PHOTOTROPHIC COMMUNITY DISTRIBUTION ALONG A GEOTHERMAL STREAM: INSIGHTS INTO CARBON CYCLING IN VERSATILE PHOTOTROPHS
Cyanobacteria are experts in oxygenic photosynthesis and have been fine-tuning this process for millions of years, while the phototrophic Chloroflexi are physiologically and metabolically diverse. Chloroflexi have many tricks up their sleeves when it comes to carbon assimilation: they can be photoautotrophs, photoheterotrophs or photomixotrophs and rely on an array of different electron donors and acceptors commonly found in hot springs (H2S, Fe2+ and other inorganic compounds).
Here, we performed a cursory survey of Chloroflexi and Cyanobacteria by 16S rRNA gene sequencing biomass from seven sites along Rabbit Creek outflow in order to determine how specific taxa and diversity within these phyla changes along the natural temperature gradient. To assess photosynthetic activity, we set up carbon assimilation microcosm experiments with biomass from each site. Rabbit Creek, a circum-neutral geothermal stream in the Midway Geyser Basin of Yellowstone National Park, provides a natural temperature gradient ranging from a near boiling source to ~45ºC downstream. Additionally, Rabbit Creek has natural gradients of sulfide and pH and width of the stream expands downstream, leading to variable flow.
We found that while Cyanobacteria and a the photoheterotrophic Roseiflexus (Chloroflexi) remained relatively consistent between 55ºC-65ºC, the rates of oxygenic photosynthesis decreased two-fold with increasing temperature. This suggests that either temperature or Roseiflexus could be impacting the physiology of Cyanobacteria. Previous work has shown that Cyanobacteria recovered from Yellowstone Hot Springs are active up to 72ºC, so it is likely that Chloroflexi could play a major role in the activity of Cyanobacteria, and the overall productivity of hot springs microbial communities in general.