origin of life Flashcards

1
Q

Bubble theories

A

Certain molecules spontaneously form bubbles.
would serve to shield hydrophobic regions from contact with water
supports ocean’s edge scenario
Alexander Oparin’s Bubble Hypothesis (1924)
Primary abiogenesis - protobionts allowed chemical complexity to develop
Many different bubble scenarios have been proposed.
no agreement about composition or how the process occurred

In the laboratory, droplets of abiotically produced organic compounds, called liposomes, form when lipids are added with proteinoids and phosphate.
The lipids form a molecular bilayer at the droplet surface, much like the lipid bilayer of a membrane.
Undergo osmotic responses
Store energy as a membrane potential
(voltage cross the surface).

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2
Q

Protobionts:

A

aggregates of abiotically produced molecules capable of isolating an internal environment different from its surroundings and showing properties of living cells.
Protobionts that formed in the “organic soup” would not have possessed refined enzymes, the products of inherited instructions.
However, some molecules produced
abiotically do have weak catalytic capacities.
There could well have been protobionts
that had a rudimentary metabolism that
allowed them to modify substances they
took in across their membranes.

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3
Q

Hereditary information in Protobionts

A

RNA genes and their polypeptide products are packaged within a membrane, thus the protobionts could have evolved as units.

Molecular cooperation could be refined because favorable components were concentrated together, rather than spread throughout the surroundings.

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4
Q

Archaebacteria

A

Extreme-condition prokaryotes

  • Lack peptidoglycan in cell walls
  • methanogens
  • extreme halophiles
  • extreme thermophiles
  • Thought to have split from Bacteria 2 bya.
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5
Q

Bacteria

A
Second major group of prokaryotes
Strong cell walls
Simpler gene structure
Contains most modern prokaryotes
includes photosynthetic bacteria
cyanobacteria
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6
Q

-Stromatolites-fossilized bacterial mats

A

Photosynthetic
Responsible of Earth’s atmospheric change
Formed in hypersaline areas where other organisms can not survive.
Modern Stromatolites Shark Bay Australia

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7
Q

First Eukaryotic Cells

A

Eukaryotes probably arose about 1.5 bya.
Internal membrane-bound structures such as mitochondria and chloroplasts are thought to have evolved via endosymbiosis.
Energy-producing bacteria were engulfed by larger bacteria.
beneficial symbiotic relationship

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8
Q

Endosymbiosis

A

Multiple endosymbiotic events
Responsible of the formation of various unicellular organisms
Green algae lineage
Red algae lineage

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9
Q

endosymbiosis theory

A

The theory holds that mitochondria, plastids such as chloroplasts, and possibly other organelles of eukaryotic cells represent formerly free-living prokaryotes taken one inside the other in endosymbiosis.

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10
Q

Which are the habitable words in our solar system?

A

Moon and Mercury are largely dry.
Venus too hot for liquid water.
Jovian planets (Jupiter and Saturn) are gaseous.
This leaves Mars and a few of the moons orbiting the Jovian planets, notably Europa.

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11
Q

What do we mean by habitable?

A
  • earth like ( oxygen, water, dry land, temperature range)
  • microbial life could survive a more extreme set of conditions
  • common basic requirements are water and stable conditions
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12
Q

What stabilises the climate?

A
  • size- a long term heat source
  • stellar evolution: incoming solar energy
  • meteor impact rate: could result in climate change
  • presence of a large natural satalitte prevents large swings in obliquity
  • oceans regulate global temperatures
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13
Q

why has earth got complex life on it

A

abundant liquid water,

environmental conditions that maintain liquid water

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14
Q

liquid water

A

influenced by temperature and atmospheric pressure

a simple requirement for identifying habitable planets.

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15
Q

where do planets with a temperature range that could support liquid water orbit?

A

the “habitable zone”

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16
Q

How do stars affect the habitable zone

A

so different stars have different luminosities (energy), brighter stars have habitable zones farther out. Stars have different luminosities throughout their lifetime.
Other factors to consider:
Albedo moves HZ inwards when the atmosphere moves the HZ outwards
Carbon dioxide stabilizes temperatures

17
Q

Carbon in temperature regulation

A

carbon dioxide acs as a thermostat as it expands to the habitable zone for earth like planets, it reduces extreme temperatures.

18
Q

what are sources of carbon?

A
  • volcanic outgassing
  • decarbonation
  • organic carbon
19
Q

What are carbon sinks

A
  • Calcium carbonate formation

- Photosynthesis

20
Q

Characteristics of habitable planet:

A

Size of planet
- Internal heat (comet impact & radiation)
- Sustain liquid water (geothermal or tidal)
Stable luminous stars necessary
- Sufficiently long lifetime for life to evolve
- Large enough so planets are not tidally lock
Galactic habitability
- Area of high metals
- Outer region of galaxy (low star density and radiation)

21
Q

Are there any exceptions to the habitable zone?

A

Yes, if there are sources of energy other than a star to keep a planet (or moon) warm.
Possible energy sources:

Radioactivity (metal composition)
Rotation and gravitation (tides by natural satellites)

22
Q

Life on Mars?

A

Early Mars:
Evidence of significant amounts of flowing liquid.
Warmer temperatures:
Heat from interior would have been higher
Warm climate from greenhouse gases or CO2 clouds
Current Mars:
Not evidence of life
Erosion may be due to underground liquid water
Carbon cycle not as active as on Earth

23
Q

life on mars pt 2

A

Percival Lowell (1855-1916) thought he saw canals on Mars.
Nevertheless, we have good evidence the liquid water once flowed on the Martian surface.
Today it contains subsurface ice which could be heated to form areas of liquid water underground.

24
Q

EVIDENCE OF WATER ON MARS?

A

Erosion could have been created by water flooding from lakes

Best evidence to date of abundant water in Mars

25
Q

NEGATIVE EVIDENCE FOR LIFE ON MARS:

A

The Viking missions took soil samples and looked for chemical changes that could be attributed to biological processes.
3 experiments suggested that life may have been present, but also ordinary chemical reactions could have caused the same results.
A fourth experiment found little organic material, the opposite of what one would expect if life were present.

26
Q

METHANE ON MARS

A

The Mars Express orbiter detected methane gas.
Methane should disappear within a few centuries due to chemical reactions.
So, something is supplying Mars with methane.
It could come from comet impacts, volcanoes, or life.
Volcanism seems to be the most likely candidate.

27
Q

Martian meteorites

A

One meteorite which landed in Antarctica 13,000 years ago and found in 1984 was clearly of Martian origin.
Inside the meteorite were complex organic materials and structures which looked like nanobacteria , very small bacteria which have been discovered on Earth.
These structures can also be made by chemical and geological means.
Contamination from being on the Earth may also explain the presence of organic materials

28
Q

life on europa?

A

Europa has enough tidal heating to possibly form a subsurface ocean underneath its icy crust.
Life there could form like the “black smokers” on Earth.
Larger life forms could exist in the vast oceans, but energy sources are limited thus limiting the size of any life there.
Hubble telescope detected oxygen in Europa
Oxygen content on the surface is low but moderate under the ice core.
May be sufficient to support life

29
Q

Europa

A

Liquid water oceans present on Jupiter’s moon Europa
Water in liquid form under ice cores
Perfect environment for life

30
Q

Liquid water oceans present on Jupiter’s moon Europa
Water in liquid form under ice cores
Perfect environment for life

A

Life on Ganymede, Callisto and Titan
Ganymede and Callisto might have subsurface oceans, but their internal heat is small and liquid water would not be very abundant.
Titan has no native liquid water, but an abundance of organic materials.
Could life evolve from the lakes of methane?
Water might be brought in from comets, but this would eventually freeze.

31
Q

what substitutes phosphorous for arsenate

A

Halomonadacea bacteria GFAJ-1, isolated from Mono Lake, substitutes arsenic for phosphorus to sustain its growth.
Nucleic acid and proteins of GFAJ-1 contain arsenate instead of phosphate.