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Article #888

Re: simple question

#888
From: Eric Rescorla
Date: Wed, 08 Apr 1992 16:15
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In article <9204080901.aa00587@Paris.ics.uci.edu> kibler@turing.ICS.UCI.EDU (Dennis Kibler) writes:
> Let me put it in a more concrete form. Suppose we use carbon
>dating to measure the age of a fossilized plant. I don't
>understand why we aren't measuring the age of the carbon,
>created I presume at the some time before the age of the earth,
>rather than the age of the plant.
The percentage of C14 in the atmosphere is ~constant over time.
As long as you're alive, you exchange carbon with the atmosphere
and maintain the atmospheric concentration of C14 in your system.
When you die, you stop exchanging and that's the zero-time.

-Ekr


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From: rescorla@rtnmr.chem.yale.edu (Eric Rescorla)
Subject: Re: simple question
Message-ID: <1992Apr8.161532.24698@cs.yale.edu>
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Date: Wed, 8 Apr 1992 16:15:32 GMT
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