云南北部泥石流多发干旱河谷区不同干扰对干扰对土壤种子库的影响

对云南北部的泥石流多发干旱河谷区不同干扰状况下的土壤种子库特征进行了研究,结果表明不同形式的干扰对土壤种子库特征产生不同形式的影响。人工种植合欢（Leucaena glauca)并屏除人和家养动物的影响使土壤种子库的种子密度增大,同时种子组成也由原来的耐旱型为主变为耐荫型为主;马桑（Coriaia sinica)种植并实行年度砍伐降低种子密度并减少了种子类,但主成分的的性质未发生改变;滑坡与水土流失将多种子带入其坡积物中,从而降低土壤种子库密度与组成种类;泥石流最破坏地表土壤层和土壤种子库的最主要因素。     

东川干热退化山地不同植被恢复方式对物种组成与土壤种子库的影响

探讨了在云南东北部干热河谷区域的严重砂石化土地上利用两种典型固氮树种进行植被恢复后对当地原有植被系统的影响。研究表明,不同植被恢复方式对地表植被和土壤种子库的影响是巨大的,物种的组成与密度都发生变化。高密度合欢(Leucaena glauca)恢复方式下,大量当地物种,尤其是一些阳性物种从地表植被中消失或生长受到抑制,生物多样性降低。参照稀灌草丛设计的马桑(Coriaria sinica)恢复方式对原有草坡地物种的数量和多样性影响不大。各种植被恢复方式的土壤种子库的萌发试验表明,合欢恢复方式(L．glauca)使土壤种子库的种子密度增大,同时种子组成也由原来的喜光耐旱为主变为耐荫型为主;马桑(C．sinica)恢复降低了种子密度并减少了种子种类,但主成分的性质未发生改变。一些当地物种仍存在于受影响后的地表植被和种子库中,使改变后的系统与当地草坡间存在着一定程度的相似性,但这种相似性随植被恢复的变化在地表植被与土壤种子库间表现不一致,显现出随干扰与植被恢复变化的非同步性。     

红壤侵蚀区植被恢复过程中土壤种子库变化特征

土壤侵蚀作为一种自然营力和自然干扰形式对土壤种子库的次分布与物种组成具有一定的影响。本研究对典型红壤侵蚀区裸地(Ⅰ号)、马尾松林地(Ⅱ、Ⅲ、Ⅳ号)和次生林(Ⅴ号)等5处不同植被恢复区的土壤种子库物种组成、储量及分布格局进行研究,探究在植被恢复过程中土壤侵蚀对土壤种子库的影响。结果表明: 研究区土壤种子库共统计到21种物种,物种丰富度低,以草本种类为主。各样地土壤种子库密度为56.7～793.3粒·m^-2,样地间差异显著,土壤种子库密度随着土壤侵蚀强度加重而明显下降。各样地浅层0～2 cm土壤种子库密度随着上坡-中坡-下坡的变化均呈增加趋势;剧烈侵蚀地和强烈侵蚀地土壤种子库主要分布在5～10 cm深层土壤内,且中上坡0～2 cm土层几乎没有种子。土壤侵蚀使得土壤种子库在土层中的分布呈现深层化,植被恢复后深层种子库积累仍需要较长的时间。     

天山中部天山云杉林土壤种子库年际变化

通过定点采样,采用萌发法对天山中部天山云杉(Picea schrenkiana Fisch.et Mey.)近熟林(101-120a)和成熟林(121-160a) 2004-2011年(8a)土壤种子库物种组成、种子密度的年际变化和不同间隔年限土壤种子库物种组成的相似性进行了分析.结果表明:(1)土壤种子库中共萌发鉴定出种子植物87种,隶属29科70属,其中乔木种子植物2种,灌木种子植物2种,草本种子植物83种,土壤种子库中草本植物种子密度远远大于木本植物种子密度;8个采样年份土壤种子库恒有种仅有6种;(2)土壤种子库种子密度及其中天山云杉种子密度存在巨大的年际变动,且不具有同步性;土壤种子库种子密度最大(2009年)值为(953.75±66.12)粒/m2,最小(2008年)值为(186.50±20.37)粒/m2,其中天山云杉种子密度最高(2006年)达到(584.50±53.58)粒/m2,最低(2005年)仅有(0.25±0.26)粒/m2;(3)天山云杉林土壤种子库年际间物种组成的相似性不高,Czekanowski相似系数均值仅为0.344,并随间隔年限的增加呈现减小—增大—减小的变化趋势.天山云杉林土壤种子库物种组成和种子密度稳定性差,年际间相差悬殊,物种组成的相似性不高,种子库中天山云杉种子密度主要受其种子库采样前一年天山云杉结实丰歉的影响,属间断型.土壤种子库年际变化特征可为天山森林的更新恢复和可持续经营提供科学依据.     

不同施肥方式对稻麦轮作田土壤杂草种子库的影响

为揭示不同施肥方式(纯施化肥、有机肥配施化肥、秸秆还田配施有机无机肥、有机无机复合肥)对稻麦两熟制地区农田土壤杂草种子库的影响, 在江苏常州金坛区进行了固定施肥试验。经过连续4年试验处理后, 对不同施肥处理下农田土壤杂草种子库杂草种子种类及密度进行了调查, 并对杂草种子多样性、数量、分布与施肥措施的关系进行了分析。结果表明, 与不施肥相比, 施肥有减少稻麦轮作田土壤杂草种子库杂草种子种类数、杂草种子群落均匀度指数和物种多样性指数的趋势, 并使稻麦轮作田土壤杂草种子库杂草种子总密度明显降低。施肥明显提高了土壤杂草种子库菵草(Beckmannia syzigachne)、日本看麦娘(Alopecurus japonicus)、看麦娘(A. aequalis)种子的密度, 施用猪粪堆肥配施化肥处理提高程度更为显著; 秸秆还田配施化肥、秸秆还田配施有机肥化肥、有机无机复合肥施用处理有减少菵草、日本看麦娘、看麦娘杂草种子密度的趋势。施肥明显降低了土壤杂草种子库阔叶杂草种子密度; 施用有机肥有增加土壤杂草种子库水苦荬(Veronica undulata)、蛇床(Cnidium monnieri)种子密度的趋势; 施用猪粪堆肥有增加土壤杂草种子库鸭舌草(Monochoria vaginalis)种子密度的趋势。因此, 不同种类杂草对不同肥料存在偏好性差异, 不同施肥方式造成了土壤杂草种子库优势物种组成的差异。     

内蒙古克氏针茅草原土壤种子库对刈割和放牧干扰的响应

种子库是潜在的植物群落并在一定程度上预示着群落的演替方向。草原牧区自退牧还草政策实施以来,草原利用方式由自由放牧为主逐步转向以围封割草为主。为研究割草和放牧对土壤种子库密度、植物功能群和种类组成的影响及其与地上植被的相似性关系,在内蒙古克氏针茅(Stipa krylovii)典型草原区设置3个不同强度的刈割处理,即无刈割对照(CK)和分别留茬15 cm(M15)、5 cm(M5)的处理,以及一个自由放牧处理(GR),土壤种子库采用环刀法多点取样结合四唑染色法测定种子活力,计数所有被检测有生命力的种子,并计算土壤种子库与地上植被在物种组成方面的相似性。结果表明:不同处理的土壤种子库密度范围为6245.0±1351.9~8155.9±909.1粒·m-2,无刈割对照的土壤种子库密度显著高于M15;从种子库的功能群组成来看,多年生杂类草种子密度最大,占种子库总量的55%~60%,1年生杂类草占36%~43%,GR与M15有显著差异;从物种组成来看,只有克氏针茅、砂韭的种子数量在刈割和放牧处理下显著低于对照。采用Sorensen指数计算土壤种子库与地上植被的物种相似性,CK、GR、M5、M15相似系数分别为0.55、0.58、0.48和0.60;研究预示,内蒙古典型草原土壤种子库对割草和自由放牧有很强的敏感性,刈割和自由放牧均降低土壤种子库密度,将降低退化克氏针茅草原的自然恢复能力。     

天津滨海典型盐碱湿地土壤种子库特征及CCA分析

选取天津滨海地区典型盐碱湿地,进行土壤种子库采样及萌发试验,同时测定土壤理化性质。采用典范对应分析法(CCA)对土壤种子库和土壤特征因子的关系进行研究。结果表明:4个样地土壤种子库储量较大,但物种组成单一,为滨海地区指示性盐生植物。与人工湿地相比,自然保护湿地具有物种丰富度高,群落结构稳定的优点,但受到干扰最小,种子库密度却最低。种子库种子萌发率曲线呈不规则的抛物形状,萌发数量曲线呈"S"型分布,土壤板结程度对萌发率有较大影响。土壤种子库垂直分层结构明显,随土壤深度加深,种子库密度降低,10～15 cm采样层仍保留大量活性种子。通过CCA分析,发现土壤种子库呈现明显的3个聚类;且土壤种子库受全盐量、有机质、pH影响较大,但土壤通透性这一因素也不容忽视。     

塔里木河下游不同退化区地表植被和土壤种子库特征

对塔里木河下游不同退化程度的4个典型断面进行了植被和土壤种子库的取样调查,采用种子萌发试验研究了不同退化区植被和土壤种子库的特征,结果表明:(1)塔里木河下游地表植被表现为严重的逆行演替,具体体现为胡杨林都为过熟林,几乎没有胸径在10cm以下的幼林;植被盖度、密度和多样性指数均维持在一个较低的水平上;随退化程度不断加重,地表植被中草本植物的相对密度、相对盖度和相对频度逐渐降低,而灌木和乔木的相对密度、相对盖度和相对频度逐渐增加;(2)研究区土壤种子库的基本特征是:土壤种子库种类贫乏、密度低、多样性指数和相似性系数不高;(3) 随退化程度的加重,土壤种子库物种数不断减少、密度明显下降、优势种组成趋于单一、表层种子库比例升高、1年生草本植物占优势逐渐向多年生草本植物和灌木植物转变及土壤种子库物种组成与地上植被物种组成上差异显著.     

松嫩草地水淹干扰后的土壤种子库特征及其与植被关系

研究了松嫩平原羊草草地不同强度水淹干扰对土壤种子库种类组成、物种多样性及其与植被物种组成的相似性关系等的影响。结果表明：（1）随着水淹强度的加重或水淹持续时间的延长,相应地段的土壤种子库物种数目和种子存量都呈减小趋势;（2）土壤种子库的种类成分在干扰样带和对照样带间差异明显,而受水淹干扰的样带之间种子库的种类组成差异不大,表明洪水漂移行使了繁殖体传播和散布的功能;（3）随水淹干扰强度增加,种子库物种多样性指数减小;（4）种子库与地上植被物种组成相似性普遍较低,其原因是主要靠营养繁殖以更新种群的多年生根茎植物经常在植被中出现而不在种子库中出现;（5）种子库与地上植被物种组成相似性随水淹干扰强度增加而下降,表明了水淹干扰对种子库与地上植被物种组成相似性有一定程度的影响。     

元江流域干热河谷灌草丛土壤种子库与地上植物群落的物种组成比较

土壤种子库与地上植被之间的关系和相似性是长期争议的群落生态学问题之一。本研究旨在通过比较元江流域干热河谷典型灌草丛群落与其土壤种子库的物种组成, 探讨土壤种子库与地上植物群落存在怎样的相似性关系。在元江干热河谷上、中、下游选取典型灌草丛群落, 采用典型样地调查法进行植物群落调查, 同时在样方内采集0-5 cm、5-10 cm、10-15 cm三层土壤样品, 采用萌发实验研究土壤种子库的种子数量和物种组成, 并与地上植物群落进行比较。结果表明: (1)全部调查样方的地上植被中共包含种子植物76种, 隶属于25科64属, 主要集中在豆科、禾本科、菊科、大戟科, 群落物种组成以多年生草本为主、灌木为辅; (2)土壤种子库中共发现33种植物, 隶属于14科32属, 以旱生型禾本科、豆科、菊科物种为主; (3)土壤种子库中的植物种子密度在表层土壤中最高, 随着土层的加深而递减; (4)各样方的土壤种子库与地上群落共有物种数较少, 相似性较低; 土壤种子库密度与地上群落的种群密度没有显著的相关性。总体而言, 本研究发现元江流域干热河谷典型灌草丛群落其土壤种子库与地上群落之间没有显著的相关性, 并且地上群落和土壤种子库都有外来入侵种类。     

普洱市周边地区4种土地利用类型土壤种子库特征

通过对云南普洱市周边地区次生季风常绿阔叶林、针阔混交林、人工更新形成的针叶林及茶园等4种土地利用类型的野外调查及土壤种子库的萌发实验,探讨其土壤种子库的密度大小、物种丰富度和组成及与地上植被的关系。结果表明:干扰强度与频度不同导致土地利用类型之间土壤种子库密度与物种丰富度存在较大差异,土壤种子库密度大小顺序为:针叶林(248.67±116.86)粒·m-2>针阔混交林(186.00±43.27)粒·m-2>次生季风常绿阔叶林(107.33±16.48)粒·m-2>茶园(51.67±10.17)粒·m-2;茶园土壤种子库物种丰富度要显著低于其他类型。4种土地利用类型土壤种子库生活型组成差异极显著,主要以草本植物组成,以菊科与禾本科占优势;针阔混交林的草本植物种子密度最多,非森林的原生物种是草本植物的主要组成;针叶林外来物种的种子密度要显著高于其他类型,紫茎泽兰(Eupatorium adenophorum)是其主要组成。土壤种子库与地上植被的相似性系数较低,其大小顺序为:次生季风常绿阔叶林(0.175)<针阔混交林(0.176)<针叶林(0.215)。     

Small seed bank in grasslands and tree plantations in former grassland sites in the South Brazilian highlands

The soil seed bank can be an important source for vegetation regeneration, and data on the similarity between aboveground vegetation and the seed bank can provide information about successional pathways after disturbances or land-use change. We conducted this study in natural grasslands in the subtropical highland region in southern Brazil. We evaluated the effect of silviculture on richness, density, and composition of the seed bank at former grassland sites converted to pine plantations 25 years ago. We worked at six grassland sites and three pine plantation sites and used the seedling emergence method. Seed bank density and richness in grasslands were lower than those reported in similar environments in other regions. Species richness and density varied considerably within each vegetation type; therefore, richness and density were not statistically significant, while composition varied among vegetation types. In terms of species, the pine plantation seed bank was a small subset of the grassland seed bank. Seeds of typical grassland species were missing in the pine plantation, but also had only low abundances in the grassland, and similarity of seed bank and vegetation were low (less than 20%). The low seed density found in this study, including in grasslands areas, indicates that regeneration of species from the soil seed bank likely is of a limited role for the maintenance of plant populations after disturbances in this system. Our data further suggest that natural regeneration after tree planting in grasslands is reduced due to seed limitation.     

森林草原过渡带持久土壤种子库沿降水梯度的格局

为了解全球气候变化背景下森林草原过渡带持久土壤种子库对未来降水减少的响应,本研究以呼伦贝尔森林草原过渡带为研究区域,沿降水梯度采集0～10 cm土层的持久土壤种子库样本,研究种子库密度、物种组成、多样性及其与地上植被的关系,并利用结构方程模型研究年降水量对持久土壤种子库的直接影响及其通过地上植被和土壤有效氮、有效磷、土壤pH值产生的间接影响。结果表明: 随着降水量的降低,种子库密度和物种丰富度有增加趋势,森林草原过渡带草地土壤种子库物种多样性高于森林。土壤种子库与地上植被相似性整体较低。结构方程模型结果显示,年降水量对种子库的密度和物种丰富度的总效应为负效应,标准路径系数为-0.051和-0.122。年降水量对种子库的密度和物种丰富度的直接效应为正效应,降水量通过土壤全氮对种子库密度和物种丰富度产生显著的间接正效应,通过土壤pH和土壤有效磷对种子库物种丰富度产生显著的间接负效应,通过土壤pH对种子库密度产生显著的间接负效应。气候变化下降水减少会改变植物应对风险的策略,森林草原过渡带的持久土壤种子库对应对未来可能发生的降水减少具有一定的缓冲作用。     

Soil seed bank in different vegetation types in the Loess Plateau region and its role in vegetation restoration

In the Loess Plateau region, soil erosion is a serious problem. Vegetation restoration is an effective approach to control soil erosion and improve ecosystems. The soil seed bank generally plays an important role in vegetation restoration after disturbance. Thus, we reviewed soil seed bank studies to reveal the soil seed bank characteristics and its role in vegetation restoration in three vegetation types (forest, forest‐steppe, and steppe). We selected 38 seed bank studies and analyzed several seed bank characteristics, such as seed density, species composition, and the relationship between seed size and seed bank. We also assessed the role of the soil seed bank in vegetation restoration. The soil seed bank density ranged from 2,331 ± 1,993 to 6,985 ± 4,047 seeds/m² among the different vegetation types. In the soil seed bank, perennial herbs and grasses accounted for 51.5% of the total species. Native species that were dominant or common in the standing vegetation usually had relatively high seed bank densities. Moreover, species with smaller seeds generally had higher soil seed bank densities. The present study indicates that the soil seed bank plays a significant role in spontaneous vegetation restoration, especially during the early successional stages in abandoned slope farmlands and grazing‐excluded grasslands. However, species with large seeds or transient soil seed banks should be reintroduced through seeding to accelerate target species restoration. More studies on soil seed banks need to be conducted to comprehensively reveal their characteristics.     

Effects of disturbance intensity on seasonal dynamics of alpine meadow soil seed banks on the Tibetan Plateau

Background and Aims

Information on soil seed bank processes is crucial for understanding vegetation dynamics. Despite the documented importance of soil seed banks in many ecosystems, their role is not fully understood in some sensitive habitats, such as the alpine meadows of the Tibetan Plateau.

Methods

We studied the seasonal dynamics of the germinable soil seed bank under four disturbance intensities in an alpine meadow on the Tibetan Plateau as well as seed size distribution relative to disturbance intensity. Composition of the seed bank was compared with that of the standing vegetation.

Results

Density of buried seeds increased with disturbance intensity, but species richness and species diversity decreased. Seed density and species richness of the seed bank varied seasonally in all layers (0–2, 2–7, 7–12 cm) and the whole (0–12 cm). The species composition of seed bank was not significantly influenced by season. There was no trend in seed size distribution as disturbance increased. Seasonal seed bank turnover rates increased with increase in disturbance. The result of the NMDS showed that species composition of seed bank and vegetation exhibited a fairly uniform pattern in each season.

Conclusions

Although as a whole the species composition of the vegetation and seed bank showed a relatively low degree of similarity in each season, similarity was highest in the most disturbed habitat. There was no alteration in species composition of seed bank regardless of disturbance intensity, but seed density decreased as disturbance increased. Disturbances in alpine plant communities might increase persistence of regeneration niches. Regeneration from the seed bank together with vegetative reproduction contributed to aboveground vegetation in highly disturbed habitats. Clonal species played an important role in regeneration of vegetation in slightly disturbed areas, where there was little contribution of ruderals from soil seed banks.     

Variation in soil seed bank species composition of a dry coniferous forest: spatial scale and sampling considerations

In order to assess the effects of disturbance on soil seed bank spatial structure, variation in seed bank species composition was analyzed at two spatial scales in mature (undisturbed) and recently disturbed stands of Interior Douglas-fir forest in south-central British Columbia. Coarse-scale analysis among stands 10–100 km apart using Multi-Response Permutation Procedures showed that individual mature stands were mainly characterized by unique seed bank species compositions. Disturbance had an homogenizing effect on seed bank species composition at the coarse scale––there was less variability among stands following disturbance by both low and high severity fires, and by non-salvage logging. In contrast, finer scale analysis among sampling units c. 10 m apart showed that heterogeneity in seed bank species composition was greater on severely burned and logged sites, commensurate with greater levels of soil disturbance, than on lightly burned and undisturbed sites. Despite the high intensity of seed bank sampling (sixty 25 cm² soil samples from each of 16 sites), species-area curves leveled off only when infrequent species were removed from the dataset. The number of seed bank samples required to account for the common species ranged from 84 on severely burned sites, to 196 on undisturbed sites; more than the 240 samples collected per disturbance class in this study would have been required to account for the remaining infrequent species. Overall, this study highlights the importance of sampling intensively within multiple stands to capture the variation in species composition inherent to these dry coniferous forest soil seed banks.     

Disturbance Effects on the Seed Bank of Mexican Cloud Forest Fragments1

The density and floristic composition of the soil seed bank was assessed in six cloud forest fragments with different levels of human disturbance in central Veracruz, Mexico. A total of 8416 seeds germinated in 60 soil samples, at 5‐cm depth, corresponding to 107 species, 85 genera, and 48 families. Significant differences were found among study sites in seed densities with values ranging from 873 to 3632/m². Tree species contributed 20 percent of the total soil seed bank in four sites and herbs accounted for the majority of the species in each site. Among tree species, Trema micrantha displayed the highest seed density, accounting for 84 percent of the germinated seeds. In general, the tree species composition of the soil seed bank did not closely reflect the composition of the tree community. Results suggest that disturbance produced by human activities (trail use, selective cutting of trees, livestock) may influence the size and composition of the soil seed bank in forest fragments. Sites where human activity has been reduced showed the highest proportion of dormant seeds.     

Seed bank diversity in mesic grasslands in relation to vegetation type,management and site conditions

Questions: 1. Do different management types (i.e. hay meadow, silage meadow, meadow‐pasture, pasture) have different impact on the size and composition of the seed bank of mesic grassland (Arrhenatheretalia)? 2. How strong is the effect of management on the seed bank in relation to above‐ground vegetation, edaphic factors and land‐use history? 3. Are there differences in C‐S‐R plant strategy types and seed longevity under different management regimes? Location: Lahn‐Dill Highlands in central‐western Germany. Methods: Above‐ground vegetation and the soil seed bank of 63 plots (at 21 sites) in mesic grasslands were studied. Differences between management types in quantitative seed bank traits and functional characteristics were tested by ANOVA. The impact of management, above‐ground vegetation, site conditions and land‐use history on seed bank composition were analysed by partial CCA. Results: Management had no significant impact on species richness and density of the seed bank but significantly influenced their floristic composition and functional characteristics. CCA revealed that even after adjustment for soil chemical parameters and above‐ground vegetation management still had significant impact on seed bank composition. ANOVA revealed that silage meadows contained higher proportions of R‐strategy compared to hay meadows. In contrast, in hay meadows and meadow‐pastures proportions of S‐strategy were higher than in silage meadows. Conclusions: The type of grassland management has little impact on quantitative seed bank traits. Management types with a high degree of disturbance lead to an increase of species following a ruderal strategy in the seed bank. Irrespective of management type only a limited proportion of characteristic grassland species is likely to re‐establish from the seed bank after disappearance from above‐ground vegetation.