Ecosystem effects of CO 2 concentration: evidence from past climates
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[1] P. Friedlingstein,et al. Carbon-biosphere-climate interactions in the last glacial maximum climate , 1995 .
[2] P. Friedlingstein,et al. The climate induced variation of the continental biosphere: A model simulation of the Last Glacial Maximum , 1992 .
[3] A. Weaver,et al. Carbon storage on exposed continental shelves during the glacial‐interglacial transition , 2006 .
[4] K. Willis,et al. Effect of global atmospheric carbon dioxide on glacial–interglacial vegetation change , 2000 .
[5] J. Guiot,et al. Reconstruction of the Grande Pile Eemian using inverse modeling of biomes and δ13C , 2006 .
[6] Changhui Peng,et al. New coupled model used inversely for reconstructing past terrestrial carbon storage from pollen data: validation of model using modern data , 2009 .
[7] H. Faure,et al. CARBON STORAGE AND CONTINENTAL LAND SURFACE CHANGE SINCE THE LAST GLACIAL MAXIMUM , 1996 .
[8] J. Guiot,et al. Palaeoprecipitation reconstruction by inverse modelling using the isotopic signal of loess organic matter: application to the Nußloch loess sequence (Rhine Valley, Germany) , 2005 .
[9] T. Crowley. Ice Age terrestrial carbon changes revisited , 1995 .
[10] R. Sage. The evolution of C 4 photosynthesis , 2003 .
[11] I. C. Prentice,et al. BIOME3: An equilibrium terrestrial biosphere model based on ecophysiological constraints, resource availability, and competition among plant functional types , 1996 .
[12] Khelifa,et al. Impact of lower atmospheric carbon dioxide on tropical mountain ecosystems , 1997, Science.
[13] Benjamin Smith,et al. Reconstructing and Modeling Past Changes in Terrestrial Primary Productivity , 2001 .
[14] I. Prentice,et al. A general model for the light-use efficiency of primary production , 1996 .
[15] S. Cowling,et al. Simulated ecosystem threshold responses to co-varying temperature, precipitation and atmospheric CO2 within a region of Amazonia , 2006 .
[16] Kenneth L. Denman Canada. Couplings between changes in the climate system and biogeochemistry , 2008 .
[17] H. Fischer,et al. Simulating changes in the terrestrial biosphere during the last glacial/interglacial transition , 2004 .
[18] R. Sage,et al. The evolution of C4 photosynthesis. , 2004, The New phytologist.
[19] S S I T C H,et al. Evaluation of Ecosystem Dynamics, Plant Geography and Terrestrial Carbon Cycling in the Lpj Dynamic Global Vegetation Model , 2022 .
[20] J. Duplessy,et al. Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the Holocene , 1988 .
[21] G. Farquhar,et al. Terrestrial carbon-storage from the last glacial maximum to the present , 1996 .
[22] Michael Lautenschlager,et al. Modelling Global Vegetation Patterns and Terrestrial Carbon Storage at the Last Glacial Maximum , 1993 .
[23] J. Guiot,et al. The climate in Europe during the Eemian: a multi-method approach using pollen data , 2008 .
[24] P. Warnant,et al. CARAIB - A global model of terrestrial biological productivity , 1994 .
[25] M. Sykes,et al. Reply to Williams et al. , 2000, Quaternary Research.
[26] M. G. Ryan,et al. Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO2]-induced enhancement , 2006, Proceedings of the National Academy of Sciences.
[27] S. Idso. A Problem for Paleoclimatology? , 1989, Quaternary Research.
[28] H. Policy,et al. Increase in C3 plant water-use efficiency and biomass over Glacial to present C02 concentrations , 1993, Nature.
[29] F I Woodward,et al. Ecophysiological responses of plants to global environmental change since the Last Glacial Maximum. , 1993, The New phytologist.
[30] D. Schimel,et al. Mechanisms of shrubland expansion: land use, climate or CO2? , 1995 .
[31] R. Ceulemans,et al. Forest response to elevated CO2 is conserved across a broad range of productivity. , 2005, Proceedings of the National Academy of Sciences of the United States of America.
[32] T. Crowley. Ice age carbon , 1991, Nature.
[33] F. Street-Perrott. Palaeo-perspectives: changes in terrestrial ecosystems , 1994 .
[34] I. Terashima,et al. Is photosynthesis suppressed at higher elevations due to low CO2 pressure , 1995 .
[35] F. Chapin,et al. Permafrost and the Global Carbon Budget , 2006, Science.
[36] C. Peng,et al. A data-based re-appraisal of the terrestrial carbon budget at the last glacial maximum , 1993 .
[37] J. Kaplan,et al. Biospheric carbon stocks reconstructed at the Last Glacial Maximum: comparison between general circulation models using prescribed and computed sea surface temperatures , 2002 .
[38] S. Cowling. Tropical forest structure: a missing dimension to Pleistocene landscapes , 2004 .
[39] C. Peng,et al. Reconstruction of past terrestrial carbon storage in the Northern Hemisphere from the Osnabrück Biosphere Model and palaeodata , 1995 .
[40] F. I. Woodward,et al. The importance of low atmospheric CO2 and fire in promoting the spread of grasslands and savannas , 2003 .
[41] W. Parton,et al. Progressive Nitrogen Limitation of Ecosystem Responses to Rising Atmospheric Carbon Dioxide , 2004 .
[42] R. Sage,et al. Interactive effects of low atmospheric CO2 and elevated temperature on growth, photosynthesis and respiration in Phaseolus vulgaris , 1998 .
[43] M. Lautenschlager,et al. Estimating the change of carbon in the terrestrial biosphere from 18 000 BP to present using a carbon cycle model. , 1994, Environmental pollution.
[44] R. Marchant,et al. CO2- and temperature-controlled altitudinal shifts of C4- and C3-dominated grasslands allow reconstruction of palaeoatmospheric pCO2 , 2002 .
[45] P. Bartlein,et al. Do Low CO 2 Concentrations Affect Pollen-Based Reconstructions of LGM Climates? A Response to Physi , 2000 .
[46] I. Prentice. Biome Modelling and the Carbon Cycle , 1993 .
[47] I. C. Prentice,et al. Carbon balance of the terrestrial biosphere in the Twentieth Century: Analyses of CO2, climate and land use effects with four process‐based ecosystem models , 2001 .
[48] G. Farquhar,et al. Do slow‐growing species and nutrient‐stressed plants consistently respond less to elevated CO2? A clarification of some issues raised by Poorter 1998 ) , 2000 .
[49] J. Ehleringer,et al. C4 photosynthesis, atmospheric CO2, and climate , 1997, Oecologia.
[50] J. Berry,et al. A biochemical model of photosynthetic CO2 assimilation in leaves of C3 species , 1980, Planta.
[51] Simon Brewer,et al. Dominant factors controlling glacial and interglacial variations in the treeline elevation in tropical Africa , 2007, Proceedings of the National Academy of Sciences.
[52] T. Stocker,et al. High-resolution carbon dioxide concentration record 650,000–800,000 years before present , 2008, Nature.
[53] D. Ellsworth,et al. Functional responses of plants to elevated atmospheric CO2– do photosynthetic and productivity data from FACE experiments support early predictions? , 2004 .
[54] G. Eglinton,et al. Glacial–interglacial environmental changes inferred from molecular and compound-specific δ13C analyses of sediments from Sacred Lake, Mt. Kenya , 1999 .
[55] A. Palmer,et al. ResearchLetter Is Climate Change a Possible Explanation for Woody Thickening in Arid and Semi-Arid Regions? , 2007 .
[56] Laurent Labeyrie,et al. Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation , 1988 .
[57] P. Valdes,et al. Modeling the dynamics of terrestrial carbon storage since the Last Glacial Maximum , 2002 .
[58] Graham D. Farquhar,et al. Carbon Dioxide and Vegetation , 1997, Science.
[59] Beerling. New estimates of carbon transfer to terrestrial ecosystems between the last glacial maximum and the Holocene , 1999 .
[60] J. Maley,et al. Late Quaternary palaeoenvironments in the Lake Barombi Mbo (West Cameroon) deduced from pollen and carbon isotopes of organic matter , 1994 .
[61] C. Delire,et al. Modelling the glacial-interglacial changes in the continental biosphere , 1998 .
[62] G. Farquhar,et al. The CO 2 Dependence of Photosynthesis, Plant Growth Responses to Elevated Atmospheric CO 2 Concentrations and Their Interaction with Soil Nutrient Status. I. General Principles and Forest Ecosystems , 1996 .
[63] Robert J. Scholes,et al. The Carbon Cycle and Atmospheric Carbon Dioxide , 2001 .
[64] Yang Wang,et al. Expansion of C4 ecosystems as an indicator of global ecological change in the late Miocene , 1993, Nature.
[65] T. Johannessen,et al. A high resolution palaeoclimatic record for the last 27,500 years in tropical West Africa from the carbon and nitrogen isotopic composition of lacustrine organic matter , 1992 .
[66] T. Ku,et al. Carbon isotopic variations on glacial‐to‐interglacial time scales in the ocean: Modeling and implications , 1992 .
[67] F. Woodward,et al. Increases in terrestrial carbon storage from the Last Glacial Maximum to the present , 1990, Nature.
[68] M. Maslin,et al. Paleovegetation Simulations of Lowland Amazonia and Implications for Neotropical Allopatry and Speciation , 2001, Quaternary Research.
[69] Jolly,et al. Effect of Low Glacial Atmospheric CO2 on Tropical African Montane Vegetation , 1997, Science.
[70] J. Guiot,et al. East Asian Monsoon and paleoclimatic data analysis: a vegetation point of view , 2008 .
[71] J. Guiot,et al. A few prospective ideas on climate reconstruction: from a statistical single proxy approach towards a multi-proxy and dynamical approach , 2009 .
[72] Sandy P. Harrison,et al. Climate and CO2 controls on global vegetation distribution at the last glacial maximum: analysis based on palaeovegetation data, biome modelling and palaeoclimate simulations , 2003 .
[73] G. Ramstein,et al. Climate of the Past Discussions is the access reviewed discussion forum of Climate of the Past How cold was Europe at the Last Glacial Maximum? A synthesis of the progress achieved since the first PMIP model-data comparison , 2007 .
[74] S. Aref,et al. Inter-annual variation in the response of Pinus taeda tree growth to long term Free Air Carbon dioxide Enrichment (FACE) , 2005 .
[75] Guy F. Midgley,et al. A proposed CO2‐controlled mechanism of woody plant invasion in grasslands and savannas , 2000 .
[76] M. Maslin,et al. Balancing the deglacial global carbon budget: the hydrate factor , 2001 .
[77] Christian Körner,et al. Biosphere responses to CO2 enrichment. , 2000 .
[78] Sandy P. Harrison,et al. Climate change and Arctic ecosystems: 2. Modeling, paleodata‐model comparisons, and future projections , 2003 .
[79] C. Loehle. Predicting Pleistocene climate from vegetation in North America , 2007 .
[80] F. Joos,et al. A Paleo-perspective on changes in atmospheric CO2 and climate , 2004 .
[81] John L. Monteith,et al. A reinterpretation of stomatal responses to humidity , 1995 .
[82] F. Woodward,et al. Global response of terrestrial ecosystem structure and function to CO2 and climate change: results from six dynamic global vegetation models , 2001 .
[83] H. W. Polley,et al. Nitrogen and Water Requirements of C 3 Plants Grown at Glacial to Present Carbon Dioxide Concentrations , 1995 .
[84] Paul J. Valdes,et al. Transient simulations of Holocene atmospheric carbon dioxide and terrestrial carbon since the Last Glacial Maximum , 2004 .
[85] S. Long,et al. Review Tansley Review , 2022 .
[86] Denis-Didier Rousseau,et al. Climate reconstruction from pollen and δ 13 C records using inverse vegetation modeling – Implication for past and future climates , 2009 .
[87] R. B. Jackson,et al. Increases in nitrogen uptake rather than nitrogen-use efficiency support higher rates of temperate forest productivity under elevated CO2 , 2007, Proceedings of the National Academy of Sciences.
[88] I. Fung,et al. The sensitivity of terrestrial carbon storage to climate change , 1990, Nature.
[89] G. Farquhar,et al. Terrestrial carbon storage at the LGM , 1994, Nature.
[90] S. Long,et al. What have we learned from 15 years of free-air CO2 enrichment (FACE)? A meta-analytic review of the responses of photosynthesis, canopy properties and plant production to rising CO2. , 2004, The New phytologist.
[91] P. Bartlein,et al. Do Low CO2 Concentrations Affect Pollen-Based Reconstructions of LGM Climates? A Response to “Physiological Significance of Low Atmospheric CO2 for Plant–Climate Interactions” by Cowling and Sykes , 2000, Quaternary Research.
[92] Simon Brewer,et al. Climatic changes in Eurasia and Africa at the last glacial maximum and mid-Holocene: reconstruction from pollen data using inverse vegetation modelling , 2007 .
[93] L. François,et al. The Late Quaternary History of Biogeochemical Cycling of Carbon , 2003 .
[94] R. Siegwolf,et al. Carbon Flux and Growth in Mature Deciduous Forest Trees Exposed to Elevated CO2 , 2005, Science.
[95] Michael Sarnthein,et al. Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years , 1988 .
[96] Jelle Bijma,et al. Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes , 1997, Nature.
[97] D. Jolly,et al. Mid‐Holocene and glacial‐maximum vegetation geography of the northern continents and Africa , 2000 .
[98] I. R. Cowan,et al. Stomatal conductance correlates with photosynthetic capacity , 1979, Nature.
[99] A. Palmer,et al. Is Climate Change a Possible Explanation for Woody Thickening in Arid and Semi-Arid Regions? , 2007 .
[100] Bjarne Stroustrup. The Evolution of C , 1987 .
[101] S. Gerber,et al. Sensitivity of a dynamic global vegetation model to climate and atmospheric CO2 , 2004 .
[102] M. Maslin,et al. Estimating the carbon transfer between the ocean, atmosphere and the terrestrial biosphere since the last glacial maximum , 1995 .
[103] S. Aref,et al. Annual basal area increment and growth duration of Pinus taeda in response to eight years of free‐air carbon dioxide enrichment , 2006 .
[104] A. Sharon. Simulated effects of low atmospheric CO2 on structure and composition of North American vegetation at the Last Glacial Maximum , 1999 .
[105] Jean-Jacques Boreux,et al. Inverse vegetation modeling by Monte Carlo sampling to reconstruct palaeoclimates under changed precipitation seasonality and CO2 conditions: application to glacial climate in Mediterranean region , 2000 .
[106] Christopher B. Field,et al. Environmental control of leaf area production: Implications for vegetation and land‐surface modeling , 2003 .
[107] S. Cowling. Plants and Temperature--CO2 Uncoupling , 1999, Science.
[108] T. Ikeda,et al. Carbon cycling and climate change during the last glacial cycle inferred from the isotope records using an ocean biogeochemical carbon cycle model , 2003 .
[109] N. Zeng. Glacial-interglacial atmospheric CO2 change —The glacial burial hypothesis , 2003 .
[110] T. Stocker,et al. Stable Carbon CycleClimate Relationship During the Late Pleistocene , 2005, Science.
[111] Changhui Peng,et al. Estimating changes in terrestrial vegetation and carbon storage: Using palaeoecological data and models , 1998 .
[112] D. Cole,et al. Influence of atmospheric CO2 on the decline of C4 plants during the last deglaciation , 1994, Nature.
[113] N. Shackleton. Carbon-13 in Uvigerina: Tropical Rainforest History and the Equatorial Pacific Carbonate Dissolution Cycles , 1977 .
[114] S. Cowling. Plant carbon balance, evolutionary innovation and extinction in land plants , 2001 .
[115] Chris Jones,et al. Illuminating the Modern Dance of Climate and CO2 , 2008, Science.
[116] H. Faure,et al. A new estimate of changing carbon storage on land since the last glacial maximum, based on global land ecosystem reconstruction , 1998 .
[117] Martin T. Sykes,et al. Physiological Significance of Low Atmospheric CO2 for Plant–Climate Interactions , 1999, Quaternary Research.
[118] G. Ramstein,et al. Carbon stocks and isotopic budgets of the terrestrial biosphere at mid-Holocene and last glacial maximum times , 1999 .
[119] James S. Clark,et al. Effects of climate and atmospheric CO2 partial pressure on the global distribution of C4 grasses: present, past, and future , 1998, Oecologia.