Pseudomonas syringae: Bioprecipitation Mechanisms and Implications: Difference between revisions

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<ref>[http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3847443/ Bartlett et al.: Oncolytic viruses as therapeutic cancer vaccines. Molecular Cancer 2013 12:103.]</ref>
<ref>[http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3847443/ Bartlett et al.: Oncolytic viruses as therapeutic cancer vaccines. Molecular Cancer 2013 12:103.]</ref>
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<br><br>Authored for BIOL 238 Microbiology, taught by [mailto:slonczewski@kenyon.edu Joan Slonczewski], 2016, [http://www.kenyon.edu/index.xml Kenyon College].

Revision as of 01:02, 22 April 2016

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The bioprecipitation cycle diagram with two key factors that highlight the system. First, micro-organisms such as P.syringae that conduct the ice nucleation process. Second, the water vapor from plants, oceans, and aquatic environments that these micro-organism use in the atmosphere http://onlinelibrary.wiley.com/doi/10.1111/gcb.12447/epdf.


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  1. ↑ Morris, C.E. et al. “Bioprecipitation: a feedback cycle linking Earth history, ecosystem dynamics and land use through biological ice nucleators in the atmosphere.” 2014. Global Change Biology 20: 341–351.
  2. ↑ Bartlett et al.: Oncolytic viruses as therapeutic cancer vaccines. Molecular Cancer 2013 12:103.



Authored for BIOL 238 Microbiology, taught by Joan Slonczewski, 2016, Kenyon College.

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