Detrital carbonate peaks on the Labrador shelf, a 13–7ka template for freshwater forcing from the Hudson Strait outlet of the Laurentide Ice Sheet into the subpolar gyre-Reference-Cited by-同舟云学术

Detrital carbonate peaks on the Labrador shelf, a 13–7ka template for freshwater forcing from the Hudson Strait outlet of the Laurentide Ice Sheet into the subpolar gyre

Published:2015-01 Issue: Volume:107 Page:62-80
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Jennings Anne^ORCID,Andrews John,Pearce Christof,Wilson Lindsay,Ólfasdótttir Sædís

Funder

U.S. National Science Foundation

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference93 articles.

1. Icebergs and iceberg-rafted detritus (IRD) in the North Atlantic: facts and assumptions;Andrews;Oceanography,2000

2. Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4;Andrews;J. Quat. Sci.,2012

3. A Heinrich-like event, H-0 (DC-0): source(s) for detrital carbonate in the North Atlantic during the Younger Dryas chronozone;Andrews;Paleoceanography,1995

4. Radiocarbon dates obtained through geographical branch field observations;Andrews;Geogr. Bull.,1967

5. Surface (sea floor) and near-surface (box cores) sediment mineralogy in Baffin Bay as a key to sediment provenance and ice sheet variations;Andrews;Can. J. Earth Sci.,2011

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