goals for this section 1.explain the feedback mechanism believed to have maintained earth's...
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Goals for this section1. EXPLAIN the feedback mechanism believed to have
maintained Earth's average temperature within the range of liquid water over 100s of millions of years, as the Sun got brighter.
2. Based on albedo, solar radiation, and atmospheric gases, CONSTRUCT logical chains of events that would result in major glaciations or warm periods on Earth.
3. IDENTIFY and EXPLAIN the primary trends and climate events of the past 65 million years based on oxygen isotope data.
Long-Term Climate Evolution: Quiz 5: Nov 30-Dec 1
Final review is Dec 4: Submit Qs on Discussion Board
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RELEVANCE
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4.5
billi
on y
ears
ago
– E
arth
for
ms
2.5-
2.3
billi
on y
ears
ago
–
Hu
ron
ian
gla
ciat
ion
s
800-
600
mill
ion
year
s ag
o –
Sn
ow
bal
l E
arth
WARMWARM
What next? More ICE
SNOWBALLEARTH
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Ice in Australia, which was then at the equator
Evidence for Snowball Earth
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Clicker Question: How could having all continents bundled near the equator help trigger a global glaciation?
A. The continents must have had high mountains where glaciers could form
B. Warm temperatures in the tropics would keep silicate weathering rates high
C.There would be less volcanism if all the continents were in the tropics
D.The poles could freeze more easily if they were water-coveredE. All of the above
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Getting into Snowball Earth
Continents at low latitudes chem weathering CO2 colder
Ice expansion albedo runaway ice-albedo feedback SNOWBALL
Ho
ffma
n &
Sch
rag
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Clicker question: What’s the most likely factor to help Earth escape from the “snowball” scenario? A. Increased burial of organic carbon (e.g. coal
deposits)B. Increased solar outputC. Lower sea levelD. Volcanic activityE. Biological production of oxygen
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Escape from Snowball Earth Tectonics & volcanism CO2
Ho
ffma
n &
Sch
rag
Ice cover prevents chem weathering CO2 even more… greenhouse finally gets strong enough to melt ice ice-albedo feedback
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Clicker question: Once the ice sheets starting melting, more land surface was exposed. What kind of feedback loop between ice and albedo would be triggered as the Earth came out of the Snowball scenario?
A. Positive feedback loopB. Negative feedback loopC. NeitherD. Both
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300-
270
mill
ion
year
s ag
o –
Per
mo
-Car
bo
nif
ero
us
gla
ciat
ion
s
4.5
billi
on y
ears
ago
– E
arth
for
ms
2.5-
2.3
billi
on y
ears
ago
–
Hu
ron
ian
gla
ciat
ion
s
800-
600
mill
ion
year
s ag
o –
Sn
ow
bal
l E
arth
WARMWARM
Warm again, cold again…
WA
RM
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Clicker question: The Permo-Carboniferous glaciations happened when all the continents were together in the supercontinent Pangaea. What effect would the process of assembling a supercontinent have on greenhouse gas concentrations? Greenhouse gases would ______. A. IncreaseB. DecreaseC. Stay the same
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CO
LD!
Decreased atmospheric CO2 as Pangaea formed
Causes of the P-C glaciations
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Causes of the P-C glaciations
Formation of coal deposits
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ICE
COAL DEPOSITS
Ice cover during the P-C glaciations
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Clicker question: Why didn’t the Earth turn into a snowball this time?
A. As the continental ice sheets grew, sea level fell.
B. Glaciers excavated the new swamp deposits.
C. Ice cover on polar continents decreased silicate weathering.
D. Swamps output additional oxygen.
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4.5
billi
on y
ears
ago
– E
arth
for
ms
2.5-
2.3
billi
on y
ears
ago
–
Hu
ron
ian
gla
ciat
ion
s
800-
600
mill
ion
year
s ag
o –
Sn
ow
bal
l E
arth
WARMWARM
Warm again, cold again, warm again…
WA
RM
300-
270
mill
ion
year
s ag
o –
Per
mo
-Car
bo
nif
ero
us
gla
ciat
ion
s
WA
RM
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Pangaea was breaking apartHigher rates of seafloor spreadingIncreased CO2 from volcanoes
Causes of the post-glacial warming
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4.5
billi
on y
ears
ago
– E
arth
for
ms
2.5-
2.3
billi
on y
ears
ago
–
Hu
ron
ian
gla
ciat
ion
s
800-
600
mill
ion
year
s ag
o –
Sn
ow
bal
l E
arth
WARMWARM
Finally, the past 65 million years
WA
RM
300-
270
mill
ion
year
s ag
o –
Per
mo
-Car
bo
nif
ero
us
gla
ciat
ion
s
WA
RM
Last
2.5
mill
ion
year
s –
Ple
isto
cen
e g
laci
atio
ns
XNo more dinos!
70 60 50 40 30 20 10 0 Million years ago
LOW
“T
empe
ratu
re”
HIG
H
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Warming prior to 50 Ma
70 60 50 40 30 20 10 0 Million years ago
LOW
“T
empe
ratu
re”
HIG
H
Subduction of carbon-rich sediments under Asia
Warm
ing
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Cooling after 50 Ma
70 60 50 40 30 20 10 0 Million years ago
LOW
“T
empe
ratu
re”
HIG
H
Collision produced mountains and increased chemical weathering
Long-term cooling
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Benthic Forams: CaCO3
Estimating past temperatures
Ocean
Sediments
Deep ocean temperature
18O
For an ICE-FREE WORLD
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??
H218O H2
16OH216O
Distillation of water Fractionation of oxygen isotopes
H216O (light) & H2
18O (heavy)
H216O
H216O
H216O
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?
Clicker Q: How would the oxygen isotopic composition of the water in an ice sheet compare to the oxygen isotopic composition of ocean water during an ice age?
A. Ice would be heavier than oceanB. Ice would be lighter than oceanC. Ice would be the same as ocean
?
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16O“lighter”
18O“heavier”
H216O
H218O H2
16OH216O
Evidence: Distillation of water Fractionation of oxygen isotopes
16O (light) & 18O (heavy)
Sea level Ice sheet size
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Temperature or 18O in the ocean 18O in the shells
Foraminifera: CaCO3
CaC16O16O16OCaC16O16O18OCaC16O18O18O
lighter
heavier
[ ]18O =18O/16Osample
18O/16Ostandard
-1 * 1000
18O/16O measured in shells
Higher 18O colder water temperatures (and/or more ice)
Lower 18O warmer water temperatures (and/or less ice)
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Estimates of past temperatures
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Who’s driving?
Total “forcing” based on temperature estimates
Changes in solar radiation and albedo
Changes in greenhouse gases
Pleistocene Glaciations
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Causes of the Pleistocene glaciations:
India-Asia collision – decreased greenhouseIce-albedo feedbacks once ice formed on Antarctica
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Summary: Long-term Climate Evolution • The “faint young Sun” paradox can be resolved by higher greenhouse gas concentrations in Earth’s early atmosphere.• Each of the 4 major glacial periods in Earth’s history occurred under different circumstances with different perturbations and feedbacks (construct the logical chains of events for each):
• Huronian – rise of atmospheric oxygen, drawing down methane• Snowball Earth – continents in tropics, high weathering rates, ice-albedo feedbacks• Permo-Carboniferous – mountain building and organic carbon burial• Pleistocene – mountain building (Himalayas), then ice- albedo feedbacks
• Oxygen isotope records from the past 65 My record temperature changes that help resolve the three main climate driving forces in this period – the Sun, albedo, and greenhouse.