greenhouse and icehouse Flashcards
what is the cenozoic?
the greatest geologic era divided into periods
what periods is the cenoxoic divided into?
paleogene, neogene, quaternary
what are the periods of the cenozoic then divided into?
epochs
- paleocene and eocene
what is Foraminifera?
pin head size single celled protozoa with a shell made of CaCO3
what is the ratio of oxygen isotope in their shells sensitive to?
temp and ice vol
when was the paleocene?
65-55Ma
when was the Eocene?
53-34 Ma
what indicates rapid acidification of the ocean?
dissolution of carbonate sediments
what is the volcanic trigger hyp?
- 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
what are methane hydrates?
- gas molecules trapped inside a frozen water lattice
where do methane hydrates form?
in the pore spaces in sediments and occur in a layer of ocean sediments stabilise day high pressure and cold temps
how can methane hydrates be stabilised?
- increasing temp of overlying water
- depressurisation by lowering sl
- slope failure
how long does it take for the ocean to be replenished with alkalinity from silicate weathering?
> 100 kyr
hyp for the Paleocene-Eocene Thermal Maximum
- warming of intermediate depth ocean waters destabilised methane hydrate
- outgassing of methane added to warming causing more methane to be released
+ve feedback
what is the total of CH4 released during PETM?
1500 GtC
what can you learn from the PETM?
- 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
when was the interval of extreme warmth?
55 Ma
who stated the Himalayan uplift hyp?
Raymo and Ruddiman (1992)
what was the Himalayan uplift hyp?
- 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
problems with the Himalayan hyp
- global erosion has been constant for at least the past 10 mar, despite mountain building
when was the miocene?
23-5.3 Ma
what stabilised the miocene?
- 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
what are the 3 stages of grassland spread?
- eocene 33 Ma desert grasslands
- early miocene 17 Ma ungulates, horse
- late miocene 7 Ma C4 grasses
when was the Pliocene?
5.3-2.58 Ma
when was hominia?
6 Ma
where is the origin of hominia?
great Rift Valley