Soil ecological stoichiometry reveals microbial nutrient limitation with alpine meadow degradation in northeastern Tibetan Plateau

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
{"title":"Soil ecological stoichiometry reveals microbial nutrient limitation with alpine meadow degradation in northeastern Tibetan Plateau","authors":"","doi":"10.1016/j.catena.2024.108358","DOIUrl":null,"url":null,"abstract":"<div><p>Alpine meadow degradation results in an imbalance of soil nutrient supply, with soil microorganisms playing a pivotal role as regulators of soil nutrient cycling. However, the metabolic limitations of soil microorganisms during the process of alpine meadow degradation have not been adequately elucidated. The objective of this study was to uncover the characteristics and driving factors underlying the metabolic limitations imposed on soil microorganisms during alpine meadow degradation. Here, we assessed the levels of total and available nutrients in soil, as well as microbial biomass and extracellular enzyme activities (including cellobiosidase [CBH], β-1,4-glucosidase [BG], β-1,4-N-acetylglucosaminidase [NAG], L-leucine aminopeptidase [LAP], and alkaline phosphatase [AP]) in degraded alpine meadows located on the northeastern Tibetan Plateau. The results demonstrated that alpine meadow degradation led to a reduction in soil C, N, and P contents, as well as available nutrients, microbial biomass, and soil extracellular enzyme activities. Analysis using the vector-threshold element ratio (VT) model revealed an increasing trend in microbial C limitation with the progression of alpine meadow degradation. In the 0–20 cm soil layer, microbial N limitation gradually weakened and shifted towards P limitation; however, an opposite pattern was observed in the 20–40 cm soil layer with worsening alpine meadow degradation. Additionally, alpine meadow degradation enhanced the microbial carbon use efficiency (CUE), which was negatively correlated with microbial C limitation but was positively correlated with N &amp; P limitations. Moreover, there was a weakening of soil microbial homeostasis associated with increased alpine meadow degradation levels, where available nutrients played a crucial role in driving nutrient limitations for soil microbes in degraded alpine meadows. The findings of this study contribute to enhancing the understanding of the key factors governing soil microbial nutrient limitation in degraded alpine meadows, thereby providing valuable theoretical support for improving soil quality and health in such alpine meadow ecosystems on the Qinghai-Tibetan Plateau.</p></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":null,"pages":null},"PeriodicalIF":5.4000,"publicationDate":"2024-09-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816224005551","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0

Abstract

Alpine meadow degradation results in an imbalance of soil nutrient supply, with soil microorganisms playing a pivotal role as regulators of soil nutrient cycling. However, the metabolic limitations of soil microorganisms during the process of alpine meadow degradation have not been adequately elucidated. The objective of this study was to uncover the characteristics and driving factors underlying the metabolic limitations imposed on soil microorganisms during alpine meadow degradation. Here, we assessed the levels of total and available nutrients in soil, as well as microbial biomass and extracellular enzyme activities (including cellobiosidase [CBH], β-1,4-glucosidase [BG], β-1,4-N-acetylglucosaminidase [NAG], L-leucine aminopeptidase [LAP], and alkaline phosphatase [AP]) in degraded alpine meadows located on the northeastern Tibetan Plateau. The results demonstrated that alpine meadow degradation led to a reduction in soil C, N, and P contents, as well as available nutrients, microbial biomass, and soil extracellular enzyme activities. Analysis using the vector-threshold element ratio (VT) model revealed an increasing trend in microbial C limitation with the progression of alpine meadow degradation. In the 0–20 cm soil layer, microbial N limitation gradually weakened and shifted towards P limitation; however, an opposite pattern was observed in the 20–40 cm soil layer with worsening alpine meadow degradation. Additionally, alpine meadow degradation enhanced the microbial carbon use efficiency (CUE), which was negatively correlated with microbial C limitation but was positively correlated with N & P limitations. Moreover, there was a weakening of soil microbial homeostasis associated with increased alpine meadow degradation levels, where available nutrients played a crucial role in driving nutrient limitations for soil microbes in degraded alpine meadows. The findings of this study contribute to enhancing the understanding of the key factors governing soil microbial nutrient limitation in degraded alpine meadows, thereby providing valuable theoretical support for improving soil quality and health in such alpine meadow ecosystems on the Qinghai-Tibetan Plateau.

Abstract Image

土壤生态化学计量揭示了青藏高原东北部高寒草甸退化对微生物养分的限制
高山草甸退化导致土壤养分供应失衡,而土壤微生物作为土壤养分循环的调节者,在其中发挥着举足轻重的作用。然而,土壤微生物在高寒草甸退化过程中的代谢限制尚未得到充分阐明。本研究旨在揭示高山草甸退化过程中土壤微生物代谢限制的特征和驱动因素。在此,我们评估了青藏高原东北部高寒草甸退化土壤中的总养分和可利用养分水平,以及微生物生物量和细胞外酶活性(包括纤维生物糖苷酶[CBH]、β-1,4-葡萄糖苷酶[BG]、β-1,4-N-乙酰葡萄糖苷酶[NAG]、L-亮氨酸氨肽酶[LAP]和碱性磷酸酶[AP])。结果表明,高寒草甸退化导致土壤碳、氮、磷含量以及可利用养分、微生物生物量和土壤胞外酶活性降低。利用矢量-阈值元素比(VT)模型进行的分析表明,随着高山草甸退化的加剧,微生物的碳限制呈上升趋势。在 0-20 厘米的土层中,微生物对氮的限制逐渐减弱,并转向对磷的限制;然而,在 20-40 厘米的土层中,随着高山草甸退化的加剧,观察到了相反的模式。此外,高山草甸退化提高了微生物的碳利用效率(CUE),CUE 与微生物的碳限制呈负相关,但与氮和磷限制呈正相关。此外,随着高山草甸退化程度的增加,土壤微生物的平衡也会减弱,在退化的高山草甸中,可用养分对土壤微生物的养分限制起着至关重要的作用。本研究的发现有助于加深对退化高寒草甸土壤微生物养分限制关键因素的理解,从而为改善青藏高原此类高寒草甸生态系统的土壤质量和健康状况提供有价值的理论支持。
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 求助全文
来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
文献相关原料
公司名称 产品信息 采购帮参考价格
×
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
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
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 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信