Lecture 8 Flashcards

1
Q

Precambrian

A
  • Archean and Proterozoic Eons comprise in interval of time informally called Precambrian, which spans 87% of the geologic time scale
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2
Q

Hadean Eon

A

The oldest of the Precambrian eons; the time between Earth’s origin and the formation of the first rocks that have been preserved.

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3
Q

Hadean Atmosphere

A
  • Early Earth had a molten surface or thin, unstable crust
  • Sustained by heat from abundant meteorites striking the
    Earth and the decay of radioactive elements
  • Primitive atmosphere probably comprised of Hydrogen
    (H2) and Helium (He)
  • Primitive gases lost to space early in Earth’s history
  • Weak gravity prohibited retention of lighter gases
  • Dispersed by strong solar winds
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4
Q

Archean Eon

A
  • Earliest organisms developed in an atmosphere lacking oxygen.
  • The first oceans formed as
    rain from the skies
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5
Q

Miller Experiment

A

An experiment that reproduced the conditions under which life began on Earth and amino acids and other organic compounds were manufactured.

First laboratory synthesis of amino acids

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6
Q

Where did life originate?

A

Life probably began in the sea

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7
Q

hyperthermophiles

A

Organisms that grow in extremely high temperatures (90 degrees C)

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8
Q

chemosynthesis

A

Process by which some organisms, such as certain bacteria, use chemical energy to produce carbohydrates

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9
Q

Stromatolites

A

Oldest known fossils formed from many layers of bacteria and sediment.

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10
Q

Proterozoic Eon

A
  • Early life like today’s earth.
  • Almost half of earth’s history.
  • 90% of Earth’s continental crust by the middle Proterozoic.
  • Life forms evolved slowly
  • First tine oxygen is used.
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11
Q

Proterozoic Atmosphere

A
  • More oxygen then Archean
  • Current oxygen level is at 21%
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12
Q

Snowball Earth - Late Proterozoic

A

Late Proterozoic, earth was mostly glaciers and snowy.

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13
Q

Rodinia

A

A supercontinent older than Pangaea that formed about 1.1 billion years ago and began to break up about 750 million years ago.

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14
Q

Grenville Orogeny

A

An episode of deformation that took place in the eastern United States and Canada during the Neoproterozoic.

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15
Q

Pannotia

A

A supercontinent that existed during the Neoproterozoic. Was very short-lived.

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16
Q

Banded Iron Formations (BIFs)

A

A sedimentary deposit that consists of alternating thin layers of iron oxides (such as magnetite or hematite) and iron-poor minerals (such as shale or chert). Jasper Knob in Michigan. Banded iron formations, which formed over a billion years ago, are often used today as a source of low-grade iron ore.

  • It signals oxygen getting turned on (Input of oxygen)
17
Q

Is ultraviolet light harmful?

A

Yes