马齿苋中草酸钙晶体形态及积累特征

马齿苋(Portulaca oleracea L.)是营养价值较高的常用野生蔬菜,含有丰富的矿质元素,但目前人们对其钙养分的存在状态还缺乏认识,因此本研究对马齿苋茎和叶进行了显微观察,以了解马齿苋是否含有固定钙的草酸钙晶体以及晶体的积累特征。结果表明,马齿苋积累的草酸钙晶体,属于簇晶类型,直径为25~50μm;分布于茎的髓部和叶的叶肉组织中,叶中晶体多,每1 mm²叶片约含有287个晶体,而茎中含晶体少,每1 mm²茎横切面上只含有26多个晶体。叶中的草酸总含量、可溶性草酸和不溶性草酸含量均高于茎中,草酸分布模式与草酸钙晶体分布模式一致。显然,由于草酸钙晶体的积累,马齿苋中的钙相当一部分以难溶状态存在。     

Phosphorus fractions and dynamics as affected by land-use changes in the Central Mexican highlands

Land-use change from forest to agriculture in the volcanic ash-derived soils of Mexico has increased over recent decades. It is likely that land uses and management practices, particularly fertilizer use have affected phosphorus (P) distribution and availability. The objective of this study was to evaluate the effects of land-use types (native forest and maize mono-cropping), and the related P addition, on the forms and distribution of soil P and their isotopic exchangeability. An Andisol, sampled from a cropping site, along with the contiguous area under native forest was treated with ³²P-labelled potassium phosphate (KH₂³²PO₄). The soil samples were extracted after incubation times of 7, 21, 35 and 49 days. Phosphorus content and ³²P recovery in fractions sequentially extracted were assessed for each incubation time. Total soil P was dominated by inorganic fractions (79 to 86%) in both land-use types. Resin-Pi, bicarbonate extractable inorganic P (Bic-Pi) and sodium hydroxide extractable inorganic P (NaOH_0.1-Pi) were all raised with P addition. However, the proportion of organic P fraction was reduced under cropped soil. The recovery of ³²P in soils with P addition indicates that resin-Pi, Bic-Pi and NaOH_0.1-Pi comprised nearly all the exchangeable P. In native soils with no P addition, more than 19% of the ³²P was recovered in Bic-Po and NaOH_0.1-Po forms. This finding indicates that organic P cycling is crucial when soil Pi reserves are presented in an inadequate amount. Ecologically based management has to be designed for replenishment and succeeding maintenance of soil organic P compounds to increase sustainable agricultural production.     

Crop use and profile distribution of phosphorus in soils that developed on mafic rocks in southern Portugal

The phytoavailability of soil phosphorus (P) depends on the different forms in which it occurs and how these forms change after the application of P fertiliser to the soil. Forms of P in the A, B and C horizons of eleven pedons that developed on mafic rocks were characterised by a fractionation method before and after fertilisation with single superphosphate, and a micropot experiment was conducted to assess the short-term use of P fertiliser by rye (Secale cereale L.). The main sources of P to the crop were (i) phosphate adsorbed on mineral surfaces and pedogenic Fe, Al or Ca phosphates in the A horizon and (ii) Ca-phosphates in B and C horizons. In the C horizons, poor in Fe/Al phases and clay, the precipitated Ca-P showed low solubility, resulting in a reduction in shoot biomass. The apparent P recovery by rye was similar in the A (36%) and B (29%) but decreased in the C (15%) horizons. The partial factor productivity (g g^?1) decreased from the A (58) to B (11) and C (5) horizons. P phytoavailability decreased with increasing profile depth because the transformation of P fertiliser to poorly soluble Ca-P forms increased with depth.     

CYP2J3样基因在不同生长速率凡纳滨对虾中的差异表达

为了获得对虾生长差异的分子机制,通过比较不同生长速率凡纳滨对虾的转录组(速长组和慢长组),获得了一条编码P450的差异表达基因,经过cDNA全长验证后命名为LvCYP2J3-like,其开放阅读框为1 488 bp,编码495个aa,含有一个完整的P450功能域,功能分析表明,该基因可能参与了蜕皮激素的灭活。方差分析表明,LvCYP2J3-like在不同组织、发育阶段和蜕皮周期的表达量都存在显著性差异,并且速长群体的表达量显著性低于慢长群体。表明该基因参与了发育和蜕皮过程,其表达量与环境胁迫关系密切。在LvCYP2J3-like和其预测转录因子基因中分别发现了4和11个速长组和慢长组等位基因频率显著差异的单核苷酸多态性(SNP)标记,说明这些基因遗传差异与其活性和表达量相关,从而影响生长速率。研究结果为凡纳滨对虾遗传和育种研究提供了参考资料。     

Fish assemblage production estimates in Appalachian streams across a latitudinal and temperature gradient

Production of biomass is central to the ecology and sustainability of fish assemblages. The goal of this study was to empirically estimate and compare fish assemblage production, production‐to‐biomass (P/B) ratios and species composition for 25 second‐ to third‐order streams spanning the Appalachian Mountains (from Vermont to North Carolina) that vary in their temperature regimes. Fish assemblage production estimates ranged from 0.15 to 6.79 g m^?2 year^?1, and P/B ratios ranged from 0.20 to 1.07. There were no significant differences in mean assemblage production across northern cold‐water, southern cold‐water and southern cool‐water streams (p = .35). Two warm‐water streams, not included in these comparisons, had the highest mean production and biomass values. Mean assemblage P/B was significantly higher in northern cold‐water streams relative to southern cold‐water and cool‐water streams (p = .01). Species evenness in production declined with stream temperature and differed significantly across the lower latitude cold‐water, cool‐water and warm‐water streams and the higher latitude (i.e. more northern) cold‐water streams. Our fish assemblage production estimates and P/B ratios were both lower and higher compared to previously published estimates for similar stream habitats. This study provides empirical fish assemblage production estimates to inform future research on southern Appalachian streams and on the potential impacts of varying temperature regimes on cold‐water, cool‐water and warm‐water fish production in the coming decades as climate change continues to threaten fish assemblages.     

杨树PtRRI基因的组织特异性表达模式分析

[目的]模式植物在木本植物中鉴定的许多重要调控因子家族在木本植物中出现了基因家族成员扩张,但ARRs家族作为细胞分裂素响应调节因子在杨树基因组中成员数量反而减少,其在木本植物中如何行使功能需要进一步研究。[方法]本研究通过生物信息学构建PtRRI启动子与GUS融合表达载体,检测植物激素处理后PtRRI表达量和检测PPtRRI::GUS转基因植株在生根过程中GUS信号等方法,对杨树PtRRI基因的组织特异性表达模式进行分析。[结果]表明:PtRRI在杨树根部、形成层、木质部表达量相对较高,PtRRI转录受6-BA激素诱导,与其在不定根发育过程中激素调控下的表达相一致。[结论]PtRRI基因可能参与杨树的次级生长。     

Phosphorus desorption affected by drying and wetting cycles in Ferralsols and Luvisols of Brazilian Northeast

Semiarid soils are subjected to wetting and drying cycles which influence sorption and desorption of applied phosphorus fertilizer. Phosphorus desorption was determined in soils from toposequences of two soil groups (Ferralsol and Luvisol) from a semiarid area, subjected to wetting and drying cycles. Samples from surface and subsurface horizons of upslope, midslope, and downslope positions were incubated for 4 months with phosphorus doses corresponding to 0, 5, 10, 25, 50, 75, and 100% of the maximum adsorption capacity, under constant moisture (80% water retention capacity) or 12 cycles of wetting and drying. Phosphorus desorption was lower in the Ferralsol than in the Luvisol, and lower in the subsurface than in the surface horizons, probably due to greater clay, Fe, and Al oxides contents, but they were similar among slope positions, of same mineralogy. Desorption tended to be greater in samples submitted to wetting and drying cycles but differences were small. P recovery reached 40–50% in the Luvisol, and 30–40% in the Ferralsol. The relatively low P retention capacity suggests a high residual effect of the P applied. Therefore, in relation to P losses, water retention techniques are less important than those that prevent soil erosion.     

宁夏典型草原不同退耕年限草地植物-土壤生态化学计量特征

为了研究宁夏典型草原不同退耕年限草地优势植物及土壤C、N、P化学计量特征,本研究以宁夏南部典型草原区退耕草地为对象,分别对退耕0、1、3、5、6、8、11、15、20年草地优势植物及土壤碳、氮、磷等生态化学计量特征进行研究。结果表明,各植物全氮含量均表现为地上部分大于地下部分,且猪毛蒿整体全氮含量较其他植物高。全磷含量除赖草外也表现为地上部分大于地下部分。退耕1年狗尾草和退耕3年赖草有机碳含量表现为地下部分大于地上部分,其余各退耕年限地上部分大于地下部分。优势植物C∶N、C∶P、N∶P整体表现为退耕20年长芒草最大。赖草和猪毛蒿最小。退耕6年以上20年以内土壤有机碳含量由表层向深层逐层递减;全氮含量退耕0~6年呈波动式变化,退耕8年后全氮含量由表层向深层逐层递减;全磷含量变化趋势与全氮相同。研究区土壤C∶N变化范围为7.08~19.62,C∶P变化范围为6.60~35.25,N∶P变化范围为0.82~2.17。各层土壤C∶N平均值变化范围为11.18~15.03,C∶P平均值变化范围为14.09~24.55,N∶P平均值变化范围为1.06~1.98;除C∶N接近我国土壤C∶N均值外,研究区土壤C∶P和N∶P均低于我国土壤C∶P和N∶P均值。并且相应地表优势植物C∶N、C∶P、N∶P明显高于表层土壤。本研究中土壤C∶N与土壤有机碳之间相关性不显著,与全N呈负相关,意味着C∶N主要受N控制,而C∶P与有机碳呈显著正相关,与全P相关性不显著。土壤N∶P与土壤全N含量呈显著正相关,与土壤全P含量相关性不显著,说明主要受N控制,而土壤全N含量随退耕年限的增加呈波动式上升趋势。植物与土壤碳、氮、磷相关性显示:植物全N与土壤N之间相关性不显著(P0.05),植物全P与土壤全N、全P呈极显著的相关关系(P0.01),与土壤有机碳和N∶P呈显著的相关关系(P0.05)。