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Did You Know?

Cyanobacterial mounds were most abundant before the evolution of shelly macroscopic organisms, but they still exist today (stromatolites are microbial mounds with a laminated internal structure).

Ancient reefs buried within stratigraphic sections are of considerable interest to geologists because they provide paleo-environmental information about the location in Earth's history.

Bryozoans and crinoids, common contributors to marine sediments during the Mississippian (for example), produced a very different kind of mound.

Corals and calcareous algae grow on top of one another and form a three-dimensional framework that is modified in various ways by other organisms and inorganic processes.

In addition, calcite has been reported in the initial post-larval calcification in a few scleractinian corals.

Mounds are built by microorganisms or by organisms that don't grow a skeletal framework.