Hot Sulphur Springs Research Articles

Application of otolith morphometrics in delineating population structure of Aphaniops stoliczkanus (Teleostei: Aphaniidae) in southern Iranian waters

AbstractWidely distributed Species in different geological and ecological environments often exhibit great intraspecific diversity. Aphaniops stoliczkanus (Day, 1872) is an endemic species of Middle East occurring over a vast geographic range in different basins. This species has been observed in freshwater, brackish water and hot sulphur springs; therefore, its populations are known to exhibit considerable morphological variation. In the present study, we have investigated the poorly studied populations of A. stoliczkanus of the Hormuz and Makran basins of Iran in terms of otolith morphology and morphometrics. According to the results, these populations can be divided into two distinct groups including east and west of the Strait of Hormuz. Our results also provide evidence that there is a relationship between otolith morphology and the environment, serving as environmental factors that may influence the formation of specific regions in the otolith shape. Despite the remarkable morphological similarities among otoliths in geographically close populations of Charak and Chiruyeh, our data purposed that geographically these populations have different dorsal tip shapes in their otolith. In comparison to the data from other studies, the otoliths of Qeshm Island appear to resemble the overall shape of otolith found in Oman very closely. However, it is believed that Qeshm Island population was separated from the Hormuz basin populations during the Holocene Sea level rise. Also, the outcomes of this study provide insights into the potential role of environmental factors in shaping intraspecific diversity and the migration patterns of this species within the Persian Gulf.

Contribution to a Sustainable Society: Biosorption of Precious Metals Using the Microalga Galdieria.

The red microalga Galdieria sp. is an extremophile that inhabits acidic hot sulphur springs and grows heterotrophically to a high cell density. These characteristics make Galdieria suitable for commercial applications as stable mass production is the key to success in the algae business. Galdieria has great potential as a precious metal adsorbent to provide a sustainable, efficient and environmentally benign method for urban mining and artisanal small-scale gold mining. The efficiency and selectivity in capturing precious metals, gold and palladium from metal solutions by a Galdieria-derived adsorbent was assessed relative to commercially used adsorbents, ion exchange resin and activated charcoal. As it is only the surface of Galdieria cells that affect metal adsorption, the cell content was analysed to determine the manner of utilisation of those metabolites. Galdieria was shown to be protein-rich and contain beneficial metabolites, the levels of which could shift depending on the growth conditions. Separating the cell content from the adsorbent could improve the adsorption efficiency and reduce CO2 emissions during the metal collection process. The commercial applications of Galdieria appear promising: growth is quick and dense; the precious metal adsorption capacity is highly efficient and selective in acidic conditions, especially at low metal concentrations; and the cell content is nutrient-rich.

Characterization of MspNI (G/GWCC) and MspNII (R/GATCY), novel thermostable Type II restriction endonucleases from Meiothermus sp., isoschizomers of AvaII and BstYI

MspNI and MspNII, isoschizomers of prototype Type II restriction endonucleases AvaII and BstYI, were extracted from an extreme thermophile bacterium belonging to the genus Meiothermus, isolated from the hot sulphur springs in north Himalayan region of India where temperature and pH ranged from 60 to 80°C and 7.5 to 8.5, respectively. The two enzymes were purified to homogeneity using Cibacron-Blue 3GA Agarose, Q-Sepharose and SP-Sepharose chromatography and were homodimers with subunit molecular weights of 27 and 45kDa, respectively. Restriction mapping and run-off sequencing of MspNI and MspNII cleaved pBR322 DNA showed that they recognized and cleaved 5'-G/GWCC-3' and 5'-R/GATCY-3' sites, respectively. MspNI and MspNII worked optimally at 60 and 70°C, 6 and 5mM MgCl(2), respectively and showed no star activity in organic solvents. Both were resistant to sequence methylation and were stable up to 25 PCR cycles.

Gill Ectoparasites of Juvenile Rainbow Trout and Brown Trout in the Upper Colorado River

Abstract During 1996 and 1997, 112 rainbow trout Oncorhynchus mykiss and 204 brown trout Salmo trutta, all young of the year, were sampled from a 40-km study area of the upper Colorado River and were examined for gill parasites. Ambiphrya, Chilodonella, Ichthyobodo, Apiosoma, Trichodina, Trichodinella, Tripartiella, Epistylis, and an unidentified cochliopodid amoeba were the representative protozoan genera observed on fish examined. Significant month–year–species interactions (P = 0.0295) were revealed, reflecting the changes in infestation prevalence among months, years, and species of salmonid. Greater ectoparasite richness was observed in downstream sections of the study area, most notably near Hot Sulphur Springs, Colorado. Peaks of infestation intensity and ectoparasite richness occurred in August and September of both years, presumably because of high mean water temperatures and low flows during that time.

Cryptoendolithic growth of the red alga Galdieria sulphuraria in volcanic areas

The habitat of the acido- and thermophilic red algae Galdieria sulphuraria and Cyanidium caldarium was examined in acidic hot sulphur springs in the vicinity of Naples (Italy). These species grew on soil and rocks, but a large part of the populations was cryptoendolithic. The endolithic algal layer (1–3 mm in thickness) was covered by amorphous silica (1–2 mm in thickness) containing traces of hydrotroilite (FeS.nH2O) and elemental sulphur. Organotrophic bacteria and fungi were not found in the algal layer. Light penetration measurements showed that 0·1–1% of the sunlight reached the upper part of the algal layer. Thus, low-light-adapted algae should be able to perform some photosynthesis in this endolithic habitat. Under conditions where light is even more limited, e.g. in winter or after darkening of the covering layer, many of the cells might not survive. Aqueous extracts of these algae are excellent growth substrates for Galdieria sulphuraria. Therefore, we propose that compounds released from dead cells in the endolithic layer are used by the surrounding Galdieria cells for heterotrophic metabolism. This would increase their chance of surviving prolonged periods under detrimental conditions.

Cryptoendolithic growth of the red alga Galdieria sulphuraria in volcanic areas

The habitat of the acido- and thermophilic red algae Galdieria sulphuraria and Cyanidium caldarium was examined in acidic hot sulphur springs in the vicinity of Naples (Italy). These species grew on soil and rocks, but a large part of the populations was cryptoendolithic. The endolithic algal layer (1–3 mm in thickness) was covered by amorphous silica (1–2 mm in thickness) containing traces of hydrotroilite (FeS.nH2O) and elemental sulphur. Organotrophic bacteria and fungi were not found in the algal layer. Light penetration measurements showed that 0·1–1% of the sunlight reached the upper part of the algal layer. Thus, low-light-adapted algae should be able to perform some photosynthesis in this endolithic habitat. Under conditions where light is even more limited, e.g. in winter or after darkening of the covering layer, many of the cells might not survive. Aqueous extracts of these algae are excellent growth substrates for Galdieria sulphuraria. Therefore, we propose that compounds released from dead cells in the endolithic layer are used by the surrounding Galdieria cells for heterotrophic metabolism. This would increase their chance of surviving prolonged periods under detrimental conditions.

Sources and biochemical composition of suspended particulate material in a submarine cave with sulphur water springs

Sources, biochemical composition and nutritional value of suspended particulate material were investigated from February 1994 to February 1995 in a submarine cave (Grotta Azzurra, Capo Palinuro, southwestern Italy) with hot sulphur springs and associated mats of chemolithoautotrophic bacteria in its innermost dark part (Snow Hall). Concentrations of total suspended material (TSM), particulate inorganic material (PIM), organic carbon (POC), organic nitrogen (PON), chlorophyll a (Chl a), phaeopigments (Phaeo), carbohydrates (TCH), proteins (TPR) and lipids (TLI) were measured at four stations along an outside–inside transect, in order to address whether the quantity and quality of suspended particles varied over time with increasing distance from the entrance of the cave and estimate the relative contribution of chemosynthesis versus photosynthesis in supplying POC to cave heterotrophs. The abundance and biochemical composition of suspended material available to filter-feeders varied over time, but no significant quantitative or qualitative differences were detected along the outside–inside transect. Concentrations of TSM and of its different compounds (PIM, POC, PON, Phaeo, TCH, TPR, TLI) were homogeneous among the four stations or fluctuated without any consistent trend, with no apparent ageing and degradation of organic material in the innermost dark station. Conversely, concentrations of Chl a significantly decreased from outside to inside the cave at all sampling periods. It is suggested that suspended POC in Grotta Azzurra consists of mixed assemblages of particles coming from advection of photosynthetic material from the open sea and local inputs of carbon by sulphur-oxidizing bacteria. Based on POC/Chl a ratios, the relative contributions of chemosynthesis versus photosynthesis in supplying POC to benthic heterotrophs was estimated to be 31 and 69%, respectively.

The regional effects of the effluents from the Mishraq sulphur mines in Iraq on the hydrological system

ABSTRACT Sulphur is mined at Mishraq near Mosul, Iraq, by the injection of superheated water. The production area is adjacent to and in contact with the River Tigris. With time an increasing number of hot sulphur springs have erupted in and near the river. Geological and hydrological studies have shown that faults, fractures and cavities in the predominantly limestone rocks increase the hydraulic conductivity and seepage coefficient. The most effective method of controlling the large-scale flow of sulphur into the river was by pumping a barrier of cold water into observation wells bored into areas of high hydraulic conductivity, in order to solidify the sulphur.

Radioactivity of rivers and lakes in parts of Garland and Hot Spring counties, Arkansas

A wide range of radon content in surface waters was noted incidental to studies of radon in spring and well waters of Hot Springs and Potash Sulphur Springs, Garland County, Arkansas. Subsequently a reconnaissance survey of radioactivity of nearby streams and lakes showed the radon contents of streams range from 0.0084 to 1.07 millimicrocuries per liter of water, and those of lakes range from less than 0.001 to 0.123 millimicrocuries. Streams flowing over Ordovician black shales contained an average of 0.275 millimicrocurie radon per liter of water. Those flowing over black Stanley shale of Mississippian age contained an average of 0.046 millimicrocurie radon per liter of water.The radon content in Potash Sulphur Creek where it flows over the uranium-bearing rocks of the Potash Sulphur Springs syenite complex ranged from 0.09 to 3.16 millimicrocuries per liter of water. Ground water in a drill hole in uranium-bearing rock contained an average of 58.75 millimicrocuries per liter of water. Waters from small springs were shown to lose as much as 41.3 percent of total radon content in the first 4 feet of surface flow below the point of emergence. The methods of radon determination in the field are believed applicable to prospecting for low-grade uraniferous deposits, especially in black shale areas, in areas of heavy overburden, and in areas of saturation by ground water where ordinary detection devices may be somewhat limited.