Serpentine soil is an uncommon soil type produced by weathered ultramafic rock such as peridotite and its metamorphic derivatives such as serpentinite. More precisely, serpentine soil contains minerals of the serpentine subgroup, especially antigorite, lizardite, and chrysotile or white asbestos, all of which are commonly found in ultramafic rocks. The term "serpentine" is commonly used to refer to both the soil type and the mineral group which forms its parent materials.
Serpentine soils exhibit distinct chemical and physical properties and are generally regarded as poor soils for agriculture. The soil is often reddish, brown, or gray in color due to its high iron and low organic content. Geologically, areas with serpentine bedrock are characteristically steep, rocky, and vulnerable to erosion, which causes many serpentine soils to be rather shallow.[1] The shallow soils and sparse vegetation lead to elevated soil temperatures[2] and dry conditions.[1] Due to their ultramafic origin, serpentine soils also have a low calcium-to-magnesium ratio and have low levels of many essential nutrients such as nitrogen (N), phosphorus (P), and potassium (K). Serpentine soils contain high concentrations of heavy metals, including chromium, iron, cobalt, and nickel.[3] Together, these factors create serious ecological challenges for plants living in serpentine soils.
- ^ a b Brady, Kristy U.; Kruckeberg, Arthur R.; Bradshaw Jr., H.D. (2005). "Evolutionary Ecology of Plant Adaptation to Serpentine Soils". Annual Review of Ecology, Evolution, and Systematics. 36: 243–266. doi:10.1146/annurev.ecolsys.35.021103.105730.
- ^ Kruckeberg, Arthur R (2002). Geology and plant life : the effects of landforms and rock types on plants. University of Washington Press. ISBN 978-0-295-98203-8. OCLC 475373672.[page needed]
- ^ Chiarucci, Alessandro; Baker, Alan J. M. (2007). "Advances in the ecology of serpentine soils". Plant and Soil. 293 (1–2): 1–2. Bibcode:2007PlSoi.293....1C. doi:10.1007/s11104-007-9268-7. S2CID 35737876.