Thesis (M.S.)--Mississippi State University. Department of Biological Sciences. / Title from title screen. Includes bibliographical references.

No description available.

The FeMo cofactor is one of two types of prosthetic group found in the larger of the two nitrogenase component proteins, called the MoFe protein, and it is strongly implicated as the substrate binding and reduction site. The glutamine-191 residue in the Alpha-subunit of the MoFe protein of A. vinelandii nitrogenase was targeted for substitution because its side chain is involved in a hydrogen-bond network from one of the terminal carboxylates of the homocitrate component of FeMo cofactor through to the backbone NH of Alpha Gly-61, which is adjacent to Alpha Cys-62, which ligates to the P cluster (the second type of prosthetic group in the MoFe protein). A variety of altered MoFe proteins produced by the A. vinelandii mutant strains, namely the Alpha Pro-191, Alpha Ser-191, Alpha Thr-191, Alpha His-191, Alpha Glu-191, and Alpha Arg-191 altered MoFe proteins, have been purified to homogeneity and the catalytic properties of these altered MoFe proteins have been compared to those of wild type MoFe protein. Unlike wild type, the six altered MoFe proteins have decreased catalytic activity on substrate reduction and exhibited H2 evolution that was partially inhibited by added CO. Moreover, some of altered MoFe proteins with lower specific activity for the C2H4 production can produce C2H6 from C2H2. The results from the pH and activity studies indicate that the substitutions on the MoFe protein have an effect on the contribution of the responsible acid-base group(s) involved in proton transfer for H+- and C2H2-reduction. Furthermore, the inhibition by CO of hydrogen evolution by these altered MoFe proteins is likely from a lowering of the rate of both electron and proton transfer to the H+- reduction site(s). Some altered MoFe proteins but not wild type MoFe protein can produce C2H6 from C2H2. This observation suggested a lower apparent binding affinity for C2H2 and a slower proton transfer to C2H2 reduction with these altered MoFe proteins, which allow the intermediate to stay at the site longer and be further reduced by two electrons and two protons to give C2H6. These changes in the biochemical properties of these altered MoFe proteins indicate that the Alpha Gln-191 residue is intimately involved in substrate binding and reduction including proton delivery to substrate. / Ph. D.

Os modelos de evolução de vias metabólicas estão baseados em técnicas moleculares e bioinformática e nem sempre levam em consideração o contextos fisiológico e ecológico do organismo. Assim, tomando como plataforma o metabolismo de nitrogênio, procurou-se estabelecer uma hipótese evolutiva para o uso de α-aminoácidos por metazoários como fonte de nitrogênio. O objetivo é traçar essa história evolutiva, contextualizando fisiológica e ecologicamente as alterações que ocorreram no perfil de utilização desses compostos. Para traçar essa história evolutiva, recorreu-se a dados disponíveis na literatura partindo-se dos elementos moleculares/metabólicos que compõem o ciclo do nitrogênio e em qual contexto geológico e evolutivo se deu tal história. Os dados obtidos, reorganizados e reestruturados nesse novo contexto, permitiram conclusões originais no presente trabalho, a saber: (1) a capacidade de fixação de nitrogênio atmosférico foi um fator de seleção natural positiva na transição da atmosfera redutora para oxidante; (2) os organismos fixadores de nitrogênio são bem mais disseminados do que o admitido classicamente; (3) o produto final da fixação biológica de nitrogênio in vivo são α- aminoácidos, e foram um fator de pressão seletiva para os organismos incapazes de fixar nitrogênio; (4) os metazoários evoluíram posteriormente a esse cenário e seu aparato metabólico está mais adaptado para o aproveitamento líquido do nitrogênio obtido apenas na forma de α-aminoácidos. / Metabolic pathway evolution models are molecular and computational based, and do not take account the physiological and ecological contexts in which organisms are inserted. Thus using the nitrogen metabolism as a platform, an evolutionary hypothesis on the α-amino acids utilization by metazoans was proposed. The objective of the present work is to trace an evolutionary history of the nitrogen usage by metazoans taking account the profile changes on a physiological and ecological basis. In order to trace this evolutionary history, a scrutiny were performed in the specialized literature aiming at data about the molecular and metabolic elements which perform the nitrogen cycle and in which geologic and evolutive context has passed such history. The reorganization of obtained data in a new context allowed original conclusions in the present work as follows: (1) the capability of fixing the atmospheric nitrogen was a positive selection factor in the atmospheric condition transition from reductive to oxidant; (2) nitrogen fixing organisms are far most wide spread than classically admitted; (3) α-amino acids are the biological nitrogen fixation end product in vivo, and are a selective factor for non-fixing organisms; (4) metazoans evolved afterwards in these scenario and their metabolic apparatus is adapted to the nitrogen net utilization obtained in the α-amino acid form.

Os modelos de evolução de vias metabólicas estão baseados em técnicas moleculares e bioinformática e nem sempre levam em consideração o contextos fisiológico e ecológico do organismo. Assim, tomando como plataforma o metabolismo de nitrogênio, procurou-se estabelecer uma hipótese evolutiva para o uso de α-aminoácidos por metazoários como fonte de nitrogênio. O objetivo é traçar essa história evolutiva, contextualizando fisiológica e ecologicamente as alterações que ocorreram no perfil de utilização desses compostos. Para traçar essa história evolutiva, recorreu-se a dados disponíveis na literatura partindo-se dos elementos moleculares/metabólicos que compõem o ciclo do nitrogênio e em qual contexto geológico e evolutivo se deu tal história. Os dados obtidos, reorganizados e reestruturados nesse novo contexto, permitiram conclusões originais no presente trabalho, a saber: (1) a capacidade de fixação de nitrogênio atmosférico foi um fator de seleção natural positiva na transição da atmosfera redutora para oxidante; (2) os organismos fixadores de nitrogênio são bem mais disseminados do que o admitido classicamente; (3) o produto final da fixação biológica de nitrogênio in vivo são α- aminoácidos, e foram um fator de pressão seletiva para os organismos incapazes de fixar nitrogênio; (4) os metazoários evoluíram posteriormente a esse cenário e seu aparato metabólico está mais adaptado para o aproveitamento líquido do nitrogênio obtido apenas na forma de α-aminoácidos. / Metabolic pathway evolution models are molecular and computational based, and do not take account the physiological and ecological contexts in which organisms are inserted. Thus using the nitrogen metabolism as a platform, an evolutionary hypothesis on the α-amino acids utilization by metazoans was proposed. The objective of the present work is to trace an evolutionary history of the nitrogen usage by metazoans taking account the profile changes on a physiological and ecological basis. In order to trace this evolutionary history, a scrutiny were performed in the specialized literature aiming at data about the molecular and metabolic elements which perform the nitrogen cycle and in which geologic and evolutive context has passed such history. The reorganization of obtained data in a new context allowed original conclusions in the present work as follows: (1) the capability of fixing the atmospheric nitrogen was a positive selection factor in the atmospheric condition transition from reductive to oxidant; (2) nitrogen fixing organisms are far most wide spread than classically admitted; (3) α-amino acids are the biological nitrogen fixation end product in vivo, and are a selective factor for non-fixing organisms; (4) metazoans evolved afterwards in these scenario and their metabolic apparatus is adapted to the nitrogen net utilization obtained in the α-amino acid form.

In aquatic environments the availability of nitrogen (N) generally limits primary production. N2-fixing prokaryotes (diazotrophs) can convert N2 gas into ammonium and provide significant input of N into the oceans. Cyanobacteria are thought to be the main N2-fixers but diazotrophs also include a wide range of heterotrophic bacteria. However, their activity and regulation in the water column is largely unknown. In this thesis the distribution, diversity, abundance, and activity of marine and estuarine heterotrophic diazotrophs was investigated. With molecular methods targeting the nifH gene, encoding the nitrogenase enzyme for N2 fixation, it was shown that diverse nifH genes affiliating with heterotrophic bacteria were ubiquitous in surface waters from ten marine locations world-wide and the estuarine Baltic Sea. Through enrichment cultures of Baltic Sea surface water in anaerobic N-free medium, heterotrophic N2 fixation was induced showing that there was a functional N2-fixing community present and isolates of heterotrophic diazotrophs were obtained. In Sargasso Sea surface waters, transcripts of nifH related to heterotrophic bacteria were detected indicating heterotrophic N2-fixing activity. Nitrogenase expression is thought to be highly regulated by the availability of inorganic N and the presence of oxygen. Low oxygen zones within the water column can be found in association with plankton. The presence of diazotrophs as symbionts of heterotrophic dinoflagellates was investigated and nifH genes related to heterotrophic diazotrophs rather than the cyanobacterial symbionts were found, suggesting that a symbiotic co-existence prevailed. Oxic-anoxic interfaces could also be potential sites for heterotrophic N2 fixation. The Baltic Sea contains large areas of anoxic bottom water. At the chemocline and in anoxic deep water heterotrophic diazotrophs were diverse, abundant and active. These findings extend the currently known regime of N2 fixation to also include ammonium-rich anaerobic waters. The results of this thesis suggest that heterotrophic diazotrophs are diverse and widely distributed in marine and estuarine waters and that they can also be active. However, limits in the knowledge on their physiology and factors which regulate their N2 fixation activity currently prevent an evaluation of their importance in the global marine N budget.

L’atmosphère terrestre est très riche en azote (N2). Mais cet azote diatomique est sous une forme très stable, inutilisable par la majorité des êtres vivants malgré qu’il soit indispensable pour la synthèse de matériels organiques. Seuls les procaryotes diazotrophiques sont capables de vivre avec le N2 comme source d’azote. La fixation d’azote est un processus qui permet de produire des substances aminées à partir de l’azote gazeux présent dans l’atmosphère (78%). Cependant, ce processus est très complexe et nécessite la biosynthèse d’une vingtaine de protéines et la consommation de beaucoup d’énergie (16 molécules d’ATP par mole de N2 fixé). C’est la raison pour laquelle ce phénomène est rigoureusement régulé. Les bactéries photosynthétiques pourpres non-sulfureuses sont connues pour leur capacité de faire la fixation de l’azote. Les études faites à la lumière, dans le mode de croissance préféré de ces bactéries (photosynthèse anaérobie), ont montré que la nitrogénase (enzyme responsable de la fixation du diazote) est sujet d’une régulation à trois niveaux: une régulation transcriptionnelle de NifA (protéine activatrice de la transcription des gènes nif), une régulation post-traductionnelle de l’activité de NifA envers l’activation de la transcription des autres gènes nif, et la régulation post-traductionnelle de l’activité de la nitrogénase quand les cellules sont soumises à un choc d’ammoniaque. Le système de régulation déjà décrit fait intervenir essentiellement une protéine membranaire, AmtB, et les deux protéines PII, GlnB et GlnK. Il est connu depuis long temps que la nitrogénase est aussi régulée quand une culture photosynthétique est exposée à la noirceur, mais jusqu’aujourd’hui, on ignore encore la nature des systèmes intervenants dans cette régulation. Ainsi, parmi les questions qui peuvent se poser: quelles sont les protéines qui interviennent dans l’inactivation de la nitrogénase lorsqu’une culture anaérobie est placée à la noirceur? Une analyse de plusieurs souches mutantes, amtB- , glnK- , glnB- et amtY- poussées dans différentes conditions de limitation en azote, serait une façon pour répondre à ces interrogations. Alors, avec le suivi de l’activité de la nitrogénase et le Western Blot, on a montré que le choc de noirceur provoquerait un "Switch-off" de l’activité de la nitrogénase dû à une ADP-ribosylation de la protéine Fe. On a réussit aussi à montrer que ii tout le système déjà impliqué dans la réponse à un choc d’ammoniaque, est également nécessaire pour une réponse à un manque de lumière ou d’énergie (les protéines AmtB, GlnK, GlnB, DraG, DraT et AmtY). Or, Rhodobacter capsulatus est capable de fixer l’azote et de croitre aussi bien dans la micro-aérobie à la noirceur que dans des conditions de photosynthèse anaérobies, mais jusqu'à maintenant sa régulation dans l’obscurité est peu étudiée. L’étude de la fixation d’azote à la noirceur nous a permis de montrer que le complexe membranaire Rnf n’est pas nécessaire à la croissance de R. capsulatus dans de telles conditions. Dans le but de développer une façon d’étudier la régulation de la croissance dans ce mode, on a tout d’abord essayé d’identifier les conditions opératoires (O2, [NH4 + ]) permettant à R. capsulatus de fixer l’azote en microaérobie. L’optimisation de cette croissance a montré que la concentration optimale d’oxygène nécessaire est de 10% mélangé avec de l’azote. / The atmosphere of the Earth is very rich in nitrogen (N2). However, diatomic nitrogen is very stable and therefore unusable by the majority of life forms even though it is necessary for the synthesis of a variety of organic compounds. Only diazotrophic procaryotes are capable of using N2 as nitrogen source. Their nitrogen fixation allows the production of aminated compounds from atmospheric nitrogen (78 %). However, this process is very complex and requires the biosynthesis of about twenty proteins and the consumption of a lot of energy (16 molecules of ATP per molecule of N2 fixed), thus necessitating its tight regulation. The purple non-sulfur photosynthetic bacteria are known for their ability to carry out nitrogen fixation. Studies conducted in the light, the preferred mode of growth of these bacteria (anaerobic photosynthetic), have shown that nitrogenase (the enzyme responsible for dinitrogen fixation) is subject to regulation at three levels: transcriptional regulation of NifA (activator protein for the transcription of nif genes), posttranslational regulation of the activity of NifA to activate nif gene transcription, and posttranslational regulation of nitrogenase activity when cells are subjected to an ammonium shock. The control system already described involves essentially a membrane protein, AmtB and both PII proteins, GlnK and GlnB. It has long been known that nitrogenase is regulated when light is suddenly removed from a culture, but until now it is unclear whether these systems are also involved in the regulation of nitrogen fixation in dark. Thus, one outstanding question is what are the proteins involved in the inactivation of nitrogenase when a light-grown culture is placed in the dark? An analysis of several mutant strains; amtB-, glnK-, glnB-, and amtY- under different conditions of nitrogen deficiency was used to address this question. Using measurements of nitrogenase activity and Fe protein modification by Western blotting, we were able to show that darkness causes a "switch-off” of nitrogenase due to ADP- ribosylation of Fe protein. Thus, the system that has already been described as involved in the response to a lack of ammonia, is also required for a response to a lack of light or energy (AmtB, GlnK, GlnB, DraG, and DraT, and AmtY). However, Rhodobacter capsulatus is also able to fix nitrogen and grow micro-aerobically in the dark as well as photosynthetically under anaerobic conditions, but so far its regulation in the dark has been little studied. The study of nitrogen fixation in the dark allowed us to show that the Rnf membrane complex is not required for growth of R. capsulatus in such conditions. In order to develop a way to study its regulation during this growth mode, we have attempted to identify the operating conditions (O2, [NH4+]), allowing R. capsulatus to fix nitrogen micro-aerobically. The optimization of this conditions has shown that the optimal concentration of oxygen required is 10% mixed with nitrogen.

L’azote est l’élément le plus abondant dans l’atmosphère terrestre avec un pourcentage atteignant 78 %. Composant essentiel pour la biosynthèse des matériels organiques cellulaires, il est inutilisable sous sa forme diatomique (N2) très stable par la plupart des organismes. Seules les bactéries dites diazotrophiques comme Rhodobacter capsulatus sont capables de fixer l’azote moléculaire N2 par le biais de la synthèse d’une enzyme, la nitrogénase. Cette dernière catalyse la réduction du N2 en ammonium (NH4) qui peut alors être assimilé par d’autres organismes. La synthèse et l’activité de la nitrogénase consomment beaucoup d’énergie ce qui implique une régulation rigoureuse et son inhibition tant qu’une quantité suffisante d’ammonium est disponible. Parmi les protéines impliquées dans cette régulation, la protéine d’intérêt AmtB est un transporteur membranaire responsable de la perception et le transport de l’ammonium. Chez R. capsulatus, il a été démontré que suite à l’addition de l’ammonium, l’AmtB inhibe de façon réversible (switch off/switch on) l’activité de la nitrogénase en séquestrant la protéine PII GlnK accompagnée de l’ajout d’un groupement ADP ribose sur la sous unités Fe de l’enzyme par DraT. De plus, la formation de ce complexe à lui seul ne serait pas suffisant pour cette inactivation, ce qui suggère la séquestration d’une troisième protéine, DraG, afin d’inhiber son action qui consiste à enlever l’ADP ribose de la nitrogénase et donc sa réactivation. Afin de mieux comprendre le fonctionnement de l’AmtB dans la régulation et le transport de l’ammonium à un niveau moléculaire et par la même occasion la fixation de l’azote, le premier volet de ce mémoire a été d’introduire une mutation ponctuelle par mutagénèse dirigée au niveau du résidu conservé W237 de l’AmtB. La production d’hydrogène est un autre aspect longtemps étudié chez R. capsulatus. Cette bactérie est capable de produire de l’hydrogène à partir de composés organiques par photofermentation suite à l’intervention exclusive de la nitrogénase. Plusieurs études ont été entreprises afin d’améliorer la production d’hydrogène. Certaines d’entre elles se sont intéressées à déterminer les conditions optimales qui confèrent une production maximale de gaz tandis que d’autres s’intéressent au fonctionnement de la bactérie elle même. Ainsi, le fait que la bioproduction de H2 par fermentation soit catalysée par la nitrogénase cela implique la régulation de l’activité de cette dernière par différents mécanismes dont le switch off par ADP ribosylation de l’enzyme. De ce fait, un mutant de R. capsulatus dépourvu d’AmtB (DG9) a été étudié dans la deuxième partie de cette thèse en termes d’activité de la nitrogénase, de sa modification par ADP ribosylation avec la détection des deux protéines GlnK et DraG qui interviennent dans cette régulation pour connaitre l’influence de différents acides aminés sur la régulation de la nitrogénase et pour l‘utilisation future de cette souche dans la production d’H2 car R. capsulatus produit de l’hydrogène par photofermentation grâce à cette enzyme. Les résultats obtenus ont révélé une activité de la nitrogénase continue et ininterrompue lorsque l’AmtB est absent avec une activité maximale quand la proline est utilisée comme source d’azote durant la culture bactérienne ce qui implique donc que l’abolition de l’activité de cette protéine entraine une production continue d’H2 chez R. capsulatus lorsque la proline est utilisée comme source d’azote lors de la culture bactérienne. Par ailleurs, avec des Western blots on a pu déterminer l’absence de régulation par ADP ribosylation ainsi que les expressions respectives de GlnK et DraG inchangées entre R. capsulatus sauvage et muté. En conclusion, la nitrogénase n’est pas modifiée et inhibée lorsque l’amtB est muté ce qui fait de la souche R. capsulatus DG9 un candidat idéal pour la production de biohydrogène en particulier lorsque du glucose et de la proline sont respectivement utilisés comme source de carbone et d'azote pour la croissance. / Nitrogen is the most abundant element in the Earth's atmosphere with a percentage of 78 %. This element is essential for the biosynthesis of cellular organic material and is unusable in its stable diatomic form (N2) by most organisms. Only bacteria called diazotrophs such as Rhodobacter capsulatus are able to fix molecular nitrogen N2 through the synthesis of the nitrogenase enzyme. The latter catalyzes the reduction of N2 to NH4 which can then be absorbed by other organisms. The synthesis and activity of nitrogenase consumes a lot of energy and therefore implies a strict regulation and its inhibition when a sufficient amount of ammonium is available. Among the proteins involved in this regulation, is the membrane transporter AmtB which is responsible for the sensing and transportation of ammonia. In R. capsulatus, it was shown that following the addition of ammonium, AmtB reversibly inhibits (switch off / switch on) nitrogenase activity by sequestering the PII protein GlnK accompanied by the addition of an ADP ribose group onto the Fe subunit of the enzyme by DraT. In addition, the formation of this complex alone would not be sufficient for this inactivation, suggesting the sequestration of a third protein, DraG is required to inhibit its action of removing the ADP ribose from the nitrogenase and therefore its reactivation. To better understand the role of the AmtB in the fixation of nitrogen, regulation and transport of ammonium at the molecular level, the first part of this study was to introduce a point mutation by directed mutagenesis in the conserved residue W237 of AmtB . Hydrogen production is another property of R. capsulatus that has been studied for a long time. This bacterium is capable of producing hydrogen from organic compounds following photofermentation and the exclusive enzymatic intervention of nitrogenase. Several studies have been undertaken to improve the production of hydrogen. Some of them were involved in determining the optimum conditions that give maximum gas production while others were interested in improving the growth of the bacterium itself. Thus, since the bio-production of H2 by fermentation is catalyzed by the nitrogenase, it is important to study the regulation of the activity of this enzyme by different mechanisms such as the switch off by ADP ribosylation. Therefore, a mutant of R. capsulatus (DG9) lacking AmtB was studied in the second part of this thesis for its nitrogenase activity, its modification by GlnK-DraG, and to see the effects of different amino acids used in the growth medium on the regulation and therefore the future use of this strain for the production of H2. The results showed a continuous and uninterrupted activity of the nitrogenase when AmtB was absent with a maximum activity when proline was used as a nitrogen source for bacterial growth. In addition, Western blots were used to demonstrate the effect of ADP ribosylation on regulation and that the expression of GlnK and DraG were unchanged between the wild –type and mutant R. capsulatus. In conclusion, nitrogenase is not modified or inhibited when mutated amtB what makes the R. capsulatus strain DG9 an ideal candidate for biohydrogen production especially when glucose and proline are respectively used as source carbon and nitrogen for growth.

β-N-methylamino-L-alanine (BMAA) is one of the more recently discovered bioactive compounds produced by cyanobacteria. BMAA is a non-protein amino acid reported present in human brain tissues of patients deceased from a neurodegenerative disease, such as Alzheimer´s disease or amyotrophic lateral sclerosis (ALS). This observation in combination with its neurotoxic effects in eukaryotes (in vivo and in vitro) and its potential to incorporate into (human) proteins, causing protein aggregation, suggests BMAA as a possible causative environmental agent for neurodegenerative diseases. Due to the ubiquitous nature of cyanobacteria with a wide occurrence in both aquatic and terrestrial environments, BMAA could be globally spread. Hence, investigations of a possible coupling between BMAA and neurodegeneration are urgently needed as well as to identify sources of BMAA in Nature. The aim of this thesis was to examine the potential occurrence of BMAA in bloom forming cyanobacteria of the Baltic Sea and its possible transfer to other organisms of this ecosystem. Of importance was also to reveal any likely routes for human BMAA exposure in the Baltic Sea region and to further investigate BMAA as a triggering agent for neurodegenerative diseases. Acknowledged difficulties of analysing BMAA in biological samples also inferred method development as part of the experimental studies. Investigating the role of BMAA in its producers was another purpose of the thesis, which may be crucial for future management of BMAA-producing cyanobacteria. By screening natural populations of the major filamentous bloom forming cyanobacteria of the Baltic Sea, we discovered the presence of BMAA throughout the entire summer season of two consecutive years, using a highly specific analytical method (liquid chromatography-tandem mass spectrometry; LC-MS/MS). BMAA was found to bioaccumulate in zooplankton and fish, as well as in mussels and oysters from the Swedish west coast. To improve the understanding of BMAA analyses in natural samples, the formation of carbamate adducts in the presence of bicarbonate was examined. Using two derivatization techniques in combination with LC-MS/MS, we could show that BMAA detection was not hindered by carbamate formation. Exogenously added BMAA inhibited nitrogen fixation in the model cyanobacterium Nostoc sp. PCC 7120, which was also hampered in growth and displayed signs of nitrogen starvation. Finally, BMAA was detected in cerebrospinal fluid in three of 25 Swedish test individuals, and represents the first confirmation of BMAA in the human central nervous system using LC-MS/MS as the primary analytical method. However, the association of BMAA to neurodegenerative diseases could not be verified as BMAA was present in both control individuals (two) and in one ALS-patient. Nevertheless, the finding of a known neurotoxic compound in the human central nervous system is alarming and potential consequences should be investigated. The discovery of the neurotoxic compound BMAA in Baltic Sea organisms, and in the central nervous system of humans potentially consuming fish from this ecosystem is concerning and warrants continued investigations of BMAA occurrence and human exposure. Further knowledge on the function and regulation of BMAA may help in developing strategies aiming to minimise human exposure. / <p>At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 3: Manuscript.</p>

L’atmosphère terrestre est très riche en azote (N2). Mais cet azote diatomique est sous une forme très stable, inutilisable par la majorité des êtres vivants malgré qu’il soit indispensable pour la synthèse de matériels organiques. Seuls les procaryotes diazotrophiques sont capables de vivre avec le N2 comme source d’azote. La fixation d’azote est un processus qui permet de produire des substances aminées à partir de l’azote gazeux présent dans l’atmosphère (78%). Cependant, ce processus est très complexe et nécessite la biosynthèse d’une vingtaine de protéines et la consommation de beaucoup d’énergie (16 molécules d’ATP par mole de N2 fixé). C’est la raison pour laquelle ce phénomène est rigoureusement régulé. Les bactéries photosynthétiques pourpres non-sulfureuses sont connues pour leur capacité de faire la fixation de l’azote. Les études faites à la lumière, dans le mode de croissance préféré de ces bactéries (photosynthèse anaérobie), ont montré que la nitrogénase (enzyme responsable de la fixation du diazote) est sujet d’une régulation à trois niveaux: une régulation transcriptionnelle de NifA (protéine activatrice de la transcription des gènes nif), une régulation post-traductionnelle de l’activité de NifA envers l’activation de la transcription des autres gènes nif, et la régulation post-traductionnelle de l’activité de la nitrogénase quand les cellules sont soumises à un choc d’ammoniaque. Le système de régulation déjà décrit fait intervenir essentiellement une protéine membranaire, AmtB, et les deux protéines PII, GlnB et GlnK. Il est connu depuis long temps que la nitrogénase est aussi régulée quand une culture photosynthétique est exposée à la noirceur, mais jusqu’aujourd’hui, on ignore encore la nature des systèmes intervenants dans cette régulation. Ainsi, parmi les questions qui peuvent se poser: quelles sont les protéines qui interviennent dans l’inactivation de la nitrogénase lorsqu’une culture anaérobie est placée à la noirceur? Une analyse de plusieurs souches mutantes, amtB- , glnK- , glnB- et amtY- poussées dans différentes conditions de limitation en azote, serait une façon pour répondre à ces interrogations. Alors, avec le suivi de l’activité de la nitrogénase et le Western Blot, on a montré que le choc de noirceur provoquerait un "Switch-off" de l’activité de la nitrogénase dû à une ADP-ribosylation de la protéine Fe. On a réussit aussi à montrer que ii tout le système déjà impliqué dans la réponse à un choc d’ammoniaque, est également nécessaire pour une réponse à un manque de lumière ou d’énergie (les protéines AmtB, GlnK, GlnB, DraG, DraT et AmtY). Or, Rhodobacter capsulatus est capable de fixer l’azote et de croitre aussi bien dans la micro-aérobie à la noirceur que dans des conditions de photosynthèse anaérobies, mais jusqu'à maintenant sa régulation dans l’obscurité est peu étudiée. L’étude de la fixation d’azote à la noirceur nous a permis de montrer que le complexe membranaire Rnf n’est pas nécessaire à la croissance de R. capsulatus dans de telles conditions. Dans le but de développer une façon d’étudier la régulation de la croissance dans ce mode, on a tout d’abord essayé d’identifier les conditions opératoires (O2, [NH4 + ]) permettant à R. capsulatus de fixer l’azote en microaérobie. L’optimisation de cette croissance a montré que la concentration optimale d’oxygène nécessaire est de 10% mélangé avec de l’azote. / The atmosphere of the Earth is very rich in nitrogen (N2). However, diatomic nitrogen is very stable and therefore unusable by the majority of life forms even though it is necessary for the synthesis of a variety of organic compounds. Only diazotrophic procaryotes are capable of using N2 as nitrogen source. Their nitrogen fixation allows the production of aminated compounds from atmospheric nitrogen (78 %). However, this process is very complex and requires the biosynthesis of about twenty proteins and the consumption of a lot of energy (16 molecules of ATP per molecule of N2 fixed), thus necessitating its tight regulation. The purple non-sulfur photosynthetic bacteria are known for their ability to carry out nitrogen fixation. Studies conducted in the light, the preferred mode of growth of these bacteria (anaerobic photosynthetic), have shown that nitrogenase (the enzyme responsible for dinitrogen fixation) is subject to regulation at three levels: transcriptional regulation of NifA (activator protein for the transcription of nif genes), posttranslational regulation of the activity of NifA to activate nif gene transcription, and posttranslational regulation of nitrogenase activity when cells are subjected to an ammonium shock. The control system already described involves essentially a membrane protein, AmtB and both PII proteins, GlnK and GlnB. It has long been known that nitrogenase is regulated when light is suddenly removed from a culture, but until now it is unclear whether these systems are also involved in the regulation of nitrogen fixation in dark. Thus, one outstanding question is what are the proteins involved in the inactivation of nitrogenase when a light-grown culture is placed in the dark? An analysis of several mutant strains; amtB-, glnK-, glnB-, and amtY- under different conditions of nitrogen deficiency was used to address this question. Using measurements of nitrogenase activity and Fe protein modification by Western blotting, we were able to show that darkness causes a "switch-off” of nitrogenase due to ADP- ribosylation of Fe protein. Thus, the system that has already been described as involved in the response to a lack of ammonia, is also required for a response to a lack of light or energy (AmtB, GlnK, GlnB, DraG, and DraT, and AmtY). However, Rhodobacter capsulatus is also able to fix nitrogen and grow micro-aerobically in the dark as well as photosynthetically under anaerobic conditions, but so far its regulation in the dark has been little studied. The study of nitrogen fixation in the dark allowed us to show that the Rnf membrane complex is not required for growth of R. capsulatus in such conditions. In order to develop a way to study its regulation during this growth mode, we have attempted to identify the operating conditions (O2, [NH4+]), allowing R. capsulatus to fix nitrogen micro-aerobically. The optimization of this conditions has shown that the optimal concentration of oxygen required is 10% mixed with nitrogen.