Minerotrophic refers to environments that receive nutrients primarily through groundwater that flows through mineral-rich soils or rock,[1] or surface water flowing over land.[2] Minerotrophic, “minerogenous”, and “geogenous” are now often used interchangeably, although the latter two terms refer primarily to hydrological systems, while the former refers to nutrient dynamics.[3] The hydrologic process behind minerotrophic wetlands results in water that has acquired dissolved chemicals which raise the nutrient levels and reduce the acidity.[3] This in turn affects vegetation assemblages and diversity in the wetland in question.[4] If dissolved chemicals include chemical bases such as calcium or magnesiumions, the water is referred to as base-rich and is neutral or alkaline.[3] In contrast to minerotrophic environments, ombrotrophic environments get their water mainly from precipitation, and so are very low in nutrients and more acidic.[5] Of the various wetland types, fens and rich fens are often minerotrophic while poor fens and bogs are often ombrotrophic.[1]Marshes and swamps may also be fed through groundwater sources to a degree.[6]
^ abEnvironment Canada (2014). Ontario wetland evaluation system: Northern Manual, 1st edition, version 3.2. Queen’s printer for Ontario.