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Becky.zhang (talk | contribs) (Growth response of a sample fungal species (Cladosporium cladosporioides) to 109Cd or 32P radionuclides, as compared to a non-irradiated control environment [1]. Response was measured by a “return angle”, defined as the angle betwe...) |
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Growth response of a sample fungal species (Cladosporium cladosporioides) to 109Cd or 32P radionuclides, as compared to a non-irradiated control environment [[#References|[1]]]. Response was measured by a “return angle”, defined as the angle between the point of maximal radioactivity in the culture medium and the direction of growth of the end portion of a hyphum from each C. cladosporioides spore. A mean “return angle” less than 90 degrees is indicative of mean hyphal growth towards the source of radioactivity. Figure adapted from Microbiology of Extreme Soils Fig. 16.2 [[#References|[10]]] | Growth response of a sample fungal species (Cladosporium cladosporioides) to 109Cd or 32P radionuclides, as compared to a non-irradiated control environment [[#References|[1]]]. Response was measured by a “return angle”, defined as the angle between the point of maximal radioactivity in the culture medium and the direction of growth of the end portion of a hyphum from each C. cladosporioides spore. A mean “return angle” less than 90 degrees is indicative of mean hyphal growth towards the source of radioactivity. Figure adapted from Microbiology of Extreme Soils Fig. 16.2 [[#References|[10]]]. |
Latest revision as of 06:56, 13 December 2012
Growth response of a sample fungal species (Cladosporium cladosporioides) to 109Cd or 32P radionuclides, as compared to a non-irradiated control environment [1]. Response was measured by a “return angle”, defined as the angle between the point of maximal radioactivity in the culture medium and the direction of growth of the end portion of a hyphum from each C. cladosporioides spore. A mean “return angle” less than 90 degrees is indicative of mean hyphal growth towards the source of radioactivity. Figure adapted from Microbiology of Extreme Soils Fig. 16.2 [10].
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