Imbalanced intracellular nutrient stoichiometries drive the regional structural variation of microeukaryotic communities in paddy fields.

IF 5.1 Q1 ECOLOGY ISME communications Pub Date : 2024-10-10 eCollection Date: 2024-01-01 DOI:10.1093/ismeco/ycae119
Pengfei Sun, Eleonora Silvano, Yin Chen, Yonghong Wu
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Abstract

Periphytons serve as critical microbial nutrient sinks at the soil-water interface, influencing biogeochemical cycles and nutrient migration in paddy fields. Despite their importance, the impact of accumulated intracellular nutrients on the spatial dynamics and community assembly of periphytons, particularly their microeukaryote communities, remains unclear. To address this gap, we examined the nutrient accumulation potential and its effects on microeukaryotes in periphytons from 220 paddy fields spanning up to 3469 km across three temperature zones. Our study reveals that the periphytons exhibit varying capacities to accumulate carbon, nitrogen, and phosphorus, leading to imbalanced intracellular nutrient stoichiometries (carbon-to-nitrogen ratio = 10.3 ± 2.1, carbon-to-phosphorus ratio = 30.9 ± 13.1, nitrogen-to-phosphorus ratio = 3.1 ± 1.3). This stoichiometric imbalance induces intracellular environmental heterogeneity, which partially influences the local species richness of microeukaryotic communities and their regional structural variations on a large scale. Contrary to the typical latitudinal diversity gradient theory, local microeukaryotic species richness follows a distance-decay model, with both deterministic and stochastic processes contributing to community assembly. These results underscore the complex interplay of environmental filtering, species interactions, and dispersal dynamics in shaping the structure and adaptability of microeukaryotic communities within periphytons. This study contributes to a broader understanding of the factors driving regional structural variations of microeukaryotes at the soil-water interface in agricultural landscapes.

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细胞内养分比例失调导致稻田中微真核生物群落的区域结构变化。
附生植物是土壤-水界面上重要的微生物养分汇,影响着稻田的生物地球化学循环和养分迁移。尽管其重要性不言而喻,但细胞内积累的营养物质对围岩的空间动态和群落组合(尤其是微真核细胞群落)的影响仍不清楚。为了填补这一空白,我们研究了来自三个温带、跨度长达 3469 千米的 220 块水稻田的营养积累潜力及其对围岩中微真核生物的影响。我们的研究发现,围岩积累碳、氮和磷的能力各不相同,导致细胞内养分平衡失调(碳氮比 = 10.3 ± 2.1,碳磷比 = 30.9 ± 13.1,氮磷比 = 3.1 ± 1.3)。这种化学计量失衡引起了细胞内环境的异质性,部分影响了微真核细胞群落的局部物种丰富度及其大尺度的区域结构变化。与典型的纬度多样性梯度理论相反,本地微真核细胞物种丰富度遵循距离衰减模型,确定性过程和随机过程都有助于群落的形成。这些结果凸显了环境过滤、物种相互作用和扩散动力学在塑造围岩内微真核生物群落的结构和适应性方面的复杂相互作用。这项研究有助于人们更广泛地了解农业景观土壤-水界面微真核细胞区域结构变化的驱动因素。
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