oa Decoupling of Nw Pacific from Global Climate Evolution Linked to the Mid-Pleistocene Transition and Mid-Brunhes Event

References

1. Chalk, T. B. et al.
   , 2017. Causes of ice age intensification across the Mid-Pleistocene Transition. PNAS114(50), 13114–13119.
   [Google Scholar]
2. Cronin, T. M. et al.
   , 2017. Enhanced Arctic Amplification Began at the Mid-Brunhes Event ~400,000 years ago. Nature Scientific Reports7:14475.
   [Google Scholar]
3. Kars, M. A. C. et al.
   , 2017. Impact of climate change on the magnetic mineral assemblage in marine sediments from Izu rear arc, NW Pacific Ocean, over the last 1 Myr. Palaeogeography, Palaeoclimatology, Palaeoecology480, 53–69.
   [Google Scholar]
4. Kender, S. et al.
   , 2018. Closure of the Bering Strait caused Mid-Pleistocene Transition cooling. Nature Communications9:5386.
   [Google Scholar]
5. Lisiecki, L.E., Raymo, M.E.A.
   , 2005. Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography20, PA1003.
   [Google Scholar]
6. Martínez-Garcia, A. et al.
   , 2011. Southern Ocean dust-climate coupling over the past four million years. Nature476, 312–315.
   [Google Scholar]
7. Rohling, E. J. et al.
   , 2014. Sea-level and deep-sea-temperature variability over the past 5.3 million years. Nature508, 477–482.
   [Google Scholar]