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干湿交替频率对土壤细菌群落结构的影响。

Influence of drying-rewetting frequency on soil bacterial community structure.

作者信息

Fierer N, Schimel J P, Holden P A

机构信息

Department of Ecology, Evolution, and Marine Biology, University of California, Santa Barbara, CA 93106, USA.

出版信息

Microb Ecol. 2003 Jan;45(1):63-71. doi: 10.1007/s00248-002-1007-2. Epub 2002 Dec 10.

Abstract

Soil drying and rewetting represents a common physiological stress for the microbial communities residing in surface soils. A drying-rewetting cycle may induce lysis in a significant proportion of the microbial biomass and, for a number of reasons, may directly or indirectly influence microbial community composition. Few studies have explicitly examined the role of drying-rewetting frequency in shaping soil microbial community structure. In this experiment, we manipulated soil water stress in the laboratory by exposing two different soil types to 0, 1, 2, 4, 6, 9, or 15 drying-rewetting cycles over a 2-month period. The two soils used for the experiment were both collected from the Sedgwick Ranch Natural Reserve in Santa Ynez, CA, one from an annual grassland, the other from underneath an oak canopy. The average soil moisture content over the course of the incubation was the same for all samples, compensating for the number of drying-rewetting cycles. At the end of the 2-month incubation we extracted DNA from soil samples and characterized the soil bacterial communities using the terminal restriction fragment length polymorphism (T-RFLP) method. We found that drying-rewetting regimes can influence bacterial community composition in oak but not in grass soils. The two soils have inherently different bacterial communities; only the bacteria residing in the oak soil, which are less frequently exposed to moisture stress in their natural environment, were significantly affected by drying-rewetting cycles. The community indices of taxonomic diversity and richness were relatively insensitive to drying-rewetting frequency. We hypothesize that drying-rewetting induced shifts in bacterial community composition may partly explain the changes in C mineralization rates that are commonly observed following exposure to numerous drying-rewetting cycles. Microbial community composition may influence soil processes, particularly in soils exposed to a significant level of environmental stress.

摘要

土壤干燥和再湿润是表层土壤中微生物群落常见的生理应激。干燥-再湿润循环可能会导致相当一部分微生物生物量发生裂解,并且由于多种原因,可能直接或间接影响微生物群落组成。很少有研究明确考察干燥-再湿润频率在塑造土壤微生物群落结构中的作用。在本实验中,我们在实验室中通过在两个月的时间内将两种不同类型的土壤暴露于0、1、2、4、6、9或15次干燥-再湿润循环来控制土壤水分胁迫。用于实验的两种土壤均取自加利福尼亚州圣伊内斯的塞奇威克牧场自然保护区,一种来自一年生草地,另一种来自橡树冠层下方。所有样品在培养过程中的平均土壤水分含量相同,以补偿干燥-再湿润循环的次数。在为期两个月的培养结束时,我们从土壤样品中提取DNA,并使用末端限制性片段长度多态性(T-RFLP)方法对土壤细菌群落进行表征。我们发现,干燥-再湿润处理会影响橡树下土壤中的细菌群落组成,但对草地土壤中的细菌群落没有影响。这两种土壤具有内在不同的细菌群落;只有生活在橡树下土壤中的细菌,它们在自然环境中较少受到水分胁迫,会受到干燥-再湿润循环的显著影响。分类多样性和丰富度的群落指数对干燥-再湿润频率相对不敏感。我们推测,干燥-再湿润引起的细菌群落组成变化可能部分解释了在经历多次干燥-再湿润循环后通常观察到的碳矿化速率变化。微生物群落组成可能会影响土壤过程,特别是在受到显著环境胁迫的土壤中。

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