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Biology - Chp 17 - History Of Life - PowerPoint


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Biology - Chp 17 - History Of Life - PowerPoint

  1. 1. Chapter 17The History of Life
  2. 2. 17-1 The Fossil Record• Studying life’s history is one of the most fascinating and challenging parts of biology
  3. 3. 17-1 The Fossil Record• And researchers go about it in different ways
  4. 4. Fossils and Ancient Life• From the study of fossils, Paleontologists infer what past life forms were like and the environment that they lived• They also classify them and arrange them in the order in which they lived• Together, all of this information is called The fossil record
  5. 5. What the Fossil Record Shows• Fossils occur in a particular order• Life has changed over time• More than 99 percent of all species that have ever lived have become extinct
  6. 6. Extinct• When a species dies out
  7. 7. How Fossils Form• For a fossil to form, either the remains of the organism or some trace of its presence must be preserved• The formation of fossils depends on a precise combination of conditions• Most fossils form in sedimentary rock
  8. 8. Interpreting Fossil Evidence• More often than not, a Paleontologist must analyze and interpret a fossil from a few fossil bits• When they study fossils, they look at anatomical similarities and differences between the fossil and living organisms• Also a fossils age is extremely important• Paleontologists determine the age of a fossil using 2 techniques
  9. 9. 1. Relative Dating• The relative age of a fossil is determined by comparing its placement with that of fossils in other layers of rock
  10. 10. Index Fossils• Used to compare the relative ages of fossils
  11. 11. To be used as an index fossil, a species must1. Be easily recognized2. Existed for a short period of time3. Have a wide geographical range
  12. 12. 2. Radioactive dating• Used to determine the absolute age of rocks using radioactive elements• Radioactive elements decay or break down into non-radioactive elements at a steady rate
  13. 13. Half life• The length of time required for half of the radioactive atoms in a sample to decay• In radioactive dating, scientists calculate the age of a sample based on the amounts of remaining radioactive isotopes it contains
  14. 14. Geologic Time Scale• Paleontologists use divisions of the Geologic time scale to represent evolutionary time
  15. 15. Eras• Divides the time between the Precambrian and Present
  16. 16. Periods• Subdivides eras
  17. 17. Cambrian Explosion
  18. 18. Ordovician
  19. 19. Silurian
  20. 20. Devonian
  21. 21. Carboniferous
  22. 22. Permian
  23. 23. Triassic
  24. 24. Jurassic
  25. 25. Cretaceous
  26. 26. Tertiary
  27. 27. Quaternary
  28. 28. What would it take to bring on a new geological era?1. Change the atmospheres composition, thus modifying plants2. Change the distribution and diversity of species, thereby changing the future fossil record3. Acidify the oceans, which will modify the mineral deposits on the ocean floor• Does this sound familiar?
  29. 29. New era being proposed• “Anthropocene”• New era characterized by the domination of the planet by one species…us.
  30. 30. 17 – 4 Patterns of Evolution• Biologists often use the term macroevolution to refer to large- scale evolutionary patterns and the processes that occur over long periods of time
  31. 31. Six important topics in macroevolution are1. Extinction2. Adaptive radiation3. Convergent evolution4. Coevolution5. Punctuated equilibrium6. Changes in developmental genes
  32. 32. Extinction• More than 99% of all species that have ever lived are now extinct• Usually extinctions happen the way Darwin proposed• Sometimes mass extinctions wipe out entire ecosystems• Many times mass extinctions are followed by a burst of evolution that produces many new species
  33. 33. Adaptive Radiation• When a single species or a small group of species has evolved into diverse forms that live in different ways
  34. 34. Convergent Evolution• When unrelated organisms come to resemble one anotherEx.) sharks and dolphins
  35. 35. Q: How does this happen?A: Adaptive radiation can happen in different places and times but in ecologically similar environments
  36. 36. Analogous Structures• Structures which look and function similarly but are made up of parts that don’t share a common evolutionary history
  37. 37. Coevolution• The process in which 2 species evolve in response to changes in each otherEx.) plants + pollinators plants + herbivorous insects bats + moths
  38. 38. Plants and Pollinators
  39. 39. Hammer Orchid
  40. 40. Bats vs. MothsAn Evolutionary Arms Race
  41. 41. Rough Skinned Newt vs. Garter Snake
  42. 42. Punctuated Equilibrium• There is no question among Biologists that evolution has happened and is happening today• There are however questions about how fast evolution happens• Darwin thought that evolution was slow and steady. He called this idea Gradualism• This idea is supported by fossil evidence• However, the fossil record also shows changes that have happened over relatively short periods of time (hundred of thousands-even million-of years)
  43. 43. Punctuated Equilibrium• Long stable periods of equilibrium interrupted by brief periods of more rapid change• This may be the result of genetic isolation
  44. 44. Developmental Genes and Body Plans • Biologists have long suspected that changes in the genes for growth and differentiation during embryological development could produce transformations in body size and shape • Until recently, researchers had only limited ability to affect gene activity in embryos
  45. 45. Developmental Genes and Body Plans • We can now perform experiments with gene expression by turning genes on or off and examining the results • Small changes in the timing of cell differentiation and gene expression can make the difference between two completely different phenotypes