Biomineralization in plants as a long-term carbon sink.
Carbon sequestration in the global carbon cycle is almost always attributed to organic carbon storage alone, while soil mineral carbon is generally neglected. However, due to the longer residence time of mineral carbon in soils (10(2)-10(6) years), if stored in large quantities it represents a potentially more efficient sink. The aim of this study is to estimate the mineral carbon accumulation due to the tropical iroko tree ( Milicia excelsa) in Ivory Coast. The iroko tree has the ability to accumulate mineral carbon as calcium carbonate (CaCO(3)) in ferralitic soils, where CaCO(3) is not expected to precipitate. An estimate of this accumulation was made by titrating carbonate from two characteristic soil profiles in the iroko environment and by identifying calcium (Ca) sources. The system is considered as a net carbon sink because carbonate accumulation involves only atmospheric CO(2) and Ca from Ca-carbonate-free sources. Around one ton of mineral carbon was found in and around an 80-year-old iroko stump, proving the existence of a mineral carbon sink related to the iroko ecosystem. Conservation of iroko trees and the many other biomineralizing plant species is crucial to the maintenance of this mineral carbon sink.
Cailleau
Guillaume
G
Institut de Géologie, Université de Neuchâtel, Rue Emile Argand 11, 2007 Neuchâtel, Switzerland.
Braissant
Olivier
O
Verrecchia
Eric P
EP
D002119:Calcium Carbonate; D002244:Carbon / Q000378:metabolism*; D018521:Plant Physiological Phenomena; D027824:Rosaceae / Q000502:physiology; D012987:Soil; D014197:Trees / Q000502:physiology
D012987:Soil; D002244:Carbon; D002119:Calcium Carbonate