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Chiara Tyndall Hansjo¨rg Lehnherr Ursula Sandmeier Eva Kulik & Thomas A. Bickle 《Molecular microbiology》1997,23(4):729-736
Eco R124I, Eco DXXI and Eco prrI are the known members of the type IC family of DNA restriction and modification systems. The first three are carried on large, conjugative plasmids, while Eco prrI is chromosomally encoded. The enzymes are coded by three genes, hsdR , hsdM and hsdS . Analysis of the DNA sequences upstream and downstream of the type IC hsd loci shows that all are highly homologous to each other and also to sequences present in the bacteriophage P1 genome. The upstream sequences include functional phd and doc genes, which encode an addiction system that stabilizes the P1 prophage state, and extend to and beyond pac , the site at which phage DNA packaging begins. Downstream of the hsd loci, P1 DNA sequences begin at exactly the same place for all of the systems. For Eco DXXI and Eco prrI the P1 homology extends for thousands of base pairs while for Eco R124I an IS 1 insertion and an associated deletion have removed most of the P1-homologous sequences. The significance of these results for the evolution of DNA restriction and modification systems is discussed. 相似文献
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Cryptococcus neoformans and Candida albicans produced a pink pigment from media containing tryptophan. Approximately 30% of the C. neoformans strains produced large amounts of the pink (purple after 6 days) pigment in the absence of light whereas 70% of the Cryptococcus neoformans strains, as well as C. laurentii, C. albidus, C. diffluens, and C. albicans also produced the pink pigment with light being required for significant early production (2–6 days). Significant production did occur for Cryptococcus but not Candida species in the dark after extended incubation (10–25 days). C. terreus produced brown pigments from tryptophan and C. luteolus produced a trace of a buff pigment. Most Candida species produced either pink or brown pigments but not both. In contrast, many Cryptococcus species producing the pink pigment simultaneously produced brown pigments. C. terreus, C. albidus, and C. diffluens produced brown pigments from anthranilic acid whereas C. neoformans, C. laurentii, C. luteolus, and the medically important Candida species did not produce significant amounts of pigments from anthranilic acid. Cryptococcus and Candida species were autofluorescent when tryptophan was a major nitrogen source whereas yeast cell autofluorescence was not observed when anthranilic acid was used. Pigmentation of some Cryptococcus species also the substrate.Operated for the U.S. Department of Energy under contract number EY-76-C-05-0033This article is based on work supported by the Division of Biomedical and Environmental Research. 相似文献
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Analysis of the c-myc P2 promoter. 总被引:1,自引:0,他引:1
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Lindsay P. Chiquoine Scott R. Abella Joshua L. Greenwood Adria DeCorte 《Restoration Ecology》2020,28(Z2):S32-S44
Carbon addition has been proposed as an alternative to herbicide and manual removal methods to treat non‐native plants and reduce non‐target effects of treatments (e.g. impacts on native plants; surface disturbance). On Mojave Desert pavement and biocrust substrates after experimental soil disturbance and carbon addition (1,263 g C/m2 as sucrose), we observed declines in lichens and moss cover in sucrose‐treated plots. To further explore this unforeseen potential side effect of using carbon addition as a non‐native plant treatment, we conducted biocrust surveys 5 and 7 years after treatments, sampled surface soils to observe if treatments additionally affected soil filamentous cyanobacteria, and conducted laboratory trials testing the effects of different levels of sucrose on cyanobacteria and desert mosses. Sucrose addition to biocrust plots reduced lichen and moss cover by 33–78% and species richness by 40–80%. Sucrose reduced biocrust cover in biocrust plots to levels similarly detected in pavement plots (<1%). While cyanobacteria in the field did not appear to be affected by sucrose, laboratory tests showed negative effects of sucrose on both cyanobacteria and mosses. Cyanobacteria declined by 41% 1 month after exposure to 5.4 g C/m2 equivalent solutions. We detected injury to photosynthesis in mosses after 96 hour exposure to 79–316 g C/m2 equivalent solutions. Caution is warranted when using carbon addition, at least in the form and concentration of sucrose, as a treatment for reducing non‐native plants on sites where conserving biocrust is a goal. 相似文献
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Josep Peñuelas Jordi Sardans Marc Estiarte Romà Ogaya Jofre Carnicer Marta Coll Adria Barbeta Albert Rivas‐Ubach Joan Llusià Martin Garbulsky Iolanda Filella Alistair S. Jump 《Global Change Biology》2013,19(8):2303-2338
We review the evidence of how organisms and populations are currently responding to climate change through phenotypic plasticity, genotypic evolution, changes in distribution and, in some cases, local extinction. Organisms alter their gene expression and metabolism to increase the concentrations of several antistress compounds and to change their physiology, phenology, growth and reproduction in response to climate change. Rapid adaptation and microevolution occur at the population level. Together with these phenotypic and genotypic adaptations, the movement of organisms and the turnover of populations can lead to migration toward habitats with better conditions unless hindered by barriers. Both migration and local extinction of populations have occurred. However, many unknowns for all these processes remain. The roles of phenotypic plasticity and genotypic evolution and their possible trade‐offs and links with population structure warrant further research. The application of omic techniques to ecological studies will greatly favor this research. It remains poorly understood how climate change will result in asymmetrical responses of species and how it will interact with other increasing global impacts, such as N eutrophication, changes in environmental N : P ratios and species invasion, among many others. The biogeochemical and biophysical feedbacks on climate of all these changes in vegetation are also poorly understood. We here review the evidence of responses to climate change and discuss the perspectives for increasing our knowledge of the interactions between climate change and life. 相似文献
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