Responses of dune mosses to experimental burial by sand under natural and greenhouse conditions

Sand movement is a predominant feature of mobile coastal and lake-shoreline sand dunes. Plants growing in these environments are able to withstand and survive periods of burial by sand. Although mosses are important dune stabilizers in temperate dunes, there are few studies focused on their response to burial by sand. In this study we examined the effects of burial by sand on 11 moss species that grow naturally on Lake Huron sand dunes and occur in a gradient of habitats from the foredunes along the shore to forested areas. Artificial burial treatments (sand depth of 0, 1, 3, 5 and 7 cm) were imposed under greenhouse and field conditions. We measured final plant cover and calculated the speed of emergence and an interpretive index (tolerance index) to compare burial responses among species by calculating a burial ratio which standardized the initial size of each species. In the greenhouse, Ceratodon purpureus and Ditrichum flexicaule recorded the highest mean speeds of emergence and Dicranum scoparium, Plagiothecium laetum, Dicranum flagellare and Brachythecium sp. 1 the lowest. In the field the trends were similar although the speed of emergence was much slower. Three types of response to burial were evident in plant cover: neutral, inhibition and stimulation. Although all eleven studied species were able to emerge from the different depths of burial, we observed that species colonizing areas with high sand mobility and deposition (C. purpureus and D. flexicaule) were the most tolerant and emerged from depths of up to 35 times their height. Species growing inland, at the base of trees (Dicranum scoparium, Brachythecium sp. 2, Plagiomnium cuspidatum and Dicranum flagellare) showed the least tolerance of burial.     

Seedling growth variation in response to sand burial in four <Emphasis Type="Italic">Artemisia</Emphasis> species from different habitats in the semi-arid dune field

We compared seedling growth of four Artemisia species dominated at different habitats to determine whether interspecific seedling growth variation of a same genus in tolerance to burial can be used to explain plant distribution in the sand dune field. Interdune lowland species, Artemisia gmelinii, stabilized dune species, A. frigida, semi-stabilized dune species, A. halodendron, and active dune species, A. wudanica were selected. Seedlings grown for 3 weeks were treated at five burial depths for three burial times in pot experiments. Species from the habitats with little burial had smaller survival rate, dry weight and stem elongation speed than those from the habitats with intensive burial when buried. Furthermore, when buried, the former tended to adjust biomass allocation between shoot and root and produce adventitious buds, while the latter tended to maintain a constant root:shoot ratio and produce adventitious roots. We conclude that (1) seedlings of species with a long evolutionary history of exposure to sand burial (from the active sand dune), show quicker stem growth when buried than do seedlings of species from the habitats with little or no sand burial; (2) seedlings of species which do not change root:shoot ratio might be more tolerant of sand burial than those do; (3) seedlings of species from the habitats with intensive sand burial is prone to produce adventitious roots and seedlings of species from the habitats with little or no sand burial tend to produce adventitious buds when buried.     

沙埋与供水对毛乌素沙地两种重要沙生植物幼苗生长的影响

沙埋与水分是影响毛乌素沙地植物存活、生长的关键因子。通过沙埋与供水的野外控制实验,研究了毛乌素沙地重要物种柠条(Caragana korshinskii)与羊柴(Hedysarum laeve)幼苗存活及生长对沙埋和供水的反应。结果表明:适量的沙埋(0.25H-0.50H沙埋,H为苗高)与供水(柠条50mm/月,羊柴75mm/月)可以促进幼苗生长,过量的沙埋与供水则会抑制生长甚至导致幼苗死亡。柠条幼苗在50mm/月供水,0.25H、0.50H沙埋,羊柴幼苗在75mm/月供水,0.25H、0.50H沙埋下具有较高的相对生长速率和净同化速率;幼苗在1.0H和1.25H沙埋下全部死亡。供水量较小、沙埋较浅时,两种植物根冠比均较高;当供水量最大时,柠条幼苗根冠比在沙埋最深和没有沙埋时较大,而羊柴幼苗根冠比仍在没有沙埋时最高。     

Plant species and community responses to sand burial on the machair of the Outer Hebrides,Scotland

Question: Is there a critical depth of burial by sand beyond which species and communities fail to recover, and does repeated incremental burial have a greater impact than a single large deposition? Location: The machair on the calcareous sand dunes on South Uist, in the Outer Hebrides of Scotland, UK. Methods: Eight turves were collected from each of four machair sub‐community types. After acclimatization in an unheated polythene tunnel, they were buried with sterilized machair shell sand, either by one single burial to 5 cm or by five applications of 1 cm of sand at approximately seven‐week intervals. Species response was recorded on five occasions. Results: Within machair sub‐communities, burial by sand reduced the abundance (local rooted frequency) of plants more than it reduced species richness. Intermittent burial was more damaging than a single burial event. Those species with the highest pre‐burial frequencies tended to dominate recovery in the sub‐community as a whole. Species occurring across all four sub‐community types exhibited varying responses to community burial between the differing types. Samples from slack sub‐communities had distinctly different response characteristics from those of foredunes and unploughed and three‐year fallow dune grassland. Conclusions: The perennial life‐form of many machair species has been evolutionarily selected for and dominates throughout the machair habitat. Account needs to be taken of competitive interaction between species in relation to burial response. The results of the investigation show that the hypotheses of Gilbertson et al. and Kent et al. on ‘machair stratification’ require refinement in that frequency of shallow burial can be as important as overall burial depth.     

Do partially buried dune plants grow in optimal trajectories?

Plant adaptations minimising costs of burial responses are vital in mobile dune ecosystems. Conventionally, the burial responses of dune plants have been measured as vertical growth. However, a model developed here shows that growth normal to accumulating non-horizontal dune surfaces requires up to 18% less stem production than vertical growth. To determine whether dune plants grow with this optimal geometry a field survey of growth trajectories was made for three coastal plants, and a greenhouse experiment tested whether plants could actively change growth trajectories away from vertical. In the field and greenhouse partial burial resulted in shifts towards vertical growth, indicating that negative gravitropism is the major response to burial, and reduces the amount of stem needed to respond to burial relative to unburied growth trajectories. However, for two species in the field many buried stems grew closer to optimal (shorter) than vertical, mostly on northward, sun-facing dunes. Thus phototropism is the major stimulus for non-vertical growth, and coincides with optimal trajectories on north-facing dunes. Arctotheca populifolia also displayed non-vertical growth after burial on steep south-facing dunes, but responded to burial in the greenhouse with vertical growth. Measurements of the pressure of sand avalanches occurring on dune slipfaces and stem elasticity indicated that deep avalanches were sufficient to orient the flexible shoots of A. populifolia towards optimal trajectories. Thus, dune plants respond to burial by actively modulating growth towards vertical via negative gravitropism, and passively towards non-vertical—more optimal—trajectories via phototropic growth and the influence of sand avalanches.     

Spatial and temporal variability during primary succession on tropical coastal sand dunes

Abstract. We studied primary succession on mobile tropical coastal sand dunes over an 8‐yr period. Every six months, we monitored changes in species composition and sand movement in permanent quadrats located on the windward slopes, the arms and the crests. Our results indicate that sand movement decreased over time but was significantly higher on the slopes and crests than on the arms. In all cases, there were seasonal fluctuations in sand movement which increased during the period with strong northerly winds and decreased during the rainy season. Sand movement was significantly correlated with species distribution. Plant cover and species richness increased at all three locations. Diversity increased on the slope, decreased on the arms and remained unchanged on the crest. However, the equitability values indicated the dominance of a few species, especially at the end of the study period. Temporal trends and species turnover rates differed among locations. Species turnover occurred first on the arms (1994), then on the crests (1998) and lastly on the slopes (at the end of the study period). In all cases the tall grass, Schizachyrium scoparium var. littoralis, became dominant over the endemic legume, Chamaecrista chamaecristoides var. chamaecristoides. Similar to temperate dunes, primary succession on tropical sand dunes was spatially and temporally heterogeneous.     

荒漠绿洲边缘区泡泡刺种群对风沙干扰的响应

研究了位于黑河中游荒漠绿洲外缘 (荒漠与绿洲过渡带 )戈壁与沙漠两种生境下泡泡刺种群对风沙干扰的响应。结果表明 ,因风沙干扰的响应 ,泡泡刺种群以斑块状格局形式存在 ;独立灌丛沙堆的形成途径主要有 4种 :种子发育、根蘖繁殖、较大的沙堆退化 (生境破碎化 )和邻近沙堆的兼并。水分条件是泡泡刺种群生长的重要制约因素 ,长期对有限的水分资源竞争 ,使其大小和空间分布都形成了明显的特征。绿洲与戈壁交错带 (类似戈壁生境 )样地的泡泡刺种群的沙埋深度、种群高度、种群盖度、种群大小、生物量都小于绿洲与沙漠交错带 (类似沙漠生境 )样地的泡泡刺种群的相应的种群特征变量 ,而绿洲与戈壁交错带样地的泡泡刺种群密度却大于绿洲与沙漠交错带样地的相应的种群特征变量。绿洲与戈壁交错带样地的泡泡刺种群密度为33.3株 / m2 ,而绿洲与沙漠交错带样地的泡泡刺种群密度为 2 5 .4株 / m2 。两样地泡泡刺种群的沙埋深度、种群高度、盖度、密度及大小存在着显著差异 ,只有生物量无显著差异。两样地中泡泡刺的沙埋深度对泡泡刺种群特征的影响明显 ,无论戈壁还是沙漠生境 ,沙埋深度与种群高度、种群大小、种群生物量明显正相关。适度沙埋可以促进泡泡刺种群的生长 ,但当沙埋深度超过10 0 cm时 ,又会对泡泡刺种群     

Biomass reallocation and the mobilization of leaf resources support dune plant growth after sand burial

The stimulation of dune plant growth in response to burial is a vital attribute allowing survival in areas of mobile sand. Numerous resource-related and physiological mechanisms of growth stimulation have been suggested in the past, but few have been tested comparatively. Manipulation experiments using Scaevola plumieri, an important subtropical coastal dune forming species, demonstrated that physiological shifts were of great importance in determining the nature of the stimulation response to burial. The production of stem length and replacement of leaf area were stimulated by burial, whereas net mass production was similar between buried and unburied treatments. Remobilization of buried leaf resources, seasonal effects, and a shift in biomass allocation to stem production played the greatest role in the compensatory growth response. Other factors, such as increased soil nutrients, changes in photosynthesis, and changes in the costs of producing tissue were of less importance. Thus, the stimulated growth of species adapted to live on mobile dunes is explained by a number of resource-related and physiological mechanisms acting in concert.     

Effects of denudation and burial on growth and reproduction of <Emphasis Type="Italic">Artemisia ordosica</Emphasis> in Mu Us sandland

Plants in a dune environment have a high risk of being denudated by wind or buried by sand. We conducted a field experiment to assess growth and reproductive performance as well as biomass allocation of Artemisia ordosica after denudation and burial. Height growth decreased after denudation, but remained constant after burial; biomass was reduced by severe burial, but not by moderate ones. Vegetative growth measured by current-year generated vegetative branches declined with increasing severity of burial. Reproductive maturity was not affected by either denudation or burial, and reproduction decreased only after severe denudation. After denudation, biomass allocated to reproduction was greatly reduced, as shown by strongly reduced biomass allocation to fruits and whole reproductive branches, but that allocated to current-year vegetative growth was maintained. Biomass allocation to reproduction and vegetative growth remained rather stable after burial. Current-year reproductive-to-vegetative-biomass ratio was lower after denudation than after burial, indicating that vegetative growth was more favored by A. ordosica after denudation. These modifications are adaptive in the fluctuating environment of mobile sand dunes where denudation and burial frequently occur.     

沙埋对中间锦鸡儿幼苗生长发育的影响

在沙地环境中,沙埋是影响植物幼苗存活的一个重要因素。中间锦鸡儿(C arag ana interm ed ia)是浑善达克沙地和毛乌素沙地固定和半固定沙丘上常见的一种沙生灌木。为了研究沙埋对其幼苗存活以及生长的影响,对出土后生长了1个月的中间锦鸡儿实生苗进行沙埋实验,实验处理:TC为对照,T1为沙埋幼苗地上部的1/3,T2为沙埋幼苗地上部的1/2,T3为沙埋到幼苗的近顶端。实验持续4周,每周收获1次。结果表明:TC、T1和T2没有幼苗死亡,T3有20%的幼苗死亡;沙埋对中间锦鸡儿幼苗的生物量、根冠比、根生物量比和茎生物量比有显著影响,叶片生物量比各处理没有显著差异,沙埋对幼苗的叶面积没有显著影响,在第1周T2和T3的小叶片面积显著大于TC,在其余3周,TC与T1、T2的小叶片面积没有显著差异,与全埋则有显著差异;沙埋对幼苗的相对生长速率(RGR)和净同化速率(N AR)产生显著影响,实验结束时,T3处理幼苗的RGR和N AR显著地小于其它3个处理。上述结果表明,部分沙埋(T1、T2)对沙生灌木中间锦鸡儿幼苗的生长发育没有显著的影响,而全部沙埋(T3)对其幼苗的生长发育产生显著的抑制,中间锦鸡儿是一个比较耐沙埋的物种。     

沙埋和种子大小对固沙禾草沙鞭的种子萌发与幼苗出土的影响

该文研究了野外条件下不同深度的沙埋对沙鞭(Psammochloa villosa)种子萌发和幼苗出土的影响,以及温室条件下种子大小对不同深度沙埋后的种子萌发和幼苗出土的影响。结果表明,沙埋深度显著影响沙鞭的种子萌发率、幼苗出土率和种子休眠率。沙子表面的种子不能萌发。2 cm的浅层沙埋时的种子萌发率和幼苗出土率最高,1 cm 沙埋的种子萌发率和幼苗出土率次之。沙埋深度超过2 cm之后,沙鞭的种子萌发率和幼苗出土率与沙埋深度呈负相关。2 cm的种子休眠率最低。从2 ~12 cm,种子休眠率随着沙埋深度的增加而增加。在幼苗能够出土的深度(1~6 cm),幼苗首次出土所需的时间随着沙埋深度的增加而延长。种子大小对沙鞭的种子萌发率没有显著影响。但是在深层沙埋(6 cm)时,与小种子相比,大种子产生的幼苗的出土率较高。从2~6 cm,大种子形成的幼苗的茎长度都较长。     

Notes on Lejeuneaceae: I. Microlejeunea diversiloba (Spr.) K.M.

Abstract

Previous work on the bryophytic component of dune communities has demonstrated changes in the representation of species with the progress of succession. The ability of some to act as pioneers and the restriction of others to later stages may be associated with their reactions to recurrent burial by wind-blown sand.

Eighteen species were selected for experimental investigation of the effects of sand burial, along the following lines:

(a) Transplants. Samples of eight species were transplanted to four sites representing different stages of the dune succession. Where the sand increment over 11 months exceeded about 4 cm. none survived but species found naturally in mobile dune areas emerged from about 3 cm. Those belonging to fixed dune communities survived only in the absence of burial, although on excavation all species showed some upward growth through the covering sand.

(b) Experimental burial, Method I: samples of the same eight species, grown in pots standing in water but not watered from above, were buried in sand to depths of 1, 2, 4, 5 and 6 cm. The maximum depth through which emergence took place was 4 cm., from which Ceratodon purpureus, Bryum pendulum and Brachythecium albicans reappeared. From shallower layers, however, a greater rate of emergence was shown by Tortula ruraliformis. Pseudoscleropodiun purum and Climacium dendroides did not survive depths greater than 2 cm., and 1cm. was the maximum for Hylocomium splendns and Rhytidiadelphus squarrosus.

Method II. Sample strips of fourteen species were placed in aquarium tanks and, apart from a small portion len exposed, were buried under a sand slope grading up to 7 cm. in depth. Watering was from above and the humidity was kept high by glass lids. The time taken for the appearance of shoots from increasing depths was recorded, also the periods required for reestablishment from increasing depths of 50% and 100% of the original shoot density. For species tested by both methods the results were in most cases similar. Marked powen of recolonization were also shown by Polytrichum piliferum, P. juniperinum and Pohlia annotina.

In P. annotina, Ceratodon purpureus and Dicramum scoparium re-establishment by means of vertically extending rhizoids producing protonemata at the surface is described.

The maximum depth from which the various species can emerge, the depths from which effective recolonization of the surface is achieved within a fairly short time, the ability to produce rhizoids in the overlying sand and the growth-form of the shoots on emergence are regarded as the most significant aspects of reaction to burial, in relation to the role of the species in their natural habitats.     

Zonation of vegetation on lacustrine coastal dunes: effects of burial by sand

More than 50 years ago it was proposed that zonation of major plant species on coastal dunes was determined by salt spray. Here, we argue against this hypothesis because (i) salt concentrations rarely exceed toxic levels; (ii) high precipitation in temperate latitudes washes the salt off the plants; (iii) major salt spray events occur in late autumn and winter when plants are dormant; and (iv) zonation also occurs on lacustrine dunes. Instead, we show evidence that zonation may be caused by burial because plant distribution was correlated with sand deposition and species were eliminated when burial exceeded their limits of tolerance, thus creating zones of different plant species. We conclude that in temperate regions (i) burial by sand may be among the most important factors in zonation, while salt spray may play a secondary role; and (ii) single environmental factors cannot be the determinants of a phenomenon as complex as species zonation.     

Responses of Hedysarum Laeve, a guerrilla clonal semi-shrub in the Mu Us sandland, to local sand burial

In arid and semi-arid inland deserts,one of the environmental stresses for plants is recurrent sand burial,which can influence the physical and biotic microenvironments of the plants and soil.Previous studies have shown that different levels of sand burial have different effects on plants.Slight sand burial could increase the height increment,leaf biomass and the number of new ramets of the plants while heavy sand burial could impair the growth of the plants and even decrease their chances of survival.In other words,below a certain threshold level of burial,the growth of plants is stimulated probably because of multiple factors.However,as the level of burial increases,the positive response starts to decline until it becomes a negative value.Arid and semi-arid inland deserts are frequently colonized and stabilized by many rhizomatous clonal plants.Clonal physiological integration often helps clonal plants buffer local environmental stress encountered by ramets.A rhizomatous clonal semishrub,Hedysarum laeve (H.laeve),is the dominant plant species and important for vegetation restoration in the Mu Us sandland.To investigate whether clonal integration can increase the threshold of sand burial and help rhizomatous H.laeve tolerate heavy sand burial,we conducted a field experiment.The results showed that slight sand burial could accelerate ramet growth and enhance leaf biomass,stem biomass and shoot biomass,while heavy sand burial reducesed the biomass of the plant and impairs survival and growth of the ramets.Clonal integration increased the threshold of sand burial.Under heavy sand burial,ramets connected to other ramets not buried in sand were more in terms of height increment,stem biomass,leaf biomass and shoot biomass compared to the ramets encountering sand burial but disconnected from other ramets.It suggested that clonal physiological integration could help H.laeve ramets tolerate relatively heavy sand burial.We also discussed that clonal integration plays a role in H.laeve presence in the Mu Us sandland.     

Is zonation on coastal sand dunes determined primarily by sand burial or by salt spray? A test in New Zealand dunes

There has long been controversy on which environmental factor is the predominant determinant of community zonation on sand dunes. It is demonstrated here that, on a dune system in southern New Zealand, several environmental factors that could limit growth all vary along the sea-to-inland sand dune zonation: soil moisture, soil nutrients, wind exposure, sand burial, salt spray and soil salinity. Correlation of the responses of 30 species to experimental stress (burial, darkness, rooting-medium salinity and salt spray) with the zonation of the species in the field indicates that, in the four dune systems studied, sand burial and salt are both important, with salt generally being the more important. However, the relative importance of the factors differs between sites.     

毛乌素沙地游击型克隆半灌木羊柴对局部沙埋的反应

不同程度的沙埋是生长在干旱和半干旱区内陆沙丘的植物经常遭遇的事件,沙埋可以改变植物所处的生物和非生物环境条件。已有研究表明不同程度的沙埋对于植物的影响不同。轻微程度的沙埋可以增加植物高度、促进生物量的积累和新生分株的产生。如果沙埋强度不断增加,对植物的影响由正效应逐渐转变为负效应。即超过一定沙埋阈值后,沙埋会削弱植物的生长,甚至影响植物的存活。干旱和半干旱区内陆沙丘中常常生长着许多克隆植物,克隆整合常常可以缓解克隆植物分株所遭受的局部环境胁迫。根茎型克隆植物羊柴(Hedysarum laeve)是毛乌素沙地的优势半灌木之一,也是当地重要的固沙植物。为了探讨克隆整合的作用是否可以提高沙埋阈值,并有助于羊柴忍受高强度的沙埋,以其为研究对象开展了野外实验。结果表明:轻微程度的沙埋(例如沙埋深度是原始羊柴分株高的10%~20%)可以加速羊柴分株的高生长,提高叶片生物量、茎生物量以及整个地上部分的生物量。高强度的沙埋(例如沙埋深度是原始羊柴分株高的80%~100%)会削弱羊柴分株的存活和生长。在与不遭受沙埋分株相连的情况下,羊柴分株遭受沙埋的阈值高于没有分株相连的,而且在高强度的沙埋下,前者(有分株相连的遭受沙埋的分株)比后者(没有分株相连的遭受沙埋的分株)在株高增量、茎生物量、叶片生物量以及地上分株生物量上都要显著高。这暗示着克隆整合提高了羊柴遭受沙埋的阈值并有助于羊柴分株忍受高强度的沙埋。     

沙埋对半灌木羊柴幼苗的存活、生长和生物量分配的影响

羊柴(Hedysarum laeve Maxim.)是中国北方沙地飞播进行植被恢复与重建的主要植物种.在晚春与夏初的出苗期 ,羊柴幼苗经常遭受不同深度的沙埋.研究旨在探明沙埋对羊柴幼苗存活、生长和生物量分配格局的影响.6周的沙埋试验结果显示:当沙埋深度达到其株高时,约有70%的幼苗死亡 ;沙埋深度达到其株高的133%时,可使羊柴幼苗全部死亡;沙埋深度分别为株高的33%和67% 时,羊柴幼苗的整株生物量、叶片生物量、根系生物量以及相对生长率都相应地高于非沙埋的对照(即:0%沙埋).与非沙埋的对照相比,羊柴幼苗在33%和67%沙埋条件下并不显著地改变其生物量分配格局;并且羊柴幼苗的叶数和株高与对照无明显差异,但试验期内的新生叶数是沙埋处理(即:33%、67%和100%沙埋)的幼苗明显地高于非沙埋的对照.     

沙埋对半灌木羊柴幼苗的存活、生长和生物量分配的影响

羊柴 (HedysarumlaeveMaxim .)是中国北方沙地飞播进行植被恢复与重建的主要植物种。在晚春与夏初的出苗期 ,羊柴幼苗经常遭受不同深度的沙埋。研究旨在探明沙埋对羊柴幼苗存活、生长和生物量分配格局的影响。6周的沙埋试验结果显示 :当沙埋深度达到其株高时 ,约有 70 %的幼苗死亡 ;沙埋深度达到其株高的 133%时 ,可使羊柴幼苗全部死亡 ;沙埋深度分别为株高的 33%和 6 7%时 ,羊柴幼苗的整株生物量、叶片生物量、根系生物量以及相对生长率都相应地高于非沙埋的对照 (即 :0 %沙埋 )。与非沙埋的对照相比 ,羊柴幼苗在 33%和 6 7%沙埋条件下并不显著地改变其生物量分配格局 ;并且羊柴幼苗的叶数和株高与对照无明显差异 ,但试验期内的新生叶数是沙埋处理 (即 :33%、6 7%和 10 0 %沙埋 )的幼苗明显地高于非沙埋的对照。     

Factors influencing the natural regeneration of the pioneering shrub Calligonum mongolicum in sand dune stabilization plantations in arid deserts of northwest China

Calligonum mongolicum is a successful pioneer shrub to combat desertification, which is widely used for vegetation restoration in the desert regions of northwest China. In order to reveal the limitations to natural regeneration of C. mongolicum by asexual and sexual reproduction, following the process of sand dune stabilization, we assessed clonal shoots, seedling emergence, soil seed bank density, and soil physical characteristics in mobile and stabilized sand dunes. Controlled field and pot experiments were also conducted to assess germination and seedling emergence in different dune soil types and seed burial depths. The population density of mature C. mongolicum was significantly different after sand dune stabilization. Juvenile density of C. mongolicm was much lower in stabilized sand dunes than mobile sand dune. There was no significant difference in soil seed bank density at three soil depths between mobile and stabilized sand dunes, while the emergence of seedlings in stabilized dunes was much lower than emergence in mobile dunes. There was no clonal propagation found in stabilized dunes, and very few C. mongolicum seedlings were established on stabilized sand dunes. Soil clay and silt content, air‐filled porosity, and soil surface compaction were significantly changed from mobile sand dune to stabilized dunes. Seedling emergence of C. mongolicm was highly dependent on soil physical condition. These results indicated that changes in soil physical condition limited clonal propagation and seedling emergence of C. mongolicum in stabilized sand dunes. Seed bank density was not a limiting factor; however, poor seedling establishment limited C. mongolicum's further natural regeneration in stabilized sand dunes. Therefore, clonal propagation may be the most important mode for population expansion in mobile sand dunes. As a pioneer species C. mongolicum is well adapted to propagate in mobile sand dune conditions, it appears unlikely to survive naturally in stabilized sand dune plantations.     

沙漠植物分层侧影与积沙成丘的关系

选用民勤沙区常见的几种固沙植物,在民勤西沙窝沙漠边缘设置了108个植物和沙堆样方,通过对不同植物的分层侧影宽度、分层侧影面积和侧影中心等指标的测定和对比分析,得出如下结果:1)可积沙成丘植物的侧影为三角形或柱形,即由地面向上侧影宽度变小,侧影中心在近地面30 cm高度内,具备这一条件的植物为丛生灌木。而不能积沙成丘的植物侧影为菱形,侧影中心距地面高度在30 cm以上。2)风沙流以及沙尘暴中的沙粒主要集中在近地表0—30 cm高度内流动,这便是植物侧影越低,越易积沙成丘的重要原因之一。3)沙埋后茎秆能产生不定根的植物可形成高于植株几倍至数十倍高度的沙堆/沙丘,而不具备这一属性的植物,有些虽然能形成沙堆,但沙堆受植物高度限制,即沙堆高度不会超过植株高度。4)侧影面积大小是反映植物防风固沙功能的一个十分重要的指标,能积沙成丘是植物阻固流沙的物质体现,形成的沙堆越高大则表明植物阻固流沙的功能越强,但不能积沙成丘的植物如梭梭、沙拐枣、沙蒿等也是具有一定防风阻沙效果的。