Asynchronous Antarctic and Greenland ice-volume contributions to the last interglacial sea-level highstand

Asynchronous Antarctic and Greenland ice-volume contributions to the last interglacial sea-level highstand

The relative contributions of the Greenland and Antarctic Ice Sheets to Last Interglacial sea level rise remain debated, as do the timing and magnitude. Here, data show that the Antarctic Ice Sheet dominated particularly high levels of sea-level rise during the early Last Interglacial.

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Autores principales: Eelco J. Rohling, Fiona D. Hibbert, Katharine M. Grant, Eirik V. Galaasen, Nil Irvalı, Helga F. Kleiven, Gianluca Marino, Ulysses Ninnemann, Andrew P. Roberts, Yair Rosenthal, Hartmut Schulz, Felicity H. Williams, Jimin Yu
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2019
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Science
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Acceso en línea:https://doaj.org/article/e20a20a211e24487bbf968302680e299
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https://doaj.org/article/e20a20a211e24487bbf968302680e299

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