Lecture Title: Patterns & Processes in Life History
Instructor: Ray Troll
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!
Focuses on the environmental conditions conducive to the origin of life.
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.
Hypothesized four steps leading to life:
Abiotic synthesis of organic molecules.
Formation of organic polymers, consisting of repeating units.
Formation of protocells, which are membrane-bound cell precursors.
Formation of ribozymes, RNA-based catalysts facilitating biochemical reactions.
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
Encouragement for questions and clarification throughout the lecture series.