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preserved remains of an organism or its activity
Vast majority of fossils are made of rock and contain no organic material
Rarely an organism’s actual tissue is preserved
What are examples of exceptions to the fossils not retaining organic material?
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Organism Dies and Its Body Tissue Decomposes

Remains are Covered with Layers of Sediment

Sedimentation Continues, Compressing Remains under Pressure

Water Percolates through Remains, Causing All Organic Tissue to be Replaced by Minerals

Geological Uplift and Erosion Bring Fossil to Surface where it Must be Discovered before It is Destroyed by Weather

Fossilization is an Extremely Rare Event
Fossils Have to be Uncovered
Fossils are Rarely Found Complete
Soft Body Parts are Rarely Fossilized
most dead organisms are eaten or broken down by decomposers
remains have to be quickly covered by sediment to fossilize; if not, weathering processes will destroy them
“weathering” reveals fossils and palaeontologists have to be lucky to find them before they are destroyed
there may be billions of fossils that are never discovered
most organisms are reconstructed from only a few fossilized bones or bone fragments

plants and invertebrates lack a bony skeleton so don’t tend to fossilize
impressions of these organisms may be found

fossil record used to determine evolutionary relationship between extant (living) and extinct (no longer living) species
shows change in morphology over time
available fossil evidence
Gradualism - change occurs very slowly and steadily over a long period of time
Since change is slow, theory of gradualism predicts existence of transitional forms in fossil record

Punctuated Equilibrium - species do not change much over long periods of time
When change does occur, it is rapid and followed by a new equilibrium
