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Domain similarities
Eukarya and Archaea: introns and histones
Archaea and Bacteria: no nucleus, circular DNA
all: DNA, cell membrane, proteins, ribosome
hierarchy
domain
kingdom
phylum
class
order
family
genus
species
domain eukarya
plantae, Animalia, fungi, protista
phylogeny
study of relationships between different organisms
show patterns to show common ancestry (not always based on physical structures)
taxa
group of organisms
order of earth timeline
proto cells
anaerobic respiration
glycolysis
photosynthesis (some oxygen)
aerobic respiration
eukaryotic organisms (spike in oxygen)
multicellular organisms
animals
miller-grey experiment
early earth simulation to show environment (primordial reducing atmosphere)
electric spark (lightning storm) in chamber with inorganic molecules, provides energy
water added to boiling chamber to generate heat and flows into electric chamber
resulted in organic molecules/amino acids (more than 1 carbon)
conserved processes across domains/kingdoms
glycolysis
DNA/RNA synthesis
cell division
transcription/translation - make proteins
photosynthesis
cyanobacteria
unique ability of photosynthesis in thylakoid membrane (cyanobacteria, protists, plants)
prokaryotes
no chloroplast
endosymbiosis
how prokaryotes developed into eukaryotes
membrane unfolds creating nucleus and other membrane bound organelles
swallows smaller cells (chloroplast and mitochondria)
endosymbiosis evidence
mitochondria and chloroplast
have own DNA
double membrane
used to be ribosomes
binomial nomenclature
genus + species (scientific name)
rate of evolution of DNA sequences
rRNA changes slowly and useful for taxa that diverged a long time ago
mtDNA evolves rapidly and is useful for recent evolutionary events like human evolution
molecular clock
approach for measuring absolute time of evolutionary change based on observation that some genes appear to evolve at constant rates
domain comparison
nuclear envelope: bacteria x archaea x eukarya ✔
membrane enclosed organelles: bacteria x archaea x eukarya ✔
introns: bacteria x archaea ✔ eukarya ✔
histones associated with DNA: bacteria x archaea ✔ eukarya ✔
circular chromosome: bacteria ✔ archaea ✔ eukarya x
extinction from phylogenetic tree
species don’t reach present time
domain with active site
most percentage of homologous amino acids because active site is highly conserved
conservation across domains
glycolysis
photosynthesis
DNA structure/replication
protein synthesis
cytoskeleton
kingdom conservation
membrane bound organelles
linear chromosomes
endomembrane system
evidence for phylogenies
fossils
anatomy/morphology
embryology/development
molecular traits (amino acid sequence in proteins or base sequence in DNA)
behavioral traits
fossils (as evidence)
strengths: determine time, extinct species, transitional
weakness: not all species leave fossils, fossil record incomplete
anatomy/morphology
strength: homologous structures indicate evolutionary relations
weakness: analogous structures do not reflect ancestry
some taxa have little diversity (bacteria)
some morphology reflects environment/diet
embryology/development
strength: reveal similarities in structures not evident in adults
weakness: similarities between species may be lost in later development
molecular traits
strengths: large number of traits, allow study of evolution between closely related species, most accurate
weak: no/little data for extinct species, variation within species blurs differences between species
behavioral traits
strength: some behavior are genetic, ex: frog calls
weak: behavior may be culturally transmitted/learned, ex: bird calls
plesiomorphy
shared primitive/ancestral characteristic, at base of a tree
apomorphy
shared derived characteristic, believed to have evolved within tree so can separate on group in tree from rest
homoplasy
characteristic shared by members but not present in common ancestor (from convergence)
outgroup
group of organisms as reference group for determination of evolutionary relationship among related organisms (comparison group)
fossils
sedimentary rocks, occurs where sediment accumulation is high and organisms with hard parts
rock strata
stacked-up layers of sedimentary rock
cannot determine exact dates, only relativity
radiometric dating
decay of isotopes to determine age of rocks/fossils, based on half life
absolute age
iron oxide bands
evidence of great oxygenation event
adaptive radiation
a rapid increase in the number of species with a common ancestor
new habitats/ecological niches
carbon 14
the more remaining, the younger
alternative hypothesis
shows there is an effect between two things
null hypothesis
no effect