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1
G31184.1
G31184.1
http://dx.doi.org/10.1130/G31184.1
CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization
P356
Q53100360-27648803-5096-43E5-A0D8-2F448A10F2F9
P356
G31184.1
http://dx.doi.org/10.1130/G31184.1