Sea-level variation during MIS 11 constrained by stepwise Osaka Bay extensions and its relation with climatic evolution

Quaternary Science Reviews

Volumn 29, Issue 15-16, 2010, Pages 1863-1879

  Kariya, Chie ^a   Hyodo, Masayuki ^a   Tanigawa, Koichiro ^a   Sato, Hiroshi ^b  

^a KOBE UNIVERSITY   (Japan)

^b UNIVERSITY OF HYOGO   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

ACCUMULATION RATES; ANTARCTICA; CLIMATIC EVOLUTION; COASTAL SEDIMENTS; DRILL CORE; ENVIRONMENTAL CHANGE; GEOLOGICAL DATA; INTERGLACIALS; LAST INTERGLACIAL; LONG DURATION; MARINE OXYGEN ISOTOPES; MAXIMUM TEMPERATURE; OSAKA BAY; OXYGEN ISOTOPIC; SULFUR ANALYSIS;

CORE DRILLING; ISOTOPES; OXYGEN; SEDIMENTOLOGY; SULFUR;

SEA LEVEL;

ABUNDANCE; ACCUMULATION RATE; CORE ANALYSIS; DIATOM; ENVIRONMENTAL CHANGE; GEOLOGICAL RECORD; HYPSITHERMAL; INTERGLACIAL; MARINE ENVIRONMENT; MARINE SEDIMENT; NUMERICAL MODEL; OXYGEN ISOTOPE; PALEOCLIMATE; PALYNOLOGY; SEA LEVEL CHANGE; SULFUR; TEMPERATURE EFFECT;

ANTARCTICA; HONSHU; JAPAN; KINKI; OSAKA BAY;

EID: 77954817184     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2010.04.005     Document Type: Article

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