Nitrogen and phosphorus addition exerted different influences on litter and soil carbon release in a tropical forest

被引:18
|
作者
Zhang, Jingfan [1 ,2 ,3 ]
Zhou, Jinge [1 ,2 ,3 ]
Lambers, Hans [4 ]
Li, Yingwen [1 ]
Li, Yongxing [1 ]
Qin, Guoming [1 ,2 ]
Wang, Mei [5 ]
Wang, Jun [1 ]
Li, Zhian [1 ,3 ]
Wang, Faming [1 ,3 ]
机构
[1] Chinese Acad Sci, Key Lab Vegetat Restorat & Management Degraded Ec, CAS Engn Lab Ecol Restorat Isl & Coastal Ecosyst, South China Bot Garden,Xiaoliang Res Stn Trop Coa, Guangzhou 510000, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Southern Marine Sci & Engn Guangdong Lab Guangzho, Guangzhou 510000, Peoples R China
[4] Univ Western Australia, Sch Biol Sci, Perth, WA 6009, Australia
[5] South China Normal Univ, Sch Geog, Guangzhou 510631, Peoples R China
基金
中国国家自然科学基金;
关键词
C release; South China; Mineralization; Decomposition; Soil microbial composition; Enzyme; NUTRIENT LIMITATION; ENZYME-ACTIVITIES; MICROBIAL COMMUNITIES; PLANT LITTER; N DEPOSITION; DECOMPOSITION; AVAILABILITY; RESPIRATION; BIOMASS; FUNGAL;
D O I
10.1016/j.scitotenv.2022.155049
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Terrestrial soils release large amount of carbon dioxide (CO2) each year, which are mainly derived from litter and soil carbon (C) decomposition. Nutrient availability, especially nitrogen (N) and phosphorus (P), plays an important role in both litter and soil C decomposition. Therefore, understanding the underlying mechanism is crucial for mitigating CO2 emission and climate changes. Here, we assessed patterns of litter and soil C decomposition after 11 yrs. in-situ N and P addition in a tropical forest where corn leaves or corn roots were added as litter C. The total CO2 efflux was quantified and partitioned using C-13 isotope signatures to determine the sources (litter or soil C) every three months. In addition, Changes in C-degrading enzyme activities: beta-1,4-glucosidase (BG), phenol oxidase (PHO) and peroxidase (PER), and microbial biomarkers were assessed to interpret the underlying mechanism. Total C-release was enhanced up to17% by the long-term N addition but inhibited up to 15% by P addition. Precisely, N addition only accelerated the litter decomposition and increased about 42% and 6% of the litter C release at 0-5 cm and 5-10 cm soil depths, respectively; while P addition only impeded the soil C decomposition and decreased about 9% and 11% of the soil C release at 0-5 cm and 5-10 cm, respectively. The enhanced C release under N addition might be attributed to the enhanced microbial biomass, the ratio of fungi to bacteria and C-degrading enzyme activities. However, P addition resulted in the reverse result in microbial properties and C-degrading enzyme activities, associated with a decreased C release. Our study suggests that the long-term N and P addition selectively affected the litter and soil C decomposition because of their different physiochemical properties and this tendency might be more pronounced in tropical forests exposed to increasing atmospheric N deposition in the future. The study indicates that the different patterns of litter and soil C decomposition under climate change should be taken account in the future C management strategies.
引用
收藏
页数:13
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