Page 182 - Algae Anatomy, Biochemistry, and Biotechnology
P. 182

Biogeochemical Role of Algae                                                165

                 anaerobic bacteria that reduce nitrate used as electron acceptor in respiration to nitrogen gas. We
                 must stress that a realistic depiction of the N cycle would have an almost infinite number of inter-
                 mediary steps along the circumference of a circle, connected by a spider web of internal, crisscross-
                 ing complex connections.
                     It is one of nature’s great ironies that though all life forms require nitrogen compounds the most
                 abundant portion of it (98%) is buried in the rocks, therefore deep and unavailable, and the rest of
                 nitrogen, the N 2 gas (2%), can be utilized only by very few organisms. This gas cannot be used by
                 most organisms because the triple bond between the two nitrogen atoms makes the molecule almost
                 inert. In order for N 2 to be used for growth this gas must be “fixed” in the forms directly accessible
                 to most organisms, that is, ammonia and nitrate ions.
                     A relatively small amount of fixed nitrogen is produced by atmospheric fixation (5–8%) by
                 means of the high temperature and pressure associated with lightning. The enormous energy of
                 this phenomenon breaks nitrogen molecules and enables their atoms to combine with oxygen in
                 the air forming nitrogen oxides. These molecules dissolve in rain, forming nitrates that are
                 carried to the Earth. Another relatively small amount of fixed nitrogen is produced industrially
                 (industrial fixation) by the Haber-Bosch process, in which atmospheric nitrogen and hydrogen
                 (usually derived from natural gas or petroleum) can be combined to form ammonia (NH 3 ) using
                 an iron-based catalyst, very high pressures and a temperature of about 6008C. Ammonia can be
                 used directly as fertilizer, but most of it is further processed to urea (NH 2 ) 2 CO and ammonium
                 nitrate (NH 4 NO 3 ).
                     The major conversion of N 2 into ammonium, and then into proteins, is a biotic process achieved
                 by microorganisms, which represents one of the most metabolically expensive processes in biology.
                 Biological nitrogen fixation can be represented by the following equation, in which two moles
                 of ammonia (but in solution ammonia exists only as ammonium ion, that is, NH 3 þ
                                 2
                           þ
                 H 2 O $ NH 4 þ OH ) are produced from one mole of nitrogen gas, at the expense of 16 moles
                 of ATP and a supply of electrons and protons (hydrogen ions):
                                       þ
                                N 2 þ 8H þ 8e þ 16ATP  ! 2NH 3 þ H 2 þ 16ADP þ 16P i        (4:2)

                 All known nitrogen-fixing organisms (diazotrophs) are prokaryotes, and the ability to fix nitrogen
                 is widely, though paraphyletically, distributed across both the bacterial and archaeal domains. In
                 cyanobacteria nitrogen-fixation is an inducible process, triggered by low environmental levels of
                 fixed nitrogen.
                     The capacity of nitrogen fixation in diazotrophs relies solely upon an ATP-hydrolyzing, redox
                 active enzyme complex termed nitrogenase. In many of these organisms nitrogenase comprises
                 about 10% of total cellular proteins and consists of two highly conserved components, an iron
                 protein (Fe-protein) and a molybdenum-iron (MoFe-protein). The Fe-protein is a g 2 homodimer
                 composed of a single Fe 4 S 4 cluster bound between identical 32–40 kDa subunits. The Fe 4 S 4
                 cluster is redox-active and is similar to those found in small molecular weight electron carrier
                 proteins such as ferredoxins. It is the only known active agent capable of obtaining more than
                 two oxidative states and transfers electrons to the MoFe-protein. The MoFe-protein is a a 2 b 2
                 heterotetramer; the ensemble is approximately 250 kDa. The a subunit contains the active site
                 for dinitrogen reduction, typically a MoFe 7 S 9 metal cluster (termed FeMo-cofactor), although
                 some organisms contain nitrogenases wherein Mo is replaced by either Fe or V. These so-called
                 alternative nitrogenases are found only in a limited subset of diazotrophs and, in all cases
                 studied so far, are present secondary to the MoFe-nitrogenase. The MoFe-nitrogenase has been
                 found to be more specific for and more efficient in binding N 2 and reducing it to ammonia
                 than either of the alternative nitrogenases. The catalytic efficiency of these alternative nitrogenases
                 is lower than that of the MoFe-nitrogenase. In addition to variations in metal cofactors, the nitro-
                 genase complex is non-specific and reduces triple and double bond molecules other than N 2 . These
   177   178   179   180   181   182   183   184   185   186   187