Rats Generate Vibrissal Sensory Evidence until Boundary Crossing Triggers a Decision

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Effects of plant hedgerows on soil erosion and soil fertility on sloping farmland in the purple soil area

Effect of using plant hedgerows on controlling soil and water losses has received wide recognition and this technology has been applied in many areas in the world. Yet, studies on the effect of using plant hedgerows on soil fertility on sloping lands are rare. Carrying out an eight-year fixed field experiment, the authors investigated the effect of two different hedgerows against the control treatment on soil fertility. Results showed that clay particles tended to accumulate in front of the plant hedgerows and began to erode downward below the hedgerows along the contour lines across the field. Distribution of soil organic matter and all plant nutrients except potassium (K) showed the same pattern as the clay particles. Potassium, however, was evenly distributed in the field without any noticeable influence from the hedgerows. Since the fixed experiment started, soil phosphorus (P) kept accumulating, while soil organic matter and K were in depletion. The results accordingly suggested better nutrient management practices on the sloping lands by using properly reduced rates of P and increased rates of farm manure and K. Taking the sloping field as a whole, special attention in nutrient management should be given to the soil strips —the portions below the plant hedgerows suffering from more serious soil erosion.     

红壤和风沙土添加不同化学结构有机碳对外源碳去向及累积贡献的影响

植物凋落物碳输入显著影响陆地生态系统土壤CO₂排放和有机碳(SOC)形成,然而,针对不同质地土壤添加不同化学结构外源碳去向依然不清楚。本研究将¹³C标记的葡萄糖、淀粉和纤维素添加至红壤和风沙土,比较2种质地土壤添加不同化学结构外源碳在土壤释放的CO₂、SOC、可溶性有机碳(DOC)和微生物生物量碳(MBC)库的净累积量、回收率及贡献比例上的差异。结果表明: 添加外源有机碳显著提高了CO₂、SOC、DOC和MBC的δ¹³C值,且随着外源有机碳化学结构复杂性的增加,CO₂的δ¹³C峰值依次延迟出现;外源有机碳种类、土壤类型和培养时间均显著改变外源碳去向及其在各碳库的贡献比例;在风沙土中,外源有机碳更多被矿化为CO₂,且CO₂库的外源碳净累积量和回收率大小依次为葡萄糖>淀粉>纤维素;红壤添加外源碳转变为SOC的累积量和回收率显著高于风沙土,且红壤SOC库的外源碳净累积量和回收率大小顺序也为葡萄糖>淀粉>纤维素。可见,外源有机碳化学结构和土壤质地共同调控外源碳去向及累积贡献。     

Host plants and edaphic factors influence the distribution and diversity of ectomycorrhizal fungal fruiting bodies within rainforests from Tshopo,Democratic Republic of the Congo

Ectomycorrhizal fungi constitute an important component of forest ecosystems that enhances plant nutrition and resistance against stresses. Diversity of ectomycorrhizal (EcM) fungi is, however, affected by host plant diversity and soil heterogeneity. This study provides information about the influence of host plants and soil resources on the diversity of ectomycorrhizal fungal fruiting bodies from rainforests of the Democratic Republic of the Congo. Based on the presence of fungal fruiting bodies, significant differences in the number of ectomycorrhizal fungi species existed between forest stand types (p < 0.001). The most ectomycorrhizal species‐rich forest was the Gilbertiodendron dewevrei‐dominated forest (61 species). Of all 93 species of ectomycorrhizal fungi, 19 demonstrated a significant indicator value for particular forest stand types. Of all analysed edaphic factors, the percentage of silt particles was the most important parameter influencing EcM fungi host plant tree distribution. Both host trees and edaphic factors strongly affected the distribution and diversity of EcM fungi. EcM fungi may have developed differently their ability to successfully colonise root systems in relation to the availability of nutrients.     

Sequence boundary and related sedimentary and diagenetic facies formed on Middle Permian mid-oceanic carbonate platform: Core observation of Akiyoshi Limestone,Southwest Japan

Detailed core observation of the Akiyoshi Limestone, Southwest Japan, reveals a sequence boundary and related sedimentary and diagenetic facies formed on a late Murgabian (Middle Permian) mid-oceanic carbonate platform. The sequence boundary lies upon karstified bioclastic grainstone and is overlain by peritidal lime- and dolo-mudstone. The karstified bioclastic grainstone, which had been affected by subaerial exposure and early diagenetic processes, is characterized by crystal silts, prismatic, bladed and dogtooth cements, blackened limestone features, and alveolar textures. The overlying peritidal lime- and dolo-mudstone is 8 m thick and exhibits fenestrae, fissures, laminations, black pebbles, and low-diversity biota composed exclusively of ostracodes and calcispherids. The sequence boundary almost coincides with a major fusulinoidean biostratigraphic boundary. A sea-level fall in the late Murgabian resulted in a biotic turnover and formed the sequence boundary and the karst textures. The following relatively slow transgression resulted in the deposition of the thick transgressive peritidal unit.     

Puroindolines: the molecular genetic basis of wheat grain hardness

The variation in grain hardness is the single most important trait that determines end-use quality of wheat. Grain texture classification is based primarily on either the resistance of kernels to crushing or the particle size distribution of ground grain or flour. Recently, the molecular genetic basis of grain hardness has become known, and it is the focus of this review. The puroindoline proteins a and b form the molecular basis of wheat grain hardness or texture. When both puroindolines are in their `functional' wild state, grain texture is soft. When either one of the puroindolines is absent or altered by mutation, then the result is hard texture. In the case of durum wheat which lacks puroindolines, the texture is very hard. Puroindolines represent the molecular-genetic basis of the Hardness locus on chromosome 5DS and the soft (Ha) and hard (ha) alleles present in hexaploid bread wheat varieties. To date, seven discrete hardness alleles have been described for wheat. All involve puroindoline a or b and have been designated Pina-D1b and Pinb-D1b through Pinb-D1g. A direct role of a related protein, grain softness protein (as currently defined), in wheat grain texture has yet to be demonstrated.     

Desert perennials as plant and soil indicators in Eastern Arabia

Soils of different Eastern Arabian vegetation types, dominated by five desert perennials have been analysed for their texture, salinity and surface hardness. The vegetation types were analysed for plant species richness and composition. Special emphasis was given to Abu Dhabi's widespread terrestrial perennials Cyperus conglomeratus Rottb., Haloxylon salicornicum (Moq.) Bge., Pennisetum divisum (Gmel.) Henr., Seidlitzia rosmarinus Ehrenb. ex Bge. and Zygophyllum mandavillei Hadidi. The results show some important relationships between soils and plants. C. conglomeratus indicates the lowest soil salinity levels and the finest texture. P. divisum indicates the highest species richness and S. rosmarinus indicates the lowest species richness. Z. mandavillei indicates the highest salinity levels, the largest soil particle size, and the hardest soil surfaces.     

Influence of O2 availability on NO and N2O release by nitrification and denitrification in soils

The availability of O₂ is believed to be one of the main factors regulating nitrification and denitrification and the release of NO and N₂O. The availability of O₂ in soil is controlled by the O₂ partial pressure in the gas phase and by the moisture content in the soil. Therefore, we investigated the influence of O₂ partial pressures and soil moisture contents on the NO and N₂O release in a sandy and a loamy silt and differentiated between nitrification and denitrification by selective inhibition of nitrification with 10 Pa acetylene. At 60% whc (maximum water holding capacity) NO and N₂O release by denitrification increased with decreasing O₂ partial pressure and reached a maximum under anoxic conditions. Under anoxic conditions NO and N₂O were only released by denitrification. NO and N₂O release by nitrification also increased with decreasing O₂ partial pressure, but reached a maximum at 0.1–0.5% O₂ and then decreased again. Nitrification was the main source of NO and N₂O at O₂ partial pressures higher than 0.1–0.5% O₂. At lower O₂ partial pressures denitrification was the main source of NO and N₂O. With decreasing O₂ partial pressure N₂O release increased more than NO release, indicating that the N₂O release was more sensitive against O₂ than the NO release. At ambient O₂ partial pressure (20.5% O₂) NO and N₂O release by denitrification increased with increasing soil moisture content. The maximum NO and N₂O release was observed at soil moisture contents of 65–80% whc and 100% whc, respectively. NO and N₂O release by nitrification also increased with increasing soil moisture content with a maximum at 45–55% whc and 90% whc, respectively. Nitrification was the main source of NO and N₂O at soil moisture contents lower than 90% whc and 80% whc, respectively. Higher soil moisture contents favoured NO and N₂O release by denitrification. Soil texture had also an effect on the release of NO and N₂O. The coarse-textured sandy silt released more NO than N₂O compared with the fine-textured loamy silt. At high soil moisture contents (80–100% whc) the fine-textured soil showed a higher N₂O release by denitrification than the coarse-textured soil. We assume that the fine-textured soil became anoxic at a lower soil moisture content than the coarse-textured soil. In conclusion, the effects of O₂ partial pressure, soil moisture and soil texture were consistent with the theory that denitrification increasingly contributes to the release of NO and in particular N₂O when conditions for soil microorganisms become increasingly anoxic.