Negative δ18O–δ13C relationship of pedogenic carbonate from northern China indicates a strong response of C3/C4 biomass to the seasonality of Asian monsoon precipitation

Title
Negative δ18O–δ13C relationship of pedogenic carbonate from northern China indicates a strong response of C3/C4 biomass to the seasonality of Asian monsoon precipitation
Authors
Keywords
-
Journal
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Volume 317-318, Issue -, Pages 32-40
Publisher
Elsevier BV
Online
2011-12-16
DOI
10.1016/j.palaeo.2011.12.007

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