Transcriptional response of bathypelagic marine bacterioplankton to the Deepwater Horizon oil spill.

The Deepwater Horizon blowout released a massive amount of oil and gas into the deep ocean between April and July 2010, stimulating microbial blooms of petroleum-degrading bacteria. To understand the metabolic response of marine microorganisms, we sequenced ≈ 66 million community transcripts that revealed the identity of metabolically active microbes and their roles in petroleum consumption. Reads were assigned to reference genes from ≈ 2700 bacterial and archaeal taxa, but most assignments (39%) were to just six genomes representing predominantly methane- and petroleum-degrading Gammaproteobacteria. Specific pathways for the degradation of alkanes, aromatic compounds and methane emerged from the metatranscriptomes, with some transcripts assigned to methane monooxygenases representing highly divergent homologs that may degrade either methane or short alkanes. The microbial community in the plume was less taxonomically and functionally diverse than the unexposed community below the plume; this was due primarily to decreased species evenness resulting from Gammaproteobacteria blooms. Surprisingly, a number of taxa (related to SAR11, Nitrosopumilus and Bacteroides, among others) contributed equal numbers of transcripts per liter in both the unexposed and plume samples, suggesting that some groups were unaffected by the petroleum inputs and blooms of degrader taxa, and may be important for re-establishing the pre-spill microbial community structure.

Iron stress genes in marine Synechococcus and the development of a flow cytometric iron stress assay.

Marine Synechococcus are frequently found in environments where iron (Fe) is a limiting nutrient. To understand their capacity to respond to Fe stress, we screened picoplankton genomes and the Global Ocean Survey metagenome for known Fe stress genes. Many open ocean strains of Synechococcus lack most known genes for Fe stress, while coastal and upwelling strains contain many, suggesting that maintaining multiple Fe limitation compensation strategies is not a selective advantage in the open ocean. All genomes contained iron deficiency-induced protein A (IdiA) and its complementary Fe(3+) transport proteins. The ubiquity of IdiA was exploited to develop an in situ Fe stress bioassay based on immunolabelling and flow cytometry. As a test of field applicability, we used the assay on natural Synechococcus populations from one station in the Costa Rica Upwelling Dome where total Fe ranged from <0.08 to 0.14 nM in the upper water column. The bioassay found Fe stress in 5-54% of the population. Based on our findings, we believe that when reactive strains are present this assay can reveal environmental and clade-specific differences in the response of Synechococcus to Fe stress.