Structural and dynamic studies of a non-self-complementary dodecamer DNA duplex.

A non-self-complementary dodecamer duplex d(CCTAAATTTGCC).d(GGCAAATTTAGG) has been investigated in solution by high resolution 1H NMR. Almost complete resonance assignment of both non-exchangeable and exchangeable protons, has been achieved. The duplex is essentially B-type, with distortions apparent at the AT and TA steps. These distortions and their affects on dynamics have been probed by the measurement of base-pair lifetimes, and observation of water of hydration. Base-pair opening rates were derived from measurements of T1's and effects on linewidths of the T and G imino protons on addition of an exchange catalyst. Our results are generally in line with observations reported for other systems, but we see only a slight drop in the A.T base-pair lifetime on moving out from the central region. This observation is reinforced by the detection of DNA-water nOe's for residues distributed throughout the dodecamer sequence.     

在中国壮族家系中发现的一例-α~T/-α~Q复合β~0β~0珠蛋白基因型

本文报道在我国广西隆林壮族中发现一个罕見的HbQ复合α,β地中海贫血家系。先证者女,18岁,贫血面容,肝脾肿大。化学结构分析确证本Hb变异体为HbQ Thailand[α74(EF3)Asp→His]。血红蛋白组成以及α和β珠蛋白基因分析结果表明,先证者的珠蛋白基因型为-α~Q/-α~T复合β°/β°(IVSI-1G→T/Codon17A→T);先证者父的基因型为-‘α~Q/-复合β~O/β~A(IVSI-1G→T/β~A);先证母的基因型为-α~T/αα复合β~O/β~A(Codon17A→T/β~A)。     

The detection and attribution of extreme reductions in vegetation growth across the global land surface

Negative extreme anomalies in vegetation growth (NEGs) usually indicate severely impaired ecosystem services. These NEGs can result from diverse natural and anthropogenic causes, especially climate extremes (CEs). However, the relationship between NEGs and many types of CEs remains largely unknown at regional and global scales. Here, with satellite-derived vegetation index data and supporting tree-ring chronologies, we identify periods of NEGs from 1981 to 2015 across the global land surface. We find 70% of these NEGs are attributable to five types of CEs and their combinations, with compound CEs generally more detrimental than individual ones. More importantly, we find that dominant CEs for NEGs vary by biome and region. Specifically, cold and/or wet extremes dominate NEGs in temperate mountains and high latitudes, whereas soil drought and related compound extremes are primarily responsible for NEGs in wet tropical, arid and semi-arid regions. Key characteristics (e.g., the frequency, intensity and duration of CEs, and the vulnerability of vegetation) that determine the dominance of CEs are also region- and biome-dependent. For example, in the wet tropics, dominant individual CEs have both higher intensity and longer duration than non-dominant ones. However, in the dry tropics and some temperate regions, a longer CE duration is more important than higher intensity. Our work provides the first global accounting of the attribution of NEGs to diverse climatic extremes. Our analysis has important implications for developing climate-specific disaster prevention and mitigation plans among different regions of the globe in a changing climate.     

Accelerated organic matter decomposition in thermokarst lakes upon carbon and phosphorus inputs

Mineralization of dissolved organic matter (DOM) in thermokarst lakes plays a non-negligible role in the permafrost carbon (C) cycle, but remains poorly understood due to its complex interactions with external C and nutrient inputs (i.e., aquatic priming and nutrient effects). Based on large-scale lake sampling and laboratory incubations, in combination with ¹³C-stable-isotope labeling, optical spectroscopy, and high-throughput sequencing, we examined large-scale patterns and dominant drivers of priming and nutrient effects of DOM biodegradation across 30 thermokarst lakes along a 1100-km transect on the Tibetan Plateau. We observed that labile C and phosphorus (P) rather than nitrogen (N) inputs stimulated DOM biodegradation, with the priming and P effects being 172% and 451% over unamended control, respectively. We also detected significant interactive effects of labile C and nutrient supply on DOM biodegradation, with the combined labile C and nutrient additions inducing stronger microbial mineralization than C or nutrient treatment alone, illustrating that microbial activity in alpine thermokarst lakes is co-limited by both C and nutrients. We further found that the aquatic priming was mainly driven by DOM quality, with the priming intensity increasing with DOM recalcitrance, reflecting the limitation of external C as energy sources for microbial activity. Greater priming intensity was also associated with higher community-level ribosomal RNA gene operon (rrn) copy number and bacterial diversity as well as increased background soluble reactive P concentration. In contrast, the P effect decreased with DOM recalcitrance as well as with background soluble reactive P and ammonium concentrations, revealing the declining importance of P availability in mediating DOM biodegradation with enhanced C limitation but reduced nutrient limitation. Overall, the stimulation of external C and P inputs on DOM biodegradation in thermokarst lakes would amplify C-climate feedback in this alpine permafrost region.     

赤子爱胜蚯蚓(Eisenia Foetida)纤溶酶的研究,Ⅳ纤溶酶组成成分的分子量测定

本文报告了用SephadexG—100柱层析法纯化样品和聚丙烯酰胺凝胶电泳测定纤溶酶组成成分的分子量的研究结果。经柱层析分离的纤溶酶电泳测定分子量结果为11条带,分别为68,000、49,000、42,000、41,000、36,000、29,000、27,000、26,000、25,000、21,000和12,000。而纤溶酶的主要组分集中在21.000与42.000之间,为其活性组分。     

广西、云南的PSEUDOSCHWAGERINA化石及其地层意义

该文记述了广西宜山马脑山剖面及云南八宝小独山剖面Pseudoschwaserina属34种(亚种),分析了两剖面Pseudoschwagerina动物群的面貌,讨论了Pseudoschwagerina的地层意义。研究表明,两剖面Pseudoschwagerina动物群具有地方性种稀少的共同特点,大多数种皆为广相型分子。从动物群的组成上看,广西、云南Pseudoschwagerina动物群与我国贵州、北美及俄罗斯等地的Pseudoschwagerina动物群有较大的相似性。但是,目前归入 Pseudoschwagerina名下的各种在形态上有着较大的差异,造成不同地区合Pseudoschwagerina地层带化石难以直接对比。根据对两剖面Pseudoschwagerina地层分布规律的研究以及国内、外Pseudochwagerina地理分布的资料,笔者建议选用 Pseudoschwagerina uddeni,P.beedei,P.robusta等 Pseudoschwagerina的典型分子做为含Pseudoschwagerina地层划分、对比的首要标准类群,选用P.uddeni和P.robusta分别做为确定Pseudoschwagerina带底、顶界线的首要标准种,以便于含Pseudoschwagerina地层的全球性的对比。     

Protein enrichment of sweet potato residue with co-culture of amylolytic fungi by solid-state fermentation

Protein enrichment of sweet potato residue with amylolytic moulds by solid-state fermentation was higher than that obtained with amylolytic yeasts. The optimum initial moisture content for protein enrichment was 66% to 75%. Incrementally added nitrogen sources to the culture at zero time and at 24 h considerably improved the final protein content. During the cultivation, the moisture, ash and ATP contents increased, while the pH value decreased. A 1:1 co-culture of amylolytic mycelial fungi yielded a product with 32.4% crude protein after 4 days incubation at 30 degrees C.     

Acid-Catalyzed nucleophilic substitution and racemization of 3-methoxy-N-desmethyldiazepam enantiomers in methanol

pK_a1 values of 3-methoxy-N-desmethyldiazepam in acetonitrile and methanol containing various acid concentrations were determined by spectrophotometry to be 3.5 and 1.3, respectively. Temperature-dependent racemization of enantiomeric 3-methoxy-N-desmethyldiazepam in methanol containing 0.5 M H₂SO₄ was studied by circular dichroism spectropolorimetry and the racemization reactions were found to follow apparent first-order kinetics. Thermodynamic parameters of the racemization reaction were found to be: E_act = 18.8 kcal/mol, and at 25°C: ΔH^? = 18.3 kcal/mol, ΔS^? = ?14.8 entropy unit, and ΔG^? = 22.7 kcal/mol, respectively. The racemization had an isotope effect (k_H/k_D) of 1.6 at 42°C. Based on the results of this report and those of earlier reports by other investigators, a nucleophilically solvated C3 carbocation intermediate resulting from either a P (plus) or an M (minus) conformation is proposed to be an intermediate and responsible for the stereoselective nucleophilic substitution and the subsequent racemization of 3-methoxy-N-desmethyldiazepam enantiomers. © 1993 Wiley-Liss, Inc.     

Sub-Cellular Distribution of Zinc in Different Vegetative Organs and Their Contribution to Grains Zinc Accumulation in Rice Under Different Nitrogen and Zinc Supply

Journal of Plant Growth Regulation - Zinc is an important micronutrient for the growth and development of human body and plants. Proper use of nitrogen fertilizer and foliar application of Zn have...