Abstract
Microbial calcification has been identified as a significant source of carbonate sediment production in modern marine and lacustrine environments around the globe. This process has been linked to the production of modern whitings and large, micritic carbonate deposits throughout the geological record. Recent research has advanced our understanding of the microbial calcification mechanism as a photosynthetically driven process. However, little is known of the effects of this process on inorganic carbon cycling or of the effects of changing atmospheric CO2 concentrations on microbial calcification mechanisms.
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