Planktic foraminifer-based sea-surface temperature reconstruction for sediment cores JM97-948/2A and MD95-2011 from the Vøring Plateau, eastern Norwegian Sea

The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6000 years before present (6 ka). For the marine realm, Holoce...

Full description

Bibliographic Details
Main Authors: Andersson, Carin, Pausata, Francesco S R, Jansen, Eystein, Risebrobakken, Bjørg, Telford, Richard J
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.820584
https://doi.org/10.1594/PANGAEA.820584