Thèses sur le sujet « Carbon isotope composition »
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Barral, Cuesta Abel. « The carbon isotope composition of the fossil conifer Frenelopsis as a proxy for reconstructing Cretaceous atmospheric CO2 ». Thesis, Lyon, 2016. http://www.theses.fr/2016LYSE1148.
Texte intégralThe Cretaceous was a period characterized by strongly marked climate change and major carbon cycle instability. Atmospheric CO2 has repeatedly been pointed out as a major agent involved in these changing conditions during the period. However, long-term trends in CO2 described for the Cretaceous are not consistent with those of temperature and the large disturbance events of the carbon cycle described for the period. This raises a double question of whether descriptions of the long-term evolution of atmospheric CO2 made so far are accurate or, if so, atmospheric CO2 was actually a major driver of carbon cycle and climate dynamics as usually stated. In this thesis the close relationship between the carbon isotope composition of plants and atmospheric CO2 is used to address this question. Based on its ecological significance, distribution, morphological features and its excellent preservation, the fossil conifer genus Frenelopsis is proposed as a new plant proxy for climate reconstructions during the Cretaceous. The capacity of carbon isotope compositions of Frenelopsis leaves (d13Cleaf) to reconstruct past atmospheric CO2, with regards to both carbon isotope composition (d13CCO2) and concentration (pCO2), is tested based on materials coming from twelve Cretaceous episodes. To provide a framework to test the capacity of d13Cleaf to reconstruct d13CCO2 and allowing for climate estimates from carbon isotope discrimination by plants (?13Cleaf), a new d13CCO2 curve for the Cretaceous based on carbon isotope compositions of marine carbonates has been constructed. Comparison with d13Cleaf-based d13CCO2 estimates reveals that although d13CCO2 and d13Cleaf values follow consistent trends, models developed so far to estimate d13CCO2 from d13Cleaf tend to exaggerate d13CCO2 trends because of assuming a linear relationship between both values. However, given the hyperbolic relationship between ?13Cleaf and pCO2, by considering an independently-estimated correction factor for pCO2 for a given episode, d13Cleaf values may be a valuable proxy for d13CCO2 reconstructions. ?13Cleaf estimates obtained from d13CCO2 and d13Cleaf values were used to reconstruct the long-term evolution of pCO2. The magnitude of estimated pCO2 values is in accordance with that of the most recent and relevant model- and proxy-based pCO2 reconstructions. However, these new results evidence long-term drawdowns of pCO2 for Cretaceous time intervals in which temperature maxima have been described
Gromov, Sergey S. [Verfasser]. « Stable isotope composition of atmospheric carbon monoxide : a modelling study / Sergey S. Gromov ». Mainz : Universitätsbibliothek Mainz, 2014. http://d-nb.info/1051305497/34.
Texte intégralCzuba, Eva. « Development of a technique to study stable carbon isotope composition of NMHCs in ambient air ». Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape2/PQDD_0020/MQ56169.pdf.
Texte intégralUpsdell, Brynn. « The carbon and nitrogen composition of suspended particulate matter in Lake Erie, selected tributaries, and its outflow ». Thesis, University of Waterloo, 2005. http://hdl.handle.net/10012/1219.
Texte intégralHamilton, Bryan T. « Small Mammals in portions of Great Basin National Park Susceptible to Groundwater Withdrawal : Diversity and Stable Isotope Perspectives ». BYU ScholarsArchive, 2009. https://scholarsarchive.byu.edu/etd/1705.
Texte intégralXia, Yang. « Impact of varying NH₄⁺˸NO₃⁻ ratios in nutrient solution on C-isotope composition of leaf- and root-respired CO₂ and putative respiratory substrates in C₃ plants ». Thesis, Université Paris-Saclay (ComUE), 2019. http://www.theses.fr/2019SACLS222.
Texte intégralC-isotope composition of leaf- and root-respired CO₂ in the dark and that of putative respiratory substrates including soluble sugars and organic acids (malate and citrate), PEPc activity, as well as leaf gas exchanges were determined on bean (Phaseolus vulgaris L.) and spinach (Spinacia oleracea L.) plants grown in sand with varying ratios of NH₄⁺: NO₃⁻ in supplied N. Leaf-respired CO₂ was ¹³C enriched under NO₃⁻ nutrition and became progressively ¹³C depleted with increasing amount of NH₄⁺ in supplied N, while C-isotope composition of root-respired CO₂ remained unchanged across N-type gradient. We suggested that a higher amount of ¹³C enriched C-pools fixed by PEPc through anaplerotic pathway contributed to respired CO₂ in leaves under NO₃⁻ nutrition. However, a similar effect in roots expected under NH4+ nutrition was masked because of a rather ¹³C depleted C source (respired CO₂) refixation by PEPc. Unexpectedly, the changes in C-isotope composition of individual metabolites and their amounts as well as PEPc activity exhibited different patterns between the two species. Double labelling experiments (¹³C and ¹⁵N) are needed for better understanding the impact of metabolic plasticity of TCA on isotopic gap between malate and citrate and on C-isotope composition of respired CO₂ in different species under varying N-type nutrition
Yang, Chengfan. « Li isotope study of Yangtze River sediments : new constraints on climate, weathering and carbon cycle relationships ». Electronic Thesis or Diss., Sorbonne université, 2020. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2020SORUS433.pdf.
Texte intégralIn order to better understand the weathering-climate feedback, a series of studies was carried out in the Changjiang (Yangtze) Basin. First, the operation of the Three Gorges Dam (TGD) changed downstream sediment geochemical compositions. Before 2003, large amounts of upstream-derived sediments deposited and experienced further weathering in the mid-lower basin. Since 2003, strong riverbed sediment resuspension changed the roles of the mid-lower reaches from important sinks to major sources of sediments delivered to the sea. As a consequence, an intensified weathering intensity of downstream sediment was observed.Second, dissolved δ7Li exhibit a conservative behavior in the Changjiang Estuary. During the process of SPM transported offshore, weathering product flocculated and deposited, while primary minerals resuspended. The combined effect resulted in the UCC-like SPM δ7Li values. There is a Li isotope fractionation between the dissolved load and exchangeable phase. However, this process shows negligible impact on δ7Li of dissolved load and particulates. Third, weathering response to climate is complex in large river basins. During the Younger Dryas, the positive excursion of clay δ7Li is consistent with enhanced incongruent weathering, in response to temperature cooling. The minor variation of clay δ7Li at 11 – 2 ka likely indicate stable weathering and mile climate variation. Over the last 2 kyr, the fluctuation of clay δ7Li is mostly caused by intensification of human activities. In summary, this thesis sheds new lights on the weathering-climate feedback over geologic past, and provides perspectives on how human activities affect natural processes
Allan, Wendy Lynne. « Variation in the stable carbon isotope composition of needle and annual rings in Pseudotsuga menziesii (Mirb.) Franco and its relation to water use needle nitrogen content and productivity ». Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1996. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp05/mq21902.pdf.
Texte intégralRabarijaona, Arivoara. « L'efficience intrinsèque d'utilisation de l'eau (WUEi) du chêne sessile conditionne-t-elle sa résilience à la sécheresse ? » Electronic Thesis or Diss., Paris, AgroParisTech, 2023. http://www.theses.fr/2023AGPT0016.
Texte intégralAssisted migration constitute a possibility to adapt forest ecosystems face to the increase in drought intensity and frequency. However, this strategy requires identification of drought-resistant populations and characterization of the diversity within them. Water use efficiency (WUE) is a key trait to assess for this choice, as it reflects a trade-off between carbon assimilation and water loss through transpiration. By combining dendrochronology and stable isotope analysis, this thesis investigates the effect of WUE on the growth performance and resilience to drought of sessile oak (Quercus petraea).Firstly, WUE was compared among 16 populations whose individuals, from seeds originating from sites along a wide range of pedoclimate gradient, had grown in the common garden Sillegny. Significant differences in WUE were found among these populations, but these differences were not correlated with the pedoclimatic conditions of the sites of origin. However, populations from provenances with sandy soils showed a larger increase in WUE in response to the drought of 2003 (compared to the wet year of 2000) than populations from provenances with silty soils. In addition, trees with higher WUE showed larger radial growth only in wet years. Although these results suggest an adaptation of the sessile oak, reflected by the plasticity of WUE to drought, the variability of WUE within populations was higher compared to the differences among populations.Then, the phenotypic variability of WUE was studied within two populations with contrasting soil and climate conditions, at the Blois (wet) and the Harth (dry) sites. All the trees within each plot were sampled, with a particular focus on the relationship between WUE and radial growth. While stomatal control appeared to be the key factor in inter-annual variations in WUE, the inter-individual (intra-annual) variability in WUE was driven more by net CO2 assimilation, which is strongly affected by tree social status. The intra-annual relationships between WUE and growth appeared more significant as the competition among trees within the stand intensified (particularly when trees become mature), and when light availability became a limiting factor rather than water (in a humid site, at Blois).Finally, the effect of WUE expressed by trees at a young age on growth trajectory was assessed within the Blois and the Harth stands. At the Harth site, trees with higher WUE during their young age were the most dominant in 2021, suggesting selection for higher WUE in dry environment. In contrast, at the Blois site, the effect of WUE at the young age on the social status of the trees ceased after 60 years. The response of trees to drought was not significantly affected by WUE at the young age at the Blois site and only during the first decades at the Harth site. Moreover, the plasticity of WUE to drought might play a diminishing role in the selection process as trees age and were exposed to changing environmental conditions.WUE is a complex trait influenced by multiple factors, including genetics, microenvironmental conditions, and tree age. Given that intra-population variations were more pronounced than differences among populations, and that the relationship between WUE and resilience to drought was tenuous, the selection of drought-adapted sessile oak populations cannot be only based on WUE
Fichtler, Esther [Verfasser], Martin [Akademischer Betreuer] Worbes et Rupert [Akademischer Betreuer] Wimmer. « Ecological information of ring width, stable carbon isotope composition and wood anatomical variables in tropical tree rings - A contribution to dendrochronology in the tropics / Esther Fichtler. Gutachter : Martin Worbes ; Rupert Wimmer. Betreuer : Martin Worbes ». Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2012. http://d-nb.info/1042262241/34.
Texte intégralTriolo, Roberta. « Hierarchy of factors impacting grape berry mass at different scales and its direct and indirect effects on grape and wine composition ». Thesis, Bordeaux, 2016. http://www.theses.fr/2016BORD0336/document.
Texte intégralFinal berry mass is the result of the integrated effect of several factors. They also influence berry composition. The present work was designed to study the simultaneous effect of major factors influencing berry mass and composition, to hierarchize their impact at different scales, to distinguish their direct and indirect effect on berry composition and to compare the profile of wines made from large and small berries. The study was carried out simultaneously on two vineyards located in the Saint Emil ion (France) and Alcamo (Sicily) areas, during 2014 and 2015. On the first site, vines were planted on two soil types, while on the second site two different irrigation treatments were applied. Depending on the scale, some factors homogeneously impacted the berry mass and composition. At the intra-parcel scale, vine water status represented the most impacting factor, while berry seed number did not have significant effect. Opposite results were obtained when the investigation was carried out at the intra-bunch and intra-plant scales. At large scale, factors impacted directly and indirectly berry compounds and grape juices and wines produced from smaller berries were more concentrated. Neither at intra-bunch, nor at intra-plant scales, berry size effect on juice composition was significant. Only anthocyanin concentration was related to berry size at all scales. This fact was particularly obvious in berries produced under limited water conditions. Water deficit increased the skin to flesh ratio, independently of berry size. This means that small and large berries, produced from a single parcel with homogenous water uptake conditions, tend to have similar enological profiles
Denis, Marie. « Mécanismes de solubilisation et transfert de matières organiques dissoutes à l'échelle d'un bassin versant agricole : apport de l'étude de la composition moléculaire ». Thesis, Rennes 1, 2017. http://www.theses.fr/2017REN1S045/document.
Texte intégralDissolved organic matter (DOM), as sources of nutrient or pollutant dissemination pathway are implied in numerous environmental issues. Although DOM have been the subject of numerous studies for several decades, the mechanisms implied for their solubilization and their transport from soils to aquatic systems are still a matter of discussion. Based on DOM molecular composition determined using thermally assisted hydrolysis and methylation –gas chromatography – mass spectrometry (THM-GC-MS), this thesis aims to provide a better understanding of their solubilization and transfer mechanisms at the scale of an agricultural headwater catchment. This work was conducted on the experimental headwater catchment of Kervidy-Naizin (France, Environmental Research Observatory AgrHys) in order to determine the processes implied at two temporal scales. At the scale of a rain event, this work has clarified the impact of hydrological conditions on the DOM dynamics. At annual scale, the use of carbon isotope signature (δ13C) and DOM molecular composition allowed to clarify the DOM transfer mechanisms at the slope scale. The use of THM-GC-MS appears to be a suitable tool for the study of DOM dynamics. The results thus obtained allowed to highlight the role of hydrological conditions and in particular the water-table level in the solubilization and transfer of DOM
Nel, Jacques A. « Vegetation and microbial determinants of soil carbon isotopic composition ». Master's thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/28072.
Texte intégralShelkov, Denis Alexander. « N and C isotropic composition of different varieties of terrestrial diamonds and carbonado ». Thesis, Open University, 1997. http://oro.open.ac.uk/54608/.
Texte intégralBurke, Roger Allen Jr. « Stable Hydrogen and Carbon Isotopic Compositions of Biogenic Methanes ». Scholar Commons, 1985. https://scholarcommons.usf.edu/etd/7658.
Texte intégralBuckingham, Sarah. « Dissolved Organic Carbon In Topsoils : Concentration,Flux and Isotopic Composition ». Thesis, Lancaster University, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.531683.
Texte intégralYates, Paul David. « The content and stable isotopic composition of carbon in spherical micrometeorites ». Thesis, Open University, 1992. http://oro.open.ac.uk/54849/.
Texte intégralLaunois, Thomas. « Modélisation de la composition isotopique des cernes d'arbres (13C et 18O) et des transferts de COS entre l'atmosphère et la biosphère continentale pour quantifier les flux bruts de carbone ». Thesis, Versailles-St Quentin en Yvelines, 2014. http://www.theses.fr/2014VERS0039/document.
Texte intégralIn the context of global climate change, the behavior of the terrestrial biosphere can be durably affected by the increased frequency and intensity of extreme climatic events, which can decrease the photosynthetic assimilation of carbon and/or increase the respiration rate of the ecosystems. Therefore, quantifying the carbon storage capacity of the ecosystems and predicting their sensitivity to climate changes strongly rely on our capacity to separately estimate the photosynthesis and respiration rates at different scales. The gross primary productivity (GPP) is however not directly measurable. Indirect approaches have been proposed to estimate the biospheric gross fluxes (GPP and respiration), combining for instance stable isotopologues of CO2 (13C and 18O), and, more recently, the measure of carbonyl sulfide (COS) concentrations in the atmosphere. In this context, my PhD work followed two complementary approaches. In the first approach, isotopic measurements and tree-ring widths were used, because both of them are linked to the photosynthetic activity. The inter-annual variations of the photosynthetic fluxes simulated with the ORCHIDEE continental biosphere model were evaluated and compared with in situ measurements. The second approach consisted in using atmospheric measurements of OCS concentrations and in exploring their potential to constrain the current estimates of the GPP in dynamic global vegetation models (DGVM), by (1) establishing a new global budget of sources and sinks of this gas, (2) optimizing the source and sink terms of this cycle and (3) estimating the potential of this new tracer to validate/invalidate the simulated GPP when using current DGVMs
Lockheart, Matthew James. « Isotope compositions and distributions of individual compounds as indicators for environmental conditions : comparisons between contemporary and Clarkia fossil leaves ». Thesis, University of Bristol, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.389098.
Texte intégralBonne, Jean-Louis. « Observations continues de la composition atmosphérique au sud Groenland ». Electronic Thesis or Diss., Versailles-St Quentin en Yvelines, 2015. http://www.theses.fr/2015VERS008V.
Texte intégralSouth Greenland is a key region placed under Arctic and Northern Atlantic influences, whichis poorly documented in terms of atmospheric monitoring. The aim of my thesis is to conductand use the first regional atmospheric observations of CO2, O2, CH4 and isotopic compositionof water vapour and precipitation performed in Ivittuut, a coastal site in south-west Greenland.Which information can we infer from these atmospheric observations, in terms of localatmospheric processes and large scale atmospheric transport variations? Can we use these observationsto document the surface-air exchanges of these compounds, which represent an importantpart of the water and carbon biogeochemical cycles?After validating the observations regarding international precision recommandations, I havebeen able to analyse the variabilities at different time scales, resulting from different specificprocesses. This highlighted the fact the atmospheric composition of our site is weakly influencedby local processes, either for local greenhouse gases sources or small scale atmosphericvariations affecting water vapour isotopic composition. This facilitates the interpretation of ourobservations in terms of large scale atmospheric transport signals.To better understand the observed variations, I related our data series with other observationsoriginating from different sites, and with outputs from different atmospheric models. Ihave first witnessed the links between variations of atmospheric composition and large synopticscale atmospheric transport changes. Then, I have identified the spatial representativity of ourobservations and contributed to the evaluation of atmospheric models. The case study of astrong heat wave covering Greenland during summer 2012 allowed me to study the transport ofwater vapour within an air mass between different stations. It allowed me to provide the firstexperimental observation of deuterium excess conservation during atmospheric transport.Finally, combining observations and atmospheric simulations, I have documented surfaceairexchanges of the observed compounds: first by the attribution of observed values of CH4and water vapour isotopic composition to their simulated potential origins, secondly by thecomparison of observed variations with the direct simulation of atmospheric transport of eitherCH4 sources estimated from inventories or simulated CO2 and O2 air-sea fluxes from an oceanmodel
Kanpanon, Nicha. « La composition isotopique en carbone est-elle un indicateur écophysiologie pertinent de l’efficience d’utilisation de l’eau de l’hévéa ? » Thesis, Université de Lorraine, 2015. http://www.theses.fr/2015LORR0240/document.
Texte intégralThe rubber (Hevea brasiliensis) plantations extend to non-traditional area in Thailand where dryer conditions has been reported to impair the growth of rubber trees and latex production. Physiological parameters helpful for breeding adapted genotypes are required, such as water use efficiency (WUE). Carbon isotope discrimination is widely used as a proxy for WUE that can easily be used for selection and breeding programs for drought tolerance. Leaf δ13C and leaf gas exchange were measured on young saplings of 10 rubber clones growing in pot in a common garden. The range of leaf δ13C among 10 clones was narrow and the correlation between δ13C and WUEi was significant under high vapour pressure deficit only, which means the prediction of WUE by δ13C would have low precision. There were large δ13C variations among the genotypes at all seasons in a collection of 49 wild genotypes of rubber in Northeastern Thailand. δ13C was rather stable with a good correlation between rainy and dry season. The genetic variability of δ13C is promising for breeding if a good correlation between δ13C of leaf and WUE can be established. The lack of correlation between δ13C of latex (δ13C-L) and of leaf soluble compounds (δ13C-S) collected from tapped and untapped 20 year-old rubber trees suggests that recent photosynthates are mixed in the large pool of stored carbohydrates that are involved in latex regeneration after tapping. Thus δ13C of latex is not a relevant indicator of WUE of rubber trees
Murray, Andrew P. « Factors controlling the abundance and carbon isotopic composition of land-plant derived compounds in crude oils ». Thesis, Curtin University, 1998. http://hdl.handle.net/20.500.11937/1100.
Texte intégralRieley, Gareth. « Molecular and isotropic studies of natural environments : distributions and stable carbon isotopic compositions of individual lipids ». Thesis, University of Bristol, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.385652.
Texte intégralLaunois, Thomas. « Modélisation de la composition isotopique des cernes d'arbres (13C et 18O) et des transferts de COS entre l'atmosphère et la biosphère continentale pour quantifier les flux bruts de carbone ». Electronic Thesis or Diss., Versailles-St Quentin en Yvelines, 2014. http://www.theses.fr/2014VERS0039.
Texte intégralIn the context of global climate change, the behavior of the terrestrial biosphere can be durably affected by the increased frequency and intensity of extreme climatic events, which can decrease the photosynthetic assimilation of carbon and/or increase the respiration rate of the ecosystems. Therefore, quantifying the carbon storage capacity of the ecosystems and predicting their sensitivity to climate changes strongly rely on our capacity to separately estimate the photosynthesis and respiration rates at different scales. The gross primary productivity (GPP) is however not directly measurable. Indirect approaches have been proposed to estimate the biospheric gross fluxes (GPP and respiration), combining for instance stable isotopologues of CO2 (13C and 18O), and, more recently, the measure of carbonyl sulfide (COS) concentrations in the atmosphere. In this context, my PhD work followed two complementary approaches. In the first approach, isotopic measurements and tree-ring widths were used, because both of them are linked to the photosynthetic activity. The inter-annual variations of the photosynthetic fluxes simulated with the ORCHIDEE continental biosphere model were evaluated and compared with in situ measurements. The second approach consisted in using atmospheric measurements of OCS concentrations and in exploring their potential to constrain the current estimates of the GPP in dynamic global vegetation models (DGVM), by (1) establishing a new global budget of sources and sinks of this gas, (2) optimizing the source and sink terms of this cycle and (3) estimating the potential of this new tracer to validate/invalidate the simulated GPP when using current DGVMs
Bonne, Jean-Louis. « Observations continues de la composition atmosphérique au sud Groenland ». Thesis, Versailles-St Quentin en Yvelines, 2015. http://www.theses.fr/2015VERS008V/document.
Texte intégralSouth Greenland is a key region placed under Arctic and Northern Atlantic influences, whichis poorly documented in terms of atmospheric monitoring. The aim of my thesis is to conductand use the first regional atmospheric observations of CO2, O2, CH4 and isotopic compositionof water vapour and precipitation performed in Ivittuut, a coastal site in south-west Greenland.Which information can we infer from these atmospheric observations, in terms of localatmospheric processes and large scale atmospheric transport variations? Can we use these observationsto document the surface-air exchanges of these compounds, which represent an importantpart of the water and carbon biogeochemical cycles?After validating the observations regarding international precision recommandations, I havebeen able to analyse the variabilities at different time scales, resulting from different specificprocesses. This highlighted the fact the atmospheric composition of our site is weakly influencedby local processes, either for local greenhouse gases sources or small scale atmosphericvariations affecting water vapour isotopic composition. This facilitates the interpretation of ourobservations in terms of large scale atmospheric transport signals.To better understand the observed variations, I related our data series with other observationsoriginating from different sites, and with outputs from different atmospheric models. Ihave first witnessed the links between variations of atmospheric composition and large synopticscale atmospheric transport changes. Then, I have identified the spatial representativity of ourobservations and contributed to the evaluation of atmospheric models. The case study of astrong heat wave covering Greenland during summer 2012 allowed me to study the transport ofwater vapour within an air mass between different stations. It allowed me to provide the firstexperimental observation of deuterium excess conservation during atmospheric transport.Finally, combining observations and atmospheric simulations, I have documented surfaceairexchanges of the observed compounds: first by the attribution of observed values of CH4and water vapour isotopic composition to their simulated potential origins, secondly by thecomparison of observed variations with the direct simulation of atmospheric transport of eitherCH4 sources estimated from inventories or simulated CO2 and O2 air-sea fluxes from an oceanmodel
Murray, Andrew P. « Factors controlling the abundance and carbon isotopic composition of land-plant derived compounds in crude oils ». Curtin University of Technology, Centre for Petroleum and Environmental Organic Geochemistry, 1998. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=10771.
Texte intégralSoutheast Asia. However, small amounts of bicadinanes were found in an oil from outside the paleogeographic range of the dipterocarp family, indicating a more general source. Retention indices based on the regular hopane series were calculated for the main bicadinane and methyl bicadinane isomers and for a group of oleanoid triterpanes.Source rock depositional setting proved to be the primary control on the shape of the n-alkane isotope profile, with negatively sloping curves being characteristic of fluvio-deltaic and marginal lacustrine oils and flat or positively sloping curves typical of marine oils. The difference is probably related to the bacterial reworking of higher plant matter in the fluvio-deltaic environment. A slight isotopic anomaly at n-C(subscript)17 correlates with the abundance of algal-derived steranes and may indicate a minor marine contribution to the source of an fluvio-deltaic oil. A study of sediments from the South Sumatra Basin and New Zealand showed that the n-alkane isotope profile is determined mainly by source matter type and is little influenced by thermal maturity or depositional environment.Based on the results of the work described above, three aspects were chosen for further examination. These were: a) the factors controlling the carbon isotopic composition of n-alkanes and of resin-derived compounds in terrigenous oils; b) the influence of source, maturity and biodegradation on the abundance of bicadinanes, especially the effect of maturity on the isomer distribution, and c) the factors controlling the abundance of oleananes and rearranged oleananes in oils and Ancient sediments, especially the role of depositional environment.A preliminary study using sediments, from the Visayan Basin (Philippines) showed the bicadinane isomeric distribution to be sensitive to maturity. This suggested new maturity parameters which would be ++
resistant to even severe biodegradation and largely immune to interference from diagenetic effects. A more detailed study of a marine-fluvio-deltaic depositional sequence from the South Sumatra Basin confirmed that the maturity indices based on bicadinanes and aromatic analogs were less subject to non-maturity influences than those based on the steranes and aromatic hydrocarbons. The values obtained for the bicadinane indices were compared with the maturity required for oil generation as estimated by kinetic modelling and with conventional maturity indicators such as sterane epimerisation and the methyl phenanthrene index. Values for several of the indices were also measured for 17 Tertiary-age oils from Southeast Asia, Papua New Guinea, New Zealand and Australia. The main bicadinane maturity indicator (BMI-1) continues to change into the oil window and hence is useful in ranking the relative maturity of oils as well as sediments. Values of BMI-1 for two oils having unusually low sterane maturities were found to be normal and, in the light of this observation, the conventional explanation for low sterane epimerisation of many Tertiary-age oils was critically evaluated.The oleananes, as markers for the angiosperms, provide valuable source and age information when present in an oil. Nevertheless, their abundance is not quantitatively related to the land plant input and indeed their presence results from a small "leak" in diagenetic processes leading primarily to aromatic oleanoids. Evidence is presented that contact of plant matter with seawater during early diagenesis enhances the expression of oleananes in a mature sediment or oil. Oleananes are absent or present at very low concentrations in samples from the base of an Eocene coal seam affected by post-depositional seawater intrusion. However, their abundance increases toward the top of the seam in correlation with ++
% organic sulphur, dibenzothiophene/phenanthrene and the homohopane index. Similarly, in deltaic sediments from the South Sumatra Basin, oleanane/hopane is strongly correlated with indicators of marine influence such as C[subscript 27]/C[subscript 29] steranes and of oxic/anoxic conditions such as the homohopane index. In each case, increasing oleanane abundance is accompanied by a reduction in the extent of aromatisation and, for the South Sumatra Basin, the proportion of A-ring contracted oleananes. An angiosperm-derived Miocene coal from the Philippines, deposited under freshwater conditions, shows abundant aromatic oleanoids but no oleananes. These results show that oleananes need to be used with caution as age and source markers in fluvio- deltaic and lacustrine petroleum systems. On the other hand, their sensitivity to early diagenetic conditions may make them useful in locating effective source rocks in such systems.Compounds derived from plant resins are major components of some terrigenous oils. Although recent studies have elucidated the molecular structure of resinites, very little information was available on the carbon isotope composition of resinites prior to the present study. No carbon isotope studies of resin-derived compounds in oils had been performed. Hence, carbon stable isotope analyses were carried out on a set of modern and fossil resins of diverse origins and compound specific isotope analysis was used to characterise individual hydrocarbons in resin pyrolysates and oils derived from resinitic source matter. The results showed that "Class V' resinites derived from gymnosperms are enriched in the heavy carbon isotope compared with the angiosperm-derived "Class W' resinites. Furthermore, both the fossil resinites themselves and individual hydrocarbons derived from them are isotopically heavy compared with modern plant resins. The reasons for ++
these differences and their implications for petroleum geochemical studies are discussed.
Perga, Marie-Elodie. « Origines et flux de carbone en lacs : étude par analyse de la composition en isotopes stables du carbone et de l'azote du zooplancton et des poissons ». Chambéry, 2004. http://www.theses.fr/2004CHAMS031.
Texte intégralFish communities occupy the top of food chains. How fish obtain their constitutive carbon depends consequently of all the carbon pathways at the downer levels of the food web. This trophic position confers to fish a potential role of integrators of the underlying processes, at the ecosystem scale. Moreover, stable isotopes composition of an organism depends on all the pathways that transfer carbon up to this organism. Consequently, we wondered in what extent the stable isotopes composition of fish could be a proxy of the trophic functioning of lakes. To address this assumption, whitefish, Coregonus lavaretus, a zooplanktivorous salmonid common in alpine lake, was, in a first time, used as biological model. A preliminary study had revealed the stable isotope composition of whitefish was quite variable among alpine lakes. According to our idea, this variability mirrors differences in the carbon pathways of the food web of these lakes. To understand what was reflected by this variability, we studied initially in what extent it resulted from intrinsic factors (such as lake size or trophic status). This study has then lead us to deepen the role played by the zooplankton compartment in carbon pathways up to Whitefish. In the final stage of this first part, the isotopic composition of whitefish appeared as a proxy for lake trophic functioning. Changes in environmental factors can alter carbon pathways in food webs. If fish are efficient integrators of carbon pathways, impacts of perturbations should be mirrored on their isotopic compositions. Impacts of two anthropogenic perturbations of stable isotope composition of fish were then evaluated : the first one relates to eutrophication - restoration of two alpine lakes, the second one to water levels changes in two Malian reservoirs. Results from these two studies reveal that major changes, ensuing from these perturbation, in carbon origins and fluxes within lake food webs are recorded in the isotopic history of fish communities
Berry, Stephanie C. Carleton University Dissertation Biology. « The influence of vegetation and soil carbon dioxide exchange on the concentration and isotopic composition of atmospheric carbon dioxide within plant canopies ». Ottawa, 1994.
Trouver le texte intégralColeman, Joanna Michelle. « Controls on the distribution and carbon isotopic composition of archaeal biomarkers in organic-rich and methanogenic marine sediments ». Thesis, University of Bristol, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.416770.
Texte intégralWan, Zhenzhu. « Stable Carbon and Nitrogen Isotopic Studies of Devonian Land Plants -- An Indicator of Paleoclimate and Paleoenvironmental Changes ». University of Cincinnati / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1343068259.
Texte intégralWestgate, Timothy David. « Compositional and carbon isotopic characteristics of abiogenically derived hydrocarbons at the Kidd Creek Mine, Timmins, Ontario ». Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0013/MQ40763.pdf.
Texte intégralTarits, Corinne. « Etude des variations de composition isotopique du carbone et de l'oxygène dans le domaine de la précipitation spontanée homogène du carbonate de calcium : modélisation du comportement isotopique du carbone dans ce domaine ». Paris 5, 1990. http://www.theses.fr/1990PA05P617.
Texte intégralCarvajal-Ortiz, Humberto. « Carbon isotopic composition of plant-derived organic matter in tropical sedimentary sequences as a recorder of Late Cretaceous-Early Paleogene changes in the carbon cycle ». [Ames, Iowa : Iowa State University], 2007.
Trouver le texte intégralPearce, Andrew M. « Carbon and oxygen isotopic compositions of some late Proterozoic and early Cambrian carbonates in the southern Adelaide geosyncline / ». Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bp359.pdf.
Texte intégral"National grid reference: Noarlunga SI (54-4) 6627 IV Cassini SI (53-16) 6326 I Stokes Bay SI (53-16) 6326 IV." Includes bibliographical references.
Zakharova, Anna. « Soil organic matter dynamics : influence of soil disturbance on labile pools ». Thesis, University of Canterbury. School of Biological Sciences, 2014. http://hdl.handle.net/10092/9944.
Texte intégralZymela, Steve. « Carbon, oxygen and strontium isotopic composition of diagenetic calcite and siderite from the Upper Cretaceous Cardium formation of western Alberta ». Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/NQ30184.pdf.
Texte intégralZymela, Steve. « Carbon, oxygen and strontium isotopic composition of diagenetic calcite and siderite from the Upper Cretaceous Cardium Formation of Western Alberta / ». *McMaster only, 1996.
Trouver le texte intégralGangloff, Sophie. « Evaluation of the mechanisms of trace elements transport (Pb, Rare Earth Elements,... ) and the elemental and isotopic fractionation (Ca and Sr) at the interface water-soil-plant ». Thesis, Strasbourg, 2016. http://www.theses.fr/2016STRAH002/document.
Texte intégralThis work is focused on the study of a profile of soil and soil solutions collected on an experimental plot covered with spruce. All these samples come from the watershed of the Strengbach (environment - OHGE Hydrogeochimique Observatory), were sampled at different depths (5, 10, 30 and 60 cm) and during the period between 2009 and 2013. Characterizations of soil extracts by infrared spectroscopy allowed to highlight changes in the organic functional groups with depth and that these changes have a significant impact on the behaviour of the cations (major and trace) in the soil. Ultrafiltration experiments helped to identify flows of colloidal and dissolved organic carbon as well as those of the major and trace-element present in soil solutions. The joint use of isotope tracers (87Sr / 86Sr and δ44 / 40 Ca) and chemical (Rare Earth Elements) have highlighted processes taking place at the water-soil-plant interface, as the uptake by root or soil alteration
Grice, Kliti. « Distributions and stable carbon isotopic compositions of individual biological markers from the Permian Kupferschiefer (Lower Rhine Basin, N.W. Germany) ». Thesis, University of Bristol, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.283943.
Texte intégralJansen, Kirstin. « Stable Isotopes and Metabolite Profiles as Physiological Markers for the Drought Stress Sensitivity in Douglas-Fir Provenances (Pseudotsuga menziesii (MIRB.) FRANCO) ». Doctoral thesis, Humboldt-Universität zu Berlin, 2018. http://dx.doi.org/10.18452/19617.
Texte intégralIn Central Europe, more frequent periods of dry and hot weather are expected in the future with economic losses in the forestry sector. Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) is discussed as a timber species alternative to the economically important but drought-sensitive spruce (Picea abies (L.) H. Karst.). Two subspecies, the coastal (FDC) and the interior Douglas-fir (FDI), are native to an extensive natural range in North America, offering a great potential for the selection of productive and drought tolerant provenances. Our goal was to investigate the drought response of different Douglas-fir provenances on the morphological and physiological level, as well as the mechanisms underlying drought resistance or susceptibility. A provenance trial in southwestern Germany established in 1958 allowed the study of 50-year-old Douglas-fir trees of diverse provenances along a height gradient. Under controlled conditions, we simulated the effects of a heat wave on young trees of two provenances. We analyzed carbon and oxygen stable isotopic composition, leaf gas exchange, changes in metabolism and tree growth. FDC from humid regions responded to drought with strong growth decline and a medium to strong stomatal closure, supported by enhanced instantaneous photoprotection. FDC from regions with very dry summer conditions showed a small growth decline and anisohydric regulation of stomatal conductance under drought, supported by high levels of osmotic adjustment. High monoterpene emissions might contribute to the drought resistance. FDI from an arid region showed high assimilation rates, low growth potential and a high antioxidant, photoprotective, drought and heat protective potential. The provenances differ greatly in their dry reaction and their protective mechanisms. The cultivation of drought resistant crops will be beneficial at sites predicted to accumulate arid summer periods.
Bouyer, Laure. « Impact de la disponibilité en nutriments sur le fonctionnement hydrique et carboné de peupliers dans des contextes de sécheresse variés ». Thesis, Orléans, 2019. http://www.theses.fr/2019ORLE3100.
Texte intégralThe availability of water and nutrients are two main factors limiting tree growth and forest productivity. Despite the strong legacy of research on forest nutrition, the role of nutrients in modulating tree drought responses remains largely unknown. This thesis aimed to evaluate the role of nutrient availability on key traits related to water and carbon relations such as growth and its determinants, water-use efficiency (WUE), vulnerability to cavitation, or non-structural carbohydrate (NSC) contents, in poplars under contrasting drought intensities. Research experiments relied on two complementary experimental designs, one in a greenhouse and the other in an outdoor common garden, and considered a maximum of four genotypes primarily selected for their contrasting growth and stomatal regulation. The main findings are as follows: 1) a higher nutrient availability increases growth and WUE under moderate drought, 2) a higher nutrient availability does not necessarily increase the risk of xylem hydraulic failure, 3) NSC depletion, in particular starch, co-occurs with massive xylem embolism under lethal drought, and 4) a higher nutrient availability reduces NSC storage, especially under moderate drought. This study shows for the first time the temporal covariance between the dynamics of xylem hydraulic failure and carbon starvation in a fast-growing but highly vulnerable tree species, and gives an example of how these relationships are modulated by nutrient availability
Melo, Antonio Willian Flores de. « Avaliação do estoque e composição isotópica do carbono do solo no Acre ». Universidade de São Paulo, 2004. http://www.teses.usp.br/teses/disponiveis/91/91131/tde-29072004-160525/.
Texte intégralThe State of Acre is located in the extreme west of Brazil, occupying an area that had great geological influence from the mountain chain of Andes. The soils present pedologic characteristics very different from the ones found in the remaining of Brazilian Amazon, prevailing Inceptisols, Alfisols, and Ultisols, generally eutrophic, young and little weathered. Not much is known about the impact of the use of the earth on the organic matter in these soil conditions. This work had as objectives to estimate the stock of carbon of the main classes of soils of the State of Acre and to compare with studies carried out for the Amazon area. To evaluate the effect of the change in the use and covering of the earth on the stock of carbon and isotopic composition of the organic matter in two soil conditions in Acre. To reach the objectives the work was performed in two scales, local and regional. The first case estimated the stocks of carbon up to one meter deep, using a map of soils in the scale 1:1.000.000 and analytic data of pedologic profiles accomplished in the area. The second case determined the concentration of carbon, d13C and density of the soil of samples collected at 12-15, 20 year-old pasture lands, and forest in the depths 0-5, 5-10, 10-20, 20-30, 30-40, 50-60, 70-80 e 90-100 cm, in Ultisols (well drained) and Alfisols (poorly drained). The soils of Acre store around 1 Pg of carbon in the first meter of depth, around 75% of this value is concentrated on the first 30 cm. The soils of Acre present smaller concentration of carbon (6.5 kg m-2, average) when compared with the average of the soils of the Amazon, although they present better fertility. The main reason for this result is the large rate of incident decomposition on these soils due to the constant drought cycles and moistening. These cycles are associated with the physical characteristics (mainly structure) incipient of these soils that impede the percolation of the pluvial waters saturating very quickly and favoring superficial flow off. As the water concentrates on the surface of the soil, it tends to evaporate easily. The effect of the change in the covering and land use on stock and dynamics of the organic matter of the soils happens differently in Ultisols (well drained) and Alfisols (poorly drained). In the two conditions of soils there was a tendency to decrease the total stock of carbon and increase carbon of C4 origin, however, in Ultisols it was very stressed. Pasture lands on Alfisols presented larger stock of carbon (average of 8.4 kg m-2 to 1 m), however, the data of d13C showed that most of carbon was remaining of the forest and a small proportion was introduced by the pasture land (< 40 % to 0-5 cm in 20 yr old pasture). The inverse fact occurred with pasture lands on Ultisols that presented smaller stock (average of 6.4 kg m-2 to 1 m) and great proportion of carbon of the pasture land (> 70 % to 0-5 cm in 20 yr old pasture). This result suggests two conclusions. 1) the rate of carbon decomposition in Alfisols is smaller than in Ultisols, and the time of residence of the organic matter is larger. Ultisols tend to lose carbon more readily with the change in the land use and covering of the land. 2) pasture productivity is low on Alfisols, indicating that besides soil fertility other characteristics, as structure, should be considered in order to establish the management practice to obtain the best output from the grass.
Brandon, Margaux. « Les changements majeurs de la productivité biologique au cours du Quaternaire et leurs impacts sur les cycles du carbone et de l’oxygène ». Thesis, université Paris-Saclay, 2020. http://www.theses.fr/2020UPASJ010.
Texte intégralDuring glacial-interglacial cycles of the Quaternary, the atmospheric CO₂ (pCO₂) concentration is associated with important variations, in particular during transitions between glacial and interglacial periods, also called terminations, with increases of up to 100 ppm of pCO₂ in a few thousand years. While the roles of oceanic circulation and sea-ice cover on pCO₂ are studied for several years now, little is known on the impact of biological productivity. The goal of this thesis is to reconstruct the past changes in biological productivity and to estimate their contributions on atmospheric pCO₂ variations over the last 800 000 years (ka), with particular attention to Termination V (~425 ka) and Marine Isotope Stage (MIS) 11, the interglacial period around 400 ka. Two different approaches were combined to reconstruct global and local variations of biological productivity. Measurements of Δ¹⁷O of O₂ in the air trapped in the Antarctic EPICA Dome C ice core between 400 and 800 ka allowed to complete the pre-existing record and trace back variations of global biosphere productivity expressed in oxygen fluxes over the past 800 ka. Micropaleontological (coccoliths, foraminifera) and geochemical (TOC, CaCO₃, XRF) analyses were performed on a sediment core of the Indian sector of the Southern Ocean (MD04-2718) to reconstruct the changes in biological pump efficiency over the past 800 ka. The results obtained during this thesis showed that, at the scale of glacial-interglacial cycles, global biospheric productivity and Southern Ocean carbonate production are more important during interglacial periods compared to glacial periods, minimizing the impact of marine organic productivity on atmospheric pCO₂. Termination V and MIS 11 register the strongest biosphere productivity of the past 800 ka and the highest marine carbonate production of the past 9 interglacial periods in the Southern Ocean. While the important carbonate production is a source of CO₂ for the atmosphere, the rise in biosphere productivity would counterbalance the increase in pCO₂ through photosynthesis
劉, 衛., Wei LIU, 純. 森泉, Jun MORIIZUMI, 弘実 山澤, Hiromi YAMAZAWA, 孝夫 飯田 et Takao IIDA. « Depth Profiles of Radiocarbon and Carbon Isotopic Compositions of Organic Matter and CO_2 in a Japanese Forest Area((2)Summaries of Research Using AMS) ». 名古屋大学年代測定資料研究センター, 2006. http://hdl.handle.net/2237/13664.
Texte intégralLicari, Laetitia. « Ecological preferences of Benthic Foraminifera in the Eastern South Atlantic : distribution patterns, stable carbon isotopic composition, and paleoceanographic implications = Ökologische Ansprüche benthischer Foraminiferen im östlichen Südatlantik / ». Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2006. http://www.gbv.de/dms/bs/toc/514912308.pdf.
Texte intégralChiapini, Mariane. « Genesis and organic matter chemistry of sombric horizons in subtropical soils (Paraná State, Brazil) ». Universidade de São Paulo, 2017. http://www.teses.usp.br/teses/disponiveis/11/11140/tde-18052017-184016/.
Texte intégralA matéria orgânica do solo (MOS) desempenha um papel importante no ciclo global do carbono. Portanto, é importante entender a estabilidade da MOS, que está relacionada a vários processos. As suas propriedades intrínsecas podem estar relacionadas com a sua estabilidade, por exemplo, o \"black carbon\" é considerado relativamente resistente à degradação. Na maioria dos solos, os horizontes escuros coincidem com as camadas ou horizontes superficiais devido ao maior acúmulo de matéria orgânica, mas nos estados do sul do Brasil, a presença de solos com horizontes subsuperficiais escurecidos é frequentemente observada. O horizonte subsuperficial escurecido destes solos assemelha-se a um horizonte sômbrico. Aspectos sobre sua origem, formação e preservação ainda não foram totalmente elucidados. O objetivo deste trabalho é compreender a formação de horizontes \'sômbricos\' em solos da região de Tijucas do Sul (Paraná, Brasil). Foram descritos e coletados cinco perfis de solo, dos quais três estão localizados em uma topossequência e continham um horizonte similar ao sômbrico (P1-P3), um solo de referência representativo da área (P5) e um solo intermediário (P4) que apresentou uma morfologia entre o solo de referência e os solos com horizonte \'sômbrico\'. Para este fim, a MOS foi estudada pela sua composição molecular através da técnica de pirólise acoplada à cromatografia gasosa e espectrometria de massa (pirólise-GC-MS). Além disso, estudou-se a composição isotópica 13C (δ 13C) e a composição fitolítica, a fim de compreender as condições paleoclimáticas que foram relacionados com as condições ambientais passadas usando técnicas de datação com 14C, e suportados pelas análises clássicas de solo. As amostras dos horizontes foram submetidas ao fracionamento químico MOS, gerando duas frações: fração extraível com NaOH (EXT) e resíduo (RES). A morfologia dos perfis mostrou uma intensa atividade biológica nos horizontes A e uma ampla distribuição de microfragmentos de carvão. Observouse também a continuidade lateral de horizontes \'sômbricos\' em solos da topossequência (P1-P3), diferenciando-os dos horizontes A enterrados. A distribuição da MOS nas frações estudadas pela pirólise foi a mesma para os cinco perfis: EXT> RES. Os produtos relacionados a incêndios florestais como os poliaromáticos (PAHs, BC) foram encontrados em todos os perfis, mas em maior abundância relativa nos horizontes sômbricos, indicando uma maior incidência de incêndio durante a formação destes horizontes. Os PAHs podem estar relacionados com a manutenção da cor escura dos horizontes \'sômbricos\'. Em relação às condições paleoclimáticas observou-se que os horizontes subsuperficiais escurecidos foram desenvolvidos durante o Holoceno Médio sob vegetação composta principalmente por gramíneas C4 com arbustos, evidenciando um clima mais seco correspondente a maior incidência de incêndio.
Kallel, Nejib. « Variation de la composition isotopique de l'oxygène et du carbone des foraminifères : traceur de la circulation océanique pendant le dernier maximum glaciaire et lors de la dernière déglaciation ». Paris 11, 1988. http://www.theses.fr/1988PA112124.
Texte intégralOxygen and carbon isotopic composition of benthic foraminifera from different oceanic sediment cores have been used to reconstruct the pattern of intermediate and deep ocean circulation during last glacial maximum (18,000 years BP) in the Indian and Pacifie oceans. Results show that the glacial oceanic circulation was significantly different from the modern one. A deep hydrological front separated intermediate water of the Indian and Equatorial Pacifie from underlying deep water. Glacial intermediate water was weil ventilated and has approximately the same temperatures than today. By contrast, glacial deep water was cooler by severa!degrees than modern one. In the Pacifie ocean, deep water was more ventilated than that in the Southern Indian ocean indicating the formation of relatively ventilated deep water in the South Pacifie or the increase of the influence of the North Pacifie Intermediate Water. As late as 12,500 yr BP deep oceanic circulation was similar to the glacial one. The decrease of the influence of the North Pacific Intermediate Water has appeared at about 12,500 yr BP and the onset of the active formation of the North Atlantic Deep Water has appeared at about 9,000 yr BP. Holocene conditions have been reached at about 8,000 yr BP in ali oceans and at ali water depths
Tarantola, Alexandre. « Les mécanismes rédox contrôlant la chimie du carbone dans les fluides de l'anchi-métamorphisme : composition des paléofluides, géochimie isotopique, cristallochimie des minéraux phylliteux dans la partie externe des alpes centrales (Suisse) ». Nancy 1, 2005. http://www.theses.fr/2005NAN10163.
Texte intégralThis works characterizes the mechanisms at which occurs the transition between CH4- and H2O- dominated fluid zone in the anchi-metamorphic rocks of the External part of Central Alps, Switzerland. Fluid inclusion trapped in fibre quartz during crack-and-seal mechanism record increasing metamorphic conditions during Alpine orogene. The end of the CH4-zone is characterized by a marked increase of CO2 at 270 ± 5°C. The decrease of CH4 and CO2 in the H2O-zone is contemporaneous with presence of calcite, totally filling Alpine fissures. Isotopic fractionation (delta13C) between methane and calcite is in agreement with homogenisation temperatures of fluid inclusion. DeltaD(H2O) and delta13C(CO2) values of fluid inclusions at the end of the CH4-zone characterise methane oxidation. In agreement with Mössbauer spectroscopy and EELS analyses, neoformation of chlorite and muscovite from detrital biotite is considered as the Fe-reduction driving force of the oxidation of fluid
Aboglila, Salem Abdulghni-O. « Organic and isotopic geochemistry of source-rocks and crude oils from the East Sirte Basin (Libya) ». Thesis, Curtin University, 2010. http://hdl.handle.net/20.500.11937/2118.
Texte intégralSun, Shuwen [Verfasser], Gesine [Akademischer Betreuer] Mollenhauer, Gesine [Gutachter] Mollenhauer et Tommaso [Gutachter] Tesi. « Characterization of terrestrial organic carbon in the Amazon System : insights from biomarkers and their isotopic composition (Delta-C-13 and Delta 14C) / Shuwen Sun ; Gutachter : Gesine Mollenhauer, Tommaso Tesi ; Betreuer : Gesine Mollenhauer ». Bremen : Staats- und Universitätsbibliothek Bremen, 2018. http://d-nb.info/1163012912/34.
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