The Unknown Vygotsky: On the Experience of a Literary Translation from Hebrew

Following is the first publication of a previously unknown translation by L.S. Vygotsky from Hebrew of a fictional short story by M.J. Berdyczewski, a Jewish writer popular at the beginning of the twentieth century. The commentary by the authors of this article reconstructs the context of Vygotsky’s life situation during the prerevolutionary period. Particular attention is focused on the questions of ethnic and cultural self-determination that were confronting him. The cultural contexts essential for an understanding and interpretation of the artistic and world-view features of the text of the short story are explored. A comparison is drawn to show the connection between the themes addressed in the story and the substantive problems that Vygotsky would subsequently deal with as a professional psychology: the artistic inner experience, moral choice, and cultural mediation.     

基于CSSLs群体定位和图位克隆水稻长芒基因GAD1-2

水稻是世界上最早驯化的重要粮食作物之一。水稻芒可以保护水稻种子不被鸟琢食,是水稻重要的驯化性状之一。芒在野生稻中普遍存在,对野生稻的生存和传播至关重要,然而在驯化和人工选择过程中该性状逐渐被淘汰。定位和克隆水稻长芒相关基因是研究水稻芒驯化遗传机制的基础。本研究以籼稻恢复系东南恢810为受体、漳浦野生稻为供体构建的146个染色体片段置换系(chromosome segment substitution lines, CSSLs)为研究材料,调查了146个CSSLs株系和双亲的芒长,结果表明在4个置换系中检测到1个控制水稻芒长主效基因GAD1-2,位于水稻第8号染色体;利用重叠代换作图法,将GAD1-2定位在Ind8-10和RM4936标记之间,遗传距离约为4.75 Mb。选择分离群体中的显性单株,利用开发的标记,最终将GAD1-2 基因定位在两个 Indel 标记之间,两者间的物理距离约为27 kb,该区域内只有两个候选基因Os08g0485500和Os08g0485400。经测序和分析表明,Os08g0485500是GAD1-2的候选基因,GAD1-2在保守的ORF区域存在6个碱基缺失,导致丝氨酸和半胱氨酸这两个氨基酸缺失,从而表现长芒的性状;在Os08g0485500基因位点已克隆了1个控制水稻芒长的GAD1基因,推测GAD1-2与GAD1为等位基因。本研究为进一步理解水稻起源演化和水稻芒长发育基因的遗传机制奠定了基础。     

Enhanced plasminogen activation by staphylokinase in the presence of streptokinase beta/betagamma domains: plasminogen kringles play a role

Presence of isolated beta or betagamma domains of streptokinase (SK) increased the catalytic activity of staphylokinase (SAK)-plasmin (Pm) complex up to 60%. In contrast, fusion of SK beta or betagamma domains with the C-terminal end of SAK drastically reduced the catalytic activity of the activator complex. The enhancement effect mediated by beta or betagamma domain on Pg activator activity of SAK-Pm complex was reduced greatly (45%) in the presence of isolated kringles of Pg, whereas, kringles did not change cofactor activity of SAK fusion proteins (carrying beta or betagamma domains) significantly. When catalytic activity of SAK-microPm (catalytic domain of Pm lacking kringle domains) complex was examined in the presence of isolated beta and betagamma domains, no enhancement effect on Pg activation was observed, whereas, enzyme complex formed between microplasmin and SAK fusion proteins (SAKbeta and SAKbetagamma) displayed 50-70% reduction in their catalytic activity. The present study, thus, suggests that the exogenously present beta and betagamma interact with Pg/Pm via kringle domains and elevate catalytic activity of SAK-Pm activator complex resulting in enhanced substrate Pg activation. Fusion of beta or betagamma domains with SAK might alter these intermolecular interactions resulting in attenuated functional activity of SAK.     

CHARGE CONTRAST IMAGING OF EXCEPTIONALLY-PRESERVED FOSSILS

Abstract:  Charge contrast images are a variant of secondary electron images acquired by operating a variable pressure scanning electron microscope in low vacuum mode; i.e. a gas is present in the specimen chamber. Spatial variation in the amount of charge that accumulates on the surface of the specimen is expressed as differences in greyscale tone; areas that are charging less are darker in tone. The precise mechanisms by which charge contrast images are generated are not known fully. Various different properties of a mineral may create a charge contrast; electrical conductivity is known to be one potentially important variable. As carbon is highly conductive but typical host lithologies (carbonates, silicates) less so or dielectric, the technique is potentially very suitable for imaging organically preserved fossils such as those from the Solite and Jehol biotas. It can also be applied to Burgess Shale fossils: complex films comprising 'aluminosilicates' with or without carbonaceous remains. Charge contrast images reveal anatomical detail not visible using either optical or other scanning electron microscope-based imaging methods.     

Enhancement of YD spin relaxation by the CaMn4 cluster in photosystem II detected at room temperature: A new probe for the S-cycle

The long-lived, light-induced radical Y_D^• of the Tyr161 residue in the D2 protein of Photosystem II (PSII) is known to magnetically interact with the CaMn₄ cluster, situated ∼ 30 Å away. In this study we report a transient step-change increase in Y_D^• EPR intensity upon the application of a single laser flash to S₁ state-synchronised PSII-enriched membranes from spinach. This transient effect was observed at room temperature and high applied microwave power (100 mW) in samples containing PpBQ, as well as those containing DCMU. The subsequent decay lifetimes were found to differ depending on the additive used. We propose that this flash-induced signal increase was caused by enhanced spin relaxation of Y_D^• by the OEC in the S₂ state, as a consequence of the single laser flash turnover. The post-flash decay reflected S₂ → S₁ back-turnover, as confirmed by their correlations with independent measurements of S₂ multiline EPR signal and flash-induced variable fluorescence decay kinetics under corresponding experimental conditions. This flash-induced effect opens up the possibility to study the kinetic behaviour of S-state transitions at room temperature using Y_D^• as a probe.     

The role of modern and fossil cyanobacterial borings in bioerosion and bathymetry

Measurements on modern coral reefs at Lee Stocking Island (Bahamas) illustrate that boring cyanobacteria species make a major contribution to microboring bioerosion rates. Borings attributed to cyanobacteria also occur in fossil environments. Bioerosional studies on Permian and Triassic reefs show similar intensities to those observed on modern equivalents. The importance of borings assigned to cyanobacterial activity is even more apparent in paleobathymetry. Comparison of the bathymétrie ranges known from modern and fossil microborings demonstrates a preference of boring cyanobacteria for shallow marine environments. Furthermore, some traces are linked to distinct portions of the shallow euphotic zone. They significantly contribute to characterize typical microboring assemblages, which are used for paleodepth reconstructions. In contrast to these stenobathic species, one cyanobacterial species turned out to be eurybathic. It has been recorded as deep as the dysphotic zone but may even extend to the aphotic zone.     

New and poorly known Cenozoic clown beetle compressions from France (Insecta: Coleoptera: Histeridae)

Summary

Two French fossil Histeridae are described or revised, viz. Hister cerestensis n. sp. from the Oligocene of Céreste (Lubéron) and Plegaderus pitoni (Theobald, 1935), n. comb. from the Pliocene of Chambon Lake (Puy-de-Dôme). Morphometric data are used to compare fossil and extant taxa, with multivariate statistics. A list of the fossil Histeridae is given.     

The latitudinal position of peak marine diversity in living and fossil biotas

Aim Peak marine taxonomic diversity has only rarely occurred at or near the equator during the Phanerozoic Eon, in contrast to the present‐day pattern. This fundamental difference is difficult to reconcile because the latitude at which peak diversity occurs for living marine taxa has not yet been explicitly determined at a broad taxonomic and spatial scale. Here, we attempt to determine this value in order to compare the contemporary and fossil patterns directly. Location Our data are global in coverage. Methods We used a literature compilation of 149 present‐day marine latitudinal diversity gradients. We summed the number of marine taxa that exhibited peak diversity within 10° latitudinal bins. In addition, we recorded locality data, general habitat (benthic/pelagic), and the taxonomic level of the study organisms. Results We found that peak diversity for most sampled marine taxa currently occurs between 10° and 20° N, even after correcting for a Northern Hemisphere sampling bias. Moreover, this peak position is a global phenomenon: it is found across habitats and higher taxa, within all sampled ocean basins, and on both sides of the Atlantic and Pacific oceans. Benthic taxa, which dominate our data, exhibit one peak at 10°–20° N, while pelagic taxa exhibit a peak at 10°–20° N and an additional peak at 10°–20° S, producing a distinct trough at the equator. Main conclusions Our data indicate that peak marine diversity for many taxa is currently within 10°–20° N rather than at the equator, and that this is not likely to result from either undersampling at lower latitudes or the pattern being dominated by a particular taxon. Possible explanations may include a coincidence with the intertropical convergence zone, a mid‐domain effect, abundant shallow marine habitat, or high ocean temperatures at latitudes nearest the equator. Regardless of its exact cause, the position of peak diversity should be considered a fundamental feature of the latitudinal diversity gradient that must be accounted for within attempts to explain the latter’s existence.     

Estimating changes in mean population age using the death distributions of live‐captured medflies

1. A simple, low‐cost approach to estimating population ageing was introduced based on a modified version of the captive cohort method – a technique developed earlier (Carey et al., Aging Cell, 7 , 426–437, 2008) in which information on the remaining lifespans of live‐captured medflies of unknown age is used to estimate the overall population age structure. 2. To test this approach approximately 1200 medflies near Volos, Greece were live captured from daily sampling over a 3‐month field season. 3. This simplified method reported: (i) an extraordinary post‐capture longevity of wild medflies in early season (>200 days in longest lived); (ii) a decrease of 50–75 days in the mean longevity from early‐season to late‐season flies; (iii) seasonality of frailty as indicated by the shorter‐lived flies in late autumn; (iv) cessation of fly emergence in late season as indicated by the absence of long‐lived individuals (indicating newly emerged at capture) sampled in the autumn; and (v) increase in mean age from about 20 days in early season to approximately 60 days in late season. 4. The applications of this simplified captive cohort method are discussed, including its use in the analysis of insect vector populations, Drosophila ecology and ageing in the wild, demographic toxicology, and age bias in sampling.     

早熟金柚果皮挥发油的提取及GC-MS分析

采用水蒸气蒸馏法提取早熟金柚果皮挥发油,通过正交实验优选获得早熟金柚果皮挥发油提取的工艺参数,结果表明：早熟金柚果皮挥发油的最佳提取工艺是将柚皮粉碎60 s,加水5倍,提取6 h。采用GC-MS联用技术对早熟金柚果皮挥发油的化学成分进行分离鉴定,共分离出44个峰,鉴定出了其中的25种化合物,占峰面积的98.43%。用面积归一化法测定了各个组分的相对百分含量,其主要成分有柠檬烯（65.82%）、β-月桂烯（25.52%）、4-侧柏烯（1.78%）、紫苏烯（0.44%）、氧化芳樟醇（0.42%）。