Snow Exclusion Does Not Affect Soil Ammonia-Oxidizing Bacteria and Archaea Communities

被引:2
|
作者
Zhang, Li [1 ]
You, Chengming [1 ]
Liu, Sining [1 ]
Wang, Lixia [1 ]
Tan, Bo [1 ]
Xu, Zhenfeng [1 ]
Li, Han [1 ]
机构
[1] Sichuan Agr Univ, Inst Ecol & Forestry, Forestry Ecol Engn Upper Reaches Yangtze River Ke, Chengdu 611130, Peoples R China
来源
FORESTS | 2022年 / 13卷 / 09期
基金
中国国家自然科学基金;
关键词
winter; forest soil; amoA; community diversity; community composition; enzyme activities; EASTERN TIBETAN PLATEAU; MICROBIAL COMMUNITIES; NITROGEN MINERALIZATION; WINTER; FOREST; RESPIRATION; COVER; DEPTH; BIOMASS; SENSITIVITY;
D O I
10.3390/f13091483
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Soil ammonia-oxidizing microorganisms play important roles in nitrogen (N) cycling in cold ecosystems, but how changes in snow cover will affect their distribution and associated functional characteristics remains unclear. A snow manipulation experiment was conducted to explore the effects of snow exclusion on soil ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) communities and functional characteristics in a spruce forest in the eastern Tibet Plateau. Results showed that the amoA gene abundance and community composition of AOA and AOB did not differ between snow regimes but varied among winter periods. AOA and AOB gene abundances showed a decreasing trend during the snow cover melting period. During the deep snow cover period, Thaumarchaeota and Crenarchaeota in the AOA community decreased significantly, while Proteobacteria and Nitrosospira in the AOB community increased significantly. The main factors affecting the changes in AOA and AOB community diversity and composition were soil MBN, nitrate nitrogen, and temperature, while AOA and AOB community diversity and composition were also significantly correlated with soil enzyme activities related to N cycling. These results recommend that the season-driven variations strongly affected soil ammonia-oxidizing community and functional characteristics more than momentary snow cover change. Such findings offer new insights into how soil N-cycling processes would respond to reduced snowfall in high-altitude regions.
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收藏
页数:13
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