Bibliographies thématiques / Climate change, Carbon Dioxide, foraminifera

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Littérature scientifique sur le sujet « Climate change, Carbon Dioxide, foraminifera »

Auteur : Grafiati
Publié le 10 mars 2023

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Articles de revues sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Raitzsch, Markus, Jelle Bijma, Torsten Bickert, Michael Schulz, Ann Holbourn et Michal Kučera. « Atmospheric carbon dioxide variations across the middle Miocene climate transition ». Climate of the Past 17, no 2 (26 mars 2021) : 703–19. http://dx.doi.org/10.5194/cp-17-703-2021.

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Abstract. The middle Miocene climate transition ∼ 14 Ma marks a fundamental step towards the current “ice-house” climate, with a ∼ 1 ‰ δ18O increase and a ∼ 1 ‰ transient δ13C rise in the deep ocean, indicating rapid expansion of the East Antarctic Ice Sheet associated with a change in the operation of the global carbon cycle. The variation of atmospheric CO2 across the carbon-cycle perturbation has been intensely debated as proxy records of pCO2 for this time interval are sparse and partly contradictory. Using boron isotopes (δ11B) in planktonic foraminifers from Ocean Drilling Program (ODP) Site 1092 in the South Atlantic, we show that long-term pCO2 varied at 402 kyr periodicity between ∼ 14.3 and 13.2 Ma and follows the global δ13C variation remarkably well. This suggests a close link to precessional insolation forcing modulated by eccentricity, which governs the monsoon and hence weathering intensity, with enhanced weathering and decreasing pCO2 at high eccentricity and vice versa. The ∼ 50 kyr lag of δ13C and pCO2 behind eccentricity in our records may be related to the slow response of weathering to orbital forcing. A pCO2 drop of ∼ 200 µatm before 13.9 Ma may have facilitated the inception of ice-sheet expansion on Antarctica, which accentuated monsoon-driven carbon cycle changes through a major sea-level fall, invigorated deep-water ventilation, and shelf-to-basin shift of carbonate burial. The temporary rise in pCO2 following Antarctic glaciation would have acted as a negative feedback on the progressing glaciation and helped to stabilize the climate system on its way to the late Cenozoic ice-house world.
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Stuhr, Marleen, Louise P. Cameron, Bernhard Blank-Landeshammer, Claire E. Reymond, Steve S. Doo, Hildegard Westphal, Albert Sickmann et Justin B. Ries. « Divergent Proteomic Responses Offer Insights into Resistant Physiological Responses of a Reef-Foraminifera to Climate Change Scenarios ». Oceans 2, no 2 (1 avril 2021) : 281–314. http://dx.doi.org/10.3390/oceans2020017.

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Reef-dwelling calcifiers face numerous environmental stresses associated with anthropogenic carbon dioxide emissions, including ocean acidification and warming. Photosymbiont-bearing calcifiers, such as large benthic foraminifera, are particularly sensitive to climate change. To gain insight into their responses to near-future conditions, Amphistegina lobifera from the Gulf of Aqaba were cultured under three pCO2 conditions (492, 963, 3182 ppm) crossed with two temperature conditions (28 °C, 31 °C) for two months. Differential protein abundances in host and photosymbionts were investigated alongside physiological responses and microenvironmental pH gradients assessed via proton microsensors. Over 1000 proteins were identified, of which > 15% varied significantly between treatments. Thermal stress predominantly reduced protein abundances, and holobiont growth. Elevated pCO2 caused only minor proteomic alterations and color changes. Notably, pH at the test surface decreased with increasing pCO2 under all light/dark and temperature combinations. However, the difference between [H+] at the test surface and [H+] in the seawater—a measure of the organism’s mitigation of the acidified conditions—increased with light and pCO2. Combined stressors resulted in reduced pore sizes and increased microenvironmental pH gradients, indicating acclimative mechanisms that support calcite test production and/or preservation under climate change. Substantial proteomic variations at moderate-pCO2 and 31 °C and putative decreases in test stability at high-pCO2 and 31 °C indicate cellular modifications and impacts on calcification, in contrast to the LBFs’ apparently stable overall physiological performance. Our experiment shows that the effects of climate change can be missed when stressors are assessed in isolation, and that physiological responses should be assessed across organismal levels to make more meaningful inferences about the fate of reef calcifiers.
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Johnson, Markes E. « Geological Oceanography of the Pliocene Warm Period : A Review with Predictions on the Future of Global Warming ». Journal of Marine Science and Engineering 9, no 11 (2 novembre 2021) : 1210. http://dx.doi.org/10.3390/jmse9111210.

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Atmospheric carbon dioxide reached a record concentration of 419 parts per million in May 2021, 50% higher than preindustrial levels at 280 parts per million. The rise of CO2 as a heat-trapping gas is the principal barometer tracking global warming attributed to a global average increase of 1.2 °C over the last 250 years. Ongoing global warming is expected to perturb extreme weather events such as tropical cyclones (hurricanes/typhoons), strengthened by elevated sea-surface temperatures. The melting of polar ice caps in Antarctica and Greenland also is expected to result in rising sea levels through the rest of this century. Various proxies for the estimate of long-term change in sea-surface temperatures (SSTs) are available through geological oceanography, which relies on the recovery of deep-sea cores for the study of sediments enriched in temperature-sensitive planktonic foraminifera and other algal residues. The Pliocene Warm Period occurred between ~4.5 and 3.0 million years ago, when sea level and average global temperatures were higher than today, and it is widely regarded as a predictive analog to the future impact of climate change. This work reviews some of the extensive literature on the geological oceanography of the Pliocene Warm Period together with a summary of land-based studies in paleotempestology focused on coastal boulder deposits (CBDs) and coastal outwash deposits (CODs) from the margin of the Pacific basin and parts of the North Atlantic basin. Ranging in age from the Pliocene through the Holocene, the values of such deposits serve as fixed geophysical markers, against which the micro-fossil record for the Pliocene Warm Period may be compared, as a registry of storm events from Pliocene and post-Pliocene times.
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Langebroek, P. M., A. Paul et M. Schulz. « Constraining atmospheric CO<sub>2</sub> ; content during the Middle Miocene Antarctic glaciation using an ice sheet-climate model ». Climate of the Past Discussions 4, no 4 (12 août 2008) : 859–95. http://dx.doi.org/10.5194/cpd-4-859-2008.

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Abstract. Foraminiferal oxygen isotopes from deep-sea sediment cores suggest that a rapid expansion of the Antarctic ice sheet took place in the Middle Miocene around 13.9 million years ago (Ma). The origin for this transition is still not understood satisfactorily. Among the proposed causes are a drop in the partial pressure of atmospheric carbon dioxide (pCO2) in combination with orbital forcing. An additional complication is the large uncertainty in the magnitude and age of the reconstructed pCO2 values and the low temporal resolution of the available record in the Middle Miocene. We used an ice sheet-climate model with an energy and mass balance module to assess variations in ice-sheet volume induced by pCO2 and insolation forcing and to better constrain atmospheric CO2 in the Middle Miocene. The ice-sheet sensitivity to atmospheric CO2 was tested in several scenarios using constant pCO2 forcing or a regular decrease in pCO2. Small, ephemeral ice sheets existed under relatively high atmospheric CO2 conditions (between 400–450 ppm), whereas more stable, large ice sheets occurred when pCO2 is less than 400 ppm. Transitions between the states were largely CO2-induced, but were enhanced by extremes in insolation. In order to explain the Antarctic glaciation in the Middle Miocene as documented by the oxygen isotope records from sediment cores, pCO2 must have decreased by approximately 150 ppm in about 30 ka, crossing the threshold pCO2 of 400 ppm around 13.9 Ma. Forcing the ice sheet-climate model with cyclic pCO2 variations at a period of 100 ka and amplitudes of approximately 40 ppm generated late Pleistocene glacial-interglacial like ice-volume variations, where the ice volume lagged pCO2 by 11–16 ka.
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Langebroek, P. M., A. Paul et M. Schulz. « Antarctic ice-sheet response to atmospheric CO<sub>2</sub> ; and insolation in the Middle Miocene ». Climate of the Past 5, no 4 (22 octobre 2009) : 633–46. http://dx.doi.org/10.5194/cp-5-633-2009.

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Abstract. Foraminiferal oxygen isotopes from deep-sea sediment cores suggest that a rapid expansion of the Antarctic ice sheet took place in the Middle Miocene around 13.9 million years ago. The origin for this transition is still not understood satisfactorily. One possible cause is a drop in the partial pressure of atmospheric carbon dioxide (pCO2) in combination with orbital forcing. A complication is the large uncertainty in the magnitude and timing of the reconstructed pCO2 variability and additionally the low temporal resolution of the available pCO2 records in the Middle Miocene. We used an ice sheet-climate model of reduced complexity to assess variations in Antarctic ice sheet volume induced by pCO2 and insolation forcing in the Middle Miocene. The ice-sheet sensitivity to atmospheric CO2 was tested for several scenarios with constant pCO2 forcing or a regular decrease in pCO2. This showed that small, ephemeral ice sheets existed under relatively high atmospheric CO2 conditions (between 640–900 ppm), whereas more stable, large ice sheets occurred when pCO2 was less than ~600 ppm. The main result of this study is that the pCO2-level must have declined just before or during the period of oxygen-isotope increase, thereby crossing a pCO2 glaciation threshold of around 615 ppm. After the decline, the exact timing of the Antarctic ice-sheet expansion depends also on the relative minimum in summer insolation at approximately 13.89 million years ago. Although the mechanisms described appear to be robust, the exact values of the pCO2 thresholds are likely to be model-dependent.
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Basilios, Koumbakis. « Climate change and CO2 Carbon dioxide ». International Journal of Scientific and Management Research 05, no 03 (2022) : 79–76. http://dx.doi.org/10.37502/ijsmr.2022.5308.

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This paper is about climate change, its relationship with carbon dioxide, the Greenhouse Effect and Renewable Energy Sources. Through a historical reference, the original view of the Greenhouse Effect is introduced, while based on facts of greenhouse gases and solar radiation is been proved the unrelated interconnection of the “accused” gas with the accusations against it. Factors responsible for the increase in temperature in ambient air are examined and their contribution to this increase is calculated. Also, is been examined the operation of the most known renewable energy sources and their contribution to the increase of the air temperature, as well as, their contribution to intense weather phenomena. The paper responds factually to the causes that create the changes in the climate and raises questions about the policy pursued on this issue, in the direction of solving the problem or reducing its impact. The aim of the project is to present to the general public, the scientific community and politicians, different from conventional facts, so that they have in their hands a tool for better use of renewable energy sources and real protection of the environment.
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Farquhar, G. D. « CLIMATE CHANGE : Carbon Dioxide and Vegetation ». Science 278, no 5342 (21 novembre 1997) : 1411. http://dx.doi.org/10.1126/science.278.5342.1411.

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Anderson, Norman D. « Carbon Dioxide and Global Climate Change ». Science Activities : Classroom Projects and Curriculum Ideas 29, no 3 (septembre 1992) : 31–38. http://dx.doi.org/10.1080/00368121.1992.10113036.

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Watson, A. J. « Man made carbon dioxide and climate change ». Science of The Total Environment 57 (décembre 1986) : 264–65. http://dx.doi.org/10.1016/0048-9697(86)90031-8.

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Keeling, C. D. « Climate change and carbon dioxide : An introduction ». Proceedings of the National Academy of Sciences 94, no 16 (5 août 1997) : 8273–74. http://dx.doi.org/10.1073/pnas.94.16.8273.

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Thèses sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Pang, Oi-ting Brenda, et 彭愷婷. « Climate change : the role of carbon dioxide ». Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B46732937.

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Martin, M. J. « Models of the interactive effects of rising ozone, carbon dioxide and temperature on canopy carbon dioxide exchange and isoprene emission ». Thesis, University of Essex, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.339238.

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Ramsell, Philip G. « An alternative climate change levy scheme for manufacturing industries ». Thesis, Open University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270013.

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Sandu, Suwin. « Assessment of carbon tax as a policy option for reducing carbon-dioxide emissions in Australia ». Electronic version, 2007. http://hdl.handle.net/2100/535.

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University of Technology, Sydney. Faculty of Engineering.
This research has analysed the economy-wide impacts of carbon tax as a policy option to reduce the rate of growth of carbon-dioxide emissions from the electricity sector in Australia. These impacts are analysed for energy and non energy sectors of the economy. An energy-oriented Input–Output framework, with ‘flexible’ production functions, based on Translog and Cobb-Douglas formulations, is employed for the analysis of various impacts. Further, two alternative conceptions of carbon tax are considered in this research, namely, based on Polluter Pays Principle (PPP) and Shared Responsibility Principle (SRP). In the first instance, the impacts are analysed, for the period 2005–2020, for tax levels of $10 and $20 per tonne of CO2, in a situation of no a-priori limit on CO2 emissions. The analysis shows that CO2 emissions from the electricity sector, when carbon tax is based on PPP, would be 211 and 152 Mt, for tax levels of $10 and $20, respectively (as compared to 250 Mt in the Base Case scenario, that is, the business-as-usual-case). The net economic costs, corresponding with these tax levels, expressed in present value terms, would be $27 and $49 billion, respectively, over the period 2005-2020. These economic costs are equivalent to 0.43 and 0.78 per cent of the estimated GDP of Australia. Further, most of the economic burden, in this instance, would fall on the electricity sector, particularly coal-fired electricity generators – large consumers of direct fossil fuel. On the other hand, in the case of a carbon tax based on SRP, CO2 emissions would be 172 and 116 Mt, for tax levels of $10 and $20, respectively. The corresponding net economic costs would be $47 (0.74 per cent of GDP) and $84 (1.34 per cent of GDP) billion, respectively, with significant burden felt by the commercial sector – large consumers of indirect energy and materials whose production would contribute to CO2 emissions. Next, the impacts are analysed by placing an a-priori limit on CO2 emissions from the electricity sector – equivalent to 108 per cent of the 1990 level (that is, 138 Mt), by the year 2020. Two cases are analysed, namely, early action (carbon tax introduced in 2005) and deferred action (carbon tax introduced in 2010). In the case of early action, the analysis suggests, carbon tax of $25 and $15, based on PPP and SRP, respectively, would be required to achieve the above noted emissions target. The corresponding tax levels in the case of deferred action are $51 and $26, respectively. This research also shows that the net economic costs, in the case of early action, would be $32 billion (for PPP) and $18 billion (for SRP) higher than those in the case of deferred action. However, this research has demonstrated, that this inference is largely due to the selection of particular indicator (that is, present value) and the relatively short time frame (that is, 2005–2020) for analysis. By extending the time frame of the analysis to the year 2040, the case for an early introduction of carbon tax strengthens. Overall, the analysis in this research suggests that an immediate introduction of carbon tax, based on SRP, is the most attractive approach to reduce the rate of growth of CO2 emissions from the electricity sector and to simultaneously meet economic and social objectives. If the decision to introduce such a tax is deferred, it would be rather difficult to achieve not only environmental objectives but economic and social objectives as well.
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Corbo, Alessandro. « Biochar as a carbon dioxide removal solution : An assessment of carbon stability and carbon dioxide removal potential in Sweden ». Thesis, KTH, Hållbar utveckling, miljövetenskap och teknik, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-281918.

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Biochar is increasingly gaining momentum in the context of climate change mitigation and its production in Sweden could potentially become a large-scale system. Carbon stability in biochar is a crucial factor to assess its the carbon sequestration potential. Currently specific methodologies to assess biochar carbon site-specific stability are missing. This work aims at filling in part this knowledge gap assessing stability for Sweden specific soil conditions. Moreover, this work aims at assessing biomass feedstock availability for biochar production from a system perspective and aims at estimating biochar production and carbon dioxide removal potentials in Sweden. Preliminary carbon stability specific thresholds are provided for soils at 10°C temperature and, thus, representative for Sweden conditions. Carbon dioxide removal functions are obtained for different feedstock categories (woody, herbaceous, biosolids and animal waste) dependent on pyrolysis conditions (Highest Treatment Temperature), and conditions for maximum carbon removal are assessed. The need for future analysis in order to validate the presented results is highlighted. Future work should focus on collecting new experimental results of biochar mineralisation based on the requirements presented in this work. An opportunity mapping for biochar production system is provided, focusing on some aspects of the interaction of the former with existing systems (agricultural, energy production and waste management). From the results of the opportunity mapping, an inventory of the available feedstock for biochar production is presented including woody residues, sewage sludge, manure, garden waste and straw. From the available feedstocks, biochar production and carbon dioxide removal potentials are estimated to range respectively between 0.9 and 1.7 million tbiochar/year and between 2 and 4.2 million tons CO2 sequestered per year (in a 100 years perspective). In terms of carbon dioxide removal potential, biochar production can significantly contribute to the goals set by Sweden in terms of climate change mitigation and emission offsetting for 2030 and 2045, potentially covering all the measures needed from carbon sinks from forest and land. It was found that the most significant contribution derives from the availability of woody residues in Sweden, whose analysis should be prioritised for future assessment of feasibility of biochar large scale production.
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Sobek, Sebastian. « Carbon Dioxide Supersaturation in Lakes – Causes, Consequences and Sensitivity to Climate Change ». Doctoral thesis, Uppsala : Acta Universitatis Upsaliensis (AUU) : Universitetsbiblioteket [distributör], 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-5920.

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Campbell, Justin E. « The Effects of Carbon Dioxide Fertilization on the Ecology of Tropical Seagrass Communities ». FIU Digital Commons, 2012. http://digitalcommons.fiu.edu/etd/693.

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Increasing atmospheric CO2 concentrations associated with climate change will likely influence a wide variety of ecosystems. Terrestrial research has examined the effects of increasing CO2 concentrations on the functionality of plant systems; with studies ranging in scale from the short-term responses of individual leaves, to long-term ecological responses of complete forests. While terrestrial plants have received much attention, studies on the responses of marine plants (seagrasses) to increased CO2(aq) concentrations remain relatively sparse, with most research limited to small-scale, ex situ experimentation. Furthermore, few studies have attempted to address similarities between terrestrial and seagrass responses to increases in CO2(aq). The goals of this dissertation are to expand the scope of marine climate change research, and examine how the tropical seagrass, Thalassia testudinum responds to increasing CO2(aq) concentrations over multiple spatial and temporal scales. Manipulative laboratory and field experimentation reveal that, similar to terrestrial plants, seagrasses strongly respond to increases in CO2(aq) concentrations. Using a novel field technique, in situ field manipulations show that over short time scales, seagrasses respond to elevated CO2(aq) by increasing leaf photosynthetic rates and the production of soluble carbohydrates. Declines in leaf nutrient (nitrogen and phosphorus) content were additionally detected, paralleling responses from terrestrial systems. Over long time scales, seagrasses increase total above- and belowground biomass with elevated CO2(aq), suggesting that, similar to terrestrial research, pervasive increases in atmospheric and oceanic CO2(aq) concentrations stand to influence the productivity and functionality of these systems. Furthermore, field experiments reveal that seagrass epiphytes, which comprise an important component of seagrass ecosystems, additionally respond to increased CO2(aq) with strong declines in calcified taxa and increases in fleshy taxa. Together, this work demonstrates that increasing CO2(aq) concentrations will alter the functionality of seagrass ecosystems by increasing plant productivity and shifting the composition of the epiphyte community. These results have implications for future rates of carbon storage and sediment production within these widely distributed systems.
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Cotrufo, Maria Francesca. « Effects of enriched atmospheric concentration of carbon dioxide on tree litter decomposition ». Thesis, Lancaster University, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.282385.

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Singleton-Jones, Paul. « Elevated carbon dioxide and gas exchange in groundnut and sorghum ». Thesis, University of Nottingham, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243686.

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Scholz, Stephane. « GLOBALIZATION AND CARBON DIOXIDE EMISSION TRAJECTORIES IN DEVELOPING COUNTRIES, 1980-2006 ». Diss., The University of Arizona, 2011. http://hdl.handle.net/10150/202970.

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Global energy sector carbon dioxide emissions between 2007 and 2010 have been growing much faster than projected by the Intergovernmental Panel on Climate Change (IEA 2011). Roughly 75% of this growth can be attributed to developing countries that are increasingly manufacturing goods destined for consumption in the developed world (Peters et al. 2011). This study examines the energy sector carbon dioxide emissions and emission trajectories of 64 developing countries from 1980 to 2006. Approximately 50% of these countries have relatively flat slopes when their emissions are plotted over time or against gross domestic product per capita. To shed some light on how this is possible, two competing theories of globalization are tested. World-systems theory argues that global economic integration is predicated on core-periphery exploitation, which leads to unsustainable development. World-society theory, on the other hand, contends that global social integration diffuses modern environmental values, which leads to structural isomorphism and sustainable development. World-society diffusion in this study is approximated by the network measure of degree centrality, which is calculated from shared ratifications of international environmental treaties. To find out if these opposing dynamics significantly impact emissions and emission trajectories independently, or in conjunction, three different methods are used: Prais-Winsten panel regression with panel-corrected standard errors, cross-section ordinary least squares regression and fuzzy set qualitative comparative analysis.Findings from the panel regressions indicate that network centrality in global environmental treaty regimes has a significant, albeit weak, negative effect on carbon dioxide emissions. This effect is further attenuated by high levels of world-system exploitation, as measured by International Monetary Fund (IMF) credit. The first set of cross-section regressions indicate that network centrality has a significant, but weak, negative effect on emission trajectories plotted against GDP per capita when restricted to those countries that have low levels of IMF credit. The second set of cross-section regressions indicate that network centrality has a significant, but once again weak, negative effect on emission trajectories plotted over time when restricted to those countries that have low levels of foreign direct investment (FDI). The fuzzy set qualitative comparative analyses reveal that world-society diffusion is only implicated in two out of five sufficient configurations for membership in the outcome set of countries with relatively flat emission trajectories plotted against GDP per capita. Furthermore, world-society diffusion, at least as approximated in terms of network centrality in international environmental treaty regimes, is not implicated in any of the sufficient configurations when the outcome involves membership in the set of countries with relatively flat emission trajectories plotted over time. In these analyses it is the absence of economic growth that is most often implicated, followed by low levels of FDI and IMF credit.
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Livres sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Bow, James. Earth's climate change : Carbon dioxide overload. St. Catharines, Ontario : Crabtree Publishing, 2016.

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editor, Mahapatra Richard, et Centre for Science and Environment (New Delhi, India), dir. Climate change now : The story of carbon colonisation. New Delhi : Centre for Science and Environment, 2018.

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United States. Congressional Budget Office., dir. The economics of climate change : A primer. Washington, DC : Congressional Budget Office, 2003.

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Laboratory, Lawrence Livermore National, dir. Energy and climate change : Report of the DOE Multi-Laboratory Climate Change Committee. Chelsea, Mich : Lewis Publishers, 1990.

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Agency, International Energy, et Organisation for Economic Co-operation and Development., dir. Transport, energy, and climate change. Paris : OECD, 1997.

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National Academy of Sciences (U.S.), dir. National Academy of Sciences colloquium : Carbon dioxide and climate change. Washington, D.C : The Academy, 1997.

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author, Schware Robert 1952, dir. Climate change and society : Consequences of increasing atmospheric carbon dioxide. New York, NY : Routledge, 2018.

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Carbon abatement costs and climate change finance. Washington, DC : Peterson Institute For International Economics, 2011.

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Capturing carbon : The new weapon in the war against climate change. New York : Columbia University Press, 2010.

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1956-, Blockstein David E., Wiegman Leo et National Council for Science and the Environment (U.S.), dir. The climate solutions consensus. Washington : Island Press, 2010.

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Chapitres de livres sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Bauman, Yoram, et Grady Klein. « Carbon Dioxide ». Dans The Cartoon Introduction to Climate Change, 39–50. Washington, DC : Island Press/Center for Resource Economics, 2014. http://dx.doi.org/10.5822/978-1-61091-570-0_4.

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Ramirez-Corredores, Maria Magdalena, Mireya R. Goldwasser et Eduardo Falabella de Sousa Aguiar. « Carbon Dioxide and Climate Change ». Dans SpringerBriefs in Applied Sciences and Technology, 1–14. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-19999-8_1.

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Roberts, Walter Orr. « Social Resiliency and Carbon Dioxide : Preliminary Remarks ». Dans World Climate Change, 1–3. New York : Routledge, 2021. http://dx.doi.org/10.4324/9780429268113-2.

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Bajaj, Pushp, et Saurabh Thakur. « Carbon Dioxide Capture and Sequestration to Achieve Paris Climate Targets ». Dans Climate Change, 215–33. Cham : Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-86290-9_13.

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Wolfe, David W., et Jon D. Erickson. « Carbon Dioxide Effects on Plants : ». Dans Agricultural Dimensions of Global Climate Change, 153–78. Boca Raton : Routledge, 2022. http://dx.doi.org/10.1201/9781315136967-8.

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Allen, L. H., J. T. Baker, S. L. Albrecht, K. J. Boote, D. Pan et J. C. V. Vu. « Carbon Dioxide and Temperature Effects on Rice ». Dans Climate Change and Rice, 258–77. Berlin, Heidelberg : Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-85193-3_25.

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Seneweera, S., et R. M. Norton. « Plant Responses to Increased Carbon Dioxide ». Dans Crop Adaptation to Climate Change, 198–217. Oxford, UK : Wiley-Blackwell, 2011. http://dx.doi.org/10.1002/9780470960929.ch15.

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Schuiling, R. D. « Carbon Dioxide Sequestration, Weathering Approaches to ». Dans Geoengineering Responses to Climate Change, 141–67. New York, NY : Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-5770-1_7.

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Qaderi, Mirwais M., et David M. Reid. « Crop Responses to Elevated Carbon Dioxide and Temperature ». Dans Climate Change and Crops, 1–18. Berlin, Heidelberg : Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-88246-6_1.

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Graham, Jacob D., et Nathan I. Hammer. « Photocatalytic Water Splitting and Carbon Dioxide Reduction ». Dans Handbook of Climate Change Mitigation, 1755–80. New York, NY : Springer US, 2012. http://dx.doi.org/10.1007/978-1-4419-7991-9_46.

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Actes de conférences sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Gabriel, Kamiel, et Huawei Han. « Towards a Long-Term Solution to Carbon Dioxide Storage ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277202.

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Kumar, Rajnish, Praveen Linga et Peter Englezos. « Pre and Post Combustion Capture of Carbon Dioxide via Hydrate Formation ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277200.

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LACKNER, KLAUS S. « CONSENSUS AND DISAGREEMENT ON CLIMATE CHANGE DUE TO CARBON DIOXIDE ». Dans International Seminar on Nuclear War and Planetary Emergencies 34th Session. WORLD SCIENTIFIC, 2006. http://dx.doi.org/10.1142/9789812773890_0049.

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Tourneux, David, Maria Iliuta, Faical Larachi et Sylvie Fradette. « Aqueous 2-amino-2-hydroxymethyl-1,3-propanediol as Potential Carbon Dioxide Capture Solutions ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277265.

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Dey, Anindo, et Adisorn Aroonwilas. « Carbon Dioxide Absorption Characteristics of Blended Monoethanolamine and 2-Amino-2-methyl-1-propanol ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277219.

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Ugrekhelidze, A. T. « COMBATING CLIMATE CHANGE ». Dans INNOVATIVE TECHNOLOGIES IN SCIENCE AND EDUCATION. DSTU-Print, 2020. http://dx.doi.org/10.23947/itno.2020.285-288.

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This article examines the problem of the release of a large amount of carbon dioxide on the example of the territory of the European Union. In addition, examples of possible solutions to this problem are given due to a number of adopted laws in the field of additional taxes, as well as the prohibition of harmful emissions and subsidies to industries using harmless renewable energy.
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Kheshgi, Haroon, Fredde Cappelen, Arthur Lee, Steve Crookshank, Alain Heilbrunn, Tom Mikus, Wishart Robson, William John Senior, Tim John Stileman et Luke Warren. « Carbon Dioxide Capture and Geological Storage : Contributing to Climate Change Solutions ». Dans SPE International Health, Safety & Environment Conference. Society of Petroleum Engineers, 2006. http://dx.doi.org/10.2118/98583-ms.

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Rosen, Marc. « An Exergy-Based Method for Allocating Carbon Dioxide Emissions from Cogeneration Systems - Part I : Comparison with Other Methods ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277239.

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Rosen, Marc. « An Exergy-Based Method for Allocating Carbon Dioxide Emissions from Cogeneration Systems - Part II : Justification for Exergy Basis ». Dans 2006 IEEE EIC Climate Change Conference. IEEE, 2006. http://dx.doi.org/10.1109/eicccc.2006.277240.

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Asghar, Aisha, Naseem Iqbal et Tayyaba Noor. « Comparison of BDC linker based MOFs for carbon dioxide trapping ; curb climate change ». Dans 2020 IEEE Green Technologies Conference(GreenTech). IEEE, 2020. http://dx.doi.org/10.1109/greentech46478.2020.9289756.

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Rapports d'organisations sur le sujet "Climate change, Carbon Dioxide, foraminifera"

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Oechel, W. Response of a tundra ecosystem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. Office of Scientific and Technical Information (OSTI), mai 1990. http://dx.doi.org/10.2172/228115.

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Oechel, W. C. Response of a tundra ecosystem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. Final report. Office of Scientific and Technical Information (OSTI), novembre 1996. http://dx.doi.org/10.2172/307995.

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Oechel, W. C. Response of a tundra ecosystem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. [Annual report]. Office of Scientific and Technical Information (OSTI), juin 1991. http://dx.doi.org/10.2172/230264.

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Oechel, W. C. Response of a tundra ecosystem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. [Annual report]. Office of Scientific and Technical Information (OSTI), décembre 1989. http://dx.doi.org/10.2172/230286.

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Oechel, W. C. Response of a tundra ecosytem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. Final report. Office of Scientific and Technical Information (OSTI), novembre 1996. http://dx.doi.org/10.2172/594481.

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Oechel, W. C. Response of a tundra ecosystem to elevated atmospheric carbon dioxide and CO{sub 2}-induced climate change. Annual technical report. Office of Scientific and Technical Information (OSTI), février 1993. http://dx.doi.org/10.2172/230308.

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Oechel, Walter C. Response of a Tundra Ecosystem to Elevated Atmospheric Carbon Dioxide and CO2-Induced Climate Change : A Renewal Research Proposal. Office of Scientific and Technical Information (OSTI), avril 1992. http://dx.doi.org/10.2172/230262.

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Veland, Siri, et Christine Merk. Lay person perceptions of marine carbon dioxide removal (CDR) – Working paper. OceanNETs, juillet 2021. http://dx.doi.org/10.3289/oceannets_d3.3.

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This working paper presents first insights on lay public perceptions of marine carbon dioxide removal (CDR) approaches. In seven focus groups, three in Germany and four in Norway (including one pilot) the researchers asked members of the lay public to share their views of the ocean and the effects of climate change, four CDR approaches, as well as their reflections on responsible research and innovation (RRI) of marine CDR. The four CDR methods were ocean iron fertilization, ocean alkalinity enhancement, artificial upwelling, and blue carbon management through restoration of coastal and marine ecosystems. In addition, respondents were asked to compare the four approaches. Our findings indicate that the public will be very supportive of blue carbon management irrespective of its actual carbon sequestration potential, due in part to the perceived bad state of marine ecosystems worldwide. Participants were skeptical whether any of the CDR approaches could have relevant effect on carbon sequestration and long-term storage; they reasoned about issues such as the ability to scale up treatments in time and space, unforeseen or unforeseeable effects on ecosystems in time and space, and the role of industry in the implementation process. They argued that despite the potential availability of marine CDR, industry and the general public should stop polluting behaviors and practices. Nevertheless, the participants universally agreed that further research on all four CDR methods should be pursued to better understand effects on climate, ecosystems, local communities, and the economy.
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Aryal, Jeetendra Prakash. Contribution of Agriculture to Climate Change and Low-Emission Agricultural Development in Asia and the Pacific. Asian Development Bank Institute, octobre 2022. http://dx.doi.org/10.56506/vaoy9373.

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The agriculture sector in Asia and the Pacific region contributes massively to climate change, as the region has the largest share of greenhouse gas (GHG) emissions from agriculture. The region is the largest producer of rice, a major source of methane emissions. Further, to achieve food security for the increasing population, there has been a massive increase in the use of synthetic fertilizer and energy in agricultural production in the region over the last few decades. This has led to an enormous rise in nitrous oxide (N2O; mostly from fertilizer-N use) and carbon dioxide (mostly from energy use for irrigation) emissions from agriculture. Besides this, a substantial increase in livestock production for meat and dairy products has increased methane emissions, along with other environmental problems. In this context, this study conducts a systematic review of strategies that can reduce emissions from the agriculture sector using a multidimensional approach, looking at supply-side, demand-side, and cross-cutting measures. The review found that though there are huge potentials to reduce GHG emissions from agriculture, significant challenges exist in monitoring and verification of GHG emissions from supply-side measures, shifting to sustainable consumption behavior with regard to food consumption and use, and the design and implementation of regulatory and incentive mechanisms. On the supply side, policies should focus on the upscaling of climate-smart agriculture primarily through expanding knowledge and improving input use efficiency in agriculture, while on the demand side, there is a need to launch a drive to reduce food loss and waste and also to move towards sustainable consumption. Therefore, appropriate integration of policies at multiple levels, as well as application of multiple measures simultaneously, can increase mitigation potential as desired by the Paris Agreement and also help to achieve several of the United Nations’ SDGs.
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Aryal, Jeetendra P. Contribution of Agriculture to Climate Change and Low-Emission Agricultural Development in Asia and the Pacific. Asian Development Bank Institute, octobre 2022. http://dx.doi.org/10.56506/wdbc4659.

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The agriculture sector in the Asia and Pacific region contributes massively to climate change, as the region has the largest share of greenhouse gas (GHG) emissions from agriculture. The region is the largest producer of rice, a major source of methane emissions. Further, to achieve food security for the increasing population, there has been a massive increase in the use of synthetic fertilizer and energy in agricultural production in the region over the last few decades. This has led to an enormous rise in nitrous oxide (N2O) (mostly from fertilizer-N use) and carbon dioxide (mostly from energy use for irrigation) emissions from agriculture. Besides this, a substantial increase in livestock production for meat and dairy products has increased methane emissions, along with other environmental problems. In this context, we conduct a systematic review of strategies that can reduce emissions from the agriculture sector using a multidimensional approach, looking at supply-side, demand-side, and cross-cutting measures. The review found that though there is a huge potential to reduce GHG emissions from agriculture, significant challenges exist in monitoring and verification of GHG emissions from supply-side measures, shifting to sustainable consumption behavior with regard to food consumption and use, and the design and implementation of regulatory and incentive mechanisms. On the supply side, policies should focus on the upscaling of climate-smart agriculture primarily through expanding knowledge and improving input use efficiency in agriculture, while on the demand side, there is a need to launch a drive to reduce food loss and waste and also to move toward sustainable consumption. Therefore, appropriate integration of policies at multiple levels, as well as application of multiple measures simultaneously, can increase mitigation potential as desired by the Paris Agreement and also help to achieve several of the United Nations’ Sustainable Development Goals.
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