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Dissolved organic matter defines microbial communities during initial soil formation after deglaciation
Shen, Jie; Liang, Ziyan1; Kuzyakov, Yakov2,7; Li, Weitao3; He, Yuting4; Wang, Changquan5; Xiao, Yang; Chen, Ke6; Sun, Geng8; Lei, Yanbao8
2023
Source PublicationSCIENCE OF THE TOTAL ENVIRONMENT
ISSN0048-9697
Volume878Issue:xPages:-
AbstractEcosystem succession and pedogenesis reshuffle the composition and turnover of dissolved organic matter (DOM) and its interactions with soil microbiome. The changes of these connections are especially intensive during initial pedogenesis, e.g. in young post-glacial areas. The temporal succession and vertical development of DOM effects on microbial community structure remains elusive. Using Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FTICR MS), high-throughput sequencing, and molecular ecological networks, we characterized the molecular diversity of water-extractable DOM and identified its links to microbial communities in soil profiles along deglaciation chronosequence (12, 30, 40, 52, 80, and 120 years) in the southeastern Tibetan Plateau. Low-molecular-weight compound content decreased, whereas the mid- and high-molecular-weight compounds increased with succession age and soil depth. This was confirmed by the increase in double bond equivalents and averaged oxygen-to-carbon ratios (O/ C), and decrease in hydrogen-to-carbon ratios (H/C), which reflect DOM accumulation and stabilization. Microbial community succession shifted towards the dominance of oligotrophic Acidobacteria and saprophytic Mortierellomycota, reflecting the increase of stable DOM components (H/C < 1.5 and wider O/C). Less DOM-bacterial positive networks during the succession reduced specialization of labile DOM production (such as lipid- and protein-like compounds), whereas more DOM-fungal negative networks increased specialization of stable DOM decomposition (such as tannin-and condensed aromatic-like compounds). Consequently, DOM stability is not intrinsic during initial pedogen-esis: stable DOM compounds remain after fast bacterial utilization of labile DOM compounds, whereas fungi decom-pose slowly the remaining DOM pools.
KeywordHAILUOGOU GLACIER NUTRIENT LIMITATION PRIMARY SUCCESSION MASS-SPECTROMETRY GONGGA MOUNTAIN CARBON CHRONOSEQUENCE FOREFIELD CHEMISTRY BACTERIAL
Subject AreaEnvironmental Sciences & Ecology
DOI10.1016/j.scitotenv.2023.163171
Indexed BySCI
Language英语
WOS IDWOS:000976387900001
Citation statistics
Document Type期刊论文
Identifierhttps://ir.xtbg.ac.cn/handle/353005/13453
Collection2012年后新成立研究组
Affiliation1.Chinese Acad Sci, Chengdu Inst Biol, China Croatia Belt & Rd Joint Lab Biodivers & Ecos, CAS Key Lab Mt Ecol Restorat & Bioresource Utiliza, Chengdu 610041, Peoples R China
2.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Surface Proc & Ecol Regulat, Chengdu 610041, Peoples R China
3.RUDN Univ, Peoples Friendship Univ Russia, Moscow 117198, Russia
4.Chinese Acad Sci, CAS Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Menglun 666303, Yunnan, Peoples R China
5.Chengdu Popularizat Agr Tech Stn, Chengdu 610041, Peoples R China
6.Sichuan Agr Univ, Coll Resources, Chengdu 611130, Peoples R China
7.Southwest Univ Sci & Technol, Sch Life Sci & Engn, Mianyang 621010, Peoples R China
8.Kazan Fed Univ, Inst Environm Sci, Kazan 420049, Russia
9.Chinese Acad Sci, Chengdu Inst Biol, Number 9 Renmin South Rd, Chengdu 610041, Sichuan, Peoples R China
Recommended Citation
GB/T 7714
Shen, Jie,Liang, Ziyan,Kuzyakov, Yakov,et al. Dissolved organic matter defines microbial communities during initial soil formation after deglaciation[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2023,878(x):-.
APA Shen, Jie.,Liang, Ziyan.,Kuzyakov, Yakov.,Li, Weitao.,He, Yuting.,...&Lei, Yanbao.(2023).Dissolved organic matter defines microbial communities during initial soil formation after deglaciation.SCIENCE OF THE TOTAL ENVIRONMENT,878(x),-.
MLA Shen, Jie,et al."Dissolved organic matter defines microbial communities during initial soil formation after deglaciation".SCIENCE OF THE TOTAL ENVIRONMENT 878.x(2023):-.
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