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16 Cards in this Set

  • Front
  • Back
2 Phases That Life Emerged on Earth
1) chemical evolution
2) biological evolution
chemical evolution
evolution of the organic molecules, biopolymers, and systems of chemical reactions needed to form the first protocells (1 billion years)
biological evolution
evolution from single-celled prokaryotic bacteris to single-celled eukaryotic creature, and then to multicellular organisms (3.7-3.8 billion years)
The cosmic dust that condensed into earth turned molten from:
1) meteorite impacts
2) heat produce by radioactive decay of chemical elements in its interior
Chemicals that dominated the primitive atmosphere:
1) cabon dioxide
2) nitrogen
3) water vapor
4) other - methane, ammonia, hydrogen sulfide, hydron chloride
organic molecules needed for life formed from inorganic chemicals found in earth's primitive atmosphere under the influence of readily available:
1) energy from electrical discharges (lightning)
2) heat from volcanoes
3) intense ultraviolet (UV) rays
4) other forms of solar radiation
Other possibilities are that necessary organic molecules formed:
+ on dust particles in space and reached the earth on meteorites or comets
+ formed deep within the earth
+ formed around mineral-rich and very hot hydrothermal vents
hydrothermal vents
vents that sit atop crack in the ocean floor leading to subterranean chambers of molten rock
protocells
small globules that could take up materials from their environments and grow and divide (much like living cells)
reactions that formed protocells could have occured:
1) in the earth's warm shallow waters
2) deep within the earth
3) around thermal hydrothermal vents on the ocean bottom
fossils
mineralized or petrified replicas of skeletons, bones, teeth, shells, leave,s and seeds, or impressions of such items
other sources of fossil information:
1) chemical and radioactive dating of fossils
2) nearby ancient rocks
3) material in cores drilled out of buried ice
4) the DNA of organisms alive today
biological evolution / evolution
the change in a population's genetic makeup (gene pool) through successive generations
theory of evolution
all species descended from earlier, ancestral species
microevolution
the small genetic changes that occur in a population
macroevolution
used to describe long-term, large-scale evolutionary changes through which
1) new species are formed from ancestral species
2) other species are lost through extinction