The effect of fire and ants on the seed-bank of a shrub in a semi-arid grassland

Abstract Invasion of grasslands by woody plants following the introduction of domestic stock is a worldwide phenomenon. Burning is frequently recommended as a remedial measure but for a pastoral enterprise it is costly and the frequency of the fires required is of critical economic importance. The size and longevity of the soil seed-bank is an essential part of the response of shrub populations to prescribed fire regimes. In this study the seed-bank of the semi-arid zone shrub Dodonaea attenuata in Eragrostis eriopoda tussock grassland was examined in relation to harvesting by ants and the burning history of the sites. On unburnt sites, more than 3500 seeds per m2 entered the seed-bank in the summer 1984–85 but sites burnt 5 years previously produced less than one-third of that number. Burnt shrubs did not flower for 5 years and no seeds survived in the soil through to 1985. Burning immediately prior to seed ripening destroyed the seed crop but burning after seed-fall stimulated a greater germination in the following spring than on unburnt treatments. Ants rapidly harvested most of the seeds produced and after 20 months the combined effects of ant harvesting and germination had reduced the seed-bank at unburnt sites to 8–21 seeds per m2 and at sites burnt 7 years previously to less than two seeds per m2. Seeds were initially harvested in summer by Pheidole spp. of ants for their elaiosome and then discarded in middens outside the entrance to the ant nest. During the subsequent cool season the seeds were taken back into the nest and stored at depths ranging from 2 to 30cm. It was concluded that ants provided short-range dispersal (< 10 m) and promoted the contagious distribution of D. attenuata, which is advantageous for a fire-susceptible, arid-zone shrub invading a grassland liable to be burnt: seedlings derived from seeds in ant storage chambers near the soil surface and in sparse grass situations caused by competition from shrubs may obtain some survival advantage. Prescribed fire has potential as a management tool for controlling population density of D. attenuata because, depending upon season and frequency, it reduces seed rain by killing shrubs, suppresses flowering activity and destroys seed crops on the plant. Under the influence of a regime of regular burning, such as prevailed prior to the European pastoral industry, the limited soil seed-bank would have been a major constraint on D. attenuata populations.     

Seed rain and soil seed bank of Picea asperata Mast. in subalpine coniferous forest of western Sichuan,China

Abstract

Dragon spruce (Picea asperata Mast.) is widely planted on clear-cuts from natural subalpine coniferous forests in western Sichuan. To assess the natural regeneration potential of this species in spruce plantations of different ages, field studies on the seed rain, seed bank, and seedling recruitment were conducted in 20-year, 30-year, and 60-year plantations, and in a retained natural forest ca. 150 years old for comparison. Moreover, a series of temperature and light regimes were also designed in March 2003 to test germination/dormancy responses of the P. asperata seeds to different conditions. In the plantations considered, both the densities of seed rain and soil seed bank increased with increasing stand age, whereas they were both low beneath the natural forest partially due to low adult density of P. asperata adult trees. P. asperata has a transient seed bank, and ca. 60% of seeds were found in the litter layer. Seed decay and seed predation were the two most important factors affecting soil seed bank dynamics, which caused a number of seed losses from the soil. Only a small fraction germinated and produced seedlings, and the indices of the losses from the seed bank via germination in the 30-year plantation, 60-year plantation and natural forest were 4.75, 5.10, and 2.80%, respectively. High seedling mortality was observed after seedling emergence, and most of the germinated seedlings died out within one growing season. The P. asperata seeds showed a high percent germination and no significant differences under most light and temperature regimes except for full sunlight or temperature below 5°C. In conclusion, despite a substantial number of seed produced, the high depletion of soil seed, the low seedling output, and high seedling mortality may obscure the natural regeneration potential of this tree species.     

Seed dormancy/germination traits of seven Persicaria species and their implication in soil seed-bank strategy

In order to predict species-specific potential to form persistent soil seed-banks and to characterize the dynamics of their seed-banks, the seed dormancy/germination traits of seven Persicaria (Polygonum s.lat.) species sharing lakeshore habitats in central Japan were examined. Strict light requirements for seed germination were not observed in any of the species examined. Although all species required moist chilling (0–6 weeks) to break seed dormancy and were sensitive to temperature fluctuation, the degree of both responses varied between species. Seed germination of Persicaria hydropiper (L.) Spach, Persicaria lapathifolia (L.) S.F. Gray, and Persicaria longiseta (De Bruyn) Kitag. was more accelerated by temperature fluctuation and required shorter chilling periods compared with Persicaria japonica (Meisn.) H. Gross, Persicaria maackiana (Regel) Nakai, Persicaria thunbergii (Sieb. et Zucc.) H. Gross, and Persicaria sieboldi (Maisn.) Onki. Secondary dormancy was induced in all species at higher temperatures (24 and 30°C). A persistent seed-bank strategy suggested by the dormancy/germination traits of the studied species was also demonstrated by seedling emergence from surface soils collected from the natural habitat immediately before seed dispersal, as well as by viable seed persistence for 13 months in the field in a seed burial experiment. In the natural habitat, the species with longer chilling requirements occurred in various microhabitats, including the interior of moist tall grasslands, whereas the species having higher sensitivity to temperature fluctuation were most frequently found in sparsely vegetated microhabitats.     

锡林郭勒草原自然保护区土壤动物初步调查

土壤动物的生存、活动与栖息地环境密切相关。一方面栖息地生态因子决定着土壤动物的生存与活动;另一方面,土壤动物对土壤有机质的改变、土壤微生物的生存、植物的生长等诸生态因子的变化起着一定的促进作用。因此随着草原生态系统研究的日趋深入,土壤动     

Floristic assessment of an Afromontane grassland fragmentation experiment in a pine plantation

Twenty-four grassland fragments were established in an area of high botanical diversity planted with Pinus patula plantations. This area is representative of the eastern Drakensberg escarpment, containing a large number of endemic plant taxa. The experimental fragments comprise six replicates of two fragment sizes (0.25 and 1.5 ha), with a similar grouping of control plots in adjacent undisturbed grassland designated for conservation. The plots form the basis of a long-term study on fragmented plant and animal communities. Vegetation surveys were performed using nearest neighbour step point and Braun–Blanquet techniques. Analysis of similarity (anosim ) indicates that in neither the large nor small fragments do the control plots differ significantly in floristic structure from the experimental fragments. Five variations of the Themeda triandra-dominated grassland were identified, corresponding to slight variations in ground moisture. The experimental fragments and control plots were sufficiently similar to be analysed as replicates within the fragmentation study. This forms the foundation for the long-term analysis of plant communities within the fragments, as well as for analyses of insect and vertebrate communities within the fragments.     

Plant and soil microbial responses to defoliation in temperate semi-natural grassland

There is much interest in understanding the nature of feedback mechanisms between plants and soil organisms in grazed ecosystems. In this study, we examine the effects of different intensities of defoliation on the growth of three dominant grass species, and observe how these plant responses relate to the biomass and activity of the microbial community in the root zone. Our data show that grassland plants with varying tolerances to grazing have markedly different growth responses to defoliation, and that these responses vary with the intensity of cutting. Defoliation of grasses which are tolerant to grazing, namely Festuca rubra and Cynosurus cristatus, leads to a reduction in root mass and an increase in the allocation of resources to shoots. In contrast, defoliation of a grass with low tolerance to grazing, Anthoxanthum odoratum, had little effect on root mass, but increased the relative allocation of resources below-ground. In all plant species, defoliation led to an increase in soil microbial biomass and C use efficiency in the root zone. This response was greatest in the root zone of A. odoratum and is likely to be related to changes in root exudation pattern following defoliation. The significance of these changes in relation to soil nutrient dynamics and plant nutrient uptake during regrowth require further exploration. This revised version was published online in June 2006 with corrections to the Cover Date.     

羊草草原土壤动物群落多样性的研究

对东北羊草草原不同生境土壤动物群落多样性研究表明 ,生境条件愈优越 ,土壤动物的多样性指数愈高 ,种类则愈丰富 .土壤动物群落的多样性与土壤有机质和全N含量呈正相关 ,与 pH呈负相关 ,与土壤自然含水量和全P含量关系不明显 .土壤动物群落多样性随土层深度的增加而减少 ,且表聚性明显 .     

不同草原植被碱化草甸土的酶活性

在羊草草原不同植物群落土壤中,脲酶、磷酸酶和纤维素酶活性的变化是羊草群 落＞拂子茅群落＞碱茅群落＞虎尾草群落＞碱蓬群落＞光碱斑．脱氢酶是拂子茅群落＞ 羊草群落＞虎尾草群落＞碱茅群落＞碱蓬群落＞光碱斑．脲酶、磷酸酶和纤维素酶的时间 变化曲线呈抛物线型,最大值均出现在８月,最小值出现在６月或１０月．脱氢酶变化的最 大值出现在６月,然后逐渐减弱,１０月出现最低值．关联分析表明各土壤因子对脲酶作用 大小的关联序为全 Ｎ＞有机质＞土壤容重＞全 Ｐ＞ ＰＨ ;磷酸酶为全 Ｐ＞有机质＞ ｐＨ＞全 Ｎ＞土壤容重;脱氢酶为全Ｎ＞有机质＞全Ｐ＞土壤容重＞ｐＨ;纤维素酶为全Ｎ＞有机质 ＞全 Ｐ＞ｐＨ＞土壤容重．脲酶、磷酸酶和纤维素酶活性与微生物生物量关系随着微生物生 物量的增加酶活性逐渐增强．脱氢酶与微生物生物量的关系不明显．     

The persistence of calcareous grassland species in the soil seed bank under developing and established scrub

The relationships between the composition of the soil seed bank, the field layer vegetation, and the scrub canopy were investigated along a 69 m transect, grading from incipient woodland, through scrub, into intensively rabbit-grazed calcareous grassland. The results are used to assess the persistence of species associated with open calcareous grassland in the seed bank under developing scrub. Scrub age, composition and density, changed along the transect from the woodland to open grassland. A total of 35 forb and grass species were found in the field layer. The pattern evident in the scrub layer was also reflected in the herbaceous vegetation. The field layer in the most closed portion of the transect, where the scrub was oldest, was dominated by shade-tolerant species normally associated with woodland habitats. The abundance of these species decreased along the transect as the scrub age declined, and the field layer became increasingly dominated by species typical of open grassland. A total of 47 species germinated from the seed bank. Few species were recorded in the seed bank along the entire length of the transect. Overall, the seed bank was dominated by Hypericum perforatum and Centaurium erythraea, which accounted for 38.2% and 28.6% of emerging seedlings respectively. As with a number of similar studies, the composition of the seed bank had a low correspondence with the composition of the field layer vegetation. The results also emphasise that the composition of the seed bank can be viewed as an ecological palimpsest, with germinable seed of species from each stage of the old-field succession occurring in the soil. The seed bank is an important component in the re-vegetation of an area after disturbance such as scrub removal. This study supports the findings of previous research in showing that relatively few characteristic calcareous grassland species form persistent seed banks. The soil seed bank would therefore appear to be of limited value in the restoration of such grassland following scrub removal.     

模拟增温对川西亚高山西类针叶林土壤酶活性的影响

采用开顶式生长室(open top chamber,OTC)模拟增温,同步监测了亚高山人工针叶林和天然针叶林表层土壤温、湿度的变化,以及模拟增温初期土壤转化酶、脲酶、过氧化氢酶和多酚氧化酶活性的变化.结果表明:在整个生长季节中,OTC使人工林和天然林5 am土壤日平均温度分别增加0.61 oC和0.56 ℃,10 am体积含水量分别下降4.10%和2.55%;模拟增温增加了土壤转化酶、脲酶、过氧化氢酶和多酚氧化酶活性.增温与林型的交互作用对土壤脲酶和过氧化氢酶活性有显著影响,而对转化酶和多酚氧化酶影响不显著.增温对过氧化氢酶活性的影响与季节变化相关.在各处理下,天然林土壤酶活性显著高于人工林.土壤酶活性季节动态与土壤温度有着较大相关性,而与土壤水分季节变化关系不明显.模拟增温易于增加土壤酶活性,但增温效应和林型、酶种类和季节变化有一定关系;亚高山针叶林土壤酶活性主要受控于土壤温度,而与土壤水分关系不大.     

The effects of soil horizons and faunal excrement on bacterial distribution in an upland grassland soil

The density and spatial location of bacteria were investigated within different horizons of an upland grassland soil before and after a liming treatment to increase the numbers of large soil fauna. Bacterial cells were located by image analysis of stained thin sections and densities calculated from these data. Excrement from macro- and meso-fauna was identified using micromorphology and the densities of bacteria on specific areas of excrement measured by image analysis. There were significant differences among horizons in the density of bacterial cells, with the minimum density found in the horizon with least evidence of earthworm activity, but no difference in density between the organic H and organo-mineral Ah horizons. Soil improvement by liming significantly increased bacterial densities in all three horizons, with the greatest increase found in the horizon with the smallest density before liming. There were no differences in bacterial density between areas dominated by excrement from earthworms and excrement from enchytraeids, although densities in both areas were significantly increased by liming. Variability in bacterial density at spatial scales of less than 1 mm was linked to the occurrence of excrement. Bacterial densities within areas of both types of excrement were significantly greater than those in the surrounding soil. However, the frequency distribution of the ratios of density in excrement to that in the soil was bimodal, with a majority of occurrences having a ratio near 1 and only some 20-30% having a much larger ratio. These variations can probably be explained by variations in the age of the excrement and its suitability as a substrate.     

Denitrification in the top and sub soil of grassland on peat soils

Denitrification is an important process in the nitrogen (N) balance of intensively managed grassland, especially on poorly drained peat soils. Aim of this study was to quantify the N loss through denitrification in the top and sub soil of grassland on peat soils. Sampling took place at 2 sites with both control (0 N) and N fertilised (+ N) treatments. Main difference between the sites was the ground water level. Denitrification was measured on a weekly basis for 2 years with a soil core incubation technique using acetylene (C₂H₂) inhibition. Soil cores were taken from the top soil (0–20 cm depth) and the sub soil (20–40 cm depth) and incubated in containers for 24 hours. The denitrification rate was calculated from the nitrous oxide production between 4 and 24 hours of incubation. Denitrification capacities of the soils and the soil layers were also determined.The top soil was the major layer for denitrification with losses ranging from 9 to 26 kg N ha^–1 yr^–1 from the O N treatment. Losses from the top soil of the + N treatment ranged from 13 to 49 kg N ha^–1 yr^–1. The sub soil contributed, on average, 20% of the total denitrification losses from the 0–40 layer. Losses from the 0–40 cm layer were 2 times higher on the + N treatment than on the O N treatment and totalled up to 70 kg N ha^–1 yr^–1. Significant correlation coefficients were found between denitrification activity on the one hand, and ground water level, water filled pore space and nitrate content on the other, in the top soil but not in the sub soil. The denitrification capacity experiment showed that the availability of easily decomposable organic carbon was an important limiting factor for the denitrification activity in the sub soil of these peat soils.     

Loss of nitrogen in compacted grassland soil by simultaneous nitrification and denitrification

The soils of mid-Wales in grazed permanent pasture usually exhibit stagnogley features in the top 4–10 cm even though on sloping sites, they are freely drained. Nitrogen is often poorly recovered under these conditions. Our previous studies suggest that continuing loss of available N through concurrent nitrification and denitrification might provide an explanation for poor response to fertilizer N. The work described was designated to further test this proposition. When NH ₄ ⁺ –N was applied to the surface of intact cores, equilibrated at –5kPa matric potential, about 70% of NH ₄ ⁺ –N initially present was lost within 56 days of incubation. Study of different sections of the cores showed a rise in NO ₃ ^- level in the surface 0–2.5 cm soil layer but no significant changes below this depth. The imbalance between NO ₃ ^- accumulation and NH ₄ ⁺ disappearance during the study indicated a simultaneous nitrification and denitrification in the system. Furthermore, the denitrification potential of the soil was 3–4 times greater than nitrification potential so no major build-up of NO ₃ ^- would be expected when two processes occur simultaneously in micro-scale. When nitrification was inhibited by nitrapyrin, a substantial amount of NH ₄ ⁺ –N remained in the soil and persisted till the end of the incubation. The apparent recovery of applied N increased and of the total amount of N applied, 50% more was recovered relative to without nitrapyrin. It appears that addition of nitrapyrin inhibited nitrification, and consequently denitrification, by limiting the supply of NO ₃ ^- for denitrifying organisms. Emission of N₂O from the NH ₄ ⁺ amended soil cores further confirmed that loss of applied N was the result of both nitrification and denitrification, which occurred simultaneously in adjacent sites at shallow depths. This N loss could account for the poor response to fertilizer N often observed in pastoral agriculture in western areas of the UK.     

Response of clonal plasticity of Fargesia nitida to different canopy conditions of subalpine coniferous forest

The aim of this study is to explore the effects of canopy conditions on clump and culm numbers, and the morphological plasticity and biomass distribution patterns of the dwarf bamboo species Fargesia nitida. Specifically, we investigated the effects of canopy condi-tions on the growth and morphological characteristics of F. nitida, and the adaptive responses of F. nitida to dif-ferent canopy conditions and its ecological senses. The results indicate that forest canopy had a significant effect on the genet density and culm number per clump, while it did not affect the ramet density. Clumps tended to be few and large in gaps and forest edge plots, and small under forest understory plots. The ramets showed an even distribution under the closed canopy, and clus-ter distribution under gaps and forest edge plots. The forest canopy had a significant effect on both the ramets'biomass and biomass allocation. Favourable light conditions promoted ramet growth and biomass accumulation. Greater amounts of biomass in gaps and forest edge plots were shown by the higher number of culms per clump and the diameter of these culms. Under closed canopy, the bamboos increased their branching angle, leaf biomass allocation, specific leaf area and leaf area ratio to exploit more favourable light conditions in these locations. The spacer length, specific spacer length and spacer branching angles all showed significant differences between gaps and closed canopy conditions. The larger specific spacer length and spacer branching angle were beneficial for bamboo growth, scattering the ramets and exploiting more favourable light conditions. In summary, this study shows that to varying degrees, F nitida exhibits both a wide ecological amplitude and high degree of morphological plasticity in response to differing forest canopy conditions. More-over, the changes in plasticity enable the plants to optimize their light usage efficiency to promote growth and increase access to resources available in heteerogeneous light environoments.     

小蠹虫对针叶类寄主树木的选择危害机制

小蠹虫对寄主植物的选择是一个非常复杂的过程,也是近年来小蠹虫生态学研究的一个热门话题。文章对国内外小蠹虫寄主搜寻、寄主识别,以及适宜寄主选择等机制等方面的最新研究成果进行了系统报道。     

sofsog: a suite of programs to avoid inbreeding in plantation designs

Cost-effective ways of controlling inbreeding in conservation or productive plantations imply the allocation of individuals reducing the possibility of close relatives' mating and, consequently, limiting inbreeding. sofsog is a suite of programs, which helps to design plantation sites. First, if the plantation scheme involves several plots, it allows distribution of individuals available among different sites minimizing within-site global coancestry. Then, it yields a plantation design for each site, either following the classical permutated neighbourhood strategy or the recently developed method by Fernández and González-Martínez. This new method allows the implementation of different pollen dispersion kernels, and to include in the designing strategy any available information on individual relationships, reproductive success, differences in phenology, etc., via weighting or penalization matrices. Additionally, the package includes a tool for calculating the molecular coancestry (Identity By State) from codominant marker data.