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Carbon isotopes of marl and lake sediment organic matter reflect terrestrial landscape change during the late Glacial and early Holocene (16,800 to 5,540
Aaron F. Diefendorf, William P. Patterson, Chris Holmden, Henry T. MullinsVolume:
39
Language:
english
Pages:
15
DOI:
10.1007/s10933-007-9099-9
Date:
January, 2008
File:
PDF, 719 KB
english, 2008