Biological carbon fixation | EPFL Graph Search

Biological carbon fixation or сarbon assimilation is the process by which inorganic carbon (particularly in the form of carbon dioxide) is converted to organic compounds by living organisms. The compounds are then used to store energy and as structure for other biomolecules. Carbon is primarily fixed through photosynthesis, but some organisms use a process called chemosynthesis in the absence of sunlight. Organisms that grow by fixing carbon are called autotrophs, which include photoautotrophs (which use sunlight), and lithoautotrophs (which use inorganic oxidation). Heterotrophs are not themselves capable of carbon fixation but are able to grow by consuming the carbon fixed by autotrophs or other heterotrophs. "Fixed carbon", "reduced carbon", and "organic carbon" may all be used interchangeably to refer to various organic compounds. Chemosynthesis is carbon fixation driven by chemical energy, rather than from sunlight. Sulfur- and hydrogen-oxidizing bacteria often use the Calvin cycle or the reductive citric acid cycle. The primary form of inorganic carbon that is fixed is carbon dioxide (CO2). It is estimated that approximately 258 billion tons of carbon dioxide are converted by photosynthesis annually. The majority of the fixation occurs in terrestrial environments, especially the tropics. The gross amount of carbon dioxide fixed is much larger since approximately 40% is consumed by respiration following photosynthesis. Seven autotrophic carbon fixation pathways are known. The Calvin cycle fixes carbon in the chloroplasts of plants and algae, and in the cyanobacteria. It also fixes carbon in the anoxygenic photosynthesis in one type of Pseudomonadota called purple bacteria, and in some non-phototrophic Pseudomonadota. Of the five other autotrophic pathways, two are known only in bacteria (the reductive citric acid cycle and the 3-hydroxypropionate cycle), two only in archaea (two variants of the 3-hydroxypropionate cycle), and one in both bacteria and archaea (the reductive acetyl CoA pathway).

Diel quenching of Southern Ocean phytoplankton fluorescence is related to iron limitation

Nina Schuback

Evaluation of photosynthetic competency in time and space is critical for better estimates and models of oceanic primary productivity. This is especially true for areas where the lack of iron (Fe) limits phytoplankton productivity, such as the Southern Ocean. Assessment of photosynthetic competency on large scales remains challenging, but phytoplankton chlorophyll a fluorescence (ChlF) is a signal that holds promise in this respect as it is affected by, and consequently provides information about, the photosynthetic efficiency of the organism. A second process affecting the ChlF signal is heat dissipation of absorbed light energy, referred to as non-photochemical quenching (NPQ). NPQ is triggered when excess energy is absorbed, i.e. when more light is absorbed than can be used directly for photosynthetic carbon fixation. The effect of NPQ on the ChlF signal complicates its interpretation in terms of photosynthetic efficiency, and therefore most approaches relating ChlF parameters to photosynthetic efficiency seek to minimize the influence of NPQ by working under conditions of sub-saturating irradiance. Here, we propose that NPQ itself holds potential as an easily acquired optical signal indicative of phytoplankton physiological state with respect to Fe limitation. We present data from a research voyage to the Subantarctic Zone south of Australia. Incubation experiments confirmed that resident phytoplankton were Fe-limited, as the maximum quantum yield of primary photochemistry, F-v/F-m, measured with a fast repetition rate fluorometer (FRRf), increased significantly with Fe addition. The NPQ "capacity" of the phytoplankton also showed sensitivity to Fe addition, decreasing with increased Fe availability, confirming previous work. The fortuitous presence of a remnant warm-core eddy in the vicinity of the study area allowed comparison of fluorescence behaviour between two distinct water masses, with the colder water showing significantly lower F-v/F-m than the warmer eddy waters, suggesting a difference in Fe limitation status between the two water masses. Again, NPQ capacity measured with the FRRf mirrored the behaviour observed in F-v/F-m, decreasing as F-v/F-m increased in the warmer water mass. We also analysed the diel quenching of underway fluorescence measured with a standard fluorometer, such as is frequently used to monitor ambient chlorophyll a concentrations, and found a significant difference in behaviour between the two water masses. This difference was quantified by defining an NPQ parameter akin to the Stern-Volmer parameterization of NPQ, exploiting the fluorescence quenching induced by diel fluctuations in incident irradiance. We propose that monitoring of this novel NPQ parameter may enable assessment of phytoplankton physiological status (related to Fe availability) based on measurements made with standard fluorometers, as ubiquitously used on moorings, ships, floats and gliders.

2020

Coral photosymbiosis: Linking phylogenetic identity to single cell metabolic activity in mixed symbiont populations

Anders Meibom, Isabelle Domart-Coulon, Maoz Fine, Béatrice Gaume

Tropical reef-building corals live in symbiosis with a wide range of micro-organisms, including unicellular Symbiodinium dinoflagellates also called zooxanthellae. These photosynthetic endosymbionts live inside the coral gastroderm cells. Although corals can feed on planktonic preys, the dinoflagellates significantly contribute to the nutrition of their host by transferring a large fraction (up to 90%) of photosynthates that are produced through the fixation of dissolved inorganic carbon (DIC) and nitrogen (nitrate or ammonium). Nine major clades (A-I) of Symbiodinium have been identified by molecular genetic analyses. Each clade presents distinct physiological features and the specific association between coral species and Symbiodinium clade determines the phenotype of the holobiont. Differences in the photosynthetic response to irradiance, rates of carbon fixation, and thermal tolerance can be attributed to symbiont clade. Several Symbiodinium clades can simultaneously exist within a single coral and the host can dynamically modify the proportion between dominant and background clades to adapt to changing environmental conditions. Investigating at the cellular level the metabolic exchanges between coral and Symbiodinium is of great interest to understand e.g. the bleaching process (loss of zooxanthellae) which often leads to coral death. We are aiming at quantitatively image the differential metabolic activity between symbiont clades in the same host, in the intact symbiosis. Previous studies have used mass bulk techniques to investigate the metabolism of symbionts at the colony scale. However, such studies cannot determine the specific contribution of the individual cells, as a function of their distribution in the coral host tissue. We have developed a SIMS-ISH method combining nanoscale secondary ion mass spectrometry (NanoSIMS) and in situ hybridization (ISH) for the simultaneous in situ identification of Symbiodinium genotype, and visualization of symbiont-host metabolic exchange at the level of individual cell. We focus on two reef-building coral species Pocillopora damicornis and Stylophora pistillata for which a large amount of complementary metabolic data exists. We designed specific fluorescent DNA probes to identify clade C Symbiodinium in P. damicornis and clade A in S. pistillata, and in mixed cultures. We combined the probes with pulse-chase experiments using isotopically labeled seawater (13C-bicarbonate and 15N-nitrate) to attribute a particular metabolism to a specific clade. This combined method enables us to phylogenetically identify metabolically active cells from a NanoSIMS isotopic/elemental image. The precise correlation between TEM and the NanoSIMS isotopic maps allows us to follow the turnover and translocation of metabolites with sub-cellular precision in both the symbionts and the host. Due to the complex nature of the coral symbiosis, the ability to discriminate the phylogenetic identity and metabolic role of specific Symbiodinium populations in situ is crucial to understand the effects of environmental stress on the coral holobiont plasticity. Moreover, analyzing symbiotic associations in situ provides a unique insight into the spatio-temporal patterns of metabolic interactions in holobionts. This analytical breakthrough promises to open entirely new areas of research focused on understanding the dynamics of interactions between animals and the microbial world.

2017

Identification and characterization of proteins supporting dehalorespiration in Desulfitobacterium hafniense strain TCE1

Laure Prat

Respiration is a fundamental catalytic process in the aerobic and anaerobic energy metabolism of many prokaryotic and most eukaryotic organisms. The major difference between these organisms is that various organic and inorganic substrates can be used to donate or accept electrons in the bacterial and archaeal kingdoms, in various ranges of redox potentials in order to drive aerobic (with oxygen as electron acceptor) and anaerobic respiratory pathways. During the last few decades, several bacterial strains have been reported to use chlorinated compounds as terminal electron acceptor under anaerobic conditions, in a process called dehalorespiration. Among more than thirty dehalorespiring bacterial strains isolated to date, the Dehalococcoides group and the Gram-positive genus Desulfitobacterium comprise the largest number of reductively dehalogenating pure cultures. While most Dehalococcoides isolates appeared as highly specialized bacteria that depend strictly on dehalorespiration for growth, members of the genus Desulfitobacterium are very versatile microorganisms with regards to the electron donors and acceptors utilized. Globally, this remarkable prokaryotic respiratory flexibility is guaranteed by an elaborate reservoir of complex redox enzymes. Regarding the specific electron transport chain involved in dehalorespiration, rather little knowledge has been obtained so far with the exception of the key enzyme, the reductive dehalogenase, well described in several dehalorespiring bacteria, and of little information on b-type cytochromes and menaquinones. The overall objective of this thesis was to identify new possible components of the electron transport chain by comparative proteomic analysis, to investigate the presence/absence of a regulatory pathway leading to the biosynthesis of the reductive dehalogenase, and finally to characterize newly identified proteins that might support the dehalorespiration process. A comparative 2D proteomic analysis was performed on Desulfitobacterium hafniense strain TCE1, a bacterium capable of using tetrachloroethene (PCE) as electron acceptor. Soluble and membrane-associated proteins were analyzed from cells cultivated on different couples of electron donors and acceptors, lactate – fumarate (LF), lactate – PCE (LP), hydrogen – fumarate (HF), and hydrogen – PCE (HP). Cells growing on LP or HP revealed 72 and 93 protein spots in membrane fraction, and 49 and 12 spots in soluble fraction that correspond to increasingly expressed proteins compared to their fumarate-grown counterparts. More than 80 proteins were identified by mass spectrometry analysis, among which the key enzyme in the dehalorespiration process, the PCE reductive dehalogenase (PceA), as well as interesting candidates which could support dehalorespiration. The possible role of these proteins was analyzed in further details. Involved in energy and carbon metabolisms, electron transfer flavoproteins (ETF) and proteins related to the Wood-Ljungdahl pathway of CO2 fixation were identified in HP growth conditions. Proteins associated to stress response such as the phage shock protein PspA, and to regulatory pathways, the transcriptional repressor CodY, were also observed and discussed. Although only slightly induced by PCE, an additional protein displaying homology to sulfur-transferases was found in a large abundance in the fraction of membrane-associated proteins. This protein was named PhsE, as the corresponding gene belongs to a gene operon with homology to the molybdoenzyme thiosulfate/polysulfide reductase operons (phs/psr) found in Salmonella typhimurium or Wolinella succinogenes. PhsE protein architecture resembles to the class of tandem-domain rhodaneses, with the particularity to contain two active-site cysteines. It is also characterized by the presence of a typical lipoprotein signal peptide (LSP), which anchors PhsE on the outside of the cytoplasmic membrane. In the genome sequence of D. hafniense strain Y51, phsE (DSY3892) is part of an apparent operon encoding one out of about sixty different members of the complex iron-sulfur molybdoenzyme (CISM) family. PhsA, the catalytic molybdoenzyme, displays significant sequence homology with the thiosulfate/polysulfide reductase (PhsA/PsrA) subfamily. So far no other CISM operon has been described with a sulfur-transferase encoding gene. Despite the numerous functions proposed for rhodanese in cyanide detoxification, Fe/S cluster formation, oxidative stress protection, sulfur mobilization and involvement in general sulfur metabolism, the question of the physiological role of PhsE remains open. The expression of the Phs complex appeared to be influenced by the addition of sulfide in the culture medium, generally used as reducing agent in anaerobic cultures. Sulfide is known to affect the intracellular redox status. Therefore, it is hypothesized that PhsE might be involved in the control of the redox balance of the cell, notably by scavenging potentially toxic reduced sulfur species. To support data obtained at the protein level during proteomic analysis, genes and the corresponding messenger RNA from D. hafniense strain TCE1 were studied. While in silico DNA sequence analysis did not reveal any obvious features regulating the transcription of pceA, puzzling results were obtained in proteomic analysis showing an almost complete absence of PceA in cells grown on fumarate. To characterize this phenomenon, starting from a routinely PCE-grown inoculum, strain TCE1 was repeatedly transferred on medium containing fumarate as electron acceptor. The pool of pceA gene in the total culture DNA decreased significantly already after fifteen successive sub-cultures on fumarate, suggesting a shift in strain TCE1 population upon relief of the PCE selection pressure. Consequently the level of pceA mRNA and PceA protein also followed the same trend. Secondly, a PCE pulse experiment was performed in an anaerobic continuous culture of strain TCE1 on fumarate. It revealed that PCE itself has no power of induction on genetic level, except for the positive effect observed on pspA transcripts which encodes a protein involved in cell membrane integrity. Finally the expression study of the phsFABCDE gene cluster revealed that all phs genes are co-transcribed, and most likely build an operon. Thus phsE seemed to be strictly coregulated with the phs operon, and not under the influence of another promoter. In conclusion, proteomic analysis enabled to investigate the general physiological status of Desulfitobacterium hafniense strain TCE1 during dehalorespiration. A tentative model of the dehalorespiration pathway is proposed in summarizing recent data obtained on the topology of the PCE reductive dehalogenase and on sequence similarity with proteins involved in other anaerobic respiratory pathways. Regarding the possible support of PhsE towards the dehalorespiration, the complicated chemistry of sulfur does not allow to clearly attribute a function to the Phs complex, but there are indications that it might build a 'sulfur' oxidoreductase which could catalyze the conversion of sulfide to polysulfide with concomitant electron transfer to the quinone pool. The sulfide oxidation activity might be useful to D. hafniense to scavenge toxic sulfur species, avoiding that they disturb the redox balance of the cell, and redox-sensitive enzymatic complexes.

EPFL2009