Biomolecules and Dating Methods Flashcards

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Ancestry, genetics and migration in Britain • Based on genetics of ~2000 Britons with grandparents within 80 km • 17 geographical groups – Flow of Anglo Saxon genes – Little trace of Viking

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2
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Eulau, Germany • Late Neolithic (Corded Ware culture): 2700- 22/2000 BC Family buried together Violence: projectile points, perimortem fractures, defence injuries to forearms

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3
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Dendrochronology Master Chronology - can be dated back to 11kya. West European master chronology of oaks. Used to calibrate radiocarbon dates but can also be used for direct dating.

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4
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Bronze Age tomb from Qatna, Syria. Patches of purple dye made from sea creatures. Very rare to find preserved dye- showed what colour clothes and remnents of them would have been. Found via Analysis of lipid residues • Do not dissolve easily in water (hydrophobic).

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5
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Oldest door in Britain • Westminster Abbey Chapter House • Dendro dated to AD 924 - 1030

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6
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Middle Awash Herto AMH 154-160ky by Ar-Ar (Clark et al. 2003; Nature) ‘oldest modern human’

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7
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DNA -Deoxyribonucleic acid. Mostly in cell nucleus, some in mitochondria • Very specific • Degrades easily; survives best in cold and dry conditions • Can be subject to contamination!!

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8
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Our history of milk drinking. Lactase persistence allele ( 13910*T) frequency is less in Southern Europe so more people are lactose intolerant there.

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9
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Ancient DNA • Preservation • Contamination • Expense • Mitochondrial DNA (from mother only) • Nuclear DNA (from all ancestors)

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10
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Maize starch residues from Peru • Associated with lithics and coprolites from Late Archaic period (3000 – 1800 BC)

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11
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Proteins

  • In hair (keratin), bone (collagen), skin, dentine, fingernails …
  • Contains: – Carbon – Hydrogen – Oxygen – Nitrogen
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12
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Carbohydrates • Simple (monosaccharides) and complex polysaccharide) sugars • Very soluble in water • Under-represented bioarchaeologically • High in foods such as sugars and cereals

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13
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Bones • The organic component of bone (approx. 20 %), made up of proteins (carbon nitrogen, oxygen, hydrogen …) • (The mineral component is hydroxy apatite). Diet can be seen in bone collagen through carbon and nitrogen isotope make up.

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14
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Plants use C3 in cold conditions. Plants use C4 for photosysnthesis in hot conditions. C3 filters out 13C a lot, and C4 filters out 13C a bit- they retain 13C as they need to avoid warerloss. Tissue will represent what kind of plants you eat due to the presence of 13C.

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15
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Radiocarbon dating

  • Used for dating carbon-containing materials, e.g. bone collagen, wood, seeds, hair, shell, leather
  • Destructive – mgs to grams required
  • Only calibrated back to ca. 20 kya
  • Maximum limit of 40 – 60,000 years
  • A radioactive isotope of carbon ( 14C) is formed in the upper atmosphere
  • Incorporated into plants (and hence foodchain) by photosynthesis
  • While an organism (e.g. plant) is alive, 14C is constantly being replenished; however once it dies, the amount of 14C decreases
  • Time for half of the 14C atoms left to decay Half life of 14C is 5,730 yrs Originally thought to be 5,568 yrs; for historical reasons this is still used to calculate the radiocarbon date
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16
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Uranium-thorium dating is a radiometric dating technique commonly used to determine the age of calcium carbonate materials such as coral.

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A varve is an annual layer of sediment or sedimentary rock. Similar to dendrochronology, varve layers can be counted and a mastetr chronology created back to 52,800 years.

18
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Calibration curve for radiocarbon dates using dendrochronology, u-series dated corals, and varves.

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Dendrochronology

  • Dating limit currently approx. 10kya
  • Seasonal growth in wood
  • Counting rings gives age (of tree! Not date)
  • Width of annual rings in wood varies according to climate, local conditions Dating wood (often very precisely) by matching patterns of annual growth

Ring porous (image) = oak, ash, elm or diffuse porous = birch, maple, cherry

20
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Outer ring = sapwood - required for accurate felling date

Inner core = heartwood

Outer edge = bark

21
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Potassium-Argon and Argon-Argon dating

  • 40K decays to 40Ar (half life 1250 million years)
  • Argon is a gas: when a rock is molten (e.g. volcanic eruption) all argon should be released. When solidifies, 40Ar is trapped in rock as 40K decays
  • Therefore by measuring the accumulation of 40Ar in a volcanic layer, can date time passed since the eruption - can date artefacts between layers of volcanic ash.

Need to measure current abundance of parent and daughter isotopes, either: 40K and 40Ar (K-Ar dating) or 39Ar and 40Ar (Argon-Argon dating)

22
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U series dating

• Radioactive isotopes of Uranium decay to various radiogenic (and insoluble) isotopes, e.g. thorium, protactinium

Dating of stalagmites and flowstones

• The daughter isotopes (Th, Pa) will only start to accumulate once the carbonates have precipitated; therefore can measure relative amounts and date when flowstone formed

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Thermo- and optically stimulated luminescence dating

Measuring luminescence which builds up in crystal lattices due to exposure to background radiation

This luminescence is released on heating/light; then it builds up again

Date: how long since last heating/light

Materials: fired pottery, burnt flints, aeolian sediments

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Analysis of lipid residues

  • Do not dissolve easily in water (hydrophobic)
  • Waxes
  • Oils
  • Fats
  • Sterols