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- W323949053 abstract "Summary 18 Constraints on Earth’s glacial history come from the deep-sea oxygen isotope (δ O) record. The growth of Antarctic ice during the early Cenozoic is modelled to have driven changes in seawater δ 18 O of up to 0.5‰ (DeConto & Pollard, 2003). Larger shifts in the mean δ 18 O of seawater therefore require some storage of ice in both hemispheres. In order to study the evolution of the cryosphere, we developed high-resolution records of seawater δ 18 O for three Pacific sites. The seawater δ 18 O reconstructions show that several large (>0.65‰) shifts in seawater δ O occurred throughout the middle Eocene to early Oligocene. Our records of seawater δ 18 O indicate there was ice stored on Antarctica and in the Northern Hemisphere at about 44.5 Ma, 42 Ma, 38 Ma, and after 34 Ma. Citation: Tripati, A.K., C.F. Dawber, H. Macintyre, J. Backman, H. Elderfield, P. Ferretti (2007), Evidence for synchronous glaciation of andAntarctica and the Northern Hemisphere during the Eocene and Oligocene: Insights from Pacific records of the oxygen isotopic composition of seawater:" @default.
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- W323949053 date "2007-01-01" @default.
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- W323949053 title "Evidence for synchronous glaciation of Antarctica and the Northern Hemisphere during the Eocene and Oligocene: Insights from Pacific records of the oxygen isotopic composition of seawater" @default.
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