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土壤微生物演替的模式与环境驱动因素

Patterns and Environmental Drivers of Soil Microbial Succession.

作者信息

Yu Zhi, Zeng Xiao-Min, Cheng Xiaoli, Zhang Quanfa, Zhang Kerong

机构信息

State Key Laboratory of Lake and Watershed Science for Water Security, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, People's Republic of China.

University of the Chinese Academy of Sciences, Chinese Academy of Sciences, Beijing, People's Republic of China.

出版信息

Glob Chang Biol. 2025 Sep;31(9):e70475. doi: 10.1111/gcb.70475.

Abstract

Succession has been a central theme of ecology for over a century, yet the patterns and drivers of soil microbial succession remain less well understood. Here, we analyzed the raw sequencing data of 5184 soil samples involving microbial succession, including primary succession, forest and grassland secondary succession. We provide the first evidence that the β-diversity (β-total, compositional dissimilarity between communities) of soil bacterial and fungal communities both decreased significantly with successional age in the three successional types. This indicates that convergent succession (i.e., decrease in β-total with time) is prevalent and independent of successional types and initial conditions. Partitioning β-total into species addition and replacement revealed that species addition dominates in early succession and then declines with successional age, whereas species replacement shows an increasing pattern over succession and ultimately dominates the late-successional communities. The convergent succession is mainly attributed to the directional species replacement and is driven by the changes in soil properties. In primary succession, β-total in bacterial communities is negatively correlated with soil total nitrogen (TN), soil organic carbon (SOC), NO -N, and NH -N, and β-total in fungal communities is negatively related to soil TN, NH -N, and NO -N. In forest secondary succession, β-total in bacterial communities is negatively correlated with TN and SOC, and β-total in fungal communities is negatively related to TN, SOC, and NH -N. In grassland secondary succession, β-total in bacterial communities is positively associated with the changes in soil pH (ΔpH), and β-total in fungal communities is negatively related to TN and SOC. Except for grassland bacterial succession, soil microbial communities generally shift from r-strategy (copiotrophs) to K-strategy (oligotrophs) during succession. Together, our study fills the knowledge gap in soil microbial succession patterns and highlights the universality of community convergence as predicted by the classical macroecological model.

摘要

一个多世纪以来,演替一直是生态学的核心主题,但土壤微生物演替的模式和驱动因素仍未得到充分理解。在这里,我们分析了5184个涉及微生物演替的土壤样本的原始测序数据,包括原生演替、森林和草地次生演替。我们提供了首个证据,表明在这三种演替类型中,土壤细菌和真菌群落的β多样性(β总和,即群落间的组成差异)均随演替年龄显著降低。这表明趋同演替(即β总和随时间减少)是普遍存在的,且与演替类型和初始条件无关。将β总和分解为物种增加和物种替代表明,物种增加在演替早期占主导地位,然后随演替年龄下降,而物种替代在演替过程中呈增加趋势,并最终在演替后期群落中占主导地位。趋同演替主要归因于定向的物种替代,并由土壤性质的变化驱动。在原生演替中,细菌群落的β总和与土壤全氮(TN)、土壤有机碳(SOC)、NO₃-N和NH₄-N呈负相关,真菌群落的β总和与土壤TN、NH₄-N和NO₃-N呈负相关。在森林次生演替中,细菌群落的β总和与TN和SOC呈负相关,真菌群落的β总和与TN、SOC和NH₄-N呈负相关。在草地次生演替中,细菌群落的β总和与土壤pH变化(ΔpH)呈正相关,真菌群落的β总和与TN和SOC呈负相关。除草地细菌演替外,土壤微生物群落在演替过程中通常从r策略(富营养菌)转变为K策略(贫营养菌)。总之,我们的研究填补了土壤微生物演替模式方面的知识空白,并突出了经典宏观生态模型所预测的群落趋同的普遍性。

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