新疆阿勒泰地区近440年来大气δ13C变化

化石燃料的大量使用和森林的过度砍伐,引起大气中CO₂浓度的大幅度增加,同时由于Suess效应,大气CO₂中的δ¹³C在不断地下降。植物中δ¹³C的变化是大气CO₂浓度和同位素比值变化的敏感指示器。文中利用树木年轮δ¹³C序列和植物碳同位素分馏模型,尝试恢复了新疆阿勒泰地区近440年来大气δ¹³C的变化。结果表明,1850年之前,从树木年轮δ¹³C序列恢复的大气δ¹³C相对恒定在-6.60‰(R²=0.052),而1850年之后,该大气δ¹³C明显降低(R²=0.65),平均约为-7.04‰,平均年降低0.0084‰。这一结果高于从冰芯气泡所恢复的大气δ¹³C,1850年～1981年冰芯大气δ¹³C平均年降低约0.00657‰这可能与从树木年轮δ¹³C序列恢复的大气δ¹³C有更高的分辨率及树木生长点大气δ¹³C不同于全球大气δ¹³C值有关。     

典型滨岸草地生态系统碳稳定同位素组成及分布特征

通过测定上海市青浦区东风港百慕大、白花三叶草、高羊茅和白茅等4种典型滨岸草本植物各组织以及不同垂直深度土壤有机质δ¹³C值,对滨岸草地生态系统的植物-土壤碳稳定同位素特征进行了分析.结果表明: 白花三叶草、高羊茅属于C3植物,百慕大、白茅属于C4植物,其茎叶、凋落物和根系各组织间δ¹³C值无显著差异.C3和C4植物样带表层土壤有机质δ¹³C值随着土壤深度递增而呈现截然不同的变化特征,这与样带本底δ¹³C值以及碳稳定同位素分馏效应有关,同时还受植物根系分布深度的影响.植物输入是土壤有机碳(SOC)的最主要来源,植物有机体δ¹³C组成对土壤有机质δ¹³C值有直接影响,植物各组分δ¹³C值与土壤有机质δ¹³C值均存在极显著相关.4种草本植物样带SOC含量与δ¹³C值均呈极显著相关,其中,C3植物样带SOC含量与δ¹³C值呈线性负相关,C4植物样带SOC含量与δ¹³C值呈线性正相关.     

聚四氟乙烯塑料管研磨法对测定C4植物碳同位素比值的影响

聚四氟乙烯(PTFE)塑料管研磨法是测定植物碳同位素比率(δ¹³C)值常用的前处理方法。该方法处理样品高效快捷,但对植物δ¹³C可能存在污染。本研究利用人工气候室开展双因素交互试验,包括空气相对湿度(50%和80%)和空气δ¹³C(¹³C富集和贫化的空气)两个因素,对比了PTFE塑料管研磨法和不锈钢管研磨法处理C4植物糙隐子草δ¹³C的结果。结果表明: 在相同湿度条件下,不同空气δ¹³C处理的植物¹³C分馏值(Δ¹³C,矫正了光合作用底物的δ¹³C差异)原本可以视为重复,但由于PTFE塑料颗粒的混入,相同湿度不同¹³C丰度空气培养下植物叶片Δ¹³C平均差值为4.8‰。该污染效应导致单个叶片δ¹³C测定的误差高达8‰。考虑到C4植物的Δ¹³C较低(通常为1‰~8‰),这种污染效应已经超出了可以接受的误差范围。通过建立类似Keeling曲线的二元混合模型对误差进行了有效消除,并准确估算了植物样品和污染物的δ¹³C。说明广泛采用的PTFE管研磨方法对研究C4植物Δ¹³C并不适用,将导致较大的误差。对精度要求较高的研究内容建议使用不锈钢瓶进行研磨。     

长白山阔叶红松林演替序列植物-凋落物-土壤碳同位素特征

稳定碳同位素组成能精确指示生态系统碳循环过程,可以为深入研究森林演替进程对碳循环过程和固碳潜力的影响提供关键信息.利用稳定碳同位素技术对长白山阔叶红松林演替序列3种林分——中龄杨桦次生林、成熟杨桦次生林、阔叶红松林的叶片、树干、根系、凋落物和土壤δ¹³C值及碳、氮元素含量进行测定.结果表明: 各演替序列优势树种叶片δ¹³C从冠上到冠下均呈降低趋势;树干δ¹³C表现为树皮小于木质部;根系δ¹³C表现为细根小于粗根.阔叶红松林未分解凋落物δ¹³C小于半分解及全分解凋落物,次生林相反;土壤δ¹³C沿深度逐渐增加.总体上,δ¹³C值叶片<凋落物<根系<树干<土壤,说明植物各器官之间有明显的碳同位素分馏效应,且相同器官不同部位之间也存在差异;植物δ¹³C沿演替方向先减小后增加,土壤δ¹³C沿演替方向不断增加,且变化规律可以通过氮元素含量与碳同位素分馏效应的关系解释,说明长白山阔叶红松林演替过程优势树种和碳周转速率的变化影响了碳同位素分馏.     

新疆阿勒泰地区近440年来大气δ^13C变化

化石燃料的大量使用和森林的过度砍伐,引起大气中CO₂浓度的大幅度增加,同时由于Suess效应,大气CO₂中的δ¹³C在不断地下降．植物中δ¹³C的变化是大气CO₂浓度和同位素比值变化的敏感指示器．文中利用树木年轮δ¹³C序列和植物碳同位素分馏模型,尝试恢复了新疆阿勒泰地区近440年来大气δ¹³C的变化．结果表明,1850年之前,从树木年轮δ¹³C序列恢复的大气δ¹³C相对恒定在-6．60％0(R²=0．052),而1850年之后,该大气δ¹³C明显降低(R²=0．65)。平均约为-7．04‰,平均年降低0．0084‰．这一结果高于从冰芯气泡所恢复的大气δ¹³C,1850年～1981年冰芯大气δ¹³C平均年降低约0．0065‰．这可能与从树木年轮δ¹³C序列恢复的大气δ¹³C有更高的分辨率及树木生长点大气δ¹³C不同于全球大气δ¹³C值有关．     

土壤剖面碳氮稳定同位素自然丰度的垂直分布模式及其影响机制

土壤碳、氮稳定同位素自然丰度(δ¹³C和δ¹⁵N)随土壤深度变化的研究,对揭示碳、氮元素生物地球化学循环机制具有重要意义。本文在概述土壤剖面δ¹³C和δ¹⁵N垂直分布特征的基础上,重点介绍了土壤δ¹³C和δ¹⁵N垂直分布模式的影响机制。土壤剖面δ¹³C垂直分布模式的影响机制主要有3种: 1)植被δ¹³C值的历史变化;2)植物群落C3-C4植物优势度变化;3)分解过程中¹³C富集的微生物源碳的积累。此外,讨论了¹³C休斯效应对土壤剖面δ¹³C垂直分布模式的影响。土壤剖面δ¹⁵N垂直分布模式的影响机制主要有4种: 1)反硝化过程产生的¹⁵N贫化气体的损失;2)分解过程中¹⁵N富集的微生物源氮的积累;3)菌根将¹⁵N贫化的含氮化合物转移到植物而在深层土壤积累¹⁵N富集的菌根真菌残留物;4)土壤有机质-矿物相互作用。最后提出了未来土壤剖面碳、氮稳定同位素自然丰度的垂直分布模式研究应该关注的重点。     

沙棘属植物叶片碳稳定同位素含量与气候的关系

本试验以131个沙棘属植物种群为研究对象,通过测定其叶片碳稳定同位素(δ¹³C)值,分析了碳稳定同位素特征与环境因子之间的关系。结果表明: 沙棘属植物叶片的δ¹³C值介于-24.65‰～-29.11‰,平均值为-26.97‰,属于C3植物,叶片δ¹³C值变异系数为种内大于种间,表明环境因子是影响沙棘属植物叶片δ¹³C含量变化的主导因素。沙棘属植物叶片的δ¹³C值与经纬度的变化无显著相关,与海拔呈显著负相关。通过建立回归方程: δ¹³C(‰)=0.118VAP-0.007GST-0.000028RDA-20.721(R²=0.212,P<0.0001),说明影响沙棘属叶片δ¹³C值最主要的因素是水蒸气压(VAP)、生长季温度(GST)和太阳辐射(RDA)。研究结果可为沙棘属植物对全球气候变化的响应提供理论依据。     

鬼箭锦鸡儿叶片和土壤碳稳定同位素特征及其影响因素

为探究高海拔地区的植物碳(C)循环过程与其生境的关系,以生长在高山地区的豆科灌木鬼箭锦鸡儿为研究对象,沿着横跨我国东西部山区的样带采集35个样点的鬼箭锦鸡儿叶片和土壤样品,分析了鬼箭锦鸡儿叶片碳稳定同位素组成(δ¹³C)、土壤δ¹³C、叶片和土壤δ¹³C差值(Δδ¹³C)在不同采样点的特征及其与气候因子、叶片和土壤元素的关系。结果表明:鬼箭锦鸡儿叶片δ¹³C的变化范围为-30.9‰～-27.1‰,平均值为-28.4‰,土壤δ¹³C的变化范围为-26.2‰～-23.2‰,平均值为-25.3‰,Δδ¹³C的变化范围为2.0‰～7.7‰,平均值为3.1‰;叶片δ¹³C显著低于土壤δ¹³C,且随着叶片δ¹³C增加,土壤δ¹³C先降低后升高;叶片δ¹³C与生长季均温和叶片C含量呈显著负相关,土壤δ¹³C与相对湿度和最暖月均温呈显著负相关,与土壤碳∶氮(C∶N)呈显著正相关,随土壤C含量的增加土壤δ¹³C先降低后升高,Δδ¹³C与叶片C含量、土壤C含量和土壤C∶N呈显著正相关;气候因子对叶片δ¹³C和Δδ¹³C具有直接影响,同时也通过对叶片和土壤元素的影响,间接导致叶片δ¹³C、土壤δ¹³C和Δδ¹³C的改变。高海拔地区的气候因子、叶片和土壤元素共同影响鬼箭锦鸡儿的C循环过程。     

13C脉冲标记揭示放牧对高寒草甸同化碳分配的影响

放牧是人类对草地进行利用的重要方式之一, 放牧影响草地生态系统的结构和功能, 改变植物光合碳(C)分配, 进而改变土壤有机碳的储存。青藏高原的高寒草甸是世界上海拔最高的草地生态系统, 寒冷季节长等独特的环境特点使其具有高的土壤有机碳含量。为了揭示长期轻度放牧对植物光合碳分配及植物光合碳在各库之间运移的影响, 基于在青藏高原矮嵩草草甸开展的长期冬季轻度放牧和围栏封育实验, 利用 ¹³C示踪方法揭示了放牧对光合碳在植物地上、地下组织的分配以及光合碳在植物、土壤各碳库中的运移和滞留。研究结果发现, 在 ¹³C标记之后第30天, 冬季轻度放牧样地的植物地上部分内 ¹³C约占开始时 ¹³C含量的32%, 根和土壤中的 ¹³C约占22%, 植物地上部分呼吸中的 ¹³C量约占30%。在放牧和围封这两个不同处理中, 土壤中光合碳的滞留以及光合碳随土壤呼吸释放的速率存在显著差异。长期冬季轻度放牧促使植物将更多的光合碳输入到根和土壤碳库中。与围栏封育处理相比较, 放牧处理下的 ¹³C从植物地上部分输入到地下的速率较快, 通过土壤呼吸释放的速率也快, 而植物地上部分和植物地上部分呼吸中 ¹³C的量较低。另外, 高寒矮嵩草草甸土壤C储量在冬季轻度放牧和围栏封育处理下没有显著差异。我们的研究表明, 尽管冬季轻度放牧改变了植物光合碳分配在地上和地下碳库中的分配, 但是没有显著影响土壤碳库储量。     

高寒草甸不同坡向条件下植物叶片δ13C及水分利用效率的变化

通过对高寒草甸不同坡向条件下25科86种C3植物叶片稳定性碳同位素组成(δ¹³C)的测定,研究了高寒草甸C3植物δ¹³C和水分利用效率对坡向变化的响应以及环境因子对其产生的影响,分析了坡向上控制植物δ¹³C变化的主要环境因子.结果表明: 从北坡到南坡的生境梯度上,土壤含水量不断减少,而土壤温度及光照强度不断增加,植物群落结构也发生了相应变化.5个坡向中,植物叶片δ¹³C值为-31.19‰~-21.80‰,均值为(27.18±0.13)‰;生长季植物叶片δ¹³C均值在南坡最高,其次为西南坡、西坡、西北坡,最低值出现在北坡.坡向间δ¹³C值的差异主要是由不同坡向土壤含水量和土壤温度,以及光照强度的不同导致的,其中土壤含水量是主要的限制因子.北坡-南坡梯度上植物叶片δ¹³C值随土壤含水量下降、土壤温度及光照强度升高而变大,表明不同坡向植物的水分利用状况对干旱胁迫的响应不同,植物逐渐提高了水分利用效率以适应干旱胁迫的生境.     

Bioremediation of Polyaromatic Hydrocarbon-Contaminated Sediments in Aerated Bioslurry Reactors

Treatment of dredged sediments contaminated by polyaromatic hydrocarbons (PAHs) is a significant problem in the New York/New Jersey (NY/NJ) Harbor. 0.5 m³-scale slurry-phase bioreactors were used to determine whether bioaugmentation with a PAH-degradative bacterial consortium, or with the salt marsh grass S. alterniflora, could enhance the biodegradation of PAHs added to dredged estuarine sediments from the NY/NJ Harbor. The results were compared to biodegradation effected by the indigenous sediment microbial community. Sediments were diluted 1:1 in tap water and spiked to a final concentration of 20 mg/kg dry weight sediment of phenanthrene, anthracene, acenaphthene, fluorene, fluoranthene, and pyrene. The sediment slurry was then continuously sparged with air over 3 months. In all bioreactors a rapid reduction of greater than 95% of the initial phenanthrene, acenaphthene, and fluorene occurred within 14 days. Pyrene and fluoranthene reductions of 70 to 90% were achieved by day 77 of treatment. Anthracene was more recalcitrant and reductions ranged from 30 to 85%. Separate experiments showed that the sediment microbial communities mineralized ¹⁴C-pyrene and ¹⁴C-phenanthrene. PAH degradation, and the number of phenanthrene-degrading bacteria, were not enhanced by microbial or plant bioaugmentation. These data demonstrate that bioaugmentation is not required to effect efficient remediation of PAH-contaminated dredged sediments in slurry-phase bioreactors.     

Monitoring Anaerobic Natural Attenuation of Petroleum Using a Novel In Situ Respiration Method in Low-Permeability Sediment

Assessing petroleum biodegradation rates is an important part of predicting natural attenuation in subsurface sediments. Monitoring carbon dioxide (CO₂) and methane (CH₄) produced in situ, and their radiocarbon ¹⁴C), stable carbon (¹³C) and deuterium (D). signature provide a novel method to assess anaerobic microbial processes. Our objectives were to: (1) estimate the rate of anaerobic petroleum hydrocarbon (PH) mineralization by monitoring the production of soil gas CH₄ and CO₂ in the vadose zone of low-permeability sediment, (2) evaluate the dominant microbial processes using δ¹³C and δD, and (3) determine the proportion of CH₄ and CO₂ attributable to anaerobic mineralization of PH using ¹⁴C analysis. Argon was sparged into the subsurface to dilute existing CO₂ and CH₄ concentrations. Vadose zone CO₂, CH₄, oxygen, total combustible hydrocarbons, and argon concentrations were measured for 75 days. CO₂ and CH₄ samples were collected on day 86 and analyzed for ¹⁴C, δ¹³C, and δD. Based on CH₄ soil gas production, the anaerobic biodegradation rate was estimated between 0.017 to 0.055 mg/kg soil-d. CH₄ ¹⁴C (2.6 pMC), δ¹³C (-45.64‰), and δD (-316‰) values indicated that fermentation of PH was the sale source of CH₄ in the vadose zone. CO₂ ¹⁴C (62 pMC) indicated that approximately 47% of the total CO₂ was from PH mineralization and 53% from plant root respiration. Although low-permeability sediment increases the difficulty of completely replacing in situ soil gas and assuring anaerobic conditions, this novel respiration method distinguished between anaerobic processes responsible for PH degradation.     

A review of the use of isotopic and nuclear techniques in animal production

Isotopic and nuclear techniques play an important role in food and agriculture, health and industry. This paper discusses the use of these techniques and highlights potential for their use in the area of Animal Production. These techniques are discussed in two parts: (1) Isotopic methods and (2) non-isotopic nuclear methods. The isotopic techniques discussed are: stable- (¹⁵N) and radio-isotope (³⁵S or ³²P) incorporation methods for measuring microbial mass in vitro and in vivo; ¹²⁵I-labelled bovine serum albumin and ¹⁴C-labelled polyethylene glycol assays for measuring tannin in feeds; a method based on the feeding of isotope-labelled protein (¹⁵N or ¹²⁵I) complexed with tannin for ranking different tannins for their abilities to release protein for digestion in vivo; ¹⁴C-uric acid and ¹⁴C-allantoin infusion methods for development of models describing excretion of purine derivatives in urine and microbial protein supply to ruminants, which permit assessment of nutritional status of animals and determination of nutritional quality of feed resources; a ¹⁵N isotope dilution technique using ¹⁵N-leucine to distinguish feed and endogenous secretions at the ileum, for determination of true digestibility of protein-rich tree leaves and aquatic plants in pigs; progesterone radioimmunoassay (RIA) for enhancing reproductive efficiency of ruminants, and RIA based leptin and insulin like growth factor assays for assessing the nutritional status of animals; feeding of ¹⁵N enriched plant material to generate ¹⁵N-labelled excreta for research on the fate of excreta N in the environment; ¹⁵N, ¹³C and ³⁴S isotopic methods for nutrient budgeting and for following the nutrient pathways in the soil–plant–animal continuum; ³²P- or ³³P-labelled fertilizers for estimating the efficiency of P utilization in legume leaf production used for livestock feeding; double labelled water (¹⁸O and ²H labelled) method for estimating energy expenditures of grazing animals, body composition, basal metabolic rate, and milk output in cows with calves; NaH¹³CO₃/NaH¹⁴CO₃ infusion for estimation of the carbon dioxide production, which in turn is used to estimate energy expenditure in free-ranging animals; ³H- or ¹⁴C-labelled methane and ¹⁴C-labelled volatile fatty acids dilution technique for direct and indirect (using stoichiometry of carbohydrate fermentation) for determination of methane emission from livestock; ¹⁵N dilution technique requiring labeling the soil with ¹⁵N fertilizer (¹⁵N-ammonium sulphate or ¹⁵N-urea) for estimation of nitrogen fixation by leguminous trees and pastures.

The non-isotopic nuclear techniques that have been used or have the potential for use are: dual energy X-ray absorptionmetry and computer tomography for body composition determination; nuclear magnetic resonance techniques, fast atom bombardment mass spectroscopy, and mass ionisation spectroscopy for identification and structure determination of bioactive moieties of plant origin having potential for rumen manipulation or controlling internal parasites; gamma irradiation for inactivating antinutrients such as protease inhibitors, lectin, phytic acid, non-starch polysaccharides and oligosaccharides in feeds; induced mutations with gamma radiation, electron beam and fast neutrons for producing useful mutants of forage plants with improved yield, nutrient profiles and uptake.     

Degradation of Atrazine by Hornwort in Aquatic Systems

Hornwort (Ceratophyllum deinersuin) incubated in the presence of 1 mg L^{-1 14}C atrazine in an aqueous nutrient solution became radioactive. Microscopic autoradiography was used to investigate the localization of ¹⁴C atrazine in a hornwort/epiphyte system. Radioactivity was present within the plant tissue (and also in the nutrient solution), with larger quantities in mature tissue, including stems compared with young tissue. An irregular distribution of black silver granules (which indicate radioactivity) was observable on the plant surface, suggesting the possible involvement of epiphytes (plant surface microorganisms) in the degradation process. Labeled compounds in the extracted plant included atrazine and a major metabolite that may have been an artrazine-glutathione connjugate. Concentrations of atrazine and the metabolite, and the fraction of the metabolite (based on total radioactivity), all in the extracted plant, were dependent on the initial atrazine concentration in the solution. The degradation process was light dependent and the analyses of the nutrient solution indicated that the first half-life of atrazine in the presence of hornwort was 5 days under day/night conditions, while only about 30% of initial atrazine disappeared after 3 weeks under complete dark. The major metabolite in the solution was identified as deethylatrazine.     

Transport in C4 mesophyll chloroplasts. Characterization of the pyruvate carrier

1. Evidence is presented for high rates of carrier-mediated uptake of pyruvate into the stroma of intact mesophyll chloroplasts of the C₄ plant Digitaria sanguinalis, but not the chloroplasts of the C₃ plant Spinacea oleracea. Uptake of pyruvate in the dark with the C₄ mesophyll chloroplasts was followed using two techniques: uptake of [¹⁴C]pyruvate as determined by silicon oil centrifugal filtration and uptake as indicated by absorbance changes at 535 nm (shrinkage/swelling) after addition of 0.1 M pyruvate salts.

2. Uptake of the pyruvate anion by an electrogenic carrier is suggested to be the major mode of transport. Chloroplast swelling was observed in potassium pyruvate plus valinomycin and uptake of [¹⁴C]pyruvate was inhibited by membrane-permeant anions. Valinomycin reduced uptake in the absence of external potassium and the inhibition could be reversed by addition of external potassium.

3. Uptake of pyruvic acid (or a pyruvate ⁻/OH⁻ antiport) is ruled unlikely since [¹⁴C]pyruvate uptake was relatively independent of the pH gradient across the envelope and addition of pyruvate to chloroplasts did not result in an alkalization of the medium. The low rate of swelling observed in ammonium pyruvate may be due to non-mediated permeation of pyruvic acid, which is possible only at high pyruvate concentrations.

4. The concentration of pyruvate in the stroma increased with external concentration over the range tested (up to 40 mM) but the concentration ratio (internal/external) was always less than one. The steady-state concentration of [¹⁴C]pyruvate in the stroma was dependent on the ionic strength of the medium, with saturation at roughly I = 0.04 M, while accumulation of the membrane-permeant cation tetraphenylmethylphosphonium decreased with increasing ionic strength. This suggests that ionic strength modifies a membrane potential (inside negative) across the envelope and that pyruvate uptake responds to the magnitude and direction of that potential (−80 mV at low ionic strength).

5. Chloride and inorganic phosphate were potent inhibitors of [¹⁴C]pyruvate uptake. Of the sulfhydryl reagents tested, N-ethylmaleimide was not inhibitory while mersalyl completely blocked [¹⁴C]pyruvate uptake and swelling in potassium pyruvate plus valinomycin. Pyruvate uptake, as measured by valinomycin induced swelling in potassium pyruvate, was highly temperature sensitive, with an energy of activation of 39 kcal/mol above 9 °C.

6. Phenylpyruvate, -ketoisovalerate, -ketoisocaproate, -cyano-4-hydroxycinnamic acid and -cyanocinnamic acid inhibited [¹⁴C]pyruvate but not [¹⁴C]-acetate uptake in the dark and also reduced pyruvate metabolism by the chloroplasts in the light.     

Activation of [C]chlorobiphenyls to protein-binding metabolites by rat liver microsomes

The irreversible binding of [¹⁴C]2,2′-di- and [¹⁴C]2,4,5,2′,4′,5′-hexachlorobiphenyl ([¹⁴C]DCB and [¹⁴C]HCB) to protein was studied in the presence of rat liver microsomes and a NADPH-generating system. Protein-bound radioactivity was found with [¹⁴C]DCB but not with [¹⁴C]HCB. The binding of ¹⁴C-metabolites was increased by pretreatment of the rats with phenobarbital or polychlorinated biphenyls. Protein binding was linear for 80 min. In contrast, monohydroxy-metabolites of DCB were formed and degraded within 40 min. Inhibition of secondary oxidation of DCB by scavening superoxide anions or by glucuronidation of the monophenols markedly decreased the protein binding. Addition of trichloropropene oxide or styrene oxide, both inhibitors of epoxide hydrase, did not significantly stimulate the binding. The results suggest that the majority of reactive metabolites of DCB arise from secondary metabolism, i.e., the subsequent oxidation of the phenolic metabolites. Arene oxides, the primary products, appear to play a minor role in the protein binding of DCB.     

Bradykinin effects on phospholipid metabolism and its relation to arachidonic acid turnovers in neuroblastoma × glioma hybrid cells (NG 108-15)

In neuroblastoma × glioma hybrid cells (NG 108-15) labelled with [³²P]-trisodium phosphate, [³H]-inositol and [¹⁴C]-arachidonic acid, bradykinin stimulated the hydrolysis of phosphatidylinositol 4,5-bisphosphate (PIP₂) while it had no effect on the release of [¹⁴C]-arachidonic acid (AA). The effect on PIP, was time- and dose-dependent with a maximal effect on [³H]-inositol- and [³²P]-labelled cells after 10–30 s of stimulation with 10⁻⁶ M bradykinin. However, the hydrolysis of [¹⁴C]-AA labelled PIP₂ was delayed compared to the effect on [³H]- and [¹⁴C]-PIP₂ and was not detectable until after 60 s of stimulation. Bradykinin stimulation resulted in an increased formation of [³H]-inositol phosphates (IP) and [³²P]- and [¹⁴P]- and [¹⁴C]-phosphatidic acid (PA) but the time course for PA formation did not allow the time-course for PIP₂ hydrolysis. A reduced labelling of [²³P]- and [¹⁴C]-phosphatidylcholine was also found in stimulated cells suggesting that PA may derive from other sources than PIP₂. In conclusion, our results indicate that bradykinin activates phospholipase C, but not phospholipase A₂, in NG 108-15 cells.     

Differential production of prostaglandins D2 and E2 and of unusual prostanoid by chick spinal cord and meninges in vitro

In order to specify the source of locally synthesized prostaglandin (PG) E₂ which is able to saturate the large class of low affinity PGE₂ receptors in chick spinal cord, bioconversion of [1-¹⁴C]arachidonic acid into prostanoids was studied in homogenates of chick spinal cord and meninges first without addition of exogenous glutathione (GSH). Homogenates of spinal cord produced ¹⁴C-labeled PGE₂, PGD₂ and PGF₂. Homogenates of meninges accumulated much larger amounts of [¹⁴C]PGE₂ than spinal cord and surprisingly a ¹⁴C-labeled arachidonate metabolite referred to as compound Y. Compound Y generation, which was inhibited by indomethacin and enhanced by esculetin, was therefore mediated through the cyclooxygenase pathway. The fact that no labeled compound Y was detected in homogenates incubated with [³H]PGD₂ or [³H]PGE₂ indicated that compound Y was not degradation product of PG_s. Secondly, after addition of exogenous GSH, ¹⁴C-labeled compound Y was totally converted into [¹⁴C]PGE₂. The compound Y which is converted into PGF_s after a strong reduction with NaBH₄ and into PGE₂ after a mild reduction with GSH-hemin system or SnCl₂ was therefore assumed to be a 15 hydroperoxy-PGE₂ (15 HP-PGE₂). These results suggest that PGE₂ can be synthesized in meninges either by the classical isomerization of PGH₂ or by isomerization of PGG₂ followed by a GSH-sensitive reaction.     

红壤丘陵区水田和旱地土壤可溶性有机碳矿化对水分的响应

以亚热带红壤丘陵区典型水田和旱地土壤为研究对象,向土壤中添加¹⁴C标记稻草,培养30 d后,提取与原位土壤中结构相似的¹⁴C可溶性有机碳(DOC);将¹⁴C DOC加入水田和旱地土壤中,并设置45%、60%、75%、90%和105%田间持水量(WHC)5个水分梯度,在标准状态下(25 ℃)培养100 d,监测¹⁴C DOC在土壤中的矿化过程.结果表明: 培养100 d后,两种土壤中28.7%～61.4%的标记DOC被矿化为CO₂,且5个水分条件下,水田土壤DOC的矿化率均显著高于旱地,这主要是由于水田土壤DOC的结构组成比旱地土壤更简单.好气条件(56%～75%WHC)有利于两种土壤DOC的分解,淹水条件(105%WHC)则有利于DOC的积累.土壤处于好气条件(45%～90%WHC)时,DOC的生物可分解率及易分解态所占比例均随着含水量的增加而增加.100 d内,水田和旱地易分解态DOC分别占其累积矿化量的80.5%～91.1%和66.3%～72.4%,说明DOC的生物可分解率主要由其易分解态组分所占比例决定.