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学者姓名：罗敏
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Abstract ：
Increased nitrogen (N) loading and sea-level rise (SLR) are two dominant drivers of global change that threaten tidal marshes and the ecosystem services they provide, including the sequestration of organic carbon. Nevertheless, the mechanisms through which N loading enrichment, SLR inundation increase, and their combined effects impact the rates and pathways of soil organic carbon (SOC) mineralization in tidal marshes remain poorly understood. We utilized a factorial design in an oligohaline tidal marsh, utilizing in situ weirs to simulate SLR inundation increase by manipulating the duration of flooding with or without nitrogen enrichment as NaNO3 plus NH4Cl or with a combination of increased flood duration and nitrogen. After nearly 2 years, the addition of N increased total SOC mineralization (CMR), soil microbial Fe(III) reduction (FeRR), NO3– reduction (NRR), and SO42– reduction (SRR) but decreased methanogenesis (MGR). The abiotic factor Fe(III)/Fe(II) ratio and dissolved organic carbon (DOC), and the biotic factors, β-glucosidase (BG), and phenol oxidase (PHO) activity explained the increased SOC mineralization rates following N enrichment. Increased flood duration did not change CMR, but increased flooding offset the stimulatory effects of N addition on CMR, FeRR, SRR, NRR and MGR. The contributions of Fe(III) reduction and SO42– reduction pathways to SOC mineralization increased in all experimental treatments, FeRR, SRR, NRR, and MGR were significantly positively correlated with the abundance of Geobacter, dsrA, nrfA, and mcrA. SLR inundation increase did not increase soil carbon loss in this oligohaline marsh and may counteract the simulation of soil C loss due to N enrichment. © 2024
Keyword ：
Carbon decomposition Carbon decomposition Functional microbes Functional microbes Inundation Inundation Nitrogen loading enrichment Nitrogen loading enrichment Oligohaline marsh Oligohaline marsh Sea-level rise Sea-level rise
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| GB/T 7714 | Tong, C. , Tan, J. , Luo, M. et al. Inundation counteracts the promoting effect of nitrogen enrichment on soil organic carbon mineralization in a tidal marsh [J]. | Fundamental Research , 2024 . |
| MLA | Tong, C. et al. "Inundation counteracts the promoting effect of nitrogen enrichment on soil organic carbon mineralization in a tidal marsh" . | Fundamental Research (2024) . |
| APA | Tong, C. , Tan, J. , Luo, M. , Huang, J. , Xiao, S. , Liu, B. et al. Inundation counteracts the promoting effect of nitrogen enrichment on soil organic carbon mineralization in a tidal marsh . | Fundamental Research , 2024 . |
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Keyword ：
aquatic ecosystems aquatic ecosystems carbon cycle carbon cycle dry-wet cycling dry-wet cycling greenhouse gases (GHGs) greenhouse gases (GHGs) microbial metabolism microbial metabolism
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| GB/T 7714 | Zhang, Peng , Luo, Min , Fu, Chuancheng et al. Editorial: Microbial-driven carbon turnover from dry-wet cycling regions [J]. | FRONTIERS IN MICROBIOLOGY , 2024 , 15 . |
| MLA | Zhang, Peng et al. "Editorial: Microbial-driven carbon turnover from dry-wet cycling regions" . | FRONTIERS IN MICROBIOLOGY 15 (2024) . |
| APA | Zhang, Peng , Luo, Min , Fu, Chuancheng , Xiao, Leilei . Editorial: Microbial-driven carbon turnover from dry-wet cycling regions . | FRONTIERS IN MICROBIOLOGY , 2024 , 15 . |
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针对新时代背景下“双一流”高校人才培养的发展需求，在“三创五育”理念指导下，解析基于产学研合作理论引入的DIE模式的内涵，系统阐述了DIE理念贯彻下的教学系统设计并付诸实践，旨在打破教学系、研究所、企业之间的壁垒，为学生学习、实践提供更多样化的渠道。问卷调查结果表明DIE模式在本科生团队协作、学术创造、自信心树立等方面有切实作用，为培养全面发展的高素质本科人才提供了参考。
Keyword ：
DIE模式 DIE模式 “三创五育” “三创五育” “双一流”高校 “双一流”高校 本科人才培养 本科人才培养
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| GB/T 7714 | 许章华 , 张超飞 , 罗敏 et al. “三创五育”背景下“双一流”高校本科人才培养的DIE模式初探及评价 [J]. | 高等理科教育 , 2024 , 9 (02) : 53-61 . |
| MLA | 许章华 et al. "“三创五育”背景下“双一流”高校本科人才培养的DIE模式初探及评价" . | 高等理科教育 9 . 02 (2024) : 53-61 . |
| APA | 许章华 , 张超飞 , 罗敏 , 杨远垚 , 刘智才 . “三创五育”背景下“双一流”高校本科人才培养的DIE模式初探及评价 . | 高等理科教育 , 2024 , 9 (02) , 53-61 . |
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氮素是影响湿地甲烷代谢过程的重要因素之一。氮输入是否影响湿地甲烷排放，增加全球气候变暖的风险，一直受到科学界的高度关注。目前关于氮输入对湿地甲烷排放影响的几篇meta-analysis文章的主要结论均为氮输入促进湿地甲烷排放，但是多篇研究性论文的结果为氮输入抑制或不影响湿地甲烷排放，由此可见氮输入对湿地甲烷排放的影响十分复杂。湿地甲烷代谢包括湿地甲烷产生、氧化和传输过程以及最终的甲烷排放，综述不同形态氮输入对水稻田、内陆湿地和滨海湿地甲烷排放通量影响的复杂性；分析湿地甲烷产生速率和途径、甲烷好氧氧化和硝酸盐/亚硝酸盐型厌氧甲烷氧化对不同形态氮输入的响应及机制。硝态氮输入对湿地甲烷产生具有抑制作用已成共识，然而其它形态氮输入对湿地土壤甲烷产生的影响具有较大的不确定性，氮输入影响湿地甲烷产生的机制主要包括电子受体-底物竞争机制、离子毒性机制、促进植物生长-碳底物供给增加机制以及pH调控机制等。氮输入对湿地好氧甲烷氧化影响的研究多集中在水稻田和泥炭湿地，影响的结果包括促进、抑制或影响不显著；氮输入促进湿地土壤硝酸盐/亚硝酸盐型厌氧甲烷氧化。本文着重分析氮输入对湿地甲烷代谢影响不确定性的成因，指出湿地甲烷代谢对氮输入的响应是一个生态系统层面的生物地球化学过程，并提出氮输入是最具争议效应的驱动因素之一，其对甲烷代谢的影响很难得出明确的模式，可能需要考虑湿地土壤特征（本底氮含量、有机碳含量、土壤C:N值等）以及植物群落类型和特征，最后提出今后在氮输入对湿地甲烷代谢影响方面应加强的研究领域。
Keyword ：
不确定性 不确定性 氮输入 氮输入 湿地 湿地 生态系统特征 生态系统特征 甲烷产生和氧化 甲烷产生和氧化 甲烷通量 甲烷通量
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| GB/T 7714 | 仝川 , 罗敏 , 谭季 . 湿地甲烷代谢对氮输入响应的复杂性及其机制分析 [J]. | 生态学报 , 2024 , (04) . |
| MLA | 仝川 et al. "湿地甲烷代谢对氮输入响应的复杂性及其机制分析" . | 生态学报 04 (2024) . |
| APA | 仝川 , 罗敏 , 谭季 . 湿地甲烷代谢对氮输入响应的复杂性及其机制分析 . | 生态学报 , 2024 , (04) . |
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海平面上升直接改变河口感潮沼泽的水文和盐度特征，是河口感潮沼泽面临的主要环境问题之一。总结了海平面上升对河口感潮沼泽碳动态影响的研究方法和实验平台，分别从海平面上升引发的盐水入侵和水淹增加2个方面综述海平面上升对河口感潮沼泽CH_4和CO_2排放通量、产生速率和土壤有机碳厌氧矿化途径等方面的影响及其机制。盐水入侵显著降低河口感潮淡水沼泽CH_4产生速率和排放通量，导致土壤有机碳厌氧矿化途径从CH_4产生为主向硫酸盐异化还原为主转变，然而盐水入侵对CO_2排放通量的影响具有不确定性。水淹增加对河口感潮沼泽CH_4和CO_2排放通量影响的报道相对较少，已有研究表明CO_2排放通量随着水淹高度增加而降低。最后提出海平面上升对河口感潮沼泽碳动态影响研究应加强的领域，以期为海平面上升对河口感潮沼泽含碳温室气体动态的影响研究提供参考。
Keyword ：
水淹增加 水淹增加 河口感潮沼泽 河口感潮沼泽 海平面上升 海平面上升 盐水入侵 盐水入侵 碳动态 碳动态
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| GB/T 7714 | 仝川 , 罗敏 , 胡敏杰 et al. 海平面上升对河口感潮沼泽湿地CH_4和CO_2产生和排放的影响：机制与复杂性 [J]. | 地球科学进展 , 2024 , 39 (05) : 441-453 . |
| MLA | 仝川 et al. "海平面上升对河口感潮沼泽湿地CH_4和CO_2产生和排放的影响：机制与复杂性" . | 地球科学进展 39 . 05 (2024) : 441-453 . |
| APA | 仝川 , 罗敏 , 胡敏杰 , 王纯 , 刘白贵 , 展鹏飞 . 海平面上升对河口感潮沼泽湿地CH_4和CO_2产生和排放的影响：机制与复杂性 . | 地球科学进展 , 2024 , 39 (05) , 441-453 . |
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Sea-Level Rise (SLR) directly changes the hydrology and salinity of estuarine tidal wetlands and is one of the primary drivers of global change that significantly impacts ecosystem processes. Herein, various methodologies and experimental facilities (marsh organs, weirs, and flow-through mesocosms) for manipulating SLR are systematically reviewed. This study provides a comprehensive summary of the effects and mechanisms associated with SLR regarding the fluxes and production rates of CH4 and CO2, and the pathways and rates of soil organic carbon mineralization from the perspectives of SLR-saltwater intrusion and inundation increase. Saltwater intrusion due to SLR notably decreases CH4 production rates and fluxes. It induces a shift in the pathways of soil organic carbon mineralization, transitioning from CH4 production to microbial SO2-4 reduction in tidal freshwater marshes. The main mechanism reducing saltwater intrusion-induced CH4 flux is the increased presence of the electron acceptor SO2-4, which hinders soil CH4 production. The impact of SLR through saltwater intrusion on CO2 emissions in tidal freshwater marshes exhibits distinct uncertainty. Owing to the inherent challenges in experimentally manipulating SLR in situ, few reports concerning the effects of SLR-related inundation on CH4 and CO2 fluxes and production rates exist. However, some studies have suggested that an increase in inundation height leads to a reduction in CO2 emissions. Additionally, this study consolidates information surrounding electron acceptors and microbial mechanisms associated with SLR that influence the pathways and rates of soil organic carbon mineralization in coastal tidal wetlands. Finally, this study outlines the specific domains that warrant further exploration in future research on the impact of SLR on the production and emission of carbon greenhouse gases in estuarine tidal marshes. © 2024 Science China Press. All rights reserved.
Keyword ：
Carbon dynamics Carbon dynamics Estuarine tidal marsh Estuarine tidal marsh Inundation increase Inundation increase Saltwater intrusion Saltwater intrusion Sea level rise Sea level rise
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| GB/T 7714 | Tong, C. , Luo, M. , Hu, M. et al. Effects of Sea Level Rise on Production and Emission of CH4 and CO2 in Estuarine Tidal Marshes: Mechanism and Complexity; [海平面上升对河口感潮沼泽湿地 CH4和 CO2 产生和排放的影响：机制与复杂性] [J]. | Advances in Earth Science , 2024 , 39 (5) : 441-453 . |
| MLA | Tong, C. et al. "Effects of Sea Level Rise on Production and Emission of CH4 and CO2 in Estuarine Tidal Marshes: Mechanism and Complexity; [海平面上升对河口感潮沼泽湿地 CH4和 CO2 产生和排放的影响：机制与复杂性]" . | Advances in Earth Science 39 . 5 (2024) : 441-453 . |
| APA | Tong, C. , Luo, M. , Hu, M. , Wang, C. , Liu, B. , Zhan, P. . Effects of Sea Level Rise on Production and Emission of CH4 and CO2 in Estuarine Tidal Marshes: Mechanism and Complexity; [海平面上升对河口感潮沼泽湿地 CH4和 CO2 产生和排放的影响：机制与复杂性] . | Advances in Earth Science , 2024 , 39 (5) , 441-453 . |
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Rising sea levels have increased the risk of intense flooding in tidal wetlands, potentially leading to rises in soil iron-bound organic carbon (Fe-OC) contents by inhibiting microbial activity. However, flooding-induced Fe-OC accumulation may be attenuated by root activities of tidal wetland plants, which remains under-investigated in tidal wetlands. Here we established manipulative "marsh organ" filed experiments with soils collected from an oligohaline tidal wetland and introduced the indigenous plant species Phragmites australis (Cav.) Trin. ex Steud. These "marsh organ" mesocosms were then subjected to three flooding water-level treatments over a period of 3.5 years. Overall, root biomass, root porosity, and rhizosphere ferric iron-to-ferrous iron [Fe(III):Fe(II)] ratio increased with flooding levels, indicating that enhanced flooding promotes root oxygen loss of tidal wetland plants. The abundances of Fe-oxidizing bacteria (Gallionella) and Fe-reducing bacteria (Geobacter) increased, whereas the abundance of sulfate-reducing bacteria (dsrA gene) decreased with increased flooding, indicating a diversion of Fe from Fe-sulfur associations towards microbially-mediated Fe redox cycling. The soil organic carbon (SOC) pool did not change with increased flooding; however, the Fe-OC-to-SOC ratio (fFe-OC) increased from 9 to 18%. The fFe-OC was strongly related to soil amorphous Fe(III) concentrations and the activities of soil C-acquiring enzymes, both of which were affected by rhizosphere Fe(III):Fe(II) ratios. Thus, increased root oxygen loss, along with enhanced flooding, facilitated increases in amorphous Fe(III) concentrations and C acquiring enzyme activity. Increased soil amorphous Fe(III) concentrations further promoted Fe-OC accumulation, whereas increased soil C-acquiring enzyme activities reduced the labile organic C pool. Overall, the dominance of the Fe-OC pool increased under enhanced flooding, owing to increased oxygen loss from the roots. Therefore, we outlined that soil C stability will increase in tidal wetland ecosystems that are exposed to future sea-level rise.
Keyword ：
Flooding Flooding Iron-bound organic carbon Iron-bound organic carbon Root oxygen loss Root oxygen loss Sea-level rise Sea-level rise Soil organic carbon Soil organic carbon Tidal wetland Tidal wetland
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| GB/T 7714 | Hu, Dehong , Lan, Wenjing , Luo, Min et al. Increase in iron-bound organic carbon content under simulated sea-level rise: A "marsh organ" field experiment [J]. | SOIL BIOLOGY & BIOCHEMISTRY , 2023 , 187 . |
| MLA | Hu, Dehong et al. "Increase in iron-bound organic carbon content under simulated sea-level rise: A "marsh organ" field experiment" . | SOIL BIOLOGY & BIOCHEMISTRY 187 (2023) . |
| APA | Hu, Dehong , Lan, Wenjing , Luo, Min , Fan, Tianning , Chen, Xin , Tan, Ji et al. Increase in iron-bound organic carbon content under simulated sea-level rise: A "marsh organ" field experiment . | SOIL BIOLOGY & BIOCHEMISTRY , 2023 , 187 . |
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Emissions of methane (CH4), a major greenhouse gas, should be cut by at least 30% by 2030 according to the last Conference of the Parties, CoP26. Aquaculture pond is a major CH4 emitter, yet the microbial mechanisms ruling methanogenesis by degradation of organic matter in sediments remain unclear. In particular, the respective roles of hydrogenotrophic and acetoclastic methanogenesis, and the impact of aquaculture farming practices are unknown. We studied methanogenesis in the surface sediments from a freshwater and an oligohaline pond before, during, and after shrimp farming. Hydrogenotrophic and acetoclastic contributions were distinguished by acetoclastic inhibition with methylfluoride (CH3F), and by C-13-analysis of CO2 and CH4. We also monitored the methanogenic community structure, dissolved organic carbon (DOC) levels, carbon to nitrogen (C/N) ratios, and humification indices derived from Fourier transform infrared spectroscopy. The results reveal that aquaculture farming practices increased methanogenesis rates, and these increases were explained by higher levels of DOC and lower C/N ratios during farming. Of the total methane produced, 51%-78% was by hydrogenotrophic methanogenesis. However, the total methane contribution from acetoclastic methanogenesis increased from approximately 22% before farming to approximately 45% during and after farming, with a decreasing isotope fractionation factor alpha c and an increasing relative abundance of Methanosaeta acetoclastic methanogen. All hu-mification indices decreased during and after farming compared to before farming due to the input of polysaccharide-rich aquafeed. The close relationship between the humification indices and methanogenesis pathways indicates that the changes in sediment substrate quality drove the variation in the methanogenesis pathways. Increases in salinity decreased the methanogenesis rates but did not change the methanogenesis pathways. Overall, our findings reveal that aquaculture farming practices increase methanogenesis rates and favor acetoclastic over hydrogenotrophic methanogenesis, and that adjusting shrimp diets, increasing salinity, and removing residual aquafeed could reduce methanogenesis.
Keyword ：
Acetoclastic methanogenesis Acetoclastic methanogenesis Coastal aquaculture pond Coastal aquaculture pond Hydrogenotrophic methanogenesis Hydrogenotrophic methanogenesis Isotopic fractionation factors Isotopic fractionation factors Methane Methane Methanogenic community structure Methanogenic community structure
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| GB/T 7714 | Tan, Ji , Lichtfouse, Eric , Luo, Min et al. Aquaculture drastically increases methane production by favoring acetoclastic rather than hydrogenotrophic methanogenesis in shrimp pond sediments [J]. | AQUACULTURE , 2023 , 563 . |
| MLA | Tan, Ji et al. "Aquaculture drastically increases methane production by favoring acetoclastic rather than hydrogenotrophic methanogenesis in shrimp pond sediments" . | AQUACULTURE 563 (2023) . |
| APA | Tan, Ji , Lichtfouse, Eric , Luo, Min , Liu, Yuxiu , Tan, Fengfeng , Zhang, Changwei et al. Aquaculture drastically increases methane production by favoring acetoclastic rather than hydrogenotrophic methanogenesis in shrimp pond sediments . | AQUACULTURE , 2023 , 563 . |
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Two mesocosms, with and without plants, were established in the tidal wetlands of the Minjiang Estuary, Southeast China. Each mesocosm contained three elevation treatments: control (CK), CK-20cm, and CK-40cm. The CO2 and CH4 emission fluxes under each elevation treatment in the planted and unplanted mesocosms were investigated. Overall, the results showed that increased flooding did not significantly change the total biomass or stem heights of the plants, but it increased the belowground biomass and decreased the aboveground biomass. In the planted mesocosms, the soil redox potential (ORP) and dissolved organic carbon (DOC) concentration increased with increasing flooding. In the unplanted mesocosms, the DOC concentration also increased with increasing flooding, but the soil ORP did not change. In the planted mesocosms, compared to the CK treatment, CO2 emission flux increased by 43% and 61%, respectively and CH4 emission flux increased by 66% and 84%, respectively for the CK-20cm and CK-40cm treatments. In the unplanted mesocosms, the emission fluxes of CO2 and CH4 did not significantly change with increasing flooding. Within 50 to 100 years of sea level rises in the future, the sustained-flux global warming potential of vegetated tidal wetland will increase, while the soil organic carbon storage will decrease. Conversely, in unvegetated tidal wetlands, the sustained-flux global warming potential will decrease, while the storage of soil organic carbon will not change. © 2023 Chinese Society for Environmental Sciences. All rights reserved.
Keyword ：
CO2 and CH4 eflux CO2 and CH4 eflux increased flooding increased flooding Minjiang Estuary Minjiang Estuary redox potential redox potential sea level rise sea level rise tidal wetland tidal wetland
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| GB/T 7714 | Tan, F.-F. , Luo, M. , Zhang, C.-W. et al. Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils [植物调节湿地 CO2 和 CH4 排放对淹水增强的响应] [J]. | China Environmental Science , 2023 , 43 (1) : 424-435 . |
| MLA | Tan, F.-F. et al. "Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils [植物调节湿地 CO2 和 CH4 排放对淹水增强的响应]" . | China Environmental Science 43 . 1 (2023) : 424-435 . |
| APA | Tan, F.-F. , Luo, M. , Zhang, C.-W. , Chen, X. , Huang, J.-F. . Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils [植物调节湿地 CO2 和 CH4 排放对淹水增强的响应] . | China Environmental Science , 2023 , 43 (1) , 424-435 . |
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In order to scientifically assess the impact of land use/cover changes on carbon cycle of coastal blue carbon wetland ecosystem，it is important to reveal the effect of conversion of estuarine marshes to aquaculture ponds on soil extracellular enzyme activity and greenhouse gases production. Soil samples（0~30cm）from the Phragmites australis marshes，Cyperus malatensis marshes and Spartina alterniflora marshes，and 0~30 cm sediment samples from the shrimp ponds reclaimed from the above marshes were collected in the Min River estuary. The soil/sediment extracellular enzyme activity，and CO2，CH4 production potentials were measured via anaerobic incubation experiment. Compared with the marshes，the average value of activity of 4 extracellular enzymes in the shrimp ponds decreased by 27.3%. The production potentials of carbon greenhouse gases significantly changed after estuarine marshes converting to shrimp ponds. The CO2 production potentials of the P. australis marshes，C. malaccensis marshes，S. altemiflora marshes increased by 5.1%，38.5% and 38.8%，respectively，and the CH4 production potentials reduced by 24.9%，11.1% and 21.1%，respectively，and the organic carbon anaerobic mineralization rates increased by 4.9%，38.6% and 38.4%，respectively. The SOC content was key factor affecting the soil/sediment extracellular enzyme activity. The extracellular enzyme activity and conductivity were main factors controlling organic carbon anaerobic mineralization rate of the marshes soils and shrimp ponds sediments，respectively. The study results show that conversion from marsh to shrimp ponds in the Min River estuary increase organic carbon anaerobic mineralization rate，which may cause more loss of soil organic carbon，and is unfavorable to reach carbon goal of peak and neutrality and to mitigate global climate warming. © 2023 Science Press. All rights reserved.
Keyword ：
CH4 production potential CH4 production potential CO2 production potential CO2 production potential extracellular enzymes extracellular enzymes marshes marshes Min River estuary Min River estuary shrimp ponds shrimp ponds
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| GB/T 7714 | Hu, F. , Cao, Q. , Huang, J. et al. Effects of conversion of estuarine marshes to shrimp ponds on soil extracellular enzymes and CO2 and CH4 production potentials; [河口沼泽湿地转化为养虾塘对土壤胞外酶活性及 CO2和CH4产生潜力的影响] [J]. | Acta Scientiae Circumstantiae , 2023 , 43 (6) : 460-470 . |
| MLA | Hu, F. et al. "Effects of conversion of estuarine marshes to shrimp ponds on soil extracellular enzymes and CO2 and CH4 production potentials; [河口沼泽湿地转化为养虾塘对土壤胞外酶活性及 CO2和CH4产生潜力的影响]" . | Acta Scientiae Circumstantiae 43 . 6 (2023) : 460-470 . |
| APA | Hu, F. , Cao, Q. , Huang, J. , Luo, M. , Guo, P. , Tong, C. . Effects of conversion of estuarine marshes to shrimp ponds on soil extracellular enzymes and CO2 and CH4 production potentials; [河口沼泽湿地转化为养虾塘对土壤胞外酶活性及 CO2和CH4产生潜力的影响] . | Acta Scientiae Circumstantiae , 2023 , 43 (6) , 460-470 . |
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