Lecture 6 Flashcards

1
Q

4 requirements for life

A
  1. metabolism
  2. response to stimuli
  3. homeostasis
  4. reproduction with potential for error
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2
Q

are viruses alive?

A

no, lack metabolism and homeostasis, cannot reproduce without host cell

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3
Q

fossil

A

a preserved remnant/ evidence of organisms that lived in the past

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4
Q

strata

A

distinct layers in rock

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5
Q

why is our understanding of the diversity and distribution of past life is biased and incomplete?

A

fossils more likely to form if hard, aquatic, inshore, and decomposing organisms absent after death

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6
Q

3 types of fossils

A
  1. trace fossils (evidence of behaviour)
  2. cast (minerals fill space in sediment where organism decayed)
  3. petrified (tissues replaced by minerals)
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7
Q

ichnology

A

study of trace fossils

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8
Q

sub-fossil

A

high % organic material (thin carbon film, amber, tar, peat, frozen)

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9
Q

relative dating

A

done via sedimentary stratigraphy, can’t tell how long ago fossil was created but can tell which fossil came 1st, 2nd, etc

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10
Q

index/indicator fossils

A

help to read incomplete or scrambled layers, existed for a brief time with wide geographic distribution

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11
Q

geologic time scale

A

created based on the appearance and disappearance of major taxa, major events correlated with changes in eon, era, period or epoch

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12
Q

radiometric dating

A

measurement of radioactive isotopes in fossils or rocks to determine absolute dates for geologic time scale

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13
Q

Carbon 12

A

common, 6 neutrons

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14
Q

Carbon 14

A

8 neutrons, decays to N-14

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15
Q

half-life

A

when 50% of atoms in a given amount of radioactive substance have decayed

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16
Q

carbon dating

A

when organism dies, C-12 stays but C-14 decays - increasing ratio of C-12:C-14 in fossils allows fossils to be dated

17
Q

half-life of carbon

A

5730 years, carbon dating only good for young fossils up to 75 000 years old

18
Q

half-life of uranium

A

4.5 billion years, better for older fossils

19
Q

continental drift

A

relative locations of land masses have changed over time, fossils provided first evidence

20
Q

Pangaea

A

first supercontinent

21
Q

Gondwana

A

Australia, Antarctica, and South America, same genus of fossil plant found

22
Q

2 mass extinctions

A
  1. End-Permian

2. End-Cretacious

23
Q

End-Permian

A

245 MYA, 60% of families and 90% of marine species extinct, formation of Pangaea

24
Q

End-Cretacious

A

65 MYA, at Cretaceous-Paleogene boundary, 20% of families including non-avian dinosaurs and ammonites extinct, climate change or asteroid strike

25
planet formed
4.6 BYA, bombarded by large chunks of rocks until 3.9 BYA
26
oldest fossil evidence of life
3.5 BYA, hypothesized to have existed up to 3.9 BYA - single-celled prokaryotes
27
prokaryotes
lack membrane-bound organelles, DNA not contained in nucleus, only type of fossil evidence for 1.5 BYA
28
stromatolites
where many of the oldest prokaryotic fossils are found, many species of prokaryotes living together on substrate, sediments accumulate, grow up through sediment, creates banded rock
29
cyanobacteria aka blue-green algae
oxygen began accumulating 2.7 BYA when photosynthetic cyanobacteria started using sun’s energy to split water into hydrogen & oxygen
30
banded iron rock
first oxygen released through photosynthesis probably reacted with dissolved iron in oceans to create iron oxide, iron oxide precipitated out
31
early 02
toxic to early life, attacks chemical bonds
32
obligate anaerobes
descendants of species that could survive only in very little 02, present in rotting oxygen-free substrates and guts of animals
33
spontaneous generation
until 1800’s, how we thought that microbes arose
34
Louis Pasteur's beef broth experiment
broth spoiled only if bacterial spores could drop from the air, disproved spontaneous generation
35
how early cell-like structures may have arisen
free-floating amino acids created, and spontaneous formation of hollow lipid vesicles
36
Montmorillonite
volcanic clay 4 BYA that vesicles form faster in
37
Where did life originate?
original: shallow water bodies now: hot, mineral-rich deep-sea vents
38
panspermia hypothesis
first prokaryotes came from space, supported by nanobes in meteorite
39
most important condition for life to arise
free non-toxic water