The ATPases ofPropionigenium modestum andBacillus alcalophilus. Strategies for ATP synthesis under low energy conditions

1992 ◽  
Vol 1101 (2) ◽  
pp. 236-239
Author(s):  
Peter Dimroth
2021 ◽  
Vol 7 (1) ◽  
pp. 42
Author(s):  
Deyamira Matuz-Mares ◽  
Oscar Flores-Herrera ◽  
Guadalupe Guerra-Sánchez ◽  
Lucero Romero-Aguilar ◽  
Héctor Vázquez-Meza ◽  
...  

Respiratory supercomplexes are found in mitochondria of eukaryotic cells and some bacteria. A hypothetical role of these supercomplexes is electron channeling, which in principle should increase the respiratory chain efficiency and ATP synthesis. In addition to the four classic respiratory complexes and the ATP synthase, U. maydis mitochondria contain three type II NADH dehydrogenases (NADH for reduced nicotinamide adenine dinucleotide) and the alternative oxidase. Changes in the composition of the respiratory supercomplexes due to energy requirements have been reported in certain organisms. In this study, we addressed the organization of the mitochondrial respiratory complexes in U. maydis under diverse energy conditions. Supercomplexes were obtained by solubilization of U. maydis mitochondria with digitonin and separated by blue native polyacrylamide gel electrophoresis (BN-PAGE). The molecular mass of supercomplexes and their probable stoichiometries were 1200 kDa (I1:IV1), 1400 kDa (I1:III2), 1600 kDa (I1:III2:IV1), and 1800 kDa (I1:III2:IV2). Concerning the ATP synthase, approximately half of the protein is present as a dimer and half as a monomer. The distribution of respiratory supercomplexes was the same in all growth conditions. We did not find evidence for the association of complex II and the alternative NADH dehydrogenases with other respiratory complexes.


2019 ◽  
Vol 66 (4) ◽  
pp. 435-444 ◽  
Author(s):  
Liang Lü ◽  
Chen-Yang Cai ◽  
Xi Zhang ◽  
Alfred F Newton ◽  
Margaret K Thayer ◽  
...  

Abstract Staphylinoidea (Insecta: Coleoptera) is one of the most species-rich groups in animals, but its huge diversity can hardly be explained by the popular hypothesis (co-radiation with angiosperms) that applies to phytophagous beetles. We estimated the evolutionary mode of staphylinoid beetles and investigated the relationship between the evolutionary mode and palaeoclimate change, and thus the factors underlying the current biodiversity pattern of staphylinoid beetles. Our results demonstrate that staphylinoid beetles originated at around the Triassic–Jurassic bound and the current higher level clades underwent rapid evolution (indicated by increased diversification rate and decreased body size disparity) in the Jurassic and in the Cenozoic, both with low-energy climate, and they evolved much slower during the Cretaceous with high-energy climate. Climate factors, especially low O2 and high CO2, promoted the diversification rate and among-clade body size disparification in the Jurassic. In the Cenozoic, however, climate factors had negative associations with diversification rate but little with body size disparification. Our present study does not support the explosion of staphylinoid beetles as a direct outcome of the Cretaceous Terrestrial Revolution (KTR). We suppose that occupying and diversifying in refuge niches associated with litter may elucidate rapid radiations of staphylinoid beetles in low-energy conditions.


2008 ◽  
Vol 2008 (1) ◽  
pp. 835-841 ◽  
Author(s):  
Tim Nedwed ◽  
Tom Coolbaugh

ABSTRACT Beaker and basin dispersant-effectiveness tests are used to help determine if application of dispersants in a real oil-spill incident is worthwhile. This paper provides evidence indicating that these tests negatively bias expected dispersion at sea because beakers and basins do not allow the spreading of oil slicks that occurs after application of dispersant in the unbounded open ocean. One reason is that closed system walls and/or oil-slick containment methods impose physical boundaries that restrict oil spreading. In addition to these physical constraints, surfactant films developed after applying dispersant form on the water surface surrounding an oil slick and act as chemical herders to keep slicks thick. This occurs in the field during a real incident and in beaker and basin dispersant-effectiveness tests. Surfactant films on the water surface, however, are fragile and can't persist in the open ocean but can persist throughout the short duration of standard dispersant-effectiveness tests. This paper provides a background discussion of how surfactant films contaminate the water surface on the perimeter of oil slicks to restrict spreading in both open and closed systems and evidence that these fragile films don't persist in the open ocean. The discussion is followed by a description of lab tests that showed even minimal water-surface contamination from the surfactants in a widely available dispersant significantly restricted spreading to keep slicks thick. Thick oil slicks, by their nature, will obviously require more turbulence to disperse than a thin film of the same oil. Thus, it is believed that the restricted slick spreading inherent in dispersant-effectiveness tests completed in basins and beakers results in significantly lower performance than would be expected at sea not only for heavier oils but for all oils in tests simulating low-energy conditions.


1987 ◽  
Vol 1987 (1) ◽  
pp. 263-267
Author(s):  
D. I. Little ◽  
D. L. Scales

ABSTRACT The objective of this experiment was to assess the effectiveness of a new Type III chemical dispersant on stranded, lightly weathered crude oil and emulsified medium fuel oil (mousse). The oils were applied to field plots on contrasting sediment shorelines (salt marsh and sand flat), where both oils had been shown to be persistent. On the salt marsh, dispersant-treated oils usually were detected at lower sediment total hydrocarbon (THC) concentrations than were the untreated oils. However, clear trends were not visible until heavy rain removed the oiled, dead vegetation. Subsequently, the THC concentrations measured in the treated crude plots were reduced by half, and stable, lower concentrations were measured in the mousse plots. On the sand flat, the dispersant-treated mousse was detected at consistently lower THC concentrations than was the untreated mousse. The crude-oil-treated plots showed more temporal variability than the mousse-treated plots. Dispersant-treated crude ultimately was detected at half the concentration found in the untreated crude plots. Although on the salt marsh both dispersant-treated oils were more damaging in the short term to the plant community, the longer-term effects of higher untreated oil concentrations may prove more destabilizing to the salt-marsh habitat as a whole. After erosion, untreated oil may be resuspended to form oil slicks, when public interest in the original spill and the sense of responsibility for its cleanup have all but disappeared. Under the slightly higher-energy conditions of the sand flat, dispersant use did not dramatically alter the fate of most of the oil. The approximately 10% that remained in the beach was less obvious visually and was removed faster than the untreated oil. The practical implication of this is that if the cleanup authorities can resist amenity and conservationist pressures to disperse the residual oil, such tidal flats will eventually self-clean. Earlier formulations of chemical dispersant either have been relatively ineffective or have increased contamination on low-energy sediment shores. Several explanations may be advanced for the effectiveness of this dispersant on both oil types. First, it helped prevent the formation of surface oiled pavements and, thus, the burial of oil layers. Second, the contact time of oils and dispersant (>2 hours pre-tidal coverage) may have contributed to the reductions in oil concentrations. Third, at both sites there was sufficient energy input to assist dispersion.


2017 ◽  
Vol 120 (2) ◽  
pp. 293-302 ◽  
Author(s):  
E.M. Bordy ◽  
S. Spelman ◽  
D.I. Cole ◽  
P. Mthembi

Abstract The Lower Permian Pietermaritzburg Formation is a mudrock-dominated, upward-coarsening stratigraphic unit in the lower Ecca Group (Karoo Supergroup) in the northeastern part of the main Karoo Basin of South Africa. The formation extends over most of the KwaZulu-Natal Province, and due to its lithology and the local climate, it is usually poorly exposed; hence the description is mainly based on borehole records. From a measured thickness of about 430 m south of the type area around Pietermaritzburg, the formation thins progressively northwards and pinches out against the Dwyka Group and pre-Karoo basement north of latitude 26° 30' S. This Lower Permian formation is considered a stratigraphic equivalent of the Prince Albert Formation in the southern part of the main Karoo Basin. The Pietermaritzburg Formation only preserves scattered, fragmentary plant fossil and invertebrate trace fossils, which are diagnostic of marine conditions (e.g. Helminthopsis). Based on its sedimentary facies characteristics and ichnofossil assemblages, the unit was probably deposited under low energy conditions on a northerly shallowing marine shelf that initially experienced deepening (during a major Artinskian transgression) and then shallowing in the early Kungurian.


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