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This was an active margin throughout the Late Mesozoic, and in total some 7 km+ of Cretaceous sedimentary rocks accumulated in a series of fore-, intra- and back-arc basins. The Fossil Bluff Group of eastern Alexander Island can be traced from the Jurassic\u2013Cretaceous boundary into the Upper Albian and represents a broad-scale shallowing-upward sequence from deep marine to a prominent Upper Albian fluvial interval in which high-density forests developed at a palaeolatitude of 75\u00b0 S. The Cretaceous sequence exposed in the James Ross Island group continues right through the Upper Cretaceous to the Cretaceous\u2013Paleogene boundary. The Campanian\u2013Maastrichtian succession in particular is over 2 km in total thickness and richly fossiliferous. The improved Cretaceous stratigraphy of Antarctica is an invaluable terrestrial record of climatic change at a high palaeolatitude. This includes a gradual increase in temperature to the Cretaceous Thermal Maximum, and then a decline to the Cretaceous\u2013Paleogene boundary. There may be no simple link between these palaeotemperature changes and Cretaceous patterns of biotic radiation and extinction.<\/jats:p>","DOI":"10.1144\/sp545-2023-153","type":"journal-article","created":{"date-parts":[[2023,12,7]],"date-time":"2023-12-07T06:17:49Z","timestamp":1701929869000},"page":"811-835","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":4,"title":["Cretaceous stratigraphy of Antarctica and its global significance"],"prefix":"10.1144","volume":"545","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-5027-9965","authenticated-orcid":false,"given":"J. 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