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在氮和磷限制的竞争假说下植物对高浓度二氧化碳的响应。

Plant responses to elevated CO under competing hypotheses of nitrogen and phosphorus limitations.

作者信息

Zhu Qing, Riley William J, Tang Jinyun, Bouskill Nicholas J

机构信息

Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA.

出版信息

Ecol Appl. 2024 Apr;34(3):e2967. doi: 10.1002/eap.2967. Epub 2024 Mar 12.

Abstract

The future ecosystem carbon cycle has important implications for biosphere-climate feedback. The magnitude of future plant growth and carbon accumulation depends on plant strategies for nutrient uptake under the stresses of nitrogen (N) versus phosphorus (P) limitations. Two archetypal theories have been widely acknowledged in the literature to represent N and P limitations on ecosystem processes: Liebig's Law of the Minimum (LLM) and the Multiple Element Limitation (MEL) approach. LLM states that the more limiting nutrient controls plant growth, and commonly leads to predictions of dramatically dampened ecosystem carbon accumulation over the 21st century. Conversely, the MEL approach recognizes that plants possess multiple pathways to coordinate N and P availability and invest resources to alleviate N or P limitation. We implemented these two contrasting approaches in the E3SM model, and compiled 98 in situ forest N or P fertilization experiments to evaluate how terrestrial ecosystems will respond to N and P limitations. We find that MEL better captured the observed plant responses to nutrient perturbations globally, compared with LLM. Furthermore, LLM and MEL diverged dramatically in responses to elevated CO concentrations, leading to a two-fold difference in CO fertilization effects on Net Primary Productivity by the end of the 21st century. The larger CO fertilization effects indicated by MEL mainly resulted from plant mediation on N and P resource supplies through N fixation and phosphatase activities. This analysis provides quantitative evidence of how different N and P limitation strategies can diversely affect future carbon and nutrient dynamics.

摘要

未来的生态系统碳循环对生物圈 - 气候反馈具有重要意义。未来植物生长和碳积累的规模取决于植物在氮(N)与磷(P)限制压力下获取养分的策略。文献中广泛认可两种典型理论来代表生态系统过程中的氮和磷限制:利比希最小因子定律(LLM)和多元素限制(MEL)方法。LLM指出,限制作用更强的养分控制着植物生长,通常会导致预测21世纪生态系统碳积累大幅减少。相反,MEL方法认识到植物拥有多种途径来协调氮和磷的有效性,并投入资源来缓解氮或磷的限制。我们在E3SM模型中实施了这两种截然不同的方法,并汇总了98个森林氮或磷施肥的原位实验,以评估陆地生态系统将如何应对氮和磷的限制。我们发现,与LLM相比,MEL能更好地在全球范围内捕捉到观察到的植物对养分扰动的反应。此外,LLM和MEL在对二氧化碳浓度升高的反应上有很大差异,到21世纪末,导致二氧化碳施肥对净初级生产力的影响相差两倍。MEL所显示的更大的二氧化碳施肥效应主要源于植物通过固氮和磷酸酶活性对氮和磷资源供应的调节作用。该分析提供了定量证据,证明不同的氮和磷限制策略如何能以不同方式影响未来的碳和养分动态。

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