Low temperature S0 biomineralization at a supraglacial spring system in the Canadian High Arctic
Version of Record online: 19 MAY 2011
© 2011 Blackwell Publishing Ltd
Volume 9, Issue 4, pages 360–375, July 2011
How to Cite
GLEESON, D. F., WILLIAMSON, C., GRASBY, S. E., PAPPALARDO, R. T., SPEAR, J. R. and TEMPLETON, A. S. (2011), Low temperature S0 biomineralization at a supraglacial spring system in the Canadian High Arctic. Geobiology, 9: 360–375. doi: 10.1111/j.1472-4669.2011.00283.x
- Issue online: 20 JUN 2011
- Version of Record online: 19 MAY 2011
- Received 10 May 2010; accepted 03 April 2011
Figure S1. Follow-up imaging on sulfur structures within enrichments and co-cultures of Marinobacter and Flavobacteria.
Figure S2. Follow-up imaging of sulfur structures within co-cultures of Marinobacter and Shewanella, showing central masses comprising one or more spherical mineral aggregates, curved filaments and wholly or partially mineralized rigid sheaths.
Figure S3. Different stages in formation of sulfur structures by consortia.
|GBI_283_sm_FigureS1-S3.pdf||341K||Supporting info item|
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