Carbon cycling in subarctic tundra; seasonal variation in ecosystem partitioning based on in situ C pulse-labelling

Carbon assimilation and allocation were studied in a tundra ecosystem in northern Scandinavia. Seasonal variation in the below-ground carbon allocation to dissolved organic carbon (DOC), coarse-, fine-, and hair roots was investigated using in situ ¹⁴C pulse-labelling, adding 2-3 MBq ¹⁴CO₂ dm⁻² to the above-ground vegetation. Combining the allocation data with regression models of the seasonal carbon flux made it possible to estimate a temporally explicit ecosystem carbon allocation budget.The ecosystem was a net source of CO₂, losing on average 0.97 g C m⁻² d⁻¹ to the atmosphere, with little variation through the season. There was, however, significant temporal variation in partitioning of recently assimilated carbon. Allocation to below-ground compartments over 32 days following labelling increased from 18% in June to 55% in September. Above-ground allocation showed the opposite trend. Hair roots and DOC were strong sinks in the autumn. Transport of newly assimilated carbon occurred rapidly throughout the season, ¹⁴C appearing in all sampled pools within 4 h of labelling.The seasonal variation in carbon partitioning observed in this study has implications for the residence time of assimilated carbon in the ecosystem. A relatively greater allocation to rapidly decomposing pools, such as hair roots and DOC, would tend to reduce incorporation into woody tissue, increasing the overall rate of carbon cycling and decreasing ecosystem storage. The results of this study will be of value for building and validating mechanistic models of ecosystem carbon flow in tundra and subarctic ecosystems.     

CaCl2对细颗粒泥沙静水絮凝沉降的影响

细颗粒泥沙的絮凝或分散对土壤渗透性、土壤可蚀性有重要作用,是水土保持研究的重要内容.在CaCl2浓度为0～1.0 mmol/L,泥沙浓度为10 g/L时,用吸管法研究了CaCl2对细颗粒泥沙絮凝沉降的影响.结果表明:泥沙沉降分2个阶段,分选沉降段和絮凝沉降段;在絮凝沉降段,CaCl2浓度越大,絮凝沉降越快.但较高浓度时,细颗粒泥沙平均沉速反而随CaCl2浓度增大而逐渐减小;泥沙浓度随时间呈指数衰减;细颗粒泥沙絮凝临界粒径为0.03 mm.     

施加钙对锶胁迫下麻疯树生长及生理生化的影响

为了研究外源钙对锶胁迫下麻疯树生理生化的影响,本试验以麻疯树为研究材料,施加88Sr2+(200mg·kg-1)与不同浓度Ca2+(0、100和200mg·kg-1),处理30、70和120 d后取样,测定生长指标及生理生化等指标,以此研究Ca2+对麻疯树所受Sr2+胁迫的调节作用。结果表明:施加Ca2+促进了株高和叶面积增加,并在前期大量促进叶绿素的合成;最大荧光Fm和最大光化学效率Fv/Fm等荧光参数随着处理时间逐渐升高并在120 d时显著高于对照组,表明Ca2+降低了胁迫对PSII反应中心的损害;施加Ca2+后幼苗SOD、POD和CAT活性明显降低,说明88Sr2+胁迫对抗氧化防御系统的刺激有所降低;丙二醛与脯氨酸含量的降低也表明施加Ca2+缓解了幼苗所受88Sr2+胁迫。通过对比,低浓度Ca2+能够更好地缓解胁迫,对株高、株茎和叶面积的促进作用明显高于高浓度Ca2+处理。在处理30 d时,低浓度Ca2+对叶绿素含量、Fv/Fm和电子传递速率ETR的调节效果更明显。因此,Ca2+可以在一定程度上缓解88Sr2+对麻疯树幼苗的胁迫,并且低浓度Ca2+的缓解效果更明显。研究结果为木本植物修复放射性核素污染土壤提供了一定的科学依据。     

三峡库区消落带湿地土壤有机碳及其组分特征

湿地生态系统土壤有机碳库的组分变化对于全球碳平衡起着极其重要的作用。本研究选取三峡库区消落带湿地3个海拔梯度的土壤,以从未淹没的样地作为对照,研究消落带湿地不同海拔梯度土壤有机碳组分的特征。结果表明:土壤有机碳、易氧化有机碳、水溶性碳水化合物有机碳和和微生物生物量碳均以消落带小于未淹没样地。在消落带,海拔最低、淹没持续时间较长且正处于水位波动期的样地土壤有机碳、易氧化碳和微生物生物量碳显著低于其他样地,而土壤矿化碳显著高于其他样地。相关性分析表明,土壤有机碳与微生物生物量碳(R~2=0.94)的正相关性显著高于与易氧化有机碳(R~2=0.88)、水溶性有机碳(R~2=0.73)及其水溶性碳水化合物(R~2=0.70)之间的正相关性,但是与矿化碳之间无显著的相关性。因此,土壤微生物生物量碳是消落带湿地土壤有机碳随不同海拔梯度变化的最敏感的组分。     

重金属超富集植物龙葵对镉响应的蛋白组学分析

龙葵是典型的重金属超富集植物,但是我们对其重金属耐受和超富集的分子机理仍不完全清楚。为了从蛋白组学层面探究重金属超富集植物龙葵如何响应金属镉,本研究采用双向电泳和MALDI-TOF MS分析方法,鉴定了重金属超富集植物龙葵叶片和根中Cd胁迫下差异表达的蛋白。双向电泳在根和叶片中分别至少得到927和1 025个蛋白点,其中Cd胁迫下差异表达的蛋白点在根中有45个,叶片中有57个。采用MALDITOF MS分析,在根和叶片中分别鉴定了9个和12个蛋白点,分别代表了9个和6个差异表达的蛋白。生物信息学分析表明,这些蛋白涉及到激素合成、防御响应、能量代谢和细胞结构等。这些结果为进一步揭示重金属超富集植物龙葵响应Cd胁迫的分子调节机制,以及为通过现代生物技术手段进行重金属污染的植物修复提供了理论依据。     

外源NO对Ca(NO3)2胁迫下黄瓜幼苗生长和抗氧化系统的影响

本研究以黄瓜为试材,采用营养液水培,研究了外源NO对Ca(NO3)2胁迫下黄瓜幼苗生长和抗氧化酶系的影响.结果显示,在70mmol·L-1的Ca(NO3)2胁迫下,植株生长受到抑制,干重和叶绿素含量显著下降,叶片和根系抗氧化酶SOD、POD、CAT和APX活性均升高,膜脂过氧化产物MDA及可溶性 蛋白含量增加.而叶面喷施NO供体SNP显著缓解了Ca(NO3)2胁迫对黄瓜幼苗生长的抑制,植株干重显著增加.同时,抗氧化酶活性、可溶性蛋白和叶绿素含量也有不同程度的上升,MDA含量显著下降.以上表明,NO能够增强黄瓜幼苗对Ca(NO3)2胁迫的耐性.喷施SNP对正常营养液培养的黄瓜幼苗无显著影响.     

Effect of soil physical properties on soybean nodulation and N2 fixation at the early growth stage in heavy soil field in Hachirougata Polder,Japan

We studied the effect of the soil physical properties on soybean nodulation and N₂ fixation in the heavy soil of an upland field (UF) and an upland field converted from a paddy field (UCPF) in the Hachirougata polder, Japan. Seeds of the soybean cultivar Ryuho were sown in each field with or without inoculation of Bradyrhizobium japonicum A1017. The soybean plants were sampled at 35 (V3) and 65 (Rl) d after sowing (DAS), and then nodulation and the percentage of N derived from N₂ fixation in the xylem sap were determined. The soil physical properties were different between UF and UCPF, especially the air permeability and soil water regime. Nodule growth was restricted in UCPF irrespective of rhizobial inoculation, though rhizobial infection was not inhibited by the unfavorable soil physical conditions. Soybean plant growth was closely related to the nodule mass and N₂ fixation activity, and the inoculation of a superior rhizobium strain was effective only at 35 DAS. These results indicate that soybean nodulation and N₂ fixation was considerably affected by the physical properties of heavy soil, and that it is important to maintain the N₂ fixation activity and inoculate the soybean plants with a superior rhizobium strain at a later growth stage in order to increase soybean production in heavy soil fields.     

转5-烯醇式丙酮酰莽草酸-3-磷酸合酶(EPSPS)基因抗草甘膦烟草和棉花的获得

以从抗草甘膦的荧光假单胞菌(Pseudomonas fluorescens)G2中克隆的、并按双子叶植物偏爱密码子改造的5-烯醇式丙酮酰莽草酸-3-磷酸合酶(EPSPS)基因aroAG2M为目的基因,用菊花Rubisco小亚基的启动子驱动,在基因的5'端加叶绿体定位信号肽,构建植物表达载体。用根癌农杆菌(Agrobacterium tumefaciens)介导的叶盘法转化烟草(Nicotiana tabacum)获得转基因植株,PCR检测表明,外源基因已整合到烟草基因组中。转基因和非转基因植株6～8叶龄苗的叶片涂抹不同浓度的草甘膦异丙胺盐,表明转基因植株可抗4‰浓度的草甘膦,而非转基因对照植株则在2‰草甘膦时即死亡。花粉管通道法转化棉花(Gossypium hirsutum),得到3株具有草甘膦抗性的转基因植株,PCR和Southern检测显示,外源基因已整合到棉花基因组中,田间喷洒草甘膦异丙胺盐水剂,表明T1代转基因植株具有草甘膦抗性。     

CO2 emission in an intensively cultivated loam as affected by long-term application of organic manure and nitrogen fertilizer

A long-term field experiment was conducted to examine the influence of mineral fertilizer and organic manure on the equilibrium dynamics of soil organic C in an intensively cultivated fluvo-aquic soil in the Fengqiu State Key Agro-Ecological Experimental Station (Fengqiu county, Henan province, China) since September 1989. Soil CO₂ flux was measured during the maize and wheat growing seasons in 2002-2003 and 2004 to evaluate the response of soil respiration to additions and/or alterations in mineral fertilizer, organic manure and various environmental factors. The study included seven treatments: organic manure (OM), half-organic manure plus half-fertilizer N (NOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (PK) and control (CK). Organic C in soil and the soil heavy fraction (organo-mineral complex) was increased from 4.47 to 8.61 mg C g⁻¹ and from 3.32 to 5.68 mg C g⁻¹, respectively, after the 13 yr application of organic manure. In contrast, organic C and the soil heavy fraction increased in NPK soil to only 5.41 and 4.38 mg C g⁻¹, respectively. In the CK treatment, these parameters actually decreased from the initial C concentrations (4.47 and 3.32 mg C g⁻¹) to 3.77 and 3.11 mg C g⁻¹, respectively. Therefore, organic manure efficiently elevated soil organic C. However, only 66% of the increased soil organic C was combined with clay minerals in the OM treatment. Cumulative soil CO₂ emissions from inter-row soil in the OM and NPK treatments were 228 and 188 g C m⁻² during the 2002 maize growing season, 132 and 123 g C m⁻² during the 2002/2003 wheat growing season, and 401 and 346 g C m⁻² yr⁻¹ in 2002-2003, respectively. However, during the 2004 maize growing season, cumulative soil CO₂ emissions were as high as 617 and 556 g C m⁻², respectively, due to the contribution of rhizosphere respiration. The addition of organic manure contributed to a 16% increase in soil CO₂ emission in 2002-2003 (compared to NPK), where only 27%, 36% and 24% of applied organic C was released as CO₂ during the 2002 and 2004 maize growing seasons and in 2002-2003, respectively. During the 2002/2003 wheat growing season, soil CO₂ flux was significantly affected by soil temperature below 20 °C, but by soil moisture (WFPS) during the 2004 maize growing season at soil temperatures above 18 °C. Optimum soil WFPS for soil CO₂ flux was approximately 70%. When WFPS was below 50%, it no longer had a significant impact on soil CO₂ flux during the 2002 maize growing season. This study indicates the application of organic manure composted with wheat straw may be a preferred strategy for increasing soil organic C and sequestering C in soil.     

Changes in chemical and biological properties of a sodic clay subsoil with addition of organic amendments

An experiment was performed to examine the chemical and biological effects on high clay sodic subsoil following the incorporation and incubation with organic amendments. The main treatments consisted of amendments with wheat shoots, lucerne pellets and peat, and these were compared to gypsum addition. Additional treatments were residues of chickpea and canola, chicken manure and sawdust. All materials were finely ground and added to crushed and sieved soil at the rate of 1% by weight. Wheat, canola and chickpea residues and chicken manure resulted in modest reductions in soil sodicity. Carbon and N mineralization were related to the soluble C/total N ratio in the amendment. The initial mineralization of wheat amendment was rapid due to its soluble C content, but then slowed to have the lowest loss, of around one third of added C, of all the plant residues after 174 days. In comparison, lucerne-amended soil increased total N and lost almost half of its C after the 174-day incubation. The canola stubble amendment showed the highest carbon loss, losing 64% of its added C. The addition of gypsum resulted in high soil electrical conductivity which suppressed respiration, compared to the control soil, indicating a detrimental effect on microbial activity due to the high electrolyte concentration in the soil. The peat amendment, with a low-soluble C content, showed a similar respiration rate to the control soil, confirming that a source of soluble C is important for the initiation of rapid biological activity. Soil pH was significantly increased (by 0.6 of a pH unit) with addition of chicken manure, and still remained higher than control soil after 174 days of incubation. Lucerne was the only plant residue to increase soil pH, with the effect being sustained for 56 days. The study demonstrated how some organic amendments can improve chemical fertility and biological activity in high clay sodic subsoil, and at the same time contribute, after 25 weeks incubation, to an increase in carbon content.