Reconstruction of Indian monsoon variability over the past 230,000 years: Planktic foraminiferal evidence from the NW Arabian Sea open-ocean upwelling area

Marine Micropaleontology

Volumn 63, Issue 3-4, 2007, Pages 143-154

  Ishikawa, Satoko ^a   Oda, Motoyoshi ^a  

^a TOHOKU UNIVERSITY   (Japan)

Author keywords

Insolation; Late Quaternary; Monsoon; NW Arabian Sea; Open ocean upwelling area; Planktic foraminiferal productivity

Indexed keywords

ABUNDANCE; CLIMATE VARIATION; CORE ANALYSIS; DOMINANCE; GLACIAL-INTERGLACIAL CYCLE; GLOBAL WARMING; INSOLATION; MASS SPECTROMETRY; MONSOON; OPEN OCEAN; OXYGEN ISOTOPE; PLANKTONIC FORAMINIFERA; POPULATION DYNAMICS; QUATERNARY; RECONSTRUCTION; SEDIMENTATION; UPWELLING; WARMING;

ARABIAN SEA; ASIA; EURASIA; INDIAN OCEAN; MIDDLE EAST; OMAN;

FORAMINIFERA; GLOBIGERINA BULLOIDES; GLOBIGERINITA GLUTINATA; GLOBIGERINOIDES RUBER; GLOBIGERINOIDES SACCULIFER; NEOGLOBOQUADRINA DUTERTREI; NEOGLOBOQUADRINA INCOMPTA;

EID: 34247871178     PISSN: 03778398     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marmicro.2006.11.004     Document Type: Article

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