Theme 5C: The history of life Flashcards

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1
Q

What was the Earth’s early atmosphere like?

A
  • Originally very little oxygen
  • Oxygen did not exist in a molecular state
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2
Q

What type of energy input was used to transform some of the compounds in the earth to form the first organic compounds?

A
  • Lightning!
  • This was replicated in the Urey-Miller experiment
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3
Q

When was there a rapid expansion of life?

A
  • During the Phanerozoic eon.
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4
Q

Where were some of the first prokaryotes found?

A
  • Found in stromatolites due to the presence of cyanobacteria
  • Stromatolites appear in fossils dating back to 2.7 billion years ago, decline in abundance by 500 million years ago
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5
Q

How did cyanobacteria contribute to the change in the Earth’s atmosphere?

A
  • Cyanobacteria obtain their energy through photosynthesis, so gaseous oxygen is produced as a by-product
  • Converted the Earth’s atmosphere into an oxidizing one
  • Rusting of the Earth
  • Led to the near-extinction of oxygen-intolerant organisms
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6
Q

What was the great oxygenation event?

A
  • When free oxygen accumulated in the atmosphere about 2.5 billion years ago, with an increase about 850 million years ago
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7
Q

What is some of the major evidence regarding the great oxygenation event?

A
  • Banded iron formation in different rocks
  • Major changes in the number of rock types formed after this event
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8
Q

What could explain the long gap before oxygen was able to develop in the atmosphere?

A
  • There was a long period of anoxygenic photosynthesis
  • The oxygen that was being produced by the cyanobacteria was most likely being absorbed by the ocean, changing the chemistry of the ocean
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9
Q

What’s the endosymbiotic theory?

A
  • The origin of key eukaryotic organelles result of a symbiosis between separate single-celled organisms
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10
Q

What’re some of the major evidence supporting the endosymbiotic theory?

A
  • Organelles are bound by membranes
  • Organelles have their own DNA
  • Mitochondrial DNA sequences similar to bacteria/chloroplast DNA sequences similar to those of some cyanobacteria
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11
Q

What’s the Paleozoic era?

A
  • One of the major episodes in the history of life
  • When the Cambrian explosion occurred, invasion of land, the appearance of gymnosperms, major groups of tetrapods
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12
Q

What was the Cambrian explosion?

A
  • Rapid appearance of many groups of organisms about 530 million years ago.
  • Preceded by the appearance of small shell parts (calcium carbonate was more abundant)
  • Unusually high number of sites with soft-body preservation
  • Includes evidence of arthropods, echinoderms, and a large number of extinct forms
  • Features of many modern groups started to apear such as mouths, heads, eyes, and legs
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13
Q

Why was there such an increase in oxygen in the atmosphere after the Cambrian explosion?

A
  • Eukaryotic algae developed
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14
Q

Why was there such a high rate of mutations in organisms found during the Cambrian explosion?

A
  • The organisms do not have the same proofreading capabilities that we have now, so many mutations were able to occur, creating a lot of variation among the species.
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15
Q

What is mass extinction?

A
  • When the rate of extinction greatly exceeds the rate of speciation (i.e., more than 75% of known species in a geographically short interval)
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16
Q

Why are mass extinctions significant to evolution?

A
  • Niches are cleared and ecological opportunities are made available to the organisms that remain
  • Trims the phylogenetic tree (‘dead clades walking’)