a maple leaf in the sun |
Yesterday, in the parking lot at work,
a maple leaf rested on the pavement. The golden-hued morning light
caught the leaf highlighting the red-tending-to-maroon tones. The
leaf sharply contrasted the cold grey of the pavement, its vividness
catching my eye. What if I picked up the leaf and saved it? Could
archeologists in the far future figure out when the leaf fell from
the tree?
Currently, we can estimate how old
plant-based objects are using radiocarbon dating - often just called
carbon dating. In 1949, Willard Libby and his team accurately
estimated the age of the wood in an ancient Egyptian barge – a
barge with a recorded age. This process works through knowing the
ratio of carbon-12 (the ordinary stuff) to carbon-14 (a radioactive
isotope) in the atmosphere.
Carbon-14 isn't particularly stable and
decays quickly. It has a half-life of about 5,730 years - only a
moment of time compared to the approximately 4.5 billion year
half-life of uranium-238 (which is roughly the age of Earth).
Continuously formed in the atmosphere by cosmic rays, carbon-14
reacts with oxygen becoming carbon dioxide. Plants take up some of
this carbon dioxide along with carbon dioxide formed from the more
abundant carbon-12. When the plant dies, no more carbon dioxide is
taken in and the existing carbon-14 begins to decay.
If we assume the carbon-12 to carbon-14
ratio was the same when the plant died to now, using the decay rate
of carbon-14 will give us the item's age (back to about 60,000
years). But, we know this ratio has fluctuated over time. To
compensate, the age results are calibrated to something known like
written records or tree rings. The biggest change to the carbon-12 to
carbon-14 ratio has occurred in modern times through nuclear testing.
Carbon-14 levels in the atmosphere were boosted around 1950 and
peaked in the 1960's (at which time, testing bans were agreed to).
So, could a future archeologist figure
out the are of my leaf using carbon dating? Probably not accurately
because we've messed with the carbon-12 to carbon-14 ratio in our
atmosphere. It would be more accurate for that archeologist to look
at the date of this article.
As a tangent: At the end of the day
when I returned to my car, the leaf was still there. Without the
sunlight shining on it, the leaf looked brown and uninteresting.
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