scholarly journals Assessment of the content of biogenic elements in the evaporation pond of the “Caspi Bitum” plant

2021 ◽  
Vol 69 (4) ◽  
Author(s):  
G. Zh. Kenzhetaev ◽  
S. Syrlybekkyzy ◽  
L J Taizhanova ◽  
I I Kirvel ◽  
J K Altybaeva
Keyword(s):  
Biogenic Elements ◽  
Evaporation Pond

Mars: was There an Ancient Eden?

1997 ◽  
Vol 161 ◽  
pp. 203-218 ◽  
Author(s):  
Tobias C. Owen
Keyword(s):  
Positive Answer ◽  
Biogenic Elements ◽  
Habitable Zones ◽  
The Face ◽  
The Origin Of Life ◽  
Early Mars ◽  
Favorable Conditions ◽  
Open Question ◽  
Rocky Planets ◽  
Impact Erosion

AbstractThe clear evidence of water erosion on the surface of Mars suggests an early climate much more clement than the present one. Using a model for the origin of inner planet atmospheres by icy planetesimal impact, it is possible to reconstruct the original volatile inventory on Mars, starting from the thin atmosphere we observe today. Evidence for cometary impact can be found in the present abundances and isotope ratios of gases in the atmosphere and in SNC meteorites. If we invoke impact erosion to account for the present excess of129Xe, we predict an early inventory equivalent to at least 7.5 bars of CO2. This reservoir of volatiles is adequate to produce a substantial greenhouse effect, provided there is some small addition of SO2(volcanoes) or reduced gases (cometary impact). Thus it seems likely that conditions on early Mars were suitable for the origin of life – biogenic elements and liquid water were present at favorable conditions of pressure and temperature. Whether life began on Mars remains an open question, receiving hints of a positive answer from recent work on one of the Martian meteorites. The implications for habitable zones around other stars include the need to have rocky planets with sufficient mass to preserve atmospheres in the face of intensive early bombardment.

Analytical Electron Microscopy of Extraterrestrial Ice Analogs

1990 ◽  
Vol 48 (1) ◽  
pp. 594-595
Author(s):  
D.F. Blake ◽  
LJ. Allamandola ◽  
G. Palmer ◽  
A. Pohorille
Keyword(s):  
Solar System ◽  
Analytical Electron Microscopy ◽  
Biogenic Elements ◽  
Widespread Occurrence ◽  
Interstellar Ice ◽  
Analytical Electron ◽  
History Of ◽  
Interstellar Material ◽  
Astrophysical Ices ◽  
Interstellar Molecular Clouds

The natural history of the biogenic elements H, C, N, O, P and S in the cosmos is of great interest because it is these elements which comprise all life. Material ejected from stars (or pre-existing in the interstellar medium) is thought to condense into diffuse bodies of gravitationally bound gas and dust called cold interstellar molecular clouds. Current theories predict that within these clouds, at temperatures of 10-100° K, gases (primarily H2O, but including CO, CO2, CH3OH, NH3, and others) condense onto submicron silicate grains to form icy grain mantles. This interstellar ice represents the earliest and most primitive association of the biogenic elements. Within these multicomponent icy mantles, pre-biotic organic compounds are formed during exposure to UV radiation. It is thought that icy planetesimals (such as comets) within our solar system contain some pristine interstellar material, including ices, and may have (during the early bombardment of the solar system, ∼4 Ga) carried this material to Earth.Despite the widespread occurrence of astrophysical ices and their importance to pre-biotic organic evolution, few experimental data exist which address the relevant phase equilibria and possible structural states. A knowledge of the petrology of astrophysical ice analogs will allow scientists to more confidently interpret astronomical IR observations. Furthermore, the development and refinement of procedures for analyzing ices and other materials at cryogenic temperatures is critical to the study of materials returned from the proposed Rosetta comet nucleus and Mars sample return missions.

The Influence of Phytoplankton Primary Production on the Cycle of Biogenic Elements in the Coastal Waters off Sevastopol, Black Sea

2018 ◽  
Vol 44 (3) ◽  
pp. 240-247 ◽  
Author(s):  
V. N. Egorov ◽  
V. N. Popovichev ◽  
S. B. Gulin ◽  
N. I. Bobko ◽  
N. Yu. Rodionova ◽  
...  
Keyword(s):  
Primary Production ◽  
Black Sea ◽  
Coastal Waters ◽  
Biogenic Elements ◽  
Phytoplankton Primary Production

scholarly journals Extremely Halophilic Biohydrogen Producing Microbial Communities from High-Salinity Soil and Salt Evaporation Pond

Fuels ◽  
2021 ◽  
Vol 2 (2) ◽  
pp. 241-252
Author(s):  
Dyah Asri Handayani Taroepratjeka ◽  
Tsuyoshi Imai ◽  
Prapaipid Chairattanamanokorn ◽  
Alissara Reungsang
Keyword(s):  
Microbial Communities ◽  
High Throughput ◽  
High Throughput Sequencing ◽  
High Salinity ◽  
Amplicon Sequencing ◽  
Spatial Proximity ◽  
Lignocellulosic Waste ◽  
Evaporation Pond ◽  
Operational Taxonomic Units ◽  
Determining Factor

Extreme halophiles offer the advantage to save on the costs of sterilization and water for biohydrogen production from lignocellulosic waste after the pretreatment process with their ability to withstand extreme salt concentrations. This study identifies the dominant hydrogen-producing genera and species among the acclimatized, extremely halotolerant microbial communities taken from two salt-damaged soil locations in Khon Kaen and one location from the salt evaporation pond in Samut Sakhon, Thailand. The microbial communities’ V3–V4 regions of 16srRNA were analyzed using high-throughput amplicon sequencing. A total of 345 operational taxonomic units were obtained and the high-throughput sequencing confirmed that Firmicutes was the dominant phyla of the three communities. Halanaerobium fermentans and Halanaerobacter lacunarum were the dominant hydrogen-producing species of the communities. Spatial proximity was not found to be a determining factor for similarities between these extremely halophilic microbial communities. Through the study of the microbial communities, strategies can be developed to increase biohydrogen molar yield.

Protein-mediated selenium biomethylation in evaporation pond water

1990 ◽  
Vol 9 (12) ◽  
pp. 1453-1462 ◽  
Author(s):  
E. T. Thompson-Eagle ◽  
W. T. Frankenberger
Keyword(s):  
Pond Water ◽  
Evaporation Pond

The structure and diversity of microbiomes of glacial cryoconites (North Caucasus Region)

2021 ◽  
Author(s):  
Ekaterina Ivanova ◽  
Grigory Gladkov ◽  
Anastasiia Kimeklis ◽  
Arina Kichko ◽  
Evgeny Andronov ◽  
...  
Keyword(s):  
Microbial Biomass ◽  
Microbial Consortia ◽  
Biogenic Elements ◽  
Biomass Estimation ◽  
Taxonomic Structure ◽  
Rrna Gene ◽  
North Caucasus ◽  
Vegetative Cover ◽  
Glacier Surface ◽  
Amino Acid Synthesis

<p>Studying the diversity and abundance of cryoconite biota is relevant due to global climate warming, since organo-mineral particles in their composition have a significant impact on the ice albedo decrease and, thus, increase the rate of glacier melting. Since cryoconites are "hot spots" for biota development and the only loci where soil-like bodies can form on glaciers, they contribute significantly to the cycles of biogenic elements of ice and oligotrophic ecosystems.</p><p>Samples were collected from cryoconites from the Garabashi (GBg_c) and Shkhelda (SHKg_c) glaciers as well as from moraine (Garabashi); nearby soils (Chernozem, Forest-meadow, and organo-accumulative soil) were used as controls.</p><p>GBg_c samples were characterized by potentially higher values of microbial biomass (abundance of 16 S rRNA gene copies and ITS), with maximal values in samples taken from the cracked glacier. In contrast, minimal abundance values of the studied taxonomic markers in SHKg_c were determined. The values for the samples of nearby soils occupied an intermediate position. These results may be partially explained by different colors of cryoconites, determined by differences in their biochemical composition and origin: the GBg_c were represented by "black dust", with low values of albedo and, accordingly, higher values of temperature and moisture, apparently, more favorable for microbial activity compared to the "gray" dust of the SHKg_c.</p><p>Taxonomic structure analysis revealed a specific pattern of GBg_c samples– an oligotrophic psychrophilic community with a pronounced cyanobacterial dominance was detected. Despite significant differences between cryoconites and nearby moraine in the presence of major autotrophic representatives (cyanobacteria Tychonema, Phormidesmis), the heterotrophic component is similar and is represented by a very specific set of soil microorganisms of Bacteroides, Shingomonas, Burkholderiales groups, apparently, due to the flushing out of part of the microbiome from the autotrophic microbial consortia of the glacier, explaining, as well, the grouping of these samples in the Bray-Curtis NMDS ordination. No autotrophic microbiota predominance was detected in SHKg_c, these microbiomes were typical for soils without vegetative cover, as well as without biofilms on the surface (Verrucromicrobia, Sphingomonacia, Bacteroides). A low number of phylotypes was detected for the community of the GBg_c and Сhernozem. Moreover, the alpha-diversity indices were inversely proportional to the results of microbial biomass estimation, which can be explained by greater "homogeneity" (and, apparently, narrower functional specialization) of more numerous communities.</p><p>The metabolic profile of cryoconites (according to Picrust2) is characterized by the predominance of aerobic metabolic enzymes (cytochrome c) and proteins (amino acid synthesis), indicating a potentially high level of metabolic activity of the cryoconite microbial community. These results can be explained by the reparative needs of microbial cells under the conditions of oxygenic stress and extremely low temperatures. In contrast to the control soils (especially, Chernozem), relatively low levels of the catalytic pathway and carbon exchange were determined for the cryoconites’ metabolic pathways, possibly associated with both low available carbon stocks and supply of the glacier surface, as compared to soils with higher stocks of available forms of mineral nutrition.</p><p>The work is supported by RFBR  project No 19-05-50107. </p>

Effects of glycine–metal compounds onAscaridia galli-infected chickens expressed by a kinetic model

2004 ◽  
Vol 78 (1) ◽  
pp. 25-32 ◽  
Author(s):  
M. Gabrashanska ◽  
S.E. Teodorova ◽  
M. Galvez-Morros ◽  
M. Mitov
Keyword(s):  
Body Weight Gain ◽  
Biogenic Elements ◽  
Model Parameters ◽  
Ascaridia Galli ◽  
Mineral Deficiency ◽  
Metal Compounds ◽  
High Infection ◽  
Gain Reduction ◽  
Reduction Of Mortality ◽  
Host Parasite

AbstractThe biogenic elements zinc, manganese and cobalt are essential for metabolic processes in animals. Compounds of nGly.Me2+A. mH2O (Me2+=Zn2+, Mn2+, Co2+; A=Cl−, SO42−, n=1, 2; m=2, 5), as supplements in the diet, were used separately on different experimental groups of male Hisex chickens to correct the mineral deficiency caused byAscaridia galliinfections. An amelioration of body weight gain, reduction of mortality and restoration of trace element levels were estimated in infected chickens. A mathematical model has been proposed forA. gallipopulation kinetics in chickens, taking into account the stimulating effect of these elements on the nematodes. The model parameters are considered as phenomenological constants of the host–parasite system. An agreement with experimental data is observed using, for the parametersψ,α,μandμs, values equal to those calculated in previously investigatedA. galli–chicken systems. For parameterν(immunological constant) the same value was obtained as in a previous experiment with high infection. This model is likely to be suitable for a range of host–nematode systems, including varying degrees of infection and treatment with different trace elements.

scholarly journals Preface: The Oligotrophy to the UlTra-oligotrophy PACific Experiment (OUTPACE cruise, 18 February to 3 April 2015)

2017 ◽  
Vol 14 (13) ◽  
pp. 3207-3220 ◽  
Author(s):  
Thierry Moutin ◽  
Andrea Michelangelo Doglioli ◽  
Alain de Verneil ◽  
Sophie Bonnet
Keyword(s):  
Biological Diversity ◽  
New Caledonia ◽  
Austral Summer ◽  
South Pacific ◽  
Adaptive Strategy ◽  
French Polynesia ◽  
Biogenic Elements ◽  
General Context ◽  
Western Boundary ◽  
South Pacific Ocean

Abstract. The overall goal of OUTPACE (Oligotrophy to UlTra-oligotrophy PACific Experiment) was to obtain a successful representation of the interactions between planktonic organisms and the cycle of biogenic elements in the western tropical South Pacific Ocean across trophic and N2 fixation gradients. Within the context of climate change, it is necessary to better quantify the ability of the oligotrophic ocean to sequester carbon through biological processes. OUTPACE was organized around three main objectives, which were (1) to perform a zonal characterization of the biogeochemistry and biological diversity of the western tropical South Pacific during austral summer conditions, (2) to study the production and fate of organic matter (including carbon export) in three contrasting trophic regimes (increasing oligotrophy) with a particular emphasis on the role of dinitrogen fixation, and (3) to obtain a representation of the main biogeochemical fluxes and dynamics of the planktonic trophic network. The international OUTPACE cruise took place between 18 February and 3 April 2015 aboard the RV L'Atalante and involved 60 scientists (30 onboard). The west–east transect covered  ∼  4000 km from the western part of the Melanesian archipelago (New Caledonia) to the western boundary of the South Pacific gyre (French Polynesia). Following an adaptive strategy, the transect initially designed along the 19° S parallel was adapted along-route to incorporate information coming from satellite measurements of sea surface temperature, chlorophyll a concentration, currents, and diazotroph quantification. After providing a general context and describing previous work done in this area, this introductory paper elucidates the objectives of OUTPACE, the implementation plan of the cruise and water mass and climatological characteristics and concludes with a general overview of the other papers that will be published in this special issue.

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