Ch 26: The Origin & Diversity of Life Flashcards

0
Q

Ribosome activity

A
- RNA may have been first 
  genetic material
- Amino acids polymerized
  into proteins
- Metabolic paths emerged
- lipid bubbles could inc. 
  chance of metabolic
  reactions 
     - leads to cell
       membranes
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1
Q

Plate Tectonics

A

Continents moved over geological time.

Earth’s crust formed rigid slabs of rock (plates) under continents and oceans

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2
Q

Microfossils

A
  • Fossilized forms of micro life
  • Oldest: 3.5 billion years ago
  • Resemble present-day
    prokaryotes
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3
Q

Endomembrane system

A

Nuclear membrane, only found in eukaryotes, accounts for increased complexity
Golgi apparatus and endoplasmic reticulum facilitate intracellular transport

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4
Q

Endosymbiosis

A
Cells "eat" other cells and 
become multicellular
      -how mitochondria and 
       chloroplasts entered euk
       cells
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5
Q

Mitochondria & Chloroplast evolution

A

Mitochondria:
descendants of relatives of purple sulfur bacteria and the parasite rickettsia.

Chloroplasts:
derived from cyanobacteria

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6
Q

Multi-cellularity

A
  • Allowed organisms to deal with environment in many ways
  • Allows for differentiation of cells into tissues
  • Evolved independently in eukaryotes supergroups
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7
Q

Sexual reproduction

A

-Allows greater genetic diversity
-meiosis
-crossing over
-First eukaryotes probably haploid
-diploid arose independently on
sep occasions (fusion of haploid
cells)

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8
Q

Cambrian explosion

A
  • Evo innovations occurred when life primarily aquatic

- 1st multicell animals appeared 50 mil years ago following explosion

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9
Q

Moving onto land

A
  • Plants, then animals, colonized terrestrial environments after Cambrian radiation
  • plants photosynthesis created o2 in ozone layer
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10
Q

Compartmentalization

A
- Allows increased subcellular 
  specialization
- Nuclear membrane allows for 
   additional levels of control of 
   transcription/translation
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11
Q

Hadean Era

A

Formation of Earth
4.5 BYA
Earth cools around 4 BYA

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12
Q

Archean Era

A

Life emerged (prokaryotes)
Formation of Rodinia
3.5–2.5 BYA

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13
Q

Proterozoic Era

A
Eukaryotes
First multicellular organisms
Appearance of animals and plants
Cyanobacteria
Appearance of oxygen in the atmosphere
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14
Q

Fossilization

A
  • Organisms buried in sediment
  • Calcium in bone shell or other
    hard tissue mineralizes
  • Surrounding sediment hardens
    to form rock
  • Erosion must expose fossils
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15
Q

Aging fossils

A

Relative age:
position of the fossil in the sediment

Absolute age: 
age of fossils is estimated by rates of radioactive decay
      -Isotopes transform at
        precise known rates into    
        non-radioactive forms
        (rate of decay = Half life)
16
Q

Miller and Urey

A

Exper. recreated early atmos.

Assembly:
Reducing atm mix of gases, H with no O gas, placed over water, temp below 100°C

Results:
simulated lightning sparks, & small organic molecules inc. amino acids