Phosphorus alleviation of nitrogen‐suppressed methane sink in global grasslands

Grassland ecosystems account for more than 10% of the global CH₄ sink in soils. A 4‐year field experiment found that addition of P alone did not affect CH₄ uptake and experimental addition of N alone significantly suppressed CH₄ uptake, whereas concurrent N and P additions suppressed CH₄ uptake to a lesser degree. A meta‐analysis including 382 data points in global grasslands corroborated these findings. Global extrapolation with an empirical modelling approach estimated that contemporary N addition suppresses CH₄ sink in global grassland by 11.4% and concurrent N and P deposition alleviates this suppression to 5.8%. The P alleviation of N‐suppressed CH₄ sink is primarily attributed to substrate competition, defined as the competition between ammonium and CH₄ for the methane mono‐oxygenase enzyme. The N and P impacts on CH₄ uptake indicate that projected increases in N and P depositions might substantially affect CH₄ uptake and alter the global CH₄ cycle.     

Influence of temperature on the δ13C values and distribution of methanotroph‐related hopanoids in Sphagnum‐dominated peat bogs

Methane emissions from peat bogs are mitigated by methanotrophs, which live in symbiosis with peat moss (e.g. Sphagnum). Here, we investigate the influence of temperature and resultant changes in methane fluxes on Sphagnum and methanotroph‐related biomarkers, evaluating their potential as proxies in ancient bogs. A pulse‐chase experiment using ¹³C‐labelled methane in the field clearly showed label uptake in diploptene, a biomarker for methanotrophs, demonstrating in situ methanotrophic activity in Sphagnum under natural conditions. Peat cores containing live Sphagnum were incubated at 5, 10, 15, 20 and 25°C for two months, causing differences in net methane fluxes. The natural δ¹³C values of diploptene extracted from Sphagnum showed a strong correlation with temperature and methane production. The δ¹³C values ranged from ?34‰ at 5°C to ?41‰ at 25°C. These results are best explained by enhanced expression of the methanotrophic enzymatic isotope effect at higher methane concentrations. Hence, δ¹³C values of diploptene, or its diagenetic products, potentially provide a useful tool to assess methanotrophic activity in past environments. Increased methane fluxes towards Sphagnum did not affect δ¹³C values of bulk Sphagnum and its specific marker, the C₂₃ n‐alkane. The concentration of methanotroph‐specific bacteriohopanepolyols (BHPs), aminobacteriohopanetetrol (aminotetrol, characteristic for type II and to a lesser extent type I methanotrophs) and aminobacteriohopanepentol (aminopentol, a marker for type I methanotrophs) showed a non‐linear response to increased methane fluxes, with relatively high abundances at 25°C compared to those at 20°C or below. Aminotetrol was more abundant than aminopentol, in contrast to similar abundances of aminotetrol and aminopentol in fresh Sphagnum. This probably indicates that type II methanotrophs became prevalent under the experimental conditions relative to type I methanotrophs. Even though BHP concentrations may not directly reflect bacterial activity, they may provide insight into the presence of different types of methanotrophs.     

Where old meets new: An ecosystem study of methanogenesis in a reflooded agricultural peatland

Reflooding formerly drained peatlands has been proposed as a means to reduce losses of organic matter and sequester soil carbon for climate change mitigation, but a renewal of high methane emissions has been reported for these ecosystems, offsetting mitigation potential. Our ability to interpret observed methane fluxes in reflooded peatlands and make predictions about future flux trends is limited due to a lack of detailed studies of methanogenic processes. In this study we investigate methanogenesis in a reflooded agricultural peatland in the Sacramento Delta, California. We use the stable‐and radio‐carbon isotopic signatures of wetland sediment methane, ecosystem‐scale eddy covariance flux observations, and laboratory incubation experiments, to identify which carbon sources and methanogenic production pathways fuel methanogenesis and how these processes are affected by vegetation and seasonality. We found that the old peat contribution to annual methane emissions was large (~30%) compared to intact wetlands, indicating a biogeochemical legacy of drainage. However, fresh carbon and the acetoclastic pathway still accounted for the majority of methanogenesis throughout the year. Although temperature sensitivities for bulk peat methanogenesis were similar between open‐water (Q₁₀ = 2.1) and vegetated (Q₁₀ = 2.3) soils, methane production from both fresh and old carbon sources showed pronounced seasonality in vegetated zones. We conclude that high methane emissions in restored wetlands constitute a biogeochemical trade‐off with contemporary carbon uptake, given that methane efflux is fueled primarily by fresh carbon inputs.     

Methane emissions reduce the radiative cooling effect of a subtropical estuarine mangrove wetland by half

The role of coastal mangrove wetlands in sequestering atmospheric carbon dioxide (CO₂) and mitigating climate change has received increasing attention in recent years. While recent studies have shown that methane (CH₄) emissions can potentially offset the carbon burial rates in low‐salinity coastal wetlands, there is hitherto a paucity of direct and year‐round measurements of ecosystem‐scale CH₄ flux (F_CH4) from mangrove ecosystems. In this study, we examined the temporal variations and biophysical drivers of ecosystem‐scale F_CH4 in a subtropical estuarine mangrove wetland based on 3 years of eddy covariance measurements. Our results showed that daily mangrove F_CH4 reached a peak of over 0.1 g CH₄‐C m^?2 day^?1 during the summertime owing to a combination of high temperature and low salinity, while the wintertime F_CH4 was negligible. In this mangrove, the mean annual CH₄ emission was 11.7 ± 0.4 g CH₄‐C m^–2 year^?1 while the annual net ecosystem CO₂ exchange ranged between ?891 and ?690 g CO₂‐C m^?2 year^?1, indicating a net cooling effect on climate over decadal to centurial timescales. Meanwhile, we showed that mangrove F_CH4 could offset the negative radiative forcing caused by CO₂ uptake by 52% and 24% over a time horizon of 20 and 100 years, respectively, based on the corresponding sustained‐flux global warming potentials. Moreover, we found that 87% and 69% of the total variance of daily F_CH4 could be explained by the random forest machine learning algorithm and traditional linear regression model, respectively, with soil temperature and salinity being the most dominant controls. This study was the first of its kind to characterize ecosystem‐scale F_CH4 in a mangrove wetland with long‐term eddy covariance measurements. Our findings implied that future environmental changes such as climate warming and increasing river discharge might increase CH₄ emissions and hence reduce the net radiative cooling effect of estuarine mangrove forests.     

Enantiopure ethyl 2,3-dibromopropionate: Enantioselective synthesis vs preparative HPLC enantioseparation of racemate on multigram scale

Racemic ethyl 2,3-dibromopropionate, commercially available at low price, is a key intermediate used in the synthesis of several heterocycle fragments, which are present in many biologically active compounds. Surprisingly, the enantiomers are not commercially available and have never been described in the literature. In this work, we undertook two different strategies to obtain these enantiomers, which are enantioselective synthesis and preparative HPLC enantioseparation of commercially available racemate on multigram scale. The first strategy has proved inadequate because racemization occurred during the synthesis (ee ≈ 9-50%). Conversely, the second strategy produced a very good enantioseparation of commercially available racemate (ee > 99.5% for both enantiomers) on multigram scale.     

定点突变提高解淀粉芽孢杆菌JP-21脲酶应用特性

氨基甲酸乙酯(Ethylcarbamate,EC)是一种存在于发酵食品和酒精饮料中的可致癌物,过量摄入可能会影响人体健康。酶法降解是减少发酵食品中氨基甲酸乙酯及其前体尿素含量的有效方法之一。脲酶具有氨基甲酸乙酯水解酶和尿素酶两种活性,因此在减少发酵食品中氨基甲酸乙酯及其前体尿素方面具有良好的应用前景。目前脲酶降解发酵酒精饮料中氨基甲酸乙酯面临的主要问题是脲酶对氨基甲酸乙酯的催化活性及亲和力较低,因而其降解效果不理想。文中成功在大肠杆菌Escherichia coli中表达了来源于解淀粉芽孢杆菌Bacillus amyloliquefaciens JP-21的脲酶,表达水平为尿素酶3 291.74 U/L,氨基甲酸乙酯水解酶227.26 U/L。通过模拟脲酶中催化亚基UreC与氨基甲酸乙酯对接的结构,确定了M326和M374这两个影响酶与底物结合的位点。采用点饱和突变获得了3株氨基甲酸乙酯水解酶活性提高的突变体M374A、M374T和M326V,以EC为底物时的Km分别为101.84mmol/L、129.49 mmol/L和121.67 mmol/L,比野生型分别降低了37.47%–50.82%。突变体可以降解黄酒中97%的尿素,M374T对黄酒中EC的降解效果最好,可将黄酒中EC从513.90μg/L降至393.57μg/L,降解率是野生脲酶的1.97倍。研究结果对今后改造脲酶催化特性和改善其应用特性具有重要意义,可为开发减控发酵食品中的微生物代谢氨(胺)类危害物策略提供参考。     

毛梗豨莶乙酸乙酯部位化学成分及生物活性研究

毛梗豨莶草(Siegesbeckia glabresce)的乙酸乙酯萃取部位具有显著的抑制细胞坏死性凋亡(necroptosis)的活性。为明确毛梗豨莶草的活性成分,该研究采用正相硅胶柱色谱谱(二氯甲烷:甲醇20:1～0:1)、反相ODS柱色谱(30%～100% 甲醇)、Sephadex LH-20柱色谱、重结晶等方法对毛梗豨莶草乙酸乙酯萃取部位进行了化学成分分离和纯化,并根据理化性质和波谱数据进行了结构鉴定。结果表明:从毛梗豨莶乙酸乙酯部位分离并鉴定了9个化合物,分别为3,7-二甲氧基槲皮素(1)、芹菜素(2)、奥卡宁(3)、okanin-4''-O-β-D-6″-trans-p-coumaroylglucoside(4)、1H-Indole-3-carbaldehyde(5)、对羟基苯甲醛(6)、3,5-二甲氧基-4-羟基苯甲醛(7)、3,4-divanillyltetrahydrofuran(8)、buddlenol D(9)。除化合物1和化合物6外,其余7个化合物均为首次从豨莶属植物中分离得到     

施硅对增温稻田CH4和N2O排放的影响

夜间增温幅度大于白天是气候变暖的显著特征。夜间增温影响水稻生产及CH4和N2O排放。硅是作物有益元素,施硅可提高产量,减少稻田CH4排放。增温或施硅单因子对稻田CH4和N2O排放影响已有报道,但二者耦合如何影响水稻生产及稻田CH4和N2O排放,尚不清楚。通过田间模拟试验,研究了夜间增温下施硅对水稻生长、产量及温室气体持续增温/冷却潜势和排放强度的影响。采用铝箔反光膜夜间(19:00-6:00)覆盖水稻冠层进行模拟夜间增温试验。增温设2水平,即常温对照(CK)和夜间增温(NW);施硅量设2水平,即Si0(不施硅)和Si1(钢渣硅肥,200 kgSiO2/ha)。结果表明,施硅可缓解夜间增温对水稻根系活力的抑制作用,降低夜间增温对水稻地上部、地下部干重和产量的抑制作用。夜间增温显著提高CH4累计排放量,而施硅显著降低CH4累计排放量。夜间增温下施硅处理稻田CH4累计排放量在分蘖期、拔节期、抽穗-扬花期和灌浆成熟期比未施硅处理分别低48.12%、49.16%、61.59%和39.13%。夜间增温或施硅均促进稻田N2O排放,夜间增温下施硅在上述生育期以及全生育期的累计排放量依次比对照高78.17%、51.45%、52.01%、26.14%和40.70%。研究认为,施硅可缓解夜间增温对稻田综合增温潜势和排放强度的促进作用。     

典型温带雨养泥炭沼泽湿地地下部二氧化碳和甲烷浓度变化规律及其影响因素

为研究北方泥炭沼泽湿地二氧化碳（CO₂）和甲烷（CH₄）浓度随深度的变化规律及其影响因素,选取欧洲北部典型雨养泥炭地贝尔山湿地（BBM）和舒特兹山湿地（SBM）两个采样点,通过原位采集泥炭剖面温室气体、孔隙水以及土壤样品,结合傅里叶变换红外光谱（FTIR）技术、碳氮同位素技术,探讨泥炭土壤的分解程度及温室气体浓度变化的关系。研究结果表明：（1）BBM采样点地下部的CO₂浓度变化规律总体呈现随深度波动减少趋势,值多在3000 μmol/L附近波动,最大值为4210.74 μmol/L（120 cm）,SBM采样点的CO₂浓度随深度先增后减,60 cm以上在1800 μmol/L附近波动,60 cm以下在3000 μmol/L附近波动,最大值为4191.94 μmol/L（90 cm）;BBM和SBM地下部CH₄浓度都随深度增大,并且在60cm以下浓度增加较快,BBM最大值为735.90 μmol/L（260 cm）,SBM最大值为543.51 μmol/L（170 cm）。（2）BBM和SBM的δ¹³C_CH4的值均较小,表明大部分的¹²CH₄仍被储存在泥炭土壤中,而两个采样点的δ¹³C_CO2和分馏系数α_c均随深度增加,表明泥炭土中产甲烷方式为浅层以乙酸产甲烷为主,深层以H₂还原CO₂为主。（3）C/N、碳氮同位素比值、FTIR均显示SBM和BBM的有机质分解程度较低,因为两个采样点的低可溶性有机碳浓度和低pH值不利于分解,表明该地储存着大量有机碳。通过探讨北温带典型泥炭地温室气体的浓度变化规律及其影响因素,结果可为全球泥炭湿地碳排放提供理论支撑。     

水位下降对若尔盖泥炭地垂直剖面土壤甲烷产生及厌氧氧化潜势的影响

泥炭地是主要的甲烷（CH₄）排放源,甲烷循环过程对水位变化响应敏感。研究选取两块具有水位差异的泥炭地土壤,通过厌氧培养实验探究水位变化对泥炭地甲烷产生和甲烷厌氧氧化（Methane Anaerobic Oxidation,AOM）潜势的影响,并分析影响其潜势大小的生物地球化学因子。结果显示,高水位泥炭地（0 cm） CH₄产生累积量为（0.89±0.01）μg/g,要显著高于低水位（-30 cm：（0.70±0.03）μg/g）泥炭地甲烷产生量,但低水位AOM累积量要显著高于高水位泥炭地（0 cm：（2829.93±35.99）μg/g）,低水位泥炭地AOM量为（3588.06±24.78）μg/g。通过相关性分析发现甲烷产生潜势与含水量和DOC具有显著相关性,AOM潜势与含水量、pH、DOC具有显著相关性,含水量和DOC是影响若尔盖泥炭地甲烷产生及AOM潜势大小的重要因子。此外,发现高水位泥炭地甲烷产生潜势对温度升高的响应较为明显,特别是表层土壤（0-20 cm）。本研究明确了水位变化对若尔盖泥炭地甲烷产生及AOM潜势的影响特征,估算了全国泥炭地甲烷产生及AOM潜势的大小,以期为减缓全球气候变暖提供一定的理论支撑。