C. G. B. and K. M. contributed equally to this work.
Chemolithoautotrophic denitrification of epsilonproteobacteria in marine pelagic redox gradients
Version of Record online: 26 SEP 2012
© 2012 Society for Applied Microbiology and Blackwell Publishing Ltd
Special Issue: Marine Microbial Ecophysiology and Metagenomics
Volume 15, Issue 5, pages 1505–1513, May 2013
How to Cite
Bruckner, C. G., Mammitzsch, K., Jost, G., Wendt, J., Labrenz, M. and Jürgens, K. (2013), Chemolithoautotrophic denitrification of epsilonproteobacteria in marine pelagic redox gradients. Environmental Microbiology, 15: 1505–1513. doi: 10.1111/j.1462-2920.2012.02880.x
- Issue online: 18 APR 2013
- Version of Record online: 26 SEP 2012
- Accepted manuscript online: 29 AUG 2012 11:01PM EST
- Manuscript Accepted: 23 AUG 2012
- Manuscript Revised: 13 JUL 2012
- Manuscript Received: 25 OCT 2011
- German Federal Ministry of Education and Research (BMBF)
Table S1. In this table we present the raw data regarding nitrate and hydrogen sulfide concentrations as well as dark carbon dioxide fixation measured directly in samples from Baltic Sea redox gradients. As secondary data we deduced flow rates by Eddy diffusion of nitrate and hydrogen sulfide from the measured concentrations and depths. n.d., not determined.
Table S2. In this table we present prokaryotic cell numbers determined by epifluorescence microscopy throughout a typical Baltic Sea redox gradient. Overall, cell numbers were determined by DAPI staining, whereas eubacterial (EUB) and GD17 cell numbers were determined by CARD-FISH. GD17 cells contribute by 17% to the total prokaryotic community at the chemocline at 87.5 m water depth.
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