Variations in microbial residue carbon and its contribution to soil organic carbon after vegetation restoration on farmland: The case of Guinan County

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Organic Geochemistry Pub Date : 2024-02-01 DOI:10.1016/j.orggeochem.2024.104753
Na Li , Yalin Wang , Lin Wei , Xungang Wang , Qian Zhang , Tongqing Guo , Xianli Xu , Na Zhao , Shixiao Xu
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Abstract

Microbial residue carbon (C) serves as a significant source of soil organic carbon (SOC). However, the contribution of microbial residue C to SOC accumulation after the restoration of farmland vegetation remains unclear, making it challenging to comprehend the role of microorganisms in the accumulation and transformation of SOC after vegetation restoration on farmland. Based on field investigations in Guinan County, Qinghai Province, our study focused on the microbial residue C content and its contribution to SOC in farmland, grassland, and shrub forest, employing the analysis of biomarkers. The results indicated that the microbial residue C content increased with the rise of SOC, soil total nitrogen (STN), and enzyme activities. Compared to farmland, grassland displayed significantly lower levels of SOC and STN, leading to reduced microbial residue C content, notably impacting the C content of fungal residues. Despite slightly lower levels of SOC and STN compared to farmland, shrub forest exhibited higher soil microbial residue C content, notably within bacterial residue C, due to elevated soil enzyme activities. The contribution of microbial residue C to SOC decreased as SOC content increased. In farmland boasting higher SOC content, the contribution of microbial residue C to SOC was notably lower compared to shrub forest and grassland with lower SOC content. In conclusion, compared to farmland, both shrub forest and grassland exhibited higher contributions of microbial residue C to SOC, which is favorable for the sequestration of stable SOC.

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农田植被恢复后微生物残留碳的变化及其对土壤有机碳的贡献:以贵南县为例
微生物残留碳(C)是土壤有机碳(SOC)的重要来源。然而,微生物残留碳对农田植被恢复后土壤有机碳积累的贡献尚不清楚,这使得人们难以理解微生物在农田植被恢复后土壤有机碳积累和转化中的作用。本研究以青海省贵南县的实地调查为基础,采用生物标志物分析方法,重点研究了农田、草地和灌木林中微生物残留 C 的含量及其对 SOC 的贡献。结果表明,微生物残余物 C 含量随着 SOC、土壤全氮(STN)和酶活性的增加而增加。与农田相比,草地的 SOC 和 STN 水平明显较低,导致微生物残留物 C 含量减少,尤其影响了真菌残留物的 C 含量。尽管 SOC 和 STN 水平略低于农田,但灌木林的土壤微生物残余物 C 含量较高,尤其是细菌残余物 C 含量,这是由于土壤酶活性提高所致。随着 SOC 含量的增加,微生物残余 C 对 SOC 的贡献率也在下降。在 SOC 含量较高的农田中,与 SOC 含量较低的灌木林和草地相比,微生物残余物 C 对 SOC 的贡献率明显较低。总之,与农田相比,灌木林和草地的微生物残余物 C 对 SOC 的贡献率都较高,有利于稳定 SOC 的固碳。
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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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