Responses of plant community coverage to simulated warming and nitrogen addition in a desert steppe in Northern China

被引:19
|
作者
Wang, Zhen [1 ,2 ]
Li, Yuanheng [2 ]
Hao, Xiying [3 ]
Zhao, Mengli [1 ]
Han, Guodong [1 ]
机构
[1] Inner Mongolia Agr Univ, Coll Ecol & Environm Sci, Dept Grassland Sci, Hohhot 010019, Inner Mongolia, Peoples R China
[2] Chinese Acad Agr Sci, Inst Grassland Res, Hohhot 010010, Peoples R China
[3] Agr & Agri Food Canada, Lethbridge Res Ctr, Lethbridge, AB, Canada
基金
中国国家自然科学基金;
关键词
Desert steppe ecosystem; Global warming; Grassland; Nitrogen application; SEASONAL WATER AVAILABILITY; ECOSYSTEM CARBON EXCHANGE; CLIMATE-CHANGE; PRIMARY PRODUCTIVITY; SPECIES RICHNESS; ELEVATED CO2; C-4; GRASSES; GRASSLAND; BIOMASS; GROWTH;
D O I
10.1007/s11284-015-1265-3
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Grassland communities occupy about 25 % of global land area and global warming could alter grassland plant community coverage. A field study was conducted to investigate the impact of soil warming (surface soil temperature increased by 1.3 A degrees C) and nitrogen addition (100 kg N ha(-1) year(-1)) on a desert steppe community in Inner Mongolia, China, from 2006 to 2011. Although there were strong intra- and inter-annual variations, in general, warming had little effect on coverage of the four major species (two cool season C-3 species: Convolvulus ammannii and Stipa breviflora, and two warm season C-4 species: Cleistogenes songorica and Kochia prostrata) over six growing seasons. The C-3/C-4 coverage ratio consistently decreased with warming, with the decrease being statistically significant for one-third of sampling dates. Warming caused a reduction (from 27.6 to 25.1 %) in peak season total plant community coverage. N addition did not affect the four main species, four functional groups (perennial grass, perennial forb, shrub and annual-biennial) or the total plant community over the 6 years, except when precipitation was high (231 mm in 2008). The small reduction in plant community coverage demonstrated the resilience of desert steppe to warming. There could be a shift of C-3 to C-4 species because of warming, as indicated by the decrease in C-3/C-4 ratio, but confirmation of this trend requires further study.
引用
收藏
页码:605 / 614
页数:10
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