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From Greenhouse to Icehouse – The Eocene/Oligocene - UMass ...

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368 J. E. Francis et al.<br />

Author's personal copy<br />

Wilson, T. J. (1999). Cenozoic structural segmentation of the Transantarctic<br />

Mountains rift flank in southern Vic<strong>to</strong>ria Land, Antarctica. In: F. M. Van der<br />

Wateren, & S. Cloetingh (Eds). Lithosphere dynamics and environmental change of<br />

the Cenozoic West Antarctic rift system. Global Planet. Change, 23, 105<strong>–</strong>127.<br />

Wrenn, J. H., & Beckmann, S. W. (1982). Maceral, <strong>to</strong>tal organic carbon, and palynological<br />

analyses of Ross Ice Shelf Project Site J-9 Cores. Science, 216, 187<strong>–</strong>189.<br />

Wrenn, J. H., & Hart, G. F. (1988). Paleogene dinoflagellate cyst biostratigraphy of<br />

Seymour Island, Antarctica. In: R. M. Feldmann, & M. O. Woodburne (Eds).<br />

Geology and Paleon<strong>to</strong>logy of Seymour Island, Antarctic Peninsula. Geological<br />

Society of America Memoir., Vol. 169, pp. 321<strong>–</strong>447.<br />

Zachos, J. C., Breza, J. R., & Wise, S. W. (1992). Early <strong>Oligocene</strong> ice-sheet<br />

expansion on Antarctica <strong>–</strong> Stable iso<strong>to</strong>pe and sedimen<strong>to</strong>logical evidence from<br />

Kerguelen Plateau, Southern Indian Ocean. Geology, 20, 569<strong>–</strong>573.<br />

Zachos, J., Pagani, M., Sloan, L., Thomas, E., & Billups, K. (2001). Trends, rhythms,<br />

and aberrations in global climate 65 Ma <strong>to</strong> present. Science, 292, 686<strong>–</strong>693.<br />

Zachos, J. C., Quinn, T. M., & Salamy, K. A. (1996). High-resolution (104 years)<br />

deep-sea foraminiferal stable iso<strong>to</strong>pe records of the <strong>Eocene</strong><strong>–</strong><strong>Oligocene</strong> climate<br />

transition. Paleoceanography, 11, 251<strong>–</strong>266.<br />

Zastawaniak, E., Wrona, R., Gazdzicki, A. J., & Birkenmajer, K. (1985). Plant<br />

remains from the <strong>to</strong>p part of the Point Hennequin Group (Upper <strong>Oligocene</strong>),<br />

King George Island (South Shetland Islands, Antarctica). Studia Geologica Pol.,<br />

81, 143<strong>–</strong>164.

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