西伯利亚蝗气门结构及呼吸代谢对高温胁迫的响应

【目的】掌握西伯利亚蝗Gomphocerus sibiricus的气门结构和呼吸代谢应对高温胁迫的响应策略。【方法】运用扫描电镜观察西伯利亚蝗气门超显微结构,多通道昆虫呼吸仪测定18~42℃处理下西伯利亚蝗的O_2吸收率、CO_2释放率、代谢率和呼吸商。【结果】西伯利亚蝗共有10对气门,胸部2对,腹部8对,呈圆形或椭圆形,内侧着生有筛板,呈刺凸状,分布密集。18~42℃范围内,随温度升高,西伯利亚蝗呼吸代谢呈先上升后下降的趋势。18℃时西伯利亚蝗雌雄成虫的O_2吸收率、CO_2释放率和代谢率值显著小于其他温度下的相应值(P<0.05),雌虫分别为0.0022 m L/min、0.0019 m L/min和0.0210 m L/(g·min),雄虫分别为0.0016 m L/min、0.0016 m L/min和0.0236 m L/(g·min);21~27℃范围内,西伯利亚蝗雌雄成虫的呼吸代谢变化平稳,超过30℃呼吸代谢各指标值迅速上升,至36℃时雌雄成虫的O_2吸收率和代谢率值均显著大于其他温度下的相应值(P<0.05);雌虫分别为0.0071 m L/min和0.0592 m L/(g·min),雄虫分别为0.0089 m L/min和0.1108 m L/(g·min),39℃时CO_2释放率显著大于其他温度下的相应值(P<0.05),雌雄成虫分别为0.0074 m L/min和0.0067 m L/min。【结论】依据西伯利亚蝗呼吸代谢随温度变化特征可以判断,随气候持续变暖,西伯利亚蝗仍将是新疆高山、亚高山草原的重要致灾类群。     

驯化对始红蝽(Pyrrhocoris apterus)耐寒能力的影响及越冬适应策略

为阐明越冬期间始红蝽应对低温胁迫的耐寒策略及其影响因素,从生理生化水平探讨始红蝽成虫的耐寒能力,逐月测定了12月至翌年3月始红蝽低温驯化前后的过冷却点、低温存活率、LT_(50)以及始红蝽体内耐寒物质含量。结果表明,越冬期间始红蝽自然种群过冷却点最低为(-14.01±0.53)℃,-5、-10℃驯化30min后的始红蝽过冷却点最低降至为(-19.32±0.86)℃、(-25.56±1.09)℃。0℃驯化30min后暴露于-5、-10、-15℃1h的最高存活率依次为100%、39.1%±8.6%、10%;始红蝽自然种群LT_(50)最低为-8.53℃,0℃驯化后降至-9.21℃。越冬期间雌雄始红蝽体内自由水/结合水比值和游离蛋白质含量先下降后上升,12月达到最大值,雌雄分别为144.50±26.22和140.32±21.92,(15.81±0.10)mg/g和(15.47±0.01)mg/g;脂肪、海藻糖和甘油含量先上升后下降,2月达到最大值,雌雄脂肪含量分别为(16.33±0.48)mg/g和(13.15±1.32)mg/g,海藻糖含量分别为(11.98±0.01)mg/g和(10.88±0.02)mg/g,甘油含量分别为(14.74±0.01)mg/g和(15.06±0.03)mg/g。研究证明,低温驯化后始红蝽的过冷却点和LT_(50)明显降低,低温存活率显著提高,越冬期间始红蝽可通过调整体内抗逆物质含量以增强虫体耐寒能力。     

北京山区典型暖温带落叶阔叶林大气CO_2浓度、草本层光合作用及土壤释放CO_2变化特点(英文)

为探讨森林生态系统植被、土壤等不同组分与大气CO_2交换特点,利用中型同化箱(40cm×40cm×2Ocm)及红外CO_2分析仪装置对北京山区典型暖温带森林生态系统辽东栎(Quercus liaotungensisKoidz.)林草本层净光合作用、土壤释放CO_2及林外(高出林冠2m)与林内(低于林冠2m)大气CO_2变化进行测定。结果表明:夏季及秋季大气CO_2浓度分别为(323±10)μmol·mol~(-1)和(330±1)μmol·mol~(-1);在一天内连续24h的测定中,大气与林内CO_2浓度的差值最大时可分别达-46和-61μmol·mol~(-1)。夏季草本层净光合强度为(2.59±1.05)μmol CO_2·m~(-2)·s~(-1),是秋季((1.31±0.39)μmol CO_2·m~(-2)·s~(-1))的2倍;夏季土壤呼吸释放CO_2的强度明显高于秋季,分别为(5.18±0.75)μmol CO_2·m~(-2)·s~(-1)和(1.96±0.57)μmol CO_2·m~(-2)·s~(-1)。土壤释放CO_2强度与地面温度之间存在显著相关,其关系式为Y=-0.8642 0.3101X(r=0.7164,P<0.001,n=117)。大气CO_2浓度的低值及草本层光合强度高值约出现在14:00左右;而在夜间土壤释放CO_2强度增加,表现为大气CO_2浓度升高。     

温度对意大利蝗呼吸代谢的影响

【目的】意大利蝗Calliptamus italicus L.是新疆荒漠、半荒漠草原的主要危害种类,前期研究表明其发生与新疆气候变暖显著相关,本研究进一步探讨气候变暖条件下意大利蝗的呼吸代谢适应机制。【方法】应用多通道昆虫呼吸仪测定了15, 20, 25, 30和35℃不同温度条件下意大利蝗成虫的呼吸率、代谢率、CO₂释放率、Q₁₀(每升高10℃呼吸率的变化幅度)及呼吸商并分析其变化特征。【结果】15℃时意大利蝗成虫的呼吸率、代谢率、CO₂释放率均显著低于其他温度（P<0.01）, 35℃时3项指标值显著高于其他温度（P<0.01）,表明低于15℃和高于35℃的温度条件都对意大利蝗的呼吸代谢产生明显影响;在20~30℃之间,意大利蝗的呼吸率、代谢率及CO2释放率变化幅度小且平稳,差异均不显著（P>0.01）,表明该温度范围是意大利蝗生长发育的适宜温度条件。不同温度下意大利蝗呼吸率的Q₁₀值显示, 20~30℃温度范围内的 Q₁₀值最小,为1.03, 15~25℃的Q10值为1.43, 25~35℃的Q10值最大,为2.42,说明意大利蝗的呼吸代谢活动对温度变化敏感,并表明20~30℃是意大利蝗生长发育的适宜范围。各温度条件下意大利蝗呼吸商的差异不显著（P>0.01）,平均为0.9450,判断意大利蝗呼吸代谢消耗的底物主要为糖类物质。【结论】意大利蝗生长发育的适宜温度范围是20~30℃,预示着在气候持续变暖背景下,意大利蝗仍将是新疆草原最重要的生物灾害之一。     

土壤温度和水分对油松林土壤呼吸的影响

用LI-COR 6400-09土壤呼吸测定系统,在太原天龙山自然保护区对油松林的土壤呼吸进行了4a测定.结果表明,土壤呼吸具有明显的季节变化特点,最大值出现在8月份,在6～10 μmol m~(-2) s~(-1) 之间,最小值出现在12月份和3月份,在0.5 μmol m~(-2) s~(-1)左右.2005、2006、2007和2008年土壤呼吸CO_2的年平均值分别为(4.71±3.74)、(3.08±2.91)、(2.96±2.58) μmol m~(-2) s~(-1)和(2.12±1.54) μmol m~(-2) s~(-1);4a的CO_2总平均值为(3.27±2.95) μmol m~(-2) s~(-1).4个测定年土壤呼吸的平均值总体差异显著.4个测定年土壤CO_2释放C量分别为1103.5、882.8、918.4 g m~(-2)和666.3 g m~(-2),总C平均值为892.8 g m~(-2),具有明显的年际差异.指数方程可以很好的表达土壤呼吸与10 cm深度土壤温度的关系,R~2值4a分别为0.39,0.60,0.68和0.71,Q_(10)值分别为3.10,4.41、4.05和5.18,用4a全部数据计算的Q_(10)值为4.31.土壤水分对土壤呼吸的作用较弱,R~2值4a分别仅为0.31、0.25、0.13和0.02,但是夏季土壤干旱对土壤呼吸的抑制作用非常明显,可使土壤呼吸下降50%以上.夏季土壤干旱是导致土壤呼吸年际变化的主要原因.4个包括土壤温度和水分的双变量模型均可以很好地模拟土壤呼吸的季节变化, 拟合方程的R~2值从0.58到0.79.     

不同碱度条件下中华水韭昼夜CO_2气体交换的特征

运用pH-drift的方法研究了在不同碱度条件下中华水韭(Isoetes sinensis)的沉水叶片昼夜CO_2吸收的特征.结果表明中华水非的沉水叶片具有昼夜吸收水中CO_2的能力,而不具备利用水中的HCCO3的能力,进一步证明了水生植物中华水韭的光合碳同化途径具有景天酸代谢(CAM)的特征.中华水韭沉水叶片光照条件下对水中CO_2的吸收速率在一定的浓度范围内正相关于水中的CO_2浓度.光照条件下,中华水韭的pH-drift实验的pH补偿点分别为(8.1±0.3)和(7.9±0.1)mmol·L~(-1),最终[C_T]/Alk值为(1.009±0.01)和(1.022±0. 004).碱度对中华水韭夜晚CO_2的吸收速率有显著的影响(F=38.73,P<0.0001).总碱度1.70mmol·L~(-1)溶液中的中华水韭沉水叶片在相对较低的CO_2浓度(0.04±0.001mmol·L~(-1))水平下即表现出对CO_2的净吸收.调查了野外一处中华水韭沉水种群的生境pH值及CO_2浓度的昼夜变化,发现水体碱度约为1.59mmol·L~(-1),一昼夜的pH值波动不大,平均为(6.1±0.04),昼夜CO_2浓度存在波动,午夜水中的CO_2浓度是午后的近3倍.     

始红蝽越冬聚集行为对其能量代谢的影响

聚集行为是动物适应不良环境的一种生态对策。始红蝽Pyrrhocoris apterus在成虫滞育越冬期间具有显著的聚集行为。采用LI-6400型光合仪测定了5种聚集度(分别用1头、5头、10头、20头和50头的群体大小表示)下始红蝽的呼吸量,通过呼吸量计算得到各聚集度始红蝽的呼吸速率(rate of respiration,Rr)及能量代谢速率(rate of metabolism,Rm),旨在明确聚集行为是否能够对始红蝽越冬时的能量代谢产生影响。结果表明： 不同聚集度间始红蝽的Rm值存在显著性差异; 并且随聚集度的增加,Rm值与聚集度呈显著负相关,Rm值依次为0.052,0.044,0.041,0.037和0.033 W/g。结果说明聚集行为可以有效降低始红蝽新陈代谢速率,有利于种群成功越冬。     

CO_2释放量和呼吸商如何正确计算?

用瓦氏检压技术测定呼吸时,怎样正确计算CO_2的释放量和呼吸商?《植物生理学实验》(薛应龙主编,第96页)一书中是这样写的:“不加碱的反应瓶,压力计上的读数变化是呼吸作用放出的CO_2和吸收的O_2的总结果。若以油料种子为例,放出的CO_2量比吸收的O_2量要少,所以反应瓶中的压力减少,压力计上的△h为     

横断山脉大绒鼠最大代谢率的季节性差异

最大代谢率对于动物的生存、繁殖和分布具有关键作用。实验用开放式呼吸仪测定了大绒鼠(Eothenomys miletus)夏季和冬季的冷诱导最大代谢率和运动最大代谢率。大绒鼠夏季的冷诱导最大代谢率O2为(7.24±0.61)ml/(g.h),运动最大代谢率O2为(7.69±0.59)ml/(g.h);冬季的冷诱导最大代谢率O2为(8.61±0.42)ml/(g.h),运动最大代谢率O2为(7.51±0.51)ml/(g.h)。冷诱导最大代谢率冬夏之间具有差异显著,而运动最大代谢率则差异不显著。结果表明:栖息于横断山脉的大绒鼠由于受到低温的胁迫,导致其冷诱导最大代谢率季节性变化较大,而运动最大代谢率则相对稳定。     

一种昆虫呼吸代谢测定方法的改进

为了探索精准、简易的昆虫呼吸代谢测定办法,本文基于Sable小动物呼吸测量系统,比较了应用Sable呼吸测量系统配置的8通道气路转换器呼吸室和采用鲁尔接头注射器作为替代呼吸室测试昆虫的呼吸代谢。结果表明:应用测量系统自带呼吸室和应用替代呼吸室检测棉铃虫蛹O_2消耗量(前者为0.2425(±0.0143) mL/g·h,后者为0.2389(±0.0146) mL/g·h)和CO_2释放量(前者为0.1562(±0.0098) mL/g·h,后者为0.1639(±0.0092) mL/g·h),两种测试方法无显著差异。与采用系统配置8通道气路转换器和自带呼吸室每测试7个样本耗时2.30 h相比较,应用替代呼吸室测试21个样本仅耗时2.75 h,明显节省测试时间。应用替代呼吸室,从呼出二氧化碳动态亦可以区分黑纹粉蝶不同虫态或不同发育状态的呼吸代谢差异。通过对两种测试方法的分析,推荐应用鲁尔接头注射器作为替代呼吸室的改进方法进行昆虫呼吸代谢生理的研究。     

Growth and net photosynthetic rates of <Emphasis Type="Italic">Hosta</Emphasis> ‘blue vision’ during acclimatization in bright,natural light with CO<Subscript>2</Subscript> enrichment

Summary Hosta ‘Blue Vision’, a shade-adapted perennial, was successfully acclimatized in high, natural light conditions in the research Acclimatron^TM at Clemson University, Clemson, SC during the summer of 2000. The supplemental CO₂ levels achieved during acclimatization were 710±113, 2396±121, and 5641±119 μmol mol⁻¹, approximately 2×, 6×, and 15× ambient CO₂. Plants were maintained in H₂O-saturated atmospheres and protected from temperature increases associated with high light intensity. In the 5 wk following ex vitro transfer, plantlet roots grew at the 2× CO₂ level, but shoot biomass was unaffected. Results for the 6× and 15× CO₂ levels were comparable and provided the best plantlet growth. The “doubling time’ that is characteristic of exponential growth was 10.8 and 9.8 d for root and shoot dry weights, respectively. There was no indication of light saturation of net photosynthetic rate (NPR) over the photosynthetic photon flux density (PPFD) range of 100–1200 μmolm⁻²s⁻¹ experienced during this study. An interaction between CO₂ and light intensity levels was detected for NPR of Hosta ‘Blue Vision’ with CO₂ saturation occurring at approximately 2800 μmol mol⁻¹. regardless of light level. Furthermore, at the optimal CO₂ level, NPR increased quadratically as light intensity increased, and NPR was greatest at the maximum light intensity (PPFD: 1200 μmol m⁻²s⁻¹).     

Decrease in respiratory rate in a wolf spider,Pardosa astrigera (L. Koch), under starvation

Effects of starvation on the suryival period and the respiratory rate in adults of a wolf spider, Pardosa astrigera (L. Koch ), were investigated. The spiders used were divided into four groups: well-fed, starved and two limited food groups; in the latter two, each spider was supplied with one leafhopper every second or third day. Adult males and females of P. astrigera could survive for a long time; 28.8±2.7 days and 54.4±18.9 days, respectively, without any food. The longevities shown here were 73.8% for males and 78.6% for females of those of well-fed spiders, indicating that P. astrigera adults have a strong tolerance to starvation. The respiratory rate of well-fed adults showed no tendency to increase or decrease with their aging; the mean respiratory rates were 4.86×10⁻⁴ mg CO₂/mg f.w. (fresh body weight)/hr for males and 3.80×10⁻⁴ mg CO₂/mg f.w./hr for females. The respiratory rates of starved spiders increased during the first two days of starvation but decreased markedly from the third to the twelfth day, and thereafter retained an almost constant level for each sex. The mean respiratory rates after the twelfth day of starvation were 2.49×10⁻⁴ mg CO₂/mg f.w./hr for males and 2.76×10⁻⁴ mg CO₂/mg f.w./hr for females; these values were respectively 48.4% and 63.0% of those prior to starvation. The fresh body weight of starved spiders decreased linearly with time but the rate was small. The respiratory rates of the limited food groups tended to decline with time and thereby their weight losses were minimized. The decrease in the respiratory rate under starvation was considered not to be due to spider exhaustion or senescence but due to an intrinsic change in behaviour and/or metabolism, because when the spiders were supplied with ample food for five days after starvation, the respiratory rate and the body weight rapidly recovered to near the levels prior to starvation. It is suggested that starved spiders use a higher ratio of fat as catabolic substrate than normally fed or satiated ones. Feeding strategies of poikilo-therm predators are discussed.     

High Metabolic Rates in Beach Cast Communities

Metabolic hotspots at land–water interfaces are important in supporting biogeochemical processes. Here we confirm the generality of land–aquatic interfaces as biogeochemical hot spots by extending this concept to marine beach cast materials. In situ atmospheric pCO_2, from a respiration chamber (10 cm in diameter and 20 cm high) inserted into wrack deposits, was determined using a high-precision (±1 ppm) non-dispersive infrared gas analyzer (EGM-4, PP-systems) at 1 minute recording intervals. The wrack deposits supported high metabolic activities, with CO₂ fluxes averaging (±SE) 6.62 ± 0.88 μmol C m⁻² s⁻¹, compared to median value of 0.98 μmol C m⁻² s⁻¹ (mean 2.21 ± 1.25 μmol C m⁻² s⁻¹) for bare sand adjacent to deposits. Wrack metabolic rates ranged 40-fold across beaches, from a minimum of 0.57 ± 0.22 μmol C m⁻² s⁻¹ to a maximum of 20.8 ± 5.04 μmol C m⁻² s⁻¹, both derived from beaches with deposits dominated by Sargassum. Rates tended to increase significantly (F test, P < 0.05) from the shoreline to reach maximum rates at about 10 m from the shoreline, declining sharply further from the shoreline, and increased with increasing thickness of the deposits (maximum about 10 cm deep), declining for thicker deposits. Wrack differing in composition had similar metabolic rates, although deposits consisting of a mixture of seagrass and algae tended to show somewhat higher rates. Our results show a meter square of wrack deposit supports a metabolic rate equivalent to that supported by 3 m² of living seagrass or macroalgal habitat. In wrack, the marine environment provides organic material and moisture and the land environment provides oxygen to render wrack ecosystems an efficient metabolic reactor. Intense wrack metabolism should also be conducive to organismal growth by supporting the development of a cryptic, but diverse wrack-based food web.     

Latency of oxygen toxicity of the central nervous system in rats as a function of carbon dioxide production and partial pressure of oxygen

Oxygen toxicity of the central nervous system (CNS) can occur as convulsions and loss of consciousness, with no warning symptoms. A quantitative study of the effect of metabolic rate on sensitivity to oxygen toxicity was made in the rat. A group of 19 rats were exposed (126 exposures) to 12 combinations of four pressures (456, 507, 608 and 709 kPa) and three ambient temperatures (15, 23 and 29°C) until the appearance of the first electrical discharge (FED) preceding clinical convulsions. Carbon dioxide production (V˙CO₂) was also measured. A thermoneutral zone (mean V˙CO₂ 0.87 ml · g⁻¹ · h⁻¹) existed between the temperatures of 24 and 29°C; at temperatures lower than this, the metabolic rate increased by 1.2 to 4 times the resting level. Latency of FED decreased linearly with the increase in V˙CO₂ at all four oxygen pressures. The slopes (absolute value) and intercepts decreased with the increase in oxygen pressure. This linear relationship made possible the derivation of an equation which described latency of the FED as a function of both oxygen pressure and metabolic rate. Various environmental and other physiological factors that have been said to influence sensitivity to CNS oxygen toxicity, enhancing the effect of the partial pressure of oxygen, can be explained by their effect on metabolic rate. It is suggested that in situations where there is a risk of oxygen toxicity of the CNS, that risk would be reduced by a lower metabolic rate. Accepted: 4 May 1998     

Changes in the metabolic rate of the foraging honeybee: effect of the carried weight or of the reward rate?

The metabolic rate of free flying honeybees (Apis mellifera ligustica) foraging on a multiple automatic feeder was measured in complete absence of perturbation. Each time the sucrose flow rate was doubled, the metabolic rate increased by 18.2 ± 2.0% (14.7 μl CO₂ min⁻¹) and final crop load by 25.1 ± 2.4% (7.04 μl). The possibility that the heavier load carried by the bees caused the increase in the metabolic rate was analyzed in detail. It was found that, for the same weight in the crop, the metabolic rate increased with the increasing reward rate. Therefore, a factor other than the carried weight might account for this increase: a motivational drive, whose intensity may depend on the reward rate at the food source. Although at higher reward rates metabolic rate increased during the visit, at lower reward rates it remained constant, suggesting that the effect of the carried weight on the metabolic rate might be controlled by this motivational drive. The hypothesis that honeybees maximize individual efficiency by reducing their crop load loses support, as foraging costs are not determined by the carried weight. The functional meaning of the reduction in crop load would be to increase the informational exchange at the hive. Accepted: 8 January 2000     

Root respiratory quotient and nitrate uptake in hydroponically grown non-mycorrhizal and mycorrhizal wheat

 Oxygen and CO₂ fluxes were measured in hydroponically grown mycorrhizal and non-mycorrhizal Triticum aestivum L. cv. Hano roots. The NO₃ ^– uptake of the plants was used to estimate the amount of root respiration attributable to ion uptake. Plants were grown at 4 mM N and 10 μM P, where a total and viable mycorrhizal root colonisation of 48% and 18%, respectively, by Glomus mosseae (Nicol. and Gerd.) Gerd. and Trappe (BEG 107) was observed. The O₂ consumption and NO₃ ^– uptake rates were similar and the CO₂ release was higher in mycorrhizal than in non-mycorrhizal wheat. This resulted in a significantly higher respiratory quotient (RQ, mol CO₂ mol^–1 O₂) in mycorrhizal (1.27±0.13) than in non-mycorrhizal (0.79±0.05) wheat. As the biomass and N and P concentrations in mycorrhizal and non-mycorrhizal wheat were the same, the higher RQ resulted from the mycorrhizal colonisation and not differences in nutrition per se. Accepted: 26 March 1999     

Land-use conversion effects on CO2 emissions: from agricultural to hybrid poplar plantation

Land-use changes such as deforestation have been considered one of the main contributors to increased greenhouse gas emissions, while verifiable C sequestration through afforestation projects is eligible to receive C credits under the Kyoto Protocol. We studied the short-term effects on CO₂ emissions of converting agricultural land-use (planted to barley) to a hybrid poplar (Populus deltoids × Populus × petrowskyana var. Walker) plantation in the Parkland region in northern Alberta, where large areas are being planted to hybrid poplars. CO₂ emissions were measured using a static gas chamber method. No differences were found in soil temperature, volumetric moisture content, or soil respiration rates between the barley and Walker plots. The mean soil respiration rate in 2005 was 1.83 ± 0.19 (mean ± 1 SE) and 1.89 ± 0.13 μmol CO₂ m⁻² s⁻¹ in the barley and Walker plots, respectively. However, biomass production was higher in the barley plots, indicating that the agricultural land-use system had a greater ability to fix atmospheric CO₂. The C balance in the land-use systems were estimated to be a small net gain (before considering straw and grain removal through harvesting) of 0.03 ± 0.187 Mg C ha⁻¹ year⁻¹ in the barley plots and a net loss of 3.35 ± 0.080 Mg C ha⁻¹ year⁻¹ from the Walker poplar plots. Over the long-term, we expect the hybrid poplar plantation to become a net C sink as the trees grow bigger and net primary productivity increases.     

不同恢复方式下大兴安岭重度火烧迹地林地土壤温室气体通量

为研究大兴安岭重度火烧迹地在不同恢复方式下林地土壤CO₂、CH₄和N₂O排放特征及其影响因素,采用静态箱/气相色谱法,在2017年生长季（6月-9月）对3种恢复方式（人工更新、天然更新和人工促进天然更新）林地土壤温室气体CO₂、CH₄、N₂O通量进行了原位观测。研究结果表明：（1）3种恢复方式林地土壤在生长季均为大气CO₂、N₂O的源,CH₄的汇;生长季林地土壤CO₂排放通量大小关系为人工促进天然更新（（634.40±246.52）mg m^-2 h^-1） > 人工更新（（603.63±213.22）mg m^-2 h^-1） > 天然更新（（575.81±244.12）mg m^-2 h^-1）,3种恢复方式间无显著差异;人工更新林地土壤CH₄吸收通量显著高于人工促进天然更新;天然更新林地土壤N₂O排放通量显著高于其他两种恢复方式。（2）土壤温度是影响3种恢复方式林地土壤温室气体通量的关键因素;土壤水分仅对人工更新林地土壤N₂O通量有极显著影响（P < 0.01）;3种恢复方式林地土壤CO₂通量与大气湿度具有极显著的响应（P < 0.01）;土壤pH仅与天然更新林地土壤CO₂通量显著相关（P < 0.05）;土壤全氮含量仅与人工促进天然更新林地土壤CH₄通量显著相关（P < 0.05）。（3）基于100年尺度,由3种温室气体计算全球增温潜势得出,人工促进天然更新（1.83×10⁴ kg CO₂/hm²） > 人工更新（1.74×10⁴ kg CO₂/hm²） > 天然更新（1.67×10⁴ kg CO₂/hm²）。（4）阿木尔地区林地土壤年生长季CO₂和N₂O排放量为8.85×10⁶ t和1.88×10² t,CH₄吸收量为1.05×10³ t。     

土壤氮水交互对马尾松和杉木COS和CO2通量的影响

羰基硫(COS)和CO_2化学结构相似,且植物对COS和CO_2具有共吸收特性,因此可利用COS作为示踪物来估算生态系统总初级生产力,而不同植物吸收COS和CO_2对环境因子变化的响应差异较大。以南亚热带典型树种马尾松(Pinus massoniana)和杉木(Cunninghamia lanceolata)为研究对象,设置2个氮水平及3个土壤水分梯度处理。采取顶空套袋法采集气体样品,用预浓缩—气质联用仪分析样品COS浓度,同时测量植物光合参数。结果表明:马尾松和杉木吸收COS,吸收速率均值分别为39.58—127.27 pmol m~(-2) s~(-1)和0.81—66.92 pmol m~(-2) s~(-1)。整体而言,施氮可促进植物吸收COS,但除施氮对马尾松COS通量有显著影响外(P0.05),施氮、土壤水分和两者交互作用对马尾松和杉木的COS和CO_2通量及其比值均无显著性影响。施氮情况下,高土壤水分处理促进马尾松COS吸收而低土壤水分处理促进杉木COS吸收。中等土壤水分和高土壤水分条件下马尾松和杉木COS通量与气孔导度呈正相关关系。线性拟合结果表明,植物COS通量(F_(COS))与CO_2通量(F_(CO_2))呈极显著正相关(P0.01),马尾松和杉木F_(COS)/F_(CO_2)值分别为1.48×10~(-6)和1.01×10~(-6)。中等土壤水分条件均可提高马尾松F_(COS)/F_(CO_2)比值,而低土壤水分条件下施氮增加杉木F_(COS)/F_(CO_2)比值,高土壤水分条件下施氮降低杉木F_(COS)/F_(CO_2)比值。低土壤水分和高土壤水分使马尾松蒸汽压亏缺增大,促使气孔导度减小从而降低净光合速率。低土壤水分和高土壤水分下施氮导致杉木气孔导度增加从而增强净光合速率。研究结果不仅对进一步了解区域氮沉降和降水对树木COS通量及F_(COS)/F_(CO_2)的影响有重要意义,而且可为模型估算总初级生产力提供区域性数据支持。     

CARBON SKELETON SOURCES FOR AMMONIUM ASSIMILATION IN N-SUFFICIENT AND N-LIMITED CELLS OF CYANIDIUM CALDARIUM (RHODOPHYTA)1

The possible origin of carbon skeletons for ammonium assimilation in Cyanidium caldarium (Tilden) Geitler was investigated. N-sufficient cells assimilated ammonium at a rate of 182 ± 18 μmol·mL packed cell volume (pcv)^-1· h^-1. Removal of CO₂ or darkening almost immediately prevented ammonium assimilation. N-limited cells in light assimilated ammonium at a rate of 493 ± 45 μmol · mL pcv^-1· h^-1 in the presence of CO₂ and at a lower rate of 168 ± 17 μmol · mL pcv^-1· h^-1 in the absence of CO₂. In darkness they assimilated ammonium at a rate of 293 ± 29 μmol · mL pcv^-1 h^-1 in the presence of CO₂, only 60% of the assimilation rate in light. In the absence of CO₂, ammonium was assimilated at a similar rate of 325 ± 14 μmol · mL pcv^-1· h^-1. Under the latter conditions, however, assimilation was inhibited after 40 min and ceased after 70 min; it resumed upon resupply of CO₂. We suggest that N-sufficient cells of C. caldarium obtain carbon skeletons for ammonium assimilation exclusively by photosynthetic reactions. Upon N-limitation they develop the ability, apparently through derepression or activation of regulatory enzyme system(s), to obtain a consistent quantity of additional carbon skeletons and ATP from mobilization of carbon reserves. This enables the N-limited cell to assimilate ammonium not only in light but also in darkness, and at a higher rate than N-sufficient cells. The fact that ammonium assimilation in light occurs at a higher rate than in darkness suggests that ammonium assimilation in light is the sum of both light and dark ammonium assimilation, which implies separate metabolic reactions for the two processes. These results suggest the existence of two distinct and differently controlled pathways in N-limited cells, but not in N-sufficient cells, through which carbon skeletons for ammonium assimilation originate. An important role for dark CO₂ fixation in dark or light ammonium assimilation is also indicated.