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12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.
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12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

Dec 17, 2015

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Branden Byrd
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Page 1: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Specific environmental conditions are necessary in order for fossils to form.

Page 2: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Fossils are preserved remains or traces of animals, plants, and other organisms from the past.

Fossils can form in several ways.

• Only a tiny percentage of living things became fossils.

Page 3: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Permineralization occurs when minerals carried by water are deposited around a hard structure.

Skeleton of a veloci-raptor

Page 4: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

An organism dies in a location, such as a river bed, where sediments can rapidly cover its body.

Over time, pressure from additional sediment compresses the body, and minerals slowly replace all hard structures, such as bone.

Earthquakes or erosion may expose the fossils millions of years after formation.

Page 5: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

A natural cast forms when flowing water removes all of the original tissue, leaving an impression.

Crinoid - marine animal

Page 6: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Trace fossils record the activity of an organism.

Footprints from a Dimetrodon dinosaur

Page 7: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Amber-preserved fossils are organisms that become trapped in tree resin that hardens after the tree is buried.

Amber-preserved wasp

Page 8: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Preserved remains form when an entire organism becomes encased in material such as ice or volcanic ash.

Ice preserved remains of a 5000 year old man found in the Alps

Page 9: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Relative dating estimates the time during which an organism lived.

– It compares the placementof fossils in layers of rock.

Page 10: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Radiometric dating uses decay of unstable isotopes to calculate the age of a material.

– Isotopes are atoms of an element that differ in their number of neutrons.

neutrons protons

Page 11: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

A half-life is the amount of time it takes for half of an isotope to decay.

Page 12: 12.1 The Fossil Record Specific environmental conditions are necessary in order for fossils to form.

12.1 The Fossil Record

Half Life Problems

If an element has a half life of 20 years, how many years would it take for the element to decay to 25% of its original amount?

If an element has a half life of 50 years and 150 years have gone by than what percent of the original amount is left?

40 years

12.5 %