.7. Discussion
Mangroves provide a unique ecological environment for diverse microbial communities, which are fundamental to the functioning of the habitats. In the mangrove system, activities of microbes are predominant in decomposing organic matter, making protein rich detritus food for fishes, recycling of nutrients, carbon fluxes as well as climate change. A variety of abiotic and biotic factors influenced the density of microorganisms. All these factors change with time and spatial heterogeneity. The microbes areadapted to varied physical and chemical conditions of mangrove systems (Kathiresan, 2000; Holguin et al., 2001a, 2001b; Kathiresan and Bingham, 2001; Kathiresan and Qasim, 2005; Rajendran and Kathiresan, 2007; Sahoo and Dhal, 2009; Kathiresan, 2011). Microbial density in relation to soil depth and type of mangrove forests are largely unknown for mangrove sediment, although it is known for seasonal changes. Bearing this in mind the present study was undertaken to analyze the microbial density in relation to the soil physical and chemical characteristics in a mangrove forest, located in southeast coast of India. Mangrove is a detritus-based ecosystem and hence is colonized with a rich population of saprophytic microorganisms, distributed all through the seasons in order to decompose the organic matter, available in the biotope. For instance, the highest counts of azotobacters or fungi were recorded in premonsoon, yeasts or thraustochytrids in monsoon, Trichoderma in summer, and THB or lactobacilli in postmonsoon. The counts of nitrogen fixing autotrophic cyanobacteria were recorded maximum in postmonsoon and the nitrogen fixing azotobacters in monsoon (Table 1). In general wet seasons appeared to be favourable for microbial colonization. This is accordance with the fact that the degree of wetness is an important factor regulating microbial cycling of organic matter in the mangrove soil (Alongi et al., 1993, 2005a, 2005b).