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The clear glacial–interglacial pattern of δ18OUvi in core M125-50-3 allows for the construction of a robust age model for this site by tuning its benthic-isotope record to the LR04 benthic stack (Lisiecki and Raymo, 2005) and indicates that it extends to ∼ 135 ka (Fig
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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