Oman has been recognised as the leading country in terms of recent developments in public health. However, there is a shortage of mental health services, which poses challenges for people seeking such services, particularly those from rural areas. This often results in delayed treatment and longer periods of untreated mental illness.

Mollusk shells from archeological deposits are often exposed to high temperatures through human-caused or natural heating events. While heat exposure affects reliability of mollusk shells for environmental reconstructions based on geochemistry, it can provide a valuable source of information on past human behaviors and human–environment interactions. We analyzed burned and not-burned bivalve and gastropod specimens collected within two megalithic circular structures in the HAS1 settlement in Oman (Late Iron Age and Classical Period). Through a multi-methodological approach, we investigated shell microstructure using scanning electron microscopy (SEM), shell mineralogy using X-ray diffraction (XRD), and shell stable-isotopic composition (δ18O, δ13C) using isotope-ratio mass spectrometry (IRMS) to infer the temperatures these specimens were exposed to and to reconstruct the processes responsible for heating the shells. Thermal response of aragonite and calcite shells having different microstructures were also determined. We found that mollusk shells at this site were exposed to three temperature ranges: a) no exposure or <300°C, b) between 250°C and 500°C, and c) ≥500°C. The heat source was likely a fire which engulfed the entire settlement, which is also supported by evidence of carbonized wooden poles found in situ inside the circular structures.

Our hospital is one of the tertiary care hospitals in Oman receiving coronavirus disease (COVID-19; C19) patients. To meet the expected surge of patients, a number of changes was made to the emergency department (ED), especially regarding capacity building and patient flow. At first, few changes were made to the main ED, which mainly includes the addition of a COVID suspect room with the use of a separate resuscitation area. The major drawback of the abovementioned system was the inability to see more than 2 patients simultaneously. A later separate COVID emergency department (CED) was used. In the CED, pending admissions was the major problem, as the C19 ward and C19 intensive care unit were becoming full; this problem was solved through central command help. In the normal ED, the main problem was the presentation of C19-positive patients sometimes hiding their symptoms and reaching inside the main ED, exposing the staff and patients. In order to combat this problem, all patients with an acute respiratory problem, even if C19 is not suspected, were taken to the corner cubicle. In this report, the changes made in the ED to combat C19 spread are discussed.

Triliths are megalithic monuments scattered across the coastal plains of southern and southeastern Arabia. They consist of aligned standing stones with a parallel row of large hearths and form a space, the meaning of which is undoubtedly significant but nonetheless still unknown. This paper presents a new radiocarbon (14C) dataset acquired during the two field seasons 2018–2019 of the TSMO (Trilith Stone Monuments of Oman) project which investigated the spatial and temporal patterns of the triliths. The excavation and sampling of trilith hearths across Oman yielded a dataset of 30 new 14C dates, extending the use of trilith monuments to as early as the Iron Age III period (600–300 BC). The earlier dates are linked to two-phase trilith sites in south-central Oman. The three 14C pairs collected from the two-phase trilith sites indicated gaps between the trilith construction phases from 35 to 475 years (2 σ). The preliminary spatio-temporal analysis shows the geographical expansion of populations using trilith monuments during the 5th to 1st century BC and a later pull back in the 1st and 2nd century AD. The new 14C dataset for trilith sites will help towards a better understanding of Iron Age communities in southeastern Arabia.

This paper explores the usages of four concepts – sunna, sīra, āthār, and nasab – mainly in early Ibāḍī epistles, but also in other types of Ibāḍī literature, to examine how early Ibāḍīs understood the legacy of the Prophet Muḥammad, and their relation to that legacy. It argues that before the sixth/twelfth century a notion of communal pedigree occupied pride of place in early Ibāḍī conceptualizations of legality and legitimacy. Thus, Ibāḍī sunna was “communal sunna”. The accumulated weight of Ibāḍī tradition – what is known as āthār in Ibāḍī literature – operated authoritatively as a counterpart to sunna; and the Ibāḍī siyar tradition did not focus on the Prophet exclusively, but rather described the scholarly community as an imagined whole. Moreover, Ibāḍīs explicitly articulated their communal pedigree in “teacher lines” (called nasab al-dīn or nasab al-islām) in Omani literature, and through the structure of their ṭabaqāt/siyar works in North Africa. Appreciating the importance of this communal pedigree, and the nexus of concepts through which it was articulated, helps us to understand the relative lack of emphasis placed on collecting and documenting ḥadīth (Ibāḍīs employ ḥadīth, but they did not use isnāds, nor did they appear to have a ḥadīth collection until the sixth/twelfth century), as well as the general absence of Prophetic biography among them (which also does not appear until the sixth/twelfth century).

Sixty new or updated records of plants species are reported from the Sultanate of Oman, as a result of fieldwork and research undertaken. Five taxa represent new records for Arabia, twenty-seven taxa are new records for Oman, and twenty-eight records represent an extended distribution within Oman. Some previously doubtful records are confirmed. Brief comments are given on the phytogeography, taxonomy and ecology of the taxa. Most new records have been collected in mountainous areas, either in southern Oman or in northern Oman, mainly in areas that previously were botanically poorly known.

A new species of Lavandula (Lamiaceae) is described from the Western Hajar Mountains of Oman. The species is fully described and illustrated. Habitat details and an assessment of its conservation status are provided.

Kaolin deposits >10 m thick overlie unconformably a Mesozoic ophiolite sequence at Jabal Humr, Masirah Island, Oman. The clay's mineralogical and chemical composition, plasticity and moisture content were measured to determine its genesis and suitability for commercial usage. The clay-rich raw material contains 76–94% kaolinite and varying amounts of quartz (micro sheets coating kaolinite) and calcite as well as secondary sulfates. The mode of occurrence, an associated shallow-marine iron oolite/pisolite unit, various secondary minerals which can only form in a gossan environment (oxidation zone of a much older sulfide deposit), and minerals such as gypsum that are highly unstable within a laterite, have led to the conclusion that the Jabal Humr kaolinite deposit cannot have the lateritic origin that has been suggested previously. Rather, it must have formed in a coastal marine environment with a subsequent strong geochemical overprint from the underlying gossan environment, after being enveloped by Tertiary carbonates. A high plasticity and its light colour after firing indicate that this material is suitable for industrial use, especially in pottery. Occasional high contents of up to ∼25% extremely fine-grained quartz (sheet-like, <50 nm thick) reduce the need for quartz addition during the processing for ceramic materials; such natural kaolinite-quartz mixtures already produce a suitable blend of materials. The possible occurrence of spalling during or after firing, caused by the sporadic presence of accessory calcite, can be avoided by by further addition of quartz which leads to the formation of calcium silicate.

The Endangered Arabian tahr Arabitragus jayakari is a rare and little known mountain ungulate, endemic to the 650 km mountain chain of northern Oman and the United Arab Emirates. To investigate the species’ status and distribution we conducted a systematic camera-trap survey across its entire range. We used occupancy modelling to quantify habitat associations and create a predictive distribution model for the species. We found that tahr preferred steep, rugged mountain habitats, and occupancy was much higher in protected areas. Arabian tahr were subject to anthropogenic threats, with occupancy decreasing with closer proximity to villages, and with increasing numbers of domestic goats. Tahr occupancy was also negatively associated with elevation and rainfall, with peak occupancy at 800–1,000 m. Although previous assessments have associated the entire Hajar Mountain range with the Arabian tahr, we found that only 23.9%, or 6,986 km2, of the mountain range was occupied. This reduction in area of occupancy reflects recent population declines, but also our improved methods of assessment. Based on our findings, future conservation efforts should focus on creating more protected areas, control measures to partition goats from core habitats of the Arabian tahr, and restoration and captive reinforcement within suitable habitats unoccupied by Arabian tahr. As infrastructure development is a threat to the Arabian tahr, our occurrence probability map provides a useful tool for spatial planning of developments to reduce impacts on the species.

Speleothems from Hoti Cave in northern Oman provide a record of continental pluvial periods over the last 330,000 yr. Periods of rapid speleothem deposition occurred from 6000 to 10,500, 78,000 to 82,000, 120,000 to 135,000, 180,000 to 200,000, and 300,000 to 330,000 yr ago, with little or no growth during the intervening periods. During each of these five pluvial periods, δD values of water extracted from speleothem fluid inclusions (δD FI) are between −60 and −20‰ (VSMOW) and δ18O values of speleothem calcite (δ18OC) are between −12 and −4‰ to (VPDB). These values are much more negative than modern rainfall (for δD) or modern stalagmites (for δ18O). Previous work on the isotopic composition of rainfall in Oman has shown that northern and southern moisture sources are isotopically distinct. Combined measurements of the δD values of fluid-inclusion water with calculated δ18O values from peak interglacial speleothems indicate that groundwater was predominantly recharged by the southern (Indian Ocean) moisture source, when the monsoon rainfall belt moved northward and reached Northern Oman during each of these periods.

We compared the effectiveness of various methods for surveying medium and large wild mammals in southern Oman. Working with volunteers recruited by Biosphere Expeditions, wildlife professionals and local rangers, we used direct observation, camera traps, sign surveys (tracks and/or dung) and molecular scatology to study 66 sampling units of 2 × 2 km (grid cells) in an area of 32 × 36 km during a 4-week period in February–March 2011. Sixteen mammal species were recorded, and the largest numbers of species were recorded by sign surveys and camera traps (both n = 9); sign surveys, direct sightings and DNA scatology recorded species across the largest number of grid cells. For species with a sample size large enough for comparison (i.e. detected in ≥ 8 grid cells), DNA scatology proved most effective for detecting caracal Caracal caracal, signs for hyaena Hyaena hyaena, ibex Capra nubiana, porcupine Hystrix indica and hyrax Procavia capensis, and signs and direct sightings for mountain gazelle Gazella gazella. Clustering, in which records from multiple methods are either adjacent or overlapping, was highest (≥ 76%) for the wolf Canis lupus, porcupine, ibex and gazelle. Our results indicate the best methods to detect and record the distributions of individual species in the study area, and demonstrate the advantage of using multiple methods to reduce the risk of false absences or partial detections. Our findings also highlight the potential of clustering as a means of cross-checking results of observations that are skill-dependent, which is particularly useful when employing a large workforce.

In 1836, a British naval surgeon named J.G. Hulton collected lexical data on the Jibbali language spoken on the Omani island of Al-Ḥallaniya (Khuriya Muriya). This is the earliest Jibbali data known to have been collected by a European, and remains today the only published data on the dialect of that island. Wolf Leslau analysed this data (BSOAS XII, 1947, pp. 5–19) but Hulton's valuable material can now be reconsidered thanks to recent advances in our understanding of Jibbali and the other Modern South Arabian languages.

Sixty new or updated records of plant species are reported from the Sultanate of Oman, as a result of field work and herbarium research. Four taxa represent new records for Arabia, 26 are new records for Oman, and 30 represent an extended distribution within Oman. Some previously doubtful records are confirmed. Brief comments are given on the phytogeography and ecology of the taxa. Most new records have been made in mountainous areas, either in southern or northern Oman, mostly in areas that previously were botanically very poorly known or unexplored.