控制sch单养雄蚕品种雌雄蚕孵出比例的催青处理因素研究

研究结果表明 :在RH 6 0 %状态下 ,控制性比的温度和下限时间负相关达到显著水平 ;控制性比的高温处理适于干燥状态下进行 ;处理后雌蚕孵化整齐度明显低于雄蚕孵化整齐度 ,雌雄蚕孵化整齐度均随处理温度的升高而下降 ,尤以雌蚕更为明显。由此提出了在RH 6 0 %状态下sch单养雄蚕品种控制性比的起点温度及温度、时间范围。认为高温催青用下限温度配合 1日收蚁法效果好 ,高温处理以后的胚胎适于在RH 80 %～ 85 %的湿度中保护     

黑豆豆芽工厂化生产关键技术研究

利用黑龙江黑豆、吉林黑豆、上海黑豆3个黑豆品种进行工厂化生产的最佳品种和孵化环境条件试验。结果表明，黑龙江黑豆最适合工厂化生产，其生产最佳孵化环境为：孵化车间采用淋水间隔3.5 h、温度控制在23~25℃、湿度保持在75%以上，发芽后84 h 采收最适宜。     

Reproductive biology,early ontogeny,and effect of temperature on development in wolffish: comparison with salmon

Peculiarities of reproduction, early ontogeny, methods of egg incubation, and influence of temperature on development are compared in wolffish (Anarhichas lupus L.) and in salmonids, mainly Atlantic salmon (Salmo salar L.). Reproductive indices of females are similar in both species, but differ in males due to the small production of sperm in wolffish, a difference explained by internal fertilization in the latter species. The rate of embryonal development until the beginning of differentiation of fin fold at the same temperature is similar in both species, but the period from activation to hatching is more than twice as long in wolffish as in Atlantic salmon. Wolffish hatch at a more advanced stage with a small remnant of yolk sac and begin to feed shortly thereafter. As in Atlantic salmon, eggs and larvae of wolffish have a wide range of temperature resistance except before and after hatching. Based on the difference of life cycles in wolffish and salmon, technologies for their artificial breeding are compared.     

固始鸡孵化期间蛋壳内钙鳞含量变化规律研究

对固始鸡种蛋孵化期间蛋壳中钙、磷含量进行了测定,结果表明:孵化期间蛋壳内钙、磷含量变化呈现不同规律。0～6胚龄,蛋壳中钙、磷变化均不明显;从12胚龄开始,钙含量突然降低,并以递增趋势持续至21胚龄;磷含量明显变化是从9胚龄开始,12胚龄达最大,随后逐渐降低,18～21胚龄保持不变,所以6～18胚龄是蛋壳中磷的主要转移期;同时,各胚龄阶段蛋壳中钙、磷比例也呈规律性变化。     

催青环境及分段收蚁对原蚕性别调控研究

试验结果表明 ,通过改变催青环境和分段收蚁可以人工调控家蚕的性别比例。在原种催青期中高温干燥处理 ,可使原蚕品种 872和鲁玉 蚕比例分别提高 1 3 %和 2 4% ,达极显著和显著水平 ;对原蚕 795和871品种分段收蚁 ,第 1天可提高♀性比例 1 0 %～ 2 0 % ,最后一天 (第 3天 )提高 蚕比例 ,795品种最高为2 8%～ 3 6% ,达极显著水平。     

A GC/MS method for the assessment of N and C incorporation into soil amino acid enantiomers

Identifying the transformation process of amino acid enantiomers was essential to probe into the fate, turnover and aging of soil nitrogen due to their important roles in the biogeochemical cycling. If this can be achieved by differentiating between the newly biosynthesized and the inherent compounds in soil, then the isotope tracer method can be considered most valid. We thereby developed a gas chromatography/mass spectrometry (GC/MS) method to trace the ¹⁵N or ¹³C isotope incorporation into soil amino acid enantiomers after being incubated with ¹⁵NH₄⁺ or U-¹³C-glucose substrates. The most significant fragments (F) as well as the related minor ions were monitored by the full scan mode and the isotope enrichment in amino acids was estimated by calculating the atom percentage excess (APE). ¹⁵NH₄⁺ incorporation was evaluated according to the relative abundance increase of m/z F+1 to F for neutral and acidic amino acids and F+2 to F (mass 439) for lysine. The assessment of ¹³C enrichment in soil amino acids was more complicated than that of ¹⁵N due to multi-carbon atoms in amino acid molecules. The abundance ratio increment of m/z F+n to F (n is the original skeleton carbon number in each fragment) indicated the direct conversion from the added glucose to amino acids, but the total isotope incorporation from the added ¹³C can only be calculated according to all target isotope fragments, i.e. the abundance ratio increment summation from m/z (Fa+1) through m/z (Fa+T) represented the total incorporation of the added ¹³C (Fa is the fragment containing all original skeleton carbons and T is the carbon number in the amino acid molecule). This method has a great advantage especially for the evaluation of high-abundance isotope enrichment in organic compounds compared with GC/C/IRMS. And in principle, this technique is also valid for amino acids besides enantiomers if stereoisomers are not concerned. Our assessment approach could shine a light on investigating the biochemical mechanism of microbial transformation of N and C in soils of terrestrial ecosystem.     

Carbon dynamics determined by natural C abundance in microcosm experiments with soils from long-term maize and rye monocultures

Understanding carbon dynamics in soil is the key to managing soil organic matter. Our objective was to quantify the carbon dynamics in microcosm experiments with soils from long-term rye and maize monocultures using natural ¹³C abundance. Microcosms with undisturbed soil columns from the surface soil (0-25 cm) and subsoil (25-50 cm) of plots cultivated with rye (C₃-plant) since 1878 and maize (C₄-plant) since 1961 with and without NPK fertilization from the long-term experiment ‘Ewiger Roggen’ in Halle, Germany, were incubated for 230 days at 8 °C and irrigated with 2 mm 10⁻² M CaCl₂ per day. Younger, C₄-derived and older, C₃-derived percentages of soil organic carbon (SOC), dissolved organic carbon (DOC), microbial biomass (C_mic) and CO₂ from heterothropic respiration were determined by natural ¹³C abundance. The percentage of maize-derived carbon was highest in CO₂ (42-79%), followed by C_mic (23-46%), DOC (5-30%) and SOC (5-14%) in the surface soils and subsoils of the maize plots. The percentage of maize-derived C was higher for the NPK plot than for the unfertilized plot and higher for the surface soils than for the subsoils. Specific production rates of DOC, CO₂-C and C_mic from the maize-derived SOC were 0.06-0.08% for DOC, 1.6-2.6% for CO₂-C and 1.9-2.7% for C_mic, respectively, and specific production rates from rye-derived SOC of the continuous maize plot were 0.03-0.05% for DOC, 0.1-0.2% for CO₂-C and 0.3-0.5% for C_mic. NPK fertilization did not affect the specific production rates. Strong correlations were found between C₄-derived C_mic and C₄-derived SOC, DOC and CO₂-C (r≥0.90), whereas the relationship between C₃-derived C_mic and C₃-derived SOC, DOC and CO₂-C was not as pronounced (r≤0.67). The results stress the different importance of former (older than 40 years) and recent (younger than 40 years) litter C inputs for the formation of different C pools in the soil.     

苹果黑星病潜育期及其病原菌产孢量研究

2002至2004年间,对苹果黑星病潜育期及其病原菌产孢量研究结果表明,苹果黑星病在嘎啦、富士、秦冠3个品种上的潜育期分别为11.1 d、13.2 d、15.7 d;温度对潜育期有很大影响,日平均温度为18℃时,最适宜发病;病菌在3个品种叶片上的产孢量存在显著差异,其产孢量分别为2.8263×104、7.4168×103和1.1465×103孢子/mm2。     

不同孵育时间对猪精子转染外源DNA效果的影响

建立稳定的精子载体法技术体系对家畜的转基因育种等研究具有重要意义.为获得公猪精子与DNA最佳共孵育时间,优化建立猪精子载体法技术体系,本研究通过定量PCR、荧光显微镜检测和精液常规分析方法等,研究分析猪精子与DNA不同共孵育时间对猪精子活力、活率、DNA转染率、吸附DNA和内化DNA量的影响.结果表明,多聚乙烯亚胺(polyethyleneimine,PEI)包裹的标记DNA与精子共孵育15、30、60和90 min后,随着孵育时间的延长,精子活力和活率有极显著下降(P＜0.01),而精子转染率呈极显著(P＜0.01)或显著(P＜0.05)上升,吸附外源DNA量和内化外源DNA量也呈上升趋势,但是30 min后不同孵育时间之间差异不显著(P＞0.05).此外,随着共孵育时间的延长,与精子转染率提高幅度相比,精子活力和活率的下降幅度更明显.综合考虑精子活力、活率、转染率、吸附DNA量和内化DNA量等参数,猪精子与外源DNA共孵育时间以30 min为最佳.     

Low reproductive success of leatherback turtles, Dermochelys coriacea, is due to high embryonic mortality

We examined the mechanism responsible for low reproductive success in leatherback turtles (Dermochelys coriacea) at Playa Grande, Costa Rica: low egg fertilization versus high rates of embryonic death. Leatherbacks at this beach had a high rate of fertility (=93.3%±2.5%, n=819). We incubated 10 eggs from every clutch encountered of 19 females during 3 months of the 1998-1999 nesting season. Fertility rate of some females decreased during the nesting season, but overall was high. Detection of fertility was difficult using standard methods because fertility rates cannot be determined accurately from nests excavated after hatching because of egg decomposition. Removal and incubation of eggs from nests provided a better estimate. Embryonic death, particularly in the beginning of incubation before embryos are visible to the unaided eye, was the cause of low hatching success in this population. Hatching success increased with increasing fertility and differed between females, with some mothers having 71-81% success and others 23-32%. Embryonic death and not low egg fertility drives poor recruitment at Playa Grande. Improved conservation of this species at Playa Grande will require a better understanding of the mechanism behind embryonic death.