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草甸草原中植物多元素耦合对氮添加和磷添加的不同响应

Divergent responses of plant multi-element coupling to nitrogen and phosphorus addition in a meadow steppe.

作者信息

Yang Yang, Jin Meini, Liu Jushan

机构信息

Institute of Grassland Science, School of Life Sciences, Key Laboratory of Vegetation Ecology, Ministry of Education, Northeast Normal University, Changchun, China.

出版信息

BMC Plant Biol. 2025 Jan 25;25(1):110. doi: 10.1186/s12870-025-06129-1.

Abstract

The intricate biogeochemical cycling of multiple elements plays a pivotal role in upholding a myriad of ecosystem functions. However, our understanding of elemental stoichiometry and coupling in response to global changes remains primarily limited to plant carbon: nitrogen: phosphorus (C: N: P). Here, we assessed the responses of 11 elements in plants from different functional groups to global changes. Investigating the stoichiometric ratios and interrelationships of these elements in response to global change is crucial for advancing our understanding of nutrient cycling dynamics in ecosystems. We found that N deposition induced stoichiometric imbalances in Gramineae, leading to a reduction in elemental coupling. This disruption in elemental coupling could potentially affect plant growth and ecosystem functioning. However, leguminous plants, which possess specialized nitrogen fixation mechanisms, were unaffected, suggesting that their ability to independently regulate N may help them maintain stable nutrient ratios despite external N inputs. These findings highlight functional differences among plant groups in their response to global changes, with important implications for ecosystem resilience and nutrient dynamics. In summary, these diverse responses underscore the importance of understanding the underlying mechanisms to be able to better predict the future trajectory of terrestrial biogeochemical cycles under global N enrichment.

摘要

多种元素复杂的生物地球化学循环在维持众多生态系统功能方面发挥着关键作用。然而,我们对元素化学计量及其在响应全球变化时的耦合关系的理解主要仍局限于植物碳:氮:磷(C:N:P)。在此,我们评估了来自不同功能组的植物中11种元素对全球变化的响应。研究这些元素在响应全球变化时的化学计量比和相互关系,对于深化我们对生态系统中养分循环动态的理解至关重要。我们发现,氮沉降导致禾本科植物出现化学计量失衡,进而导致元素耦合减少。这种元素耦合的破坏可能会影响植物生长和生态系统功能。然而,具有特殊固氮机制的豆科植物未受影响,这表明它们独立调节氮的能力可能有助于它们在有外部氮输入的情况下保持稳定的养分比例。这些发现凸显了不同植物组在响应全球变化时的功能差异,对生态系统恢复力和养分动态具有重要意义。总之,这些多样的响应强调了理解潜在机制的重要性,以便能够更好地预测全球氮富集情况下陆地生物地球化学循环的未来轨迹。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c864/11762877/945c1016c28b/12870_2025_6129_Fig1_HTML.jpg

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