OF PLANET EARTH
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Page 168 and 169: PP‐21BIOMARKER HYDROCARBON COMPOS
Page 170 and 171: PP‐22BIOMARKER HYDROCARBONS IN KA
Page 172 and 173: PP‐23EVOLUTION OF TRILOBITE BIOFA
Page 174 and 175: COMPARATIVE ANALYSIS OF BIOMARKER H
Page 176 and 177: CYANO‐BACTERIAL MATS OF HOT SPRIN
Page 178 and 179: PP‐26THE BIOGEOGRAPHICAL EVOLUTIO
Page 180 and 181: PP‐27MICROBIAL COMMUNITIES OF OIL
Page 182 and 183: PP‐28MICROEVOLUTIONARY PROCESSES
Page 184 and 185: BIOGENIC AND ABIOGENIC BIOMORPHIC S
Page 186 and 187: PP‐29are combine nodules forming
Page 188 and 189: PP‐30have led to divergence of la
Page 190 and 191: PP‐31observed in the modern micro
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Page 194 and 195: PP‐33similarities in their three
Page 196 and 197: PP‐34been formed already in the e
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PP‐35The epochs of global cooling
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PP‐37MULTIPLE PATHS TO ENCEPHALIZ
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PP‐38FIRST MIKROIHNOFOSSILS FIND
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PP‐39THE ROLE OF ECHINOIDS IN SHA
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PP‐40BIOMARKER HYDROCARBONS OF TH
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THE STRUCTURE OF MICROBIAL COMMUNIT
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PP‐42Plate 1. Middle Ordovician,
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PP‐43ecosystems of large (up to 6
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PP‐44expansion goes through 40 °
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PP‐45(Ketris and Judovich, 2009),
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SURVIVAL OF HALOPHILES AT DIFFERENT
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PP‐47ISOPRENOID BIOMARKERS AND MI
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SOME PECULIARITIES IN THE DISTRIBUT
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PP‐51EVOLUTION OF INFAUNAL SCAVEN
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PP‐52EARLY PROTEROZOIC BIOMORPHIC
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PP‐53FROM OFFSHORE TO ONSHORE:A N
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PRODUCTS FROM BIRCH BARK FOR TREATI
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PP‐55THE STRUCTURE OF MICROBIAL C
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233PP‐56
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PP‐58EARLY CAMBRIAN EVOLUTION OF
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PP‐59matter (OM) of the Kuonamka
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PP‐60Fig. 1. Masschromatograms fo
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PP‐61multiply. According to prof.
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PP‐62investigation of dietary pat
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PP‐63for almost all discs. Radial
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PP‐64BIOMARKERS IN PRECAMBRIAN KA
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MICROFOSSILS OF BACTERIAL, MUSHROOM
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PP‐66BIOSTRUCTURE OF ASSEMBLAGES
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Abramson Natalia IosifovnaZoologica
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Gerasimov MikhailSpace Research Ins
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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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OP‐33Barskov I.S.TAXONOMICAL AND
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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
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