Microenvironments of reduced salinity harbour biofilms in Dead Sea underwater springs
Version of Record online: 19 JAN 2014
© 2013 Society for Applied Microbiology and John Wiley & Sons Ltd
Environmental Microbiology Reports
Special Issue: Microbial Community Ecology
Volume 6, Issue 2, pages 152–158, April 2014
How to Cite
Häusler, S., Noriega-Ortega, B. E., Polerecky, L., Meyer, V., de Beer, D. and Ionescu, D. (2014), Microenvironments of reduced salinity harbour biofilms in Dead Sea underwater springs. Environmental Microbiology Reports, 6: 152–158. doi: 10.1111/1758-2229.12140
- Issue online: 4 MAR 2014
- Version of Record online: 19 JAN 2014
- Accepted manuscript online: 24 DEC 2013 05:43AM EST
- Manuscript Accepted: 13 DEC 2013
- Manuscript Received: 4 JUN 2013
Fig. S1. Image of rocks collected from the streams. Biofilm growth is mostly limited to the equator of the rocks. Green biofilms are located on the upper side.
Fig. S2. Example of flow velocities measured in situ above a cobble at a vertical distance of 2 cm. Panel (A) shows all three cartesian components of the velocity vector (z-component corresponds to the vertical direction), as well as the vector magnitude, as a function of time. Panel (B) shows the projections of the velocity vector in the vertical plane (the time axis is collapsed).
Fig. S3. Salinity distributions above the surface of rocks immersed in hypersaline water (300 g L−1) and exposed to freshwater flow from below at a vertical flow velocity of 7 cm s−1. Shown are examples for a rock without a biofilm and for two rocks partially covered with biofilms. Colour bar values are in g L−1.
Video Clip S1. An in situ colour injection experiment showing the freshwater flow around a rock at the edge of a spring. The main flow of the spring is not visible in this close-up video.
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