The core properties of microbial genomes, including GC content and genome size, are known to vary widely among different bacteria and archaea . Several hypotheses have been proposed to explain this genomic variability, but the fundamental drivers that shape bacterial and archaeal genomic properties remain uncertain . Here, we report the existence of a sharp genomic transition zone below the photic zone, where bacterial and archaeal genomes and proteomes undergo a community-wide punctuated shift. Across a narrow range of increasing depth of just tens of metres, diverse microbial clades trend towards larger genome size, higher genomic GC content, and proteins with higher nitrogen but lower carbon content. These community-wide changes in genome features appear to be driven by gradients in the surrounding environmental energy and nutrient fields. Collectively, our data support hypotheses invoking nutrient limitation as a central driver in the evolution of core bacterial and archaeal genomic and proteomic properties.
Up and down go the cyanobacteria
Plankton move together in strikingly coordinated daily patterns, sinking at night to avoid being eaten and rising to the surface in daylight to photosynthesize. Otteson
et al.
found similar activity patterns in even the smallest of planktonic organisms, such as photosynthetic bacteria (see the Perspective by Armbrust). Because it's hard to take regular samples in the open ocean, the authors built a robotic sampler and set it adrift for several days in the mid-Pacific. The captured bacteria showed immediate responses to changes in light, temperature, and salinity in ways that could affect the ocean's carbon and nitrogen cycles.
Science
, this issue p.
207
; see also p.
134
As part of an ongoing survey of microbial community gene expression in the ocean, we sequenced and compared B38 Mbp of community transcriptomes and B157 Mbp of community genomes from four bacterioplankton samples, along a defined depth profile at Station ALOHA in North Pacific subtropical gyre (NPSG). Taxonomic analysis suggested that the samples were dominated by three taxa: Prochlorales, Consistiales and Cenarchaeales, which comprised 36-69% and 29-63% of the annotated sequences in the four DNA and four cDNA libraries, respectively. The relative abundance of these taxonomic groups was sometimes very different in the DNA and cDNA libraries, suggesting differential relative transcriptional activities per cell. For example, the 125 m sample genomic library was dominated by Pelagibacter (B36% of sequence reads), which contributed fewer sequences to the community transcriptome (B11%). Functional characterization of highly expressed genes suggested taxon-specific contributions to specific biogeochemical processes. Examples included Roseobacter relatives involved in aerobic anoxygenic phototrophy at 75 m, and an unexpected contribution of low abundance Crenarchaea to ammonia oxidation at 125 m. Read recruitment using reference microbial genomes indicated depth-specific partitioning of coexisting microbial populations, highlighted by a transcriptionally active high-light-like Prochlorococcus population in the bottom of the photic zone. Additionally, nutrient-uptake genes dominated Pelagibacter transcripts, with apparent enrichment for certain transporter types (for example, the C4-dicarboxylate transport system) over others (for example, phosphate transporters). In total, the data support the utility of coupled DNA and cDNA analyses for describing taxonomic and functional attributes of microbial communities in their natural habitats.
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