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The enigmatic SAR202 cluster up close: shedding light on a globally distributed dark ocean lineage involved in sulfur cycling
M. Mehrshad, F. Rodriguez-Valera, MA. Amoozegar, P. López-García, R. Ghai,
Jazyk angličtina Země Anglie, Velká Británie
Typ dokumentu časopisecké články, práce podpořená grantem
NLK
PubMed Central
od 2011
Europe PubMed Central
od 2011 do Před 1 rokem
ProQuest Central
od 2007-05-01 do Před 1 rokem
Health & Medicine (ProQuest)
od 2007-05-01 do Před 1 rokem
Oxford Journals Open Access Collection
od 2007
- MeSH
- Chloroflexi klasifikace genetika izolace a purifikace metabolismus MeSH
- fylogeneze MeSH
- genomika MeSH
- metagenom MeSH
- metagenomika MeSH
- mikrobiota MeSH
- mořská voda mikrobiologie MeSH
- oceány a moře MeSH
- síra metabolismus MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Geografické názvy
- oceány a moře MeSH
The dark ocean microbiota represents the unknown majority in the global ocean waters. The SAR202 cluster belonging to the phylum Chloroflexi was the first microbial lineage discovered to specifically inhabit the aphotic realm, where they are abundant and globally distributed. The absence of SAR202 cultured representatives is a significant bottleneck towards understanding their metabolic capacities and role in the marine environment. In this work, we use a combination of metagenome-assembled genomes from deep-sea datasets and publicly available single-cell genomes to construct a genomic perspective of SAR202 phylogeny, metabolism and biogeography. Our results suggest that SAR202 cluster members are medium sized, free-living cells with a heterotrophic lifestyle, broadly divided into two distinct clades. We present the first evidence of vertical stratification of these microbes along the meso- and bathypelagic ocean layers. Remarkably, two distinct species of SAR202 cluster are highly abundant in nearly all deep bathypelagic metagenomic datasets available so far. SAR202 members metabolize multiple organosulfur compounds, many appear to be sulfite-oxidizers and are predicted to play a major role in sulfur turnover in the dark water column. This concomitantly suggests an unsuspected availability of these nutrient sources to allow for the high abundance of these microbes in the deep sea.
Citace poskytuje Crossref.org
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