Past Climate Flashcards

(34 cards)

1
Q

What data can we use to determine past climate in the quaternary?

A

Oxygen isotopes
(Ice cores)

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2
Q

How can oxygen isotopes help determine past climate?

A

Comparison of O16 and O18 (when in ice, it used to be water)
- O16 is lighter so more O16 will evaporate
- O18 is heavier so more O18 will condense
- the amount of O18 will depleted as the air moves northwards, as it gets colder
- in colder eras, even less O18 will evaporate from the equator, and then will fall more quickly. Very little will make it to the poles in a glacial

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3
Q

What physical evidence can be used to determine the oxygen isotopes ratio?

A

Ice cores
Foraminifera (forams)

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4
Q

How can ice cores be used to determine the oxygen isotopes ratio?

A
  • banded: lighter = winter, darker = summer
  • the bands vary in width due to: compaction, different levels of snowfall, some years more melting/snow blown away
  • there are very small fluctuations/changes in the O18 concentration going back in time, showing different temperatures and how they changed
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5
Q

How can forams be used to determine the oxygen isotopes ratio?

A

Minute marine shelled creatures
- shells made of CaCO3 (CONTAINS OXYGEN)
- shells preserve 18:16O ratio so keep a record of the climate going back millions of years

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6
Q

What paleoclimatic factors can ice cores indicate?

A
  • Oxygen isotope ratio
  • atmospheric gas concentration in bubbles (CO2, CH4)
  • volcanic eruptions in ash layers that can be dated radiometrically

(can go back 600,000 years)

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7
Q

What other factors often correlate with oxygen isotope ratio?

A

CO2 concentration
Temperature

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8
Q

How do warmer and cooler climates influence the 18O concentrations in
a) Ice cores
b) Sea

A

a) WARMER = more 18O
COOLER = less 18O

b) WARMER = less 18O
COOLER = more 18O

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9
Q

How do places at the same latitude compare with climate?

A

the climate differs

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10
Q

What factors can we use to find out Quaternary climate in Britain?

A
  1. DEPOSITS
  2. STRIATIONS AND ERRATICS
  3. POLLEN
  4. BEETLES (COLEOPTERA)
  5. TREE RINGS (DENDROCHRONOLOGY)
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11
Q

What kinds of deposits can be used to find out Quaternary climate in Britain?

A
  • glacial
  • periglacial
  • fluvio-glacial
  • interglacial
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12
Q

How can striations and erratics be used to find out Quaternary climate in Britain?

A
  • orientation and distance
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13
Q

How can pollen be used to find out Quaternary climate in Britain?

A
  • very abundant
  • super readily preserved
  • tells us the plants growing
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14
Q

How can beetles be used to find out Quaternary climate in Britain?

A
  • more mobile than trees and therefore pollen
  • rapidly responds to a change in climate
  • hard parts are readily preserved
  • some live in a very narrow temperature range

e.g. beetles in the fossil record found in the UK are now found in Northern Norway

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15
Q

How can tree rings be used to find out Quaternary climate in Britain?

A
  • each ring is a new year
  • Fat = good. Lots of precipitation, they grow faster
  • Thin = poor, less precipitation
  • scientists build tree ring chronologies by starting with living progressively older specimens (including archaeological wood) whose outer rings overlap with the inner rings of more recent specimens
  • can put together to make up an history
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16
Q

How would you describe deciduous forest?

A
  • warm and temperate summers
  • nutrient rich soils
  • has seasons so trees drop leaves in colder winter
17
Q

How would you describe boreal forest?

A
  • cold and frigid temperatures year round
  • dry winters
  • acidic, nutrient poor soils
18
Q

How would you describe tundra?

A
  • cold region with permafrost underneath
  • frost moulded landscape
  • treeless
19
Q

What is ecological succession?

A

the change in an ecological community over time, from a relativelysparse landscape to a stable community of several different plants and animals

20
Q

What is the process of ecological succession?

A
  1. Bare rock (glacial retreat?). No soil, no plants, the ground is exposed to weather with no shade
  2. Pioneer community - the first to colonise the land. They pave the way for the next stage of organisms
  3. Each stage results in the creation of more soil, bigger plants, more shade
  4. Succession moves through a series of successional stages, called seres
  5. Ultimately it ends up with a climatic climax
  6. Climatic climax in the climax community for that particular climate. In the UK this is often oak woodland
21
Q

Describe the vegetation structure during succession

How quickly does this happen?

A
  1. Bare rock
  2. Lichens
  3. Mosses
  4. Grasses
  5. Herbaceous plants
  6. Small to large shrubs
  7. Large shrubs
  8. Established trees

Happens over hundreds of years

22
Q

What is the name for ecological succession that started on a rock?

23
Q

How many stages are in the Lithosere?

24
Q

Describe the stages in the Lithosere

A
  1. A bare exposed rock site colonised by bacteria and then lichens
    - they are pioneer species able to tolerate the lack of soils and water and widely fluctuating temps
  2. Decay of lichens enables moss growth. Mosses retain water. Death of lichens and growth of mosses assist weathering and formation of organic matter that can be exploited by more complex plants
  3. Thus, grasses, ferns and small herbs colonise e.g. in water-retaining pockets
    - their eventual death and decay further adds to the organic matter, increasing nutrient levels and water availability
  4. Small shrubs e.g. gorse, bramble and broom colonise. they shade out some of the smaller grass species
  5. Pioneer trees such as birch, hawthorn and N-fixing Alder colonise and out-compete smaller species
  6. Larger trees such as ash colonise and out-compete smaller species. Slower growing deciduous trees such as oak colonise and shade out smaller species
    - a stable, climax community forms such as a temperature deciduous woodland
25
What are the two types of sea level change?
Isostatic Eustatic
26
What is isostasis?
the theory that the Earth's crust is near to a state of equilibrium without any tendency to move up or down, and that large blocks of the crust behave like blocks floating in liquid
27
What is isostatic adjustment? Give an example
the vertical movement of the Earth's crust resulting from a lack of isostatic equilibrium e.g. the rise of the land after the removal of the weight of an ice sheet
28
Describe the process of isostatic sea level change Is it slow or fast?
- lithosphere is floating on the asthenosphere - when ice builds up it causes the lithosphere to sink - the mantle underneath oozes sideways making a bulge - where the ice is thickest, the most sinking occurs - isostatic sea level change is the levels of sea changing because land is sinking or rising, with the mantle flowing outwards or back This is a very slow process
29
What is eustatic sea level rise?
- when there is ice on the land there will be less water in the sea - this lowers the global sea levels - this happens quickly
30
What is the evidence for seal level fall?
Raised beaches - beaches, cliffs, sea caves above high tide - they must have been at sea level for the cliffs and caves to have formed
31
What is the evidence for sea level fall?
Fjord Ria Drowned forest
32
What is a fjord?
- a long, narrow body of water that reaches far inland - a flooded glacial through with steep walls of rock one either side - deepest inland where the glacial force is strongest - when the ice melted, the land started to rise isostatically, which caused sea level fall. However the melting caused eustatic sea level rise - if the rise is greater than the fall, you end up with fjords and drowned valleys
33
What is a ria?
- a coastal inlet formed by the partial submergence of an unglaciated river valley - it is a drowned river valley that remains open to the sea - they are formed because of sea level rise - these tend to be shallower than fjords as there hasn't been glacial action deepening them - they are also more winding and have more tributaries
34