Bacillus luciferensis sp. nov., from volcanic soil on Candlemas Island, South Sandwich archipelago. (25/153)

Aerobic, endospore-forming bacteria were found in soil taken from an active fumarole on Lucifer Hill, Candlemas Island, South Sandwich archipelago. Amplified rDNA restriction analysis, SDS-PAGE, repetitive element primed-PCR (rep-PCR) and routine phenotypic tests suggested that six of the isolates represent a novel taxon, and 16S rDNA sequence comparisons support the proposal of a novel species, Bacillus luciferensis sp. nov., the type strain of which is strain LMG 18422(T) (= CIP 107105(T)).  (+info)

Volcanic ash and respiratory symptoms in children on the island of Montserrat, British West Indies. (26/153)

BACKGROUND: In July 1995 the volcano on the West Indian island of Montserrat erupted after being inactive for several hundred years. Since then, clouds of ash have been released intermittently from the volcano. Some of this ash is <10 micro m in diameter and therefore respirable. Concerns were raised that the particles might cause respiratory problems. AIMS: To evaluate whether ashfalls had any effect on the respiratory health of children in Montserrat. METHODS: A survey of asthma diagnoses, respiratory symptoms, exercise induced bronchoconstriction (EIB), and current and previous exposure to volcanic ash was carried out in schools in Montserrat during February 1998. RESULTS: Questionnaire information was available for nearly 80% of the 443 children on the school rolls. The prevalence of wheeze symptoms in the previous 12 months was 18% in children aged 12 years and under and 16% in children aged 13 years and over. In children aged 12 and under, the prevalence of wheeze was greater in those who had ever been heavily or moderately exposed to volcanic ash compared with the group who had only ever been exposed to low levels (wheeze in last 12 months: odds ratio (OR) 4.30; wheeze ever: OR 3.45). The prevalence of EIB in 8-12 year olds was about four times higher in those who were currently heavily exposed to volcanic ash (OR 3.85) compared to those currently exposed to low levels. CONCLUSIONS: Volcanic ash emissions adversely affected the respiratory health of Montserrat children. The findings emphasise the need to limit exposures of children to volcanic ash and ensure the appropriate management of respiratory symptoms.  (+info)

Response of a deciduous forest to the Mount Pinatubo eruption: enhanced photosynthesis. (27/153)

Volcanic aerosols from the 1991 Mount Pinatubo eruption greatly increased diffuse radiation worldwide for the following 2 years. We estimated that this increase in diffuse radiation alone enhanced noontime photosynthesis of a deciduous forest by 23% in 1992 and 8% in 1993 under cloudless conditions. This finding indicates that the aerosol-induced increase in diffuse radiation by the volcano enhanced the terrestrial carbon sink and contributed to the temporary decline in the growth rate of atmospheric carbon dioxide after the eruption.  (+info)

Climate-driven increases in global terrestrial net primary production from 1982 to 1999. (28/153)

Recent climatic changes have enhanced plant growth in northern mid-latitudes and high latitudes. However, a comprehensive analysis of the impact of global climatic changes on vegetation productivity has not before been expressed in the context of variable limiting factors to plant growth. We present a global investigation of vegetation responses to climatic changes by analyzing 18 years (1982 to 1999) of both climatic data and satellite observations of vegetation activity. Our results indicate that global changes in climate have eased several critical climatic constraints to plant growth, such that net primary production increased 6% (3.4 petagrams of carbon over 18 years) globally. The largest increase was in tropical ecosystems. Amazon rain forests accounted for 42% of the global increase in net primary production, owing mainly to decreased cloud cover and the resulting increase in solar radiation.  (+info)

Lunar lava tube radiation safety analysis. (29/153)

For many years it has been suggested that lava tubes on the Moon could provide an ideal location for a manned lunar base, by providing shelter from various natural hazards, such as cosmic radiation, meteorites, micrometeoroids, and impact crater ejecta, and also providing a natural environmental control, with a nearly constant temperature, unlike that of the lunar surface showing extreme variation in its diurnal cycle. An analysis of radiation safety issues on lunar lava tubes has been performed by considering radiation from galactic cosmic rays (GCR) and Solar Particle Events (SPE) interacting with the lunar surface, modeled as a regolith layer and rock. The chemical composition has been chosen as typical of the lunar regions where the largest number of lava tube candidates are found. Particles have been transported all through the regolith and the rock, and received particles flux and doses have been calculated. The radiation safety of lunar lava tubes environments has been demonstrated.  (+info)

Contributions of atmospheric CO and hydrogen uptake to microbial dynamics on recent Hawaiian volcanic deposits. (30/153)

A series of sites were established on Hawaiian volcanic deposits ranging from about 18 to 300 years old. Three sites occurred in areas that supported tropical rain forests; the remaining sites were in areas that supported little or no plant growth. Sites >26 years old consumed atmospheric CO and hydrogen at rates ranging from about 0.2 to 5 mg of CO m(-2) day(-1) and 0.1 to 4 mg of H(2) m(-2) day(-1), respectively. Respiration, measured as CO(2) production, for a subset of the sites ranged from about 40 to >1,400 mg of CO(2) m(-2) day(-1). CO and H(2) accounted for about 13 to 25% of reducing equivalent flow for all but a forested site, where neither substrate appeared significant. Based on responses to chloroform fumigation, hydrogen utilization appeared largely due to microbial uptake. In contrast to results for CO and hydrogen, methane uptake occurred consistently only at the forest site. Increasing deposit age was generally accompanied by increasing concentrations of organic matter and microbial biomass, measured as phospholipid phosphate. Exoenzymatic activities (acid and alkaline phosphatases and alpha- and beta-glucosidases) were positively correlated with deposit age in spite of considerable variability within sites. The diversity of substrates utilized in Biolog Ecoplate assays also increased with deposit age, possibly reflecting changes in microbial community complexity.  (+info)

Transfer factors of radioiodine from volcanic-ash soil (Andosol) to crops. (31/153)

In order to obtain soil-to-plant transfer factors (TFs) of radioiodine from volcanic-ash soil to agricultural crops, we carried out radiotracer experiments. The mean values of TFs (on a wet weight basis) of radioiodine from Andosol to edible parts of crops were as follows: water dropwort, 0.24; lettuce, 0.00098; onion, 0.0011; radish, 0.0044; turnip, 0.0013 and eggplant, 0.00010. The mean value of the TFs of radioiodine for edible parts of wheat (on a dry weight basis) was 0.00015. We also studied the distributions of iodine in crops. There was a tendency for the TFs of leaves to be higher than those of tubers, fruits and grains. A very high TF was found for water dropwort, because this plant was cultivated under a waterlogged condition, in which iodine desorbed from soil into soil solution with a drop in the Eh value. The data obtained in this study should be helpful to assess the long-lived 129I (half life: 1.57 x 10(7) yr) pathway related to the fuel cycle.  (+info)

c-jun mRNA expression and profilin mRNA amplification in rat alveolar macrophages exposed to volcanic ash and sulfur dioxide. (32/153)

Local residents exposed to heavy falls of ash discharged by Mt. Sakurajima, an active volcano, have been reported to develop acute and chronic inflammation of the respiratory tract. The present study aimed to determine the primary cause of this inflammation using an experimental model. Wistar rats were exposed for 5 days (4 h/d) to air containing 100 mg/m3 volcanic ash (mass median aerodynamic diameter, 4.3 microm; geometric standard deviation, 1.7) with or without 1.5 ppm sulfur dioxide (SO2). The lungs were then lavaged, and mRNA was extracted from alveolar macrophages and assessed by reverse transcription-polymerase chain reaction (RT-PCR). In the lavage fluid, no change in cellularity or increase in the content of tumor necrosis factor (TNF)-alpha was detected. However, at 1 h following exposure, 80% of macrophages were seen to have phagocytosed the volcanic ash. This percentage was unchanged at 24 h after exposure. Profilin mRNA content of the macrophages was elevated, and c-jun mRNA was expressed. Alveolar macrophages exposed to volcanic ash and SO2, therefore, are likely to have some inflammatory and fibrogenic potential.  (+info)