Purification and properties of glutamine synthetase from the archaebacterium Halobacterium salinarium

The effect of ammonium on assimilatory nitrate reduction in the haloarchaeon Haloferax mediterranei

Physiology, regulation and biochemical aspects of the nitrogen assimilation are well known in Prokarya or Eukarya but they are poorly described in Archaea domain. The haloarchaeon Haloferax mediterranei can use different nitrogen inorganic sources (NO (3) (-) , NO (2) (-) or NH (4) (+) ) for growth. Different approaches were considered to study the effect of NH (4) (+) on nitrogen assimilation in Hfx. mediterranei cells grown in KNO(3) medium. The NH (4) (+) addition to KNO(3) medium caused a decrease of assimilatory nitrate (Nas) and nitrite reductases (NiR) activities. Similar effects were observed when nitrate-growing cells were transferred to NH (4) (+) media. Both activities increased when NH (4) (+) was removed from culture, showing that the negative effect of NH (4) (+) on this pathway is reversible. These results suggest that ammonium causes the inhibition of the assimilatory nitrate pathway, while nitrate exerts a positive effect. This pattern has been confirmed by RT-PCR. In the presence of both NO (3) (-) and NH (4) (+) , NH (4) (+) was preferentially consumed, but NO (3) (-) uptake was not completely inhibited by NH (4) (+) at prolonged time scale. The addition of MSX to NH (4) (+) or NO (3) (-) cultures results in an increase of Nas and NiR activities, suggesting that NH (4) (+) assimilation, rather than NH (4) (+ ) per se, has a negative effect on assimilatory nitrate reduction in Hfx. mediterranei.

beta-Glutamate as a substrate for glutamine synthetase

The conversion of beta-glutamate to beta-glutamine by archaeal and bacterial glutamine synthetase (GS) enzymes has been examined. The GS from Methanohalophilus portucalensis (which was partially purified) is capable of catalyzing the amidation of this substrate with a rate sevenfold less than the rate obtained with alpha-glutamate. Recombinant GS from the archaea Methanococcus jannaschii and Archaeoglobus fulgidus were considerably more selective for alpha-glutamate than beta-glutamate as a substrate. All the archaeal enzymes were much less selective than the two bacterial GS (from Escherichia coli and Bacillus subtilis), whose specific activities towards beta-glutamate were much smaller than rates with the alpha-isomer. These results are discussed in light of the observation that beta-glutamate is accumulated as an osmolyte in many archaea while beta-glutamine (produced by glutamine synthetase) is used as an osmolyte only in M. portucalensis.