Base-richness

In ecology, base-richness is the level of chemical bases in water or soil, such as calcium or magnesium ions. Many organisms prefer base-rich environments. Chemical bases are alkalis, hence base-rich environments are either neutral or alkaline. Because acid-rich environments have few bases, they are dominated by environmental acids (usually organic acids). However, the relationship between base-richness and acidity is not a rigid one – changes in the levels of acids (such as dissolved carbon dioxide) may significantly change acidity without affecting base-richness.

Base-rich terrestrial environments are characteristic of areas where underlying rocks (below soil) are limestone. Seawater is also base-rich, so maritime and marine environments are themselves base-rich.

Base-poor environments are characteristic of areas where underlying rocks (below soil) are sandstone or granite, or where the water is derived directly from rainfall (ombrotrophic).

Examples of base-rich environments

• Calcareous grassland
• Fen
• Limestone pavement
• Maquis shrubland
• Yew woodland

Examples of base-poor environments

• Bog
• Heath (habitat)
• Poor fen
• Moorland
• Pine woodland
• Tundra

See also

• Soil
• Calcicole
• Calcifuge

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