The effects of climatic warming on phyllosphere microbial communities remain *** this study,the effects of long-term(>10 years)experimental warming on phyllosphere epiphytic bacterial and fungal communities of Care...
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The effects of climatic warming on phyllosphere microbial communities remain *** this study,the effects of long-term(>10 years)experimental warming on phyllosphere epiphytic bacterial and fungal communities of Carex alrofusca,Kobresia pygmaea,Potentilla bifurca and Stipa capillacea were examined in the northern ***,warming increased bacterial α-diversity,but reduced fungalα-diversity across the four host *** altered the bacterial and fungal community compositions mainly by increasing Actinobacteria,Firmicutes and pathotrophsaprotroph fungi,and reducing Basidiomycota and symbiotroph fungi across the four host *** increased the relative effect of the‘drift&others’process in the bacterial community,but reduced the relative effect of the‘dispersal limitation’process in the bacterial community and the relative effect of the‘homogeneous selection’process in the fungal community across the four host *** overall warming effects on the bacterial and fungal communities may be due to overall warming effects on temperature,leaf morphology structure and physicochemical properties,ecological processes of community assembly and topological parameters of species co-occurrence networks of bacteria and *** altered the bacterial species co-occurrence network mainly by increasing the vertex,clustering coefficient and heterogeneity,while reducing the average path length and network diameter across host *** altered the fungal species co-occurrence network mainly by increasing the network diameter and reducing the vertex across host *** effects on bacterial and fungal communities varied among host plants,which may be due to the diverse responses to warming of plant height,leaf malondialdehyde,ecological processes of community assembly and topological parameters of species co-occurrence ***,warming can alter phyllosphere epiphytic bacterial and fungal communities of alpine *** changes va
Coastal wetlands possess significant carbon sequestration rates and storage capabilities. Clarifying the methods for evaluating coastal wetland carbon sinks and identifying existing issues are essential for accurately...
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Coastal wetlands possess significant carbon sequestration rates and storage capabilities. Clarifying the methods for evaluating coastal wetland carbon sinks and identifying existing issues are essential for accurately assessing coastal blue carbon,understanding the carbon balance between terrestrial-coastal-marine ecosystems, and advancing the “dual carbon” goal. This paper reviews the detailed processes of coastal wetland carbon cycling and summarizes the challenges and difficulties in defining, delineating, and identifying the boundaries of coastal wetlands. We generalize current carbon sink evaluation methods across different dimensions by constructing a “black box theory”. In addition, based on the “white box theory”, we propose a net ecosystem carbon balance model for carbon sink assessment, providing a theoretical foundation for enhancing the understanding of coastal wetland carbon sinks and optimizing the evaluation system for coastal blue carbon functionality. We also systematically summarize the current status of carbon sources and sinks in China's coastal wetlands and propose a technical framework for emission reduction and carbon sequestration enhancement through integrated management of coastal zones and wetlands and regulation of key wetland ecological processes, with the aim of increasing the potential of blue carbon in mitigating climate change. Finally, based on the current research gaps, we outline future research priorities for coastal wetland blue carbon.
Tibetan Plateau,as one of the most carbon intensive regions in China,is crucial in the carbon cycle,and accurately estimating its vegetation carbon density(C_(VEG))is essential for assessing regional and national carb...
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Tibetan Plateau,as one of the most carbon intensive regions in China,is crucial in the carbon cycle,and accurately estimating its vegetation carbon density(C_(VEG))is essential for assessing regional and national carbon ***,the spatial distribution of regional C_(VEG) is not available remains highly uncertain due to lack of systematic research,especially for different ***,we investigated the spatial distribution patterns and driving factors of C_(VEG) among different plant organs(leaf,branch,trunk and root)by systematically field grid-sampling 2040 field-plots of plant communities over the Tibetan Plateau from 2019 to *** results showed that the carbon content of plant organs ranged from 255.53 to 515.58 g kg^(-1),with the highest in branches and the lowest in *** the different plant functional groups,the highest C_(VEG) was found in evergreen coniferous forests,and the lowest in desert grasslands,with an average C_(VEG) of 1603.98 g m^(-2).C_(VEG) increased spatially from northwest to southeast over the Tibetan Plateau,with MAP being the dominant ***,the total vegetation carbon stock on the Tibetan Plateau was estimated to be 1965.62 Tg for all vegetation *** on the comprehensive field survey dataset,the Random Forest model effectively predicted and mapped the spatial distribution of C_(VEG)(including aboveground,belowground,and the total biomass carbon density)over the Tibetan Plateau with notable accuracy(validation R2 values were 71%,56%,and 64%for C_(AGB),C_(BGB),and C_(VEG),respectively)at a spatial resolution of 1 km×1 *** findings can help improve the accuracy of regional carbon stock estimations and provide parameters for carbon cycle model optimization and remote sensing calibration in the future.
The land application of livestock manure has been widely acknowledged as a beneficial approach for nutrient recycling and environmental ***,the impact of residual antibiotics,a common contaminant of manure,on the degr...
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The land application of livestock manure has been widely acknowledged as a beneficial approach for nutrient recycling and environmental ***,the impact of residual antibiotics,a common contaminant of manure,on the degradation of organic compounds and nutrient release in Eutric Regosol is not well ***,we studied,how oxytetracycline(OTC)and ciprofloxacin(CIP)affect the decomposition,microbial community structure,extracellular enzyme activities and nutrient release from cattle and pig manure using litterbag incubation *** showed that OTC and CIP greatly inhibited livestock manure decomposition,causing a decreased rate of carbon(28%-87%),nitrogen(15%-44%)and phosphorus(26%-43%)*** relative abundance of gramnegative(G-)bacteria was reduced by 4.0%-13%while fungi increased by 7.0%-71%during a 28-day incubation ***-occurrence network analysis showed that antibiotic exposure disrupted microbial interactions,particularly among G-bacteria,G+bacteria,and *** changes in microbial community structure and function resulted in decreased activity of urease,β-1,4-N-acetyl-glucosaminidase,alkaline protease,chitinase,and catalase,causing reduced decomposition and nutrient release in cattle and pig *** findings advance our understanding of decomposition and nutrient recycling from manure-contaminated antibiotics,which will help facilitate sustainable agricultural production and soil carbon sequestration.
The primary mechanism driving plant species loss after nitrogen (N) addition has been often hypothesized to be asymmetric competition for light, resulting from increased aboveground biomass. However, it is largely unk...
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Rapid economic growth is generally accompanied by urban-rural inequality, with much attention focused on its appearance like urban-rural income gap, while the underlying causes remain underexplored. Water is an indisp...
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Nitrous oxide (N2O) emissions from soil are an important contributor to global warming, particularly from intensively fertilized croplands. Biochar is commonly applied to reduce N2O emissions and raise soil fertility ...
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Nitrous oxide (N2O) emissions from soil are an important contributor to global warming, particularly from intensively fertilized croplands. Biochar is commonly applied to reduce N2O emissions and raise soil fertility by regulating soil structure, microbial processes, and crop nitrogen use efficiency. However, the effects of biochar on N2O emissions from fertilized croplands depend on its sources and production conditions, including feedstocks, pyrolysis temperatures, properties and application rates. To generalize findings from individual studies, we synthesized 550 observations that simultaneously measured N2O emissions, nitrification enzyme activity (NEA), denitrification enzyme activity (DEA), and relevant functional genes (AOA, AOB, narG, nirK, nirS, and nosZ) to assess their responses to biochar production conditions, properties and application rates across cropland ecosystems. Wheat straw biochar increased the abundances of all functional genes related to N2O emissions and DEA, while pyrolysis temperatures exceeding 450 ℃ decreased DEA. Low-temperature pyrolysis biochar was particularly effective in reducing N2O emissions. The abundance of denitrifiers and DEA-related genes increased with the pH, ash content, and cation exchange capacity (CEC) of biochar. As biochar application rates increased, N2O emissions were reduced, largely due to an increase in nosZ gene abundance and soil pH. A common biochar application rate of 20 t ha−1 decreased N2O emissions by 19%, primarily through reduced denitrification, while 50 t ha−1 reduced N2O emissions by 48%. Biochar preparation conditions, and property changes had no significant effects on N2O emissions at application rates below 20 t ha−1. When application rates exceeded 20 t ha−1, biochar pyrolysis temperature and properties influenced N2O emissions, indicating a threshold application rate, beyond which biochar affects N2O emissions. Biochar regulates the soil N cycle and N2O emissions primarily through denitrificatio
Soil carbon(C)reservoirs,encompassing both organic(SOC)and inorganic(SIC)forms,represent the largest terrestrial carbon sink,surpassing the carbon stored in vegetation and the atmosphere combined[1].In light of the pr...
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Soil carbon(C)reservoirs,encompassing both organic(SOC)and inorganic(SIC)forms,represent the largest terrestrial carbon sink,surpassing the carbon stored in vegetation and the atmosphere combined[1].In light of the pressing concerns surrounding global warming and its cascading effects on climate dynamics,the scientific community has devoted significant attention to delineating the quantity,typology,and spatial distribution of soil C[2],[3].While research efforts have predominantly concentrated on SOC,given its substantial contribution to soil C content compared with SIC,it is important to recognize that SIC also plays a significant role,particularly in deeper soil horizons[4].Notably,in arid and semi-arid regions,which encompass approximately 41%of the Earth’s terrestrial surface,SIC is the dominant form of soil C[5],[6],with SIC pools in both top and deep soils exceeding SOC by factors ranging from 2 to 10[7].Consequently,there is a critical imperative to accurately quantify both SOC and SIC stocks across various soil depths in these water-limited regions[7].
Carbonyl sulfide (COS) is an effective tracer for estimating Gross Primary Productivity (GPP) in the carbon *** the largest contribution to the atmosphere,anthropogenic COS emissions must be accurately *** this st...
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Carbonyl sulfide (COS) is an effective tracer for estimating Gross Primary Productivity (GPP) in the carbon *** the largest contribution to the atmosphere,anthropogenic COS emissions must be accurately *** this study,an anthropogenic COS emission inventory from 2015 to 2021 was constructed by applying the bottom-up approach based on activity data from emission ***’s anthropogenic COS emissions increased from approximately 171 to 198 Gg S yr-1from 2015–2021,differing from the trends of other *** an initial decline in COS emissions across sectors during the early stage of the COVID-19 pandemic,a rapid rebound in emissions occurred following the resumption of economic *** 2021,industrial sources,coal combustion,agriculture and vehicle exhaust accounted for 76.8%,12.3%,10.5%and 0.4%of total COS emissions,*** aluminum industry was the primary COS emitter among industrial sources,contributing40.7%of total ***,Shanxi,and Zhejiang were the top three provinces in terms of anthropogenic COS emissions,reaching 39,21 and 17 Gg S yr-1,***-level regions (hereafter province) with high COS emissions are observed mainly in the eastern and coastal regions of China,which,together with the wind direction,helps explain the pattern of high COS concentrations in the Western Pacific Ocean in *** Green Contribution Coefficient of COS (GCCCOS) was used to assess the relationship between GDP and COS emissions,highlighting the disparity between GDP and COS contributions to green *** part of this analysis,relevant recommendations are proposed to address this *** COS emission inventory in our study can be used as input for the Sulfur Transport and Deposition Model (STEM),reducing uncertainties in the atmospheric COS source?sink budget and promoting understanding of the atmosphere sulfur cycle.
Plant photosynthesis significantly regulates atmospheric CO₂ but is often limited by nitrogen (N) availability. While N deposition could alleviate this limitation and enhance gross ecosystem productivity (GEP), its lo...
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