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Biofilms are a group of at least one kinds of microorganisms that can develop on a wide range of surfaces. Microorganisms that structure biofilms incorporate microscopic organisms, parasites and protists. One basic case of a biofilm dental plaque: a vile development of microscopic organisms that structures on the surfaces of teeth. Lake filth is another model. Biofilms have been discovered developing on minerals and metals. They have been discovered submerged, underground or more the ground. They can develop on plant tissues and creature tissues, and on embedded clinical gadgets, for example, catheters and pacemakers. Every one of these particular surfaces has a typical characterizing highlight: they are wet. These situations are "occasionally or persistently suffused with water,". Biofilms flourish upon soggy or wet surfaces. Biofilms have set up themselves in such conditions for quite a while. Fossil proof of biofilms dates to about 3.25 billion years back. For instance, biofilms have been found in the 3.2 billion-year-old remote ocean aqueous rocks of the Pilbara Craton in Australia. Comparative biofilms are found in aqueous situations, for example, natural aquifers and remote ocean vents.