Topic 9: Origin of Life Flashcards

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1
Q

The three main biological polymers,
nucleic acids, proteins, and
polysaccharides, are built from:

A

five
nucleotide bases, 20 amino acids, and
a few sugars

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2
Q

What an entity needs to be considered alive:

A

Organization, metabolism, stimuli, homeostasis, adaptation, reproduction

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3
Q

Organization

A

structurally
composed of one or more cells
(basic units of life)

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4
Q

Metabolism

A

a system of
management of energy and
materials via chemical reactions

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5
Q

Stimuli

A

Response to stimuli: via changes in
growth, alteration of chemical
reactions, or movement

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6
Q

Homeostasis

A

maintenance of
some internal chemical and/or
thermal consistency relative to
variation outside of the organism

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7
Q

Adaptation

A

the ability to change
over time in response to the
environment

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8
Q

Reproduction

A

ability to produce

new individual organisms

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9
Q

Viruses

A
  • have nucleic acids that can replicate, mutate, and respond to natural selection
  • lack metabolism and homeostasis, and cannot reproduce without using the cellular machinery of a host cell
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10
Q

Earth formed ___ years ago

A

4.6 billion

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11
Q

First replicating life:

A

3.9 billion years ago

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12
Q

The geologic record is divided into:

A

the Archaean, the Proterozoic, and

the Phanerozoic eons

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13
Q

Three eras of phanerozoic

A

Paleozoic, Mesozoic, and Cenozoic

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14
Q

Fossils

A

the preserved
remains/evidence of organisms that
lived in the past.

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15
Q

Fossils are used for:

A

calibrate
phylogenies, record extinct species (e.g.
linkage between dinosaurs and modern
birds), and link evolutionary events (e.g.
mass extinctions) with geological and
environmental changes on Earth.

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16
Q

Probability of an organism (or part of)

becoming fossilized increases if:

A
  • Existed for a long time.
  • Was abundant and widespread.
  • Hard rather than soft-bodied.
  • Aquatic rather than terrestrial.
  • Inshore marine rather than offshore
    marine.
  • Decomposing organisms were absent
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17
Q

Types of fossils recorded

A

Cast, Replacement, trace, preserved

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18
Q

Cast fossils

A

A cast forms when minerals fill
space in sediment where the
organism decayed after having
been buried

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19
Q

Replacement fossil

A

fossils
have had their tissues replaced by
minerals

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20
Q

Trace fossils

A

record evidence of

behavior (tracks, burrows, feces).

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21
Q

Preserved fossils

A

retain the original
organic material (carbon films,
amber, tar or peat, frozen)

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22
Q

Sedimentary strata reveal ____

ages of fossils

A

relative

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23
Q

Radioactive dating

A
Radioactive decay of isotopes of
various elements provides a means
of determining the age of fossils or
rocks. Radioactive isotopes decay
from one form to
another at a known
constant rate.
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24
Q

Half life of C14

A

5,730 years

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25
Q

time when there was a supercontinent

A

1.1 billion, 600

million, and 250 million years ago.

26
Q

Plate tectonics theory

A
considers
that Earth’s crust is composed of
large plates that have been slowly
moving since about 3.4 billion
years ago
27
Q

Continental drift during pangea

A
  • Deepening of ocean basins.
    − Reduction in shallow water habitats.
    − Colder and drier climate inland.
28
Q

Continental drift effect on biodiversity

A
  • Changes to the environment and climate as
    continents move north or south.
    − Opportunities for diversification. (e.g. when land masses are isolated, each can develop unique
    species via allopatric speciation.)
    − Mass extinctions.
29
Q

The fossil record shows that most
species that have ever lived are
now ___

A

extinct

30
Q

In each of the 5 mass extinctions, ___ of species went extinct

A

50%

31
Q

Permian mass extinction

A
  • the boundary between the Paleozoic and Mesozoic eras
  • 252 million years ago
  • greatest extinction
  • caused by extensive volcanism in Siberia
  • during formation of Pangea (more shallow shorelines and reduced temperature gradient)
32
Q

Cretaceous mass extinction

A
  • separates Mesozoic from Cenozoic
  • 65.5 million years
  • 20% of families went extinct
  • extinction of dinos
  • Presence of iridium in sedimentary rocks suggests a massive meteorite impact about 65 mya
33
Q

It can take ____ years for biodiversity to recover after a mass-extinction

A

5 to 100 million

years

34
Q

Mass extinctions can lead to

A

adaptive radiation

35
Q

Adaptive radiation

A

the rapid
evolution of diversely adapted
species from an ancestral species

36
Q

When does adaptive radiation happen

A

Adaptive radiation occurs when a
change in the environment makes
new ecological niches available

37
Q

Adaptive radiations may follow

A

mass extinctions, the evolution of novel characteristics, colonization of new regions

38
Q

Mass extinctions

A

By eliminating so many species, mass
extinctions can pave the way for
adaptive radiations

39
Q

Evolution of novel characteristics

A

The adaptive radiation of
photosynthetic prokaryotes, land
plants, insects, and tetrapods was
enabled by novel adaptations

40
Q

Colonization of new regions

A

Adaptive radiations can occur when
organisms colonize new
environments with little competition

41
Q

Earth’s first billion years

A
  • The surface began to cool; unstable crust floated on the molten magma.
  • Steaming gasses from cooling rock formed an atmosphere lacking oxygen.
  • Atmospheric temperatures dropped:
    gasses condensed and rained down.
  • Basins filled with water, forming transient
    oceans.
  • Between 3.8 and 4.1 bya bombardment of Earth by asteroids and comets would have vaporized water, preventing seas from forming and sterilizing the planet’s surface
  • Earth’s early atmosphere likely contained water vapour and chemicals from volcanic eruptions (nitrogen, nitrogen oxides, carbon dioxide, methane, ammonia,
    hydrogen, hydrogen sulphide)
42
Q

hypothesized

sequence of stages for evolution of simple cells

A
1. Abiotic synthesis of small organic
molecules.
2. Joining of small organic molecules
into organic polymers (organic
macromolecules).
3. Packaging of molecules into
protocells.
4. Origin of self-replicating molecules.
43
Q

Abiotic synthesis of small organic molecules

A

inorganic to organic

- possibly due to terrestrial origins or extraterrestrial oragins

44
Q

Terrestrial origins of organic molecules on earth

A

organic molecule synthesis driven by energy sources, e.g. UV light, electrical discharges. Earth’s early atmosphere was initially hypothesized to be a reducing environment.

45
Q

Miller & Urey demonstrated:

A

the abiotic synthesis of organic molecules in a reducing atmosphere

46
Q

Instead of forming in the
atmosphere, abiotic synthesis may
have occurred:

A

near volcanoes or
deep-sea hydrothermal vents where
strongly reducing conditions are
found

47
Q

Abiotic synthesis of organic polymers

A

Wetting and drying cycles of water on hot surfaces, such sand, clay, or rock, may have concentrated small organic molecules, triggering the spontaneous formation of organic polymers

48
Q

Polyphosphates cause polymerization

of amino acids into

A

peptides

49
Q

Packaging of molecules into protocells

A
- Free-floating amino acids, proteins,
and nucleic acids would not have
been able to behave like cells
- there needed to be replication and metabolism
- In water, lipids and other organic
molecules can spontaneously form
hollow vesicles with a lipid bilayer
A sphere would have been able to
keep (or export) its products
50
Q

− Protocells

A

fluid-filled
vesicles with a membrane-like
structure

51
Q

w lipid vesicles form faster in the presence of

A

volcanic clay

52
Q

Lipid vesicles exhibit

A

simple reproduction and metabolism, and can maintain an internal chemical environment. Vesicles can increase in size and divide on their own.

53
Q

earliest genetic material was

A

RNA

54
Q

RNA

A
- RNA is single-stranded, fragile, and
self-replicating.
− RNA can store genetic information.
− Self-replicating RNA molecules have
been experimentally demonstrated.
− RNA could have provided a template
for the later evolution of DNA, a more
stable genetic material
55
Q

Some RNA molecules (ribosomes) can catalyze ______

A

chemical reactions

56
Q

The oldest fossil evidence of life is

of

A

prokaryotes (~3.5-3.7 bya)

57
Q

Prokaryotes

A

− Single-celled (unicellular).
− DNA is not contained in a nucleus.
− Lack membrane-bound organelles

58
Q

Two domains of prokaryotes

A

bacteria and archaea

59
Q

The oldest known fossils are

A

stromatolites

60
Q

Stromatolites

A

rocks formed by the accumulation of sedimentary layers on prokaryote mats (date back to 3.5-
3.7 bya)

61
Q

Oxygen revolution

A
− Oxygen began accumulating in the
atmosphere ~2.7 bya.
− Oceanic photosynthetic prokaryotes
(cyanobacteria) used the sun’s energy
to fix CO2, producing O2 as a byproduct.
− Initially, O2 produced by cyanobacteria
reacted with iron dissolved in oceans,
precipitating to form banded iron
formations
62
Q

Earth’s early prokaryotes evolved in O

2-free conditions and used

A

anaerobic metabolism