Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4-Reference-Cited by-同舟云学术

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Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4

Published:2012-05-17 Issue:5 Volume:27 Page:475-484
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J. Quaternary Sci.

Author:

Andrews J. T.,Barber D. C.,Jennings A. E.,Eberl D. D.,Maclean B.,Kirby M. E.,Stoner J. S.

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/jqs.2535/fullpdf

Reference69 articles.

1. The Statistical Analysis of Compositional Data

2. Late Quaternary stratigraphy and paleoecology of Northwest Labrador Sea;Aksu;Marine Micropaleontology,1985

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

4. Comment on ‘Catastrophic ice shelf breakup as the source of Heinrich event icebergs’ by C.L. Hulbe et al;Alley;Palaeoceanography,2005

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1. Growth of the Laurentide and Innuitian ice sheets during MIS 5 recorded in distal marine sediment;Quaternary Science Reviews;2024-03

2. Chronology of detrital carbonate events in Baffin Bay reveals different timing but similar average recurrence time of North American-Arctic and Laurentide ice sheet collapse events during MIS 3;Earth and Planetary Science Letters;2023-07

3. Late Quaternary changes in sediment sources in the Labrador Sea;Canadian Journal of Earth Sciences;2023-02-01

4. Authigenic and Detrital Carbonate Nd Isotope Records Reflect Pulses of Detrital Material Input to the Labrador Sea During the Heinrich Stadials;Paleoceanography and Paleoclimatology;2023-01-28

5. Pulsebeat of early Holocene glaciation in Baffin Bay from high-resolution beryllium-10 moraine chronologies;Quaternary Science Reviews;2021-10

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