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使用稳定同位素辅助代谢组学方法追踪泥炭丘泥炭碳动态中的引发效应。

Tracing priming effects in palsa peat carbon dynamics using a stable isotope-assisted metabolomics approach.

作者信息

Ayala-Ortiz Christian, Hough Moira, Eder Elizabeth K, Hoyt David W, Chu Rosalie K, Toyoda Jason, Blazewicz Steven J, Crill Patrick M, Varner Ruth, Saleska Scott R, Rich Virginia I, Tfaily Malak M

机构信息

Department of Environmental Science, University of Arizona, Tucson, AZ, United States.

College of Forest Resources and Environmental Sciences, Michigan Technological University, Houghton, MI, United States.

出版信息

Front Mol Biosci. 2025 Aug 22;12:1621357. doi: 10.3389/fmolb.2025.1621357. eCollection 2025.

Abstract

INTRODUCTION

Peatlands store up to a third of global soil carbon, and in high latitudes their litter inputs are increasing and changing in composition under climate change. Although litter significantly influences peatland carbon and nutrient dynamics by changing the overall lability of peatland organic matter, the physicochemical mechanisms of this impact-and thus its full scope-remain poorly understood.

METHODS

We applied multimodal metabolomics (UPLC-HRMS, H NMR) paired with C Stable Isotope-Assisted Metabolomics (SIAM) to track litter carbon and its potential priming effects on both existing soil organic matter and carbon gas emissions. Through this approach, we achieved molecule-specific tracking of carbon transformations at unprecedented detail.

RESULTS

Our analysis revealed several key findings about carbon dynamics in palsa peat. Microbes responded rapidly to litter addition, producing a short-term increase in CO emissions, fueled nearly exclusively by transformations of litter carbon. Litter inputs significantly contributed to the organic nitrogen pool through amino acids and peptide derivatives, which served as readily accessible nutrient sources for microbial communities. We traced the fate of plant-derived polyphenols including flavonoids like rutin, finding evidence of their degradation through heterocyclic C-ring fission, while accumulation of some polyphenols suggested their role in limiting overall decomposition. The SIAM approach detected subtle molecular changes indicating minimal and transient priming activity that was undetectable through conventional gas measurements alone. This transient response was characterized by brief microbial stimulation followed by rapid return to baseline metabolism. Pre-existing peat organic matter remained relatively stable; significant priming of its consumption was not observed, nor was its structural alteration.

DISCUSSION

This suggests that while litter inputs temporarily increase CO emissions, they don't sustain long-term acceleration of stored carbon decomposition or substantially decrease peat's carbon store capacity. Our findings demonstrate how technological advancements in analytical tools can provide a more detailed view of carbon cycling processes in complex soil systems.

摘要

引言

泥炭地储存了全球土壤碳的三分之一,在高纬度地区,气候变化导致其凋落物输入量增加且组成发生变化。尽管凋落物通过改变泥炭地有机质的整体活性显著影响泥炭地的碳和养分动态,但其影响的物理化学机制以及全面范围仍知之甚少。

方法

我们应用多模态代谢组学(超高效液相色谱-高分辨率质谱联用、核磁共振氢谱)结合碳稳定同位素辅助代谢组学(SIAM)来追踪凋落物碳及其对现有土壤有机质和碳气体排放的潜在激发效应。通过这种方法,我们以前所未有的详细程度实现了对碳转化的分子特异性追踪。

结果

我们的分析揭示了关于帕尔萨泥炭地碳动态的几个关键发现。微生物对凋落物添加反应迅速,导致二氧化碳排放量短期增加,几乎完全由凋落物碳的转化提供燃料。凋落物输入通过氨基酸和肽衍生物对有机氮库有显著贡献,这些物质为微生物群落提供了易于获取的营养源。我们追踪了植物源多酚(包括芦丁等黄酮类化合物)的去向,发现了它们通过杂环碳环裂变降解的证据,而一些多酚的积累表明它们在限制整体分解中发挥作用。SIAM方法检测到细微的分子变化,表明存在最小且短暂的激发活性,仅通过传统气体测量无法检测到。这种短暂反应的特征是微生物短暂刺激后迅速恢复到基线代谢。先前存在的泥炭有机质保持相对稳定;未观察到其消耗的显著激发,也未观察到其结构改变。

讨论

这表明虽然凋落物输入会暂时增加二氧化碳排放,但它们不会持续长期加速储存碳的分解,也不会大幅降低泥炭的碳储存能力。我们的研究结果表明分析工具的技术进步如何能够提供更详细的复杂土壤系统中碳循环过程的视图。

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