Pseudomonas syringae: Bioprecipitation Mechanisms and Implications

From MicrobeWiki, the student-edited microbiology resource
Revision as of 01:54, 26 April 2016 by Byrdb (talk | contribs)
This is a curated page. Report corrections to Microbewiki.

Overview

Fig.2 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.


By Brandon Byrd


Introduce the topic of your paper. What is your research question? What experiments have addressed your question? Applications for medicine and/or environment?
Sample citations: [1]



A citation code consists of a hyperlinked reference within "ref" begin and end codes.

History

Include some current research, with at least one figure showing data.

Every point of information REQUIRES CITATION using the citation tool shown above.

Bioprecipitation and
ItalicP.syringae’s Role in Bioprecipitation

Include some current research, with at least one figure showing data.

Section 3

Include some current research, with at least one figure showing data.

Section 4

Conclusion

References

  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.



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

Retrieved from "https://microbewiki.kenyon.edu/index.php?title=Pseudomonas_syringae:_Bioprecipitation_Mechanisms_and_Implications&oldid=121794"