Chin J Plant Ecol ›› 2023, Vol. 47 ›› Issue (1): 1-24.DOI: 10.17521/cjpe.2022.0107
Special Issue: 青藏高原植物生态学:生态系统生态学; 凋落物; 土壤呼吸; 生物多样性
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YANG Yuan-He1,2,*(), ZHANG Dian-Ye1, WEI Bin1,2, LIU Yang1,3, FENG Xue-Hui1,2, MAO Chao1,4, XU Wei-Jie1,2, HE Mei1, WANG Lu1,2, ZHENG Zhi-Hu1,2, WANG Yuan-Yuan1, CHEN Lei-Yi1, PENG Yun-Feng1
Received:
2022-03-26
Accepted:
2022-06-27
Online:
2023-01-20
Published:
2022-10-25
Contact:
*YANG Yuan-He,E-mail:yhyang@ibcas.ac.cn
Supported by:
YANG Yuan-He, ZHANG Dian-Ye, WEI Bin, LIU Yang, FENG Xue-Hui, MAO Chao, XU Wei-Jie, HE Mei, WANG Lu, ZHENG Zhi-Hu, WANG Yuan-Yuan, CHEN Lei-Yi, PENG Yun-Feng. Nonlinear responses of community diversity, carbon and nitrogen cycles of grassland ecosystems to external nitrogen input[J]. Chin J Plant Ecol, 2023, 47(1): 1-24.
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Fig. 1 Multi-level nitrogen (N) manipulation experiment in an alpine steppe on the Qingzang Plateau (photo credit: LIU Yang). This experiment was maintained by Dr. YANG Yuan-He’s group in Institute of Botany, Chinese Academy of Sciences, and located in Sanjiaocheng sheep farm, Gangca County, Qinghai Province. It was conducted since May 2013, with eight N levels (0, 1, 2, 4, 8, 16, 24, 32 g·m-2·a-1). The form of N fertilizer is NH4NO3.
Fig. 2 Responses of multidimensional biodiversity to nitrogen input and their primary mechanisms. Orange arrows indicate downward trends, while green arrows indicate non-significant changes.
Fig. 3 Responses of vegetation productivity and its allocation to nitrogen (N) input and their primary mechanisms. ANPP, aboveground net primary productivity; P, phosphorus. The positive sign means the stimulating effects of N input, and vice versa.
Fig. 5 Responses of various soil carbon fractions to nitrogen input and their primary mechanisms. MAOC, mineral-associated organic carbon; POC, particulate organic carbon; SOC, soil organic carbon. The arrow-up or positive sign means the stimulating effects of nitrogen input, and vice versa.
Fig. 6 Responses of nitrous oxide (N2O) emissions to nitrogen (N) input and their primary mechanisms in tropical and temperate (A) as well as alpine grasslands (B). AOA, ammonia-oxidizing archaea.
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