to run the analysis. Lifeless condensate of water‐steam mixture (t = 108‐175 °C) contains 18organic compounds that belong to 5 homologous series: aromatic hydrocarbons(naphthalene, 1,2‐methylnaphtaline, biphenyl, phenathrene, fluorene, squalene, 1,3‐diethylbenzene, and trichlorobenzene), n‐alkanes (decane, dodecane, tridecane,tetradecane, pentadecane, hexadecane, and heptadecane), aldehyde (oktadekanal), ketone(2‐heptadekanon), and alcohol (2‐undetsenol‐1). 10 homologous series have been found inhot solutions (t = 60‐99 °C) inhabited by thermophilic and hyperthermophilicmicroorganisms: aromatic hydrocarbons, n‐alkanes, alkenes, aldehydes, dietoxyalkanes,naphthenes, fatty acids, methyl ethers of fatty acids, monoglycerides, and steroids.Investigating gas‐steam jets in 7 hydrothermal fields in Kamchatka, Isidorov et al (1992)discovered 64 volatile organic compounds of the following homologous series: n‐alkanes,alkenes, cycloalkanes, aromatic hydrocarbons, terpenes and terpenoids, alcohols, ketones,ethers, esters, thiols, disulfides, halogenalkanes, halogenalkenes. Mukhin et al (1979)detected glycine of probably abiotic origination in the lifeless condensate, and 12 aminoacids of biological genesis – in hot solutions of 4 thermal fields in Kamchatka. Availability ofthe abiotic contribution is supposed at least for the following series/compounds: aromatics,alkanes, Cl‐alkanes, glycine.Summary. The explored hydrothermal environments characterizes by: a) spatialgradients and temporal fluctuations of the thermodynamic parameters in rising fluid; b)availability of various biologically important organic molecules (simple amino acids, lipidprecursors, hydrocarbons) that could be involved into self‐assembly/synthesis of prebioticmicrosystems on the early Earth. Basing on this data, laboratory experiments on prebioticchemistry under changeable conditions can be carried out.References[1]. Isidorov VA, Zenkevich IG, Karpov GA (1992) Seismology 13 (3), 287‐293[2]. Kompanichenko, VN (2009). Planetary and Space Science 57, 468‐476[3]. Mukhin LM, Bondarev VB, Vakin EA et al (1979) Doklady AN USSR 244 (4), 974‐977111
PRE‐TRANSLATIONAL ORIGIN OF THE GENETIC CODERodin S.N. 1,2 , Eörs Szathmáry 2,3 and Rodin A.S. 2,41 Beckman Research Institute of the City of Hope, Duarte, CA 91010, USA2 Collegium Budapest, Szentháromság u. 2, H‐1014 Budapest, Hungary3 Parmenides Center for the Study of Thinking, Kirchplatz 1, D‐82049 Munich, Germany4 Human Genetics Center, SPH, University of Texas, Houston, TX 77225, USAThe major challenge to the understanding of the genetic code origins is the archetypal“key‐lock vs. frozen accident” dilemma (Crick, 1968). Recently we have re‐examined thedilemma (Rodin et al., 2009, 2011) in light of modular structures of tRNAs and aminoacyl‐tRNAsynthetases (aaRS) (actually bringing the code into action), and the updated library of aminoacid‐binding sites of RNA aptamers selected in vitro (Yarus et al., 2009; Yanus et al., 2010).The aa‐binding sites of arginine, isoleucine and tyrosine contain both their cognatetriplets, anticodons and codons. We observed that this puzzling error‐prone simultaneouspresence is associated with palindrome‐dinucleotides (Rodin et al., 2011). For example, onebaseshift to the left brings arginine codons CGN, with CG at 1‐2 positions, to the respectiveanticodons NCG, with CG at 2‐3 positions. Technically, the concomitant presence of codonsand anticodons is also expected in the reverse situation, with codons containing palindromedinucleotidesat their 2‐3 positions, and anticodons exhibiting them at 1‐2 positions. A closeranalysis reveals that, surprisingly, RNA binding sites for Arg, Ile and Tyr “prefer”, exactly asin the actual genetic code, anticodon(2‐3)/codon(1‐2) tetramers to their anticodon(1‐2)/codon(2‐3) counterparts, despite the seemingly perfect symmetry of the latter. However,since in vitro selection of aa‐specific RNA aptamers apparently had nothing to do withtranslation, this striking preference provides a new strong support for the notion of thegenetic code emerging before translation, in response to catalytic (and possibly other) needsof ancient RNA life.Consistent with the pre‐translational origin of the code are our updated phylogeneticstudy of tRNA genes (Rodin et al., 2009) and a new model of gradual (Fibonacci iterationlike)evolutionary growth of tRNAs – from a primordial coding triplet and 5’‐DCCA‐3’ (D is abase‐determinator) to the eventual 76 base‐long cloverleaf‐shaped molecule (Rodin et al.2011). The pre‐translational genetic code origin is also consistent with the partition of aaRSsin two structurally unrelated classes with sterically mirror modes of tRNA recognition (Erianiet al., 1990; Delarue, 2007). This partition seems to have protected proto‐tRNAs withcomplementary anticodons from otherwise very likely confusion, the only “exception” being112
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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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PP‐17organizing photosynthetic pi
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PP‐19YOUNGEST OIL OF PLANET EARTH
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PP‐20MID‐CHAIN BRANCHED MONOMET
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PP‐21BIOMARKER HYDROCARBON COMPOS
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PP‐22BIOMARKER HYDROCARBONS IN KA
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PP‐23EVOLUTION OF TRILOBITE BIOFA
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COMPARATIVE ANALYSIS OF BIOMARKER H
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CYANO‐BACTERIAL MATS OF HOT SPRIN
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PP‐26THE BIOGEOGRAPHICAL EVOLUTIO
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PP‐27MICROBIAL COMMUNITIES OF OIL
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PP‐28MICROEVOLUTIONARY PROCESSES
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BIOGENIC AND ABIOGENIC BIOMORPHIC S
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PP‐29are combine nodules forming
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PP‐30have led to divergence of la
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PP‐31observed in the modern micro
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PP‐32by the ammonite Arctocephali
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PP‐33similarities in their three
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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