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The Paleocene-Eocene Thermal Maximum (PETM) is marked by (select all answers that apply):
A δ13C excursion to higher values
A δ18O excursion to higher values
A major release of CO2 from marine carbonates marked by oxygen stable isotope measurements
A major release of methane from gas hydrates marked by carbon stable isotope measurements
A δ13C excursion to lower values
A δ18O excursion to lower values
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