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Chinese Journal of Applied Ecology ›› 2018, Vol. 29 ›› Issue (1): 59-67.doi: 10.13287/j.1001-9332.201801.006

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Effects of warming and nitrogen addition on community production and biomass allocation in an alpine meadow.

ZONG Ning1, DUAN Cheng1,2, GENG Shou-bao1,2, CHAI Xi1,2, SHI Pei-li1,2*, HE Yong-tao1   

  1. 1Key Laboratory of Ecosystem Network Observation and Modelling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
    2University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2017-05-31 Online:2018-01-18 Published:2018-01-18
  • Contact: * E-mail: shipl@igsnrr.ac.cn
  • Supported by:
    The work was supported by the West Light Foundation of the Chinese Academy of Sciences (2015), the National Science Foundation for Young Scientists of China (41703079), the National Natural Science Foundation of China (31470506), the Youth Innovation Research Team Project (LENOM2016Q0004) and the National Key Research and Development Program (2016YFC0501803, 2016YFC0502001).

Abstract: A long-term experiment, involving exogenous N addition and simulated warming, was conducted in an alpine meadow in Damxung, northern Tibet, to study how warming and N addition influence community production and biomass allocation. The results showed that warming resulted in a warm but dry microsite, that was, air temperature increased by 1.6 ℃ and soil surface temperature increased by 1.4 ℃, and soil water content decreased by 4.7%. Under no N addition treatments, warming significantly decreased plant aboveground biomass by 61.5%, 108.8% and 77.1% in 2012, 2013 and 2014, respectively. Under high N treatments (40 and 80 kg N·hm-2·a-1), warming had no significant effect on aboveground biomass. These findings indicated that the effect of warming might be dependent on N addition level, and N addition could compensate for soil N loss caused by warming. Warming led to an increase in root/shoot by 98.6%, 60.7% and 97.8% in 2012, 2013 and 2014 under no N addition treatments, respectively. Under the ambient condition, the change percentages of aboveground and belowground biomass of plant communities first increased and then decreased along an N gradient, with the saturation thresholds of above- and below-ground biomass for N addition 56.0 and 55.5 kg N·hm-2·a-1, respectively. Under the warming condition, above- and belowground biomass increased linearly with increasing N addition. These findings suggested that warming modulated the response patterns of alpine meadows to exogenous N input, which was mainly caused by decreased soil inorganic N under warming. The estimation of N thresholds highlights that alpine meadows are more sensitive to future N deposition than other types of grasslands.