Lecture 12:Turmoil in the Greenhouse Flashcards

1
Q

What is the Cenozoic era most commonly recognised for?

A

When aspects of life as they are known today started to emerge

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2
Q

What was the name of the extinction event at the end of the cretaceous period in the Mesozoic? Breakdown the abbreviation.

A

KPG/End Cretaceous extinction event. KPG refers to K (Cretaceous) and PG (Paleogene)

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3
Q

What was the major warming event that took place during the Cenozoic?

A

Palaeocene-Eocene Thermal Maximum (PETM Maximum)

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4
Q

Describe the correlation of carbon dioxide and atmospheric temperature up to the Miocene epoch?

A

there is some correlation between them, however this starts to disappear as the Miocene approaches. the co2 stabilises while temperature shows an increase

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5
Q

What do temperature records of the cenozoic era come from?

A

Foraminifera Shells

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6
Q

Explain how foraminifera shells are a proxy for temperature

A

Their shells are made up of calcium carbonates that include oxygen. The isotopic composition of the oxygen molecules is dependant on temperature. When the climate is colder, the shells are made up more of 18O whereas when the climate is warmer the shells feature an increase in the concentration of 16O.

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7
Q

Why is 18O more present in foraminifera shells during colder periods?

A

18O is harder to evaporate because it is denser, this means during colder periods when there is less thermal energy to evaporate the oxygen molecules, they are unable to be evaporated and so remain in the ocean where they will be the last isotope left to form the foraminifera shells that lie at the bottom of the ocean

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8
Q

Aside from foraminifera shells, how does the oxygen isotopic signature convey temperature?

A

During the colder periods, 16O is the only oxygen isotope that can be evaporated and thus eventually precipitated. When it is precipitated, and because it is cold, it forms ice and so in colder periods the oxygen isotopic signature of ice/glaciers is more concentrated with 16O

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9
Q

What makes the analysis of foraminifera shell formation more complex?

A

During colder periods the foraminifera naturally prefer to use 16O even though there is less of it in the oceans as it has been precipitated on land. So you have two conflicting source of foraminifera formation.

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10
Q

What do foraminifera shells also tell us about the earth system?

A

Changes in the biosphere and the carbon cycle

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11
Q

How do calcium carbonate shells (foraminifera shells) provide information about the carbon cycle?

A

They use carbon in their shell formation, as well as the oxygen, and the isotope which is preferred is 12C. This means if the shells are made up more of 12C then it suggests that there is an abundant supply. The supply of this isotope increases with temperature so when there is more of it present in the record we can say that it was a warmer period (e.g. PETM)

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12
Q

What event demonstrated how 12C increased with temperature?

A

Paleocene-Eocene Thermal Maximum (PETM)

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13
Q

What transition occurred in the animal ecology following the KPG extinction?

A

During the cretaceous, the dinosaurs were present and when they became extinct, the environmental niches left behind were replaced with mammals

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14
Q

What was the rate of increase in mammal mass following the KPG extinction?

A

They grew at a linear rate from 150g to 1kg on average across 1myr

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15
Q

Who claimed that the increase in mammal size following the KPG extinction was a result of increased oxygen?

A

Falkowski et al. (2005)

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16
Q

Why was Falkowski et al.s theory proved wrong?

A

Oxygen levels were already quite high and were higher than today - for the transition from dinosaurs to mammals Tim lenton believes that there must have been a reduction in oxygen levels

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17
Q

What does Tim Lenton believe the reason was for the transition following the KPG event?

A

A new environmental opportunity arose

18
Q

What was the state of the continents during the PETM?

A

They were starting to be distributed across the world in to positions that are more recognisable today

19
Q

What happened to the temperature of the earth during/following the PETM? Why was this?

A

Climate warmed by around 5 degrees Celsius in 20kyr which coincided with a rise in carbon dioxide

20
Q

How do ocean floor cores provide evidence of atmospheric carbon content?

A

Colour - when they are lighter and whiter the carbon content is not as high but when they appear darker there is more carbon

21
Q

Why do the ocean cores change colour in response to atmospheric carbon?

A

the lighter colours derive from a greater presence of calcium carbonates in soil, but they become darker because more carbon increases acidity of oceans which promotes dissolution of the carbonates meaning the whiteness is dissolved

22
Q

How can we visually identify the PETM from the ocean cores?

A

A sudden transition in colour from whiter colours to darker colours

23
Q

How long does it take for the calcium carbon content in ocean floor cores to reappear and why?

A

A long time because ~2000Gt of carbon needs to be deposited in sediments before the calcium carbonates can recover

24
Q

What shift occurred in the ocean floor record around 40Ka?

A

Negative shift in 13C i.e. it decreased in concentration because 12C experienced a massive injection

25
Q

Why was there a massive negative shift in the 13C isotope around 40Ka?

A

complex process carried out by photosynthesis, methanotrophs and methanogens in which they prefer to lock up 13C isotopes and produce 12C-rich methane in its place

26
Q

What is the volcanic trigger hypothesis for why the methane concentration (comprised mostly of 12C) in the ocean floor started to increase and why the PETM happened?

A

At time of PETM, MAR opening led to basalt flows that cooked sedimentary rocks on top of crust. this opened the sedimentary rocks up which allowed organic carbon and methane to escape to the atmosphere leading to an increase in the GHG layer and the temperature of the earth.

27
Q

What evidence is there for the increase in atmospheric methane 40Ka being a result of volcanic trigger?

A

Rocks found in NW Canada, Ireland and Scotland were dated and coincided with the PETM event.

28
Q

Of the carbon that did not escape the sedimentary rock record, what purpose does it serve today?

A

It formed the fossil fuels that are drilled from the North Sea today

29
Q

What is the second way the volcanic trigger hypothesis is thought to have caused the PETM?

A

Escape of mantle from MAR melted the methane hydrates on the bottom of the ocean floor, destabilising them which meant methane escaped to the atmosphere

30
Q

What possible feedback would have increased the destabilisation of the methane hydrates? What is the limitation of this feedback?

A

increased methane to the atmosphere would increase then GHG which would have increased ocean warming further promoting melting. However, it takes thousands of years for this feedback to make a significant impact because heat diffusion down to ocean depths is so slow

31
Q

What are methane hydrates? How are they formed? How do they become unstable?

A

Hydrate lattices that have methane inside which is extremely flammable. Formed under high pressure and cold conditions. They become unstable when melted as the temperature increases and in turn the pressure decreases.

32
Q

What are therefore the various explanations for increased methane concentration to increase?

A

Biosphere - photosynthesis, methanotrophs, methanogens
Volcanic Trigger - release from sedimentary rocks
Volcanic trigger - Methane hydrates
Champagne cork effect

33
Q

What is the champagne cork effect?

A

Occurs at slope between ocean crust and continental crust. If some sediments are made unstable then this can cause a tumbling of other sediments that are positioned on top which releases more and more hydrates

34
Q

How many carbons were released to the atmosphere from the various sources?

A

Thousands of billions

35
Q

What can happen to methane as it enters the atmosphere?

A

It can react with oxygen to increase the GHG layer more

36
Q

How long can it take for carbon to be removed from the atmosphere?

A

Thousands of years

37
Q

What will happen to the oceans as a result of increased carbon in the atmosphere?

A

The oceans will increase in acidity.

38
Q

What is the main way that carbon is removed from the atmosphere? How long can it take for the climate to cool down through this process?

A

Silicate weathering - it can take >100kyr

39
Q

With knowledge of how long it can take for the climate to cool down to before levels via silicate weathering what does it highlight?

A

How prolonged the impact of anthropogenically-induced climate change could be

40
Q

What other events occurred after the PETM?

A

Similar increases and reductions in the atmospheric carbon that get smaller and smaller in significance over time

41
Q

How much carbon is stored within methane hydrates that are present on the ocean floor today? Put this in to context

A

1000Gt - more stored than what is in the amount of oil we have today

42
Q

What lesson can we take from the PETM?

A

There was an expected increase of 5 degrees Celsius which took over hundreds of thousands of years to decline. We should therefore avoid increasing carbon in the atmosphere to dangerous levels which we are more than close to doing