ABSTRACT
The fourth most abundant nutrient element in plants, nitrogen is a key constituent of nucleotides, proteins, and other vital metabolites of plants. It is an integral part of a plant regulating several growth processes. Inorganic nitrogen sources, nitrate (NO3 -) and ammonium (NH4 +), are the two forms, in which the majority of nitrogen is taken up from the soil. But soil ecosystems flourishing with various types of bacteria and microfauna pose a great challenge for nitrogen availability to plants. Consequently, optimizing the nitrogen levels in both natural and agricultural ecosystems is essential it is a limiting nutrient for plants. Thus, approximately 90 million metric tonnes of nitrogen fertilizers are applied to the soil each year worldwide. However, abundance of gaseous nitrogen in the atmosphere (78% by volume) in molecular form (N2) does not guarantee its accessibility to plants, as it has to be converted to biologically usable form with the assistance of microbial population to break the highly stable triple covalent bond of nitrogen. So, finally, inorganic nitrogen either taken from atmospheric (as N2) or soil pool (as NO3 -or NH4 +) has to undergo a series of complex biochemical reactions and processes to be converted to organic nitrogen in the form of amino acids or other nitrogenous metabolites. This process of incorporation of mineral nutrients (i.e., nitrogen into various organic forms such as proteins, nucleic acid, hormones, etc.) is termed nitrogen assimilation. In NO3 - assimilation, the nitrogen in NO3 - is converted to a higher-energy form in nitrite (NO2 -) by nitrate reductase enzyme in the cytosol then to a yet higher-energy form, ammonium (NH4 +), by nitrite reductase in chloroplasts and plastids, and finally into the amide nitrogen of glutamine. Plants such as legumes form symbiotic relationships with nitrogen-fixing bacteria to convert molecular nitrogen (N2) into ammonia (NH3), which however is protonated to form the ammonium ion (NH4 +) and subsequently into organic forms. The nitrate supply to the roots is proportional to the amount of absorbed nitrate that is translocated to the shoot, where it is assimilated.
So, we endeavor to elucidate how nitrogen traverses between its primary global pools (i.e., atmosphere, soil (and associated groundwater), and biomass), the biology and biochemistry of biological nitrogen fixation, NO3 – uptake & reduction (to NH4 +), numerous routes of assimilation of nitrogen as ammonium, and nitrate nitrogen along with a detailed view of synthesis of amino acids.