The Late Quaternary evolution of water masses in the eastern Indian Ocean between Australia and Indonesia, based on benthic foraminifera faunal and carbon isotopes analyses

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 247, Issue 3-4, 2007, Pages 382-401

  Murgese, Davide S ^a   De Deckker, Patrick ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Antarctic Intermediate Water; Benthic foraminifer accumulation rate; Bulimina aculeata; Delta 13C; Indian Ocean water masses; Last Glacial Maximum; Productivity; South Java Upwelling

Indexed keywords

ACCUMULATION RATE; ANTARCTIC INTERMEDIATE WATER; BENTHIC FORAMINIFERA; CARBON ISOTOPE; DISSOLVED OXYGEN; FAUNA; ISOTOPIC ANALYSIS; LAST GLACIAL MAXIMUM; OCEANIC CIRCULATION; OCEANIC CURRENT; ORGANIC MATTER; PALEOCEANOGRAPHY; PALEOPRODUCTIVITY; Q FACTOR; QUATERNARY; SEA SURFACE; UPWELLING; WATER MASS;

ASIA; AUSTRALASIA; AUSTRALIA; BANDA SEA; EURASIA; GREATER SUNDA ISLANDS; INDIAN OCEAN; INDONESIA; INDONESIAN SEAS; JAVA; LEEUWIN CURRENT; MALAY ARCHIPELAGO; PACIFIC OCEAN; SOUTHEAST ASIA; SUNDA ISLES; WESTERN AUSTRALIA;

BOLIVINA ROBUSTA; BULIMINA ACULEATA; CIBICIDOIDES WUELLERSTORFI; EPISTOMINELLA EXIGUA; FORAMINIFERA; GLOBOCASSIDULINA SUBGLOBOSA; NUMMOLOCULINA IRREGULARIS; UVIGERINA PROBOSCIDEA;

EID: 34047178361     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2006.11.002     Document Type: Article

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