Source, timing, frequency and flux of ice-rafted detritus to the Northeast Atlantic margin, 30-12 ka: Testing the Heinrich precursor hypothesis

Boreas

Volumn 39, Issue 3, 2010, Pages 576-591

  Haapaniemi, Anna I ^a   Scourse, James D ^b   Peck, Victoria L ^c   Kennedy, Hilary ^b   Kennedy, Paul ^b   Hemming, Sidney R ^d   Furze, Mark F A ^e   Pienkowski, Anna J ^f   Austin, William E N ^g   Walden, John ^g   Wadsworth, Emilie ^g   Hall, Ian R ^h  

^a UNIVERSITY OF HELSINKI   (Finland)

^b BANGOR UNIVERSITY   (United Kingdom)

^c BRITISH ANTARCTIC SURVEY   (United Kingdom)

^d Department of Earth and Environmental Sciences   (United States)

^e MACEWAN UNIVERSITY   (Canada)

^f UNIVERSITY OF ALBERTA   (Canada)

^g UNIVERSITY OF ST ANDREWS   (United Kingdom)

^h CARDIFF UNIVERSITY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

DETRITUS; HEINRICH EVENT; ICE MARGIN; ICE-RAFTED DEBRIS; LAURENTIDE ICE SHEET; MERIDIONAL CIRCULATION; OVERTURN; PALEOCLIMATE; PLANKTONIC FORAMINIFERA; SEA ICE;

ATLANTIC OCEAN; ATLANTIC OCEAN (NORTHEAST);

EID: 77954814543     PISSN: 03009483     EISSN: 15023885     Source Type: Journal    
DOI: 10.1111/j.1502-3885.2010.00141.x     Document Type: Article

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