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Index >> Microbial Ecology of Different Ecosystems>> Marine Ecosystem Downwelling

Marine Ecosystem Downwelling

Downwelling
The vertical downward movement of a fluid due to density differences or the downward displacement of fluid when two fluid masses converge is called downwelling. In the ocean, it often refers to where Ekman transport causes surface waters to converge or impinge on the coast, displacing surface water downward and thickening the surface layer.

Biota of the Sea
The marine environment is subjected to many changes including change in pressure, light intensity, turbidity, dissolved salts, etc. Based on these factors bacteria in the marine environment can be categorised into three groups:

Barotolerant They grow best at normal atmospheric pressure but can grow between 0-400 atm.

Moderate barophiles These grow at 400 atm and also grow at 1 atm.

Extreme barophiles These are bacteria growing only at higher pressure 6000-11000 m depth at a pressure of 600-1100 atm where the temperature is 2-3°C. These bacteria live in the guts of deep sea invertebrates like amphipods and holothurians

As with freshwater environment, the uppermost layer of the marine, ecosphere is the surface tension layer, where the marine ecosphere interfaces with the atmosphere. The seawater-air interface is the habitat for the pleuston, the marine equivalent of the neuston, which includes bacterial and algal inhabitants. Pseudomonas and various pigmented genera such as Erythrobacter, Erythromicrobium, Protominobacter and Roseobacter are major bacterial population. A higher proportion of pleuston bacteria have been reported to utilise carbohydrates than do bacteria in the underlying water. Population of primary producers, including cyanobacteria, diatoms and Phaeophycophyta are sometimes found in the pleuston layer.

 

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