Paired δ18O signals of Neogloboquadrina pachyderma (s) and Turborotalita quinqueloba show thermal stratification structure in Nordic Seas

Marine Micropaleontology

Volumn 48, Issue 1-2, 2003, Pages 107-125

  Simstich, Johannes ^a,b   Sarnthein, Michael ^b   Erlenkeuser, Helmut ^b  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b UNIVERSITY OF KIEL   (Germany)

Author keywords

Habitat; Norwegian Sea; Planktonic foraminifera; Stable isotopes

Indexed keywords

OXYGEN ISOTOPE; PALEOCEANOGRAPHY; PALEOCLIMATE; PLANKTONIC FORAMINIFERA; STABLE ISOTOPE; STRATIFICATION; THERMAL STRUCTURE; THERMOHALINE CIRCULATION;

NORWEGIAN SEA;

FORAMINIFERA; NEOGLOBOQUADRINA PACHYDERMA; TURBOROTALIA QUINQUELOBA; TURBOROTALITA QUINQUELOBA;

EID: 0037407783     PISSN: 03778398     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0377-8398(02)00165-2     Document Type: Article

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