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how did life arise? 1
small organic molecules were synthesized (ex. amino acids and nitrogenous bases)
how did life arise? 2
small molecules polymerized into macromolecules (ex. proteins and nucleic acids)
how did life arise? 3
molecules packaged into protocells
protocells
membrane-containing droplets
how did life arise? 4
self-replicating molecules allow for inheritance (RNA)
ribozyme
first RNA catalysts
when did earth form?
4.6 billion years ago
what did earth's early atmosphere contain?
water vaper and chemicals released by volcanic eruptions, such as nitrogen, nitrogen oxides, carbon dioxide, methane, ammonia, hydrogeb, hydrogen sulfide)
oparin and haldane
hypothesized a reducing environment
miller and urey
lab experiments proved the abiotic synthesis of organic molecules (like amino acids)
alternative theory 1
first organic compounds were synthesized near volcanoes or deep-sea vents
small organic molecules would polymerize when
concentrated on hot sand, clay, rock
what can lipids do in water?
form vesicles with a lipid bilayer
the first genetic material was?
RNA, not DNA
ribozymes do what?
make complementary copies of short stretches of RNA
the first living organisms have been documented
3.5 billion years ago
3.5 bya there was no
oxygen
when did oxygen appear?
2.7 billion years ago
what allowed for the production of oxygen?
cyanobacteria would undergo photosynthesis
what is strata?
layers of rock
incomplete record
many organisms not preserved, fossils destroyed, or not yet found
fossil record is biased towards
existed for a long time, abundant, widespread, had hard parts
radiomentric dating
a way to find the age of fossil using the half-life
half-life
the time required for half the parent isotope to decay
relative dating
uses order of rock strata to determine the relative age of fossils
each era ends and starts with
ends with major extinction and starts with adaptiove radiation
timeline
3.5 bya - first prokaryotes
2.7 bya - oxygen in atmosphere
2.1 bya - first eukaryotes
1.2 - first multicellular eukaryotes
500 mya - colonization of land
stromalites
the oldest fossil- rocks formed by the aaccumulation of sedimentary layers on bacterial mats
banded iron formations
oxygen that reacted with dissolved iron and precipitated out to form
oxygen revolution
caused the extinction of many prokaryotic groups
endosymbiont theory
mitochondria and chloroplasts were formerly small prokaryotes living within larger host cells
cambrian explosion
the sudden appearance of fossils resembling modern animal phyla
plants and fungi
mutually beneficial and likely colonized land together
the rise and fall of groups depend on
speciation and extinction rates within the group
plate tectonics
earth's crust is composed of plates floating on earth's mantle
interactions between plates cause
the formation of mountains and islands, and earthquakes
the distribution of fossils and living groups reflects
the movement of continents
mass extinction
a large extinction of species in a relatively short period of time
factors that contribute to mass extinctions
volcanoes, glocal warming, redcued temperature gradient, reduced mixing of ocean waters
alternative theory 2
organic molecules could have been transported to earth by a meteorite
adaptive radiation
evolution from a common ancestor of many species adapted to diverse environments
adaptive radiation may follow
mass extinctions, evolution of novel characteristics, colonization of new regions
heterochrony
evolutionary change in the timing or rate of an organism's development
heterochrony examples
human and chimpanzee skulls
paedomorphosis
the rate of reproductive development accelerates compared with somatic development
homeotic genes
genes that determine basic features of where a body part is
homeotic gene example
wings on a bird
hox genes
class of homeotic genes. changes in these genes can have a profound impact on morphology
exaptations
structures that evolve in one context but become co-opted for another function