4.1 Article

Changes in the soil microbial communities of different soil aggregations after vegetation restoration in a semiarid grassland, China

期刊

SOIL ECOLOGY LETTERS
卷 3, 期 1, 页码 6-21

出版社

SPRINGERNATURE
DOI: 10.1007/s42832-020-0055-1

关键词

Vegetation restoration; Plant succession; Phospholipid fatty acid (PLFA); Soil aggregate fractions; Soil microorganism group

资金

  1. National Natural Sciences Foundation of China [41807060, 41977061]
  2. National Special Research and Development Project during the Thirty Five-year Plan Period [2017YFC0504702]

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The stability of soil aggregate fractions and the duration of vegetation restoration significantly affect microbial community composition. Different sizes of soil aggregate fractions influence microbial diversity under different years of vegetation restoration, with the highest microbial diversity observed in large particle size aggregates.
Soil aggregate fractions can regulate microbial community composition and structure after vegetation restoration. However, there has been less focus on the effects of soil aggregate fractions on the distributions of microbial communities. Here, we used phospholipid fatty acid (PLFA) analysis to explore the effects of different years of vegetation restoration (a 35-year-old Thymus mongolicus community (Re-35yrs) and a 2-year-old nongrazing grassland (Ug-2yrs)) on microbial communities within different soil aggregate sizes (< 0.25 mm, 0.25-1 mm, 1-2 mm, 2-3 mm, 3-5 mm and >5 mm). The results indicated that the amount of total PLFA in Re-35yrs was 10 times greater than that in Ug-2yrs. The soil aggregate stability increased with increasing duration of vegetation restoration. In Re-35yrs, the total PLFA shown an increase as the soil aggregate size increased, and the highest values were observed in 3-5 mm. Ug-2yrs differed from Re-35yrs, the soil microbial diversity was higher in medium particle sizes (1-2 mm and 2-3 mm) and lower in microaggregates (<0.25 mm and 0.25-1 mm) and macroaggregates (3-5 mm and >5 mm). Soil microbial diversity was highest in large particle size aggregates, which resulted in low environmental stress and strong stability. The same tendency was observed in the high values of cyc/prec, S/M and soil organic matter, which indicated a lower turnover speed (F/B) of fungal energy utilization and a higher fixation rate. After years of natural restoration, the soil microbial community generally transformed from nutrient-rich to heterotrophdominant, especially in microaggregates (reflected in the G(+)/G(-) ratio).

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