Definition: Macroevolution refers to large-scale evolutionary changes that occur over geologic time, leading to the diversification of life forms.
Lecturers:
Rod Page: Evolution and Diversity, Evolutionary Trees, Molecular Phylogenies
Barbara Mable: Biometrics and Biodiversity
Sofie Spatharis: Functional Diversity and Biodiversity Conservation
Others: M Llewellyn, S White
Main Topics Covered:
Introduction to Evolution and Diversity
Evolutionary Trees
Molecular Phylogenies
Reconstructing Ancestors
Measures of Biodiversity (Molecular, Taxonomic, Functional)
Biodiversity and Conservation Practices
Macroevolution: Rates and Dates
Biogeography
Key Equation: Amount of Evolution = Rate × Time
Examples:
Slow rate over a long period can lead to significant evolutionary changes.
Fast rate over a short period can also produce large changes.
Change Types:
Continuous Change: Ongoing small changes over time.
Episodic Change: Sudden bursts of change typically after significant geological or environmental events.
Separating Rates from Dates:
Addressing whether diversity is due to age or rate of evolution is crucial for understanding evolutionary trees.
Diversity & Evolution:
Hawaiian honeycreepers showcase significant diversity, their evolutionary history may reflect lengthy adaptation and evolutionary radiation.
Comparative Analysis:
Two alternative hypotheses regarding honeycreepers and thrushes:
Honeycreepers are older than thrushes but evolved at the same rate.
Honeycreepers have evolved more quickly than thrushes, leading to greater biodiversity.
Fossil Record: Essential for dating evolutionary events but often incomplete.
Molecular Data: Used to estimate divergence times and evolutionary rates based on genetic differences.
Assumptions:
Fossil records are reasonably complete to provide minimum age estimates for various evolutionary lineages.
Examples of Evolutionary Lineage:
Coelacanths illustrate how certain species show virtually no evolutionary change over millions of years.
Geographic events significantly shape biological events, linking fossils and extant species over time.
Punctuated Equilibrium: Long periods of stasis in species interspersed with short bursts of rapid evolution.
Gradualism: Slow, continuous change within a species over time.
Final Notes:
Understanding rates of evolution requires solid dates obtained through fossils, biogeography, and other evidentiary associations.
The relationship between speciation rates and molecular evolution is an active area of research, highlighting the complexity of evolutionary mechanisms.