Characteristics of Soil Microbial Community Structure in the Rhizospheric Soil of Ammopiptanthus mongolicus by Phospholipid Fatty Acid (PLFA)

Abstract

To measure and manage plant growth in arid and semi-arid sandlands, improved understanding of the spatial patterns of desert soil resources and the role of soil microbes is required. The rhizosphere soils of Ammopiptanthus mongolicus in Wuhai, Dengkou, and Alxa, Inner Mongolia, China were collected in July 2015. Soil microbial community structure in the rhizosphere of A.mongolicus was analyzed by phospholipid fatty acid (PLFA) combined with Sherlock microbial identification system. The results showed that the soil microbial PLFA had a higher diversity and 41, 31 and 48 kinds of phospholipid fatty acids were respectively detected in the rhizosphere of A.mongolicus in three different sites. 16:0, 16:0 10-methy1, 18:1ω9c and 16:1ω7c were the dominant PLFA, and the PLFA of 16:0 (indicating bacteria) had a maximum value. However, the differences in contents of 16:0 10-methy, 18:1ω9c and 16:1ω7c were found in the three sites. Soil microbial community in the rhizosphere of A.mongolicus had obvious spatial heterogeneity:the gram positive bacteria were the dominant microorganisms in all soil samples. AM fungi, gram positive bacteria, gram negative bacteria and fungi were all characterized by Alxa > Wuhai > Dengkou, and total PLFA content of actinomycetes followed the order of Wuhai > Alxa > Dengkou. AM fungi occupied the biggest proportion in the soil fungal biomass, especially in Dengkou and Alxa, which accounted for 91% and 92%, respectively. We concluded that AM fungi were an important component of soil microorganisms in the desert ecosystem. AM fungi, gram positive bacteria, gram negative bacteria, fungi and actinomycetes were positively correlated with soil acid and alkaline phosphatase, total glomalin, ammonia nitrogen and pH. G+/G- were extremely negatively correlated with soil urease, organic carbon and easily extractable glomalin. However, the fungi/bacteria were extremely positively correlated to soil urease, organic carbon and easily extractable glomalin. The results of this study support the conclusion that soil acid and alkaline phosphatase, total glomalin, ammonia nitrogen and pH were the main factors influencing soil microbial biomass and activities in desert zone.Moreover, the changing pattern of soil microbial community might be useful to monitor desertification and soil degradation.