Cite as: Cold Spring Harb. Protoc.; 2009; doi:10.1101/pdb.prot5341
| Protocol |
Department of Biological Sciences, Northern Arizona University, Flagstaff, AZ 86011, USA
Corresponding author (Egbert.Schwartz{at}nau.edu).
INTRODUCTION
When analyzing environmental samples of microorganisms by stable isotope probing (SIP), labeling the DNA with H218O, instead of organic or nitrogenous compounds, offers important advantages because water cannot be used as an energy, carbon, or nitrogen source. As a result, addition of the label is unlikely to influence microbial growth rates in soil directly, and microbial communities can be exposed to the label for long periods of time because they are not exposed to abnormally high substrate concentrations. Because all organisms incorporate water into their DNA, performing SIP with H218O is a method for identifying microorganisms that have grown during incubation with H218O, as well as microorganisms that have not grown (i.e., did not incorporate the label) but survived the incubation. This protocol describes the use of SIP with H218O to study soil microorganisms.
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