Fluid flow stimulates chemosynthesis in a Greek salad of hydrothermal
microbes

Date:
April 22, 2022
Source:
Woods Hole Oceanographic Institution
Summary:
A new study uses an innovative approach to examine a shallow-water
hydrothermal system and the production of microbes there in situ
and near natural conditions as a model to assess the importance
of hydrothermal fluid circulation on chemosynthesis.



FULL STORY ==========================================================================
Most visitors to Paliochori Beach on the Greek island Milos may not be
aware of the bay's shallow-water hydrothermal community, a veritable Greek salad of microbes, that is within snorkeling distance from the shoreline.


==========================================================================
The hydrothermalism in the coastal sediments of Paliochori Bay strongly
affects biogeochemical processes there and supports chemosynthesis,
which allows certain microorganisms such as sulfur-oxidizing bacteria
to use chemical energy rather than light, as photosynthetic plants or
algae do, to convert carbon dioxide into cell material.

However, the impact of fluid flow on the composition of the microbial
community and the rates of chemosynthetic production have been unknown
because it is challenging to measure microbial processes under natural conditions, particularly in hydrothermal systems.

A new study uses an innovative approach to examine the bay's shallow-water hydrothermal system and the production of microbes there in situ and near natural conditions as a model to assess the importance of hydrothermal
fluid circulation on chemosynthesis.

By examining microbial communities directly within the
hydrothermally-impacted sandy sediments in the bay, the study demonstrates
"the importance of fluid flow in shaping the composition and activity of microbial communities of shallow-water hydrothermal vents, identifying
them as hotspots of microbial activity," according to the paper, "Fluid
flow stimulates chemoautotrophy in hydrothermally influenced coastal sediments," published in Communications Earth & Environment,a Nature
Portfolio journal.

In addition, "the study shows how productive the shallow water
hydrothermal vents actually are, and how quickly the microbes adapt to
changing conditions," says co-lead author Stefan Sievert, associate
scientist in the Woods Hole Oceanographic Institution's (WHOI's)
Biology Department.



========================================================================== During the study, researchers carried out two sets of stable isotope
probing experiments using carbon dioxide labelled with the stable carbon isotope 13C as a tracer to determine the microbes' capability for carbon fixation, which is the conversion of carbon dioxide into biomass. The
study deployed incubation devices along a transect at a vent in the bay
and injected the tracer at different depths into the sediment, either
in open or closed fluid flow modes, and left the devices in place for
either 6 hours or 24 hours before picking them up again.

The amount of carbon fixation was determined by measuring the
incorporation of the labelled carbon dioxide into fatty acids, a key
component making up the cell membrane, in combination with assessing the compositionof the microbial community using DNA- and RNA-based approaches.

The study "extends the current knowledge on dark carbon fixation in
coastal sandy sediments to those areas that are impacted by hydrothermal activity," according to the paper. The researchers' data reveal that
active fluid flow at this sandy sediment shallow-water hydrothermal
vent site sustains carbon fixation rates that are among the highest
determined for coastal margin sediments, highlighting the influence of hydrothermalism in supporting chemoautotrophic production by supplying
the required chemicals in the form of electron donors such as hydrogen
sulfide, and acceptors such as oxygen.

Extrapolating the production at the studied vent site to the overall
venting area in the bay of about 4 acres, 7 metric tons of carbon are
produced there per year. "That is about the same annual production per
area as a 4-acre corn field," says Sievert.

The study also found a very active microbial community that is able to
respond quickly to environmental changes. The chemosynthetic production at Milos is mainly driven by Campylobacteria, which dominated the communities
in the open incubations, but declined in the closed incubations. Other bacteria, in particular Gammaproteobacteria, also increased in open
flow incubations, while others, such as Deltaproteobacteria and Thermodesulfobacteria increased in closed incubations. In general,
the community switched from a community dominated by chemosynthetic
microbes to one with a higher proportion of heterotrophic microbes, i.e., microbes that use organic carbon for food, just as people do. The study
found that the microbial community changed in response to different
conditions within a matter of hours, which is very fast and took the investigators by surprise.

Making the microbe rate measurements and identifying the various
microbes at the hydrothermal vent site was a collaborative
effort. That collaboration included Sievert's expertise in the use of
the incubation device and identifying the microbes based on DNA- and
RNA-based techniques. In addition, the lab of co-lead author Solveig
Bu"hring, a researcher at the University of Bremen, contributed data
on the incorporation of the labelled carbon dioxide into the microbes'
fatty acids.

"What drives me to do this research is my curiosity to understand how
things work. I'm interested in knowing what the microbes are doing and
how they are helping the ecosystem to function," says Sievert.

"Each individual microbe is so small, yet their combined impact is so
immense," he adds. "Microbes are kind of the engines of our planet,
basically driving all of the biogeochemical cycles, such as the nitrogen
and sulfur cycles." This work was funded by the National Science
Foundation (NSF, USA) through grant OCE-1124272 and by the Deutsche Forschungsgemeinschaft through the Emmy Noether-Program. In addition,
Sievert received support from the WHOI Investment in Science Fund. The
authors are also grateful to the General Directorate of Antiquities
and Cultural Heritage in Athens for granting them permission for sample acquisition and processing.


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========================================================================== Related Multimedia:
* Areas_of_hydrothermal_activity_in_Paliochori_Bay ========================================================================== Journal Reference:
1. Stefan M. Sievert, Solveig I. Bu"hring, Lara K. Gulmann, Kai-Uwe
Hinrichs, Petra Pop Ristova, Gonzalo V. Gomez-Saez. Fluid flow
stimulates chemoautotrophy in hydrothermally influenced coastal
sediments.

Communications Earth & Environment, 2022; 3 (1) DOI:
10.1038/s43247-022- 00426-5 ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2022/04/220422114742.htm

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