Fig. 10From: The Misery Point cliff, Mayaguana Island, SE Bahamas: a unique record of sea-level highstands since the Early PleistoceneProbable timing of depositional and erosional events at the Misery Point cliff, Mayaguana (red circles). Benthic oxygen-isotope curve is from Lisieki and Raymo (2005); time scales in the lower part of the diagram are from Ogg and Pillans (2008). Abbreviations from top to bottom: CTM = Cockburn Town Member; OHF = Owl’s Hole Formation; PM = paleomagnetic record; H = Holocene; Tar. = TarantianBack to article page