Subterranean glacial spillways: an example from the karst of South Wales, UK

Many karst areas in the UK have been glaciated one or more times during the last 0.5 Ma, yet there are few documented examples of caves in these regions being affected by glacial processes other than erosion. The karst of South Wales is one area where sub or pro-glacial modification of pre-existing caves is thought to occur. Evidence from the Ogof Draenen cave system suggests that caves can sometimes act as subterranean glacial ‘underspill’ channels for melt-water. This cave, one of the longest in Britain with a surveyed length of over 70 km, underlies the interfluve between two glaciated valleys. Sediment fills and speleo-morphological observations indicate that melt-water from a high level glacier in the Afon Lwyd valley (>340m asl) filled part of the cave and over-spilled into the neighbouring Usk valley, temporarily reversing non-glacial groundwater flow directions in the cave. It is suggested that this may have occurred during a Middle Pleistocene glaciation

NW UK continental margin : chronology and isotope geochemistry

Until recently, a significant proportion of the crystalline basement from the NW UK continental shelf was virtually terra incognita in comparison with similar rocks on the mainland. A significant increase in the geological understanding of this region’s crystalline rocks is provided by new data from 42 boreholes, some of which were only drilled in 2001. The samples are from a ~550 km long transect of the UK continental shelf, extending from ~50 km west of Shetland in the northeast to Stanton High, south of the Outer Hebrides and westward to include Rockall High. Petrography and geochemistry show the main lithologies are amphibolite to granulite facies amphibolites and gneisses, and include classic Archaean TTG’s, metabasic rocks, granite (s.s), and granitic pegmatites. A long history of crustal growth is indicated by U-Pb zircon ages and Nd model ages. Archaean gneisses that developed in two main episodes dominate much of the study area. The older gneisses (c. 2.8 Ga) represent new continental crust while genesis of the later gneisses (c. 2.74-2.70 Ga) involved crustal recycling. Both groups are very similar to onshore Lewisian gneisses. Important areas of known Proterozoic crust were also characterized, confirming the results of previous studies. Geochemistry and Nd isotope systematics of Stanton High documents extensive Archaean crust re-working in the Proterozoic, as well as addition of new continental crust. Stanton High U-Pb zircon ages (1799-1791.5 Ma) are similar to the Rhinns terrane (c. 1800 Ma). Westward, Rockall High borehole samples yield a 1744.9 Ma U-Pb age, distinct from Stanton High – Rhinns rocks. Nd data indicate addition of mantle-derived juvenile crust, as previously noted elsewhere on Rockall High. An isolated granulite facies metabasic rock on the NE portion of the Hebrides shelf was dated at 1633.5 Ma, also representing a new addition of crust. The new data provide important constraints for regional correlations and palaeotectonic reconstructions. The Archaean rocks are almost certainly related to the Lewisian: given current models, they probably also correlate to the Nagssugtoquidian in Greenland, while the Rockall and Stanton Highs, together with the Rhinns terrane, have affinities to the Ketilidian of Greenland and the Svecofennian of Scandinavia

Speleothem U-series constraints on scarp retreat rates and landscape evolution: an example from the Severn valley and Cotswold Hills gull-caves, UK

Modelling landscape evolution requires quantitative estimates of erosional processes. Dating erosional landscape features such as escarpments is usually difficult because of the lack of datable deposits. Some escarpments and valley margins are associated with the formation of mass-movement caves, sometimes known as ‘gull’ or ‘crevice’ caves, which are typically restricted to within 0.5 km of the valley margin or scarp edge. As in other caves, these mass-movement cavities may host speleothems. As gull-caves develop only after valley incision, uranium-series dating of speleothems within them can provide a minimum age for the timing of valley excavation and scarp formation. Here we present data from several gull-caves in the Cotswold Hills, which form the eastern flank of the Severn valley in southern England. U-series ages from these gull-caves yield estimates for both the minimum age of the Cotswold escarpment and the maximum scarp retreat rate. This is combined with data from geological modelling to propose a model for the evolution of the Severn valley and the Cotswold Hills. The data suggest that the location of the escarpment and regional topography is determined not by valley widening and scarp retreat, but by the in situ generation of relief by differential erosion

Contribution of an accurate growth rate reconstruction of a stalagmite from the Kanaan Cave-Lebanon to the understanding of humidity variations in the Levant during the MIS 5

Lying at the transition between temperate Mediterranean domain and subtropical deserts, the Levant is a key area to study the palaeoclimatic response over glacial-interglacial cycles. This paper presents a dated last interglacial (MIS 5) stalagmite (129–84 ka) from the Kanaan Cave, Lebanon. Variations in growth rate, morphology and petrology have been measured to derive a palaeoclimatic record. The speleothem growth curve shows rapid growth rates during the peak of MIS 5e (126-124 ka), moderate growth rates between 103.5 and 99 ka and very low growth rates from 99 to 84 ka. On the basis of the good correlation between the speleothem morphology and growth rates with the isotopic response of continental records from northern and southern Levant, we relate high growth rate to wet conditions during the maximum MIS 5e and MIS 5c. The peak in growth rates corresponds to sapropel events in the eastern Mediterranean. Low growth rates during MIS 5d and 5b indicate a transition to drier conditions

COVID-19 confessions: a qualitative exploration of healthcare workers experiences of working with COVID-19

Objectives To gain insight into the experiences and concerns of front-line National Health Service (NHS) workers while caring for patients with COVID-19. Design Qualitative analysis of data collected through an anonymous website (www.covidconfidential) provided a repository of uncensored COVID-19 experiences of front-line NHS workers, accessed via a link advertised on the Twitter feed of two high profile medical tweeters and their retweets. Setting Community of NHS workers who accessed this social media. Participants 54 healthcare workers, including doctors, nurses and physiotherapists, accessed the website and left a ‘story’. Results Stories ranged from 1 word to 10 min in length. Thematic analysis identified common themes, with a central aspect being the experience and psychological consequence of trauma. Specific themes were: (1) the shock of the virus, (2) staff sacrifice and dedication, (3) collateral damage ranging from personal health concerns to the long-term impact on, and care of, discharged patients and (4) a hierarchy of power and inequality within the healthcare system. Conclusions COVID-19 confidential gave an outlet for unprompted and uncensored stories of healthcare workers in the context of COVID-19. In addition to personal experiences of trauma, there were perceptions that many operational difficulties stemmed from inequalities of power between management and front-line workers. Learning from these experiences will reduce staff distress and improve patient care in the face of further waves of the pandemic

Myeloperoxidase to Risk Stratify Emergency Department Patients with Chest Pain

Previous studies suggest that serum myeloperoxidase (MPO) is a potentially useful biomarker to risk stratify troponin-negative patients with suspected myocardial ischemia. We hypothesized that the relationship between initial serum MPO levels would correlate with 30-day adverse cardiac outcomes for low risk emergency department (ED) patients with suspected myocardial ischemia. This prospective cohort study enrolled ED patients with chest pain or suspected myocardial ischemia, non-diagnostic ECG, and initially negative cardiac troponin I. We defined 30-day adverse cardiac events as death, myocardial infarction, or coronary revascularization. We calculated summary statistics, standard deviation (SD), odds ratios (OR), 95% confidence intervals (CI), and receiver operating characteristics (ROC). We enrolled 159 patients who had a mean age of 55 ± 13, were 56% female, of whom 5.2% suffered at least one adverse cardiac event. MPO test characteristics were poor, with an ROC area of only 0.47 (CI 0.23-0.71). MPO levels were not associated with adverse events (OR 0.99, CI 0.98-1.01, p=0.62). The optimal ROC cutpoint to predict adverse cardiac events had poor sensitivity and specificity (57% and 52%, respectively). Mean MPO concentrations in the event group did not differ from the non-event group. In this limited cohort of low risk ED patients with chest pain, we were unable to demonstrate utility of MPO for risk stratification. If confirmed in larger studies, these findings may call into question the routine use of MPO for low-risk chest pain

Head movements and sound localization

Most research on auditory localization has been conducted with listeners motionless. Nine experiments were conducted to investigate whether and how head motion assists sound localization. In three preliminary experiments, fairly unconstrained responding was made possible by using a partial spherical screen to obscure sources in the left lateral horizontal plane (HP) and the upper-left lateral vertical plane (LVP). The signal was 2-kHz low-pass noise, which thus offered no high-frequency pinna-based spectral cues. As expected, listeners were unable to localize the low-pass noise if they remained motionless throughout the duration of the signal. With a 3-s signal, it was observed that listeners achieved much greater accuracy in terms of front-back discrimination and elevation judgement, if they were permitted to move naturally or if they employed head rotation, about a vertical axis. Following these preliminary experiments, the test equipment was upgraded, so that all regions of auditory space were equally likely to contain sound sources. ... Some remarks are made, in conclusion, about the functions and bases for sound localization in everyday listening conditions

Long-term glacial and fluvial system coupling in southern Greece and evidence for glaciation during Marine Isotope Stage 16

Pleistocene glacial activity was a major influence on runoff and sediment supply in many river systems across the Mediterranean. The geomorphological impacts of changes in sediment supply between glaciated headwater terrains and downstream depocentres spanning several glacial cycles are, however, poorly understood. By applying uranium-series and optically stimulated luminescence dating to fluvial and glacial sediments preserved on Mount Chelmos (2355 m a.s.l.) in southern Greece, we show how changes in the long-term coupling between glacial and fluvial systems are preserved within a major glaciofluvial outwash fan system that functioned during multiple cold stages. We also present evidence in the form of a cemented till unit, stratigraphically below younger Middle Pleistocene glacial deposits, yielding a U-series age close to the limit of the technique, indicating glaciation during Marine Isotope Stage (MIS) 16 - one of the most severe cold stages recorded in the Mediterranean. This is the first time such early glaciation has been directly recorded in Greece and the wider Balkans and is defined here as the Valvousian Stage based on glacial deposits on Mount Chelmos. Geomorphological and geochronological data point to the formation of a more extensive plateau ice field over Chelmos during MIS 12, another severe glacial period in the Balkans that corresponds with the Skamnellian Stage glaciation of Northern Greece. During this phase, very strong coupling of glacial and fluvial systems led to meltwater flood events transferring large volumes of sediment to lower valley zones culminating in the formation of an extensive glaciofluvial outwash fan complex and glaciofluvial terraces. A smaller plateau ice field during MIS 6 and localised valley glaciers between MIS 5d to 5c correlate with the Vlasian and early Tymphian Stage glaciations in Greece, respectively. The delivery of much less meltwater and sediment through a single valley during MIS 6 and MIS 5b to MIS 4 signalled the transition to progressively weaker glacial and fluvial system coupling. After MIS 4 the uncoupling of depositional zones from sediment sources in glaciated catchments led to fluvial incision of glaciofluvial outwash deposits in several valleys. Despite this incision, the glaciofluvial outwash fans preserve a record of glacial and fluvial system interactions during the Middle Pleistocene and early stages of the Late Pleistocene