Cookies

We use cookies to ensure that we give you the best experience on our website. By continuing to browse this repository, you give consent for essential cookies to be used. You can read more about our Privacy and Cookie Policy.


Durham Research Online
You are in:

Holocene interactions between glacier retreat, sea‐ice formation and Atlantic Water advection at the inner Northeast Greenland continental shelf.

Syring, Nicole and Lloyd, Jeremy M. and Stein, Ruediger and Fahl, Kirsten and Roberts, Dave H. and Callard, Louise and O'Cofaigh, Colm (2020) 'Holocene interactions between glacier retreat, sea‐ice formation and Atlantic Water advection at the inner Northeast Greenland continental shelf.', Paleoceanography and paleoclimatology., 35 (11). e2020PA004019.

Abstract

During the past four decades significant decrease in Arctic sea ice and a dramatic ice mass loss of the Greenland Ice Sheet (GIS) has been coincident with global warming and an increase in atmospheric CO2. In Northeast Greenland significant mass loss from the outlet glaciers Nioghalvfjerdsbræ (79NG) and Zachariæ Isstrøm (ZI) and intensive seasonal breakup of the local Norske Øer Ice Barrier (NØIB) have also been observed since 2000. In order to better understand the processes driving these modern changes, studies of paleoclimate records are important and of major societal relevance. A multiproxy study including organic‐biogeochemical and micropaleontological proxies was carried out on a marine sediment core recovered directly in front of 79NG. Data from Core PS100/270 evidenced a strong inflow of warm recirculating Atlantic Water across the Northeast Greenland shelf from the early Holocene between ~10 and 7.5 ka. An overall high in phytoplankton productivity occurred within a stable sea‐ice margin regime, accompanied by 79NG retreat most probably triggered by peak solar insolation and changes in the local ocean circulation. Enhanced basal melt of the underside of 79NG at ~ 7.5 ka then led to the total disintegration of the ice shelf. The released freshwater would have driven water column stratification and promoted the formation of the local landfast ice barrier, which is shown by lowered biomarker values and foraminifera abundances towards the end of the early Holocene. Near perennial sea‐ice conditions with short summers and 79NG retreat to the inner fjord then prevailed from ~7.5 ka to ~0.8 ka.

Item Type:Article
Full text:Publisher-imposed embargo
(AM) Accepted Manuscript
File format - PDF
(4006Kb)
Full text:(VoR) Version of Record
Available under License - Creative Commons Attribution.
Download PDF
(8909Kb)
Status:Peer-reviewed
Publisher Web site:https://doi.org/10.1029/2020PA004019
Publisher statement:©2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Date accepted:15 October 2020
Date deposited:20 October 2020
Date of first online publication:11 November 2020
Date first made open access:12 November 2020

Save or Share this output

Export:
Export
Look up in GoogleScholar