Hydrothermal vents have been discovered across the globe’s
oceans in areas of ocean ranging from abyssal to intertidal. Though there have
been many studies conducted upon deep-sea hydrothermal vents there has been comparatively
little done upon shallow water hydrothermal vents; that is vents that exist at
a depth of 200m or less. The author has outlined the possibility that both
phototrophy and chemotrophy work in tandem
in the shallow water vent ecosystem as the vent is closer to the surface
of the water and therefore has access to sunlight. Another key difference
between these vents and their deep-sea counterparts is that the plumes of
volcanic water that erupt from the shallow water vents reach the surface, which
can have quite a profound impact on the ecosystems around it. Whereas the
plumes of deep-sea hydrothermal vents are restricted to quite a narrow zone.
This study analysed the bacterial communities of two
different vents over eight samples, four from a white vent and four from a
yellow vent. The authors used pyrosequencing to produce 32 bacterial and
archaeal DNA and RNA based tag libraries. They also attempted to address the
biogeochemical that are mediated by the microbial community.
The results of statistical testing revealed that the
pyrosequencing produced estimates of richness that were higher than the
analyses of clone libraries, the data for this was not shown within the paper
which would have otherwise helped to reinforce that point by providing evidence
which can be seen by the reader. However, it must also be noted that the inclusion
of such data may have served only to confuse or swamp the reader with a number
of different figures. There was also
evidence to suggest that there is a high dominance of abundant taxa and
generally low richness of communities. Further analysis showed that there is
quite a high degree of diversity within the dominant taxa which can perhaps
suggest that many species are responsible for the high diversity of the bacterial
and archaeal libraries. It was also found that the libraries separated into
distinct clusters that correspond to the two vents.
As was predicted by the authors Cyanobacteria were very prevalent within the samples taken and made
up a large proportion of the RNA pool, this provides further evidence for the
idea that photosynthesis takes place in tandem with chemolithotrophy. It has
also been noted that this is unique to shallow water vents for reasons given
above. The significance of this is yet to be discussed and has not been covered
within this paper. It could be speculated that the presence of Cyanobacteria co-occurring with
chemolithotrophic bacteria could be due only to the fact that sunlight can
reach the shallow water vents. Another possibility is that the Cyanobacteria form a symbiotic
relationship with other bacteria such as members of the genus Thiomicrospira as these bacteria have
the capacity to obtain Carbon from CO2, though what the Cyanobacteria would gain from the
relationship is not apparent.
ZhangY., Zhao Z., Chen CA., Tang K., Su J., Jiao N., 2012, Sulfur Metabolizing Microbes Dominate
Microbial Communities in Andesite-Hosted Shallow-Sea Hydrothermal Systems, PLOS
one, 7 (9), e44593
Hi Daniel,
ReplyDeleteI was just wondering what the differences were between the two vents. Also, was there a difference in the abundances of certain taxa found between the two vents?
Thanks,
Sophie
Hi Daniel,
ReplyDeleteThis is interesting, I had never heard of shallow water vent before. Were there any lithotrophic bacteria common to both deep and shallow vents?
Thanks, Harri
Daniel - that's an interesting study. In my book, there is a colour plate of a shallow vent in which chemosynthetic bacteria are actually colonizing alongside red and green macroalgae. On the other hand, there is a report from 2005 about an obligately phototrophic bacterium growing in a 2500 m hydrothermal vent (http://www.ncbi.nlm.nih.gov/pmc/articles/PMC1166624/) How does it do it? Apparently, using the faint glow of light that comes from the vents. Ah, life is full of surprises.
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