The Cromer cycle refers to a specific periodic cycle in the context of paleoceanography and paleoclimatology, primarily relating to Earth's climate and glacial-interglacial cycles. Named after mathematician and geophysicist Sir Edward Cromer, this cycle is believed to encompass changes in Earth's climatic conditions over hundreds of thousands of years, influenced by variations in the Earth's orbit around the sun, as well as other geological and environmental factors.
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