Oxygen isotope composition of diatoms as Late Holocene climate proxy at Two-Yurts Lake, Central Kamchatka, Russia

Global and Planetary Change

Volumn 134, Issue , 2015, Pages 118-128

  Meyer, Hanno ^a   Chapligin, Bernhard ^a   Hoff, Ulrike ^a,b   Nazarova, Larisa ^a,c   Diekmann, Bernhard ^a  

^a ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^b UNIVERSITY OF TROMSØ   (Norway)

^c KAZAN FEDERAL UNIVERSITY   (Russian Federation)

Author keywords

Aleutian Low; Biogenic silica; Diatom oxygen isotopes; Holocene; Palaeoclimate; Palaeolimnology

Indexed keywords

ALGAE; CLIMATE CHANGE; LAKES; OXYGEN; PHYTOPLANKTON; SEDIMENTS; SILICA;

ALEUTIAN LOW; BIOGENIC SILICA; HOLOCENES; OXYGEN ISOTOPES; PALAEOCLIMATE; PALAEOLIMNOLOGY;

ISOTOPES;

ATMOSPHERIC PRESSURE; CLIMATE VARIATION; DIATOM; HOLOCENE; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; LACUSTRINE DEPOSIT; LAKE WATER; OXYGEN ISOTOPE; PALEOCLIMATE; PALEOLIMNOLOGY; PROXY CLIMATE RECORD; SILICA;

ALASKA; ALEUTIAN ISLANDS; KAMCHATKA; PACIFIC OCEAN; RUSSIAN FEDERATION; SEA OF OKHOTSK; SIBERIA; UNITED STATES;

BACILLARIOPHYTA; CHIRONOMIDAE;

EID: 84946549148     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gloplacha.2014.04.008     Document Type: Article

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