Trace fossil

A trace fossil, also called an ichnofossil (pronunciation: /ˈɪknoʊfɒsᵻl/; Greek: ιχνος ikhnos "trace, track"), is a geological record of biological activity. Trace fossils may consist of impressions made on the substrate by an organism: for example, burrows, borings (bioerosion), urolites (erosion caused by evacuation of liquid wastes), footprints and feeding marks, and root cavities. The term in its broadest sense also includes the remains of other organic material produced by an organism — for example coprolites (fossilized droppings) or chemical markers — or sedimentological structures produced by biological means - for example, stromatolites. Trace fossils contrast with body fossils, which are the fossilized remains of parts of organisms' bodies, usually altered by later chemical activ

Trace fossil

A trace fossil, also called an ichnofossil (pronunciation: /ˈɪknoʊfɒsᵻl/; Greek: ιχνος ikhnos "trace, track"), is a geological record of biological activity. Trace fossils may consist of impressions made on the substrate by an organism: for example, burrows, borings (bioerosion), urolites (erosion caused by evacuation of liquid wastes), footprints and feeding marks, and root cavities. The term in its broadest sense also includes the remains of other organic material produced by an organism — for example coprolites (fossilized droppings) or chemical markers — or sedimentological structures produced by biological means - for example, stromatolites. Trace fossils contrast with body fossils, which are the fossilized remains of parts of organisms' bodies, usually altered by later chemical activ