都江堰地区灌丛内袍栎橡子的捕食和搬运

从2000年9月至2002年12月,以四川都江堰常绿阔叶林灌丛内的优势种--枹栎(Quercus serrata)为研究对象,研究了昆虫、鼠类和真菌对枹栎橡子的捕食和搬运.结果表明(1)取食橡子的鼠类的群落结构和数量在年间差异较小,这可能与三年间袍栎橡子的产量相对稳定有关;(2)袍栎橡子的虫蛀率在三年间存在显著性差异,范围在14.17%-32.49%之间;(3)鼠类的就地取食和搬运是影响种子库内橡子命运的主要因素;(4)橡子虫蛀率的变化影响鼠类的觅食活动.鼠类对饱满橡子和虫蛀橡子的选择性取食和搬运可能影响许多坚果植物(栎树)的自然更新过程[动物学报50(4)535-540,2004].     

青藏高原高寒灌丛2003-2016年生长季的不同月份CO2通量对气温日较差的响应

全球气候变化引起的气温日较差（ADT）减小,将会对高寒生态系统的碳平衡造成深刻影响。基于涡度相关系统,利用2003-2016年的涡度相关系统观测资料,做了青藏高原高寒灌丛在生长季（6-9月）不同月份的ADT对CO₂通量影响的研究。结果表明：2003-2016年的生长季中,最高气温（MaxTa）和最低气温（MinTa）呈先升高后降低的单峰变化趋势,ADT没有呈现明显的变化趋势。逐日总初级生产力（GPP）和生态系统呼吸（Re）呈先增加后降低的单峰趋势,逐日净生态系统CO₂交换（NEE）呈先下降后上升的"V"型变化趋势。高寒灌丛在生长季为碳汇,整个生长季总NEE、GPP和Re平均值分别为（-161.2±30.1）、（501.9±60.2）、（340.7±54.4） gCm^-2。在高寒灌丛生长季（6-9月）的每个月份,MaxTa、MinTa和ADT分别是GPP（P<0.001）、Re（P<0.001）和NEE（P<0.01）变化的主要控制因子。高寒灌丛的ADT的增大有利于生态系统的碳固持,暗示在未来气候变化背景下ADT的减小将会削弱高寒灌丛生态系统的碳汇能力。     

青藏高原东缘窄叶鲜卑花灌丛生长季土壤无机氮对增温和植物去除的响应

为了揭示气候变暖背景下高寒灌丛土壤氮转化过程, 该文研究了青藏高原东缘窄叶鲜卑花(Sibiraea angustata)灌丛生长季节土壤硝态氮和铵态氮含量对增温和去除植物的响应。结果表明: 窄叶鲜卑花灌丛土壤硝态氮和铵态氮含量具有明显的季节动态。整个生长季节, 土壤硝态氮含量呈先增加后降低的趋势, 而铵态氮含量均表现为一直增加的趋势。在生长季初期和中期, 各处理土壤硝态氮含量均显著高于铵态氮含量, 而在生长季末期土壤硝态氮含量均显著低于铵态氮含量, 说明该区域土壤氮转化过程在生长季初期和中期以硝化作用为主, 而在生长季末期以氨化作用为主。不同时期土壤硝态氮和铵态氮含量对增温和去除植物的响应不同: 增温对硝态氮的影响主要发生在生长季中期和末期, 且因植物处理的不同而有显著差异, 增温仅在生长季中期使不去除植物样方铵态氮含量显著升高。去除植物对土壤硝态氮的影响仅表现在对照样方(不增温), 去除植物显著提高了生长季初期和中期土壤硝态氮含量, 显著降低了生长季末期土壤硝态氮含量; 同时去除植物显著降低了增温样方生长季中期土壤铵态氮含量。灌丛植被在生长季初期和中期可能主要吸收土壤硝态氮, 其吸收过程不受土壤增温的影响。     

荒漠草原人工灌丛化对蒸散发及其组分的影响——以盐池县为例

我国西北防沙治沙工程中大量的种植中间锦鸡儿(Caragana intermedia)会导致荒漠草原发生灌丛化现象,研究人工灌丛化对荒漠草原蒸散发的影响,不仅能够揭示半干旱区人为活动对生态系统水循环的影响机理,还可以指导区域生态治理实践。以宁夏盐池县荒漠草原为例,基于植被的生理生态参数和荒漠草原水热条件,采用生物地球化学模型(Biome Bio-Geochemical Cycles,Biome-BGC)和地球呼吸系统模拟模型(Breathing Earth System Simulator,BESS)结合的方法,模拟荒漠草原生态系统人工灌丛引入前后蒸散发及其组分的变化,定量研究荒漠草原人工灌丛化对区域生态水文循环中蒸散发的影响。结果表明,人工灌丛的引入使植被结构及特征发生了变化,叶面积指数(Leaf Area Index,LAI)年最大值由0.20增加为0.67,改变了植被年内与年际变化特征。荒漠草原人工灌丛化后,生态系统年均蒸散发由251.74 mm增加到了281.42 mm;人工灌丛化对生长季的蒸散发增强明显,8月蒸散发峰值时,日均蒸散发由1.27 mm/d增加到1.56 mm/d。...     

Effects of nitrogen enrichment on root exudative carbon inputs in Sibiraea angustata shrubbery at the eastern fringe of Qinghai-Xizang Plateau

Aims Understanding the responses of root exudative carbon (C) to increasing nitrogen deposition is important for predicting carbon cycling in terrestrial ecosystems. However, fewer studies have investigated the dynamics of root exudation in shrubbery ecosystems compared to forests and grassland ecosystems. This objective of this study was to determine the effects of nitrogen fertilization on the rate and C flux of root exudates.Methods Three levels of nitrogen addition treatments were applied to a Sibiraea angustata shrubbery ecosystem situated at the eastern fringe of Qinghai-Xizang Plateau, including N₀ (without nitrogen application), N₅ (nitrogen addition rate of 5 g·m^-2·a^-1), and N₁₀ (nitrogen addition rate of 10 g·m^-2·a^-1), respectively, in 5 m ´ 5 m plots. Root exudates were collected in June, August and October of 2015, using a modified culture-based cuvette system. Root biomass in each plot was measured with root core method.Important findings The rates of root exudates on biomass, length, and surface area basis all displayed apparent seasonal variations during the experimental period, with the magnitude ranked in the order of: August > June > October, consistent with changes in soil temperature at 5 cm depth. With increases in the nitrogen addition rate, the rate of root exudates on biomass, length, and area basis all trended lower. Compared with the control (N₀), the N₅ and N₁₀ treatments significantly reduced fine root biomass in the Sibiraea angustata shrubbery, by 23.36% and 33.84%, respectively. The decreasing root exudation and fine root biomass in response to nitrogen addition significantly decreased C flux of root exudates. Our results provide additional evidences toward a robust theoretical foundation for better understanding soil C-nutrient cycling process mediated by root exudation inputs in Alpine shrubbery ecosystems under various environmental changes.     

Mammalian herbivory in post-fire chaparral impacts herbaceous composition but not N and C cycling

火后灌丛中哺乳动物食草性影响草本植物组成而不影响氮和碳循环 经典理论预测，草食动物通过选择性植物啃食和富含氮的排泄物的沉积影响草本植物组成和土壤氮循环，其影响取决于生态系统氮的有效性。据预测，草食动物在氮有效性高时可加速氮循环，而在氮有效性低时减慢其循环。然而，在自然系统中对这些理论的实验验证比较有限，并且有些结果相互矛盾。美国加利福尼亚州广泛分布的灌木林地为验证这些理论提供了一个可行的系统。它们易于发生周期性的林冠火，这会暂时移除活的灌木覆盖物，使土壤中的矿质氮沉积，并利于各种草本植物组合在3–5 年内形成主导景观。灌丛也越来越容易受到草本植物的入侵；哺乳动物的食草性可能会限制灌丛下层非本地草本植物的建立。我们设置一项为期两年的植食动物-围封实验，评估火灾后早期灌丛演替期间哺乳动物食草性对草本植物组合和土壤氮和碳循环的影响。我们预测，在火灾后高氮条件下，哺乳类食草动物不会更倾向于取食固氮草本植物，会加速氮循环并减少非本地草本植物的丰富度。研究结果表明，排除哺乳类食草动物后，尽管草本植物的现存生物量增加了54%，但固氮与非固氮草本植物的相对丰富度没有改变，也没有改变氮和碳循环的指标。在两年的实验期间内，草食动物对养分循环的影响可能并不显著，草食动物活动的物理影响可能抵消了植物凋落物和动物粪/尿输入的影响。哺乳类食草动物主要以典型的非本地草本植物为食，略微降低了它们的相对丰度；然而，在火灾后的前两年，哺乳动物的食草性并不能有效地阻止侵入性草本植物对灌丛的入侵，也不能改变植物的碳和氮循环。     

Biomass allocation patterns of Loropetalum chinense

Aims Biomass is the most fundamental quantitative character of an ecosystem. Biomass allocation patterns reflect the strategies of plants to adapt various habitat conditions and play a vital role in evolution, biodiversity conservation and global carbon cycle. Loropetalum chinense shrub is one of the most dominant shrub types in subtropical China. The objectives of this study were to quantify the allometric relationships and the biomass allocation pattern among organs, and to investigate the effects of body size, shrub regeneration origin and site factors on allometry and biomass allocation.
Methods Individual samples of L. chinense were harvested from shrublands in subtropical China and were further divided into leaves, stems and roots. The allometric relationships between different organs were modeled with standard major axis (SMA) regression and the biomass allocation to different organs was quantified. The effects of body size, shrub regeneration origin and other habitat factors on allometry and allocation were examined using Pearson’s correlation analysis and multiple linear regressions.
Important findings The isometric scaling relationships between shoot and root changed to allometric relationships with increasing basal diameter. The scaling relationships between leaf and stem and between leaf and root were isometric for smaller diameter classes, while for larger diameter classes they were allometric. These relationships were significantly different among shrub regeneration origin types. The scaling relationships between different organs were not affected by habitat factors; while the coverage of shrub layer and slope affected biomass allocation due to their influences on the allometric relationships between different organs at the initial stage of growth. The mean dry mass ratios of leaf, stem, root and the mean root to shoot ratio were 0.11, 0.55, 0.34 and 0.65, respectively. With the increase of basal diameter class, stem mass ratio (0.50-0.64) increased, while leaf mass ratio (0.12-0.08) and root mass ratio (0.38-0.28) decreased, and consequently root to shoot ratio (0.91-0.43) also decreased. In secondary shrublands, the leaf mass ratio was 0.12 and the root mass ratio was 0.33, while these values were 0.07 and 0.36 respectively in natural shrublands. The ratio of aboveground allocation was significantly correlated to shrub layer coverage (r = 0.44, p < 0.05). Leaf mass ratio was significantly correlated to slope (r = -0.36, p < 0.05) and root mass ratio was significantly correlated to mean annual temperature (r = 0.34, p < 0.05). Results showed that with the increase of body size, the scaling relationships between different organs of L. chinense changed from isometric to allometric, and more biomass was allocated to aboveground part, and concretely, to stems. Human disturbance affected biomass allocation by its influences on the allometric relationships between different organs, and by increasing biomass allocation to leaves and decreasing allocation to roots. Reduced light resource promoted the biomass allocation to aboveground part, and higher slope resulted in decreased biomass allocation to leaves, while higher mean annual temperature promoted biomass allocation to roots. The variation in annual precipitation had no significant influences on biomass allocation. The biomass allocation strategies of L. chinense partially support the optimal partitioning theory.     

小叶锦鸡儿(Caragana microphylla)灌丛对草本群落特征的影响

基于干旱、半干旱草原灌丛化现象的发展，探究灌木与草本之间的关系对深刻理解灌丛化对草原植物群落特征的影响机制具有重要意义。然而，很少有研究考虑草地类型和灌丛斑块大小对灌木和草本植物之间关系的影响。在内蒙古典型草原和荒漠草原的自由放牧草地上选择了18个小叶锦鸡儿灌丛化样地进行野外采样，并调查了不同大小灌丛和周围草地的植物群落特征。运用单因素方差分析(one-way ANOVA)和最小显著差异法(LSD)来检验不同大小灌丛斑块内外的植被群落特征(高度、密度、地上生物量、凋落物量)和植物多样性指数(Shannon-Wiener指数、Pielou指数、丰富度指数、群落Sprensen相似性系数)的差异性。结果表明：(1)与草地相比，两种草原类型的灌丛产生、捕获了更多的凋落物，灌丛的保育作用显著提高了斑块内草本植物的高度，但灌丛占用了生存空间和资源，从而降低了斑块内草本植物的密度和地上生物量。(2)灌丛对多年生草本植物的地上生物量有明显的抑制作用，但对两种草原类型的一、二年生草本植物没有显著影响(典型草原中的小灌丛除外)。(3)两种草原类型的灌丛对草本植物多样性的影响存在差异。典型草原灌丛内多样性...