Phosphorus enrichment mediates the responses of plant lignin and microbial necromass accumulation to nitrogen addition in subalpine forest soil

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE Geoderma Pub Date : 2025-06-01 Epub Date: 2025-04-27 DOI:10.1016/j.geoderma.2025.117317
Ruyi Luo , Yakov Kuzyakov , Ji Chen , Wei Qiang , Yan Zhang , Xueyong Pang
{"title":"Phosphorus enrichment mediates the responses of plant lignin and microbial necromass accumulation to nitrogen addition in subalpine forest soil","authors":"Ruyi Luo ,&nbsp;Yakov Kuzyakov ,&nbsp;Ji Chen ,&nbsp;Wei Qiang ,&nbsp;Yan Zhang ,&nbsp;Xueyong Pang","doi":"10.1016/j.geoderma.2025.117317","DOIUrl":null,"url":null,"abstract":"<div><div>It is widely recognized that increased nitrogen (N) and phosphorus (P) inputs play critical roles in plant carbon (C) inputs and microbial growth and activity, thereby profoundly affecting the composition and dynamics of soil organic C (SOC). However, whether and how plant- and microbial-derived C and their associated SOC fractions respond to the interaction between N and P additions remain unclear. Here, an 8-year N and P addition experiment was conducted in a subalpine forest on the eastern Tibetan Plateau. We used amino sugars and lignin phenols as biomarkers for quantifying microbial necromass and plant lignin components, respectively, and separated SOC into distinct functional C pools, such as particulate organic C (POC) and mineral-associated organic C (MAOC). The results revealed that N addition decreased the retention of lignin phenols in SOC without P input, whereas no significant changes occurred under N addition with P input. In contrast, N addition increased the microbial necromass contribution to SOC under no P input, whereas N addition effects were absent under P input. Regarding N addition alone, the decrease in plant lignin was likely associated with lower lignin inputs from the root litter, while the increase in microbial necromass was largely attributed to suppressed necromass decomposition via a reduction in N-acquisition enzyme activity. Moreover, the POC and MAOC pools and their ratios to SOC were insensitive to N addition, regardless of P input. Collectively, our findings provide novel insights into the importance of P availability in mediating N addition-induced accumulation of plant lignin and microbial necromass in subalpine forest soil, highlighting the necessity of incorporating the interaction between N and P additions on plant- and microbial-derived components into terrestrial C cycling models to improve the prediction of SOC dynamics and storage under future nutrient enrichment scenarios.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"458 ","pages":"Article 117317"},"PeriodicalIF":6.6000,"publicationDate":"2025-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoderma","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016706125001557","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2025/4/27 0:00:00","PubModel":"Epub","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0

Abstract

It is widely recognized that increased nitrogen (N) and phosphorus (P) inputs play critical roles in plant carbon (C) inputs and microbial growth and activity, thereby profoundly affecting the composition and dynamics of soil organic C (SOC). However, whether and how plant- and microbial-derived C and their associated SOC fractions respond to the interaction between N and P additions remain unclear. Here, an 8-year N and P addition experiment was conducted in a subalpine forest on the eastern Tibetan Plateau. We used amino sugars and lignin phenols as biomarkers for quantifying microbial necromass and plant lignin components, respectively, and separated SOC into distinct functional C pools, such as particulate organic C (POC) and mineral-associated organic C (MAOC). The results revealed that N addition decreased the retention of lignin phenols in SOC without P input, whereas no significant changes occurred under N addition with P input. In contrast, N addition increased the microbial necromass contribution to SOC under no P input, whereas N addition effects were absent under P input. Regarding N addition alone, the decrease in plant lignin was likely associated with lower lignin inputs from the root litter, while the increase in microbial necromass was largely attributed to suppressed necromass decomposition via a reduction in N-acquisition enzyme activity. Moreover, the POC and MAOC pools and their ratios to SOC were insensitive to N addition, regardless of P input. Collectively, our findings provide novel insights into the importance of P availability in mediating N addition-induced accumulation of plant lignin and microbial necromass in subalpine forest soil, highlighting the necessity of incorporating the interaction between N and P additions on plant- and microbial-derived components into terrestrial C cycling models to improve the prediction of SOC dynamics and storage under future nutrient enrichment scenarios.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
磷富集介导亚高山森林土壤木质素和微生物坏死团积累对氮添加的响应
氮(N)和磷(P)输入的增加对植物碳(C)输入和微生物的生长和活动起着至关重要的作用,从而深刻影响土壤有机碳(SOC)的组成和动态。然而,植物和微生物来源的碳及其相关的有机碳组分是否以及如何响应N和P添加之间的相互作用仍不清楚。本文在青藏高原东部亚高山森林进行了为期8年的氮磷添加试验。我们使用氨基糖和木质素酚作为生物标志物分别定量微生物坏死组织和植物木质素成分,并将有机碳分为不同的功能碳池,如颗粒有机碳(POC)和矿物相关有机碳(MAOC)。结果表明,施氮降低了土壤中木质素酚类物质的保留率,而施氮加磷对土壤中木质素酚类物质保留率无显著影响。相反,在无磷输入条件下,施氮增加了微生物群落对有机碳的贡献,而在施磷条件下,施氮效果不明显。仅就N添加而言,植物木质素的减少可能与根系凋落物木质素输入的减少有关,而微生物坏死团的增加主要归因于通过N获取酶活性的降低抑制了坏死团的分解。此外,POC和MAOC池及其与SOC的比值对N添加不敏感,与P输入无关。总的来说,我们的研究结果为氮有效性在亚高山森林土壤中介导N添加诱导的植物木质素积累和微生物坏死块的重要性提供了新的见解,强调了将植物和微生物衍生成分的N和P添加之间的相互作用纳入陆地碳循环模型的必要性,以改善未来养分富集情景下有机碳动态和储存的预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
期刊最新文献
Spatially explicit impact of enhanced leaf litter leaching on the forest soil microbiome Organic amendments reshaped the chemical composition of soil organic matter: A meta-analysis Slope-dependent erosion control by rock fragments: experiments and model improvements Anecic earthworms and residue management synergistically enhance soil carbon sequestration via macroaggregate formation Mineral associated organic matter fractions have an outsized role in nitrogen mineralization and denitrification
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1