Jennifer M. DeBruyn

Global Biogeography and Quantitative Seasonal Dynamics of Gemmatimonadetes in Soil

ABSTRACT Bacteria belonging to phylum Gemmatimonadetes comprise approximately 2% of soil bacterial communities. However, little is known of their ecology due to a lack of cultured representation. Here we present evidence from biogeographical analyses and seasonal quantification of Gemmatimonadetes in soils, which suggests an adaptation to low soil moisture.

Microbial control of diatom bloom dynamics in the open ocean

[1] Diatom blooms play a central role in supporting foodwebs and sequestering biogenic carbon to depth. Oceanic conditions set bloom initiation, whereas both environmental and ecological factors determine bloom magnitude and longevity. Our study reveals another fundamental determinant of bloom dynamics. A diatom spring bloom in offshore New Zealand waters was likely terminated by iron limitation, even though diatoms consumed <1/3 of the mixed-layer dissolved iron inventory. Thus, bloom duration and magnitude were primarily set by competition for dissolved iron between microbes and small phytoplankton versus diatoms. Significantly, such a microbial mode of control probably relies both upon out-competing diatoms for iron (i.e., K-strategy), and having high iron requirements (i.e., r-strategy). Such resource competition for iron has implications for carbon biogeochemistry, as, blooming diatoms fixed three-fold more carbon per unit iron than resident non-blooming microbes. Microbial sequestration of iron has major ramifications for determining the biogeochemical imprint of oceanic diatom blooms. Citation: Boyd, P. W., et al. (2012), Microbial control of diatom bloom dynamics in the open ocean, Geophys. Res. Lett., 39, L18601, doi:10.1029/2012GL053448.

Microbial Distributions and the Impact of Phosphorus on Bacterial Activity in Lake Erie

Abstract In light of recent suggestions concerning the relaxation of controls on phosphorus loading in Lake Erie, and in consideration of our current lack of baseline information on microbial communities in this system, a two-part analysis of the microbial ecology of the lake has been conducted. A comprehensive survey of the surface waters collected data on phytoplankton abundance, bacterial productivity and abundance, and viral abundance that were previously not available for Lake Erie. In parallel, phosphorus amendment experiments were conducted in each of the three hydrologically distinct basins of the lake to determine the effect of increased phosphorus loading on bacterial abundance and productivity. After 72 hours incubation, the addition of phosphorus had a significant impact on the microbial food web. A proliferation of different size classes of phytoplankton was accompanied by increases in bacterial production, but not necessarily bacterial abundance. Observations confirmed previous studies suggesting that the microbial communities in each of the three basins responded differently to the addition of phosphorus. Accompanying nutrient data suggest that the responses were due to limitation by other factors in the presence of excess phosphorus; namely that phytoplankton became nitrogen limited whereas bacteria became carbon limited. These results confirm the importance of the microbial food web in understanding the impact of phosphorus loading on the biotic carbon flow in the Lake Erie ecosystem.

Characterization and field trials of a bioluminescent bacterial reporter of iron bioavailability

To better understand Fe cycling in marine and freshwater systems, we have developed a biomolecular tool to track the perceived bioavailability of Fe to heterotrophic bacteria. Bioluminescent reporters, constructed by fusing the fepA–fes promoter of Escherichia coli (an Enterobactin biosynthesis gene regulated by the ferric uptake regulatory [Fur] system) to a luxCDABE cassette, were integrated into the chromosome of a halotolerant Pseudomonas putida, which uses the Fur system to regulate high-affinity Fe uptake. The resultant P. putida bioreporter has been successfully tested both in lab and field studies. Laboratory cultures were maintained at a range of concentrations of total Fe (0–25 nM) or limited by the addition of concentrations of wellcharacterized siderophores (desferrioxamine B [DFB], ferrichrome, 2,2V-dipyridyl [DP] and Rhodotorulic acid [RA], 0–200 nM) and used to establish the dynamic range of this reporter system. Analysis of sample incubations after only 4 h suggest that both of the trihydroxamate-type siderophores DFB and ferrichrome efficiently reduced Fe availability, resulting respectively in a 1.77- and 1.88-fold increase in luminescence relative to Fe-replete conditions. In contrast, additions of the dihydroxamate-type siderophore RA and the synthetic chelator DP resulted in no response from the system, suggesting that cells could access Fe complexed to these compounds without activating high-affinity Fe transport systems. Field studies were performed in the central basin of Lake Erie, which has previously been shown to undergo sporadic Fe limitation during summer stratification. DFB concentrations were titrated across a range of 0–50 nM into unfiltered water to manipulate Fe availabilities. Bioreporters expressed Fe stress (ca. a 2-fold increase in luminescence) at concentrations of DFB equivalent to the total (dissolved+particulate) Fe in the system (c30 nM), indicative of the concentration of bioavailable Fe. In a similar experiment with 0.2-Am pre-filtered water (2.25–5.24 nM Fe), a 6-fold increase in luminescence (relative to controls) was observed at the lowest (15 nM) concentration of chelators. The results of this study demonstrate the validity of bioreporters as a complimentary tool to measurements of total Fe. Moreover, these results suggest that a significant source of

Functional and Structural Succession of Soil Microbial Communities below Decomposing Human Cadavers

The ecological succession of microbes during cadaver decomposition has garnered interest in both basic and applied research contexts (e.g. community assembly and dynamics; forensic indicator of time since death). Yet current understanding of microbial ecology during decomposition is almost entirely based on plant litter. We know very little about microbes recycling carcass-derived organic matter despite the unique decomposition processes. Our objective was to quantify the taxonomic and functional succession of microbial populations in soils below decomposing cadavers, testing the hypotheses that a) periods of increased activity during decomposition are associated with particular taxa; and b) human-associated taxa are introduced to soils, but do not persist outside their host. We collected soils from beneath four cadavers throughout decomposition, and analyzed soil chemistry, microbial activity and bacterial community structure. As expected, decomposition resulted in pulses of soil C and nutrients (particularly ammonia) and stimulated microbial activity. There was no change in total bacterial abundances, however we observed distinct changes in both function and community composition. During active decay (7 - 12 days postmortem), respiration and biomass production rates were high: the community was dominated by Proteobacteria (increased from 15.0 to 26.1% relative abundance) and Firmicutes (increased from 1.0 to 29.0%), with reduced Acidobacteria abundances (decreased from 30.4 to 9.8%). Once decay rates slowed (10 - 23 d postmortem), respiration was elevated, but biomass production rates dropped dramatically; this community with low growth efficiency was dominated by Firmicutes (increased to 50.9%) and other anaerobic taxa. Human-associated bacteria, including the obligately anaerobic Bacteroides, were detected at high concentrations in soil throughout decomposition, up to 198 d postmortem. Our results revealed the pattern of functional and compositional succession in soil microbial communities during decomposition of human-derived organic matter, provided insight into decomposition processes, and identified putative predictor populations for time since death estimation.

Horizontal transfer of PAH catabolism genes in Mycobacterium: evidence from comparative genomics and isolated pyrene-degrading bacteria.

Biodegradation of high molecular weight polycyclic aromatic hydrocarbons (PAHs), such as pyrene and benzo[a]pyrene, has only been observed in a few genera, namely fast-growing Mycobacterium and Rhodococcus. In M. vanbaalenii PYR-1, multiple aromatic ring hydroxylating dioxygenase (ARHDOs) genes including pyrene dioxygenases nidAB and nidA3B3 are localized in one genomic region. Here we examine the homologous genomic regions in four other PAH-degrading Mycobacterium (strains JLS, KMS, and MCS, and M. gilvum PYR-GCK), presenting evidence for past horizontal gene transfer events. Seven distinct types of ARHDO genes are present in all five genomes, and display conserved syntenic architecture with respect to gene order, orientation, and association with other genes. Duplications and putative integrase and transposase genes suggest past gene shuffling. To corroborate these observations, pyrene-degrading strains were isolated from two PAH-contaminated sediments: Chattanooga Creek (Tennessee) and Lake Erie (western basin). Some were related to fast-growing Mycobacterium spp. and carried both nidA and nidA3 genes. Other isolates belonged to Microbacteriaceae and Intrasporangiaceae presenting the first evidence of pyrene degradation in these families. These isolates had nidA (and some, nidA3) genes that were homologous to Mycobacterial ARHDO genes, suggesting that horizontal gene transfer events have occurred.

Complete genome sequence of Thauera aminoaromatica strain MZ1T

Thauera aminoaromatica strain MZ1T, an isolate belonging to genus Thauera, of the family Rhodocyclaceae and the class the Betaproteobacteria, has been characterized for its ability to produce abundant exopolysaccharide and degrade various aromatic compounds with nitrate as an electron acceptor. These properties, if fully understood at the genome-sequence level, can aid in environmental processing of organic matter in anaerobic cycles by short-circuiting a central anaerobic metabolite, acetate, from microbiological conversion to methane, a critical greenhouse gas. Strain MZ1T is the first strain from the genus Thauera with a completely sequenced genome. The 4,496,212 bp chromosome and 78,374 bp plasmid contain 4,071 protein-coding and 71 RNA genes, and were sequenced as part of the DOE Community Sequencing Program CSP_776774.

Temporal changes in particle-associated microbial communities after interception by nonlethal sediment traps.

Using marine sediment traps (named RESPIRE for REspiration of Sinking Particles In the subsuRface ocEan) designed to collect sinking particles and associated microbial communities in situ, we collected and incubated marine aggregates/particles in the southern Pacific Ocean from separate phytoplankton bloom events in situ. We determined the phylogenetic affiliation for the microorganisms growing on aggregates by pyrosequencing partial 16S rRNA gene amplicons. Water column samples were also collected and sequenced for comparison between sinking-particle-associated and planktonic bacterial communities. Statistically significant differences were found between the water column and sediment trap bacteria. Relative abundances of Pelagibacter sp. and multiple members of the Flavobacteria, Actinobacteria, and α-Proteobacteria were elevated in water column samples, while trap samples contained members of the Roseobacter clade of α-Proteobacteria in high relative abundances. Our findings indicated that rapid changes - within 24 h of collection - occurred to the microbial community associated with aggregates from either bloom type. There was a little change in the bacterial assemblage after the initial 24-h incubation period. The most abundant early colonizer was a Sulfitobacter sp. This study provides further evidence that Roseobacters are rapid colonizers of marine aggregates and that colonization can occur on short timescales. This study further demonstrates that particle origin may be insignificant regarding the heterotrophic bacterial population that degrades them.

Viral and bacterial abundance and production in the Western Pacific Ocean and the relation to other oceanic realms

We completed a transect through the Western Pacific Warm Pool to examine how environmental variables may influence viral and bacterial abundance and production rates in this globally important oceanic region. Of the variables analyzed, viral abundance and production had the most significant relationship to bacterial cell abundance: viral parameters were not significantly correlated to the measured environmental variables, including temperature. Bacterial production rates were significantly correlated to temperature in open ocean waters, but not in waters close to land masses. Analyses of 16S rRNA gene by pyrosequencing indicated only minor changes in eubacterial community structure across the transect, with α-proteobacteria dominating all sampled populations. Diversity within the prokaryotic community did not correlate directly with viral abundance or activity. Comparisons to two other ocean-scale transects (> 8000 km of open ocean in total) in the Atlantic Ocean indicated that correlations between viral and bacterial abundance and production relative to environmental variables are regime dependent. In particular, correlations to temperature showed remarkable differences across the three transects. Collectively, our observations suggest that seemingly similar oceanic regions may have very different microbial community responses to environmental variables. Our observations and analyses demonstrate that ocean-scale generalizations may not apply in the case of viral ecology.

The Microbiome of Ehrlichia-Infected and Uninfected Lone Star Ticks (Amblyomma americanum)

The Lone Star tick, Amblyomma americanum, transmits several bacterial pathogens including species of Anaplasma and Ehrlichia. Amblyomma americanum also hosts a number of non-pathogenic bacterial endosymbionts. Recent studies of other arthropod and insect vectors have documented that commensal microflora can influence transmission of vector-borne pathogens; however, little is known about tick microbiomes and their possible influence on tick-borne diseases. Our objective was to compare bacterial communities associated with A. americanum, comparing Anaplasma/Ehrlichia -infected and uninfected ticks. Field-collected questing specimens (n = 50) were used in the analyses, of which 17 were identified as Anaplasma/Ehrlichia infected based on PCR amplification and sequencing of groEL genes. Bacterial communities from each specimen were characterized using Illumina sequencing of 16S rRNA gene amplicon libraries. There was a broad range in diversity between samples, with inverse Simpson’s Diversity indices ranging from 1.28–89.5. There were no statistical differences in the overall microbial community structure between PCR diagnosed Anaplasma/Ehrlichia-positive and negative ticks, but there were differences based on collection method (P < 0.05), collection site (P < 0.05), and sex (P < 0.1) suggesting that environmental factors may structure A. americanum microbiomes. Interestingly, there was not always agreement between Illumina sequencing and PCR diagnostics: Ehrlichia was identified in 16S rRNA gene libraries from three PCR-negative specimens; conversely, Ehrlichia was not found in libraries of six PCR-positive ticks. Illumina sequencing also helped identify co-infections, for example, one specimen had both Ehrlichia and Anaplasma. Other taxa of interest in these specimens included Coxiella, Borrelia, and Rickettsia. Identification of bacterial community differences between specimens of a single tick species from a single geographical site indicates that intra-species differences in microbiomes were not due solely to pathogen presence/absence, but may be also driven by vector life history factors, including environment, life stage, population structure, and host choice.