scholarly journals Linking changes in the soil microbial community to C and N dynamics during crop residue decomposition

2021 ◽  
Vol 20 (11) ◽  
pp. 3039-3059
Author(s):  
Cyrine REZGUI ◽  
Isabelle TRINSOUTROT-GATTIN ◽  
Marie BENOIT ◽  
Karine LAVAL ◽  
Wassila RIAH-ANGLET
2013 ◽  
Vol 43 (9) ◽  
pp. 777-784 ◽  
Author(s):  
Ya-Lin Hu ◽  
Kangho Jung ◽  
De-Hui Zeng ◽  
Scott X. Chang

Chronic nitrogen (N) and (or) sulfur (S) deposition to boreal forests in the Athabasca oil sands region (AOSR) in Alberta, Canada, has been caused by oil sands mining and extraction/upgrading activities. It is important that we understand the response of microbial community function to chronic N and S deposition as microbial populations mediate soil carbon (C) and N cycles and affect ecosystem resilience. To evaluate the impact of N and (or) S deposition on soil microbial community functions, we conducted a simulated N and S deposition experiment in a boreal mixedwood forest with the following four treatments: control (CK), N addition (+N, 30 kg N·ha−1 as NH4NO3), S addition (+S, 30 kg S·ha−1 as NaSO4), and N plus S addition (+NS, 30 kg N·ha−1 + 30 kg S·ha−1), from 2006 to 2010. Nitrogen and (or) S deposition did not change soil organic carbon, total N, dissolved organic C and N, or soil microbial biomass C and N. Soil microbial community-level physiological profiles, however, were strongly affected by 5 years of N and (or) S addition. Soil β-glucosidase activity in the +NS treatment was greater than that in the +S treatment, and S addition decreased soil arylsulfatase; however, urease and dehydrogenase activities were not affected by the simulated N and (or) S deposition. Our data suggested that N and (or) S deposition strongly affected soil microbial community functions and enzymatic activities without changing soil microbial biomass in the studied boreal forest.


2006 ◽  
Vol 280 (1-2) ◽  
pp. 143-155 ◽  
Author(s):  
B. Govaerts ◽  
K. D. Sayre ◽  
J. M. Ceballos-Ramirez ◽  
M. L. Luna-Guido ◽  
A. Limon-Ortega ◽  
...  

2010 ◽  
Vol 10 (8) ◽  
pp. 1598-1605 ◽  
Author(s):  
Haohao Lu ◽  
Weixiang Wu ◽  
Yingxu Chen ◽  
Hailong Wang ◽  
Medha Devare ◽  
...  

2020 ◽  
Vol 202 (10) ◽  
pp. 2809-2824 ◽  
Author(s):  
Marcos V. M. Sarto ◽  
Wander L. B. Borges ◽  
Doglas Bassegio ◽  
Carlos A. B. Pires ◽  
Charles W. Rice ◽  
...  

2021 ◽  
Author(s):  
Ilonka C. Engelhardt ◽  
Pascal A. Niklaus ◽  
Florian Bizouard ◽  
Marie-Christine Breuil ◽  
Nadine Rouard ◽  
...  

2012 ◽  
Vol 50 ◽  
pp. 126-133 ◽  
Author(s):  
C. Le Guillou ◽  
D.A. Angers ◽  
P.A. Maron ◽  
P. Leterme ◽  
S. Menasseri-Aubry

2021 ◽  
Vol 16 (3) ◽  
pp. 226-237
Author(s):  
Aleksandra E. Selezneva ◽  
Kristina V. Ivashchenko ◽  
Sofia V. Sushko ◽  
Anna I. Zhuravleva ◽  
Nadezhda D. Ananyeva ◽  
...  

In mountain areas, one of the noticeable results of modern climate change is rapid shift of treelines to subalpine and alpine meadows. Such vegetation shifts is associated with a change in quality of the plant residues entering the soils, which in turn can affect the mineralization activity (basal respiration) and functional diversity of the soil microbial community. Therefore, the study was aimed at assessing the soil microbial (basal respiration and functional diversity) and chemical (C, N, C/N, pH) properties (0-10 cm) along the reserved and grazed forest-meadow transects of the Northwestern Caucasus (Karachay-Cherkess Republic), as well as evaluating an effect of vegetation type and land use on variation of these soil properties. It was found that the C and N contents (for both land usees), pH and basal respiration (reserved slope) significantly increase from forest to meadow soils. In contrary, the microbial functional diversity decreased from forest to meadow soils, which might be due to less diverse organic compounds entering the soil only with grass residues than their combination with forest litter. Two-way ANOVA showed that soil microbial functional diversity, pH, C and N along the studied forest-meadow transects was mostly associated with vegetation type (1439 % of the explained variation), and C/N and basal respiration - with land use (3336 % of the explained variation). Thus, a land use change will have a more significant effect on the mineralization activity of soil microbial community than a treeline shifts.


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