Trace element variability in crust-bearing and non crust-bearing Neogloboquadrina incompta, P-D intergrade and Globoconella inflata from the Southwest Pacific Ocean: Potential paleoceanographic implications

Marine Micropaleontology

Volumn 100, Issue , 2013, Pages 21-33

  Bolton, Annette ^a,b   Marr, Julene P ^a  

^a VICTORIA UNIVERSITY OF WELLINGTON   (New Zealand)

^b NANYANG TECHNOLOGICAL UNIVERSITY   (Singapore)

Author keywords

Calcite crust; Globoconella inflata; Laser ablation inductively coupled plasma mass spectrometry; Neogloboquadrina incompta; P D intergrade; Southwest Pacific Ocean; Trace elements

Indexed keywords

CALCITE; CRUST; INDUCTIVELY COUPLED PLASMA METHOD; MICROPALEONTOLOGY; PALEOCEANOGRAPHY; PALEOTEMPERATURE; PLANKTONIC FORAMINIFERA; TRACE ELEMENT;

PACIFIC OCEAN; PACIFIC OCEAN (SOUTHWEST);

FORAMINIFERA; GLOBOCONELLA; NEOGLOBOQUADRINA DUTERTREI; NEOGLOBOQUADRINA INCOMPTA; NEOGLOBOQUADRINA PACHYDERMA;

EID: 84879322020     PISSN: 03778398     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.marmicro.2013.03.008     Document Type: Article

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