scholarly journals Effects of nitrogen addition on plant-soil-microbe stoichiometry characteristics of different functional group species in Bothriochloa ischemum community

Author(s):  
ZiWen Zhao ◽  
YanLi Qin ◽  
Yang Wu ◽  
WenJing Chen ◽  
Sha Xue ◽  
...  
2019 ◽  
Vol 108 (1) ◽  
pp. 337-352 ◽  
Author(s):  
Pil U. Rasmussen ◽  
Alison E. Bennett ◽  
Ayco J. M. Tack

Ecohydrology ◽  
2010 ◽  
Vol 4 (6) ◽  
pp. 757-790 ◽  
Author(s):  
Chitsomanus P. Muneepeerakul ◽  
Rachata Muneepeerakul ◽  
Fernando Miralles-Wilhelm ◽  
Andrea Rinaldo ◽  
Ignacio Rodriguez-Iturbe

2013 ◽  
Vol 145 (2) ◽  
pp. 171-183 ◽  
Author(s):  
C.M. Ernst ◽  
C.M. Buddle

AbstractSeasonal patterns in the taxonomic and functional structure of epigeic Coleoptera assemblages in wet and mesic habitats were studied in Kugluktuk, Nunavut, Canada. Using pan and pitfall traps, 2638 beetles were collected between 21 June and 13 August 2010. Fifty species (including 17 new territory records) in 11 families were identified. The biomass of each specimen was estimated, and each was assigned to a functional group. Species composition differed between habitats throughout the active season and there was a rapid compositional turnover even though species diversity was similar in both habitats and among sampling periods. The functional beetle assemblages in the two habitats were different, and both assemblages experienced seasonal turnover in function; this effect was more pronounced in the mesic habitats. The beetle fauna in both habitats was predominantly entomophagous. We also examined the influence of seasonal weather patterns on assemblage structure: there is a significant relationship between mean daily temperature and assemblage structure. This relationship indicates that changes in weather (or longer-term changes in climate) could affect the diversity and ecological function of insects in this system. Given the significance of insects in the north, this could result in important changes to northern ecology.


Author(s):  
Elisabeth Ramm ◽  
Chunyan Liu ◽  
Per Ambus ◽  
Klaus Butterbach-Bahl ◽  
Bin Hu ◽  
...  

Abstract The paradigm that permafrost-affected soils show restricted mineral nitrogen (N) cycling in favor of organic N compounds is based on the observation that net N mineralization rates in these cold climates are negligible. However, we find here that this perception is wrong. By synthesizing published data on N cycling in the plant-soil-microbe system of permafrost ecosystems we show that gross ammonification and nitrification rates in active layers were of similar magnitude and showed a similar dependence on soil organic carbon (SOC) and total nitrogen (TN) concentrations as observed in temperate and tropical systems. Moreover, high protein depolymerization rates and only marginal effects of C:N stoichiometry on gross N turnover provided little evidence for N limitation. Instead, the rather short period when soils are not frozen is the single main factor limiting N turnover. High gross rates of mineral N cycling are thus facilitated by released protection of organic matter in active layers with nitrification gaining particular importance in N-rich soils, such as organic soils without vegetation. Our finding that permafrost-affected soils show vigorous N cycling activity is confirmed by the rich functional microbial community which can be found both in active and permafrost layers. The high rates of N cycling and soil N availability are supported by biological N fixation, while atmospheric N deposition in the Arctic still is marginal except for fire-affected areas. In line with high soil mineral N production, recent plant physiological research indicates a higher importance of mineral plant N nutrition than previously thought. Our synthesis shows that mineral N production and turnover rates in active layers of permafrost-affected soils do not generally differ from those observed in temperate or tropical soils. We therefore suggest to adjust the permafrost N cycle paradigm, assigning a generally important role to mineral N cycling. This new paradigm suggests larger permafrost N climate feedbacks than assumed previously.


Author(s):  
Shamina Imran Pathan ◽  
Maria Teresa Ceccherini ◽  
Francesco Sunseri ◽  
Antonio Lupini
Keyword(s):  

2019 ◽  
Vol 11 (19) ◽  
pp. 5226 ◽  
Author(s):  
Juan Cao ◽  
Ruirui Yan ◽  
Xiaoyong Chen ◽  
Xu Wang ◽  
Qiang Yu ◽  
...  

Grazing affects nutrient cycling processes in grasslands, but little is known by researchers about effects on the nutrient stoichiometry of plant–soil–microbe systems. In this study, the influence of grazing intensity (0, 0.23, 0.34, 0.46, 0.69, and 0.92 AU ha−1) on carbon (C), nitrogen (N) and phosphorus (P) and their stoichiometric ratios in plants, soil, and microbes was investigated in a Hulunber meadow steppe, Northeastern China. The C:N and C:P ratios of shoots decreased with grazing increased. Leaf N:P ratios <10 suggested that the plant communities under grazing were N-limited. Heavy grazing intensities increased the C:N and C:P ratios of microbial biomass, but grazing intensity had no significant effects on the stoichiometry of soil nutrients. The coupling relationship of C:N ratio in plant–soil–microbial systems was tightly significant compared to C:P ratio and N:P ratio according to the correlation results. The finding suggested grazing exacerbated the competition between plants and microorganisms for N and P nutrition by the stoichiometric changes (%) in each grazing level relative to the no grazing treatment. Therefore, for the sustainability of grasslands in Inner Mongolia, N inputs need to be increased and high grazing intensities reduced in meadow steppe ecosystems, and the grazing load should be controlled within G0.46.


2016 ◽  
Vol 104 (6) ◽  
pp. 1608-1617 ◽  
Author(s):  
Roeland Cortois ◽  
Thomas Schröder‐Georgi ◽  
Alexandra Weigelt ◽  
Wim H. Putten ◽  
Gerlinde B. De Deyn

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