Far infrared maps of the ridge between OMC-1 and OMC-2

Dust continuum emission from a 6 ft x 20 ft region surrounding OMC-1 and OMC-2 were mapped at 55 and 125 microns with 4 ft resolution. The dominant features of the maps are a strong peak at OMC-1 and a ridge of lower surface brightness between OMC-1 and OMC-2. Along the ridge the infrared flux densities and the color temperature decreases smoothly from OMC-1 to OMC-2. OMC-1 is heated primarily by several optical and infrared stars situated within or just at the boundary of the cloud. At the region of minimum column density between OMC-1 and OMC-2 the nearby B0.5 V star NU Ori may contribute significantly to the dust heating. Near OMC-2 dust column densities are large enough so that, in addition to the OMC-2 infrared cluster, the nonlocal infrared sources associated with OMC-1 and NU Ori can contribute to the heating

Far infrared and submillimeter brightness temperatures of the giant planets

The brightness temperatures of Jupiter, Saturn, Uranus, and Neptune in the range 35 to 1000 micron. The effective temperatures derived from the measurements, supplemented by shorter wavelength Voyager data for Jupiter and Saturn, are 126.8 + or - 4.5 K, 93.4 + or - 3.3 K, 58.3 + or - 2.0 K, and 60.3 + or - 2.0 K, respectively. The implications of the measurements for bolometric output and for atmospheric structure and composition are discussed. The temperature spectrum of Jupiter shows a strong peak at approx. 350 microns followed by a deep valley at approx. 450 to 500 microns. Spectra derived from model atmospheres qualitatively reproduced these features but do not fit the data closely

Submarine landslides on the upper southeast Australian passive continental margin – preliminary findings

The southeast Australian passive continental margin is narrow, steep and sediment-deficient, and characterized by relatively low rates of modern sedimentation. Upper slope (\u3c1200m) sediments comprise mixtures of calcareous and terrigenous sand and mud. Three of twelve sediment cores recovered from geologically-recent, submarine landslides located offshore New South Wales/Queensland (NSW/QLD) are interpreted to have sampled failure surfaces at depths of between 85 cm and 220 cm below the present-day seabed. Differences in sediment physical properties are recorded above and below the three slide-plane boundaries. Sediment taken directly above the inferred submarine landslide failure surfaces and presumed to be post-landslide, returned radiocarbon ages of 15.8 ka, 20.7 ka and 20.1 ka. The last two ages correspond to adjacent slide features, which are inferred to be consistent with their being triggered by a single event such as an earthquake. Slope stability models based on classical soil mechanics and measured sediment shearstrengths indicate that the upper slope sediments should be stable. However, multibeam sonar data reveal that many upper slope landslides occur across the margin and that submarine landsliding is a common process. We infer from these results that: a) an unidentified mechanism regularly acts to reduce the shear resistance of these sediments to the very low values required to enable slope failure, and/or b) the margin experiences seismic events that act to destabilise the slope sediments

The global dynamics of RNA stability orchestrates responses to cellular activation

Transcriptomics is used to quantify changes in accumulated levels of mRNAs following cellular activation. These changes arise from the opposing fluxes of transcription and mRNA decay, both of which affect the functional dynamics of global gene expression. A study published recently in BMC Genomics focuses on the contribution made by mRNA stability in shaping the kinetics of gene responses in mammalian cells

Knowledge, attitudes, and practices of Australian oncology health professionals on complementary medicines

Background: Approximately half of people with cancer are using complementary and alternative medicine (CAM), presenting safety concerns due to potential interactions with conventional cancer treatment. Oncology staff have a role to play in ensuring the safe use of CAMs and so, this study examined their knowledge, attitudes, and practices regarding CAMs. Aim: This study aimed to assess the knowledge, attitudes, and practices of Australian doctors, nurses, and pharmacists regarding CAM use in oncology. Method: Members of three national oncology professional associations took part in an online questionnaire, which determined their knowledge, attitudes, and practices regarding CAM. Results: Ninety-nine completed surveys were obtained from nine doctors, 70 nurses, and 20 pharmacists. Most respondents (68.4%) felt that they did not have adequate knowledge of CAMs to respond to patients' questions. Assessment of attitudes found respondents generally believed that CAMs have a complementary role in oncology but indicated their concerns for the safety of patients. Respondents indicated in practice they would discuss CAMs with less than half of patients (40.6%), with a lack of scientific data and guidelines for CAM use presenting significant barriers to these discussions. Conclusion: Our study suggests that oncology health professionals' knowledge of CAMs potentially leads to a lack of confidence in providing advice to patients and concerns for patient safety. This impacts their discussion of CAMs and lack of disclosure from patients about their use of CAMs. Education on CAMs in oncology would assist in increasing professionals' confidence in discussing these therapies, leading to increased patient disclosure of CAMs and safer treatment decision making for people with cancer

Perspectives of Complementary and Alternative Medicine use by cancer patients in a regional hospital in North Queensland, Australia

Objectives: This study aimed to investigate CAMs used, and reasons for and disclosure of this use by cancer patients in a regional hospital in North Queensland, Australia. Methods: Patients attending the Day Oncology Unit of the Townsville University Hospital were invited to participate in a self-completed questionnaire or telephone interview regarding perspectives of their CAM use. Data were analysed using descriptive statistics and chi-squared and independent t-tests were performed to allow comparison between the responses by CAM users and non-users. Results: 102 completed questionnaires were used in the analysis, where 40.2 % of respondents were found to be using some form of CAM. Cannabis, magnesium, and massage were the most prominent therapies used, with cannabis use in cancer, not commonly reported in prior literature. The main reasons given for using CAM were to treat symptoms of cancer, side-effects of treatment or to improve general health. Two-thirds of these respondents disclosed their CAM use to health professionals mostly to obtain a professional opinion or due to concerns of interactions with cancer treatment. CAM users were statistically more likely to have used CAM prior to their cancer diagnosis and have lower emotional wellbeing than non-users. Non-CAM users indicated that a lack of knowledge of CAM or concerns regarding interactions with cancer treatment were the most popular reasons for not adopting these therapies. Conclusion: While lower than the averages of previously published CAM use, our study highlights that there is still a significant group of cancer patients in the North Queensland region using CAMs

Bipartite Anterior Extraperitoneal Teratoma: Evidence for the Embryological Origins of Teratomas?

Teratomas are thought to arise from totipotent primordial germ cells (PGCs) Dehner (1983) which may miss their target destination Moore and Persaud (1984). Teratomas can occur anywhere from the brain to the coccygeal area but are usually in the midline close to the embryological position of the gonadal ridges Bale (1984), Nguyen and Laberge (2000). We report a case of a bipartite anterior extraperitoneal teratoma. This is an unusual position for a teratoma, but one which may support the “missed target” theory of embryology