The Turonian (93.5 to 89.3 million years ago) was one of the warmest periods of the Phanerozoic eon. It has been argued that there may have been several stages of continental ice growth during the period, reflected in both erosional surfaces and geochemical records associated with possible glaciation-induced sea-level falls.
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/isotopic-evidence-glaciation-during-cretaceous-supergreenhouse
[2] http://admin.indiaenvironmentportal.org.in/category/author/andre-bornemann
[3] http://admin.indiaenvironmentportal.org.in/category/author/richard-d-norris
[4] http://admin.indiaenvironmentportal.org.in/category/author/oliver-friedrich-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oceans-and-seas
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/global-warming
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-impacts
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/glacial-melt
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/science
