Lecture 8 Slides

Lecture Overview

  • Lecture Title: Patterns & Processes in Life History

  • Instructor: Ray Troll

Lecture Objectives

By the end of this lecture, you should be able to:

  • Summarize conditions on early Earth that made the origin of life possible.

  • Explain how the fossil record documents the history of life.

  • Recall key events in life’s history: origins of unicellular and multicellular organisms, colonization of land.

  • Explain how the rise and fall of organisms reflect differences in rates of speciation and extinction.

  • Describe mass extinctions and the resulting adaptive radiations.

  • Note: Key terms are bolded for emphasis!

Part 1: Conditions on Early Earth

  • Focuses on the environmental conditions conducive to the origin of life.

Key Events in Life’s History

  • Single-celled organisms: The first form of life.

  • Photosynthesis: Its evolution significantly impacted atmospheric conditions.

  • Eukaryotes: The first eukaryotic cells appeared.

  • Multicellularity: The emergence of multicellular organisms marked evolutionary progress.

  • Settlement of Land: Organisms began to inhabit terrestrial environments.

  • Timeline correlates these events with geological periods.

The Origin of Life

  • Hypothesized four steps leading to life:

    1. Abiotic synthesis of organic molecules.

    2. Formation of organic polymers, consisting of repeating units.

    3. Formation of protocells, which are membrane-bound cell precursors.

    4. Formation of ribozymes, RNA-based catalysts facilitating biochemical reactions.

Early Atmosphere and Organic Molecules

  • Early atmosphere was rich in organic molecules formed from simpler molecules.

  • Energy from lightning and UV radiation facilitated chemical reactions.

  • Resulted in a 'primordial soup' from which life eventually arose.

Miller-Urey Experiment

  • Conducted in 1953 by Stanley Miller and Harold Urey.

  • Simulated early Earth atmosphere and showed abiotic processes could create amino acids.

  • Demonstrated that organic molecules could be produced from non-living materials under specific conditions.

Changes Since Life Began

  • Fossil Record: Evidence of significant macroevolutionary changes over geological time.

    • Emergence of terrestrial vertebrates and photosynthesis are key milestones.

    • Mass extinctions have long-term impacts on life's evolution.

Fossil Record Limitations

  • Limitations include:

    • Taxonomic bias (certain taxa are favored).

    • Habitat bias (some habitats are represented more than others).

    • Temporal bias (some time periods are over-represented).

    • Bias toward abundant species in fossil reviews.

Fossils and their Age

  • Relative Age: Determined from their position in rock strata.

  • Absolute Age: Determined via radiometric dating, tracking the decay of isotopes (e.g., C-14).

  • Each isotope has a known half-life, allowing for calculation of age based on decay percentage.

Timeline of Life on Earth

  • Cosmic Calendar: A visual representation of life's history divided over a year:

    • Major events are highlighted by month.

    • This facilitates understanding of Earth’s 13.8 billion year history in a simplified manner.

  • Key events include:

    • Formation of supercontinents.

    • Evolution of vertebrates and land plants.

    • Extinction events marking significant geological epochs.

Geological Eons

  • Eons Information:

    • Hadean, Archaean, Proterozoic, and Phanerozoic labeled as major timeframes based on significant events like mass extinctions.

    • Total timeframes before the current eons encapsulate roughly 4 billion years.

Mass Extinctions

  • Major extinctions: Permian (96% of species disappeared) & Cretaceous (75% of species, including non-avian dinosaurs).

  • These events lead to significant shifts in biodiversity and paved the way for adaptive radiations in different ecological niches.

Adaptive Radiation

  • Occurs when organisms diversify from a common ancestor into new forms.

  • Notable examples:

    • Mammals radiating after the extinction of dinosaurs.

    • Colonization of land plants, insects, and tetrapods.

Summary: The Rise and Fall of Species

  • Changes over time documented by the fossil record, showcasing both extinction events and the emergence of new species.

  • Adaptive radiations occur following extinctions, indicating ongoing evolutionary processes.

Presentation and Engagement

  • Encouragement for questions and clarification throughout the lecture series.

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