Presence of pH2-sensitive circulating interferon among Callithrix jacchus marmosets

Significant and relatively stable levels of serum-interferon were demonstrated in a Callithrix jacchus population. This circulating interferon was acid-sensitive in all cases, classifying it as immune or "gamma-type" interferon. Our results in these hematopoietic chimeras suggest that the presence of immune-type or at least pH 2-sensitive interferon could be related to the presence of two allogenic lymphocyte populations in each marmoset.     

Social implications of gummivory in marmosets

Gummivory or exudate feeding is a major dietary specialization which has received relatively little attention in the literature. While plant exudates contribute to the diet of many primate species, we suggest that the callitrichid species Cebuella pygmaea and Callithrix jacchus are obligate exudate feeders under free-ranging conditions. Callithrix jacchus provides an excellent model for examining the effects of exudate feeding and foraging upon social behavior, since other callitrichid species of similar body size do not share this dietary specialization. We review the effects of exudate foraging on specific social behaviors observed both in field and laboratory populations of C. jacchus. By comparing this species to closely related species, exudate foraging is seen to (1) be retained under laboratory conditions, (2) increase the frequency of territorial marking behavior while decreasing the frequency of overt aggression in males, (3) decrease the duration of infant care, and (4) increase the number of nonadults in social groups but not affect group size. The evidence presented supports the hypothesis that the consequences of exudate foraging in C. jacchus are fundamental and socially complex. © 1994 Wiley-Liss, Inc.     

A comparison of craniofacial growth between two colonies of marmosets (Callithrix jacchus)

General and craniofacial measurements from young marmosets in a recently established Australian colony are presented and compared with similar data published for a long-established colony in the United Kingdom. Statistically significant differences between the colonies were those associated with large error variances, suggesting difficulties in locating certain landmarks rather than real differences in growth. Thus, direct comparison can be made between craniofacial growth studies conducted at these two different marmoset colonies.     

Family composition and the characteristics of parental care during the nursing phase of captive common marmosets (Callithrix jacchus)

Cooperative care of the young by the father, older siblings, and unrelated group members is observed in a number of species, but inCallithrix jacchus parental care by the father is considered to be part of the reproductive behavior of the species. Nevertheless, the way the presence of potential helpers influences the costs of caring for the parents is not well understood. In this study we describe the suckling phase of youngC. jacchus, in families with and without older siblings, assessing the effect of siblings on the amount of care given by the father and mother. Six family groups were observed: three consisting of the mated pair and two newborn infants, and three with one or two additional sub-adult siblings. Our results suggest that the presence of older siblings as helpers affects the parents' participation in caregiving by altering maternal investment through the control of nursing and by reducing the costs of carrying for the father.     

Allometry,merism, and tooth shape of the upper deciduous M2 and permanent M1

The aims of this study were to investigate the effect of allometry on the shape of dm² and M¹ crown outlines and to examine whether the trajectory and magnitude of scaling are shared between species. The sample included 160 recent Homo sapiens, 28 Upper Paleolithic H. sapiens, 10 early H. sapiens, and 33 H. neanderthalensis (Neandertal) individuals. Of these, 97 were dm²/M¹ pairs from the same individuals. A two‐block partial least squares analysis of paired individuals revealed a significant correlation in crown shape between dm² and M¹. A principal component analysis confirmed that Neandertal and H. sapiens dm² and M¹ shapes differ significantly and that this difference is primarily related to hypocone size and projection. Allometry accounted for a small but significant proportion of the total morphological variance. We found the magnitude of the allometric effect to be significantly stronger in Neandertals than in H. sapiens. Procrustes distances were significantly different between the two tooth classes in Neandertals, but not among H. sapiens groups. Nevertheless, we could not reject the null hypothesis that the two species share the same allometric trajectory. Although size clearly contributes to the unique shape of the Neandertal dm² and M¹, the largest H. sapiens teeth do not exhibit the most Neandertal‐like morphology. Hence, additional factors must contribute to the differences in dm² and M¹ crown shape between these two species. We suggest an investigation of the role of timing and rate of development on the shapes of the dm² and M¹ may provide further answers. Am J Phys Anthropol 154:104–114, 2014. © 2014 Wiley Periodicals, Inc.     

现代中国人群形成与分化的形态证据——亚洲与非洲现代人群上颌第一臼齿齿尖相对面积的对比分析

现代人群形成与分化造成的具有地域差别的人群标志性体质特征是研究人群之间关系的重要信息。作为臼齿形态测量的组成部分,上颌第一臼齿齿尖相对面积在人类演化以及现代人群关系上的研究价值已经引起了人类学界的关注。然而,迄今对上颌第一臼齿齿尖相对面积在世界各地的现代人群之间是否具有地域性差异还不是很清楚。本文对代表亚洲和非洲现代人群的208枚上颌第一臼齿齿尖相对面积的研究发现,上颌第一臼齿四个主要齿尖相对面积在亚洲和非洲现代人群之间都存在明显差异。亚洲现代人上颌第一臼齿近中齿尖(原尖和前尖)相对面积较大,而远中齿尖(后尖和次尖)相对面积较小。非洲现代人上颌第一臼齿各齿尖相对面积均较亚洲人群具有更大的变异,尤其在原尖和次尖相对面积上。采用判别分析可以将69.2%的标本正确地判别归入其原来所属的组群。通过与化石人类相关数据的对比发现,非洲现代人比亚洲现代人在原尖和次尖相对面积以及前尖/后尖相对面积比例上更加接近于人类演化的早期形式。现有的证据显示,亚洲和非洲现代人群在齿尖相对面积的分化至少可以追溯到全新世早期,更加精确的分化时间需要结合更新世晚期甚至中期化石人类数据去获得。本研究揭示出的非洲现代人上颌第一臼齿齿尖相对面积的高异质性(heterogeneity)和相对原始性在现代人形成与分化方面的作用尚需进一步的研究。     

Muscle architecture of the upper limb in the orangutan

We dissected the left upper limb of a female orangutan and systematically recorded muscle mass, fascicle length, and physiological cross-sectional area (PCSA), in order to quantitatively clarify the unique muscle architecture of the upper limb of the orangutan. Comparisons of the musculature of the dissected orangutan with corresponding published chimpanzee data demonstrated that in the orangutan, the elbow flexors, notably M. brachioradialis, tend to exhibit greater PCSAs. Moreover, the digital II-V flexors in the forearm, such as M. flexor digitorum superficialis and M. flexor digitorum profundus, tend to have smaller PCSA as a result of their relatively longer fascicles. Thus, in the orangutan, the elbow flexors demonstrate a higher potential for force production, whereas the forearm muscles allow a greater range of wrist joint mobility. The differences in the force-generating capacity in the upper limb muscles of the two species might reflect functional specialization of muscle architecture in the upper limb of the orangutan for living in arboreal environments.     

Microbiological and Geochemical Characterization of Microbial Fe(III) Reduction in Salt Marsh Sediments

Population densities of anaerobic Fe(III)-reducing bacteria (FeRB) and aerobic heterotrophs were inversely correlated in the surficial (0-2 cm) layers of Sapelo Island, Georgia, salt marsh sediments. In surficial sediments where densities of aerobic heterotrophs were low, the density of culturable FeRB correlated positively with the concentration of amorphous Fe(III) oxyhydroxides extractable by ascorbate. High FeRB densities and a decrease with depth of ascorbate-extractable Fe(III) were observed in the upper 6 cm of a tidal creek core. Culturable sulfate-reducing bacteria (SRB) and SRB-targeted rRNA signals were also detected in the upper 6-cm depth. The disappearance of FeRB below 6 cm, however, coincided with a large increase in the abundance of SRB. Thus, when FeRB are not limited by the availability of readily reducible amorphous Fe(III) oxyhydroxides, FeRB may outcompete SRB for growth substrates. Shewanella putrefaciens- and Geobacteraceae-targeted rRNA signals were at or below detection limits in all sediment samples, indicating that these FeRB are not predominant members of the active FeRB populations. The ubiquitous presence of FeRB at the sites studied challenges the traditional view that dissimilatory Fe(III) reduction is not an important pathway of organic carbon oxidation in salt marsh sediments.     

微生物还原Cr(VI)的研究进展

随着现代工业的发展, 水环境中的重金属对人类健康和环境带来严重的危害, 其中的Cr(VI)具有强烈的毒性。微生物在代谢过程中可以将Cr(VI)还原为Cr(III), 有效降低Cr(VI)的毒性。本文从可还原Cr(VI)的微生物、微生物还原Cr(VI)的机理、还原过程中存在的问题及发展方向等方面进行了综述。     

微生物还原Cr(VI)的研究进展

随着现代工业的发展,水环境中的重金属对人类健康和环境带来严重的危害,其中的Cr(VI)具有强烈的毒性.微生物在代谢过程中可以将Cr(VI)还原为Cr(Ⅲ),有效降低Cr(VI)的毒性.本文从可还原Cr(VI)的微生物、微生物还原Cr(VI)的机理、还原过程中存在的问题及发展方向等方面进行了综述.     

Climate and vegetation in China V. Effect of climatic factors on the upper limit of distribution of evergreen broadleaf forest

In order to clarify correlations between the upper limit of distribution of evergreen broadleaf forest and climatic factors, 62 stands distributed at the upper limit of the forest were collected from various parts of China, and their thermal and precipitation factors were estimated. Among six thermal climatic indices, i.e., warmth index (WI), coldness index (CI) and annual mean (AMT), January mean (JMT), mean minimum (MMT) and minimum (MT) temperatures, the CI at the stands showed the smallest range of variance, and it was therefore considered to be the most significant for interpreting the upward distribution of the forest. However, the distribution of the forest in mountain areas in southwestern China could not be explained by lower temperatures in winter such as CI but by a cumulative temperature such as WI. The continentality and precipitation factors were also important for delimiting the distribution of the forest. In addition, the relation between the distribution of the forest and the MMT was noted, and it was concluded that the MMT was an effective thermal index for explaining the upper limit of distribution of evergreen broadleaf forest in China.     

Stereochemical Control in Microbial Reduction. Part 10. Asymmetric Reduction of Alkyl 3-Methyl-2-Oxobutanoate with Immobilized Bakers' Yeast in Hexane

Esters of 3-methyl-2-oxobutanoic acid are reduced with bakers' yeast by three methods: free bakers' yeast in water, immobilized bakers' yeast in water, and immobilized bakers' yeast in hexane. Although (R)-hydroxy esters are obtained in all cases, the enantiomeric excess varies from 3% (reduction of the methyl ester with free bakers' yeast in water) to 93% (reduction of the butyl ester with immobilized bakers' yeast in hexane) depending on the structure of substrate and on the reaction conditions. The mechanism of the present stereochemical control is discussed.     

干旱指标研究进展

干旱作为全球最为常见的自然灾害之一,已经对我国的农业生产造成了严重影响。为更好地预测影响作物的干旱并及时采取应对措施,综述了国内外广泛应用的各类干旱指标,包括气象指标、土壤墒情指标、作物生理生态指标及其它综合监测指标等,评述了各类干旱指标的优缺点以及在农业上的适用性,探讨了未来以作物干旱为核心的干旱指标研究拟重视的方面,以为减缓和预防干旱对农业的不良影响及制订科学的政策提供依据。     

The Influence of Carbon Source on the Products of Dissimilatory Iron Reduction

We have examined the influence of carbon source on both the rate of iron reduction and the mineralogy of the reduction products with Shewanella putrefaciens strain W3-18-1. When pyruvate was the carbon source, the secondary products were spherules composed of siderite. When uridine was used as the carbon source, the products were hexagonal plate-like structures identified as iron carbonate hydroxide hydrate, also known as carbonate green rust, a precursor to fougerite. When lactate was used as the carbon source, products were a mixture of iron carbonate hydroxide and magnetite. In terms of reaction stoichiometry, there were differences in the amount of acetate produced depending on the starting organic carbon source. Incubation with pyruvate produced a relatively large amount of acetate compared to incubation with uridine and lactate. There were also differences in the final pH of the cultures. While the pH for incubations with lactate started at 8.6 and ended between 8.0–8.3, the pH of cultures incubated with uridine was found to be almost a full unit lower at the conclusion of the experiment (～7.4). Solubility diagrams based on the chemistry found in our experiments predict that the production of Fe²⁺ _(aq) should always lead to the formation of magnetite. However, strain W3-18-1 produced different minerals depending on the carbon source utilized as the electron acceptor.     

Reduction of N2 by Fe2+ via Homogeneous and Heterogeneous Reactions

Because of their high kinetic barrier and thermodynamic favorability under moderately reducing atmospheric composition photochemical approaches appear to be ideally suited to the direct reduction of solvated nitrogen gas. Ferrous iron has been investigated as an electron donor, as it has a highly tunable redox character and is environmentally ubiquitous. Recent advances in mineralogy connected to the field of environmental remediation have led to the identification of an important class of rusts which have reductive potentials comparable to Fe(0). These materials possess redox couples that are, potentially, capable of overcoming the kinetic barrier to the production of NH₃. In this study, we attempted to produce ammonia from N₂ by oxidizing white rust both photochemically and in a dark reaction. All results indicated the reaction was inhibited by competing reactions; primarily the reduction of H₂O to H₂. However, the dark reactions showed limited potential for reduction up to 1.4 mM. As a result, we turned to the question of closure temperature; the minimum temperature of rapid reaction based on a choice of reductant, which we demonstrate a model for its estimation. Due to the high thermodynamic energy of the intermediate, we conclude that aqueous photochemical reduction under the conditions studied here is an unlikely prebiotic source for reactive, i.e. reduced, nitrogen.     

Electrochemical behavior of S,S-bridged adducts of square planar metalladithiolene complexes [M(S2C2Ph2)2](M=Ni, Pd, and Pt)

The electrochemical behavior of the S,S^′-bridged adducts of square planar metalladithiolene complexes was investigated by using cyclic voltammetry and electrochemical spectroscopies (visible, near-IR, and ESR). The norbornene-bridged S,S^′-adduct [Ni(S₂C₂Ph₂)₂(C₇H₈)] (2a; C₇H₈=norbornene) formed by [Ni(S₂C₂Ph₂)₂] (1a) and quadricyclane (Q) was dissociated by an electrochemical reduction, and anion 1a⁻ and norbornadiene (NBD) were formed. Q was isomerized to NBD in the overall reaction. The o-xylyl-bridged S,S^′-adduct [Ni(S₂C₂Ph₂)₂(CH₂)₂(C₆H₄)] (3a; (CH₂)₂(C₆H₄)=o-xylyl) was also dissociated by an electrochemical reduction, and this reaction gave the o-xylyl radical (o-quinodimethane). The reduction of complex 3a in the presence of excess o-xylylene dibromide underwent the catalytic formation of o-quinodimethane. The butylene-bridged S,S^′-adduct [Ni(S₂C₂Ph₂)₂(CH₂)₄] (4a; (CH₂)₄=butylene) was stable on an electrochemical reduction. The lifetimes of reduced species of these adducts 2a-4a were influenced by the stability of the eliminated group (stability: NBD > o-xylyl radical (o-quinodimethane) > butylene radical). Therefore, the reduced species are stable in the sequence 4a⁻ > 3a⁻ > 2a⁻. Although the palladium complex [Pd(S₂C₂Ph₂)₂] (1b) was easier to reduce than the nickel complex 1a or the platinum complex [Pt(S₂C₂Ph₂)₂] (1c), their S,S^′-adducts were easier to reduce in the order of Ni adduct > Pd adduct > Pt adduct.     

广东西樵山细石叶石核的开发策略

长期以来,细石叶技术的发展和传播是更新世末期到全新世初期文化传播、人群迁徙和生态适应研究领域探讨的重要课题。20世纪50年代,发现于广东西樵山石器制造场的大批细石叶技术产品,突破了传统意义上对细石叶技术流行、传播范围的认识。早期研究中不少学者就西樵山细石叶制品的形态特征、分布情况进行了介绍,随后鲜见后续研究,缺乏对技术内涵、石核开发策略的深入解析,亦未开展对其所指示的文化传播与人口迁徙问题的探讨。本文选取收藏于中山大学人类学博物馆的343件细石叶石核,通过对石料、毛坯类型、台面类型和数量、剥片面等多方位观察以及对相关技术数值的测量统计,建构西樵山细石叶石核开发策略的模式。这项工作总结了西樵山细石叶技术的特点,并与其他区域的细石叶技术进行对比,加深了对出现在亚热带地区的细石叶技术的认识,为尝试进一步讨论其可能的技术源流和指示人口迁徙与文化传播提供了基础。     

Metric dental change in the European upper paleolithic and mesolithic.

Evolutionary trends for dental reduction are presented for European Upper Paleolithic and Mesolithic samples. The analysis demonstrates that the greatest decrease in tooth size occurs between the two divisions of the Upper Paleolithic, while little and insignificant change characterizes the Late Upper Paleolithic/Mesolithic transition. Trends for tooth size over this period indicate that (1) human evolution does not stop with the appearance of "anatomically modern Homo sapiens," (2) changes in tooth size fluctuate with increases in the efficiency and complexity of cultural systems, and (3) the Early Upper Paleolithic sample should be considered transitional between Wurm II European Neanderthals and later Upper Paleolithic and Mesolithic groups.     

Reduction, integration and emergence in biochemical networks

Most studies of molecular cell biology are based upon a process of decomposition of complex biological systems into their components, followed by the study of these components. The aim of the present paper is to discuss, on a physical basis, the internal logic of this process of reduction. The analysis is performed on simple biological systems, namely protein and metabolic networks. A multi-sited protein that binds two ligands x and y can be considered the simplest possible biochemical network. The organization of this network can be described through a comparison of three systems, i.e. XY, X and Y. X and Y are component sub-systems that collect states x(i) and y(j), respectively, i.e. protein states that have bound either i molecules of x (whether or not these states have also bound y), or j molecules of y (whether or not these states have bound x). XY is a system made up of the specific association of X and Y that collects states x(i)y(j). One can define mean self-informations per node of the network, , and . Reduction of the system XY into its components is possible if, and only if, ,is equal to the sum of and . If is smaller than the sum of and , the system is integrated, for it has less self-information than the set of its components X and Y. It can also occur that , be larger than the sum of and . Hence, the system XY displays negative integration and emergence of self-information relative to its components X and Y. Such a system is defined as complex. Positive or negative integration of the system implies it cannot be reduced to its components. The degree of integration can be measured by a function , called mutual information of integration. In the case of enzyme networks, emergence of self-information is associated with emergence of catalytic activity. Moreover, if the enzyme reaction is part of a metabolic sequence, its mutual information of integration can be increased by an effect of context of this sequence.     

Factors controlling upper Jurassic ammonite assemblages in north-central Mexico

Lower Kimmeridgian to Lower Tithonian (Upper Jurassic) sections studied at Sierra de Palotes (Durango) and Sierra de Catorce (San Luis Potosí), Mexico, show low-energy deposits in which the composition of fossil macroinvertebrate assemblages, including megabenthos, reflects biostratinomic control. Monotonous siltstones provide continuous records of ammonite assemblages and reflect dominant deposition of shells in living areas; meanwhile, discontinues records were forced by episodic post-mortem transportation of shells, which was especially accentuated under storm influence. Rhythmic marly-silty limestones and marls illustrate a fossil record probably determined by minor transgressive-regressive pulses. The major changes in lithofacies are reflected by condensed silty and phosphatic mudstones deposited during significant floodings affecting areas under dominant terrigenous sedimentation. These changes determined more or less significant variations in the composition of fossil assemblages according to their relation to changing ecological conditions. However, shifting ecospaces exhibit no direct relationship to changes in lithofacies. Post-mortem transportation, operating in relation to both marine floodings and changes in the pattern of upper-water currents, was the main biostratinomic factor affecting the areal distribution of ammonite populations. Shell transportation and sedimentation rate controlled preservation and ultimately influenced diversity in recorded ammonite assemblages. The post-mortem behaviour (interpreted from shell structure and preservation), and therefore distribution, of ammonite shells points to shallow-water environments during the Kimmeridgian - Early Tithonian in areas (such as SE Durango and San Luís Potosí) close to the changing boundary between dominant carbonate and terrigenous sedimentation. No reworking affecting ammonite biostratigraphy has been identified in the sections studied.