4.7 Article

Soil bacterial community response to vegetation succession after fencing in the grassland of China

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 609, 期 -, 页码 2-10

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.scitotenv.2017.07.102

关键词

Available nutrients; HiSeq prosequencing; Soil bacteria; Vegetation succession; Yunwu Mountain

资金

  1. National Natural Science Foundation of China [41671280]
  2. Key Projects in the National Science & Technology Pillar Program during the Twelfth Five-year Plan Period [2015BAC01B01]
  3. Special-Funds of Scientific Research Programs of State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau [A314021403-C6]

向作者/读者索取更多资源

Natural succession is an important process in terrestrial system, playing an important role in enhancing soil quality and plant diversity. Soil bacteria is the linkage between soil and plant, has an important role in aboveground community dynamics and ecosystem functioning in terrestrial ecosystems, driving the decomposition of soil organic matter and plant litter. However, the role of soil bacteria in the secondary succession has not been well understood, particularly in the degraded soil of Loess Plateau. In this study, we investigated soil nutrients and soil bacterial community during the secondary succession after a long-term fencing in the grassland, in the Yuwu Mountain, northwest China. The chronosequence included 1 year, 12 years, 20 years and 30 years. The soil bacterial community composition was determined by the Illumina HiSeq sequencing method. The data showed that soil bacterial diversity had no significant changes along the chronosequence, but soil bacterial community compositions significantly changed. Proteobacteria, Acidobacteria and Actinobacteria were the main phyla in all the samples across succession. With the accumulation of soil organic matter and nutrients, the relative abundance of Actinobacteria decreased, whereas Proteobacteria increased. These shifts may be caused by the increase of the available nutrients across the secondary succession. In the younger sites, soils were dominated by oligotrophic groups, whereas soil in the late-succession site were dominated by copiotrophic groups, indicating the dependence of soil bacterial community composition on the contents of soil available nutrients. (C) 2017 Elsevier B.V. All rights reserved.

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