Activity

2012

• IS THE MID-EOCENE CLIMATIC OPTIMUM REPRESENTED IN WESTERN WASHINGTON? A CASE FOR THE MAPLE FALLS MEMBER OF THE CHUCKANUT FORMATION, USA
  T180 Quantitative Cenozoic Terrestrial Climate Reconstructions in the Northern Hemisphere: Evidence from Paleo-Proxies and Beyond (Posters)
  Tuesday, 6 November 2012

  9:00 AM - 6:00 PM

  Hall B