Permanently waterlogged soil is normally
very deficient in nitrate, because rates of
decomposition of organic matter, and therefore of remineralisation of nutrients, are
severely reduced in the absence of oxygen, and because of denitrification by
anaerobic bacteria. Seasonally flooded wetlands, on the other hand, go through a
drying period when decomposition and nitrification can occur, releasing nutrients
back into the system. Fringe wetlands bathed by water with a relatively rapid
turnover will have a constantly replenished nutrient supply and can be very nutrient
rich.