{"title":"岩溶含水层中微生物群落和溶解有机质分子转化与氮命运的联系","authors":"Ruixuan Gai, Jing Bao, Wei Xiu, Fang Guo, Qiang Li, Qiang Zhang","doi":"10.1029/2025JG008961","DOIUrl":null,"url":null,"abstract":"<p>Understanding the biogeochemical processes governing carbon and nitrogen cycling in karst aquifers is critical. However, the specific pathways through which dissolved organic matter (DOM) influences nitrogen cycling under varying degrees of aquifer confinement remain poorly understood. This study addresses this knowledge gap by analyzing geochemical characteristics, DOM compositions, and microbial communities in three types of aquifer media, karst fissure media (KFM), karst conduit media (KCM), and karst window groundwater (KWG), at the Zengpiyan karst site in southern China, using carbon isotopes, Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS), and amplicon sequencing. Results indicated that longer hydraulic residence time in KFM was associated with enhanced denitrification, whereas shorter residence in KCM/KWG favored nitrification. DOM was dominated by terrestrial lignin-like molecular formulas (55.92%), but residence time shaped molecular composition and biodegradation: KFM showed lower nominal oxidation state of carbon (NOSC<sub>wa</sub>, −0.60 ± 0.37) yet a higher end-member index (I<sub>bio</sub>, 0.37 ± 0.05), reflecting microbial preferential consumption of labile, high NOSC fractions, leaving recalcitrant lignin-like molecular formulas. Core taxa <i>Comamonas</i> and an unclassified Comamonadaceae genus were associated with lignin-like molecular formulas degradation and denitrification, while <i>Nitrospira</i> contributed to nitrification via lignin-like molecular formula-derived intermediates. Together they formed a “lignin-like molecular formulas degradation, ammonification, nitrification” cascade, with 53.82% of DOM degradation reactions involving nitrogen loss through CHON transformations. Overall, extended residence time in karst aquifers enables sequential degradation of recalcitrant lignin-like molecular formulas under low NOSC conditions via synergistic interactions between microbes, refining conceptual models of C-N coupling in hydrologically heterogeneous karst systems.</p>","PeriodicalId":16003,"journal":{"name":"Journal of Geophysical Research: Biogeosciences","volume":"130 9","pages":""},"PeriodicalIF":3.5000,"publicationDate":"2025-09-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Linking Microbial Communities and Molecular Transformations of Dissolved Organic Matter to the Fate of Nitrogen in Karst Aquifers\",\"authors\":\"Ruixuan Gai, Jing Bao, Wei Xiu, Fang Guo, Qiang Li, Qiang Zhang\",\"doi\":\"10.1029/2025JG008961\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Understanding the biogeochemical processes governing carbon and nitrogen cycling in karst aquifers is critical. However, the specific pathways through which dissolved organic matter (DOM) influences nitrogen cycling under varying degrees of aquifer confinement remain poorly understood. This study addresses this knowledge gap by analyzing geochemical characteristics, DOM compositions, and microbial communities in three types of aquifer media, karst fissure media (KFM), karst conduit media (KCM), and karst window groundwater (KWG), at the Zengpiyan karst site in southern China, using carbon isotopes, Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS), and amplicon sequencing. Results indicated that longer hydraulic residence time in KFM was associated with enhanced denitrification, whereas shorter residence in KCM/KWG favored nitrification. DOM was dominated by terrestrial lignin-like molecular formulas (55.92%), but residence time shaped molecular composition and biodegradation: KFM showed lower nominal oxidation state of carbon (NOSC<sub>wa</sub>, −0.60 ± 0.37) yet a higher end-member index (I<sub>bio</sub>, 0.37 ± 0.05), reflecting microbial preferential consumption of labile, high NOSC fractions, leaving recalcitrant lignin-like molecular formulas. Core taxa <i>Comamonas</i> and an unclassified Comamonadaceae genus were associated with lignin-like molecular formulas degradation and denitrification, while <i>Nitrospira</i> contributed to nitrification via lignin-like molecular formula-derived intermediates. Together they formed a “lignin-like molecular formulas degradation, ammonification, nitrification” cascade, with 53.82% of DOM degradation reactions involving nitrogen loss through CHON transformations. Overall, extended residence time in karst aquifers enables sequential degradation of recalcitrant lignin-like molecular formulas under low NOSC conditions via synergistic interactions between microbes, refining conceptual models of C-N coupling in hydrologically heterogeneous karst systems.</p>\",\"PeriodicalId\":16003,\"journal\":{\"name\":\"Journal of Geophysical Research: Biogeosciences\",\"volume\":\"130 9\",\"pages\":\"\"},\"PeriodicalIF\":3.5000,\"publicationDate\":\"2025-09-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysical Research: Biogeosciences\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JG008961\",\"RegionNum\":3,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Biogeosciences","FirstCategoryId":"93","ListUrlMain":"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JG008961","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Linking Microbial Communities and Molecular Transformations of Dissolved Organic Matter to the Fate of Nitrogen in Karst Aquifers
Understanding the biogeochemical processes governing carbon and nitrogen cycling in karst aquifers is critical. However, the specific pathways through which dissolved organic matter (DOM) influences nitrogen cycling under varying degrees of aquifer confinement remain poorly understood. This study addresses this knowledge gap by analyzing geochemical characteristics, DOM compositions, and microbial communities in three types of aquifer media, karst fissure media (KFM), karst conduit media (KCM), and karst window groundwater (KWG), at the Zengpiyan karst site in southern China, using carbon isotopes, Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS), and amplicon sequencing. Results indicated that longer hydraulic residence time in KFM was associated with enhanced denitrification, whereas shorter residence in KCM/KWG favored nitrification. DOM was dominated by terrestrial lignin-like molecular formulas (55.92%), but residence time shaped molecular composition and biodegradation: KFM showed lower nominal oxidation state of carbon (NOSCwa, −0.60 ± 0.37) yet a higher end-member index (Ibio, 0.37 ± 0.05), reflecting microbial preferential consumption of labile, high NOSC fractions, leaving recalcitrant lignin-like molecular formulas. Core taxa Comamonas and an unclassified Comamonadaceae genus were associated with lignin-like molecular formulas degradation and denitrification, while Nitrospira contributed to nitrification via lignin-like molecular formula-derived intermediates. Together they formed a “lignin-like molecular formulas degradation, ammonification, nitrification” cascade, with 53.82% of DOM degradation reactions involving nitrogen loss through CHON transformations. Overall, extended residence time in karst aquifers enables sequential degradation of recalcitrant lignin-like molecular formulas under low NOSC conditions via synergistic interactions between microbes, refining conceptual models of C-N coupling in hydrologically heterogeneous karst systems.
期刊介绍:
JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology