Fine scale sediment structure and geochemical signature between eastern and western North Atlantic during Heinrich events 1 and 2

Quaternary Science Reviews

Volumn 46, Issue , 2012, Pages 136-150

  Rashid, H ^a   Saint Ange, F ^b,e   Barber, D C ^c   Smith, M E ^a   Devalia, N ^d  

^a OHIO STATE UNIVERSITY   (United States)

^b GEOLOGICAL SURVEY OF CANADA   (Canada)

^c BRYN MAWR COLLEGE   (United States)

^d MCGILL UNIVERSITY   (Canada)

^e DALHOUSIE UNIVERSITY   (Canada)

Author keywords

Cumberland sound ice shelf; Heinrich iceberg rafting; Hudson Strait ice stream; Radiogenic isotopes; Trinity Trough ice stream

Indexed keywords

CUMBERLAND SOUND ICE-SHELF; HEINRICH ICEBERG-RAFTING; HUDSON STRAIT; RADIOGENIC ISOTOPES; TRINITY TROUGH ICE-STREAM;

CARBONATION; ISOTOPES; OCEAN CURRENTS; QUARTZ; SEA ICE;

SEDIMENTOLOGY;

CARBONATE; DEPOSITIONAL ENVIRONMENT; DETRITUS; EXTREME EVENT; FORAMINIFERA; GEOCHEMICAL METHOD; HEINRICH EVENT; ICE SHEET; ICEBERG; OCEANIC CURRENT; OXYGEN ISOTOPE; PELAGIC ENVIRONMENT; RESOLUTION; SEDIMENT ANALYSIS; SURFICIAL SEDIMENT;

ATLANTIC OCEAN; CANADA; HUDSON STRAIT; LABRADOR SEA;

FORAMINIFERA; NEOGLOBOQUADRINA PACHYDERMA;

EID: 84862135383     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2012.04.026     Document Type: Article

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