Research Articles |
|
|
|
|
Responses of gross primary productivity to different sizes of precipitation events in a temperate grassland ecosystem in Inner Mongolia, China |
GUO Qun1, LI Shenggong1, HU Zhongmin1*, ZHAO Wei1, 2, YU Guirui1, SUN Xiaomin1, LI Linghao3, LIANG Naishen4, BAI Wenming3 |
1 Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
2 University of Chinese Academy of Sciences, Beijing 100049, China;
3 State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China;
4 Global Carbon Cycle Research Section Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba 305-8506, Japan |
|
|
Abstract Changes in the sizes of precipitation events in the context of global climate change may have profound impacts on ecosystem productivity in arid and semiarid grasslands. However, we still have little knowledge about to what extent grassland productivity will respond to an individual precipitation event. In this study, we quantified the duration, the maximum, and the time-integrated amount of the response of daily gross primary productivity (GPP) to an individual precipitation event and their variations with different sizes of precipitation events in a typical temperate steppe in Inner Mongolia, China. Results showed that the duration of GPP-response (τR) and the maximum absolute GPP-response (GPPmax) increased linearly with the sizes of precipitation events (Pes), driving a corresponding increase in time-integrated amount of the GPP-response (GPPtotal) because variations of GPPtotal were largely explained by τR and GPPmax. The relative contributions of these two parameters to GPPtotal were strongly Pes-dependent. The GPPmax contributed more to the variations of GPPtotal when Pes was relatively small (<20 mm), whereas τR was the main driver to the variations of GPPtotal when Pes was relatively large. In addition, a threshold size of at least 5 mm of precipitation was required to induce a GPP-response for the temperate steppe in this study. Our work has important implications for the modeling community to obtain an advanced understanding of productivity-response of grassland ecosystems to altered precipitation regimes.
|
Received: 25 March 2015
Published: 10 February 2016
|
Fund: This study was jointly supported by the National Natural Science Foundation of China (31400425, 31570437, 41301043, 31420103917), the National Key Project of Scientific and Technical Supporting Program (2013BAC03B03), the Funding for Talented Young Scientists of IGSNRR (2013RC203), and the Social Foundation of Beijing Academy of Social Sciences (154005). |
Cite this article:
GUO Qun, LI Shenggong, HU Zhongmin, ZHAO Wei, YU Guirui, SUN Xiaomin, LI Linghao, LIANG Naishen, BAI Wenming. Responses of gross primary productivity to different sizes of precipitation events in a temperate grassland ecosystem in Inner Mongolia, China. Journal of Arid Land, 2016, 8(1): 36-46.
URL:
http://jal.xjegi.com/10.1007/s40333-015-0136-7 OR http://jal.xjegi.com/Y2016/V8/I1/36
|
|
|
Austin A T, Yahdjian L, Stark J M, et al. 2004. Water pulses and biogeochemical cycles in arid and semiarid ecosystems. Oecologia, 141(2): 221–235.Bai Y F, Wu J G, Xing Q, et al. 2008. Primary production and rain use efficiency across a precipitation gradient on the Mongolia Plateau. Ecology, 89(8): 2140–2153.Beier C, Beierkuhnlein C, Wohlgemuth T, et al. 2012. Precipitation manipulation experiments--challenges and recommendations for the future. Ecology Letters, 15(8): 899–911.Chen S P, Lin G H, Huang J H, et al. 2009. Dependence of carbon sequestration on the differential responses of ecosystem photosynthesis and respiration to rain pulses in a semiarid steppe. Global Change Biology, 15(10): 2450–2461.Cherwin K, Knapp A. 2012. Unexpected patterns of sensitivity to drought in three semi-arid grasslands. Oecologia, 169(3): 845–852.Easterling D R, Meehl G A, Parmesan C, et al. 2000. Climate extremes: Observations, modeling, and impacts. Science, 289(5487): 2068–2074.FAO. 1974. Soil Map of the World 1:5,000,000. Volumes 1–10. Paris: Food and Agriculture Organization of the United Nations and UNESCO.Fay P A, Carlisle J D, Knapp A K, et al. 2003. Productivity responses to altered rainfall patterns in a C4-dominated grassland. Oecologia, 137(2): 245–251.Hao Y B, Wang Y F, Mei X R, et al. 2010. The response of ecosystem CO2 exchange to small precipitation pulses over a temperate steppe. Plant Ecology, 209(2): 335–347.Hao Y B, Kang X M, Cui X Y, et al. 2012. Verification of a threshold concept of ecologically effective precipitation pulse: From plant individuals to ecosystem. Ecological Informatics, 12: 23–30.Harper C W, Blair J M, Fay P A, et al. 2005. Increased rainfall variability and reduced rainfall amount decreases soil CO2 flux in a grassland ecosystem. Global Change Biology, 11(2): 322–334.He Z B, Zhao W Z, Liu H, et al. 2012. The response of soil moisture to rainfall event size in subalpine grassland and meadows in a semi-arid mountain range: A case study in northwestern China’s Qilian Mountains. Journal of Hydrology, 420–421: 183–190.Heisler-White J L, Knapp A K, Kelly E F. 2008. Increasing precipitation event size increases aboveground net primary productivity in a semi-arid grassland. Oecologia, 158(1): 129–140.Heisler-White J L, Blair J M, Kelly E F, et al. 2009. Contingent productivity responses to more extreme rainfall regimes across a grassland biome. Global Change Biology, 15(12): 2894–2904.Hu Z M, Fan J W, Zhong H P, et al. 2007. Spatiotemporal dynamics of aboveground primary productivity along a precipitation gradient in Chinese temperate grassland. Science in China Series D: Earth Sciences, 50(5): 754–764.Hu Z M, Yu G R, Fu Y L, et al. 2008. Effects of vegetation control on ecosystem water use efficiency within and among four grassland ecosystems in China. Global Change Biology, 14(7): 1609–1619.Hu Z M, Yu G R, Zhou Y L, et al. 2009. Partitioning of evapotranspiration and its controls in four grassland ecosystems: Application of a two-source model. Agricultural and Forest Meteorology, 149(9): 1410–1420.Hu Z M, Yu G R, Fan J W, et al. 2010. Precipitation-use efficiency along a 4500-km grassland transect. Global Ecology and Biogeography, 19(6): 842–851.Huang G, Li Y, Padilla F M. 2015. Ephemeral plants mediate responses of ecosystem carbon exchange to increased precipitation in a temperate desert. Agricultural and Forest Meteorology, 201: 141–152.Huxman T E, Snyder K A, Tissue D, et al. 2004a. Precipitation pulses and carbon fluxes in semiarid and arid ecosystems. Oecologia, 141(2): 254–268.Huxman T E, Cable J M, Ignace D D, et al. 2004b. Response of net ecosystem gas exchange to a simulated precipitation pulse in a semi-arid grassland: the role of native versus non-native grasses and soil texture. Oecologia, 141(2): 295–305.Intergovernmental Panel on Climate Change (IPCC). 2013. Long-term Climate Change: Projections, Commitments and Irreversibility. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, USA: Cambridge University Press.Jobbágy E G, Sala O E. 2000. Controls of grass and shrub aboveground production in the Patagonian steppe. Ecological Applications, 10(2): 541–549.Knapp A K, Fay P A, Blair J M, et al. 2002. Rainfall variability, carbon cycling, and plant species diversity in a mesic grassland. Science, 298(5601): 2202–2205.Knapp A K, Beier C, Briske D D, et al. 2008. Consequences of more extreme precipitation regimes for terrestrial ecosystems. BioScience, 58(9): 811–821.Kurc S A, Small E E. 2007. Soil moisture variations and ecosystem-scale fluxes of water and carbon in semiarid grassland and shrubland. Water Resources Research, 43(6): W06416.Lauenroth W K, Bradford J B. 2012. Ecohydrology of dry regions of the United States: water balance consequences of small precipitation events. Ecohydrology, 5(1): 46–53.Li F, Zhao W Z, Liu H. 2013. The response of aboveground aboveground net primary productivity of desert vegetation to rainfall pulse in the temperate desert region of northwest China. PLoS ONE, 8(9): e73003.Li X J, Li X R, Song W M, et al. 2008. Effects of crust and shrub patches on runoff, sedimentation, and related nutrient (C, N) redistribution in the desertified steppe zone of the Tengger Desert, Northern China. Geomorphology, 96(1–2): 221–232.Li X R, Ma F Y, Long L Q, et al. 2001. Soil water dynamics under sand-fixing vegetation in shapotou area. Journal of Desert Research, 21(3): 217–222. (in Chinese)Liang N S, Inoue G, Fujinuma Y. 2003. A multichannel automated chamber system for continuous measurement of forest soil CO2 efflux. Tree Physiology, 23(12): 825–832.Liu B, Zhao W Z, Wen Z J. 2012. Photosynthetic response of two shrubs to rainfall pulses in desert regions of northwestern China. Photosynthetica, 50(1): 109–119.Lloyd J, Taylor J A. 1994. On the temperature dependence of soil respiration. Functional Ecology, 8(3): 315–323.Loik M E, Breshears D D, Lauenroth W K, et al. 2004. A multi-scale perspective of water pulses in dryland ecosystems: climatology and ecohydrology of the western USA. Oecologia, 141(2): 269–281.Parton W, Morgan J, Smith D, et al. 2012. Impact of precipitation dynamics on net ecosystem productivity. Global Change Biology, 18(3): 915–927.Reichstein M, Tenhunen J D, Roupsard O, et al. 2002. Ecosystem respiration in two Mediterranean evergreen Holm Oak forests: drought effects and decomposition dynamics. Functional Ecology, 16(1): 27–39.Ross I, Misson L, Rambal S, et al. 2012. How do variations in the temporal distribution of rainfall events affect ecosystem fluxes in seasonally water-limited Northern Hemisphere shrublands and forests? Biogeosciences, 9: 1007–1024.Swemmer A M, Knapp A K, Snyman H A. 2007. Intra-seasonal precipitation patterns and above-ground productivity in three perennial grasslands. Journal of Ecology, 95(4): 780–788.Tan Z H, Zhang Y P, Liang N S, et al. 2013. Soil respiration in an old-growth subtropical forest: Patterns, components, and controls. Journal of Geophysical Research: Atmospheres, 118(7): 2981–2990.Thomey M L, Collins S L, Vargas R, et al. 2011. Effect of precipitation variability on net primary production and soil respiration in a Chihuahuan Desert grassland. Global Change Biology, 17(4): 1505–1515.Walter J, Grant K, Beierkuhnlein C, et al. 2012. Increased rainfall variability reduces biomass and forage quality of temperate grassland largely independent of mowing frequency. Agriculture, Ecosystems & Environment, 148: 1–10.Xia J Y, Niu S L, Ciais P, et al. 2015. Joint control of terrestrial gross primary productivity by plant phenology and physiology. Proceedings of the National Academy of Sciences of the United States of America, 112(9): 2788–2793.Yandjian L, Gherardi L, Sala O E. 2011. Nitrogen limitation in arid-subhumid ecosystems: A meta-analysis of fertilization studies. Journal of Arid Environments, 75(8): 675–680.Yepez E A, Huxman T E, Ignace D D, et al. 2005. Dynamics of transpiration and evaporation following a moisture pulse in semiarid grassland: A chamber-based isotope method for partitioning flux components. Agricultural and Forest Meteorology, 132(3–4): 359–376.Zeppel M J B, Wilks J V, Lewis J D. 2014. Impacts of extreme precipitation and seasonal changes in precipitation on plants. Biogeosciences, 11: 3083–3093.Zhang B C, Cao J J, Bai Y F, et al. 2013. Effects of rainfall amount and frequency on vegetation growth in a Tibetan alpine meadow. Climatic Change, 118(2): 197–212.Zhang Y G, Moran M S, Nearing M A, et al. 2013. Extreme precipitation patterns and reductions of terrestrial ecosystem production across biomes. Journal of Geophysical Research: Biogeosciences, 118(1): 148–157. |
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
|
Shared |
|
|
|
|
|
Discussed |
|
|
|
|