Effects of litter quality and climate change along an elevation gradient on litter mass loss in an alpine meadow ecosystem on the Tibetan plateau

2009 ◽  
pp. 77-88
Author(s):  
Guangping Xu ◽  
Yigang Hu ◽  
Shiping Wang ◽  
Zhenhua Zhang ◽  
Xiaofeng Chang ◽  
...  
Plant Ecology ◽  
2009 ◽  
Vol 209 (2) ◽  
pp. 257-268 ◽  
Author(s):  
Guangping Xu ◽  
Yigang Hu ◽  
Shiping Wang ◽  
Zhenhua Zhang ◽  
Xiaofeng Chang ◽  
...  

2010 ◽  
Vol 16 (5) ◽  
pp. 1606-1617 ◽  
Author(s):  
CAIYUN LUO ◽  
GUANGPING XU ◽  
ZENGGUO CHAO ◽  
SHIPING WANG ◽  
XINGWU LIN ◽  
...  

1993 ◽  
Vol 20 (3) ◽  
pp. 127-159 ◽  
Author(s):  
B. Berg ◽  
M. P. Berg ◽  
P. Bottner ◽  
E. Box ◽  
A. Breymeyer ◽  
...  

2014 ◽  
Vol 2014 ◽  
pp. 1-9 ◽  
Author(s):  
Gang Fu ◽  
Xianzhou Zhang ◽  
Chengqun Yu ◽  
Peili Shi ◽  
Yuting Zhou ◽  
...  

Alpine meadows are one major type of pastureland on the Tibetan Plateau. However, few studies have evaluated the response of soil respiration (Rs) to grazing along an elevation gradient in an alpine meadow on the Tibetan Plateau. Here three fenced enclosures were established in an alpine meadow at three elevations (i.e., 4313 m, 4513 m, and 4693 m) in July 2008. We measuredRsinside and outside the three fenced enclosures in July–September, 2010-2011. Topsoil (0–20 cm) samples were gathered in July, August, and September, 2011. There were no significant differences forRs, dissolved organic C (DOC), and belowground root biomass (BGB) between the grazed and ungrazed soils. Soil respiration was positively correlated with soil organic C (SOC), microbial biomass (MBC), DOC, and BGB. In addition, bothRsand BGB increased with total N (TN), the ratio of SOC to TN, ammonium N (NH4+-N), and the ratio ofNH4+-N to nitrate N. Our findings suggested that the negligible response ofRsto grazing could be directly attributed to that of respiration substrate and that soil N may indirectly affectRsby its effect on BGB.


2015 ◽  
Vol 5 (1) ◽  
Author(s):  
Tao Zhang ◽  
Yangjian Zhang ◽  
Mingjie Xu ◽  
Juntao Zhu ◽  
Michael C. Wimberly ◽  
...  

Ecosystems ◽  
2021 ◽  
Author(s):  
Janna Wambsganss ◽  
Grégoire T. Freschet ◽  
Friderike Beyer ◽  
Jürgen Bauhus ◽  
Michael Scherer-Lorenzen

AbstractDecomposition of dead fine roots contributes significantly to nutrient cycling and soil organic matter stabilization. Most knowledge of tree fine-root decomposition stems from studies in monospecific stands or single-species litter, although most forests are mixed. Therefore, we assessed how tree species mixing affects fine-root litter mass loss and which role initial litter quality and environmental factors play. For this purpose, we determined fine-root decomposition of 13 common tree species in four European forest types ranging from boreal to Mediterranean climates. Litter incubations in 315 tree neighborhoods allowed for separating the effects of litter species from environmental influences and litter mixing (direct) from tree diversity (indirect). On average, mass loss of mixed-species litter was higher than those of single-species litter in monospecific neighborhoods. This was mainly attributable to indirect diversity effects, that is, alterations in microenvironmental conditions as a result of tree species mixing, rather than direct diversity effects, that is, litter mixing itself. Tree species mixing effects were relatively weak, and initial litter quality and environmental conditions were more important predictors of fine-root litter mass loss than tree diversity. We showed that tree species mixing can alter fine-root litter mass loss across large environmental gradients, but these effects are context-dependent and of moderate importance compared to environmental influences. Interactions between species identity and site conditions need to be considered to explain diversity effects on fine-root decomposition.


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