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拉萨河流域青稞系统土壤微生物群落对多幅度增温的响应(英文)
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  • 英文篇名:Response of Microbial Communities in Soil to Multi-level Warming in a Highland Barley System of the Lhasa River
  • 作者:付刚 ; 孙维 ; 李少伟 ; 钟志明
  • 英文作者:FU Gang;SUN Wei;LI Shaowei;ZHONG Zhiming;Lhasa Plateau Ecosystem Research Station, Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences;
  • 关键词:红外辐射器 ; 微生物量 ; 磷脂脂肪酸 ; 增温幅度
  • 英文关键词:infrared heater;;microbial biomass;;phospho lipid fatty acid;;warming level
  • 中文刊名:JORE
  • 英文刊名:资源与生态学报(英文版)
  • 机构:中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室拉萨高原生态系统研究站;
  • 出版日期:2019-07-29
  • 出版单位:Journal of Resources and Ecology
  • 年:2019
  • 期:v.10
  • 基金:National Natural Science Foundation of China(31370458,31600432,41807331);; Bingwei Outstanding Young Talents Program of Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences(2018RC202);; National Key Research Projects of China(2016YFC0502005,2016YFC0502006,2017YFA0604801);; Youth Innovation Research Team Project of Key Laboratory of Ecosystem Network Observation and Modeling(LENOM2016Q0002);; Tibet Science and Technology Major Projects of Pratacultural Industry(XZ201801NA02)
  • 语种:英文;
  • 页:JORE201904005
  • 页数:6
  • CN:04
  • ISSN:11-5885/P
  • 分类号:32-37
摘要
目前有关青藏高原农田土壤微生物量及群落组成对实验增温的响应还未见报道。2014年5月,在西藏的一个青稞田布设了三个增温梯度实验(即对照、低幅度增温和高幅度增温)。低幅度增温和高幅度增温分别显著提高了土壤15cm深处的土壤温度1.02℃和1.59℃。2014年9月14日,对青稞田0–10 cm和10–20 cm的土壤进行了取样,之后通过磷脂脂肪酸法分析了土壤微生物群落组成。低幅度增温没有显著影响0–10cm和10–20cm的土壤总磷脂脂肪酸量、真菌、细菌、丛植菌根真菌、放线菌、革兰氏阳性细菌、革兰氏阴性细菌、原生动物、真菌与细菌比、革兰氏阳性细菌与革兰氏阴性细菌比、土壤微生物群落组成;高幅度增温显著增加了土壤0–10 cm的74.4%的土壤总磷脂脂肪酸、78.0%的真菌、74.0%的细菌、66.9%的丛植菌根真菌、81.4%的放线菌、67.0%的革兰氏阳性细菌、74.4%的革兰氏阴性细菌,高幅度增温显著改变了0–10 cm的土壤微生物群落组成。高幅度增温对土壤10–20cm的土壤微生物群落组成、总的磷脂脂肪酸量、真菌、细菌、丛植菌根真菌、放线菌、革兰氏阳性细菌、革兰氏阴性细菌、原生动物、真菌与细菌比以及革兰氏阳性细菌与革兰氏阴性细菌比也都无显著影响。因此,土壤微生物群落组成对西藏青稞田实验增温的响应与增温幅度有关。
        No studies have examined the effect of experimental warming on the microbial biomass and community composition of soil in agricultural ecosystem on the Qinghai-Tibet Plateau. Thus it is unclear whether the influences of experimental warming on microbial communities in soil are related to warming magnitude in croplands on this Plateau. This study performed warming experiment(control, low-and high-level) in a highland barley system of the Lhasa River in May 2014 to examine the correlation between the response of microbial communities in soil to warming and warming magnitude. Topsoil samples(0–10 and 10–20 cm) were collected on September 14, 2014. Experimental warming at both low and high levels significantly increased soil temperature by 1.02 ℃ and 1.59 ℃, respectively at the depth of 15 cm. Phospho lipid fatty acid(PLFA) method was used to determine the microbial community in soil. The low-level experimental warming did not significantly affect the soil's total PLFA, fungi, bacteria, arbuscular mycorrhizal fungi(AMF), actinomycetes, gram-positive bacteria(G+), gram-negative bacteria(G–), protozoa, the ratio of fungi to bacteria(F/B ratio), and ratio of G+ to G–(G+/G– ratio) at the 0–10 and 10–20 cm depth. The low-level experimental warming also did not significantly alter the composition of microbial community in soil at the 0–10 and 10–20 cm depth. The high-level experimental warming significantly increased total PLFA by 74.4%, fungi by 78.0%, bacteria by 74.0%, AMF by 66.9%, actinomycetes by 81.4%, G+ by 67.0% and G– by 74.4% at the 0–10 cm depth rather than at 10–20 cm depth. The high-level experimental warming significantly altered microbial community composition in soil at the 0–10 cm depth rather than at 10-20 cm depth. Our findings suggest that the response of microbial communities in soil to warming varied with warming magnitudes in the highland barley system of the Lhasa River.
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