Geological Implications of Bioerosion:

Bioerosion is a major process in carbonate shoreline sculpting.

Bioerosion produces significant amounts of fine-grained sediment.

Bioerosion plays a role in carbon and calcium geochemical cycling.

Trace fossils of bioeroders can be used to determine relative sea level changes over time on rocky shores.

Borings show distinct ecological and evolutionary changes in endolithic communities over time.

 

(Return to the First Page or the main Bioerosion page or Wooster's Geology Department Homepage)

 

 Main Bioerosion Page

 Bioeroding Organisms

 Common Macroborings

 Marine Hard Substrates

 Geology Department

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