Nejvíce citovaný článek - PubMed ID 25350155
Investigations of phytoplankton responses to iron stress in seawater are complicated by the fact that iron concentrations do not necessarily reflect bioavailability. Most studies to date have been based on single species or field samples and are problematic to interpret. Here, we report results from an experimental cocultivation model system that enabled us to evaluate interspecific competition as a function of iron content and form, and to study the effect of nutritional conditions on the proteomic profiles of individual species. Our study revealed that the dinoflagellate Amphidinium carterae was able to utilize iron from a hydroxamate siderophore, a strategy that could provide an ecological advantage in environments where siderophores present an important source of iron. Additionally, proteomic analysis allowed us to identify a potential candidate protein involved in iron acquisition from hydroxamate siderophores, a strategy that is largely unknown in eukaryotic phytoplankton.
- Klíčová slova
- (s)PLS-DA, (sparse) partial least squares discriminant analysis, AUC, area under curve, Amphidinium carterae, AtpE, ATP synthase, BCS, bathocuproinedisulfonic acid disodium salt, CREG1, cellular repressor of E1A stimulated genes 1, DFOB, desferrioxamine B, EDTA, ethylenediaminetetraacetic acid, ENT, enterobactin, FACS, fluorescence-activated cell sorting, FBAI, fructose-bisphosphate aldolase I, FBAII, fructose-bisphosphate aldolase II, FBP1, putative ferrichrome-binding protein, FOB, ferrioxamine B, Flow cytometry, ISIP, iron starvation induced protein, Iron, LHCX, light-harvesting complex subunits, LL, long-term iron limitation, LR, iron enrichment, Marine microalgae, NBD, nitrobenz-2-oxa-1,3-diazole, NPQ, nonphotochemical quenching, PAGE, polyacrylamide gel electrophoresis, PSI, photosystem I, PSII, photosystem II, PetA, cytochrome b6/f, Proteomics, PsaC, photosystem I iron-sulfur center, PsaD, photosystem I reaction center subunit II, PsaE, photosystem I reaction center subunit IV, PsaL, photosystem I reaction center subunit XI, PsbC, photosystem II CP43 reaction center protein, PsbV, cytochrome c-550, RR, long-term iron sufficiency, SOD1, superoxide dismutase [Cu-Zn], Siderophores,
- Publikační typ
- časopisecké články MeSH
UNLABELLED: The model pennate diatom Phaeodactylum tricornutum is able to assimilate a range of iron sources. It therefore provides a platform to study different mechanisms of iron processing concomitantly in the same cell. In this study, we follow the localization of three iron starvation induced proteins (ISIPs) in vivo, driven by their native promoters and tagged by fluorophores in an engineered line of P. tricornutum. We find that the localization patterns of ISIPs are dynamic and variable depending on the overall iron status of the cell and the source of iron it is exposed to. Notwithstanding, a shared destination of the three ISIPs both under ferric iron and siderophore-bound iron supplementation is a globular compartment in the vicinity of the chloroplast. In a proteomic analysis, we identify that the cell engages endocytosis machinery involved in the vesicular trafficking as a response to siderophore molecules, even when these are not bound to iron. Our results suggest that there may be a direct vesicle traffic connection between the diatom cell membrane and the periplastidial compartment (PPC) that co-opts clathrin-mediated endocytosis and the "cytoplasm to vacuole" (Cvt) pathway, for proteins involved in iron assimilation. Proteomics data are available via ProteomeXchange with identifier PXD021172. HIGHLIGHT: The marine diatom P. tricornutum engages a vesicular network to traffic siderophores and phytotransferrin from the cell membrane directly to a putative iron processing site in the vicinity of the chloroplast.
- Klíčová slova
- P. tricornutum, diatoms, fluorescent proteins, iron, iron starvation induced proteins, proteome, siderophores,
- Publikační typ
- časopisecké články MeSH
Oceanic phytoplankton species have highly efficient mechanisms of iron acquisition, as they can take up iron from environments in which it is present at subnanomolar concentrations. In eukaryotes, three main models were proposed for iron transport into the cells by first studying the kinetics of iron uptake in different algal species and then, more recently, by using modern biological techniques on the model diatom Phaeodactylum tricornutum. In the first model, the rate of uptake is dependent on the concentration of unchelated Fe species, and is thus limited thermodynamically. Iron is transported by endocytosis after carbonate-dependent binding of Fe(III)' (inorganic soluble ferric species) to phytotransferrin at the cell surface. In this strategy the cells are able to take up iron from very low iron concentration. In an alternative model, kinetically limited for iron acquisition, the extracellular reduction of all iron species (including Fe') is a prerequisite for iron acquisition. This strategy allows the cells to take up iron from a great variety of ferric species. In a third model, hydroxamate siderophores can be transported by endocytosis (dependent on ISIP1) after binding to the FBP1 protein, and iron is released from the siderophores by FRE2-dependent reduction. In prokaryotes, one mechanism of iron uptake is based on the use of siderophores excreted by the cells. Iron-loaded siderophores are transported across the cell outer membrane via a TonB-dependent transporter (TBDT), and are then transported into the cells by an ABC transporter. Open ocean cyanobacteria do not excrete siderophores but can probably use siderophores produced by other organisms. In an alternative model, inorganic ferric species are transported through the outer membrane by TBDT or by porins, and are taken up by the ABC transporter system FutABC. Alternatively, ferric iron of the periplasmic space can be reduced by the alternative respiratory terminal oxidase (ARTO) and the ferrous ions can be transported by divalent metal transporters (FeoB or ZIP). After reoxidation, iron can be taken up by the high-affinity permease Ftr1.
- Klíčová slova
- iron, iron uptake, micro-algae, ocean, phytoplankton,
- Publikační typ
- časopisecké články MeSH
- přehledy MeSH
Iron uptake by diatoms is a biochemical process with global biogeochemical implications. In large regions of the surface ocean diatoms are both responsible for the majority of primary production and frequently experiencing iron limitation of growth. The strategies used by these phytoplankton to extract iron from seawater constrain carbon flux into higher trophic levels and sequestration into sediments. In this study we use reverse genetic techniques to target putative iron-acquisition genes in the model pennate diatom Phaeodactylum tricornutum We describe components of a reduction-dependent siderophore acquisition pathway that relies on a bacterial-derived receptor protein and provides a viable alternative to inorganic iron uptake under certain conditions. This form of iron uptake entails a close association between diatoms and siderophore-producing organisms during low-iron conditions. Homologs of these proteins are found distributed across diatom lineages, suggesting the significance of siderophore utilization by diatoms in the marine environment. Evaluation of specific proteins enables us to confirm independent iron-acquisition pathways in diatoms and characterize their preferred substrates. These findings refine our mechanistic understanding of the multiple iron-uptake systems used by diatoms and help us better predict the influence of iron speciation on taxa-specific iron bioavailability.
- Klíčová slova
- diatom, ferric reductase, iron acquisition, phytoplankton, siderophore,
- MeSH
- biologická dostupnost MeSH
- biologický transport MeSH
- CRISPR-Cas systémy MeSH
- druhová specificita MeSH
- FMN-reduktasa genetika metabolismus MeSH
- fylogeneze MeSH
- galium metabolismus MeSH
- genový knockout MeSH
- klimatické změny MeSH
- membránové transportní proteiny genetika metabolismus MeSH
- mikrobiota MeSH
- mořská voda chemie MeSH
- oxidace-redukce MeSH
- proteiny vnější bakteriální membrány metabolismus MeSH
- receptory buněčného povrchu metabolismus MeSH
- rekombinantní fúzní proteiny metabolismus MeSH
- rozsivky genetika růst a vývoj metabolismus MeSH
- siderofory metabolismus MeSH
- železo metabolismus MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Research Support, U.S. Gov't, Non-P.H.S. MeSH
- Názvy látek
- ferric citrate iron reductase MeSH Prohlížeč
- FMN-reduktasa MeSH
- galium MeSH
- membránové transportní proteiny MeSH
- proteiny vnější bakteriální membrány MeSH
- receptory buněčného povrchu MeSH
- rekombinantní fúzní proteiny MeSH
- siderofory MeSH
- siderophore receptors MeSH Prohlížeč
- železo MeSH
In vast areas of the ocean, the scarcity of iron controls the growth and productivity of phytoplankton. Although most dissolved iron in the marine environment is complexed with organic molecules, picomolar amounts of labile inorganic iron species (labile iron) are maintained within the euphotic zone and serve as an important source of iron for eukaryotic phytoplankton and particularly for diatoms. Genome-enabled studies of labile iron utilization by diatoms have previously revealed novel iron-responsive transcripts, including the ferric iron-concentrating protein ISIP2A, but the mechanism behind the acquisition of picomolar labile iron remains unknown. Here we show that ISIP2A is a phytotransferrin that independently and convergently evolved carbonate ion-coordinated ferric iron binding. Deletion of ISIP2A disrupts high-affinity iron uptake in the diatom Phaeodactylum tricornutum, and uptake is restored by complementation with human transferrin. ISIP2A is internalized by endocytosis, and manipulation of the seawater carbonic acid system reveals a second-order dependence on the concentrations of labile iron and carbonate ions. In P. tricornutum, the synergistic interaction of labile iron and carbonate ions occurs at environmentally relevant concentrations, revealing that carbonate availability co-limits iron uptake. Phytotransferrin sequences have a broad taxonomic distribution and are abundant in marine environmental genomic datasets, suggesting that acidification-driven declines in the concentration of seawater carbonate ions will have a negative effect on this globally important eukaryotic iron acquisition mechanism.
- MeSH
- biologický transport MeSH
- endocytóza MeSH
- fytoplankton klasifikace genetika metabolismus MeSH
- genom genetika MeSH
- koncentrace vodíkových iontů MeSH
- lidé MeSH
- molekulární evoluce MeSH
- mořská voda chemie MeSH
- rozsivky genetika metabolismus MeSH
- transferin metabolismus MeSH
- uhličitany metabolismus MeSH
- vodní organismy klasifikace genetika metabolismus MeSH
- železo metabolismus MeSH
- Check Tag
- lidé MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Research Support, U.S. Gov't, Non-P.H.S. MeSH
- Názvy látek
- transferin MeSH
- uhličitany MeSH
- železo MeSH
Iron is an essential micronutrient involved in many biological processes and is often limiting for primary production in large regions of the World Ocean. Metagenomic and physiological studies have identified clades or ecotypes of marine phytoplankton that are specialized in iron depleted ecological niches. Although less studied, eukaryotic picophytoplankton does contribute significantly to primary production and carbon transfer to higher trophic levels. In particular, metagenomic studies of the green picoalga Ostreococcus have revealed the occurrence of two main clades distributed along coast-offshore gradients, suggesting niche partitioning in different nutrient regimes. Here, we present a study of the response to iron limitation of four Ostreococcus strains isolated from contrasted environments. Whereas the strains isolated in nutrient-rich waters showed high iron requirements, the oceanic strains could cope with lower iron concentrations. The RCC802 strain, in particular, was able to maintain high growth rate at low iron levels. Together physiological and transcriptomic data indicate that the competitiveness of RCC802 under iron limitation is related to a lowering of iron needs though a reduction of the photosynthetic machinery and of protein content, rather than to cell size reduction. Our results overall suggest that iron is one of the factors driving the differentiation of physiologically specialized Ostreococcus strains in the ocean.
BACKGROUND: Low iron bioavailability is a common feature of ocean surface water and therefore micro-algae developed original strategies to optimize iron uptake and metabolism. The marine picoeukaryotic green alga Ostreococcus tauri is a very good model for studying physiological and genetic aspects of the adaptation of the green algal lineage to the marine environment: it has a very compact genome, is easy to culture in laboratory conditions, and can be genetically manipulated by efficient homologous recombination. In this study, we aimed at characterizing the mechanisms of iron assimilation in O. tauri by combining genetics and physiological tools. Specifically, we wanted to identify and functionally characterize groups of genes displaying tightly orchestrated temporal expression patterns following the exposure of cells to iron deprivation and day/night cycles, and to highlight unique features of iron metabolism in O. tauri, as compared to the freshwater model alga Chalamydomonas reinhardtii. RESULTS: We used RNA sequencing to investigated the transcriptional responses to iron limitation in O. tauri and found that most of the genes involved in iron uptake and metabolism in O. tauri are regulated by day/night cycles, regardless of iron status. O. tauri lacks the classical components of a reductive iron uptake system, and has no obvious iron regulon. Iron uptake appears to be copper-independent, but is regulated by zinc. Conversely, iron deprivation resulted in the transcriptional activation of numerous genes encoding zinc-containing regulation factors. Iron uptake is likely mediated by a ZIP-family protein (Ot-Irt1) and by a new Fea1-related protein (Ot-Fea1) containing duplicated Fea1 domains. The adaptation of cells to iron limitation involved an iron-sparing response tightly coordinated with diurnal cycles to optimize cell functions and synchronize these functions with the day/night redistribution of iron orchestrated by ferritin, and a stress response based on the induction of thioredoxin-like proteins, of peroxiredoxin and of tesmin-like methallothionein rather than ascorbate. We briefly surveyed the metabolic remodeling resulting from iron deprivation. CONCLUSIONS: The mechanisms of iron uptake and utilization by O. tauri differ fundamentally from those described in C. reinhardtii. We propose this species as a new model for investigation of iron metabolism in marine microalgae.
- Klíčová slova
- Iron, Marine phytoplankton, Ostreococcus, RNA-seq analysis,
- MeSH
- biologická adaptace MeSH
- Chlorophyta klasifikace genetika metabolismus MeSH
- Eukaryota genetika metabolismus MeSH
- fotoperioda MeSH
- fylogeneze MeSH
- fytoplankton genetika metabolismus MeSH
- fyziologický stres MeSH
- homeostáza MeSH
- měď metabolismus MeSH
- oxidace-redukce MeSH
- regulace genové exprese účinky záření MeSH
- rostlinné proteiny genetika metabolismus MeSH
- shluková analýza MeSH
- signální transdukce MeSH
- sloučeniny železa metabolismus MeSH
- stanovení celkové genové exprese MeSH
- transkriptom MeSH
- vysoce účinné nukleotidové sekvenování MeSH
- železo metabolismus MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Názvy látek
- měď MeSH
- rostlinné proteiny MeSH
- sloučeniny železa MeSH
- železo MeSH
In large regions of the open ocean, iron is a limiting resource for phytoplankton. The reduction of iron quota and the recycling of internal iron pools are among the diverse strategies that phytoplankton have evolved to allow them to grow under chronically low ambient iron levels. Phytoplankton species also have evolved strategies to cope with sporadic iron supply such as long-term storage of iron in ferritin. In the picophytoplanktonic species Ostreococcus we report evidence from observations both in the field and in laboratory cultures that ferritin and the main iron-binding proteins involved in photosynthesis and nitrate assimilation pathways show opposite diurnal expression patterns, with ferritin being maximally expressed during the night. Biochemical and physiological experiments using a ferritin knock-out line subsequently revealed that this protein plays a central role in the diel regulation of iron uptake and recycling and that this regulation of iron homeostasis is essential for cell survival under iron limitation.
- Klíčová slova
- Ostreococcus, circadian, ferritin, iron, phytoplankton,
- MeSH
- chemická precipitace MeSH
- cirkadiánní rytmus * účinky léků genetika účinky záření MeSH
- ferritin genetika metabolismus MeSH
- fytoplankton účinky léků genetika růst a vývoj metabolismus MeSH
- hmotnostní spektrometrie MeSH
- homeostáza * účinky léků genetika účinky záření MeSH
- kinetika MeSH
- mikrobiální viabilita účinky léků účinky záření MeSH
- mořská voda mikrobiologie MeSH
- proteiny vázající železo metabolismus MeSH
- regulace genové exprese účinky léků účinky záření MeSH
- světlo MeSH
- transkriptom genetika MeSH
- western blotting MeSH
- železo metabolismus farmakologie MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Názvy látek
- ferritin MeSH
- proteiny vázající železo MeSH
- železo MeSH
