- 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 20 and 21: PL‐8or DNA replication, transcrip
- Page 22: PL‐10THE METAL CLUES OF LIFEFedon
- Page 26 and 27: DNA molecules that are replicated,
- Page 28 and 29: in ocean. The primary biosphere had
- Page 30 and 31: OP‐1ROLE OF COMETS IN THE ORIGIN
- Page 32 and 33: OP‐2GRAVITATIONAL INSTABILITY IN
- Page 34 and 35: OP‐2Typical sizes of gravitationa
- Page 36 and 37: OP‐4VUV PHOTOPHYSICS OF PREBIOTIC
- Page 38: OP‐5STAGES OF CHEMICAL EVOLUTION
- Page 41 and 42: OP‐7ABIOGENIC SYNTHESIS OF OLIGOP
- Page 44 and 45: OP‐8participation of the antenna,
- Page 47 and 48: OP‐11NATURAL SELECTION IN PREBIOL
- Page 49 and 50: OP‐12ABIOGENIC MODEL OF PHOTOPHOS
- Page 51 and 52: OP‐13STATISTICS OF GENOME SIZE AN
- Page 53 and 54: OP‐14WOLBACHIA - A NASCENT NEW OR
- Page 55 and 56: OP‐15SPACE FLIGHT EXPERIMENTS WIT
- Page 57 and 58: OP‐16EVOLUTIONARY TRENDS OF GENOM
- Page 59 and 60: OP‐17HABITALS AND ENERGETICS OF F
- Page 61 and 62: OP‐18EVOLUTION OF REPLICATORS ON
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- Page 65 and 66: OP‐21EVOLUTION OF GEOLOGICAL PROC
- Page 67 and 68: OP‐22GLOBAL REORGANIZATION IN THE
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OP‐23THE EFFECT OF IMPACT‐INDUC
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OP‐24CUATRO CIENEGAS: A PRECAMBRI
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OP‐25In shallow‐water marine as
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OP‐26small population will be bet
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OP‐27lichenized fungi to tolerate
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OP‐28mineral layers is restricted
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OP‐29mutations and/or inbreeding.
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OP‐30ConclusionSuccessive duplica
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OP‐31The most frequent associatio
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OP‐33too.regions.TAXONOMICAL AND
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OP‐34MICROEVOLUTIONARY PROCESSES
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OP‐35THE STEPS OF VASCULAR PLANT
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OP‐37THE DAWN OF THE AEROBIC BIOS
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OP‐38THE OLDEST EVIDENCE OF BIOTU
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OP‐39SCIENTIFIC SURVEY ON LAKE BA
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OP‐40PERMAFROST ASTROBIOLOGY: TER
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OP‐41LOOKING FOR LIVE IN HIGH TEM
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OP‐43RISE AND FALL OF THE Y‐CHR
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OP‐44penetrated into Eurasia, and
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irth of true biology [4]. Studies o
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FLUCTUATING HYDROTHERMAL ENVIRONMEN
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PRE‐TRANSLATIONAL ORIGIN OF THE G
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COULD CHRONIC STRESS INDUCED BY POL
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A UNIVERSAL TREND OF NUCLEOTIDE ASS
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References[1]. I.K. Jordan et al (2
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PP‐67The work supported by RFBR g
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COMPLEX HETEROTROPHIC EUKARYOTES AT
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MOLECULAR DATA IN THE STUDIES OF EV
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wrong interpretation I can refer to
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iefed in [8]. Below, we describe th
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POSTER PRESENTATIONS
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PP‐1atoms and molecules, but also
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PP‐2Figure 2: a, b: three‐phase
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PP‐3bioproductivity. Influence of
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PP‐4be practically unchanged at t
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PP‐5Two types of preservation of
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PP‐7CHROMATO‐MASS‐SPECTROMETR
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PP‐8The fourth most significant s
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PP‐9thousands of starting models
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PP‐10FUNGAL‐LIKE ELEMENTS IN TH
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PP‐11COSMIC PERIODICITY IN PHANER
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PP‐12Comparison of molecular evol
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PP‐13value in comparison with its
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PP‐14indicates the chemical excha
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PP‐16FROM PRIMARY DNAs TO CELLS:
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PP‐17ORGANIC UNIVERSE & SPONTANEO
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PP‐18TUNGUSKA IN THE LIGHT OF NEC
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PP‐19time scale, in Pliocene‐Lo
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PP‐20In 2010, these hydrocarbons
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PP‐21Oils from the Kuyumbinskoye
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PP‐22Cambrian oils from the Angar
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PP‐23The oldest Trilobite Biofaci
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PP‐24Pr/Ph1; tricyclane index
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PP‐25cyanobacterial mat, mineralo
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PP‐26genera existing at that time
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PP‐27an introduction of alk genes
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PP‐28More specialized species hav
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PP‐29picture there is Mossbauer s
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PP‐30AUTOCATALYTIC PRIMORDIAL MET
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PP‐31COMPARISON OF THE PALEOPROTE
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PP‐32STRATIGRAPHIC AND GEOGRAPHIC
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PP‐33BIOLOGICAL INPUT OF PROTEASE
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PP‐34EARLY STAGES OF MOLLUSCAN EV
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PP‐35VARIATIONS IN MARINE ANIMAL
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PP‐36FORMATION OF NUCLEOBASES FRO
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PP‐37climatic temperature constra
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PP‐38fragments amygdule basalts w
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PP‐39walls of coral limestone in
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PP‐40Udokan trough exhibits great
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PP‐42HOLLOW SPINES IN RADIOLARIAN
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PP‐43CAUSE‐EFFECT RELATIONSHIP
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PP‐44DYNAMICS OF CARPINUS BETULUS
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PP‐45PARTITION OF MICROELEMENTS I
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PP‐45According to these data, the
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PP‐46bacterial cultures, except H
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PP‐48BACTERIAL MINERALOFORMATION
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PP‐50STATISTICAL EVALUATION OF TH
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PP‐51224
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PP‐52226
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PP‐53invasion of terrestrial envi
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PP‐54particularly in industrializ
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PP‐56EVOLUTION OF ORGANISM-SEDIME
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PP‐57THE GENETIC RELATIONSHIP OF
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PP‐59BLACK SHALE BIOMARKERS FROM
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PP‐60HOPANES IN LOWER AND MIDDLE
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PP‐61MOTIVE FORCES AND STAGES OF
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PP‐62THE EXTREME LIFE OF A WATER
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PP‐63MORPHOGENETIC (?) TRENDS IN
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PP‐63Thus there are some morphoge
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PP‐64characteristic for marine or
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PP‐65Sections of Daldarma formati
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PP‐66Chaetomium genus. Comparativ
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Bogina MariaInstitute of Geology of
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Khan Adil HakeemGovt.Katurba Colleg
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Nazarova Ariadna FilippovnaSevertso
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Spiridonov Aleksey AlexeevichBoresk
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ContentPLENARY LECTURES ...........
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OP‐6Shematovich V.I.ASTROCHEMISTR
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OP‐24Siefert J.CUATRO CIENEGAS: A
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OP‐42Stoyanovskaya O.P."BUTTERFLY
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PP‐7.PP‐8.PP‐9.Gerasimov M.V.
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PP‐25.PP‐26.PP‐27.Lazareva E.
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PP‐44.PP‐45.PP‐46.PP‐47.PP
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PP‐64.PP‐65.PP‐66.PP‐67.Sha