Effects of grazing intensity and grazing exclusion on litter decomposition in the temperate steppe of Nei Mongol,China

Aims Grazing intensity and grazing exclusion affect ecosystem carbon cycling by changing the plant community and soil micro-environment in grassland ecosystems. The aims of this study were: 1) to determine the effects of grazing intensity and grazing exclusion on litter decomposition in the temperate grasslands of Nei Mongol; 2) to compare the difference between above-ground and below-ground litter decomposition; 3) to identify the effects of precipitation on litter production and decomposition. Methods We measured litter production, quality, decomposition rates and soil nutrient contents during the growing season in 2011 and 2012 in four plots, i.e. light grazing, heavy grazing, light grazing exclusion and heavy grazing exclusion. Quadrate surveys and litter bags were used to measure litter production and decomposition rates. All data were analyzed with ANOVA and Pearson’s correlation procedures in SPSS. Important findings Litter production and decomposition rates differed greatly among four plots. During the two years of our study, above-ground litter production and decomposition in heavy-grazing plots were faster than those in light-grazing plots. In the dry year, below-ground litter production and decomposition in light-grazing plots were faster than those in heavy-grazing plots, which is opposite to the findings in the wet year. Short-term grazing exclusion could promote litter production, and the exclusion of light-grazing could increase litter decomposition and nutrient cycling. In contrast, heavy-grazing exclusion decreased litter decomposition. Thus, grazing exclusion is beneficial to the restoration of the light-grazing grasslands, and more human management measures are needed during the restoration of heavy-grazing grasslands. Precipitation increased litter production and decomposition, and below-ground litter was more vulnerable to the inter-annual change of precipitation than above-ground litter. Compared to the light-grazing grasslands, heavy-grazing grasslands had higher sensitivity to precipitation. The above-ground litter decomposition was strongly positively correlated with the litter N content (R² = 0.489, p < 0.01) and strongly negatively correlated with the soil total N content (R² = 0.450, p < 0.01), but it was not significantly correlated with C:N and lignin:N. Below-ground litter decomposition was negatively correlated with the litter C (R² = 0.263, p < 0.01), C:N (R² = 0.349, p < 0.01) and cellulose content (R² = 0.460, p < 0.01). Our results will provide a theoretical basis for ecosystem restoration and the research of carbon cycling.     

Aquatic macrophyte breakdown in an Appalachian river

Weight loss from Podostemum ceratophyllum, Elodea canadensis, Potamogeton crispus, Justicia americana, and Typha latifolia was measured by exposing air dried leaf material in 15 cm² nylon mesh bags (3 mm octagonal openings). Breakdown rates for these species were 0.037, 0.026, 0.02l, 0.016, and 0.007 day^–1, respectively. In general, these rates are much faster than reported rates of tree leaf breakdown in streams. Shredders accounted for 35% of the macroinvertebrates found on the leaf bags. However, macroinvertebrate densities on the aquatic macrophyte tissue were well below densities commonly found on leaf bags in small streams. The rapid breakdown of aquatic macrophytes in the New River suggests that organic matter from this source may constitute a significant pulse in the annual energy dynamics of the river.     

恩诺沙星残留对土壤微生物功能的影响

研究了恩诺沙星残留对土壤呼吸作用、纤维分解作用、氨化作用、硝化作用的影响 ,结果表明 ,相对较低浓度恩诺沙星残留(0 .0 1μg/ g土 ,0 .1μg/ g土 )刺激土壤呼吸作用 ,相对较高浓度恩诺沙星残留 (1μg/ g土 )对土壤呼吸作用产生抑制 ,药物作用活性维持期为 6 d;恩诺沙星残留对土壤纤维分解作用影响较不明显 ;较低浓度恩诺沙星残留 (0 .0 1μg/ g土 ,0 .1μg/ g土 )对土壤氨化作用有刺激作用 ,而较高浓度恩诺沙星残留 (1μg/ g土 ,10μg/ g土 )则会对其起抑制作用 ,药物作用活性期为 9d;不同浓度恩诺沙星对土壤硝化作用影响极其显著 ,当恩诺沙星浓度达到 1μg/ ml时 ,在 3～ 9d内 ,对土壤硝化作用有一定抑制作用。当恩诺沙星浓度达到 10μg/ ml时 ,强烈抑制了土壤硝化作用 ,直到本试验结束时 ,其抑制作用未见减弱。结果表明恩诺沙星残留影响了土壤微生物这些功能 ,因而可能影响到土壤特性和土壤中一些生态过程     

北方森林土壤呼吸和木质残体分解释放出的CO2通量

北方森林因其面积大、土壤碳储量高以及对全球暖化响应敏感而在全球碳平衡和气候系统中起着至关重要的作用。土壤呼吸和木质残体分解释放出的 CO2 通量是北方森林生态系统输入大气圈的最主要的碳源。量化这个通量并深刻理解其中的机理过程 ,是评价和预测北方森林在全球变化中的作用必不可少的内容。综述了北方森林生态系统土壤呼吸和木质残体分解释放出的 CO2 通量随生态系统类型及环境条件而变化的一般格局以及自养呼吸和异氧呼吸在土壤表面 CO2 通量中的相对贡献 ;分析了影响北方森林土壤呼吸的主要生物物理因子 ;讨论了该领域研究存在的问题和今后的研究方向 ;并强调木质残体分解释放出的 CO2 通量虽然在以往的森林生态系统碳平衡研究中常被忽略 ,但在火灾频繁的北方森林中不容忽视     

Mass loss and macroinvertebrate colonisation of fish carcasses in riffles and pools of a NW Italian stream

In this study, we analysed the decomposition of trout carcasses in a low-order Apennine stream, with the aim to investigate the mass loss rate in a Mediterranean lotic system, and to examine the influence of microhabitats on the invertebrates colonising fish carcasses. In May 2003, we put 56 dead rainbow trout (Oncorhynchus mykiss) in the stream, placing seven sets (four trout each) in both riffle and pool habitats. At four dates, we removed one trout per set to measure its dry mass and determine the associated macroinvertebrate assemblage. Fifty-eight macroinvertebrate taxa colonised the carcasses, with significant differences between the erosive and depositional microhabitats. Riffle trouts hosted richer and denser colonist communities than pool trouts. Chironomidae, Serratella ignita, Habrophlebia sp., Dugesia sp. and Protonemura sp. were the five most abundant taxa. Decomposition was initially very rapid in both environments and then tapered off over time. The mass loss rate was higher (k= –0.057 day^–1) than that found in other studies. Higher Mediterranean temperatures probably increase the process. Although we found no significant difference between riffles and pools, mass loss was more regular in erosive habitats, underlining the importance of local, small-scale conditions. In small, low-order, heterotrophic streams, fish carcasses represent an important resource and shelter for rich and diversified invertebrate assemblages.     

氯酸盐生态毒理研究进展

氯酸盐是一类毒性强氧化剂。20世纪,氯酸钠曾被作为非选择性除草剂和脱叶剂在农业生产中大量施用。近年来,氯酸钾作为龙眼产期调控剂也在反季节龙眼生产中应用。然而,氯酸根离子强氧化性对生物体有明显的毒害效应,且其分解产物亚氯酸根和次氯酸根离子对水体和土壤等环境也存在较强的污染效应。本文在介绍氯酸盐理化性质基础上,初步分析了氯酸盐对植物、动物、微生物和人体的毒害效应,探讨了氯酸盐在土壤和水体中的环境行为,提出了如何在生产实践中安全使用氯酸盐,并就氯酸盐在生态环境中的检测方法和生物降解等研究前沿进行了展望。     

兼性厌氧纤维素降解菌的筛选和产酶研究

从我国天津地区堆肥中分离筛选出一株兼性厌氧的纤维素分解细菌D1,初步鉴定为纤维单孢菌(Cellulomonas sp.)。产酶最适碳源为葡萄糖,氮源为复合蛋白胨,酶的最适作用温度和pH值是50℃和6．4,在70℃以下和pH在5．2～8．4里稳定。     

Fine root dynamics and trace gas fluxes in two lowland tropical forest soils

Fine root dynamics have the potential to contribute significantly to ecosystem‐scale biogeochemical cycling, including the production and emission of greenhouse gases. This is particularly true in tropical forests which are often characterized as having large fine root biomass and rapid rates of root production and decomposition. We examined patterns in fine root dynamics on two soil types in a lowland moist Amazonian forest, and determined the effect of root decay on rates of C and N trace gas fluxes. Root production averaged 229 (±35) and 153 (±27) g m^?2 yr^?1 for years 1 and 2 of the study, respectively, and did not vary significantly with soil texture. Root decay was sensitive to soil texture with faster rates in the clay soil (k=?0.96 year^?1) than in the sandy loam soil (k=?0.61 year^?1), leading to greater standing stocks of dead roots in the sandy loam. Rates of nitrous oxide (N₂O) emissions were significantly greater in the clay soil (13±1 ng N cm^?2 h^?1) than in the sandy loam (1.4±0.2 ng N cm^?2 h^?1). Root mortality and decay following trenching doubled rates of N₂O emissions in the clay and tripled them in sandy loam over a 1‐year period. Trenching also increased nitric oxide fluxes, which were greater in the sandy loam than in the clay. We used trenching (clay only) and a mass balance approach to estimate the root contribution to soil respiration. In clay soil root respiration was 264–380 g C m^?2 yr^?1, accounting for 24% to 35% of the total soil CO₂ efflux. Estimates were similar using both approaches. In sandy loam, root respiration rates were slightly higher and more variable (521±206 g C m² yr^?1) and contributed 35% of the total soil respiration. Our results show that soil heterotrophs strongly dominate soil respiration in this forest, regardless of soil texture. Our results also suggest that fine root mortality and decomposition associated with disturbance and land‐use change can contribute significantly to increased rates of nitrogen trace gas emissions.     

Facilitative interactions rather than resource partitioning drive diversity-functioning relationships in laboratory fungal communities

We manipulated the number of saprotrophic fungi in either a complex multi-resource substratum (sterilized forest soil), or a single-resource substratum (powdered cellulose). The substrates were inoculated with five common species of soil fungi in all possible combinations (from monocultures to five species in combination). In both substrates, the rate of organic matter decomposition was positively associated with species richness. The effect of fungal diversity was much stronger in the uniform single-resource substrate ( r ² = 0.455, P  < 0.0001) than in soil ( r ² = 0.154, P  < 0.0001). The results document that species richness of microbial decomposers strongly affects decomposition processes, at least at the species poor end of the diversity gradient. Both, 'sampling effect' and 'species complementarity effect' contributed to the community response with the latter being much more pronounced in uniform substrate than in soil. This indicates that facilitative interactions are more important than resource partitioning for positive effects of species richness.