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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

✍ Scribed by Aaron F. Diefendorf; William P. Patterson; Chris Holmden; Henry T. Mullins


Publisher
Springer Netherlands
Year
2007
Tongue
English
Weight
719 KB
Volume
39
Category
Article
ISSN
0921-2728

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