A Heinrich-like event, H-0 (DC-0): Source(s) for detrital carbonate in the North Atlantic during the Younger Dryas Chronozone-Reference-Cited by-同舟云学术

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A Heinrich-like event, H-0 (DC-0): Source(s) for detrital carbonate in the North Atlantic during the Younger Dryas Chronozone

Published:1995-10 Issue:5 Volume:10 Page:943-952
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Andrews J. T.,Jennings Anne E.,Kerwin M.,Kirby M.,Manley W.,Miller G. H.,Bond G.,MacLean B.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/v010/i005/95PA01426/95PA01426.pdf

Reference73 articles.

1. Late Quaternary sedimentation in Baffin Bay;Aksu;Can. J. Earth Sci.,1987

2. Ice-rafted debris associated with binge-purge oscillations of the Laurentide Ice Sheet;Alley;Paleoceanography,1994

3. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event;Alley;Nature,1993

4. Late-glacial radiocarbon and palynostratigraphy on the Swiss Plateau;Ammann;Boreas,1989

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