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Spatiotemporal patterns of the maximum primary productivity and driving factors in the eastern China’s forests.

SHI Xu-xia1, SONG Zhao-peng1, HOU Jihua1*, ZHANG Lei-ming2, NIU Shu-li2, WANG An-zhi3, XIANG Wen-hua4, WANG Hui-min2   

  1. (1College of Forestry, Beijing Forestry University, Beijing 100083, China; 2Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 4Faculty of Life Science and Technology, Central South University of Forestry and Technology, Changsha 410004, China).
  • Online:2019-07-10 Published:2019-07-10

Abstract: The response of ecosystem carbon cycle to temperature is one of the major topics in the research field of global change ecology. The general pattern of the response of gross primary productivity (GPP) to temperature usually shows that GPP increases with temperature at the lower temperature range to reach a maximum value (GPPmax), and then declines as temperature increases further. Thus,GPPmax represents the photosynthetic potential of vegetation at the optimum temperature. However, our understanding on the spatial and temporal patterns and main driving factors of GPPmax in forest ecosystems are still limited. In this study, we analyzed the temporal and spatial distribution of GPPmax and main influencing factors in five typical forest ecosystems based on flux data (temperate coniferous and broad-leaved mixed forest of Changbaishan, subtropical Chinese fir (Cunninghamia lanceolata) plantation of Huitong, subtropical evergreen coniferous forest of Qianyanzhou, subtropical evergreen broadleaf and coniferous mixed forest of Dinghushan, and tropical monsoon forest of Xishuangbanna) along the NorthSouth Transect of Eastern China (NSTEC), which covered tropical, subtropical, and temperate climate zones. The results showed that the temperature response of GPP showed a unimodal pattern, with GPPmax occurring at the optimum temperature in each year for all ecosystems. GPPmax at the optimum temperature in forests were ranked following the order: Changbaishan > Qianyanzhou > Xishuangbanna > Huitong > Dinghushan. Temperature played the most important role in driving the spatial variation of GPPmax across sites, with GPPmax decreasing with the increases of temperatur. Solar radiation, precipitation and VPD affected GPPmax. For the interannual variation of GPPmax in each site, GPPmax in Changbaishan was mainly controlled by air temperature and by soil water content in Huitong, Qianyanzhou, and Dinghushan forests. We failed to find the main factors affecting interannual variation of tropical rainforest in Xishuangbanna. Our results benefit the understanding of GPP variation under climate change and provide evidence and parameter for accurate simulation of carbon cycle.

Key words: continuous cropping, potato, root exudates, palmitic acid, dibutyl phthalate, Rhizoctonia solani.