Additive effects of warming and grazing on fine-root decomposition and loss of nutrients in an alpine meadow

Author:

Zhou Yang12,Lv Wang-Wang12,Wang Shi-Ping13,Zhang Li-Rong4,Sun Jian-Ping12,Jiang Li-Li12,Liu Pei-Pei12,Wang Qi1,Li Bo-Wen12,Wang A12,Hong Huan12,Zhang Su-Ren12,Xia Lu5,Ji Nan12,Xie Zheng-Xin5,Luo Cai-Yun6,Zhang Zhen-Hua6,Wang Chang-Hui7,Wang Jin-Zhi8,Yang Ci9,Dorji Tsechoe12

Affiliation:

1. Key Laboratory of Alpine Ecology, Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100101 , China

2. University of the Chinese Academy of Sciences , Beijing 100049 , China

3. CAS Center for Excellence in Tibetan Plateau Earth Science of the Chinese Academy of Sciences , Beijing 100101 , China

4. Department of Resources and Environment, Hebei Normal University for Nationalities , Chengde 067600 , China

5. Science College, Tibet University , Lhasa 850001 , China

6. Northwestern Institute of Plateau Biology, Chinese Academy of Sciences; Qinghai Provincial Key Laboratory of Restoration Ecology of Cold Area , Xining 810008 , China

7. Grassland College, Shanxi Agriculture University , Taigu 030801 , China

8. Wetland Institute, Chinese Academy of Forestry , Beijing 100093 , China

9. Center for Meteorology, Meteorological Bureau of Tibet Autonomous Region , Lhasa 850000 , China

Abstract

Abstract Fine-root decomposition is a critical process regulating ecosystem carbon cycles and affecting nutrient cycling and soil fertility. However, whether interaction between warming and grazing affects fine-root decomposition is still under-researched in natural grasslands. A two-factorial experiment with asymmetric warming (i.e. daytime vs. nighttime and growing season vs. nongrowing season) and moderate grazing (i.e. about average 50% forage utilization rate) was conducted to explore whether warming and grazing affect fine-root decomposition and loss of nutrients during a 2-year decomposition period in an alpine meadow on the Tibetan Plateau. Both warming and grazing facilitated carbon cycling through increase in fine-root decomposition, and influenced element cycling which varies among elements. The effects of warming and grazing on fine-root decomposition and loss of nutrients were additive. Both warming and grazing significantly increased cumulative percentage mass loss and total organic carbon loss of fine roots during the 2-year experiment. Only warming with grazing treatment reduced percentage nitrogen loss, whereas warming, regardless of grazing, decreased percentage phosphorus loss. Warming and grazing alone increased percentage loss of potassium, sodium, calcium and magnesium compared with control. There were no interactions between warming and grazing on fine-root decomposition and loss of nutrients. There was greater temperature sensitivity of decreased phosphorus loss than that of decreased nitrogen loss. Different temperature sensitivities of percentage loss of nutrients from fine-root decomposition would alter ratios of the available nutrients in soils, and may further affect ecosystem structure and functions in future warming.

Funder

National Natural Science Foundation of China

Strategic Priority Research Program

Chinese Academy of Sciences

Joint Key Research Fund

Tibet Autonomous Region

Second Tibetan Plateau Scientific Expedition and Research

Publisher

Oxford University Press (OUP)

Subject

Plant Science,Ecology,Ecology, Evolution, Behavior and Systematics

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