Presentation is loading. Please wait.

Presentation is loading. Please wait.

Change over Time ©2008 Susan Anderson.

Similar presentations


Presentation on theme: "Change over Time ©2008 Susan Anderson."— Presentation transcript:

1 Change over Time ©2008 Susan Anderson

2 Darwin British Naturalist Journey to Galapagos / South America Saw:
New/different SPECIES Fossils similar to living organisms (where had these organisms gone?) He asked why were those organisms on the islands different from those on the mainland?

3 Adaptations Example for Darwin: Finches Different beaks
Different foods Less competition

4 Evolution Gradual change over time to become better adapted to their environment. Gradualism Punctuated Equilibria

5 Natural Selection “Survival of the Fittest” Extinction
Overproduction – not all offspring survive Competition- usually indirect (food, space) Variations – genetic Selection- helpful variations accumulate, unfavorable ones disappear

6 Formation of New Species
Sometimes a group is separated from the rest of its species. (river, mountain range, weather carries them) If a group is separated long enough, they may evolve different traits. “Geographic Isolation”

7 Continental Drift Large scale geographic isolation.
Members were separated when the continents split. Example: Animals isolated on Australia are unlike other mammals.

8 Review What is evolution?
Name something Darwin observed that he thought was the result of evolution Some insects look just like sticks. How could this be an advantage to the insects? How could the “stick trait” have evolved through natural selection?

9 Fossil Record Sedimentary Rock Petrified Molds/Casts Preserved
Most fossils are found in this type of rock Why? Petrified Minerals dissolved in the water around remains soaks in and replaces the remains, changing them to rocks Molds/Casts Remains get dissolved and leave behind a hollow space (mold), then it’s filled with minerals (cast) Preserved Can be found in tar or amber

10 Dating Fossils Relative Dating Absolute Dating
Only be used when the rock layers have been preserved in their original sequence Doesn’t tell actual age, only which fossils are older or younger Absolute Dating Uses radioactive elements to determine exact age of fossils HALF LIFE – the time it takes for half the atoms of a sample to decay

11 Review Describe how fossils form in sedimentary rock.
Explain the process of absolute dating. How are gradualism and punctuated equilibrium similar? How are gradualism and punctuated equilibrium different?

12 Other Evidence Homologous Structures Embryology DNA similarities

13 Branching Tree Diagrams
A diagram the shows how scientists think different groups of organisms are related.

14 Review Name three types of evidence from modern day organisms that scientists use to determine evolutionary relationships. What are homologous structures? Most scientists today consider similarities in DNA to be the best indicator of how closely two species are related. Why do you think this is the case?


Download ppt "Change over Time ©2008 Susan Anderson."

Similar presentations


Ads by Google