Holocene East Asian monsoon variation inferred from species assemblage and shell chemistry of the ostracodes from Hulun Lake, Inner Mongolia

Quaternary Research

Volumn 75, Issue 3, 2011, Pages 512-522

  Zhai, Dayou ^a   Xiao, Jule ^a   Zhou, Lang ^a   Wen, Ruilin ^a   Chang, Zhigang ^a   Wang, Xu ^a   Jin, Xindi ^a   Pang, Qiqing ^b   Itoh, Shigeru ^c  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b HEBEI GEO UNIVERSITY   (China)

^c Paleo Labo Co Ltd   (Japan)

Author keywords

East Asian monsoon; Holocene; Hulun Lake; Inner Mongolia; Ostracodes; Stable isotope; Trace element

Indexed keywords

EAST ASIAN MONSOON; HOLOCENE; HULUN LAKE; INNER MONGOLIA; OSTRACODES; STABLE ISOTOPE;

ANOXIC SEDIMENTS; ATMOSPHERIC THERMODYNAMICS; CHEMICAL ANALYSIS; INDICATORS (CHEMICAL); ISOTOPES; SALINITY MEASUREMENT; TRACE ELEMENTS;

LAKES;

HOLOCENE; HYDROLOGICAL CHANGE; MONSOON; OSTRACOD; PALEOCLIMATE; SEDIMENT CORE; STABLE ISOTOPE; TRACE ELEMENT;

CHINA; HULUN LAKE; NEI MONGGOL;

DARWINULA STEVENSONI; ILYOCYPRIS; OSTRACODA;

EID: 79955463017     PISSN: 00335894     EISSN: 10960287     Source Type: Journal    
DOI: 10.1016/j.yqres.2011.02.008     Document Type: Article

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