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Did You Know?

Corals, including some major extinct groups Rugosa and Tabulata, have been important reef builders through much of the Phanerozoic since the Ordovician period.

Excellent examples of biostromes formed by cyanobacteria occur in the Great Salt Lake of Utah (USA), and in Shark Bay, Western Australia.Cyanobacteria do not have skeletons and individuals are microscopic.

However, bryozoan and crinoid meadows can persist over time and produce compositionally distinct bodies of sediment with depositional relief. in the Louisiade Archipelago.

However, other organism groups, such as calcifying algae, especially members of the red algae Rhodophyta, and mollusks (especially the rudist bivalves during the Cretaceous period) have created massive structures at various times.

A microbial mound might be built exclusively or primarily by cyanobacteria.

However, other organism groups, such as calcifying algae, especially members of the red algae Rhodophyta, and mollusks (especially the rudist bivalves during the Cretaceous period) have created massive structures at various times.