Bottom water oxygenation history in southeastern Arabian Sea during the past 140 ka: Results from redox-sensitive elements

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 280, Issue 3-4, 2009, Pages 396-405

  Pattan, J N ^a   Pearce, N J G ^b  

^a NATIONAL INSTITUTE OF OCEANOGRAPHY   (India)

^b ABERYSTWYTH UNIVERSITY   (United Kingdom)

Author keywords

Bottom water oxygen; Last Glacial Maxima; Marine Isotope Stage; Oceanic circulation; Oxic; Redox sensitive elements (Re, U, Mo, Cd, V, Sb and Tl); Sediment core; Southeastern Arabian Sea; Suboxic

Indexed keywords

BOTTOM WATER; CONCENTRATION (COMPOSITION); LAST GLACIAL MAXIMUM; MARINE ISOTOPE STAGE; MARINE SEDIMENT; MASS BALANCE; OCEANIC CIRCULATION; OXYGENATION; PALEOPRODUCTIVITY; REDOX CONDITIONS; SEDIMENT CHEMISTRY; SEDIMENT CORE;

ARABIAN SEA; INDIAN OCEAN;

EID: 69249222510     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2009.06.027     Document Type: Article

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