How Old Is It? The Story of Dating in Archeaology — John Shaqi
How Old Is It? The Story of Dating in ArcheaologySchoenwetter, James
Science
How Old Is It? The Story of Dating in Archeaology
Schoenwetter, James
Archaeological dating; Dendrochronology; Radiocarbon dating
The carbon-14 isotope is about average in life span. It has been
determined that in any group of C-14 isotopes half of them will lose two
of their ping-pong balls and become C-12 isotopes in 5,730 years, plus
or minus 40. This is known as the _half-life_ of the C-14 isotope. The
“plus or minus 40” allows for laboratory error in terms of years.
Now all living things contain carbon atoms, and some of those atoms are
C-14 isotopes. The amount of C-14 isotopes in a living organism quickly
reaches a stable percentage after which there is no increase or decrease
while the organism is alive. After it dies, the C-14 supply is not
replenished, and with the passing of 5,730 plus or minus 40 years, it
has half the number of C-14 isotopes it had when alive. In 11,460 plus
or minus 80 years, it will have one quarter as many as it had when
alive.
The geochronologist takes a certain weight of carbon-bearing matter from
an organism which once lived. With simple chemistry he can determine the
number of carbon atoms in the material, usually charcoal, wood, bone or
shell. He places the material in a chamber equipped with geiger counters
and records the number of C-14 isotopes converting to C-12 isotopes
within a certain number of hours or days. Since he knows how many carbon
atoms there are in the specimen, he knows how many C-14 isotopes there
would be if the specimen were alive. He also knows that as the number of
C-14 atoms decreases the number of clicks on the geiger counter will
decrease too. For example, if there are 2,000 C-14 isotopes, the
decomposition of half of these over a period of approximately 5,730
years would register 1,000 clicks on the counter. In the next 5,730 year
period there would be 1,000 isotopes left, and only 500 of them would
decompose to register as geiger counter clicks.
The geochronologist does the counting and analysis of the results and
sends the information back to the archaeologist in the form of the
number of years that have elapsed since the carbon was part of a living
creature; for example, 1,500 plus or minus 150 years BP (before
present). The archaeologist, converting this to the Christian calendar
in 1964, would come up with A.D. 464 plus or minus 150 years. When was
the sample actually alive? We don’t know exactly, but statistically we
have a ninety-five percent chance of being right if we say sometime
between A.D. 164 and 764. This clock ticks in centuries. But the
radiocarbon clock doesn’t tick very long, even in centuries, before
running down. By the time 30,000 to 40,000 years have gone by, the C-14
in any sample is almost gone, and there is too little left to give
enough geiger counter clicks unless one is willing to wait a lifetime to
record two or three clicks.
Public-domain text, read in full here on John Shaqi.
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