Minerotrophic
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- 3 chapters
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Through Hydrology, Acid and Base (chemistry)
Hydrology
The hydrological setting of a wetland strongly influences its characteristics. Chemical ions are transported to wetlands via their hydrological system, and in turn affect pH, conductivity, and nutrient levels. Chemical and nutrient dynamics may differ depending on a minerotrophic wetland’s hydrological setting, which could include water discharge dominated, recharge dominated, or some combination of both. These characteristics also vary seasonally, as average groundwater levels increase and decrease at different times of the year. This seasonality can raise water below ground or above the surface to become free standing. Additional factors such as geological conditions, soil type, and surface morphology may also influence the characteristics of a wetland in tandem with hydrological setting.
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Vegetation communities
Stable water and nutrient availability via groundwater systems allows for a diverse array of plant species to grow in minerotrophic wetlands. This also allows for peat to accumulate provided the water does not flow too quickly. A minerotrophic wetland may be alkaline or weakly acidic, which also influences vegetation communities. Rich fens are often characterized by alkaline hydrologic conditions, allowing for more plant diversity. These areas may be dominated by brown mosses of the family Amblystegiaceae and sedges in the genus Carex. Acidic poor fens are often dominated by peat mosses of the genus Sphagnum which tend to further increase acidity.
Examples
A notable example of a minerotrophic wetland is the Everglades, a large subtropical wetland located in Western Florida, USA.

