Lecture 3- Milankovitch cycles etc. Flashcards

1
Q

Sapropels

A

Organic rich black muds- layers of high carbon concentrations

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2
Q

Sapropels- low salinity lids

A

Prevent oxygen rich water being formed as low salinity fresh water sits on the surface

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3
Q

Sapropels and precession

A

Sapropels sit on precession spikes (strong indication insolation and rainfall at source of the Nile)

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4
Q

Urbain Leverrier

A

Applied Newton’s gravitational laws to orbits/masses of planets

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5
Q

Eccentricity change- 100,000 years

A

1-6%

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6
Q

Obliquity change (tilt)- 41,000 years

A

24.5 to 22.1 degrees

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7
Q

When tilt is decreased…

A

Polar regions receive less sunlight

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8
Q

When tilt is increased…

A

Polar regions receive more sunlight…

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9
Q

Precession of the equinoxes

A

Caused by the ‘wobble’ of the earth’s axis

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10
Q

Cause of decrease in summer radiation

A

Caused by a decrease in axial tilt

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11
Q

Tilt cycle (41,000)

A

Predominates at poles, gets smaller at equator

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12
Q

Precession (22,000)

A

Is small at poles, larger at equator

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13
Q

Eccentricity cycle (100,000)

A

Amount of energy change involved in the eccentricity
cycle is small

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14
Q

Problem with dating glaciers

A

Morraine of previous glaciers are bulldozed- only evidence of the most recent glacier

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15
Q

Carbonate ooze (depth)

A

<4000m

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16
Q

2 types of info found from carbonate ooze:

A
  1. Species distribution of foraminifera reflects temperature and
    nutrients
  2. Shells lock isotopic (C & O) concentrations from water
    of formation
17
Q

Carbonate compensation depth

A

More carbonate can be dissolved in Atlantic ocean as CCD is deeper

18
Q

Why is CCD deeper in Atlantic

A

Organic matter rains down and oxidised carbonates move down the water column and make the water more acidic

19
Q

Atlantic cores

A

Faster sedimentation: more resolution

20
Q

Assumptions made when tuning

A
  • An orbital signal is present
  • Time lag
  • Which component of orbital change the
    record responds to
  • Continuous and complete record
21
Q

Issues with using magnetic susceptibility for global changes

A

Only useful for regional changes

22
Q

The further you go back in time

A

The more difficult it is to use ice sheet models as your main measure

23
Q

What is the relationship between obliquity and glaciation?

A

Higher obliquity tends to reduce glaciation, while lower obliquity tends to favour glacial growth, as it results in milder summer temperatures and more ice accumulation over time.