div class=trans-pagebuttonPage 1button div class=trans-image amp-img class=trans-thumb alt=Page 1: University of Liverpool · The evolution of the Antarctic climate from a Cretaceous greenhouse into the Neogene icehouse is captured within a rich record of fossil leaves wood pollen src=https:reader034fdocumentsnetreader034viewer20220502015f548a270250f02d561e58f4html5thumbnails1jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 2button div class=trans-image amp-img class=trans-thumb alt=Page 2: University of Liverpool · The evolution of the Antarctic climate from a Cretaceous greenhouse into the Neogene icehouse is captured within a rich record of fossil leaves wood pollen src=https:reader034fdocumentsnetreader034viewer20220502015f548a270250f02d561e58f4html5thumbnails2jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 3button div class=trans-image amp-img class=trans-thumb alt=Page 3: University of Liverpool · The evolution of the Antarctic climate from a Cretaceous greenhouse into the Neogene icehouse is captured within a rich record of fossil leaves wood pollen src=https:reader034fdocumentsnetreader034viewer20220502015f548a270250f02d561e58f4html5thumbnails3jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 4button div class=trans-image amp-img class=trans-thumb alt=Page 4: University of Liverpool · The evolution of the Antarctic climate from a Cretaceous greenhouse into the Neogene icehouse is captured within a rich record of fossil leaves wood pollen src=https:reader034fdocumentsnetreader034viewer20220502015f548a270250f02d561e58f4html5thumbnails4jpg width=142 height=106 layout=responsive amp-img divdiv