植物光合作用对大气CO2浓度升高的反应

近年来大气中ＣＯ２浓度急剧增加使人们重新对研究ＣＯ２浓度升高对植物光合作用影响感兴趣。预计在未来的１００ａ中,大气ＣＯ２浓度还将不断增长并达到当今的２倍。ＣＯ２排放量的增加不仅加剧了地球上的温室效应,也将改变全球生态系统中碳的平衡。离浓度ＣＯ２对植物光剑作用的影响表现为短期和长期效应。短时间地供给高浓度ＣＯ２促进阿 光合作用,而长时间生长在高浓度ＣＯ２下抒使某些植物光合能力下降,出现了光合适应现象     

CO2 浓度升高对水稻根系分泌物的影响——总有机碳、甲酸和乙酸含量变化

在大气ＣＯ２浓度升高条件下采用水培方法对水稻根系生长及根系分泌物进行了初步研究,ＣＯ２浓度倍增对水培水稻的根系生长具有明显的促进作用,约为７０％,但是根冠比却有所降低,水稻根系单位干重总有机碳,乙酸以及甲酸的释放量在ＣＯ２浓度倍增条件下变化不明显,但是单株奶系分泌物总量,乙酸以及甲酸的释放总量在ＣＯ２倍增处理下明显增加,推测水稻根系分泌物的增加是高浓度ＣＯ２下稻田ＣＨ４排放增加的重要原因之一。     

几种热带雨林与荒漠植物暗呼吸作用对高CO_2浓度的响应

使用 Ｌ Ｉ６４００ 便携式光合作用测定系统测定了美国生物圈二号内长期生长在高 Ｃ Ｏ２ 浓度（＞ １５００μｍ ｏｌ／ｍ ｏｌ）下 ５种热带雨林植物与 ５ 种荒漠植物暗呼吸强度的变化。结果表明：在 ３５０～４００μｍ ｏｌ／ｍ ｏｌ下 ５ 种雨林植物的平均暗呼吸强度为（０５６±０１９）μｍ ｏｌ Ｃ Ｏ２／ｍ ２·ｓ;荒漠植物平均为（０９８±０７２）μｍ ｏｌ Ｃ Ｏ２／ｍ ２·ｓ。在 Ｃ Ｏ２ 浓度升高时大部分 Ｃ３ 植物暗呼吸作用升高,并呈一定的线形关系。当 Ｃ Ｏ２ 浓度加倍时,雨林植物暗呼吸强度升高６１％ ;荒漠 Ｃ３ 植物升高１３４％ ,而 Ｃ４ 植物变化不明显或略有下降。因而认为,长期高 Ｃ Ｏ２ 浓度可促进 Ｃ３ 植物的暗呼吸作用。     

大气CO_2浓度升高对植物的直接影响——国外十余年来模拟实验研究之主要手段及基本结论

本文针对国外近十几年来在ＣＯ２浓度升高对植物的直接影响方面所开展的生理生态学研究方法、动态、基本结论、存在问题等内容做了简要的介绍。大气ＣＯ２浓度在过去２００年内已增加了８０μｍｏｌ·ｍｏｌ－１,生长在高ＣＯ２环境下的植物,其生理生态、形态及化学成分等方面将会发生相应的变化。表现在光合作用速率出现不同程度的提高;呼吸作用受抑制;气孔密度减少,水分利用效率增加;生物量及产量增加;一些关键蛋白质及酶、非结构性碳水化合物含量增加;组织中的氮、硫等元素含量降低;根系及花的发育也随ＣＯ２浓度的升高而提前等。不同光合途径（Ｃ３、Ｃ４及ＣＡＭ）及不同植被类型（自然植被、栽培植被）的植物随ＣＯ２浓度发生的上述指标的变化在长期反应与短期反应方面具有很大的差异。另外,实验控制条件如温度、光照、水分、养分甚至实验装置（如花盆）的大小对预测结果也有很大的影响。     

提高CO2浓度对两种亚热带树苗光合作用的影响

鼎湖山季风常绿阔叶林的主要优势乔木树种裂壳锥（Ｃａｓｔａｎｏｐｓｉｓｆｉｓｓａ （Ｃｈａｍ ｐ．ｅｘ Ｂｅｎｔｈ．） Ｒｅｈｄ．ｅｔＷｉｌｓ．）和荷木（Ｓｃｈｉｍ ａ ｓｕｐｅｒｂａ Ｇａｒｄｎ．ｅｔＣｈａｍ ｐ．）幼苗,盆栽于自然条件（ＣＯ２ 浓度３５０ μＬ·Ｌ－ １）或高ＣＯ２ 浓度为５００ μＬ·Ｌ－ １和空气ＣＯ２（３５０ μＬ·Ｌ－ １）的半开顶式气罩中。在生长最旺盛的６～９ 月份,高浓度ＣＯ２ 条件下生长的叶片,其光合速率比在自然条件下生长的提高７９％ ～９５％ 。当叶片在３５０ μＬ·Ｌ－ １和５００ μＬ·Ｌ－ １的ＣＯ２ 浓度下测定时,其光合速率无明显差异。高浓度ＣＯ２ 下生长的叶片其光合速率－ＣＯ２ 浓度响应曲线比对照（３５０ μＬ·Ｌ－ １）高,叶绿素和类胡萝卜素含量低,但叶绿素ａ 和ｂ 的比值及类胡萝卜素和叶绿素的比值不变。高浓度ＣＯ２ 下生长的叶片气孔导度明显降低。两种植物在８５ ｄ 的高浓度ＣＯ２ 的生长过程中,并未出现光合速率下调现象     

大气CO2浓度升高与森林群落结构的可能性变化

大气ＣＯ２浓度升高的所引起的森林生态系统稳定性的变化会导致森林在结构和功能上的变动,概述了大气ＣＯ２浓度升高和陆地森林生态系统可能性变化之间的相互关系的研究情况。由于大气ＣＯ２浓度升高出现了额外多的Ｃ,供应,讨论了以这些额外多的Ｃ经大气－植物－土壤途径的流动走向,来研究大气ＣＯ２浓度的升高,与森林结构的相互作用,探讨了大气ＣＯ２浓度升高对森林植物生长、冠层结构、引发的生物量增量的分配、凋落物质量和     

大气CO2浓度和温度升高对水稻叶片及群体光合作用的影响

大气ＣＯ２浓度升高对植物光合作用的影响研究多集中在单叶水平,在高ＣＯ２及高温下对植物单叶及群体光合进行比较的研究少有报道,而群体水平的研究则是预测生态系统反应所不可缺少的。采用田间开顶式培养室研究了大气ＣＯ２浓度和温度升高对水稻（ＯｒｙｚａｓａｔｉｖａＬ．）叶片及群体光合作用的影响。发现ＣＯ２浓度和温度对水稻叶片光合作用有协同促进作用,而对群体光合作用的促进则随时间的推移而减弱;单叶光合受到的促进作用大于群体光合;叶面积指数只在营养生长期受到促进,冠层叶片含氮量受ＣＯ２影响降低。群体呼吸（包括茎杆）增加及冠层叶片早衰可能是后期ＣＯ２对群体光合促进作用下降的原因。     

大气中二氧化碳浓度升高对光合作用的影响(下)

ＣＯ２浓度加倍对光合色素含量的影响ＣＯ２浓度加倍有利于植物叶片单位鲜重或单位叶面积的叶绿素和类胡萝卜素含量的提高。叶绿素含量的提高,显然有助于植物捕获更多光能供光合作用所利用。因为在ＣＯ２浓度加倍条件下,植物要充分利用环境资源,增加对ＣＯ２的同化,需要通过增加叶片叶绿素的含量,或扩大叶面积来提高对光能的捕获能力,以满足碳同化时能量的需求。此外,ＣＯ２浓度加倍;能降低叶绿素ａ／ｂ比值,说明它更有利形成叶绿素ｂ。以含等量叶绿素的叶绿体所作的实验表明,来自生长在ＣＯ２浓度加倍条件下的植物叶绿体,对光能…     

植物暗呼吸作用对大气CO2浓度升高的响应

植物暗呼吸作用对ＣＯ２浓度升高的响应目前存在两种截然相反的观点：一种认为暗呼吸作用将随着ＣＯ２浓度的升高而下降,可能的原因有胞间ＣＯ２浓度升高、呼吸酶活性改变及暗固定ＣＯ２作用的加强等直接原因;另一种认为暗呼吸作用将随ＣＯ２浓度的升高而提高,影响因素可归结为碳水化合物含量增加、高ＣＯ２浓度刺激其他呼吸途径和生长加快等间接原因。由于目前国际上在实验手段、材料及呼吸作用表达方式等方面的不一致性,这些观点尚难定论,需要更多的实验数据来进一步验证。     

高CO2浓度下豆科4种乔木幼苗的生理生化反应

本文对４种豆科乔木幼苗在高ＣＯ２浓度（５５０×１０－６±５０×１０－６）和在对照ＣＯ２浓度（约为３５０×１０－６）下生长的幼苗的一些生理生化指标进行了比较研究。初步结果显示：高ＣＯ２浓度能缩短幼苗子叶的存活时间。高ＣＯ２环境下生长的４种幼苗叶片中的可溶性蛋白、可溶性糖、纤维素、Ｎ、Ｐ、Ｋ、Ｍｇ的含量（均为全量）较对照ＣＯ２环境下生长的幼苗的相应值低,而淀粉含量则较高。其中以全氮、可溶性糖差异较显著。以单位鲜重表示的幼苗叶片叶绿素（Ｃｈｌ）和类胡萝卜素（Ｃａｒ）含量降低。高ＣＯ２浓度下生长的４种幼苗（３０天龄）叶片中硝酸还原酶活性比对照ＣＯ２浓度下生长的幼苗的值低。高ＣＯ２浓度下生长的４种幼苗叶片的平均蒸腾速率有不同程度的降低,而气孔阻力升高。幼苗对高ＣＯ２环境的反应与种的生态特性有关。喜光的大叶合欢幼苗对高ＣＯ２环境的反应较大,喜光而具一定耐荫性的猴耳环幼苗次之,而耐荫的光叶红豆和茸荚红豆幼苗则较小     

Atmospheric CO(2) and mycorrhiza effects on biomass allocation and nutrient uptake of nodulated pea (Pisum sativum L.) plants

The effect of ambient and elevated atmospheric CO(2) on biomass partitioning and nutrient uptake of mycorrhizal and non-mycorrhizal pea plants grown in pots in a controlled environment was studied. The hypothesis tested was that mycorrhizae would increase C assimilation by increasing photosynthetic rates and reduce below-ground biomass allocation by improving nutrient uptake. This effect was expected to be more pronounced at elevated CO(2) where plant C supply and nutrient demand would be increased. The results showed that mycorrhizae did not interact with atmospheric CO(2) concentration in the variables measured. Mycorrhizae did not affect photosynthetic rates, had no effect on root weight or root length density and almost no effect on nutrient uptake, but still significantly increased shoot weight and reduced root/shoot ratio at harvest. Elevated CO(2) increased photosynthetic rates with no evidence for down-regulation, increased shoot weight and nutrient uptake, had no effect on root weight, and actually reduced root/shoot ratio at harvest. Non-mycorrhizal plants growing at both CO(2) concentrations had lower shoot weight than mycorrhizal plants with similar nutritional status and photosynthetic rates. It is suggested that the positive effect of mycorrhizal inoculation was caused by an enhanced C supply and C use in mycorrhizal plants than in non-mycorrhizal plants. The results indicate that plant growth was not limited by mineral nutrients, but partially source and sink limited for carbon. Mycorrhizal inoculation and elevated CO(2) might have removed such limitations and their effects on above-ground biomass were independent, positive and additive.     

Rhizosphere interactions, carbon allocation, and nitrogen acquisition of two perennial North American grasses in response to defoliation and elevated atmospheric CO2

Carbon allocation and N acquisition by plants following defoliation may be linked through plant-microbe interactions in the rhizosphere. Plant C allocation patterns and rhizosphere interactions can also be affected by rising atmospheric CO(2) concentrations, which in turn could influence plant and microbial responses to defoliation. We studied two widespread perennial grasses native to rangelands of western North America to test whether (1) defoliation-induced enhancement of rhizodeposition would stimulate rhizosphere N availability and plant N uptake, and (2) defoliation-induced enhancement of rhizodeposition, and associated effects on soil N availability, would increase under elevated CO(2). Both species were grown at ambient (400 μL L(-1)) and elevated (780 μL L(-1)) atmospheric [CO(2)] under water-limiting conditions. Plant, soil and microbial responses were measured 1 and 8 days after a defoliation treatment. Contrary to our hypotheses, we found that defoliation and elevated CO(2) both reduced carbon inputs to the rhizosphere of Bouteloua gracilis (C(4)) and Pascopyrum smithii (C(3)). However, both species also increased N allocation to shoots of defoliated versus non-defoliated plants 8 days after treatment. This response was greatest for P. smithii, and was associated with negative defoliation effects on root biomass and N content and reduced allocation of post-defoliation assimilate to roots. In contrast, B. gracilis increased allocation of post-defoliation assimilate to roots, and did not exhibit defoliation-induced reductions in root biomass or N content. Our findings highlight key differences between these species in how post-defoliation C allocation to roots versus shoots is linked to shoot N yield, but indicate that defoliation-induced enhancement of shoot N concentration and N yield is not mediated by increased C allocation to the rhizosphere.     

Emission of Plutella xylostella-induced compounds from cabbages grown at elevated CO2 and orientation behavior of the natural enemies

Several plant species defend themselves indirectly from herbivores by producing herbivore-induced volatile compounds that attract the natural enemies of herbivores. Here we tested the effects of elevated atmospheric CO(2) (720 micromol mol(-1)) concentration on this indirect defense, physiological properties, and constitutive and induced emissions of white cabbage (Brassica oleracea ssp. capitata, cvs Lennox and Rinda). We monitored the orientation behavior of the generalist predator Podisus maculiventris (Heteroptera: Pentatomidae) and the specialist parasitoid Cotesia plutellae (Hymenoptera: Braconidae) to plants damaged by Plutella xylostella (Lepidoptera: Plutellidae) in the Y-tube olfactometer. Elevated CO(2) levels did not affect stomatal densities but reduced specific leaf area and increased leaf thickness in cv Lennox. In addition to enhanced constitutive monoterpene emission, P. xylostella-damaged cabbages emitted homoterpene (E)-4,8-dimethyl-1,3,7-nonatriene, sesquiterpene (E,E)-alpha-farnesene, and (Z)-3-hexenyl acetate. Growth at elevated CO(2) had no significant effect on the emissions expressed per leaf area, while minor reduction in the emission of homoterpene (E)-4,8-dimethyl-1,3,7-nonatriene and (E,E)-alpha-farnesene was observed at elevated CO(2) in one of two experiments. The generalist predator P. maculiventris discriminated only between the odors of intact and P. xylostella-damaged cv Rinda plants grown at ambient CO(2) concentration, preferring the odor of the damaged plants. The specialist parasitoid C. plutellae preferred the odor of damaged plants of both cultivars grown at ambient CO(2) but did not detect damaged cv Lennox plants grown at elevated CO(2). The results suggest that elevated atmospheric CO(2) concentration could weaken the plant response induced by insect herbivore feeding and thereby lead to a disturbance of signaling to the third trophic level.     

大气二氧化碳浓度增加对木本植物BVOCs释放的影响

植物挥发性有机化合物(biogenic volatile organic compounds,BVOCs)在近地表臭氧和二次有机气溶胶生成中有重要作用,而大气CO2浓度上升对植物BVOCs释放有显著影响。利用Meta-analysis方法对已发表的数据进行整合分析发现:(1)总体而言,大气CO2浓度增加会导致不同木本植物(常绿与落叶)BVOCs释放降低;(2)就不同木本植物BVOCs释放而言,大气CO2浓度增加主要导致落叶植物BVOCs释放速率降低,而常绿植物则以增加为主;(3)就植物释放BVOCs种类而言,大气CO2浓度增加显著降低异戊二烯的释放速率,对单萜烯释放速率则无显著影响。结果可为阐明陆地生态系统BVOCs释放对全球CO2浓度增加的响应提供依据。     

大气CO2浓度升高和N沉降对南亚热带主要乡土树种叶片元素含量的影响

大气CO₂浓度升高和N沉降以及二者之间的耦合作用对陆地森林生态系统的影响是当前国际生态学界关注的热点之一。该实验运用大型开顶箱(open-top chamber, OTC)研究: 1)高CO₂浓度(700 μmol×mol^-1) +高N沉降(100 kg N×hm^-2×a^-1) (CN); 2)高CO₂浓度(700 μmol×mol^-1)和背景N沉降(CC); 3)高N沉降(100 kg N×hm^-2×a^-1)和背景CO₂浓度(NN); 4)背景CO₂和背景N沉降(CK) 4种处理对南亚热带主要乡土树种木荷(Schima superba)、红锥(Castanopsis hystrix)、肖蒲桃(Acmena acuminatissima)、红鳞蒲桃(Syzygium hancei)、海南红豆(Ormosia pinnata)叶片元素含量的影响。研究结果表明, 大气CO₂浓度升高对5种乡土树种叶片元素含量有较大的影响, 除海南红豆叶片的Ca含量外, 其他树种的叶片元素含量在高CO₂浓度处理下都显著升高(p < 0.05); 而在N沉降处理下, 5个树种的叶片K和Ca含量都降低。大气CO₂浓度升高与N沉降处理对5种乡土树种植物叶片元素含量影响的交互作用不是很明显, 仅仅木荷和红鳞蒲桃的叶片Ca和Mn以及海南红豆的叶片Mn含量在大气CO₂浓度上升和N沉降交互处理下显著下降, 而肖蒲桃的叶片P含量在大气CO₂浓度上升和N沉降交互处理下显著上升。     

Photosynthetic acclimation to rising atmospheric carbon dioxide concentration

With rising level of CO2 in the atmosphere plants are expected to be exposed to higher concentration of CO2. Since, CO2 is a substrate limiting photosynthesis particularly in C3 plants in the present atmosphere, the impact of elevated CO2 would depend mainly on how photosynthesis acclimates or adjusts to the long term elevated level of CO2. Photosynthetic acclimation is a change in photosynthetic efficiency of leaves due to long term exposure to elevated CO2. This change in photosynthetic efficiency could be a biochemical adjustment that may improve the overall performance of a plant in a high CO2 environment or it could be due to metabolic compulsions as a result of physiological dysfunction. Acclimation has generally become synonymous with the word response, if long term exposure to elevated CO2 decreases the photosynthesis rate (Pn) at a given CO2 level, it is called negative acclimation, if it stimulates Pn at a given CO2 level, it is called positive acclimation. Photosynthetic acclimation is clearly revealed by comparing Pn of ambient and elevated CO2 grown plants at same level of CO2. Species level differences in acclimation to elevated CO2 have been reported. The physiological basis of differential photosynthetic acclimation to elevated CO2 is discussed in relation to the regulation of photosynthesis and photosynthetic carbon partitioning at cellular level.     

水华鱼腥藻生长与光合作用对大气CO2浓度升高的响应

 为了探讨大气CO2浓度升高对水华藻类的影响,利用水华鱼腥藻(Anabena flos_aquae)作为实验材料,研究了大气CO2浓度加倍对其生长和光合作用的影响,结果显示大气CO2浓度升高导致水华鱼腥藻的生物量、光饱和光合速率、光合效率和光系统II的光化学效率（Fv/Fm）明显提高,但对暗呼吸速率和光饱和点没有明显影响。CO2加倍条件下藻细胞光合作用对无机碳的亲和力降低,表明其利用HCO-3的能力受到抑制。     

Auxin modulates the enhanced development of root hairs in Arabidopsis thaliana (L.) Heynh. under elevated CO(2)

Root hairs may play a critical role in nutrient acquisition of plants grown under elevated CO(2) . This study investigated how elevated CO(2) enhanced the development of root hairs in Arabidopsis thaliana (L.) Heynh. The plants under elevated CO(2) (800 μL L(-1)) had denser and longer root hairs, and more H-positioned cells in root epidermis than those under ambient CO(2) (350 μL L(-1)). The elevated CO(2) increased auxin production in roots. Under elevated CO(2) , application of either 1-naphthoxyacetic acid (1-NOA) or N-1-naphthylphthalamic acid (NPA) blocked the enhanced development of root hairs. The opposite was true when the plants under ambient CO(2) were treated with 1-naphthylacetic acid (NAA), an auxin analogue. Furthermore, the elevated CO(2) did not enhance the development of root hairs in auxin-response mutants, axr1-3, and auxin-transporter mutants, axr4-1, aux1-7 and pin1-1. Both elevated CO(2) and NAA application increased expressions of caprice, triptychon and rho-related protein from plants 2, and decreased expressions of werewolf, GLABRA2, GLABRA3 and the transparent testa glabra 1, genes related to root-hair development, while 1-NOA and NPA application had an opposite effect. Our study suggests that elevated CO(2) enhanced the development of root hairs in Arabidopsis via the well-characterized auxin signalling and transport that modulate the initiation of root hairs and the expression of its specific genes.     

Elevated CO2, rhizosphere processes,and soil organic matter decomposition

The rhizosphere is one of the key fine-scale components of C cycles. This study was undertaken to improve understanding of the potential effects of atmospheric CO2 increase on rhizosphere processes. Using C isotope techniques, we found that elevated atmospheric CO2 significantly increased wheat plant growth, dry mass accumulation, rhizosphere respiration, and soluble C concentrations in the rhizosphere. When plants were grown under elevated CO2 concentration, soluble C concentration in the rhizosphere increased by approximately 60%. The degree of elevated CO2 enhancement on rhizosphere respiration was much higher than on root biomass. Averaged between the two nitrogen treatments and compared with the ambient CO2 treatment, wheat rhizosphere respiration rate increased 60% and root biomass only increased 26% under the elevated CO2 treatment. These results indicated that elevated atmospheric CO2 in a wheat-soil system significantly increased substrate input to the rhizosphere due to both increased root growth and increased root activities per unit of roots. Nitrogen treatments changed the effect of elevated CO2 on soil organic matter decomposition. Elevated CO2 increased soil organic matter decomposition (22%) in the nitrogen-added treatment but decreased soil organic matter decomposition (18%) without nitrogen addition. Soil nitrogen status was therefore found to be important in determining the directions of the effect of elevated CO2 on soil organic matter decomposition.