Genotypic changes in a population level through time
Macroevolution
Can be seen over a few generations, used interchangeably with the term speciation
Macroevolution
Creation of new species and taxonomic groups, Diversification of species (divergent evolution), Accumulation of traits due to series of microevolution
Macroevolution: Patterns in the history of life
Macroevolution
The study of evolutionary changes occurring at the level of species and above, explores the broader patterns and processes of evolution over long periods of time
Speciation
The formation of new species
Macroevolution generally refers to evolution above the species level
There are no firsthand accounts to be read, instead we reconstruct the history of life using all available evidence: geology, fossils, and living organisms (similarities)
Basic evolutionary mechanisms like mutation, gene flow (migration), genetic drift, and natural selection are at work and can help explain many large-scale patterns in the history of life
Taxonomical groups go from the most inclusive to more exclusive (species level)
Speciation events are seen through Phylogenetic tree/cladograms
Understanding phylogenies is like reading a family tree, the root represents the ancestral lineage, and the tips represent the descendants
When a lineage splits (speciation), it is represented as branching on a phylogeny
Phylogenies trace patterns of shared ancestry between lineages
A clade is a grouping that includes a common ancestor and all the descendants (living and extinct) of that ancestor
Clades are nested within one another, forming a nested hierarchy
The Linnaean system of classification assigns every organism a domain, kingdom, phylum, class, order, family, genus, and species, which is not based on evolution
Biologists are switching to a classification system that reflects the organisms' evolutionary history
Speciations are seen via Phylogenetic tree/cladograms
Patterns in macroevolution
Stasis
Character change
Lineage-splitting (or speciation)
Extinction
Stasis means that lineages don't change much for a long time, some are called living fossils
Character change can happen quickly or slowly, in a single direction or reverse itself
Patterns of lineage-splitting can be identified by constructing and examining a phylogeny
Extinction is extremely important in the history of life, it can be frequent or rare, or occur simultaneously across many lineages (mass extinction)
The geologic time scale (GTS) is a system of chronological dating that relates geological strata (stratigraphy) to time
Fossil record refers to the placement of fossils throughout the surface layers of the Earth
Mass extinction is the extinction of a large number of species within a relatively short period of geological time
A population is a group of individuals of the same species occupying a particular habitat
The habitat includes the geographical place where an organism lives and its interactions with other organisms
Each population has a gene pool which is the sum of genes in a population at a given time
Evolution is the permanent change in gene frequencies within a population
Population genetics is the study of genetic variability within a population and of the forces that act on it
Natural selection is a biological theory that explains why organisms seem to match their environmental niches so well
Each individual is subjected to several selection pressures at any point of its life, affecting its chance of survival and reproduction
The main types of natural selection in a population
Stabilizing selection
Disruptive selection
Directional selection
Sexual selection
Polymorphism
Artificial selection is the process of intentional or unintentional modification of a species through human actions which encourage the breeding of certain traits over others
Speciation refers to the evolutionary process of formation of a new species from previously existing species
Evolution can be studied using evidences such as fossils, homologous structures and similarities in genes and biochemistry
Mass extinction refers to the extinction of a large number of species within a relatively short period of geologic time, thought to be due to factors such as catastrophic global events or widespread environmental change that occurred too rapidly for most species to adapt.
Scientists have come up with a number of theories that they believe caused mass extinctions. These include catastrophic methane release, floods, basalt eruptions, climate change, and impact events.