东北草原区C3,C4植物的生态分布及其适应盐碱环境的生理特性

用５种实验方法对东北草原区２３３种植物光合类型进行鉴定,并对其相对分布 随纬度变化关系及其与土壤含盐量和ＰＨ值的关系进行分析．在此基础上对几种典型Ｃ３、 Ｃ４牧草适应于盐碱环境的生理特点进行深入研究结果表明,在所鉴定的２３３种植物中, Ｃ３植物有 １４４种,隶属于 ２８科 ９４属,Ｃ４植物有 ８９种;隶属于 １７科 ５５属,在高纬度地区 Ｃ３植物表现出更高的生长优势,在纬度较低和盐碱化区域,Ｃ４植物分布具相对优势．尤其 在盐碱化程度较重的地区,Ｃ４植物成为明显的优势种,分布上的差别决定于它们对环境 适应机制上的差异Ｃ３植物对盐碱环境适应机制主要通过积累脯氨酸等有机溶质进行渗 透调节,而Ｃ４植物主要通过液泡中离子区域化积累作用进行调节,并且与Ｃ３植物相比对 盐碱环境具更强的适应能力．     

中国南亚热带和北温带地区禾本科C3与C4草本植物花果期差异研究

为揭示不同地区禾本科C₃与C₄植物花果期受气候因子的影响,以广东省和内蒙古自治区分别代表南亚热带和北温带地区,从植物志中分别获得两地395和265种禾本科草本植物的3个花果期特征(始花期、末花果期和生殖期长),比较开花物候的差异,并通过一般线性模型探究其与气候因子(年均温与年均降水量)的相关性。结果表明,南亚热带与北温带地区C₃植物的始花期均比C₄植物早。两地C₄共有种在南亚热带地区具有更早的始花期、更晚的末花果期和更长的生殖期,而C₃共有种的末花果期在两地无显著差异,但在南亚热带地区始花期更早,生殖期更长。随年均温升高,北温带地区禾本科植物的始花期提前,而南亚热带地区则延后;随年均降水量升高,两地禾本科植物始花期与末花果期均延迟;禾本科植物生殖期长与年均温和年均降水量均不存在相关性。跨地区分析表明,末花果期、生殖期长与年均温和年均降水量均正相关,而与始花期不相关。禾本科C₃植物比C₄植物对地区间气候差异响应更敏...     

开放式空气CO2浓度增高条件下C3作物(水稻)与C4杂草(稗草)的竞争关系

通过田间试验,研究了FACE(开放式空气CO₂浓度升高)条件下C₃作物水稻(Oryza sativa)和C₄杂草稗草(Echinochloa crusgalli)的生长和竞争关系.结果表明,FACE条件下C₃植物水稻生物量和产量增加,叶片数增加,分蘖数增加,叶面积系数(LAI)增大;而C₄植物稗草相反.FACE条件下水稻和稗草叶面积均减少,而净同化率(NAR)均增加.FACE条件下水稻稗草比例为1:1时,水稻与稗草的生物量比率、产量比率、LAI比率、茎蘖比率和NAR比率均增加,水稻稗草的竞争关系发生变化,水稻(C₃植物)竞争能力增加,稗草(C₄植物)竞争能力下降.     

开放式空气CO2浓度升高与作物/杂草的竞争关系

CO₂浓度升高对植物的光合作用、呼吸作用和水分利用等生理过程产生直接影响,进而影响植物的生长和繁殖.CO₂浓度升高对于具有C₃光合途径的植物较具C₄光合途径的植物更为有益.由于许多重要的杂草是C₄植物,而许多重要的作物是C₃植物,CO₂浓度升高对杂草/作物的相互关系将有重要影响.本文就全球CO₂浓度升高和气候变化对杂草/作物之间竞争关系影响进行综述,同时针对目前研究现状和可持续农业的需要,提出CO₂浓度升高条件下杂草/作物之间竞争关系及未来农田杂草治理方面理论与实践中有待解决的问题.     

东北草原区的C3,C4牧草及其生态分布的初步研究

本文用RuBPCase活性/PEPCase活性的比值,鉴定东北草原区牧草资源中C_3、C_4植物。供测定45种中35种为首次鉴定。辅助观察禾草类Kranz结构。在此基础上,对其中11种C_3、C_4优势牧草的地理分布、物候谱及其相对优势度与土壤pH值和含盐量之间的关系进行了研究。结果表明,C_3植物30种,隶属于10科24属,C_4植物15种,隶属于5科9属。与C_3植物相比,在高温、强光照和降水量大的季节,C_4植物显示其更高的相对生长优势,在纬度较低和盐碱化区域,C_4植物具有相对分布优势。C.4草相对优势度与土壤pH值和含盐量的相关系数分别为0.826和0.760,而C_3植物均为负值。     

Effects of plant intraspecific variation on the prediction of C3/C4 vegetation ratio from carbon isotope composition of topsoil organic matter across grasslands

植物种内变异对草地表层有机质碳同位素组成预测C₃/C₄植被比的影响植物群落中C₃和C₄植物的比例和组成对诸多生态系统过程具有重要影响。解析C₃和C₄植物碳同位素的环境驱动过程与调控因子,对于从土壤碳同位素的角度来预测C₃/C₄植被比和组成具有重要意义。本研究旨在评估草原植物碳同位素特征的种内变异将如何影响C₃和C₄植物的碳同位素组成以及C₃/C₄植被比的预测。沿中国北方草原的自然干旱梯度选择26个植物群落,通过分析植物和土壤的碳同位素组成,采用混合模型来预测C₄植物对土壤有机碳的相对贡献。本研究对比分析了如下3种情境：(1)考虑C₃和C₄植物碳同位素的种内和种间效应;(2)仅考虑碳同位素的种间变异;(3)忽略碳同位素的种内和种间变异。研究结果表明,植物碳同位素组成沿中国北方草原自然干旱梯度的变化具有物种特异性。C₃和C₄植物的碳同位素组成与干旱指数之间呈显著负相关关系,但C₃植物比C₄植物对环境的干旱变化更为敏感。植物碳同位素特征的种内变异在驱动C₃植物功能群碳同位素沿干旱梯度的分布格局中发挥着重要作用。如果忽略植物碳同位素特征的种内变异将会显著高估C₄植物的相对贡献。本研究结果表明,草原植物碳同位素特征的种内变异对于准确预测C₃/C₄植被组成具有重要意义。     

不同光合类型牧草对干旱-复水的光合生理响应及生长适应策略

基于干旱频率增加、强度增大这一全球降水变化背景, 探究干旱-复水条件下不同功能群(C₃和C₄)植物的光合生理响应及生长适应策略有助于预测降水格局变化条件下草地的植被组成和生态系统功能。该研究采用盆栽实验, 以松嫩草地生长的一年生C₃ (4种)和C₄ (3种)牧草为实验材料, 设置了对照、中度干旱和重度干旱3个水分处理水平, 在干旱末期及复水期对植物进行气体交换、生物量和比叶质量的测量。在干旱条件下, 各物种净光合速率和气孔导度均呈下降趋势, 水分利用效率呈上升趋势。干旱对不同植物光合指标的影响存在功能群差异, 随干旱程度的增加C₄植物逐渐丧失光合优势, 重度干旱对C₄植物净光合速率的影响较C₃植物更加明显。由于干旱条件下C₃植物光合固碳主要受气孔限制而C₄植物主要受代谢限制, 因此复水后C₄植物净光合速率恢复速度较C₃植物慢。干旱条件下, 各物种的生物量降低, 根冠比和比叶质量升高, 干旱对C₃植物各生长指标的影响均大于C₄植物; 复水处理后, C₃植物生物量随干旱强度增加呈下降趋势, 而C₄植物的生物量与对照相比无显著差异。     

中国东北草原植物中的C3和C4光合作用途径

以光合作用关键羧化酶ＰＥＰＣ和ＲｕＢＰＣ活性化,并且参照叶片ＣＯ补偿浓度,δ＾１３Ｃ值和叶片解剖结构特点来鉴定东北草原区２３３种植物的Ｃ３,或Ｃ４光全作用途径,这些植物隶属于１４４属７３科,其中１３７种为首次鉴定。８９种具有Ｃ４光合作用途径,隶属于５５属１７科;１４４种人有Ｃ３光俣作用途径;隶属于９４属２８在多数Ｃ４种分布在禾本科、莎草科、苋科和藜科。苋属、地肤属、狗昌属和虎尾草属中的均为Ｃ４植物     

C3与C4植物的环境调控

环境条件决定着不同光合类型植物的地理分布范围和区域 ,一般来说 ,C4 植物分布于高温、强光的环境而 C3植物分布于阴凉、湿润的环境 ,且 C4 比 C3植物光合速率高。但环境条件影响着不同光合类型植物的光合潜能的发挥 ,C4 植物在高温、强光、干旱条件下所表现出来的优势在其它环境条件下未必就显现出来。环境条件甚至可以引起 C3、C4 光合途径间的相互转化 ,这使得目前几种鉴别植物光合类型的方法出现不一致的结果。因此 ,在判断植物的光合类型时 ,要注意多种手段的综合利用 ,同时注意植物所处环境条件的影响。     

C3和C4植物光合途径的适应性变化和进化

高等植物大多为C₃植物, C₄植物和景天酸代谢(Crassulacean acid metabolism, CAM)植物是由C₃植物进化而来的。C₄途径的多源进化表明, 光合途径由C₃途径向C₄途径的转变相对简单。该文分析研究了植物光合途径的进化前景, 指出C₄植物是从C₃植物进化而来的高光效种类, 且地质时期以来降低的大气CO₂浓度和升高的大气温度以及干旱和盐渍化是C₄途径进化的外部动力。C₃植物的C₄途径的发现说明植物的光合途径并非是一成不变的, C₃和C₄植物的光合特征具有极大的可塑性, 某些环境的变化会引起植物光合途径在C₃和C₄途径之间转变。C₃植物具有的C₄途径是环境调控的产物, 是对逆境的适应性进化结果, 因而光合途径的转变也适用于干旱地区植被的适应性生存机理研究。该文还利用国外最新的C₄光合进化模型介绍了植物在进化C₄途径中所经历的7个重要时期(从分子基础到形态基础、结构基础, 再到物质代谢水平、光合酶活水平, 直到C₃和C₄途径协调运转时期, 最后达到形态与功能最优化阶段), 并结合全球气候变化的特点对国内外相关领域的研究进行了分析, 总结了植物光合途径的适应性转变和进化的研究成果, 为今后的相关工作提出建议。     

Surface lipid composition of C3 and C4 plants

The characteristic surface lipid compositions of several C₃ and C₄ plants are discussed. C₄ plants produce surface lipids (epicuticular waxes) made up of the ubiquitous classes of aliphatic compounds: free fatty acids, aldehydes, primary alcohols, alkanes and aliphatic linear esters. C₃ plants synthesize surface lipids comprising the ubiquitous classes and either of the two following groups of compound: (i) lβ-diketones, hydroxy lβ-diketones, alkan-2-ol esters; (il) ketones and secondary alcohols with the functional group in the middle of the hydrocarbon chain. These features are suggested to represent physioIogical characteristics of the plant and to be related to ecological adaptations. Wax class compositions might also be an ancillary method for defining the C₃ or C₄ mechanism of CO₂ assimilation in cases where uncertainty exists.     

Photosynthetic traits in C3 and C4 grassland species in mesocosm and field environments

The North American tallgrass prairie is composed of a diverse mix of C₃ and C₄ plant species that are subject to multiple resource limitations. C₄ grasses dominate this ecosystem, purportedly due to greater photosynthetic capacity and resource-use efficiency associated with C₄ photosynthesis. We tested the hypothesis that intrinsic physiological differences between C₃ and C₄ species are consistent with C₄ grass dominance by comparing leaf gas exchange and chlorophyll fluorescence variables for seven C₄ and C₃ herbaceous species (legumes and non-legumes) in two different settings: experimental mesocosms and natural grassland sites. In the mesocosms, C₄ grasses had higher photosynthetic rates, water potentials and water-use efficiency than the C₃ species. These differences were absent in the field, where photosynthetic rates declined similarly among non-leguminous species. Thus, intrinsic photosynthetic advantages for C₄ species measured in resource-rich mesocosms could not explain the dominance of C₄ species in the field. Instead, C₄ dominance in this ecosystem may depend more on the ability of the grasses to grow rapidly when resources are plentiful and to tolerate multiple limitations when resources are scarce.     

Photosynthetic carbon metabolism in Panicum milioides, a C3-C4 intermediate species: Evidence for a limited C4 dicarboxylic acid pathway of photosynthesis

Panicum milioides, a naturally occurring species with C₄-like Kranz leaf anatomy, is intermediate between C₃ and C₄ plants with respect to photorespiration and the associated oxygen inhibition of photosynthesis. This paper presents direct evidence for a limited degree of C₄ photosynthesis in this C₃-C₄ intermediate species based on:

1. (a) the appearance of 24% of the total ¹⁴C fixed following 4 s photosynthesis in ¹⁴CO₂-air by excised leaves in malate and aspartate and the complete transfer of label from the C₄ acids to Calvin cycle intermediates within a 15 s chase in ¹²CO₂-air;

2. (b) pyruvate- or alanine-enhanced light-dependent CO₂ fixation and pyruvate stimulation of oxaloacetate- or 3-phosphoglycerate-dependent O₂ evolution by illuminated mesophyll protoplasts, but not bundle sheath strands; and

3. (c) NAD-malic enzyme-dependent decarboxylation of C₄ acids at the C-4 carboxyl position, C₄ acid-dependent O₂ evolution, and ¹⁴CO₂ donation from [4-¹⁴C]C₄ acids to Calvin cycle intermediates during photosynthesis by bundle sheath strands, but not mesophyll protoplasts.

However, P. milioides differs from C₄ plants in that the activity of the C₄ cycle enzymes is only 15 to 30% of a C₄ Panicum species and the Calvin cycle and phosphoenolpyruvate carboxylase are present in both cell types. From these and related studies (Rathnam, C.K.M. and Chollet, R. (1979) Arch. Biochem. Biophys. 193, 346–354; (1978) Biochem. Biophys. Res. Commun. 85, 801–808) we conclude that reduced photorespiration in P. milioides is due to a limited degree of NAD-malic enzyme-type C₄ photosynthesis permitting an increase in pCO₂ at the site of bundle sheath, but not mesophyll, ribulosebisphosphate carboxylase-oxygenase.     

Integration and expression of Sorghum C4 phosphoenolpyruvate carboxylase and chloroplastic NADP-malate dehydrogenase separately or together in C3 potato plants

We have integrated two cDNAs expressing Sorghum photosynthetic phosphoenolpyruvate carboxylase (C₄-PEPC) and NADP-malate dehydrogenase (cpMDH), two key enzymes involved in the primary carbon fixation pathway of NADP-malic enzyme-type C₄ plants, separately or together into a C₃ plant (potato). Analysis of the transgenic plants showed a 1.5-fold increase in PEPC and cpMDH activities compared to untransformed plants. Immunolocalization confirmed an increase at the protein level of these two enzymes in the transgenic plants and indicated that the Sorghum cpMDH was specifically addressed to the chloroplasts of potato mesophyll cells. However, integration of either or both of the cDNAs into the potato genome did not appear to significantly modify either tuber starch grain content or the rate of photosynthetic O₂ production compared to control untransformed plants. The low level of transgene expression probably explains the lack of influence on carbon metabolism and photosynthetic rates. This general observation suggests that some complex mechanism may regulate the level of production of foreign C₄ metabolism enzymes in C₃ plants.     

Summer monsoon intensity controls C4/C3 plant abundance during the last 35 ka in the Chinese Loess Plateau: Carbon isotope evidence from bulk organic matter and individual leaf waxes

The natural abundance of C₃ and C₄ plants is affected by multiple environmental factors including temperature, moisture balance and atmospheric pCO₂. The relative importance of these factors is a subject of considerable debate, and may vary in different natural ecosystems. Previous studies generally focus on single loess sequences in the Chinese Loess Plateau, and conflicting conclusions on C₄/C₃ have been reached when studying carbon isotope ratios in carbonate and organic matter. In this paper we report a comprehensive carbon isotopic characterization of total organic carbon (TOC) and individual higher plant leaf waxes from five loess sequences spanning the last 35 ka from the Chinese Loess Plateau (CLP). The five coring sites encompass large gradients of annual mean temperature (9.2–13.9 °C) and precipitation (402–673 mm), allowing us to assess the controlling mechanisms on C₄/C₃ plant ratios. Glacial–interglacial sequences provide carbon isotope data for comparison with other climatic and environmental proxies such as lithology and magnetic susceptibility. Our results demonstrate that increased C₄/C₃ ratios are positively correlated with higher temperature and increased summer rainfall which characterize stronger summer monsoon in all five sites. We conclude C₄ abundance increases from the last glacial to the Holocene in response to greater monsoon activity and that the C₄ expression is suppressed in the cold and drier intervals.     

Spectroscopic and electrical properties of the [W(C3Se5)3] anion complex (C3Se5 = 1,3-diselenole-2-selone-4,5-diselenolate) and the oxidized species

[NBuⁿ₄]₂[W(C₃Se₅)₃] (C₃Se₅²⁻ = 1,3-diselenole-2-selone-4,5- diselenolate(2−)) was prepared by the reaction of Na₂[C₃Se₅] with WCl₆ in ethanol, followed by addition of [NBuⁿ₄]Br. The cyclic voltammogram in dichloromethane exhibits two oxidation peaks at −0.04 and +0.03 V (versus SCE). The complex reacted with [Fe(C₅Me₅)₂][BF₄], iodine or [TTF]₃[BF₄]₂ (TTF^·+ = the tetrathiafulvalenium radical cation) in acetonitrile to afford the oxidized complexes [Fe(C₅Me₅)₂]_0.5[W(C₃Se₅)₃], [NBuⁿ₄]_0.1[W(C₃Se₅)₃] and [TTF]_0.5[W(C₃Se₅)₃], respectively. Current-controlled electrochemical oxidation of the complex in acetonitrile gave [NBuⁿ₄]_0.6[W(C₃Se₅)₃]. The oxidized complexes exhibit electrical conductivities of 4.7×10 ⁻⁵−1.5×10⁻³ S cm⁻¹ at room temperature measured for compacted pellets. Electronic absorption, IR and ESR spectra of these complexes are discussed.     

C60-fullerenides of ytterbium and lutetium

Cp^#₂Yb (Cp^#=C₅H₄(CH₂)₂NMe₂) has been obtained by reaction of YbI₂(THF)₂ with 2 equiv. of C₅H₄(CH₂CH₂NMe₂)K in THF. The X-ray structure analysis shows a bent structure with intramolecular coordination of both nitrogen atoms to ytterbium. The reaction of C₆₀-fullerene with Cp^#₂Yb leads to the formation of the fullerenide derivative [Cp^#₂Yb]₂C₆₀, which shows an ESR signal in the solid state and in THF solution at room temperature (solid: ΔH = 50 G, G = 1.9992; solution: ΔH = 10 G, G = 2.0001) and a magnetic moment of 3.6 BM. The lutetium fullerenides CpLu(C₆₀)(DME) (3) and Cp^*Lu(C₆₀)(DME)(C₆H₅CH₃) (4), (Cp = η⁵−C₅H₅, Cp^* = η⁵−C₅Me₅), were obtained by reaction of C₆₀ with CpLu(C₁₀H₈) (DME) and Cp^*Lu(C₁₀H₈) (DME) in toluene. Both complexes are paramagnetic (μ_eff = 1.4 and 0.9 BM) and exhibit temperature-dependent ESR signals (293 K: g = 1.992 and 2.0002 respectively).     

Studies of the oxovanadium(IV)—oxalate system: syntheses and crystal structures of binuclear (Ph4P)2[(VO)2(H2O)2(C2O4)3]·4H2O and of the one-dimensional chain material, (Ph4P)[VOCl(C2O4)]

The hydrothermal reactions of (Ph₄P)[VO₂Cl₂] and H₂C₂O₄ at 150 and 125°C yield (Ph₄P)₂[V₂O₂(H₂O)₂(C₂O₄)₃]·4H₂O (1) and (Ph₄P)[VOCl(C₂O₄)] (2), respectively. The structure of the molecular anion of 1 consists of a binuclear unit of oxovanadium(IV) octahedra bridged by a bisbidentate oxalate group. The VO₆ coordination geometry at each vanadium site is defined by a terminal oxo group, an aquo ligand, and four oxygen donors — two from the bisbidentate bridging oxalate and two from the terminal bidentate oxalate. The structure of 2 consists of discrete Ph₄P⁺ cations occupying regions between [VOCl(C₂O₄)]⁻_∞ spiral chains. The structure of the one-dimensional anionic chain exhibits V(IV) octahedra bridged by bisbidentate oxalate groups. Crystal data: 1·4H₂O, monoclinic P2₁/n, A = 12.694(3), B = 12.531(3), C = 17.17(3) Å, β = 106.32(2)°, V = 2621.3(13) ų, Z = 2, D_calc = 1.501 g cm⁻³, structure solution and refinement converged at a conventional residual of 0.0518; 2, tetragonal P4₃, A = 12.145(2), C = 15.991(3) Å, V = 2358.7(12) ų, Z = 4, R = 0.0452.     

Organometallic chemistry of diphosphazanes. Rhodium(I) complexes of RN(PX2)2 (R = C6H5; X = OC6H5, OC6H4Br−p, R = CH3; X = OC6H5)

Reactions of [Rh(COD)Cl]₂ with the ligand RN(PX₂)₂ (1: R = C₆H₅; X = OC₆H₅) give mono- or disubstituted complexes of the type [Rh₂(COD)Cl₂{ν²−C₆H₅N(P(OC₆H₅)₂)₂}] or [RhCl{ν²−C₆H₅ N(P(OC₆H₅)₂)₂ }]₂ depending on the reaction conditions. Reaction of 1 with [Rh(CO)₂Cl]₂ gives the symmetric binuclear complex, [Rh(CO)Cl{μ−C₆H₅N(P(OC₆H₅)₂)₂} ₂, whereas the same reaction with 2 (R = CH₃; X = OC₆H₅) leads to the formation of an asymmetric complex of the type [Rh(CO)(μ−CO)Cl{μ−CH₃N(P(OC₆H₅)₂)₂}₂ containing both terminal and bridging CO groups. Interestingly the reaction of 3 (R = C₆H₅, X = OC₆H₄Br−p with either [Rh(COD)Cl]₂ or [Rh(CO)₂Cl]₂ leads only to the formation of the chlorine bridged binuclear complex, [RhCl{ν²−C₆H₅N(P(OC₆H₄Br−p)₂)₂}]₂. The structural elucidation of the complexes was carried out by elemental analyses, IR and ³¹P NMR spectroscopic data.