Late Quaternary ostracod and planktonic foraminiferal dissolution signals from the eastern Tasman Sea palaeoenvironmental implications

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 131, Issue 3-4, 1997, Pages 303-314

  Swanson, K ^a   Van Der Lingen, G ^b  

^a UNIVERSITY OF CANTERBURY   (New Zealand)

^b Geosci Res Investigations New Z   (New Zealand)

Author keywords

Carbonates; Challenger Plateau; Foraminifera; Foraminiferal fragmentation; Hydrogeology; Late Quaternary; Ostracod corrosion index; Ostracoda; Productivity

Indexed keywords

BIOLOGICAL PRODUCTION; CORROSION INDEX; FLUCTUATIONS; FORAMINFERA; FORAMINIFERA; OSTRACOD; PALAEOENVIRONMENT; PALAEOENVIRONMENTS; PLANKTONIC ASSEMBLAGES; PRODUCTIVITY FLUCTUATION; QUATERNARY; QUATERNARY OCEAN;

TASMAN SEA, CHALLENGER PLATEAU;

FORAMINIFERA; KRITHE; OSTRACODA;

EID: 0030779844     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0031-0182(97)00008-4     Document Type: Article

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