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17 Cards in this Set

  • Front
  • Back

conditions that made life possible

abiotic synthesis of small organic molecules (amino acids and nitrogenous bases)


which turned into macromolecules such as proteins and nucleic acids


the formation of protocells (droplets with membranes that maintained an internal chemistry)


the origin of self replicating molecules

atmosphere compounds similar to early earth

volcanoes


alkaline vents

formed amino acids

harold urey and stanley miler

tested oparin and haldane's hypotheses that earth's early atmosphere was a reducing environment where organic compounds formed

vesicles

may be precursor to life


spontaneous formation (lipids to water)


lipid bilayer


can "reproduce" on its own

RNA

first genetic material


probably inside vesicles, passed on to daughter cells which natural selection could then act on


= formation of protocells

fossil record

found mostly in sedimentary rocks in strata


biased for long existing, abundant, hard parts, widespread species

geological record

standard time scale

four eons

Hadean - origin of earth


Archaean - oldest prokaryotes


Proterozoic - oldest eukaryotes


Phanerozoic - last half billion years, time most animals have existed

three eras of phanerozoic eon

Paleozoic


Mesozoic


Cenozoic

stromatolites

earliest direct evidence of life


layered rocks that form when certain prokaryotes bind thin films of sediment

mesozoic periods

Triassic - origin of mammals, gymnosperms (cone bearing plants)


Jurassic - dinosaurs abundant and diverse, gymnosperms dominant plants


Cretaceous - flowering plants, many organisms become extinct at end

key paleozoic periods

cambrian - sudden increase in diversity of animal phyla


devonian - bony fish, first tetrapods and insects


carboniferous - origin of reptiles

first eukaryotes

nuclear envelope, mitochondria, endoplasmic reticulum, mitochondria, cytoskeleton




endozymbiont theory - mitochondria and plastids were formerly prokaryotes that began living in larger cells

plate tectonics

earth's crust is composed of plates on earth's surface

adaptive radiation

periods of evolutionary change with many new species




follows mass extinctions, evolution of new novel characteristics, the colonization of new reasons

heterochrony

evolutionary change in the rate or timing of development

paedomorphosis

sexual maturity during childhood