Littérature scientifique sur le sujet « Cycle de carbone »
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Articles de revues sur le sujet "Cycle de carbone"
Bailly, Sean. « Un cycle en pur carbone ». Pour la Science N° 504 - octobre, no 10 (10 janvier 2019) : 9b. http://dx.doi.org/10.3917/pls.504.0009b.
Texte intégralFriedlingstein, Pierre, Laurent BOPP et Patricia CADULE. « Changement climatique et cycle du carbone ». La Météorologie 8, no 58 (2007) : 21. http://dx.doi.org/10.4267/2042/18204.
Texte intégralBard, Édouard, et Richard Sempéré. « Le cycle du carbone dans l’océan ». La lettre du Collège de France, no 40 (2 septembre 2015) : 38–39. http://dx.doi.org/10.4000/lettre-cdf.2102.
Texte intégralSchlamadinger, Bernhard, Lorenza Canella, Gregg Marland et Josef Spitzer. « Bioenergy strategies and the global carbon cycle. / Stratégies bioénergétiques et cycle global du carbone ». Sciences Géologiques. Bulletin 50, no 1 (1997) : 157–82. http://dx.doi.org/10.3406/sgeol.1997.1951.
Texte intégralJonas, KOALA, KAGAMBEGA O. Raymond et SANOU Lassina. « Distribution des stocks de carbone du sol et de la biomasse racinaire dans un parc agroforestier à Prosopis africana (Guill., et Rich.) Taub au Burkina Faso, Afrique de l’Ouest ». Journal of Applied Biosciences 160 (30 avril 2021) : 16482–94. http://dx.doi.org/10.35759/jabs.160.5.
Texte intégralViovy, Nicolas, et Nathalie de Noblet. « Coupling water and carbon cycle in the biosphere. / Couplage du cycle de l'eau et du carbone dans la biosphère ». Sciences Géologiques. Bulletin 50, no 1 (1997) : 109–21. http://dx.doi.org/10.3406/sgeol.1997.1948.
Texte intégralMavouroulou Quentin, Moundounga, Ngomanda Alfred et Lepengue Nicaise Alexis. « Etat des Lieux des Incertitudes Liées à l’Estimation de la Biomasse des Arbres (Revue Bibliographique) ». European Scientific Journal, ESJ 19, no 6 (28 février 2023) : 60. http://dx.doi.org/10.19044/esj.2023.v19n6p60.
Texte intégralSéférian, Roland, Matthias Rocher, Nicolas Metzl et Philippe Ciais. « Évolution récente du cycle du carbone planétaire : facteurs humains et naturels ». La Météorologie 8, no 93 (2016) : 3. http://dx.doi.org/10.4267/2042/59931.
Texte intégralDOLLÉ, J. B., J. AGABRIEL, J. L. PEYRAUD, P. FAVERDIN, V. MANNEVILLE, C. RAISON, A. GAC et A. LE GALL. « Les gaz à effet de serre en élevage bovin : évaluation et leviers d'action ». INRAE Productions Animales 24, no 5 (8 décembre 2011) : 415–32. http://dx.doi.org/10.20870/productions-animales.2011.24.5.3275.
Texte intégralVincent, Julia, Béatrice Colin, Isabelle Lanneluc, Philippe Refait, René Sabot, Marc Jeannin et Sophie Sablé. « La biocalcification bactérienne en milieu marin et ses applications ». Matériaux & ; Techniques 110, no 6 (2022) : 606. http://dx.doi.org/10.1051/mattech/2023004.
Texte intégralThèses sur le sujet "Cycle de carbone"
Cachier-Rivault, Hélène. « Approche isotopique du cycle atmospherique du carbone particulaire ». Paris 7, 1987. http://www.theses.fr/1987PA077061.
Texte intégralBarral, 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
Piccoli, Francesca. « High-pressure carbonation : a petrological and geochemical study of carbonated metasomatic rocks from Alpine Corsica ». Thesis, Paris 6, 2017. http://www.theses.fr/2017PA066448/document.
Texte intégralThe balance between the carbon input in subduction zone, mainly by carbonate mineral-bearing rock subduction, and the output of CO2 to the atmosphere by volcanic and metamorphic degassing is critical to the carbon cycle. At fore arc-subarc conditions (75-100 km), carbon is thought to be released from the subducting rocks by devolatilization reactions and by fluid-induced dissolution of carbonate minerals. All together, devolatilization, dissolution, coupled with other processes like decarbonation melting and diapirism, are thought to be responsible for the complete transfer of the subducted carbon into the crust and lithospheric mantle during subduction metamorphism. Carbon-bearing fluids will form after devolatilization and dissolution reactions. The percolation of these fluids through the slab- and mantle-forming rocks is not only critical to carbon cycling, but also for non-volatile element mass transfer, slab and mantle RedOx conditions, as well as slab- and mantle-rock rheology. The evolution of such fluids through interactions with rocks at high-pressure conditions is, however, poorly constrained. This study focuses on the petrological, geochemical and isotopic characteristic of carbonated-metasomatic rocks from the lawsonite-eclogite unit in Alpine Corsica (France). The study rocks are found along major, inherited lithospheric lithological boundaries of the subducted oceanic-to-transitional plate and can inform on the evolution of carbon-bearing high-pressure fluids during subduction. In this work, it will be demonstrated that the interaction of carbon-bearing fluids with slab lithologies can lead to high-pressure carbonation (modeled conditions: 2 to 2.3 GPa and 490-530°C), characterized by silicate dissolution and Ca-carbonate mineral precipitation. A detailed petrological and geochemical characterization of selected samples, coupled with oxygen, carbon and strontium, neodymium isotopic systematic will be used to infer composition and multi-source origin of the fluids involved. Geochemical fluid-rock interactions will be quantified by mass balance and time-integrated fluid fluxes estimations. This study highlights the importance of carbonate-bearing fluids decompressing along down-T paths, such as along slab-parallel lithological boundaries, for the sequestration of carbon in subduction zones. Moreover, rock-carbonation by fluid-rock interactions may have an important impact on the residence time of carbon and oxygen in subduction zones and lithospheric mantle reservoirs as well as carbonate isotopic signatures in subduction zones. Lastly, carbonation may modulate the emission of CO2 at volcanic arcs over geological time scales
Tounsi, Khoudhir. « Le cycle du carbone dans l'Océan atlantique tropical ». Toulouse 3, 1990. http://www.theses.fr/1990TOU30233.
Texte intégralLabbe, Espéret Christiane. « Modélisation et conceptualisation : l'exemple du cycle du carbone ». La Réunion, 2002. http://elgebar.univ-reunion.fr/login?url=http://thesesenligne.univ.run/02_07_Labbe_Esp.pdf.
Texte intégralCachier-Rivault, Hélène. « Approche isotopique du cycle atmosphérique du carbone particulaire ». Grenoble 2 : ANRT, 1987. http://catalogue.bnf.fr/ark:/12148/cb376035474.
Texte intégralMaffre, Pierre. « Interactions entre tectonique, érosion, altération des roches silicatées et climat à l'échelle des temps géologiques : rôle des chaînes de montagnes ». Thesis, Toulouse 3, 2018. http://www.theses.fr/2018TOU30287.
Texte intégralThis thesis explores how orogenies may affect the Earth climate through the quantification of the interactions between climate dynamics, continental erosion, silicate rock weathering rate and geological carbon cycle. The first chapter describes the mechanisms linking the continental topography and its impacts on the atmospheric and oceanic circulations, with emphasis on the thermohaline circulation. The second chapter compares the effects on continental weatherability of climate dynamics and erosional changes related to the presence of mountains. The third chapter describes a dynamic model of regolith designed for global scale simulations, and describes its transient behavior, as well as its response to a CO2 degassing. Finally, the last chapter presents a numerical model of the continental isotopic cycle of lithium, so that its reliability as a proxy of the past weathering can be tested. The model explores the case study of the Amazon lithium cycle
Mariotti, Véronique. « Le cycle du carbone en climat glaciaire : état moyen et variabilité ». Versailles-St Quentin en Yvelines, 2013. http://www.theses.fr/2013VERS0071.
Texte intégralAtmospheric CO2 variations, of around 100 ppm, between glacial and interglacial climates, and 14C variations, are not well understood. This is also the case for the 20 ppm variations of CO2 associated to abrupts events at glacial times. Combining both models and data, I have shown (1) that the sinking of brines mechanism - pockets of salt rejected by sea-ice formation - around Antarctica, likely able to explain glacial-interglacial CO2 variations according to previous studies, could also explain the 14C, (2) that an oscillation of this mechanism could also induce the 20 ppm variations of CO2, during abrupt events, (3) that marine productivity was correctly simulated on the glacial-interglacial time scale and during abrupts events and (4) that for both kinds of variations, it had a limited role on CO2
Leloup, Gaëlle. « Le climat du prochain million d'années : quels scénarios pour le futur ? » Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ001.
Texte intégralWhile many studies focus on the impacts of anthropogenic greenhouse gas on climate on the timescale of the next century, very few have investigated the impacts on a longer timescale, from tens of millennia to a million years. However, due to the long lifetime of CO2 in Earth's surface reservoirs, current anthropogenic emissions are expected to impact the climate on a much longer timescale than the coming century.The objective of this thesis is to broaden the scope of existing studies on the climate of the next million years, by revisiting some of their classical hypotheses. Existing studies rarely consider a partial or total melt of the Antarctic ice sheet, and assume that atmospheric CO2 concentrations come back to pre-industrial levels after hundreds of thousands years, due to silicate weathering.In this study, we explore potential evolutions of the Antarctic ice sheet.More precisely, I have investigated the long term equilibrium of the Antarctic ice sheet under different CO2 levels, using the Earth System model of intermediate complexity iLOVECLIM, coupled to the GRISLI Antarctic ice sheet model, by first applying increasing CO2 levels until the Antarctic ice sheet retreats entirely, and then applying decreasing CO2 levels until the ice sheet regrows. Our results show that the ice sheet exhibits a strong hysteresis behavior. Due to the inclusion of the albedo-melt feedback in our setup, the transition between a glaciated Antarctic ice sheet and an ice-free Antarctic and conversely is more brutal than in previous studies not including this feedback. The CO2 threshold for both Antarctic glaciation and deglaciation varies with the orbital configuration.Additionally, I have developed a conceptual model for the geological carbon cycle that includes multiple equilibria in order to reproduce multi million year cycles in the d13C that are coherent with the data. These potential multiple equilibria in the carbon cycle could lead to a widely different atmospheric CO2 concentration evolution on long timescales, compared to existing studies.Finally, we discuss the implications of our results on a potential end of the Quaternary in the future, with a disappearance of Northern Hemisphere glaciations, but also a disappearance of the Antarctic ice sheet
Bouttes, Nathaëlle. « L’évolution du cycle du carbone au cours du Quaternaire ». Paris 6, 2010. http://www.theses.fr/2010PA066376.
Texte intégralLivres sur le sujet "Cycle de carbone"
R, Trabalka John, Reichle David E et Oak Ridge National Laboratory Life Sciences Symposium (6th : 1983 : Knoxville, Tenn.), dir. The Changing carbon cycle : A global analysis. New York : Springer-Verlag, 1986.
Trouver le texte intégral1958-, Kurz Werner Alexander, Canada-British Columbia Partnership Agreement on Forest Resource Development : FRDA II., Canadian Forest Service et British Columbia. Ministry of Forests., dir. The carbon budget of British Columbia's forests, 1920-1989 : Preliminary analysis and recommendations for refinements. Victoria, B.C : Canadian Forest Service, 1996.
Trouver le texte intégralJ, Baines Shelagh, et Worden Richard H, dir. Geological storage of carbon dioxide. London : Geological Society, 2004.
Trouver le texte intégralSmil, Vaclav. Carbon nitrogen sulfur : Human interference in grand biospheric cycles. New York : Plenum Press, 1985.
Trouver le texte intégralInternational Boreal Forest Research Association. Conference. The role of boreal forests and forestry in the global carbon budget : Proceedings. Sous la direction de Shaw Cindy 1956-, Apps Michael J et Northern Forestry Centre (Canada). Edmonton : Canadian Forest Service, Northern Forestry Centre, 2002.
Trouver le texte intégralSmyth, C. E. Decreasing uncertainty in CBM-CFS3 estimates of forest soil carbon sources and sinks through use of long-term data from the Canadian Intersite Decomposition Experiment. Victoria, B.C : Natural Resources Canada, Canadian Forest Service, Pacific Forestry Centre, 2010.
Trouver le texte intégralInstitute, World Resources, dir. Minding the carbon store : Weighing U.S. forestry strategies to slow global warming. Washington, D.C : World Resources Institute, 1991.
Trouver le texte intégralL, Gholz Henry, Linder Sune et McMurtrie R. E, dir. Environmental constraints on the structure and productivity of pine forest ecosystems : A comparative analysis. Copenhagen, Denmark : Munksgaard International, 1994.
Trouver le texte intégral1965-, McPherson Brian J., et Sundquist E. T, dir. Carbon sequestration and its role in the global carbon cycle. Washington, DC : American Geophysical Union, 2009.
Trouver le texte intégral1965-, McPherson Brian J., et Sundquist E. T, dir. Carbon sequestration and its role in the global carbon cycle. Washington, DC : American Geophysical Union, 2009.
Trouver le texte intégralChapitres de livres sur le sujet "Cycle de carbone"
Canuel, Elizabeth A., et Amber K. Hardison. « Carbon Cycle ». Dans Encyclopedia of Earth Sciences Series, 1–4. Cham : Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-39193-9_175-1.
Texte intégralCanuel, Elizabeth A., et Amber K. Hardison. « Carbon Cycle ». Dans Encyclopedia of Earth Sciences Series, 191–94. Cham : Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_175.
Texte intégralGooch, Jan W. « Carbon Cycle ». Dans Encyclopedic Dictionary of Polymers, 880. New York, NY : Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_13315.
Texte intégralReitner, Joachim, et Volker Thiel. « Carbon Cycle ». Dans Encyclopedia of Geobiology, 238. Dordrecht : Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-1-4020-9212-1_47.
Texte intégralReineke, Walter, et Michael Schlömann. « Carbon Cycle ». Dans Environmental Microbiology, 71–126. Berlin, Heidelberg : Springer Berlin Heidelberg, 2023. http://dx.doi.org/10.1007/978-3-662-66547-3_4.
Texte intégralSpellman, Frank R. « Carbon Cycle ». Dans The Science of Carbon Sequestration and Capture, 38–53. Boca Raton : CRC Press, 2023. http://dx.doi.org/10.1201/9781003432838-3.
Texte intégralBush, Martin J. « The Carbon Cycle ». Dans Climate Change and Renewable Energy, 109–41. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-15424-0_3.
Texte intégralGoudriaan, J. « Global Carbon Cycle ». Dans Climate Change and Rice, 207–17. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-85193-3_20.
Texte intégralEllis-Evans, J. Cynan. « Carbon Cycle, Biological ». Dans Encyclopedia of Astrobiology, 1–2. Berlin, Heidelberg : Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-27833-4_82-3.
Texte intégralEllis-Evans, J. Cynan. « Carbon Cycle, Biological ». Dans Encyclopedia of Astrobiology, 364–65. Berlin, Heidelberg : Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_82.
Texte intégralActes de conférences sur le sujet "Cycle de carbone"
Laakso, Thomas A., et Daniel P. Schrag. « METHANOTROPHY, AUTHIGENIC CARBONATE, AND THE NEOPROTEROZOIC CARBON CYCLE ». Dans GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-307472.
Texte intégralWilson, Siobhan, Maria L. Arizaleta, Bree Morgan, Chad A. Burton, Nina Zeyen, Maija J. Raudsepp, Ian M. Power et Timothy Williams. « SMECTITE–CARBONATE–MICROBE INTERACTIONS IN THE CARBON CYCLE ». Dans GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383974.
Texte intégralZietlow, Douglas. « Synthetic Coal Cycle Technology&trade ; : A Novel Carbon Utilization Technology ». Dans Carbon Management Technology Conference. Carbon Management Technology Conference, 2015. http://dx.doi.org/10.7122/440179-ms.
Texte intégralSanchez-Valle, Carmen, Xenia Ritter et Malcolm Massuyeau. « Mobility of carbonate-rich melts within the deep carbon cycle ». Dans Goldschmidt2022. France : European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12086.
Texte intégralRobson, Wishart, Terry Killian et Robert Siveter. « Life-Cycle Greenhouse Gas Emissions of Transportation Fuels : Issues and Implications for Unconventional Fuel Sources ». Dans Carbon Management Technology Conference. Carbon Management Technology Conference, 2012. http://dx.doi.org/10.7122/151326-ms.
Texte intégralChacartegui, R., D. Sa´nchez, F. Jime´nez-Espadafor, A. Mun˜oz et T. Sa´nchez. « Analysis of Intermediate Temperature Combined Cycles With a Carbon Dioxide Topping Cycle ». Dans ASME Turbo Expo 2008 : Power for Land, Sea, and Air. ASMEDC, 2008. http://dx.doi.org/10.1115/gt2008-51053.
Texte intégralReitberger, Roland, Farzan Banihashemi et Werner Lang. « Sensitivity and Uncertainty Analysis of Combined Building Energy Simulation and Life Cycle Assessment, Implications for the Early Urban Design Process ». Dans CAADRIA 2022 : Post-Carbon. CAADRIA, 2022. http://dx.doi.org/10.52842/conf.caadria.2022.2.629.
Texte intégralVesely, Ladislav, et Vaclav Dostal. « Effect of Multicomponent Mixtures on Cycles With Supercritical Carbon Dioxide ». Dans ASME Turbo Expo 2017 : Turbomachinery Technical Conference and Exposition. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/gt2017-64044.
Texte intégralGkountas, Apostolos A., Anastassios M. Stamatelos et Anestis I. Kalfas. « Thermodynamic Modeling and Comparative Analysis of Supercritical Carbon Dioxide Brayton Cycle ». Dans ASME Turbo Expo 2017 : Turbomachinery Technical Conference and Exposition. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/gt2017-63990.
Texte intégralMcClung, Aaron, Klaus Brun et Jacob Delimont. « Comparison of Supercritical Carbon Dioxide Cycles for Oxy-Combustion ». Dans ASME Turbo Expo 2015 : Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/gt2015-42523.
Texte intégralRapports d'organisations sur le sujet "Cycle de carbone"
Schwinger, Jörg. Report on modifications of ocean carbon cycle feedbacks under ocean alkalinization. OceanNETs, juin 2022. http://dx.doi.org/10.3289/oceannets_d4.2.
Texte intégralDiane Wickland. Carbon Cycle Interagency Working Group. Office of Scientific and Technical Information (OSTI), juillet 2003. http://dx.doi.org/10.2172/909700.
Texte intégralTrabalka, J. Atmospheric carbon dioxide and the global carbon cycle. Office of Scientific and Technical Information (OSTI), décembre 1985. http://dx.doi.org/10.2172/6048470.
Texte intégralCooper, J. F., N. Cherepy, R. Upadhye, A. Pasternak et M. Steinberg. Direct Carbon Conversion : Review of Production and Electrochemical Conversion of Reactive Carbons, Economics and Potential Impact on the Carbon Cycle. Office of Scientific and Technical Information (OSTI), décembre 2000. http://dx.doi.org/10.2172/15007473.
Texte intégralBruhwiler, L., A. M. Michalak, R. Birdsey, D. N. Huntzinger, J. B. Fisher et J. Miller. Chapter 1 : Overview of the Global Carbon Cycle. Second State of the Carbon Cycle Report. Sous la direction de R. A. Houghton, N. Cavallaro, G. Shrestha, R. Birdsey, M. A. Mayes, R. Najjar, S. Reed, P. Romero-Lankao et Z. Zhu. U.S. Global Change Research Program, 2018. http://dx.doi.org/10.7930/soccr2.2018.ch1.
Texte intégralDouglas, Thomas A., Christopher A. Hiemstra, Miriam C. Jones et Jeffrey R. Arnold. Sources and Sinks of Carbon in Boreal Ecosystems of Interior Alaska : A Review. U.S. Army Engineer Research and Development Center, juillet 2021. http://dx.doi.org/10.21079/11681/41163.
Texte intégralBorenstein, Severin. Markets for Anthropogenic Carbon Within the Larger Carbon Cycle. Cambridge, MA : National Bureau of Economic Research, juin 2010. http://dx.doi.org/10.3386/w16104.
Texte intégralMoisseytsev, A., et J. J. Sienicki. Supercritical carbon dioxide cycle control analysis. Office of Scientific and Technical Information (OSTI), avril 2011. http://dx.doi.org/10.2172/1011299.
Texte intégralHuntzinger, D. N., A. Chatterjee, D. Moore, S. Ohrel, T. O. West, B. Poulter, A. Walker et al. Chapter 19 : Future of the North American Carbon Cycle. Second State of the Carbon Cycle Report. Sous la direction de R. Birdsey, M. A. Mayes, R. Najjar, S. Reed, P. Romero-Lankao et Z. Zhu. U.S. Global Change Research Program, 2018. http://dx.doi.org/10.7930/soccr2.2018.ch19.
Texte intégralWest, T. O., N. Gurwick, M. E. Brown, R. Duren, S. Mooney, K. Paustian, E. McGlynn et al. Chapter 18 : Carbon Cycle Science in Support of Decision Making. Second State of the Carbon Cycle Report. Sous la direction de N. Cavallaro, G. Shrestha, R. Birdsey, M. A. Mayes, R. Najjar, S. Reed, P. Romero-Lankao et Z. Zhu. U.S. Global Change Research Program, 2018. http://dx.doi.org/10.7930/soccr2.2018.ch18.
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