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A 15.4-ka paleoclimate record inferred from δ13C and δ15N of organic matter in sediments from the sub-alpine Daping Swamp, western Nanling Mountains, South China

Crossref DOI link: https://doi.org/10.1007/s10933-016-9935-x

Published Online: 2016-12-28

Published Print: 2017-02

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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