Craig, referring to my message 121 writes:
It would be interesting to see if Moose geology book has more information in respect to C14 being able to fractionate or if its just c12 fractionating into c13.
The chemical processes lightly touched on in message 121
DO NOT change one isotope of Carbon into another.
Quoting myself from 121:
quote:
On the other hand, isotope exchange reactions between CO2 gas and aqueous carbonate species tend to enrich carbonates in13C.
What this is saying, as I understand it, is that when C0
3 disolved in water comes in contact with atmospheric CO
2, there is an exchange of C between the two phases. In this exchange, the
12C tends to slightly preferentially go into the atmospheric CO
2, and the
13C tends to slightly preferentially go into the disolved carbonate (CO
3). This would cause in any precipitated CO
3 (I presume as CaCO
3) to be higher in
13C.
I don't know how this process might effect
14C in the sediments. It would seem that it would also be slightly enriched. BUT the Carbon dating is NOT being done on the carbonate (per someone upthread), but rather on organic carbon from plant debris.
Moose
ps: Doing all these sub and superscripts sure is a pain.