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A chemical record of millennia. The chemistry of surface run-off, including the carbon isotopes in leaf wax from plants, builds an accurate record of local climate conditions in the lake-bed sediment. Image credit: Mike Cohea/Brown University

A chemical record of millennia. The chemistry of surface run-off, including the carbon isotopes in leaf wax from plants, builds an accurate record of local climate conditions in the lake-bed sediment. Image credit: Mike Cohea/Brown University

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