土壤盐渍化对稀有和常见细菌群落结构和功能的影响

Effects of Soil Salinization on the Structure and Function of Rare and Common Bacteria

  • 摘要: 土壤盐渍化是全球干旱区防护林长期固存的主要胁迫因子,影响着防护林细菌群落结构及其驱动的物质循环和养分活性,细菌群落由常见物种和稀有物种组成,为明晰二者在环境胁迫响应中的功能作用,该文以塔里木沙漠公路防护林长期咸水灌溉形成的土壤盐分梯度为研究系统,测定土壤细菌群落和土壤碳氮磷酶活性,使用0.01%相对丰度阈值法确定稀有物种和常见物种,使用酶多功能性和向量法表征土壤功能,探究稀有和常见细菌对盐渍化响应的敏感性及二者对土壤功能的驱动作用。结果表明:①防护林稀有细菌物种丰富度随盐分含量增加呈显著下降趋势(P<0.05);稀有细菌(ρ=0.293,P<0.01)和常见细菌群落组成(ρ=0.205,P<0.01)均受土壤盐分变化的影响,但稀有细菌群落组成呈现更大的变幅。②土壤细菌活性受磷而非氮元素的限制(向量角度>45°),随盐分含量增加,磷代谢/氮代谢功能呈显著下降(r=−0.190,P<0.05)的趋势,酶多功能性呈显著增加( r =0.253, P<0.01)的趋势。③常见细菌物种丰富度(r= 0.173,P<0.05)及群落组成(r=0.181,P<0.05)显著提升了碳代谢功能(向量长度),群落组成显著改善了土壤酶多功能性(partial r=0.177,P<0.01)。研究显示,沙漠公路防护林稀有细菌而非常见细菌主导群落对盐渍化的响应,二者对土壤功能的调控路径存在差异,而常见细菌是土壤功能变化的主要驱动者。

     

    Abstract: Soil salinization is a common stress on shelterbelts in arid regions around the world, which affects the cycling and maintenance of soil nutrients mediated by bacteria and threatens the stability of desert shelterbelt ecosystems. Bacterial communities consist of both common and rare species, but their roles in salinity stress responses remain unclear. The purpose of this study was to determine how rare and common bacteria respond to salinization, as well as the effects on soil function. Thus, soil bacterial community and carbon, nitrogen, and phosphorus-related enzyme activities along the salinity gradient in the Tarim Desert Highway shelterbelt formed by long-term saline irrigation were investigated. The rare and common bacteria were identified using the 0.01% relative abundance threshold method, and the soil function was characterized using the multifunctionality and vector methods. The results showed that: (1) The species richness of rare bacteria in the shelterbelts decreased significantly with soil salinity (P<0.05). Soil salinization significantly altered the community composition of rare bacteria (ρ=0.293, P<0.01) and common bacteria (ρ=0.205, P<0.01), with rare bacteria exhibiting greater variation. (2) Soil bacteria in the shelterbelts were limited by phosphorus but not nitrogen (vector angle >45°). As soil salinity increased, soil phosphorus/nitrogen cycling function (r=−0.190, P<0.05) and enzyme multifunctionality (r=0.253, P<0.01) decreased and increased, respectively. (3) The common bacteria were positively correlated with soil carbon cycle function (vector length) for species richness (r=0.173, P<0.05) and community composition (r=0.181, P<0.05), as well as soil enzyme multifunctionality (partial r=0.177, P<0.01) for community composition. The findings imply that the rare taxa, rather than common taxa, dominated the responses of the bacterial community in shelterbelts to salinization, and that the mechanisms of these two groups in shaping the soil function were different, with common bacteria acting as the primary driving force.

     

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