Seasonal sea-ice in the Arctic’s last ice area during the Early Holocene

Marine sediment proxies for sea ice suggest that a shift to seasonal sea ice in the Lincoln Sea during the Early Holocene was related to warmer air temperatures, similar to those projected to occur under anthropogenic warming.

Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Henrieka Detlef, Matt O’Regan, Christian Stranne, Mads Mørk Jensen, Marianne Glasius, Thomas M. Cronin, Martin Jakobsson, Christof Pearce
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Online Access:https://doi.org/10.1038/s43247-023-00720-w
https://doaj.org/article/e482466214db4374bef50d0a95ebeaf3
Description
Summary:Marine sediment proxies for sea ice suggest that a shift to seasonal sea ice in the Lincoln Sea during the Early Holocene was related to warmer air temperatures, similar to those projected to occur under anthropogenic warming.