I wonder if anyone can help. I am writing a paper at the moment on hydrothermal vent communities from the latest Cenomanian of the Troodos Ophiolite from Cyprus. These communities were living in a deep water setting, estimated to be 2.5 to 5 km, and include shelly fauna. My question is if anybody has an estimate for what the carbonate compensation depth might have been around Cenomanian-Turonian times in the Neotethys Ocean (now Eastern Mediterranean).

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