1. Evolution in the Fossil Record Evolution of phenotype Evolution of diversity

2. The Earth is Old

3. The Geological Time Scale is Based Upon the Principles of Relative Dating Younger rocks are deposited on top of older rocks Lava and sedimentary rocks were originally laid down in a horizontal position Boulders or cobbles found in a body of rock are older than their host rock Earlier fossil forms are simpler than more recent forms, and more recent forms are most similar to existing forms.

4. Geologic Column Earth’s history as told by rock strata

5. The Geologic Time Scale Chapter 4, p. 70

6. Why is the fossil record incomplete? It takes the right conditions at the right time in the right place. - some organisms are simply not likely to yield fossils - sedimentation does not occur in all habitats - fossils must survive geological events and weather the elements for millions of years before discovery

7. Process of Fossilization (1)Compression/impression/casts/molds:impressions or casts made before decomposition (like footprints). (2) Permineralized fossils: precipitation of minerals in cells before decomposition. Or Occasionally: (1) Unaltered remains: Frozen, amber embedded, peat bogs. After remains are buried by sediments:

8. amber cast Impression fossil permineralized fossils

9. Dinosaur National Park

10. Fossil Record is Biased Fossilization is higher for organisms that are: Durable and likely to be buried in an anoxic environment (low land or marine habitats) Also, there is temporal and geographic bias: Probability that an organism will be fossilized depends on the geographical area and historical time.

11. Fossils and associated rocks contain reactive elements that decay at known rates Uranium 235 --> Lead 235 = 7 x 10 8 years Carbon 14 --> Nitrogen 14 = 5730 years Parent Atom Daughter Atom Half-life Radiometric Dating

12. Time (half-lives) Surviving Parent Atoms Accumulating Daughter Atoms 1 23 1/1 1/3 1/7 Radioisotope Decay 1. Find fossil 2. Determine ratio of parent to daughter atoms 3. Determine number of elapsed half-lives 4. Estimate age of fossil

13. You are using C 14 (half-life = 5730 years) radioisotope dating to determine the age of rocks associated with a fossil. The percentage of daughter isotope atoms (N 14) ) is 87.5%. What is the age of the fossil? Try this problem 17,190 yrs

14. There are Good Examples of Macroevolution in the Fossil Record - see also (Figure 4.6) Gradualism : (e.g. limbs are intermediate) Mosaic evolution: (limbs evolved faster than braincase, tail fin, tooth structure Sarcopterygii --> Ichthyostega --> Amphibia

15. 4.6(1) Eusthenopteron, a member of the group of lobe- finned fishes from which tetrapods arose

16. 4.6(2) Eusthenopteron, a member of the group of lobe- finned fishes from which tetrapods arose

17. Other Examples From Book To Review (Chapter 4) Origin of Birds –Archaeopteryx is but one of many fossils Origin of Mammals - Gradual evolution of “reptilian” skull and jaw Origin of Cetacea –A series of fossils have recently been discovered showing adaptation to aquatic life Origin of Hominins –We are the lone survivors of an otherwise extinct radiation of bipedal African hominids