Holocene foraminiferal assemblages from Firth of Tay, Antarctic Peninsula: Paleoclimate implications

Marine Micropaleontology

Volumn 73, Issue 3-4, 2009, Pages 135-147

  Majewski, Wojciech ^a   Anderson, John B ^b  

^a INSTITUTE OF PALEOBIOLOGY   (Poland)

^b RICE UNIVERSITY   (United States)

Author keywords

benthic foraminifera; climate change; West Antarctica

Indexed keywords

BENTHIC FORAMINIFERA; CARBONATE; CLIMATE CHANGE; CLIMATE EFFECT; COOLING; CORE ANALYSIS; DOMINANCE; GLACIAL DEPOSIT; GLACIER RETREAT; HOLOCENE; PALEOCLIMATE; REMOBILIZATION; SEDIMENT BUDGET; WATER DEPTH;

EURASIA; EUROPE; SCOTLAND; TAY ESTUARY; UNITED KINGDOM; WESTERN EUROPE;

CRIBROELPHIDIUM; FORAMINIFERA; FURSENKOINA FUSIFORMIS; GLOBOCASSIDULINA; GLOBOCASSIDULINA BIORA; MILIAMMINA ARENACEA; PORTATROCHAMMINA ANTARCTICA;

EID: 71949112662     PISSN: 03778398     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marmicro.2009.08.003     Document Type: Article

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