Constraints on global mean sea level during Pliocene warmth-Reference-Cited by-同舟云学术

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Constraints on global mean sea level during Pliocene warmth

Published:2019-08-30 Issue:7777 Volume:574 Page:233-236
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Dumitru Oana A.,Austermann Jacqueline,Polyak Victor J.,Fornós Joan J.,Asmerom Yemane,Ginés Joaquín,Ginés Angel,Onac Bogdan P.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41586-019-1543-2.pdf

Reference53 articles.

1. Dutton, A. et al. Sea-level rise due to polar ice-sheet mass loss during past warm periods. Science 349, aaa4019 (2015).

2. Rohling, E. J. et al. Sea-level and deep-sea-temperature variability over the past 5.3 million years. Nature 508, 477–482 (2014); corrigendum 510, 432 (2014).

3. Raymo, M. E., Kozdon, R., Evans, D., Lisiecki, L. & Ford, H. L. The accuracy of mid-Pliocene δ18O-based ice volume and sea level reconstructions. Earth Sci. Rev. 177, 291–302 (2018).

4. De Boer, B., van de Wal, R. S. W., Bintanja, R., Lourens, L. J. & Tuenter, E. Cenozoic global ice-volume and temperature simulations with 1-D ice-sheet models forced by benthic δ18O records. Ann. Glaciol. 51, 23–33 (2010).

5. Haywood, A. M. et al. Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project. Clim. Past 9, 191–209 (2013).

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