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学者姓名：罗敏
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Abstract ：
Microbial carbon use efficiency (CUE) typically promotes soil organic carbon (SOC) storage in terrestrial ecosystems. However, this relationship remains poorly understood in coastal wetlands, where tidal flooding creates unique environmental conditions, facilitates lateral transfer and SOC loss, and mediates organic matter exchange between terrestrial and marine systems. Here we examined the CUE-SOC relationship across a tidal flooding gradient (4-25 % frequency) in a subtropical coastal wetland. Along this gradient, SOC decreased by 65 % while microbial CUE increased from 0.24 to 0.32. This inverse relationship coincided with marked compositional shifts: plant debris declined from 57 % to 18 %, while microbial necromass increased from 21 % to 35 %. The enhanced CUE was accompanied by increased turnover times alongside decreased metabolic quotient (qCO2), C-acquiring enzyme activities, soil basal respiration, and microbial biomass carbon (MBC). This enhanced efficiency stemmed from substrate-microbe interactions rather than environmental stresses, as communities transitioned from oligotrophic taxa (alpha-proteobacteria, Basidiomycota) specializing in recalcitrant terrestrial substrates to copiotrophic microorganisms (gamma-proteobacteria, Bacteroidota, Ascomycota) efficiently metabolizing labile marine compounds. Contrary to terrestrial patterns, enhanced CUE did not promote SOC storage due to three key mechanisms: (i) enhanced CUE from marine substrates could not compensate for declining plant debris accumulation; (ii) reduced microbial biomass limited necromass formation despite higher CUE; and (iii) metabolic benefits from high CUE (reduced enzyme activities and respiration rates) could not offset the substantial decrease in SOC inputs. Our findings reveal distinct CUE-SOC relationships in coastal wetlands compared to terrestrial ecosystems, highlighting the importance of considering both terrestrial and marine processes in understanding carbon cycling in these transitional environments.
Keyword ：
Carbon use efficiency Carbon use efficiency Coastal wetland Coastal wetland Microbial community composition Microbial community composition Soil organic carbon Soil organic carbon Substrate quality Substrate quality Tidal flooding gradient Tidal flooding gradient
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| GB/T 7714 | Tan, Ji , Huang, Jiafang , Quan, Wenhui et al. Divergence of microbial carbon use efficiency and soil organic carbon along a tidal flooding gradient in a subtropical coastal wetland [J]. | WATER RESEARCH , 2025 , 280 . |
| MLA | Tan, Ji et al. "Divergence of microbial carbon use efficiency and soil organic carbon along a tidal flooding gradient in a subtropical coastal wetland" . | WATER RESEARCH 280 (2025) . |
| APA | Tan, Ji , Huang, Jiafang , Quan, Wenhui , Su, Lifei , Liu, Yi , Cai, Yuanbin et al. Divergence of microbial carbon use efficiency and soil organic carbon along a tidal flooding gradient in a subtropical coastal wetland . | WATER RESEARCH , 2025 , 280 . |
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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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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 ：
Biomass Biomass Carbon dioxide Carbon dioxide Floods Floods Global warming Global warming Organic carbon Organic carbon Redox reactions Redox reactions Sea level Sea level Soils Soils Wetlands Wetlands
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| GB/T 7714 | Tan, Feng-Feng , Luo, Min , Zhang, Chang-Wei et al. Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils [J]. | China Environmental Science , 2023 , 43 (1) : 424-435 . |
| MLA | Tan, Feng-Feng et al. "Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils" . | China Environmental Science 43 . 1 (2023) : 424-435 . |
| APA | Tan, Feng-Feng , Luo, Min , Zhang, Chang-Wei , Chen, Xin , Huang, Jia-Fang . Plants moderate the effects of emission fluxes of CO2 and CH4 on increased flooding in wetland soils . | China Environmental Science , 2023 , 43 (1) , 424-435 . |
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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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Dissimilatory iron reduction (DIR) coupled with carbon cycling is increasingly being recognized as an influential process in freshwater wetland soils and sediments. The role of DIR in organic matter (OM) mineralization, however, is still largely unknown in lake sediment environments. In this study, we clarified rates and pathways of OM mineralization in two shallow lakes with seasonal hydrological connectivity and different eutrophic situations. We found that in comparison with the domination of DIR (55%) for OM mineralization in Lake Xiaoxingkai, the contribution of methanogenesis was much higher (68%) in its connected lake (Lake Xingkai). The differences in rates and pathways of sediment OM mineralization between the two lakes were attributed to higher concentrations of carbonate associated iron oxides (Fecarb) in Lake Xiaoxingkai compared to Lake Xingkai (P = 0.002), due to better deposition mixing, more contributions of terrigenous detrital materials, and higher OM content in Lake Xiaoxingkai. Results of structural equation modeling showed that Fecarb and total iron content (TFe) regulated 25% of DIR in Lake Xiaoxingkai and 76% in Lake Xingkai, accompanied by a negative effect of TFe on methanogenesis in Lake Xingkai. The relative abundance and diversity of Fe-reducing bacteria were significantly different between the two lakes, and showed a weak effect on sediment OM mineralization. Our findings emphasize the role of iron minerals and geochemical characterizations in regulating rates and pathways of OM mineralization, and deepen the understanding of carbon cycling in lake sediments. © 2022
Keyword ：
Carbon cycling Carbon cycling Dissimilatory iron reduction Dissimilatory iron reduction Iron oxides Iron oxides Methane production Methane production Organic matter mineralization Organic matter mineralization
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| GB/T 7714 | Yuan, Y. , Ding, C. , Wu, H. et al. Dissimilatory iron reduction contributes to anaerobic mineralization of sediment in a shallow transboundary lake [J]. | Fundamental Research , 2023 , 3 (6) : 844-851 . |
| MLA | Yuan, Y. et al. "Dissimilatory iron reduction contributes to anaerobic mineralization of sediment in a shallow transboundary lake" . | Fundamental Research 3 . 6 (2023) : 844-851 . |
| APA | Yuan, Y. , Ding, C. , Wu, H. , Tian, X. , Luo, M. , Chang, W. et al. Dissimilatory iron reduction contributes to anaerobic mineralization of sediment in a shallow transboundary lake . | Fundamental Research , 2023 , 3 (6) , 844-851 . |
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Tidal wetland plants can maintain high primary productivity under salinization, even with low phosphorus (P) availability. However, little is known about how they adapt to salinization-induced ecosystem P limitation over time. We established mesocosms using tidal freshwater wetland soils and the salt-tolerant plant Cyperus malaccensis and subjected them to short-term (6 months) and long-term (3.5 years) salinization. Overall, short-term salinization did not change plant or microbial biomass nitrogen/P ratios, whereas long-term salinization increased both, indicating that short-term salinization did not alter ecosystem P limitation, but long-term salinization exacerbated it. Concurrently, short-term salinization reduced the moderately labile inorganic P (Pi) pool, whereas long-term salinization also reduced the hydrolyzable organic P (Po) and primary mineral P pools. During both short- and long-term salinization, moderately labile Pi mobilization exhibited a negative correlation with Fe sulfide concentration and a positive correlation with Fe(III) concentrations. These results suggested that both short- and long-term salinization obtained P through abiotic P-acquisition strategies. Mobilization of the primary mineral P pool and hydrolyzable Po pools was negatively linked to root arbuscular mycorrhizal fungi (AMF) biomass and soil alkaline phosphomonoesterase (ALP) activity, respectively. This indicated that long-term salinization acquired P via biotic P-acquisition strategies. Specifically, soil microorganisms increased fungi predominance and thereby increased ALP activity to convert hydrolyzable Po, while tidal wetland plants enhanced root AMF associations to release carboxylate to transform primary mineral P. Overall, our results highlight that abiotic P-acquisition strategies could offset the ecosystem P limitation during short-term salinization, whereas biotic P-acquisition strategies play a more important role in soil P transformation under longterm salinization. Through biotic P-acquisition, tidal wetland ecosystems can maintain high plant primary productivity through biotic P-acquisition even under P-limited conditions, exhibiting increased resilience to sealevel rise.
Keyword ：
Alkaline phosphomonoesterase Alkaline phosphomonoesterase Arbuscular mycorrhizal fungi Arbuscular mycorrhizal fungi Phosphorus limitation Phosphorus limitation Salinization Salinization Soil phosphorus fractions Soil phosphorus fractions Tidal wetland soils Tidal wetland soils
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| GB/T 7714 | Fan, Tianning , Luo, Min , Tan, Ji et al. Incorporating biotic phosphorus-acquisition strategies into soil phosphorus transformation under long-term salinization in a tidal wetland [J]. | CATENA , 2023 , 231 . |
| MLA | Fan, Tianning et al. "Incorporating biotic phosphorus-acquisition strategies into soil phosphorus transformation under long-term salinization in a tidal wetland" . | CATENA 231 (2023) . |
| APA | Fan, Tianning , Luo, Min , Tan, Ji , Hu, Dehong , Chen, Xin , Huang, Jiafang et al. Incorporating biotic phosphorus-acquisition strategies into soil phosphorus transformation under long-term salinization in a tidal wetland . | CATENA , 2023 , 231 . |
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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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Although salinization is widely known to affect cycling of soil carbon (C) in tidal freshwater wetlands, the role of the presence or absence of plants in mediating the responses of soil organic carbon (SOC) mineralization to salinization is poorly understood. In this study, we translocated soils collected from a tidal freshwater wetland to sites with varying salinities along a subtropical estuarine gradient and established unplanted and planted (with the salt-tolerant plant Cyperus malaccensis Lam.) mesocosms at each site. We simultaneously investigated cumulative soil CO2 emissions, C-acquiring enzyme activities, availability of labile organic C (LOC), and structures of bacterial and fungal communities. Overall, in the planted mesocosm, the soil LOC content and the activities of beta-1,4-glucosidase, cellobiohydrolase, phenol oxidase, and peroxidase increased with salinization. However, in the unplanted mesocosm, soil LOC content decreased with increasing salinity, whereas all the C-acquiring enzyme activities did not change. In addition, salinization favored the dominance of bacterial and fungal copiotrophs (e.g., gamma-Proteobacteria, Bacteroidetes, Firmicutes, and Ascomycota) in the planted mesocosms. Contrarily, in the unplanted mesocosms salinization favored bacterial and fungal oligotrophs (e.g., alpha-Proteobacteria, Chloroflexi, Acidobacteria, and Basidiomycota). In both planted and unplanted mesocosms, cumulative soil CO2 emissions were affected by soil LOC content, activities of C-acquiring enzymes, and microbial C-use trophic strategies. Overall, cumulative soil CO(2 )emissions increased by 35% with increasing salinity in the planted mesocosm but decreased by 37% as salinity increased in the unplanted mesocosm. Our results demonstrate that the presence or absence of salt-tolerant plants can moderate the effect of salinity on SOC mineralization in tidal wetland soils. Future C prediction models should embed both planted and unplanted modules to accurately simulate cycling of soil C in tidal wetlands under sea level rise.
Keyword ：
Bacterial and fungal community structure Bacterial and fungal community structure Carbon-acquiring enzyme activity Carbon-acquiring enzyme activity Salinization Salinization Salt-tolerant plant Salt-tolerant plant Soil organic carbon mineralization Soil organic carbon mineralization Tidal wetland Tidal wetland
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| GB/T 7714 | Chen, Xin , Luo, Min , Tan, Ji et al. Salt-tolerant plant moderates the effect of salinity on soil organic carbon mineralization in a subtropical tidal wetland [J]. | SCIENCE OF THE TOTAL ENVIRONMENT , 2022 , 837 . |
| MLA | Chen, Xin et al. "Salt-tolerant plant moderates the effect of salinity on soil organic carbon mineralization in a subtropical tidal wetland" . | SCIENCE OF THE TOTAL ENVIRONMENT 837 (2022) . |
| APA | Chen, Xin , Luo, Min , Tan, Ji , Zhang, Changwei , Liu, Yuxiu , Huang, Jiafang et al. Salt-tolerant plant moderates the effect of salinity on soil organic carbon mineralization in a subtropical tidal wetland . | SCIENCE OF THE TOTAL ENVIRONMENT , 2022 , 837 . |
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Flooding is one of the key environmental factors affecting the carbon sequestration potential of estuarine tidal flat wetlands. In order to reveal the effect of flooding on soil carbon (C) sinks in estuarine tidal wetlands, we investigated and analyzed the soil organic carbon (SOC) storage, the contents of active SOC components, and SOC stability indicators across a tidal flat in the Jiulong River estuary in southeast China. The results showed that the SOC storage gradually decreased by 54% with the increase in flooding frequency. The change pattern of microbial biomass carbon (MBC), dissolved organic carbon (DOC), and liable organic carbon (LOC) followed the change pattern of the SOC storage. With the increase in flooding frequency, DOC/SOC and LOC/SOC increased by 80% and 26%, respectively, whereas MBC/SOC decreased by 29%. As flooding frequency increased, particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) contents decreased by 81% and 35%, respectively. The decreases in POC contents were correlated with the increases in soil pH, whereas the decreases in MAOC contents were associated with the decline in clay contents. Soil carbon stability index (CSI) increased by 246% with increasing flooding frequency. These combined results indicated that SOC storage decreased, but SOC stability increased, with the increased flooding frequency. Mineral-bound organic carbon was the main protection mechanism for the SOC stability, which was of great significance to the soil C sink of the estuarine tidal wetlands. © 2022, Science Press. All right reserved.
Keyword ：
Estuaries Estuaries Floods Floods Minerals Minerals Organic carbon Organic carbon Particles (particulate matter) Particles (particulate matter) Soils Soils Stability Stability Tides Tides Wetlands Wetlands
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| GB/T 7714 | Huang, Xiao-Qing , Tong, Chuan , Luo, Min et al. Soil Organic Carbon Storage, Active Component Contents, and Stability Along a Flooding Gradient in the Tidal Wetland of the Jiulong River Estuary [J]. | Environmental Science , 2022 , 43 (4) : 2226-2236 . |
| MLA | Huang, Xiao-Qing et al. "Soil Organic Carbon Storage, Active Component Contents, and Stability Along a Flooding Gradient in the Tidal Wetland of the Jiulong River Estuary" . | Environmental Science 43 . 4 (2022) : 2226-2236 . |
| APA | Huang, Xiao-Qing , Tong, Chuan , Luo, Min , Yang, Yang , Tan, Feng-Feng , Pan, Zhe-Yan et al. Soil Organic Carbon Storage, Active Component Contents, and Stability Along a Flooding Gradient in the Tidal Wetland of the Jiulong River Estuary . | Environmental Science , 2022 , 43 (4) , 2226-2236 . |
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