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PL‐8or DNA replication, transcription, and even translation, can occur in molecular colonies.Moreover, molecular colonies were shown to be able of linking the phenotype to genotypewhich is needed for the natural selection and of evolution.Clay as a suitable matrix for the origin of lifeClay is a porous mineral and therefore it might serve as a matrix in which pre‐bioticmolecular colonies could originate and grow. It seems that the most suitable for this purposewas montmorillonite, a layered aluminosilicate whose pores upon hydratation of the claybecome comparable in size to biopolymers. Montmorillonite was abundant on the earlyEarth, and also was found in meteorites and on Mars [7]. Due to its high ion‐exchangecapacity, it is capable of >10,000‐fold concentrating nucleotides from the surroundingsolution [8]. It also has a high affinity to polynucleotides, especially to their single strandedform [9], and hence might serve as an early substitute for SSB (single strand binding)proteins that stabilize the single stranded state of nucleic acids necessary for replication. It iscapable of catalyzing the polymerization of nucleotides [10], and the formation of theirprecursors from simple organic compounds such as methanol [11]. Moreover, its particlesincrease by 100‐fold the rate of liposome formation from a lipid emulsion and becomesinternalized by the liposomes, together with the adsorbed poly‐ and mononucleotides [12].Therefore, at some stage of evolution the molecular colonies growing in the montmorillonitematrix might become enveloped with a membrane, thereby giving rise to the first protocells.[1]. Gilbert W, de Souza SJ (1999) In The RNA World, 2nd ed. CSHL Press (Cold Spring Harbor, NY), 221–231.[2]. Szostak JW (1999) In Size Limits of Very Small Microorganisms. National Academy Press (Washington,DC), 120–125.[3]. Spirin AS (2005) Mol. Biol. (Moscow) 39, 550–556.[4]. Oberholzer T, Wick R, Luisi PL, Biebricher CK (1995) Biochem. Biophys. Res. Commun. 207, 250–257.[5]. Mansy SS, Schrum JP, Krishnamurthy M, Tobé S, Treco DA, Szostak JW (2008) Nature 454, 122–125.[6]. Chetverin AB, Chetverina HV, Munishkin AV (1991) J. Mol. Biol. 222, 3–9.[7]. Poulet F el al. (40 authors). (2005) Nature 438, 623‐627.[8]. Ferris JP, Ertem G, Agarwal VK. (1989) Orig. Life Evol. Biosph. 19, 153−164.[9]. Franchi M, Ferris JP, Gallori E (2003) Orig. Life Evol. Biosph. 33, 1–16.[10]. Huang W, Ferris JP (2006) J. Amer. Chem. Soc. 128, 8914‐8919.[11]. Williams LB, Canfield B, Voglesonger KM, Holloway JR (2005) Geology 33, 913–916.[12]. Hanczyc MM., Fujikawa SM., Szostak JW (2003) Science 302, 618‐622.19
PL‐9GENE NETWORKS AND THE EVOLUTION OF BIOLOGICAL SYSTEMSKolchanov N.A. 1,2 , Afonnikov D.A. 1,2 , Gunbin K.V. 1 , Suslov V.V. 11 Institute of Cytology and Genetics SB RAS, Novosibirsk, Russia2 Novosibirsk State University, Novosibirsk, RussiaGene network represent the functional group of coordinately expressed genes andprovide a basis underlying any morphological trait. For example, formation of each organrequires complex coordinated expression of genes hierarchically organized into the genenetwork. In this report we will discuss how molecular evolution of genes through theirhierarchically organized networks affects the evolution at the level of organism.The work supported in part by RFBR grants 09‐04‐01641‐а, 11‐04‐01771‐а; SB RASintegration projects №109, 26, 119; REC NSU (REC‐008), State contract П857 and RASprograms А.II.6 and 24.2.20
Page 2 and 3: Boreskov Institute of Catalysis of
Page 4 and 5: INTERNATIONAL SCIENTIFIC COMMITTEEA
Page 6 and 7: PLENARY LECTURES
Page 8 and 9: PL‐1first planetesimals (embryos
Page 10 and 11: PL‐2case the primary Earth substa
Page 12 and 13: PL‐310. If the high‐carbon rock
Page 14 and 15: PL‐5ON THE COMPLEXITY OF PRIMORDI
Page 16 and 17: MICROFOSSILS, BIOMOLECULES AND BIOM
Page 19: PL‐8MOLECULAR COLONIES AS A PRE
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Page 31 and 32: OP‐1developed a theory of the gre
Page 33 and 34: OP‐2field of the Sun and the fiel
Page 35 and 36: OP‐3HOT ABIOGENESIS AND EARLY BIO
Page 37 and 38: OP‐4acetic acid [5,6], acetonitri
Page 40 and 41: OP‐6processes. Mentioned above as
Page 42: OP‐7polymerization of simple mole
Page 45: OP‐9SYNTHESIS OF BIOLOGICALLY IMP
Page 48 and 49: OP‐11threshold is reached the sel
Page 50 and 51: OP‐12nanoparticles of polysilicic
Page 52 and 53: OP‐13We aimed to relate entropy m
Page 54 and 55: OP‐14gene sequence as about 100 M
Page 56 and 57: OP‐15of photochemical transformat
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Page 60 and 61: OP‐17[2]. Mulkidjanian, A. Y., Ko
Page 62 and 63: OP‐19LIFE ORIGINATION HYDRATE HYP
Page 64 and 65: OP‐20PREBIOLOGICAL EVOLUTION OF M
Page 66 and 67: OP‐21The manifestation of this ge
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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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97OP‐38
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OP‐39one of the major generalized
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OP‐40geological history was favor
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“BUTTERFLY EFFECT” IN PLANETESI
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OP‐44COEVOLUTION OF MAMMALIAN FAU
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FRAMEWORKS OF LIFE ORIGIN RESEARCH
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OP‐45[8]. Lincoln T.A., Joyce G.F
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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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Results: Considering the changes be
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PP‐67ADAPTATION OF THE PYROCOCCUS
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GROWTH OF MICROORGANISMS IN MARTIAN
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2.3. Cellular thalli (or colonies?)
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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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ABIOGENIC SELF‐ASSEMBLAGE OF THE
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PP‐2FLUID INCLUSION IN QUARTZ FRO
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PP‐3PALEOZOIC APOCALYPSE: WHAT CA
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PP‐4BIOCHEMICAL REACTION OF EARLY
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PP‐5EDIACARAN SOFT‐BODIED ORGAN
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PP‐6SOFTWARE MODELLER OF EVOLUTIO
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PP‐8THE EARLIEST STEPS OF ORGANIS
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PP‐9MODELING THE CONFIGURATIONS O
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PP‐9Acknowledgement. This work wa
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PP‐10that are much darker (probab
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PP‐12GTF2I DOMAIN: STRUCTURE, EVO
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PP‐13DEEP INSIDE INTO VERTEBRATES
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GENERATION OF MODERN MINERAL‐BIOL
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ADSORPTION OF RIBOSE NUCLEOTIDES ON
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PP‐16cells. Thus, in addition to
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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
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