Metagenomic insights
into strategies of carbon conservation and unusual sulfur biogeochemistry in a
hypersaline Antarctic lake.
Organic Lake in Antartica’s Vestfold Hills region has the
highest reported dimethylsulfide (DMS) concentration of any natural water body.
To try and better understand the microbial community, pathways and mineral
cycles involved in this unusual occurrence, shotgun metagenomics were performed
on size-fractioned samples along the lake’s depth profile. This was
complimented by physiochemial profiles of major nutrients so that links between
species, genes and chemical distribution could be made.
Microbial Community
Data from the metagenome grouped into 983 operational taxanomic
units (OTU); 76.2% Bacteria, 16.3% Eucarya and 7.5% could not be classified. Of
the 3959 SSU rRNA gene reads, only two were related to Archaea implying that this domain, usually associated with extreme
conditions, especially hypothermal and anoxic, have a minor role here.
Heterotrophic Psychroflexus,
Marinobacter and Roseovarius genera dominated the Organic lake community. Evidence
for this came in the form of OTU abundance relating to each genus. The Viridiplantae, primarily Dunaliella, performed carbon fixation as was shown by the
ribulose-bisphosphate caboxylase oxygenase (RuBisCO) homolog relatedness. Some
RuBisCO was found to relate to the Gammaproteobacteria
indicating some autotrophy in the group. The other gene used to detect
photosynthesis is prkB. In this case
its detection was not affirmative of autotrophy as, within the Marinobacter the gene is associated with
pentose phosphate metabolism, not carbon fixation.
Within the heterotrophic community strategies were identified
that may help these organism to capitalize on the limited available resources
and reduce the loss of important nutrients. In the upper mixed zone Psychroflexus was predicted to
remineralise recalcitrant polymeric algal material and particulate matter,
shown by the clustering of Psychroflexus
OTUs with Dunaliella chloroplasts in
the serration analysis and a previous study showing their abundance in
correlation with hours of sunlight. In the deep zone this function is likely
performed by Firmicutes. Both these
organisms provide labile substrates that are required by other heterotrophs in
the system. Marinobacter and Roseovarius were linked to
rhodopsin-mediated and AAnP photoheterotrophy with the AAnP abundance being
higher here than any other studied system, indicating that the use of light as
an energy scource may be an important survival strategy in this low nutrient
environment. Chemolithoheterotrophy, sulfur oxidation and CO oxidation may also
be important sources of energy and the potential for each was high in this
system.
Nitrogen cycling.
Potential for nitrogen cycling in the lake was dominated by
mineralization/assimilation pathways. It is suggested that ammonia assimilation
occurs in the upper mixed zone but accumulates in the anaerobic deep zone.
Sulfur cycling
Organic lake’s sulfur chemistry is unusual in that it has the
highest DMS concentration of any natural water body. The primary source of DMS
in this case seems to be the cleavage rather than the demythilisation of DMSP
produced by eucaryal algae. Marinobacter
and Roseaovarius seem to be the main
organisms involved. The lake has low potential for dissimilatory sulfur
cycling, represented by low abundance of dsrAB,
aprAB and soxAB genes, hence the build up of DMS.
This study
shows how important different trophic strategies are in overcoming varying
levels of nutrient availabilities and may help to further our understanding of
other uncommon ecosystem types. The utilization of photoheterotrophy and other
mixotrophic strategies allows for carbon to be used in biosynthesis enabling
growth to occur with very limited carbon sources.
Yau, S., Lauro, F. M., Williams, T. J., Demaere, M. Z.,
Brown, M. V, Rich, J., Gibson, J. A., et al. (2013). Metagenomic insights into
strategies of carbon conservation and unusual sulfur biogeochemistry in a
hypersaline Antarctic lake. The ISME
journal, 7(10), 1944–1961.
Nice read. Very interesting. Quick question: this 'demythilisation', is that a process often commonly found within microbes? I'm struggling to find anything on it. If so, why is it that these microbes aren't taking advantage of this sulfur-rich environment?
ReplyDeleteIn a typical pelagic microbe community, the phytoplankton such as prymnesiophytes like Emiliana huxleyi and many others produce DMSP, which provides protection from osmotic stress amongst other things. When phytoplankton cells lyse (by grazing or the lytic cycle) the DMSP is released. Usually around 80-90% of it will be demethylated by microbes with the end products readily assimilated into the microbial loop. The cleavage route, using DMSP lyase enzymes is usually the less dominant process and is responsible for 10-20% of the total DMSP use. However in this particular ecosystem the cleavage pathway was, unusually, the dominant process. Cleavage is the only route that releases DMS into the atmosphere hence the high DMS concentration here. Hope that answers your question.
ReplyDelete