greenhouse and icehouse Flashcards

1
Q

what is the cenozoic?

A

the greatest geologic era divided into periods

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2
Q

what periods is the cenoxoic divided into?

A

paleogene, neogene, quaternary

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3
Q

what are the periods of the cenozoic then divided into?

A

epochs

- paleocene and eocene

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4
Q

what is Foraminifera?

A

pin head size single celled protozoa with a shell made of CaCO3

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5
Q

what is the ratio of oxygen isotope in their shells sensitive to?

A

temp and ice vol

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6
Q

when was the paleocene?

A

65-55Ma

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7
Q

when was the Eocene?

A

53-34 Ma

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8
Q

what indicates rapid acidification of the ocean?

A

dissolution of carbonate sediments

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9
Q

what is the volcanic trigger hyp?

A
  • a large flood basalt intrusion from Iceland began to open the N Atlantic 56.1 Ma with the splitting of continents 55 Ma
  • 5-10 mil km^3 of basalts deposited in 1 myr intruded into fossil-fuel rich sediments
  • this released CO2 and the thermogenic methane
  • thermogenic methane is less 13C depleted than biogenic methane hence more of it would be required to explain the 13C excursion
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10
Q

what are methane hydrates?

A
  • gas molecules trapped inside a frozen water lattice
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11
Q

where do methane hydrates form?

A

in the pore spaces in sediments and occur in a layer of ocean sediments stabilise day high pressure and cold temps

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12
Q

how can methane hydrates be stabilised?

A
  • increasing temp of overlying water
  • depressurisation by lowering sl
  • slope failure
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13
Q

how long does it take for the ocean to be replenished with alkalinity from silicate weathering?

A

> 100 kyr

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14
Q

hyp for the Paleocene-Eocene Thermal Maximum

A
  • warming of intermediate depth ocean waters destabilised methane hydrate
  • outgassing of methane added to warming causing more methane to be released
    +ve feedback
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15
Q

what is the total of CH4 released during PETM?

A

1500 GtC

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16
Q

what can you learn from the PETM?

A
  • the amount of C released at the PETM is comparable to known fuel reserves today and gave at least 5C long-term warming
  • it will take at least 100 Ayr for the carbon cycle and climate to recover
17
Q

when was the interval of extreme warmth?

A

55 Ma

18
Q

who stated the Himalayan uplift hyp?

A

Raymo and Ruddiman (1992)

19
Q

what was the Himalayan uplift hyp?

A
  • uplift of the Himalayas caused increased weathering rates
  • this decreased atmospheric CO2 thus cooling the planet
  • should have caused a -ve feedback response
  • lower CO2 and temp reduce silicate weathering until it again matches degassing
20
Q

problems with the Himalayan hyp

A
  • global erosion has been constant for at least the past 10 mar, despite mountain building
21
Q

when was the miocene?

A

23-5.3 Ma

22
Q

what stabilised the miocene?

A
  • at 200-250 ppm, CO2 during the miocene upland veg was near CO2 starvation
  • this limited the effect go plants on weathering, holding CO2 stable
23
Q

what are the 3 stages of grassland spread?

A
  • eocene 33 Ma desert grasslands
  • early miocene 17 Ma ungulates, horse
  • late miocene 7 Ma C4 grasses
24
Q

when was the Pliocene?

A

5.3-2.58 Ma

25
Q

when was hominia?

A

6 Ma

26
Q

where is the origin of hominia?

A

great Rift Valley