动脉粥样硬化斑块中脂肪沉积的扫频光热波成像

动脉粥样硬化和易损斑块破裂在全球范围内具有最高的死亡率,超过传染病和癌症导致的死亡率的总和。动脉粥样硬化斑块是由一层很薄的”纤维帽”和导致血栓形成的脂质核心构成。光热波成像是基于对被目标发色团（本文中指脂肪沉积）吸收的光信号强度进行周期调制,从而实现对目标发色团释放的热（红外）信号的调制。这里,我们利用光热波成像来检测来自兔子动脉硬化模型的粥样硬化斑块中脂肪沉积的三维分布。波长为1210纳米的激光被用来靶向检测脂肪。动脉粥样硬化斑块组织在0．1到5赫兹连续扫频的激光的激发下发出光热波,光热波传播到样品表面形成红外辐射温度并被红外相机以25．6帧／秒的速度接收并录制20秒。红外相机上的每一个像素（总共256~256像素）在进行时域傅里叶变换以后得到强度和相位的频域光热波图像。某一特定频率的强度和相位光热波图像对应着脂肪沉积在动脉粥样硬化斑块样品中的横向和纵向分布。对强度和相位光热波图像的分析指出：光热波成像能够用来检测脂肪在动脉粥样硬化斑块中的三维分布,并且脂肪的分布和动脉粥样硬化斑块的形状特征有着紧密联系。     

一平浪盐矿古老岩盐沉积中可培养细菌的系统发育多样性研究

运用纯培养法和基于16S rRNA基因序列的系统发育分析对云南省一平浪盐矿古老岩盐沉积中可培养细菌的多样性进行了研究。用补充0.5~3.5mol/L NaCl的MBA和ISP2琼脂培养基从卤水、岩盐和盐土样品中分离到38株细菌,用细菌通用引物进行16S rRNA基因扩增和序列测定,用相关软件进行序列相似性搜索、比对和系统发育分析。结果表明,38个分离菌株可分为31个物种,属于4个大的系统发育类群(Proteobacteria,Bacteroidetes,Firmicutes,Actinobacteria)、17个科、24个属。多数菌株属于Proteobacteria门(18株,47.3%;Gamma-Proteobacteria,31.5%;Alpha-Proteobacteria,15.8%)和Firmicutes门(13株,34.2%)。这些分离菌株中,至少有3个菌株可能代表3个不同属的3个新物种:Y3、Y15和Y25分别代表Idiomarina属、Salinicoccus属和Saccharospirillum属的新物种;而菌株Y21有可能代表Staphylococcaceae科的一个新属。从以上结果可以看出,一平浪盐矿古老岩盐沉积中存在较为丰富的微生物物种多样性和系统发育多样性,并且潜藏着新的微生物资源。     

细菌中群体感应调节系统

细菌根据特定信号分子的浓度可以监测周围环境中自身或其它细菌的数量变化,当信号达到一定的浓度阈值时,能启动菌体中相关基因的表达来适应环境中的变化,这一调控系统被称为细菌的群体感应调节系统(QuorumSensing系统)。本文系统介绍了细菌感知种内与种间数量的群体感应调节系统,并阐述了植物针对病原菌这一信号系统的抗病策略。     

Mesoproterozoic surface oxygenation accompanied major sedimentary manganese deposition at 1.4 and 1.1 Ga

Manganese (Mn) oxidation in marine environments requires oxygen (O₂) or other reactive oxygen species in the water column, and widespread Mn oxide deposition in ancient sedimentary rocks has long been used as a proxy for oxidation. The oxygenation of Earth's atmosphere and oceans across the Archean-Proterozoic boundary are associated with massive Mn deposits, whereas the interval from 1.8–1.0 Ga is generally believed to be a time of low atmospheric oxygen with an apparent hiatus in sedimentary Mn deposition. Here, we report geochemical and mineralogical analyses from 1.1 Ga manganiferous marine-shelf siltstones from the Bangemall Supergroup, Western Australia, which underlie recently discovered economically significant manganese deposits. Layers bearing Mn carbonate microspheres, comparable with major global Mn deposits, reveal that intense periods of sedimentary Mn deposition occurred in the late Mesoproterozoic. Iron geochemical data suggest anoxic-ferruginous seafloor conditions at the onset of Mn deposition, followed by oxic conditions in the water column as Mn deposition persisted and eventually ceased. These data imply there was spatially widespread surface oxygenation ~1.1 Ga with sufficiently oxic conditions in shelf environments to oxidize marine Mn(II). Comparable large stratiform Mn carbonate deposits also occur in ~1.4 Ga marine siltstones hosted in underlying sedimentary units. These deposits are greater or at least commensurate in scale (tonnage) to those that followed the major oxygenation transitions from the Neoproterozoic. Such a period of sedimentary manganogenesis is inconsistent with a model of persistently low O₂ throughout the entirety of the Mesoproterozoic and provides robust evidence for dynamic redox changes in the mid to late Mesoproterozoic.     

Reconstruction of sedimentary environments in Holocene coastal deposits of the southwest Netherlands; the Poortvliet boring,a case study of palaeoenvironmental diatom research

Diatoms are valuable indicators of palaeosedimentary environments in coastal wetlands. In this paper, the utilization of diatoms in coastal reconstructions will be demonstrated in a case study, the Poortvliet boring (southwest Netherlands). Diatoms supply valuable information about palaeosalinity gradients and palaeotide levels in addition to the existing geological data set, obtained from sediment cores.The ecological data of taxa are usually gathered from diatom studies in recent coastal environments. The study of the Poortvliet boring shows that information can also be obtained from the past (the past as key to the past) by comparing the trends of the relative abundances of species of which the ecology is well-known to those of which the ecology is unknown. It is argued both on recent and fossil data that Cymatosira belgica and Rhaphoneis minutissima have a tychoplanktonic life form.     

The binding of zinc in root cells of crop plants by phytic acid

Appreciable quantities of Zn are bound as Zn phytate (myo-inositol kis-hexaphosphate) within small vacuoles of cortical cells in the elongation zone of root tips of zinc tolerant Deschampsia caespitosa. These Zn/P-containing globular deposits have now been shown to occur in the roots of soybean, lucerne, lupins, tomato, rapeseed, cabbage, radish, wheat and maize. The globules are most frequent in the endodermis and pericycle but may also occur in the stele and inner cortex. The X-ray data again confirmed the presence of phytate with a relatively stable proportion of Zn and a species-dependent, variable, proportion of K, Mg and Ca to P.Analysis of soybean plants by atomic absorption spectroscopy showed that the Zn concentration in the shoots doubled in response to an increase in Zn supply from 1 to 100 M while the concentration of Zn in the root symplast was approximately 22 times greater than in the shoot, suggesting restricted transport to the shoot. It is suggested that the genetic expression of the capacity to bind heavy metals by means of phytate in endodermal cells may provide a strategy for keeping the above-ground content of heavy metals low. It may be possible to incorporate the trait into transformed roots that can be utilized for the treatment of industrial wastes.     

Palaeofloristic assemblages and palaeoecology of the Lower Oligocene Bembridge Marls, Hamstead Ledge, Isle of Wight

A sequence of nine, plant-macrofossil-bearing horizons has been recognized in the Lower Oligocene from the Isle of Wight, England. The plant fossils are contained in finely laminated, olive-brown to black silty-clays and clays. Some horizons exhibit rhythmic alternation of sediment couplets; others show evidence of bioturbation and rootlet penetration. These horizons are included within a sequence of finely laminated greenish grey silty-clays and clays, largely devoid of plant macrofossil material. The plant-bearing horizons contain abundant fruits, seeds, fern sporangia, Azolla megaspores, and rare leaves. The nearest living relatives of the fossils all inhabit an aquatic or marginal aquatic environment. The associated fossil fauna includes lake bottom and lake margin species. The palynoflora of the plant-bearing and immediately underlying horizons includes large numbers of planktonic algae and limited representatives of a forest vegetation. It shows a strong relationship between the occurrences of Sparganiaceaepollenites pollen and of Typha macrofossils. Palaeoecological interpretations of this plant-fossil-bearing sequence are discussed with particular reference to modern environments.
One new genus and three new species are described. Emendations are presented for four other species. Stratiotes leaf margin teeth are described.     

Automated analysis of uronic acids by high-performance liquid chromatography with photometric and fluorimetric postcolumn labelling using 2-cyanoacetamide

A convenient method for the rapid and sensitive automated analysis of uronic acids, based on high-performance anion-exchange chromatography on a Hitachi 2633 column and photometric as well as fluorimetric postcolumn labeling with 2-cyanoacetamide, has been developed. This method allows the simultaneous determination of 1-1000 nmol of D-mannuronic and D-galacturonic acids and 5-1000 nmol of L-iduronic and D-glucuronic acids in approx 70 min with high precision by photometric monitoring. In fluorimetric monitoring the linearity range was 1-1000 nmol for all these uronic acids, but reproducibility was rather low at the lowest limit of linearity. Application of this method to the analysis of component uronic acids in some polyuronides has suggested the inadequacy of generally accepted conditions for hydrolysis.     

Localization of Possible Calcium-Binding Sites in the Cilia of Paramecium caudatum

SYNOPSIS. Electron-dense deposits indicating possible Ca-binding sites were found at the ciliary base of Paramecium caudatum fixed in a glutaraldehyde solution containing 5 mM CaCl₂. The deposits appeared mainly at the inner surface of the ciliary membrane above the "ciliary necklace" region, although they could also occur in the space between the outer and the central microtubules. In some cases a ring of exactly 9 deposits was found in a ciliary cross section of a cilium.     

Prion protein with Y145STOP mutation induces mitochondria-mediated apoptosis and PrP-containing deposits in vitro

A pathogenic truncation of an amber mutation at codon 145 (Y145STOP) in Gerstmann-Straussler-Scheinker disease (GSS) was investigated through the real-time imaging in living cells, by utilizing GFP-PrP constructs. GFP-PrP(1-144) exhibited an aberrant localization to mitochondria in mouse neuroblastoma neuro2a (N2a) and HpL3-4 cells, a hippocampal cell line established from prnp gene-ablated mice, whereas full-length GFP-PrP did not. The aberrant mitochondrial localization was also confirmed by Western blot analysis. Since GFP-PrP(1-121), as previously reported, and full-length GFP-PrP do not exhibit such mitochondrial localization, the mitochondrial localization of GFP-PrP(1-144) requires not only PrP residues 121-144 (in human sequence) but also COOH-terminal truncation in the current experimental condition. Subsequently, the GFP-PrP(1-144) induced a change in the mitochondrial innermembrane potential (DeltaPsi(m)), release of cytochrome c from the intermembrane space into the cytosol, and DNA fragmentation in these cells. Non-fluorescent PrP(1-144) also induced the DNA fragmentation in N2a and HpL3-4 cells after the proteasomal inhibition. These data may provide clues as to the molecular mechanism of the neurotoxic property of Y145STOP mutation. Furthermore, immunoelectron microscopy revealed numerous electron-dense deposits in mitochondria clusters of GFP-PrP(1-144)-transfected N2a cells, whereas no deposit was detected in the cells transfected with full-length GFP-PrP. Co-localization of GFP/PrP-immunogold particles with porin-immunogold particles as a mitochondrial marker was observed in such electron-dense vesicular foci, resembling those found in autophagic vacuoles forming secondary lysosomes. Whether such electron-dense deposits may serve as a seed for the growth of amyloid plaques, a characteristic feature of GSS with Y145STOP, awaits further investigations.