'topes rule!

posted by tom / August 02, 2006 /

Those of you who, like me, wish they understood chemistry should check out Derek Lowe's fascinating discussion of how anti-doping agencies can tell the difference between natural and artificial testosterone. I always assumed that for naturally-present performance enhancers, the amount present in the body was the only indicator of cheating — and presumably not a very accurate indicator, since different people naturally produce different levels of hormones/red blood cells/whatever.

But it turns out there are other ways to catch cheaters. For one thing, you can indentify an unnatural level of testosterone by examining the relative levels of its (inactive?) enantiomer. More interesting (and accurate) is the use of a technique (sort of) related to carbon dating. Lowe lays it out.

Speaking of carbon dating, I understood how it works, but never really got why it works — I get that carbon isotope levels have changed over time, but I always thought it was due to radioactive decay. But of course that doesn't make any sense, since an unstable isotope in a dinosaur bone should decay just as quickly as one in the atmosphere (assuming that cosmic rays aren't a big factor, which, as a non-Fantastic Four fan, I'm ready to do). Besides which, I guess C13 is a stable isotope, so the decay thing never made any sense anyway. Thankfully, Lowe fills in the gaps on all this, too. Good stuff.

UPDATE: Whoops! Forget what I said about carbon dating. Derek was kind enough to drop by in comments and lay out the actual reason that carbon dating works — it's unrelated to biological systems slowly filtering out C13, the phenomenon that's the basis for the artificial testosterone assay his post discusses.

The cosmic-rays-hitting-nitrogen business rings a bell, though, and I'm a little embarrassed to have forgotten it. Sorry for the confusion — I told you I was a dope when it comes to chemistry.

Comments

Actually, it is radioactive C-14 that's the basis for carbon dating. Its half-life is about 5700 years, so (other things being equal) there shouldn't be any of it left on Earth by now. But it's being made continuously from abundant nitrogen-14 as cosmic rays hit the upper atmosphere. That's the missing piece of information you may not have come across. This means that as long as an organism is eating and breathing, its C-14 level is staying pretty constant.

But once it dies, the clock starts ticking. No more fresh C-14 is coming in, and what's there starts to unwind. To get an age, you just measure what's left and work backwards.

There are numerous correcting factors, but the age you get just from the half-life calculation is a good first approximation. With modern instruments, the technique can be pushed past 50,000 years (but not as far as 100,000, as far as I know). Other isotope techniques start to take over at longer time scales.

Posted by: Derek Lowe on August 2, 2006 03:24 PM

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