C and N in soil organic matter density fractions under elevated atmospheric CO2: Turnover vs. stabilization

[1]  S. Blagodatsky,et al.  Turnover of soil organic matter and of microbial biomass under C3–C4 vegetation change: Consideration of 13C fractionation and preferential substrate utilization , 2011 .

[2]  Y. Kuzyakov,et al.  Source determination of lipids in bulk soil and soil density fractions after four years of wheat cropping , 2010 .

[3]  S. Blagodatsky,et al.  Elevated atmospheric CO2 increases microbial growth rates in soil: results of three CO2 enrichment experiments , 2010 .

[4]  S. Marhan,et al.  Indirect effects of soil moisture reverse soil C sequestration responses of a spring wheat agroecosystem to elevated CO2 , 2010 .

[5]  H. Wieser,et al.  Effects of elevated CO2 on grain yield and quality of wheat: results from a 3-year free-air CO2 enrichment experiment. , 2009, Plant biology.

[6]  R. Bol,et al.  Molecular turnover time of soil organic matter in particle-size fractions of an arable soil. , 2009, Rapid communications in mass spectrometry : RCM.

[7]  S. Marhan,et al.  Stimulation of microbial extracellular enzyme activities by elevated CO2 depends on soil aggregate size , 2009 .

[8]  Shuijin Hu,et al.  Enhanced litter input rather than changes in litter chemistry drive soil carbon and nitrogen cycles under elevated CO2: a microcosm study , 2009 .

[9]  M. Moscatelli,et al.  The influence of temperature and labile C substrates on heterotrophic respiration in response to elevated CO2 and nitrogen fertilization , 2009, Plant and Soil.

[10]  M. Hoosbeek,et al.  Increased Litter Build Up and Soil Organic Matter Stabilization in a Poplar Plantation After 6 Years of Atmospheric CO2 Enrichment (FACE): Final Results of POP-EuroFACE Compared to Other Forest FACE Experiments , 2009, Ecosystems.

[11]  R. B. Jackson,et al.  Soil carbon sequestration in a pine forest after 9 years of atmospheric CO2 enrichment , 2008 .

[12]  H. Weigel,et al.  Thermal stability of soil organic matter pools and their turnover times calculated by δ13C under elevated CO2 and two levels of N fertilisation , 2008, Isotopes in environmental and health studies.

[13]  H. Weigel,et al.  Soil carbon isotopic composition and soil carbon content in an agroecosystem during six years of Free Air Carbon dioxide Enrichment (FACE) , 2008, Isotopes in environmental and health studies.

[14]  Klaus Kaiser,et al.  How relevant is recalcitrance for the stabilization of organic matter in soils , 2008 .

[15]  P. Grootes,et al.  Storage and stability of organic matter and fossil carbon in a Luvisol and Phaeozem with continuous maize cropping: A synthesis § , 2008 .

[16]  S. Marhan,et al.  Soil organic matter mineralization and residue decomposition of spring wheat grown under elevated CO2 atmosphere , 2008 .

[17]  M. Schmidt,et al.  Plant and soil lipid modification under elevated atmospheric CO2 conditions: II. Stable carbon isotopic values (δ13C) and turnover , 2008 .

[18]  J. Six,et al.  The impact of long-term elevated CO2 on C and N retention in stable SOM pools , 2008, Plant and Soil.

[19]  Bernd Marschner,et al.  SOM fractionation methods: Relevance to functional pools and to stabilization mechanisms , 2007 .

[20]  Y. Kuzyakov,et al.  Effects of atmospheric CO2 enrichment on δ13C, δ15N values and turnover times of soil organic matter pools isolated by thermal techniques , 2007, Plant and Soil.

[21]  Vincent R. Gray.  Climate Change 2007: The Physical Science Basis Summary for Policymakers , 2007 .

[22]  K. Klumpp,et al.  Long-term steady state 13 C labelling to investigate soil carbon turnover in grasslands , 2007 .

[23]  Johan Six,et al.  Interactions between plant growth and soil nutrient cycling under elevated CO2: a meta‐analysis , 2006 .

[24]  J. Six,et al.  Total soil C and N sequestration in a grassland following 10 years of free air CO2 enrichment , 2006 .

[25]  Y. Kuzyakov,et al.  Effect of C3–C4 Vegetation Change on δ13C and δ15N Values of Soil Organic Matter Fractions Separated by Thermal Stability , 2006, Plant and Soil.

[26]  Valentí Rull,et al.  Unexpected biodiversity loss under global warming in the neotropical Guayana Highlands: a preliminary appraisal , 2006 .

[27]  A. Fangmeier,et al.  Atmospheric carbon dioxide enrichment effects on ecosystems — experiments and the real world , 2006 .

[28]  R. Norby,et al.  Elevated atmospheric carbon dioxide increases soil carbon , 2005 .

[29]  H. Black,et al.  Rising Atmospheric CO2 Reduces Sequestration of Root-Derived Soil Carbon , 2005, Science.

[30]  H. Flessa,et al.  Storage of organic carbon in aggregate and density fractions of silty soils under different types of land use , 2005 .

[31]  M. Kaiser,et al.  Stability and composition of different soluble soil organic matter fractions-evidence from δ13C and FTIR signatures , 2005 .

[32]  W. Schlesinger,et al.  SOIL CARBON SEQUESTRATION AND TURNOVER IN A PINE FOREST AFTER SIX YEARS OF ATMOSPHERIC CO2 ENRICHMENT , 2005 .

[33]  A. Polle,et al.  Leaf litter production and decomposition in a poplar short‐rotation coppice exposed to free air CO2 enrichment (POPFACE) , 2005 .

[34]  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.

[35]  W. Parton,et al.  Progressive Nitrogen Limitation of Ecosystem Responses to Rising Atmospheric Carbon Dioxide , 2004 .

[36]  F. S. Nakayama,et al.  Carbon isotopes and carbon turnover in cotton and wheat FACE experiments , 1995, Plant and Soil.

[37]  R. Kohli,et al.  Effect of eucalyptus oil on germination and growth of Phaseolus aureus Roxb. , 1991, Plant and Soil.

[38]  W. Horwath,et al.  Impact of elevated CO2 on soil organic matter dynamics as related to changes in aggregate turnover and residue quality , 2004, Plant and Soil.

[39]  R. Cully,et al.  Recalcitrant soil organic materials mineralize more efficiently at higher temperatures , 2003 .

[40]  W. Bowman,et al.  Variable effects of nitrogen additions on the stability and turnover of soil carbon , 2002, Nature.

[41]  Stan D. Wullschleger,et al.  Net primary productivity of a CO2-enriched deciduous forest and the implications for carbon storage , 2002 .

[42]  B. Christensen.  Physical fractionation of soil and structural and functional complexity in organic matter turnover , 2001 .

[43]  F. Miglietta,et al.  Free‐air CO2 enrichment (FACE) of a poplar plantation: the POPFACE fumigation system , 2001 .

[44]  R. Siegwolf,et al.  Carbon allocation in calcareous grassland under elevated CO2: a combined 13C pulse‐labelling/soil physical fractionation study , 2001 .

[45]  H. W. Hunt,et al.  Management options for reducing CO2 emissions from agricultural soils , 2000 .

[46]  Rattan Lal,et al.  Soil processes and the carbon cycle. , 1998 .

[47]  J. Balesdent,et al.  The significance of organic separates to carbon dynamics and its modelling in some cultivated soils , 1996 .

[48]  J. Balesdent,et al.  Measurement of soil organic matter turnover using 13C natural abundance. , 1996 .

[49]  T. Boutton,et al.  Mass spectrometry of soils , 1996 .

[50]  B. Ellert,et al.  Turnover of soil organic matter and storage of corn residue carbon estimated from natural 13C abundance , 1995 .