1.10.2 The Heterotroph Hypothesis: An Introduction Flashcards

1
Q

studies of primitive earth

A
  • based on the study of other planets and rock
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2
Q

Alexander Oparin and J. B. S. Haldane

A
  • hypothesized that the conditions of primitive Earth consisted of a reducing atmosphere, which is an appropriate atmosphere for the synthesis of carbon-containing molecules—the molecules of life.
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3
Q

biotic

A
  • living organisms in the environment
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4
Q

abiotic

A
  • nonliving environment
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5
Q

reducing atmosphere

A
  • was thought to have consisted primarily of methane (CH4), water vapor, and ammonia (NH3).
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6
Q

oxidizing atmosphere

A
  • contains high amounts of oxygen (O2). Oxygen is an
    oxidizing agent—it grabs electrons. An oxidizing atmosphere is not favorable for synthesizing organic molecules because grabbing electrons is not conducive to making bonds.
  • The chemicals in a reducing atmosphere can act as reducing agents—they donate electrons. This characteristic allows for the synthesis of organic molecules because as electrons are donated, bonds can form.
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7
Q

An abundance of __________ was absent from the Earth’s atmosphere four billion years ago.

A
  • free oxygen
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8
Q

the chemicals in a reducing atmosphere act as reducing agents by donating electrons

A
  • true
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9
Q

Evidence suggests that 4.5 billion years ago the atmosphere most likely consisted of

A
  • CH4, H2O, CO2, N2, and NH3
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10
Q

Who were the scientists responsible for proposing that primitive Earth’s atmosphere was reducing?

A
  • Oparin and Haldane
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11
Q

The Earth’s early atmosphere is thought to have primarily been a (an) ______________ atmosphere, which is conducive to the synthesis of the molecules that make up the building blocks of life.

A
  • reducing
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12
Q

Which of the following forms of energy was not available for chemical reactions on primitive earth?

A
  • fossil fuel
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