Examination of synthetic retinoid -induced apoptosis in cutaneous squamous cell carcinomas: Mechanisms and implications for chemoprevention and chemotherapy with retinoids

Non-melanoma skin cancers, including basal cell carcinoma and squamous cell carcinoma (SCC), are the most common neoplasms in the United States with a lifetime risk nearly equal to all other types of cancer combined. Retinoids are naturally occurring and synthetic analogues of vitamin A that bind to nuclear retinoid receptors and modulate gene expression as a means of regulating cell proliferation and differentiation. Retinoids have been employed for many years in the treatment of various cutaneous lesions and for cancer chemoprevention and therapy. The primary drawback limiting the use of retinoids is their toxicity, which is also associated with receptor-gene interactions. In this study, the effects of the synthetic retinoids N-(4-hydroxyphenyl)retinamide (4HPR) and 6-[3-(1-adamantyl)-4-hydroxyphenyl]-2-naphthalene carboxylic acid (CD437) were examined in cutaneous keratinocytes. Four human cutaneous SCC cell lines were examined along with normal human epidermal keratinocyte (NHEK) cells from two donors. Sensitivity to 4HPR or CD437 alone or in combination with other agents was determined via growth inhibition, cell cycle distributions, or apoptosis induction. Both synthetic retinoids were able to promote apoptosis in SCC cells more effectively than the natural retinoid all-trans retinoic acid. Apoptosis could not be inhibited by nuclear retinoic acid receptor antagonists. In NHEK cells, 4HPR induced apoptosis while CD437 promoted G1 arrest. 4HPR acted as a prooxidant by generating reactive oxygen species (ROS) in SCC and NHEK cells. 4HPR-induced apoptosis in SCC cells could be inhibited or potentiated by manipulating cellular defenses against oxidative stress, indicating an essential role for ROS in 4HPR-induced apoptosis. CD437 promoted apoptosis in SCC cells in S and G2/M phases of the cell cycle within two hours of treatment, and this rapid induction could not be blocked with cycloheximide. This study shows: (1) 4HPR- and CD437-induced apoptosis do not directly involve a traditional retinoid pathway; (2) 4HPR can act as a prooxidant as a means of promoting apoptosis; (3) CD437 induces apoptosis in SCC cells independent of protein synthesis and is potentially less toxic to NHEK cells; and (4) 4HPR and CD437 operate under different mechanisms with respect to apoptosis induction and this may potentially enhance their therapeutic index in vivo. ^

Prevalence and risk factors of asthma and work -related asthma among U.S. adults: Data from the Third National Health and Nutrition Examination Survey, 1988--1994

This cross-sectional analysis of the data from the Third National Health and Nutrition Examination Survey was conducted to determine the prevalence and determinants of asthma and wheezing among US adults, and to identify the occupations and industries at high risk of developing work-related asthma and work-related wheezing. Separate logistic models were developed for physician-diagnosed asthma (MD asthma), wheezing in the previous 12 months (wheezing), work-related asthma and work-related wheezing. Major risk factors including demographic, socioeconomic, indoor air quality, allergy, and other characteristics were analyzed. The prevalence of lifetime MD asthma was 7.7% and the prevalence of wheezing was 17.2%. Mexican-Americans exhibited the lowest prevalence of MD asthma (4.8%; 95% confidence interval (CI): 4.2, 5.4) when compared to other race-ethnic groups. The prevalence of MD asthma or wheezing did not vary by gender. Multiple logistic regression analysis showed that Mexican-Americans were less likely to develop MD asthma (adjusted odds ratio (ORa) = 0.64, 95%CI: 0.45, 0.90) and wheezing (ORa = 0.55, 95%CI: 0.44, 0.69) when compared to non-Hispanic whites. Low education level, current and past smoking status, pet ownership, lifetime diagnosis of physician-diagnosed hay fever and obesity were all significantly associated with MD asthma and wheezing. No significant effect of indoor air pollutants on asthma and wheezing was observed in this study. The prevalence of work-related asthma was 3.70% (95%CI: 2.88, 4.52) and the prevalence of work-related wheezing was 11.46% (95%CI: 9.87, 13.05). The major occupations identified at risk of developing work-related asthma and wheezing were cleaners; farm and agriculture related occupations; entertainment related occupations; protective service occupations; construction; mechanics and repairers; textile; fabricators and assemblers; other transportation and material moving occupations; freight, stock and material movers; motor vehicle operators; and equipment cleaners. The population attributable risk for work-related asthma and wheeze were 26% and 27% respectively. The major industries identified at risk of work-related asthma and wheeze include entertainment related industry; agriculture, forestry and fishing; construction; electrical machinery; repair services; and lodging places. The population attributable risk for work-related asthma was 36.5% and work-related wheezing was 28.5% for industries. Asthma remains an important public health issue in the US and in the other regions of the world. ^

Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B

Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited spatial coverage in the circum-Antarctic region. This shortcoming is partially addressed by comparing patterns of carbonate sedimentation at the Site 690 PETM reference section to those herein reconstructed for nearby Site 689. Biochemostratigraphic correlation of the two records reveals that the first ~36 ka of the carbon isotope excursion (CIE) signaling PETM conditions is captured by the Site 689 section, while the remainder of the CIE interval and nearly all of the CIE recovery are missing due to a coring gap. A relatively expanded stratigraphy and higher carbonate content at mid-bathyal Site 689 indicate that dissolution was less severe than at Site 690. Thus, the bathymetric transect delimited by these two PETM records indicates that the lysocline shoaled above Site 689 (~1,100 m) while the calcite compensation depth remained below Site 690 (~1,900 m) in the Weddell Sea region. The ensuing recovery of carbonate sedimentation conforms to a bathymetric trend best explained by gradual lysocline deepening as negative feedback mechanisms neutralized ocean acidification. Further, biochemostratigraphic evidence indicates the tail end of the CIE recovery interval at both sites has been truncated by a hiatus most likely related to vigorous production and advection of intermediate waters.

Results of micropaleontological examination and age of dredge samples collected from the lower slopes of the Kuril Basin, Sea of Okhotsk

An integrated (petrographical and micropaleontological) study of sedimentary cover samples dredged from the lower slopes of the Kuril deep-sea basin was carried out. Pliocene-Pleistocene sediments are mainly represented by tuffaceous sedimentary rocks (tuffites, tuffaceous muds, tuffaceous diatomites, tuffaceous silts, tuffaceous sandstones, etc.). Significant admixtures of pyroclastic matter, especially of volcanic glasses, indicates that sedimentation process was accompanied by explosive volcanism. The data obtained give evidence about intensification of tectonomagmatic regime within the region under study during Pliocene-Pleistocene time. By the beginning of Pliocene, a deep-sea basin with a well-manifested continental and/or island slope and a narrow shelf already existed. Pliocene-Pleistocene deposits accumulated in a cold well-aerated deep-sea basin under oxic conditions and downslope sediment transport.