process in all the hydrological models involves seawater,
somehow modified, and dissolution – precipitation associated with repeated fluctuations such as tidal pumping,
wave action, deep ocean currents, sea-level oscillations,
pulses of thermally elevated water flow, etc. The process
of dolomite formation may be penecontemporaneous with
sedimentation but it is more frequently postdepositional,
even diagenetic. Sometimes, there can be a considerable
time delay of the order of 100 m.a. between sedimentation
and dolomite formation.
The more recent realization that anaerobic bacteria can
play a role in the primary precipitation of dolomite is an
avenue for fruitful research in addressing the topic of dolomite formation and occurrence.
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