Origin of Life Flashcards

1
Q

When was earth created

A

4.6 billion years ago

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2
Q

When did life being

A

3.5 billion years ago

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3
Q

Pre-Cambrian period

A

-makes up 90% of Geological Time Scale
- made up of Hadean, Archeon, and Proterozoic eons

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4
Q

Order Eons chronologically

A

Hadeon (4.6-4bya) - Archeon (4-2.5 bya) - Proterozoic (2.5-541 mya)

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5
Q

Hadean Eon

A

-time before a reliable (fossil) record of life
- temps are extremely hot
- no oxygen
- ejected debris following giant impact collision between early earth and an ancient planet called theia is thought to have formed the moon

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6
Q

Archeon Eon

A
  • volcanic activity was considerably higher than today, with numerous lava eruptions
  • without oxygen
  • beginning of life on earth and evidence of cyanobacteria
  • life was limited to simple-celled organisms lacking nuclei (prokaryotes)
  • earths crust had cooled to allow formation of continents
  • earliest identifiable fossils (stromatolites)
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7
Q

Proterozoic Eon

A
  • appearance of oxygen to just before the proliferation of complex life (such as corals)
  • bacteria began producing oxygen, leading to the sudden rise of life forms
  • eukaryotes cells emerge, including some forms of soft-bodied multicellular organisms
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8
Q

Describe how stromatolites formed

A
  • form in shallow water
  • column shaped structures made up of layers of sedimentary rock, created by mats of cyanobacteria living on top of stromatolite
  • cyanobacteria continue to reproduce on upper surface of mats as these cells depend on light for photosynthesis
  • sediments begin to settle and accumulate on top of cyanobacteria, block sunlight, cyanobacteria slowly move to top of this sediment layer, trapped sediment within stromatolite will harden into rock
  • tiny living things, like bacteria and algae, grew together in layers on the bottom of shallow water
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9
Q

Describe how banded iron formations are created

A
  • consists of layers of iron oxides (either magnetite or hematite) separated by layers of chert, jasper or quartz
  • each layer is usually narrow
  • rock has a distinctively banded appearance because of differently colored lighter (chert, jasper, quartz) and darker iron-rich layers
  • iron and oxygen in seawater combine to form iron oxide, which settles to the ocean floor as layers of sediment.
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10
Q

Describe how red beds are formed

A
  • huge deposits of iron-rich sediment
  • once in air, 02 could react with iron in sediments on the earths surface, which produced rust-colored sedimentary rock known as red beds
  • first appeared in geologic records 2 bya
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11
Q

Explain how stromatolites, banded iron formations, and red beds are geological evidence of free oxygen on early earth during Pre-Cambrian period

A

-stromatolites needed oxygen to survive, their presence suggests oxygen was available in the environment
-iron formations created when iron in seawater combined with oxygen
-red beds are rock with a reddish color due to the presence of iron oxide, which forms when iron reacts with oxygen

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12
Q

Explain how stromatolites led to the existence of banded iron formations and red beds

A

-stromatolites were formed by tiny living organisms, like bacteria and algae, which released oxygen during their life processes
-oxygen combined with iron in the seawater, forming banded iron formations as layers of iron-rich rocks settled on the ocean floor
-oxygen continued to build up in the atmosphere, it reacted with iron in the land, leading to the formation of red beds with iron oxide-rich rocks.

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13
Q

Phanerozoic Eon

A
  • represents the period of earths history with advanced life forms
  • Paleozoic, Mesozoic, and Cenozoic eras
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14
Q

Paleozoic Era

A

-542 to 251 million years ago
- longest period of Phanerozoic Eon
- composition of air was very similar to current atmosphere (80% nitrogen and 20% oxygen)
- formation of Pangaea
- Cambrian explosion

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15
Q

Cambrian Explosion

A

535 to 525 million years ago
- most intense burst of evolution ever know
-earliest fossil appearance of many major groups of living animals

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16
Q

List and explain 6 reasons that triggered the Cambrian explosion

A
  1. Higher oxygen levels in atmosphere
    - made aerobic respiration more efficient over anaerobic respiration and fermentation
  2. Evolution of predation
    - predation exerted selection for defensive structures, body plans for rapid movement
  3. New ecological niches
    - evidence of animals burrowing under, living on, and swimming above sea floor
  4. New developmental genes
    - early animals had few or no hox genes
  5. Snowball earth hypothesis
    - planet was covered with thick sheet of ice, last thawing triggered diversification by releasing nutrients into oceans
  6. Ozone formation
    -marine organisms became mobile and were able to live in shallower areas of ocean with more sunlight exposer
17
Q

Identify when animals first appeared in the Geological Time Scale

A
  • Proterozoic era of Precambrian period
    -635-541 mya
18
Q

Adaptive radiation
exmaples

A
  • rapid production of many descendant species (with wide range or forms) from a single lineage
    ex. cambrian explosion, darwins finches, diversification of mammals following extinction of dinosaurs, australian marsupials
19
Q

List 3 hallmarks for adaptive radiation

A

-monophyletic group
- rapid speciation
- ecological diversification into many niches: niche describes range of resources that a species can use and range of conditions that it can tolerate

20
Q

Mesozoic Era

A
  • 251 to 65.5 million years ago
  • break up of Pangaea
  • Coral reefs emerged
  • Dinosaurs were dominant terrestrial vertebrates
  • known as the “Age of Reptiles”
  • Gymnosperms were dominant terrestrial plants
  • first mammals emerged (were tiny nocturnal insect-eaters)
  • warm period during this time that there was no ice caps
21
Q

Cenozoic Era

A
  • 65.5 million years ago to now
  • mammals were dominant terrestrial vertebrates
  • know as the “Age of Mammals”
  • angiosperms are most dominant terrestrial plants
  • global climate gradually cooled through this time