Abstract
Investigation of the early Palaeogene palaeoecological and palaeoclimatological evolution of the Polar Regions is
hindered by the absence of calcite microfossils in sedimentary archives, which are conventionally the main dating
tool. To overcome this problem, we have generated large datasets of organic dinoflagellate cyst (dinocyst)
assemblages fromSouthern Ocean shelf sediments over the past
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