| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8907388 | Earth and Planetary Science Letters | 2017 | 12 Pages |
Abstract
- Changes at the marine ice margin extended upstream toward the ice sheet interior.
- Glacier was thicker than present for â¼75-90% of each glacial-interglacial cycle.
- The ice surface was >200 m higher during Pliocene and Pleistocene glacial periods.
- Relative duration of deglaciation was similar in both the Pliocene and Pleistocene.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
R.S. Jones, K.P. Norton, A.N. Mackintosh, J.T.H. Anderson, P. Kubik, C. Vockenhuber, H. Wittmann, D. Fink, G.S. Wilson, N.R. Golledge, R. McKay,