Dating Flashcards

(30 cards)

1
Q

ka

A

= 1,000 years

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2
Q

14C-Age

A

= Carbon dated age
* Conventional 14C-Age = non-calibrated

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3
Q

BP

A

= Before Present [Present = 1950]
* Cal BP = Calibrated carbon date before 1950

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4
Q

BC

A

= Before Christ
* BCE = Before Current Era
* Cal BC = Calibrated carbon date in terms of BC/BCE

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5
Q

AD

A

Anno Domini (in the year of the Lord)
* Cal AD = Calibrated carbon date in terms of AD

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6
Q

“Cal”:

A

solely refers to physical objects which are based on 14C-dating; not on, e.g., written sources and coins

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7
Q

Dating methods applicable to the Holocene (7)

A
  1. “Archives” based dating:
  2. Archaeology based contextual dating
  3. Sediment core
  4. Ice core dating
  5. Vulcanic ash dating
  6. Dendrochronology
  7. 14C-dating
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8
Q

“Archives” based dating

A

Museum collection, species can be used to indicate presence in a specific time

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9
Q

Archaeology based contextual dating

A

Animal / plant remains close or in archaeological findings.
- Gives an indication that they are from the same time period

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10
Q

Sediment core

A

older layers contain older remains, relative comparison

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11
Q

Ice core dating

A

Deeper layers contain older remains, relative comparison

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12
Q

Vulcanic ash dating

A

If you know when it erupted, you know everything below has a specific age
-Vulcanic eruptions identified in GISP2 ice core

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13
Q

Dendrochronology

A

Using the tree rings can be used to indicate a time.
-In dry years rings are thinner, and in wet years they are wider
-Wood is used as a building, and it is present in the sediments. By comparing wood from different spots can create a timeline

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14
Q

14C-dating: decay curve for radiocarbon

A

14C is taken up during your living life.
- 14C is not stable, it slowly decays
- 14C-concentration is relatively stable in the atmosphere
- The 14C-concentration is like the atmosphere till death
- After death this 14C starts to decay
- Only possible for organic matter

You need to calibrate the curve, because the concentration of 14C has not always been constant. Tree rings contain a certain 14C-concentration depending on each year.

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15
Q

How does the calibration of radiocarbon work?

A

Calibration of radiocarbon determinations is in principle very simple. If you have a radiocarbon measurement on a sample, you can try to find a tree ring with the same proportion of radiocarbon. Since the calendar age of the tree rings is known, this then tells you the age of your sample.

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16
Q

two factors that complicate the calibration of radiocarbon

A
  1. the measurements on both the tree rings and the samples have a limited precision and so there will be a range of possible calendar years
  2. given the way the atmospheric radiocarbon concentration has varied, there might be several possible ranges
    These effects are most clearly seen by looking at a specific example.

This plot shows how the radiocarbon measurement 3000+-30BP would be calibrated. The left-hand axis shows radiocarbon concentration expressed in years `before present’ and the bottom axis shows calendar years (derived from the tree ring data). The pair of blue curves show the radiocarbon measurements on the tree rings (plus and minus one standard deviation) and the red curve on the left indicates the radiocarbon concentration in the sample. The grey histogram shows possible ages for the sample (the higher the histogram the more likely that age is).

-The results of calibration are often given as an age range. In this case, we might say that we could be 95% sure that the sample comes from between 1375 cal BC and 1129 cal BC

17
Q

On what 4 dimensions can a chronology be based?

A
  1. climate based
  2. Vegetation based
    * Resulting from climate change and plant species responses
    * Different species and compositions at different layers.
  3. Archaeology based
    * Based on material culture, resource use and societal structure
  4. History based
    * Based on historical events
18
Q

What are the climate based factors that you can base your chronology on?

A
  • Glacials <-> Interglacials
  • Stadial <-> Interstadial (cold vs warmer)
  • Within the Holocene interglacial
    -Roman warm period
    -Medieval climate optimum
    -Little ice age
19
Q

What is the traditional 6 period classification in The Netherlands?

A
  1. <12.500 BP = paleolithic
    Nomadic hunters
  2. 12.500- 7.300 BP = Mesolithic
    Seasonal hunter-gatherers
  3. 7.300 - 3.900 BP= Neolithic
    Agriculture
  4. 3.900 - 2.800 BP = bronze age
    Bronze tools
  5. 2.800 BP - 2.000 BP = iron age
    Iron Tools
  6. > 2.000 BP historical period
20
Q

What are the 8 (but actually 9) Holocene subperiods?

A
  1. Sub-Atlantic
    7b. Sub-Boreal
    7a. Atlantic
  2. Later boreal
  3. Early boreal
  4. Pre-Boreal
  5. Younger Dryas
  6. Allerod interstadial
  7. Older dryas
21
Q

Older dryas

A

Zone: I
Date BC: 12.000
Characteristic vegetation: Park Tundra

22
Q

Allerod Interstadial

A

Zone: II
Date BC: 10.000
Characteristic vegetation: Birch with park tundra

23
Q

Younger Dryas

A

Zone: III
Date BC: 8.800
Characteristic vegetation: Park Tundra

24
Q

Pre-Boreal

A

Zone: IV
Date BC: 8.300
Characteristic vegetation: Birch, pine forest

25
Early Boreal
Zone: V Date BC: 7.600 Characteristic vegetation: Hazel, birch, pine
26
later boreal
Zone: VI Date BC: 7.000 Characteristic vegetation: hazel pine, oak, elm, lime
27
Atlantic
Zone: VIIA Date BC: 5.500 Characteristic vegetation: alder, oak, elm, lime (mixed oak forest)
28
sub-boreal
Zone: VIIb Date BC: 3.000 Characteristic vegetation: Alder, oak, lime (elm decline)
29
Sub-atlantic
Zone: 500 Date BC: VIII Characteristic vegetation: Alder, oak, birch
30
What are the 5 historical periods in The Netherlands?
1. Roman period (only south of the Rhine): 1st– 4th century 2. Early Middle Ages: 330 – 950 AD -Merovingian: 447 – 751 AD -Carolingian: 751 – 987 AD 3. High Middle Ages: 950 – 1270 AD 4. Late Middle Ages: 1270 – 1500 AD 5. Modern Times: 16th century - present