Paleosalinity in a brackish lake during the Holocene based on stable oxygen and carbon isotopes of shell carbonate in Nakaumi Lagoon, southwest Japan

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 224, Issue 4, 2005, Pages 352-366

  Sampei, Yoshikazu ^a   Matsumoto, Eiji ^b   Dettman, David L ^a,c   Tokuoka, Takao ^a,d   Abe, Osamu ^b  

^a SHIMANE UNIVERSITY   (Japan)

^b NAGOYA UNIVERSITY   (Japan)

^c University of Arizona   (United States)

^d Tokuoka Laboratory for Study of Brackish Water Environments   (Japan)

Author keywords

13C; 18O; Estuary lake lagoon system; Holocene; Paleosalinity; Shell carbonate

Indexed keywords

BRACKISH WATER; ESTUARINE ENVIRONMENT; HOLOCENE; ISOTOPIC COMPOSITION; LAGOON; MOLLUSC; PALEOSALINITY;

ASIA; EASTERN HEMISPHERE; EURASIA; FAR EAST; JAPAN; WORLD;

MOLLUSCA;

EID: 23244440935     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2005.04.020     Document Type: Article

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