Ambient temperature tufas are formed by a combination of physico-chemical and biological precipitation processes. The former dominate higher flow regimes, where escape of CO2 directly into the atmosphere provides the stimulus for calcium carbonate precipitation....
CITATION STYLE
Pedley, M. (2000). Ambient Temperature Freshwater Microbial Tufas. In Microbial Sediments (pp. 179–186). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-662-04036-2_20
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