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    增温对高寒草甸土壤微生物多样性及功能潜力的影响

    Effects of warming on soil microbial diversity and functional potential in alpine meadows

    • 摘要:
      目的 本文旨在探明青藏高原高寒草甸生态系统不同土壤微生物类群多样性及其功能潜力对气候变暖的响应特征及机理。
      方法 基于为期6年的野外增温控制试验平台,利用不同功率红外加热方式,设置3个水平的温度处理,分别是对照、增低温( + 1.5 ℃)和增高温( + 2.5 ℃)处理。增温6年后于2020年8月采集土壤表层样品,利用微生物高通量测序手段,探讨土壤细菌和真菌群落对增温的响应特征及机制。
      结果 (1)增低温和增高温处理分别使得土壤表层温度增加了1.4 ℃和2.4 ℃(P < 0.05),土壤湿度分别下降了11%和17%(P < 0.05)。相比对照,土壤硝态氮含量在增低温和增高温处理下分别降低了66%和72%(P < 0.05)。土壤有效磷含量仅在增高温处理下显著增加了36%(P < 0.05)。(2)增温处理显著降低了土壤细菌α多样性及谱系多样性并改变了细菌群落结构(P < 0.05)。相比之下,土壤真菌以上指标均未表现出显著变化(P > 0.05)。(3)土壤细菌群落中,碳水化合物代谢以及全局和概述图谱等功能分类在增高温处理下明显促进。然而,对土壤真菌而言,增温并未显著影响共生营养型、病理营养型以及腐生营养型的功能丰度(P > 0.05)。(4)土壤细菌功能潜力与土壤总氮含量和土壤有效磷含量呈显著正相关,真菌功能潜力仅与真菌谱系多样性呈显著正相关(P < 0.05),而与土壤理化性质无显著相关性(P > 0.05)。
      结论 增温显著降低了土壤细菌α多样性以及谱系多样性,改变了其β多样性;增温通过调控土壤有效磷含量进而促进细菌群落在碳水化合物代谢等功能潜力的表达;相比之下,增温并未显著影响土壤真菌多样性、群落结构和功能潜力。研究结果表明了土壤细菌群落与真菌群落对气候变暖响应的敏感性存在差异,进而可能对生态系统功能产生不同影响。

       

      Abstract:
      Objective This study aimed to explore the response patterns of soil microbial diversity and their functional potentials to different warming levels in an alpine ecosystem on the Qinghai-Tibet Plateau of western China.
      Method We conducted a field manipulation warming experiment using infrared heating methods to set three warming treatments, including control, low-level warming (+1.5 ℃) and high-level warming (+2.5 ℃). Through soil microbial high-throughput sequencing analysis, we investigated the general patterns and mechanisms underlying soil bacterial and fungi communities in response to field warming.
      Result (1) Low-level warming and high-level warming significantly increased soil temperature in the topsoil by 1.4 and 2.4 ℃, and decreased soil moisture by 11% and 17%, respectively (P < 0.05). In contrast to the control, soil nitrate nitrogen content under low-level warming and high-level warming decreased by 66% and 72% (P < 0.05), respectively, while only high-level warming significantly stimulated soil available phosphorus content by 36% (P < 0.05). (2) Compared with control, warming significantly reduced soil bacterial α diversity and phylogenetic diversity, with notable differences in bacterial community structure (P < 0.05). But soil fungi community did not show any changes in these indicators. (3) In the soil bacterial community, functional categories such as carbohydrate metabolism and global and overview were significantly improved due to warming, while the abundance of three trophic types (i.e., symbiotroph, pathtroph, and saprotroph) of soil fungi did not change under warming. (4) Soil bacterial functional potentials were mainly and positively correlated with soil total nitrogen and available phosphorus, while fungal functional potentials were positively associated with fungal Shannon diversity index.
      Conclusion In conclusion, warming significantly reduces soil bacterial α diversity and phylogenetic diversity, alters its β diversity. Warming promotes the expression of functional potentials such as carbohydrate metabolism in the bacterial community by regulating soil available phosphorous. In contrast, warming does not influence soil fungal diversity, community structure, and functional potentials. Our findings highlight the differential temperature sensitivities of soil bacterial and fungal communities, which may affect ecosystem functions differently.

       

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