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PP‐40BIOMARKER HYDROCARBONS OF THE LOWER PROTEROZOICOF THE KODAR‐UDOKAN TROUGH (THE ALDAN SHIELD)Timoshina I.D., Fursenko E.A.Institute of Petroleum Geology and Geophysics SB RAS, Prosp. Akad. Koptyuga 3,Novosibirsk, 630090, Russia; fax: 8(383)3332301; e‐mail: TimoshinaID@ipgg.nsc.ruLower Proterozoic (1.86 Ga) organic matter (OM) in the Kodar‐Udokan trough of theAldan shield was found to be strongly metamorphosed, as evidenced by isotopically heavycarbon ( 13 С of insoluble OM ranging from ─29.5 to ─27.0‰), have the TOC values of 0.03‐0.05% and a low chloroform‐extractable bitumen content (0.0009‐0.0015%), mostly resins(64.0‐83.6%). The (fig. 1) results ofbiogeochemical studies suggest thatthis OM is aquatic, planktonic andbacteriogenic in origin, as indicated bythe distributions of normal alkanes(nC 27 /nC 17
PP‐40Udokan trough exhibits greater affinity to OM of the same age found in sediments from theLower Khani graben‐syncline and shungites from the Onega synclinorium [3], UpperProterozoic OM from the Yenisey Ridge and Baykit anteclise [4], Vendian and LowerCambrian oils from the Angara‐Lena step and Bakhta mega‐salient of the Siberian platform[5], as well as to some Precambrian oils and chloroform‐extractable bitumens from the EastEuropean platform [6‐8].This work was supported by RFBR (10‐05‐00705) and the Earth Sciences DepartmentProgram N 15.References[1]. Waples, D.W., Machihara, T. (1991) AAPG Methods in explorations, N 9, 91p.[2]. Petеrs, K.E., Moldowan, J.M. (1993) The biomarker guide: interpreting molecular fossils in petroleum andancient sediments, New Jersey, Prentice Hall, Englwood Cliffs, 363p.[3]. Kontorovich, А.E., et al. (2009) Paleontological Journal 43, N 8, p. 965‐971.[4]. Timoshina, I.D. (2004) Russian Geology and Geophysics 45, N 7, p.852‐861.[5]. Kontorovich, A.E., et al. (2005) Petroleum Frontiers 20, N 3, 11‐26.[6]. Bazhenova, O.K., et al. (1994) Dokl. RAN 337, N 3, 371‐377.[7]. Bazhenova, O.K., Aref’ev, O.A. (1998) Geokhimiya, N 3, 286‐294.[8]. Kim, N.S. (2004) Russian Geology and Geophysics 45, N 7, 875‐884.206
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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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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
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
Page 166 and 167: PP‐20MID‐CHAIN BRANCHED MONOMET
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
Page 192 and 193: PP‐32by the ammonite Arctocephali
Page 194 and 195: PP‐33similarities in their three
Page 196 and 197: PP‐34been formed already in the e
Page 198 and 199: PP‐35The epochs of global cooling
Page 200 and 201: PP‐37MULTIPLE PATHS TO ENCEPHALIZ
Page 202 and 203: PP‐38FIRST MIKROIHNOFOSSILS FIND
Page 204 and 205: PP‐39THE ROLE OF ECHINOIDS IN SHA
Page 208 and 209: THE STRUCTURE OF MICROBIAL COMMUNIT
Page 210 and 211: PP‐42Plate 1. Middle Ordovician,
Page 212 and 213: PP‐43ecosystems of large (up to 6
Page 214 and 215: PP‐44expansion goes through 40 °
Page 216 and 217: PP‐45(Ketris and Judovich, 2009),
Page 218 and 219: SURVIVAL OF HALOPHILES AT DIFFERENT
Page 220 and 221: PP‐47ISOPRENOID BIOMARKERS AND MI
Page 222 and 223: SOME PECULIARITIES IN THE DISTRIBUT
Page 224 and 225: PP‐51EVOLUTION OF INFAUNAL SCAVEN
Page 226 and 227: PP‐52EARLY PROTEROZOIC BIOMORPHIC
Page 228 and 229: PP‐53FROM OFFSHORE TO ONSHORE:A N
Page 230 and 231: PRODUCTS FROM BIRCH BARK FOR TREATI
Page 232 and 233: PP‐55THE STRUCTURE OF MICROBIAL C
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Page 236 and 237: PP‐58EARLY CAMBRIAN EVOLUTION OF
Page 238 and 239: PP‐59matter (OM) of the Kuonamka
Page 240 and 241: PP‐60Fig. 1. Masschromatograms fo
Page 242 and 243: PP‐61multiply. According to prof.
Page 244 and 245: PP‐62investigation of dietary pat
Page 246 and 247: PP‐63for almost all discs. Radial
Page 248 and 249: PP‐64BIOMARKERS IN PRECAMBRIAN KA
Page 250 and 251: MICROFOSSILS OF BACTERIAL, MUSHROOM
Page 252 and 253: PP‐66BIOSTRUCTURE OF ASSEMBLAGES
Page 254 and 255: 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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