University of Idaho Organisms and Environments  
Precambrian Times, Hadean - Proterozoic Eons Cambrian - Ordovician Periods Silurian - Permian Periods Triassic - Cretaceous Periods Tertiary - Quaternary Periods Evolutionary Timeline
History of Life  

Link

We recommend that all students take a few minutes to review the last segment of Biology 115 concerning the principles of evolution and classification before diving into the lessons below. Follow the link above to go to Biology 115: Principles of Evolution and Divergence and Diversity (Lessons 1 and 2).

 

Lecture
 

In this course, we will just be looking at all the organisms on Earth and all of the places where they live. If that seems like too much to keep track of, this first lesson presents ten key points to help bring some order to this undertaking. Although we will be considering the incredible diversity of life on Earth and the myriad different ways that organisms interact, try to look at this information in light of the ten unifying concepts presented here.

Learning Objectives

  • How do we learn about ancient life?
  • What were the first living organisms on Earth?
  • How are organisms named?
  • How did eukaryotic organisms arise?
  • What is the impact of multicellularity on complexity?
  • How did improvements in reproductive success shape evolution?
  • How is structure related to function?
  • How do organisms interact with each other and with their environments?
  • What does it take to maintain a balanced ecosystem?

 

Lecture
 

Earth is a small planet orbiting a fairly nondescript star, and the biosphere is only a thin skin on this little planet. But this little planet has been teeming with life for almost 4 billion years! We are going to find out a little bit about all that life. Where did all the organisms come from? How did they get to be the way they are? How do they interact? How does their environment affect them? How do they affect their environment? How do we keep track of all this stuff?

Learning Objectives

  • Sit for a while in amazement and wonder at the nature of our biosphere, solar system, galaxy and universe.
  • Be inspired.

 

Lecture
 

Evolution is often defined as a change in the heritable characteristics of organisms over time. It involves a complex interplay between the DNA of organisms in a population and the environment in which that population lives. Tracing evolution often involves constructing phylogenetic trees that help us visualize how organisms are related to one another and how they have changed over time. Finally, it is important to realize that evolution can occur at very different rates, depending, once again, on the interplay between the characteristics of a particular population of organisms and the environment in which those organisms survive and reproduce.

Learning Objectives

  • How is evolution defined?
  • Why is each of the following terms crucial to the definition of evolution: change, heritable characteristics, population, time?
  • Understand how a phylogenetic tree is used to show evolutionary relationships among different types of organisms.
  • Why might rates of evolution differ significantly for different organisms?

 

Lecture
 

Fossils are preserved evidence of the existence of organisms. They may be mineralized shells and skeletons, mosquitoes preserved in amber, human footprints, or casts of tree trunks. Fossils give us a glimpse of ancient ecosystems and the organisms that inhabited them, but the fossil record is incomplete and biased toward preserving certain types or parts of organisms. With a little logic, a little luck, and a good dose of radiometric dating, it is possible to deduce many things about the way organisms once lived and how they have changed through time. In this lesson we will investigate how scientists think about fossils and how they are used to understand ancient ecosystems, evolutionary relationships among different organisms, and the effects of major extinctions.

Learning Objectives

  • How do we use the Principle of Superposition to understand the relationships between different fossils?
  • What is the difference between relative and absolute time scales? How is each determined?
  • Understand the limitations of the fossil record.
  • Understand how the geologic time scale has been assembled.
  • What is a common event following mass extinctions? Why might this be?

 

Lecture
 

Humans have a great desire to classify things, and the organisms with which we share our planet seem to be particularly fascinating to us. While many different schemes have been used to classify organisms, the Linnaean system is still the basis of the hierarchical classification system used by most scientists today. Instead of thinking only about morphological attributes, however, classification today aims at elucidating the evolutionary relationships among organisms. Because these relationships can be quite complex, statistical methods are increasingly being used to build the phylogenetic trees that describe how organisms are most likely related to one another.

Learning Objectives

  • Understand the types of data used to classify organisms.
  • Understand the naming conventions of the Linnaean classification system.
  • Understand the structure/basis of different types of phylogenetic trees. What is a node? What is a clade and why is it an important concept in understanding phylogenies?

 

OASIS