C-The Rise of Oxygen Flashcards

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1
Q

What are the 3 other names for the Great Oxidation Event (GOE)?

A

Oxygen Catastrophe
Oxygen Crisis
Oxygen Holocaust

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2
Q

What was the GOE related to?

A

Evolution in an anaerobic world

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3
Q

When did the GOE occur?

A

2.4-2.1 Ga (2400-2100mya)

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4
Q

What happened in the GOE?

A

Biologically induced appearance of O2 in Earth’s atmosphere (know when it happened but controversial as to why)

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5
Q

What are proxies?

A

Indirect evidence

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6
Q

How did we arrive at the GOE Model? (2)

A

Proxies preserved physical characteristics that track changes in variables of interest (eg. oxygen levels)
Many proxies available to examine ancient-ocean atmosphere system

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7
Q

What 4 ways illustrate the GOE?

A

1) Distribution through time of detrital pyrite
2) First occurrence of terrestrial red beds
3) Fossil record of cyanobacteria and stromatolites
4) Banded iron formations

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8
Q

What is the importance of the presence of detrital pyrite?

A

Pyrite altered in presence of oxygen
Generates Ferrous Iron (Fe2+) (Iron Sulphide)
Ferrous Iron is soluble in water and reacts in presence of water and oxygen to form iron hydroxides (rust) insoluble residues (Fe3+)
Colour turns to reds, yellows and oranges
Chemically stable

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9
Q

What is the chemical formula for oxidation (ferrous iron to ferric iron (rust))?

A

4FeO + O2 = 2Fe2O3 (Fe2+ to Fe3+)

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10
Q

How can we track atmospheric oxygen?

A

Based on 1st appearance of continental/terrestrial red beds

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11
Q

When did red beds first appear?

A

Approx 2.3 Ga

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12
Q

What was the only significant source of free oxygen on Earth’s Surface?

A

Cyanobacteria (oxygenic photosynthesis)

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13
Q

What is the geological evidence of cyanobacteria (and therefore oxygen?)?

A

Fossilised?
They build distinctive biosedimentary structures (stromatolites)
Laminated sediments = good preservation potential

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14
Q

What is the problem with using cyanobacteria as a source of info for GOE?

A

Cyanobacteria not the only microbes that form stromatolites

Some stromatolites may be abiogenic (purely physical processes) which means no oxygenic photosynthesis

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15
Q

What is the estimated time frame for the origin of oxygenic photosynthesis?

A

3.8 to 2.35 Ga

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16
Q

What if you assume older ages for oxygenic photosynthesis are correct? Why is oxygenation delayed until 2.4/2.1 Ga?

A

Banded Iron Formations

17
Q

What are Banded Iron Formations?

A

Alternating laminae of chert (type of quartz: silicon dioxide) and iron oxides

18
Q

How are Banded Iron Formations formed?

A

Episodic reaction between ferrous iron (Fe2+ soluble in water)(sourced from hydrothermal systems and released to water) and O2 forms iron oxides that precipitate out onto sea floor. Chert forms at other times.

19
Q

Why are Banded Iron Formations the answer to the delay in oxygenation?

A

Can only release O2 into atmosphere when Ferric iron Fe2+ reservoir is used up (or production of O2 exceeds rate it’s being used up at)

20
Q

In what conditions do red beds form?

A

When oxygen is available

21
Q

What should happen to Banded Iron Formations when more O2 is available?

A

They should stop and red beds should begin to form

22
Q

Where can red beds be found?

A

Huronian Group, Canada

23
Q

What are red beds?

A

Strata of reddish sedimentary rocks that were deposited in hot climates under oxidising conditions

24
Q

What is the key point about lithology and biology?

A

Lithology/ lithosphere is linked to biology/biosphere and it creates a non-uniformitarian geological record