Chp 22 Flashcards

(46 cards)

1
Q

The universe began with the Big Bang about how many years ago

A

13.7 bya

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2
Q

H and He were converted to what heavier elements

A

C, N, O

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3
Q

Stars that exploded are called

A

Supernovas

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4
Q

Clouds collapsed to make

A

New stars and soar systems

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5
Q

Solar systems began

A

4.6 bya

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6
Q

Earth is how old

A

4.55 bya

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7
Q

Earth originated from aggregation of

A

Planetesimals over a period of 100-200 my

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8
Q

Earth cooled enough for outer layers to solidify and oceans to form

A

4 bya

Four cooling

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9
Q

Origin in 4 overlapping stages

A

Nucleotides and AA—>[polymerize] DNA, RNA, and proteins —>[enclosed in] membrane —>[aquired] cellular properties

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10
Q

Organic molecules

A

Little free oxygen gas

Prebiotic soup

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11
Q

Reducing atmosphere hypothesis

A

Atmosphere rich in water vapor, h2, ch4, nh3 and little o2
Miller- urey experiment of 1953
Formed precursors, AA, sugars and nitrogenous bases
Showed says techsis was possible not proven

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12
Q

Extraterrestrial hypothesis

A

Meteorites brought organic carbon to earth; may include amino acids and Nucleic acid bases
Opponents argue that most of this would be destroyed in the intense heating and collision

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13
Q

Deep sea vent

A

Molecules may have formed in the temp gradient between extremely hot vent water and cold ocean water
Supported by experiments (kirt: the only experiments were those that show fe reacts with h2s to form pyrites and give off energy that may cause n2 to form nh3
Communities that derive energy from chemicals in the vent found here

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14
Q

Prebiotic synthesis if polymers not possible in aqueous solutions because

A

Hydrolysis competes

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15
Q

Formation of Nucleic acid polymers and polypeptides on what kind of surface

A

Clay because they can bind organic molecules because of negative charges, and they attract metal ions like Mg+ that can catalyze rxns to produce polymers

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16
Q

Their experiments they added monomer building blocks and watched them aggregate

A

They positioned the nucleotides

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17
Q

Aggregate of prebiotically produced molecules and macromolecules that aquired a boundary

A

Protobiont

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18
Q

Boundary that allowed it to maintain an internal chemical environment distinct from that of its surroundings

A

Lipid bilayer

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19
Q

4 characteristics of protobionts

A
  1. Boundary Seperated external environment from internal contents
  2. Polymers inside the protobiont contained information
  3. Polymers inside the protobiont had enzymatic function
  4. Protobiont capable of self replication-not self reproduction but divide to increase in number
    Assumption that metabolic pathways formed w/in that could modify the molecules.
20
Q

Droplets that form spontaneously from the association of charged polymers

A

Coacervates

Enzymes inside can perform primitive metabolic function

21
Q

Vesicles surrounded by a lipid layer

22
Q

Clay can catalyze for action of ___ that grow and divide

23
Q

Majority of scientists favor ___ as the first macromolecules of protobionts

A

RNA –simpler

24
Q

3 key RNA functions

A
  1. Ability to store information
  2. Capacity for self replication
  3. Enzymatic functions-ribozymes
25
DNA and proteins do not have all 3 functions
True
26
Chemical within a mixture of different chemicals has special properties or advantages that cause it to increase in number compared to other chemicals in the mixture
Chemical selection
27
Hypothetical scenario with 2 steps
1. One of the RNA molecules mutates and has enzymatic ability to attach nucleotides together- advan of faster replication 2. Second mutation produces enzymes ability to synthesize nucleotides - no reliance on prebiotic synthesis
28
Information storage
DNA would have relieved RNA of informational role and allowed RNA to do other functions DNA is less likely to suffer mutations or breaks
29
Metabolism and other cellular functions
Proteins have a greater catalytic potential/efficiency Proteins can perform other tasks-cytoskeleton, transport, etc Proteins came into being as RNA can catalyze formation of peptide bonds
30
Preserved remains of past life on earth
Fossils
31
Who study fossils
Paleontologists
32
Many rocks with fossils are
Sedimentary
33
Older rock is deeper and older organisms are ___ in the rock bed
Deeper
34
Fossils can be dated using elemental isotopes in accompanying rock
Radioisotope dating
35
Length if time required for exactly one half of the original isotope to decay measures amount of a given isotope as well as the amount of the decay product usually igneous rock dated
Half life
36
Geological time scale: origin 4.55 bya to present | The four eons are:
Hadean 4.5-3.8 bya - 3.8- first prokaryo Archaean 3.8-2.5 bya- 2.5 first eukaryo Proterozoic 2.5 to 543 mya- Cambrian explosion Phanerozoic- 543 mya to present
37
Changes in living organisms the result of
genetic changes
38
Environment changes:
allow for new types of organisms | responsible for extinctions
39
Major environmental changes
``` climate temp atomosphere (o2 started accum 2.4 bya)- origin of body plans coincide with o2 rise land masses-continental drift occured flood glaciation snowball earth hyopthesis volcanic eruptions meteoric impacts ```
40
Mass extinctions- 5 large mass extinctions
near end of Ordovician, Devonian, Permian, Triassic, and Cretaceous periods boundaries between geoloci time periods are often based on these events
41
rapid extinction of mmany modern species due to human activites is sometimes referred to as the
sixth mass extinction
42
When diverse microbial life (prokaryotic cells) floursihed in primoridal oceans
archaeon eon
43
all life forms prokaryotic during hardly any free oxygen so organisms were anaerobic first cells were heterotrophs; autotropsh evolved as supply of organic molecules dwindled
Archaeon Eon
44
layered structure of calcium carbonate
stromatolites
45
Multiccellular eukary arise 1.5 bya; 2 possible origins indiv form a colony single cell divides and stays stuck together First animals invertebrates-bilateral symmetry facilitates locomtion
proterozoic eon
46
Paleozoic era- cambria, ordovician, silurian, devonian, carboniferous, permian Mesozoic era- triassic and jurassic Cenozoic era- tertiary and quaternary
Phanerozoic Eon- proliferation of multicellular eukaryotic life extensive