Functional and compositional succession of bacterioplankton in response to a gradient in bioavailable dissolved organic carbon
Version of Record online: 4 JUL 2013
© 2013 John Wiley & Sons Ltd and Society for Applied Microbiology
Special Issue: Drivers of Shifts in Microbial Community Composition
Volume 15, Issue 9, pages 2616–2628, September 2013
How to Cite
Dinasquet, J., Kragh, T., Schrøter, M.-L., Søndergaard, M. and Riemann, L. (2013), Functional and compositional succession of bacterioplankton in response to a gradient in bioavailable dissolved organic carbon. Environmental Microbiology, 15: 2616–2628. doi: 10.1111/1462-2920.12178
- Issue online: 4 SEP 2013
- Version of Record online: 4 JUL 2013
- Accepted manuscript online: 11 JUN 2013 06:03AM EST
- Manuscript Accepted: 2 JUN 2013
- Manuscript Received: 14 SEP 2012
- Swedish Research Council for Environment Agricultural Sciences and Spatial Planning. Grant Number: 210-2008-1882
- Carlsberg Foundation. Grant Number: 2008_01_0178
Fig. S1. Rarefaction curves for each sample. The number of sequences in each unique OTU per subsample was used to calculate the rarefaction.
Fig. S2. Phylogenetic reconstruction of the SAR11 clade. DNA distance and neighbour joining method, bootstrap based on 1000 replicated trees. OTUs from this study are given in bold, with the number of sequences retrieved in parentheses.
Table S1. Microbial richness and diversity estimates. The calculations were based on randomly picked OTUs normalized to 3393 sequences per sample to accommodate for the lowest number of sequences found in a sample.
Table S2. SIMPER analysis showing the contribution of the OTUs to the differences between time points. (Supplied online as Excel file).
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