High resolution evidence for linkages between NW European ice sheet instability and Atlantic Meridional Overturning Circulation

V. L. Peck, I. R. Hall, Rainer Zahn, H. Elderfield, F. Grousset, S. R. Hemming, J. D. Scourse

Research output: Contribution to journalArticleResearchpeer-review

102 Citations (Scopus)

Abstract

Published studies show that ice rafted debris (IRD) deposition preceding Heinrich (H) events H1 and H2 in the NE Atlantic was derived from the NW European ice sheets (NWEIS), possibly offering clues about ice sheet sensitivity and stability, and the mechanisms that caused periodic collapse of the Laurentide Ice Sheet (LIS). We present detailed lithological and geochemical records, including radiogenic isotope fingerprinting, of IRD deposits from core MD01-2461, proximal to the last glacial British Ice Sheet (BIS), demonstrating persistent instability of the BIS, with significant destabilisation occurring 1.5-1.9 kyr prior to both H1 and H2, dated at 16.9 and 24.1 kyr BP, respectively, in the NE Atlantic. Paired Mg/Ca and δ18O data from the surface dwelling Globigerina bulloides and subsurface dwelling Neogloboquadrina pachyderma sinistral are used to determine late-glacial variability of temperature, salinity and stratification of the upper water column. A picture emerges that the BIS was in a continuing state of readjustment and never fully reached steady state. Increased sea surface temperatures appear to have triggered the episode of NWEIS instability preceding H1. It seems most probable that the so-called 'precursor' events were not linked to the H events. However, if response to a common thermal forcing is considered, an increased response time of the LIS, up to ∼2 kyr longer than the NWEIS, may be inferred. Negative salinity excursions of up to 2.6 indicate significant incursions of melt water associated with peaks in NWEIS instability. Decreased surface density led to a more stable stratification of the upper water column and is associated with reduced ventilation of intermediate waters, recorded in depleted epibenthic δ13 C (Cibicidoides wuellerstorfi). We suggest that instability and meltwater forcing of the NWEIS temporarily weakened Atlantic Meridional Overturning Circulation, allowing transient advance of southern-sourced waters to this site, prior to H events 1 and 2. © 2006 Elsevier B.V. All rights reserved.
Original languageEnglish
Pages (from-to)476-488
JournalEarth and Planetary Science Letters
Volume243
Issue number3-4
DOIs
Publication statusPublished - 30 Mar 2006

Keywords

  • Atlantic Meridional Overturning Circulation
  • Heinrich events
  • Ice rafted debris
  • Ice sheet instability
  • NW European Ice Sheet
  • Ocean-climate linkage

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