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J.EPSL.2004.05.007
J.EPSL.2004.05.007
http://dx.doi.org/10.1016/J.EPSL.2004.05.007
Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO 2 in the Taylor Dome, Dome C and DML ice cores
P356
Q58083611-CB2602F8-7C2E-4A22-BD8C-A1633CC373B9
P356
J.EPSL.2004.05.007
http://dx.doi.org/10.1016/J.EPSL.2004.05.007