Abstract:In this study, ditch density was chosen as an indicator of disturbance intensity, and four sites with different ditch density were chosen to compare species composition and diversity among them. Four transects and sixty-seven quadrats were sampled along the ditch density gradient. The results showed that there existed a significant negative relationship between disturbance intensity and species parameters, while species diversity did not differ greatly among sites, but species composition varied considerably. With increasing disturbance intensity, the wetlands tended to be reduced in plant species diversity, and an increasing loss of indigenous wetland species was paralleled with an increasing invasion of upland species. The results also show that the rate of species turnover within communities differed among communities under different disturbance intensities. The communities with intermediate ditch density (0.6-1.2 km/km²) had higher rates than the other communities.

Abstract:Artemisia ordosica is an under-shrub species, which dominates the vegetation of the Mu Us sandy land in North China. The spatial patterns of the A. ordosica population in different sandy lands were compared with the methods of Spatial Auto-correlation Analysis, Semi-variance Analysis and Nine-Term Local Quadrat Variance (9TLQV). The results show that, by contrast with the A. ordosica population in fixed sandy land, the population in semi-fixed sandy land is of stronger auto-correlation and greater spatial heterogeneity, and meanwhile it presents more intense differentiation between patches and gaps. The spatial patterns of the A. ordosica population in semi-fixed sandy land are probably governed by drifting sand caused by strong winds. Drifting sand can easily put A. ordosica shrubs to death unless they live together in form of A. ordosica patches, where the distances between shrubs are short. In semi-fixed sandy land, patches are not only the form of the A. ordosica population to survive drifting sand, but also the foundation of the A. ordosica population to develop and broaden the area. The A. ordosica population is supposed to broaden the area through edge extending out from the patches scattering in semi-fixed sandy land. The spatial patterns of the A. ordosica population in fixed sandy land are possibly affected by intra-specific competition related to high plant coverage. This study is ecologically useful to improve the practice of vegetation restoration in sandy land. When transplanting A. ordosica shrubs to bare sandy land, one had better arrange them in form of patches separated by gaps, which can promote the survival of transplanted shrubs, and also help to take advantage of A. ordosica patches to revegetate bare gaps.

Abstract:In this paper, the community composition of Abies fargesii and the population structure of dominant species in this community were studied using a sampling plot method. The research plot was located in Shennongjia National Nature Reserve, China. Results showed that the appearance of the community was characterized by evergreen phanerophytes with microphyllous (or mesophyllous), coriaceous and single leaves. The vertical structure of the community can be clearly divided into 4 layers: arbor layer, shrub layer, herb layer and developed moss layer. Abies fargesii population was a developing population as there were more seedlings and young trees than old trees. Saplings were found more frequently in gaps than under the close canopy, which indicated a pattern of gap regeneration. The height structure of Abies fargesii population presented a reversed pyramid shape. Crown size structure of the population showed a typical reversed J shape. The relation between crown size and DBH (diameter at breast height) was closer than that between crown size and height.

Abstract:The effects of sheep urine deposition volume (0, 1, 2 or 4 L/m²) and deposition stage of plant growth (vegetative or reproductive) on the number and size of tillers/branches and the biomass of Stipa bungeana, Artemisia capillaries and Lespedeza davurica in a Chinese steppe grassland were determined. The results indicate that the response of the three plant species to sheep urine deposition differs, and is influenced by both urine deposition volume and deposition stage of plant growth. Urine deposition had a short-term scorch effect on grassland plants, which mainly occurred in the inner zone of urine patches. Urine application had a long-term positive effect on S. bungeana and a long-term negative effect on A. capillaries and L. davurica, which lasted at least two years and decreased with decrease in urine deposition volume. All species growing in the inner zone of urine patches were scorched by sheep urine deposition, some species in the marginal zone of patches were also scorched, while no species were scorched in the outer zones. The reproductive and vegetative stages of A. capillaries and the reproductive stages of S. bungeana and L. davurica were sensitive to sheep urine deposition.

Abstract:Based on routine monitoring data in Xiangxi River and its main tributary Gaolan River from September 2000 to June 2005, this paper estimates the contribution of riverine nutrients, and analyzes the monthly dynamics of concentrations and fluxes of nutrients. The results show that Xiangxi Bay annually receives 1623.49 tons of total nitrogen (TN) and 331.85 tons of total phosphorus; Xiangxi River alone accounts for 68.50% of the total nitrogen fluxes and 91.74% of the total phosphorus fluxes. In these two rivers, dissolved inorganic nitrogen (DIN) is the dominating form of nitrogen; fluxes of DIN and TN are high during summer (July), mid-spring and autumn, and relatively low in winter; non-point source pollutants that flow into rivers are the most important pathway of nitrogen. Orthophosphate is the dominating form of phosphorus in Xiangxi River, relatively low in Gaolan River; fluxes of phosphorus are high during summer and late spring, relatively low during winter and late autumn in Gaolan River, but fluctuate irregularly in Xiangxi River; phosphorus in Gaolan River is mainly caused by non-point source pollutants, while point source pollutants of phosphorus play an important role in Xiangxi River. Soil erosion probably represents the major way of non-point source pollutants, while the drainages of phosphorus diggings and factory discharges play the most important role in the point source pollutants of phosphorus. This research suggests that measures must be taken to control the point source pollutants of phosphorus in Xiangxi River in order to protect Xiangxi Bay of the Three-Gorges Reservoir.

Abstract:The effect of ducks on CH₄ emission from paddy soils and its mechanism were probed in order to decide the optimum number of ducks in the rice-duck ecosystem. Methane emission fluxes from paddy soils were measured by the static box technique. The correlations between methane emission and soil physical and chemical characteristics were also analyzed. The results showed that significant differences (p < 0.01) existed in the dissolved oxygen content of water body in the treatment fields, and the more the ducks, the higher the dissolved oxygen content. Secondly, the soil redox matter content and methanogenic bacteria population of the rice-duck ecosystem reduced more sharply than those of the no-duck rice farming, resulting in a lower methane production. Thirdly, the amount of methane emission differed between the treatments—the more the ducks, the less the methane emission. Other related analyses showed that the negative correlation was significant (p < 0.001) between the methane emission flux and dissolved oxygen content of water body. However, CH4 emission flux had significantly positive correlation (p < 0.01) with the soil redox matter content and rice field methanogenic population.

Abstract:Based on RS, GIS and Apack software, the indices of landscape pattern such as landscape area index, landscape diversity index and landscape fragmentation index were chosen in order to describe changes in the spatial pattern of alpine wetland landscape on the Zoige Plateau during 1966–2000. Results showed that alpine wetland landscape was characteristic of marsh wetlands, which had the biggest patch number and the largest area. The alpine wetland landscape had higher spatial heterogeneity. The largest area appeared in Zoige County with the highest wetland ratio; comparatively, Aba County and Luqu County had much lower wetland ratio. The total area of alpine wetland landscape decreased rapidly during 1966–1986, but it began to increase after 1986. The wetland landscape area shrank by 59857.83 hm² during 1966–2000. The alpine wetland landscape showed the characteristics of concentrated distribution in the past four decades, with higher convergence and dominance indices. The centroid of wetland landscape moved 12.54 km in the northwest direction firstly, 11.33 km in the southeast direction, and then 1.1 km in the north direction.

Abstract:Nitrogen (N) deposition can alter the rates of microbial N- and C- turnover, and thus can affect the fluxes of greenhouse gases (GHG, e.g., CO₂, CH₄, and N₂O) from forest soils. The effects of N deposition on the GHG fluxes from forest soils were reviewed in this paper. N deposition to forest soils have shown variable effects on the soil GHG fluxes from forest, including increases, decreases or unchanged rates depending on forest type, N status of the soil, and the rate and type of atmospheric N deposition. In forest ecosystems where biological processes are limited by N supply, N additions either stimulate soil respiration or have no significant effect, whereas in “N saturated” forest ecosystems, N additions decrease CO₂ emission, reduce CH₄ oxidation and elevate N₂O flux from the soil. The mechanisms and research methods about the effects of N deposition on GHG fluxes from forest soils were also reviewed in this paper. Finally, the present and future research needs about the effects of N deposition on the GHG fluxes from forest soils were discussed.

Abstract:Despite lack of efficient physical protection in the highly competitive and hostile environment, the marine invertebrates including soft corals and gorgonians can survive, mainly relying on their chemical defensive system by a series of secondary metabolites accumulating in their bodies or releasing to their surroundings. The chemical defensive functions of these secondary metabolites were found to serve as antipredatory, antimicrobial, allelopathy and antifouling agents. Study on chemical defensive substances from corals and gorgonians is one of the most important topics in marine chemical ecology. The research results could help us to understand the chemical ecological relationships between corals and their surrounding organisms. The research strategy and methodology played an enlightening role in the discovery of bioactive natural products and the generation of new drug lead compounds from marine sources. The chemical defensive substances from soft corals and gorgonians were reviewed. This review focused on the structures of these secondary metabolites as well as their functions including antipredatory, allelopathy and antifouling activities.

Abstract:Field observations were conducted near the forest boundary in Qilian Mountain to test the differences in temporal variability of soil moisture between grassland, shrubland and forest habitats, and to examine the contributions of canopy rainfall interception and plant uptake to any observed differences. It was found that considerable differences of the temporal heterogeneity of soil moisture do exist between the three habitats. The coefficient of variance (CV) in soil moisture content at 5 cm depth was significantly higher in grassland and shrubland than in forest, while that at 20 cm was significantly higher in shrubland and forest than in grassland. High canopy rainfall interception of shrubs and intense soil moisture evaporation in grassland should be responsible for the higher temporal variability of soil moisture content at 5 cm depth in the two habitats, respectively, while the differences at 20 cm depths are most likely only due to the differences in canopy rainfall interception. Water uptakes provide little contribution to the differences in CVs of soil moisture at both 5 cm and 20 cm depths. It was also found that the CV at depth of 20 cm is significantly higher than that at depth of 5 cm, suggesting that the most active depth of soil moisture does not necessarily happen on the surface.