Thanks for this question.
I think that what you have done makes sense but there are some subtleties to the model are worth considering in each case.
The model you have below is fine if the radiocarbon dates are essentially randomly drawn from the profile and there is no reason to suppose that they are more concentrated in one time period than another - this is an assumption of random deposition of 'radiocarbon-suitable' samples. In this model, all things being equal (which they won't be with radiocarbon dates in there), the model would be such that the time between Event1 and Event2 is likely to be half as long as the time between Event2 and Event3, just because the number of dates between Event2 and Event3 is double. The model will be pretty flexible, so it will allow for other possibilities too - but that will be the most likely outcome.
Boundaries are useful when there is a definite change in the depositional process. So if for example, between Event1 and Event2 there was a sterile layer with no organic material at all it would certainly be worth marking these events with Boundaries. Under a model with Boundaries, the number of dates between each Boundary does not affect the expected age in the model at all. In general a model with Boundaries will give wider ranges - covering a greater range of possibilities.
One approach that you might take is to try both types of model and see how robust the conclusions are to the different assumptions.
Christopher
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Boundary
.... elements of phase one
Boundary
... hiatus
Boundary
.... elements of phase two
Boundary
and so on. The [Tools > Models > Phases] tool sets up commonly used models for you and helps to give an idea of how to do this.
I think it only makes sense to use a depth model if the deposition is fairly well behaved (like a lake sediment) otherwise a straight sequence is probably more appropriate.
Best wishes
Christopher