Recent Development of Metallic (1T) Phase of Molybdenum Disulfide for Energy Conversion and Storage

The development of a feasible and inexpensive strategy to obtain and utilize sustainable energy is an important issue for the sustainable development of human society. Over the past decade, significant progress has been made in the development of novel functional materials for energy conversion and storage. Owing to their unique physico‐chemical properties, 2D layered materials, such as graphene and transition metal dichalcogenides, have attracted great interest in energy‐related research. 1T‐MoS₂ is a metallic phase of molybdenum disulfide (MoS₂) with extraordinary electronic conductivity, enlarged interlayer spacing, and more electrochemically active sites along the basal plane, which offers intriguing benefits for energy‐related applications compared to its semiconducting counterpart (2H‐MoS₂). This review summarizes the preparation and structure–property relationships of 1T‐MoS₂, as well as the underlying relations between the metallic (1T) and semiconducting (2H) phases of MoS₂. Recent progress in the preparation and stabilization of 1T‐MoS₂ materials and their applications for energy conversion and storage are discussed, including water splitting to form hydrogen via photo/electrocatalysis and electricity storage in lithium‐ion batteries, sodium‐ion batteries, magnesium‐ion batteries, and supercapacitors. Optimization strategies of 1T‐MoS₂ to obtain enhanced practical properties based on theoretical calculations are also presented.     

The wing base of the palaeodictyopteran genus Dunbaria Tillyard: Where are we now?

The structure of insect wing articulation is considered as reliable source of high level characters for phylogenetic analyses. However, the correct identification of homologous structures among the main groups of Pterygota is a hotly debated issue. Therefore, the reconstruction of the wing bases in Paleozoic extinct relatives is of great interest, but at the same time it should be treated with extreme caution due to distortions caused by taphonomic effects. The present study is focused on the wing base in Dunbaria (Spilapteridae). The articulation in Dunbaria quinquefasciata is mainly formed by a prominent upright axillary plate while the humeral plate is markedly reduced. Due to unique preservation of surface relief of the axillary plate, its composition shows a detailed pattern of three fused axillary sclerites and presumable position of the sclerite 3Ax. The obtained structures were compared among Spilapteridae and to other palaeodictyopterans Ostrava nigra (Homoiopteridae) and Namuroningxia elegans (Namuroningxiidae). The comparative study uncovered two patterns of 3Ax in Dunbaria and Namuroningxia, which correspond to their different suprafamilial classification. In contrast to previous studies these new results reveal the homologous structural elements in the wing base between Paleozoic Palaeodictyoptera and their extant relatives of Ephemeroptera, Odonata and Neoptera.     

The Age of Angels: spiritualism and evolutionary progressionism in a nineteenth-century geologic time chart

The term ‘Anthropocene’ often carries apocalyptic overtones of environmental devastation, but many nineteenth-century iterations of the ‘Age of Humans’ idea were explicitly optimistic. The current time period was framed as a ‘Psychozoic Era’ or ‘Age of Mind’ in which human beings took their predetermined place at the pinnacle of ‘creation’. Hiram Alvin Reid, an amateur scientist in the midwestern United States, took this line of thinking a step further. He drafted a geologic time chart in which the current ‘Age of Man’ was succeeded by a future ‘Age of Angels’, wherein humans will become higher beings. Reid was a Christian spiritualist who thought that evolution drove both physical and spiritual advancement, including the recent development of a ‘sixth sense’ that allowed humans to perceive ghosts and angels. Reid’s views, while idiosyncratic and coloured by his metaphysical beliefs, drew heavily on mainstream concepts in biology and geology. Prominent geologists like James Dana and Joseph Le Conte argued for an Age of Mind in terms that mixed scientific rigor with religious and progressionist ideas. The Psychozoic was also embraced by many progressive-minded individuals outside the natural sciences, paralleling widespread modern interest in the Anthropocene.     

Environment change, geographic migration and sickle cell anaemia

The classic model describing the interaction between sickle cell anaemia and malaria is one of the most notable achievements of population genetics. Nevertheless, only panmictic populations in steady environments have been studied theoretically to date. In this paper, environment change and geographic inhomogeneity are introduced. The rate of decrease of mutation after environment improvement is obtained. The kinetics of the spread of disease after the initial mutation, together with the genetic composition profile near the borders of malaria areas, are calculated. The results are compared with the empirical data on the mutation level in African and African-American populations. It is shown that the spread of disease and decrease in mutation are highly asymmetric: the mutation level increases exponentially and decreases much more slowly (as a power function). The mathematical and biological reasons for this behaviour are discussed.     

THE EFFECT OF INBREEDING IN DIPLOID AND TETRAPLOID POPULATIONS OF EPILOBIUM ANGUSTIFOLIUM (ONAGRACEAE): IMPLICATIONS FOR THE GENETIC BASIS OF INBREEDING DEPRESSION

The partial dominance model for the evolution of inbreeding depression predicts that tetraploids should exhibit less inbreeding depression than their diploid progenitors. We tested this prediction by comparing the magnitude of inbreeding depression in tetraploid and diploid populations of the herbaceous perennial Epilobium angustifolium (Onagraceae). Inbreeding depression was estimated in the greenhouse for three tetraploid and two diploid populations at four life stages. The mating system of a tetraploid population was estimated and compared to a previous estimate for diploids. Tetraploids showed less inbreeding depression than diploids at all life history stages, and these differences were significant for seed-set and cumulative fitness, but not for germination, survival, or plant dry mass at nine weeks. This result suggests that the genetic basis of inbreeding depression may differ among life stages. The primary selfing rate of the tetraploid population was r = 0.43, which is nearly identical to that of a diploid population (r = 0.45), indicating that differences in inbreeding depression between diploids and tetraploids are probably not due to differences in the mating system. Cumulative inbreeding depression, calculated from the four life history stages, was significantly higher for diploids () than for tetraploids (), supporting the partial dominance model of inbreeding depression.     

Morphologic variability of the coccolithophorid Calcidiscus leptoporus in the plankton, surface sediments and from the Early Pleistocene

On a global scale, morphological variability of the extant coccolithophorid Calcidiscus leptoporus (Murray and Blackman, 1898) Loeblich and Tappan was investigated in surface sediments and plankton samples and from an Early Pleistocene time-slice (1.8 Ma to 1.6 Ma). In the bivariate space coccolith diameter versus number of rays in the distal shield, Holocene samples follow a single, unimodal morphocline. Sample means of coccolith size and number of elements group in three clusters, I, II and III, which are of biogeographic significance. Clusters II and III coccoliths (mean coccolith size of 5.0 μm and 20.9 elements, and 6.6 μm and 25.6 elements, respectively) are found in a tropical belt extending from 11 °N to 17 °S with an annual minimum sea-surface temperature above 23.5 °C. Cluster I coccoliths (5.8 μm, 20.7 elements) are found in samples outside that belt. The distribution of coccoliths in the surface sediments is tentatively interpreted to be a result of mixing to a varying degree of at least three different morphotypes (‘small’, ‘intermediate’ and ‘large’), which were identified in the living plankton, and which are separated from each other at 5 μm and 8 μm mean coccolith diameter, respectively. A comparison of the surface sediments with the Early Pleistocene assemblages revealed that between 1.6 Ma and 1.8 Ma two morphoclines A and B existed, the first of which persisted until the Holocene in the form of C. leptoporus, while the second comprises only extinct morphotypes including Calcidiscus macintyrei as one end-member. During the Early Pleistocene morphocline A was more homogeneous and no clusters were evident.Morphocline B shows a clear bimodality with a separation of morphotypes at 9.5 μm. Our observations suggest that morphoclines are subsets within the total stratigraphical range of a single species, and represent the global variability of that species in a particular time interval. Morphotypes, which belong to a morphocline, represent the infra-specific variability of that species within the biogeographic and stratigraphic limits of that species.     

Genetic analysis of aMicroseris douglasii (Asteraceae) population polymorphic for an alien chloroplast type

Recent evidence suggests chloroplast introgression fromMicroseris bigelovii intoM. douglasii. We have examined 23 plants from a population ofM. douglasii polymorphic forM. douglasii andM. bigelovii chloroplast types. All 23 plants were completely homozygous for morphological and RAPD markers, and inbred lines derived by selfing have been used for DNA analysis. Chloroplast RFLP analysis identified 16 plants withM. bigelovii chloroplasts and seven withM. douglasii chloroplasts. The nuclear genomes of the 16 plants withM. bigelovii chloroplasts were examined with 22 primers for RAPD amplification products shared exclusively withM. bigelovii. Five of 268 markers appeared to be shared betweenM. bigelovii and one or more of these 16 plants on the basis of their position in gels. Detailed examination of these five amplification products showed that none of them are nuclear DNA fromM. bigelovii. Very little, if any, nuclear DNA fromM. bigelovii can be present inM. douglasii plants with chloroplasts typical ofM. bigelovii. The study demonstrates the usefulness of the RAPD technique for screening large numbers of markers to select a few potentially informative ones for rigorous examination.Dedicated to emer. Univ.-Prof. DrFriedrich Ehrendorfer on the occasion of his 70th birthday