Paleoceanographic development in the SW Barents Sea during the Late Weichselian-Early Holocene transition

Quaternary Science Reviews

Volumn 29, Issue 25-26, 2010, Pages 3442-3456

  Aagaard Sorensen S ^a   Husum, K ^a   Hald, M ^a   Knies, J ^b  

^a UNIVERSITY OF TROMSØ   (Norway)

^b GEOLOGICAL SURVEY OF NORWAY   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

ACCELERATOR MASS SPECTROMETRY; ATLANTIC WATER; BARENTS SEA; BOTTOM WATER; HIGH FLUX; HOLOCENES; ICE RAFTED DEBRIS; ICE SHEET; MELT WATER; MERIDIONAL TRANSPORT; NORTH ATLANTIC CURRENTS; NORTH COAST; OCEANOGRAPHIC CONDITIONS; PRIMARY PRODUCTION; PRIMARY PRODUCTIVITY; SCALE RESOLUTION; SEA-ICE COVER; SEDIMENT CORE; SEDIMENT SAMPLES; SIZE FRACTION; TIME-PERIODS; WATER DEPTH; YOUNGER DRYAS;

DEBRIS; GLACIERS; ISOTOPES; MASS SPECTROMETRY; MOORING; OCEANOGRAPHY; SEA ICE; SEDIMENTOLOGY; SEDIMENTS;

GLACIAL GEOLOGY;

ACCELERATOR MASS SPECTROMETRY; GLACIAL-INTERGLACIAL CYCLE; HOLOCENE; ICE COVER; ICE RAFTING; ICE SHEET; ICEBERG; MERIDIONAL CIRCULATION; PALEOCEANOGRAPHY; PHYSICOCHEMICAL PROPERTY; PLANKTONIC FORAMINIFERA; PRIMARY PRODUCTION; SEA ICE; SEDIMENT CORE; WATER DEPTH; WEICHSELIAN;

ARCTIC OCEAN; ATLANTIC OCEAN; BARENTS SEA; NORTH ATLANTIC CURRENT; NORWAY;

FORAMINIFERA;

EID: 78049434467     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2010.08.014     Document Type: Article

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