Assessing the effect of air-drying and storage on microbial biomass and community structure in paddy soils

2008 ◽  
Vol 317 (1-2) ◽  
pp. 213-221 ◽  
Author(s):  
Yueyan Liu ◽  
Huaiying Yao ◽  
Changyong Huang
2022 ◽  
Vol 326 ◽  
pp. 107798
Author(s):  
Liang Wei ◽  
Tida Ge ◽  
Zhenke Zhu ◽  
Rongzhong Ye ◽  
Josep Peñuelas ◽  
...  

2018 ◽  
Vol 20 (4) ◽  
pp. 673-685 ◽  
Author(s):  
Tatiana A. Vishnivetskaya ◽  
Haiyan Hu ◽  
Joy D. Van Nostrand ◽  
Ann M. Wymore ◽  
Xiaohang Xu ◽  
...  

Sulfate-reducing bacteria and methanogens are the primary Hg-methylators in Chinese rice paddies.


2010 ◽  
Vol 10 (8) ◽  
pp. 1510-1516 ◽  
Author(s):  
Xin Chen ◽  
Li-Mei Zhang ◽  
Ju-Pei Shen ◽  
Zhihong Xu ◽  
Ji-Zheng He

2000 ◽  
Vol 40 (3) ◽  
pp. 223-237 ◽  
Author(s):  
H. Yao ◽  
Z. He ◽  
M. J. Wilson ◽  
C. D. Campbell

2018 ◽  
Vol 15 (6) ◽  
pp. 1879-1894 ◽  
Author(s):  
Petr Kotas ◽  
Hana Šantrůčková ◽  
Josef Elster ◽  
Eva Kaštovská

Abstract. The unique and fragile High Arctic ecosystems are vulnerable to global climate warming. The elucidation of factors driving microbial distribution and activity in arctic soils is essential for a comprehensive understanding of ecosystem functioning and its response to environmental change. The goals of this study were to investigate microbial biomass and activity, microbial community structure (MCS), and their environmental controls in soils along three elevational transects in the coastal mountains of Billefjorden, central Svalbard. Soils from four different altitudes (25, 275, 525 and 765 m above sea level) were analyzed for a suite of characteristics including temperature regimes, organic matter content, base cation availability, moisture, pH, potential respiration, and microbial biomass and community structure using phospholipid fatty acids (PLFAs). We observed significant spatial heterogeneity of edaphic properties among transects, resulting in transect-specific effects of altitude on most soil parameters. We did not observe any clear elevation pattern in microbial biomass, and microbial activity revealed contrasting elevational patterns between transects. We found relatively large horizontal variability in MCS (i.e., between sites of corresponding elevation in different transects), mainly due to differences in the composition of bacterial PLFAs, but also a systematic altitudinal shift in MCS related to different habitat preferences of fungi and bacteria, which resulted in high fungi-to-bacteria ratios at the most elevated sites. The biological soil crusts on these most elevated, unvegetated sites can host microbial assemblages of a size and activity comparable to those of the arctic tundra ecosystem. The key environmental factors determining horizontal and vertical changes in soil microbial properties were soil pH, organic carbon content, soil moisture and Mg2+ availability.


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