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Abrupt changes in environmental signals recorded in an interval of strata can be the result of (1) fast changes in environmental conditions and average sedimentation rate or (2) average changes in environmental conditions and slow sedimentation rate. The new study by Dr. Emilia Jarochowska and co-authors, published in Paleoceanography and Paleoclimatology, proposes a method to estimate relative changes in depositional rates and test it in a sedimentary section

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