The zosterophyllopsids had a widespread distribution and constituted a dominant component in many plant assemblages during the Early Devonian. Although a large number of zosterophyllopsids have been documented, knowledge about the paleogeographic distribution of different genera/species remains to be expanded by further fossil evidence. In this article, new material assigned to the genus Gosslingia Heard, 1927 and designated as Gosslingia cf. G. breconensis Heard, 1927 is described from a new locality of the Lower Devonian of Guizhou Province, China. The Guizhou material shows main axes that are pseudomonopodially branched, pseudomonopodial lateral branching systems, subaxillary tubercle branches, circinate apices, elliptical xylem strand, exarch maturation of xylem, and G-type tracheids, and exhibits considerable similarities with the type and only species of Gosslingia, Gosslingia breconensis. Our finding represents the first report of Gosslingia in the South China Block and the most convincing occurrence of this genus outside of Wales, UK. Gosslingia adds to the diversity of genera shared among the Early Devonian floras of South China, western Europe, and North America, along with Distichophytum Mägdefrau, Estinnophyton Fairon-Demaret, Zosterophyllum Penhallow, and others, and indicates that the dispersal of early vascular plants among different paleocontinents was more common than previously appreciated.

Early-career secondary school music teachers navigate many challenges as they settle into the profession. These include consolidating their knowledge of subject content, gaining classroom confidence and honing skills in classroom management. In addition, their sense of belonging can be enhanced by working at collegial relationships within their faculty, across the school and feeling a part of the wider school community. These factors can elicit a ‘make or break’ response for continuing in the profession.

This paper reports on a case study of an Australian early-career secondary school music teacher, in her fifth year in the profession. The case study, as a part of a larger study, sequenced quantitative and qualitative research methods, allowing insight into the music teacher’s working life and enabled the researcher to understand factors that impact daily practice. Themes explored in the study include motivation, perception of value, stress and the difficulties of securing permanent employment. The music teacher presented a positive approach to her work through her development of resilience and shared her future goals and dreams.

This research offers suggestions on how schools and education authorities can best support early-career secondary school music teachers to enable them to become resilient, confident and valued practitioners for the future.

The teaching-learning process, both in general and in the specialty of Music Education, has evolved and its explanatory models have become increasingly complex. In view of current challenges, it is relevant to analyse the elements that are considered necessary to train music teachers to become competent professionals. This study identifies characteristics found in specialised Spanish and international scientific literature on teaching-learning processes in music teacher education, referring to their current state as well as to desirable developments and future prospects. Although a certain overlap among emergent categories in Spain and those in other countries can be observed, we also found differences of degree, as well as interesting divergences.

This collection of papers explores the intellectual history of music in global context during the period between around 1870 and 1930. Following an introduction that discusses the state of the field, each of the three papers presents a case study that explores the intersection between music and global history from diverse perspectives. The first paper discusses a Hindi music treatise published in 1896. By situating this work within multiple ‘significant geographies’, the paper highlights the limitations of ‘global’ approaches that neglect the more immediate musical, social and intellectual environments of their subjects. The second paper analyses the intersection between music and Islamic modernism in the late Ottoman Empire. It argues that a Eurocentric understanding of music history propagated by earlier reformists was succeeded at the end of the nineteenth century by an oppositional narrative that drew on the geopolitical imaginary of pan-Islamism. The final paper discusses the work of the Argentine composer Alberto Williams, particularly in relation to his views on race and national music. The paper demonstrates how contemporary scientific theories such as positivism and Social Darwinism contributed to a narrative of national musical development that created hierarchies of musical genres and excluded Argentine composers of African descent.

There exists substantial evidence that technological innovation and, more specifically, innovation creating high-tech exports is a crucial driver for economic growth. However, there is less consensus about the factors that cause high-tech exports to thrive. Most studies emphasize the crucial role played by research and development expenditures, foreign direct investments, trade openness, human capital, and patents. In this article, we instead examine the role of a different determinant, which usually is overlooked in the scholarly debate about governance institutions. We use government effectives (GE) and rule of law (ROL) as measures of governance. We employ a panel-data approach encompassing more than 100 countries between 2007 and 2019. The panel estimates show a causal relationship linking GE and the ROL with high-tech exports.

The role of adsorbed and structural Fe3+ in palygorskite and sepiolite with respect to the oxidation of hydrocortisone in aqueous suspension has been evaluated using electron spin resonance and UV-visible spectroscopy. Natural surface-adsorbed Fe3+ showed an important activity in the oxidation process, although smaller than octahedral Fe3+. The kinetics of oxidative degradation of hydrocortisone by palygorskite appear to be composed of two apparent first order reactions which may be associated with two kinds of sites for Fe in palygorskite. The lower oxidizing power of sepiolite for hydrocortisone degradation is due to its very low Fe3+ content.

Several clay-organic complexes were synthesized by placing quaternary ammonium cations on smectite by cation exchange. They were then examined for their ability to adsorb phenol and several of its chlorinated congeners. The organic cations used were: hexadecylpyridinium (HDPY+), hexadecyltri-methyl ammonium (HDTMA+), trimethylphenyl ammonium (TMPA), and tetramethylammonium (TMA+). The complexes containing long-chain alkyl (hexadecyl) groups were the most hydrophobic and adsorbed the phenols from water in proportion to their hydrophobicities, which increase with chlorine addition (phenol < chlorophenol < dichloropohenol < trichlorophenol). With n-hexane as the solvent, different adsorption was found which depended on the type and degree of solvent interactions with the compound and the clay-organic complex. Thus, the amount of adsorption of these phenols on clay-organic complexes was dependent on the relative energies of adsorbent-adsorbate and adsorbate-solvent interactions.

Microprobe analyses of optically homogeneous detrital biotites from sandstones of the Visingsö Group and the Dala Sandstone, Sweden, revealed a consistently low K content (generally <0.75 atom/formula unit) and variable amounts of Fe, Mg, Al, and Si. Electron probe profiles of some biotite grains indicated two major types of interstratification, one consisting of mainly illite layers and the other apparently consisting of chlorite layers. The layer thicknesses commonly ranged between 0.5 and 3 μm. Microprobe analyses of some thick (∼5 μm) illitic layers indicated a phengitic composition, wherein the mica was relatively rich in octahederal Fe and Mg. The chloritic layers appeared to be Fe-Mg-rich and generally had octahederal totals of <6 atom/formula unit. Variations in the chemical composition of the biotite and some of the illite and chlorite were probably due to an uneven distribution of small amounts of the interstratified phases. The illite and chlorite layers were apparently formed by pseudomorphic replacement of detrital biotites, i.e., gradual replacement of one biotite layer by one layer(s) of illite and/ or chlorite during diagenesis.

Spherical and platy kaolinite crystals were prepared under several hydrothermal conditions. Spherical kaolinite was produced mainly at high solid/water ratio (1/4) and at low temperatures (150°-200°C). Platy kaolinite predominated in products from experiments with intermediate solid/water ratios (1/256-1/16) and at high temperatures. Boehmite predominated at low solid/water ratios (1/4096) at all experimental temperatures (180°-220°C). The results indicate that the growth of the spherical kaolinite was favored at high degrees of supersaturation, whereas the growth of the platy kaolinite was favored at relatively low degrees of supersaturation.

Age-related macular degeneration (AMD) is a chronic, progressive eye condition that can affect individuals in later life and lead to loss of central visual function. In this analysis, we aimed to explore the discursive landscape of talk about AMD, drawing on extracts published in peer-reviewed qualitative studies on AMD. Drawing on procedures of qualitative meta-synthesis, we compiled a corpus of raw data extracts from 25 qualitative studies on AMD published in English, largely carried out in high-income countries. Extracts were analysed to identify dominant discourses and key interpretative repertoires (such as recurring metaphors, tropes and figures of speech). We adopted a Foucauldian discourse analytic approach, to consider the implications of dominant discourses, and their associated subject positions, for the subjective experience of living with AMD. Our analysis identified five distinct ways in which AMD was constructed in research participants' talk about experiences of AMD. They included: AMD as a mysterious affliction, linked to biological ageing; AMD as a total loss of independence; AMD as grievous loss; AMD as a condition to be stoically accepted; and – to a more limited extent – AMD as an opportunity for discovery. Drawing on theory from critical disability studies and gerontology, we suggest that the constructions identified are underpinned by broader societal discourses which construct ageing and disability in largely negative, medicalised and individualistic terms. Taking up subject positions within such discourses may compound feelings of isolation, hopelessness and powerlessness. We suggest there may be value in exploring talk about experiences of living with AMD within a broader range of everyday social, relational and environmental contexts.

A corrensite-like mineral, from near Borgotaro, Parma (Taro Valley, Italy), was studied by X-ray powder diffraction (XRD) and thermal analysis at different temperatures and water vapor pressures in the natural state and after exchange with ten different cations. In the natural state the mineral is characterized by a basal reflection at ∼29 Å shifting to ∼24 Å on heating and to ∼32 Å by glycerol treatment. The dehydration features of the homoionic minerals show that the stability of the complex of water, compensating cation, and silicate framework depends on the electrostatic energy of the water dipole in the cation field, similarly to smectite.

XRD of the exchanged mineral shows a basal reflection of ∼58 Å particularly in the NH4-, Rb-, and Ba-exchanged states. This value suggests a structure characterized by a regular sequence of silicate layers with different layer charge, that generally results in a c periodicity of ∼29 Å, but which shifts to ∼58 Å, and perhaps higher values, because of small differences in the compensating cation layers.

One-aminonaphthalene is sorbed onto the Na-saturated smectite clays, montmorillonite and hectorite, by cation exchange. In the presence of Fe3+, either in the clay structure or on the clay surface, sorption is followed by the formation of a blue-colored complex, with the continuous disappearance of aminonaphthalene from solution and the clay surface. The rate of aminonaphthalene disappearance decreases as pH increases. With time, four major products that appear to be structural isomers of N(4-aminonaphthyl)-l-naphthylamine are produced. A simplified model of this transformation is suggested to be the oxidation by Fe3+ of sorbed aminonaphthalene forming a radical cation-clay complex. A subsequent reaction between the radical-cation and a neutral aminonaphthalene molecule takes place, with the products being strongly sorbed to the clay surface.

Adsorption of p-hydroxybenzoate anion on synthetic Fe oxides, hydroxides, and oxyhydroxides (hereafter referred to as oxides) was measured at pH 5.5, and the organic-oxide interaction was characterized using diffuse-reflectance Fourier-transform infrared (DRIFT) spectroscopy. Surface complexes with ferrihydrite, hematite, goethite, and noncrystalline Fe oxide were investigated. Infrared (IR) spectra of the oxides after separation from p-hydroxybenzoate solutions showed the organic to be coordinated by an inner-sphere mechanism to the oxide surface through the carboxylate group. Bidentate binding of the carboxylate was identified to be the dominant type of complexation on the oxides. Although the IR study suggested that goethite formed the strongest surface iron-carboxylate bond, the total amount of organic adsorbed was the least on this oxide. This result suggested that bond energy was less important than adsorption site density in determining the amount of organic anion adsorption. Increasing ionic strength had little effect on adsorption by the noncrystalline Fe oxide, but dramatically decreased adsorption on hematite and goethite. This difference might have been due to anion competition for binding sites. At pH 5.5, the amount of organic adsorbed per unit weight of oxides (in 0.05 M NaClO4) followed the order: ferrihydrite > noncrystalline Fe oxide > hematite ≫ goethite. Adsorption per unit of surface area however, followed the order: ferrihydrite > hematite > noncrystalline Fe oxide ≫ goethite. The hematite adsorption reaction appeared to be driven by entropy, inasmuch as the reaction was endothermic. The difference among the oxides in surface reactivity toward p-hydroxybenzoate is hypothesized to have been caused by differences in both quantity and structural arrangement of reactive sites on the oxide surface.