We investigated the Sakar unit metamorphic rocks of the Sakar–Strandzha zone in Bulgaria, using 40Ar/39Ar dating of amphibole from the polymetamorphic basement and white mica in the overlying upper Permian metasedimentary rocks of the Paleokastro Formation. The amphibole and white mica revealed plateau ages of 140.50 ± 1.75 Ma and 126.19 ± 1.29 Ma, respectively, indicating an Early Cretaceous cooling history of the regional amphibolite-facies metamorphism to greenschist-facies conditions. Similar metamorphic grades and cooling histories of the Sakar unit share evidence with the nearby Rhodope Massif for the northern Aegean region-wide early Alpine tectonometamorphic event.

Ga proverbial wisdom holds that “hate has no medicine,” but there is a sacred court in Accra where people can calm the animosity that emerges from social conflicts. A unique form of vernacular jurisprudence has emerged at the Nae We Shrine Tribunal, which manages the consequences of civil, criminal, and supernatural crimes without raising the ire of human rights activists. Using records from this shrine court, the authors of this article demonstrate how the Tribunal offers social and spiritual wellbeing in a manner that cannot be provided by the chiefly and state judicial systems.

We describe an ultra-wide-bandwidth, low-frequency receiver recently installed on the Parkes radio telescope. The receiver system provides continuous frequency coverage from 704 to 4032 MHz. For much of the band ( ${\sim}60\%$ ), the system temperature is approximately 22 K and the receiver system remains in a linear regime even in the presence of strong mobile phone transmissions. We discuss the scientific and technical aspects of the new receiver, including its astronomical objectives, as well as the feed, receiver, digitiser, and signal processor design. We describe the pipeline routines that form the archive-ready data products and how those data files can be accessed from the archives. The system performance is quantified, including the system noise and linearity, beam shape, antenna efficiency, polarisation calibration, and timing stability.

Radar surveys across ice sheets typically measure numerous englacial layers that can often be regarded as isochrones. Such layers are valuable for extrapolating age–depth relationships away from ice-core locations, reconstructing palaeoaccumulation variability, and investigating past ice-sheet dynamics. However, the use of englacial layers in Antarctica has been hampered by underdeveloped techniques for characterising layer continuity and geometry over large distances, with techniques developed independently and little opportunity for inter-comparison of results. In this paper, we present a methodology to assess the performance of automated layer-tracking and layer-dip-estimation algorithms through their ability to propagate a correct age–depth model. We use this to assess isochrone-tracking techniques applied to two test case datasets, selected from CreSIS MCoRDS data over Antarctica from a range of environments including low-dip, continuous layers and layers with terminations. We find that dip-estimation techniques are generally successful in tracking englacial dip but break down in the upper and lower regions of the ice sheet. The results of testing two previously published layer-tracking algorithms show that further development is required to attain a good constraint of age–depth relationships away from dated ice cores. We recommend that auto-tracking techniques focus on improved linking of picked stratigraphy across signal disruptions to enable accurate determination of the Antarctic-wide age–depth structure.

A physical oceanographic, geophysical and marine geological survey of Edward VIII Gulf, Kemp Coast, collected data from conductivity–temperature–depth casts, multi-beam bathymetric swath mapping and 3.5 kHz sub-bottom surveying. Modified circumpolar deep water (mCDW) is observed in Edward VIII Gulf, as well as notable bathymetric features including mega-scale glacial lineations and a 1750 m-deep trough. Sedimentological, geochemical, rock-magnetic and micropalaeontological analysis of two kasten cores document regional palaeoclimate and palaeo-oceanographic conditions over the past 8000 years, with a warm period occurring from c. 8 to 4 ka and a shift to cooler conditions beginning at c. 4 ka and persisting until at least 0.9 ka. Sediment packages > 40 m thick within deep troughs in Edward VIII Gulf present potential targets for higher-resolution Holocene and deglacial climate studies. Despite the presence of mCDW on the shelf, inland bed topography consisting of highland terrain suggests the likelihood of relative stability of this sector of the East Antarctic Ice Sheet.

The climate crisis requires nations to achieve human well-being with low national levels of carbon emissions. Countries vary from one another dramatically in how effectively they convert resources into well-being, and some nations with low levels of emissions have relatively high objective and subjective well-being. We identify urgent research and policy agendas for four groups of countries with either low or high emissions and well-being indicators. Least studied are those with low well-being and high emissions. Understanding social and political barriers to switching from high-carbon to lower-carbon modes of production and consumption, and ways to overcome them, will be fundamental.

We propose the nasal administration of calcium-enriched physiological salts as a new hygienic intervention with possible therapeutic application as a response to the rapid and tenacious spread of COVID-19. We test the effectiveness of these salts against viral and bacterial pathogens in animals and humans. We find that aerosol administration of these salts to the airways diminishes the exhalation of the small particles that face masks fail to filter and, in the case of an influenza swine model, completely block airborne transmission of disease. In a study of 10 human volunteers (5 less than 65 years and 5 older than 65 years), we show that delivery of a nasal saline comprising calcium and sodium salts quickly (within 15 min) and durably (up to at least 6 h) diminishes exhaled particles from the human airways. Being predominantly smaller than 1 μm, these particles are below the size effectively filtered by conventional masks. The suppression of exhaled droplets by the nasal delivery of calcium-rich saline with aerosol droplet size of around 10 μm suggests the upper airways as a primary source of bioaerosol generation. The suppression effect is especially pronounced (99%) among those who exhale large numbers of particles. In our study, we found this high-particle exhalation group to correlate with advanced age. We argue for a new hygienic practice of nasal cleansing by a calcium-rich saline aerosol, to complement the washing of hands with ordinary soap, use of a face mask, and social distancing.

Sarcopenia, characterised by loss of skeletal muscle mass and strength with age, is a significant risk factor for loss of mobility and independence. The combination of low muscle mass and high fat mass in sarcopenic obesity is associated with particularly poor outcomes. Micronutrient deficiencies can occur alongside obesity despite total energy surplus, and older individuals may be at greater risk of deficiency. Research suggests vitamin C is important for musculoskeletal health, but the relationship with obesity is underexplored.

This study aimed to investigate associations of plasma vitamin C with obesity status and explore the relationship with the sarcopenic risk factor, low skeletal muscle mass.

EPIC-Norfolk cohort study data were analysed. Bioelectrical impedance analysis-estimated fat free mass (FFM; a proxy for skeletal muscle mass) was adjusted for BMI to give a scaled variable, FFMBMI. A ‘low muscle mass’ category was defined as individuals with the lowest 10% FFMBMI, representing those at high risk of sarcopenia. Plasma vitamin C (ascorbic acid) concentrations were categorised as inadequate (< 50micromol/L) or adequate (≥ 50micromol/L), and obesity status as non-obese (< 30kg/m2) or obese (≥ 30kg/m2).

Individuals were grouped according to vitamin C and obesity status: 1, non-obese and adequate vitamin C; 2, non-obese and inadequate vitamin C; 3, obese and adequate vitamin C; and 4, obese and inadequate vitamin C. Using logistic regression, the odds ratio (OR) of each vitamin/obesity status group was calculated in relation to membership of the ‘low muscle mass’ category. Analyses were sex-stratified and adjusted for age, smoking status, physical activity, social class, menopausal and HRT status in women, statin use, and corticosteroid use.

Data were analysed for 5903 men (mean 62.9 years, SD 9.0) and 7416 women (mean 61.5 years, SD 9.0). Prevalence of vitamin C inadequacy was higher in obese vs non-obese individuals (men 45.8% vs 33.0%; and women 26.0% vs 15.3%). The odds of ‘low muscle mass’ were higher in all vitamin/obesity status groups vs group 1, but the greatest odds were seen for group 4 (combined obesity and inadequate vitamin C) in men (OR 16.5, 95% CI: 12.6–21.6; p < 0.001) and women (OR 30.2, 95% CI: 23.0–39.8; p < 0.001).

In this cohort of older individuals higher prevalence of vitamin C inadequacy is associated with obese individuals. Of importance to musculoskeletal health and our understanding of sarcopenia is the observation that while vitamin C inadequacy and obesity are each independently important, their coexistence is a particularly strong predictor of sarcopenic risk.

The Ross Ice Shelf (RIS) is host to a broadband, multimode seismic wavefield that is excited in response to atmospheric, oceanic and solid Earth source processes. A 34-station broadband seismographic network installed on the RIS from late 2014 through early 2017 produced continuous vibrational observations of Earth's largest ice shelf at both floating and grounded locations. We characterize temporal and spatial variations in broadband ambient wavefield power, with a focus on period bands associated with primary (10–20 s) and secondary (5–10 s) microseism signals, and an oceanic source process near the ice front (0.4–4.0 s). Horizontal component signals on floating stations overwhelmingly reflect oceanic excitations year-round due to near-complete isolation from solid Earth shear waves. The spectrum at all periods is shown to be strongly modulated by the concentration of sea ice near the ice shelf front. Contiguous and extensive sea ice damps ocean wave coupling sufficiently so that wintertime background levels can approach or surpass those of land-sited stations in Antarctica.