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Predominant bacterial and fungal assemblages in agricultural soils during a record drought/heat wave and linkages to enzyme activities of biogeochemical cycling
Institution:1. USDA-Agricultural Research Service, Cropping Systems Research Laboratory, Lubbock, TX, USA;2. Department of Soil Science, 3411C Williams Hall, North Carolina State University, 101 Derieux Street, Raleigh, NC, USA;3. Department of Plant and Soil Sciences, Texas Tech University, Lubbock, TX, USA;4. Biological Sciences Department, Texas Tech University, Lubbock, TX, USA;5. Department of Animal, Rangeland and Wildlife Sciences & Caesar Kleberg Wildlife Research Institute, Texas A&M University-Kingsville, Kingsville, TX, USA;6. Research and Testing Laboratories, Lubbock, TX, USA;1. Department of Ecology and Evolutionary Biology, University of California, Irvine, Irvine, CA 92697, USA;2. Department of Earth System Science, University of California, Irvine, Irvine, CA 92697, USA;2. INRA, UMR 1347 Agroecology, Dijon, France;3. INRA, Plateforme GenoSol, UMR 1347 Agroecology, Dijon, France;1. Department of Soil Science, Faculty of Agriculture, Ferdowsi University of Mashhad, Mashhad, 91779-48944, Iran;2. Department of Soil and Plant Microbiome, Institute of Phytopathology, University of Kiel, Kiel, Germany;1. School of Geography and Tourism, Anhui Normal University, Wuhu, Anhui, China;2. State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China;3. Faculty of Geographical Science, Beijing Normal University, Beijing, China;4. School of Geography and Planning, Guangdong Key Laboratory for Urbanization and Geo-simulation, Guangdong Provincial Engineering Research Center for Public Security and Disaster, Sun Yat-sen University, Guangzhou, China
Abstract:Identification of microbial assemblages predominant under natural extreme climatic events will aid in our understanding of the resilience and resistance of microbial communities to climate change. From November 2010 to August 2011, the Southern High Plains (SHP) of Texas, USA, received only 39.6 mm of precipitation (vs. the historical average of 373 mm) and experienced the three hottest months (June–August 2011) since record keeping began in 1911. The objective of this study was to characterize soil bacterial (16 S rRNA gene) and fungal (internal transcribed spacer 1–4, ITS1-ITS4) species distribution and diversity via pyrosequencing during the peak of the drought/heat wave in July 2011 and when the Drought Index and temperatures were lower in March 2012. Samples were collected from two different soil types (loam and sandy loam) under two different dryland cropping histories (monoculture vs. rotation). Fungal Diversity Indexes were significantly higher after the drought/heat wave while Bacterial Indexes were similar. Bacterial phyla distribution in July 2011 was characterized by lower relative abundance of Acidobacteriaand Verrucomicrobia, and greater relative abundance of Proteobacteria, Chloroflexi, Actinobacteria and Nitrospirae than March 2012 samples. Further grouping of pyrosequencing data revealed approximately equal relative proportions of Gram positive (G+) and Gram negative (G?) bacteria in July 2011, while G? bacteria predominated in March 2012. Fungal class Dothideomycetes was approximately two times greater in July 2011 than in March 2012, while the class Sordariomycetes and a group of unidentified OTUs from Ascomycota increased from July 2011 to March 2012. Microbial community composition was less influenced by management history than by the difference in climatic conditions between the sampling times. Correspondence analysis identified assemblages of fungal and bacterial taxa associated with greater enzyme activities (EAs) of C, N, or P cycling found during the drought/heat wave. Microbial assemblages associated with arylsulfatase activity (key to S cycling), which increased after the drought/heat wave, were identified (Streptomyces parvisporogenes, Terrimonas ferruginea and Syntrophobacter sp.) regardless of the soil and management history. The distinct microbial composition found in July 2011 may represent assemblages essential to maintaining ecosystem function during extreme drought and intense heat waves in semiarid agroecosystems.
Keywords:Climate change  Pyrosequencing  Enzyme activities  Microbial diversity  Soil microbial community
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