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Fossils and early primate evolution

Fossils and early primate evolution. Chapter 6. introduction. Over 99% of everything that has ever lived on Earth has gone extinct Dinosaurs were the dominant species until 65 mya, when an asteroid hit the earth and wiped almost all of them out This left holes in the ecosystem

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Fossils and early primate evolution

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  1. Fossils and early primate evolution Chapter 6

  2. introduction • Over 99% of everything that has ever lived on Earth has gone extinct • Dinosaurs were the dominant species until 65 mya, when an asteroid hit the earth and wiped almost all of them out • This left holes in the ecosystem • One group that survived were the mammals

  3. introduction • Review: • What features do mammals have? • Hair on body • Live young • Milk to feed young • Constant body temperature

  4. introduction • Fossils have been known of since ancient Greece, and Darwin used them in formulating his theory • William Smith observed strata, or layers of rock that contained extinct life forms • Fossils are a way to document evolution of life on Earth • Phylogeny: evolutionary relationships • Chronology: place in time

  5. What are fossils? • Preserved remains of organisms • Most are bones, teeth, and shell, or things easily preserved • MOST THINGS THAT EVER LIVED WERE NEVER FOSSILIZED • This leaves big gaps in the fossil (and evolutionary) record we try to fill in • To fossilize, organism must be immediately covered with sediment, protected from animals, and be in extreme dry or cold conditions

  6. What are fossils? • Taphonomy: study of what happens to a fossil from the time it died until it is discovered • Fossils are found in different types of rock • Sedimentary: made from sediments; creates strata • Volcanic: common for hominins; important for dating

  7. Limitations in record • The more samples we have, the better we know the fossil record • Some animals well represented, some have only a few samples • Fayum Depression (Egypt) is important for primate fossils • Would primates living in tropical rainforests preserve well?

  8. Geologic time • Have to have new perspective of geologic or evolutionary time (millions of years, not day-to-day) • Earth is 4.6 billion years old • We have recorded major changes of Earth into • Eras: Paleozoic, Mesozoic, Cenozoic • Epochs (smaller divisions of eras)

  9. Geologic perspective • Also have to remember that geography was not always the same • Millions of years ago all the continents were connected into one mass called Pangaea, so this allowed animals and plants to migrate easily • Plate tectonics gradually broke this up and made the 7 continents we have today

  10. Early beginnings • Land animals evolved from aquatic animals • Lungfish had sacs that they could store air in, as well as gills • Also had bones in their fins • They could move from one pond to another • Natural selection pushed some of them on land permanently into land reptiles

  11. Amphibians are dependent on water (must lay eggs in it) • Reptiles have an amniote egg, which does not need water  land animals

  12. Mammals • After dinosaur extinction, there were different kinds of mammals • Monotremes (mammals that lay eggs) • Marsupials (have a pouch and embryonic young) • Placentals (mammals with internal fetal development) • Monotremes and marsupials are now only in Australia

  13. Mammals

  14. age • Early thinkers could not fathom the time we measure now • Had to adapt to scientific and mathematical explanations, not biblical ones • **Law of Superposition: the higher the fossil is in strata, the younger it is

  15. Dating techniques • There are two methods of dating fossils • Relative: compares fossils and tells age as older or younger in comparison • Absolute (Chronometric): uses measurements, chemicals, and math to get a numeric age frame

  16. Relative dating • Stratigraphic correlation: matches physical and chemical makeup of different sites of strata • Ex. If you know the age of volcanic ash, you can date a fossil older or younger depending on its position to ash • Chemical dating: uses chemical changes • Bones absorb flourine from soil; can compare levels to tell which is older or younger

  17. Relative dating • Biostratigraphic (Faunal) Dating: if you know when an animal lived, that can help you date the strata and other layers of strata around it • Uses index fossils: animals whose time frame is well-known

  18. Example: mammoths are so well-known that they are good index fossils for dating other nearby remains

  19. Absolute dating • Relative dating provides an order of what came first, second, later, latest…etc. • Absolute dating gives actual ages (numeric) • Radiocarbon Dating: uses the decaying of carbon (C14) to get age • **only used on things that used to be alive • **only dates back 50,000 years • Would this be helpful for ancient human ancestors?

  20. Radiocarbon dating • Carbon is an isotope that changes over time • All living things are made of carbon • When a living thing dies, the carbon starts to decay into nitrogen • Can measure how much carbon has decayed/how much is left • Half-life: the time it takes for half the carbon in the body to decay. 5,730 years

  21. Absolute dating • Another method is Radiopotassium or Potassium/Argon Dating: • volcanic rock has potassium isotopes • The potassium decays into argon • If you date the rock, you know the date of the fossil inside it because it was formed when the rock formed • Use the half-life to measure this rate • Half-life is 1.3 billion • **only used on rock, and not living things • **can date much, much older fossils • Is this helpful for dating ancient human ancestors?

  22. Molecular dating • DNA is helpful for dating as well • Idea of Molecular Clock: closely related species have more similar DNA • Also trace amount of mutations • Can use genetic DNA and mtDNA to trace ancestry and phylogeny

  23. Molecular dating • For example: What do you notice about the placement of humans in the ape phylogeny?

  24. Ancient climate • Foaminefera: tiny holes in fossil shells help us understand levels of oxygen in paleoclimate • Help us know what eras were hot and humid and which were cold and dry • How would this affect primate evolution? • Human evolution ? (Revisit these questions after we learn the human ancestors) • Also think how this would affect sea level and therefore migration between land masses

  25. Review questions • What is the difference between relative and absolute dating? What are examples? • What types of fossils would be dated with Radiocarbon and what types with Radiopotassium? • How can fossils help us recreate evolutionary relationships, ancient climate, and ancient diet?

  26. Part II

  27. Fossil Primates • Review of primate features: • Bone protects eyes • Forward-facing eyes with binocular vision • Grasping hands • Nails instead of claws • Large brain • Long gestation and parental invenstment

  28. Why Primates? • We know primate features (ch. 5) • Now focus on why and how these evolved in fossil record • Arboreal hypothesis: unique primate features are due to life in trees • Vision for leaping, hands for grasping branches, intelligence for understanding 3D space • But a lot of animals live in trees • Visual Predation Hypothesis: early primates hunted insects and unique traits helped with this • Nails and precision grip to grab bugs, vision to see them

  29. Why Primates? • But what role do the features of primates play in finding fruit, the main diet of most primates? • Vision: can see if fruit is ripe from a distance • Grasping toes let them hold on to branches while they picked fruit with hands • Angiosperm radiation hypothesis (angiosperm means flowering plant) • In Cenozoic, primates and fruit evolved together • All three hypotheses give good explanations

  30. First Primates? • In Paleocene (between 65-55 million years ago (mya)), the first primates arose • They evolved out of mammals. • …what event happened that led to mammals appearing? • Plesiadapiforms • Adaptive radiation of mammals • Many went extinct, probably because of competition with rodents • Lack many of the primate features, but had nails • Very base of the family tree • Proprimates, or the precursor to the primate line

  31. First True Primates? • Euprimates: true primates, have primate features (eyes protected by bone, grasping, nails, larger brain) • Two groups: • 1. Adapids • Ancestors of Prosimians/Strepsirrhine • Resemble lemurs • 2. Omomyids • Ancestors of Anthropoids • Resemble tarsier

  32. Anthropoids Evolve • In the Oligocene (35-24 mya), there was rapid cooling of the globe • This changed habitats • Most fossils from this time come from the Fayum site in Egypt

  33. Anthropoids Evolve • Two main groups: • 1. Parapithecids • Primitive, early anthropoids • 2-1-3-3, so may be ancestor of modern ______________________ • 2. Propliopithecids • More common group • 2-1-2-3, so ancestor of _______________________ • Aegyptopithecus is called the “dental ape” because he looked like a monkey but had a Y-5 molar

  34. Anthropoids Evolve • Two main groups: • 1. Parapithecids • Primitive, early anthropoids • 2-1-3-3, so may be ancestor of modern Platyrrhines • 2. Propliopithecids • More common group • 2-1-2-3, so ancestor of Catarrhines • Aegyptopithecus is called the “dental ape” because he looked like a monkey but had a Y-5 molar

  35. Anthropoids Evolve • Parapithecid:

  36. Anthropoids Evolve • Propliopithecid (Aegyptopithecus):

  37. Anthropoids in South America • Platyrrhines originated in Africa, but are found only in S America today • How did they get there? • Either they migrated across the ocean or through Antarctica (which was much warmer then) • Continents were closer together, oceans may have been lower, land bridges available

  38. Apes • Warmer weather accompanied another radiation of primates • Proconsul (20 mya) is an ape ancestor, the first true Hominoid • Ape-like dentition • Adaptations for eating fruit • However, still small and in trees • All four limbs equal length • Not knuckle-walker like apes today

  39. Apes Leave Africa • Apes began in Africa and then spread to Europe and Asia • Dryopithecus: Europe, larger body, teeth adapted for fruit, slow growth and development, larger brains, longer arms than legs (modern ape locomotion)

  40. Apes Leave Africa • Sivapithecus: • found in Asia • thick enamel for eating tough foods • ancestor of modern orangutans (skulls almost identical to modern orangutans)

  41. Apes Leave Africa • Gigantopithecus: • Also in Asia • largest primate to ever live • up to 10 feet tall • teeth adapted for tough food • lived up to time of humans

  42. Video • NOVA “First Primates” http://www.pbs.org/wgbh/nova/evolution/first-primates.html

  43. Use the following page for a study sheet (the next slide is the same WS you got in class) • Put any useful information under the picture (geography, features, especially who they are ancestors of) • Pg. 183 has a diagram of fossils

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