Impacts of climate change drivers on C4 grassland productivity: scaling driver effects through the plant community

Climate change drivers affect plant community productivity via three pathways: (i) direct effects of drivers on plants; (ii) the response of species abundances to drivers (community response); and (iii) the feedback effect of community change on productivity (community effect). The contribution of each pathway to driver-productivity relationships depends on functional traits of dominant species. We used data from three experiments in Texas, USA, to assess the role of community dynamics in the aboveground net primary productivity (ANPP) response of C4 grasslands to two climate drivers applied singly: atmospheric CO2 enrichment and augmented summer precipitation. The ANPP-driver response differed among experiments because community responses and effects differed. ANPP increased by 80-120g m(-2) per 100 μl l(-1) rise in CO2 in separate experiments with pasture and tallgrass prairie assemblages. Augmenting ambient precipitation by 128mm during one summer month each year increased ANPP more in native than in exotic communities in a third experiment. The community effect accounted for 21-38% of the ANPP CO2 response in the prairie experiment but little of the response in the pasture experiment. The community response to CO2 was linked to species traits associated with greater soil water from reduced transpiration (e.g. greater height). Community effects on the ANPP CO2 response and the greater ANPP response of native than exotic communities to augmented precipitation depended on species differences in transpiration efficiency. These results indicate that feedbacks from community change influenced ANPP-driver responses. However, the species traits that regulated community effects on ANPP differed from the traits that determined how communities responded to drivers.

[1]  E. Pendall,et al.  Invasive forb benefits from water savings by native plants and carbon fertilization under elevated CO2 and warming. , 2013, The New phytologist.

[2]  David T. Taylor,et al.  Climate Change and North American Rangelands: Trends, Projections, and Implications , 2013 .

[3]  M. S. Moran,et al.  Ecosystem resilience despite large-scale altered hydroclimatic conditions , 2013, Nature.

[4]  B. Wilsey,et al.  Simple plant traits explain functional group diversity decline in novel grassland communities of Texas , 2013, Plant Ecology.

[5]  R. B. Jackson,et al.  Soil-mediated effects of subambient to increased carbon dioxide on grassland productivity , 2012 .

[6]  V. Jin,et al.  Feedback from plant species change amplifies CO2 enhancement of grassland productivity , 2012, Global change biology.

[7]  Simon Scheiter,et al.  Fire and fire-adapted vegetation promoted C4 expansion in the late Miocene. , 2012, The New phytologist.

[8]  B. Hungate,et al.  Biogeochemical and ecological feedbacks in grassland responses to warming , 2012 .

[9]  L. Sack,et al.  Evolution of C4 plants: a new hypothesis for an interaction of CO2 and water relations mediated by plant hydraulics , 2012, Philosophical Transactions of the Royal Society B: Biological Sciences.

[10]  V. Jin,et al.  CO2‐caused change in plant species composition rivals the shift in vegetation between mid‐grass and tallgrass prairies , 2012 .

[11]  B. Wilsey,et al.  Biodiversity, phenology and temporal niche differences between native- and novel exotic-dominated grasslands , 2011 .

[12]  J. Nielsen‐Gammon,et al.  A New Homogenized Climate Division Precipitation Dataset for Analysis of Climate Variability and Climate Change , 2011 .

[13]  M. Simpson Global Climate Change Impacts in the United States , 2011 .

[14]  G. Combs,et al.  CO2 enrichment increases element concentrations in grass mixtures by changing species abundances , 2011, Plant Ecology.

[15]  Yiqi Luo,et al.  Nitrogen regulation of the climate-carbon feedback: evidence from a long-term global change experiment. , 2010, Ecology.

[16]  J. Megonigal,et al.  Ecosystem response to elevated CO2 levels limited by nitrogen-induced plant species shift , 2010, Nature.

[17]  S. Collins,et al.  A framework for assessing ecosystem dynamics in response to chronic resource alterations induced by global change. , 2009, Ecology.

[18]  R. B. Jackson,et al.  Primary Productivity and Water Balance of Grassland Vegetation on Three Soils in a Continuous CO2 Gradient: Initial Results from the Lysimeter CO2 Gradient Experiment , 2009, Ecosystems.

[19]  B. Wilsey,et al.  Biodiversity maintenance mechanisms differ between native and novel exotic-dominated communities. , 2009, Ecology letters.

[20]  B. Soden,et al.  Atmospheric Warming and the Amplification of Precipitation Extremes , 2008, Science.

[21]  Larry L. Tieszen,et al.  Climate controls on C3 vs. C4 productivity in North American grasslands from carbon isotope composition of soil organic matter , 2008 .

[22]  J. O H A N N E,et al.  Scaling environmental change through the community-level: a trait-based response-and-effect framework for plants , 2008 .

[23]  J. O S E P,et al.  Climate controls on C 3 vs . C 4 productivity in North American grasslands from carbon isotope composition of soil organic matter , 2008 .

[24]  Philip A. Fay,et al.  Initial response of evapotranspiration from tallgrass prairie vegetation to CO2 at subambient to elevated concentrations , 2007 .

[25]  H. W. Polley,et al.  C3–C4 composition and prior carbon dioxide treatment regulate the response of grassland carbon and water fluxes to carbon dioxide , 2007 .

[26]  H. L. Miller,et al.  Climate Change 2007: The Physical Science Basis , 2007 .

[27]  James B. Grace,et al.  Structural Equation Modeling and Natural Systems , 2006 .

[28]  G. McCabe,et al.  Shifting covariability of North American summer monsoon precipitation with antecedent winter precipitation , 2006 .

[29]  R. B. Jackson,et al.  Potential nitrogen constraints on soil carbon sequestration under low and elevated atmospheric CO2. , 2006, Ecology.

[30]  P. Reich,et al.  Species and functional group diversity independently influence biomass accumulation and its response to CO2 and N. , 2004, Proceedings of the National Academy of Sciences of the United States of America.

[31]  J. Zak,et al.  Convergence across biomes to a common rain-use efficiency , 2004, Nature.

[32]  M. R. Shaw,et al.  Water relations in grassland and desert ecosystems exposed to elevated atmospheric CO2 , 2004, Oecologia.

[33]  D. Ellsworth,et al.  Functional responses of plants to elevated atmospheric CO2– do photosynthetic and productivity data from FACE experiments support early predictions? , 2004 .

[34]  R. B. Jackson,et al.  CO2 alters water use, carbon gain, and yield for the dominant species in a natural grassland , 1994, Oecologia.

[35]  J. Derner,et al.  Increasing CO2 from subambient to superambient concentrations alters species composition and increases above-ground biomass in a C3 /C4 grassland. , 2003, The New phytologist.

[36]  J. Zak,et al.  Assessing the Response of Terrestrial Ecosystems to Potential Changes in Precipitation , 2003 .

[37]  M. Hoerling,et al.  The Perfect Ocean for Drought , 2003, Science.

[38]  J. Derner,et al.  Increasing CO 2 from subambient to superambient concentrations alters species composition and increases above-ground biomass in a C 3 / C 4 grassland , 2003 .

[39]  J. Derner,et al.  Soil‐ and plant‐water dynamics in a C3/C4 grassland exposed to a subambient to superambient CO2 gradient , 2002 .

[40]  G. L. Hutchinson,et al.  Response of C3 and C4 grasses to supplemental summer precipitation. , 2002 .

[41]  R. B. Jackson,et al.  Nonlinear grassland responses to past and future atmospheric CO2 , 2002, Nature.

[42]  R. B. Jackson,et al.  Stomatal acclimation over a subambient to elevated CO2 gradient in a C3/C4 grassland , 2002 .

[43]  H. W. Polley,et al.  Net grassland carbon flux over a subambient to superambient CO2 gradient , 2001 .

[44]  R. B. Jackson,et al.  Gas exchange and photosynthetic acclimation over subambient to elevated CO2 in a C3–C4 grassland , 2001 .

[45]  H. W. Polley,et al.  Gas exchange and photosynthetic acclimation over subambient to elevated CO 2 in a C 3 -C 4 grassland , 2001 .

[46]  J. Morgan,et al.  Elevated CO2 enhances water relations and productivity and affects gas exchange in C3 and C4 grasses of the Colorado shortgrass steppe. , 2001 .

[47]  Bill Shipley,et al.  Cause and Correlation in Biology: A User''s Guide to Path Analysis , 2016 .

[48]  H. W. Polley,et al.  Elongated chambers for field studies across atmospheric CO2 gradients. , 2000 .

[49]  S. Wand,et al.  Responses of wild C4 and C3 grass (Poaceae) species to elevated atmospheric CO2 concentration: a meta‐analytic test of current theories and perceptions , 1999 .

[50]  J. Jouzel,et al.  Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica , 1999, Nature.

[51]  A. Knapp,et al.  Biomass production and species composition change in a tallgrass prairie ecosystem after long‐term exposure to elevated atmospheric CO2 , 1999 .

[52]  K. Knapp,et al.  Biomass production and species composition change in a tallgrass prairie ecosystem after long-term exposure to elevated atmospheric CO 2 , 1999 .

[53]  R. B. Jackson,et al.  Photosynthesis, growth and density for the dominant species in a CO2-enriched grassland , 1995 .

[54]  C. D. Keeling,et al.  Atmospheric CO 2 records from sites in the SIO air sampling network , 1994 .

[55]  R. Sepanski,et al.  TRENDS '90: A compendium of data on global change , 1991 .

[56]  W. Parton,et al.  Primary Production of the Central Grassland Region of the United States , 1988 .

[57]  C. C. Black CO2 and plants, the response of plant to rising levels of atmospheric carbon dioxide: Edgar R. Lemon (Editor). Westview Press, Boulder, 1983. AAAS Selected Symposia Series, 84. XXII + 280 pp., US $25.00 (hardcover) , 1984 .