Future productivity and carbon storage limited by terrestrial nutrient availability

Nutrient limitation of plant growth can reduce net plant productivity. Model projections indicate that productivity declines when nitrogen and phosphorus limitations are considered, turning terrestrial ecosystems into a net source of CO2 by 2100.

[1]  R. Matear,et al.  Nitrogen and phosphorous limitations significantly reduce future allowable CO2 emissions , 2014 .

[2]  K.,et al.  Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models , 2012 .

[3]  T. E. Osterkamp,et al.  The effect of permafrost thaw on old carbon release and net carbon exchange from tundra , 2009, Nature.

[4]  C. Evans Nitrogen and climate change , 2006 .

[5]  J. Melillo,et al.  Soil warming, carbon–nitrogen interactions, and forest carbon budgets , 2011, Proceedings of the National Academy of Sciences.

[6]  B. Kruijt,et al.  Should phosphorus availability be constraining moist tropical forest responses to increasing CO2 concentrations , 2001 .

[7]  Sandy P. Harrison,et al.  Global Biogeochemical Cycles in the Climate System , 2001 .

[8]  R. B. Jackson,et al.  Progressive nitrogen limitation of ecosystem processes under elevated CO2 in a warm-temperate forest. , 2006, Ecology.

[9]  Pierre Friedlingstein,et al.  Terrestrial nitrogen feedbacks may accelerate future climate change , 2010 .

[10]  G. Katul,et al.  Soil fertility limits carbon sequestration by forest ecosystems in a CO2-enriched atmosphere , 2001, Nature.

[11]  Maurizio Santoro,et al.  Global covariation of carbon turnover times with climate in terrestrial ecosystems , 2014, Nature.

[12]  P. Ciais,et al.  Fertile forests produce biomass more efficiently. , 2012, Ecology letters.

[13]  J. B. Miller,et al.  Increase in observed net carbon dioxide uptake by land and oceans during the past 50 years , 2012, Nature.

[14]  Jeffrey M. Warren,et al.  CO2 enhancement of forest productivity constrained by limited nitrogen availability , 2010, Proceedings of the National Academy of Sciences.

[15]  Rachel M. Law,et al.  A global model of carbon, nitrogen and phosphorus cycles for the terrestrial biosphere , 2009 .

[16]  P. Ciais,et al.  Permafrost carbon-climate feedbacks accelerate global warming , 2011, Proceedings of the National Academy of Sciences.

[17]  W. Silver,et al.  Some aspects of ecophysiological and biogeochemical responses of tropical forests to atmospheric change. , 2004, Philosophical transactions of the Royal Society of London. Series B, Biological sciences.

[18]  Michael Obersteiner,et al.  Human-induced nitrogen–phosphorus imbalances alter natural and managed ecosystems across the globe , 2013, Nature Communications.

[19]  P. Cox,et al.  Evaluating the Land and Ocean Components of the Global Carbon Cycle in the CMIP5 Earth System Models , 2013 .

[20]  W. Parton,et al.  Patterns of new versus recycled primary production in the terrestrial biosphere , 2013, Proceedings of the National Academy of Sciences.

[21]  J. Randerson,et al.  Changes in soil organic carbon storage predicted by Earth system models during the 21st century , 2013 .

[22]  D. Clark,et al.  Field‐quantified responses of tropical rainforest aboveground productivity to increasing CO2 and climatic stress, 1997–2009 , 2013 .

[23]  G. Kowalchuk,et al.  Shifting carbon flow from roots into associated microbial communities in response to elevated atmospheric CO2 , 2010, Proceedings of the National Academy of Sciences.

[24]  Peter E. Thornton,et al.  Influence of carbon‐nitrogen cycle coupling on land model response to CO2 fertilization and climate variability , 2007 .

[25]  Benjamin Z. Houlton,et al.  Nitrogen constraints on terrestrial carbon uptake: Implications for the global carbon‐climate feedback , 2009 .

[26]  S. Gerber,et al.  Nitrogen cycling and feedbacks in a global dynamic land model , 2010 .

[27]  Benjamin Smith,et al.  Robustness and uncertainty in terrestrial ecosystem carbon response to CMIP5 climate change projections , 2012 .

[28]  E. Bernhardt,et al.  Enhanced root exudation induces microbial feedbacks to N cycling in a pine forest under long-term CO2 fumigation. , 2011, Ecology letters.

[29]  Stephen Porder,et al.  Relationships among net primary productivity, nutrients and climate in tropical rain forest: a pan-tropical analysis. , 2011, Ecology letters.

[30]  Stephen Porder,et al.  Terrestrial phosphorus limitation: mechanisms, implications, and nitrogen-phosphorus interactions. , 2010, Ecological applications : a publication of the Ecological Society of America.

[31]  Helmut Hillebrand,et al.  Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems. , 2007, Ecology letters.