posted on 2012-05-27, 00:00authored byJeff R. Havig, Jason Raymond, D'Arcy R. Meyer-Dombard, Natalya Zolotova, Everett L. Shock
Thermophilic microbes in hydrothermal ecosystems have multiple metabolic strategies for taking up carbon and nitrogen, which may result in distinct stable isotopic compositions of C and N in living biomass, as well as other biosignatures that accumulate in the geologic record. Biofilms from "Bison Pool" at Yellowstone National Park display large variations in carbon and nitrogen isotopic values as a function of downstream sampling and illustrate the presence of large shifts in ecological functions as temperature decreases. This is the first study to couple isotopic data with community genomic analysis to predict dominant carbon fixation pathways that create hydrothermal biofilm signatures. The results also suggest nitrogen limitation through the chemotrophic zone and nitrogen fixation in the lower-temperature phototrophic zone.
Funding
This research was funded in part by NSF grant EAR-0525561 and JGI user agreement SHOCK 182 051129.
History
Publisher Statement
The final version of this paper was published by AGU in Journal of Geophysical Research. Copyright 2011 American Geophysical Union. DOI: 10.1029/2010JG001415.