I'm curious why you can't? I'm guessing that seawater permeation would alter the isotope distribution, but I also wonder if the alteration is predictable in some fashion. Does seawater affect the decay rate in some fashion?
Yes, that's exactly it. You can sometimes adjust if the water was constant and you have some other clock you can calibrate to (for example the bottom of the ocean at a specific depth).
But if you have water that came and went then the errors are too large.
That would explain the discrepancy between 3,500 and 10,000 years.