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  • 1
    Publication Date: 2010-02-26
    Description: The Red Queen hypothesis proposes that coevolution of interacting species (such as hosts and parasites) should drive molecular evolution through continual natural selection for adaptation and counter-adaptation. Although the divergence observed at some host-resistance and parasite-infectivity genes is consistent with this, the long time periods typically required to study coevolution have so far prevented any direct empirical test. Here we show, using experimental populations of the bacterium Pseudomonas fluorescens SBW25 and its viral parasite, phage Phi2 (refs 10, 11), that the rate of molecular evolution in the phage was far higher when both bacterium and phage coevolved with each other than when phage evolved against a constant host genotype. Coevolution also resulted in far greater genetic divergence between replicate populations, which was correlated with the range of hosts that coevolved phage were able to infect. Consistent with this, the most rapidly evolving phage genes under coevolution were those involved in host infection. These results demonstrate, at both the genomic and phenotypic level, that antagonistic coevolution is a cause of rapid and divergent evolution, and is likely to be a major driver of evolutionary change within species.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3717453/" target="_blank"〉〈img src="https://static.pubmed.gov/portal/portal3rc.fcgi/4089621/img/3977009" border="0"〉〈/a〉   〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3717453/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Paterson, Steve -- Vogwill, Tom -- Buckling, Angus -- Benmayor, Rebecca -- Spiers, Andrew J -- Thomson, Nicholas R -- Quail, Mike -- Smith, Frances -- Walker, Danielle -- Libberton, Ben -- Fenton, Andrew -- Hall, Neil -- Brockhurst, Michael A -- 079643/Wellcome Trust/United Kingdom -- 098051/Wellcome Trust/United Kingdom -- Wellcome Trust/United Kingdom -- England -- Nature. 2010 Mar 11;464(7286):275-8. doi: 10.1038/nature08798. Epub 2010 Feb 24.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉School of Biological Sciences, Biosciences Building, University of Liverpool, Crown Street, Liverpool L69 7ZB, UK.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20182425" target="_blank"〉PubMed〈/a〉
    Keywords: Bacteriophages/genetics/*physiology ; *Biological Evolution ; *Evolution, Molecular ; Genetic Variation ; Molecular Sequence Data ; Phenotype ; Pseudomonas fluorescens/*genetics/*virology ; Selection, Genetic/genetics
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2014-11-02
    Description: The oxygenation of Earth's surface fundamentally altered global biogeochemical cycles and ultimately paved the way for the rise of metazoans at the end of the Proterozoic. However, current estimates for atmospheric oxygen (O2) levels during the billion years leading up to this time vary widely. On the basis of chromium (Cr) isotope data from a suite of Proterozoic sediments from China, Australia, and North America, interpreted in the context of data from similar depositional environments from Phanerozoic time, we find evidence for inhibited oxidation of Cr at Earth's surface in the mid-Proterozoic (1.8 to 0.8 billion years ago). These data suggest that atmospheric O2 levels were at most 0.1% of present atmospheric levels. Direct evidence for such low O2 concentrations in the Proterozoic helps explain the late emergence and diversification of metazoans.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Planavsky, Noah J -- Reinhard, Christopher T -- Wang, Xiangli -- Thomson, Danielle -- McGoldrick, Peter -- Rainbird, Robert H -- Johnson, Thomas -- Fischer, Woodward W -- Lyons, Timothy W -- New York, N.Y. -- Science. 2014 Oct 31;346(6209):635-8. doi: 10.1126/science.1258410.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department Geology and Geophysics, Yale University, CT, USA. noah.planavsky@yale.edu chris.reinhard@eas.gatech.edu. ; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, GA, USA. noah.planavsky@yale.edu chris.reinhard@eas.gatech.edu. ; Department Geology and Geophysics, Yale University, CT, USA. Department of Geology, University of Illinois, Champaign, IL, USA. ; Department of Earth Science, Carleton University, Ottawa, ON, Canada. ; Centre for Ore Deposit and Exploration Science, University of Tasmania, TAS, Australia. ; Geological Survey of Canada, Ottawa, ON, Canada. ; Department of Geology, University of Illinois, Champaign, IL, USA. ; Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA. ; Department of Earth Sciences, University of California, Riverside, CA, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25359975" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Atmosphere/*chemistry ; *Biological Evolution ; Chromium Isotopes/chemistry ; Earth (Planet) ; Geologic Sediments/chemistry ; Oxidation-Reduction ; Oxygen/*analysis ; Paleontology
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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