25th International Meeting on Organic Geochemistry IMOG 2011

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P-390 A three-year survey of fluorescent dissolved organic matter in the Arcachon Bay (South Western France) Edith Parlanti, Marie-Ange Cordier, Fabienne Ibalot Université de Bordeaux, UMR 5805 CNRS, EPOC - LPTC, Talence, France (corresponding author:e.parlanti@epoc.u-bordeaux1.fr) Transitional and 0.8 coastal 0.8 0.8 0.8environments represent Fig. 1: HIX and BIX variations for water samples complex systems 0.8 submitted 0.8 0.8 0.8 to high tidal conditions, collected in Arcachon Bay sites in 2010. intensive exchange 0.8 0.8 0.8 0.8 0.8 0.8 and 0.8 mixing 0.8 between fresh water inputs and seawater. 0.8 The 0.8 0.8 0.8aim of this work was to No marked seasonality was shown for the tributaries; apply fluorescence 0.7 0.7 spectroscopy 0.7 0.7 0.8 0.7 for tracing dissolved on the other hand a specific FDOM from each organic matter 0.7 0.7(DOM) sources 0.7 0.7 and cycling in an tributary site was observed (Fig 2.) economically 0.7 0.7 important 0.7 0.7 coastal 0.7 area: the Arcachon 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 0.8 Bay (French Atlantic 0.6 coast). 0.7 0.6This site is well known for BIX La Leyre 0.6 0.7 0.6 BIX La Leyre 0.6 0.7 BIX Banc d‘Arguin BIX Lanton tourism and 0.6 0.6French 0.6 BIX oyster production and is Bélisaire BIX Canal des étangs 0.6 0.6 BIX Grand Banc BIX Cirès particularly sensitive 0.6 to 0.6 environmental degradation 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 0.7 BIX Ile aux Oiseaux BIX Bourg 0.6 0.6 BIX Eyrac BIX La Hume and to anthropogenic 0.6 inputs 0.6 mainly due to urban, BIX Le Tès BIX Craste de Nezer agricultural, tourism 0.5 0.6 0.5 BIX Betey 0.5 0.6 0.5 BIX Betey and harbour activities. 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX 0.5 0.5 0.6 BIX Ponteils 0.6 0.5 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 0.6 BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX 0.5 0.5 0.6 BIX Ponteils 0.5 0.6 BIX Ponteils 0.5 0.5 0.5 A three-year survey 0.5 0.5 0.5 of fluorescent 0.5 dissolved organic 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 matter (FDOM) 0.5 0.5was undertaken 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 0.5 on 15 stations of the 0.4 0.5 0.4 Arcachon Bay 0.4from 2008 0.4 0.5 0.4 0.4 0.5 until 2010. Surface water samples were 0.4 0.4 collected 0 0.4 from 5 0 the Arcachon 105 1510 Bay (6 2015 2520 3025 3530 35 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0 0.4 5 0 10 5 10 5 15 10 15 10 20 15 20 15 25 20 0.4 0.4 0.4 0.4 25 20 30 25 30 25 35 30 35 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0.4 0 0.4 0.4 35 30 35 stations) with 0.4a step 0 5 0 of 0.4 sampling 5 0 10 of 10 5 15 3-4 months 15 10 20 HIX for 20 15 HIX 25 25 20 30 0 0 0 0 0 0 0 0 0 0 0 5 5 5 5 5 5 5 5 5 5 5 30 25 35 10 10 10 10 10 10 10 10 10 10 35 30 35 0.4 0 15 15 15 15 15 15 15 15 15 15 15 20 20 20 20 20 20 20 20 20 20 20 25 25 25 25 25 25 25 25 25 25 25 25 30 30 30 30 30 30 30 30 30 30 30 35 35 35 35 35 35 35 35 35 35 35 0.4 0 5 10 15 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 020 5 5 5 5 5 5 5 5 5 5 5 5 5 5 5 25 10 10 10 10 10 10 10 10 10 10 10 10 10 10 10 15 15 15 15 15 15 15 15 15 15 15 15 15 15 15 30 20 20 20 20 20 20 20 20 20 20 20 20 20 20 20 35 25 25 25 25 25 25 25 25 25 25 25 25 25 25 25 30 30 30 30 30 30 30 30 30 30 30 30 30 30 30 35 35 35 35 35 35 35 35 35 35 35 35 35 35 35 0 0.4 5 0 10 5 10 5 15 10 15 10 20 15 5 0 10 5 1510HIX 20 25 25 30 30 35 35 0.4 0 FDOM screening. On the other hand, the 9 HIX 2015 HIX2520 3025 3530 35 0 0.4 5 10 15 HIX 20 15 20 0.4 HIX25 20 25 30 25 30 35 30 35 0.4 0 5 10 15 35 0.4 0 5 10 15 HIX 20 25 30 35 0 0.4 0 5 10 15 20 25 30 35 5 0 10 5 15 10 5 0 10 5 1510main HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX 2015 HIX25 30 35 tributaries of the Bay 0 0.4 HIX 20 25 30 35 0 5 were 5 0 10 monthly sampled. 10 5 15 HIX 20 15 HIX2520 3025 3530 35 0 0.4 HIX 20 25 30 35 0.4 5 0 10 5 1510 15 10 HIX 2015 HIX HIX 20 25 30 HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX HIX 20 25 35 2520 30 3025 35 0 5 3530 35 0 10 0 5 15 HIX 2015 HIX25 30 35 0 0.4 0.40 HIX 5 0 5 10 5 10 15 10 15 5 10 HIX 20 15 HIX 20 25 30 35 10 15 HIX HIX 20 25 2520 FIG. 2: 20 30 3025 HIX and 25 35 3530 35 0 0 5 5 10 10 15 HIX 20 25 25 30 30 35 35 0 0 5 5 10 10 15 BIX variations 30 - Arcachon 35 Bay and EEM fluorescence spectra were recorded using HIX 15 20 HIX 20 25 25 30 30 35 HIX 20 25 30 35 HIX HIXa HIX tributaries. HIX Fluorolog FL3-22 SPEX – JOBIN YVON fluorometer. HIX Spatial and temporal variations of DOM fluorescence properties were observed. We observed seasonal effects and different trends in composition as well as in behaviour or production of FDOM. Fluorescence indices were also calculated and discussed (HIX -humification index, and BIX - biological autochthonous input index). These two indices showed spatial and seasonal variations of the quality of FDOM from the Arcachon Bay as shown as an example in Fig. 1 for samples collected in 2010. BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX 0.8 0.8 0.8 0.8 0.8 0.8 0.7 0.7 0.7 0.7 0.7 0.7 0.6 0.6 0.6 0.6 0.6 0.6 0.5 0.5 0.5 0.5 0.5 0.5 BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX SUMMER BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX JULY- OCTOBER MARCH WINTER JANUARY 15 20 25 30 35 15 20 25 30 35 BIX Banc d‘Arguin BIX Bélisaire BIX Grand Banc BIX Ile aux Oiseaux BIX Eyrac BIX Le Tès 0.4 0.4 0.4 0.4 0.4 0.4 15 HIX 20 0 0 0 0 0 0 5 5 5 5 5 5 25 10 10 10 10 10 10 30 15 15 15 15 15 15 20 20 20 20 20 20 35 25 25 25 25 25 25 30 30 30 30 30 30 35 35 35 35 35 35 15 HIX 20 25 30 35 15 HIX 20 25 30 35 15 HIX 20 25 30 35 15 20 25 30 HIX HIX HIX HIX HIX HIX 35 15 HIX HIX 20 25 30 35 HIX HIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX BIX The analysis of FDOM of waters from the Arcachon Bay and from its main tributaries during a three-year survey allowed to discriminate between various sources of colloidal organic matter and showed the spatial and temporal variability of the signatures of the various sources. 519
P-391 Environmental forensics-recent applications of C, H and Cl isotopes in the determination of sources of groundwater contaminants Paul Philp, Tomasz Kuder School of Geology and Geophyscis, University of Oklahoma, Norman, United States of America (corresponding author:pphilp@ou.edu) Since the commercial availability of gas chromatograph-isotope ratio mass spectrometer systems, the number of environmental forensic applications has increased exponentially. There are many well documented EPA methods used in environmental studies but these methods are of little use in environmental forensic studies, where the major goal is to find responsible parties rather than simply obtaining concentration data. In general environmental forensic studies utilize a tiered approach, with gas chromatography (GC) providing an initial indication of the contaminant type; gas chromatography-mass spectrometry (GCMS) identifying specific compounds and undertaking correlation or discrimination studies. However in many cases the results at this point may still be ambiguous and not clearly pointing to any specific source(s) for the contaminant. This is particularly true in the case of contaminated ground water where there might be a single component such as MTBE or PCE etc., where GC and GCMS, whilst telling us it is one compound, will certainly not differentiate sources of the contaminant. Differentiation of more complex mixtures such as crude oils, refined products, and PAHs may also benefit from using stable isotopes as an additional line of evidence in distinguishing potential sources. There are two major applications of stable isotopes in environmental forensics, the first being a tool to differentiate sources and the second to monitor the onset and extent of natural attenuation. This paper will provide examples from both of these areas. First though it is important to mention that early applications of stable isotopes only considered utilization of carbon isotopes, but in recent years utilization of H and, even more recently, Cl isotopes has become more widespread. A number of isotope specific challenges have become apparent along the way to developing these as routine tools for these applications. For example whilst H isotopes can be readily determined in the case of hydrocarbons, in a compound such as TCE (trichloroethylene) with only one H and 3 Cl, this requires higher contaminant concentrations for the H but at the same time may provide valuable information as to whether the TCE was an original synthetic product or formed from degradation of PCE. Determination of Cl isotopes of individual compounds is now becoming a routine tool and can be obtained through the use of GCMS and does not require GCIRMS. The outcome is that it is now possible to use 2D or 3D stable isotope fingerprinting to study both sources of contaminants as well as the onset of natural attenuation. In this paper a number of case histories will be described where stable isotopes, C, H and Cl, have been used to discriminate sources of MTBE, chlorinated solvents and hydrocarbons in the environment. Whilst this approach may not provide the silver bullet every attorney is looking for, it will certainly provide additional evidence not available from the traditional techniques of GC and GCMS. Ranges of isotope values for non-degraded samples of many of the common groundwater samples are now well established and samples with isotope values heavier than these values are typically considered to have undergone natural attenuation. At the same time it is important to point out certain misconceptions about utilization of stable isotopes in environmental forensic studies. As a result of a small number of papers published several years ago, it is believed in some areas that one can use isotope compositions of groundwater contaminants to actually identify the company that made the contaminant of interest. This is totally incorrect and any investigation into the manufacturing process involved in making these compounds will quickly show the potential for isotopic variations as a result of changing feedstocks and other variables. In brief stable isotopes are playing an invaluable role in environmental forensic investigations but a huge potential for additional applications remains. 520
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25th Inter
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Dear Conference Delegates, Preface
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Monday 19 th September 2011 - Morni
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Monday 19 th September 2011 - After
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Tuesday 20 th September 2011 - Afte
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Wednesday 21 st September 2011 - Mo
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Wednesday 21 st September 2011 - Af
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13.40 - 15.05 Poster Session 4 (In
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Friday 23 rd September 2011 - Morni
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Poster Sessions (in Kongress-Saal)
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P-026 Comparison of comprehensive t
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P-052 Incorporation of Archaeal and
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P-081 Geochemical evidence for two
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P-108 Organic geochemistry and Meso
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P-133 Can we estimate catchment-sca
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P-157 Can laterally advected interm
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P-182 The influence of hydrogen on
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P-207 Biomarkers along a holocene s
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P-232 Some experimental results on
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P-261 Natural gas generation, migra
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P-288 Re/Os fractionation during ge
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P-314 Chemometric analysis of oil-o
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P-340 Atypical fluids in offshore s
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P-366 Organic geochemical character
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P-392 Environmental forensic study
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P-416 Developing analytical protoco
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P-442 Deep-sea benthic archaea recy
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P-464 Effects of within-catchment p
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Poster Session 4 - Thursday 22 nd S
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Monday Oral Presentations 58
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O-02 Melting history of West Antarc
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O-04 Insights about the marine nitr
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O-06 Eocene out-of-India dispersal
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O-08 An integrated lipid biomarker
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O-10 Sulfur species as facilitators
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O-12 Sulfur isotope systematic of i
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O-14 Exploring the diversity of arc
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O-16 Improved genetic characterizat
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O-18 Petroleum system analysis Sout
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O-19 The borolithochromes: boron-co
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O-21 Study of the stable isotopic c
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O-23 Novel applications of trace me
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O-25 The chemical structure of inso
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O-27 Coenzyme factor 430: abundance
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O-29 Influence of temperature on me
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O-31 The fate of collembola derived
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O-33 Empirical relationship between
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O-35 Biomarker evidence for the Lat
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O-37 The seco-oleananes: identifica
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O-38 Microbial communities associat
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O-40 The importance of geochemical
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O-42 Charge history and petroleum g
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O-44 Bacterial formation of (di)eth
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O-46 Development of a novel tool fo
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O-48 Evolution of petroleum composi
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O-50 Beyond Orgas- BP’s new predi
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O-52 Nitrogen isotopes of amino aci
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O-54 Biomarker and petrographic evi
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O-55 The organic geochemistry of ca
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O-57 Exploring mass extinction even
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O-59 Black shale formation by micro
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O-61 The significant impact of weat
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O-63 Simultaneous shifts in tempera
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O-65 Fluxes and isotope composition
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O-67 Biogeochemical impact of CO2 e
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Bacteria number ml-1 Bacteria numbe
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O-71 Aquathermolysis: pressure effe
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O-73 Designing tight-shale producti
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O-74 Tracing 13C-labeled inorganic
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O-76 Carbon fluxes in phylogenetica
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O-78 Fluid property prediction from
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O-80 Denitrifying bacteria as poten
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O-82 Tetraether lipid profiles in c
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O-84 Prediction of gas volume and d
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Monday Poster Presentations 148
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P-002 Structure and function of asp
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P-004 Preliminary study of acid deg
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P-006 Chemical and geochemical char
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P-008 High resolution measurement o
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P-010 Acidic fraction analyses of B
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P-012 Heteroatom-containing compoun
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P-014 Evaluation of hydropyrolysis
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P-016 Iron isotopic compositions of
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P-018 Evaluation of accelerated sol
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P-020 Improvement of HPLC-protocols
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P-022 Open-system hydrous pyrolysis
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P-024 The phenolic characterisation
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P-026 Comparison of comprehensive t
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P-028 Characterisation of lignin de
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P-030 Trace analysis of methylated
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P-033 An evaluation of petroleum so
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P-035 Contrasting macromolecular or
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P-037 Evolution of depositional env
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P-039 Organic carbon content and ch
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P-041 Organic geochemistry of entra
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P-043 Petrological and organic geoc
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P-045 Occurrence and geochemical ch
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P-047 Characterization of lignites
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P-049 Organic matter of Lower Permi
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P-051 Kerogen sulphur, hydrogen and
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P-053 Sulfur-bound compounds in fre
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P-055 Organic matter preservation i
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P-058 Characterization of aromatic
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P-060 Biomarkers parameters used to
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P-063 Origin of crude oil with high
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P-065 Molecular maturation of Bitum
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P-067 C21-C23 steroidal tricyclic t
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P-069 The age and palaeoenvironment
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P-071 Structural characterization o
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P-074 Discussion on appliance of 25
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P-076 Lanostanes as the new biomark
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P-079 Geochemistry of ―just gener
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P-081 Geochemical evidence for two
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P-083 Thermal maturity assessment o
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P-085 Flash pyrolysis-gas chromatog
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P-087 Petroleum geochemistry of the
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P-089 Addressing thermogenic and bi
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P-091 Investigation of oil stabilit
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P-093 Organic geochemistry, petrole
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P-095 Natural petroleum fractionati
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P-097 Geochemistry of low-boiling
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P-099 Oxygen-containing compounds i
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P-101 Formation of giant deep-burie
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P-103 Geochemical characteristics o
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P-105 Challenges on the origin of o
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P-107 Caldera of the Uzon volcano a
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P-109 A saga on organic geochemistr
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P-111 An integrated inorganic and o
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P-114 Hydrocarbon generation potent
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P-116 Marine transgressional event
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P-118 The cracking kinetics of two
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P-120 The generation potential of t
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P-122 Organic geochemical character
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P-124 Compositional features of org
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P-126 The value of generation hydro
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P-128 Investigation of fish pond ma
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P-130 Bituminous mixtures of Hakemi
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P-132 Combined � 13 C - �D anal
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P-134 Biomarkers preserved in cave
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P-136 Analysis of insoluble organic
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P-139 Role and nature of organic ma
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P-141 Biosurfactants - a green alte
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P-143 Phenolic compounds in water l
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P-145 Current level of the organic
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P-147 The d13C composition of indiv
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P-149 Targeted chemical and physica
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P-151 Cu(II) complexation with humi
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P-153 Differentiation of indoor and
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P-156 A detailed study of the intac
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P-158 Unusual distribution of long-
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P-160 Biomarker signatures of metha
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P-162 Lipid biomarkers and bulk bio
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P-164 Chemotaxonomic composition an
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P-166 The role of two submarine can
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P-168 Correlation of crenarchaea an
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P-170 Microbial activity and abunda
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P-172 Microbially mediated carbonat
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P-174 Distinct microbial inventorie
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P-176 Microbial consortium mediatin
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P-178 Diversity of microbial commun
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P-180 Inhibition of anaerobic oil d
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P-182 The influence of hydrogen on
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P-184 Have they lost their heads? D
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P-187 Paleohydrological changes on
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P-189 Paleoenvironmental variations
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P-191 Highly branched isoprenoid al
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P-193 A new global calibration for
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P-195 Molecular fossils and the lat
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P-197 Sediment trap and core top st
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P-199 Detection of environmental ch
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P-201 Carbon and hydrogen isotope b
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P-203 Biogeochemical processes in H
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P-205 Lipid biomarker analysis of f
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P-207 Biomarkers along a holocene s
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P-209 A comparison of methane emiss
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P-211 Paleocene-Eocene Thermal Maxi
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P-213 Biomarker proxies indicate si
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P-215 Distributions of long-chain d
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P-217 The Vinylguaiacol/Indole or V
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P-219 The age and palaeoenvironment
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P-221 Differences in distribution o
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P-225 The change of land plant deri
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P-227 Terrestrial organic matter in
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P-229 Geochemical peculiarities of
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P-231 Bacteriohopanepolyol content
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P-233 Branched GDGTs in the Yenisei
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P-235 Simulation of organic matter
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P-237 Nature of C29 sterols in the
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P-239 Differentiation of organic ma
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P-242 Changes of Rock-Eval HI, OI,
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P-244 Identification and distributi
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P-246 Carbon isotopes and lipid bio
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P-248 Comparison of soil organic ma
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P-250 Biomarker distribution along
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Wednesday Poster Presentations 388
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P-255 Gas source classification in
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P-257 The components and carbon iso
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P-259 Stable carbon isotopes of coa
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P-261 Natural gas generation, migra
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P-264 Natural gas geochemistry of t
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P-266 Geochemical and isotopic char
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P-269 Distribution of alkylbenzenes
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P-271 Terrestrial-derived biomarker
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P-273 Preservation of β-carotane i
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P-275 Aromatic hydrocarbons in oils
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P-277 Statistical analysis of diamo
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P-279 Characterization of biomarker
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P-281 The significance of novel A-n
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P-283 Correlation between compositi
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P-285 Understanding Fluid Inclusion
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P-287 The hydrocarbon occurrence an
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P-289 Correlation of crude oils res
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P-291 Geochemical parameters for un
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P-293 Hydrocarbon biomarkers in the
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P-295 Using diamondoids to unravel
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P-297 Significance of aromatic biom
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P-299 Drilling conditions making we
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P-301 Biomarker distributions and
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P-303 Evaluation of petroleum syste
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P-305 Geochemical indices of hydroc
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P-307 Basin modelling of the Hammer
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P-309 Comparative characteristics o
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P-311 High water pressure induced c
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P-313 Calibration of absolute matur
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P-315 Organic Geochemistry of Lower
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P-317 Laboratory simulation of vert
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P-319 The study of C1-C3 gas genera
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P-321 Hydrocarbon potential of Maik
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P-323 Paleoenvironment significance
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P-325 Origin of abnormal sonic resp
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P-327 Organic geochemistry and orga
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P-329 Characterising the deposition
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P-331 Organic-geochemical character
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P-335 Geochemistry of aqua-bitumoid
Page 469 and 470: P-337 Application of electrospray i
Page 471 and 472: P-339 Geochemical characterization
Page 473 and 474: P-341 Simulation studies on the ads
Page 475 and 476: P-343 Effective diffusivities of CO
Page 477 and 478: P-345 Oil Fingerprinting associated
Page 479 and 480: P-347 Strategies for the assessment
Page 481 and 482: P-349 Fluid pressure evolution and
Page 483 and 484: P-351 The releasing of covalently-b
Page 485 and 486: P-354 Sulfur isotope fractionation
Page 487 and 488: P-356 Controls on the kinetics of t
Page 489 and 490: P-358 Sulfur compounds in liquid pr
Page 491 and 492: P-360 High pressure pyrolysis of hy
Page 493 and 494: P-362 The reaction of elemental sul
Page 495 and 496: P-365 Geochemical evaluation of the
Page 497 and 498: P-367 Geochemical controls on shale
Page 499 and 500: P-369 Evolution of pores in organic
Page 501 and 502: P-371 Preliminary investigations in
Page 503 and 504: P-373 Geochemistry of coalbed metha
Page 505 and 506: P-375 Integration of basin modeling
Page 507 and 508: P-377 Oil shales occurring in Mongo
Page 509 and 510: Thursday Poster Presentations 508
Page 511 and 512: P-381 Permissible concentration of
Page 513 and 514: P-383 Accumulation and degradation
Page 515 and 516: P-385 Source determination and dept
Page 517 and 518: P-387 The use of phospholipid fatty
Page 519: P-389 Biogeochemical process studie
Page 523 and 524: P-393 Geochemical characterization
Page 525 and 526: P-395 Source characterization using
Page 527 and 528: P-397 Impact of different operating
Page 529 and 530: P-399 Resolving sources and preserv
Page 531 and 532: P-402 New insights into soil organi
Page 533 and 534: P-404 Amino sugars as biomarkers fo
Page 535 and 536: P-406 Biogeochemistry of lake Soppe
Page 537 and 538: P-408 Sea surface salinity reconstr
Page 539 and 540: P-410 Carbon cycling in lacustrine
Page 541 and 542: P-412 Radiocarbon distributions in
Page 543 and 544: P-414 European lake sediment calibr
Page 545 and 546: P-416 Developing analytical protoco
Page 547 and 548: P-418 Extreme intra- and intermolec
Page 549 and 550: P-420 � 2 H differences among lip
Page 551 and 552: P-424 Intact polar lipid and associ
Page 553 and 554: P-426 Bacterial versus archaeal act
Page 555 and 556: P-428 Study of microbial activity a
Page 557 and 558: P-430 New bacteriochlorophyll degra
Page 559 and 560: P-432 Thermally stable anammox biom
Page 561 and 562: P-434 Impact of a high CO2 partial
Page 563 and 564: P-436 Methane oxidation in the wate
Page 565 and 566: P-438 Lipid biomarkers of archaeal
Page 567 and 568: P-440 Estimation of endospore numbe
Page 569 and 570: P-442 Deep-sea benthic archaea recy
Page 571 and 572:
P-444 Isolating and cultivating env
Page 573 and 574:
P-446 Distribution of ammonia-oxidi
Page 575 and 576:
P-448 Genetic and metabolic charact
Page 577 and 578:
P-450 Proxies based on archaeal and
Page 579 and 580:
P-453 Experimental palaeochemotaxon
Page 581 and 582:
P-455 Long term cooling and punctua
Page 583 and 584:
P-457 Molecular and isotopic eviden
Page 585 and 586:
P-459 Long-term variations of palae
Page 587 and 588:
P-461 Miocene to Pliocene environme
Page 589 and 590:
P-463 Holocene paleoclimatic variat
Page 591 and 592:
P-465 Hydrological and biogeochemic
Page 593 and 594:
P-467 Molecular hydrogen isotope sy
Page 595 and 596:
P-469 Impact of anaerobic methane o
Page 597 and 598:
P-471 Integrating biomarker and mic
Page 599 and 600:
P-473 Application of TEX86-paleothe
Page 601 and 602:
P-475 Stable isotopes (C, S) and hy
Page 603 and 604:
P-478 The first findings of 12- and
Page 605 and 606:
P-480 The 3 P’s* and the Albian o
Page 607 and 608:
P-482 Meter-scale oxygen gradients
Page 609 and 610:
P-484 Coupling of Miocene-Pliocene
Page 611 and 612:
P-486 New molecular marker and spec
Page 613 and 614:
P-488 Paleoenvironmental changes fr
Page 615 and 616:
P-491 Methoxy-serratenes as discrim
Page 617 and 618:
P-493 Vegetation and soil organic m
Page 619 and 620:
P-497 Decomposition of wheat straw
Page 621 and 622:
P-499 The relationship between peat
Page 623 and 624:
P-501 Land use and climatic effects
Page 625 and 626:
P-503 Geochemical characterization
Page 627 and 628:
P-505 Organic carbon composition an
Page 629 and 630:
P-507 Dynamics of soil organic matt
Page 631 and 632:
P-509 Exploiting isotopic, organic,
Page 633 and 634:
P-511 The effect of soil moisture o
Page 635 and 636:
P-513 Anaerobic oxidation of plant-
Page 637 and 638:
P-515 Variability of terrestrially-
Page 639 and 640:
Author Index 638
Page 641 and 642:
Anselmetti Flavio S. O-63 Ansong Ge
Page 643 and 644:
Brinkhuis Henk P-200, P-468 Britton
Page 645 and 646:
de Souza Carvalho Ismar P-017 Dedys
Page 647 and 648:
Francu Juraj P-037, P-266 Frank Ric
Page 649 and 650:
Hart Malcolm O-09 Hartkopf-Fröder
Page 651 and 652:
Jin Zhijun P-094 Jingjing Li P-179
Page 653 and 654:
Lausmaa Jukka O-58 Lavrieux Marlèn
Page 655 and 656:
Marsh Steven P-509 Marshall Chris O
Page 657 and 658:
Nemchenko- Rovenskaya Alla P-112 Ne
Page 659 and 660:
Radovic Miljana P-152 Ramanathan AL
Page 661 and 662:
Schröder Jan P-020, P-029 Schubert
Page 663 and 664:
Strelnikova Eugenia P-099 Stuart-Wi
Page 665 and 666:
Wakeham Stuart G. O-69 Walters Clif
Page 667 and 668:
Zhang Jing P-515 Zhang Jingru P-398
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25th International Meeting on Organic Geochemistry IMOG 2011

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