1. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Overview: Lost Worlds Past organisms were very different from those now alive The fossil record shows macroevolutionary changes over large time scales including – The emergence of terrestrial vertebrates – The origin of photosynthesis – Long-term impacts of mass extinctions

2. Fig. 25-1

3. Fig 25-UN1 Cryolophosaurus

4. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Conditions on early Earth made the origin of life possible Chemical and physical processes on early Earth may have produced very simple cells through a sequence of stages: 1. Abiotic synthesis of small organic molecules 2. Joining of these small molecules into macromolecules 3. Packaging of molecules into “protobionts” 4. Origin of self-replicating molecules

5. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Synthesis of Organic Compounds on Early Earth Earth formed about 4.6 billion years ago, along with the rest of the solar system Earth’s early atmosphere likely contained water vapor and chemicals released by volcanic eruptions (nitrogen, nitrogen oxides, carbon dioxide, methane, ammonia, hydrogen, hydrogen sulfide)

6. Fig. 25-2

7. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Amino acids have also been found in meteorites

8. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Abiotic Synthesis of Macromolecules Small organic molecules polymerize when they are concentrated on hot sand, clay, or rock

9. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Self-Replicating RNA and the Dawn of Natural Selection The first genetic material was probably RNA, not DNA

10. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The fossil record documents the history of life The fossil record reveals changes in the history of life on earth

11. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Fossil Record Sedimentary rocks are deposited into layers called strata and are the richest source of fossils

12. Fig. 25-4 Present Dimetrodon Coccosteus cuspidatus Fossilized stromatolite Stromatolites Tappania, a unicellular eukaryote Dickinsonia costata Hallucigenia Casts of ammonites Rhomaleosaurus victor, a plesiosaur 100 million years ago 200 175 300 270 400 375 500 525 565 600 3,500 1,500 2.5 cm 4.5 cm 1 cm

13. Fig. 25-4-1 Fossilized stromatolite Stromatolites Tappania, a unicellular eukaryote Dickinsonia costata Hallucigenia 500 525 565 600 3,500 1,500 2.5 cm 4.5 cm 1 cm

14. Fig. 25-4a-2 Present Dimetrodon Coccosteus cuspidatus Casts of ammonites Rhomaleosaurus victor, a plesiosaur 100 million years ago 200 175 300 270 400 375 4.5 cm

15. Fig. 25-4b Rhomaleosaurus victor, a plesiosaur

16. Fig. 25-4c Dimetrodon

17. Fig. 25-4d Casts of ammonites

18. Fig. 25-4e Coccosteus cuspidatus 4.5 cm

19. Fig. 25-4f Hallucigenia 1 cm

20. Fig. 25-4g Dickinsonia costata 2.5 cm

21. Fig. 25-4h Tappania, a unicellular eukaryote

22. Fig. 25-4i Stromatolites

23. Fig. 25-4j Fossilized stromatolite

24. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Few individuals have fossilized, and even fewer have been discovered The fossil record is biased in favor of species that – Existed for a long time – Were abundant and widespread – Had hard parts

25. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings How Rocks and Fossils Are Dated Sedimentary strata reveal the relative ages of fossils The absolute ages of fossils can be determined by radiometric dating A “parent” isotope decays to a “daughter” isotope at a constant rate Each isotope has a known half-life, the time required for half the parent isotope to decay

26. Fig. 25-5 Time (half-lives) Accumulating “daughter” isotope Remaining “parent” isotope Fraction of parent isotope remaining 1 2 3 4 1/21/2 1/41/4 1/81/8 1 / 16

27. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Radiocarbon dating can be used to date fossils up to 75,000 years old For older fossils, some isotopes can be used to date sedimentary rock layers above and below the fossil

28. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The magnetism of rocks can provide dating information Reversals of the magnetic poles leave their record on rocks throughout the world

29. Table 25-1

30. Table 25-1a

31. Table 25-1b

32. Fig. 25-7 Animals Colonization of land Paleozoic Meso- zoic Humans Ceno- zoic Origin of solar system and Earth Prokaryotes Proterozoic Archaean Billions of years ago 1 4 3 2 Multicellular eukaryotes Single-celled eukaryotes Atmospheric oxygen

33. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Photosynthesis and the Oxygen Revolution Most atmospheric oxygen (O 2 ) is of biological origin O 2 produced by oxygenic photosynthesis reacted with dissolved iron and precipitated out to form banded iron formations The source of O 2 was likely bacteria similar to modern cyanobacteria

34. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings By about 2.7 billion years ago, O 2 began accumulating in the atmosphere and rusting iron-rich terrestrial rocks This “oxygen revolution” from 2.7 to 2.2 billion years ago (this is when we see rust) – Posed a challenge for life – Provided opportunity to gain energy from light – Allowed organisms to exploit new ecosystems

35. Fig. 25-8

36. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The First Eukaryotes The oldest fossils of eukaryotic cells date back 2.1 billion years The hypothesis of endosymbiosis proposes that mitochondria and plastids (chloroplasts and related organelles) were formerly small prokaryotes living within larger host cells An endosymbiont is a cell that lives within a host cell

37. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The prokaryotic ancestors of mitochondria and plastids probably gained entry to the host cell as undigested prey or internal parasites In the process of becoming more interdependent, the host and endosymbionts would have become a single organism Serial endosymbiosis supposes that mitochondria evolved before plastids through a sequence of endosymbiotic events

38. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Key evidence supporting an endosymbiotic origin of mitochondria and plastids: – Similarities in inner membrane structures and functions – Division is similar in these organelles and some prokaryotes – These organelles transcribe and translate their own DNA – Their ribosomes are more similar to prokaryotic than eukaryotic ribosomes

39. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Origin of Multicellularity The evolution of eukaryotic cells allowed for a greater range of unicellular forms A second wave of diversification occurred when multicellularity evolved and gave rise to algae, plants, fungi, and animals

40. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Cambrian Explosion The Cambrian explosion refers to the sudden appearance of fossils resembling modern phyla in the Cambrian period (535 to 525 million years ago) The Cambrian explosion provides the first evidence of predator-prey interactions

41. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Continental Drift At three points in time, the land masses of Earth have formed a supercontinent: 1.1 billion, 600 million, and 250 million years ago Earth’s continents move slowly over the underlying hot mantle through the process of continental drift Oceanic and continental plates can collide, separate, or slide past each other Interactions between plates cause the formation of mountains and islands, and earthquakes

42. Fig. 25-12 (a) Cutaway view of Earth (b) Major continental plates Inner core Outer core Crust Mantle Pacific Plate Nazca Plate Juan de Fuca Plate Cocos Plate Caribbean Plate Arabian Plate African Plate Scotia Plate North American Plate South American Plate Antarctic Plate Australian Plate Philippine Plate Indian Plate Eurasian Plate

43. Fig. 25-12a (a) Cutaway view of Earth Inner core Outer core Crust Mantle

44. Fig. 25-12b (b) Major continental plates Pacific Plate Nazca Plate Juan de Fuca Plate Cocos Plate Caribbean Plate Arabian Plate African Plate Scotia Plate North American Plate South American Plate Antarctic Plate Australian Plate Philippine Plate Indian Plate Eurasian Plate

45. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Consequences of Continental Drift Formation of the supercontinent Pangaea about 250 million years ago had many effects – A reduction in shallow water habitat – A colder and drier climate inland – Changes in climate as continents moved toward and away from the poles – Changes in ocean circulation patterns leading to global cooling

46. Fig. 25-13 South America Pangaea Millions of years ago 65.5 135 Mesozoic 251 Paleozoic Gondwana Laurasia Eurasia India Africa Antarctica Australia North America Madagascar Cenozoic Present

47. Fig. 25-13a South America Millions of years ago 65.5 Eurasia India Africa Antarctica Australia North America Madagascar Cenozoic Present

48. Fig. 25-13b Pangaea Millions of years ago 135 Mesozoic 251 Paleozoic Gondwana Laurasia

49. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Mass Extinctions The fossil record shows that most species that have ever lived are now extinct At times, the rate of extinction has increased dramatically and caused a mass extinction

50. Fig. 25-14 Total extinction rate (families per million years): Time (millions of years ago) Number of families: Cenozoic Mesozoic Paleozoic E OS D C P Tr J 542 0 488444416359299251 200 145 Era Period 5 C P N 65.5 0 0 200 100 300 400 500 600 700 800 15 10 20

51. Fig. 25-15 NORTH AMERICA Chicxulub crater Yucatán Peninsula

52. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Is a Sixth Mass Extinction Under Way? Scientists estimate that the current rate of extinction is 100 to 1,000 times the typical background rate Data suggest that a sixth human-caused mass extinction is likely to occur unless dramatic action is taken

53. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Consequences of Mass Extinctions Mass extinction can alter ecological communities and the niches available to organisms It can take from 5 to 100 million years for diversity to recover following a mass extinction Mass extinction can pave the way for adaptive radiations

54. Fig. 25-16 Predator genera (percentage of marine genera) Time (millions of years ago) Cenozoic Mesozoic Paleozoic E O S DCP Tr J 542 0 488444 416 359 299251 200145 Era Period C P N 65.50 10 20 30 40 50

55. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Adaptive Radiations Adaptive radiation is the evolution of diversely adapted species from a common ancestor upon introduction to new environmental opportunities. This is what occurred with Darwin’s finches. One type of finch went to the Galapogos Islands. As they reproduced, variations occurred. If a bird was born with a good variation, they adapted and lived. IE: A beak that could break seeds. If a bird was born with a bad feature, they died.

56. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings VERY IMPORTANT: Evolution does not occur because of need. It is a random genetic event. If the random event gives an organism something useful in the environment in which it lives, then it survives. How have humans changed natural selection?

57. Fig. 25-17 Millions of years ago Monotremes (5 species) 250 150 100 200 50 ANCESTRAL CYNODONT 0 Marsupials (324 species) Eutherians (placental mammals; 5,010 species) Ancestral mammal

58. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Regional Adaptive Radiations Adaptive radiations can occur when organisms colonize new environments with little competition The Hawaiian Islands are one of the world’s great showcases of adaptive radiation

59. Fig. 25-18 Close North American relative, the tarweed Carlquistia muirii Argyroxiphium sandwicense Dubautia linearis Dubautia scabra Dubautia waialealae Dubautia laxa HAWAII 0.4 million years OAHU 3.7 million years KAUAI 5.1 million years 1.3 million years MOLOKAI MAUI LANAI

60. Fig. 25-18a HAWAII 0.4 million years OAHU 3.7 million years KAUAI 5.1 million years 1.3 million years MOLOKAI MAUI LANAI

61. Fig. 25-18b Close North American relative, the tarweed Carlquistia muirii

62. Fig. 25-18c Dubautia waialealae

63. Fig. 25-18d Dubautia laxa

64. Fig. 25-18e Dubautia scabra

65. Fig. 25-18f Argyroxiphium sandwicense

66. Fig. 25-18g Dubautia linearis

67. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Hox genes are a class of homeotic genes that provide positional information during development If Hox genes are expressed in the wrong location, body parts can be produced in the wrong location For example, in crustaceans, a swimming appendage can be produced instead of a feeding appendage

68. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Adaptive radiation- a single species or small group of species has evolved into many different species. Many from one…… Patterns of evolution

69. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Organisms undergo adaptive radiation in different places because of environmental. Convergent evolution Two similar succulent plants with one common ancestor. Euphorbia Astrophytum