Variations of East Asian summer monsoon since the last deglaciation based on Mg/Ca and oxygen isotope of planktic foraminifera in the northern East China Sea

Paleoceanography

Volumn 25, Issue 4, 2010, Pages

  Kubota, Yoshimi ^a   Kimoto, Katsunori ^b   Tada, Ryuji ^a   Oda, Hirokuni ^c   Yokoyama, Yusuke ^a   Matsuzaki, Hiroyuki ^a  

^a UNIVERSITY OF TOKYO   (Japan)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^c NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

CALCIUM; DEGLACIATION; DRAINAGE BASIN; HOLOCENE; MAGNESIUM; MIXING RATIO; MONSOON; OXYGEN ISOTOPE; PLANKTONIC FORAMINIFERA; SEA SURFACE SALINITY; SEA SURFACE TEMPERATURE; SEASONAL VARIATION; STALAGMITE; TELECONNECTION;

CHINA; EAST CHINA SEA; KUROSHIO EXTENSION; PACIFIC OCEAN; YANGTZE RIVER;

FORAMINIFERA;

EID: 78049353103     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2009PA001891     Document Type: Article

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