Ecological basis of Alpine meadow ecosystem management in Tibet: Haibei Alpine Meadow Ecosystem Research Station

Alpine meadow and shrub are the main pasture types on the Tibetan Plateau, and they cover about 35% of the total land area. In order to understand the structural and functional aspects of the alpine ecosystem and to promote a sustainable animal production system, the Haibei Alpine Meadow Research Station was established in 1976. A series of intensive studies on ecosystem structure and function, including the energy flow and nutrient cycling of the ecosystem, were the main tasks during the first 10 years. Meanwhile, studies with 5 different grazing intensities on both summer and winter pasture have been conducted. In the early years of the 1990s, the research station started to focus its research work on global warming, biodiversity and sustainable animal production systems in pastoral areas. Various methods for improving degraded pasturelands have been developed in the region.

高寒草甸生态系统陆地生物圈模式研究及应用

改进了适合于高寒草甸生态系统的陆地生态圈模式，分析了模式中温度变化与水分运动分层的物理原因，说明了气候状况对地表面能量交换的影响，给出了净辐射和蒸散量新的计算方法，提出了有很差分计算中具有二阶精度的Euler隐式格式，介绍了中国科学院海北高寒草甸生态站的气候概况和野外观测情况。最后利用本模式对高寒草甸生态站地区的土壤-植被-大气间水热交换过程进行了数值模拟，模拟值与实测值吻合较好。

高寒草甸地区陆面过程观测及耦合模式研究

对海北高寒草甸地区水热传输过程进行了系统观测,特别考虑了叶片气孔为非饱和水汽条件下的交换情况,结合修正的根系吸水公式,发展了一个多层陆气耦合模式.利用该模式对中国科学院海北高寒草甸生态试验站地区矮嵩草草甸陆气水热交换进行了数值模拟,分析了湍流交换的物理过程,给出了沿高度分布的各物理量.模拟结果与实测值吻合较好.

嵩草属植物的系统学研究

嵩草属隶属于莎草科苔草亚科苔草族，主要分布于北半球温带地区，少数种类为环北极分布，有一种产于泰国清迈，一种产于苏门达腊岛北部高山。本‘文在形态学、微形态学、解剖学和胚胎学研究的基础上，对嵩草属植物进行了全面的分类学修订，根据属内各类群之间的系统演化关系建立了一个新的属下分类系统，确认了世界范围内53种3亚种嵩草属植物，并做出5个种上等级的新组合，描述了一个新亚组。 作者研究了国内外14家标本馆（室）的3000多份腊叶标本并进行多次野外的实地观察，对嵩草属植物的形态学性状进行了详细的比较和分析，评价了它们的系统学价值及其演化趋势。在嵩草属中，花序是由小穗排列成的圆锥花序或穗状花序，花序各部分的形态性状是种及种上等级分类的基础;花序的演化趋势是由圆锥花序到穗状花序，小穗是从由数朵雄花与1朵雌花组成简化到由1朵雌花组成。但是，花序和小穗由复杂到简单的进化在嵩草属中平行地发生于不同的类群中。先出叶的性状状态是分种的主要特征之一，通常认为边缘开裂的先出叶是原始的，边缘合生而为囊状的先出叶是进化的。同样，先出叶由开裂到合生的进化也是多次发生的。此外，根状茎、秆、叶鞘、叶片、柱头及小坚果等的性状状态对于种及种上等级的分类都具有重要的意义。 应用扫描电子显微镜对38种（或亚种）嵩草属植物的小坚果表面进行了观察，证明小坚果纹饰在种及种上等级的分类中具有重要的参考价值，并能揭示种及种下等级的亲缘关系。例如，分布于喜马拉雅东部至横断山地区的3种植物，K．clarkeana、K．curvata和K．fragilis外部形态非常相似，难于区分，而其小坚果的微形态特征却可以提供3种之间关系的证据。K．clarkeana与K．fragilis果实表面的特征完全一致，且与其它植物有显著区别，应为同种植物;K．curvata与它们明显不同，也与其它种有较大差异，应为独立的种。K．gramini folia，K．cercostach ys和K. nepalensis果实表面纹饰具有一些共同的特征，说明它们之间的亲缘关系较近。K．filicina和K．duthiei也存在同样的情形。 通过对秆和叶片的横切面和表皮的解剖学观察比较，发现嵩草属植物秆的横切面表现出由三角形到圆形的一系列变化。秆的横切面明显地分两个区域，中部的髓由较大而无色的细胞组成，其中心常碎裂形成大的气腔;外围的绿色部分，由绿色组织及分布其中的气腔和外韧维管束及与其相伴的厚壁组织组成。秆的表皮与叶片下表皮非常相象。叶片横切面的外形为V形、新月形或半圆形。V形的叶片具有明显发育的中脉并且在远轴面凸起，形成脊;新月形和半圆形的叶片中脉发育不明显，也无脊。叶片的表皮细胞均为长方形，垂周壁波纹状;平列型的气孔器纵向成行排列，多局限于下表皮;上表皮近边缘及脉附近的细胞常常在细胞的一端形成乳突。秆和叶片横切面的形态对于分种及种上等级的划分具有参考价值。 胚胎学研究表明小孢子、胚囊和胚的发育与莎草科其它类群一致。花粉为假单体花粉( pseudomonad)，成熟花粉三核。胚珠倒生，厚珠心，双层珠被，珠孑L由内珠被形成。胚囊的发育为蓼型，原胚的发育为柳叶菜型灯芯草变型。首次观察到，在大孢子四分体时期，合点端和珠孔端两个大孢子细胞开始时体积都增大，而中部两个很快退化，稍后珠孔端一个也退化，合点端一个为功能大孢子，发育成为胚囊。根据胚胎学证据，不支持将嵩草属与苔草族一起另立为嵩草科。 嵩草属中较原始的一个亚属subg. Compositae主要分布于西喜马拉雅至横断山地区，还有一种见于泰国，一种产于苏门达腊，而后2种植物还具有一些最原始的形态性状。结合地史的变化推测，嵩草属可能在第三纪早期起源于古地中海的东部和北部。 根据形态学和解剖学性状的分析表明，许多性状在嵩草属中是平行演化的，如花序和小穗由复杂到简单、秆由圆柱形到三棱形、叶片横切面由V形到半圆形等。该属的属下分类应该追溯这些平行的演化线，而不能像以前的分类那样，将它们横向地划分为几个组或亚属。作者认为嵩草属有3个大的进化分支，据此将其划分为3个亚属。Subg. Compositae，12种，是较原始的一个分支。叶近基生，叶片扁平;花序多疏松圆锥状，少穗状，苞片多为叶状;小穗两性到单性，先出叶多为囊状，少边缘分离，退化小穗轴明显、扁平、较长。Subg. Blysmocarex，仅2种，是较早分化而相对隔离的一个分支。根状茎匍匐状;花序由圆锥状到穗状，小穗两性或单性;柱头2。Subg. Kobresia，种类最多。叶片扁平或内卷;秆三棱形到圆柱形;花序紧密，复杂到简单，苞片不为叶状;小穗两性或单性，先出叶由开裂到合生，退化小穗轴较小而不显著。根据该亚属呈现出的不同的性状演化系列，可以分为3个组。Sect. Kobresia花序圆锥状至穗状，小穗多为两性，少为单性，先出叶边缘分离。含3个亚组：subsect. Kobresia，8种2亚种．植株纤细，秆与叶均为丝状;subsect. Royleanae，8种l亚种，植株较粗壮，叶片扁平或对折;subsect. Sibiri-cae，4种，秆较粗，叶片内卷。Sect. Psmmostachys，仅2种，小穗两性，先出叶完全合生为囊状。Sect．Hemicarex花序一般为穗状，稀圆锥状，小穗多为单性，少两性。分为四个亚组：subsect. Forexeta，6种，叶片内卷或对折，先出叶线形，边缘分离或合生;subsect. Chlorostachys，3种，叶片扁平，小穗两性;subsect. Holmia，4种，叶片扁平，小穗单性;subsect．Utriculatae，5种，叶片丝状，先出叶完全合生为囊状，不为线形。嵩草属的属下分类纲要如下： Subgenus 1. Compositae (Clarke) Kukkonen Type: K. laxa Nees. Subgenus 2. Blysmocarex (Ivanova) S. R. Zhang Type: K. macrantha Boeck. Subgenus 3. Kobresia Section 1. Kobresia Subsection 1. Kobresia Type: K. simpliciuscula (Wahl. ) Mack. Subsection 2. Royleanae (Ivanova) S. R. Zhang Type: K. royleana (Nees) Boeck. Subsection 3. Sibiricae (Ivanova) Egorova Type: K. sibirica (Turcz. ex Ledeb. ) Boeck. Section 2. Psmmostachys Ivanova Type: K. robusta Maxim. Section 3. Hemicarex (Bentham) Clarke Subsection 4. Forexeta (Raffin. ) S. R. Zhang Type: K. cercostachys (Franch. ) C. B. Clarke. Subsection 5. Chlorostachys (Ivanova) S. R. Zhang Type: K. duthiei C B. Clarke. Subsection 6. Holmia (Boern. ) S. R. Zhang Type: K. esenbeckii (Kunth) Noltie. Subsection 7. Utriculatae S. R. Zhang Type: K. prainii Kukenthal.

疏叶骆驼刺的生物生态学研究

盐生草甸是新疆平原草地生物生产力最高的植被类型。而豆科植物疏叶骆驼刺则是盐毕草甸植被的常见种类。此项工作对疏叶骆驼刺天然分布的范围及其生态环境条件，特别是土壤水盐状况和与该植物相联系的植物群落类型进行了调查分析。本文通过对K、Na、Ca、Mg4种金属盐性元素在土壤—疏叶骆驼刺系统中的迁移进行分析，探讨该种植物在盐化土壤环境中的生长状况与主要盐性金属元素的相互关系;通过对包括土壤植物体内元素含量、土壤水盐状况、植株生长状况等指标的综合分析，研究其生态适应关系和种群与土壤水盐状况的关系;通过对植物器官形态解剖学的研究，探讨该种植物与盐生土壤环境生态适应的生物结构基础和耐盐的生理途径;通过对土壤盐化过程影响因素和土壤盐化趋势的分析，结合疏叶骆驼刺的生态学特性，探讨该种植物在新疆盐化土壤的可能利用价值。结果如下： 1、疏叶骆驼刺为中生适弱盐化的潜水草甸植物。在有潜水发育的地带，其生存适应土壤盐化环境的范围较广。 2、在天然条件下，疏叶骆驼刺以根萌生新芽繁殖方式为主。在弱盐化和土壤水分较充足的地带，可以种子繁殖再生新株。 3、作为盐生草甸植被与荒漠植被间过渡类型中常出现的种类，疏叶骆驼刺的种群消长代表了一定的土壤盐化的演替阶段。 4、该种植物的器官组织显微结构显示出其与盐化土壤环境关系上特殊的适应机制。 5、在植物的生长发育过程中，金属盐性元素的迁移积累变化的性质表明，在一定条件下，该种植物对土壤盐性具有改善作用。 6、面对新疆盐化土地使用状况和土壤盐化退化的趋势，疏叶骆驼刺的生态利用潜势很大。

全球变化不绿洲的演化趋势研究-以塔里木盆地北部渭干河绿洲为例

本文以全球变化对绿洲水文循环影响为主线，分析了地处干旱区的绿洲在全球变化下的演变趋势。以塔里木盆地北部渭干河绿洲为例，探讨了其水量平衡、非灌溉土壤积盐特性、隐域性盐化草甸植被NPP，以及绿洲土地利用／覆被变化对全球变化的响应。从不同时间尺度上分析了全球变化的两大驱动因子，气候变化和人类活动对绿洲演化的影响。运用系统动力学模型模拟了未来30年绿洲土地覆被变化在上述两驱动因子的作用下的动态演变过程。其主要结论如下： 1、从生态学的角度，绿洲可定义为：存在于干旱、半干旱区的依赖于水源而生存的隐域性绿色景观．地质时期，绿洲的演化由气候等自然因子起决定作用;人类历史时期，在气候等自然因素的大背景下，人类活动对绿洲演变的作用越来越大;近百年来，绿洲的演变则主要受人为活动干扰。 2、在不改变绿洲现有土地利用格局和水资源利用率的情况下，当年平均气温升高2.5℃，无论降水增加200%或不增加，绿洲的水资源量都将出现负平衡，全球变化将使绿洲面临更为严重的水资源短缺。 3、绿洲自然土壤0-5 0cm土层积盐速率对全球变化的响应程度依地下水埋深的大小而有所差异。地下水埋深较小，积盐速率随温度的升高增加较明显;地下水埋深较大时，积盐速率变化不明显。当地下水埋深>2m，地表积盐速率不再随气候变化而变化．地下水埋深h=2m为渭干河绿洲非灌溉土壤地表积盐速率对全球变化响应的临界深度。 4、根据绿洲地下水埋深与植被NPP的相关关系，推导出了估算盐化草甸植被NPP的模型： NPP=-O. 991+0. 0005Eo (h-0. 25h^2+0. 021h^3) +5. 276EXP (-0. 651h) 并分别估算了当前及全球变化下的NPP值。盐化草甸植被NPP随地下水埋深的增加呈指数下降。全球变化下，地下水埋深较大时，NPP的增加较明显;地下水埋深较小时，NPP的增加不明显。 5、灵敏度分析表明：NPP对地下水埋深h的变化比对地下水矿化度变化为更敏感。h=3. 3m为渭干河绿洲盐化草甸植被的胁迫深度。 6、系统动力学模型模拟表明，渭干河绿洲耕地面积的增减受水资源利用率和人口数量变化的制约。全球变化下，由于水文状况的改变，未来30年将导致绿洲耕地面积增幅下降4. 5-5.1%。绿洲水文状况和人口数量变化是决定土地利用格局变化的关键驱动因素。 7、绿洲灌溉土地的优化模式为，耕地：林地：改良草地=70: 23:7;种植业（耕地）内部的比例为，粮食作物：经济作物：人工草地=46: 31: 23。

锡林河流域一个放牧草原群落土壤呼吸及其影响因子的研究

本文综述了草原群落土壤呼吸研究的理论、方法、最新进展和主要成果。从2001年6月5日到10月15日，在内蒙古锡林河流域的一个典型草原群落放牧地段用气相色谱法对土壤呼吸进行了测定，并同期观测相应的环境因子，分析了它们之间的相互关系，并根据根系生物量和土壤呼吸的相关性外推出根系呼吸占土壤总呼吸的比例。同时，采用碱液吸收法对该草原群落和一个沼泽化草甸群落的土壤呼吸进行了比对测定，比较在不同生境下土壤呼吸速率的差异。另外，重点比较了两种常用的土壤呼吸测量方法——碱液吸收法和气相色谱法对典型草原群落土壤呼吸的测量效果。主要研究成果如下： 1．在草原群落，生物量（包括地上和地下生物量）、温度（包括气温和土壤温度）和水分及土壤呼吸的季节变化均呈不规则的波动曲线;土壤呼吸与土壤湿度高度相关，与温度尤其是土壤温度以及地下生物量之间存在着一定的相关性，但和地上生物量及绿色生物量之间几乎没有关系。 2．草原群落和草甸群落土壤呼吸的季节动态基本一致，均出现了两个峰值，分别出现在6月底和7月底，它们的变化范围分别为312.8~1738.9 mg C﹒m-2﹒d-1 和 354.6 ~2235.6 mg C﹒m-2﹒d-1，日平均土壤呼吸速率分别为785.9 mg C﹒m-2﹒d-1 和1349.6 mg C﹒m-2﹒d-1，草甸群落的土壤呼吸速率明显高于草原群落; 3．土壤水分是草原群落土壤呼吸的主要限制因子，但对草甸群落的土壤呼吸变化却基本没有影响;草甸群落中，地上总生物量与土壤呼吸速率间没有显著的相关关系，但地上部分绿色生物量与土壤呼吸间存在着显著的幂函数关系，而在草原群落中，土壤呼吸速率与地上活生物量或地上总生物量的相关关系均很弱。 4．在草原群落，根系呼吸占土壤总呼吸的比例为60.7% - 93.3%，平均为82%; 5．碱液吸收法和气相色谱法的测定结果具有很高的相关性（R2=0.7563），它们的季节动态基本一致，变化范围分别为从249.3~1795.1 mg C﹒m-2﹒d-1和从312.8~1738.9 mg C﹒m-2﹒d-1，平均值分别为634.2 mg C﹒m-2﹒d-1和802.7 mg C﹒m-2﹒d-1，碱液吸收法的测量值是气相色谱法的约1.4倍。

增温与土地利用变化对青藏高原高寒草甸生态系统温室气体通量影响的研究

随着青藏高原气候变暖进程及放牧压力与开垦面积的逐年加大，非常有必要评价青藏高原高寒草甸生态系统温室气体通量对气候变暖、放牧（包括粪尿斑）和开垦的响应和反馈。与此同时，我们进行了粪尿斑及开垦对土壤理化性质影响研究。本研究对于青藏高原高寒草甸C、N循环关键过程对全球变化响应的认识具有重要意义。 本文通过2年（2006-2007）增温（白天+1.2℃，晚上+1.7℃）与放牧耦合试验，在生长季观测了增温与放牧对高寒草甸生态系统温室气体通量的影响。研究初步表明，增温试验显著增加10 cm土壤温度1℃左右；在放牧频度相对较高的2007年，放牧也显著增加了土壤温度1℃左右。总体上，增温对土壤湿度的影响不显著。 增温可以促进土壤对CH4的吸收，而放牧对CH4通量影响不大或起到一定程度抑制作用。在较低放牧频度的2006年，放牧显著降低了植物-土壤系统CO2总释放量，增温促进了CO2的释放。而在放牧频度相对较高的2007年生长季，没有发现增温及放牧对土壤-植被系统CO2释放显著的影响。2006年放牧后，增温促进了高寒草甸土壤N2O的释放；2007年，增温不放牧小区N2O总通量较对照增加了24.6%，同时放牧处理也促进了N2O释放。基于土壤温度和土壤湿度的线性回归模型可以解释55%-89%的CH4通量变异，而土壤湿度较土壤温度对CH4通量影响更大。土壤温度是影响CO2和N2O通量的主要因子，通过拟合的指数型曲线，土壤温度可以分别解释43%-63%CO2通量变异与65%-81%N2O通量变异。 在2005年与2006年夏季放牧期间，对牦牛粪尿斑处理对高寒草甸CH4、CO2和N2O通量进行了观测。牛粪小区2年观测期内CH4平均通量为687 μg m-2 h-1，而尿斑和对照土壤吸收CH4（平均通量分别为-34 μg m-2 h-1和-39 μg m-2 h-1）。牛粪小区CO2在2005年和2006年观测期内累积释放量较对照分别增加了35.8%和49.7%，而牛尿小区与对照累积释放量差异不显著。牛尿与牛粪小区N2O累积释放量显著高于对照，在2005年牛尿与牛粪小区N2O累积释放量较对照分别增加了3.7和3.5倍，而在2006年分别增加了2.1和1.8倍。因此，在估算放牧高寒草甸生态系统N2O释放时，来自牛粪斑释放量是不能被忽略的。但在中等放牧强度下（1.45头ha-1 y-1），有粪尿斑覆盖的高寒草甸在观测期内全球变暖潜势较相同面积没有粪尿斑覆盖的草甸仅增加了1%。土壤水分孔隙度（WFPS）可以解释牛尿小区35%和对照小区36%CH4通量变异。土壤温度是控制CO2释放的主要因子之一，它可以解释所有处理40-75% CO2的变异。牛尿处理（34%）、牛粪处理（48%）及对照（56%）N2O时间变异则同时受土壤温度和WFPS的驱动。在观测期内，牛尿可以显著提高土壤的pH值。粪尿斑对土壤微生物量碳氮没有产生显著性影响，但在一定时段内能显著增加土壤无机氮含量。 通过在青藏高原高寒草甸开展的人工草地试验，初步探讨了不同土地利用方式（种植燕麦、开垦后闲置及自然恢复）对CO2、CH4和N2O通量，以及土壤无机氮和微生物量氮的影响。燕麦地、自然恢复草地及开垦闲置地与天然草地相比，吸收CH4的能力均表现为增强（CH4的吸收总量分别增加了31.9%、57.2%和71.0%）。由于燕麦地生物量低于天然草地与恢复草地，造成了燕麦地土壤-植被CO2释放量低于天然草地和恢复草地。而闲置地几乎没有植被覆盖，其CO2释放量显著低于天然草地。草地恢复8年后，CO2释放基本恢复到天然草地的水平。闲置地N2O总通量显著高于天然草地，较天然草地增加了60.5%。观测期内燕麦地与天然草地相比，N2O总通量增加了24.3%，但没有达到显著性水平。开垦及种植燕麦，增加了土壤硝态氮的含量，而自然恢复地、燕麦地、天然草地和闲置地在观测期内土壤铵态氮平均含量没有观察到显著性差异。燕麦地土壤微生物量氮平均含量最低（119.7 mg N kg-1），而自然恢复草地、天然草地和闲置地土壤微生物量氮差异不大。

Foraging habitats and utilization distributions of Black-necked Cranes wintering at the Napahai Wetland, China

One of the most endangered populations of Black-necked Cranes (Grus nigricollis), the central population, is declining due to habitat loss and degradation, but little is known about their space use patterns and habitat preferences. We examined the space use and habitat preferences of Black-necked Cranes during the winter of 2007-2008 at the Napahai wetland in northwest Yunnan, China, where approximately 300 Black-necked Cranes (>90% of the total central population) spent the winter. Euclidean distance analysis was employed to determine the habitat preferences of Black-necked Cranes, and a local nearest-neighbor, convex-hull construction method was used to examine space use. Our results indicate that Black-necked Cranes preferred shallow marsh and wet meadow habitats and avoided farmland and dry grassland. Core-use areas (50% isopleths) and total-use areas (100% isopleths) accounted for only 1.2% and 28.2% of the study area, respectively. We recommend that habitat protection efforts focus on shallow marsh and wet meadow habitats to maintain preferred foraging sites. Core-use areas, such as the primary foraging areas of Black-necked Cranes, should be designated as part of the core zone of the nature reserve. Monthly shifts in the core-use areas of the cranes also indicate that the reserve should be large enough to permit changes in space use. In addition to preserving habitat, government officials should also take measures to decrease human activity in areas used by foraging Black-necked Cranes.

凤鹛属鸟类（Yuhina, Aves）的系统发育研究

本研究以凤鹛属（Yuhina）鸟类为研究对象，分别使用分子生物学性状和形 态学性状来重建凤鹛属种间的系统发育关系，为东南亚地区鹛类的起源与进化研 究提出新的见解。分子生物学研究的内群不仅包括了凤鹛属（11 种中的10 种）， 而且还包括了菲律宾特有穗鹛属（Stachyris）和绣眼鸟属（Zosterops）等近缘种。 通过测定线粒体上两个蛋白编码基因Cyt b、ND3 的全长序列和两个RNA 编码 基因 12S, 16S 的部分序列，得到长度为2379bp 的联合序列，使用最大简约法、 最大似然法和贝叶斯法进行系统发育分析的结果表明，菲律宾岛特有的穗鹛（金 冠穗鹛S. dennistouni、纹穗鹛S. striata、怀氏穗鹛S. whiteheadi）与绣眼鸟属（暗 绿绣眼Z. japonicus、红胁绣眼Z. erythropleurus、灰腹绣眼Z. palpebrosus）聚为 一支，位于凤鹛属支系内部。通过凤鹛、菲律宾穗鹛、绣眼鸟三个类群羽冠性状 演化趋势的分析，发现羽冠性状在菲律宾特有穗鹛和绣眼鸟支系中发生丢失。与 前人的研究结果相比，新发现纹喉凤鹛Y. gularis 与棕肛凤鹛Y. occipitalis 是姐妹 群，黄颈凤鹛Y. flavicollis 和白项凤鹛Y. bakeri 是姐妹群，这两个姐妹群又聚为 一大支的关系。 在分类问题上，暗绿绣眼、红胁绣眼和灰腹绣眼在本研究中与鹛类表现出近 缘关系，与前人使用绣眼鸟属其它物种进行的相关研究显示出高度一致性，说明 绣眼鸟属的系统学地位存在很大疑问，应该扩大取样进行深入研究。栗冠凤鹛 Y. everetti 与栗耳凤鹛Y. castaniceps 聚为姐妹群的关系，但是二者之间较小的遗 传距离和形态学差别显示二者之间应该为亚种关系，而不是种级关系。依据栗耳 凤鹛特有的尾羽形态提出的Staphiada 属没有得到本分子生物学研究结果的支持 （Harrison, 1986a, b）。在白腹凤鹛Y. zantholeuca 不属于凤鹛属支系这一结果的 提示下，发现白腹凤鹛独有的形态学特征，例如羽冠由冠羽形成、鼻孔半裸露、 飞羽外翈没有异色羽缘，这些独有的特征与其特殊的系统学地位相对应。因此， 我们支持前人提出的将白腹凤鹛从凤鹛属中分出去，单独成Erpornis 属的建议 （Cibois et al., 2002）。 在历史生物地理学方面，根据菲律宾特有穗鹛和绣眼鸟的近缘关系，认为菲 律宾特有穗鹛的祖先具有与现在绣眼鸟一样的跨海迁移的能力，在中新世末期（5.74Mya）由喜马拉雅地区或印度支那起源地经大巽他地区扩散到菲律宾岛屿 上，经过长期独立进化后，形成现在高度特有的穗鹛支系。更新世冰期时，大巽 他地区海平面下降，使栗冠凤鹛得以扩散至婆罗州（1.66Mya）。在上新世初期台 湾岛成陆后，由于台湾岛与中国大陆相连，褐头凤鹛Y. brunneiceps 的祖先扩散 至台湾岛屿上（5.05Mya）。高黎贡山为第四纪冰期时凤鹛属鸟类的避难场所，因 此形成了现在凤鹛属鸟类在高黎贡山地区密集分布的格局。喜马拉雅山和青藏高 原的隆起导致青藏高原上植被带的变化和喜马拉雅山南麓在第四纪冰期中避难 所的作用，是纹喉凤鹛、棕肛凤鹛、黄颈凤鹛、白项凤鹛等种类现今在喜马拉雅 山南麓密集分布的可能原因。 在凤鹛属分子系统学的研究基础上，从形态学角度探讨凤鹛属除白领凤鹛外 其它物种之间的系统发育关系。使用最先分化出来的白领凤鹛为外群以外群比较 法进行51 个形态学特征的性状极化，使用最大简约法分析后，结果不仅支持一 些分子系统学揭示的物种之间的亲缘关系，例如，栗耳凤鹛与栗冠凤鹛姐妹群的 关系，黑颏凤鹛和褐头凤鹛姐妹群的关系，三种绣眼鸟聚为一支，再与怀氏穗鹛 聚为一个大支；而且发现了新的系统关系，黄颈凤鹛与缅甸凤鹛Y. humilis 是姐 妹群，具有浅色下体的凤鹛属物种具有较近的系统关系。分子数据和形态数据对 凤鹛属系统发育树中部节点解决能力的差异，说明凤鹛属物种之间分化间隔时间 很短。 通过综述近年来核基因在鸟类分子系统发育研究中的应用情况，建议未来研 究中增加核基因的内含子序列，例如肌球素基因内含子2（ myoglobin intron Ⅱ） 或β纤维蛋白原基因内含子7（β-fibrinogen intron7, β-fibint 7）来解决本研究 中未确定的末端分枝分歧顺序。

科尔沁沙地西部草甸植物繁殖对策

本文以科尔沁沙地西部草甸植物为研究对象，从草甸植物的繁殖体形态学、种子萌发特征、花期和果期、结种量和土壤种子库等方面分析了草甸植物的繁殖对策，探讨了草甸植物的繁殖对策与放牧、割草等干扰的关系。研究结果表明：（1）在科尔沁沙地西部草甸植被中，开花早，结果早的植物能够更好的适应自由放牧和秋季割草；（2）科尔沁沙地西部草甸割草草地极小粒种子的植物密度比大粒种子和小粒种子的植物密度小；在放牧草地小粒种子植物密度远远大于大粒种子和极小粒种子的植物密度；（3）在实验室条件下，64种草甸植物种子萌发能力的差异明显；小粒种子、长形或圆锥形种子、具芒和冠毛的繁殖体一般具有高的萌发能力；放牧草地一般由高萌发能力的一年生植物和低萌发能力的多年生植物组成；割草草地一般由低萌发能力的一年生植物和高萌发能力的多年生植物组成；（4）自由放牧草地土壤种子库密度小于秋季割草地，放牧草地种子库密度与地上植物出现频率和多度相关不显著，而割草地种子库物种与地上植物多度具有显著的相关性（r＝0.76，P＜0.01）；〔5）在科尔沁沙地西部草甸植被中，20种草甸植物具有持久种子库，其中豆科植物和一年生植物占据较大的比例。

增温对川西北高寒草甸植物群落结构及几种主要植物生长和生理的影响

由于人类活动所引起的地球大气层中温室气体的富集已导致全球地表平均温度在20世纪升高了0.6 ℃，并预测在本世纪将上升1.4-5.8 ℃。气候变暖对陆地植物和生态系统影响深远，并已成为全球变化研究的重要议题。高海拔、高纬度地带的生态系统对气候变化最敏感。而在高原和高山极端环境影响下所形成的高寒草甸生态系统极其脆弱，对由于温室效应引起的全球气候变化极其敏感，对这些变化的响应更具有超前性。 本研究以川西北高寒草甸植物群落及几种主要物种为研究对象，采用国际山地综合研究中心（ITEX）普遍所采用的增温方法-----开顶式生长室（OTC）模拟气候变暖来研究增温对高寒草甸植物群落结构、物质分配及其主要物种生长和生理的影响，以探讨高寒草甸植物响应与适应气候变暖的生物学和生态学机制。主要研究结论如下： 1、OTC的增温效果 由于地温、地表温度和气温的平均值在OTC内分别高出对照样地0.28℃、0.46℃和1.4℃，这说明本研究所采用的开顶式生长室（OTC）起到了增温的作用；同时，由于温室内与温室外接受的降水量相同，温室内由于热量条件的改善，土壤蒸发和植被的蒸腾作用增强，直接导致了OTC内土壤表层相对湿度的减少。 2、群落结构对增温的响应 由于增温时间较短，增温内外样地的物种组成并未发生改变；但增温后一定程度上改变了植物群落的小气候环境，从而导致物种间的竞争关系被破坏，种间竞争关系的破坏引起群落优势种组成发生相应的改变，在对照样地，鹅绒委陵菜、甘青老鹳草、遏蓝菜和蚤缀是占绝对优势的物种，而在OTC内，小米草、尼泊尔酸模、垂穗披碱草、发草和羊茅的重要性显著增加。 禾草和杂草由于对增温的生物学特性及其资源利用响应的不同，加之增温造成土壤含水量下降等环境因子的改变。与对照样地相比较，OTC内禾草的盖度及生物量都显著增加，而杂草的盖度和生物量则显著下降。 3、植物生长期对增温的响应 OTC内立枯和调落物的生物量在生长季末（10月份）都要小于对照样地的立枯和调落物生物量，而OTC内的地上鲜体生物量在10月份却略高于对照样地。这说明OTC内植物的衰老或死亡得以延缓，而植物的生长期得以延长。 4、群落生物量及分配对增温的响应 OTC内的地上鲜体生物量(10月份除外)和地下0-30cm的根系生物量与对照样地相比较，都出现了不同程度的减少；土壤根系的分配格局也发生了明显的改变，其中，OTC内0-10cm土层的生物量分配比例增加，而20-30cm土层生物量分配比例的减少。 5、群落碳、氮对增温的响应 增温后，OTC内植物群落地上活体和地下活根的碳浓度不同程度的高于对照样地，植物群落的碳库在OTC内也略高于对照样地；而OTC内植物群落地上活体和地下活根的氮浓度不同程度的低于对照样地，其植物群落的氮库与对照样地相比也略有下降。 6、几种主要植物的生长及物质分配对增温的响应 垂穗披碱草在增温后株高、比叶面积和地上生物量均显著地增加；尼泊尔酸模在增温后比叶面积和单株平均生物量积累显著地增加，而各组分中，增温处理使叶的生物量显著增加，而根的生物量却显著下降；鹅绒委陵菜在增温后株高、比叶面积和单株平均生物量积累显著地减少，而各组分中，增温处理使叶和茎的生物量显著减少，根的生物量却显著地增加。 尼泊尔酸模的LMR、RMR、R/S、根部碳含量、碳和氮在叶片与根部的分配比例在增温后显著地增加，而SMR、根部氮含量、碳和氮在茎部的分配比例在增温后却显著地降低；鹅绒委陵菜的RMR、R/S、碳和氮在根部的分配比例在增温后显著地增加，而SMR、LMR、碳在叶片的分配比例在增温后却显著地降低 7、几种主要植物的光合生理过程对增温的响应 增温使垂穗披碱草和尼泊尔酸模叶片中的叶绿素a、叶绿素b、总叶绿素含量显著增加；而鹅绒委陵菜叶片的叶绿素a、叶绿素b、总叶绿素含量在增温后显著减少，类胡萝卜素含量在增温后却显著增加。 增温对3种植物的气体交换产生了显著影响。其中，垂穗披碱草和尼泊尔酸模叶片的光响应曲线在增温后明显高于对照处理，A、E、gs、Pmax、、Rday、AQY和LSP显著增加，而LCP则显著降低；鹅绒委陵菜的光响应曲线在增温后则明显的低于对照处理，A、E、gs、Pmax、、Rday、AQY和LSP显著减少，而LCP则显著增加。 增温后垂穗披碱草和尼泊尔酸模叶片的Fv/Fm、Yield和qP显著增加；而鹅绒委陵菜叶片的Fv/Fm、Yield和qP则显著减少，qN却显著地增加。 8、几种主要植物的抗氧化酶系统对增温的响应 增温使垂穗披碱草和尼泊尔酸模体内抗氧化酶活性和非酶促作用有所提高，植物膜脂过氧化作用降低；鹅绒委陵菜叶片中酶促反应和非酶促反应在增温后也显著提高，但可能由于增温后的土壤干旱超过了鹅绒委陵菜叶的抗氧化保护能力，抗氧化酶活性及非酶促反应（脯氨酸、类胡萝卜素）的提高不足以完全清除干旱诱导形成的过量活性氧，因此叶片的膜脂过氧化程度仍然显著提高。 Enrichment of atmospheric greenhouse gases resulted from human activities such as fossil fuel burning and deforestation has increased global mean temperature by 0.6 ℃ in the 20th century and is predicted to increase in this century by 1.4-5.8 ℃. The global warming will have profound, long-term impacts on terrestrial plants and ecosystems. The ecoologcial consequences arising from global warming have also become the very important issuses of global change research. The terrestrial habitats of high-elevation and high-latitude ecosystems are regarded as the most sensitive to changing climate. The alpine meadow ecosystme, which resulted from the composite effects of mountain extreme climatic factors in Tibetan Plateau, is thus thought to be especially vulnerable and sensitive to global warming. In this paper, the response of plant community and several main species in the alpine meadow of Northewst Sichuan to experimemtal warming was studied by using open-top chambers (OTC). The aim of the this study was to research the warming effects on plant community structure, substance allocation, growth and physiological processes of several mian species, and to explore the biological and ecological mechanism of how the alpine meadow plants acclimate and adapt to future global warming. The results were as follows: 1. Warming effects of OTC The mean soil temperature, soil surface temperature and air temperature in OTC manipulation increased by 0.28℃、0.46℃ and 1.4℃ compared to the control during the growing season. This suggested that the OTC used in our study had increased temperature there. Meanwhile, the OTC manipulation slightly altered thermal conditions, but the same amount of precipitation was supplied to both the OTC manipulation and the control, so higher soil evaporation and plant transpiration in OTC manipulation directly lead to the decrease of soil surface water content. 2. The reponse of community structure to experimental warming The species richness was not changed by the short-term effect of OTC manipulation. However, experimental warming changed the microenvironment of plant community, therefore competitive balances among species were shift, leading to changes in species dominance. In the present study, the dominant plant species in the control plots were some forbs including Potentilla anserine, Geranium pylzowianum, Thlaspi arvense and Arenaria serpyllifolia, however, the importance value of some gramineous grasses including Elymus nutans, Deschampsia caespitosa, Festuca ovina, and some forbs including Euphrasia tatarica and Rumex acetosa significantly increased in OTC. The different biology characteristics and resource utilizations between gramineous grasses and forbs, and enhanced temperature caused change in some environment factors such as soil water content. As a result, the coverage and biomass of gramineous grasses significantly increased in OTC compared to the control, however, the coverage and biomass of forbs singnifciantly decreased in OTC compared to the control. 3. The reponse of plant growing season to experimental warming Both the standing dead and fallen litter biomass in OTC were lower than those in the control in October, and the biomass of aboveground live-vegetation in OTC was higher than that of the control. The results indicated that the senescence of plants was postponed, and the growing season was prolonged in our research. 4. The reponse of community biomass accumulation and its allocation to experimental warming Experimental warming caused the decrease of aboveground live biomass and belowground root biomass except for the aboveground live biomass in October. Experimental warming also had pronounced effects on the pattern of root biomass allocation. In the present study, the root biomass in 0-10cm soil layer increased in OTC manipulation compared to the control, however, the root biomass in the 20-30cm soil layer decreased in OTC manipulation compared to the control. 5. The reponse of community C and N content to experimental warming The C concentration and stock in aboveground live and belowground root both increased in OTC manipulation compared to the control. However, the N concentration and stock in aboveground live and belowground root both decreased in OTC manipulation compared to the control. 6. The reponse of gowth and biomass, C and N alloction of several species to experimental warming Experimental warming significantly increased the height, SLA (specific leaf area) and aboveground biomass of Elymus nutans in OTC manipulation compared to the control. The SLA and total biomass of Rumex acetosa also significantly increased in OTC manipulation compared to control, among the different components of Rumex acetosa, leaf biomass significantly increased, but root biomass significantly decreased in OTC manipulation compared to the control. However, the height, SLA and total biomass of Potentilla anserina significantly decreased in OTC manipulation compared to the control, among the different component of Potentilla anserina, leaf and stem biomass significantly decreased, but root biomass significantly increased in OTC manipulation compared to the control. The LMR (leaf mass ratio), RMR (root mass ratio), R/S (shoot/root biomass ration) and root C concentration of Rumex acetosa significantly increased in OTC manipulation compared to outside control, also, Rumex acetosa allocated relatively more C and N content to leaf and root in response to experimental warming, however, the SMR (stem mass ration) and root N concentration of Rumex acetosa significantly decreased in OTC manipulation compared to outside control, also, Rumex acetosa allocated relatively less C and N content to stem in response to experimental warming. The RMR and R/S of Potentilla anserina significantly increased in OTC manipulation compared to outside control, also, Potentilla anserina allocated relatively more C and N content to root in response to experimental warming, however, the SMR and LMR of Potentilla anserina significantly decreased in OTC manipulation compared to outside control, also, Potentilla anserina allocated relatively less C and N content to leaf in response to experimental warming. 7. The reponse of physiological processes of several species to experimental warming Experimental warming significantly increased chlorophyll a, chlorophyll b and total chlorophyll of Elymus nutans and Rumex acetosa in OTC manipulation compared to outside control. However, chlorophyll a, chlorophyll b, total chlorophyll and carotenoid of Potentilla anserina in OTC manipulation significantly decreased compared to outside control. Experimental warming had pronounced effects on gas exchange of Elymus nutans, Rumex acetosa and Potentilla anserine. In the present study, warming markedly increased the light response curves of Elymus nutans and Rumex acetosa in OTC manipulation compared to outside control, and also singnificantly increased A (net photosynthesis rate), E (transpiration rate), gs (stomatal conductance), Pmax (maximum net photosynthetic rate), Rday (dark respiration rate), AQY (apparent quantum yield) and LSP (light saturation point), but LCP (photosynthetic light compensation) of Elymus nutans and Rumex acetosa in OTC manipulation singnificantly decreased compared to outside control. However, warming markedly decreased the light response curves of Potentilla anserina in OTC manipulation compared to outside control, and also singnificantly decreased A, E, gs, Pmax, Rday, AQY and LSP, but LCP of Potentilla anserina in OTC manipulation singnificantly increased compared to outside control. Experimental warming singnificantly increased the chlorophyll fluorescence kinetics parameters such as Fv/Fm, Yield and qP of Elymus nutans and Rumex acetosa and qN of Potentilla anserina in OTC manipulation, but Fv/Fm, Yield and qP of Potentilla anserina in OTC manipulation singnificantly decreased. 8. The reponse of antioxidative systems of several species to experimental warming Experimental warming tended to increase the activities of antioxidative enzymes and stimulate the role of non-enzymes of Elymus nutans and Rumex acetosa. As a result, MDA content of Elymus nutans and Rumex acetosa decreased. The activities of antioxidative enzymes and non-enzymes of Potentilla anserina also significantly increased in OTC manipulation, but more O2- was produced because of lower soil water content, and the O2- accumulation exceeded the defense ability of antioxidative systems and non-enzymes fuctions. As a result, MDA content of Potentilla anserine still increased in OTC manipulation compared to outside control.

岷江上游高山林线附近优势树种土壤种子库和幼苗更新特征的研究

岷江上游地区高山/亚高山植被分布的坡向性分异显著，阴阳坡高山林线不仅物种组成差异明显，并且分布海拔呈现出阴坡高阳坡低的格局．阳坡林线树种主要是圆柏属乔木，林线类型多为渐变型，海拔高度大约在3 400m~3 800m；阴坡林线树种主要是冷杉，林线类型多为骤变型，海拔高度约在3 800m~4 400m．本研究采用土壤种子库物理筛选、室内萌发实验及野外群落调查等方法，对岷江上游地区阴坡岷江冷杉和阳坡祁连圆柏两类林线树种不同海拔梯度上土壤种子库以及幼苗库特征进行了调查，从土壤种子库和幼苗更新特征的角度对林线乔木树种种群更新特征进行了分析，进而对该地区高山林线在阴阳坡分布差异的原因进行了探讨，结果显示： 1．土壤种子库 阴坡：阴坡高山林线附近岷江冷杉土壤种子的平均密度大约为50.96粒/m2，其中树线以上10m处土壤种子密度为1.00粒/m2，树线处大约19.33粒/m2，林线交错带内土壤种子密度最高为136.83粒/m2，郁闭林内种子密度小于林线交错带，只有30.50粒/m2，种子平均空壳率为52％，霉变率达34%，完好种子只有6%．土壤种子库垂直分布特征为地被物层含种子比重最大，大约在67.50%左右；其次为0~2cm层，约18.84%左右；2~5cm层所占种子比例最小，约13.66%左右．霉变种子数量与土壤深度呈负相关． 阳坡：阳坡祁连圆柏土壤种子的平均密度为60.16粒/m2．树线以上10m处密度为1.92粒/m2，树线位置大约108.16粒/m2，林线交错带内平均为75.80粒/m2，郁闭林内种子密度小于林线交错带，只有20.00粒/m2．种子平均空壳率为36％，完好种子占49%，霉变率较低，大约为10%．阴阳坡林线树种土壤种子库垂直分布特征为：地被物层含种子最多，其次为0~4cm层，4~10cm层所占种子比例最小，霉变种子数量与土壤深度也呈负相关． 2． 幼苗库调查 阳坡：在树线以上区域没有发现幼苗，林线交错带内幼苗密度平均达3 250株/hm2，郁闭林内仅2 750株/ hm2．整个样地内1～2a幼苗很少甚至没有出现，3～10a的幼苗相对较多．空间分布上，祁连圆柏幼苗在林线交错带内接近随机分布，郁闭林内则介于随机分布和均匀分布之间． 阴坡：在树线以上幼苗密度为1 250株/ hm2，全部为1~2a幼苗，林线交错带内幼苗密度平均达7 000株/ hm2，郁闭林内达6 250株/ hm2．林线附近岷江冷杉幼苗丰富度以及幼苗的出现频率明显高于祁连圆柏，年龄结构也较祁连圆柏完整．岷江冷杉幼苗空间分布除了树线处幼苗的分布为随机分布，其他海拔则为集群分布． 3．从不同土壤深度的种子总量和幼苗数量的相关性检验发现，当年生幼苗数量跟表层种子总量相关性极显著, 但是两年生幼苗的数量与底层种子数量相关性显著．土壤种子在土壤中的垂直分布格局从一定程度上可以反映种子库的年际特征．岷江冷杉土壤种子库较丰富，种子散布后的存活力随着时间的变化逐渐下降，属于季节性瞬时种子库；祁连圆柏土壤种子散布格局为集群型分布，成熟种子大部分散布在母株冠幅内，属于永久性土壤种子库． 4．在阴坡林线交错带及以上区域还存在较为丰富的乔木土壤种子，并且在树线以上区域还发现了少量的岷江冷杉幼苗．从样地乔木的年龄结构发现，在林线交错带内上部到树线位置主要以幼龄林为主，且年龄结构完整，基本符合入侵性林线特征；阳坡林线交错带内幼苗出现频率很低，树线以上区域虽然存在种子库，但是没有幼苗出现，在林线交错带内乔木径级差距很大，年龄结构异常不完整，这种特征的林线将会面临两个可能结果：一种是维持现有状态，保持平衡；另外一种就是退化，但阳坡林线的实际动态趋势还有待长期定点研究． Treelines on the upper region of Minjiang River differ between the north aspect and the south aspect in their appearances, altitudes and tree species. On the north aspect, trees of Abies form a sharp and abrupt treeline ranging from 3800m to 4400m, while on the south the treeline is generally lower(3 400~3 800m), more open and gradual and mostly composed of Sabina. In this study, we examined the altitudinal gradients of soil seed banks and seedling recruitments at the treeline ecotones of a N-aspect and a S-aspect by using soil sieving, germination experiment and field investigations, analyzed the characteristics of population regeneration of tree species at the transitional zone and presented a analysis of the causes to the aspect-related difference in treeline patterns in the study area. Major results of our study include: 1． Soil seed bank N-aspect: Of the 50 plots investigated, the average density of soil seeds is 50.96/m2, in which well-formed seeds account for 6%, empty seeds 52%, parasitized seeds34%, and seeds damaged by animals 8%. The size of soil seed bank varies along altitude, being 1.00 seeds /m2 at the 10m above the treeline and ca.19.33 seeds/m2 at the upper limit of treeline. The highest density (136.83 seeds/m2) occurs at the treeline ecotone. By contrast, the density of soil seed for the closed forest is only 30.50 seeds/m2. In terms of vertical strata, 67.50% of the total seeds are at the surface layer, 18.84% at the middle layer (0~2cm) and 13.66% at deeper layer (2~5cm). The number of parasitized seeds is negatively correlated to soil depth. S-aspect: Of the 50 plots investigated, the average density of soil seeds is 60.16 seeds/m2, and the well-formed seeds account for 49%, empty seeds 36%, parasitized seeds10%, and seeds damaged by animals 1%. The size of soil seed bank varies along altitude, with 1.92 seeds/m2 recorded at the10m above the treeline，108.16 seeds/m2 at the upper limit of treeline, and 75.80 seeds/m2 at the treeline ecotone, while that for the closed forest is 20.00 seeds/m2. The number of seeds decreases with the depth of soil. As is on the N-aspect, the size of soil bank, from large to small, follows the order of the surface layer, the middle layer (0~4cm) and the bottom layer (4~10cm). The number of parasitized seeds is also negatively correlated to the depth of the soil. 2． Seedling bank N-aspect: A mean maximum seedling abundance of 31 000 seedlings/hm2 was recorded near alpine treeline at growing season. The density of seedlings is 1 250 seedlings/ha (all being 1 or 2 years old) at the alpine meadow 10m away above treeline, 7 000 seedlings/ha at treeline ecotone and 6 250 seedlings/ha for closed forest．The spatial distribution of Abies faxoniana seedlings is random at the upper limit of the treeline but clumped at other altitudes． S-aspect: No seedlings were found at the alpine meadow 10m away from the treeline. The density of seedlings was 3 250 seedlings/ha at treeline ecotone and 2 750 seedlings/ha for the closed forest．Hardly any 1 year current and 2 year-old seedlings appeared at the plots. The spatial distribution of Sabina przewalskii seedlings is random at treeline ecotone and between “random” and “even” forest closed forest． 3．Correlation tests of seedling population and seed bank at different soil layers indicated that the emergents were strongly correlated to seed bank at surface layer while the number of two-year seedlings was significantly correlated to the seed bank at the bottom of soil layer, indicating that germination mainly occurs at the soil surface while the middle or bottom layer was the reserve for non-germination or dead seeds. It can thus be postulated that Abies faxoniana soil seed bank is of seasonal transient type. By contrast, the soil seed bank of Sabina przewalskii is of persistent type and the soil seeds and seedlings of this species occurred more frequently near the islands of adult trees. 4．A good many soil seeds of both tree species were found near the treeline ecotone and above at N- and S-aspects. A few young seedlings were found above the Abies treeline. Investigation of five altitudinal transects respectively on N- and S-aspects indicated that Abies faxoniana has a more complete age structure than the stands of Sabina przewalskii. The age of firs decreased from closed forest to the upper limit of treeline, which suggests that the Abies treeline is advancing to higher altitude. While on the south aspect, only few Sabina przewalskii soil seeds and nearly no seedlings were found above the treeline ecotone. The stands exhibit extremely great difference in diameter classes with significantly incomplete age structure. This would lead to two possible results for the treelines: maintaining an equilibrium state at the current position or degenerating. But more studies should be carried out at longer time scales or larger spatial scales to understand whether the Sabina treeline is degenerating.

青藏高原东部植物生态特征在季节性雪厚度梯度上的变化

本文以青藏高原东部的高山草甸为研究对象，设置早融、中间及晚融三个融雪部位，采用实验室测量、野外测量、野外样方调查相结合的 方法，从个体、种群和群落的水平上比较研究了高山雪场植物在同一雪场样地中不同融雪梯度上的特征变异及适应，结果表明： 从早融到晚融的梯度上，随着融雪时间的逐渐推迟，表土日温差降低，冻融交替的强度减弱，土壤水份逐渐增加，总N、总P、总K 以及 可溶性的N、P 和pH 变化不明显，土壤有机质及可溶性的K 和Ca 逐渐降低。冻融交替强度上的差异以及土壤水分差异被认为是融雪梯度上 影响植物生长的主要原因。 从早融到晚融的梯度上，伴随着生态因子的改变，几种常见植物的个体特征也发生相应的变化。首先，物候期推迟。植物开始生长的时间 一般要推迟将近二十天，但同一种植物在不同的融雪部位上的衰老期趋于一致，这预示着在晚融部位同一植物的生长期要缩短。其次，个体生 长特性发生改变。黑褐穗苔草（Carex atrofusca subsp. minor (Boott) T.Koyama）和西北黄芪（Astragalus fenzelianus Pet.-Stib.）的个体生长（株高、单株叶数、单叶面积和地上生物量）表现为逐渐增加的趋势；斑唇马先蒿（Pedicularis longiflora Rudolph var. tubiformis (Klotz.) Tsoong）和川西小黄菊（Pyrethrum tatsienense (Bur. et Franch.) Ling ex Shih.）则表现为逐渐降低的趋势；长叶火绒草（Leontopodium longifolium Ling）在融雪梯度上的变化趋势不明显。再次，从繁殖特性来看，大卫马先蒿（Pedicularis davidii var. pentodon Tsoong）的单株花数、单花种子数、种子千粒重及种子萌发率随融雪的推迟呈现为逐渐增加的趋势；圆穗蓼（Polygonum macrophyllum D.Don）的种子（小坚果）千粒重和萌发率也表现为逐渐增加，其余繁殖特征变化不明显。 在种群层次上，几个常见物种的分布格局随着融雪的推迟都发生一定的变化，基本上表现为从早融的集群分布到中间或晚融部位的随机分布。物种间的联结性也发生较大的变化，由早融部位的总体上的正关联逐步过度到晚融部位上的总体上的负关联。特定种对间的联结性也发生较大的变化。恶劣环境条件（如剧烈的冻融交替）的影响以及对恶劣条件适应被认为是分布格局及种间联结性发生变化的主要原因。 在群落层次上，物种多样性的变化表现为单峰曲线的格局，即在中间部位多样性最高。早融部位强烈的冻融交替和晚融部位缩短的生长季是早融及晚融部位物种多样性不高的重要原因。几乎所有的只出现在一个融雪部位（雪深级别）上的物种都发生在中间融雪部位。这说明，中等的雪深更有利于许多高山植物的存活，而过浅过深的积雪都不利于植物的生存。另外，相距较近的融雪梯度之间的物种相似性较大，而相距较远的梯度之间物种的替代率较高，物种的相似性较小。在群落的生物量方面，地上生物量随融雪的推迟而升高，地下生物量随融雪的推迟而下降，地上与地下生物量之总和随着融雪的推迟而下降，地下生物量与地上生物量之比随着融雪的推迟而下降。早融部位的地上生物量主要集中于地上0-10cm 的范围内，表明在早融部位植物地上部分有变矮的趋势；早融部位的地下生物量在土壤各深度分布相对较均一，而晚融部位地下生物量则主要集中于地下0-10cm 的范围内。生物量的变化趋势主要与雪场中各部位的土壤水分含量及地表日温度差异有关，是植物适应特定环境的结果。 To detect the plants’ responses to snow-cover gradients in an alpine meadow of eastern Tibetan plateau, laboratory method and field sample plot method were employed, and three gradeients （early-, medium and late-melting）were established in a natural snowbed. The measurements were carried out for two years and was done on three levels——individual, population and community. The results are shown as follows : From early- to late-melting gradients, daily ground temperature difference between day and night decreased, amplitude of freeze-thaw alternation weakened, soil organic matter contents and soluble K and Ca decreased, while soil water content increased. Total N, total P, total K，pH soluble N and soluble P kept constant from early- to late-melting portions. Among these factors, the changes of intense freeze-thaw alternation and soil water contents were considered as main factors affecting plants’ growth. From early- to late-melting portions, all phenological phases postponed, e.g. phase of plant emergence postponed almost twenty days. However, the same species’ individuals at different portions withered in step, which implied that the individuals at late-melting portion possessed shorter growing season length. Along the same gradient, both Carex atrofusca subsp. minor (Boott) T. Koyama and Astragalus fenzelianus Pet.-Stib. increased their individual growth, whereas Pedicularis longiflora Rudolph var. tubiformis (Klotz.) Tsoong and Pyrethrum tatsienense (Bur. et Franch.) Ling ex Shih. decreased their individual growth. Unlike the four plants mentioned above, Leontopodium longifolium L. did not show any evident change. As to reproductive charateristics, the flowers per individual, the number of seeds per flower, the thousand seed weight and the seed germination rate of Pedicularis davidii var. pentodon showed an increasing trend; and Polygonum macrophyllum D.Don also increased its thousand seed weight and seed germination rate along the same gradient. However, the other reproductive charateristics of Polygonum macrophyllum D.Don did not change significantly. At population level, the distribution pattern of several selected species changed from cluster pattern to random pattern as the snowmelt postponed. Overall association among the species changed from positive to negative along the same gradient. Further, interspecific association also changed evidently. Adverse circumstances such as intense freeze-thaw alternation were considered as primary factors resulting in changes of population distribution pattern and interspecific association. At the level of community, species diversity showed a pattern of a unimodal trend, i.e. the highest diversity occurred at medium snow depth，perhaps because of intense freeze-thaw alternation at early-melting portions and the shortest growing season at late-melting portions. Almost all species that only appeared at one snowmelt portion occurred at medium portion, indicating that medium snow depth was more suitable for many species’ survival. Species replacement from one snowmelt portion to its neighboring portion seldom took place. However, while distance between two portions became farther, species replacement between the two portions occurred more frequently. As for biomass, aboveground biomass increased from early- to late-melting portions, whereas belowground biomass, total biomass and the ratio of belowground to aboveground all decreased along the same snow gradient. A majority of aboveground biomass distributed in a height range of 0-10 cm, suggesting that height of plants inhabiting early-melting portion be shorter compared with other portions. In addition, belowground biomass at early-melting portion was evenly distributed at different soil depth in comparison with aboveground biomass, whereas belowground biomass at late-melting portion concentrated 0-10cm soil layer below ground. The changing trend of biomass was also related to two factors. One was soil water content, and the other topsoil temperature difference between day and night.