CO<sub>2</sub> explains most orbital-period variability and inter-hemispheric phasing during the late Pleistocene

Shakun, Jeremy

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Abstract: CO<sub>2</sub> explains most orbital-period variability and inter-hemispheric phasing during the late Pleistocene (AGU25)

CO₂ explains most orbital-period variability and inter-hemispheric phasing during the late Pleistocene

Jeremy D Shakun, Boston College, Department of Earth and Environmental Sciences, Chestnut Hill, MA, United States and Peter J Huybers, Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA, United States

CO2 explains most orbital-period variability and inter-hemispheric phasing during the late Pleistocene

CO₂ explains most orbital-period variability and inter-hemispheric phasing during the late Pleistocene