North Atlantic marine radiocarbon reservoir ages through Heinrich event H4:a new method for marine age model construction

Cooling and sinking of dense saline water in the Norwegian-Greenland Sea is essential for the formation of North Atlantic Deep Water. The convection in the Norwegian-Greenland Sea allows for a northward flow of warm surface water and southward transport of cold saline water. This circulation system...

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Bibliographic Details
Published in:Geological Society, London, Special Publications
Main Authors: Olsen, Jesper, Rasmussen, Tine L., Reimer, Paula J.
Other Authors: Austin, WEN, Abbott, PM, Davies, SM, Pearce, NJG, Wastegard, S
Format: Other Non-Article Part of Journal/Newspaper
Language:English
Published: GEOLOGICAL SOC PUBLISHING HOUSE 2014
Subjects:
LAST GLACIAL PERIOD
ICE-CORE
NORTHEASTERN ATLANTIC
CLIMATIC VARIATIONS
CALIBRATION CURVE
GREENLAND ICE
NORDIC SEAS
HULU CAVE
C-14
SEDIMENTS
Greenland
Hulu
Greenland Sea
ice core
Nordic Seas
North Atlantic Deep Water
North Atlantic
Online Access:https://pure.au.dk/portal/da/publications/north-atlantic-marine-radiocarbon-reservoir-ages-through-heinrich-event-h4(b65e1279-3b22-434b-b4af-eb86b49a47fa).html
https://doi.org/10.1144/SP398.2

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