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phylogeny
branching evolutionary history of species or other groups or organisms
phylogenetic tree
a branching diagram that depicts the evolutionary relationships among species or other taxa
branches
part of the phylogenetic tree that represents populations through time
nodes
the point where two branches diverge, representing the point in time when an ancestral group split into two or more descendant groups
character
any heritable, genetic, morphological, physiological, developmental, or behavioral characteristic of an organism to be studied; aka trait
trait
any heritable, genetic, morphological, physiological, developmental, or behavioral characteristic of an organism to be studied; aka character
outgroup
any taxon that is not part of the taxonomic group being studies; researchers often select one or more outgroups that are closely related to the ingroup to help root phylogenetic trees and to determine the direction of character changes
ancestral trait
trait found in the ancestors of a particular group
derived trait
derived trait = trait that is a modified form of an ancestral trait, found in a descendant
originate via mutation, selection, genetic drift
synapomorphy
trait found in two or more taxa that is present in their most recent common ancestor, but missing in more distant ancestors
monophyletic
passes one snip test
paraphyletic
descended from a common evolutionary ancestor or ancestral group, but not including all the descendant groups.
parsimony
method that implies as few evolutionary steps as possible
coherence
trees built using different synapomorphies should agree
precambrian
ended 542 MYA
the interval between the formation of the earth (4.6 billion years), and the appearance of most animal groups about 541 mya; unicellular organisms were dominant for most of this era, and oxygen was virtually absent for the first 2 billion years
life was exclusively unicellular
cambrian
start 542 MYA; the first geological period of the Paleozoic Era, marks a pivotal time in Earth's history, spanning from roughly 538.8 to 485.4 million years ago, and is known for a period of rapid diversification of life forms
edicaran radiation
the relatively sudden evolutionary radiation of complex, soft-bodied multicellular organisms, including forerunners of modern animal phyla
cambrian explosion
the rapid diversification of animal body types and lineages that occurred durin a 50-million-year period about 541 mya at the start of the proterozoic eon
eukaryote
includes animals, plants, fungi, protists, and amoeba
era
broad, long-term timeframe marked by significant events or changes
period
specific, shorter timeframe within an era, often characterized by particular developments
paleozoic
the interval of geologic time from 541 to 252 mya during which fungi, land plants, and most animal lineages first appeared and diversifies
—began with the Cambrian explosion and ended with the extinction of almost all multicellular life-forms at the end of the permian period
mesozoic
after Permian extinction ; 252 to 66 mya, gymnosperms were the dominant plants on land and dinosaurs were the dominant vertebrates on land; ended with extinction of the dinosaurs
cenozoic
after K/T ; most recent era of geologic time, beginning 66 mya, during which mammals and birds became the dominant vertebrates on land and angiosperms became the dominant plants on land
adaptive radiation
-rapid evolutionary diversification within a lineage, producing numeric species with a wide range of adaptive forms
—following mass extinctions, surviving species are initially released from competition = expand range and diverge (and evolve new niches)
—eventually species become more specialized
mass extinction
a geologically sudden extinction event that is geographically and taxonomically widespread and kills relatively unselectively
-15% of families or 60% of species lost
-natural selection rapidly increases in order to create new speceis
-there are very long spans of time in which no new species evolve
-the surviving biota radiates to form new species
end Devonian extinction
cooling of climate = lower sea levels
-359 mya
end permian extinction
extreme global warming, low O2 in atmosphere/oceans, acidic ocean
-mother of mass extinctions
-252 mya
end cretaceous (K/T)
66 mya
-impact hypothesis = collision between earth and asteroid
massive tsunami and world-wide fires, acid rain, ash and dust that blocked out the sun
—dinos wiped out…mammals filled their niches
background extinction
an extinction that reflects the outcome of competition among species for niche space
niche differentiation
aka resource partitioning; evolutionary change in resource use
resource partitioning
aka niche differentiation; evolutionary change in resource use
character displacement
evolutionary change in species traits, allowing species to exploit different resources
biota
the animal and plant life of a particular region, habitat, or geological period
continental shelf
a gently sloping, submerged extension of a continent that stretches from the shoreline to a drop-off point called the shelf break, where the seafloor descents into the deep ocean floor
neritic zone
the shallow, sunlit part of the ocean above the continental shelf
competitive exclusion principle
two species cannot occupy the same niche simultaneously, because one will out-compete the other