毛乌素沙地锦鸡儿（Caragana）种群种子蛋白多样性及其生物学意义

应用多种聚丙烯酰胺凝胶电泳方法对纯化的锦鸡儿种子球蛋白和清蛋白进行分离和分子量测定。占总蛋白７０％左右的球蛋白包括３个不同分子量的蛋白,它们由相同的２１个亚基组成,说明是不同的聚合态。清蛋白在ＰＡＧＥ和ＳＤＳＰＡＧＥ中部分出约２０种成分。全蛋白ＰＡＧＥ结果表明最主要的球蛋白和若干清蛋白在种群内和种群间有高水平的多态性,至少有４个可能的位点编码６个蛋白。ＳＤＳＰＡＧＥ结果表明全蛋白有约５０个不同分子量的单体,其中大多数是变异的。记录了其中１７个单体的变异,初步推测由１３个位点编码。从全部１０个种群３３７份样品的ＰＡＧＥ和３３８份样品的ＳＤＳＰＡＧＥ结果计算出２３个蛋白或单体的分布频率,进一步统计出各项种群遗传结构参数。数据表明毛乌素沙地锦鸡儿的全部遗传多样性中９０％以上存在于群体内,群体间只占７．６％,说明种群间存在强大的基因而。同一植株不同种子存在不同种子蛋白和单体成分,更进一步证明锦鸡儿的异交性。蛋白质的高水平多样性及其空间分布格局证实了所报道的形态变异的结果,说明毛乌素地区的锦鸡儿的确构成一个杂种带。     

大气CO2浓度及温度升高对高山灌木鬼箭锦鸡儿(Caragana jubata)生长及抗氧化系统的影响

以CO_2浓度及温度升高为主要标志的全球气候变化将对我国西北地区脆弱的生态系统产生重要影响。利用环境控制实验研究CO_2浓度倍增(eCO_2, C_1:400μmol/mol和C_2:800μmol/mol)和温度升高(eT, T_1:20℃/10℃和T_2:23℃/13℃)对高山灌木鬼箭锦鸡儿(Caragana jubata)生长及抗氧化系统的影响。结果表明:eCO_2和eT表现出相反的生长和生理效应,eT对幼苗生长的影响要大于eCO_2对其的影响。eT使幼苗的总生物量、净光合速率(NAR)和相对生长速率(RGR)降低;但可促进地上部分生长,叶生物量比及叶面积比增加。eCO_2可减缓或补偿由eT引起的总生物量、NAR和RGR的降低,并促进地下部分生长。对抗氧化系统来说,eT使得超氧化歧化酶(SOD)、过氧化物酶(POD)及抗坏血酸过氧化物酶(APX)活性降低,还原型谷胱甘肽(GSH)和抗坏血酸(ASA)含量降低;eCO_2只增加常温下SOD酶活性,并使GSH、ASA整体水平提高。结论:温度升高和CO_2浓度倍增没有协同促进鬼箭锦鸡儿幼苗的生长和光合能力。温度升高将对幼苗生长和抗氧化系统产生不利影响,eCO_2可促进生长并可能通过抗氧剂含量增加来缓解氧化胁迫。因此,未来气候变化,尤其是温度升高将会对高寒区植物产生较大影响,CO_2浓度增加可缓解增温的不利影响。     

内蒙古半干旱草原灌丛化过程中小叶锦鸡儿引起的土壤碳、氮资源空间异质性分布

过度放牧下内蒙古半干旱草原,由于小叶锦鸡儿多度增加导致植被灌丛化,这已经成为该地草原退化时的普遍现象。草原灌丛化过程中,灌丛内凋落物的累积使得养分循环区域化,草原土壤有机碳(SOC)、土壤全氮(STN)空间异质性增强,导致灌丛沃岛形成。半干旱草原灌丛化过程机制的假说认为:灌丛斑块扩展与其引起的土壤空间异质性的增强之间存在着正反馈作用,正是这种反馈作用促使草地向灌丛地的转变。小叶锦鸡儿通过克隆生长形成不同大小的斑块,它们对应于其发育的不同阶段。因此,将不同大小的灌丛沃岛划分为小灌丛组与大灌丛组,它们代表着灌丛沃岛发育的早期与晚期两个阶段。结果表明:内蒙古半干旱草原灌丛化过程中,小叶锦鸡儿灌丛斑块引起了土壤有机碳(SOC)与土壤全氮(STN)的空间异质性,表现在水平方向上,对于0～5cm,5～10cm,10～20cm3个土壤层次,由灌丛斑块内部向外部SOC与STN均趋于降低;而在垂直方向上,对于灌丛斑块内部、边缘和外部3个位置,由0～10cm到10～20cm再到20～30cm,随着土壤深度增加SOC与STN均趋于降低。随着小叶锦鸡儿灌丛斑块扩展,SOC与STN空间异质性的分布不断增强,表现在灌丛斑块内部相对于外部(或边缘)对SOC与STN富集程度均显著增加。草原灌丛化过程SOC与STN空间异质性变化在0～5cm,5～10cm,10～20cm3个土壤层次中,以表层0～5cm的表现最为强烈。表层0～5cm土壤空间异质性的形成与灌丛自身凋落物的生产以及对灌丛外凋落物的截留有关。由此推断:退化草原灌丛化的过程中,小叶锦鸡儿灌丛斑块引起SOC与STN空间异质性的变化是一个自我增强过程,灌丛斑块扩展与其导致的SOC与STN空间异质性增强之间存在着正反馈作用。因此,以上关于半干旱草原灌丛化机制的假说对我国内蒙古半干旱草原灌丛化也是适用的。     

锦鸡儿(Caragana sinica(Buchoz) Rehd)传粉生物学研究

对唐家河国家自然保护区内锦鸡儿(Caragana sinica(Buchoz)Rehd)的花期、访问者、有效传粉者种类及行为、花蜜分泌节律和繁育系统等进行定点观察和实验处理。结果表明:锦鸡儿单花花期约5d,种群花期约20d。拥有以吸蜜为主的条蜂属(Anthophora)、熊蜂属(Bombus)和太阳鸟属(Aethopyga)3种传粉者功能群。综合访花频率和花粉落置数,茜条蜂(Pyganthophora rubricus Dours)和蓝喉太阳鸟(Aethopyga gouldiae)为主要有效传粉者,熊蜂(Bombus)为次要有效传粉者;蚂蚁(formicidae)和西方蜜蜂(Apis mellifera Linnaeus)为主要盗蜜者。套袋处理结果表明,花蜜分泌日变化中,最大花蜜量发生在16:00左右;花蜜随单花花期变化中,花蜜体积最大发生于单花第5天;分泌均呈递增趋势。花蜜分泌节律与访花频率呈正相关。繁育系统检测显示,花粉胚珠比为3779±320.92,柱头最适可授期在开花第2—3天;结合不同授粉处理表明:锦鸡儿自交不亲和,需要传粉者,为蜂媒兼鸟媒植物。     

科尔沁沙地两种典型乔灌木耗水特点

以科尔沁沙地典型固沙植物小叶锦鸡儿(Caragana microphylla Lam.5年生)和樟子松(Pinus sylvestris var. mongolica Litrin,7年生)为研究对象,栽植于可渗漏式生长箱,应用TDR水分仪测定生长季节土壤水分变化,依据土壤水分平衡理论推算单位面积植被区的蒸散量.经2a研究,在相同栽植密度下(1m×1m),樟子松植被区土壤贮水量高于小叶锦鸡儿植被区;在不同栽植密度下,小叶锦鸡儿土壤贮水量以1m×2m密度区高于1m×1m密度区.生长季节单位面积土壤蒸散量以小叶锦鸡儿(1m×1m)最高,小叶锦鸡儿(1m×2m)其次,樟子松(1m×1m)最低.单丛/株蒸散量以小叶锦鸡儿(1m×2m)最高,小叶锦鸡儿(1m×1m)其次,樟子松(1m×1m)最低.在试验所涉及的特定年龄阶段,小叶锦鸡儿植被区蒸散耗水量高于樟子松区,土壤水分含量低于樟子松区.生产实践中应根据植物耗水特点选择适宜的固沙物种和栽植方式,以保证人工固沙植被区土壤水分的收支平衡.     

内蒙古高原小叶锦鸡儿(Caragana microphylla)、中间锦鸡儿(C. davazamcii)和柠条锦鸡儿(C. korshinskii)的遗传多样性及遗传关系

采用RAPD技术对10个具较大地理跨度的小叶锦鸡儿、中间锦鸡儿和柠条锦鸡儿种群的遗传多样性和遗传关系进行了研究.共检测到678个位点,多态条带比率(PPB)为100%;特有位点41个,占6.05%.总体上3种锦鸡儿的遗传多样性表现出自东向西递减的趋势,分析表明其与生长地点年均气温呈显著负相关.AMOVA表明:3种锦鸡儿种间变异只占总体变异的6.08%,且显著性检验表明这种变异不显著;种内种群间的变异占总变异的11.90%;总变异的主要部分来自种群内部(82.02%). 3种锦鸡儿各种群总体分析结果表明:种群内变异比率Hpop/Hsp为0.8013,基因分化系数Gst为0.1603,种群每代迁移数Nm为2.6192,显示种群间存在一定强度的基因流,3种锦鸡儿间表现为异交性.3种锦鸡儿多样性高低及种群聚类分布格局都表现出一定的地理连续性.     

降雨对高寒沙地不同林龄中间锦鸡儿水分利用特征的影响

为明确不同林龄中间锦鸡儿水分来源对降雨的响应,利用稳定同位素技术测定青海共和盆地不同林龄的中间锦鸡儿(4a、9 a、17 a和31 a)在降雨前后土壤水、木质部水、地下水和雨水的δ2H、δ18O组成,运用Iso-Source模型计算植物对各潜在水源的利用比例.结果 表明:各林龄中间锦鸡儿的浅层(0～40 cm)土壤水δ...     

内蒙古退化草原中与小叶锦鸡儿相关的小尺度土壤碳、氮资源异质性动态

小叶锦鸡儿在内蒙古典型草原中有着广泛分布,从而对小空间尺度土壤资源异质性产生强烈影响。退化草原中小叶锦鸡儿能够通过克隆生长形成灌丛斑块,不同大小斑块对应于其发育的不同阶段。因此,通过对与不同大小灌丛斑块相关的土壤有机碳（SOC）、全氮（STN）空间分布状况的分析,能够推断内蒙古退化草原中、与小叶锦鸡儿相关的小尺度SOC与STN异质性动态。结果表明：在内蒙古退化草原中,就0-5cm,5-10cm,10-20cm 3个土壤层次,小叶锦鸡儿均导致了与灌丛斑块相关小尺度上SOC与STN分布的空间异质性,且随着灌丛斑块的发育,这种异质性均不断增强,其中土壤表层0-5cm碳氮资源异质性的增强最为强烈,表现在灌丛斑块内部相对于外部（或边缘）对SOC与STN富集程度均显著增加。这表明内蒙古退化草原中,随着灌丛斑块自身的扩展,与小叶锦鸡儿相关小尺度上土壤碳氮资源空间异质性趋于增强。     

Water-use process of two desert shrubs along a precipitation gradient in Horqin Sandy Land

Aims The determination of the source of plant water is an important research on the plant-water relationship in arid and semiarid regions and helps to understand the adaptation strategy of desert species to the dry environment. Plant water use pattern affects plant community composition and ecosystem water budget. This study aims to investigate the water use patterns of Caragana microphylla and Artemisia halodendron, two typical shrub species, under altered rainfall conditions in Horqin Sandy Land. Methods Water treatments include ambient rainfall (natural rainfall), 50% increase in rainfall (enhanced rainfall) and 50% decrease in rainfall (reduced rainfall) by artificially intercepting and redistributing natural rainfall. Stable hydrogen and oxygen isotope ratios (δD and δ¹⁸O) were measured for xylem water, rainfall, and soil water in different soil layers (0-120 cm depth). The possible ranges of potential water sources used by C. microphylla and A. halodendron were calculated using the IsoSource model. Important findings 1) Alteration of ambient rainfall mainly affected the soil water condition in the shallow soil (0-30 cm). Increase in rainfall significantly increased the above- and below-ground biomass, and δ¹⁸O values of soil water declined with soil depth. 2) Under the enhanced rainfall treatment, A. halodendron mainly used the soil water in the shallow soil (0-40 cm) and C. microphylla was able to extract water from multiple soil layers. Under the reduced rainfall treatment, both species increasingly relied on extracting water from deeper soil layers, 60-80 cm for A. halodendron and 60-120 cm for C. microphylla. 3) For the natural rainfall treatment, in the wet season, the upper soil water was recharged by rainfall, C. microphylla and A. halodendron extract the shallow soil water (0-60 cm). However, in the dry season, soil water content was dramatically reduced, and main water sources for C. microphylla shifted from topsoil to deeper soil, and A. halodendron can use multiple layers of soil water. In summary, A. halodendron is more capable of exploring deeper soil moisture under reduced rainfall in comparison with C. microphylla, and is likely to be more adaptive to this water-limiting desert environment.     

Population structure and spatial pattern of Caragana tibetica communities in Nei Mongol shrub-encroached grassland

Aims The community structure and function of the shrub-encroached grassland, as well as its formation mechanism, is one of hot scientific problems in vegetation science. The spatial pattern analysis is an important means for studying plant population interactions and the relationships between plant population and environment. The shrub-encroached grassland is one major vegetation type in Nei Mongol. Knowledge on the spatial pattern of shrub can improve our understanding on adaptive characteristics of shrub to steppe environment.
Methods We chose Caragana tibetica encroached grassland distributed in Ordos City as research objects. The spatial position of each C. tibetica individual in 64 m × 64 m study plot was determined by a method of “three-distance location method”, and then the spatial pattern and intraspecific associations of C. tibetica individuals was analyzed with the point pattern analysis.
Important findings The results showed that C. tibetica population was at the rising stage. The mature individuals showed a uniform distribution at the scale of less than 3.7 m, subsequently exhibiting a random distribution with an increased scale. The juvenile individuals showed an aggregation distribution at the scale of 0.3-20.4 m, but a uniform distribution at other scales. The dead C. tibetica individuals were distributed aggregately at the scale from 0.7 to 1.4 m, but randomly at other scales. An indistinctive positive association was found for live C. tibetica individuals to dead individuals at the scale of less than 9.9 m, but no associations was found between them at other scales. The mature individuals negatively interacted with juveniles at the scale of larger than 2.2 m, but unassociated at the other scales.