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causes of divergence
mutation, selection, genetic drift
biological species concept
main criteria for a species is reproductive isolation
Gradual process with no gene flow
disadvantages of biological species concept
doesn’t work for fossils, species that reproduce asexually, and pops that don’t overlap geographically
prezygotic isolating mechanisms
temporal, habitat, behavioral, gametic, and mechanical isolation
temporal isolation
breed at different times
habitat isolation
breed in different habitats
behavioral isolation
different mating rituals
gametic isolation
sperm/egg incompatibility
mechanical isolation
reproductive structures are incompatible
postzygotic mechanisms
hybrid validity and hybrid sterility
hybrid validity
embryo do not fully develop
hybrid sterility
heterogametic sex is sterile
morphospecies concept
main criteria for species is morphological traits
widely applicable
disadvantages of morphospecies concept
polymorphic species may be labeled as different species
hard to identify species that differ in non morphological traits
phylogenetic species concept
main criteria for species is evolutionary history
allopatric speciation
populations become geographically isolated
more common mode of speciation
allopatric speciation: dispersal
a population moves and colonizes a new area
allopatric speciation: vicariance
the habitat physically splits
parapatric speciation
when populations change gradually along a cline
cline
spatial gradient of character change in an environment
sympatry
living in the same geographic area
sympatric speciation
caused by an external event (disruptive selection) or an internal event (chromosome mutation)
niche
the range of resources a species can use and the conditions it can tolerate
polyploidy
an error in meiosis or mitosis that results in more than 2 sets of chromosomes
can polyploidy cause speciation?
yes
autopolyploid mechanism
nondisjunction during meiosis, 4n
autopolyploid
doubling of chromosome #
reproductively isolated from original population
instantaneous speciation
allopolyploid mechanism
error in mitosis prior to meiosis, 2n=10
allopolyploid
different species parents
viable offspring
offspring have 2 copies each of 2 sets of chromosomes
advantages of being a polyploid
higher level of heterozygosity
can tolerate higher level of self-fertilization and inbreeding
genes on duplicated chromosomes can diverge independently
speciation by polyploidization
driven by chromosome level mutation and occurs in sympatry
virtually instantaneous
what enabled the rapid diversification of plants?
genetic diversity of polyploids
when can population interbreed and converge?
when theres no prezygotic isolation
reinforcement
natural selection for traits that prevent interbreeding among populations (prezygotic isolating mechanisms)
hybrid zones
a geographic area where interbreeding between 2 populations occurs
can be stable or moving, small or big
outcomes of secondary contact between populations
fusion of pops
reinforcement
hybrid zone formation
extinction of one population
homology
trait due to common ancestry
homoplasy
similarity not due to common ancestry
synapomorphy
shared derived trait
monophyletic group (clade)
ancestor and all descendents
paraphyletic group
ancestor but not all descendents
polyphyletic group
not all ancestors and not all descendents
complications inferring trees
traits may be similar due to homoplasy
a reversal in character change may occur
some groups are based on one trait while other groups use another trait
parsimony
tree with the least amount of evolutionary changes
most logical tree
DNA sequencing
used by most scientists to determine phylogeny
using DNA to determine phylogeny
identify homologous region (conserved gene)
align sequences
compare differences
which are more common: transitions or transversions
transitions
molecular clock
DNA and protein sequences evolve at a relatively constant rate
can be used to date nodes
relies on natural theory
intact fossil
when decomposition does not occur and organic remains are preserved
compression fossil
sediments accumulate on top of remains and compress organic materials into a carbonaceous film
cast fossils
hole in organism fills with minerals that create a cast
permineralized fossils
remains decompose slowly as minerals fill the open space
trace fossils
preserved paths of animals
how to determine fossil age
nearby rock layers
ideal conditions for fossils
organism is buried quickly and decomposes slowly
fossil record
total collection of fossils found in the world
limitations of fossil record
habitat bias
taxonomic bias
temporal bias
abundance bias
fossilization habitat bias
organisms that live where sediment is actively being deposited are more likely to fossilize
fossilization taxonomic bias
organisms with hard parts are more likely to fossilize
fossilization temporal bias
more recent organisms are found more often
fossilization abundance bias
more abundant organisms are found more often
burgess shale
canadian rockies, 508 mya
cambrian explosion
lots of soft bodied organisms
olduvai gorge
tanzania, 2 mya
human evolution fossils
when was earth created
4.6 bya
when did life start
3.5-3.8 bya
precambrian
creation of earth - appearance of most animals (543 mya)
life is unicellular until the end of this period
absence of oxygen until evolution of photosynthetic bacteria (2 mya)
phanerozoic eon
end of precambrian - present
paleozoic, mesozoic, cenozoic
paleozoic era
543-248 mya
appearance of most major lineages
diversification of life
ends with mass extinction
when do land animals first appear?
paleozoic era
which era had the first bony fish, insects, and land plants?
paleozoic
mesozoic era
250 - 66 mya
dinosaur era
ends with cretaceous extinction
which era had the first mammals and angiosperms?
mesozoic
cenozoic era
66 mya - present
mammals and angiosperms abundant
modern animals appear
adaptive radiations
rapid production from a single lineage into many species
needs ecologic opportunity and/or evolution of a key morphological trait
favorable environment for diversification
lots of new niches
cambrian explosion
first animals (sponges) 635 mya
50 mil years later, animals become more complex
triggers of the cambrian explosion
higher oxygen levels
evolution of predation
more niches
hox genes
mass extinction
at least 60% of species die within 1 million years
there have been 5
5 mass extinctions
ordovician
devonian
permian
triassic
cretaceous
end-permian extinction
largest mass extinction
90% of species died
end of paleozoic
causes of permian extinction
lava flood added a ton of CO2, O2, and heat
caused severe acid rain that devastated plants
widespread cole fires released toxic ash
oceans became anoxic (lack oxygen)
sea levels dropped dramatically
end-cretaceous extinction
asteroid struck the earth 66 mya
ended 60-80% of species (most dinosaurs)
6th mass extinction
precipitated by humans
estimated current extinction rate is highest since the asteroid
3 domains of life
bacteria
archaea
eukarya
diversification of the 3 domains
horizontal transfer was crucial for eukaryote evolution
(mitochondria and chloroplasts)
archaea
single celled organisms like bacteria
anaerobic
live in diverse habitats like soil and ocean
extremophiles
bacteria
more diverse than archaea
mostly unicellular
diverse habitats, more moderate conditions
cynobacteria
photosynthetic bacteria
abundant in aquatic habitats
what was responsible for the initial increase in atmospheric O2?
cynobacteria
where did eukaryotes get their chloroplasts from?
cynobacteria
proteobacteria
very diverse phyla of bacteria
wide variety of pathogens
nitrogen fixation in plants
where did eukaryotes get their mitochondria from?
proteobacteria
evolution of land plants
moving from water gave them more CO2 and O2
moving also made a lack of water and support, and made reproduction more difficult
ancestor of plants
photosynthetic protist (algae)
adaptations of land plants
alternation of generations (diploid sporophyte, haploid gametophyte)
sporophyte embryo protected
produce spores that can handle tough environments
order of evolution of plants
vascular → nonvascular → vascular with seeds
bryophytes
simplest land plants
moss, liverworts, hornworts
no roots, stems, or leaves
live in moist environments
vascular plants main organs
stems, roots, and leaves
xylem
water and mineral transport from the roots up
phloem
two-way flow of water and food