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1.
种子出苗对种间关系和群落组成具有重要影响。种内研究表明种子质量与种子出苗之间存在正相关关系,但这种关系很少在物种水平进行检验,尤其是在不同土壤埋藏深度条件下。为此,该文开展了一个因子实验(10种植物和5种土埋深度(0、1、2、4和8cm))以检验是否在不同土层中"种子质量-种子出苗之间的正相关关系"始终存在。该文在不同土埋深度播种50粒种子(重复5次),连续30天观测种子出苗,并提出了一个耐土埋性指标。结果表明:(1) 10种植物的最适出苗深度为0–2 cm土层; 6种植物的最大出苗率发生在1 cm土埋深度。(2)种子质量与耐土埋性之间存在显著的正相关关系,种子质量越大耐土埋性越强,适宜出苗的土层越深。(3)当土层较深(4或8 cm)时,种子出苗率和持续出苗时间随种子质量增加而增大,种子出苗率与持续出苗时间之间存在正相关关系;这些关系在较浅土层(0、1或2 cm)并不存在。这些结果有助于进一步理解种子大小与出苗之间的关系,以及种子出苗过程中的策略。  相似文献   

2.
四种沙埋深度对羊草种子出苗和幼苗生长的影响   总被引:5,自引:0,他引:5  
马红媛  梁正伟  闫超  陈渊  黄立华 《生态学杂志》2007,26(12):2003-2007
模拟羊草种子自然埋藏深度状况,设计了0、1、2和3cm共4种沙埋深度实验,研究了其出苗率及幼苗生长对沙埋深度的响应。结果表明,羊草种子出苗率随埋深的增加呈下降趋势,0cm时出苗率最高为89.3%,1和2cm时分别为81.5%和78.5%,3cm时最低(73.5%),与前三者具有显著差异。埋深对地上株高生长动态的影响主要表现在,播种后25d,0~2cm处理的羊草幼苗地上株高均高于3cm处理;播种后36d,4种处理的地上株高没有显著差异。此外,随着埋深的增加,羊草幼苗的根长、根数、根冠比呈先上升后下降趋势,叶片数呈下降趋势,绝对株高则呈上升趋势。表明1~2cm沙埋深度更适宜于羊草种子出苗及幼苗生长,而0或3cm埋深不利于其出苗和幼苗生长。  相似文献   

3.
王萍  张立峰  李明 《生态学杂志》2012,31(6):1373-1377
为保障北方干旱-半干旱地区作物春播安全成苗,以完全控制环境为基础,通过人工设计水分梯度,研究了土壤水分胁迫与亚麻出苗的关系以及抗旱出苗的水分临界阈值。结果表明:亚麻出苗进程对土壤水分的反应表现出跃升、渐升和S曲线3种类型;亚麻出苗在砂质栗钙土上的水分敏感域为3.5%~6.0%,草甸栗钙土为9.0%~15.0%;以亚麻出苗速率为标准,砂质栗钙土的土壤水分临界值为5.5%,草甸栗钙土为13.0%;以亚麻抗旱保苗为标准,砂质栗钙土的土壤水分临界值为5.0%,播种量需增至常年的1.52倍,草甸栗钙土约为12.0%,播种量为常年的1.72倍。  相似文献   

4.
为探明新疆野杏(Armeniaca vulgaris)种子萌发与幼苗生长对果肉和埋土深度的响应,以期为新疆野杏的天然更新与实生苗培育提供理论参考。通过2种果皮结构(有果肉和无果肉)的种子在不同埋土深度(地表至18.0 cm的14个梯度)对新疆野杏种子萌发和幼苗生长进行研究,旨在揭示果皮结构和埋土深度对新疆野杏种子萌发与成苗能力的影响。结果表明:果肉和埋土深度显著影响野杏种子的萌发、幼苗生长与质量(P<0.05)。埋土深度<3.0 cm不利于成苗,埋土深度>6.0 cm时,萌发能力与幼苗生长量随埋土深度的增加而降低,3.0~6.0cm为适宜埋土深度。无果肉种子萌发优于有果肉种子,萌发率、萌发指数、成苗率、活力指数分别增长了37.18%、3.88%、37.18%、26.59%,幼苗高、基径、叶片数量、根冠比、幼苗质量指数分别增长了36.99%、7.48%、68.69%、20.61%、14.29%,其萌发能力与幼苗生长量显著高于有果肉种子(P<0.05)。有无果肉种子的萌发和幼苗生长指标与埋土深度呈显著负相关(P<0.05)。研究结果表明,无果肉处理对新疆野杏种...  相似文献   

5.
研究了沙埋深度和种子大小对内蒙古毛乌素沙地植被群落中占优势的柠条锦鸡儿(Caragana korshinskii Kom.)种子萌发、出苗、幼苗存活和生长的影响.结果表明,沙埋深度显著影响柠条锦鸡儿的种子萌发率、休眠率、出苗率、幼苗存活率及生物量.在0.5-2cm的浅层沙埋下,种子萌发率、出苗率、幼苗存活率及生物量最高,休眠率最低;沙埋深度≥4 cm时,柠条锦鸡儿的种子萌发率、出苗率、幼苗存活率及生物量随着沙埋深度增加显著降低,而休眠率却显著升高;沙埋深度≥12 cm时,柠条锦鸡儿种子不能够出苗,幼苗也不能够存活.种子大小对柠条锦鸡儿种子萌发率没有显著影响,但对出苗率、幼苗存活率及生物量影响显著.在各个沙埋深度下,不同大小的柠条锦鸡儿种子间的萌发率没有显著差异.当沙埋深度≤6 cm时,不同大小的柠条锦鸡儿种子在同一沙埋深度下的出苗率间没有显著差异;但当沙埋深度≥8 cm时,在同一沙埋深度下,大种子的出苗率显著高于中种子和小种子的出苗率,而中种子和小种子出苗率间没有显著差异.0.5-10 cm的沙埋深度中,除6 cm和8 cm深度下中种子和小种子萌发幼苗的生物量间没有显著差异外,其余深度下,大种子萌发的幼苗的存活率及生物量显著高于同一沙埋深度下中种子萌发的幼苗的存活率及生物量,后者又显著高于小种子萌发的幼苗的存活率及生物量.可能正是种子萌发对沙埋环境的忍耐或响应能力以及种子的多态性提高了柠条锦鸡儿在毛乌素沙地的适合度,为其在流动或半流动沙丘环境中成功定居并形成优势群落奠定了基础.  相似文献   

6.
种子类别和埋藏深度对雌性小泡巨鼠发现种子的影响   总被引:8,自引:4,他引:4  
肖治术  张知彬 《兽类学报》2004,24(4):311-314
2001年9~12月,在四川省都江堰林区实验围栏内研究了栓皮栎、袍树、栲树、石栎、青冈和油茶种子与6种埋藏深度对小泡巨鼠雌性成体发现埋藏种子的影响。结果表明:1)由于不同种子在种子大小、营养价值和单宁含量等存在差异,雌性小泡巨鼠对个体最大的石栎种子发现率最高,油茶(脂肪含量高)和栲树(单宁含量低)次之,单宁含量较高的袍树、青冈和栓皮栎则较低;2)埋藏深度与雌性小泡巨鼠发现栓皮栎种子的比例呈显负相关,即随着埋藏深度增加,小泡巨鼠发现埋藏种子的比例则减少。  相似文献   

7.
五种荒漠植物幼苗出土及生长对沙埋深度的响应   总被引:13,自引:0,他引:13  
李秋艳  赵文智 《生态学报》2006,26(6):1802-1808
研究了红砂、泡泡刺、花棒、白刺和沙拐枣5种荒漠优势植物的幼苗出土和生长对沙埋的响应,判断了幼苗的生长特征能否预测植物的定植能力。进行了0、1、2、3、5cm和8cm等6个沙埋深度处理,每个处理5个重复。结果表明:每种植物的出苗率都随着沙埋深度的增加而降低,而且遵循着指数方程关系。红砂种子的最佳沙埋深度应为0-1cm,3cm已是出苗和存活的最大沙埋深度;泡泡刺、花棒和白刺种子的最佳深埋深度为0—3cm;沙拐枣在0—8cm各个深度都有出苗现象,且出苗率没有显著差异,但8cm深度的出苗率只有4%,最佳沙埋深度约为5cm。幼苗的生长高度受沙埋深度的影响显著,在同一时间,幼苗的最大生长高度并不在0cm表层,但红砂幼苗除外。泡泡刺、花棒和白刺在0—3cm的沙埋深度的幼苗生长高度大于5-8cm沙埋深度的生长高度,但沙拐枣幼苗在5cm深度的生长高度最大。5种荒漠植物幼苗的生物量受沙埋深度的影响不显著。在同一沙埋深度下,红砂的绝对高度生长率明显低于其余4种植物,沙拐枣的绝对高度生长率高于其余4种植物幼苗;5种植物的相对高度生长率对沙埋深度的响应并不敏感。绝对高度生长率与相对高度生长率并不能预示幼苗存活成功率。  相似文献   

8.
熊韫琦  赵彩云  赵相健 《生态学报》2021,41(24):9621-9629
豚草是一种全球性的恶性入侵杂草,给我国生物多样性及经济发展造成了巨大威胁。为研究豚草种子出苗和幼苗生长的影响因素,采用盆栽实验分析了种子大小(L、M、S)与埋深(2、4 cm和6 cm)或播种密度(2、4粒/盆和8粒/盆)对豚草(Ambrosia artemisiifolia)种子的出苗和幼苗生长的影响。研究结果表明,埋深对豚草种子出苗的影响高于播种密度及种子大小的影响,较浅的埋深有利于豚草种子出苗;出苗率在不同播种密度下均具有较高水平,达到67.9%-100%,这种高出苗率是豚草在不同生境成功定植的原因之一。豚草的幼苗生长受埋深或播种密度的影响大于种子大小的影响,且小种子更易受埋深或播种密度的影响。种子大小显著影响豚草幼苗的株高和基径(P<0.05),总体上较大种子的株高和基径高于小种子,此外更小的种子会将生物量更多的分配给根以促进幼苗的生长。幼苗的株高和基径在较浅的埋深下更高,而豚草幼苗的单株生物量、单株地上和地下生物量随埋深的增加而增加。播种密度的增加会加剧豚草幼苗之间对水分、营养、光照等资源的竞争,导致其单株地上、地下及总生物量显著降低(P<0.05)。研究发现豚草在浅埋深、低密度生境中更容易入侵成功,因此可以通过对土壤进行深翻,采取替代控制,种植竞争能力强的本地植物等手段有效管理和防治豚草。  相似文献   

9.
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。  相似文献   

10.
埋藏点深度、间距及大小对花鼠发现向日葵种子的影响   总被引:4,自引:0,他引:4  
张洪茂  张知彬 《兽类学报》2006,26(4):398-402
2005 年5 ~6 月,在北京东灵山地区,通过在实验围栏内设置不同深度、间距和大小的埋藏点,研究了花鼠对向日葵种子的发现率。结果表明,花鼠发现埋藏种子的比例随埋藏深度的增加而减少,埋藏深度> 5 cm后,发现比例较低,且不再有明显变化;花鼠发现埋藏种子的比例随埋藏点间距的减小而增加,埋藏点间距<0.5 m后,发现比例较高,且不再有明显变化;花鼠发现埋藏种子的比例随着埋藏点增大而增加,埋藏点种子> 5 g后,发现比例较高,且不再有明显变化。  相似文献   

11.
Q.Y. Li  W.Z. Zhao  H.Y. Fang 《Plant Ecology》2006,185(2):191-198
A greenhouse experiment was conducted to test the effects of sand burial depth and seed mass on seedling emergence and growth of Nitraria sphaerocarpa. Seeds of Nitraria sphaerocarpa were sorted into three size-classes (large, medium, small) and artificially buried at 0, 1, 2, 3, 4, 5 and 6 cm depths in plastic pots filled with unsterilized sand. In the seven treatments, the percent emergence, seedling mass and seedling height, significantly affected by both burial depth and seed size, were highest at the optimal burial depth of 2 cm burial depth, and decreased with increasing burial depth in each seed size-class. Although seedling mass was usually greatest for large seeds and least for small seeds at each burial depth, little difference was observed in seedling height at shallow burial depths of 0–3 cm. In each seed size-class, with increasing burial depth, both root-mass ratio and aboveground stem-mass ratio decreased, while belowground stem-mass ratio increased. In each burial depth, with decreasing seed size, belowground stem-mass ratio increased, while root-mass ratio decreased.  相似文献   

12.
Lepidium vesicarium is a weed species with a wide distribution in the rangelands and dry‐land farming in East Azarbaijan, Iran. The experiments were undertaken to assay the effects of light, temperature, pH, osmotic potential, NaCl concentration and burial depth on seed germination and emergence of L. vesicarium. Germination was maintained at high levels (> 80%) over a wide day/night temperature range (10/5 to 30/20°C), but a severe reduction in the germination rate of L. vesicarium was found below 20/10°C. Germination of L. vesicarium was influenced by different light/dark regimes, as the germination rate was highest at 16 h light for the all treatments (0, 8, 12, 16 and 24 h light). Germination was 92–95% over a wide range of pH (2‐10). Germination was >50% at a water potential of ?0.7 MPa and salinity of 21 dS/m, indicating that drought and salt conditions have a minimal impact on seed germination. With increasing burial depth from 0 to 2 cm, the number of days required for 50% emergence increased and no germination was observed at burial depths deeper than 3 cm. This suggests that L. vesicarium would become troublesome in the rangelands and for growers in reduced‐tillage cropping systems. The ability to emerge from shallow depths, coupled with tolerance of a wide pH range, drought and salinity at germination, should be taken into account when managing this weed species.  相似文献   

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《植物生态学报》2017,41(11):1168
Aims Soil aggregate is an important component of soil structure, playing an important role in the physical and biological protection mechanism of soil organic carbon (SOC) through isolating SOC from microorganisms. As far as we know, there are few studies, however, on exploring the spatial distribution of soil aggregate at the regional scale. Our objective was to investigate the mass allocation and stability of soil aggregate in different types of Nei Mongol grasslands. Methods We have established 78 sites with a size of 10 m × 10 m across the transect of Nei Mongol grasslands and collected soil samples from different soil depth up to 1 m. We used wet sieving method to separate different sizes of aggregate partition and used mean mass diameter (MMD) and geometric mean diameter (GMD) in order to evaluate the stability of soil aggregate. The two-way ANOVA was used to test the difference of mass percentage and stability of soil aggregate in different grassland types and soil depths. In addition, a linear regression analysis was used to analyze the correlations of mass percentage and stability of soil aggregate with both mean annual precipitation (MAP) and mean annual temperature (MAT). Important findings The results showed that the mass percentages of soil aggregate were highest in meadow steppe, while almost equal in typical steppe and desert steppe. However, no significant patterns were found along the soil depth. The mass percentage of soil aggregate fractions were positively correlated with MAP in all soil layers, but negatively correlated with MAT except the layer of 70-100 cm. For the stability of soil aggregate, at 0-10 and 10-20 cm, MMD and GMD of meadow steppe were significantly greater than those of typical and desert steppes, whereas no significant differences among three grassland types were found for other soil layers. Besides, MMD and GMD in meadow steppe and typical steppe gradually decreased along the soil depth.  相似文献   

16.
极端干旱区由于降水稀少, 植被盖度低, 太阳辐射强烈, 以及土壤稳定性差, 导致其凋落物周转不同于非干旱区。为探究极端干旱区凋落物分解规律, 该研究利用凋落物分解袋法, 以塔克拉玛干沙漠南缘沙漠-绿洲过渡带优势物种花花柴(Karelinia caspia)、骆驼刺(Alhagi sparsifolia)和胡杨(Populus euphratica)凋落叶为研究对象, 设置不同的沙土掩埋处理: 地表、2 cm和15 cm埋深, 以模拟自然条件下凋落物分解环境, 测定分解过程中凋落物质量和水溶性盐的变化特征。结果表明: 极端干旱区凋落物分解速率与凋落物初始碳(C)含量、氮(N)含量、C:N和木质素含量的关系与非干旱区存在较大差异, 在地表处理下, 木质素含量越高, 质量损失越快。不同分解环境下凋落物质量和水溶性盐损失具有显著差异, 与15 cm埋深相比, 地表和2 cm埋深处理显著增加了凋落物的质量损失和水溶性盐总量损失。地表处理增加了凋落物分解前期的水溶性盐溶解量。该研究表明, 极端干旱区凋落物分解的驱动机制具有独特性, 由于降水稀少, 土壤微生物的活性较低, 掩埋深度不是驱动凋落物分解的主要因素, 极端干旱区凋落物的分解主要受其他非生物过程如太阳光辐射的影响。  相似文献   

17.
In this paper I develop a null model for the expected relationship between seed mass and the mass of dispersal structure (reward) for vertebrate-dispersed plant species. The model is based on the simple assumption that the reward associated with a given seed mass is commensurate with work required to move it, and predicts that reward mass should scale relative to seed mass with an exponent of 4/3 (1.3). I tested this relationship between- and within-species of vertebrate-dispersed plants from four families from tropical rain forest in north Queensland, Australia. At a community-level there was a significant isometric relationship between log mean pulp mass and log mean seed mass across species. When family membership was considered, the estimate for the common slope between families was 1.32, surprisingly similar to the exponent predicted from commensurate reward. In addition, the 95% CI of the common slope did not include unity, providing no support for isometry. There was also no evidence that the relationships between mean log pulp mass and mean log seed mass were significantly different between families. This simple null model may be a common “rule” governing mean allocation to reward in all plant–animal dispersal mutualisms and its confirmation is the first evidence that animal dispersers have shaped the evolution of seed traits. However, I found no evidence that the scaling relationships within-species were consistently predicted by commensurate reward – a “taxon-level effect”. I suggest that the taxon-level effect arises because mean seed and mean reward mass within each species arises due to community-wide, disperser-mediated selection to produce equally attractive fruits, whereas within-species allometries may be determined by selection for fruit traits that enhance either dispersal probabilities, offspring survival or both, and these will be contingent on the environmental context into which seeds are released. G. P. Cheplick  相似文献   

18.
Crosbie  Julie  Longnecker  Nancy  Davies  Fleur  Robson  Alan 《Plant and Soil》1993,(1):449-452
Seed of narrow-leafed lupin (Lupinus angustifolius L.) produced in Western Australia often has low manganese (Mn) concentration because of low Mn availability in the soil during grain filling. A major problem of lupin production is poor seedling establishment. We tested the hypothesis that low Mn concentration in lupin seeds decreases emergence.The experiment was a factorial design comparing emergence of lupins (cv. Gungurru) grown under glasshouse conditions from seed with 2 different internal Mn concentrations (7 or 35 mg Mn kg–1 DW) and with 2 external Mn fertiliser treatments (0 or 10 mg MnSO4.H2O kg–1 soil). There were no visible differences between the seeds. Emergence was monitored and plants were harvested 17 days after sowing.Emergence was approximately 60% in all pots sown with low Mn compared to 100% in pots sown with high Mn seed. Application of Mn did not increase the final emergence of low Mn seed. Seed viability was assessed by staining with tetrazolium chloride, a common test used in seed testing laboratories. All high Mn seed were viable while 34% of low Mn seed were completely or partly unstained and therefore were non-viable. We have shown that low Mn supply during seed filling may lead to production of non-viable seed that cannot be visually distinguished from viable seed..  相似文献   

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