31 research outputs found
Nutrient utilisation by Trichodesmium characterisation of molecular and physiological Processes
No full textThe activity of photosynthetic cyanobacteria capable of nitrogen (N2) fixation (diazotrophs) strongly influences oceanic primary production and global biogeochemical cycles. The niche of these organisms extends mainly across low latitude oligotrophic oceans, largely deficient in nitrate, where they introduce ‘new’ nitrogen (N) to the system. In these regions the abundant marine cyanobacterium Trichodesmium spp. accounts for a significant proportion of the fixed N flux. Despite fixation of N, the availability of phosphorus (P) and iron (Fe) remain a constraint to the activity and biogeography of diazotrophs. The genome of Trichodesmium has therefore been shaped to provide intricate adaptive strategies optimising growth under both P and Fe depletion. Characterisation of these strategies can provide information that will enhance the understanding of the organism’s biogeography in the contemporary and future ocean. In this work, molecular and physiological techniques are employed to study nutrient uptake pathways, and the metabolic response of Trichodesmium erythraeum IMS101 (Trichodesmium hereafter) to nutrient limitation. The current lack of an established system for genetic manipulation of this organism inhibits direct functional characterisation of proteins. To circumvent this, the model cyanobacteria Synechocystis sp. PCC 6803 (Synechocystis hereafter) is used as a vehicle for the heterologous expression of Trichodesmium genes. Using this technique, the suggested contribution of Trichodesmium to an emerging oceanic P redox cycle is first explored. A four-gene cluster (ptxABCD), that encodes a putative ABC transporter (ptxABC) and NAD-dependent dehydrogenase (ptxD), is demonstrated to be responsible for the organism’s ability to utilise the reduced inorganic compound phosphite. The presence and expression of this gene cluster is also confirmed in diverse field metagenomic and metatranscriptomic datasets further confirming its role in Trichodesmium species. Pathways of Fe utilisation are also investigated. Through heterologous expression the function of a currently employed Fe stress biomarker, protein Tery_3377 (IdiA), which is homologous to both Fe3+ transporters (FutA2-like) and intracellular proteins with protective function under Fe stress (FutA1-like), is elucidated. Fusing the signal sequence of this protein to GFP revealed its periplasmic localisation, and its expression in Synechocystis mutants of both futA1 and futA2 paralogues further supported involvement in Fe3+ uptake, providing evidence for its function as an Fe transporter in Trichodesmium. Finally, a physiological experiment was performed to determine the significance of direct physical contact with Saharan desert dust for acquisition of Fe by Trichodesmium. It is demonstrated that cell surface processes are fundamental in dust-Fe utilisation by this organism and transcriptomic analysis identifies a number of unique genes regulated under different Fe and dust regimes including putative cell-surface proteins not previously studied in Trichodesmium. Combined, these studies have revealed a diverse array of molecular and physiological strategies potentially employed by Trichodesmium to survive and thrive on the ephemeral supplies of nutrients encountered in oligotrophic oceans, an attribute that facilitates its significant contribution to biogeochemical cycles.<br/
Phosphite utilization by the globally important marine diazotroph Trichodesmium
No full textSpecies belonging to the filamentous cyanobacterial genus Trichodesmium are responsible for a significant fraction of oceanic nitrogen fixation. The availability of phosphorus (P) likely constrains the growth of Trichodesmium in certain regions of the ocean. Moreover, Trichodesmium species have recently been shown to play a role in an emerging oceanic phosphorus redox cycle, further highlighting the key role these microbes play in many biogeochemical processes in the contemporary ocean. Here, we show that Trichodesmium erythraeum?IMS101 can grow on the reduced inorganic compound phosphite as its sole source of P. The components responsible for phosphite utilization are identified through heterologous expression of the T. erythraeum?IMS101 Tery_0365–0368 genes, encoding a putative adenosine triphosphate (ATP)-binding cassette transporter and nicotinamide adenine dinucleotide (NAD)-dependent dehydrogenase, in the model cyanobacteria Synechocystis sp. PCC6803. We demonstrate that only combined expression of both the transporter and the dehydrogenase enables Synechocystis to utilize phosphite, confirming the function of Tery_0365-0367 as a phosphite uptake system (PtxABC) and Tery_0368 as a phosphite dehydrogenase (PtxD). Our findings suggest that reported uptake of phosphite by Trichodesmium consortia in the field likely reflects an active biological process by Trichodesmium. These results highlight the diversity of phosphorus sources available to Trichodesmium in a resource-limited ocean
Desert Dust as a Source of Iron to the Globally Important Diazotroph Trichodesmium
No full textThe marine cyanobacterium Trichodesmium sp. accounts for approximately half of the annual ‘new’ nitrogen introduced to the global ocean but its biogeography and activity is often limited by the availability of iron (Fe). A major source of Fe to the open ocean is Aeolian dust deposition in which Fe is largely comprised of particles with reduced bioavailability over soluble forms of Fe. We report that Trichodesmium erythraeum IMS101 has improved growth rate and photosynthetic physiology and down-regulates Fe-stress biomarker genes when cells are grown in the direct vicinity of, rather than physically separated from, Saharan dust particles as the sole source of Fe. These findings suggest that availability of non-soluble forms of dust-associated Fe may depend on cell contact. Transcriptomic analysis further reveals unique profiles of gene expression in all tested conditions, implying that Trichodesmium has distinct molecular signatures related to acquisition of Fe from different sources. Trichodesmium thus appears to be capable of employing specific mechanisms to access Fe from complex sources in oceanic systems, helping to explain its role as a key microbe in global biogeochemical cycles
Dynamics of extracellular superoxide production by Trichodesmium colonies from the Sargasso Sea
No full textReactive oxygen species (ROS) are key players in the health and biogeochemistry of the ocean and its inhabitants. The vital contribution of microorganisms to marine ROS levels, particularly superoxide, has only recently come to light, and thus the specific biological sources and pathways involved in ROS production are largely unknown. To better understand the biogenic controls on ROS levels in tropical oligotrophic systems, we determined rates of superoxide production under various conditions by natural populations of the nitrogen-fixing diazotroph Trichodesmium obtained from various surface waters in the Sargasso Sea. Trichodesmium colonies collected from eight different stations all produced extracellular superoxide at high rates in both the dark and light. Colony density and light had a variable impact on extracellular superoxide production depending on the morphology of the Trichodesmium colonies. Raft morphotypes showed a rapid increase in superoxide production in response to even low levels of light, which was not observed for puff colonies. In contrast, superoxide production rates per colony decreased with increasing colony density for puff morphotypes but not for rafts. These findings point to Trichodesmium as a likely key source of ROS to the surface oligotrophic ocean. The physiological and/or ecological factors underpinning morphology-dependent controls on superoxide production need to be unveiled to better understand and predict superoxide production by Trichodesmium and ROS dynamics within marine systems
Structural and functional characterisation of IdiA/FutA (Tery_3377), an iron binding protein from the ocean diazotroph Trichodesmium erythraeum
No full textAtmospheric nitrogen fixation by photosynthetic cyanobacteria (diazotrophs) strongly influences oceanic primary production and in turn affects global biogeochemical cycles. Species of the genus Trichodesmium are major contributors to marine diazotrophy, accounting for a significant proportion of the fixed nitrogen in tropical and subtropical oceans. However, Trichodesmium spp. are metabolically constrained by the availability of iron, an essential element for both the photosynthetic apparatus and the nitrogenase enzyme. Survival strategies in low-iron environments are typically poorly characterized at the molecular level, as these bacteria are recalcitrant to genetic manipulation. Here, we studied a homolog of the iron deficiency-induced A (IdiA)/ferric uptake transporter A (FutA) protein, Tery_3377, which has been used as an in situ iron-stress biomarker. IdiA/FutA has an ambiguous function in cyanobacteria, with its homologs hypothesized to be involved in distinct processes depending on their cellular localization. Using signal sequence fusions to GFP and heterologous expression in the model cyanobacterium Synechocystis sp. PCC 6803 we show that Tery_3377 is targeted to the periplasm by the twin-arginine translocase and can complement the deletion of the native Synechocystis ferric-iron ABC transporter periplasmic binding protein (FutA2). EPR spectroscopy revealed that purified recombinant Tery_3377 has specificity for iron in the Fe3+ state, and an X-ray crystallography determined structure uncovered a functional iron substrate-binding domain, with Fe3+ penta-coordinated by protein and buffer ligands. Our results support assignment of Tery_3377 as a functional FutA subunit of an Fe3+ ABC-transporter, but do not rule out that it also has dual IdiA function
Quantifying integrated proteomic responses to iron stress in the globally important marine diazotroph trichodesmium
No full textTrichodesmium is a biogeochemically important marine cyanobacterium, responsible for a significant proportion of the annual ‘new’ nitrogen introduced into the global ocean. These non-heterocystous filamentous diazotrophs employ a potentially unique strategy of near-concurrent nitrogen fixation and oxygenic photosynthesis, potentially burdening Trichodesmium with a particularly high iron requirement due to the iron-binding proteins involved in these processes. Iron availability may therefore have a significant influence on the biogeography of Trichodesmium. Previous investigations of molecular responses to iron stress in this keystone marine microbe have largely been targeted. Here a holistic approach was taken using a label-free quantitative proteomics technique (MSE) to reveal a sophisticated multi-faceted proteomic response of Trichodesmium erythraeum IMS101 to iron stress. Increased abundances of proteins known to be involved in acclimation to iron stress and proteins known or predicted to be involved in iron uptake were observed, alongside decreases in the abundances of iron-binding proteins involved in photosynthesis and nitrogen fixation. Preferential loss of proteins with a high iron content contributed to overall reductions of 55–60% in estimated proteomic iron requirements. Changes in the abundances of iron-binding proteins also suggested the potential importance of alternate photosynthetic pathways as Trichodesmium reallocates the limiting resource under iron stress. Trichodesmium therefore displays a significant and integrated proteomic response to iron availability that likely contributes to the ecological success of this species in the ocean
The molecular basis of phosphite and hypophosphite recognition by ABC-transporters
No full textInorganic phosphate is the major bioavailable form of the essential nutrient phosphorus. However, the concentration of phosphate in most natural habitats is low enough to limit microbial growth. Under phosphate-depleted conditions some bacteria utilise phosphite and hypophosphite as alternative sources of phosphorus, but the molecular basis of reduced phosphorus acquisition from the environment is not fully understood. Here, we present crystal structures and ligand binding affinities of periplasmic binding proteins from bacterial phosphite and hypophosphite ATP-binding cassette transporters. We reveal that phosphite and hypophosphite specificity results from a combination of steric selection and the presence of a P-H…π interaction between the ligand and a conserved aromatic residue in the ligand-binding pocket. The characterisation of high affinity and specific transporters has implications for the marine phosphorus redox cycle, and might aid the use of phosphite as an alternative phosphorus source in biotechnological, industrial and agricultural applications
Transcriptional responses of Trichodesmium to natural inverse gradients of Fe and P availability
No full textThe filamentous diazotrophic cyanobacterium Trichodesmium is responsible for a significant fraction of marine di-nitrogen (N2) fixation. Growth and distribution of Trichodesmium and other diazotrophs in the vast oligotrophic subtropical gyres is influenced by iron (Fe) and phosphorus (P) availability, while reciprocally influencing the biogeochemistry of these nutrients. Here we use observations across natural inverse gradients in Fe and P in the North Atlantic subtropical gyre (NASG) to demonstrate how Trichodesmium acclimates in situ to resource availability. Transcriptomic analysis identified progressive upregulation of known iron-stress biomarker genes with decreasing Fe availability, and progressive upregulation of genes involved in the acquisition of diverse P sources with decreasing P availability, while genes involved in N2 fixation were upregulated at the intersection under moderate Fe and P availability. Enhanced N2 fixation within the Fe and P co-stressed transition region was also associated with a distinct, consistent metabolic profile, including the expression of alternative photosynthetic pathways that potentially facilitate ATP generation required for N2 fixation with reduced net oxygen production. The observed response of Trichodesmium to availability of both Fe and P supports suggestions that these biogeochemically significant organisms employ unique molecular, and thus physiological responses as adaptations to specifically exploit the Fe and P co-limited niche they construct
Experiment design and bacterial abundance control extracellular H2O2 concentrations during four series of mesocosm experiments
No full textThe extracellular concentration of H2O2 in surface aquatic environments is controlled by a balance between photochemical production and the microbial synthesis of catalase and peroxidase enzymes to remove H2O2 from solution. In any kind of incubation experiment, the formation rates and equilibrium concentrations of reactive oxygen species (ROSs) such as H2O2 may be sensitive to both the experiment design, particularly to the regulation of incident light, and the abundance of different microbial groups, as both cellular H2O2 production and catalase–peroxidase enzyme production rates differ between species. Whilst there are extensive measurements of photochemical H2O2 formation rates and the distribution of H2O2 in the marine environment, it is poorly constrained how different microbial groups affect extracellular H2O2 concentrations, how comparable extracellular H2O2 concentrations within large-scale incubation experiments are to those observed in the surface-mixed layer, and to what extent a mismatch with environmentally relevant concentrations of ROS in incubations could influence biological processes differently to what would be observed in nature. Here we show that both experiment design and bacterial abundance consistently exert control on extracellular H2O2 concentrations across a range of incubation experiments in diverse marine environments.
During four large-scale (>1000 L) mesocosm experiments (in Gran Canaria, the Mediterranean, Patagonia and Svalbard) most experimental factors appeared to exert only minor, or no, direct effect on H2O2 concentrations. For example, in three of four experiments where pH was manipulated to 0.4–0.5 below ambient pH, no significant change was evident in extracellular H2O2 concentrations relative to controls. An influence was sometimes inferred from zooplankton density, but not consistently between different incubation experiments, and no change in H2O2 was evident in controlled experiments using different densities of the copepod Calanus finmarchicus grazing on the diatom Skeletonema costatum (<1 % change in [H2O2] comparing copepod densities from 1 to 10 L−1). Instead, the changes in H2O2 concentration contrasting high- and low-zooplankton incubations appeared to arise from the resulting changes in bacterial activity. The correlation between bacterial abundance and extracellular H2O2 was stronger in some incubations than others (R2 range 0.09 to 0.55), yet high bacterial densities were consistently associated with low H2O2. Nonetheless, the main control on H2O2 concentrations during incubation experiments relative to those in ambient, unenclosed waters was the regulation of incident light. In an open (lidless) mesocosm experiment in Gran Canaria, H2O2 was persistently elevated (2–6-fold) above ambient concentrations; whereas using closed high-density polyethylene mesocosms in Crete, Svalbard and Patagonia H2O2 within incubations was always reduced (median 10 %–90 %) relative to ambient waters
New insights into the distributions of nitrogen fixation and diazotrophs revealed by high-resolution sensing and sampling methods
No full textNitrogen availability limits marine productivity across large ocean regions. Diazotrophs can supply new nitrogen to the marine environment via nitrogen (N2) fixation, relieving nitrogen limitation. The distributions of diazotrophs and N2 fixation have been hypothesized to be generally controlled by temperature, phosphorus, and iron availability in the global ocean. However, even in the North Atlantic where most research on diazotrophs and N2 fixation has taken place, environmental controls remain contentious. Here we measure diazotroph composition, abundance, and activity at high resolution using newly developed underway sampling and sensing techniques. We capture a diazotrophic community shift from Trichodesmium to UCYN-A between the oligotrophic, warm (25–29 °C) Sargasso Sea and relatively nutrient-enriched, cold (13–24 °C) subpolar and eastern American coastal waters. Meanwhile, N2 fixation rates measured in this study are among the highest ever recorded globally and show significant increase with phosphorus availability across the transition from the Gulf Stream into subpolar and coastal waters despite colder temperatures and higher nitrate concentrations. Transcriptional patterns in both Trichodesmium and UCYN-A indicate phosphorus stress in the subtropical gyre. Over this iron-replete transect spanning the western North Atlantic, our results suggest that temperature is the major factor controlling the diazotrophic community structure while phosphorous drives N2 fixation rates. Overall, the occurrence of record-high UCYN-A abundance and peak N2 fixation rates in the cold coastal region where nitrate concentrations are highest (~200 nM) challenges current paradigms on what drives the distribution of diazotrophs and N2 fixation
