DIATOMS are unicellular microscopic eukaryotic algae that are found in both fresh and marine water. They are primary producers among phytoplanktons and responsible for fixing almost 25% of the atmospheric CO 2 (Ramachandra et al., 2009). Besides this, diatoms contribute to one fifth of the global biomass primary production (Leblanc et al., 2012). Unlike other algae, they have a unique feature of having cell wall being made up of silica which could tolerate harsh environmental conditions (Round et al., 1990). It is noteworthy that diatom morphology is distinct and determined mainly by the salinity, temperature, and other environmental factors of the water thus making their species diverse across fresh and marine waters (Trobajo et al., 2011). However, the leakage of marine diatoms to fresh waters has resulted into morphological transitions in diatoms (Alverson et al., 2007). Among diatom lineages, Theriot and Serieyssol (Theriot & Serieyssol, 1994) chose Thalassiosirales lineage to study the evolutionary transition between marine and fresh water diatoms. This is because Thalassiosira is essentially a marine species found mostly in marine water and rarely in fresh water. Among the completely sequenced diatoms, Thalassiosira pseudonana has a genomic history quite likely originated from a fresh water diatom (Alverson et al., 2011a;Armbrust et al., 2004). The phylogeny of Thallossiosira identified by chloroplast genes (psbC and rbcL) and nuclear genes (SSU and partial LSUrDNA) reveals that there are clades of marine and fresh water species of Cyclotella.