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Late Quaternary (Stage 2 and 3) Meltwater and Heinrich Events, Northwest Labrador Sea

Published online by Cambridge University Press:  20 January 2017

John T. Andrews ,
Helmut Erlenkeuser ,
Katherine Tedesco ,
Ali E. Aksu  and
A.J.Timothy Jull
John T. Andrews
Affiliation:
INSTAAR and Department of Geological Sciences, Box 450, University of Colorado, Boulder, Colorado 80309
Helmut Erlenkeuser
Affiliation:
Institute of Nuclear Physics, C-14 Laboratory, Kiel University, Kiel, Germany
Katherine Tedesco
Affiliation:
INSTAAR and Department of Geological Sciences, Box 450, University of Colorado, Boulder, Colorado 80309
Ali E. Aksu
Affiliation:
Department of Geology, Memorial University of Newfoundland, St John's, Newfoundland, Canada A1B 3X5
A.J.Timothy Jull
Affiliation:
NSF-Arizona AMS Facility, University of Arizona, Tucson, Arizona 85721
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Abstract

Two major meltwater events are documented in cores from the NW Labrador Sea. One occurred ca. 20,000 14C yr B.P. in association with deposition of a major detrital carbonate unit. Both prior to and after this event, δ18O values of near-surface planktonic foraminifera were 4.5%, indicating fully enriched glacial values. A younger event (ca. 14,000 14 C yr B.P.) is characterized by a dramatic change in δ18O from 4.5 to 2.0% and coincided with the retreat of ice from the outer SE Baffin Shelf, possibly into Hudson Strait. These meltwater events coincide with Heinrich (H) layers 1 and 2 from North Atlantic sediments. The 14,000 14C yr B.P. meltwater event indicates that the eastern margin of the Laurentide Ice Sheet also underwent rapid retreat at approximately the same time as other ice sheet margins around the NE North Atlantic. A third major detrital carbonate event at the base of HU87-033-009, possibly correlative with Heinrich layer 3, occurred ca. 33,960 ± 675 14 C yr B.P.; however, this is older than the accepted date for H-3 of 27,000 14C yr B.P. and may be H-4.

Type
Articles
Information
Quaternary Research , Volume 41 , Issue 1 , January 1994 , pp. 26 - 34
Copyright
University of Washington

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