Density of Monoporeia affinis and biogeochemistry in Baltic Sea sediments

This study focused on effects from Monoporeia affinis reworking and ventilation activities on benthic fluxes and mineralization processes during a simulated bloom event. The importance of M. affinis density for benthic solute (O₂, ΣNO₂⁻ + NO₃⁻, NH₄⁺ and HPO₄²⁻) fluxes and sediment reactivity (mobilization of NH₄⁺ and HPO₄²⁻) following additions of organic material to the sediment surface was experimentally investigated using sediment-water and closed sediment (jar) incubations. Three different densities of M. affinis were used to resemble a low, medium and high density situation (1300, 2500 and 6400 ind. m^− 2, respectively) of a natural amphipod community. The degradation of phytodetritus (Tetraselmis sp., 5 g C m^− 2) added to the sediment surface was followed over a period of 20 days. Benthic solute fluxes of O₂, ΣNO₂⁻ + NO₃⁻ and NH₄⁺ were generally progressively stimulated with increasing number of M. affinis, while no such correlation was found for HPO₄²⁻. Solute fluxes were initially enhanced 1 to 2 days after the addition of phytodetritius, caused by mineralization of the most labile organic material and a food-stimulated irrigation by the amphipods. There was no effect from the activity of M. affinis on total denitrification (Dtot = Dn + Dw) or denitrification utilizing nitrate from coupled nitrification/denitrification (Dn) for any of the densities examined. Denitrification utilizing overlying water nitrate (Dw) was only about 10% of Dtot. Dw was significantly enhanced for the highest M. affinis density investigated. The reactivity of the sediment decreased progressively with increasing density of M. affinis and with time of the experiment. However, enhanced ammonium production at least 6 days after the organic addition indicated excretion of N-containing organic compounds by M. affinis. In conclusion, large spatial and temporal variations in density of M. affinis may be of significant importance for benthic solute fluxes and overall mineralization of organic material in Baltic Sea sediments.     

Seasonal and Spatial Controls over Nutrient Cycling in a Pacific Northwest Prairie

West Coast prairies in the US are an endangered ecosystem, and effective conservation will require an understanding of how changing climate will impact nutrient cycling and availability. We examined how seasonal patterns and micro-heterogeneity in edaphic conditions (% moisture, total organic carbon, % clay, pH, and inorganic nitrogen and phosphorus) control carbon, nitrogen, and phosphorus cycling in an upland prairie in western Oregon, USA. Across the prairie, we collected soils seasonally and measured microbial respiration, net nitrogen mineralization, net nitrification, and phosphorus availability under field conditions and under experimentally varied temperature and moisture treatments. The response variables differed in the degree of temperature and moisture limitation within seasons and how these factors varied across sampling sites. In general, we found that microbial respiration was limited by low soil moisture year-round and by low temperatures in the winter. Net nitrogen mineralization and net nitrification were never limited by temperature, but both were limited by excessive soil moisture in winter, and net nitrification was also inhibited by low soil moisture in the summer. Factors that enhanced microbial respiration tended to decrease soil phosphorus availability. Edaphic factors explained 76% of the seasonal and spatial variation in microbial respiration, 35% of the variation in phosphorus availability, and 29% of the variation in net nitrification. Much of the variation in net nitrogen mineralization remained unexplained (R ² = 0.19). This study, for the first time, demonstrates the complex seasonal controls over nutrient cycling in a Pacific Northwest prairie.     

Influence of catclaw Mimosa monancistra on the dissipation of soil PAHs

Phytoremediation is a cost-effective biotechnology for decontamination of polycyclic aromatic hydrocarbons (PAHs)-polluted soils. A greenhouse experiment was conducted to determine the growth of Mimosa monancistra, a N2-fixing leguminous plants, and its capacity to remove phenanthrene, anthracene, and benzo(a)pyrene (BaP)from soil. The PAHs decreased shoot and root dry biomass of M. monancistra 2.7- and 3.9-fold, respectively, compared to uncontaminated soil and inhibited nodule formation. The removal of phenanthrene and anthracene was similar in vegetated and unvegetated soil, but the dissipation of BaP was significantly faster in vegetated soil as compared to unvegetated soil after 14, 56, 70, and 90 d. After 90 d, dissipation of BaP was 96% in vegetated soil and 87% in unvegetated soil. Nitrification and ammonification were not affected by the addition of PAHs as concentrations of NH4+, NO2-, and NO3- were similar in contaminated and uncontaminated vegetated soil. Growth of M. monancistra was inhibited by contamination with hydrocarbons, but removal of BaP was accelerated in the rhizosphere.     

松嫩平原农业区土壤理化性质与真菌代谢产物——球囊霉素相关土壤蛋白的关系

对不同土壤深度的真菌特征代谢产物球囊霉素相关土壤蛋白(glomalin-related soil protein,GRSP)与土壤理化性质相关关系的研究,有助于揭示土壤真菌在不同土壤深度对养分的调节作用。本研究在松嫩平原农田5个土层(0~100 cm)采集360个土样,分析了易提取球囊霉素相关土壤蛋白(EE-GRSP)、总提取球囊霉素相关土壤蛋白(T-GRSP)含量和11个土壤理化性质指标及其相关关系。结果表明:表层EE-GRSP和T-GRSP平均含量为0.74和6.0 mg·g-1,随土层加深均呈显著下降趋势;深层土壤养分储量较大,有机碳、全氮、全磷、全钾、碱解氮、速效磷和速效钾储量在深层(40~100 cm)占总储量的41.2%~62.8%;土壤p H、容重、含水量和电导率也表现了明显的垂直变化规律;各理化性质在不同土层与GRSP的相关关系不同,有机碳在全部深度与GRSP均有显著的相关关系,而p H与GRSP均在20~100 cm深度有极显著的相关性(P0.01),且与EE-GRSP、T-GRSP显著相关的理化性质指标分别在60~80、20~60 cm最多,在表层最少;GRSP在深层土壤与各指标的相关性与表层不同,可能会影响GRSP对不同土壤深度养分的调节功能;鉴于深层土壤中GRSP与养分显著相关,本研究提出,种植与土壤真菌具有共生关系的深根性植物是对富集养分的深层土壤进行生物修复的有效方法。     

矿区不同复垦措施对土壤碳矿化和酶活性的影响

矿区废弃地生态退化形势严峻,生态修复已成为矿区可持续发展的主要措施,目前关于矿区复垦后土壤碳矿化和酶活性变化的研究较少。以山西省孝义市露天矿区复垦区为研究对象,植被恢复类型包括了百脉根、苜蓿、油松和柳树-圆柏混交林,并对其分别进行不施肥(对照)、无机肥、复合肥和有机肥处理,从而研究植被类型与施肥方式对矿区土壤碳矿化和酶活性的影响。结果表明,乔本比草本恢复类型的土壤有机碳矿化潜势大,不同施肥条件的土壤有机碳矿化潜势和累积量趋势基本为:对照无机肥复合肥有机肥;4种土壤酶活性因植被恢复类型和施肥处理的不同而差异显著,不同土壤酶与降解特性不同的有机碳间相关性有所不同。土壤碳矿化累积量和酶活性均受植被恢复类型、施肥处理及两者交互作用的显著影响,因此对复垦措施敏感的土壤有机碳矿化和酶活性可作为评价复垦措施的指标。     

Biological variables as soil quality indicators: Effect of sampling time and ability to classify soils by their suitability

Soil biological variables are considered good soil quality indicators due to their high sensitivity and ability to reflect soil management effects. However, they frequently show high temporal variability. Our objectives were: (a) to analyze temporal stability and seasonal effect on biological variables, (b) to choose between autumn and spring to sample for soil biological variables, and (c) to determine biological variables able to discriminate among selected soil subgroups. Areas with minimal human disturbance were sampled in three soil orders (Mollisol, Vertisol and Alfisol) during two and a half years, each autumn and spring. Microbial biomass C and N (MBC, MBN), basal respiration (Resp), metabolic quotient (qCO₂), potential of N mineralization (PNM-AI), soil organic C (TOC) and total soil N (TON) were measured in three composite soil samples collected from homogeneous areas at 0–15 cm depth. For the studied soils, selected soil biological variables presented different levels depending on the time of sampling, spring or autumn. Hence, the importance of pointing out the time of sampling to report results of these variables in this kind of studies is remarked. In general, biological variables presented higher stability when we sampled soils in autumn compared to spring. Because of this, we used autumn soil samples to determine the best soil biological variables to discriminate among selected subgroups of soils. The separation of soil subgroups by means of discriminant analysis using just TOC and TON was scrutinized, considering that these soil variables are routinely measured in soil test laboratories. Nonetheless they were not able to discriminate properly among soil subgroups because they showed high error rates classifying the samples in the correct subgroups. In contrast, the variables PMN-AI, MBC, and MBN adequately discriminated the five soil subgroups. From the biological variables, PMN-AI and MBC were the best ones to characterize (discriminate) among the five soil subgroups. Particularly, PMN-AI was able to separate soils by their suitability for agricultural purposes.     

Carbon mineralization and distribution of nutrients within different particle-size fractions of commercially produced olive mill pomace

Composting is a realistic option for disposal of olive mill pomace (OMP) by making it suitable as a soil amendment for organic farming. The chemical and physical characteristics and contribution of particle-size fractions to total nutrients and carbon mineralization of seven commercial composts of OMP (COMP) were investigated. Higher proportions of manure, co-composted with OMP, reduced the organic matter (OM), total carbon and C:N ratio of the product, but increased the content of nutrients and fine particles. The fine particles had higher nutrient contents, but less OM and carbon and, unlike larger particles, did not exhibit any phytotoxicity. Less than 1.5% of added carbon was mineralized in whole compost, but a lower rate was found with larger particles. Separation of COMP by particle size fractionation and application as a soil conditioner is recommended for better optimization of COMP with the <1 mm fraction providing the higher quality compost.     

生源要素有效性及生物因子对湿地土壤碳矿化的影响

湿地土壤是全球碳存储的重要场所,湿地生态系统的碳循环过程对全球变化有重要指示作用。土壤碳矿化是湿地生态系统碳循环的重要环节,对于认知湿地生态系统生物地球化学循环过程具有重要的意义。综述了生源要素及生物因素对湿地土壤碳矿化的内在作用机制。土壤活性有机碳库通过调节土壤能源物质和微生物活性影响土壤碳库的有效性,是表征土壤碳矿化的敏感指标。湿地其它养分如N、P、S等元素的有效性也是影响土壤碳矿化的关键要素。电子受体(NO₃^-、SO₄^2-、Fe³⁺、Mn⁴⁺等)对湿地土壤碳矿化和有机碳转变的影响主要通过电子受体的还原过程完成,在厌氧分解过程中,湿地土壤利用难溶性电子受体可能是土壤C矿化的更重要途径。动物、植物、微生物群落和区系等则是土壤碳矿化的主要驱动因子。土壤动物区系在有机态养分矿化为无机态养分的过程有着独特的功能,能显著增加土壤碳矿化。土壤微生物的活性,决定着土壤中有机碎屑的降解速率,是土壤有机碳分解周转的主要诱导因素。湿地植物则通过影响根系、微生物呼吸底物的供应以及对小气候和土壤因子的调节而影响土壤有机质的分解。湿地生源要素和生物因子还极易与土壤理化性质如温度、水分、pH值和质地等环境因素形成交互和制约,共同影响土壤碳矿化。最后,提出了进一步研究生源要素和生物因素与湿地土壤碳矿化关系需要解决的一些重要问题。     

8-异戊烯基柑橘素促进体外培养成骨细胞成熟矿化的研究

研究8-异戊烯基柑橘素对体外培养大鼠颅骨成骨细胞(rat skull osteoblasts,ROB)的分化成熟及生物矿化的影响.取新生大鼠颅骨多次酶消化法得到成骨细胞,培养于含10%FBS的MEM培养液中,3天后首次换液,待细胞铺满皿底传代培养.以碱性磷酸酶(alkaline phosphatase,ALP)为检测指标,96孔板梯度筛选作用最佳浓度,在最佳浓度作用并成骨性诱导培养的第3、6、9、12天测ALP活性、钙盐沉积量;第12天进行ALP和钙化结节组织化学染色及计数;成骨性诱导后不同时间点提取Total RNA,RT real-time PCR法检测成纤维细胞生长因子(bFGF)、胰岛素样生长因子-1(IGF-1)、成骨相关转录因子Osterix、Runx-2和骨形态发生蛋白-2(BMP-2)的基因表达情况;成骨性诱导的第4、8、12天裂解获得细胞总蛋白,蛋白质印迹法检测人Ⅰ型胶原蛋白(COL-Ⅰ)的蛋白质表达量.研究结果表明:1×10-6 mol/L能显著促进成骨细胞的成熟分化,表现为提高ROB的ALP活性、促进钙盐沉积、增加钙化结节数量;提高bFGF、IGF-1、Osterix、Runx-2和BMP-2 mRNA表达水平;促进COL-Ⅰ的合成.由此可知终浓度为1×10-6 mol/L 8-异戊烯基柑橘素能显著促进ROB的分化成熟及生物矿化,证明8-异戊烯基柑橘素能促进成骨细胞的分化成熟及生物矿化,作为促进骨修复和抗骨质疏松的有效成分具有较大的药用价值.