ka
= 1,000 years
14C-Age
= Carbon dated age
* Conventional 14C-Age = non-calibrated
BP
= Before Present [Present = 1950]
* Cal BP = Calibrated carbon date before 1950
BC
= Before Christ
* BCE = Before Current Era
* Cal BC = Calibrated carbon date in terms of BC/BCE
AD
Anno Domini (in the year of the Lord)
* Cal AD = Calibrated carbon date in terms of AD
“Cal”:
solely refers to physical objects which are based on 14C-dating; not on, e.g., written sources and coins
Dating methods applicable to the Holocene (7)
“Archives” based dating
Museum collection, species can be used to indicate presence in a specific time
Archaeology based contextual dating
Animal / plant remains close or in archaeological findings.
- Gives an indication that they are from the same time period
Sediment core
older layers contain older remains, relative comparison
Ice core dating
Deeper layers contain older remains, relative comparison
Vulcanic ash dating
If you know when it erupted, you know everything below has a specific age
-Vulcanic eruptions identified in GISP2 ice core
Dendrochronology
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
14C-dating: decay curve for radiocarbon
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.
How does the calibration of radiocarbon work?
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.
two factors that complicate the calibration of radiocarbon
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
On what 4 dimensions can a chronology be based?
What are the climate based factors that you can base your chronology on?
What is the traditional 6 period classification in The Netherlands?
What are the 8 (but actually 9) Holocene subperiods?
Older dryas
Zone: I
Date BC: 12.000
Characteristic vegetation: Park Tundra
Allerod Interstadial
Zone: II
Date BC: 10.000
Characteristic vegetation: Birch with park tundra
Younger Dryas
Zone: III
Date BC: 8.800
Characteristic vegetation: Park Tundra
Pre-Boreal
Zone: IV
Date BC: 8.300
Characteristic vegetation: Birch, pine forest