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Continuous sedimentary records from an eastern Mediterranean cold-water coral ecosystem thriving in intermediate water depths (∼600m) reveal a temporary extinction of cold-water corals during the Early to Mid Holocene from 11.4–5.9calkyr BP. Benthic foraminiferal assemblage analysis shows low-oxygen conditions of 2mll −1 during the same period, compared to bottom-water oxygen values of 4–5mll...
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