Imbalanced stoichiometric patterns in foliar nutrient resorption response to N and P addition in grazing alpine grassland

2020 ◽  
Vol 102 ◽  
pp. 103505 ◽  
Author(s):  
Lei Li ◽  
Xiangyi Li ◽  
Bo Liu ◽  
Jiaqiang Lei ◽  
Zewei Yue ◽  
...  
Ecology ◽  
1992 ◽  
Vol 73 (5) ◽  
pp. 1868-1878 ◽  
Author(s):  
Jeffrey D. May ◽  
Keith T. Killingbeck

2018 ◽  
Vol 27 (7) ◽  
pp. 875-885 ◽  
Author(s):  
Hai-Yang Zhang ◽  
Xiao-Tao Lü ◽  
Henrik Hartmann ◽  
Adrienne Keller ◽  
Xing-Guo Han ◽  
...  

2020 ◽  
Vol 20 (1) ◽  
Author(s):  
Lilong Wang ◽  
Xinfang Zhang ◽  
Shijian Xu

Abstract Background Soil salinity is a major abiotic constraint to plant growth and development in the arid and semi-arid regions of the world. However, the influence of soil salinity on the process of nutrient resorption is not well known. We measured the pools of both mature and senesced leaf nitrogen (N), phosphorus (P), potassium (K), and sodium (Na) of desert plants from two types of habitats with contrasting degrees of soil salinity in a hyper-arid environment of northwest China. Results N, P, K revealed strict resorption, whereas Na accumulated in senesced leaves. The resorption efficiencies of N, P, and K were positively correlated with each other but not with Na accumulation. The degree of leaf succulence drives both intra-and interspecific variation in leaf Na concentration rather than soil salinity. Both community- and species-level leaf nutrient resorption efficiencies (N, P, K) did not differ between the different habitats, suggesting that soil salinity played a weak role in influencing foliar nutrients resorption. Conclusions Our results suggest that plants in hyper-arid saline environments exhibit strict salt ion regulation strategies to cope with drought and ion toxicity and meanwhile ensure the process of nutrient resorption is not affected by salinity.


2016 ◽  
Vol 6 (1) ◽  
Author(s):  
Fei Ren ◽  
Xiaoxia Yang ◽  
Huakun Zhou ◽  
Wenyan Zhu ◽  
Zhenhua Zhang ◽  
...  

Abstract High soil organic carbon content, extensive root biomass, and low nutrient availability make alpine grasslands an important ecosystem for assessing the influence of nutrient enrichment on soil respiration (SR). We conducted a four-year (2009–2012) field experiment in an alpine grassland on the Qinghai-Tibetan Plateau to examine the individual and combined effects of nitrogen (N, 100 kg ha−1year−1) and phosphorus (P, 50 kg ha−1year−1) addition on SR. We found that both N and P addition did not affect the overall growing-season SR but effects varied by year: with N addition SR increased in the first year but decreased during the last two years. However, while P addition did not affect SR during the first two years, SR increased during the last two years. No interactive effects of N and P addition were observed, and both N addition and P addition reduced heterotrophic respiration during the last year of the experiment. N and P addition affected SR via different processes: N mainly affected heterotrophic respiration, whereas P largely influenced autotrophic respiration. Our results highlight the divergent effects of N and P addition on SR and address the important potential of P enrichment for regulating SR and the carbon balance in alpine grasslands.


2012 ◽  
Vol 196 (1) ◽  
pp. 173-180 ◽  
Author(s):  
Sasha C. Reed ◽  
Alan R. Townsend ◽  
Eric A. Davidson ◽  
Cory C. Cleveland

2012 ◽  
Vol 58 (No. 10) ◽  
pp. 446-451 ◽  
Author(s):  
L.J. Li ◽  
D.H. Zeng ◽  
R. Mao ◽  
Z.Y. Yu

A factorial nitrogen (N) × phosphorus (P) addition experiment was conducted to evaluate responses of leaf nutrient resorption to increased soil N and P availability in a semiarid grassland in Keerqin Sandy Lands, China. Four plant species were selected, among which Artemisia scoparia and Chenopodium acuminatum were dominant species in the control and P-added plots, and Cannabis sativa and Phragmites communis were dominant in the N- and N + P-treated plots. Results showed that N and P resorption varied substantially among species (P < 0.01). A general trend of decrease in N resorption efficiency (NRE) and N resorption proficiency (NRP) was observed in response to increased soil N availability for all species, except P. communis only for NRE. Similarly, P resorption proficiency (PRP) decreased in response to P addition for all species, whereas P resorption efficiency (PRE) was not affected by P addition. Species responded differently in terms of PRE and PRP to N addition, whereas no changes in NRE and NRP occurred in response to P addition except P. communis for NRE. Our results suggest that increased soil nutrient availability can influence plant-mediated nutrient cycling directly by changing leaf nutrient resorption and indirectly by altering species composition in the sandy grassland.  


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