氮输入和水淹对短叶茳芏生长、养分及固碳的影响

外源氮输入显著改变河口湿地植物生长和固碳能力,进而影响河口湿地生态系统碳、氮循环过程。以闽江口湿地土著种短叶茳芏(Cyperus malaccensis)为研究对象,通过15个月的中型生态系实验,分析不同氮输入水平(CK,0 g N m~(-2)a~(-1);N8,8 g N m~(-2)a~(-1);N16,16 g N m~(-2)a~(-1))和2种水淹(T1,每天水淹时长2—3 h;T2,每天水淹时长11—12 h)处理对短叶茳芏生长、养分和固碳的影响,探讨短叶茳芏在环境变化下的生长、固碳特征。结果表明:T2处理株高极显著高于T1处理,N8、N16处理的植物株高显著高于CK处理,植物成熟季节的株高也极显著最高(P0.001)。水淹状况和植物生长期对短叶茳芏的密度有显著影响:T1处理密度极显著高于T2处理,植物成熟季节的密度也极显著最高(P0.001),但是氮输入没有显著提高植物密度。植物碳含量较为稳定,T2处理地上碳含量显著高于T1处理(P0.05),但是氮输入和植物生长期对地上碳含量影响不显著。氮输入水平、水淹状况和植物生长期则对植物地上氮含量都有显著影响(P0.05)。N8处理的植物地上生物量和固碳量极显著最高,CK处理极显著最低,植物成熟期的地上生物量和固碳量也极显著最大(P0.001),但是不同水淹处理植物生物量和固碳量无显著差异。闽江口湿地短叶茳芏具有较强的环境适应能力,在持续氮输入环境下,闽江口湿地的短叶茳芏可能向高潮滩拓展。     

植物光合碳和氮代谢之间的关系及其调节

概述了植物体内光合碳、氮代谢之间的相互作用及其代谢调控等方面的研究进展。     

浙北地区常见绿化树种光合固碳特征

高固碳能力的树种选择是营造优质碳汇林,发展碳汇林业的重要基础工作.以浙北地区常见的30种造林绿化树种为研究材料,利用LI-6400便携式光合测定仪,测定树木光合日变化及不同光强梯度下光合作用的光响应特性,并根据实验观测值进行计算,对30个树种的日净固碳量和光合生理拟合参数进行Ward法聚类分析和因子分析.结果表明:香樟的固碳量最大((11.374±1.020) g·m-2·d-1),其次为碧桃、垂柳、石栎、无患子,固碳量最小的为红叶李((2.178±0.605) g·m-2·d-1),香樟和红叶李的日净固碳量有极显著差异(P＜0.01);树木的生理特性指标分析进一步反映了树种在浙北地区生长适应性及固碳能力大小,同时,根据树木的生理特性指标进行因子分析和聚类分析的结果,香樟、碧桃在浙北地区生长适应性较好,其次为无患子、垂柳、女贞等;根据树种固碳量及生理指标综合测定分析,建议在浙北地区造林绿化中可以优先选用香樟、碧桃、垂柳、无患子、石栎、女贞这些树种.     

湛江5种红树林树种光合作用特性及光合固碳能力研究

应用Li-6400便携式光合作用测定系统,对湛江市特呈岛5种红树林树种的净光合速率日变化和光合作用—光响应曲线进行了测定,探讨了各树种的光合作用特性以及主要影响因子并评估其固碳能力大小。结果表明:在自然光照条件下,秋茄和红海榄叶片净光合速率(Pn)的日变化曲线呈单峰型,白骨壤、木榄和桐花树为双峰型,光合\"午休\"现象明显,而且峰值分别出现在10:00和14:00左右。其中,白骨壤和木榄的光合午休主要由气孔限制因素引起,桐花树主要由非气孔限制因素引起。通径分析表明,光合有效辐射(PAR)是影响白骨壤和桐花树叶片Pn的主要决策因子,而叶面大气蒸汽压亏缺(VPD)是主要限制因子;影响秋茄和红海榄叶片Pn的主要决策因子是气孔导度(Gs),主要限制因子是叶温(Tl);影响木榄叶片Pn的主要决策因子是气孔导度(Gs)。基于叶片净光合作用速率的各树种日净固碳量存在显著性差异(P0.01),秋茄的日净固碳量最大(13.83 g·m-2·d-1),其次为白骨壤和桐花树(9.48和8.24 g·m-2·d-1),木榄和红海榄的较小(6.72和6.30 g·m-2·d-1)。5种红树林树种的光补偿点(LCP)介于28.3~137.0μmol·m-2·s-1之间,显示了阳生植物的特性。光饱和点(LSP)介于169.3~1189.3μmol·m-2·s-1之间,桐花树最大,红海榄最小。5种红树林树种的表观量子效率(AQY)存在极显著差异(P0.01),白骨壤最高为0.064 mol·mol-1,木榄最低,仅为0.005 mol·mol-1。5种红树林植物叶片的光响应参数与日净固碳量的关联度大小顺序为最大净光合速率(Pmax)、LSP-LCP、AQY、LSP、LCP。     

氮沉降对森林生态系统碳吸存的影响

工业化带来的大气氮沉降增加是影响森林生态系统碳吸存的重要因素。将森林碳库分为地上和地下两部分,从3个方面综述了国内外氮沉降对森林生态系统碳吸存影响的研究现状。(1)地上部分:氮限制的温带森林,氮沉降增加了地上部分碳吸存。氮丰富的热带森林,氮沉降对地上部分碳吸存没有影响。过量的氮输入会造成森林死亡率的上升,从而降低地上部分碳吸存。(2)地下部分:相比地上部分研究得少,表现为增加、降低和没有影响3种效果。(3)目前的结论趋向于认为氮沉降促进森林生态系统碳吸存,然而氮沉降所带来的森林生态系统碳吸存能力到底有多大依然无法确定,这也将成为未来氮碳循环研究的重点问题。分析了氮沉降影响森林生态系统碳吸存的机理,介绍了氮沉降对森林生态系统碳吸存影响的4种研究方法。探讨了该领域研究的不足及未来的研究方向。     

非光合固碳微生物的碳源组合优化

二氧化碳(CO_2)过量排放而引起的全球变暖是目前全球面临的重大环境问题。微生物固碳是实现二氧化碳资源利用的一种重要方式。探索无需光照的高效固碳微生物对于更广泛环境条件下的微生物固碳具有重要意义。在从全球各大海域筛选富集出非光合微生物茵群的基础上,本文构建了在不同的电子供体条件下(铵和氢气)促进非光合微生物茵群生长的最佳混合碳源组合,得到如下结果:在以NH_4~+为电子供体的条件下,优化后的碳源组合为374.24 mgC/L碳酸钠(Na_2CO_3),54.76 mgC/L碳酸氢钠(NaHCO_3)和0 mgC/LCO_2时,最佳响应值TOC为3.06 mg/L。最佳响应值TOC低于以Na_2CO_3为单一碳源时,但高于以CO_2或NaHCO_3为单一碳源时;在以H_2为电子供体条件下,使用优化后的混合碳源为0.26 mg/L Na_2CO_3、0.59mg/L NaHCO_3和71.48mL/L CO_2时,非光合微生物菌群的固碳效率可达27.62 mg/L,较以CO_2为单一碳源提高35%左右。这可能意味着有H_2条件下非光合微生物菌群中的微生物可能以羟基丙酸固碳途径为主,而且多条固碳途径均能被混合菌群利用。     

农林复合系统固碳潜力研究进展

农林复合系统是解决当前资源枯竭、农林用地紧张和实现环境保护的一种可持续土壤管理模式。自《京都议定书》签订以来, 农林复合系统因其较高的固碳潜力引起了科学家的广泛关注。深入理解农林复合系统的固碳过程及其对气候变化、环境条件的改变和管理措施的响应, 是准确地预测农林复合系统在全球变化情景下固碳潜力的关键。该文综述了农林复合系统的概念和分类, 探讨了农林复合系统相比单一系统的固碳潜力及固碳机理, 分析了农林复合系统固碳潜力的测定方法和当前面临的挑战, 综述了气候因子、环境条件和人为管理措施对农林复合系统固碳潜力的影响。我国农林复合系统的固碳潜力相比全球其他区域还处于较低水平, 为提高我国农林复合系统的固碳潜力, 未来需要加强以下四个方面的工作: 扩大农林复合系统的分布面积、加强农林复合系统的合理配置和管理、选择适宜的物种组合和优化系统的群体结构。     

转C4光合固碳相关基因水稻的研究进展

近10年来,转C4光合固碳相关基因水稻的研究取得了长足进展,已受到国内外科学界的广泛关注。本文简要介绍并评述了有关方面的研究进展,包括水稻的C4光合固碳基因工程、转C4固碳相关基因水稻光合和光氧化的生理特性及转C4光合固碳相关基因水稻的生理育种3个方面：提出以常规育种和生物技术相结合,开展转C4光合固碳相关基因水稻的生理育种,是培育优质、高产超级稻的有效途径。     

转C4光合固碳相关基因水稻的研究进展

近10年来, 转C4光合固碳相关基因水稻的研究取得了长足进展, 已受到国内外科学界的广泛关注。本文简要介绍并评述了有关方面的研究进展, 包括水稻的C4光合固碳基因工程、转C4固碳相关基因水稻光合和光氧化的生理特性及转C4光合固碳相关基因水稻的生理育种3个方面; 提出以常规育种和生物技术相结合, 开展转C4光合固碳相关基因水稻的生理育种, 是培育优质、高产超级稻的有效途径。     

非光合固碳微生物菌群的耐盐特性及其影响因素

从海洋中分离驯化得到的非光合固碳微生物菌群(NPMC)是无需光照和供氢的化能自养微生物,若能用于贫瘠盐碱地改良,实现其在盐碱土壤中的二次固碳,对于盐碱土壤的低碳化改良具有重要的意义.本实验初步验证了NPMC的耐盐特性,以及微量元素和磷酸盐缓冲液两单因素在次高盐条件下对NPMC固碳效率的影响.并通过响应面法研究了微量元素与盐浓度对NPMC固碳效率的交互作用.结果表明,非光合固碳微生物拥有耐受高盐浓度的特性,可耐受高达100g/L以上的总盐度,因此可用于重盐碱土壤的改良.微量元素和磷酸盐缓冲液浓度的增加,都可增强NPMC的固碳效率,微量元素的促进效应高于磷酸盐缓冲液.微量元素和盐度对NPMC固碳效率的影响存在交互作用.     

Feedback of carbon and nitrogen cycles enhances carbon sequestration in the terrestrial biosphere

The efforts to explain the ‘missing sink’ for anthropogenic carbon dioxide (CO₂) have included in recent years the role of nitrogen as an important constraint for biospheric carbon fluxes. We used the Nitrogen Carbon Interaction Model (NCIM) to investigate patterns of carbon and nitrogen storage in different compartments of the terrestrial biosphere as a consequence of a rising atmospheric CO₂ concentration, in combination with varying levels of nitrogen availability. This model has separate but closely coupled carbon and nitrogen cycles with a focus on soil processes and soil–plant interactions, including an active compartment of soil microorganisms decomposing litter residues and competing with plants for available nitrogen. Biological nitrogen fixation is represented as a function of vegetation nitrogen demand. The model was validated against several global datasets of soil and vegetation carbon and nitrogen pools. Five model experiments were carried out for the modeling periods 1860–2002 and 2002–2100. In these experiments we varied the nitrogen availability using different combinations of biological nitrogen fixation, denitrification, leaching of soluble nitrogen compounds with constant or rising atmospheric CO₂ concentrations. Oversupply with nitrogen, in an experiment with nitrogen fixation, but no nitrogen losses, together with constant atmospheric CO₂, led to some carbon sequestration in organismic pools, which was nearly compensated by losses of C from soil organic carbon pools. Rising atmospheric CO₂ always led to carbon sequestration in the biosphere. Considering an open nitrogen cycle including dynamic nitrogen fixation, and nitrogen losses from denitrification and leaching, the carbon sequestration in the biosphere is of a magnitude comparable to current observation based estimates of the ‘missing sink.’ A fertilization feedback between the carbon and nitrogen cycles occurred in this experiment, which was much stronger than the sum of separate influences of high nitrogen supply and rising atmospheric CO₂. The demand‐driven biological nitrogen fixation was mainly responsible for this result. For the modeling period 2002–2100, NCIM predicts continued carbon sequestration in the low range of previously published estimates, combined with a plausible rate of CO₂‐driven biological nitrogen fixation and substantial redistribution of nitrogen from soil to plant pools.     

Acclimation response of spring wheat in a free-air CO2 enrichment (FACE) atmosphere with variable soil nitrogen regimes. 1. Leaf position and phenology determine acclimation response

We have examined the photosynthetic acclimation of wheat leaves grown at an elevated CO₂ concentration, and ample and limiting N supplies, within a field experiment using free-air CO₂ enrichment (FACE). To understand how leaf age and developmental stage affected any acclimation response, measurements were made on a vertical profile of leaves every week from tillering until maturity. The response of assimilation (A) to internal CO₂ concentration (C_i) was used to estimate the in vivo carboxylation capacity (Vc_max) and maximum rate of ribulose-1,5-bisphosphate limited photosynthesis (A _sat). The total activity of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco), and leaf content of Rubisco and the Light Harvesting Chlorophyll a/b protein associated with Photosystem II (LHC II), were determined. Elevated CO₂ did not alter Vc_max in the flag leaf at either low or high N. In the older shaded leaves lower in the canopy, acclimatory decline in Vc_max and A _sat was observed, and was found to correlate with reduced Rubisco activity and content. The dependency of acclimation on N supply was different at each developmental stage. With adequate N supply, acclimation to elevated CO₂ was also accompanied by an increased LHC II/Rubisco ratio. At low N supply, contents of Rubisco and LHC II were reduced in all leaves, although an increased LHC II/Rubisco ratio under elevated CO₂ was still observed. These results underscore the importance of leaf position, leaf age and crop developmental stage in understanding the acclimation of photosynthesis to elevated CO₂ and nutrient stress. This revised version was published online in June 2006 with corrections to the Cover Date.     

Combined effects of CO2 and light on large and small isolates of the unicellular N2-fixing cyanobacterium Crocosphaera watsonii from the western tropical Atlantic Ocean

We examined the combined effects of light and pCO₂ on growth, CO₂-fixation and N₂-fixation rates by strains of the unicellular marine N₂-fixing cyanobacterium Crocosphaera watsonii with small (WH0401) and large (WH0402) cells that were isolated from the western tropical Atlantic Ocean. In low-pCO₂-acclimated cultures (190 ppm) of WH0401, growth, CO₂-fixation and N₂-fixation rates were significantly lower than those in cultures acclimated to higher (present-day ～385 ppm, or future ～750 ppm) pCO₂ treatments. Growth rates were not significantly different, however, in low-pCO₂-acclimated cultures of WH0402 in comparison with higher pCO₂ treatments. Unlike previous reports for C. watsonii (strain WH8501), N₂-fixation rates did not increase further in cultures of WH0401 or WH0402 when acclimated to 750 ppm relative to those maintained at present-day pCO₂. Both light and pCO₂ had a significant negative effect on gross : net N₂-fixation rates in WH0402 and trends were similar in WH0401, implying that retention of fixed N was enhanced under elevated light and pCO₂. These data, along with previously reported results, suggest that C. watsonii may have wide-ranging, strain-specific responses to changing light and pCO₂, emphasizing the need for examining the effects of global change on a range of isolates within this biogeochemically important genus. In general, however, our data suggest that cellular N retention and CO₂-fixation rates of C. watsonii may be positively affected by elevated light and pCO₂ within the next 100 years, potentially increasing trophic transfer efficiency of C and N and thereby facilitating uptake of atmospheric carbon by the marine biota.     

木霉对盐渍逆境下枸杞根系氮素吸收和氮素利用效率的影响

本研究采集滨海盐渍土开展盆栽试验,分析施加有机肥、木霉菌剂及菌肥对枸杞氮素吸收、同化、积累和利用效率的影响,以揭示木霉对盐渍逆境下枸杞的促生机理。有机肥为木霉菌肥的灭菌物,不含木霉活菌,但两者氮、磷、钾等养分含量无显著差异。结果表明: 施加有机肥、木霉菌剂和菌肥处理较对照均显著提高了根系分生区NO₃^-、NH₄⁺内流速率和成熟区NO₃^-内流速率,且施加菌肥的提升幅度高于施加有机肥。与对照相比,盐渍土壤施加木霉菌剂及菌肥显著增加了根、茎、叶生物量和氮含量以及植株氮累积量,增强了枸杞根和叶中硝酸还原酶、亚硝酸还原酶和谷氨酰胺合成酶活性,提高了枸杞氮素吸收效率、光合速率、稳定碳同位素丰度值和光合氮素利用效率,而且施加菌肥的效果明显优于施加有机肥。综上,木霉能增强盐渍逆境下枸杞氮素吸收、同化和积累,提升光合固碳能力和氮素利用效率,最终促进植株生长。     

The effects of elevated CO2 on symbiotic N2 fixation: a link between the carbon and nitrogen cycles in grassland ecosystems

The response of plants to elevated CO₂ is dependent on the availability of nutrients, especially nitrogen. It is generally accepted that an increase in the atmospheric CO₂ concentration increases the C:N ratio of plant residues and exudates. This promotes temporary N-immobilization which might, in turn, reduce the availability of soil nitrogen. In addition, both a CO₂ stimulated increase in plant growth (thus requiring more nitrogen) and an increased N demand for the decomposition of soil residues with a large C:N will result under elevated CO₂ in a larger N-sink of the whole grassland ecosystem. One way to maintain the balance between the C and N cycles in elevated CO₂ would be to increase N-import to the grassland ecosystem through symbiotic N₂ fixation. Whether this might happen in the context of temperate ecosystems is discussed, by assessing the following hypothesis: i) symbiotic N₂ fixation in legumes will be enhanced under elevated CO₂, ii) this enhancement of N₂ fixation will result in a larger N-input to the grassland ecosystem, and iii) a larger N-input will allow the sequestration of additional carbon, either above or below-ground, into the ecosystem. Data from long-term experiments with model grassland ecosystems, consisting of monocultures or mixtures of perennial ryegrass and white clover, grown under elevated CO₂ under free-air or field-like conditions, supports the first two hypothesis, since: i) both the percentage and the amount of fixed N increases in white clover grown under elevated CO₂, ii) the contribution of fixed N to the nitrogen nutrition of the mixed grass also increases in elevated CO₂. Concerning the third hypothesis, an increased nitrogen input to the grassland ecosystem from N₂ fixation usually promotes shoot growth (above-ground C storage) in elevated CO₂. However, the consequences of this larger N input under elevated CO₂ on the below-ground carbon fluxes are not fully understood. On one hand, the positive effect of elevated CO₂ on the quantity of plant residues might be overwhelming and lead to an increased long-term below-ground C storage; on the other hand, the enhancement of the decomposition process by the N-rich legume material might favour carbon turn-over and, hence, limit the storage of below-ground carbon.