细胞外
土壤水分
单叠氮丙二钠
DNA
生物
微生物种群生物学
土壤微生物学
物种丰富度
环境DNA
相对物种丰度
细菌
生态学
植物
聚合酶链反应
生物多样性
丰度(生态学)
生物化学
遗传学
基因
作者
Paul Carini,Patrick J. Marsden,Jonathan W. Leff,Emily E. Morgan,Michael S. Strickland,Noah Fierer
出处
期刊:Nature microbiology
日期:2016-12-19
卷期号:2 (3)
被引量:752
标识
DOI:10.1038/nmicrobiol.2016.242
摘要
Extracellular DNA from dead microorganisms can persist in soil for weeks to years1–3. Although it is implicitly assumed that the microbial DNA recovered from soil predominantly represents intact cells, it is unclear how extracellular DNA affects molecular analyses of microbial diversity. We examined a wide range of soils using viability PCR based on the photoreactive DNA-intercalating dye propidium monoazide4. We found that, on average, 40% of both prokaryotic and fungal DNA was extracellular or from cells that were no longer intact. Extracellular DNA inflated the observed prokaryotic and fungal richness by up to 55% and caused significant misestimation of taxon relative abundances, including the relative abundances of taxa integral to key ecosystem processes. Extracellular DNA was not found in measurable amounts in all soils; it was more likely to be present in soils with low exchangeable base cation concentrations, and the effect of its removal on microbial community structure was more profound in high-pH soils. Together, these findings imply that this ‘relic DNA’ remaining in soil after cell death can obscure treatment effects, spatiotemporal patterns and relationships between microbial taxa and environmental conditions. Viability polymerase chain reaction based on the photoreactive DNA-intercalating dye propidium monoazide revealed that on average 40% of prokaryotic and fungal DNA in soil is extracellular, or from cells no longer intact, confounding estimates of richness and taxon relative abundance.
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