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As δ18OUvi values between EII and EIII are less depleted than MIS 5 samples of reference site M125-50-3, we infer that those sediments were most likely deposited during MIS 4 and did not reach into MIS 5
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https://bg.copernicus.org/articles/17/5883/2020/
org/0000-0003-1267-6190
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Departamento de Geoquímica, Universidade Federal Fluminense, Outeiro São João Baptista s/n