Extinction of deep-sea foraminifera as a result of Pliocene-Pleistocene deep-sea circulation changes in the South China Sea (ODP Sites 1143 and 1146)

Quaternary Science Reviews

Volumn 26, Issue 5-6, 2007, Pages 808-827

  Kawagata, Shungo ^a   Hayward, Bruce W ^a   Kuhnt, Wolfgang ^b  

^a Geomarine Research   (New Zealand)

^b UNIVERSITY OF KIEL   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATOLOGY; GLACIAL GEOLOGY; OCEAN HABITATS; SEAWATER;

FORAMINIFERA; MID-PLEISTOCENE CLIMATE TRANSITION (MPT); PLEISTOCENE DECLINES; WATER MASSES;

MARINE BIOLOGY;

ABUNDANCE; BENTHIC FORAMINIFERA; CLIMATE CHANGE; DEEP SEA; DEEP WATER; EXTINCTION; OCEANIC CIRCULATION; PALEOCLIMATE; PLIOCENE-PLEISTOCENE BOUNDARY; SPECIES RICHNESS; WATER MASS;

PACIFIC OCEAN; SOUTH CHINA SEA;

FORAMINIFERA;

EID: 33947513882     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2006.10.011     Document Type: Article

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