Yanuo Zou, Xiangtao Wang, Jie Wang, Lu Zhang, Lirong Liao, Guobin Liu, Zilin Song, Chao Zhang
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Key results We found meadow degradation reduced alkaline phosphatase activity by 6.3–11.22% and soil P availability by 27.1–42.4% compared to the respective values in the non-degraded meadows, but this negative impact was only observed in moderately and severely degraded meadows. Meadow degradation caused a P limitation on the phoD-harbouring community and a decline in the abundance of phoD genes and diversity of phoD-harbouring bacterial communities, with an increase in oligotrophic groups (e.g. Actinobacteria) and a reduction in copiotrophic groups (e.g. Proteobacteria). The degradation-induced reduction in soil C supply and plant biomass decreased soil P availability by lowering the activity of alkaline phosphatases, which are closely associated with phoD-harbouring bacterial structure and diversity. Alloactinosynnema and Actinomadura were identified as the key taxa contributing to alkaline phosphatases activity. Conclusions Alpine meadow degradation decreases soil P availability by altering phoD-harbouring bacterial diversity. Implications Our results revealed the mechanisms of decreased P availability during alpine meadow degradation, which can guide the restoration of degraded meadow ecosystems.","PeriodicalId":21818,"journal":{"name":"Soil Research","volume":null,"pages":null},"PeriodicalIF":1.2000,"publicationDate":"2024-05-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Alpine meadow degradation decreases soil P availability by altering phoD-harbouring bacterial diversity\",\"authors\":\"Yanuo Zou, Xiangtao Wang, Jie Wang, Lu Zhang, Lirong Liao, Guobin Liu, Zilin Song, Chao Zhang\",\"doi\":\"10.1071/sr23133\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Context Soil degradation is usually accompanied by significant changes in phosphorus (P) availability, which complicates soil management. 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Meadow degradation caused a P limitation on the phoD-harbouring community and a decline in the abundance of phoD genes and diversity of phoD-harbouring bacterial communities, with an increase in oligotrophic groups (e.g. Actinobacteria) and a reduction in copiotrophic groups (e.g. Proteobacteria). The degradation-induced reduction in soil C supply and plant biomass decreased soil P availability by lowering the activity of alkaline phosphatases, which are closely associated with phoD-harbouring bacterial structure and diversity. Alloactinosynnema and Actinomadura were identified as the key taxa contributing to alkaline phosphatases activity. Conclusions Alpine meadow degradation decreases soil P availability by altering phoD-harbouring bacterial diversity. 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引用次数: 0
摘要
背景 土壤退化通常伴随着磷(P)供应量的显著变化,这使得土壤管理变得更加复杂。然而,人们对生态系统退化对土壤磷供应量的影响仍然知之甚少,尤其是在高山生态系统中,因为高山生态系统是地球上研究最不充分和最脆弱的陆地栖息地之一。目的 评估草甸退化对高山生态系统土壤钾供应的影响。方法 在青藏高原沿退化梯度(未退化、轻度退化、中度退化和严重退化)的四片高山草甸上调查了土壤钾相关特性、phoD-harbouring细菌群落和碱性磷酸酶水平的变化。主要结果 我们发现,与未退化草甸相比,草甸退化使碱性磷酸酶活性降低了 6.3-11.22%,土壤钾供应量降低了 27.1-42.4%,但只有在中度和严重退化草甸中才能观察到这种负面影响。草甸退化导致phoD-harbouring群落的P限制,phoD基因的丰度和phoD-harbouring细菌群落的多样性下降,寡养型群落(如放线菌)增加,共养型群落(如变形菌)减少。降解引起的土壤 C 供应量和植物生物量的减少,通过降低碱性磷酸酶的活性而降低了土壤中 P 的供应量,而碱性磷酸酶与 phoD 害细菌的结构和多样性密切相关。Alloactinosynnema 和 Actinomadura 被确定为提高碱性磷酸酶活性的关键类群。结论 高山草甸退化会通过改变噬菌体多样性来降低土壤钾的可用性。意义 我们的研究结果揭示了高山草甸退化过程中钾供应量下降的机制,可为退化草甸生态系统的恢复提供指导。
Alpine meadow degradation decreases soil P availability by altering phoD-harbouring bacterial diversity
Context Soil degradation is usually accompanied by significant changes in phosphorus (P) availability, which complicates soil management. However, the effect of ecosystem degradation on soil P availability remains poorly understood, especially in the alpine ecosystem, which is one of the most understudied and vulnerable terrestrial habitats of the planet. Aims Assess the effect of meadow degradation on soil P availability in the alpine ecosystem. Methods Changes in soil P-related properties, phoD-harbouring bacterial communities, and alkaline phosphatase levels were investigated in four alpine meadows along a degradation gradient (non-degraded, lightly degraded, moderately degraded, and severely degraded) on the Tibetan Plateau. Key results We found meadow degradation reduced alkaline phosphatase activity by 6.3–11.22% and soil P availability by 27.1–42.4% compared to the respective values in the non-degraded meadows, but this negative impact was only observed in moderately and severely degraded meadows. Meadow degradation caused a P limitation on the phoD-harbouring community and a decline in the abundance of phoD genes and diversity of phoD-harbouring bacterial communities, with an increase in oligotrophic groups (e.g. Actinobacteria) and a reduction in copiotrophic groups (e.g. Proteobacteria). The degradation-induced reduction in soil C supply and plant biomass decreased soil P availability by lowering the activity of alkaline phosphatases, which are closely associated with phoD-harbouring bacterial structure and diversity. Alloactinosynnema and Actinomadura were identified as the key taxa contributing to alkaline phosphatases activity. Conclusions Alpine meadow degradation decreases soil P availability by altering phoD-harbouring bacterial diversity. Implications Our results revealed the mechanisms of decreased P availability during alpine meadow degradation, which can guide the restoration of degraded meadow ecosystems.
期刊介绍:
Soil Research (formerly known as Australian Journal of Soil Research) is an international journal that aims to rapidly publish high-quality, novel research about fundamental and applied aspects of soil science. As well as publishing in traditional aspects of soil biology, soil physics and soil chemistry across terrestrial ecosystems, the journal welcomes manuscripts dealing with wider interactions of soils with the environment.
Soil Research is published with the endorsement of the Commonwealth Scientific and Industrial Research Organisation (CSIRO) and the Australian Academy of Science.