In many regions of Canada, knowledge of the distribution of insect species is far from complete. This knowledge gap, known as the Wallacean Shortfall, is often manifest by species records separated by large, often remote areas with no records. Paradoxically, these difficult-to-access areas offer the best opportunity to study unaltered native community assemblages. Such gaps in knowledge are exemplified by ground beetles, a well-known group, yet with record gaps in many unstudied areas of Canada, including Akimiski Island, Nunavut. This postglacial rebound island, located in James Bay, has no permanently occupied human dwellings and almost no human-altered habitat. Using a combination of pitfall-malaise traps, pitfall traps, and hand captures during 2008–2014, we collected 1368 ground beetles (Coleoptera: Carabidae) as part of a larger biodiversity survey. We identified 31 species, 29 of which were first territorial records for Nunavut. Our results almost double the number of Carabidae known from Nunavut and extend the known range of eight other species. Seventeen of the species that we caught cannot fly, evidence for colonists arriving on Akimiski on floating debris. Our study fills substantial range gaps and serves as baseline information to detect future change.

The possibility of site-selective substitution of 18O into YBa2Cu3O7 was explored. Samples containing various quantities of 18O were prepared by processing in 18O2 both at 950 °C and at 400 °C. The samples were characterized by secondary ion mass spectroscopy (SIMS), temperature programmed desorption (TPD) and reduction (TPR), Raman spectroscopy, and magnetization measurements. Measurements of the shifts in the Raman active modes with 18O substitution and of the ratios of 18O to 16O by TPD, TPR, and SIMS show that even for temperatures as low as 400 °C and times as short as 2 h. 18O is not substituted exclusively into the chain site (O1) in YBa2Cu3O7. In addition, there is no consistent variation in the shifts in Tc with the degree of substitution; therefore, the isotope effect for a sample with 100% 18O cannot be predicted by a linear extrapolation of data obtained for samples with partial 18O substitution. The mechanism of oxygen substitution, the difficulties of measuring the true magnitude of the oxygen isotope shift, and the meaning of the small isotope shift are discussed.

Microbiology laboratories in Oregon were surveyed in 1981 to determine how often methicillin-resistant Staphylococcus aureus (MRSA) was being reported to physicians in the state. Results of this survey were surprising in three respects. First, the mean percent of S. aureus isolates reported by laboratories as methicillin-resistant was 8.3%. Second, a significant inverse correlation was found between the percent of reported MRSA and laboratory size (p=0.0001). Finally, laboratories which retested initially resistant isolates reported significantly less MRSA (mean 3.3%, median 1%) than those laboratories which accepted initial results (mean 20%, median 12%) (p=0.0001). Independent testing by the Centers for Disease Control of isolates reported to be MRSA confirmed that some misideiitification was occurring. Participating laboratories were notified of our initial findings and their potentially serious clinical ramifications. Laboratories were resurveyed in 1982, and a significant decrease in the reported MRSA to a mean percentage of 3.4% was observed (p=<0.002). It is unlikely that this situation is unique to Oregon, and similar misreporting of MRSA to physicians in other areas of the country may be compromising the safe and effective treatment of S. aureus infections.