I am currently writing up my PhD thesis, and I have shown that even with a sampling resolution of 1 sample per cm, the black shale I am studying shows evidence of brief fluctuations between oxic and anoxic states (probably decades to centuries in duration) in the form of in-situ benthic macrofauna.

The issue is that many of the geochemical sampling techniques I used can only resolve proxy records at a 1 cm scale, due to sample weight requirements (e.g. total lipid extraction for biomarker analysis), and multiple redox oscillations become time-averaged in these samples.

Is it possible to use some sort of model based on Bayesian statistics, to estimate the likely true frequency of oxia/anoxia in a given sampling interval (i.e. using the 1cm scale proxy data and the

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