When a chemical decays by a first order reaction (usually describes a radioactive isotope but in this case it is a chemical decay driven mostly by entropy which explains the very large temperature dependence) the reaction is dc/dt = kc where k is a constant. This means that the integral of 1/c dc equals the integral of kdt. This is ln(c)-ln(co)=kt and, therefore, the rate at which the material decays is independent of its concentration. In these cases it is convenient to describe the rate in "half life" which is the amount of time it would take for half of said material to decay. That is to say if the half life of DNA frozen at 0C is 500,000 years and we had a 1 ton sample (impossibly large), after 500,000 years we would only have 1000lbs. After 1000000 years, 500 lbs. Now that 65 million years have passed, that 1 ton sample would be reduced to 6.66 × 10^-34 grams of DNA which means (statistically) not even one molecule would remain.

this only makes time travel more necessary

It's a physics thing.

no it's more of a chemistry thing

I dont agree with you respect, but I opinion it

I don't respect your opinion, but I agree with it.

I don't opinion with your respect, but I agree with you.

yes. it is

What the duck man

He was jealous that she made so much cash

yep! yep! yep!