Biology 100/101
Lecture 26
Macroevolution: Evidence
(Print Version)


Announcements

Objectives

Web Resources

What is a Fossil?

Determing Age of Rock

Transitional Fossils

Comparative Anatomy

Vestigial Organs

Molecular Evolution

Molecular Phylogeny

Why Study Evolution

Lecture Syllabus

IB 100/101 Home Page


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Text Readings in
Lewis et al.
Testing Your Knowledge Thinking Scientifically
Ch. 17, Evidence of Evolution Pg. 343, Questions 1,2,4 Pg. 343, Questions 1-6

Much of the material cited in this lecture outline came from your textbook (Lewis et al., 2004, Life Fifth Edition). It is highly beneficial to read this chapter carefully before your final exam.

You may also ask questions and see answers to your classmates' questions in Web Crossing in the "Talk to Jim and Ed" discussion.


Objectives:

After studying this material you should be able to:

  1. Explain what a fossil is and how it is formed.
  2. Explain the methods used to determine the age of a rock or fossil.
  3. Describe what is meant by transitional fossils.
  4. Describe how comparative anatomy and embryology provide clues to evolutionary relationships among species.
  5. Explain the difference between homologous and analogous structures and why this difference is important in ascertaining evolutionary relatedness.
  6. Describe how vestigial organs provide clues to the organism's origin.
  7. Describe how the comparative analysis of DNA sequences can be used to trace evolutionary relationships.
  8. Describe what a molecular phylogeny is and be able to interpret what it means.
  9. Know these terms and the relationships among them:
  10. fossils relative dating radiometric dating
    half-life comparative anatomy vestigial organs
    comparative embryology molecular evolution comparative DNA sequencing
    phylogeny amber PCR
    molecular phylogeny transitional fossils Archaeopteryx
    homologous structure analogous structure mitochondrial DNA


Web Resources:


What is a Fossil and How is it Formed?

  • Trilobite fossil (400 mya)
  • Archaeopteryx fossil (140 mya)
  • National Geographic Dinorama
  • Australopithecus afarensis (Lucy) (3.6 mya)
  • Homo erectus (1.6 million-35,000 years ago)
  • Embryonic dinosaur teeth and skin, Fig. 17.4 (text), 89 mya
  • Oldest male fossil discovered, 425 mya!, Science, Dec. 5, 2003 issue

    • A fossil is evidence of past life.
    • An organism, or its presence (tracks, trails, footprints, burrows), is preserved in rock (as a fossil).
    • Impressions and mineralization (the replacement of parts of organisms by minerals)
    • Most fossils are the hard parts of organisms (bones, teeth, shells); soft parts are rarely preserved.
    • To be adequately preserved, an organism must be in an environment where it is protected from oxidation and bacterial decay. An aquatic environment, particularly one with a high sedimentation rate (swamps, tar pits), is best to preserve fossils.
    • Fossils, starting as from far back as 3 bya, indicate that life evolved through great stretches of time and diversified.


Determining the Age of Rocks and Fossils

  • Relative dating techniques
    • In a "normal" horizontal sequence of rocks (e.g., marine sedimentary), the oldest rock types will be on the bottom with successively younger rocks on top. Sediments are deposited gradually in a flat layer and are spread over a large area. (May not be useful in the rock has been folded.)
    • Index fossils - an assemblage of fossils that characterize a particular rock unit. Organisms have evolved and gone extinct through time. Fossil content can be used to help determine age of rock, and to correlate rocks from different localities.
  • Radiometric (absolute) dating techniques
    • This method uses naturally-occurring radioactive isotopes. Radioisotopes decay at a constant rate to form stable (or daughter) isotopes. This rate of decay is measured by half-life (how long it takes for one-half of the parent radioactive material to decay to a daughter product). The ratio of parent isotope to daughter isotope in the rock reveals the number of half-lives, or length of time in years, that has elapsed. Think of radioactive elements as "geologic clocks."
    • Half Lives for Radioactive Elements

      Radioactive Parent Stable Daughter Half life
      Potassium 40 Argon 40 1.25 billion yrs
      Rubidium 87 Strontium 87 48.8 billion yrs
      Thorium 232 Lead 208 14 billion years
      Uranium 235 Lead 207 704 million years
      Uranium 238 Lead 206 4.47 billion years
      Carbon 14 Nitrogen 14 5730 years
  • Potassium 40 and Carbon 14 are often used to assign dates to fossils.
  • Not all rocks can be dated absolutely, so a combination of techniques is used.

An Example of Radiometric Dating

Carbon 12 & Carbon 14

  • Carbon exists in the atmosphere as C12 and C14. Their ratio is almost constant; however, C12 is more common.
  • Remember the process of photosynthesis? If not, review that lecture.
    • What do plants take in, and what is the end result?

  • Plants cannot distinguish C12 from C14, so they take both in and incorporate them into their biomass.
    • The C12:C14 ratio is now the same in the plant as that in the air.
    • When an aminal eats a plant, the carbon compounds in their bodies reflect the same C12:C14 ratio as in the air!

  • When an organism dies, it can no longer acquire carbon (either by photosynthesis or eating)
    • The C14 in the dead organism's body starts decaying to Nitrogen 14.
    • After 5,730 years, half of the C14 in the organism's body has decayed to N14.
    • Remember: C12 is stable, so it doesn't decay.
  • To age a fossil, the proportion of C12 to C14 is measured to see how much C14 has decayed.
    • If the proportion is equal to half what is normally found in the air, then the fossil is 5,730 years old!
  • An advantage of C14 dating is that you can date an actual fossil, or anything that was living (becuase it contained Carbon). Many of the other elements in the table above are used to date the material in which a fossil is encased.

Science and the Shroud. An interesting application of C14 dating and the reasons why scientists usually don't rely on one piece of evidence.


Transitional Fossils


Comparative Anatomy and Embryology

How do you explain the many anatomical and embryological similarities seen among different modern species? The features originated in a common ancestor, then gradually became modified as its descendants adapted to their environments.

Homologous structures: Similar structures in different organisms having a common evolutionary origin. Example: The similarity of embryos and skeletons of vertebrates suggests common ancestry. The structures may or may not have similar functions, but they share a common origin.

Analogous structures: Structures that are similar in function among different species but that evolved independently, perhaps in response to similar environmental challenges. They are NOT inherited from a recent common ancestor.

For additional information:


Vestigial Structures

  • A structure that seems not to have a function in an organism but resembles a functional structure in another type of organism. For example, whales have useless pelvic bones and, occasionally, rear feet resembling those in other mammals. Some snakes have leg bones.
  • Humans have an appendix, gooseflesh, ear muscles, and as embryos, tails and gill slits. To possess these structures, we must have the genes for making them.
  • Evolution is not a perfect process. As environmental changes select against certain structures, others are retained, sometimes persisting even if they are not used (Lewis et al., page 334).

Molecular Evolution

"We are the products of the genes of our ancestors." All life forms based on DNA and 20 amino acids.

  • Molecules reveal relatedness. Molecular evidence for evolution includes similarities at the gene, protein, chromosomal, and genome levels.

  • Phylogeny of 8 Species Based on DNA Sequencing

    Interpretation:

    • All species are evolutionarily related and share a common ancestor.
    • Species are related based on the presence of shared and uniquely-derived point mutations.
    • Relationships can be inferred (e.g., Species E is more closely related to Species F than to any other species; Species group E and F is more closely related to species group G and H than it is to any other species group).

    In actuality, thousands of DNA nucleotides can be compared and computers are used to analyze the data and construct the phylogeny. The DNA used can be from any organism, living or dead (and from fossils too).

    A phylogeny is a diagram that depicts the lineages, or evolutionary relationships, among species. Comparative anatomical, embryological, molecular, behavioral, physiological, chemical, geographical, and fossil data can all be used, together or separately, to construct a phylogeny.

    Why should we study evolution?


    Evolution as a fact and a theory

    Evolution--the process by which the genetic composition of a population changes over time--is a FACT.

    • This process is all that is required to produce the diversity and similarity of all life on this planet today.

    • Evolution has occurred; it still is occurring; it has been directly observed, documented, demonstrated, and described. Supporting evidence for it is overwhelming (and obtained from a wide range of scientific fields).

    The mechanisms by which evolution occurs (e.g., natural selection, mutation, genetic drift) are presented as SCIENTIFIC THEORIES.

    • Several theories have been proposed and debated. It is far from clear how evolution proceeds in every detail.

    In summary, Darwin established the FACT of evolution, and proposed a THEORY, natural selection, to explain the mechanism of evolution.


    Science as a Way of Knowing the Natural World:

    • A scientist believes that the natural world is a physical reality, but that we can only construct a conceptual view of that reality based upon observation and experimentation.
    • Each of us has our own view of the natural world that is viewed through the lens of our previous experience and knowledge.
    • Science strives to be objective, and is founded in the belief that events can be explained fully by natural causes. Conversely, explanations based in supernatural causes are not considered to be scientific. Rocks of Ages: Science and Religion in the Fullness of Life, By Steven Jay Gould
    • Scientific explanations of phenomena observed in the natural world are called hypotheses (singular: hypothesis).
    • Scientific hypotheses must be testable and falsifiable. If the hypothesis is incorrect it can be tested by experimentation and/or observation and proved to be false.
    • Experimentation and observations can increase our confidence that a hypothesis is a correct explanation of a phenomenon, but can never absolutely prove a hypothesis to be true.
    • Once a hypothesis has been supported by many experiments and/or observations it is considered by the community of scientists to be a theory. (Note that this is very different from the common use of the word, meaning an opinion or a guess.)
    • The conclusions of science are subject to change. New studies, which might utilize new techniques and equipment, may produce new information that leads to the conclusion that previously accepted theories need to be modified or changed entirely.
    • Great science is replaced by greater science.