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IDES Laboratoire, University of Paris Sud-XI, Orsay, France
European climate variations over the past half-millennium reconstructed from groundwater
Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating
Open to closed system transition traced through the TDIC isotopic signature at the aquifer recharge stage, implications for groundwater 14C dating
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