Week 13 Flashcards

1
Q

Ways to build chronology (decreasing resolution)

A

LAYERS

  • trees
  • stalagmites
  • ice cores
  • Lake sediment (n.b. Datum)

RADIOMETRIC DATING

  • C
  • U-Th
  • K-At

COSMOGENIC NUCLIDES

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2
Q

Living part of tree =

A

Cambium

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3
Q

How is radiocarbon produced?

A

Cosmic ray-derives neutrons bombard N atoms

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4
Q

What affects radiocarbon?

A

Solar wind = deflects cosmic rays
Which increases with sunspots
So active sun = less radiocarbon

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5
Q

The cycle of radiocarbon

A

Plants <> atmosphere
Animals <> food
Die = 14C beta decays to 14N

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6
Q

Problems with radiocarbon

A

HALF LIFE

  • 5,700 years
  • Max dateable 50,000 years

CALIBRATION CURVE

  • b/c varies with solar activity (can’t solve equation)
  • slow changes in geomagnetic field = gradual increase in 14C production rate
RESERVOIR EFFECTS
- corals/stalagmites
- add dead C with 14C = appears older
- dead anthropogenic C (dilutes 14C)
“Corrected for reservoir of x years, ... calendar years”

BOMB SPIKE
Partial Test Band Treaty 10/10/1963

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7
Q

Before present =

A

Before 1950

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8
Q

Secular equilibrium =

A

Activity ratios of any isotopes in decay chain = 1

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9
Q

Ancient samples

Youngest

A

More than 500ka

Furthest from secular equilibrium (1)

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10
Q

U-Th principles

A

Th is insoluble
U6+ is soluble

Stalagmites/corals/shells contain no Th = daughter deficiency dating

Radioactive daughter = use activity

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11
Q

Positives of U-Th

A

Date carbonates up to 500,000 years B.P.

In calendar years without calibration curve

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12
Q

Problems with U-Th

A
Detrital Th (232Th) May contaminate
230/232 ratio
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13
Q

Elements for Cosmogenic include surface exposure dating

A

10Be

26Al

26Cl

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14
Q

10Be

A

1.5 am

O/mg/si/fe spallation

Quartz/olivine/magnetite

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15
Q

26Al

A

0.7ma

Si/Al/Fe spallation

Quartz/olivine

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16
Q

36Cl

A

0.3ma

Ca/K spallation
35Cl neutron capture

Whole rock

17
Q

Problems with Cosmogenic

A

Different surfaces bombarded different rates

Erratics

Shielded by ice