Fossils & Mass Extinction
Speciation Overview
Speciation: The process through which new biological species arise.
Global Processes Affecting Speciation
Influencing Factors:
Climate change.
Continental drift.
Both processes affect species by altering habitats and climates.
Speciation Rates
Speciation rates can increase due to geographical isolation caused by continental drift.
Gradualism vs. Punctuated Equilibrium
Gradualism: Slow and steady evolution.
Punctuated Equilibrium: Evolution occurs in quick bursts followed by long periods of stability.
Mass Extinction and Speciation
Mass Extinction: Significant loss of species (over 50%).
Leads to less competition and opens ecological niches.
It promotes adaptive radiation, facilitating the emergence of new species.
Adaptive Radiation
Definition: Rapid evolution of diversely adapted species from a common ancestor.
Often occurs after mass extinction events.
Changes in Gene Expression
Changes in how genes are expressed can result in significant evolutionary traits.
These changes may lead to adaptations in response to environmental shifts.
Continental Drift and Evolution
Plate Tectonics:
Continents are on tectonic plates that float on the mantle.
Their movement can create or destroy habitats, affecting speciation.
Impacts of Continental Drift
Alters ecological and climatic conditions leading to species diversification through:
Habitat alteration.
Changing climates (poles to equator and vice versa).
Promoting allopatric speciation by isolating populations.
Fossil Record and Speciation Patterns
Fossils of related species found miles apart indicate past connections due to continental drift.
Rapid appearance and disappearance of species in the fossil record suggest episodic changes in environments.
Punctuated Equilibria
Characterized by brief periods of rapid change (e.g., emergence and disappearance in fossils).
These periods often show symptoms of stasis followed by abrupt changes.
Gradualism may not always be recorded due to the incompleteness of the fossil record.
Implications of Mass Extinction on Speciation
After mass extinction, survivors face different competitive pressures leading to:
Adaptive radiation filling available niches due to environmental changes.
Evolution of numerous new species from few survivors.
Historical Mass Extinctions
Big Five Extinctions:
Major losses of species over Earth’s history; more than 50% extinction.
Permian Extinction:
96% loss of marine species; longest recovery times (~5-10 million years).
Cretaceous Extinction:
Over half marine species and all non-avian dinosaurs extinct.
Likely caused by an asteroid impact blocking sunlight, affecting photosynthesis.
Evolutionary Changes Post-Mass Extinction
Post-extinction environments are often conducive to adaptive radiation
Example: New species emerging quickly to exploit vacant ecological niches.
Innovative traits (like flight adaptation in animals) lead to colonization of new areas.
Case Study: Hawaiian Silversword Plants
Silversword Plants: A prime example of adaptive radiation and allopatric speciation.
Colonized Hawaiian islands circa 50 million years ago, adapting to local conditions.
Discussions on:
Speciation processes involved (e.g., founder effect).
Comparison of gene pools between Hawaiian species and mainland relatives.